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GSA Data Repository 2017364

Cassiterite U-Pb geochronology constrains magmatic-hydrothermal evolution in

complex evolved granite systems: The classical Erzgebirge tin province (Saxony and

Bohemia)

Rongqing Zhang, Bernd Lehmann, Reimar Seltmann, Weidong Sun, and Congying Li

Deposit and sample characterization

The Sadisdorf Sn-W deposit is situated approximately 12 km NW of Altenberg and 7 km

S of Dippoldiswalde in the German part of the Erzgebirge/Krušne Hory Mts. The deposit is

developed in a small granite stock with an outer phase of monzogranite and inner phase of

albite granite. The country rocks consist of Proterozoic meta-granites and paragneisses. Li-

mica greisen (outer greisen) is fine-grained and developed in the monzogranite and

topaz/quartz greisen (inner greisen) is medium-grained and developed in the albite granite.

The greisen ore body extends up to 400 × 300 m and ranges to 250 m depth. In the upper parts

of the system, Cu mineralization is predominant, deeper is Mo mineralization, and the deepest

part hosts Sn mineralization. Ore minerals are cassiterite, chalcopyrite, molybdenite and

wolframite (Seltmann, 1995; Seltmann et al., 2016). Sample SD-1 (greisen/vein) was

collected from the surface outcrops that formed due to mine collapse of the Sadisdorf Sn

deposit (Figure DR1A). 

The Ehrenfriedersdorf Sn district is located on the northern border of the Erzgebirge,

approximately 70 km SW of Dresden. It is developed in the NW of the Annaberg Anticline in

a flat to medium steep dipping metamorphic series of gneiss and mica schist. The Variscan

granitic intrusions form a four-phase post-kinematic granite complex, consisting mostly of

fine- to coarse-grained porphyritic leucogranites. The Ehrenfriedersdorf deposit comprises

several sub-deposits, i.e., Sauberg, Westfield, Northwestfield, Röhrenbohrer, Greifensteine

South and Neundorf. Vein/stringer ore zones in the exocontact are the most important and are

several meter thick and several hundreds to >1000 m long. They are steeply dipping and

extend to the granite surface. Greisen ore bodies are developed in the granite and

frequently >25 m thick. Minor skarn mineralization with sulfides and cassiterite is located in

the vicinity of the granite. Ore minerals in the veins are mostly cassiterite, wolframite,

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scheelite, molybdenite, arsenopyrite, löllingite, mica, topaz, fluorite, apatite, beryl and triplite.

Greisens are of mica or mica-topaz type, consisting mostly of mica, quartz and topaz with

minor fluorite, triplite, cassiterite, arsenopyrite and molybdenite (Hösel et al., 1994; Seltmann

et al., 2016). Samples E-148 and E-199 (quartz greisen) were collected underground at level 6

of the Sauberg mine in the Ehrenfriedersdorf deposit (Figures DR1B and DR1C). 

The Altenberg Sn deposit is situated on the eastern periphery of Altenberg, 35 km S of

Dresden, ca. 5 km from the German-Czech border. Tin mineralization is developed in the top

zone of the Altenberg granite stock. The peraluminous Li-mica granites of Altenberg intruded

into the Teplice rhyolite and the Altenberg microgranite, which forms the eastern branch of

the Altenberg-Frauenstein microgranite dike system. The Altenberg deposit is hosted by a

greisenized monzogranite stock intruded mainly in Altenberg microgranite (“granite

porphyry”). At the surface, the Altenberg stock has a diameter of about 330 m. The slopes are

steeply dipping with 70-90°. At a depth of 250 m the slopes are flattening so that the granite

stock forms an apical intrusion out of the Schellerhau granite. In the uppermost part the

granite stock is strongly greisenized down to a depth of 200 m. The greisenization is

somewhat excentric to northwest (Seltmann and Schilka, 1995; Romer et al., 2012; Seltmann

et al., 2016). Towards the top of the granite body the dark greisen zones increase in thickness

and frequency up to a compact black or black-green topaz-mica-greisen, consisting of fine-

and medium-grained quartz, dark green lithium biotite, topaz, some fluorite and cassiterite.

Ore minerals include major cassiterite and minor arsenopyrite, löllingite, wolframite,

molybdenite, native bismuth and bismuthinite (Seltmann and Schilka, 1995; Seltmann et al.,

2016). Samples ALT-1 and ALT-2 are from the underground exposures at Sammelrolle 703

and Strecke 3274 (Figures DR1D and DR1E). 

