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4
CHARACTERIZATION OF THE CONSTITUENTS OF THE STRUCTURAL CHANNELS IN BERYL
Vladimir Bermanec Darko Tibljas Stjepan Scavnicar Department of Mineralogy and Petrology Faculty of Science
University of Zagreb Demetrova I Zagreb
and
Goran Kniewald Center for Marine Research Rutter Boskovic Institute
FOB 1016 Zagreb
In addition to t~e principal elements comprising the forshymula of beryl (Be AlSi) water and carbon dioxide are al~o its essential constituents Their presence and distribution depend on the conditions prevailing durin~ the crystallization of beryl These constituents just like the lRr~P cations (Cs K ~a Li) are located within the structural channel~ which Are formed by the six-member rings of SiO~- tetrahedra
The determination of these volatile components of beryl is comparatively straightforward using IR-spectroscopy Water and carbon dioxide display well-resolved and sharp absorption maxima in the region~ 3700-3500 cm-l and 2400-2300 cm-l respecshytively The quantity of water and carbon dioxide enterin~ the beryl structure is controlled by their fugacities durni~ the crystallization process as well as by available space within the hosting structural channels
Infrared spectra were run on 25 beryls from Yugoslavia and other occurences and their compositions with respect to H 0 and
2CO2 were essentially the same An analysis of these spectra established not only the presence of water and carbon dioxide in the investigated beryls but also provided data on the orienshytation of the water molecules bull Moreover the presence or absenshyce of large cations could also be indirectly assessed
Although the concentrations of these components need not be significant even minor amounts can have profound effects with respect to the beryls symmetry and may provide an explashynation for the anomalous optical biaxiality observed on some beryl crystals
5
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A SUMARY OF THEORETICAL MODELS AND THEIR APLICATION ConprwHSTS HS OCTSHSTKTe UHKpO eneueaTK e nSneHS BO Ts6enSTS 6poj
30ur Research US Geol Survey4p41-47XXXVIII
AUBOIN3 BLANCHETR CADETJP CELETP CHARVETJCHORONOWICZJ
COUSINM AND RAMPNOUX3P ( 1970 ) ESSAI SUR LA GEOLOGIE DES DINAmiddot KBapnaTI4TIof naTMTH ~aTHT-KB3p~~aTHTM RIDES Bul Soc Geol France 12 pl060-1095
ALTHERR KREUZERH WENDII LENZH WAGNERAG KELLERJ
Sc 30 30
Be 1 1 HERREW HONDORFA ( 1982 ) A LATE OLIGOCENE EARLY MIOCENE HIGH
20 TEMPERATURE BELT IN THE ATTIC CICLADYC CRISTALINEPb 200 200 100 COMPLEX (SE PELAGONIAN GRECCE) Geol 3b E23Ga 30 30 40 97-164 Hanover 1982Mo 1 1 3
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RerOBSTS cpenHS BpenHOCT COnpzRHSTS HS 6SKSPOT e RCTO TSKS pensshy ROCKS IN YUGOSLAVIA SectVIMagmatism Volcanism
TRBRO usnKY aroneueRS S aroneueHS e K conprwHSTS HS ypSROT HHTeshy Metamorphism Proc of the X th Conqres CBGA 1973
peCHO e neKS BO BynKsHcKHTe CTeBB HS Ko~ Kusue K pensTHBHo o60rsshy
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14
SUMr1ARY
MICROELEI1ENTS IN THE VOICANIC ROCKS OF KO~UF 110UNTAIN
BBoev Faculty of Geology ~d Mining Stip
A systematic determination of the content of the microelements and the elements of the rare earths was done for the volcanics of the
Kozuf 110untain
Main characteristic of these volcanic rocks is that they are rich in barium and stroncium as well as the other LIL Large Ion Litophile I
elements
These rocks are also enriched in elements of the group of rare earth~ especially in light rare earths
This is a very important characteristic which basically diferenti _ ates them from other tertiary volcanites in 11acedonia bull
I
15
MmiEPAJIOIHKA CTYJmJA HA ~EHOKmCTAJrnTE 011 BYJIKAHCKt1TE
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OnpenyBs~eTo HS THnOT H xeUH3UOT HS rnSBHHTe KHHepSnH on BynKsHcKHTe CTeHH HS Kozy~ nnSHHHS 6eme pesnH3HpSHO BO nepHonOT HS 1985 ronHHS HS YHHBep3HTeToT BO reTHHreH S non pSKOBonCTBO HS np~purspn BOHrT OnpenyBs~eTo 6eme H3BpmeHO co uouom BS eneKTpOHCKS UHKpOCOHnS on THn ( APJI - CEM )
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4
CHARACTERIZATION OF THE CONSTITUENTS OF THE STRUCTURAL CHANNELS IN BERYL
Vladimir Bermanec Darko Tibljas Stjepan Scavnicar Department of Mineralogy and Petrology Faculty of Science
University of Zagreb Demetrova I Zagreb
and
Goran Kniewald Center for Marine Research Rutter Boskovic Institute
FOB 1016 Zagreb
In addition to t~e principal elements comprising the forshymula of beryl (Be AlSi) water and carbon dioxide are al~o its essential constituents Their presence and distribution depend on the conditions prevailing durin~ the crystallization of beryl These constituents just like the lRr~P cations (Cs K ~a Li) are located within the structural channel~ which Are formed by the six-member rings of SiO~- tetrahedra
The determination of these volatile components of beryl is comparatively straightforward using IR-spectroscopy Water and carbon dioxide display well-resolved and sharp absorption maxima in the region~ 3700-3500 cm-l and 2400-2300 cm-l respecshytively The quantity of water and carbon dioxide enterin~ the beryl structure is controlled by their fugacities durni~ the crystallization process as well as by available space within the hosting structural channels
Infrared spectra were run on 25 beryls from Yugoslavia and other occurences and their compositions with respect to H 0 and
