pubs.usgs.gov€¦ · XLS file · Web view · 2015-03-23Deposit is 4 km SE of the Duobaoshan porphyry Cu deposit and is in the same district as the Duobaoshan deposit. Three major

Region GMRAP_ID Tract_ID Coded_ID Tract_nameCentral Asia 8600 Caledonian North 142pCu8504 Mongol-SayanCentral Asia 8120 Caledonian North 142pCu8504 Mongol-SayanCentral Asia 8601 Variscan North 142pCu8507 Mongol-AltaiCentral Asia 443 Caledonian North 142pCu8504 Mongol-SayanCentral Asia 8121 Variscan Central 142pCu8506 Oyu TolgoiCentral Asia 1029 Caledonian North 142pCu8504 Mongol-SayanCentral Asia 8122 Variscan Central 142pCu8506 Oyu TolgoiCentral Asia 1030 Variscan-Indosinian North 142pCu8508a ErdenetCentral Asia 8602 Variscan Central 142pCu8506 Oyu TolgoiCentral Asia 8603 Caledonian North 142pCu8504 Mongol-SayanCentral Asia 8123 Variscan-Indosinian North 142pCu8508a ErdenetCentral Asia 8124 Variscan North 142pCu8507 Mongol-AltaiCentral Asia 8000 Jinsajiang 142pCu8702 JinsajiangCentral Asia 8605 Variscan Central 142pCu8506 Oyu TolgoiCentral Asia 8125 Variscan-Indosinian North 142pCu8508a ErdenetCentral Asia 8126 Variscan North 142pCu8507 Mongol-AltaiCentral Asia 8127 Variscan Central 142pCu8506 Oyu TolgoiCentral Asia 8128 Variscan-Indosinian North 142pCu8508a ErdenetCentral Asia 8001 Caledonian-Variscan South 142pCu8501 SolonkerCentral Asia 8002 Caledonian-Variscan South 142pCu8501 SolonkerCentral Asia 8004 Variscan West 142pCu8505 Kazakh-TarimCentral Asia 1001 Variscan West 142pCu8505 Kazakh-TarimCentral Asia 8129 Caledonian North 142pCu8504 Mongol-SayanCentral Asia 8131 Variscan-Indosinian North 142pCu8508a ErdenetCentral Asia 8608 Variscan Central 142pCu8506 Oyu TolgoiCentral Asia 8133 Variscan-Indosinian North 142pCu8508a ErdenetCentral Asia 8609 Variscan Central 142pCu8506 Oyu TolgoiCentral Asia 8610 Variscan Central 142pCu8506 Oyu TolgoiCentral Asia 8132 Variscan-Indosinian North 142pCu8508a ErdenetCentral Asia 454 Variscan North 142pCu8507 Mongol-AltaiCentral Asia 8005 Variscan West 142pCu8505 Kazakh-TarimCentral Asia 8134 Variscan North 142pCu8507 Mongol-AltaiCentral Asia 1094 Caledonian North 142pCu8504 Mongol-SayanCentral Asia 420 Caledonian West 142pCu8502 Kazakh-TianshanCentral Asia 8135 Variscan Central 142pCu8506 Oyu TolgoiCentral Asia 8136 Variscan North 142pCu8507 Mongol-AltaiCentral Asia 8137 Variscan Central 142pCu8506 Oyu TolgoiCentral Asia 8138 Variscan-Indosinian North 142pCu8508a ErdenetCentral Asia 8260 Variscan North 142pCu8507 Mongol-AltaiCentral Asia 8616 Variscan North 142pCu8507 Mongol-AltaiCentral Asia 8256 Caledonian North 142pCu8504 Mongol-SayanCentral Asia 8139 Variscan Central 142pCu8506 Oyu TolgoiCentral Asia 1043 Variscan-Indosinian North 142pCu8508a ErdenetCentral Asia 1044 Caledonian North 142pCu8504 Mongol-Sayan

Central Asia 8140 Variscan Central 142pCu8506 Oyu TolgoiCentral Asia 8006 Variscan Central 142pCu8506 Oyu TolgoiCentral Asia 8620 Caledonian North 142pCu8504 Mongol-SayanCentral Asia 1045 Caledonian North 142pCu8504 Mongol-SayanCentral Asia 1002 Jinsajiang 142pCu8702 JinsajiangCentral Asia 1003 Caledonian-Variscan South 142pCu8501 SolonkerCentral Asia 588 Variscan West 142pCu8505 Kazakh-TarimCentral Asia 8007 Caledonian-Variscan South 142pCu8501 SolonkerCentral Asia 8141 Variscan North 142pCu8507 Mongol-AltaiCentral Asia 8008 Jinsajiang 142pCu8702 JinsajiangCentral Asia 8010 Variscan West 142pCu8505 Kazakh-TarimCentral Asia 8011 Caledonian-Variscan South 142pCu8501 SolonkerCentral Asia 8142 Variscan-Indosinian North 142pCu8508a ErdenetCentral Asia 8012 Variscan West 142pCu8505 Kazakh-TarimCentral Asia 8143 Variscan-Indosinian North 142pCu8508a ErdenetCentral Asia 8145 Variscan-Indosinian North 142pCu8508a ErdenetCentral Asia 8144 Variscan-Indosinian North 142pCu8508a ErdenetCentral Asia 1053 Variscan-Indosinian North 142pCu8508a ErdenetCentral Asia 8146 Variscan-Indosinian North 142pCu8508a ErdenetCentral Asia 8147 Variscan-Indosinian North 142pCu8508a ErdenetCentral Asia 8013 Variscan West 142pCu8505 Kazakh-TarimCentral Asia 8148 Variscan Central 142pCu8506 Oyu TolgoiCentral Asia 8149 Variscan North 142pCu8507 Mongol-AltaiCentral Asia 473 Caledonian Central 142pCu8503 Gobi-AmurCentral Asia 8014 Tethyan Gangdese 142pCu8706 Tethyan GangdeseCentral Asia 452 Variscan-Indosinian North 142pCu8508a ErdenetCentral Asia 8152 Variscan North 142pCu8507 Mongol-AltaiCentral Asia 1059 Variscan North 142pCu8507 Mongol-AltaiCentral Asia 8015 Jinsajiang 142pCu8702 JinsajiangCentral Asia 8016 Tethyan Gangdese 142pCu8706 Tethyan GangdeseCentral Asia 8153 Variscan Central 142pCu8506 Oyu TolgoiCentral Asia 1060 Variscan-Indosinian North 142pCu8508a ErdenetCentral Asia 1005 Caledonian-Variscan South 142pCu8501 SolonkerCentral Asia 1062 Variscan North 142pCu8507 Mongol-AltaiCentral Asia 8156 Variscan Central 142pCu8506 Oyu TolgoiCentral Asia 8017 Caledonian Central 142pCu8503 Gobi-AmurCentral Asia 8018 Jinsajiang 142pCu8702 JinsajiangCentral Asia 8019 Qinling-Dabie 142pCu8701 Qinling-DabieCentral Asia 8629 Variscan Central 142pCu8506 Oyu TolgoiCentral Asia 8157 Variscan North 142pCu8507 Mongol-AltaiCentral Asia 8158 Variscan-Indosinian North 142pCu8508a ErdenetCentral Asia 8159 Variscan-Indosinian North 142pCu8508a ErdenetCentral Asia 8020 Variscan West 142pCu8505 Kazakh-TarimCentral Asia 8160 Variscan-Indosinian North 142pCu8508a ErdenetCentral Asia 1067 Variscan-Indosinian North 142pCu8508a Erdenet

Central Asia 8021 Qinling-Dabie 142pCu8701 Qinling-DabieCentral Asia 8022 Qinling-Dabie 142pCu8701 Qinling-DabieCentral Asia 598 Variscan West 142pCu8505 Kazakh-TarimCentral Asia 8632 Caledonian North 142pCu8504 Mongol-SayanCentral Asia 8023 Variscan West 142pCu8505 Kazakh-TarimCentral Asia 8024 Variscan West 142pCu8505 Kazakh-TarimCentral Asia 8161 Caledonian North 142pCu8504 Mongol-SayanCentral Asia 8162 Variscan North 142pCu8507 Mongol-AltaiCentral Asia 8163 Variscan Central 142pCu8506 Oyu TolgoiCentral Asia 8164 Variscan Central 142pCu8506 Oyu TolgoiCentral Asia 1068 Variscan-Indosinian North 142pCu8508a ErdenetCentral Asia 8165 Variscan-Indosinian North 142pCu8508a ErdenetCentral Asia 8166 Variscan Central 142pCu8506 Oyu TolgoiCentral Asia 453 Variscan Central 142pCu8506 Oyu TolgoiCentral Asia 8167 Variscan Central 142pCu8506 Oyu TolgoiCentral Asia 8638 Variscan Central 142pCu8506 Oyu TolgoiCentral Asia 8168 Variscan-Indosinian North 142pCu8508a ErdenetCentral Asia 8172 Variscan North 142pCu8507 Mongol-AltaiCentral Asia 8173 Variscan North 142pCu8507 Mongol-AltaiCentral Asia 1074 Variscan North 142pCu8507 Mongol-AltaiCentral Asia 688 Variscan Central 142pCu8506 Oyu TolgoiCentral Asia 8174 Variscan-Indosinian North 142pCu8508a ErdenetCentral Asia 1076 Variscan-Indosinian North 142pCu8508a ErdenetCentral Asia 8175 Caledonian North 142pCu8504 Mongol-SayanCentral Asia 8177 Variscan Central 142pCu8506 Oyu TolgoiCentral Asia 8179 Variscan Central 142pCu8506 Oyu TolgoiCentral Asia 8180 Variscan North 142pCu8507 Mongol-AltaiCentral Asia 8181 Variscan North 142pCu8507 Mongol-AltaiCentral Asia 8182 Variscan-Indosinian North 142pCu8508a ErdenetCentral Asia 1081 Variscan North 142pCu8507 Mongol-AltaiCentral Asia 442 Caledonian North 142pCu8504 Mongol-SayanCentral Asia 427 Variscan West 142pCu8505 Kazakh-TarimCentral Asia 8641 Variscan North 142pCu8507 Mongol-AltaiCentral Asia 8255 Caledonian North 142pCu8504 Mongol-SayanCentral Asia 444 Variscan North 142pCu8507 Mongol-AltaiCentral Asia 433 Variscan West 142pCu8505 Kazakh-TarimCentral Asia 416 Caledonian West 142pCu8502 Kazakh-TianshanCentral Asia 8025 Variscan West 142pCu8505 Kazakh-TarimCentral Asia 8184 Variscan-Indosinian North 142pCu8508a ErdenetCentral Asia 1012 Variscan West 142pCu8505 Kazakh-TarimCentral Asia 8026 Jinsajiang 142pCu8702 JinsajiangCentral Asia 8027 Qinling-Dabie 142pCu8701 Qinling-DabieCentral Asia 8028 Jinsajiang 142pCu8702 JinsajiangCentral Asia 8029 Variscan Central 142pCu8506 Oyu TolgoiCentral Asia 585 Variscan West 142pCu8505 Kazakh-Tarim

Central Asia 8030 Qinling-Dabie 142pCu8701 Qinling-DabieCentral Asia 8185 Variscan Central 142pCu8506 Oyu TolgoiCentral Asia 8651 Variscan Central 142pCu8506 Oyu TolgoiCentral Asia 8186 Variscan Central 142pCu8506 Oyu TolgoiCentral Asia 8032 Variscan Central 142pCu8506 Oyu TolgoiCentral Asia 8652 Variscan North 142pCu8507 Mongol-AltaiCentral Asia 8033 Caledonian Central 142pCu8503 Gobi-AmurCentral Asia 8655 Variscan-Indosinian North 142pCu8508a ErdenetCentral Asia 8187 Variscan-Indosinian North 142pCu8508a ErdenetCentral Asia 1085 Caledonian North 142pCu8504 Mongol-SayanCentral Asia 8656 Variscan North 142pCu8507 Mongol-AltaiCentral Asia 8188 Variscan Central 142pCu8506 Oyu TolgoiCentral Asia 1086 Caledonian North 142pCu8504 Mongol-SayanCentral Asia 8189 Variscan-Indosinian North 142pCu8508a ErdenetCentral Asia 606 Variscan-Indosinian North 142pCu8508a ErdenetCentral Asia 610 Variscan Central 142pCu8506 Oyu TolgoiCentral Asia 8191 Variscan Central 142pCu8506 Oyu TolgoiCentral Asia 8192 Variscan Central 142pCu8506 Oyu TolgoiCentral Asia 8193 Variscan North 142pCu8507 Mongol-AltaiCentral Asia 429 Caledonian West 142pCu8502 Kazakh-TianshanCentral Asia 8035 Caledonian-Variscan South 142pCu8501 SolonkerCentral Asia 8194 Variscan North 142pCu8507 Mongol-AltaiCentral Asia 8195 Variscan North 142pCu8507 Mongol-AltaiCentral Asia 1099 Variscan North 142pCu8507 Mongol-AltaiCentral Asia 8196 Variscan North 142pCu8507 Mongol-AltaiCentral Asia 8197 Variscan North 142pCu8507 Mongol-AltaiCentral Asia 8198 Variscan North 142pCu8507 Mongol-AltaiCentral Asia 8200 Variscan-Indosinian North 142pCu8508a ErdenetCentral Asia 8199 Variscan-Indosinian North 142pCu8508a ErdenetCentral Asia 8201 Variscan-Indosinian North 142pCu8508a ErdenetCentral Asia 8202 Variscan-Indosinian North 142pCu8508a ErdenetCentral Asia 8036 Jinsajiang 142pCu8702 JinsajiangCentral Asia 8203 Variscan-Indosinian North 142pCu8508a ErdenetCentral Asia 8246 Variscan Central 142pCu8506 Oyu TolgoiCentral Asia 8204 Variscan Central 142pCu8506 Oyu TolgoiCentral Asia 8205 Variscan Central 142pCu8506 Oyu TolgoiCentral Asia 8206 Variscan North 142pCu8507 Mongol-AltaiCentral Asia 8661 Variscan North 142pCu8507 Mongol-AltaiCentral Asia 8208 Variscan-Indosinian North 142pCu8508a ErdenetCentral Asia 611 Variscan Central 142pCu8506 Oyu TolgoiCentral Asia 8209 Caledonian North 142pCu8504 Mongol-SayanCentral Asia 8210 Variscan-Indosinian North 142pCu8508a ErdenetCentral Asia 8211 Variscan-Indosinian North 142pCu8508a ErdenetCentral Asia 590 Jinsajiang 142pCu8702 JinsajiangCentral Asia 8037 Jinsajiang 142pCu8702 Jinsajiang

Central Asia 8038 Variscan West 142pCu8505 Kazakh-TarimCentral Asia 1113 Variscan-Indosinian North 142pCu8508a ErdenetCentral Asia 8039 Variscan West 142pCu8505 Kazakh-TarimCentral Asia 8040 Tethyan Gangdese 142pCu8706 Tethyan GangdeseCentral Asia 8664 Variscan Central 142pCu8506 Oyu TolgoiCentral Asia 1114 Variscan-Indosinian North 142pCu8508a ErdenetCentral Asia 462 Qinling-Dabie 142pCu8701 Qinling-DabieCentral Asia 589 Variscan West 142pCu8505 Kazakh-TarimCentral Asia 8212 Variscan North 142pCu8507 Mongol-AltaiCentral Asia 451 Variscan North 142pCu8507 Mongol-AltaiCentral Asia 8666 Caledonian North 142pCu8504 Mongol-SayanCentral Asia 8041 Variscan West 142pCu8505 Kazakh-TarimCentral Asia 8667 Variscan Central 142pCu8506 Oyu TolgoiCentral Asia 612 Variscan-Indosinian North 142pCu8508a ErdenetCentral Asia 8669 Variscan-Indosinian North 142pCu8508a ErdenetCentral Asia 8213 Variscan-Indosinian North 142pCu8508a ErdenetCentral Asia 1118 Caledonian North 142pCu8504 Mongol-SayanCentral Asia 8214 Variscan-Indosinian North 142pCu8508a ErdenetCentral Asia 8215 Variscan-Indosinian North 142pCu8508a ErdenetCentral Asia 8042 Tethyan Gangdese 142pCu8706 Tethyan GangdeseCentral Asia 8670 Variscan North 142pCu8507 Mongol-AltaiCentral Asia 8068 Qinling-Dabie 142pCu8701 Qinling-DabieCentral Asia 8672 Variscan Central 142pCu8506 Oyu TolgoiCentral Asia 613 Variscan Central 142pCu8506 Oyu TolgoiCentral Asia 8216 Variscan Central 142pCu8506 Oyu TolgoiCentral Asia 8043 Jinsajiang 142pCu8702 JinsajiangCentral Asia 8044 Variscan West 142pCu8505 Kazakh-TarimCentral Asia 8372 Caledonian North 142pCu8504 Mongol-SayanCentral Asia 8674 Variscan Central 142pCu8506 Oyu TolgoiCentral Asia 8675 Variscan North 142pCu8507 Mongol-AltaiCentral Asia 8218 Variscan Central 142pCu8506 Oyu TolgoiCentral Asia 8045 Qinling-Dabie 142pCu8701 Qinling-DabieCentral Asia 8219 Variscan-Indosinian North 142pCu8508a ErdenetCentral Asia 8254 Caledonian North 142pCu8504 Mongol-SayanCentral Asia 8682 Variscan North 142pCu8507 Mongol-AltaiCentral Asia 8257 Caledonian North 142pCu8504 Mongol-SayanCentral Asia 8220 Variscan North 142pCu8507 Mongol-AltaiCentral Asia 1124 Variscan-Indosinian North 142pCu8508a ErdenetCentral Asia 8221 Variscan North 142pCu8507 Mongol-AltaiCentral Asia 8253 Variscan Central 142pCu8506 Oyu TolgoiCentral Asia 1126 Caledonian North 142pCu8504 Mongol-SayanCentral Asia 8222 Variscan-Indosinian North 142pCu8508a ErdenetCentral Asia 8046 Caledonian Central 142pCu8503 Gobi-AmurCentral Asia 8685 Variscan Central 142pCu8506 Oyu TolgoiCentral Asia 8224 Variscan-Indosinian North 142pCu8508a Erdenet

Central Asia 8686 Variscan-Indosinian North 142pCu8508a ErdenetCentral Asia 8687 Variscan North 142pCu8507 Mongol-AltaiCentral Asia 456 Variscan Central 142pCu8506 Oyu TolgoiCentral Asia 8226 Variscan North 142pCu8507 Mongol-AltaiCentral Asia 1131 Caledonian North 142pCu8504 Mongol-SayanCentral Asia 8227 Variscan North 142pCu8507 Mongol-AltaiCentral Asia 1132 Variscan-Indosinian North 142pCu8508a ErdenetCentral Asia 8228 Variscan Central 142pCu8506 Oyu TolgoiCentral Asia 8047 Qinling-Dabie 142pCu8701 Qinling-DabieCentral Asia 8229 Variscan North 142pCu8507 Mongol-AltaiCentral Asia 8688 Variscan-Indosinian North 142pCu8508a ErdenetCentral Asia 8048 Variscan West 142pCu8505 Kazakh-TarimCentral Asia 8230 Variscan Central 142pCu8506 Oyu TolgoiCentral Asia 8692 Variscan-Indosinian North 142pCu8508a ErdenetCentral Asia 8693 Variscan Central 142pCu8506 Oyu TolgoiCentral Asia 1134 Variscan North 142pCu8507 Mongol-AltaiCentral Asia 8231 Variscan Central 142pCu8506 Oyu TolgoiCentral Asia 8233 Variscan-Indosinian North 142pCu8508a ErdenetCentral Asia 8234 Variscan Central 142pCu8506 Oyu TolgoiCentral Asia 8378 Variscan North 142pCu8507 Mongol-AltaiCentral Asia 8235 Variscan Central 142pCu8506 Oyu TolgoiCentral Asia 1136 Variscan-Indosinian North 142pCu8508a ErdenetCentral Asia 1137 Variscan North 142pCu8507 Mongol-AltaiCentral Asia 1138 Variscan North 142pCu8507 Mongol-AltaiCentral Asia 8049 Variscan West 142pCu8505 Kazakh-TarimCentral Asia 8050 Variscan West 142pCu8505 Kazakh-TarimCentral Asia 8051 Variscan West 142pCu8505 Kazakh-TarimCentral Asia 8052 Variscan West 142pCu8505 Kazakh-TarimCentral Asia 8053 Variscan West 142pCu8505 Kazakh-TarimCentral Asia 8054 Variscan West 142pCu8505 Kazakh-TarimCentral Asia 8055 Variscan West 142pCu8505 Kazakh-TarimCentral Asia 8056 Variscan West 142pCu8505 Kazakh-TarimCentral Asia 8248 Variscan Central 142pCu8506 Oyu TolgoiCentral Asia 8249 Variscan North 142pCu8507 Mongol-AltaiCentral Asia 8250 Variscan North 142pCu8507 Mongol-AltaiCentral Asia 1139 Caledonian North 142pCu8504 Mongol-SayanCentral Asia 8251 Variscan North 142pCu8507 Mongol-AltaiCentral Asia 8236 Variscan North 142pCu8507 Mongol-AltaiCentral Asia 8237 Variscan-Indosinian North 142pCu8508a ErdenetCentral Asia 8057 Qinling-Dabie 142pCu8701 Qinling-DabieCentral Asia 8069 Variscan Central 142pCu8506 Oyu TolgoiCentral Asia 8058 Variscan Central 142pCu8506 Oyu TolgoiCentral Asia 8031 Variscan Central 142pCu8506 Oyu TolgoiCentral Asia 8059 Variscan Central 142pCu8506 Oyu TolgoiCentral Asia 8060 Caledonian West 142pCu8502 Kazakh-Tianshan

Central Asia 8061 Variscan Central 142pCu8506 Oyu TolgoiCentral Asia 8062 Variscan North 142pCu8507 Mongol-AltaiCentral Asia 8063 Jinsajiang 142pCu8702 JinsajiangCentral Asia 1142 Caledonian North 142pCu8504 Mongol-SayanCentral Asia 8238 Caledonian North 142pCu8504 Mongol-SayanCentral Asia 1144 Caledonian North 142pCu8504 Mongol-SayanCentral Asia 8064 Qinling-Dabie 142pCu8701 Qinling-DabieCentral Asia 8065 Qinling-Dabie 142pCu8701 Qinling-DabieCentral Asia 8066 Variscan North 142pCu8507 Mongol-AltaiCentral Asia 8239 Variscan-Indosinian North 142pCu8508a ErdenetCentral Asia 8240 Variscan North 142pCu8507 Mongol-AltaiCentral Asia 8067 Jinsajiang 142pCu8702 JinsajiangCentral Asia 605 Variscan-Indosinian North 142pCu8508a ErdenetCentral Asia 8703 Variscan Central 142pCu8506 Oyu TolgoiCentral Asia 8241 Caledonian North 142pCu8504 Mongol-SayanCentral Asia 8242 Variscan-Indosinian North 142pCu8508a ErdenetCentral Asia 8243 Variscan Central 142pCu8506 Oyu TolgoiCentral Asia 8244 Variscan-Indosinian North 142pCu8508a ErdenetCentral Asia 1154 Variscan-Indosinian North 142pCu8508a Erdenet

NameAgaskyrAguin davaaAgulskoyeAksugAlag BayanAltan-KhadAmar Shavagtai KhudagAmarhiidAmgalantAndobinskoe IIAr bulagArbulagA'reArgalant UulArshaantArvaikheerAuyouteAzargyn davaaBainaimiaoBaishantangBaogutuBaowenbulakeBaruunBayan golBayan GoyaBayan KharaatBayan OvooBayanbulagBayangolBayan-UulBeidabateBerkhiin OvooBigerBozshakolBronze FoxBudag tolgoiBudagtBugsein golBukhtarmaBulag ShandBumbatBunkhan KhudagBurged hyarBurigiin gorhi

Buyant UulChaganuoerChandman UulChandmaniChangdagouChehugouChihuChina OneChuluut kholvooChunduDa Hong ShanDakouziDalh ovooDananhu NanDartsagtDavaaDavaa OccurrenceDeed muruu golDeed shumuultaiDeed ustDongtujinDuchin KhuralDund BayanDuobaoshanDuolongErdenetErdeniin ShandGaikhamshigtGaochipingGarqiongGashuun hudagGezeg, No. 264 OccurrenceGongpoquanGurvan ovooHatsarHe'ersaiHongshan (Yunnan)HuangnanHutag UulIkh gazarIkh khujirtyn khureeIngetJaertasiJasyn buutsJimbe tolgoi

KaerquekaKalaguorumuKalatageKamenushinskoyeKekesaiKendenggaoerKhadatKhairkhan TugrugKhairkhan UulKhan KhudagKhanjargalant uulKhar uulKharaat UulKharmagtaiKhatsarKhatsaych UulKhavchuuKhetsiin AmKhokh ovooKhondlon ovooKhongorKhoo Ulaan UulKhoshoot golKhoshuu tolgoiKhul MoritKhurelt KhudagKhushutiinKhustKhustaiKhuv Khashaatyn occurrenceKiyalykh-UzenKoktasdzhalKulbichKYKyzyk-ChadrKyzylkainKyzyltuLalisigaoer-3571Lam zah tolgoiLamasuLangduLangshuisimiaopingLannitangLierkudukLinglong

LongweigouMandakhMandal UulMankhan ChuluuMarmot RidgeMaysky uchastokMengxiMogodMogoin golMogoinshandMogoitMogoit KhudagMorinchuluutNaranNaran BulagNariin KhudagNo. XXXIV-32No. XXXVI-2 NarangiinNogoon TolgoiNurkazganOblagaOccurrence No. 10Occurrence No. 11Occurrence No. 6Occurrence No. 7OkhashiOmnodOndor (South ore-junction)Ondor ulaanOrhinOrmiin Tsagaan nuurOsailaOvgon sant uulOvoot HyarOvotiin KharOyu TolgoiOyutOyut OvooOyut TolgoiOyut UlaanOyuut OvooOyuut UulOyuutkhonkhorPulangQiansui

QiuxingQuartziticQunjiRi'aRing DykeSairyn khondiiSaishitangSanchakouSant uulSaran UulSatyr HudagSawuerShadow MountainShandSharchuluut UulSharhadSharhad group (Ereen iher)SharkhadSharonShesuoShiveen GolShuangyangdabanaShurtiin KhundiiShuteenShuteen har TolgoiSongnuoSongshugouSoraSouth GobiSouth ValleySumbur KhudagSuolajierTagiin nuurTakhiltTakhtamygdinsky ore knotTanaTariat GolTeltiin golTemeenchuluutTemuujinTesiin OyutToilbynTongshanTourmaline HillsTsagaan Chulut

Tsagaan GozgorTsagaan OvooTsagaan-SuvargaTsavyn TsagaanTsetsuuhTsogt ChandmaniTsogt tolgoiTsohiotTuoketuoTurmalineTurquoiseTuwu-Yandong-YanxiUkhaa Khudag IIUlaan DelUlaan OvooUlaan shandUlaan TolgoiUlaan TolgoiUlan KhudUlandrykUlgei HiydUndrahUnegtei ovoo-1Unegtei ovoo-2unnamed prospectunnamed prospectunnamed prospectunnamed prospectunnamed prospectunnamed prospectunnamed prospectunnamed prospectunnamed prospectunnamed prospectunnamed prospectunnamed prospectunnamed prospectUrtyn golUsanseerWulanwuzhuerWulunbulakeWurituWuzhuergashunXiaobaliangXiemistai

XilekudukeXilketehalasuXuejipingYardag uulYargaitYashiltynYaziguolYingyugouYulekenhalasuZairanZesiinZhujidingZos UulZurumtaiZuslan tolgoiZuukhin golZuun ModZuun oortsogZuuvchiin gol

Name_otherAgaskyrskoe, Agaskyrskoye

Agul'skoeAk-Sug, AskugskoeAlagbayanAltan Khad

Ovoot

Arvaikheer (ulaan tolgoi), Arvaikheer occurrence

Azargyndavaa occurrence

BaowendulakeBaruun occurrenceBayangol occurrence

Bayankharaat, Bayankharaat occurrence

Tuimertei

Bajan-Ula, Bayan-Uul 2DabateBerhiin ovooNergui, BergerBoshchekul, Boshchekul' BoschekulKhongoot, Khunguit, Hunguut, Bronze Fox District

Bukhtarminskoe

Gun Sain Khudag I, Ulaan Tolgoi BulagBurged khyr

DongtujingDuchin Khural I, Döchiin HuralDund Bayan occurrenceDubaoshanDobuzhaErdenetiin - Ovoo, Erenetuin-Obo

Gaikhamshig

Gaerqiong

Gezeg, No. 264

Ingetyn Gol

MeilingKamenushinskoe, Kopna Mountain

Kendenggao'er

Khairkhan togrog uul

Kharaat Uul occurrence

Khuntlingiin Ovoo (from Nokleberg and others, 1999)TsakhirGua (Khoo) ulaan uul, No. 272 Occurrence, Khoo Ulaan

KMKhurelt Khudag occurrenceKhushuut

Khustai occurrence

Kijalykh-Uzen', Keyalykh-uzen, Keyalykh-Uzen'Koktasjal, KoktaszhalKulbichskoe, Kul'bichskoeKhavchig YargaitKyzyk-Chadrskoye, Kyzyk-Chadrskoe, Kyzyk-Chadrsk

Qyzyltau

Yunyingshan

Naran bulag, No. 285 Occurrence, NaranbulagNain Hudag, Nariin hudag

Samarskoe, Samarsk

Erdenetolgoi Occurrence from Nokleberg and others (1999), located 48.916667, 113.05.