The Zinnwald (Cinovec) Sn-W-Li deposit is located in the eastern Erzgebirge at the

Czech–German border. The Sn-W-Li deposit is spatially associated with the cupola of a Li-F-

rich granite stock which intruded into the Teplice rhyolite and crops out in an elliptical shape

of 1.3 × 0.3 km. The 1596 m deep CS-1 borehole showed that this granite stock consists of

lepidolite1-albite granite, zinnwaldite2 granite and lithian annite granite from shallow to deep                                                                1,2 “lepidolite, zinnwaldite” – Inherited historic field terminology, discredited by IMA (www.mindat.org):

1 Lepidolite: A series of monoclinic Li-rich micas in, or close to, the so-called polylithionite-trilithionite series. 

 3

levels (Štemprok, 2016). The cupola is separated from the enclosing Teplice rhyolite by a

pegmatite stockscheider which is irregularly developed at the contact. The ore deposit

comprises two types of W-Sn ores, i.e. irregular greisen with several tens of meters in size,

following the morphology of the granite contact, and flat thin greisen zones and quartz veins

with a thickness of about 2 m in the center of the cupola. The greisen comprises mainly of

quartz, zinnwaldite, topaz, and minor sericite, fluorite, K-feldspar, cassiterite, wolframite and

scheelite (Štemprok et al., 1995; Seltmann et al., 1998, 2016). Lithium is uniformly

distributed in rock-forming micas (zinnwaldite and lepidolite, about 9:1) of the greisen and

greisenized granite in the uppermost 100 to 200 m of the granite cupola. Sample ZW-1

(Mineral Collections NHM London, BM 1991,69), high-grade greisen/greisenized albite

granite, was collected from an underground exposure in the former Cinovec mine (Figure DR

1F). 

The Krupka Sn-W-Mo deposit is situated in the eastern part of the Erzgebirge, in the

Czech Republic, close to the Czech-German border. The country rocks are pre-Variscan

crystalline paragneisses, orthogneisses and meta-granites. The deposit is associated with Late

Carboniferous granite intrusions. These granites are categorized into biotite granite which

forms the Preiselberg massif (NW of Krupka) and albite-zinnwaldite granite. All Rb-Li, Sn-W

and Mo mineralization is genetically linked to the second granite type. In the Krupka deposit,

albite-zinnwaldite granite forms two prominent cupolas terminated by steep stocks with

intensive mineralization. The Preiselberg cupola lies at the contact of the Teplice rhyolite, the

gneiss complex and the Preiselberg biotite granite body. The Knotl cupola lies in the gneisses,

3 km to the SE of the Preiselberg cupola. Both cupolas exhibit prominent vertical zoning. In

the root zones they consist of medium-grained albite-zinnwaldite granite. Upwards, the

granite is increasingly altered up to greisens at the top level. The formation of pegmatite

stockscheider and flat molybdenite-bearing quartz veins, parallel to the granite-gneiss contact,

is characteristic. Steep veins are mineralized with cassiterite (Štemprok et al., 1994; Breiter

and Fryda, 1995). Sample KP-1 (greisen) was collected from the open pit of the Krupka

deposit (Figure DR1G). 

                                                                                                                                                                                                   2 Zinnwaldite: A series of trioctahedral micas on, or close to, the siderophyllite-polylithionite join; dark micas containing lithium. 

 4

 

Figure DR1: Photographs of the cassiterite-bearing greisen/quartz vein samples from tin

deposits in the Erzgebirge. A: Sadisdorf, sample SD-1; B and C: Ehrenfriedersdorf, samples

E-148 and E-199; D and E: Altenberg, samples ALT-1 and ALT-2; F: Zinnwald/Cinovec,

sample ZW-1; G: Krupka, sample KP-1. 

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Cathodoluminescence images

Cathodoluminescence images of cassiterite grains were taken with a Zeiss Supra 55 field

emission SEM equipped with a MonoCL4 cathodoluminescence detector at the State Key

Laboratory of Isotope Geochemistry, Guangzhou Institute of Geochemistry, Chinese

Academy of Sciences (GIG-CAS). The intensity of cathodoluminescence in zoned cassiterite

is directly related to the concentrations of the activators Ti and W (Hall and Ribbe, 1971). The

presence of Fe together with W suppresses the W-activated emission, while Fe and Ti

enhances the probability of luminescence transitions (Hall and Ribbe, 1971). The

cathodoluminescence images of the Erzgebirge tin deposits are characterized by high Ti and

W, but relatively low Nb and Ta contents, and show clear cathodoluminescence oscillatory

patterns. 

U–Pb dating method and data processing

U–Pb isotopic and trace elemental analysis of cassiterite was carried out using a LA-ICP-

MS system at the CAS Key Laboratory of Mineralogy and Metallogeny, GIG-CAS,

Guangzhou, China. The system consists of an Agilent 7900 ICP-MS coupled with a

Resonetics RESOlution S-155 laser. This laser ablation system is large (155 ×105 mm) and

can load 20 epoxy resin mounts at each turn. About 99 % ablated material was washed out in

less than 1.5 s due to its two-volume laser-ablation cell. A squid smoothing device was used

to reduce statistical error induced by laser-ablation pulses and to improve the data quality (Tu

et al., 2011; Li et al., 2012). Helium gas carrying the ablated sample aerosol was mixed with

argon carrier gas and nitrogen as additional di-atomic gas to enhance sensitivity, and finally

flowed into the ICP-MS instrument. Prior to analysis, the system was optimized using

reference material NIST SRM610 ablated with 29 µm spot size and 5 µm/s scan speed to

achieve maximum signal intensity and low oxidation rate. The spot size is adjustable (4–200

µm) and the laser pulse frequency is 1–20 Hz (Li et al., 2016). Cassiterite grains were

analyzed using a laser energy density of 4 J/cm2, a spot size of 74 µm, and a repetition rate of

6 Hz. NIST SRM 610 and an in-house cassiterite standard AY-4 were used as external

elemental and isotopic calibration standards, respectively. AY-4 was collected from the

Anyuan skarn-type tin deposit of the Furong tin ore field in the middle Nanling Range, China.