2CO2 were essentially the same An analysis of these spectra established not only the presence of water and carbon dioxide in the investigated beryls but also provided data on the orienshytation of the water molecules bull Moreover the presence or absenshyce of large cations could also be indirectly assessed
Although the concentrations of these components need not be significant even minor amounts can have profound effects with respect to the beryls symmetry and may provide an explashynation for the anomalous optical biaxiality observed on some beryl crystals
5
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6
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8 9
TASEnA xxx I II COAPIAJ HA ampAPHJYHOT H CTPO~HJYHOT BO BYnKAHCKHTE CTEHH HA KOllY nIlAHHHA ( nn )
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l1u-35 32 n-I
33
7 nl-I
28 I
18
10 20
27
29-1
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25 n-2
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29
1851 1806
1983 1983 1823
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1571 15~6
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1650 1489
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1536 1619
1577
117~
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20 1265 12 38
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81 1191 1187
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46 1281
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26 21
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1653 1772 1795 1727 1828
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1537 153 I
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71i
50 1029 1068 125~
81 1285 ~ I
950 1227 1292
59 1282
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75 IH6
86
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10
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11
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418 nnu OA ApyrB CTPBHS BO~1nKBHcKRTS CTeHB HS KozyW RUSUS ronashy
uo 0~or8T1Base H8 nSCHHTS peTKR asujH 3s CTsnSHOT H8 o~orsTYBsST( ~
H8 nSCHHTS PSTKH aeuja CnyH OAHOCOT uoust1 nBHTBHOT R HTSp~j1KOT
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12 13
~jSTS BO 3eujsTs KSne HUaUe roneuo MemSampe Ha uSTepKjsnx on KOHTHshyflHTEPATYPA
HeHTsnHSTS KOpS KropHROT OUOTS~ onHOCHO on rpSH~HOTO nonpa~je
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A SUMARY OF THEORETICAL MODELS AND THEIR APLICATION ConprwHSTS HS OCTSHSTKTe UHKpO eneueaTK e nSneHS BO Ts6enSTS 6poj
30ur Research US Geol Survey4p41-47XXXVIII
AUBOIN3 BLANCHETR CADETJP CELETP CHARVETJCHORONOWICZJ
COUSINM AND RAMPNOUX3P ( 1970 ) ESSAI SUR LA GEOLOGIE DES DINAmiddot KBapnaTI4TIof naTMTH ~aTHT-KB3p~~aTHTM RIDES Bul Soc Geol France 12 pl060-1095
ALTHERR KREUZERH WENDII LENZH WAGNERAG KELLERJ
Sc 30 30
Be 1 1 HERREW HONDORFA ( 1982 ) A LATE OLIGOCENE EARLY MIOCENE HIGH
20 TEMPERATURE BELT IN THE ATTIC CICLADYC CRISTALINEPb 200 200 100 COMPLEX (SE PELAGONIAN GRECCE) Geol 3b E23Ga 30 30 40 97-164 Hanover 1982Mo 1 1 3
V 20 100 100 AOKIK ( 1963 ) THE KERSUTITES OND AHYKEARSUTITES FROM ALKALIC Cu ROCK OF 3APAN AND SURROUNDING AREAS 3 bull Petr 4 Zn 20 20
30 100 30 198-210
Co 10 30 30 30 KAPAHATAC bullbull ( 1983 ) CAAPIAJH HEKHX HHKPOEflEHEHATA Y TEPUHJAPHHH
Ni 10 30 30 HArHATHTHHA HCT04Hor AEflA JyrOCflABHJE Y 3ABHCHOCTH O~B 10 30 40 ItHXOeOr rEOTEKTOHCKor nOflOIAJA OTHCaj 143 rnACA CpncIltRg 001 001 001 AKaAeMHje HaYKa 14 YMeTHOCTH K~~9F 900 600 1300
KAPAHATAC bullbull (197~) bullbull rEOXEHHJCKE nETPOflOWKE 14 HETAflOrEHETCKE npOBHH
UHJE KPEAHO-TEPUHJAPHE CTAPOCTH AEflA SAflKAHCKOr nOflYOshysite e1ementi osven Hg se odredeni so semikvantitativna spektroheshy CTPOBA H KAflE A3HJE nOce~Ha M3Aa~a CpncKe AK3AeMHJe mijska analiza (D30nov 1985 ) a Hg e odredena so hemijska metoda HaYKa 14 YHeTHocTH K~Hra ~2 bullbull ( NOzerova 1986 )
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CTH THnA TETHCA reoTeKToHHK3 Ho5 1983On OBSS Ta6ens ee rnens neKs BO BynKSHCK1Te creBB HS Ko~ nnSUHS
Rusue penSTBBRO 06erSTyBSampe as conpzsjoT RS onOBOTO BO onROC RS KARAMATAS (1973) ASSOCIATION OF BASIC AND ULTRAB~SIC( ULTRAMAFIC
RerOBSTS cpenHS BpenHOCT COnpzRHSTS HS 6SKSPOT e RCTO TSKS pensshy ROCKS IN YUGOSLAVIA SectVIMagmatism Volcanism
TRBRO usnKY aroneueRS S aroneueHS e K conprwHSTS HS ypSROT HHTeshy Metamorphism Proc of the X th Conqres CBGA 1973
peCHO e neKS BO BynKsHcKHTe CTeBB HS Ko~ Kusue K pensTHBHo o60rsshy
TyBse BO ConpzKHsTsas 60POT K ~nyOpOT TO jacHo yxa~a Ha 3Rs~eshy
BBeTO HS TaKS Hape~eRsTa eUsHsQBjcKs nHtepeHURjaQRjs
14
SUMr1ARY
MICROELEI1ENTS IN THE VOICANIC ROCKS OF KO~UF 110UNTAIN
BBoev Faculty of Geology ~d Mining Stip
A systematic determination of the content of the microelements and the elements of the rare earths was done for the volcanics of the
Kozuf 110untain
Main characteristic of these volcanic rocks is that they are rich in barium and stroncium as well as the other LIL Large Ion Litophile I
elements
These rocks are also enriched in elements of the group of rare earth~ especially in light rare earths
This is a very important characteristic which basically diferenti _ ates them from other tertiary volcanites in 11acedonia bull
I
15
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6
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75 20 bull J JO 5 Z7 lOS Zmiddot 17S u-u IS -)1 111
-]G UJ 25 J6znmiddot2 16 n-Z IU
bullbull U 115 Il bull
116 7 1-6
It-I- 7 165 7 ZI
10 bull 77 1Z7
J 117 to 110-15 II III-3ftM__))