Omnot occurrence, Nokleberg and others (1999)Under/Shand

Orkhin

Unnamed - Nokleberg and others (1999)Unnamed - MRAM #608Oyuu Tolgoi, Turquoise HillOyuut, Oyuut No 27

Oyut Tolgoi 2, NOT Oyu TolgoiOyuut Ulaar Ovoo, Tuviin, Zuun-KhoitOvoot Ovoo, Oyut Ovoo, No. 474

Oyut honhor, No. 465

Nilekequnji

SanchaluNo. 17 occurrence

Tsakhir khudag, Satir khudag occurrence

Suudert UulUnder/Shandwithin Mogoin Gol license

Sheveen gol

Sora porphyry, Sorsk, Sarbayskoe, Sorskoe, Sorskoye

Tagiinnuur occurrence

No. 151Temeenchuluut occurrenceVirgin

Chuluut; Chuluut part, No. 301; Tsagaanchuluut

White CairnTsagan-SuburgaHuren Tolgoi, Tsavyn Tsagaan HillsTsetsukhiin gol occurrence ? from Nokleberg and others (1999)

Occurrence No. 15

GROUPEDUkhaa Khudag

Airport North Discovery, Ulaan Khud

Olgii khiid

Unknown exploration, from Tang and others (2010) - north group - NEUnknown exploration, from Tang and others (2010) - north group -NUnknown exploration, from Tang and others (2010) - north group - SEUnknown exploration, from Tang and others (2010) - north group - centralUnknown exploration, from Tang and others (2010) - north group - SWUnknown exploration, from Tang and others (2010) - north group - WUnknown exploration, from Tang and others (2010) - north group - NWUnknown exploration, from Tang and others (2010) - southernmostUnnamed - MRAM #21Unnamed - MRAM #234Unnamed - MRAM #370Unnamed - MRAM #413Unnamed - Nokleberg (1999)

Lurgan, Elegen, Whu Shu Er Ga Shun

S24

KalaxiangerXue Je PingYrdag(?), located at 48.85, 104.65No. 270

Duck Creek

Yuleken

Zesiin occurrence

Zost Tolgoi

Zuslan tolgoi-Sharhad group No. 308Zoohiin gol, no. 289, Zookhyngol, Zuilin gol

Includes

Hudele, WDH01, WDH02, WKGSY, WDH05

Nergui, Beger 1, Beger 2, Beger 4, Beger 5

Sophie North, West Kasulu, Buchanan Heights, Dunlop Fox, Leca Pass, and Southeast Target

Gun Sain Khudag I, Ulaan Tolgoi Bulag

Duchin Khural and Duchin Khural I

Duobuza, BulongErdenet Central, Erdenet Southeast (Oyut), Tourmaline, Ikh Tal

Danbolongwa and Duoba-Jijiemu exploration permit areas

Tsagaan Ovoo

Gold Hill (Altan Tolgoi), White Vein (Tsagan Sudal), Copper Hill (Zesen Uul), Wolf (Chun)

Cughur, Aranjin, Gaans, Gaans North, Zam Duguukh

Lalisigaoer, 3571

Unnamed - Nokleberg (1999), [CAOB 1]

South

Falcon (Hartsaga), Central OV, Eagle (Burgit)

Heruga, Heruga North, South Oyu, Southwest Oyu, Central Oyu, Hugo Dummett (including north extension)

Stariy, Zuun Umnut, Khuuchin

Sanchakou, Sanchakou East

Hanzheganeng, Taketakuolasi, Xiyakesitao

Ondor

Tourmaline, Kincora Extension, Southwest target

Baruun Kheseg, Kheseg 2, Kheseg 4

Tuwu, Yandong, YanxiUkhaa Khudag and Ukhaa Khudag II

Kheseg uul

Zuslan tolgoi, Zyslan tolgoi, Shar khad

Khuvyn Khar

SiteStatus Code_cntry Country State_Prov Latitudedeposit RU Russia Khakass, Republic 54.5833prospect MN Mongolia Bulgan, Province 48.6333prospect, significant RU Russia Irkutsk, Region 54.4500deposit RU Russia Tuva, Republic 53.4360prospect, significant MN Mongolia Ömnögovi, Province 43.4000prospect, significant MN Mongolia Govi-Altay, Province 45.6333prospect MN Mongolia Dornogovi, Province 44.4633prospect MN Mongolia Selenge, Province 49.5083prospect MN Mongolia Ömnögovi, Province 43.6680prospect, significant RU Russia Gorno-Altay, Republic 52.3500prospect MN Mongolia Bulgan, Province 48.7500prospect MN Mongolia Dornod, Province 49.0000prospect CN China Yunnan, Province 27.8156prospect MN Mongolia Ömnögovi, Province 43.7670prospect MN Mongolia Selenge, Province 49.8333prospect MN Mongolia Övörhangay, Province 46.2667prospect, significant MN Mongolia Sühbaatar, Province 45.9488prospect MN Mongolia Bulgan, Province 48.8500prospect, significant CN China Nei Mongol, Autonomous Region 42.2269prospect, significant CN China Gansu, Province 40.6331deposit CN China Xinjiang Uygur, Autonomous Region 45.5011prospect CN China Xinjiang Uygur, Autonomous Region 41.3800prospect MN Mongolia Hentiy, Province 46.4000prospect MN Mongolia Bulgan, Province 49.4361prospect, significant MN Mongolia Ömnögovi, Province 43.5873prospect MN Mongolia Selenge, Province 49.8003prospect MN Mongolia Ömnögovi, Province 43.0620prospect MN Mongolia Bayanhongor, Province 44.1600prospect MN Mongolia Arhangay, Province 48.7708prospect, significant MN Mongolia Töv, Province 46.6833prospect, significant CN China Xinjiang Uygur, Autonomous Region 44.7436prospect MN Mongolia Sühbaatar, Province 47.1500prospect, significant MN Mongolia Govi-Altay, Province 45.6000deposit KZ Kazakhstan Pavlodar, Region 51.8462prospect, significant MN Mongolia Dornogovi, Province 44.0742prospect MN Mongolia Dundgovi, Province 45.9167prospect MN Mongolia Ömnögovi, Province 43.6167prospect MN Mongolia Hövsgöl, Province 49.1833prospect, significant KZ Kazakhstan East Kazakhstan, Region 49.5493prospect, significant MN Mongolia Dundgovi, Province 45.5296prospect MN Mongolia Hovd, Province 47.2100prospect MN Mongolia Dornogovi, Province 44.1826prospect MN Mongolia Bulgan, Province 48.7000prospect MN Mongolia Arhangay, Province 48.6208

prospect MN Mongolia Dornogovi, Province 44.4500prospect CN China Nei Mongol, Autonomous Region 42.6332prospect, significant MN Mongolia Dornogovi, Province 45.8202prospect MN Mongolia Govi-Altay, Province 45.3333prospect CN China Sichuan, Province 32.0800deposit CN China Nei Mongol, Autonomous Region 42.4191prospect, significant CN China Xinjiang Uygur, Autonomous Region 42.1640prospect CN China Nei Mongol, Autonomous Region 41.3500prospect MN Mongolia Sühbaatar, Province 47.3336prospect, significant CN China Yunnan, Province 27.9551prospect, significant CN China Xinjiang Uygur, Autonomous Region 42.0854prospect CN China Gansu, Province 41.6391prospect MN Mongolia Selenge, Province 49.4607prospect, significant CN China Xinjiang Uygur, Autonomous Region 42.7314prospect MN Mongolia Selenge, Province 49.3224prospect MN Mongolia Dzavhan, Province 48.9333prospect MN Mongolia Bulgan, Province 49.2626prospect MN Mongolia Bulgan, Province 48.7828prospect MN Mongolia Dzavhan, Province 48.9333prospect MN Mongolia Selenge, Province 49.4399prospect CN China Xinjiang Uygur, Autonomous Region 44.0044prospect MN Mongolia Ömnögovi, Province 44.0867prospect MN Mongolia Dornogovi, Province 46.1000deposit CN China Heilongjiang, Province 50.2403prospect, significant CN China Xizang, Autonomous Region 32.8328deposit MN Mongolia Orhon, Municipality 49.0212prospect MN Mongolia Sühbaatar, Province 47.3167prospect, significant MN Mongolia Sühbaatar, Province 47.1111prospect CN China Yunnan, Province 28.1385prospect CN China Xizang, Autonomous Region 33.3213prospect MN Mongolia Ömnögovi, Province 43.3333prospect MN Mongolia Bulgan, Province 48.6860prospect, significant CN China Gansu, Province 41.6359prospect MN Mongolia Töv, Province 46.6333prospect MN Mongolia Ömnögovi, Province 44.0000prospect CN China Xinjiang Uygur, Autonomous Region 43.8003prospect, significant CN China Yunnan, Province 28.1284prospect CN China Qinghai, Province 35.5650prospect, significant MN Mongolia Dornogovi, Province 43.1090prospect MN Mongolia Dornod, Province 49.0633prospect MN Mongolia Hövsgöl, Province 48.7167prospect, significant MN Mongolia Bulgan, Province 49.2333prospect CN China Xinjiang Uygur, Autonomous Region 45.3245prospect MN Mongolia Bulgan, Province 48.7833prospect MN Mongolia Hövsgöl, Province 49.3347

prospect CN China Qinghai, Province 36.7596prospect, significant CN China Xinjiang Uygur, Autonomous Region 37.1648prospect, significant CN China Xinjiang Uygur, Autonomous Region 42.6579prospect, significant RU Russia Kemerovo, Region 54.3025prospect CN China Xinjiang Uygur, Autonomous Region 44.7153prospect, significant CN China Xinjiang Uygur, Autonomous Region 44.2052prospect MN Mongolia Töv, Province 48.0500prospect MN Mongolia Dundgovi, Province 45.6000prospect MN Mongolia Dornogovi, Province 44.3053prospect MN Mongolia Ömnögovi, Province 44.0167prospect MN Mongolia Selenge, Province 49.6833prospect MN Mongolia Bulgan, Province 48.7014prospect, significant MN Mongolia Dornogovi, Province 44.1667prospect, significant MN Mongolia Ömnögovi, Province 44.0217prospect MN Mongolia Ömnögovi, Province 44.0000prospect MN Mongolia Ömnögovi, Province 42.8036prospect MN Mongolia Bulgan, Province 49.3333prospect MN Mongolia Töv, Province 48.0000prospect MN Mongolia Dundgovi, Province 45.7789prospect MN Mongolia Dundgovi, Province 46.5833prospect, significant MN Mongolia Ömnögovi, Province 43.1482prospect, significant MN Mongolia Bulgan, Province 48.9042prospect MN Mongolia Bulgan, Province 48.2333prospect MN Mongolia Selenge, Province 48.8334prospect, significant MN Mongolia Bayanhongor, Province 43.9789prospect MN Mongolia Ömnögovi, Province 44.3333prospect MN Mongolia Dornogovi, Province 45.8667prospect MN Mongolia Dornod, Province 49.0167prospect MN Mongolia Arhangay, Province 48.7500prospect MN Mongolia Övörhangay, Province 46.2833deposit RU Russia Khakass, Republic 54.3236deposit KZ Kazakhstan Qaraghandy, Region 50.1622prospect, significant RU Russia Gorno-Altay, Republic 51.7240prospect, significant MN Mongolia Hovd, Province 47.3839prospect, significant RU Russia Tuva, Republic 52.9333deposit KZ Kazakhstan East Kazakhstan, Region 47.5504deposit KZ Kazakhstan Aqmola, Region 51.9500prospect, significant CN China Xinjiang Uygur, Autonomous Region 44.1214prospect MN Mongolia Selenge, Province 49.7000prospect, significant CN China Xinjiang Uygur, Autonomous Region 44.6736prospect, significant CN China Yunnan, Province 28.1952prospect, significant CN China Shaanxi, Province 33.8290prospect, significant CN China Yunnan, Province 28.1144prospect CN China Xinjiang Uygur, Autonomous Region 46.6667prospect CN China Xinjiang Uygur, Autonomous Region 42.1297

prospect CN China Qinghai, Province 39.0958prospect MN Mongolia Dornogovi, Province 44.3833prospect MN Mongolia Selenge, Province 42.7187prospect MN Mongolia Dornogovi, Province 44.3833prospect, significant CN China Nei Mongol, Autonomous Region 43.7300prospect RU Russia Irkutsk, Region 54.7833prospect CN China Xinjiang Uygur, Autonomous Region 44.1955prospect MN Mongolia Bulgan, Province 48.5658prospect, significant MN Mongolia Bulgan, Province 49.2552prospect MN Mongolia Govi-Altay, Province 45.6000prospect MN Mongolia Övörhangay, Province 45.8201prospect MN Mongolia Dornogovi, Province 44.5833prospect, significant MN Mongolia Uvs, Province 49.3667prospect MN Mongolia Selenge, Province 49.2500prospect, significant MN Mongolia Dzavhan, Province 48.5803prospect, significant MN Mongolia Dornogovi, Province 44.2208prospect MN Mongolia Ömnögovi, Province 44.3167prospect MN Mongolia Ömnögovi, Province 44.3333prospect MN Mongolia Dornogovi, Province 45.9500deposit KZ Kazakhstan Qaraghandy, Region 50.0269prospect, significant CN China Nei Mongol, Autonomous Region 41.2226prospect MN Mongolia Dornod, Province 48.9222prospect MN Mongolia Dornod, Province 48.8556prospect MN Mongolia Dornod, Province 48.9833prospect MN Mongolia Dornod, Province 48.9333prospect MN Mongolia Hentiy, Province 47.6500prospect MN Mongolia Bayanhongor, Province 46.4500prospect MN Mongolia Bulgan, Province 48.8306prospect, significant MN Mongolia Dzavhan, Province 48.8833prospect MN Mongolia Selenge, Province 50.0500prospect, significant MN Mongolia Bulgan, Province 48.7905prospect, significant CN China Yunnan, Province 27.9027prospect MN Mongolia Selenge, Province 49.7000prospect MN Mongolia Ömnögovi, Province 44.0376prospect MN Mongolia Ömnögovi, Province 44.0167deposit MN Mongolia Ömnögovi, Province 43.0136prospect, significant MN Mongolia Övörhangay, Province 46.7472prospect, significant MN Mongolia Dundgovi, Province 45.7000prospect, significant MN Mongolia Dzavhan, Province 49.2667prospect, significant MN Mongolia Dornogovi, Province 44.5722prospect, significant MN Mongolia Bulgan, Province 48.4974prospect, significant MN Mongolia Selenge, Province 49.6333prospect MN Mongolia Bulgan, Province 48.1667deposit CN China Yunnan, Province 28.0385prospect, significant CN China Yunnan, Province 28.1763

prospect, significant CN China Xinjiang Uygur, Autonomous Region 44.1439prospect MN Mongolia Dzavhan, Province 48.9500prospect CN China Xinjiang Uygur, Autonomous Region 43.6800prospect CN China Xizang, Autonomous Region 31.0537prospect MN Mongolia Ömnögovi, Province 43.1235prospect MN Mongolia Arhangay, Province 48.6833deposit CN China Qinghai, Province 35.3101prospect, significant CN China Xinjiang Uygur, Autonomous Region 42.3583prospect MN Mongolia Dornod, Province 49.1342prospect, significant MN Mongolia Bayanhongor, Province 45.7630prospect, significant MN Mongolia Govi-Altay, Province 46.0500prospect, significant CN China Xinjiang Uygur, Autonomous Region 47.2459prospect, significant MN Mongolia Ömnögovi, Province 42.7106prospect, significant MN Mongolia Bulgan, Province 48.7750prospect, significant MN Mongolia Bulgan, Province 49.1909prospect MN Mongolia Selenge, Province 49.6075prospect MN Mongolia Bulgan, Province 48.8167prospect MN Mongolia Selenge, Province 49.5622prospect MN Mongolia Selenge, Province 49.7667prospect, significant CN China Xizang, Autonomous Region 31.4006prospect MN Mongolia Uvs, Province 49.3481prospect, significant CN China Xinjiang Uygur, Autonomous Region 35.5462prospect MN Mongolia Bayanhongor, Province 44.1808prospect MN Mongolia Ömnögovi, Province 43.9420prospect MN Mongolia Ömnögovi, Province 43.9833prospect CN China Yunnan, Province 28.1437prospect CN China Xinjiang Uygur, Autonomous Region 43.5597deposit RU Russia Khakass, Republic 54.0107prospect MN Mongolia Ömnögovi, Province 42.6277prospect, significant MN Mongolia Dornod, Province 48.0948prospect MN Mongolia Ömnögovi, Province 44.3833prospect, significant CN China Qinghai, Province 36.7630prospect MN Mongolia Dzavhan, Province 48.9667prospect MN Mongolia Hovd, Province 47.5442prospect RU Russia Amur, Region 54.0833prospect MN Mongolia Hovd, Province 47.1588prospect MN Mongolia Töv, Province 46.8167prospect, significant MN Mongolia Selenge, Province 49.5333prospect MN Mongolia Dornod, Province 49.0500prospect MN Mongolia Sühbaatar, Province 45.2501prospect MN Mongolia Dzavhan, Province 49.5167prospect MN Mongolia Selenge, Province 49.7333prospect, significant CN China Heilongjiang, Province 50.1166prospect MN Mongolia Ömnögovi, Province 44.0953prospect MN Mongolia Bulgan, Province 49.0817

prospect MN Mongolia Töv, Province 48.5960prospect, significant MN Mongolia Övörhangay, Province 45.8948deposit MN Mongolia Dornogovi, Province 43.8605prospect, significant MN Mongolia Bayanhongor, Province 45.9500prospect MN Mongolia Dzavhan, Province 48.6000prospect MN Mongolia Dundgovi, Province 45.8167prospect MN Mongolia Selenge, Province 49.1333prospect MN Mongolia Ömnögovi, Province 43.9000prospect, significant CN China Qinghai, Province 35.9304prospect MN Mongolia Töv, Province 46.7167prospect MN Mongolia Bulgan, Province 48.2012deposit CN China Xinjiang Uygur, Autonomous Region 42.1038prospect MN Mongolia Ömnögovi, Province 44.0333prospect MN Mongolia Bulgan, Province 48.2012prospect MN Mongolia Dornogovi, Province 44.4464prospect MN Mongolia Övörhangay, Province 46.8574prospect MN Mongolia Dornogovi, Province 44.4000prospect MN Mongolia Bulgan, Province 48.2167prospect, significant MN Mongolia Ömnögovi, Province 43.1244prospect, significant RU Russia Gorno-Altay, Republic 49.6167prospect MN Mongolia Dornogovi, Province 43.6000prospect MN Mongolia Bulgan, Province 48.7000prospect, significant MN Mongolia Töv, Province 46.7379prospect, significant MN Mongolia Töv, Province 46.7292prospect CN China Xinjiang Uygur, Autonomous Region 46.0988prospect CN China Xinjiang Uygur, Autonomous Region 46.0835prospect CN China Xinjiang Uygur, Autonomous Region 45.9517prospect CN China Xinjiang Uygur, Autonomous Region 45.9651prospect CN China Xinjiang Uygur, Autonomous Region 45.8639prospect CN China Xinjiang Uygur, Autonomous Region 45.9538prospect CN China Xinjiang Uygur, Autonomous Region 46.0183prospect CN China Xinjiang Uygur, Autonomous Region 45.3834prospect MN Mongolia Ömnögovi, Province 43.3833prospect MN Mongolia Töv, Province 47.2500prospect MN Mongolia Töv, Province 46.6347prospect MN Mongolia Övörhangay, Province 45.5833prospect MN Mongolia Övörhangay, Province 46.7167prospect MN Mongolia Dornod, Province 49.2330prospect MN Mongolia Selenge, Province 49.4167prospect CN China Qinghai, Province 37.2535prospect, significant CN China Xinjiang Uygur, Autonomous Region 45.3581prospect, significant CN China Nei Mongol, Autonomous Region 43.4467prospect CN China Nei Mongol, Autonomous Region 42.3794prospect CN China Nei Mongol, Autonomous Region 45.2734prospect CN China Xinjiang Uygur, Autonomous Region 46.7048

prospect CN China Xinjiang Uygur, Autonomous Region 46.8570prospect CN China Xinjiang Uygur, Autonomous Region 46.5709deposit CN China Yunnan, Province 28.0089prospect MN Mongolia Selenge, Province 48.8667prospect MN Mongolia Arhangay, Province 48.7833prospect MN Mongolia Selenge, Province 48.9333prospect CN China Qinghai, Province 37.1402prospect CN China Qinghai, Province 35.3729prospect CN China Xinjiang Uygur, Autonomous Region 46.6027prospect MN Mongolia Bulgan, Province 48.8167prospect MN Mongolia Dornod, Province 49.1000prospect CN China Yunnan, Province 28.5523prospect, significant MN Mongolia Dzavhan, Province 48.7260prospect, significant MN Mongolia Ömnögovi, Province 43.2857prospect MN Mongolia Selenge, Province 48.9000prospect, significant MN Mongolia Bulgan, Province 49.2149deposit MN Mongolia Bayanhongor, Province 43.9824prospect MN Mongolia Bulgan, Province 48.8000prospect MN Mongolia Selenge, Province 49.0833

Longitude Depo_Type Depo_Subty Age_Ma89.2000 Porphyry Cu-Mo Cu-Mo

103.8583 Porphyry Cu96.2167 Porphyry Cu-Mo96.5834 Porphyry Cu Cu-Mo 516

107.7167 Porphyry Cu98.1000 Porphyry Cu

107.7268 Porphyry Cu105.0219 Porphyry Cu107.1182 Porphyry Cu


99.8388 Porphyry Cu107.7750 Porphyry Cu105.9000 Porphyry Cu102.8000 Porphyry Cu116.1620 Porphyry Cu103.3639 Porphyry Cu112.5020 Porphyry Cu 396

99.4466 Porphyry Cu84.4781 Porphyry Cu 31188.6333 Porphyry Cu 275

111.2167 Porphyry Cu103.6474 Porphyry Cu101.7067 Porphyry Cu106.2448 Porphyry Cu106.1452 Porphyry Cu

99.5000 Porphyry Cu100.6833 Porphyry Cu104.8833 Porphyry Cu 222

81.4257 Porphyry Cu 301112.3333 Porphyry Cu

97.2500 Porphyry Cu74.2897 Porphyry Cu 481

107.8743 Porphyry Cu 333.6104.3000 Porphyry Cu105.9667 Porphyry Cu

99.7000 Porphyry Cu83.8280 Porphyry Cu Cu-Mo

105.8025 Porphyry Cu, Au (Mo)93.1166 Porphyry Cu


108.3000 Porphyry Cu110.4490 Porphyry Cu 263111.4317 Porphyry Cu, skarn-related


118.5070 Porphyry Cu 257.593.0235 Porphyry Cu 322







82.4045 Porphyry Cu, skarn-related106.3160 Porphyry Cu111.0833 Porphyry Cu125.7779 Porphyry Cu 485

83.4406 Porphyry Cu 118104.1316 Porphyry Cu 240.7112.5167 Porphyry Cu112.6850 Porphyry Cu

99.8345 Porphyry Cu, skarn-related80.3887 Porphyry Cu 112


97.2475 Porphyry Cu 334104.8000 Porphyry Cu105.3167 Porphyry Cu

95.2516 Porphyry Cu 40599.8890 Porphyry Cu, skarn-related 214



99.5014 Porphyry Cu

90.9891 Porphyry Cu 21975.4668 Porphyry Cu91.8175 Porphyry Cu85.7772 Porphyry Cu81.7814 Porphyry Cu 31783.2784 Porphyry Cu 315

105.6000 Porphyry Cu104.5000 Porphyry Cu108.1987 Porphyry Cu105.9833 Porphyry Cu106.1500 Porphyry Cu103.3159 Porphyry Cu107.7833 Porphyry Cu106.1995 Porphyry Cu Cu-Au 330105.3833 Porphyry Cu106.5127 Porphyry Cu104.1667 Porphyry Cu106.4167 Porphyry Cu104.8294 Porphyry Cu104.9667 Porphyry Cu102.9264 Porphyry Cu101.9215 Porphyry Cu103.1667 Porphyry Cu104.8095 Porphyry Cu

98.3649 Porphyry Cu104.1333 Porphyry Cu110.9333 Porphyry Cu112.8417 Porphyry Cu-Mo102.1167 Porphyry Cu103.6333 Porphyry Cu

89.9072 Porphyry Cu Cu-Mo 47076.1622 Porphyry Cu Cu-Au 29286.7520 Porphyry Cu-Mo92.8833 Porphyry Cu 51496.7833 Porphyry Cu84.3305 Porphyry Cu 32572.3333 Porphyry Cu Cu-Au 44582.9451 Porphyry Cu 359

105.8000 Porphyry Cu80.9754 Porphyry Cu 36699.9723 Porphyry Cu

110.1330 Porphyry Cu99.8064 Porphyry Cu88.8333 Porphyry Cu92.8107 Porphyry Cu 288

93.4079 Porphyry Cu108.2500 Porphyry Cu 292.3105.1028 Porphyry Cu108.4667 Porphyry Cu113.6910 Porphyry Cu

98.8500 Porphyry Cu (?)95.3070 Porphyry Cu 413




97.7814 Porphyry Cu 273108.0182 Porphyry Cu 333.2105.7500 Porphyry Cu107.1667 Porphyry Cu110.5000 Porphyry Cu

76.7272 Porphyry Cu Cu-Au 410106.3280 Porphyry Cu, skarn-related113.0500 Porphyry Cu113.5292 Porphyry Cu113.4000 Porphyry Cu113.4500 Porphyry Cu110.5333 Porphyry Cu



99.8654 Porphyry Cu104.9333 Porphyry Cu105.9992 Porphyry Cu106.0500 Porphyry Cu106.8535 Porphyry Cu Cu-Au 372104.1333 Porphyry Cu 285104.6000 Porphyry Cu

95.9750 Porphyry Cu109.4296 Porphyry Cu 330103.8584 Porphyry Cu106.1833 Porphyry Cu102.9500 Porphyry Cu

99.9864 Porphyry Cu Cu-Au 21399.8906 Porphyry Cu 217

83.0267 Porphyry Cu97.8333 Porphyry Cu82.4667 Porphyry Cu85.9709 Porphyry Cu, skarn-related 88


99.7906 Porphyry Cu, skarn-related Cu-Au 22694.7555 Porphyry Cu 278



106.1483 Porphyry Cu104.2167 Porphyry Cu103.7639 Porphyry Cu105.6140 Porphyry Cu102.5667 Porphyry Cu105.6305 Porphyry Cu104.9500 Porphyry Cu

88.9311 Porphyry Cu, skarn-related 11692.1222 Porphyry Cu81.6731 Porphyry Cu98.3602 Porphyry Cu


99.9615 Porphyry Cu 22183.8413 Porphyry Cu90.1986 Porphyry Cu Cu-Mo 396.5


91.0157 Porphyry Cu, skarn-related 23897.2500 Porphyry Cu92.7870 Porphyry Cu

123.8333 Porphyry Cu (?)93.1741 Porphyry Cu

104.4333 Porphyry Cu105.2333 Porphyry Cu113.4000 Porphyry Cu112.1190 Porphyry Cu

95.8167 Porphyry Cu105.3000 Porphyry Cu125.7680 Porphyry Cu 485107.7509 Porphyry Cu103.8978 Porphyry Cu

104.5930 Porphyry Cu102.8991 Porphyry Cu108.3441 Porphyry Cu 370100.1694 Porphyry Cu

98.9500 Porphyry Cu104.3667 Porphyry Cu105.7000 Porphyry Cu107.6500 Porphyry Cu


92.5576 Porphyry Cu 323106.2000 Porphyry Cu102.9799 Porphyry Cu109.5385 Porphyry Cu104.1268 Porphyry Cu 214108.1000 Porphyry Cu102.8667 Porphyry Cu106.9066 Porphyry Cu 361.4


84.9336 Porphyry Cu84.7486 Porphyry Cu84.8483 Porphyry Cu84.6566 Porphyry Cu84.5090 Porphyry Cu84.4013 Porphyry Cu84.4441 Porphyry Cu84.0366 Porphyry Cu

106.5000 Porphyry Cu105.2667 Porphyry Cu104.8500 Porphyry Cu102.7333 Porphyry Cu103.1333 Porphyry Cu113.4793 Porphyry Cu105.4167 Porphyry Cu




89.2245 Porphyry Cu 32790.0597 Porphyry Cu 37799.8095 Porphyry Cu 225


91.3165 Porphyry Cu 22499.7202 Porphyry Cu90.0192 Porphyry Cu 377




99.2196 Porphyry Cu Cu-Mo102.0667 Porphyry Cu105.0500 Porphyry Cu

Age_method Age_stratMiddle DevonianCaledonianVariscan

Re-Os Late CambrianVariscanCaledonianVariscanVariscanVariscanCaledonianVariscanVariscanTriassicVariscanVariscanVariscan

VariscanVariscan

Ar-Ar Early Devonian Caledonian to VariscanRe-Os Middle Carboniferousunknown Early Permian

CaledonianVariscanVariscanVariscanVariscanVariscanVariscan

K-Ar Late TriassicRe-Os Late Carboniferous

VariscanCaledonian

Rb-Sr Early OrdovicianU-Pb zircon Early Carboniferous

VariscanVariscanVariscanVariscanEarly PermianCambrianVariscanVariscanCaledonian

VariscanU-Pb Early Permian

CaledonianCaledonianCarboniferous to Triassic

Re-Os Early PermianU-Pb Middle Carboniferous

Caledonian to VariscanVariscanTriassicVariscanCaledonian to VariscanVariscanVariscanVariscanVariscanVariscanVariscanVariscanVariscan

VariscanVariscanVariscan

U-Pb Early OrdovicianRe-Os Early CretaceousRe-Os Middle Triassic

VariscanVariscanTriassic

U-Pb Early CretaceousVariscanVariscan

Rb-Sr Early CarboniferousVariscanVariscan

U-Pb Early DevonianRb-Sr Late Triassic

Late TriassicVariscanVariscanVariscanVariscan


U-Pb Late Triassic Paleozoic to Triassic Variscan

CambrianU-Pb Middle CarboniferousRe-Os Middle Carboniferous

CaledonianVariscanVariscanVariscanVariscanVariscanVariscan

Re-Os Early CarboniferousVariscanVariscanVariscanVariscanVariscanVariscanVariscanVariscanVariscanCaledonianVariscanVariscanVariscanVariscanVariscanVariscan

Ar/Ar Early Ordovicianunknown Late Carboniferous

VariscanRe-Os Late Cambrian

Variscanunknown Early CarboniferousRb-Sr ? Late OrdovicianRe-Os Early Carboniferous

VariscanU-Pb Late Devonian

TriassicPaleozoicTriassicVariscan

U-Pb Early Permian

VariscanU-Pb zircon Late Carboniferous

VariscanVariscanVariscanVariscan

U-Pb Late SilurianVariscanVariscanCaledonianVariscanVariscanCaledonianVariscan

inference Early PermianU-Pb zircon Early Carboniferous


unknown Late Silurian Caledonian to Variscan

VariscanVariscanVariscanVariscanVariscanVariscanVariscanVariscanVariscanVariscanTriassicVariscanVariscanVariscan

Re-Os (Mo); U-Pb (zircon) Late DevonianInterpolated from histogram in Tong and others (2010) Early Permian