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This cassiterite sample has been well studied using ID-TIMS with a U–Pb age of 158.2 ± 0.4

Ma (Yuan et al., 2011). NIST SRM 610 was analyzed twice for every ten analyses of the

tested sample; AY-4 was analyzed twice for every five analyses of the tested sample. Each

spot analysis incorporated a background acquisition of approximately 20 s followed by 40 s

sample data acquisition. Isotopes were measured in time-resolved mode. For U–Pb dating and

trace elemental analysis, dwell times for each mass scan are 15 ms for 204Pb, 206Pb, 208Pb, 238U,

25 ms for 207Pb, and 8 ms for all other elements. 118Sn is used as an internal standard for

calibrating the trace elements of cassiterite. Raw data reduction was performed off-line by

ICPMSDataCal software. The uncertainty of single population, ratio uncertainty of the AY-4

reference material, and decay constant uncertainties were propagated to the ultimate results of

the samples during the process of data reduction by ICPMSDataCal (Liu et al., 2010). Data

uncertainties for isotopic ratios in the cassiterite samples are 1 σ (Li et al., 2016). Isoplot 4.0

was used to calculate the U–Pb ages and draw concordia diagrams and weighted 206Pb/238U

mean ages (Ludwig, 2012). 

Wetherill concordia U–Pb plots and weighted 206Pb/238U mean ages were drawn and

calculated with analytical spots of concordances ≥95% for each sample (bold in DR Table 1).

Tera-Wasserburg U-Pb plots were drawn with all spots for each sample. For individual

samples, the Wetherill concordia U-Pb age, weighted 206Pb/238U mean age and Tera-

Wasserburg lower intercept U-Pb age agree well with each other within the uncertainties

(Table 1, main text). 

Samples SD-1 and ZW-1 were analyzed in two sessions, i.e. in 2015 and 2017,

respectively. The session for SD-1 in 2015 gave a Wetherill U–Pb concordia age of 325.9 ±

3.9 Ma, which agrees well with the dating result of 326.6 ± 7.0 Ma of the session in 2017;

Sessions for ZW-1 in 2015 and 2017 yielded Wetherill U–Pb concordia ages of 322.9 ± 6.0

Ma and 321.1 ± 3.6 Ma, respectively (Figure DR2). The consistent dating results in two

different sessions in different years demonstrate that our dates are reproducible in the long

term.

Figure DR3 shows the Wetherill concordia plots for the seven cassiterite samples from the

five tin deposits in the Erzgebirge/Krušné hory metal province analyzed, and Figure DR4

shows the corresponding Tera-Wasserburg plots. The complete analytical data set is in Table

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DR1.

 

References

Breiter, K., and Fryda, J., 1995, The Krupka tin deposit, in Breiter, K., and Seltmann, R., eds., Ore

mineralizations of the Krušné hory Mts (Erzgebirge): Excursion Guide, Prague, Czech Geological

Survey, p. 103-111. 

Hall, M.R., and Ribbe, P.H., 1971, An electron microprobe study of luminescence centers in cassiterite：

American Mineralogist, v. 56, p. 31–45. 

Hösel, G., Meyer, H., Seltmann, R., and Tägl, U., 1994, Tin-bearing deposits of the Ehrenfriedersdorf

district, in Seltmann, R., Kämpf, H., and Möller P., eds., Metallogeny of Collisional Orogens, Prague,

Czech Geological Survey, p. 129-136. 

Li, C.Y., Zhang, H., Wang, F.Y., Liu, J.Q., Sun, Y.L., Hao, X.L., Li, Y.L., and Sun, W.D., 2012, The

formation of the Dabaoshan porphyry molybdenum deposit induced by slab rollback: Lithos, v. 150, p.

101-110.

Li, C.Y., Zhang, R.Q., Ding, X., Ling, M.X., Fan, W.M., and Sun, W.D., 2016, Dating cassiterite using

laser ablation ICP-MS: Ore Geology Reviews, v. 72, p. 313-322.

Liu, Y.S., Gao, S., Hu, Z.C., Gao, C.G., Zong, K.Q., and Wang, D.B., 2010. Continental and oceanic crust

recycling-induced melt–peridotite interactions in the Trans-North China Orogen: U–Pb dating, Hf

isotopes and trace elements in zircons from mantle xenoliths: Journal of Petrology, v. 51, p. 537-571.