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5 I n IlZ -J IZ 71
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04 OB8S Ts6ens ce rne4s 4eKS x conpZRRsTS BS CTPOHURjYUOT BO Bynxsshy
BCKKTe CTeRR RS Kozr~ ce 4BHZW BO rpSRKQaTe BS 950 na no 1565 nnM
x XSKO TSXBS e as 15 nSTR noroneMs 04 C04PXHBSTS BS CTPOHUHjYUOT
BO RRTepMenHjspHRTe CTeHR BO 3eMjHHsTS Xops
OBSKBOTO roneMO 060rSTyBsae HS 6apHjYUOT R CTPORUHjYUOT j8SHO a60shy
pyas 38 060rsTyaaaeTO B8 npBM8pRROT M8rMSTCKR pSCTon co OBHe 4B8
eneMeRTS
ESPRjYUOT R CTPORURjYUOT npRn8rS8T RS TSKS HSpeQeRST8 rpyn8 RS nIttH
eneMeHTR XOR BO npoueCRTe BS nspuRjsnHoTo Toneae BS npMspRROT R3shy
BOp ce KOHueRTpRpsne R 060rSTyBSne BO ~nYKnHSTS ~S3a 04HOCHO TRe
ce RKounsTK6HnHH eneMeHTa HHBHOT xoe~RUHeHT RS 4RCTPH6YURjS e
nOMSn 04 enRHRUs
UHPKOmtJY1tl Hi10EHJY1tI H IAltI)mtJYll
C04PZRR8TS RS IIHPKOHHjYMOT H KH06RjYUOT BO BynKBHcKKTe CTeRK HS
K~ nnsHKHS e 04pe4eHs co nOMom HS peHTreRO ~nyopecueHTHS MeT04s
S C04PZHHSTS RS xa~HajYUOT e onpe4eHs co nOMom RS HeYTpOHS SKTRBSshy
UKjS
bullbull
8 9
TASEnA xxx I II COAPIAJ HA ampAPHJYHOT H CTPO~HJYHOT BO BYnKAHCKHTE CTEHH HA KOllY nIlAHHHA ( nn )
Ho Ba Sr Ho Ba Sr
l1u-35
l1u-35 32 n-I
33
7 nl-I
28 I
18
10 20
27
29-1
HaK-31
25 n-2
19 22
29
1851 1806
1983 1983 1823
1937 1588
1571 15~6
1456
1596 1706
1315 162lt
1650 1489
1745
1536 1619
1577
117~
1365 127~
13H
20 1265 12 38
II 78 II 27
81 1191 1187
1353 II 80
46 1281
IH9
1198 1222
1173
l1u-3 27 11 -1
9 15 lI-6
11 -~
5 31
13 ny-I
30 6
MaK-32
HaK-30 ny-2
26 21
lI-3
1539
1315 2332 16~7
1620 1810 22~9
1605 2019 1518
1653 1772 1795 1727 1828
1851
1537 153 I
1723
~ I
930
71i
50 1029 1068 125~
81 1285 ~ I
950 1227 1292
59 1282
1320
75 IH6
86
AHanM3MTe ce BDweHM BO MHCTMTYTOT aa reoxeMMja M KMHeoanorMja nOM ~KaAeMMjaTa Ha HaYKMTe Ha CoaeTCKMOT CojY3 HOCX8a ( 1985 J( lIJoHoa HeToAa - PeHTreHo nygDeC~eHTHa ~ KBaHTMTaTMBHa
lI TAnJlA XtXLl toAI HA llHKOJOT bull M05MJ) 1ltUYHOT
to UJIlCAHun CTEMM itA KOX naAMNIt
MI 0 bullbull lib Of 0 bullbull JIb
ny- SI Ja na 17 II 55 d2 5a a1 ll adO a 5 a
1116 5 JU n-1 10 ftmiddot 16 0 ISO
11 51 77 1middot6 ft- UO
JIH I JU1 7J JU1 I
I I 5 150 110
~ I I I
T
I
I l no II
J 110 10 0 100 dSI
Na]] 110 7 5 IllS I
110
110 10 )2 210 bull II 0 5 no n 110 I-J 0
lSO
J 0 co nmiddot o yobullbull~bullbullshy~o ~~omiddot (a~n 1IS ) llrEM Alt eterRoc
xJOT bullbullbullbullbullbullbullbull co TClCa AICTII bullbull HaTobullbull CHlIIan_ac 1la
AHanSBTW~KBTe UO~STO~H 3S 60~PXBHSTS HS URPKOHHjYHOT HB06HjygOT R
XS~HHjygOT BO BynKsHCKBTe CTeHH HS Kozyt unSHRBS ce ~S~eHB BO
Ts6enSTS XXXIV O~ OBSS Ts6ens ce rne~s ~eKS CO~PZHHSTS HS UHPKOHH
jygOT BO BynK8HcxHTe CTeHR HS Ko~ ce ~BBXB BO rpSHR~Te HS 100
DS ~o 290 DDH a CO~PZHHSTS Ha HB06BjYUOT BO rpSH~Te HS 1 us ~o
11 DUM ~S~HBjyKOT ce ~BHZB BO rpSHUUWTe HS 54 us ~o 89 nnM
reHepsnHo rne~aHO co~pZWHaTS HS UWPKOHBjyKOT BO BynKsHcxHTe CTSH~
HS Kozyt e penSTRBHO roneMS S CO~PZBHSTS Ha HR06wjyKOT e aHOManRO
RBCKS BO O~ROC HS Co~pZHHaTS HS HB06HjYMOT W UWPKOHHjygOT BO~BqHR
CTeHH BO 3eMjRHsTs KOpS
10
ElIEUEHTH Ol IPYIJATA IrA PETIltH 3E11n1
OA eneUeHTaTe HS rpynsTB peTKH asujB BO BynKBHcKHTe CTeHH H8 Kozy~ UnSHHH8 ce OApeAsHB aTpKjYUOT nBHTBHOT QepBjYUOT H~OnHjYUOT
CBU8PHjYUOT eyppUHjYUOT TSP~HjYUOT HTSP~BjYUOT nyTeQHjYVOT
OBMS SnSUSHTB CS OApeAeHK co uouom H8 HB1TPOHCK8 8KTHB8QHOHB USTOshy
8 a HTPMj1uOT e OAPSASR co pSHTrSHO tn10pSCQeHTHB ueTOAB
COAepZHH8TB HB BTPKj1UOT BO B1nKBHCKBTS CTSbullbull H8 KozyW unBHHH8 S 8AeHB BO T8~snBT8 xxxvi
TAUDA IIXVI COIfAJ tIA ITPUYIIOT 10 UlKAMCUTI eTlN IIA ItO nnWHA (fin-)
Hbullbull IT_Jy H bull bull IIDII1middot
u 1-3 Il alllH 7 U ) l2 -)) 31
27 JZ -1 ZI n-I
23 Jl 1$ 5 7 7A-6 ZI nl- 23-III I
1$
23 31 JZ II 1$ 13
Zlr-I 5 2 7
76 5 U JZ bullbull -)2 7 alll-) 1 II bullbull -)0 5 n-z 21 1$ 3 n- 2l
2 ZI 5
AtI~1 ca ~ lIeTTIITo rJ raollbullbullbullJa
np Al bull HY_TO bullbull cbullbullbull COT CoJy O RoCII bullbull aJolllbullbullbull5 l TO bullbullrabullbullbullIIYOlllaCbullbull bullbull ( bullbullbull1oI0fG )
O OB8~ T8~en8 ce rnSAB ASK8 COAPZMH8T8 H8 HTPKj1UOT BO~K8HCKHTS CTSHH H8 Ko~ CS ABHZK BO rp8HMQRTe H8 25 uuu a T8B Bse RSKOj8
11
8HOU8nHOCT BO OAHOC HS COAPZRRBT8 HB HTPRj1uoT BO CnMQHH CTSHR OA
asujRHsTS KOpS
nOASTO~TS 3S COAPZMH8TS HS OCT8H8THTe PSTKH asujH ce ABAeHM BO
Ts~ensT8 XXXVII
TAUI XXXVII 1 C04PJ HIMT( 3[JIf 10 I1RICAHCKMH UIENM
HA ICOJ) ( TaDTop_Jan bullbull r J ) ( nn )
JCU JClS JCl9 JesIi-flt La U
c III 107 150 211 212
114 5 4l 59 77 12
s 7 5 bullbull 99 119 142
E 111 117 193 20 160
n 07 0 7 160 110
Yb 20 1 23 33 25
L 010 039 034 051 030
LaS I bullbull 11l 5 12 73
LaY II 393 US 296 lbnIYb
Q 153 1 197 112
JEt 2572 228 3013 COIl 4117
cY 0
20 272 57 76 n
)60 KbullbullpIIT OA _CTO CTpa oI lCobullbullbullocuu
n kbullbullbullbull bull J o OA A bull ollopo
ole) bullbull T-T all J Ia CTp KoaJ bullbull
Je19 nur J OA KOlj bullbull
ole nTII 0 AM na01bullbullbull
OA ASASHSTB TS~Sn8 CS rnSAB AeKB BO B1nKSKCKBTS CTSHH HB Ko~
Un8HHR8 BUSUe pSnBTHBHO roneuo 0~Or8TYBSS HB COAPZMHBTS H8 PSTKMT(
asujH M TOB 0~Or8T1BBS BORSKOR TRUOSM HS CTeHH B3HeC1BS ~PR R
418 nnu OA ApyrB CTPBHS BO~1nKBHcKRTS CTeHB HS KozyW RUSUS ronashy
uo 0~or8T1Base H8 nSCHHTS peTKR asujH 3s CTsnSHOT H8 o~orsTYBsST( ~
H8 nSCHHTS PSTKH aeuja CnyH OAHOCOT uoust1 nBHTBHOT R HTSp~j1KOT
PenBTRBKo roneUOTO 0~OrsTYBs8 H8 neCHRTS PSTKM aeujR KBKO R roneshy
UOTO 0~or8T1B8S HS TBK8 H8peQSKRTS nHn enBUeHTB jSCHO 1K8Z1BB8T
HB ~8KTOT ASK8 UpMUSpHROT USTspHjan BO OCKOBB nOTSKH1B8 OA nOAp8shy
12 13