PermianVariscan

U-Pb zircon Early CarboniferousCaledonianVariscanVariscan

Re-Os Late TriassicAr-Ar Late Triassic


Ar-Ar Late CretaceousVariscanVariscan

K-Ar Late TriassicU-Pb Early Permian

VariscanK-Ar Early Carboniferous

CaledonianU-Pb Early Carboniferous

VariscanVariscanVariscanVariscanCaledonianVariscanVariscan

Re-Os Early CretaceousVariscanCarboniferousVariscan

Rb-Sr Middle CarboniferousVariscan

U-Pb Late TriassicVariscan

Ar-Ar Early DevonianVariscanVariscan?Variscan

Re-Os Middle TriassicVariscanCambrianVariscanCambrianVariscanVariscanVariscanVariscanCaledonianVariscan

Re-Os Early OrdovicianVariscanVariscan

VariscanVariscan

Re-Os Late DevonianVariscanCaledonianVariscanVariscanVariscan

Paleozoic to TriassicVariscanVariscan

Re-Os Early CarboniferousVariscanVariscanVariscan

unknown Late TriassicVariscanVariscan

U-Pb zircon Early CarboniferousVariscanVariscanVariscanVariscanVariscan

Variscan Variscan Variscan Variscan Variscan Variscan Variscan Variscan

VariscanVariscanVariscanCaledonianVariscanVariscanVariscan

U-Pb Late TriassicCarboniferousVariscan

Re-Os Early Carboniferous VariscanU-Pb Late Silurian

U-Pb Early CarboniferousRe-Os Middle Devonianunknown Late Triassic

CaledonianCaledonianCaledonian

U-Pb Late Triassic Paleozoic to TriassicRe-Os Middle Devonian

VariscanVariscan

Variscanunknown Early Triassic

VariscanCaledonianVariscanVariscanVariscanVariscan

Age_refNokleberg (2010)inferenceinferenceBerzina and Berzina (2008)inferenceinferenceinferenceinferenceinferenceinferenceinferenceinferenceHou and others (2007)inferenceinferenceinferenceinferenceinferenceLi and others (2008)inferenceLiu and others (2009b)W.J. Nokleberg (written commun., 2006)inferenceinferenceinferenceinferenceinferenceinferenceinferenceLamb and Cox (1998)Zhang and others (2006)inferenceinferenceKudryavtsev (1996)Blight and others (2010)inferenceinferenceinferenceinferenceGobi-Khurakh LLC (2013)Lyndhurst Enterprises Pty. Ltd. (2011)inferenceinferenceinference

inferenceLiu and others (2007)inferenceinferenceinferenceLiu and others (2010a)Wu and others (2006)inferenceinferenceHou and others (2007)inferenceinferenceinferenceinferenceinferenceinferenceinferenceinferenceinferenceinferenceinferenceinferenceinferenceGe and others (2007)She and others (2006)Watanabe and Stein (2000)inferenceinferenceHou and others (2007)Qu and Xin (2006)inferenceinferenceXu and others (2010)inferenceinferenceCheng and others (2010)Hou and others (2007), Li and others (2011)inferenceinferenceinferenceinferenceinferenceinferenceinferenceinference

Li and others (2008)inferenceMiao and others (2007)A.F. Chitalin (written commun., 2009)Zhang and others (2008b)Jia and others (2011)inferenceinferenceinferenceinferenceinferenceinferenceinferenceunknowninferenceinferenceinferenceinferenceinferenceinferenceinferenceinferenceinferenceinferenceinferenceinferenceinferenceinferenceinferenceinferenceSotnikov and others (1995, 1999)Singer and others (2008)inferenceLyndhurst Enterprises Pty. Ltd. (2011)Inference (proximity to Aksug - 402.5 Ar-Ar, Sotnikov and others (2003), Berzina and others (2005)Singer and others (2008)Kudryavtsev (1996)Xue and others (2011), Zhang and others (2010b), Tang and others (2010)inferenceTang and others (2010)Li and others (2011)Yan and others (2007)Hou and others (2007)inferenceZhang and others (2006)

Xu and others (2004)Blight and others (2010)inferenceinferenceinferenceinferenceWang and others (2009, 2010b)inferenceinferenceinferenceinferenceinferenceinferenceinferenceBadarch and others (1999)Blight and others (2010)inferenceinferenceinferenceSeltmann and Porter (2005)inferenceinferenceinferenceinferenceinferenceinferenceinferenceinferenceinferenceinferenceinferenceLi and others (2011)inferenceinferenceinferenceKhashgerel and others (2009)Tong and others (2010)Ivanhoe Mines Ltd. (2001)inferenceBlight and others (2010)inferenceinferenceinferenceLeng and others (2008)Li and others (2011)

Jia and others (2011)inferenceinferenceXin and Qu (2006)inferenceinferenceWu and others (2010)Li and others (2004)inferenceWatanabe and others (1999)inferenceGuo and others (2010)inferenceinferenceinferenceinferenceinferenceinferenceinferenceZhao and others (2009)inferenceDequan and others (2005)inferenceBatkhishig and others (2010)inferenceLeng and others (2008)inferenceBerzina and others (2005)inferenceinferenceinferenceWu and others (2010)inferenceLyndhurst Enterprises Pty. Ltd. (2011)inferenceLyndhurst Enterprises Pty. Ltd. (2011)inferenceinferenceinferenceinferenceinferenceinferenceGe and others (2007)inferenceinference

inferenceinferenceWatanabe and Stein (2000)inferenceinferenceinferenceinferenceinferenceinferenceinferenceinferenceRui and others (2002); Re-Os 343 ± 26, Zhang and others (2004)inferenceinferenceinferenceunknowninferenceinferenceKhashgerel and others (2009)inferenceinferenceinferenceinferenceinferenceTang and others (2010)Tang and others (2010)Tang and others (2010)Tang and others (2010)Tang and others (2010)Tang and others (2010)Tang and others (2010)Tang and others (2010)inferenceinferenceinferenceinferenceinferenceinferenceinferenceWu and others (2010)Dequan and others (2005)inferenceNie and others (2005)inferenceShen and others (2010b)

Wang and others (2010c)Xue and others (2010)Rui and others (2005)inferenceinferenceinferenceWu and others (2010)inferenceXue and others (2010)inferenceinferenceFei and Li (2010)Singer and others (2008)inferenceinferenceinferenceinferenceinferenceinference

Comm_major Comm_minor Tonnage_Mt Cu_pct Mo_pct Au_ppm Ag_ppm Con_Cu_t Au_MoMo, Cu Ag, Re 310.476 0.032 0.05 1.64 99352.3

Cu-Mo Au, AgCu, Mo, Au, Ag 805.2 0.52 0.014 0.156 0.99 4187040 11.1Cu MoCu Mo, AgCu

Cu

CuCu

Cu MoCu

Cu, Mo Au, AgCu Cu, Mo, Au, Ag 225 0.28 0.011 0.1 1.8 630000 9.1Cu, Mo Cu

CuCuCu, AuCu Mo, Au

Cu, Mo AuCu, MoCu Pb, Ag, Bi, SbCu Au, Pd, PGECu, Au, Mo Pt, Pd, Re 1000 0.67 0.0023 0.049 1.61 6700000 28.6Cu, Au Mo, AsCu, MoCu Al

Cu Pb, ZnCu, Au MoCuCu Mo

CuCu, Mo, Au Ag, Pb, ZnCu, FeCuCu, Mo Ag, AuCu, Mo 178.6 0.14 0.07 250040Mo, Cu Cu, Au

CuCu MoCu, Au

Au Cu

CuCu AgCuCu, Mo Au, Ag, Pt 644 0.52 0.02 0.255 6.1 3348800 12.75Cu, Au MoCu, Mo 2370 0.38 0.013 9006000Cu Mo, PbCu AgCuCuCu AgCu, MoCuCu MoCu Mo, Ag, AuCuCuCuCuCu, Zn, Pb

CuCu

Cu, Pb, ZnCu Pb, ZnCu, Au Cu AuCu, Mo, AuCu, MoCu AgCu Pb, Co, As, CrCuCu Au, Ag

Cu Cr, Ni, CoCu, Au MoCu Mo, Pb, Au, AgCu

CuCu, ZnCu MoCuCu

Cu, AuCu Pb, AsCuCu Mo, Au, Ag, WCu

Cu Mo, W 30 1 0.05 300000Cu, Au, Ag 57 0.62 0.72 3.8 353400Cu, MoCu, Au, MoCu, Mo Au, AgCu Mo 542 0.3 0.005 1626000Cu, Mo, Au, Ag Mo 65.8 0.48 0.015 0.2 6.56 315840 13.3Cu, Mo

Cu, Mo, Au ZnCuCuCuCu, Mo Cu

Cu, AuCuCuCuCu, Mo, Au

Cu, MoCuCuCuCuCuCu, Mo

Cu MoCuCuCu MoCu ZnCu, Mo, Au, Ag Au 213 0.81 0.01 0.26 2.5 1725300 26Cu Au

CuCu Au

CuCu

Cu, Mo AuCu Ag, Zn, AsCu, Mo Au 3754.56 0.98 0.01 0.38 36794688 38Cu, Zn AgCu, Au, MoCuCu, MoCuCu Mo, AuCu AuCu, Mo, Au, Ag 1229 0.34 0.01 0.18 1.27 4178600 18Cu

Cu, Mo

Cu, Mo CuCu, Au

Cu, Au, Ag Pb, Zn 128 1.13 0.48 1446400Cu, Mo

Cu, Mo Au, AgCuCu, AuCuCu MoCu Mo, Au, Ag, Ba

Cu Mo

Cu, MoCuCuCuCuCu MoCuCu, AuCu, Mo, Au, Ag 323.5 0.17 0.058 0.017 2.3 549950 0.3CuCu, Au AgCuCu, Mo

Cu, Au

Cu, AuCu PbCu

Cu

Cu, Au MoCu, AuCu

CuCuCu Mo, Au, Ag 240 0.53 0.018 0.084 2.6 1272000 4.7Cu Au

Cu Mo

Cu Pb, AgCu, AuCu MoCuCu, Au, Ag Mo, Pb, Zn 674.34 0.61 0.01 0.1 1.28 4113474 10Cu Ag, MoCuCuCuCu

Cu MoCuCu Mo

Cu MoCuCuCuCuCuCuCuCuCuCu MoCuCu Zn, Sn, AuCu MoCuCu, Mo W, Pb, ZnCu MoCu, MoCuCu Mo, Cu, AuCu, AuCu, Mo

Cu, MoCu, Mo, Au AgCu Au, Ag 60 0.5 0.06 1.4 300000

Cu Au

Cu, MoCu, Zn, PbCu, Mo, Au Ag

Cu, ZnCu MoCuCuCuMo, Cu 650 0.063 0.046 409500

G_T_comCu, Mo, Au, and ore tonnage from SMR (2011), and includes 509.1 t silver, and 5.9 t rhenium. A.F. Chitalin (written commun., 2009) indicates probable reserve of 155 Kt Mo (0.05%), 0.1 Mt Cu (0.032%).

Average grade of 0.07% Mo.Reported: 5 to 96 ppb Pt, 16 to 924 ppb Pd; 14 to 50 ppb Re; Ave. Cu/Mo in ores: 40-70; Mo Contained Total Reserves & Resources mt = 113000; Au Contained Total Reserves & Resources oz = 4038000; Ag Contained Total Reserves & Resources oz = 25551000.Drilling in 2008 confirmed presence of chalcopyrite below 650 m.Average grade of 0.1-1.5% Cu, 0.1-0.15% Mo, 0.005-0.01% Ag.

A.F. Chitalin (written commun., 2009) indicates Cu 0.22 pct min, 0.93 pct max, 0.37 pct ave; Au 1.1 gpt min., 9.7 gpt max., and 6.2 gpt ave.

Cu grades from 0.35 to 0.78%.

Exploratory drilling & trenching define Cu metal reserve >500,000 tons with a mean grade of 0.91%; Mo is 20,000 tons with a mean grade of 0.06%, and Au is 30 tons with a mean grade of 0.98g/t (Jian and others, 2007). Ag g/t 2.84 (Singer and others, 2008).Resource of 17.9 Mt @ 1.17% Cu and 14 g/t Au.Individual g/t data in Tang and others (2010).

Grab samples to 0.98% Cu and 5.5 g/t Au.

At area 0.6 x 2.3 km, %: >0.1 Cu, >0.002 Mo, >0.1 g/t Au; A zone 300 by 900 m contains >0.3 wt% Cu, 0.005 wt% Mo.Cu-rich zone overlies Mo-rich zone; dacites are calc-alkaline; granite porphyry is A-type; Source of prospect indicates that it may be Cu-Mo subtype.

Drill intersection of 24 m assayed at 0.5% Cu, 0.1g/t Au, 0.1g/t Pd. Rock samples assayed up to 2.8% Cu, 1.37 g/t Pd, 0.5 g/t Au, and 0.29 g/t Pt.Ussoltsev (2011) estimated geological resource of 1,169 Mt of ore at a copper grade of 0.36%, a gold grade of 0.21 g/t, a silver grade of 4.9 g/t and molybdenum and rhenium by-products.Exploration 1971-77 by Soviet and Mongolian geologists indicated a preliminary resource of 39,000 t of Cu at a grade of 0.31%. Subsequent drilling (2005, 2010, 2011) has encountered similar grades.

Tens of thousands of tons Cu metal (speculated, Laznicka 1976).3 drill holes as deep as 700 m indicate a prognostic resource of 37,800 t of Cu.

Many rock chip samples greater than 5% Cu.

Also reported 111Kt of Cu at 0.5%; 50 Kt of Mo at 0.12%.Small deposit with grades of 0.4% Cu, 0.03% Mo. Source of prospect indicates that it may be Mo-Cu subtype.

Approximate resource of 800 Kt Cu.Completed a ten hole diamond drilling program in 2008; Hole FDD007 intersected 18m @ 0.27% Cu from 18m and 5m @ 0.01% Mo from 17m.

Quartz-epidote-pyrite-clay alteration; gold values from grab samples occur up to 1.04 grams per tonne gold with elevated copper. Source of prospect indicates that it may be Au-Cu subtype.

Proven reserves: 1.79Mt Cu, 61,300 t Mo, 60.29 t Au, 777.08 t Ag from ZiJin Mining Group Co. 2011.Inferred resource of 5.38 Mt of Cu @ 0.72%; 41 t Au @ 0.23 g/t. Source of prospect indicates that it may be Cu-Au subtype.Data from Singer and others (2008).

Average grade is 1-2.02% Cu.

Old mining district undergoing reevaluation.

Approximate resource of 1,000 Kt Cu.

Drill results include >30 m at >0.5% Cu and >0.03 g/t Au.

Average grade of 0.07 to 1% Cu, to 0.05% Mo, to 0.002% Ag.

Cu grades of 0.2 - 1.06%.Intersection 40-110 m: 0.81% Cu, 0.7 to 9.0 g/t Au; chip samples average 0.88 g/t Au; approximate reserve estimate 8.6 Mt ore. Source of prospect indicates that it may be Cu-Au subtype.Partial resource of 27.4 Mt @ 0.46% Cu - could be a massive sulfide deposit.

Previous small-scale mining. Source of prospect indicates that it may be Cu-Mo subtype.

0.001-1.0% Cu reported by Nokleberg and others (2003).The resource reported in Singer and others (2008) [229 Mt at 0.35% Cu] is only partial, but drilling has apparently been suspended.

Chip samples: 1.84% Au, 0.43 g/t Au, >300 ppm Mo.Trench sampling: 18m at 1.84% Cu and 0.43 g/t Au; Drill Intercept of 50m at 1.0% Cu and 0.3 g/t Au.Two rock chip samples contain 0.1 g/t Au and 2.3-6.6 g/t Ag. Soil sampling reveals anomaly aureoles of Ba (0.03-0.09%), Cu (0.005-0.009%) and Mo (0.004-0.008%). Grade of 0.12-0.25% Cu, rare 0.005-0.2% WO3, 0.005-0.05% Mo & Sn up to 0.01%.

116 m @ 2.4% Cu, 7.2 g/t Ag from 30 m; 75 m @ 2.4% Cu, 5.7 g/t Ag from 48 m; 34 m @ 3.4% Cu, 14.7 g/t Ag from 92 m from Voyager Resources (2013).

Cu tonnage is calculated from Cu grade and ore tonnage from Singer and others (2008).Grade and tonnage from Singer and others (2008); Seltmann and others (2009) reported a grade of 0.76% Cu, 0.9g/t Au, 3.8g/t Ag and an ore reserve tonnage of 0.37Mt Cu.Multiple grades reported (A.F. Chitalin, written commun., 2009): Cu 0.2-0.3%, Mo 0.005-0.01%. Cu 0.46% min., 0.61% max., 0.5% average; Mo 0.01% min., 0.13% max., 0.05% average; Au 0.01 gpt min., 3.3 gpt max., 0.2 gpt average.Individual assays in the 55+ m wide porphyry-style alteration zone ranged up to 0.28% copper and 1.5 g/t gold; arsenic and silver were significantly elevated (Lyndhurst Enterprises Pty. Ltd., 2011).Grade of 0.1-0.3% Cu.

Grade reported by Seltmann and others (2009) 0.48% Cu, 0.05% Mo; 0.2 g/t Au, 6.56 g/t Ag. Cu tonnage is calculated from Cu grade and ore tonnage.Small resource at Cu grades of 0.1 to 0.2% and Mo grades of 0.06 to 0.3%. Source of prospect indicates that it may be Cu-Mo subtype.

Resource of > 1 Mt metal at copper grades of 0.3 to 3.7% Cu and 0.6 to 0.7% Zn. Source of prospect indicates that it may be Cu-Mo subtype.claimed resource of 500 Kt Cu from Li and others (2011).Reported resource of 134 Kt of Cu @ 1% suggests it could be a skarn deposit.Approximate resource of 1,000 Kt Cu.

Widespread Cu, Au, and Mo geochemical anomalies; Source of prospect indicates that it may be Cu-Mo subtype.

Geologic mapping continued by Xanadu in 2011, based on results to date indicating strong possiblilty of discovering additional mineralised porphyry copper.

Average grade of 0.02-1.0% Cu, 0.003-0.008% Mo.

Average grade of 0.08% Cu, 0.0005% Mo in granite porphyry; 0.03 % Cu -0.001% Mo in granodiorite porphyry; 0.01% Cu and up to 0.001% Mo in diorite.0.1 to 0.3% Cu in 0.2 x 0.9 km bedrock area.

Average grade of 0.001-0.008% Cu, 0.001-0.005% Mo, 0.001-0.008% Pb and Zn.

Cu grade of ore minerals varies from 0.001% to 0.01%, rare 0.1%.claimed resource of 500 Kt Cu from Li and others (2011).

Average grade of 0.85% Cu, 192.3 g/t Ag, 0.01%W.Grab samples with > 1% Cu and anomalous Au and Mo.Four main ore zones form an E-W trend with average grades of (1) 0.36% Cu, 0.039% Ni and 0.04% Co, (2) 0.52% Cu, 05% Ni and 0.006% Co, with two samples containing 0.16 g/t Pd and 0.4 g/t Au, (3) 0.27% Cu and 0.031% Ni, and 0.38-0.78% Cu.0.3 to 5.1% Cu and 0.0035 to 0.006% Mo in 0.25 x 0.7 km bedrock area.Average grade of 0.001 - 0.6% Cu, 0.01 Mo, 0.01 - 0.02% W.Samples contains up to 1.5-2.16% Cu and 0.006-0.2% Zn; Soil samples reveal 4 anomalies: Cu 0.01-0.02%, ranging 4.7; 1.3; 0.6 & 3.8 sq. km.

Li and others (2011) give an average Pt grade 1.34 ppb, Pd, 4.95 ppb; Chen and others (2008): 6,400 t of Mo at 0.004%, 29 t of Au at 0.18 g/t.claimed resource of 500 Kt Cu from Li and others (2011).

Was producing 130 tonnes of ore per day, with an average grade of 1.2% Cu and 1 to 1.5g/t Au. Deep-seated porphyry Cu-Au deposit possible. Source of prospect indicates that it may be Cu-Au subtype..

Part of a 25 km long NE-SW mineral trend that includes Kendenggaoer and Lalisigaoer-3571, which have previous small-scale mining and Cu grades of 0.1% to 0.2%, respectively.

Cu grades 0.1–0.4% in porphyry part.Medium size deposit, with grades of 0.38 to 0.83% Cu. Source of prospect indicates that it may be Cu-Mo subtype.

The resource reported in Singer and others (2008) [101 Mt at 0.06% Cu] is only partial, but drilling has apparently been suspended.Drilling encountered intercepts of up to 3% Cu over 2 m intervals.Hanzheganeng occurrence Initial exploration, including limited drilling, indicates Cu grades of 0.1 to 4.5%, however Liu and others (2010d) call Hanzheganeng an epithermal deposit.Grab samples to 2.76% Cu and 1.64 g/t Au.Grade of 0.1-0.5% Cu, 0.0001%-0.1% Mo. Probable reserves of 500,000 tonnes Cu.Cu up to 0.42% in lithocap samples.

A skarn deposit, with indications of porphyry mineralization below; indicates extension of the Bangong-Nujiang porphyry belt.

Cu 1.02%.

200Kt Mo @0.04–0.10% in stockwork, 0.1–0.5% in breccia, ave. 0.058%; 500–600Kt Cu @0.02–0.20% in stockwork, 0.02–0.3% in breccia; Sotnikov and others (2001) reports 460 ppm (0.046%) Cu & wide range (<1 to 5400 ppm) for Mo; Ave. Cu/Mo in ores: 2-4.

Intercept of 221m at 0.2% Cu, 0.09 g/t Au, 3.7 g/t Ag.

Average Cu grade 1.34%.

Many intercepts of >0.1 % Cu and 0.1 g/t Au.

Average Cu grade of 0.44%, Mo of 0.023%; Ore area contains partial reserves of 910,000 tons Cu and 40,000 tons Mo, with average grades of 0.48% Cu and 0.02% Mo, from Zeng and others (2013).

Drilling in 2007 encountered 10 m averaging 0.552% Cu and 0.017g/t Au.

Average gold grade of 0.9 g/t estimated for entire property.

Cu grade 0.22 – 2.56%; Au grade 0.01 – 6.53 g/t. Source of prospect indicates that it may be Cu-Au subtype.

Tuwu, though being mined, has no certified resource information, only estimates.

Grade 0.2% Cu, 0.2% Mo. Source of prospect indicates that it may be Cu-Au subtype.Grade 0.3% Cu.

Consist of ore body that extends for 60-65 m, with width 200 m. Mineral composition is 50-69% quartz, 1-10% chalcopyrite, 10-35% pyrite, 1-10% malachite, 10-35% hematite.Average grade is 0.05-1.25% Cu.

Cu 0.55%,maximum 3.98%; Au 0.98 g/t.Two intercepts: 13.6 meters of 0.57% Cu; 2.5 meters of 0.19% Cu; values up to 0.88 g/t Au occur erratically down hole.

Li and others (2011) report a copper resource of 1.2 Mt.

Average grade of a single ore sample is 0.56%.Average grade of 0.2% Cu, 0.01% Mo. Resource of 100,000 tonnes Mo. Source of prospect indicates that it may be Cu-Mo subtype.Grab samples to 5.5% Cu and 0.19 g/t Au.

Grade 0.086% Cu.Cut off grade 0.03% Mo; inferred Re grade of about 150 g/t in concentrate.

Comments1The prospect area is 2.9 sq. km. Mining and geological conditions of Agaskyr deposit imply its development by open-pit operations (SMR 0211).Porphyry Cu - Mo (Ag, Re).Occurrence, large from Nokleberg and others (2006).Tonage, grades, and contained Cu are for total reserves and resources.Small Cu-oxide resource near surface.Consists of alteration zone (quartization, sericitization, limonitization,epidotization) to 5000 m long with width 100 to 300 m.Porphyry Cu (Au,Ag).Porphyry Cu - Mo (Ag, Re).Limited information.Deposit type uncertain. Cu-Au or Cu-Mo.Porphyry Cu - Mo (Ag, Re).The Central Mongolian metallogenic belt is dominated by skarn and porphyry Cu deposits.One of 6 Cu occurrences along ~40km mineral trend associated with andesitic volcaniclastic units and coeval hypabyssal intrusions (diorite, quartz diorite, etc.) formed in the Early Triassic (249 Ma; see Wenchang and others., 2011).Limited information.Porphyry Cu - Mo (Ag, Re).Source of prospect indicates that it may be Cu-Mo subtype.

Porphyry Cu - Mo (Ag, Re).Classification in dispute. Jian and others (2007) describe as early VMS characterized by banded Cu-bearing pyrite ores with superimposed Silruian (?) porphyry Cu. Li and others (2007, 2008) suggest it's an orogenic copper deposit.Medium-sized Cu deposit.Discovered in 1985-90; drilled out in 2002-2008 with 62 drill holes.Occurrence.Designated as a porphyry Cu by Nokleberg and others (1999); as a Granitoid related stockwork/ metasomatite Cu by Dejidmaa and others (2002).Porphyry Cu - Mo (Ag, Re).Copper oxide mineralization in altered volcanic tuff and siltstone; strike length of 1.5 km.Active prospect 2004–2011, limited information; This project was aquired by Erdenet Gold Inc. from Gallant Minerals Ltd. In 2005 (Erdene Gold Inc., 2006).Circular area of alteration (limonite and silicification) with anomalous copper and gold values in grab samples.Devonian host rocks; limited information.Porphyry Cu - Mo (Ag, Re).Abundant quartz-tourmaline-chalcopyrite veins and quartz-tourmaline breccias (Lamb and Cox, 1998); Exposed; an 39Ar/40Ar isotopic age is 220-233 Ma (Late Triassic) from Nokleberg and others (2003).Some drilling, active exploration.Designated as a porphyry Cu by Nokleberg and others (1999); as a Granitoid Granitoid related Au by Dejidmaa and others (2002), MRAM #188 located approximately 1 km to the S of point.Mineralized zones in thinly-covered pediment. Alkalic Cu-Au-PGE porphyry system.Mine is under construction, with production expected by 2015. Resource includes (Singer and others, 2008)); 0.59 to 1.04 g/t Pt, 0.28 to 0.37 g/t Pd in concentrate; 230 to 1,500 ppm (ave. 882 ppm) Re in Mo; Re will be produced.A 2004 Ivanhoe Mines investor information release uses different property names for this area. The names and locations of new owners Kincora Copper Ltd. are used here, but includes some geologic information from the 2004 Ivanhoe document.Porphyry Cu (Au,Ag).Source of prospect indicates that it may be Cu-Mo subtype.Porphyry Cu-Mo (Ag, Re), Deposit related to Calc-Alkaline and Alkaline Granitic Intrusions, Porphyry & Granitic Pluton-hosted Deposit from Dejidmaa and others (2002).Volcanic-associated epithermal vein/stockwork (Seltmann and others, 2009).Under active exploration in 2010.Stream-sediment, soil, and rock chip samples anomalous in Cu.Two prospects were grouped with this prospect (Bunkhan Khudag). The original location for Bunkhan Khudag was (44.199999, 107.883332). The original location for both Gun Sain Khudag I and Ulaan Tolgoi Bulag was 44.199999, 107.933332.Porphyry Cu-Mo (Ag, Re), Deposit related to Calc-Alkaline and Alkaline Granitic Intrusions, Porphyry & Granitic Pluton-hosted Deposit from Dejidmaa and others (2002).Porphyry Cu-Mo (Ag, Re), Deposit related to Calc-Alkaline and Alkaline Granitic Intrusions, Porphyry & Granitic Pluton-hosted Deposit from Dejidmaa and others (2002).

Porphyry Cu (Au, Ag).Liu and others (2007) classify Chaganoer as a porphyry Cu deposit.At the surface, the prospect is a large Cu-Fe (magnetite) skarn.Alteration zone to 400 long with width 8 to 10 m. Within the zone appeared the veins, vein-like body of quartz with shot and thin coating ore minerals.Confirmed as Indosinian by uncitable Chinese report.Molybdenite–chalcopyrite mineralization of the deposit mainly occurs as veinlets in stockwork ore and dissemination in breccia ore (Zeng and others, 2011).

Yanshanian tract designation based on abundant nearby K age rocks.Porphyry Cu-Mo (Ag, Re), Deposit related to Calc-Alkaline and Alkaline Granitic Intrusions, Porphyry & Granitic Pluton-hosted Deposit from Dejidmaa and others (2002).

Cu mineralisation occurs in a series of east-west zones controlled by the intrusion of porphyry dykes and sills into basaltic and andesitic volcanic and tuffaceous rocks.Raw prospect, no drilling.Porphyry Cu - Mo (Ag, Re).Porphyry gold and copper mineralization occur in a quartz monzonite host rock, which is locally brecciated and intruded with quartz stockwork veinlets.Porphyry Cu - Mo (Ag, Re).Porphyry Cu-Mo (Ag, Re).Porphyry Cu - Mo (Ag, Re).Porphyry Cu - Mo (Ag, Re).Porphyry Cu-Mo (Ag, Re).Porphyry Cu - Mo (Ag, Re).Possibly a Cu-Mo subtype based on its proximity to Lailisigao’er and 3571 (grouped in this database), and Kendenggao’er from Zhang and others (2010b).Two prospect points, Duchin Khural and Duchin Khural I, within 3km of each other were combined; See also Duchin Khural I site located at N44.083333, E106.366667.According to Nokleberg and others (1999), Dund Bayan is designated a porphyry copper occurrence by Ts. Gotovsuren, of the Monrud Company, Mineral Exploration and Mining Company, Ulaanbaatar, Mongolia. No other information available.A very large deposit with more than 3 Mt of contained copper; related to an Ordovician granodiorite pluton.two deposits, Duobuza and Bulong, combined because adjacent.Mineralization at depth between the known, but undeveloped Erdenet Central & Erdenet SE orebodies, along with drill results on the NW margins of the existing mine, demonstrate there is nearly continuous mineralization extending >10 km along a NW-SE trend.Source of prospect indicates that it may be Cu-Mo subtype.Upper Paleozoic based on nearby rocks of appropriate composition.Medium Cu skarn.112 Ma U-Pb date on intrusion.Nokleberg and others (1999) indicates site as a porphyry Cu-Mo.The source of this prospect, W.J. Nokleberg (written commun., 2006), indicates it is a Cu-Mo porphyry, but only indicates Mo as the commodity.Some mining of Au.Consists of diorite, syenite porphyry dikes and quartz-tourmaline vein.Source of prospect indicates that it may be Cu-Mo subtype.Large sericite-pyrite alteration zone, with copper minerals.Hongshan is primarily a skarn deposit - 1,500 x 800 m.Active exploration; Two permit areas are noted in a 2010 Lora Exploration investor presentation.Large exploration license with multiple targets.