Ludwig, K.R., 2012, Isoplot: A geochronological toolkit for Microsoft Excel: Special Publication no. 5,

Berkeley Geochronology Center, 70 p.

Romer, R.L., Förster, H.-J., Kroner, U., Müller, A., Rössler, R., Rötzler, J., Seltmann, R., and Wenzel, T.,

2012, Granites of the Erzgebirge - relation of magmatism to the metamorphic and tectonic evolution

 8

of the Variscan Orogen. Scientific Technical Report 12/15, GFZ German Research Centre for

Geosciences, 122 pp.

Seltmann, R., 1995, Tin mineralization in the Sadisdorf district, in Breiter, K., and Seltmann, R., eds., Ore

mineralizations of the Krušné hory Mts (Erzgebirge): Excursion Guide, Prague, Czech Geological

Survey, p. 85-91.

Seltmann, R., Armstrong R., Oliver, K., Broadbent, C., and FAME Work Package WP2 team, 2016, Report

on the economic potential of skarn, pegmatite and greisen ore deposits of Europe. EC H2020 Flexible

and Mobile Economic Processing Technologies – FAME: Natural History Museum London, 184 pp.

URL: www.fame-project.eu 

Seltmann, R., Förster, H.-J., Gottesmann, B., Sala, M., Wolf, D., and Štemprok, M., 1998, The Zinnwald

greisen deposit related to postcollisional A-type silicic magmatism in the Variscan Eastern

Erzgebirge/Krušné hory, in Breiter, K., eds., Genetic significance of phosphorus in fractionated

granites: Excursion Guide, IGCP Project 373, International Conference in Perslak, Prague, Czech

Geological Survey, p. 33–50. 

Seltmann, R., and Schilka, W., 1995, The Altenberg tin deposit – geology, mineralization and mining

history, in Breiter, K., and Seltmann, R., eds., Ore mineralizations of the Krušné hory Mts

(Erzgebirge): Excursion Guide, Prague, Czech Geological Survey, p. 93-101. 

Štemprok, M., 2016, Drill hole CS-1 penetrating the Cinovec/Zinnwald granite cupola (Czech Republic):

an A-type granite with important hydrothermal mineralization: Journal of Geosciences, v. 61, p. 395-

423.

Štemprok, M., Durisova, J., and Halls, C., 1994, Observations on a molybdenite-bearing vein dike from the

Krupka Sn-W-Mo district in the Eastern Krušné hory (Erzgebirge), Czech Republic, in Seltmann, R.,

Kämpf, H., and Möller P., eds., Metallogeny of Collisional Orogens, Prague, Czech Geological

 9

Survey, p. 207-217. 

Štemprok, M., Seltmann, R., and Breiter, K., 1995, The Cinovec/Zinnwald Sn-W-Li deposit, in Breiter, K.,

and Seltmann, R., eds., Ore mineralizations of the Krušné hory Mts (Erzgebirge): Excursion Guide,

Prague, Czech Geological Survey, p. 77-83. 

Tu, X.L., Zhang, H.L., Deng, W.F., Liang, H.Y., Liu, Y.Y., and Sun, W.D., 2011, Application of

RESOlution in-situ laser ablation ICP-MS in trace element analyses: Geochimica, v. 40, p. 83-98.

Yuan, S.D., Peng, J.T., Hao, S., Li, H.M., Geng, J.Z., and Zhang, D.L., 2011, In situ LA-MC-ICP-MS and

ID-TIMS U–Pb geochronology of cassiterite in the giant Furong tin deposit, Hunan Province, South

China: New constraints on the timing of tin-polymetallic mineralization: Ore Geology Reviews, v. 43,

p. 235-242.

 

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Figure DR2. Wetherill U–Pb concordia plots for cassiterite from the Sadisdorf and Zinnwald

tin deposits in the Erzgebirge/Krušné hory metal province. A: Sadisdorf, sample SD-1

analyzed in 2015; B: Sadisdorf, sample SD-1 analyzed in 2017; C: Zinnwald/Cinovec, sample

ZW-1 analyzed in 2015; D: Zinnwald/Cinovec, sample ZW-1 analyzed in 2017. 

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Figure DR3. Wetherill concordia U–Pb plots for cassiterite from tin deposits in the

Erzgebirge/Krušné hory metal province. A: Sadisdorf, sample SD-1; B and C:

Ehrenfriedersdorf, samples E-148 and E-199; D and E: Altenberg, samples ALT-1 and ALT-2;

F: Zinnwald/Cinovec, sample ZW-1; G: Krupka, sample KP-1. 

 

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Figure DR4. Tera-Wasserburg U–Pb concordia plots for cassiterite from tin deposits in the

Erzgebirge/Krušné hory metal province. A: Sadisdorf, sample SD-1; B and C:

Ehrenfriedersdorf, samples E-148 and E-199; D and E: Altenberg, samples ALT-1 and ALT-2;

F: Zinnwald/Cinovec, sample ZW-1; G: Krupka, sample KP-1.