~jSTS BO 3eujsTs KSne HUaUe roneuo MemSampe Ha uSTepKjsnx on KOHTHshyflHTEPATYPA
HeHTsnHSTS KOpS KropHROT OUOTS~ onHOCHO on rpSH~HOTO nonpa~je
HS KOHTRueaTsnHSTS KOpS bull ropHKOT OMOTS~
OCTUlATM IIKKPO EJIEIIEHTH ARTH3G (1976) BEHAVOIR OF TRACE ELEMENTS DURING MAGMATIC PROCESES
A SUMARY OF THEORETICAL MODELS AND THEIR APLICATION ConprwHSTS HS OCTSHSTKTe UHKpO eneueaTK e nSneHS BO Ts6enSTS 6poj
30ur Research US Geol Survey4p41-47XXXVIII
AUBOIN3 BLANCHETR CADETJP CELETP CHARVETJCHORONOWICZJ
COUSINM AND RAMPNOUX3P ( 1970 ) ESSAI SUR LA GEOLOGIE DES DINAmiddot KBapnaTI4TIof naTMTH ~aTHT-KB3p~~aTHTM RIDES Bul Soc Geol France 12 pl060-1095
ALTHERR KREUZERH WENDII LENZH WAGNERAG KELLERJ
Sc 30 30
Be 1 1 HERREW HONDORFA ( 1982 ) A LATE OLIGOCENE EARLY MIOCENE HIGH
20 TEMPERATURE BELT IN THE ATTIC CICLADYC CRISTALINEPb 200 200 100 COMPLEX (SE PELAGONIAN GRECCE) Geol 3b E23Ga 30 30 40 97-164 Hanover 1982Mo 1 1 3
V 20 100 100 AOKIK ( 1963 ) THE KERSUTITES OND AHYKEARSUTITES FROM ALKALIC Cu ROCK OF 3APAN AND SURROUNDING AREAS 3 bull Petr 4 Zn 20 20
30 100 30 198-210
Co 10 30 30 30 KAPAHATAC bullbull ( 1983 ) CAAPIAJH HEKHX HHKPOEflEHEHATA Y TEPUHJAPHHH
Ni 10 30 30 HArHATHTHHA HCT04Hor AEflA JyrOCflABHJE Y 3ABHCHOCTH O~B 10 30 40 ItHXOeOr rEOTEKTOHCKor nOflOIAJA OTHCaj 143 rnACA CpncIltRg 001 001 001 AKaAeMHje HaYKa 14 YMeTHOCTH K~~9F 900 600 1300
KAPAHATAC bullbull (197~) bullbull rEOXEHHJCKE nETPOflOWKE 14 HETAflOrEHETCKE npOBHH
UHJE KPEAHO-TEPUHJAPHE CTAPOCTH AEflA SAflKAHCKOr nOflYOshysite e1ementi osven Hg se odredeni so semikvantitativna spektroheshy CTPOBA H KAflE A3HJE nOce~Ha M3Aa~a CpncKe AK3AeMHJe mijska analiza (D30nov 1985 ) a Hg e odredena so hemijska metoda HaYKa 14 YHeTHocTH K~Hra ~2 bullbull ( NOzerova 1986 )
KAPAHATAC (1983) OCOSEHOCTH H nOJABYB~HBAItE TEKTOHHKE nn04A Y OSflA
CTH THnA TETHCA reoTeKToHHK3 Ho5 1983On OBSS Ta6ens ee rnens neKs BO BynKSHCK1Te creBB HS Ko~ nnSUHS
Rusue penSTBBRO 06erSTyBSampe as conpzsjoT RS onOBOTO BO onROC RS KARAMATAS (1973) ASSOCIATION OF BASIC AND ULTRAB~SIC( ULTRAMAFIC
RerOBSTS cpenHS BpenHOCT COnpzRHSTS HS 6SKSPOT e RCTO TSKS pensshy ROCKS IN YUGOSLAVIA SectVIMagmatism Volcanism
TRBRO usnKY aroneueRS S aroneueHS e K conprwHSTS HS ypSROT HHTeshy Metamorphism Proc of the X th Conqres CBGA 1973
peCHO e neKS BO BynKsHcKHTe CTeBB HS Ko~ Kusue K pensTHBHo o60rsshy
TyBse BO ConpzKHsTsas 60POT K ~nyOpOT TO jacHo yxa~a Ha 3Rs~eshy
BBeTO HS TaKS Hape~eRsTa eUsHsQBjcKs nHtepeHURjaQRjs
14
SUMr1ARY
MICROELEI1ENTS IN THE VOICANIC ROCKS OF KO~UF 110UNTAIN
BBoev Faculty of Geology ~d Mining Stip
A systematic determination of the content of the microelements and the elements of the rare earths was done for the volcanics of the
Kozuf 110untain
Main characteristic of these volcanic rocks is that they are rich in barium and stroncium as well as the other LIL Large Ion Litophile I
elements
These rocks are also enriched in elements of the group of rare earth~ especially in light rare earths
This is a very important characteristic which basically diferenti _ ates them from other tertiary volcanites in 11acedonia bull
I
15
MmiEPAJIOIHKA CTYJmJA HA ~EHOKmCTAJrnTE 011 BYJIKAHCKt1TE
CTEmi HA KOlKY~ II1IAlOOIA
BBoeB PynspcKo-reonomKH ~sKynTeT - mTHn
OnpenyBs~eTo HS THnOT H xeUH3UOT HS rnSBHHTe KHHepSnH on BynKsHcKHTe CTeHH HS Kozy~ nnSHHHS 6eme pesnH3HpSHO BO nepHonOT HS 1985 ronHHS HS YHHBep3HTeToT BO reTHHreH S non pSKOBonCTBO HS np~purspn BOHrT OnpenyBs~eTo 6eme H3BpmeHO co uouom BS eneKTpOHCKS UHKpOCOHnS on THn ( APJI - CEM )
TIPH OB8S onpenyB~e HS rnSBHHTe UHHepSDK aeueHH ce upHuepo~ on Bsjshya8CTsneHHTe CTeBK BO pSUKHTe BS BYnKSHCKHOT KounneKC HS Kozy~ unSHHHE TIPH oBHe HCnHTyBS~S ce n06HeHK noroneu 6poj BS uonSToaH HO uopsnu OrpSHHqeHOCTS HS npoCTopOT oBneKS ce npKKSZSHH csuo nen on HHB KSKO rnSBHH uHHepsnH BO BynKsHcKHTe CTeHH HS Kozy~ nnSHHHS ce onpeshyneHH nnsrHoKnSCH K-~enncnST nHCKyHH nKpoKceHH OCTSH~HOT nen on CTeH8TS ro qHHH UHKPOKpHCTsneCTSTS OCHoBBS KSCS qHj COCTSB e HCTO TSKS onpeneH HO TOj Hee upenueT HS OBOj Tpyn
TIJIAr~OKJIAC~
TIn8rHoKnSCHTe ce HSj3scTsneHH KKHepsnH BO psuKHTeHS BynKsBcKHTe CTeshyHH HS Kozy~ nnsHHHs THe upBeHcTBeHo ce UOjSByBSST KSKO ~eHOKpHCTsnH
S ce nojsBYBSST H KSKO uHKponHTH BO OCHOBHSTS uscs Tpe6s ns BsuoueshyHSK neKs BO OBOj Tpyn Ke 6HnST UPHKSZSHK CSUO pe3ynTsTHTe n06HeHH co nOKom HS eDKTpoHCKS MHKpO COHns S KHKpO~H3HOBpstcKHTe KspSKTepHCTHKH He ce COCTSBeH nen HS OBOj Tpyn Hs 6S3S HS roneuHoT 6poj HS Kepe~s H3BpmeHH co nouom HS eDeKTpoHcKS KHKpocoHns BO nnSrHOKnSCHTe on Kozyt UDSHHHS ce 3s6eneZBHH TpH cnyshyqSeBH KOH ce onHeCyBSST HS xouoreHHTeTOT HS apHsTs H nHncTpH6y~jsTs
HS uoenHHHTe KounOH8HTH BO HHB
1 Cnyqsj Kors Husue HopusnHs aOHsnHocT onHocHo conpzHHSTS HS KsnaHjyuoT ousrs onejKH on aeHTpsDHHTe nenOBK HS apHsTs KOH uepH~epHshyJSTS S npH TOS pSCTe conpZHHSTS HS sn6HTCKSTS KOUUOHeHTS
2 Cnyqsj Kors HKsue OCUHnsawu BO COCTSBOT BS UDsrHoKnscHTe
bullbull
8 9
TASEnA xxx I II COAPIAJ HA ampAPHJYHOT H CTPO~HJYHOT BO BYnKAHCKHTE CTEHH HA KOllY nIlAHHHA ( nn )
Ho Ba Sr Ho Ba Sr
l1u-35
l1u-35 32 n-I
33
7 nl-I
28 I
18
10 20
27
29-1
HaK-31
25 n-2
19 22
29
1851 1806
1983 1983 1823
1937 1588
1571 15~6
1456
1596 1706
1315 162lt
1650 1489
1745
1536 1619
1577
117~
1365 127~
13H
20 1265 12 38
II 78 II 27
81 1191 1187
1353 II 80
46 1281
IH9
1198 1222
1173
l1u-3 27 11 -1
9 15 lI-6
11 -~
5 31
13 ny-I
30 6
MaK-32
HaK-30 ny-2
26 21
lI-3
1539
1315 2332 16~7
1620 1810 22~9
1605 2019 1518
1653 1772 1795 1727 1828