Porphyry Cu-Mo (Ag, Re).Active prospect 2004–2011; limited information.Near Baogutu.Porphyry Cu - Mo (Ag, Re).Porphyry Cu-Mo (Ag, Re).

Designated as Cu-Mo porphyry occurrence by W.J. Nokleberg (written commun., 2006), but classified as a Pb-Zn-Cu polymetallic vein by Dejidmaa and others (2002). Possibily porphyry related?.

Classified as a porphyry Cu.Classified as a porphyry Cu.Miao and others (2007) says epithermal, like Zijinshan.Copper sulfide minerals in shear zones in a dacite porphyry that intrudes pyroclastic rocks.25 km east of Beidabate.Porphyry superimposed on skarn.Source of prospect indicates that it may be Cu-Au subtype.Designated as a porphyry Cu by Nokleberg and others (1999); as a Granitoid related stockwork/ metasomatite Cu by Dejidmaa and others 2002.Porphyry Cu (Au, Ag).Porphyry Cu (Au,Ag).A lens that extends for 50 m and from 5-10 m wide grades up to 0.014% Cu, 0.0015% Mo, 0.010% Pb, 0.050% Zn from W.J.Nokleberg (written commun., 2006).Porphyry Cu - Mo (Ag, Re).According to Nokleberg and others (1999), Kharaat Uul is designated a porphyry copper occurrence by Ts. Gotovsuren, of the Monrud Company, Mineral Exploration and Mining Company, Ulaanbaatar, Mongolia.Monzodiorite, monzonite, and diorite intrude Devonian sedimentary rocks in a 25 sq km mineralized area. At least four mineralized zones are present.Granitoid related Au-Ag-Cu.Active prospect 2004–2011; limited information.Porphyry Cu - Mo (Ag, Re).Cu(Fe, Au, Ag, Mo) skarn.Porphyry Cu (Au,Ag).Consists of quartz-tourmaline vein trending NW for 500-700 m with width 5 to 10 m.Porphyry copper prospect in southern Mongolia, 330 km west of Oyu Tolgoi.Consists of disseminated Cu minerals in intensively altered subvolcanic syenite porphyry intruding Permian siliceous volcanic rock. Silicifica and argillite alteration occur along a NW-trending fault zone.Porphyry Cu - Mo (Ag, Re).Porphyry Cu - Mo (Ag, Re).Intercepts: 168 m of 0.75% Cu & 5.4 g/t Ag from 76 m; 140 m of 0.6% Cu 5.3 g/t Ag from 4 m, including 62 m at 0.9% Cu & 7.7g/t Ag from 16 m, & 18 m at 1% Cu & 6.5g/t Ag from 16 m; 80 m of 0.8% Cu & 10.3g/t Ag from 60 m to end of hole.According to Nokleberg and others (1999), Khurelt Khudag is designated a porphyry copper occurrence by Ts. Gotovsuren, of the Monrud Company, Mineral Exploration and Mining Company, Ulaanbaatar, Mongolia. No other information available.Designated as a porphyry Cu by Nokleberg and others (1999); as a Granitoid related Au, primarily Au with Ag, Cu by Dejidmaa and others (2002).Occurrence.Porphyry Cu - Mo (Ag, Re).Cu- bearing zone trends NW for 200m with width of 4 m.Consists of a lensoid body that occurs along the contact of the Tuim granitoid pluton that intrudes Cambrian carbonate rock. Deposit occurs in a district that is 900 m long and ranges from 1 to 50 to 80 m thick.Exposed. The deposit is hosted in the andesite-basalt porphyrites and tuffs penetrated by granitoids of the Koktaszhalsky massif of tonalite-granodiorite-plagiogranite formation.Deposit minerals occur in two zones of hydrothermally-altered rock up to 5-6 km long and 200-500 m wide.Large area of stream-sediment, soil, and rock chip samples anomalous in Cu, Au, Mo, and As.Seltmann and Porter (2005) report age as Early Palaeozoic (Caledonian - Ordovician to Silurian).Au 3,894,000 ounces.100% of the deposit area is covered by loam. Discovered in 1970 while checking a magnetic anomaly.Sr and Nd isotopes suggest continental arc setting.Porphyry Cu - Mo (Ag, Re).Sr and Nd isotopes suggest continental arc setting.

Eastern Tianshan porphyry copper-gold belt. Medium deposit.

Porphyry Cu (Au, Ag).Active prospect 2004–2011; limited information.Porphyry Cu (Au, Ag).Calc-alkaline volcano-intrusive complex with widespread hydrothermal alteration; multiple intrusive phases.Possible Cu resource of 3.5 MT from A.F. Chitalin (written commun., 2009).Chalcopyrite-quartz veinlet stockwork; explored by trenches.Active prospect 2004–2011; limited information.Previous exploration between 1999 and 2004 identified a large (> 7 square km) zone of porphyry related advanced argillic alteration that is highly anomalous in Cu, Mo, Au, Ag and Ba.Consists of brecciated zone up to 10 to 100 m long with width 1.5 to 10 m. Within the zone appeared the veins, vein-like body and small stockwork of quartz with ore minerals.Drilling in 2007.Porphyry Cu (Au, Ag).Hosted in Middle and Late Cambrian granodiorite plutons intruding Neoproterozoic basement from W.J. Nokleberg (written commun., 2006).Porphyry Cu - Mo (Ag, Re).Consists of a Early Cambrian sedimentary and volcanic unit intruded by Middle to Late Cambrian Telmen Complex, the Late Devonian Tes Complex and Late Permian dikes.Deposit extends along the external contact of granodiorite and granosyenite massif. This zone divided into 3 subzones. These subzones are parallel and each is about 50 m wide and extend for 1000 m in a nearly EW direction.Granitoid related Au-Ag-Cu.Source of prospect indicates that it may be Cu-Mo subtype.Tract assignment based on location = Cretaceous plutonics.Hosted in the Devonian Middle Paleozoic segment of the Kazakh-Mongol arc (Yakubchuk, 2004; Seltmann and Porter, 2005).Nearby Oblaga Cu-Au skarn small-scale mining in 1987. Recently abandoned. Was producing 130 tonnes of ore per day, with an average grade of 1.2% Cu and 1 to 1.5g/t Au. Deep-seated porphyry Cu-Au deposit possible.Erdenetolgoi Occurrence from Nokleberg and others (1999), located 48.916667, 113.05.No. 11 occurrence from Nokleberg and others (1999) located close at 48.85, 113.533333.Same as Eastveiw digitiazed MRAM map point # 195.Same as Eastveiw digitiazed MRAM map point # 196.Porphyry Cu (Au, Ag).One prospect was grouped with this prospect. The original location of South was (46.451667, 99.301666).See also Shand. Consists of a broad zone of poorly mineralized rock as described in JICA-JOGMEC (2004).Porphyry Cu-Mo (Ag, Re).Porphyry Cu - Mo (Ag, Re), Deposit related to Calc-Alkaline and Alkaline Granitic Intrusions, Porphyry and Granitic Pluton-hosted Deposit from Dejidmaa and others (2002).Consists of weak Cu minerals in altered Late Permian rhyolite and dacite porphyry, their tuffs, tuff breccia and ignimbrite of the Khustai unit, intruded by syenite porphyry, quartz porphyry stocks and granite and felsite dikes.

Porphyry Cu - Mo (Ag, Re).A series of monzodiorite/diorite stocks that host a quartz stockwork, with anomalous copper, gold, and molybdenum.Designated as a porphyry Cu by Nokleberg and others (1999); as a Granitoid related Au by Dejidmaa and others (2002).G-T March 2010, from Ivanhoe Integrated Development Plan (IDP-10). Grades calculated by weighted average; Mo grade an estimate based on partial information.Consists of NW trending fracture zone with quartz veins 30-40m thick, 150m long.An area of Cu-bearing magnetite skarns and hydrothermal breccia pipes in Permian granitoid rocks.Consists of Cu sulfides in a Middle Cambrian gabbro and hornblendite stocks that occur along the Khangai fault system for 6.0 km and ranges up to 1.5 km wide.Copper and molybdenum mineralization in several altered areas, including a copper-stained tourmaline breccia-pipe complex.Porphyry Cu - Mo (Ag, Re).Consists of sulfide-bearing fault fractured, mylonitized & silica-altered zone in Permian volcanic rock. Host volcanic rock is white & contain pyrite & chalcopyrite disseminations & malachite & azurite coatings. Zone of silica replacement is oxidized.Porphyry Cu - Mo (Ag, Re).30% of the deposit area is covered by Quaternary moraine.

Source of prospect indicates that it may be Cu-Mo subtype.Porphyry Cu - Mo (Ag, Re).Porphyry Cu deposits connected with Late-Hercynian hypabyssal intrusive rocks.Related to bimodal suite of rocks.4 km-long geophysical anomalies coincident with Cu-oxide minerals.Porphyry Cu - Mo (Ag, Re).updated tonnage per China Nonferrous Metals news on internet.Potassic, phyllic, and proplylitic alteration; Fluid inclusions mostly low-salinity and less than 300 deg C.The Central Mongolian metallogenic belt is dominated by skarn and porphyry Cu deposits.

1,245 m of drilling in 2005–2006.Sr and Nd isotopes suggest island arc setting for the Hanzheganeng occurrence.Copper oxide mineralization at surface discovered in 2002 by Apiva Ventures; 5 drill holes in 2004.See also Ondor. Consists of a Cu sulfide zone with surface dimensions of 350 by 1100 m. The zone occurs in the SW and western part and along the contact of a granodiorite porphyry stock.Advanced argillic altered area is 7 km2 and may represent a high-sulfidation lithocap above a porphyry Cu system.Porphyry Cu - Mo (Ag, Re).Porphyry Cu - Mo (Ag, Re).Source of prospect indicates that it may be Cu-Mo subtype.Porphyry Cu - Mo (Ag, Re).

Hydrothermal altered grab samples anomalous in copper and/or gold.Orogenic porphyry-type sub-categories.Active prospect 2004–2011; limited information.Magmatic ring structure with diameter about 15 km, includes widespread advanced argillic alteration (alunite).Source of prospect indicates that it may be Cu-Mo subtype.In central segment of Zhongdian porphyry belt.Lenticular ore bodies; 480 by 28 m and 250 by 32 m.Note that all grades are based on petrologic samples, not mining.Active prospect 2004–2011; limited information.Eleven holes drilled in 2004.Porphyry Cu (Au,Ag).

Porphyry Cu - Mo (Ag, Re).Stream-sediment, soil, and rock chip samples anomalous in Cu and Au.Cu (Mo, U, Co) in skarn associated with granite-granodiorite and gabbro-plagiogranite intrusions from Rundkvist (2001).Stream-sediment, soil, and rock chip samples anomalous in Cu and Au.Porphyry Cu (Au,Ag).More than 3,600 m of drilling in 2005–2007 by Fortress/Phelps Dodge of large IP anomaly encountered many intercepts of >0.1 % Cu and 0.1 g/t Au.The Central Mongolian metallogenic belt is dominated by skarn and porphyry Cu deposits.Active prospect 2004–2011; Drilling has confirmed porphyry-related mineralization and alteration.Average grade of 0,005-0.1% Cu, 0.01-0.08% Zn, 0.002-0.05% Pb., from W.J. Nokleberg (written commun., 2006).Porphyry Cu - Mo (Ag, Re).Being mined, but no information was available about the resource. For the purposes of this assessment, it is considered a significant prospect with a very high probability of being a deposit.Former Ivanhoe property.Source of prospect indicates that it may be Cu-Mo subtype.

Rock-chip sampling: 0.1 to 5% Cu, 0.5 to 4.9 g/t Au, and 100 to 2000 ppm Mo. Drilling: 150 m at 0.37% Cu and 0.08 g/t Au; 64 m at 0.44% Cu and 0.06 g/t Au; 80 m at 0.35% Cu and 0.07 g/t Au..

Hydrothermall altered grab samples anomalous in copper and/or gold.Acquired in 2007 from Xstrata Cu.Tsagaansuvarga metallogenic belt.A high-sulfidation epithermal system that probably overlies porphyruy Cu system.Probably the same as Tsetsukhiin gol occurrence from Nokleberg and others (1999).Source of prospect indicates that it may be Cu-Mo subtype.Porphyry Cu - Mo (Ag, Re).Porphyry Cu (Au, Ag).

Source of prospect indicates that it may be Cu-Mo subtype.Active prospect 2004–2011; limited information.Yandong exposed, Tuwu partially covered, Yanxi totally covered; Tuwu, Yandong, and Yangxi combined because of proximity, continuity.Combined prospect site Ukhaa Khudag with Ukhaa Khudag II, which are approximately within 1.5 km of one another.Active prospect 2004–2011; limited information.Active prospect 2004–2011; limited information.Consist of quartz-tourmaline veinlet breccia and sericite-albite alteration zones.Porphyry Cu (Au, Ag).Porphyry Cu - Mo (Ag, Re).prospect ~15 km NNE of Oyu Tolgoi, 2 km^2 area Cu mineralization.Iron oxide copper-gold (IOCG) type? (Cu-Fe-Y-Yb-Co-Mo).Dejidmaa and others (2002) indicates porphyry Cu-Mo(Ag, Re); related to Calc-Alkaline and Alkaline Granitic Intrusion.Porphyry Cu - Mo (Ag, Re).

Consists of NE trending zone that extends for 200 m with width 4.0 m.Occurs within Carboniferous volcanic rock in the Keramay arc area (see Tang and others, 2010, fig. 1).Occurs within Carboniferous volcanic rock in the Keramay arc area (see Tang and others, 2010, fig. 1).Occurs within Carboniferous volcanic rock in the Keramay arc area (see Tang and others, 2010, fig. 1).Occurs within Carboniferous volcanic rock in the Keramay arc area (see Tang and others, 2010, fig. 1).Occurs within Carboniferous volcanic rock in the Keramay arc area (see Tang and others, 2010, fig. 1).Occurs within Carboniferous volcanic rock in the Keramay arc area (see Tang and others, 2010, fig. 1).Occurs within Carboniferous volcanic rock in the Keramay arc area (see Tang and others, 2010, fig. 1).Overlay of Ordovician volcano-sedimentary units proximal to Silurian volcano-sedimentary units. Occurs within Carboniferous volcanic rock in the Keramay arc area (see Tang and others, 2010, fig. 1).Source of prospect indicates that it may be Cu-Mo subtype.Designated as a porphyry Cu by Nokleberg and others (1999); as a Granitoid related stockwork/ metasomatite Cu by Dejidmaa and others 2002.Consists of quartz vein trending NW for 40m with width 0.8 to 1.2 m.Designated as a porphyry Cu-Mo by Nokleberg and others (1999); as a Granitoid related stockwork/ metasomatite Cu by Dejidmaa and others 2002.According to Nokleberg and others (1999), this unnamed occurrence is designated a porphyry copper occurrence by Ts. Gotovsuren, of the Monrud Company, Mineral Exploration and Mining Company, Ulaanbaatar, Mongolia. No other information available.Cu-Mo occurrence; some base metal mineralization.Source of prospect indicates that it may be Cu-Mo subtype.Source of prospect indicates that it may be Cu-Mo subtype.Orogenic porphyry-type sub-categories.Weakly copper anomalous zones occur further down hole, suggesting a surface enrichment.Became an Ivanhoe Mines/Inner Mongolia Bureau of Geology Cu-Au porphyry exploration project in 2005.Classified as porphyry Cu; no further information.One drill hole in geochemical anomaly.

Cu zone below Mo zone.Variscan, Yanshanian ages also.Singer and others (2008) deposit # 590 [Pulang] is ~ 3km from this deposit.Porphyry Cu - Mo (Ag, Re).Active prospect 2004–2011; limited information.Porphyry Cu - Mo (Ag, Re).Source of prospect indicates that it may be Cu-Mo subtype. Porphyry Cu, skarn-related.Probably a skarn deposit.Variscan, Yanshanian ages also.Porphyry Cu - Mo (Ag, Re).The Central Mongolian metallogenic belt is dominated by skarn and porphyry Cu deposits.Related to Si-rich granite. Associated with a fine-grained alkaline granite dike swarm.Combined Zos Uul & Zos Tolgoi.Copper oxide mineralization.Anomalous Cu concentrations throughout the area.The name of the deposit, Zuukhin gol, is from JICA-JOGMEC (2004).Discovered in 2002 by Harrods Minerals, at least 3 separate orebodies are present.Porphyry Cu - Mo (Ag, Re).Porphyry Cu - Mo (Ag, Re).

Comments2A.F. Chitlalin includes a location for Agaskyr at 54.9889 89.3428, which is located about 46 km N-NE. He also lists Agaskyrskoye at same location as this point.Deposit related to Calc-Alkaline and Alkaline Granitic Intrusions.Porphyry Mo(-Cu) associated with granite-granodiorite and leucogranite intrusions.Minerals dated: molybdenite, sericite.

Middle to LateCambrian intrution of granodiorite.Deposit related to Calc-Alkaline and Alkaline Granitic Intrusions.Deposit related to Calc-Alkaline and Alkaline Granitic Intrusions.New exploration in 2012 by Xanadu Mines Ltd.

Deposit related to Calc-Alkaline and Alkaline Granitic Intrusions.The belt is interpreted as forming along an overlapping active Carboniferous to Late Permian continental margin arc that was tectonically linked to a subduction zone on the margin of Mongol-Ohotsk Ocean.

New exploration in 2012 by Xanadu Mines Ltd.Deposit related to Calc-Alkaline and Alkaline Granitic Intrusions.Porphyry Mo (Ag,Re).

Deposit related to Calc-Alkaline and Alkaline Granitic Intrusions.Li and others (2007, 2008) suggest it's an orogenic copper deposit.Not explored as porphyry target.Hydrothermal alteration (potassic, phyllic, propylitic) is associated with both the main phase diorites and late diorite porphyry.

Might actually be a skarn or greisen.Deposit related to Calc-Alkaline and Alkaline Granitic Intrusions.Drilling in 2005.Ground magnetic and gradient survey (2005) show very strong NE-SW & NW-SE trending linear features which intersect strong aleration & associated Cu mineralization.2 drill holes encountered weak copper mineralization.

Deposit related to Calc-Alkaline and Alkaline Granitic Intrusions.Alteration zone is nearly oval, is 3 km wide and extends northeast for 5 km; ). The dominance of sericite, advanced argillic, silica alterations at the surface suggests a relatively shallow porphyry Cu system.

Might actually be a skarn or greisen.Initial drilling in 2005, with follow-up geophysical and geochemical surveys in 2006 and 2007.Deposit is exposed. Main ore-related intrusion is a porphyryitic tonalite that is the final representative of a suite of dioritic, quartz dioritic and tonalitic rocks.Associated with Bronze Fox intrusive complex, a weakly oxidized calc-alkaline I-type intrusive center; rocks range from granodiorite to monzonite.Deposit related to Calc-Alkaline and Alkaline Granitic Intrusions.

Related to lower Carboniferous subvolcanic dikes and stocks of Na-rich quartz-feldspar and feldspar porphyries. Classification unclear; could be epithermal.

Was an Ivanhoe target with anomalous Au chip samples in 2004.Three MRAM points have the mineral ID of 266, two are Porphyry Cu - Mo (Ag, Re) and one is granitoid related Au.

Deposit related to Calc-Alkaline and Alkaline Granitic Intrusions.

Mineralized area >3 km long.Middle to LateCambrian intrution of granodiorite and granite.Indosinian age from Hou and others (1991).Latest Permian to Early Triassic age interval Cu–Mo or Mo mineralization that has not been previously recognized (Zeng and others, 2011).

Drilling has confirmed that the stratigraphy and mineralisation dips south at 450 but there are also high-angle porphyry dykes that are altered and mineralised.

Deposit related to Calc-Alkaline and Alkaline Granitic Intrusions.Owner: Yunnan Geology and Mining CO. LTD; April 5, 2006 - Field programs were underway.Deposit related to Calc-Alkaline and Alkaline Granitic Intrusions.Deposit related to Calc-Alkaline and Alkaline Granitic Intrusions.Deposit related to Calc-Alkaline and Alkaline Granitic Intrusions.Deposit related to Calc-Alkaline and Alkaline Granitic Intrusions.Deposit related to Calc-Alkaline and Alkaline Granitic Intrusions.Deposit related to Calc-Alkaline and Alkaline Granitic Intrusions.

Some workers believe the deposit might be Jurassic in age, but a Re-Os date of about 506 Ma is provided by Zhao and others (1997).

Erdenet, a site known since prehistoric time, was recognized as a major copper deposit in 1941, intensively explored during the 1960s, and began production in 1978.Porphyry Cu - Mo (Ag, Re).

Source of prospect indicates that it may be Cu-Mo subtype.Possibly Dejidmaa and others (2002) mineral point #264, which is located is located approximately 16km N-NW of our location.

Granitoid related Au-Ag-Cu.High Sr/Y in intrusive rock.

New exploration in 2012 by Xanadu Mines Ltd.


Deposit related to Calc-Alkaline and Alkaline Granitic Intrusions.Deposit related to Calc-Alkaline and Alkaline Granitic Intrusions.

Danbolongwa Permit area (used as the location for Huangnan) is located in a region of As anomalies and is close to a Late Triassic diorite unit.

A weak zone of secondary enrichment slightly occurs, is 1-3 m thick, and consists of bornite, chalcocite, and covellite.

Previous small-scale mining.Porphyry Au-Cu (Ag,Re).Might actually be a skarn or greisen.Deposit related to Calc-Alkaline and Alkaline Granitic Intrusions.Deposit related to Calc-Alkaline and Alkaline Granitic Intrusions.Deposit related to Calc-Alkaline and Alkaline Granitic Intrusions.Deposit related to Calc-Alkaline and Alkaline Granitic Intrusions.According to Nokleberg and others (2003), Kharaat Uul is designated a Cu (±Fe, Au, Ag, Mo) skarn.The area is variably oxidized to a depth of several tens of meters. Cu-Au mineralization is developed as both quartz- and sulfide-rich stockworks.Deposit related to Calc-Alkaline and Alkaline Granitic Intrusions.

Deposit related to Calc-Alkaline and Alkaline Granitic Intrusions.Deposit related to Calc-Alkaline and Alkaline Granitic Intrusions.Deposit related to Calc-Alkaline and Alkaline Granitic Intrusions.Nokleberg and others (1999) indicates this occurrence is porphyry Cu-Mo, while W.J. Nokleberg (written commun., 2006) indicates Cu porphyry.Discovered 2005 by Asia Gold Resources, renewed drilling by Voyager Resources in 2011, 2012.Source of prospect indicates that it may be Cu-Mo subtype.Deposit related to Calc-Alkaline and Alkaline Granitic Intrusions.Deposit related to Calc-Alkaline and Alkaline Granitic Intrusions.Intercepts include 30 m at 1.4% Cu and 21.9g/t Ag from 68 m.

Might actually be a skarn or greisen.

Deposit related to Calc-Alkaline and Alkaline Granitic Intrusions.Upper Jurassic-Early Cretaceous andesite and basalt intruded by Early Cretaceous granite.Deposit minerals occur in veinlets, masses & disseminations in skarn. Molybdenite occurs in zones in silica-altered granitoid in quartz veinlets containing disseminated molybdenite, chalcopyrite and other sulfides.The quartz-sulfide stockwork is mainly developed in the hanging wall of the apophysis and is accompanied by an intense silicification that has led to the formation of monoquartz rocks.Deposit minerals occur in streaks and disseminations along with some quartz and quartz-carbonate veins also are noted. Content of Cu and Mo in deposits is irregular with the result that separate lenses of bodies formed. Occurrence.

Medium deposit size (Nokleberg and others, 2006).

The Seltmann and others (2009) Qyzyltau porphyry CuMo occurrence notes other minerals as Pb, Zn, Au, Bi; major ore minerals (chalco, bornite), minor ore minerals (moly, py, chalco, dig, cov, tenn, enar, sphal, gal, marc).

Deposit related to Calc-Alkaline and Alkaline Granitic Intrusions.Most mineralized rock is skarn.


Deposit related to Calc-Alkaline and Alkaline Granitic Intrusions.Evolving view: porphyry Cu-Mo lodes, to Porphyry Mo + skarn Cu (King Solomon Mines Ltd., 2009).Possibly an occurrence instead of a prospect.

Middle to LateCambrian intrution of diorite and Permian dyke of granosyenite porphyry.Acquired in 2007 from Xstrata Cu.Deposit related to Calc-Alkaline and Alkaline Granitic Intrusions.

Deposit related to Calc-Alkaline and Alkaline Granitic Intrusions.The thickness of the formation ranges up to 1055 m. Most of deposit consists of intrusive rock of the Telmen Complex.One prospect from Nokleberg and others (1999) was grouped with this significant prospect location. The original location called "Unnamed - Nokleberg (1999), [CAOB 1]" was ( 44.233333, 108.05).Deposit related to Calc-Alkaline and Alkaline Granitic Intrusions.Porphyry Cu (Au,Ag).

Open pit operation. Underground in development.Was Ivanhoe prospect in 2003, but no mention since.Same as Eastveiw digitized Dejidmaa and others (2002) MRAM # 188.Same as Eastveiw digitized Dejidmaa and others (2002) MRAM # 197.


Deposit related to Calc-Alkaline and Alkaline Granitic Intrusions.Deposit related to Calc-Alkaline and Alkaline Granitic Intrusions.

Zones of intensive breccia, epidote alteration, silica alteration, limonitization and weak Cu minerals. Cu minerals occur in sublongitudinal zone with a length of 5.0-6.0 km and width of approximately 2.0 km.

Deposit related to Calc-Alkaline and Alkaline Granitic Intrusions.Five km of trenching in a 3 km by 500 m mineralized zone .Strong IP anomaly and magnetic highs.Might actually be a skarn or greisen.High sulphidation style mineralization has partially telescoped on to underlying Cu-Au Porphyries, mineralizing intrusions are cross-cut by later biotite-granodiorites.

The sulfides occur around of amphibole grains, and in rare small nests and disseminations in quartz and quartz-feldspar veins in outer contact zone of some small stocks.An Ivanhoe prospect in 2001-2002; present status not known.Deposit related to Calc-Alkaline and Alkaline Granitic Intrusions.An IP anomaly occurs at the centre of the occurrence. Intensive pyrite alteration of andesite occurs at depth from 68.1 m to 115.7 m. Silica and pyrite-altered zone also shows lower resistivity anomaly.Deposit related to Calc-Alkaline and Alkaline Granitic Intrusions.The original grade and tonnage cited by Singer has been superseded.


Drilling encountered thick zones of argillic alteration and weak copper mineralization.Deposit related to Calc-Alkaline and Alkaline Granitic Intrusions.

lenticular ore body 200-700 m long, extends to 167 m depth.The belt is interpreted as forming along an overlapping active Carboniferous to Late Permian continental margin arc that was tectonically linked to a subduction zone on the margin of Mongol-Ohotsk Ocean.

Dropped in 2007.Liu and others (2010d) indicate that Sawuer is a region and that three deposits are included in this region (Hanzheganeng, Taketakuolasi, Xiyakesitao).In 2006, judged to be largely structurally controlled and dropped.Cu tonnage is calculated from Cu grade and ore tonnage.Andalusite in alteration assemblage implies deep exhumation.Deposit related to Calc-Alkaline and Alkaline Granitic Intrusions.Deposit related to Calc-Alkaline and Alkaline Granitic Intrusions.


Dropped in 2006.100m, 0.2-0.5m wide.

Cu-bearing tourmaline breccias are common. Area was explored by Czech-Mongolian expedition in 1980s and became an Ivanhoe prospect in 2002.Porphyry Cu (Au, Ag).

Silicification and propylitic alteration.Cu and Mo grades from Berzina & others (2005, tables 1 &3); Tonnage (Mt) calculated using 550Kt mid-value between 500-600Kt (table 1) with grade of 0.17% (table 3); Au and Ag grades from Sotnikov & others (2001).

Based upon proximity to Lower Cretaceous map units labeled "dacite, rhyolite, quartz porphyry", might actually be younger in age.Deposit related to Calc-Alkaline and Alkaline Granitic Intrusions.


Possibly an occurrence instead of a prospect.

Deposit related to Calc-Alkaline and Alkaline Granitic Intrusions.Sericite, chlorite, and clay alteration.The belt is interpreted as forming along an overlapping active Carboniferous to Late Permian continental margin arc that was tectonically linked to a subduction zone on the margin of Mongol-Ohotsk Ocean.

Deposit is hosted in Middle and Late Cambrian granodiorite plutons intruding Neoproterozoic basement.Deposit related to Calc-Alkaline and Alkaline Granitic Intrusions.Deposit related to a granodiorite intrusion with a central porphyritic zone dated at 311-283.1 Ma (Nokleberg and others, 2003). May include skarn.A 2004 Ivanhoe Mines investor inforamtion release uses different property names for this area. The names and locations of new owners Kincora Copper Ltd. are used here, but includes some geologic information from the 2004 Ivanhoe document.Mentioned in JICA-JOGMEC (2004), and the point was moved about 13 km NW of the MRAM point.

Dropped in 2007.

Three prospects from Nokleberg and others (1999) were grouped into this deposit location, the original locations were: Baruun Kheseg (43.866667, 108.316667), Kheseg 2 (43.849999 108.333332), Kheseg 4 (43.849999 108.3).A total of 14 DDH, probably mostly in 2003-2004 by UGL.

Porphyry Cu (Au,Ag).Deposit related to Calc-Alkaline and Alkaline Granitic Intrusions.Deposit related to Subaerial Extrusive Rocks and Dyke Complexes.

Consists of hydrothermal quartz-tourmaline zone trending NW for 200 m with width 0.6 to 4.0 m. minor limonite and hematite.Detailed trenching over area of argillically altered volcanics and intrusions.Main ore body 1400 m long and 30 to 100 m wide, but extends more than 500m deep.Dike-like outcrops visible to the S and SE of the point location.

Middle to Late Triassic andesite tuff intruded by Late Triassic monzodiorite.Deposit related to Calc-Alkaline and Alkaline Granitic Intrusions.Deposit related to Calc-Alkaline and Alkaline Granitic Intrusions.Permian Khanbogd pluton appears to hornfels (gar, cpx, act, ep, chl, pyrrh) and cut off prospect at depth.

Porphyry & Granitic Pluton-hosted Deposit.Deposit related to Calc-Alkaline and Alkaline Granitic Intrusions.