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Table DR1 LA-ICPMS U-Pb dating results for cassiterite from tin deposits in the Erzgebirge/Krušné hory metal province.

Spots Total Pb ppm Th

ppm U

ppm Isotopic ratios

Rho Age (Ma)

Concordance 207Pb/206Pb 1σ 207Pb/235U 1σ 206Pb/238U 1σ 207Pb/206Pb 1σ 207Pb/235U 1σ 206Pb/238U 1σ

SD-1-02 0.05 0.00 0.82 0.054391 0.005729 0.389236 0.040652 0.052831 0.002678 0.49 387.1 238.9 333.8 29.7 331.9 16.4 99%

SD-1-03 0.05 0.00 0.98 0.058518 0.007982 0.383173 0.055487 0.052401 0.003305 0.44 550.0 300.7 329.4 40.8 329.2 20.2 99%

SD-1-09 0.05 0.00 0.86 0.057599 0.008284 0.386048 0.046463 0.052258 0.002217 0.35 522.3 519.4 331.5 34.1 328.4 13.6 99%

SD-1-11 0.64 0.00 10.83 0.050896 0.004728 0.378874 0.042936 0.051902 0.000870 0.15 235.3 216.6 326.2 31.6 326.2 5.3 99%

SD-1-12 0.67 0.00 11.45 0.049092 0.007038 0.388118 0.075125 0.051815 0.001026 0.10 153.8 303.7 333.0 55.0 325.7 6.3 97%

SD-1-13 0.68 0.00 11.15 0.048210 0.006796 0.399426 0.080161 0.052713 0.001247 0.12 109.4 303.7 341.2 58.2 331.2 7.6 97%

SD-1-14 0.04 0.00 0.60 0.058831 0.008096 0.396794 0.057044 0.053388 0.002451 0.32 561.1 303.7 339.3 41.5 335.3 15.0 98%

SD-1-17 0.02 0.00 0.39 0.051146 0.007826 0.373799 0.048047 0.051999 0.004179 0.63 255.6 309.2 322.5 35.5 326.8 25.6 98%

SD-1-21 0.32 0.00 5.52 0.053398 0.003634 0.394133 0.031772 0.052092 0.000925 0.22 346.4 158.3 337.4 23.1 327.4 5.7 96%

SD-1-22 0.37 0.00 6.76 0.052185 0.005132 0.381627 0.044337 0.051253 0.000869 0.15 294.5 225.9 328.2 32.6 322.2 5.3 98%

SD-1-24 0.31 0.00 5.52 0.051132 0.004125 0.378197 0.039246 0.052282 0.001114 0.21 255.6 188.9 325.7 28.9 328.5 6.8 99%

SD-1-25 0.22 0.00 4.04 0.052711 0.003396 0.370874 0.027057 0.050282 0.000886 0.24 316.7 148.1 320.3 20.0 316.3 5.4 98%

SD-1-26 0.10 0.00 1.81 0.055627 0.005298 0.384689 0.031707 0.052569 0.001770 0.41 438.9 212.9 330.5 23.3 330.3 10.8 99%

SD-1-27 0.15 0.00 2.79 0.054259 0.005737 0.377335 0.040794 0.051704 0.001323 0.24 388.9 243.5 325.1 30.1 325.0 8.1 99%

SD-1-29 0.14 0.00 2.57 0.054243 0.005396 0.389620 0.036633 0.053022 0.001149 0.23 388.9 225.9 334.1 26.8 333.0 7.0 99%

SD-1-33 0.06 0.00 0.99 0.053822 0.006525 0.384954 0.053245 0.051849 0.001972 0.27 364.9 275.9 330.7 39.1 325.9 12.1 98%

SD-1-37 0.05 0.00 0.78 0.053542 0.009107 0.382377 0.083424 0.052534 0.003739 0.33 350.1 348.1 328.8 61.4 330.1 22.9 99%

SD-1-04 0.06 0.00 0.90 0.082796 0.023460 0.477394 0.063357 0.053658 0.004392 0.62 1264.8 573.6 396.3 43.6 336.9 26.9 83%

SD-1-05 0.04 0.00 0.77 0.062988 0.007593 0.422378 0.049662 0.052127 0.002430 0.40 709.3 259.2 357.7 35.5 327.6 14.9 91%

SD-1-07 0.06 0.00 0.95 0.066019 0.014667 0.430538 0.068311 0.053124 0.002990 0.35 807.1 478.2 363.6 48.5 333.7 18.3 91%

SD-1-18 0.37 0.00 5.79 0.049485 0.008014 0.428648 0.105412 0.052798 0.001578 0.12 172.3 337.0 362.2 75.1 331.7 9.7 91%

SD-1-19 0.45 0.00 7.16 0.051551 0.007853 0.432806 0.095751 0.053113 0.001441 0.12 264.9 318.5 365.2 68.0 333.6 8.8 90%