1851
1537 153 I
1723
~ I
930
71i
50 1029 1068 125~
81 1285 ~ I
950 1227 1292
59 1282
1320
75 IH6
86
AHanM3MTe ce BDweHM BO MHCTMTYTOT aa reoxeMMja M KMHeoanorMja nOM ~KaAeMMjaTa Ha HaYKMTe Ha CoaeTCKMOT CojY3 HOCX8a ( 1985 J( lIJoHoa HeToAa - PeHTreHo nygDeC~eHTHa ~ KBaHTMTaTMBHa
lI TAnJlA XtXLl toAI HA llHKOJOT bull M05MJ) 1ltUYHOT
to UJIlCAHun CTEMM itA KOX naAMNIt
MI 0 bullbull lib Of 0 bullbull JIb
ny- SI Ja na 17 II 55 d2 5a a1 ll adO a 5 a
1116 5 JU n-1 10 ftmiddot 16 0 ISO
11 51 77 1middot6 ft- UO
JIH I JU1 7J JU1 I
I I 5 150 110
~ I I I
T
I
I l no II
J 110 10 0 100 dSI
Na]] 110 7 5 IllS I
110
110 10 )2 210 bull II 0 5 no n 110 I-J 0
lSO
J 0 co nmiddot o yobullbull~bullbullshy~o ~~omiddot (a~n 1IS ) llrEM Alt eterRoc
xJOT bullbullbullbullbullbullbullbull co TClCa AICTII bullbull HaTobullbull CHlIIan_ac 1la
AHanSBTW~KBTe UO~STO~H 3S 60~PXBHSTS HS URPKOHHjYHOT HB06HjygOT R
XS~HHjygOT BO BynKsHCKBTe CTeHH HS Kozyt unSHRBS ce ~S~eHB BO
Ts6enSTS XXXIV O~ OBSS Ts6ens ce rne~s ~eKS CO~PZHHSTS HS UHPKOHH
jygOT BO BynK8HcxHTe CTeHR HS Ko~ ce ~BBXB BO rpSHR~Te HS 100
DS ~o 290 DDH a CO~PZHHSTS Ha HB06BjYUOT BO rpSH~Te HS 1 us ~o
11 DUM ~S~HBjyKOT ce ~BHZB BO rpSHUUWTe HS 54 us ~o 89 nnM
reHepsnHo rne~aHO co~pZWHaTS HS UWPKOHBjyKOT BO BynKsHcxHTe CTSH~
HS Kozyt e penSTRBHO roneMS S CO~PZBHSTS Ha HR06wjyKOT e aHOManRO
RBCKS BO O~ROC HS Co~pZHHaTS HS HB06HjYMOT W UWPKOHHjygOT BO~BqHR
CTeHH BO 3eMjRHsTs KOpS
10
ElIEUEHTH Ol IPYIJATA IrA PETIltH 3E11n1
OA eneUeHTaTe HS rpynsTB peTKH asujB BO BynKBHcKHTe CTeHH H8 Kozy~ UnSHHH8 ce OApeAsHB aTpKjYUOT nBHTBHOT QepBjYUOT H~OnHjYUOT
CBU8PHjYUOT eyppUHjYUOT TSP~HjYUOT HTSP~BjYUOT nyTeQHjYVOT
OBMS SnSUSHTB CS OApeAeHK co uouom H8 HB1TPOHCK8 8KTHB8QHOHB USTOshy
8 a HTPMj1uOT e OAPSASR co pSHTrSHO tn10pSCQeHTHB ueTOAB
COAepZHH8TB HB BTPKj1UOT BO B1nKBHCKBTS CTSbullbull H8 KozyW unBHHH8 S 8AeHB BO T8~snBT8 xxxvi
TAUDA IIXVI COIfAJ tIA ITPUYIIOT 10 UlKAMCUTI eTlN IIA ItO nnWHA (fin-)
Hbullbull IT_Jy H bull bull IIDII1middot
u 1-3 Il alllH 7 U ) l2 -)) 31
27 JZ -1 ZI n-I
23 Jl 1$ 5 7 7A-6 ZI nl- 23-III I
1$
23 31 JZ II 1$ 13
Zlr-I 5 2 7
76 5 U JZ bullbull -)2 7 alll-) 1 II bullbull -)0 5 n-z 21 1$ 3 n- 2l
2 ZI 5
AtI~1 ca ~ lIeTTIITo rJ raollbullbullbullJa
np Al bull HY_TO bullbull cbullbullbull COT CoJy O RoCII bullbull aJolllbullbullbull5 l TO bullbullrabullbullbullIIYOlllaCbullbull bullbull ( bullbullbull1oI0fG )
O OB8~ T8~en8 ce rnSAB ASK8 COAPZMH8T8 H8 HTPKj1UOT BO~K8HCKHTS CTSHH H8 Ko~ CS ABHZK BO rp8HMQRTe H8 25 uuu a T8B Bse RSKOj8
11
8HOU8nHOCT BO OAHOC HS COAPZRRBT8 HB HTPRj1uoT BO CnMQHH CTSHR OA
asujRHsTS KOpS
nOASTO~TS 3S COAPZMH8TS HS OCT8H8THTe PSTKH asujH ce ABAeHM BO
Ts~ensT8 XXXVII
TAUI XXXVII 1 C04PJ HIMT( 3[JIf 10 I1RICAHCKMH UIENM
HA ICOJ) ( TaDTop_Jan bullbull r J ) ( nn )
JCU JClS JCl9 JesIi-flt La U
c III 107 150 211 212
114 5 4l 59 77 12
s 7 5 bullbull 99 119 142
E 111 117 193 20 160
n 07 0 7 160 110
Yb 20 1 23 33 25
L 010 039 034 051 030
LaS I bullbull 11l 5 12 73
LaY II 393 US 296 lbnIYb
Q 153 1 197 112
JEt 2572 228 3013 COIl 4117
cY 0
20 272 57 76 n
)60 KbullbullpIIT OA _CTO CTpa oI lCobullbullbullocuu
n kbullbullbullbull bull J o OA A bull ollopo
ole) bullbull T-T all J Ia CTp KoaJ bullbull
Je19 nur J OA KOlj bullbull
ole nTII 0 AM na01bullbullbull
OA ASASHSTB TS~Sn8 CS rnSAB AeKB BO B1nKSKCKBTS CTSHH HB Ko~
Un8HHR8 BUSUe pSnBTHBHO roneuo 0~Or8TYBSS HB COAPZMHBTS H8 PSTKMT(
asujH M TOB 0~Or8T1BBS BORSKOR TRUOSM HS CTeHH B3HeC1BS ~PR R
418 nnu OA ApyrB CTPBHS BO~1nKBHcKRTS CTeHB HS KozyW RUSUS ronashy
uo 0~or8T1Base H8 nSCHHTS peTKR asujH 3s CTsnSHOT H8 o~orsTYBsST( ~
H8 nSCHHTS PSTKH aeuja CnyH OAHOCOT uoust1 nBHTBHOT R HTSp~j1KOT
PenBTRBKo roneUOTO 0~OrsTYBs8 H8 neCHRTS PSTKM aeujR KBKO R roneshy
UOTO 0~or8T1B8S HS TBK8 H8peQSKRTS nHn enBUeHTB jSCHO 1K8Z1BB8T
HB ~8KTOT ASK8 UpMUSpHROT USTspHjan BO OCKOBB nOTSKH1B8 OA nOAp8shy
12 13
~jSTS BO 3eujsTs KSne HUaUe roneuo MemSampe Ha uSTepKjsnx on KOHTHshyflHTEPATYPA
HeHTsnHSTS KOpS KropHROT OUOTS~ onHOCHO on rpSH~HOTO nonpa~je
HS KOHTRueaTsnHSTS KOpS bull ropHKOT OMOTS~
OCTUlATM IIKKPO EJIEIIEHTH ARTH3G (1976) BEHAVOIR OF TRACE ELEMENTS DURING MAGMATIC PROCESES
A SUMARY OF THEORETICAL MODELS AND THEIR APLICATION ConprwHSTS HS OCTSHSTKTe UHKpO eneueaTK e nSneHS BO Ts6enSTS 6poj
30ur Research US Geol Survey4p41-47XXXVIII
AUBOIN3 BLANCHETR CADETJP CELETP CHARVETJCHORONOWICZJ
COUSINM AND RAMPNOUX3P ( 1970 ) ESSAI SUR LA GEOLOGIE DES DINAmiddot KBapnaTI4TIof naTMTH ~aTHT-KB3p~~aTHTM RIDES Bul Soc Geol France 12 pl060-1095
ALTHERR KREUZERH WENDII LENZH WAGNERAG KELLERJ
Sc 30 30
Be 1 1 HERREW HONDORFA ( 1982 ) A LATE OLIGOCENE EARLY MIOCENE HIGH
20 TEMPERATURE BELT IN THE ATTIC CICLADYC CRISTALINEPb 200 200 100 COMPLEX (SE PELAGONIAN GRECCE) Geol 3b E23Ga 30 30 40 97-164 Hanover 1982Mo 1 1 3
V 20 100 100 AOKIK ( 1963 ) THE KERSUTITES OND AHYKEARSUTITES FROM ALKALIC Cu ROCK OF 3APAN AND SURROUNDING AREAS 3 bull Petr 4 Zn 20 20
30 100 30 198-210
Co 10 30 30 30 KAPAHATAC bullbull ( 1983 ) CAAPIAJH HEKHX HHKPOEflEHEHATA Y TEPUHJAPHHH
Ni 10 30 30 HArHATHTHHA HCT04Hor AEflA JyrOCflABHJE Y 3ABHCHOCTH O~B 10 30 40 ItHXOeOr rEOTEKTOHCKor nOflOIAJA OTHCaj 143 rnACA CpncIltRg 001 001 001 AKaAeMHje HaYKa 14 YMeTHOCTH K~~9F 900 600 1300
KAPAHATAC bullbull (197~) bullbull rEOXEHHJCKE nETPOflOWKE 14 HETAflOrEHETCKE npOBHH