Lower Mesozoic granite, Late Paleozoic granosyenite.Proximal to Late Carboniferous adakitic and high-Mg diorite–granodiorite porphyry plutons (A-type) and dikes known for Cu–Au mineralization in the Baogutu area of the western Junggar region (see Tang and others, 2010, fig. 1).Proximal to Late Carboniferous adakitic and high-Mg diorite–granodiorite porphyry plutons (A-type) and dikes known for Cu–Au mineralization in the Baogutu area of the western Junggar region (see Tang and others, 2010, fig. 1).Proximal to Late Carboniferous adakitic and high-Mg diorite–granodiorite porphyry plutons (A-type) and dikes known for Cu–Au mineralization in the Baogutu area of the western Junggar region (see Tang and others, 2010, fig. 1).Proximal to Late Carboniferous adakitic and high-Mg diorite–granodiorite porphyry plutons (A-type) and dikes known for Cu–Au mineralization in the Baogutu area of the western Junggar region (see Tang and others, 2010, fig. 1).Proximal to Late Carboniferous adakitic and high-Mg diorite–granodiorite porphyry plutons (A-type) and dikes known for Cu–Au mineralization in the Baogutu area of the western Junggar region (see Tang and others, 2010, fig. 1).Proximal to Late Carboniferous adakitic and high-Mg diorite–granodiorite porphyry plutons (A-type) and dikes known for Cu–Au mineralization in the Baogutu area of the western Junggar region (see Tang and others, 2010, fig. 1).Proximal to Late Carboniferous adakitic and high-Mg diorite–granodiorite porphyry plutons (A-type) and dikes known for Cu–Au mineralization in the Baogutu area of the western Junggar region (see Tang and others, 2010, fig. 1).Proximal to Late Carboniferous adakitic and high-Mg diorite–granodiorite porphyry plutons (A-type) and dikes known for Cu–Au mineralization in the Baogutu area of the western Junggar region (see Tang and others, 2010, fig. 1).Porphyry Cu (Au, Ag).Might actually be a skarn or greisen.

Might actually be a skarn or greisen.

One prospect was grouped with this prospect. The original location of Kheseg uul was (49.2417, 113.5206).Porphyry Cu - Mo (Ag, Re).

East Junggar system basin Paleozoic convergent arec, the wave shell transition [translation?], carboniferous calc-alkaline construction of shallow intrusive rocks, lens, vein orebodies, 20-250m long, 5-30m thick.

Drill pads, trenches, and exploration workings visible.

resistivity anomalies at depth.


Deposit related to Calc-Alkaline and Alkaline Granitic Intrusions.Porphyry Cu, skarn-related.

Deposit related to Calc-Alkaline and Alkaline Granitic Intrusions.The belt is interpreted as forming along an overlapping active Carboniferous to Late Permian continental margin arc that was tectonically linked to a subduction zone on the margin of Mongol-Ohotsk Ocean.

Consists of Late Permian and Early Triassic granitoids that intrude Paleoproterozoic metamorphic rock, Paleoproterozoic granite, Cambrian gabbro, granodiorite and granite and Early Devonian volcanic rock & Permian granosyenite & granite.Drilling in 2005; exploration license 4519x.Western, eastern and southern margins of the granite porphyry stock.Stockwork is 2.0 km by 2.2 km.Total of 128 drill holes, 2003–2011.Deposit related to Calc-Alkaline and Alkaline Granitic Intrusions.Deposit related to Calc-Alkaline and Alkaline Granitic Intrusions.

Comments3Classified as porphyry Mo by Rundkvist (2001), Kirkham and Dunne (2000), and Volkov and others (2006), but based upon data from SMR (2011), probable Mo-Cu deposit subtype.Porphyry and Granitic Pluton-hosted Deposit.Gangue minerals are quartz, feldspar, sericite, and carbonate.Singer and others (2008) reports 515 Ma (518±2 – 511±2; Re-Os), and 368±1 – 362±8 (Ar-Ar). Age is transitional between Silurian and Devonian (Caledonian and Variscan).

Porphyry & Granitic Pluton-hosted Deposit.Porphyry and Granitic Pluton-hosted Deposit.

Porphyry and Granitic Pluton-hosted Deposit.

Porphyry and Granitic Pluton-hosted Deposit.Deposits related to Calc-Alkaline and Alkaline Granitic Intrusions.


Porphyry and Granitic Pluton-hosted Deposit.Location is approximately 30+ km NW of the Asia Gold & BHP Billiton JV property, according to a map from the 23rd IAGS Symposium, Peréz (2007).Two target areas of co-incident silification, sericite/pyrite alteration & elevated Cu in soil & chargeablitiy outlined.

Porphyry and Granitic Pluton-hosted Deposit.The deposit consists of stockwork veinlets and veins of quartz, pyrite, chalcopyrite, and molybdenite that occur in or near porphyritic intrusions. High-level intrusive porphyry is contemporaneous with abundant dikes, faults, and breccia pipes.

Mineralized centers include Nergui, Biger 1, Biger 2, Biger 3, Biger 4, and Biger 5.

Mineralization is sheeted quartz-chalcopyrite (±arsenopyrite) veins.At least 48 holes (both RC and core) have been drilled on the property.Porphyry & Granitic Pluton-hosted Deposit.

Mineralized zone is elongated, fault controlled.; Veinlet and stockwork mineralization predominated over pervasive disseminations.



Porphyry and Granitic Pluton-hosted Deposit.Porphyry & Granitic Pluton-hosted Deposit.Porphyry and Granitic Pluton-hosted Deposit.Porphyry and Granitic Pluton-hosted Deposit.Porphyry & Granitic Pluton-hosted Deposit.Porphyry and Granitic Pluton-hosted Deposit.

Elongate (NW-SE) mineralized zone in Selenge Intrusive Complex.Deposit related to Calc-Alkaline and Alkaline Granitic Intrusions.

Deposits related to Subaerial Extrusive Rocks and Dyke Complexes.

Duoba-Jijiemu Permit area includes Yanshanian age granodiorite units, indicating that Huangnan might be younger (Jurassic-Cretaceous), thus included as part of the Mesozoic East Asia Porphyry Copper Assessment (Ludington and others, 2010).

Porphyry & Granitic Pluton-hosted Deposit.

Porphyry and Granitic Pluton-hosted Deposit.Porphyry & Granitic Pluton-hosted Deposit.

Associated with bimodal (basalt-rhyolite) assemblage rocks.

Deposits related to Calc-Alkaline and Alkaline Granitic Intrusions.

Porphyry and Granitic Pluton-hosted Deposit.Porphyry & Granitic Pluton-hosted Deposit.Porphyry and Granitic Pluton-hosted Deposit.Porphyry and Granitic Pluton-hosted Deposit.According to Nokleberg (2003), Kharaat Uul is a small deposit; age is noted as Pt [Proterozoic].Deposit features mineralized tourmaline breccias.Granitoid Related vein, stockwork, metasomatic Deposit.

Porphyry and Granitic Pluton-hosted Deposit.Skarn Deposit.Porphyry & Granitic Pluton-hosted Deposit.Deposit related to Calc-Alkaline and Alkaline Granitic Intrusions.

Porphyry and Granitic Pluton-hosted Deposit.Porphyry and Granitic Pluton-hosted Deposit.Aranjin prospect (43.9843, 98.3520): comprises 4 large outcrops of quartz tourmaline breccia; rock chip sampling has returned up to 2% copper; 29 reverse circulation holes, 3 diamond holes and 3 diamond core tailed reverse circulation holes completed.


Deposit has been mined and is small.Three orebodies: Northern, Bolshaya and Southern, all located in one mineralized zone 80-120 m.Source of prospect indicates that it may be Cu-Mo subtype. Host rock is altered to silica, sericite, pyritie, carbonate and locally to barite.

Stockwork and vein deposit minerals occur in strong-altered host rock with sericite, silica and chlorite.

The oxidated ores consist from malachite, azurite, chalcocite. Rock wall alteration: Feldsphatization, albitization, biotitization, beresitization.






Was an Ivanhoe target with anomalous Au chip samples in 2004.Granitoid Related vein, stockwork, metasomatic Deposit.Deposit related to Calc-Alkaline and Alkaline Granitic Intrusions.

Early stage porphyry-style mineralization is predominantly composed of disseminations and stockworks (Seltmann and Porter, 2005).


Porphyry and Granitic Pluton-hosted Deposit.Porphyry & Granitic Pluton-hosted Deposit.

Three quartz-rich bodies, up to 10 m by 50 m, have weak chalcopyrite disseminations and malachite and azurite coatings.

Porphyry and Granitic Pluton-hosted Deposit.Deposit Ovotiin Khar located approximately 4 km SE, unclear if they are the same occurrence.Deposit Ovoot Hyar located approximately 4 km NW, unclear if they are the same occurrence.Discovered by D. P. Cox, USGS emeritus.

See Nokleberg and others (2003) for additonal information.Two prospects were grouped with this significant prospect. The original location for these prospects were: Khuuchin (44.583, 109.466) and Zuun Umnut (44.569, 109.502).Porphyry and Granitic Pluton-hosted Deposit.

Porphyry and Granitic Pluton-hosted Deposit.Singer grade and tonnage is superseeded from new information.

Deposit extends 2.0 km on surface and is approximately 200 m wide. There are nine areas of dissemination and stringers of Cu minerals .



W.J. Nokleberg (written commun., 2006) indicates this site as a Por Cu with Pb, Zn. Nokleberg and others (1999) indicates this site as Zn with Pb, Cu - Polymetallic vein.

The Sawuer region has many syngenetic and epigenetic metallic ore deposits, including porphyry Cu, epithermal and orogenic Au.

New exploration in 2012 by Xanadu Mines Ltd.Porphyry and Granitic Pluton-hosted Deposit.Porphyry and Granitic Pluton-hosted Deposit.


Mineralization.

Geochemisty of igneous rocks, including Sr/Y ratios, indicates an 'adakitic' composition, favorable for porphyry Cu mineralization.Deposit related to Subaerial Extrusive Rocks and Dyke Complexes.

Dominant type of alteration: Potassic, albitic; hydrothermal alterations (K-feldspathization, albitization, sericitization).



Porphyry and Granitic Pluton-hosted Deposit.Dropped in 2007.

Porphyry and Granitic Pluton-hosted Deposit.Deposit is 4 km SE of the Duobaoshan porphyry Cu deposit and is in the same district as the Duobaoshan deposit.The Southwest target [also known as Southwest] is located 44.040248N, 107.680396E, indicated by Ivanhoe based on soil geochemistry.

Approximately 47 km E-NE of this location (48.641336, 105.221487) is a cluster of granitoid related Au occurrences and deposits called Tsagaan gozgor (Dejidmaa and others (2002), Nokleberg and others (1999).

Advanced argillic alteration, with the occurrence of chalcopyrite, is prevalent throughout the property.

Deposit related to Calc-Alkaline and Alkaline Granitic Intrusions.Porphyry and Granitic Pluton-hosted Deposit.Porphyry and Granitic Pluton-hosted Deposit.

Porphyry and Granitic Pluton-hosted Deposit.Porphyry and Granitic Pluton-hosted Deposit.

Source of prospect indicates that it may be Cu-Mo subtype.Porphyry and Granitic Pluton-hosted Deposit.

Because of spatial association with Ordivician volcano-sedimentary rocks, might be Ordivician in age.Deposits related to Subaerial Extrusive Rocks and Dyke Complexes.Granitoid related stockwork, viens, metasomatite Cu; Deposits related to Calc-Alkaline and Alkaline Granitic Intrusions (Dejidmaa and others, 2002).

Kheseg uul designated as Cu-Mo porphyry occurrence by W.J. Nokleberg (written commun., 2006), but classified as a Pb-Zn-Cu polymetallic vein by Dejidmaa and others (2002). Possibily porphyry related?.Deposit related to Calc-Alkaline and Alkaline Granitic Intrusions.

Small.




Also occurring is extensive hydrothermal alteration with quartz-sericite and quartz replacements in bodies ranging up to 20 m by 40 m.Location is approximately 30+ km W of the Asia Gold & BHP Billiton JV property, according to a map from the 23rd IAGS Symposium, Peréz (2007).The porphyry stock and dikes and host rocks are intensively altered to silica, sericite, and pyrite. The size of the stockwork is 2.0 by 2.2 km.

Additional targets to the north and west have been identified, including Khuvyn Khar indicating at 34 m., 1.34% Cu and 9 g/t Ag from Erdene Resource Development Corp. (2013).Porphyry and Granitic Pluton-hosted Deposit.Porphyry and Granitic Pluton-hosted Deposit.

Comments4Same location with various names [Agaskyrskoe, Agaskyrskoye] from Seltmann and others (2009) and Rundkvist (2001).

Consists of a Cu-Mo stockwork hosted in Proterozoic schist and gneiss intruded by a Paleozoic granitoid stock. The host rocks are altered to K-feldspar, silica, and sericite.A.F. Chitalin (written commun., 2009) indicates probable reserves of 4.2 Mt Cu (0.5%), 115 tt Mo (0.15%); inferred reserves of 6.2 Mt Cu, 115 tt Mo, 93 t Au (0.2%). Prefeasibility study considered by OOO Golevskaya GRK.

Porphyry & Granitic Pluton-hosted Deposits.

Mineral site location possibly incorrect. This location is 0.5 km from Zargyn Khar Ovoo which is included in Dejidmaa and others (2002) as MRAM #18 and Nokleberg and others (1999).target areas in the NE-SW trending structure in the grantie porphyry in SW Central are & in felsic volcanics in the W central area.

See Nokleberg and others (2003) for additonal information.

Beger 2 - Ore body consists of alteration (choloritization, epditization, hematitization) zone up to 1500 m long with width 200-300 m. Beger 4 - Ore body is the shlieren arc-like forms 20-30m long, with width 0.5-4.0 m.

Southeast Target is located ~6 km SE of the main cluster of Bronze Fox targets (Sophie North, West Kasulu, Buchanan Heights, Dunlop Fox, Leca Pass) at 44.0394 N, 107.9365 E.

Syn-mineralization propylitic and quartz-sericite alteration.

Igneous rocks are calc-alkaline, I-type, magnetite series, medium to high K, and enriched in LIL, depleted in Nb, Ta, and Ti.Porphyry and Granitic Pluton-hosted Deposit.

Granitoid Related vein, stockwork, metasomatic Deposits.

Nokleberg (2010) classifies it as a porphyry, while Petrov and others (2009) indicates it is a VMS.

Porphyry and Granitic Pluton-hosted Deposits.

Porphyry & Granitic Pluton-hosted Deposit.

Cughur prospect (43.9776, 98.3458): fault-repeat mineralization to NE; 50 m at 0.82% Cu and 1.87g/t Ag from 6 m, within 200 m of core mineralization; 41 reverse circulation, 12 diamond core and 16 diamond core tailed reverse circulation holes completed.

Singer and others (2008) locate this deposit 35 km SW and could be the location of the porphyry Mo Nichkuryupskoye occurrence.

Deposit in an inner contact zone in a stock of Devonian granite porphyry and Late Cambrian volcanic-sedimentary host rock.

A typical feature of the deposit is the large number of subparallel, vein-like bodies with different thickness several meters to 140 m, while their length averages 600 m along the strike and around 500 m down dip.


Late stage mineralization localized in the core of the earlier monzonite intrusive and porphyry mineralization. Mineable high grade ore has been delineated to a depths of 1400 m (Seltmann and Porter, 2005).

Occurrence, W.J. Nokleberg (written commun., 2006), See Nokleberg and others (2003) for additonal information.

Middle Cambrian gabbro and hornblendite stocks intrude Paleoproterozoic gneiss, schist and amphibolite.

The fault weak zone includes the Naranbulag occurrence [25 km SW] and other Cu minerals occurring N of the latter and explosive bodies. .

Blight and others (2010) (U-Pb, 325.5 +/- 1 Ma), Batkhishig and others (2010) (Rb-Sr, 321 +/- 9 Ma).Porphyry and Granitic Pluton-hosted Deposit.

This deposit is boarder-line Caledonian-Variscan, but is surrounded by predominately Caledonian rocks, therefore assigned to Caledonian tract; 40Ar/39Ar dating has shown the age of the porphyries to be 405 to 388 Ma.

Three major ore bodies in the Tongshan deposit were discovered in the mineralized zone. Sulfides occur as disseminated grains and veins. Intensely zoned alteration.


Porphyry & Granitic Pluton-hosted Deposits.


Quartz-sulfide vein and stockwork occur in altered rock, particularly in the western, eastern and southern margins of the granite porphyry stock.Mineral site location possibly incorrect.

Comments5

A hydrothermal alteration zone contains some intensely brecciated and silicified areas.

Zargyn Khar Ovoo is variably referred to a porphyry Cu (Dejidmaa and others, 2002) and replacement Cu (Nokleberg and others (1999).

Hosted in a Jurassic volcanic-plutonic system that includes small porphyritic intrusions of diorite to granite from Nokleberg and others (2003).

Beger 5 - Ore body consist of siliceous alteration (sericitization, potassium feldspathization) zone up to 25 m long with width 2,0 m.

There is an additonal target 20 to 25 km to the N-NE called North Fox which is also being investigated (no additional information available).

Host rock age is D2-C1, from Laznicka (1976).

Deposits have been variously classified as: Erdenet, Cu, Mo; Erdenet Central, Cu; Erdenet SE (Oyut), Cu, Mo ; Tourmaline, Cu.

W.J. Nokleberg (written commun., 2006) location of ~ 105° is likely a typo per Nokleberg and others (1999).

Exploration targets of between 50-150 million tons at 0.8-1.5% Cu in hydrothermal breccias (not including larger copper porphyry stock targets). Tourmaline breccia with Cu mineralization; Mineralization over 4km of strike length; Large IP anomaly.

Deposit in Kuznetsk Alatay granitoid area.

The orebodies strike northwesterly and dip southerly at 50-60 . They occur mostly as plate-like or lens-shaped stockwork.

Early stage porphyry-style Cu mineralization associated with monzonite, followed by late stage overprinting of high grade, high sulfidation Cu-Au mineralization associated with diorite porphyry and numerous breccia pipes (Seltmann and Porter, 2005).

Host volcanic rock is altered to sericite, kaolinite and local intense silica.

See Nokleberg and others (2003) for additonal information.

Alternate location (43.949812, 107.643657) is in the center of a region which appears to show wide trenching E, W, and S., and a drill pad SW of the point; also Singer and others (2008) approximately 27 km NW of point: 44.166667, 107.5.

The size of the stockwork is 2.0 km by 2.2 km.

loc_comLocaton is from Nokleberg and others (2003); other locations are variable, up to 60 km difference within the cluster.Did not see better location in google earth.Location based on the cluster of points from Nokleberg and others (1999, 2003,2006) and A.F. Chitalin, wirtten commun. (2009). Alternate location from Rundkvist (2001) at: 54.762555 96.352942.Location is based on a map provided by A.F. Chitalin, written commun., 2009.Accurate location.Did not see a better location in google earth.Nokleberg and others (1999) and Dejidmaa and others (2002) point located about 9.5 km SE of this one; moved, using Google Earth Imagery to large area of dark rock.Moved ~2.5km NW to an area that appears altered.Location approximate; based on map in Xanadu Mines Ltd. (2012b) press release.Location based on A.F. Chitalin, wirtten commun. (2009).Similar name as Arbulag, but very diferent location; Did not see better location in google earth.Similar name as Ar bulag, No 269, but very different location; Did not see better location in google earth.Location from Fig. 13 in Hou and others (2007).Location approximate; based on map in Xanadau press release.Did not see better location in google earth.Did not see better location in google earth, large area of disturbance from point to ~ 7 km to the east through the south east.Location from Zeng and others (2009).Did not see better location in google earth, large are of small pit impressions.Location from Google Earth Imagery, disturbed ground that best fits Jian and others (2007) maps and descriptions.Location from Google Earth Imagery, extensive workings visible. Appears to be underground or surface mining, No open pit.Accurate location.Did not see better location in google earth.Did not see better location in google earth.Did not see better location in google earth.Location is uncertain.Accurate location.Accurate location.Very approximate location.Did not see better location in google earth.Did not see better location in google earth.Accurate location.Did not see better location in google earth.Location is the center prospect (Beger 4) of NW-SE-trending string of 5 prospects, roughly on-trend with the Mogoinshand prospect to the east. Nergui: 45.5999N, 97.2999E; Beger 1: 45.6167N 97.2E; Beger 2: 45.5999N 97.2917E; Beger 5: 45.6167N, 97.1833E.Not sure of location; point placed at center of industrial development, but drill roads not obvious.Altered area is visible.Did not see better location in google earth.Did not see better location in google earth.Did not see better location in google earth.Seltmann and others (2009) location, moved approximately 0.5 km SE, Roads, drill pads, and exploration (mining?) workings visible.very general location digitized from a figure from a 2012 presentation from Gobi KhurakhLLC website.Accurate location.Location in visible altered area.Did not see better location in google earth, Alternate loction 48.866667, 102.816667 from Dejidmaa and others (2002).Did not see better location in google earth.

Did not see better location in google earth.Location Accurate, from Liu and others (2007).Location approximate.Did not see better location in google earth.Location approximate.Accurate location.Accurate location.Accurate location.Did not see better location in google earth.Location from Fig. 13 in Hou and others (2007).Location derived from Midas Resources Limited (2008) map.Accurate location.Moved ~3km SE to an area that appears altered.Location derived from map at Jinshan Gold Mines (2008); location rough.Moved, using Google Earth Imagery - .8km north-northwest of point.Did not see better location in google earth.Moved, using Google Earth Imagery - .5km south-southwest of point.Moved, using Google Earth Imagery to distrubed area.Did not see better location in google earth.Location based on Dejidmaa and others (2002).Location approximate.Did not see better location in google earth, area shows what appears to be long trenching (?) cross linear dike (?) outcroppings.Did not see better location in google earth.Location from Ge and others (2007); adjusted to more Accurate position using Google Earth imagery.Accurate location.Accurate location; point moved to center of the pit using Google Earth imagery.Did not see better location in google earth.Did not see better location in google earth.Location approximate.Approximate location.Did not see better location in google earth.Moved, using Google Earth Imagery to copper coloured disturbed area.Accurate location.Based on Nokleberg and others (1999) location.Did not see better location in google earth.Accurate location.Location from Fig. 13 in Hou and others (2007).The location is within the Danbolongwa Permit area, which is close to a Late Indosinian (Late Triassic) age diorite; The Duoba-Jijiemu Permit area is about 20 km SW of this location and is associated with Jurassic-Cretaceous age granodiorites.Location is one of the several copper occurrences within the Hutag Uul property; based on map in Xanadau Mines Ltd. (2012b).Did not see better location in google earth.Did not see better location in google earth.Location based on Nokleberg and others (1999), alternate locations: 49.219077, 104.016836 from Dejidmaa and others (2002); 49.225, 104.022222 from W.J. Nokleberg (written commun., 2006); most likely close to this cluster of three points.Accurate location.Did not see better location in google earth, centered in an area of ground disturbances.Did not see better location in google earth.

Accurate location.Location approximate.Did not see better location in google earth.Open pit visible on Google Earth.Location approximate.Accurate location.Did not see better location in google earth.Did not see better location in google earth.Location in visible altered area.Did not see better location in google earth.Did not see better location in google earth.Moved, using Google Earth Imagery to disturbed area near the road.Did not see better location in google earth, cluster of points.Accurate location, centered on a grid of drill roads and pads.Did not see better location in google earth.Generalized location.Location is based on Nokleberg and others (1999).Did not see better location in google earth.Did not see better location in google earth.Nokleberg and others (1999) and Dejidmaa and others (2002) location.Accurate location.Did not see better location in google earth.Location is based on W.J. Nokleberg (written commun., 2006).Moved, using Google Earth Imagery - 2.7 km east-northeast of point.Location based on a map from Voyager Resources (2012), it is the approximate center of the cluster of prospects (all the prospects are no more than 1.5 km away from this center point).Did not see better location in google earth.Did not see better location in google earth.Did not see better location in google earth.Nokleberg and others (1999) location used; alternative location from Dejidmass and others (2002): 48.746, 102.0647.Location based on Nokleberg and others (1999).Location is Accurate and mid point between Nokleberg and other (1999) and Rundkvist (2001), located in the Tuim hole of the old Keyalykh-Uzen mine.Location from Singer and others (2008); alternative Location from Rundkvist (2001) 50.07655, 76.159014.Location based on disturbed area in Google Earth, alternative locations from A.F. Chitalin, written commun. (2009): Kublich, 51.683333, 86.766667 & Kulbichskoe, 51.7, 86.75; Rundkvist (2001): 51.73895, 86.827801.Accurate location.Did not see better location in google earth.Location is in the approximate center of an area with pervasive alteration and limonite.Location from Singer and others (2008); alternative Location from Seltmann and others (2009) 51.868109, 72.526932.Generalized, but accurate location.Location is based on W.J. Nokleberg (written commun., 2006).Accurate location.Location from Li and others (2011).Location approximate.Location from Fig. 13 in Hou and others (2007).Location approximate.Accurate location.

Location approximate.Did not see better location in google earth.Generalized location based on Erdene Gold Inc. (2004).Did not see better location in google earth.Accurate location.Location based on A.F. Chitalin, written commun. (2009).Accurate location.Generalized location based on Erdene Gold Inc. (2004).Location approximate; based on map in Xanadu Mines Ltd. (2011b).Did not see better location in google earth.Generalized location based on Erdene Gold Inc. (2004).Did not see better location in google earth.Did not see better location in google earth, not a likely location though.Location based on W.J. Nokleberg (written commun., 2006).Moved, using Google Earth Imagery, record # 335 = 336 ???; 25 km NE of Naranbulag, which has something showing on Google Earth.Moved, using Google Earth Imagery - to nearest ground disturbance.Did not see better location in google earth, in the area of much mining activity [20 km long, 15 km wide].Did not see better location in google earth, area of some activity, especially north.Did not see better location in google earth.Did not see better location in google earth.Looks like a good location in google earth.Did not see better location in google earth.Moved to W.J. Nokleberg (written commun., 2006) location.Did not see better location in google earth.Did not see better location in google earth.Did not see better location in google earth, ground disturbance to north and west.Did not see better location in google earth.Did not see better location in google earth.Location is based on W.J. Nokleberg (written commun., 2006).Did not see better location in google earth.Location from Nokleberg and others (2006).Location from Li and others (2011).Did not see better location in google earth.Accurate location.Did not see better location in google earth.Moved to central location along deposit trend as determined from Ivanhoe reports and Google Earth Imagery.Location from W.J. Nokleberg. (written commun., 2006).VERY approximate location; is 320 km SW of UB, and is 10 km ESE of UGL's 'Boro Ovoo' which is also unlocated.Did not see better location in google earth.Accurate location.Did not see better location in google earth, several diggings in ridge to east and just downslope of point.Did not see better location in google earth.Did not see better location in google earth, several disturbed areas.Singer location is about 14 km west of this location [3 km from the Xuejiping deposit]. Accurate location.Location from Li and others (2011).

Did not see a better location in google earth.Did not see better location in google earth.Did not see a better location in google earth.Accurate location.Accurate location.Did not see better location in google earth.Accurate location.Accurate location.Did not see better location in google earth.Accurate location, centered on a grid of drill roads and pads.Location in based on Nokleberg and others (1999, 2003), alternative Location: 46.05, 96.45 from Dejidmaa and others (2002).very approximate location.Accurate location.Did not see better location in google earth.Accurate location.Moved, using Google Earth Imagery to disturbed area.Did not see better location in google earth.Moved, using Google Earth Imagery to disturbed area.Did not see better location in google earth.Accurate location.Location base on Dejidmaa and others (2002).Location is approximate, digitized Location from Dequan and others (2005) moved out of glacier area to a rock formation obvious in google earth, no infomormation.Generalized location based on Erdene Gold Inc. (2004).Accurate location; relocated based on map figures in Batkhishig and others (2010) and Bignall and others (2005). Note that the lower latitude on Batkhishig, figure 2 should be 43° 53' 15", not 44° 53' 15".Possible drill roads and trenching visible on Google Earth.Location approximate.Very poor location.Good location.Generalized location based on Erdene Gold Inc. (2004).Very general location: near Choibalsan, but otherwise, no information, point located in an area that has linear ground disturbance, however, much of the area around the town shows mining activity.Did not see better location in google earth.Accurate location.Did not see better location in google earth.Accurate location.Location based on A.F. Chitalim, written commu. (2009). Alternate location from Rundkvist (2001) 54.04640, 123.658031 about 12 km to the S\SW of this location.Accurate location.Did not see better location in google earth.Location is approximate, located within .5 km of Dejidmaa and others (2002) location: 49.529587, 105.227516.Did not see better location in google earth.Location approximate.Did not see better location in google earth.Did not see better location in google earth, many small pits to west.Location from Zeng and others (2009).Accurate location; target location based on soil geochemistry.Moved to drilled area as per Google Earth Imagery and JICA-JOGMEC (2004) report.

Very approximate location.Generalized location.Location Accurate, derived from Mongolyn Alt (MAK) Group (2012).Accurate location.Did not see better location in google earth.Did not see better location in google earth.Did not see better location in google earth.Did not see better location in google earth.Location approximate.Did not see better location in google earth, in a large area of disturbance.Generalized location based on Erdene Gold Inc. (2004).Generalized, but accurate location.Did not see better location in google earth; See also Ukhaa Khudag located at N44.033332 and E106.200000 (nothing visible).Generalized location based on Erdene Gold Inc. (2004).Generalized location based on Erdene Gold Inc. (2004).Moved, using Google Earth Imagery onto road and what appears to be 3 pits.Did not see better location in google earth.Did not see better location in google earth.Position estimated on Google Earth Imagery from maps in primary references, no evidence on ground.Did not see better location in google earth.Did not see better location in google earth.Did not see better location in google earth.Moved, using Google Earth Imagery.Did not see better location in google earth, in a large area of disturbance.Digitized from Tang and others (2010) map, identified as "Unknown exploration".Digitized from Tang and others (2010) map, identified as "Unknown exploration".Digitized from Tang and others (2010) map, identified as "Unknown exploration".Digitized from Tang and others (2010) map, identified as "Unknown exploration".Digitized from Tang and others (2010) map, identified as "Unknown exploration".Digitized from Tang and others (2010) map, identified as "Unknown exploration".Digitized from Tang and others (2010) map, identified as "Unknown exploration".Digitized from Tang and others (2010) map, identified as "Unknown exploration".Location based on Nokleberg and others (1999): alternate Location: 106.506386, 43.422844 (Dejidmaa and others, 2002), not obvious in Google Earth.Did not see better location in google earth.Did not see better location in google earth.Did not see better location in google earth, activity 10 km north-northeast and 16 km northeast.Did not see better location in google earth.Moved slightly SW to altered, disturbed area using Google Earth.Did not see better location in google earth.Location approximate.Approximate location, moved from the origianl digitized Dequan and others (2005) point.Approximate location.Accurate location, based on exploration workings visible.Location from Zeng and others (2009).Location approximate.