SD-1-30 0.03 0.00 0.64 0.061882 0.013128 0.430950 0.066965 0.052452 0.002981 0.37 733.3 466.6 363.9 47.6 329.6 18.3 90%

SD-1-31 0.06 0.00 0.99 0.065021 0.009034 0.423853 0.043590 0.053366 0.002694 0.49 775.9 296.3 358.8 31.1 335.2 16.5 93%

SD-1-32 0.04 0.00 0.64 0.080409 0.019232 0.401125 0.063671 0.051483 0.002376 0.29 1207.1 481.0 342.5 46.2 323.6 14.6 94%

SD-1-34 0.05 0.00 0.80 0.062827 0.008184 0.447405 0.053487 0.053148 0.002259 0.36 701.9 284.2 375.5 37.5 333.8 13.8 88%

SD-1-39 0.07 0.00 1.25 0.057651 0.004873 0.412406 0.036833 0.052495 0.002057 0.44 516.7 189.8 350.6 26.5 329.8 12.6 93%

SD-1-10 0.09 0.00 0.92 0.155467 0.011305 1.276483 0.101146 0.060337 0.002527 0.53 2407.1 123.0 835.3 45.1 377.7 15.4 24%

SD-1-15 0.02 0.00 0.27 0.078528 0.011055 0.592636 0.074304 0.052929 0.004605 0.69 1161.1 281.5 472.5 47.4 332.5 28.2 65%

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SD-1-16 0.01 0.00 0.23 0.184402 0.038085 0.809518 0.088795 0.053312 0.005196 0.89 2694.4 347.8 602.2 49.9 334.8 31.8 42%

SD-1-20 0.47 0.00 6.77 0.070544 0.011265 0.682992 0.191279 0.053255 0.002637 0.18 944.1 333.3 528.6 #### 334.5 16.1 55%

SD-1-23 0.10 0.01 1.10 0.193925 0.022181 1.401615 0.098846 0.059064 0.003214 0.77 2775.6 188.9 889.6 41.8 369.9 19.6 17%

SD-1-28 0.08 0.00 1.33 0.077615 0.008128 0.559880 0.059988 0.052326 0.001823 0.33 1136.7 205.1 451.4 39.1 328.8 11.2 68%

SD-1-35 0.03 0.00 0.43 0.096575 0.015289 0.605287 0.066312 0.054726 0.003780 0.63 1559.0 301.7 480.6 42.0 343.5 23.1 66%

SD-1-36 0.04 0.00 0.60 0.085122 0.015558 0.506513 0.073002 0.052442 0.003912 0.52 1318.2 360.0 416.1 49.2 329.5 24.0 76%

SD-1-38 0.11 0.00 1.55 0.124581 0.011226 0.852804 0.054019 0.052828 0.002280 0.68 2033.3 161.0 626.2 29.6 331.9 14.0 38%

SD-1-40 0.08 0.00 1.35 0.069645 0.007024 0.500420 0.044799 0.053031 0.002222 0.47 917.6 213.9 412.0 30.3 333.1 13.6 78%

SD-1-2-2 0.09 0.00 1.71 0.062869 0.010921 0.389552 0.068353 0.050954 0.002287 0.26 705.6 375.9 334.0 49.9 320.4 14.0 95%

SD-1-2-3 0.11 0.00 2.09 0.057990 0.009615 0.375485 0.050404 0.053593 0.002521 0.35 527.8 370.3 323.7 37.2 336.5 15.4 96%

SD-1-2-5 0.07 0.00 1.29 0.053553 0.011336 0.381958 0.072201 0.051051 0.002718 0.28 353.8 418.5 328.5 53.0 321.0 16.7 97%

SD-1-2-7 0.13 0.00 2.40 0.058476 0.010405 0.376892 0.062986 0.051259 0.002289 0.27 546.3 396.3 324.7 46.4 322.2 14.0 99%

SD-1-2-9 0.13 0.00 2.40 0.067914 0.011609 0.391567 0.038869 0.051963 0.002418 0.47 864.8 360.0 335.5 28.4 326.6 14.8 97%

SD-1-2-12 0.14 0.00 2.77 0.057993 0.008659 0.371286 0.045051 0.051304 0.002738 0.44 527.8 331.4 320.6 33.4 322.5 16.8 99%

SD-1-2-13 0.17 0.00 3.18 0.051820 0.006076 0.370497 0.041065 0.050908 0.001846 0.33 276.0 248.1 320.0 30.4 320.1 11.3 99%

SD-1-2-23 0.05 0.00 0.85 0.056573 0.012692 0.363319 0.047904 0.051554 0.004415 0.65 476.0 429.6 314.7 35.7 324.1 27.1 97%

SD-1-2-27 0.55 0.00 10.84 0.055019 0.004035 0.376189 0.024819 0.051749 0.001213 0.36 413.0 164.8 324.2 18.3 325.3 7.4 99%

SD-1-2-30 1.24 0.00 24.16 0.055577 0.004730 0.390502 0.031033 0.053049 0.001232 0.29 435.2 188.9 334.7 22.7 333.2 7.5 99%