UHJE KPEAHO-TEPUHJAPHE CTAPOCTH AEflA SAflKAHCKOr nOflYOshysite e1ementi osven Hg se odredeni so semikvantitativna spektroheshy CTPOBA H KAflE A3HJE nOce~Ha M3Aa~a CpncKe AK3AeMHJe mijska analiza (D30nov 1985 ) a Hg e odredena so hemijska metoda HaYKa 14 YHeTHocTH K~Hra ~2 bullbull ( NOzerova 1986 )
KAPAHATAC (1983) OCOSEHOCTH H nOJABYB~HBAItE TEKTOHHKE nn04A Y OSflA
CTH THnA TETHCA reoTeKToHHK3 Ho5 1983On OBSS Ta6ens ee rnens neKs BO BynKSHCK1Te creBB HS Ko~ nnSUHS
Rusue penSTBBRO 06erSTyBSampe as conpzsjoT RS onOBOTO BO onROC RS KARAMATAS (1973) ASSOCIATION OF BASIC AND ULTRAB~SIC( ULTRAMAFIC
RerOBSTS cpenHS BpenHOCT COnpzRHSTS HS 6SKSPOT e RCTO TSKS pensshy ROCKS IN YUGOSLAVIA SectVIMagmatism Volcanism
TRBRO usnKY aroneueRS S aroneueHS e K conprwHSTS HS ypSROT HHTeshy Metamorphism Proc of the X th Conqres CBGA 1973
peCHO e neKS BO BynKsHcKHTe CTeBB HS Ko~ Kusue K pensTHBHo o60rsshy
TyBse BO ConpzKHsTsas 60POT K ~nyOpOT TO jacHo yxa~a Ha 3Rs~eshy
BBeTO HS TaKS Hape~eRsTa eUsHsQBjcKs nHtepeHURjaQRjs
14
SUMr1ARY
MICROELEI1ENTS IN THE VOICANIC ROCKS OF KO~UF 110UNTAIN
BBoev Faculty of Geology ~d Mining Stip
A systematic determination of the content of the microelements and the elements of the rare earths was done for the volcanics of the
Kozuf 110untain
Main characteristic of these volcanic rocks is that they are rich in barium and stroncium as well as the other LIL Large Ion Litophile I
elements
These rocks are also enriched in elements of the group of rare earth~ especially in light rare earths
This is a very important characteristic which basically diferenti _ ates them from other tertiary volcanites in 11acedonia bull
I
15
MmiEPAJIOIHKA CTYJmJA HA ~EHOKmCTAJrnTE 011 BYJIKAHCKt1TE
CTEmi HA KOlKY~ II1IAlOOIA
BBoeB PynspcKo-reonomKH ~sKynTeT - mTHn
OnpenyBs~eTo HS THnOT H xeUH3UOT HS rnSBHHTe KHHepSnH on BynKsHcKHTe CTeHH HS Kozy~ nnSHHHS 6eme pesnH3HpSHO BO nepHonOT HS 1985 ronHHS HS YHHBep3HTeToT BO reTHHreH S non pSKOBonCTBO HS np~purspn BOHrT OnpenyBs~eTo 6eme H3BpmeHO co uouom BS eneKTpOHCKS UHKpOCOHnS on THn ( APJI - CEM )
TIPH OB8S onpenyB~e HS rnSBHHTe UHHepSDK aeueHH ce upHuepo~ on Bsjshya8CTsneHHTe CTeBK BO pSUKHTe BS BYnKSHCKHOT KounneKC HS Kozy~ unSHHHE TIPH oBHe HCnHTyBS~S ce n06HeHK noroneu 6poj BS uonSToaH HO uopsnu OrpSHHqeHOCTS HS npoCTopOT oBneKS ce npKKSZSHH csuo nen on HHB KSKO rnSBHH uHHepsnH BO BynKsHcKHTe CTeHH HS Kozy~ nnSHHHS ce onpeshyneHH nnsrHoKnSCH K-~enncnST nHCKyHH nKpoKceHH OCTSH~HOT nen on CTeH8TS ro qHHH UHKPOKpHCTsneCTSTS OCHoBBS KSCS qHj COCTSB e HCTO TSKS onpeneH HO TOj Hee upenueT HS OBOj Tpyn
TIJIAr~OKJIAC~
TIn8rHoKnSCHTe ce HSj3scTsneHH KKHepsnH BO psuKHTeHS BynKsBcKHTe CTeshyHH HS Kozy~ nnsHHHs THe upBeHcTBeHo ce UOjSByBSST KSKO ~eHOKpHCTsnH
S ce nojsBYBSST H KSKO uHKponHTH BO OCHOBHSTS uscs Tpe6s ns BsuoueshyHSK neKs BO OBOj Tpyn Ke 6HnST UPHKSZSHK CSUO pe3ynTsTHTe n06HeHH co nOKom HS eDKTpoHCKS MHKpO COHns S KHKpO~H3HOBpstcKHTe KspSKTepHCTHKH He ce COCTSBeH nen HS OBOj Tpyn Hs 6S3S HS roneuHoT 6poj HS Kepe~s H3BpmeHH co nouom HS eDeKTpoHcKS KHKpocoHns BO nnSrHOKnSCHTe on Kozyt UDSHHHS ce 3s6eneZBHH TpH cnyshyqSeBH KOH ce onHeCyBSST HS xouoreHHTeTOT HS apHsTs H nHncTpH6y~jsTs
HS uoenHHHTe KounOH8HTH BO HHB
1 Cnyqsj Kors Husue HopusnHs aOHsnHocT onHocHo conpzHHSTS HS KsnaHjyuoT ousrs onejKH on aeHTpsDHHTe nenOBK HS apHsTs KOH uepH~epHshyJSTS S npH TOS pSCTe conpZHHSTS HS sn6HTCKSTS KOUUOHeHTS
2 Cnyqsj Kors HKsue OCUHnsawu BO COCTSBOT BS UDsrHoKnscHTe
10
ElIEUEHTH Ol IPYIJATA IrA PETIltH 3E11n1
OA eneUeHTaTe HS rpynsTB peTKH asujB BO BynKBHcKHTe CTeHH H8 Kozy~ UnSHHH8 ce OApeAsHB aTpKjYUOT nBHTBHOT QepBjYUOT H~OnHjYUOT
CBU8PHjYUOT eyppUHjYUOT TSP~HjYUOT HTSP~BjYUOT nyTeQHjYVOT
OBMS SnSUSHTB CS OApeAeHK co uouom H8 HB1TPOHCK8 8KTHB8QHOHB USTOshy
8 a HTPMj1uOT e OAPSASR co pSHTrSHO tn10pSCQeHTHB ueTOAB
COAepZHH8TB HB BTPKj1UOT BO B1nKBHCKBTS CTSbullbull H8 KozyW unBHHH8 S 8AeHB BO T8~snBT8 xxxvi
TAUDA IIXVI COIfAJ tIA ITPUYIIOT 10 UlKAMCUTI eTlN IIA ItO nnWHA (fin-)
Hbullbull IT_Jy H bull bull IIDII1middot
u 1-3 Il alllH 7 U ) l2 -)) 31
27 JZ -1 ZI n-I
23 Jl 1$ 5 7 7A-6 ZI nl- 23-III I
1$
23 31 JZ II 1$ 13
Zlr-I 5 2 7
76 5 U JZ bullbull -)2 7 alll-) 1 II bullbull -)0 5 n-z 21 1$ 3 n- 2l
2 ZI 5
AtI~1 ca ~ lIeTTIITo rJ raollbullbullbullJa
np Al bull HY_TO bullbull cbullbullbull COT CoJy O RoCII bullbull aJolllbullbullbull5 l TO bullbullrabullbullbullIIYOlllaCbullbull bullbull ( bullbullbull1oI0fG )
O OB8~ T8~en8 ce rnSAB ASK8 COAPZMH8T8 H8 HTPKj1UOT BO~K8HCKHTS CTSHH H8 Ko~ CS ABHZK BO rp8HMQRTe H8 25 uuu a T8B Bse RSKOj8
11
8HOU8nHOCT BO OAHOC HS COAPZRRBT8 HB HTPRj1uoT BO CnMQHH CTSHR OA
asujRHsTS KOpS
nOASTO~TS 3S COAPZMH8TS HS OCT8H8THTe PSTKH asujH ce ABAeHM BO
Ts~ensT8 XXXVII
TAUI XXXVII 1 C04PJ HIMT( 3[JIf 10 I1RICAHCKMH UIENM
HA ICOJ) ( TaDTop_Jan bullbull r J ) ( nn )
JCU JClS JCl9 JesIi-flt La U
c III 107 150 211 212
114 5 4l 59 77 12
s 7 5 bullbull 99 119 142
E 111 117 193 20 160
n 07 0 7 160 110
Yb 20 1 23 33 25
L 010 039 034 051 030
LaS I bullbull 11l 5 12 73
LaY II 393 US 296 lbnIYb
Q 153 1 197 112
JEt 2572 228 3013 COIl 4117
cY 0
20 272 57 76 n
)60 KbullbullpIIT OA _CTO CTpa oI lCobullbullbullocuu
n kbullbullbullbull bull J o OA A bull ollopo
ole) bullbull T-T all J Ia CTp KoaJ bullbull
Je19 nur J OA KOlj bullbull
ole nTII 0 AM na01bullbullbull
OA ASASHSTB TS~Sn8 CS rnSAB AeKB BO B1nKSKCKBTS CTSHH HB Ko~
Un8HHR8 BUSUe pSnBTHBHO roneuo 0~Or8TYBSS HB COAPZMHBTS H8 PSTKMT(
asujH M TOB 0~Or8T1BBS BORSKOR TRUOSM HS CTeHH B3HeC1BS ~PR R
418 nnu OA ApyrB CTPBHS BO~1nKBHcKRTS CTeHB HS KozyW RUSUS ronashy
uo 0~or8T1Base H8 nSCHHTS peTKR asujH 3s CTsnSHOT H8 o~orsTYBsST( ~