Accurate location.Accurate location.Accurate location.Did not see better location in google earth.Location approximate.Did not see better location in google earth.Location approximate.Location approximate.Accurate location.Did not see better location in google earth.Did not see better location in google earth.Location approximate.Moved, using Google Earth Imagery to disturbed area northeast of point; nothing visible on Google Earth at this location but airstrip nearby.Location is uncertain, point is based on Bayan Goya which is documented to be located 30 km north of Zuraumtai.Did not see better location in google earth.Moved to drill pads, location described in JICA-JOGMEC (2004) report.Accurate location.Did not see better location in google earth.Did not see better location in google earth.

arc_type tect_featunknown unknownIsland Arc? Tuva-Mongol Arc?unknown unknown (Agulsk metallogenic belt)Island Arc Tuva-Mongol ArcIsland Arc Kazakh-Mongol ArcContinental Arc Orkhon-Selenge ArcIsland Arc Kazakh-Mongol ArcContinental Arc Orkhon-Selenge ArcIsland Arc Kazakh-Mongol arcunknown unknownContinental Arc Orkhon-Selenge ArcContinental Arc Orkhon-Selenge ArcIsland Arc Yidun Island ArcIsland Arc Kazakh-Mongol arcContinental Arc Orkhon-Selenge ArcContinental Arc Orkhon-Selenge ArcIsland Arc Kazakh-Mongol ArcContinental Arc Orkhon-Selenge ArcContinental Arc Baolidao Magma SuiteIsland Arc East Tienshan Metallogenic BeltContinental Arc Balkash-Yili Arc (West Junggar)Island Arc Dananhu-Tousuquan ArcIsland Arc Tuva-Mongol ArcContinental Arc Orkhon-Selenge ArcIsland Arc Kazakh-Mongol ArcContinental Arc Ervana Arc Terrane (Erdene Gold Inc., 2007b); Orkhon-Selenge ArcIsland Arc Kazakh-Mongol ArcIsland Arc Kazakh-Mongol ArcContinental Arc Orkhon-Selenge ArcContinental Arc Orkhon-Selenge ArcContinental Arc Balkash-Yili Arc (Kokirqin)Continental Arc Orkhon-Selenge ArcIsland Arc Tuva-Mongol ArcIsland Arc Kipchak ArcIsland Arc Kazakh-Mongol ArcContinental Arc Orkhon-Selenge ArcIsland Arc Kazakh-Mongol ArcContinental Arc Orkhon-Selenge Arcunknown unknownContinental Arc Orkhon-Selenge ArcIsland Arc Tuva-Mongol ArcIsland Arc Kazakh-Mongol ArcContinental Arc Orkhon-Selenge ArcIsland Arc? Tuva-Mongol Arc?

Island Arc Kazakh-Mongol ArcIsland Arc Kazakh-Mongol ArcIsland Arc Tuva-Mongol ArcIsland Arc Tuva-Mongol ArcIsland Arc Yidun Island ArcCollision-related Halatu Magma SuiteIsland Arc Dananhu-Tousuquan ArcContinental Arc Baolidao Magma SuiteContinental Arc Orkhon-Selenge ArcIsland Arc Yidun Island ArcIsland Arc Dananhu-Tousuquan ArcIsland Arc East Tienshan Metallogenic BeltContinental Arc Orkhon-Selenge ArcIsland Arc Dananhu-Tousuquan ArcContinental Arc Orkhon-Selenge ArcContinental Arc Orkhon-Selenge ArcContinental Arc Orkhon-Selenge ArcContinental Arc Orkhon-Selenge ArcContinental Arc Orkhon-Selenge ArcContinental Arc Orkhon-Selenge ArcContinental Arc Balkash-Yili Arc (Kokirqin)Island Arc Kazakh-Mongol ArcContinental Arc Orkhon-Selenge ArcIsland Arc Da Hinggan Mts.Island Arc Bangong-Nujiang ArcContinental Arc Orkhon-Selenge ArcContinental Arc Orkhon-Selenge ArcContinental Arc Orkhon-Selenge ArcIsland Arc Yidun Island ArcIsland Arc Bangong-Nujiang ArcIsland Arc Kazakh-Mongol ArcContinental Arc Orkhon-Selenge ArcIsland Arc East Tienshan Metallogenic BeltContinental Arc Orkhon-Selenge ArcIsland Arc Kazakh-Mongol ArcContinental Arc Junggar metallogenic beltIsland Arc Yidun Island ArcPost-subduction Belt unnamed beltIsland Arc Kazakh-Mongol arcContinental Arc Orkhon-Selenge ArcContinental Arc Orkhon-Selenge ArcContinental Arc Orkhon-Selenge ArcContinental Arc Balkash-Yili Arc (West Junggar)Continental Arc Orkhon-Selenge ArcContinental Arc Orkhon-Selenge Arc

Post-subduction Belt unnamed beltPost-subduction Belt unnamed beltIsland Arc Dananhu-Tousuquan ArcIsland Arc? Tuva-Mongol Arc?Continental Arc Balkash-Yili Arc (Kokirqin)Continental Arc Balkash-Yili Arc (Kokirqin)Island Arc? Tuva-Mongol Arc?Continental Arc Orkhon-Selenge ArcIsland Arc Kazakh-Mongol ArcIsland Arc Kazakh-Mongol ArcContinental Arc Orkhon-Selenge ArcContinental Arc Orkhon-Selenge ArcIsland Arc Kazakh-Mongol ArcIsland Arc Kazakh-Mongol ArcIsland Arc Kazakh-Mongol ArcIsland Arc Kazakh-Mongol ArcContinental Arc Orkhon-Selenge ArcContinental Arc Orkhon-Selenge ArcContinental Arc Orkhon-Selenge ArcContinental Arc Orkhon-Selenge ArcIsland Arc Kazakh-Mongol ArcContinental Arc Orkhon-Selenge ArcContinental Arc Orkhon-Selenge ArcIsland Arc? Tuva-Mongol Arc?Island Arc Kazakh-Mongol ArcIsland Arc Kazakh-Mongol ArcContinental Arc Orkhon-Selenge ArcContinental Arc Orkhon-Selenge ArcContinental Arc Orkhon-Selenge ArcContinental Arc Orkhon-Selenge ArcContinental Arc Kiyalykh-Uzen metallogenic beltContinental Arc Balkash-Yili Arcunknown unknownIsland Arc Tuva-Mongol Arcunknown unknownIsland Arc Zharma-Saur ArcIsland Arc Kipchak ArcContinental Arc Balkash-Yili Arc (Kokirqin)Continental Arc Orkhon-Selenge ArcContinental Arc Balkash-Yili Arc (Kokirqin)Island Arc Yidun Island ArcPost-subduction Belt unnamed beltIsland Arc Yidun Island ArcIsland Arc Kazakh-Mongol ArcIsland Arc Dananhu-Tousuquan Arc

Post-subduction Belt unnamed beltIsland Arc Kazakh-Mongol ArcIsland Arc Kazakh-Mongol ArcIsland Arc Kazakh-Mongol ArcIsland Arc Kazakh-Mongol Arcunknown unknownContinental Arc Junggar metallogenic beltContinental Arc Orkhon-Selenge ArcContinental Arc Orkhon-Selenge ArcIsland Arc Tuva-Mongol ArcContinental Arc Orkhon-Selenge ArcIsland Arc Kazakh-Mongol ArcIsland Arc Tuva-Mongol ArcContinental Arc Orkhon-Selenge ArcContinental Arc Orkhon-Selenge ArcIsland Arc Kazakh-Mongol ArcIsland Arc Kazakh-Mongol ArcIsland Arc Kazakh-Mongol ArcContinental Arc Orkhon-Selenge ArcIsland Arc Kipchak ArcContinental Arc Baolidao Magma SuiteContinental Arc Orkhon-Selenge ArcContinental Arc Orkhon-Selenge ArcContinental Arc Orkhon-Selenge ArcContinental Arc Orkhon-Selenge ArcContinental Arc Orkhon-Selenge ArcContinental Arc Orkhon-Selenge ArcContinental Arc Orkhon-Selenge ArcContinental Arc Orkhon-Selenge ArcContinental Arc Orkhon-Selenge ArcContinental Arc Orkhon-Selenge ArcIsland Arc Yidun Island ArcContinental Arc Orkhon-Selenge ArcIsland Arc Kazakh-Mongol ArcIsland Arc Kazakh-Mongol ArcIsland Arc Kazakh-Mongol ArcContinental Arc Orkhon-Selenge ArcContinental Arc Orkhon-Selenge ArcContinental Arc Orkhon-Selenge ArcIsland Arc Kazakh-Mongol ArcIsland Arc? Tuva-Mongol Arc?Continental Arc Orkhon-Selenge ArcContinental Arc Orkhon-Selenge ArcIsland Arc Yidun Island ArcIsland Arc Yidun Island Arc

Continental Arc Balkash-Yili Arc (Kokirqin)Continental Arc Orkhon-Selenge ArcContinental Arc Balkash-Yili Arc (Kokirqin)Island Arc Bangong-Nujiang ArcIsland Arc Kazakh-Mongol ArcContinental Arc Orkhon-Selenge ArcPost-subduction Belt unnamed beltIsland Arc Dananhu-Tousuquan ArcContinental Arc Orkhon-Selenge ArcContinental Arc Orkhon-Selenge ArcIsland Arc Tuva-Mongol ArcIsland Arc Zharma-Saur ArcIsland Arc Kazakh-Mongol ArcContinental Arc Orkhon-Selenge ArcContinental Arc Orkhon-Selenge ArcContinental Arc Orkhon-Selenge ArcIsland Arc? Tuva-Mongol Arc?Continental Arc Orkhon-Selenge ArcContinental Arc Orkhon-Selenge ArcIsland Arc Bangong-Nujiang Arcunknown unknownPost-subduction Belt unnamed beltIsland Arc Kazakh-Mongol ArcIsland Arc Kazakh-Mongol ArcIsland Arc Kazakh-Mongol ArcIsland Arc Yidun Island ArcContinental Arc Balkash-Yili Arc (Kokirqin)unknown unknownIsland Arc Kazakh-Mongol ArcContinental Arc Orkhon-Selenge ArcIsland Arc Kazakh-Mongol ArcPost-subduction Belt unnamed beltContinental Arc Orkhon-Selenge ArcIsland Arc Tuva-Mongol Arcunknown unknownIsland Arc Tuva-Mongol ArcContinental Arc Orkhon-Selenge ArcContinental Arc Orkhon-Selenge ArcContinental Arc Orkhon-Selenge ArcIsland Arc Kazakh-Mongol ArcIsland Arc? Tuva-Mongol Arc?Continental Arc Orkhon-Selenge ArcIsland Arc Da Hinggan MtsIsland Arc Kazakh-Mongol ArcContinental Arc Orkhon-Selenge Arc

Continental Arc Orkhon-Selenge ArcContinental Arc Orkhon-Selenge ArcIsland Arc Kazakh-Mongol ArcContinental Arc Orkhon-Selenge ArcIsland Arc? Tuva-Mongol Arc?Continental Arc Orkhon-Selenge ArcContinental Arc Orkhon-Selenge ArcIsland Arc Kazakh-Mongol ArcPost-subduction Belt unnamed beltContinental Arc Orkhon-Selenge ArcContinental Arc Orkhon-Selenge ArcIsland Arc Dananhu-Tousuquan ArcIsland Arc Kazakh-Mongol ArcContinental Arc Orkhon-Selenge ArcIsland Arc Kazakh-Mongol ArcContinental Arc Orkhon-Selenge ArcIsland Arc Kazakh-Mongol ArcContinental Arc Orkhon-Selenge ArcIsland Arc Kazakh-Mongol Arcunknown unknownIsland Arc Kazakh-Mongol ArcContinental Arc Orkhon-Selenge ArcContinental Arc Orkhon-Selenge ArcContinental Arc Orkhon-Selenge ArcContinental Arc Balkash-Yili Arc (West Junggar)Continental Arc Balkash-Yili Arc (West Junggar)Continental Arc Balkash-Yili Arc (West Junggar)Continental Arc Balkash-Yili Arc (West Junggar)Continental Arc Balkash-Yili Arc (West Junggar)Continental Arc Balkash-Yili Arc (West Junggar)Continental Arc Balkash-Yili Arc (West Junggar)Continental Arc Balkash-Yili Arc (West Junggar)Island Arc Kazakh-Mongol ArcContinental Arc Orkhon-Selenge ArcContinental Arc Orkhon-Selenge ArcIsland Arc Tuva-Mongol ArcContinental Arc Orkhon-Selenge ArcContinental Arc Orkhon-Selenge ArcContinental Arc Orkhon-Selenge ArcPost-subduction Belt unnamed beltIsland Arc Kazakh-Mongol ArcIsland Arc Kazakh-Mongol ArcIsland Arc Kazakh-Mongol ArcIsland Arc Kazakh-Mongol ArcIsland Arc Kipchak Arc

Island Arc Kazakh-Mongol Arcunknown Kalaxianger BeltIsland Arc Yidun Island ArcIsland Arc? Tuva-Mongol Arc?Island Arc? Tuva-Mongol Arc?Island Arc? Tuva-Mongol Arc?Post-subduction Belt unnamed beltPost-subduction Belt unnamed beltunknown Kalaxianger BeltContinental Arc Orkhon-Selenge ArcContinental Arc Orkhon-Selenge ArcIsland Arc Yidun Island ArcContinental Arc Orkhon-Selenge ArcIsland Arc Kazakh-Mongol ArcIsland Arc? Tuva-Mongol Arc?Continental Arc Orkhon-Selenge ArcIsland Arc Kazakh-Mongol ArcContinental Arc Orkhon-Selenge ArcContinental Arc Orkhon-Selenge Arc

Ore_min1molybdenite, scheelite, chalcopyrite (Seltmann and others, 2010)

molybdenite, chalcopyrite, pyrite, sphalerite, pyrrhotite, magnetite, and scheelite, altered to K-feldspar, silica, and sericitebiotite, bornite, carbonate, chalcocite, chalcopyrite, chlorite, copper, enargite, galena, hematite, magnetite, merenskyite [(Pd,Pt)Te2], molybdenite, pyrite, sericite, sphalerite, tennantite/tetrahedritemalachite, azurite, chalcopyritechalcopyrite, bornite, malachite, native copper

chalcopyrite, pyrite, galena, sphalerite, cyprite

chalcopyrite, bornite, galena, gold, molybdenite, pyrite, pyrrhotite, sphalerite

chalcopyrite, pyrite, molybdenite,

malachite, azurite, pyrite

actinolite, albite, biotite, bornite, carbonate, chalcocite, chalcopyrite, chlorite, covellite, epidote, fahlore, galena, galenobismutite, hematite, kaolinite, magnetite, malachite, marcasite, molybdenite, montmorillonite, muscovite/sericite, pyrite,chalcopyrite, molybdenite

chalcopyrite, bornite, molybdenite, chalcocite, pyrite, copper oxide mineralschalcopyrite, molybdenite, electrum, pyrite, malachite/azurite, bornite, covellite, galena, sphalerite, marcasitepyrite, chalcopyrite, bornite, covellite, cuprite, molybdenite, malachite, azurite

chalcopyrite, molybdenitepyrite, chalcopyrite, malachite

chalcopyrite, pyrite, sphalerite, galena

chalcopyrite, bornite, malachite, native copper

chalcopyrite, molybdenitemolybdenite, chalcopyrite, chalcocite, bornite, chalcocite, pyrite

chalcopyrite,pyrite, malachite, bornite, chalcocite

chalcopyrite, bornite, molybdenitechalcopyrite, gold, chalcocite, bornite, molybdenite, copper, cuprite, malachite, azuritepyrite, chalcopyrite, molybdenite, bornite, tennantite, galena, sphalerite

chalcopyrite, pyrite, bornite, chalcocite, covellite, malachite, galenacopper, chalcopyrite, azurite

chalcopyrite, pyrite, molybdenite

chalcopyrite, pyrite, malachite

chalcopyrite, pyritechalcopyrite, pyritechalcopyrite, bornite, chalcanthite, chalcocite, covellite, electrum, gold, pyritechalcopyrite, bornite, tennantite, sphalerite, galena, pyrite, pyrrhotite, molybdenite

chalcopyrite, pyrite, arsenopyrite, pyrrhotite, molybdenite, bornite

chalcopyrite, pyrite, marcasite, arsenopyritechalcopyrite, bornite, molybdenite, gold, pyrite, calaverite, chalcocite, chrysocolla, copper, cuprite, galena, sphalerite, azurite/malachite

chalcopyrite, magnetite, pyrite, sericite

chalcocite, malachite, azurite

magnetite, chalcopyrite, pyrite, arsenopyrite, pentlandite, sphalerite, pyrrhotite, molybdenite, fahlore galena, enargite and scheeliteactinolite, azurite/malachite, bornite, chalcocite, chalcopyrite, chlorite, chrysocolla, copper, covellite, epidote, gold, hematite, ilmenite, magnetite, molybdenite, pyrite, sericite, tennantite/tetrahedritechalcopyrite, pyrite, molybdenite, sphalerite, fahlore, magnetitepyrite, chalcopyrite, malachitebornite, chalcopyrite, galena, magnetite, molybdenite, pyrite, sericite, sphaleritealbite, atacamite, azurite/malachite, biotite, carbonate, chalcocite, chalcopyrite, chlorite, covellite, epidote, gypsum, hematite, iron oxides, malachite, pyrite, pyrrhotite, scheelite, sericitealbite, anhydrite/gypsum, apatite, azurite/malachite, biotite, bismuth, bornite, carbonate, chalcocite, chalcopyrite, covellite, digenite, galena, gold, hematite, magnetite, marcasite, molybdenite, muscovite/sericite, pyrite, silver, sphalerite, tennantite, zeolite

chalcopyrite, molybdenite, pyrite

malachite, azurite, chalcopyrite, chalcocite, tetrahedrite, pyrite

chalcopyrite, pyrite,molybdenite

sulfide, malachite, native copper

chalcopyrite, galena, magnetite, molybdenite, pyrite, sericite, sphaleritebornite, carbonate, chalcopyrite, chlorite, molybdenite, pyrite, tourmaline

bismuth, bornite, carbonate, chalcocite, chalcopyrite, chlorite, covellite, epidote, galena, gold, molybdenite, pyrite, sericite, silver, sphalerite, tetrahedrite

sericite, kaolinite and silica

alunite, apatite, malachite, barite, biotite, bornite, carbonate, chrysocolla, arsenosulvanite [Cu3(As,V)S4], chalcocite, chlorite, copper, covellite, chalcopyrite, kaolinite/illite/dickite, epidote, fluorite, hematite, goethite/limonite, magnetite,malachite; minor chalcopyrite

chalcopyrite, pyrite, ilmenite, magnetite, bornite and millerite and rare sphalerite, arsenopyrite, chalcocite, pentlandite and native goldchalcopyrite, bornite, pyrite, azurite, malachite

pyrite, chalcopyrite, malachite, azurite, rare sphalerite and molybdenite

chalcopyrite, bornite, chalcocite,malachite, molybdenite, pyrite, pyrrhotite

chalcopyrite, molybdenite

albitophyre copper ore; malachite oxide orechalcopyrite, pyrite,bornite, sphalerite, covellite, malachite

chalcopyrite, pyrrhotite, pyrite, tetrahedrite, galena, sphalerite, arsenopyrite, bornitechalcopyrite, pyrite, molybdenite, chalcocite

biotite, bornite, chalcopyrite, fahlore, galena, gold, hematite, magnetite, molybdenite, pyrite, sphalerite

chalcopyrite, pyrite,pyrrhotite, malachite

chalcopyrite, molybdenite, sphalerite, galena, magnetite and hematite

chalcopyrite, bornite, pyrrhotite, molybdenite, chalcocite, galena, sphalerite, malachite

chalcopyrite, bornite, pyrite

chalcopyrite, bornitepyrite, molydbenite, chalcopyrite, sphalerite, galena

chalcopyrite, bornite, pyrite, molybdenite

pyrite, chalcopyrite, malachite

pyrite, chalcopyrite, malachite

pyrite, chalcopyrite, bornite, molybdenite and minor amount of sphalerite and galena

albite, amphibole, anhydrite/gypsum, azurite/malachite, barite, biotite, bornite, carbonate, chalcocite, chalcopyrite, chlorite, chrysocolla, cinnabar, copper, covellite, cuprite, epidote, fluorite, galena, hematite, magnetite, marcasite,gold, chalcopyrite

chalcopyrite, pyrite, bornite, sphalerite, galenachalcopyrite, malachite

chalcopyrite, bornite, chalcocite, pyrite, molybdenite, covellite, digenite, rickardite [Cu7Te5], sphalerite

malachite, azurite, pyrite, chalcopyrite

chalcopyrite, pyrite, molybdenite, bornite

malachite, azurite, minor limonite, hematitemalachite and azurite

sphalerite

chalcopyrite, pyrite, pyrrhotite, bornite, cassiterite, molybdenite

molybdenite, chalcopyrite

molybdenite, pyrite, chalcopyrite, marcasitechalcopyrite, pyrite, molybdenitechalcopyrite, pyrite, molybdenite, sphalerite, galena

chalcopyrite, pyrite, molybdenite, sphalerite, galena, bornitechalcopyrite, pyrite, galena, sphalerite, molybdenitechalcopyrite, pyrite, molybdenite

chalcopyrite, bornite, pyrite, galenacarbonate, chalcopyrite, chlorite, epidote, galena, magnetite, molybdenite, pyrite, sericite, sphalerite

chalcopyrite, bornite, molybdenite.pyrite, chalcopyrite, molybdenite, malachite, chrysocolla

Ore_min2

alteration: K-feldspar, biotite; phyllic; chlorite

pyrophyllite, pyrrhotite, rutile, sphalerite, tourmaline

bismuthinite, brochantite, chalcanthite, chalcocite, cubanite, hessite, mackinawite, pentlandite, pyrrhotite, sylvanite, silver, tetrahedrite/tennantite

sericitic alteration is dominant

tetrahedrite, bornite

silica, sericite, pyritie, carbonate and locally to barite.

molybdenite, pyrite, pyrophyllite, rutile, sericite, sphalerite, svanbergite [SrAlll3(PO4)(SO4)(OH6)], tennantite, tenorite, zunyite

silica, K feldspar, albite, biotite, sericite, epidote, chlorite, and carbonate

molybdenite, powellite, pyrite, sericite, sphalerite, tennantite, tenorite, tourmaline

molybdenite, quartz-molybdenite and quartz-pyrite-chalcopyrite-molybdenite, stringers and disseminations.

chlorite-sericite-calcite-pyrite. kaolinite, pyrophyllite, alunite. pyrite, goethitie, hematite, limonite, magnetitite, chalcopyrite, malachite, sphalerite, galena

Ore_min3

pervasive sericite and argillic alteration

extensively altered to silica, sericite and pyrite

Ign_rock1rhyolite, dacite, tuff, limestone, schist, syenite porphyry, monzogranite porphyry (Seltmann and others, 2010); granite-granodiorite and leucogranite intrusions (Rundkvist, 2001)

schist and gneiss intruded by a granitoid stockgranodiorite porphyry, quartz diorite porphyry, Magma type: calc-alkalinebasalt, basaltic tuff, brecciagranodiorite

granite, diorite, granite porphyry

granodiorite porphyryadamellite porphyry, felsitediorite porphyry, quartz diorite, granodiorite porphyryandesite, andesite-dacite porphyry

volcanic tuff

andesite, basaltrhyodacite dikes, rhyolite porphyry dikes

andesite porphyry, breccia, granodiorite porphyry, quartz monzodiorite porphyry, quartz syenite porphyry;n.d.;andesite dike, andesitic trachybasalt, granite, granodiorite, trachyandesite, tuff-breccia, tuff-conglomerate, tuffaceous sandstone, tuffaceousrhyolite porphyry, granite porphyry, dacite

granosyenite, monzodiorite, diorite, gabbrobreccia, diorite porphyry, granodiorite porphyry, syenite porphyry, tonalite porphyry, gabbro, rhyolite, andesite porphyry, andesitic tuff, diabase, trachyandesite porphyry, trachydacite porphyrymonzodiorite, granodiorite, tonalite, diorite porphyry, lamprophyre

quartz diorite, granosyenite, syenite, granodioritegabbro, diorite, quartz diorite, granodiorite, granite, andesite

granodiorite, monzogranite, granite, andesite

granodiorite and granitegranodiorite and quartz dioritesyenogranite, monzogranite, dioritediorite, diorite porphyry, plagiogranite porphyryandesite diorite, monzodiorite porphyry, syenite, syenite porphyry, syenodiorite porphyry, granite, granodiorite, andesite,andesite porphyry, basalt, basaltic andesite

andesite porphyry, felsic porphyry,volcanic rocksdiorite, granodiorite, monzogranite

quartz monzonite

andesite porphyry, dacite porphyry, monzogranite, granodiorite, diorite, quartz diorite, granodiorite porphyry, granite, quartz monzonitequartz diorite porphyry, granodiorite porphyry, andesite, basaltic andesitegranodiorite porphyry, breccia, andesite porphyry, andesitic dacite, aplite, dacite porphyry, diorite porphyry, felsite, felsite porphyry, granite porphyry, granodiorite porphyry, pegmatite, tonalite porphyry, trachyte porphyry

granodiorite porphyry

granodiorite porphyry, dacite porphyryandesite, andesite-dacite porphyry

granodiorite porphyry, tonalite porphyry, diorite porphyry

quartz diorite, granodiorite

granodioritegranodiorite porphyry, diorite, monzogranitequartz porphyry, rhyolite porphyry, granite porphyrydacite porphyry, tuffgranodioritegranodiorite

diorite, diorite porphyry, monzdiorite, quartz diorite, explosive breccia, monzonite porphyry, monzodiorite porphyry, andesite

trachyandesite, andesite, tuffbreccia, feldspar porphyry, hornfels; monzodiorite, monzonite, sandstone, siltstone

quartz monzonite

andesite and basalt intruded by granitequartz monzonite, quartz monzonite porphyry, skarn, diorite (Singer and others, 2008), diorite, granodiorite, syenite and diorite from Kuznetsov and others (1971)granite porphyry, hornfels, tonalite porphyrycontact zone of granite porphyry and volcanic-sedimentary rockgabbro, diorite, quartz diorite, granodiorite, granite, andesitegranodiorite porphyry; Cu-Mo porphyry bodies that occur in contact zone between country rock and quartz porphyry and granite porphyry intrusive stockshornfels, andesite porphyry, diorite porphyry, granodiorite porphyry;sandstone, siltstone;andesite, granite, granodiorite, sandstone, tuffaceous conglomerate, tuffaceous sandstone, tuffbreccia, granite porphyry, granodiorite porphyry, monzodioritegranodiorite porphyry, monzogranite porphyry

monzogranite porphryry, plagiogranite, granodiorite porphyry, diorite porphyry, diabase

monzogranite porphyrydiorite porphyry

granite, granite porphyry

granodiorite porphyry, monzogranite porphyry, syenogranite porphyry;andesite, rhyolite

granodiorite porphyry

diorite and granosyenite porphyry dike

granodiorite plutons

granite, granite porphyry, granodiorite porphyry, diorite porphyrygranodiorite, granosyenite, sedimentary rocks, volcanic rocks

breccia, granodiorite porphyry, monzonite porphyry. Hosted by monzonite to granodiorite porphyries (Seltmann and Porter, 2005).monzodiorite, quartz monzonite, monzonite, andesite

syenite porphyry, quartz porphyry stocks and granite and felsite dikes

monzodiorite, diorite

quartz monzodiorite; andesite dike, breccia, diorite, monzodiorite porphyry, syenite dike, syenite porphyry, syenodiorite porphyry;argillite, granite, granodiorite, shale; andesite, andesite flow breccia, andesite porphyry, basalt

granitoidgabbro and hornblendite stocks intrude gneiss, schist and amphibolitegranodiorite porphyry, granosyenite porphyry, syenite porphyry, granite, granosyenite

quartz diorite porphyry, quartz monzonite porphyry, granodiorite, andesite, dacite

granodiorite

albite rhyolite porphyry (core); breccia porphyry; quartz albitophyremonzogranite, diabase

quartz diorite, diorite porphyry, granodiorite porphyry, tonalite porphyryquartz diorite, granodiorite, granodiorite porphyry, plagiogranite porphyry, diorite, tonalite

diorite porphyry, granodiorite porphyry, hornfels, syenite porphyry;limestone, metamorphic rocks;dacitic tuff, sandstone, siltstone, tuffaceous sedimentary rocks

diorite, andesite porphyry, granodiorite porphyry, monzonite porphyry

explosive breccia, granodiorite porphyry

granodiorite, quartz diorite, diorite, granite

biotite granite, volcanic rock

diorite porphyry, granite porphyry, monzodiorite porphyry, quartz syenite porphyry;andesite, diorite, granodiorite, monzonite, tuff, tuff breccia, tuffaceous sandstone, tuffaceous siltstone

quartz diorite porphyry, quartz monzonite porphyry, diorite porphyrydiorite, quartz diorite, granitesub-alkaline granite porphyries; monzodiorites, quartz-monzodiorites, monzonites, leucogranites with monzogabbro-porphyrite, monzodiorite-porphyrite, syenite-porphyry dikes

monzogranite, granodiorite

gabbro, diorite, quartz diorite, granodiorite, granite, andesite

gabbro, diorite, quartz diorite, granodiorite, granite, andesite

granodiorite, granite, andesite, tuff, tuff breccia

aplite, diorite porphyry, explosive breccia, feldspar porphyry, gabbro porphyry, granite porphyry, quartz syenite porphyry, syenite porphyry, syenodiorite porphyry, andesite porphyry, gabbro, granite, granodiorite, granosyenite porphyry,andesite, rhyolite

granosyenite porphyry

granodiorite porphyry plagiogranite porphyry, diorite porphyry, basalt, andesite, rhyolite, plagioclase porphyry, breccia, body size < 1 km2

andesite tuff intruded by monzodiorite

quartz monzodiorite

granite, granosyenite

volcanic-sedimentary sequence

granite, plagiogranite

monzodiorite, granodiorite porphyry, granite, rhyodacite, andesite

volcanic rocks

diorite, granodiorite, monzogranite porphyrygranodiorite porphyry, quartz diorite porphyry, quartz monzonite porphyryquartz diorite, quartz monzonite

granodiorite, granite, syenogranite, dioritedioritegranodiorite porphyry, quartz diorite porphyry, quartz monzonite porphyry

granitegranodiorite and granite massif and porphyry in stocks and dikes

granite porphyry

granodiorite, dacite porphyry, andesite, quartz monzonite, syenite,

Ign_rock2

volcanic-plutonic system, porphyritic diorite to granite

diabase, gabbro (dikes)

basaltic andesite, carbonaceous claystone, conglomerate, dacite, lapilli tuff, pillow basalt, rhyolite, sandstone, syenite, tuffaceous siltstone, tuffite.