SD-1-2-31 0.40 0.00 7.87 0.058141 0.009462 0.381397 0.050060 0.052932 0.002194 0.32 600.0 362.9 328.1 36.8 332.5 13.4 98%

SD-1-2-34 0.10 0.00 1.95 0.059516 0.011833 0.373477 0.062706 0.050580 0.003187 0.38 587.1 442.5 322.2 46.4 318.1 19.6 98%

SD-1-2-36 0.10 0.00 1.84 0.063218 0.011867 0.378105 0.066361 0.051981 0.003013 0.33 716.7 407.4 325.6 48.9 326.7 18.5 99%

SD-1-2-1 0.09 0.00 1.60 0.062676 0.013968 0.375774 0.091173 0.054666 0.003047 0.23 698.2 461.1 323.9 67.3 343.1 18.6 94%

SD-1-2-4 0.09 0.00 1.99 0.067901 0.009226 0.351234 0.039132 0.046303 0.002455 0.48 864.8 285.2 305.6 29.4 291.8 15.1 95%

SD-1-2-6 0.06 0.00 0.91 0.108756 0.032406 0.537433 0.087417 0.060712 0.004742 0.48 1788.9 568.5 436.7 57.7 380.0 28.8 86%

SD-1-2-8 0.36 0.01 6.70 0.071888 0.007585 0.467252 0.042526 0.050779 0.001798 0.39 983.3 215.9 389.3 29.4 319.3 11.0 80%

SD-1-2-10 0.15 0.00 2.89 0.071273 0.013578 0.450885 0.085300 0.052978 0.002942 0.29 964.8 402.8 377.9 59.7 332.8 18.0 87%

SD-1-2-11 0.07 0.00 1.18 0.070953 0.011545 0.471593 0.061928 0.054602 0.003356 0.47 966.7 337.0 392.3 42.7 342.7 20.5 86%

SD-1-2-14 0.70 0.00 14.10 0.037995 0.003161 0.263800 0.018790 0.051011 0.001102 0.30 237.7 15.1 320.7 6.8 70% SD-1-2-15 0.47 0.00 9.35 0.040616 0.003546 0.287415 0.023354 0.051267 0.001396 0.34 256.5 18.4 322.3 8.6 77% SD-1-2-16 0.64 0.00 12.56 0.038752 0.003140 0.266403 0.018502 0.051033 0.001285 0.36 239.8 14.8 320.9 7.9 71% SD-1-2-17 0.60 0.00 11.27 0.044033 0.003247 0.307613 0.020860 0.050927 0.001225 0.35 272.3 16.2 320.2 7.5 83% SD-1-2-18 0.75 0.03 14.91 0.034932 0.002586 0.244171 0.016713 0.051345 0.001967 0.56 221.8 13.6 322.8 12.1 62%

 15

SD-1-2-19 0.89 0.00 17.10 0.033836 0.002310 0.242388 0.015275 0.050768 0.001011 0.32 220.4 12.5 319.2 6.2 63% SD-1-2-20 0.04 0.00 0.67 0.089916 0.021002 0.480570 0.083035 0.056518 0.004831 0.49 1433.3 459.3 398.5 56.9 354.4 29.5 88%

SD-1-2-21 0.03 0.00 0.58 0.105633 0.028682 0.492401 0.088738 0.047824 0.004884 0.57 1725.6 517.4 406.5 60.4 301.1 30.0 70%

SD-1-2-22 0.09 0.06 0.76 0.210113 0.032477 1.571777 0.196661 0.069632 0.005165 0.59 2906.5 253.9 959.1 77.6 433.9 31.1 24%

SD-1-2-24 0.09 0.00 1.80 0.048754 0.010163 0.321549 0.079920 0.052024 0.002593 0.20 200.1 364.8 283.1 61.4 326.9 15.9 85%

SD-1-2-25 0.05 0.00 0.84 0.105663 0.024072 0.634631 0.099424 0.060770 0.005604 0.59 1725.6 429.5 499.0 61.8 380.3 34.1 73%

SD-1-2-26 0.04 0.00 0.76 0.066935 0.022636 0.380804 0.066865 0.048523 0.003543 0.42 835.2 581.5 327.6 49.2 305.4 21.8 92%

SD-1-2-28 0.04 0.00 0.70 0.141267 0.034937 0.677701 0.121871 0.055507 0.004790 0.48 2242.9 439.4 525.4 73.8 348.2 29.3 59%

SD-1-2-29 0.08 0.00 0.94 0.228926 0.033394 1.494869 0.172810 0.058073 0.004038 0.60 3055.6 235.0 928.3 70.3 363.9 24.6 12%

SD-1-2-32 0.12 0.00 2.22 0.069556 0.011264 0.407467 0.047129 0.052143 0.002762 0.46 916.7 338.9 347.0 34.0 327.7 16.9 94%

SD-1-2-33 0.11 0.00 1.97 0.080309 0.010733 0.587064 0.071613 0.056088 0.002255 0.33 1205.6 265.3 469.0 45.8 351.8 13.8 71%