H8 nSCHHTS PSTKH aeuja CnyH OAHOCOT uoust1 nBHTBHOT R HTSp~j1KOT
PenBTRBKo roneUOTO 0~OrsTYBs8 H8 neCHRTS PSTKM aeujR KBKO R roneshy
UOTO 0~or8T1B8S HS TBK8 H8peQSKRTS nHn enBUeHTB jSCHO 1K8Z1BB8T
HB ~8KTOT ASK8 UpMUSpHROT USTspHjan BO OCKOBB nOTSKH1B8 OA nOAp8shy
12 13
~jSTS BO 3eujsTs KSne HUaUe roneuo MemSampe Ha uSTepKjsnx on KOHTHshyflHTEPATYPA
HeHTsnHSTS KOpS KropHROT OUOTS~ onHOCHO on rpSH~HOTO nonpa~je
HS KOHTRueaTsnHSTS KOpS bull ropHKOT OMOTS~
OCTUlATM IIKKPO EJIEIIEHTH ARTH3G (1976) BEHAVOIR OF TRACE ELEMENTS DURING MAGMATIC PROCESES
A SUMARY OF THEORETICAL MODELS AND THEIR APLICATION ConprwHSTS HS OCTSHSTKTe UHKpO eneueaTK e nSneHS BO Ts6enSTS 6poj
30ur Research US Geol Survey4p41-47XXXVIII
AUBOIN3 BLANCHETR CADETJP CELETP CHARVETJCHORONOWICZJ
COUSINM AND RAMPNOUX3P ( 1970 ) ESSAI SUR LA GEOLOGIE DES DINAmiddot KBapnaTI4TIof naTMTH ~aTHT-KB3p~~aTHTM RIDES Bul Soc Geol France 12 pl060-1095
ALTHERR KREUZERH WENDII LENZH WAGNERAG KELLERJ
Sc 30 30
Be 1 1 HERREW HONDORFA ( 1982 ) A LATE OLIGOCENE EARLY MIOCENE HIGH
20 TEMPERATURE BELT IN THE ATTIC CICLADYC CRISTALINEPb 200 200 100 COMPLEX (SE PELAGONIAN GRECCE) Geol 3b E23Ga 30 30 40 97-164 Hanover 1982Mo 1 1 3
V 20 100 100 AOKIK ( 1963 ) THE KERSUTITES OND AHYKEARSUTITES FROM ALKALIC Cu ROCK OF 3APAN AND SURROUNDING AREAS 3 bull Petr 4 Zn 20 20
30 100 30 198-210
Co 10 30 30 30 KAPAHATAC bullbull ( 1983 ) CAAPIAJH HEKHX HHKPOEflEHEHATA Y TEPUHJAPHHH
Ni 10 30 30 HArHATHTHHA HCT04Hor AEflA JyrOCflABHJE Y 3ABHCHOCTH O~B 10 30 40 ItHXOeOr rEOTEKTOHCKor nOflOIAJA OTHCaj 143 rnACA CpncIltRg 001 001 001 AKaAeMHje HaYKa 14 YMeTHOCTH K~~9F 900 600 1300
KAPAHATAC bullbull (197~) bullbull rEOXEHHJCKE nETPOflOWKE 14 HETAflOrEHETCKE npOBHH
UHJE KPEAHO-TEPUHJAPHE CTAPOCTH AEflA SAflKAHCKOr nOflYOshysite e1ementi osven Hg se odredeni so semikvantitativna spektroheshy CTPOBA H KAflE A3HJE nOce~Ha M3Aa~a CpncKe AK3AeMHJe mijska analiza (D30nov 1985 ) a Hg e odredena so hemijska metoda HaYKa 14 YHeTHocTH K~Hra ~2 bullbull ( NOzerova 1986 )
KAPAHATAC (1983) OCOSEHOCTH H nOJABYB~HBAItE TEKTOHHKE nn04A Y OSflA
CTH THnA TETHCA reoTeKToHHK3 Ho5 1983On OBSS Ta6ens ee rnens neKs BO BynKSHCK1Te creBB HS Ko~ nnSUHS
Rusue penSTBBRO 06erSTyBSampe as conpzsjoT RS onOBOTO BO onROC RS KARAMATAS (1973) ASSOCIATION OF BASIC AND ULTRAB~SIC( ULTRAMAFIC
RerOBSTS cpenHS BpenHOCT COnpzRHSTS HS 6SKSPOT e RCTO TSKS pensshy ROCKS IN YUGOSLAVIA SectVIMagmatism Volcanism
TRBRO usnKY aroneueRS S aroneueHS e K conprwHSTS HS ypSROT HHTeshy Metamorphism Proc of the X th Conqres CBGA 1973
peCHO e neKS BO BynKsHcKHTe CTeBB HS Ko~ Kusue K pensTHBHo o60rsshy
TyBse BO ConpzKHsTsas 60POT K ~nyOpOT TO jacHo yxa~a Ha 3Rs~eshy
BBeTO HS TaKS Hape~eRsTa eUsHsQBjcKs nHtepeHURjaQRjs
14
SUMr1ARY
MICROELEI1ENTS IN THE VOICANIC ROCKS OF KO~UF 110UNTAIN
BBoev Faculty of Geology ~d Mining Stip
A systematic determination of the content of the microelements and the elements of the rare earths was done for the volcanics of the
Kozuf 110untain
Main characteristic of these volcanic rocks is that they are rich in barium and stroncium as well as the other LIL Large Ion Litophile I
elements
These rocks are also enriched in elements of the group of rare earth~ especially in light rare earths
This is a very important characteristic which basically diferenti _ ates them from other tertiary volcanites in 11acedonia bull
I
15
MmiEPAJIOIHKA CTYJmJA HA ~EHOKmCTAJrnTE 011 BYJIKAHCKt1TE
CTEmi HA KOlKY~ II1IAlOOIA
BBoeB PynspcKo-reonomKH ~sKynTeT - mTHn
OnpenyBs~eTo HS THnOT H xeUH3UOT HS rnSBHHTe KHHepSnH on BynKsHcKHTe CTeHH HS Kozy~ nnSHHHS 6eme pesnH3HpSHO BO nepHonOT HS 1985 ronHHS HS YHHBep3HTeToT BO reTHHreH S non pSKOBonCTBO HS np~purspn BOHrT OnpenyBs~eTo 6eme H3BpmeHO co uouom BS eneKTpOHCKS UHKpOCOHnS on THn ( APJI - CEM )
TIPH OB8S onpenyB~e HS rnSBHHTe UHHepSDK aeueHH ce upHuepo~ on Bsjshya8CTsneHHTe CTeBK BO pSUKHTe BS BYnKSHCKHOT KounneKC HS Kozy~ unSHHHE TIPH oBHe HCnHTyBS~S ce n06HeHK noroneu 6poj BS uonSToaH HO uopsnu OrpSHHqeHOCTS HS npoCTopOT oBneKS ce npKKSZSHH csuo nen on HHB KSKO rnSBHH uHHepsnH BO BynKsHcKHTe CTeHH HS Kozy~ nnSHHHS ce onpeshyneHH nnsrHoKnSCH K-~enncnST nHCKyHH nKpoKceHH OCTSH~HOT nen on CTeH8TS ro qHHH UHKPOKpHCTsneCTSTS OCHoBBS KSCS qHj COCTSB e HCTO TSKS onpeneH HO TOj Hee upenueT HS OBOj Tpyn
TIJIAr~OKJIAC~
TIn8rHoKnSCHTe ce HSj3scTsneHH KKHepsnH BO psuKHTeHS BynKsBcKHTe CTeshyHH HS Kozy~ nnsHHHs THe upBeHcTBeHo ce UOjSByBSST KSKO ~eHOKpHCTsnH
S ce nojsBYBSST H KSKO uHKponHTH BO OCHOBHSTS uscs Tpe6s ns BsuoueshyHSK neKs BO OBOj Tpyn Ke 6HnST UPHKSZSHK CSUO pe3ynTsTHTe n06HeHH co nOKom HS eDKTpoHCKS MHKpO COHns S KHKpO~H3HOBpstcKHTe KspSKTepHCTHKH He ce COCTSBeH nen HS OBOj Tpyn Hs 6S3S HS roneuHoT 6poj HS Kepe~s H3BpmeHH co nouom HS eDeKTpoHcKS KHKpocoHns BO nnSrHOKnSCHTe on Kozyt UDSHHHS ce 3s6eneZBHH TpH cnyshyqSeBH KOH ce onHeCyBSST HS xouoreHHTeTOT HS apHsTs H nHncTpH6y~jsTs
HS uoenHHHTe KounOH8HTH BO HHB
1 Cnyqsj Kors Husue HopusnHs aOHsnHocT onHocHo conpzHHSTS HS KsnaHjyuoT ousrs onejKH on aeHTpsDHHTe nenOBK HS apHsTs KOH uepH~epHshyJSTS S npH TOS pSCTe conpZHHSTS HS sn6HTCKSTS KOUUOHeHTS
2 Cnyqsj Kors HKsue OCUHnsawu BO COCTSBOT BS UDsrHoKnscHTe
12 13
~jSTS BO 3eujsTs KSne HUaUe roneuo MemSampe Ha uSTepKjsnx on KOHTHshyflHTEPATYPA
HeHTsnHSTS KOpS KropHROT OUOTS~ onHOCHO on rpSH~HOTO nonpa~je
HS KOHTRueaTsnHSTS KOpS bull ropHKOT OMOTS~
OCTUlATM IIKKPO EJIEIIEHTH ARTH3G (1976) BEHAVOIR OF TRACE ELEMENTS DURING MAGMATIC PROCESES