Dev_Status

Active

Exploration

ExplorationExploration

Exploration, Advanced

DepositFeasibilityExplorationExploration

ExplorationExplorationExplorationExploration

Exploration

ExplorationDevelopmentExploration


Exploration

ExplorationMiningExplorationExploration

ExplorationExplorationExploration

Exploration

Exploration

MiningExplorationProduction


Exploration




ExplorationMining, Advanced Exploration

Exploration

Exploration

Exploration

Exploration

Exploration

Exploration

ExplorationExplorationExplorationExplorationExplorationExploration

Exploration

Exploration

Exploration

Exploration

Exploration

ProductionExploration

Exploration

Exploration

Development

Exploration

Exploration

PreproductionExploration

Exploration


MiningExploration


Exploration


Exploration

ExplorationExplorationActive open pitExploration

Exploration

Exploration

Exploration

Exploration

Exploration

MiningExploration

ExplorationExplorationDepositExploration

Exploration

Mining?


ExplorationExplorationExplorationExplorationExplorationExplorationExplorationExploration

Exploration

Exploration


ExplorationExplorationExploration, advanced


Exploration

Exploration

Development

SourceKirkham and Dunne (2000), Rundkvist (2001), A.F. Chitalin (written commun., 2009), Nokleberg and others (1999)Dejidmaa and others (2002)Nokleberg and others (1999), Nokleberg and others (2003), Nokleberg and others (2006), Rundkvist (2001)Nokleberg and others (2003), Nokleberg and others (2006), Kirkham and Dunne (2000), Singer and others (2008), Nokleberg and others (1999)Nokleberg and others (1999), Dejidmaa and others (2002)W.J. Nokleberg (written commun., 2006), McFaul and others (2000)Nokleberg and others (1999), Dejidmaa and others (2002)Dejidmaa and others (2002)literatureliteratureDejidmaa and others (2002), W.J. Nokleberg (written commun., 2006)McFaul and others (2000), W.J. Nokleberg (written commun., 2006)literatureliteratureDejidmaa and others (2002)Nokleberg and others (1999), Dejidmaa and others (2002)literatureNokleberg and others (1999), Dejidmaa and others (2002)Singer and others (2008), Nokleberg and others (2003), Nokleberg and others (2006), Kamitani and others (2007)Kamitani and others (2007)literatureMcFaul and others (2000)Nokleberg and others (1999), Dejidmaa and others (2002)Nokleberg and others (1999), Dejidmaa and others (2002)literatureNokleberg and others (1999), Dejidmaa and others (2002)literatureliteratureDejidmaa and others (2002)Singer and others (2008), Nokleberg and others (2003), Kirkham and Dunne (2000), Dejidmaa and others (2002), Nokleberg and others (1999)Nokleberg and others (1999), Singer and others (2008)Nokleberg and others (1999), Dejidmaa and others (2002)Nokleberg and others (1999)Singer and others (2008), Kirkham and Dunne (2000), Kamitani and others (2007), Rundkvist (2001)Nokleberg and others (1999), Nokleberg and others (2003), Nokleberg and others (2006), Dejidmaa and others (2002), Kamitani and others (2007)Nokleberg and others (1999), Dejidmaa and others (2002)Nokleberg and others (1999)Dejidmaa and others (2002)Seltmann and others (2009), Laznicka (1976, table 2), Kirkham and Dunne (2000)literatureliteratureNokleberg and others (1999), Dejidmaa and others (2002)Dejidmaa and others (2002), W.J. Nokleberg (written commun., 2006)Dejidmaa and others (2002), W.J. Nokleberg (written commun., 2006)

Nokleberg and others (1999), Dejidmaa and others (2002)literatureliteratureDejidmaa and others (2002), McFaul and others (2000)literatureliteratureSinger and others (2008)literatureNokleberg and others (1999), Dejidmaa and others (2002), W.J. Nokleberg (written commun., 2006)literatureliteratureliteratureDejidmaa and others (2002)literatureDejidmaa and others (2002)Dejidmaa and others (2002)Dejidmaa and others (2002)Dejidmaa and others (2002), W.J. Nokleberg (written commun., 2006)Dejidmaa and others (2002)Dejidmaa and others (2002), Nokleberg and others (1999)literatureNokleberg and others (1999)Nokleberg and others (1999)Singer and others (2008), Kirkham and Dunne (2000), Kamitani and others (2007), W.J.Nokleberg, written commun. (2006)literatureSinger and others (2008), Dejidmaa and others (2002), Kirkham and Dunne (2000), Volkov and others (1999 [2006])Nokleberg and others (1999), Dejidmaa and others (2002)Nokleberg and others (1999), Dejidmaa and others (2002)literatureliteratureNokleberg and others (1999)W.J. Nokleberg (written commun., 2006)Kamitani and others (2007), W.J. Nokleberg (written commun., 2006)Nokleberg and others (1999), W.J. Nokleberg (written commun., 2006), Dejidmaa and others (2002)Nokleberg and others (1999), Dejidmaa and others (2002)literatureKamitani and others (2007)literatureliteratureW.J. Nokleberg (written commun., 2006)Nokleberg and others (1999), Dejidmaa and others (2002)Nokleberg and others (1999), Dejidmaa and others (2002), W.J. Nokleberg (written commun., 2006)literatureDejidmaa and others (2002)Dejidmaa and others (2002), W.J. Nokleberg (written commun., 2006)

literatureliteratureSinger and others (2008)Nokleberg and others (1999), Nokleberg and others (2003), Nokleberg and others (2006), Rundkvist (2001), A.F. Chitalin (written commun., 2009)literatureliteratureNokleberg and others (1999), Dejidmaa and others (2002)Nokleberg and others (1999), Dejidmaa and others (2002)Nokleberg and others (1999), Dejidmaa and others (2002)Nokleberg and others (1999), Dejidmaa and others (2002)Dejidmaa and others (2002), W.J.Nokleberg, written commun. (2006)Dejidmaa and others (2002), W.J.Nokleberg, written commun. (2006)Nokleberg and others (1999)Nokleberg and others (1999), Dejidmaa and others (2002), Singer and others (2008)Nokleberg and others (1999), Dejidmaa and others (2002)literatureNokleberg and others (1999), Dejidmaa and others (2002)Nokleberg and others (1999), Dejidmaa and others (2002)Dejidmaa and others (2002)Nokleberg and others (1999), W.J. Nokleberg (written commun., 2006), Dejidmaa and others (2002)Singer and others (2008)Nokleberg and others (1999), Nokleberg and others (2003), Nokleberg and others (2006), Dejidmaa and others (2002)Dejidmaa and others (2002), W.J.Nokleberg, written commun. (2006)Dejidmaa and others (2002), W.J.Nokleberg, written commun. (2006)literatureNokleberg and others (1999)Nokleberg and others (1999), Dejidmaa and others (2002)W.J. Nokleberg (written commun., 2006)Nokleberg and others (1999), Dejidmaa and others (2002)Nokleberg and others (1999)Singer and others (2008), Rundkvist (2001), Nokleberg and others (1999)Singer and others (2008), Seltmann and others (2009), Rundkvist (2001)Nokleberg and others (1999), Nokleberg and others (2003), Nokleberg and others (2006), Rundkvist (2001)literatureSinger and others (2008)Singer and others (2008)Singer and others (2008), Seltmann and others (2009), Rundkvist (2001)literatureDejidmaa and others (2002), W.J.Nokleberg, written commun. (2006)literatureliteratureliteratureliteratureKamitani and others (2007)Singer and others (2008)

literatureNokleberg and others (1999), Dejidmaa and others (2002)literatureNokleberg and others (1999), Dejidmaa and others (2002)literatureA.F. Chitalin (written commun., 2009)literatureliteratureDejidmaa and others (2002)Nokleberg and others (1999), Dejidmaa and others (2002)literatureNokleberg and others (1999), Dejidmaa and others (2002)Nokleberg and others (1999), W.J. Nokleberg (written commun., 2006)Dejidmaa and others (2002), W.J. Nokleberg (written commun., 2006)Dejidmaa and others (2002), Singer and others (2008), Nokleberg and others (2003), Nokleberg and others (2006)Dejidmaa and others (2002), Singer and others (2008), Nokleberg and others (1999), Nokleberg and others (2003), Nokleberg and others (2006), Kamitani and others (2007)Nokleberg and others (1999), Dejidmaa and others (2002)Nokleberg and others (1999), Dejidmaa and others (2002)Nokleberg and others (1999)Singer and others (2008)literatureMcFaul and others (2000), W.J. Nokleberg (written commun., 2006), Nokleberg and others (1999)McFaul and others (2000), Nokleberg and others (1999), W.J. Nokleberg (written commun., 2006)McFaul and others (2000), W.J. Nokleberg (written commun., 2006)McFaul and others (2000), W.J. Nokleberg (written commun., 2006)Nokleberg and others (1999), Dejidmaa and others (2002)Nokleberg and others (1999), Kirkham and Dunne (2000)Dejidmaa and others (2002)Dejidmaa and others (2002), W.J. Nokleberg (written commun., 2006)Dejidmaa and others (2002)Dejidmaa and others (2002), Nokleberg and others (1999), Nokleberg and others (2003), Nokleberg and others (2006),literatureDejidmaa and others (2002)Nokleberg and others (1999), Dejidmaa and others (2002)Nokleberg and others (1999), Dejidmaa and others (2002)Singer and others (2008), Kirkham and Dunne (2000), Dejidmaa and others (2002), Nokleberg and others (2003), Nokleberg and others (2006)Nokleberg and others (1999), Dejidmaa and others (2002)literatureNokleberg and others (1999), Nokleberg and others (2003), Hedenquist and Daneshfar (2003)Singer and others (2008), Nokleberg (1999), Nokleberg (2003), Nokleberg (2006), Dejidmaa and others (2002)Nokleberg and others (1999), Dejidmaa and others (2002)Nokleberg and others (1999), Nokleberg and others (2003), Nokleberg and others (2006), Dejidmaa and others (2002)Nokleberg and others (1999), Dejidmaa and others (2002)Singer and others (2008)literature

literatureDejidmaa and others (2002)literatureliteratureliteratureDejidmaa and others (2002)Singer and others (2008)Singer and others (2008), Dequan and others (2005)Nokleberg and others (1999), W.J. Nokleberg (written commun., 2006)Singer and others (2008), Nokleberg and others (2003), Nokleberg and others (2006), Kirkham and Dunne (2000)Nokleberg and others (1999), Nokleberg and others (2003), Nokleberg and others (2006), Dejidmaa and others (2002)literatureliteratureSinger and others (2008), Dejidmaa and others (2002), Nokleberg and others (2003), Nokleberg and others (2006), Nokleberg and others (1999)literatureDejidmaa and others (2002)Dejidmaa and others (2002)Nokleberg and others (1999)Dejidmaa and others (2002)literatureDejidmaa and others (2002)Dequan and others (2005)literatureSinger and others (2008), Nokleberg and others (1999), Nokleberg and others (2003)Nokleberg and others (1999), Dejidmaa and others (2002)literatureliteratureNokleberg and others (2003), Rundkvist (2001), Seltmann and others (2009), A.F. Chitalin (written commun., 2009)literatureliteratureNokleberg and others (1999), Dejidmaa and others (2002)literatureNokleberg and others (1999), Dejidmaa and others (2002)literatureA.F. Chitalin (written commun., 2009), Rundkvist (2001)literatureNokleberg and others (1999), Dejidmaa and others (2002)Dejidmaa and others (2002)Nokleberg and others (1999), W.J. Nokleberg (written commun., 2006)literatureNokleberg and others (1999), W.J. Nokleberg (written commun., 2006)W.J. Nokleberg (written commun., 2006), Dejidmaa and others (2002)Nokleberg and others (2003), Nokleberg and others (2006), W.J. Nokleberg (written commun., 2006)literatureNokleberg and others (1999), Dejidmaa and others (2002), W.J. Nokleberg (written commun., 2006)

literatureliteratureSinger and others (2008), Kirkham and Dunne (2000), Nokleberg and others (1999)literature, W.J. Nokleberg (written commun., 2006)Dejidmaa and others (2002)Nokleberg and others (1999), Dejidmaa and others (2002)Dejidmaa and others (2002), W.J. Nokleberg (written commun., 2006)Nokleberg and others (1999), Dejidmaa and others (2002)literatureNokleberg and others (1999)literatureSinger and others (2008)Nokleberg and others (1999)literatureliteratureMcFaul and others (2000), W.J. Nokleberg (written commun., 2006)Nokleberg and others (1999), Dejidmaa and others (2002)Dejidmaa and others (2002)literatureA.F. Chitalin (written commun., 2009)Nokleberg and others (1999), Dejidmaa and others (2002)Dejidmaa and others (2002), W.J. Nokleberg (written commun., 2006)McFaul and others (2000), W.J. Nokleberg (written commun., 2006), Nokleberg and others (1999)W.J. Nokleberg (written commun., 2006), Dejidmaa and others (2002), Nokleberg and others (1999)literatureliteratureliteratureliteratureliteratureliteratureliteratureliteratureNokleberg and others (1999), Dejidmaa and others (2002)Nokleberg and others (1999), Dejidmaa and others (2002)Nokleberg and others (1999), Dejidmaa and others (2002)Nokleberg and others (1999), Dejidmaa and others (2002)Nokleberg and others (1999)McFaul and others (2000), W.J. Nokleberg (written commun., 2006)Nokleberg and others (1999), Dejidmaa and others (2002), W.J. Nokleberg (written commun., 2006)literatureDequan and others (2005)literatureliteratureliteratureliterature

literatureliteratureliteratureDejidmaa and others (2002), W.J. Nokleberg (written commun., 2006)Dejidmaa and others (2002), Nokleberg and others (1999), W.J.Nokleberg, written commun. (2006)Dejidmaa and others (2002), W.J.Nokleberg, written commun. (2006)literatureliteratureliteratureDejidmaa and others (2002), W.J.Nokleberg, written commun. (2006)Nokleberg and others (1999), W.J. Nokleberg (written commun., 2006)literatureSinger and others (2008), Nokleberg and others (2003), Nokleberg and others (2006)literatureDejidmaa and others (2002), W.J. Nokleberg (written commun., 2006)Nokleberg and others (1999), Dejidmaa and others (2002), W.J. Nokleberg (written commun., 2006)Dejidmaa and others (2002)Dejidmaa and others (2002), W.J. Nokleberg (written commun., 2006)Dejidmaa and others (2002), W.J. Nokleberg (written commun., 2006)

Source_ID460, 437

4731021, 602, 9691078, 722, 351, 443

2716757

624152

26916767

145350

276465, 114, 1609, 2237

471

16598274127

160

266454, 590, 780, 212

454188

420, 132, 7, 506604, 1531, 632, 3754

426

254657, 97, 500

628, 629, 630266329

427

242, 16758

588

134

141

322245272270247142

473, 657, 5

452, 297, 144178191

467, 1146371

10

384

264288

281212

5981037, 454, 482

605429432601161280

(615), 616, 453597

143676428327688

605, 1146, 272472311

358

257

442, 516427, 169, 6971088, 733, 718

444433

416, 126, 473

148

449585

429

430

273239

425

292285, 606, 612, 1135434, 610, 614, 1527, 3753

596627

429

16740167761674116742

71???, 874

302243108

268, 1092, 1165

137614608

455, 810, 34, 622, 1573208

623611, 624, 1504, 443

474690, 1112, 162

465590

246

258462

589, 67

451, 625, 1392, 2001644, 1344

612, 303, 636, 1175

150263

136

245

613, 52823

1366, 544, 97, 112

625

242

802

205151

147126, 908

301

456, 398

297427327

24

586, 587

16728428464

4118

27116729

210

21234370413

16782153

52

309270307

265

605/607, 646

308289

4256326

Updater UpdatedMark Mihalasky 7/18/2013Tom Frost (3/23/2010), Mark Mihalasky 6/20/2013Steve Ludington 5/29/2013Vladimir Berger (1/11/2010), Steve Ludington (2/6/2012), Mark Mihalasky 5/17/2013Steve Ludington 6/6/2012Warren Nokleberg, Steve Ludington 6/4/2012Tom Frost (3/3/2010), Mark Mihalasky 6/20/2013Tom Frost (3/23/2010), Mark Mihalasky 6/20/2013Steve Ludington 6/4/2012Steve Ludington 5/29/2013Tom Frost (3/23/2010), Mark Mihalasky 6/20/2013Tom Frost (3/24/2010), Mark Mihalasky 6/19/2013Steve Ludington (5/9/2013), Mark Mihalasky 6/20/2013Steve Ludington 6/4/2012Tom Frost (3/23/2010), Mark Mihalasky 6/20/2013Tom Frost 3/3/2010), Mark Mihalasky 6/20/2013Steve Ludington 6/4/2012Tom Frost (3/23/2010), Mark Mihalasky 6/20/2013Steve Ludington, Mark Mihlasky (12/6/2011), Mark Mihalasky 7/11/2013Steve Ludington 6/4/2012Tom Frost & Steve Ludington (2/24/2012), Mark Mihalasky 5/17/2013Warren Nokleberg (12/14/2009), Steve Ludington 6/4/2012Warren Nokleberg (12/14/2009), Mark Mihalasky 6/25/2013Tom Frost (3/23/2010), Mark Mihalasky 6/20/2013Steve Ludington (5/3/2012), Mark Mihlasky 8/1/2013Steve Ludington (3/25/2012), Mark Mihalasky 5/6/2013Steve Ludington 6/6/2012Steve Ludington 6/6/2012Tom Frost (3/23/2010), Mark Mihalasky 6/20/2013Jane Hammarstrom, Steve Ludington (3/23/2010), Mark Mihalasky 6/19/2013Steve Ludington 6/4/2012Tom Frost 3/3/2010), Mark Mihalasky 6/25/2013Steve Ludington (3/25/2012), Mark Mihalasky 5/3/2013Steve Ludington (2/20/2012), Mark Mihalasky 7/9/2013Mark Mihalasky 7/29/2013Warren Nokleberg, Tom Frost (12/14/2009), Mark Mihalasky 6/20/2013Tom Frost (3/23/210), Steve Ludington 6/4/2012Tom Frost (3/23/210), Steve Ludington 6/4/2012Mark Mihalasky (1/14/2012), Steve Ludington 5/29/2013Steve Ludington 5/7/2013Steve Ludington 6/4/2012Steve Ludington 6/4/2012Tom Frost (3/23/210), Steve Ludington 6/4/2012Tom Frost (3/23/210), Steve Ludington 6/4/2012

Tom Frost (3/3/2010), Mark Mihalasky 6/20/2013Steve Ludington 6/4/2012Steve Ludington 6/4/2012Warren Nokleberg (12/14/2009), Steve Ludington (6/4/2012), Mark Mihalasky 7/23/2013Steve Ludington 5/9/2013Mark Mihalasky (11/4/2011), Steve Ludington 6/12/2013Steve Ludington 6/4/2012Steve Ludington 6/4/2012Tom Frost (3/23/210), Steve Ludington 6/4/2012Steve Ludington 6/4/2012Steve Ludington 6/4/2012Steve Ludington 6/4/2012Tom Frost (3/23/2010), Mark Mihalasky 6/20/2013Steve Ludington 6/4/2012Mark Mihalasky 6/20/2013Mark Mihalasky 6/20/2013Mark Mihalasky 6/20/2013Mark Mihalasky 6/20/2013Mark Mihalasky 6/20/2013Mark Mihalasky 6/20/2013Steve Ludington (2/24/2012), Mark Mihalasky 8/5/2013Tom Frost, Mark Mihalasky (1/24/2012), Steve Ludington 6/4/2012Tom Frost (3/3/2010), Mark Mihalasky 6/24/2013Steve Ludington (9/10/2011), Mark MIhalasky 7/24/2013Steve Ludington 5/29/2013Steve Ludington (2/4/2012), Mark Mihalasky 1/16/2013Tom Frost (3/3/2010), Mark Mihalasky 6/20/2013Mark Mihalasky (2/9/2012), Steve Ludington 6/4/2012Steve Ludington 5/9/2013Steve Ludington 5/9/2013Tom Frost (3/23/2010), Mark Mihalasky 6/26/2013Mark Mihalasky 8/1/2013Steve Ludington (9/2/2011), Mark Mihalasky 6/4/2012Warren Nokleberg (12/14/2009), Mark Mihalasky 6/26/2013Tom Frost 3/23/2010), Mark Mihalasky 6/20/2013Steve Ludington 6/4/2012Steve Ludington 6/4/2012Steve Ludington 5/9/2013Steve Ludington 6/4/2012Mark Mihalasky 6/4/2012Mark Mihalasky 6/20/2013Steve Ludington (3/25/2012), Mark Mihalasky 1/25/2013Steve Ludington 6/4/2012Mark Mihalasky 6/20/2013Mark Mihalasky 6/20/2013

Steve Ludington 5/9/2013Steve Ludington 6/4/2012Steve Ludington 6/4/2012Steve Ludington 5/29/2013Steve Ludington 6/12/2013Steve Ludington 6/4/2012Tom Frost 3/3/2010), Mark Mihalasky 6/20/2013Tom Frost (3/3/2010), Mark Mihalasky 6/25/2013Steve Ludington 6/20/2013Tom Frost (3/3/2010), Mark Mihalasky 6/20/2013Mark Mihalasky 6/7/2012Mark Mihalasky 6/20/2013Tom Frost (3/3/2010), Mark Mihalasky 6/24/2013Steve Ludington 4/27/2012), Mark Mihalasky 4/26/2013Tom Frost (3/3/2010), Mark Mihalasky 6/20/2013Steve Ludington (3/25/2012), Mark Mihalasky 1/25/2013Mark Mihalasky 6/20/2013Tom Frost (3/3/2010), Mark Mihalasky 6/20/2013Warren Nokleberg (12/14/2009), Mark Mihalasky 6/20/2013Tom Frost, Mark Mihalasky 6/4/2012Steve Ludington 6/4/2012Tom Frost (3/3/210), Steve Ludington 6/4/2012Mark Mihalasky 6/20/2013Mark Mihalasky 6/20/2013Steve Ludington (5/3/2012), Mark Mihlasky 7/31/2013Tom Frost (3/3/2010), Mark Mihalasky 6/24/2013Tom Frost (3/3/2010), Mark Mihalasky 6/25/2013Mark Mihalasky 6/4/2012Tom Frost (3/3/2010), Mark Mihalasky 6/20/2013Mark Mihalasky 1/24/2013Steve Ludington, Mark Mihalasky 7/18/2013Jane Hammarstrom (10/11/2011), Steve Ludington (8/6/2012), Mark Mihalasky 7/16/2013Steve Ludington 5/29/2013Steve Ludington 6/4/2012Mark Mihalasky (2/7/2012), Steve Ludington 5/29/2013Jane Hammarstrom (11/1/2011), Steve Ludington (6/4/2012), Mark Mihalasky 7/17/2013Mark Mihalasky 7/16/2013Steve Ludington 6/4/2012Mark Mihalasky 6/20/2013Steve Ludington 6/12/2013Steve Ludington 6/4/2012Steve Ludington 6/4/2012Steve Ludington 6/4/2012Steve Ludington 6/4/2012Steve Ludington 6/4/2012

Steve Ludington 5/9/2013Tom Frost (3/3/2010), Mark Mihalasky 6/20/2013Steve Ludington (3/25/2012), Mark Mihalasky 1/25/2013Tom Frost (3/3/2010), Mark Mihalasky 6/20/2013Mark Mihalasky 1/31/2013Steve Ludington 6/4/2012Steve Ludington 6/4/2012Steve Ludington (3/25/2012), Mark Mihalasky 1/25/2013Steve Ludington (9/11/2011), Mark Mihalasky 6/20/2013Warren Nokleberg (12/14/2009), Mark Mihalasky 6/25/2013Steve Ludington (3/25/2012), Mark Mihalasky 5/3/2013Tom Frost (3/3/2010), Mark Mihalasky 6/20/2013Mark Mihalasky 5/8/2013Mark Mihalasky 6/20/2013Tom Frost (3/3/210), Steve Ludington (6/4/2012), Mark Mihalasky 7/9/2013Steve Ludington 6/4/2012Tom Frost (3/3/2010), Mark Mihalasky 6/20/2013Tom Frost (3/3/2010), Mark Mihalasky 6/20/2013Tom Frost (3/3/210), Steve Ludington 6/4/2012Mark Mihalasky 7/16/2013Mark Mihalasky 4/24/2013Mark Mihalasky 6/7/2012Mark Mihalasky 6/4/2012Mark Mihalasky 6/4/2012Mark Mihalasky 6/4/2012Tom Frost (3/3/2010), Mark Mihalasky 6/20/2013Steve Ludington 6/4/2012Mark Mihalasky 6/4/2012Mark Mihalasky 6/20/2013Mark Mihalasky 6/20/2013Tom Frost (3/3/210), Steve Ludington (6/4/2012), Mark Mihalasky 7/11/2013Steve Ludington 6/4/2012Mark Mihalasky 6/20/2013Steve Ludington 6/4/2012Tom Frost (3/3/2010), Mark Mihalasky 6/25/2013Tom Frost, Mark Mihalasky (6/10/2011), Mark Mihalasky 6/12/2013Warren Nokleberg, Tom Frost, Mark Mihalasky (1/31/2012), Steve Ludington 6/12/2013Steve Ludington 5/29/2013Mark Mihalasky 7/19/2013Steve Ludington 6/4/2012Tom Frost (3/3/2010), Mark Mihalasky 6/20/2013Tom Frost (3/3/2010), Mark Mihalasky 4/25/2013Tom Frost (3/3/2010), Mark Mihalasky 6/20/2013Steve Ludington 6/4/2012Steve Ludington 6/6/2012

Steve Ludington 6/4/2012Mark Mihalasky 6/20/2013Warren Nokleberg, Steve Ludington 6/13/2013Steve Ludington 5/9/2013Steve Ludington 6/4/2012Mark Mihalasky 6/20/2013Steve Ludington (9/12/2011), Mark Mihalasky 6/10/2013Steve Ludington 6/4/2012Mark Mihalasky 6/19/2013Tom Frost, Jane Hammarstrom (3/23/2010), Steve Ludington (6/4/2012), Mark Mihalasky 7/9/2013Steve Ludington (4/19/2012), Mark Mihalasky 5/8/2013Steve Ludington, Mark Mihalasky 7/26/2013Steve Ludington 6/4/2012Tom Frost (3/3/210), Steve Ludington 6/4/2012Steve Ludington 6/4/2012Mark Mihalasky 6/20/2013Mark Mihalasky 6/20/2013Tom Frost (3/3/210), Steve Ludington 6/4/2012Mark Mihalasky 6/20/2013Mark Mihalasky (12/7/2011), Steve Ludington 5/29/2013Steve Ludington 5/29/2013Mark Mihalasky (2/21/2012), Steve Ludington 6/4/2012Steve Ludington (3/25/2012), Mark Mihalasky 1/25/2013Tom Light (7/2/2010), Steve Ludington 6/4/2012Tom Frost (3/3/2010), Mark Mihalasky 6/20/2013Steve Ludington 5/9/2013Steve Ludington 6/4/2012Mark Mihalasky (10/10/2011), Steve Ludington (2/6/2012), Mark Mihalasky 5/29/2013Steve Ludington (3/25/2012), Mark Mihalasky 1/25/2013Steve Ludington (3/1/2012), Mark Mihalasky 5/8/2013Tom Frost (3/3/2010), Mark Mihalasky 6/20/2013Steve Ludington 6/12/2013Mark Mihalasky 6/20/2013Steve Ludington 6/4/2012Steve Ludington 6/4/2012Steve Ludington 6/4/2012Tom Frost (3/3/2010), Mark Mihalasky 6/20/2013Steve Ludington 6/4/2012Mark Mihalasky 6/19/2013Steve Ludington (3/25/2012), Mark Mihalasky 1/25/2013Mark Mihalasky 6/19/2013Mark Mihalasky 6/20/2013Steve Ludington (9/10/2011), Mark Mihalasky 7/19/2013Mark Mihalasky 4/23/2013Tom Frost (3/3/2010), Mark Mihalasky 6/20/2013

Steve Ludington 6/4/2012Steve Ludington (3/25/2012), Mark Mihalasky 5/3/2013Steve Ludington 6/4/2012Steve Ludington 6/4/2012Mark Mihalasky (2/9/2012), Steve Ludington 5/29/2013Tom Frost, Warren Nokleberg (3/3/2010), Mark Mihalasky 6/20/2013Mark Mihalasky 6/20/2013Tom Frost (3/23/2010), Mark Mihalasky 6/20/2013Steve Ludington 6/4/2012Tom Frost (3/3/2010), Mark Mihalasky 6/20/2013Steve Ludington (3/25/2012), Mark Mihalasky 4/30/2013Steve Ludington (2/22/2011), Mark Mihalasky 6/12/2013Tom Frost (3/3/210), Steve Ludington 6/4/2012Steve Ludington (3/25/2012), Mark Mihalasky 5/17/2013Steve Ludington (3/25/2012), Mark Mihalasky 1/25/2013Warren Nokleberg (12/14/2009), Steve Ludington 6/4/2012Tom Frost (3/3/2010), Mark Mihalasky 6/20/2013Mark Mihalasky 6/20/2013Tom Frost (7/30/210), Steve Ludington 6/4/2012Mark Mihalasky 5/8/2013Tom Frost (3/23/2010), Mark Mihalasky 6/26/2013Mark Mihalasky 6/20/2013Warren Nokleberg (12/14/2009), Steve Ludington 6/4/2012Warren Nokleberg (12/14/2009), Steve Ludington 6/4/2012Steve Ludington (9/2/2011), Mark Mihalasky 7/25/2013Steve Ludington (9/2/2011), Mark Mihalasky 7/25/2013Steve Ludington (9/2/2011), Mark Mihalasky 7/25/2013Steve Ludington (9/2/2011), Mark Mihalasky 7/25/2013Steve Ludington (9/2/2011), Mark Mihalasky 7/25/2013Steve Ludington (9/2/2011), Mark Mihalasky 7/25/2013Steve Ludington (9/2/2011), Mark Mihalasky 7/25/2013Steve Ludington (9/2/2011), Mark Mihalasky 7/25/2013Tom Frost (3/23/210), Steve Ludington 7/25/2013Tom Frost (3/23/2010), Mark Mihalasky 7/25/2013Warren Nokleberg (12/14/2009), Steve Ludington 7/25/2013Tom Frost (3/23/2010), Mark Mihalasky 7/25/2013Tom Frost (3/23/2010), Mark Mihalasky 7/25/2013Steve Ludington 6/4/2012Tom Frost (3/23/2010), Mark Mihalasky 6/20/2013Steve Ludington 5/28/2013Mark Mihalasky (2/17/2012), Steve Ludington 6/4/2012Steve Ludington 2/11/2013Steve Ludington 5/9/2013Steve Ludington 6/4/2012Steve Ludington 6/4/2012

Steve Ludington 6/4/2012Steve Ludington 5/29/2013Steve Ludington 6/4/2012Mark Mihalasky 6/20/2013Steve Ludington (5/29/2013), Mark Mihalasky 8/5/2013Mark Mihalasky 6/20/2013Steve Ludington 5/28/2013Steve Ludington 5/9/2013Steve Ludington 6/12/2013Mark Mihalasky 6/20/2013Mark Mihalasky 6/19/2013Steve Ludington (5/9/2013), Mark Mihalasky 6/11/2014Tom Frost (3/23/2010), Mark Mihlasky 7/17/2013Steve Ludington (3/2/2012), Mark Mihalasky 7/3/2013Mark Mihalasky 7/2/2013Mark Mihalasky 6/7/2012Steve Ludington (6/6/2012), Nark Mihalasky 8/2/2013Mark Mihalasky 6/20/2013Mark Mihalasky 6/20/2013

Ref_short1Kirkham and Dunne (2000), Rundkvist (2001), Seltmann and others (2010), A.F. Chitalin (written commun., 2009), Nokleberg and others (1999, 2003), Nokleberg (2010), SMR (2011), Yakubchuk (2011), Volkov and others (2006)Dejidmaa and others (2002)Petrov and Mkrtychan (1976), Nokleberg and others (1999, 2003, 2006), Rundkvist (2001), A.F. Chitalin, wirtten commun. (2009)Berzina and Berzina (2008), Berzina and Korobeinikov (2007), Berzina and others (2001, 2003, 2005, 2007), Chetvertakov (1991), Chetvertakov and Yarovoi (1989), Khomichev (1986), Popov and others (1988), Sotnikov and others (2001, 2003)Nokleberg and others (1999), Dejidmaa and others (2002), Central Asia Minerals (2012)W.J. Nokleberg (written commun., 2006), McFaul and others (2000), Dejidmaa and others (2002)Nokleberg and others (1999), Dejidmaa and others (2002)Dejidmaa and others (2002)Xanadu Mines Ltd. (2012b)A.F. Chitalin (written commun., 2009)Dejidmaa and others (2002), W.J. Nokleberg (written commun., 2006)McFaul and others (2000), W.J. Nokleberg (written commun., 2006)Hou and others (2007), Li and others (2011), Wenchang and others (2011)Xanadu Mines Ltd. (2012b)Dejidmaa and others (2002)Nokleberg and others (1999), Dejidmaa and others (2002)Zeng and others (2009)Nokleberg and others (1999), Dejidmaa and others (2002)Chen and Tang (1993), Nie and others (2004), Li and others (2005, 2007, 2008), Nokleberg and others (2003, 2006), Zhang and Rui (1992), Zhang and others (1993), Kamitani and others (2007), Singer and others (2008)Yin (2003), Yin and others (2009), Kamitani and others (2007)Liu and others (2009b), Shen and others (2009, 2010a), Zhang and others (2010a), Song and others (2007), Tang and others (2010), Pirajno and others (2011)Yan and others (2007), W.J. Nokleberg (written commun., 2006), McFaul and others (2000)Nokleberg and others (1999), Dejidmaa and others (2002)Nokleberg and others (1999), Dejidmaa and others (2002)Asia Gold (2005), Peréz (2007), Nokleberg and others (1999), Dejidmaa and others (2002)Nokleberg and others (1999), Dejidmaa and others (2002), Erdene Resource Development Corp. (2006, 2011a)Cinits and Parker (2007)Great Paragon Group LLC (2012)Dejidmaa and others (2002)Koval' and others (1988, 1989), Lamb and Cox (1998), Nokleberg and others (1999, 2003), Sillitoe and others (1996), Singer and others (2008), Kirkham and Dunne (2000), Dejidmaa and others (2002)Zhang and others (2006, 2010a), Tang and others (2010), Wang (2008), Nokleberg and others (1999), Singer and others (2008)Nokleberg and others (1999), Dejidmaa and others (2002)Nokleberg and others (1999), Dejidmaa and others (2002), Erdene Resource Development Corp. (2006), Erdene Gold Inc. (2007b), Erdene Resource Development Corp. (2011a)Kazakhmys PLC (2012), Mining Journal (2011), Berzina and others (2005), Singer and others (2008), Kaufman (1992), Kolesnikov and others (1986), Kudryavtsev (1996), Mutschler and others (2000), Pavlova (1978)Woodhouse and Bozada (2011), Nokleberg and others (1999, 2003, 2006), Dejidmaa and others (2002), W.J. Nokleberg (written commun., 2006), Blight and others (2010), Ivanhoe Mines Ltd. (2004a), Kamitani and others (2007), Kincora Copper (2012)Nokleberg and others (1999), Dejidmaa and others (2002)Nokleberg and others (1999)Dejidmaa and others (2002)Sidorov and others (2006), Seltmann and others (2009), Laznicka (1976, and references therein), Kirkham and Dunne (2000)Gobi-Khurakh LLC (2012), Gobi-Khurakh LLC (2013)Lyndhurst Enterprises Pty. Ltd. (2011)Nokleberg and others (1999), Dejidmaa and others (2002)Dejidmaa and others (2002), W.J. Nokleberg (written commun., 2006)Dejidmaa and others (2002), W.J. Nokleberg (written commun., 2006)

Nokleberg and others (1999), Dejidmaa and others (2002)Liu and others (2007)Ivanhoe Mines Ltd. (2001)Dejidmaa and others (2002), McFaul and others (2000), Nokleberg and others (2006)Hou and others (1991), Yan and others (2007)Wan and others (2009), Zeng and others (2010, 2011), Liu and others (2010a)Han and Zhao (2003), Qin and others (2002), Zhang and others (2010a), Wu and others (2006), Singer and others (2008)PR Newswire, [2007?]Nokleberg and others (1999), Dejidmaa and others (2002), W.J. Nokleberg (written commun., 2006)Hou and others (2007), Li and others (2011), Zou and others (2009)Midas Resources Limited (2008)Sun and others (2010), Xu and others (2010)Dejidmaa and others (2002)Jinshan Gold Mines (2006, 2008)Dejidmaa and others (2002)Dejidmaa and others (2002)Dejidmaa and others (2002)Dejidmaa and others (2002), W.J. Nokleberg (written commun., 2006)Dejidmaa and others (2002)Dejidmaa and others (2002), Nokleberg and others (1999)Zhang and others (2010b)Nokleberg and others (1999)Nokleberg and others (1999)

Li and others (2007, 2008, 2011), Xie and others (2009), She and others (2006)Singer and others (2008), Dejidmaa and others (2002), Berzina and others (1999, 2001, 2005), Watanabe and Stein (2000), JICA-JOGMEC (2004), Gavrilova and Maksimyuk (1990), Gerel and others (2005), Munkhtsengel and others (2006)Nokleberg and others (1999), Dejidmaa and others (2002)Nokleberg and others (1999), Dejidmaa and others (2002)Hou and others (2007)Qu and Xin (2006), Xie and others (2009)Nokleberg and others (1999)W.J. Nokleberg (written commun., 2006), Dejidmaa and others (2002)Xu and others (2010), Zhang and others (2011), Yan and others (2007), Kamitani and others (2007), W.J. Nokleberg (written commun., 2006)B.Y. Dolgov (written commun., 1984), Dejidmaa and others (2002), Nokleberg and others (1999), W.J. Nokleberg (written commun., 2006)Nokleberg and others (1999), Dejidmaa and others (2002)Cheng and others (2010)Hou and others (2007), Li and others (2011), Kamitani and others (2007)Lara Exploration (2010), Dunbar (2008), Ludington and others (2012)Xanadu Mines Ltd. (2011b), Xanadu Mines Ltd. (2012a)W.J. Nokleberg (written commun., 2006), Dejidmaa and others (2002), Nokleberg and others (1999)Nokleberg and others (1999), Dejidmaa and others (2002)Nokleberg and others (1999), Dejidmaa and others (2002), W.J. Nokleberg (written commun., 2006), Erdene Resource Development Corp. (2011a, b)Liu and others (2009a)Dejidmaa and others (2002)Dejidmaa and others (2002), W.J. Nokleberg (written commun., 2006)

Zeng and others (2013 and references therein), Ge and others (2007), Zhao and others (1997, 2005), Singer and others (2008), Kirkham and Dunne (2000), Kamitani and others (2007), W.J.Nokleberg (written commun., 2006)

Li and others (2008), Wu and others (2010)Wang and others (2010a)Miao and others (2007), Gao and others (2006), Qin and others (2002, 2003), Singer and others (2008)A.F. Chitalin (written commun., 2009), Lapukhov (1975), Kuznetsov (1982), Nokleberg and others (1999, 2003, 2006), Nokleberg (2010), Rundkvist (2001), Petrov and others (2009)Zhang and others (2008b, 2010b), Li and others (2007)Jia and others (2011), Dequan and others (2005)Nokleberg and others (1999), Dejidmaa and others (2002)Nokleberg and others (1999), Dejidmaa and others (2002)Nokleberg and others (1999), Dejidmaa and others (2002)Nokleberg and others (1999), Dejidmaa and others (2002)Dejidmaa and others (2002), W.J. Nokleberg (written commun., 2006)Dejidmaa and others (2002), W.J. Nokleberg (written commun., 2006)Nokleberg and others (1999, 2003), Kamitani and others (2012)Singer and others (2008), Berzina and others (1999), Kirwin and others (2005a,b), Nokleberg and others (1999, 2003), Sillitoe and others (1996), Dejidmaa and others (2002), Nokleberg (2010), Ivanhoe Mines Ltd. (2002a)Nokleberg and others (1999), Dejidmaa and others (2002)Erdene Resource Development Corp. (2011a, b)Nokleberg and others (1999), Dejidmaa and others (2002)Nokleberg and others (1999), Dejidmaa and others (2002)Dejidmaa and others (2002)Nokleberg and others (1999), W.J. Nokleberg (written commun., 2006), Dejidmaa and others (2002)Singer and others (and references therein, 2008), Voyager Resources (2011a), Business Wire (2005), Southgobi Energy Resources Ltd.(2007)B. Gurlkhaajav and others (written commun., 1974), H. Gonchigjav and others (written commun., 1984), Nokleberg and others (1999, 2003, 2006), Dejidmaa and others (2002)Dejidmaa and others (2002), W.J. Nokleberg (written commun., 2006)Dejidmaa and others (2002), W.J. Nokleberg (written commun., 2006)Voyager Resources (2011b, 2012, 2013), Proactive Investors (2012), Intierra (2009)Nokleberg and others (1999)Nokleberg and others (1999), Dejidmaa and others (2002)W.J. Nokleberg (written commun., 2006)Nokleberg and others (1999), Dejidmaa and others (2002)Nokleberg and others (1999), W.J. Nokleberg (written commun., 2006)Rundkvist (2001), Singer and others (2008), Laznicka (1976), Levchenko (1975), Kuznetsov and others (1971), Sotnikov and others (1995, 1999), Nokleberg and others (1999), Nokleberg (2010)Kolesnikov and others (1986), Pavlova (1978), Plyushchev (1993), Shatov and others (1996), Zhukov and others (1998), Singer and others (2008), Seltmann and others (2009), Rundkvist (2001)Nokleberg and others (1999, 2003, 2006), Rundkvist (2001), Domarev and Vysokoostrovskaya (1959), Nikolskaya (1961), Kuznetsov and others (1966), A.F. Chitalin, written commun. (2009)Lyndhurst Enterprises Pty. Ltd. (2011)Singer and others (2008, and references therein), Sotnikov and others (2003), Berzina and others (2005), Seltmann and Porter (2005), Nokleberg and others (2006)Pavlova (1978), Shevchenko (1973), Zhukov and others (1998), Singer and others (2008, and references therein)Singer and others (2008), Seltmann and others (2009), Rundkvist (2001), Castle (2007), Kolesnikov and others (1986), Kudryavtsev (1996), Zhukov and others (1998)Xue and others (2011), Zhang and others (2010b), Tang and others (2010)Dejidmaa and others (2002), W.J. Nokleberg (written commun., 2006)Zhang and others (2008a, 2010b), Tang and others (2010), Dequan and others (2005)Li and others (2011)Yan and others (2007)Hou and others (2007), Li and others (2011)Chinese Academy of Geological Sciences (1992), Kamitani and others (2007)Han and others (2003, 2006), Zhang and others (2004, 2006), Rui and others (2002), Singer and others (2008)

Xu and others (2004)Nokleberg and others (1999), Dejidmaa and others (2002), Blight and others (2010)Dejidmaa and others (2002), Erdene Resource Development Corp. (2011a, b), Erdene Gold Inc. (2004)Nokleberg and others (1999), Dejidmaa and others (2002)King Solomon Mines Ltd (2009, 2011?)A.F. Chitalin (written commun., 2009), Intierra (2009)Liang and others (2010), Wang and others (2009, 2010b)Erdene Resource Development Corp. (2011a, b), Erdene Gold Inc. (2004)Dejidmaa and others (2002), Xanadu Mines Ltd. (2011a, b)Dejidmaa and others (2002), Nokleberg and others (1999)Erdene Gold Inc. (2004, 2007b)Nokleberg and others (1999), Dejidmaa and others (2002)Nokleberg and others (1999), W.J. Nokleberg (written commun., 2006)Dejidmaa and others (2002), W.J. Nokleberg (written commun., 2006)Dejidmaa and others (2002), Singer and others (2008), Nokleberg and others (1999, 2003, 2006), Sotnikov and others (1985), Badarch and others (1999)Blight and others (2010), Nokleberg and others (1999, 2003, 2006), Singer and others (2005, 2008), Dejidmaa and others (2002), Kamitani and others (2007)Nokleberg and others (1999), Dejidmaa and others (2002)Nokleberg and others (1999), Dejidmaa and others (2002)Nokleberg and others (1999)Singer and others (2008), White and others (2001), Plyushchev (1993), Seltmann and Porter (2005), Shatov and others (1996), Zhukov and others (1998), Ussoltsev (2011), Yakubchuk (2004)Sen and others (2005), H. Williams and others (unpub. Data, 2003)McFaul and others (2000), W.J. Nokleberg (written commun., 2006), Nokleberg and others (1999), Dejidmaa and others (2002)McFaul and others (2000), Nokleberg and others (1999), W.J. Nokleberg (written commun., 2006), Dejidmaa and others (2002)McFaul and others (2000), W.J. Nokleberg (written commun., 2006)McFaul and others (2000), W.J. Nokleberg (written commun., 2006)Nokleberg and others (1999), Dejidmaa and others (2002)Dejidmaa and others (2002), Nokleberg and others (1999), Kirkham and Dunne (2000)Dejidmaa and others (2002), JICA-JOGMEC (2004)Dejidmaa and others (2002), W.J. Nokleberg (written commun., 2006)Dejidmaa and others (2002)Dejidmaa and others (2002), Nokleberg and others (1999, 2003, 2006), B. Gurlkhaajav and others (written commun., 1974), W.J. Nokleberg (written commun., 2006)Li and others (2011)Dejidmaa and others (2002)Nokleberg and others (1999), Dejidmaa and others (2002), Ivanhoe Mines Ltd. (2002b)Nokleberg and others (1999), Dejidmaa and others (2002)Singer and others (2008), Ivanhoe Mines Ltd. (2003a, 2010a,b, 2011), Kavalieris and others (2011), Khashgerel and others (2009), Kirwin (2006), Kirwin and others (2005a), Perelló and others (2001), Kirkham and Dunne (2000)Tong and others (2010), Nokleberg and others (1999), Dejidmaa and others (2002), W.J. Nokleberg. (written commun., 2006)Ivanhoe Mines Ltd. (2001)Nokleberg and others (1999, 2003), Hedenquist and Daneshfar (2003), UNESCAP (1999)Nokleberg and others (1999, 2003, 2006), Sotnikov and others (1985), Blight and others (2010), Singer and others (2008), Dejidmaa and others (2002), Ivanhoe Mines Ltd. (2001), Blight and others (2008)Nokleberg and others (1999), Dejidmaa and others (2002), W.J. Nokleberg (written commun., 2006)Nokleberg and others (1999, 2003, 2006), Dejidmaa and others (2002), Sotnikov and others (1985), Purevsuren and others (written commun., 1986)Nokleberg and others (1999), Dejidmaa and others (2002)Ren (1997), Wang and others (2007), Zeng and others (2004), Hou and others (2007), Li and others (2011), Chen and others (2008), Leng and others (2008), Singer and others (2008, and references therein)Li and others (2011)

Jia and others (2011)Dejidmaa and others (2002)Zhao (1999), Zhang and others (2010b), Liu and others (2011), Yan and others (2007), Dequan and others (2005), W.J. Nokleberg (written commun., 2006)Xin and Qu (2006)Cinits and Parker (2007)Dejidmaa and others (2002)Encyclopedia of the Nations ( 2001?), Zhao and Lin (1993), Wu and others (2010), Singer and others (2008)Qin and others (2002, 2009), Sun and others (2009), Li and others (2004), Zhang and others (2004), Dequan & others (2005), Singer and others (2008, and references therein)Nokleberg and others (1999), W.J. Nokleberg (written commun., 2006)Singer and others (2008), Ivanhoe Mines Ltd. (2001, 2004b), Jargalsaihan and others (1996), Nokleberg and others (2003, 2006), Sotnikov and others (1985), Watanabe and others (1999), Kirkham and Dunne (2000)Nokleberg and others (1999, 2003, 2006), Fortress Minerals Corporation (2007), Dejidmaa and others (2002)Liu and others (2010d), Guo and others (2010), Shen and others (2007)Apiva Ventures Ltd (2002), Monton (2004)Singer and others (2008), Dejidmaa and others (2002), Nokleberg and others (1999, 2003, 2006), Sotnikov and others (1985), Nokleberg (2010)Xanadu Mines Ltd. (2011b), Xanadu Mines Ltd. (2012a)Dejidmaa and others (2002)Dejidmaa and others (2002)Nokleberg and others (1999)Dejidmaa and others (2002)Zhao and others (2009)Fortress Minerals Corporation (2007), Dejidmaa and others (2002)Dequan and others (2005)Erdene Resource Development Corp. (2011a, b), Erdene Gold Inc. (2004)Singer and othes (2008), Ivanhoe Mines Ltd. (2002b, 2003b), Singer and others (2005), Bignall and others (2005), Ooka and others (1998), Batkhishig and others (2010), Blight and others (2010)Nokleberg and others (1999), Dejidmaa and others (2002)Leng and others (2008)Liu and others (2005)Nokleberg and others (1999, 2003), Rundkvist (2001), Seltmann and others (2009), A.F. Chitalin (written commun., 2009), Berzina and others (2005, 2011), Sotniko and others (2001)Erdene Resource Development Corp. (2011a, b), Erdene Gold Inc. (2004)UGL Enterprises Ltd. (2004)Nokleberg and others (1999), Dejidmaa and others (2002)Liu and others (2010c), Wu and others (2010)Nokleberg and others (1999), Dejidmaa and others (2002)Lyndhurst Enterprises Pty. Ltd. (2011)A.F. Chitalin (written commun., 2009), Rundkvist (2001)Lyndhurst Enterprises Pty. Ltd. (2011)Nokleberg and others (1999), Dejidmaa and others (2002)Dejidmaa and others (2002), Fortress Minerals Corporation (2007)Nokleberg and others (1999), W.J. Nokleberg (written commun., 2006)Erdene Resource Development Corp. (2011a, b), InfoMine [2005?]Nokleberg and others (1999), W.J. Nokleberg (written commun., 2006)W.J. Nokleberg (written commun., 2006), Dejidmaa and others (2002)Ge and others (2007), Zeng and others (2009, 2013), Yan and others (2007), Nokleberg and others (2003, 2006), W.J. Nokleberg (written commun., 2006), Zhao and others (1997)Woodhouse and Bozada (2011), Kincora Copper (2012)Nokleberg and others (1999), Dejidmaa and others (2002), W.J. Nokleberg (written commun., 2006), JICA-JOGMEC (2004)

Fortress Minerals Corporation (2007), Dejidmaa and others (2002), Nokleberg and others (1999)Erdene Gold Inc. (2007a)Berzina and others (1999), Jargalsaihan and others (1996), Sotnikov and others (1980, 1985), Lamb and Cox (1998), Watanabe and Stein (2000), Singer and others (2008), Kirkham and Dunne (2000), Nokleberg and others (1999), Mongolyn Alt (MAK) Group (2012)W.J. Nokleberg (written commun., 2006), Mining-Mongolia.net (2012)Dejidmaa and others (2002), Nokleberg and others (1999)Nokleberg and others (1999), Dejidmaa and others (2002)Dejidmaa and others (2002), W.J. Nokleberg (written commun., 2006)Nokleberg and others (1999), Dejidmaa and others (2002)Wu and others (2010)Dolgov and others (1984), Nokleberg and others (1999)Erdene Resource Development Corp. (2011a, b), Erdene Gold Inc. (2004)Han and others (2003, 2006), Qin and others (2003), Zhang and others (2004, 2006, 2008c, 2010a), Zhu and others (2003), Dequan and others (2005), Rui and others (2002), Gow (2011), Mao and others (2005)Nokleberg and others (1999)Erdene Resource Development Corp. (2011a, b), Erdene Gold Inc. (2004)Erdene Resource Development Corp. (2011a, b), Erdene Gold Inc. (2004)Altanzul (n.d.), McFaul and others (2000), W.J. Nokleberg (written commun., 2006)Nokleberg and others (1999), Dejidmaa and others (2002)Dejidmaa and others (2002)Khashgerel and others (2009), Ivanhoe Mines Ltd. (2010b, 2011)A.F. Chitalin (written commun., 2009)Nokleberg and others (1999), Dejidmaa and others (2002)Dejidmaa and others (2002), W.J. Nokleberg (written commun., 2006)Dejidmaa and others (2002), McFaul and others (2000), W.J. Nokleberg (written commun., 2006), Nokleberg and others (1999)Dejidmaa and others (2002), Nokleberg and others (1999), W.J. Nokleberg (written commun., 2006)Tang and others (2010)Tang and others (2010)Tang and others (2010)Tang and others (2010)Tang and others (2010)Tang and others (2010)Tang and others (2010)Tang and others (2010)Nokleberg and others (1999), Dejidmaa and others (2002)Nokleberg and others (1999), Dejidmaa and others (2002)Nokleberg and others (1999), Dejidmaa and others (2002)Nokleberg and others (1999), Dejidmaa and others (2002)Nokleberg and others (1999)McFaul and others (2000), W.J. Nokleberg (written commun., 2006), Nokleberg and others (1999), Dejidmaa and others (2002)Nokleberg and others (1999), Dejidmaa and others (2002), W.J. Nokleberg (written commun., 2006)Wu and others (2010)Dequan and others (2005)King Solomon Mines Ltd (2007)Nie and others (2005), Ivanhoe Mines Ltd. (2005)Zeng and others (2009)Shen and others (2010b)

Wang and others (2010c), Zhang and others (2011)Xue and others (2010), Yang and others (2005), Xiang and others (2009), Zhang and others (2010a)Hou and others (2007), Natural Resources Canada (2008), Li and others (2011), Cao and others (2010), Rui and others (2005), Singer and others (2008)Dejidmaa and others (2002), W.J. Nokleberg (written commun., 2006)Dejidmaa and others (2002), Nokleberg and others (1999), W.J. Nokleberg (written commun., 2006), Erdene Gold Inc. (2004), Erdene Resource Development Corp. (2011b)Dejidmaa and others (2002), W.J. Nokleberg (written commun., 2006)Wu and others (2010)Wu and others (2010)Xue and others (2010), Liu and others (2010b), Xiang and others (2009), Zhang and others (2010a)Dejidmaa and others (2002), W.J. Nokleberg (written commun., 2006)Nokleberg and others (1999), W.J. Nokleberg (written commun., 2006)Zhong and others (2010), Fei and Li (2010), Yin and Yang (2008), Fei and others (2010)Bayandorj and others (written commun., 1980), Sotnikov and others (1981, 1985), Singer and others (2008), Nokleberg and others (2003, and references therein), Nokleberg and others (2006), Nokleberg (2010)Asia Gold (2005), Peréz (2007)Dejidmaa and others (2002), W.J. Nokleberg (written commun., 2006), Nokleberg (2010)Nokleberg and others (1999), Dejidmaa and others (2002), W.J. Nokleberg (written commun., 2006), JICA-JOGMEC (2004)Dejidmaa and others (2002), Clark and Baudry (2011), Erdene Resource Development Corp. (2013)Dejidmaa and others (2002), W.J. Nokleberg (written commun., 2006)Dejidmaa and others (2002), W.J. Nokleberg (written commun., 2006)

Ref_short2

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Ussoltsev (2011), Kamitani and others (2007), Kirkham and Dunne (2000), Rundkvist (2001), Seltmann and Porter (2005), Shatov (1999), Sokolov (1998), Zhukov and others (1998)

Du and Chen (1984), Fan (1986), Mu and Liu (1996)

Kamitani and others (2007), Sotnikov and others (1985, 2001), Sillitoe and others (1996), Kirkham and Dunne (2000), Jargalsaihan and others (1996), Khacin and others (1977), Koval' and others (1989), Lamb and Cox (1998)

Shin and others (2005), Porter Geoconsultancy (2004), Seltmann and Porter (2005)

Dejidmaa and others (2002), Nokleberg and others (2003, 2006)

Nokleberg and others (1999, 2003)

Singer and others (2008)

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http://apps1.gdr.nrcan.gc.ca/gsc_minerals/gquerycache/porph/DG/dg500.htmlhttp://www.gobikhurakh.mn/upload/2012-02-27%20Presentation%20for%20Gobi%20Khurakh%20LLC.pdf; http://www.gobikhurakh.mn/pages/projects/project:Bulag%20Shand%20projecthttp://altanrio.com/wp-content/uploads/2012/01/Chandman-Yol-Technical-Report-NI-43-101.pdf

http://www.prnewswire.com/news-releases/newport-gold-inc-and-noront-resources-ltd-china-one-project-inner-mongolia-china-58833777.html

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http://www.jinshanmines.com/i/pdf/2006-02-21_NR.pdf, http://www.goldletterint.com/documents/pdf/JINSHAN_GLSP_Dec08Update.pdf

http://www.laraexploration.com/i/pdf/Lara-Corporate-pres-PDAC.pdf

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HeadingRegionGMRAP_IDTract_IDCoded_IDTract_nameNameName_otherIncludesSiteStatusCode_cntryCountryState_ProvLatitudeLongitudeDepo_TypeDepo_SubtyAge_MaAge_methodAge_stratAge_refComm_majorComm_minorTonnage_MtCu_pctMo_pctAu_ppmAg_ppmCon_Cu_tAu_MoG_T_comComments1Comments2Comments3Comments4Comments5Loc_comarc_typetect_featOre_min1Ore_min2Ore_min3Ign_rock1Ign_rock2Dev_Status

SourceSource_IDUpdaterUpdatedRef_short1Ref_short2Ref_web

ExplanationArea of study, Northeastern Asia for this reportUnique GMRAP-defined identifier for each recordInformal name of permissive tract from a previous report, often this is the same as the tract name.Coded, unique identifier assigned to permissive tract.Informal name of permissive tractSite nameOther names used for the site.Names of deposits that have been combined with the primary deposit as a result of the spatial aggregation rule used for calculating grades and tonnages. For porphyry copper, the spatial rule is 2 km. Values are "deposit", "significant prospect" or "prospect". Deposit means the site has both tonnage and grade reported for the principal commodity (Cu for porphyry copper), significant prospect has grade and tonnage comments, and prospect applies to all other sites. Country abbreviation, RUS for Russia.Country in which the deposit is located.State or Province of the Country.Latitude in decimal degrees (WGS84).Longitude in decimal degrees (WGS84).General deposit type (Porphyry Cu).Only deposits may be classified as the general type or a subtype. Subtype may be based on ratio of Au (g/t) to Mo in (wt%). For prospects, possible subtype, if any, is indicated in the comments field, and is derived from the literature and other reports.Ages are reported in millions of years before the present based on reported absolute ages. This field is blank if no absolute age determination was available. Method for absolute age determination.Stratigraphic age of deposit.Short reference for age information. Inference means the age assignment was subjective, based on geologic inference.Major commodities, expressed as chemical symbols.Minor commodities (byproducts, coproducts), expressed as chemical symbols.Tonnage in millions of metric tons.Average copper grade in weight percent.Average molybdenum grade in weight percent.Average gold grade in grams per metric ton (g/t).Average silver grade in grams per metric ton (g/t).Contained copper in metric tons, calculated.Ratio of Au (g/t) to Mo (wt. %), calculated.Comments regarding grade and tonnage, when available.Comments regarding deposits and prospects.Continuation of comments.Continuation of comments.Continuation of comments.Continuation of comments.Comments regarding the quality of location data.Type of arc associated with the deposit "Island arc" or "Continental arc".Name of the tectonic arc or belt associated with the deposit.Ore and other sulfide minerals present, as reported in literature cited.Continuation of ore comments.Continuation of ore comments.Names of igneous rocks associate with the deposit or prospect, as reported in literature cited.Continuation of Igneous rock comments.Development Status - the nature of operations at the time the deposit record was created; most values are exploration (the default) and mining, when mining operations are known at the site.

Source of the record if the data are from an existing database. When source was other than from a specific database, “literature” is entered. Deposit ID from the spatial sources listed in order of source citation.Name of person last updating the record.Date of update or addition to this database.Short reference. Full references are found in following tabs of file.Continuation of short references.Website used for record.

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