A SUMARY OF THEORETICAL MODELS AND THEIR APLICATION ConprwHSTS HS OCTSHSTKTe UHKpO eneueaTK e nSneHS BO Ts6enSTS 6poj
30ur Research US Geol Survey4p41-47XXXVIII
AUBOIN3 BLANCHETR CADETJP CELETP CHARVETJCHORONOWICZJ
COUSINM AND RAMPNOUX3P ( 1970 ) ESSAI SUR LA GEOLOGIE DES DINAmiddot KBapnaTI4TIof naTMTH ~aTHT-KB3p~~aTHTM RIDES Bul Soc Geol France 12 pl060-1095
ALTHERR KREUZERH WENDII LENZH WAGNERAG KELLERJ
Sc 30 30
Be 1 1 HERREW HONDORFA ( 1982 ) A LATE OLIGOCENE EARLY MIOCENE HIGH
20 TEMPERATURE BELT IN THE ATTIC CICLADYC CRISTALINEPb 200 200 100 COMPLEX (SE PELAGONIAN GRECCE) Geol 3b E23Ga 30 30 40 97-164 Hanover 1982Mo 1 1 3
V 20 100 100 AOKIK ( 1963 ) THE KERSUTITES OND AHYKEARSUTITES FROM ALKALIC Cu ROCK OF 3APAN AND SURROUNDING AREAS 3 bull Petr 4 Zn 20 20
30 100 30 198-210
Co 10 30 30 30 KAPAHATAC bullbull ( 1983 ) CAAPIAJH HEKHX HHKPOEflEHEHATA Y TEPUHJAPHHH
Ni 10 30 30 HArHATHTHHA HCT04Hor AEflA JyrOCflABHJE Y 3ABHCHOCTH O~B 10 30 40 ItHXOeOr rEOTEKTOHCKor nOflOIAJA OTHCaj 143 rnACA CpncIltRg 001 001 001 AKaAeMHje HaYKa 14 YMeTHOCTH K~~9F 900 600 1300
KAPAHATAC bullbull (197~) bullbull rEOXEHHJCKE nETPOflOWKE 14 HETAflOrEHETCKE npOBHH
UHJE KPEAHO-TEPUHJAPHE CTAPOCTH AEflA SAflKAHCKOr nOflYOshysite e1ementi osven Hg se odredeni so semikvantitativna spektroheshy CTPOBA H KAflE A3HJE nOce~Ha M3Aa~a CpncKe AK3AeMHJe mijska analiza (D30nov 1985 ) a Hg e odredena so hemijska metoda HaYKa 14 YHeTHocTH K~Hra ~2 bullbull ( NOzerova 1986 )
KAPAHATAC (1983) OCOSEHOCTH H nOJABYB~HBAItE TEKTOHHKE nn04A Y OSflA
CTH THnA TETHCA reoTeKToHHK3 Ho5 1983On OBSS Ta6ens ee rnens neKs BO BynKSHCK1Te creBB HS Ko~ nnSUHS
Rusue penSTBBRO 06erSTyBSampe as conpzsjoT RS onOBOTO BO onROC RS KARAMATAS (1973) ASSOCIATION OF BASIC AND ULTRAB~SIC( ULTRAMAFIC
RerOBSTS cpenHS BpenHOCT COnpzRHSTS HS 6SKSPOT e RCTO TSKS pensshy ROCKS IN YUGOSLAVIA SectVIMagmatism Volcanism
TRBRO usnKY aroneueRS S aroneueHS e K conprwHSTS HS ypSROT HHTeshy Metamorphism Proc of the X th Conqres CBGA 1973
peCHO e neKS BO BynKsHcKHTe CTeBB HS Ko~ Kusue K pensTHBHo o60rsshy
TyBse BO ConpzKHsTsas 60POT K ~nyOpOT TO jacHo yxa~a Ha 3Rs~eshy
BBeTO HS TaKS Hape~eRsTa eUsHsQBjcKs nHtepeHURjaQRjs
14
SUMr1ARY
MICROELEI1ENTS IN THE VOICANIC ROCKS OF KO~UF 110UNTAIN
BBoev Faculty of Geology ~d Mining Stip
A systematic determination of the content of the microelements and the elements of the rare earths was done for the volcanics of the
Kozuf 110untain
Main characteristic of these volcanic rocks is that they are rich in barium and stroncium as well as the other LIL Large Ion Litophile I
elements
These rocks are also enriched in elements of the group of rare earth~ especially in light rare earths
This is a very important characteristic which basically diferenti _ ates them from other tertiary volcanites in 11acedonia bull
I
15
MmiEPAJIOIHKA CTYJmJA HA ~EHOKmCTAJrnTE 011 BYJIKAHCKt1TE
CTEmi HA KOlKY~ II1IAlOOIA
BBoeB PynspcKo-reonomKH ~sKynTeT - mTHn
OnpenyBs~eTo HS THnOT H xeUH3UOT HS rnSBHHTe KHHepSnH on BynKsHcKHTe CTeHH HS Kozy~ nnSHHHS 6eme pesnH3HpSHO BO nepHonOT HS 1985 ronHHS HS YHHBep3HTeToT BO reTHHreH S non pSKOBonCTBO HS np~purspn BOHrT OnpenyBs~eTo 6eme H3BpmeHO co uouom BS eneKTpOHCKS UHKpOCOHnS on THn ( APJI - CEM )
TIPH OB8S onpenyB~e HS rnSBHHTe UHHepSDK aeueHH ce upHuepo~ on Bsjshya8CTsneHHTe CTeBK BO pSUKHTe BS BYnKSHCKHOT KounneKC HS Kozy~ unSHHHE TIPH oBHe HCnHTyBS~S ce n06HeHK noroneu 6poj BS uonSToaH HO uopsnu OrpSHHqeHOCTS HS npoCTopOT oBneKS ce npKKSZSHH csuo nen on HHB KSKO rnSBHH uHHepsnH BO BynKsHcKHTe CTeHH HS Kozy~ nnSHHHS ce onpeshyneHH nnsrHoKnSCH K-~enncnST nHCKyHH nKpoKceHH OCTSH~HOT nen on CTeH8TS ro qHHH UHKPOKpHCTsneCTSTS OCHoBBS KSCS qHj COCTSB e HCTO TSKS onpeneH HO TOj Hee upenueT HS OBOj Tpyn
TIJIAr~OKJIAC~
TIn8rHoKnSCHTe ce HSj3scTsneHH KKHepsnH BO psuKHTeHS BynKsBcKHTe CTeshyHH HS Kozy~ nnsHHHs THe upBeHcTBeHo ce UOjSByBSST KSKO ~eHOKpHCTsnH
S ce nojsBYBSST H KSKO uHKponHTH BO OCHOBHSTS uscs Tpe6s ns BsuoueshyHSK neKs BO OBOj Tpyn Ke 6HnST UPHKSZSHK CSUO pe3ynTsTHTe n06HeHH co nOKom HS eDKTpoHCKS MHKpO COHns S KHKpO~H3HOBpstcKHTe KspSKTepHCTHKH He ce COCTSBeH nen HS OBOj Tpyn Hs 6S3S HS roneuHoT 6poj HS Kepe~s H3BpmeHH co nouom HS eDeKTpoHcKS KHKpocoHns BO nnSrHOKnSCHTe on Kozyt UDSHHHS ce 3s6eneZBHH TpH cnyshyqSeBH KOH ce onHeCyBSST HS xouoreHHTeTOT HS apHsTs H nHncTpH6y~jsTs
HS uoenHHHTe KounOH8HTH BO HHB
1 Cnyqsj Kors Husue HopusnHs aOHsnHocT onHocHo conpzHHSTS HS KsnaHjyuoT ousrs onejKH on aeHTpsDHHTe nenOBK HS apHsTs KOH uepH~epHshyJSTS S npH TOS pSCTe conpZHHSTS HS sn6HTCKSTS KOUUOHeHTS
2 Cnyqsj Kors HKsue OCUHnsawu BO COCTSBOT BS UDsrHoKnscHTe
14
SUMr1ARY
MICROELEI1ENTS IN THE VOICANIC ROCKS OF KO~UF 110UNTAIN
BBoev Faculty of Geology ~d Mining Stip
A systematic determination of the content of the microelements and the elements of the rare earths was done for the volcanics of the
Kozuf 110untain
Main characteristic of these volcanic rocks is that they are rich in barium and stroncium as well as the other LIL Large Ion Litophile I
elements
These rocks are also enriched in elements of the group of rare earth~ especially in light rare earths
This is a very important characteristic which basically diferenti _ ates them from other tertiary volcanites in 11acedonia bull
I
15
MmiEPAJIOIHKA CTYJmJA HA ~EHOKmCTAJrnTE 011 BYJIKAHCKt1TE
CTEmi HA KOlKY~ II1IAlOOIA
BBoeB PynspcKo-reonomKH ~sKynTeT - mTHn
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