SD-1-2-35 0.17 0.00 2.04 0.158138 0.021277 1.205734 0.126339 0.062321 0.002944 0.45 2436.1 229.6 803.2 58.2 389.7 17.9 30%

E148-01 0.03 0.00 0.27 0.058757 0.013309 0.381541 0.083219 0.051937 0.005994 0.53 566.7 420.3 328.2 61.2 326.4 36.7 99%

E148-02 0.47 0.00 8.28 0.051563 0.009232 0.373355 0.068687 0.051467 0.000881 0.09 264.9 366.6 322.1 50.8 323.5 5.4 99%

E148-03 0.25 0.00 3.99 0.051354 0.005668 0.393308 0.052844 0.053323 0.001276 0.18 257.5 242.6 336.8 38.5 334.9 7.8 99%

E148-05 0.08 0.00 1.24 0.054375 0.006726 0.397546 0.061693 0.052981 0.002109 0.26 387.1 279.6 339.9 44.8 332.8 12.9 97%

E148-06 0.38 0.00 6.51 0.053620 0.005099 0.391813 0.039476 0.053007 0.000887 0.17 353.8 221.3 335.7 28.8 333.0 5.4 99%

E148-07 1.13 0.00 7.34 0.052182 0.006365 0.386574 0.052170 0.052397 0.000874 0.12 294.5 255.5 331.9 38.2 329.2 5.4 99%

E148-09 0.08 0.00 1.32 0.049972 0.006354 0.383680 0.066603 0.052446 0.002198 0.24 194.5 270.3 329.7 48.9 329.5 13.5 99%

E148-10 0.14 0.00 2.39 0.053626 0.005932 0.366703 0.042176 0.049905 0.001534 0.27 353.8 251.8 317.2 31.3 313.9 9.4 98%

E148-12 0.05 0.00 0.74 0.058591 0.009294 0.388846 0.054186 0.053188 0.002601 0.35 553.7 351.8 333.5 39.6 334.1 15.9 99%

E148-16 0.01 0.00 0.19 0.071885 0.021269 0.395462 0.097423 0.052293 0.005201 0.40 983.3 628.8 338.4 70.9 328.6 31.9 97%

E148-17 0.07 0.00 1.09 0.056172 0.007555 0.369291 0.045442 0.050703 0.001765 0.28 457.5 301.8 319.1 33.7 318.8 10.8 99%

E148-18 0.18 0.00 2.82 0.052379 0.005757 0.381752 0.044975 0.052286 0.001171 0.19 301.9 284.2 328.3 33.1 328.5 7.2 99%

E148-20 0.05 0.00 0.68 0.061067 0.013186 0.379001 0.060621 0.053160 0.003017 0.35 642.6 475.0 326.3 44.6 333.9 18.5 97%

E148-22 0.12 0.00 1.79 0.052963 0.006214 0.372784 0.045619 0.052188 0.001534 0.24 327.8 268.5 321.7 33.7 327.9 9.4 98%

E148-23 0.07 0.00 0.95 0.050749 0.008740 0.385121 0.079053 0.051970 0.002575 0.24 227.8 355.5 330.8 58.0 326.6 15.8 98%

E148-24 0.63 0.00 10.81 0.053127 0.008514 0.376532 0.062491 0.050695 0.000964 0.11 344.5 316.6 324.5 46.1 318.8 5.9 98%

E148-26 0.35 0.00 5.85 0.053270 0.005205 0.390177 0.045000 0.051349 0.001052 0.18 338.9 222.2 334.5 32.9 322.8 6.5 96%

E148-27 0.30 0.00 4.65 0.051651 0.007142 0.404039 0.074007 0.052557 0.001342 0.14 333.4 227.8 344.6 53.5 330.2 8.2 95%

E148-30 0.13 0.00 2.01 0.052371 0.006732 0.372676 0.053869 0.051178 0.001506 0.20 301.9 270.3 321.6 39.8 321.8 9.2 99%

E148-37 0.07 0.00 1.10 0.053356 0.008007 0.383272 0.056108 0.052946 0.002151 0.28 342.7 311.1 329.4 41.2 332.6 13.2 99%

 16

E148-38 0.47 0.00 8.62 0.052187 0.003686 0.371655 0.027316 0.050954 0.000719 0.19 294.5 165.7 320.9 20.2 320.4 4.4 99%

E148-29 0.35 0.00 5.55 0.059479 0.010126 0.428742 0.076833 0.050745 0.001414 0.16 583.4 375.9 362.3 54.6 319.1 8.7 87%

E148-13 0.07 0.00 0.77 0.060698 0.007268 0.457053 0.055630 0.054483 0.002178 0.33 627.8 265.7 382.2 38.8 342.0 13.3 88%

E148-25 0.06 0.00 0.73 0.063976 0.011641 0.433750 0.069493 0.054354 0.002448 0.28 742.6 391.5 365.8 49.2 341.2 15.0 93%

E148-33 0.04 0.00 0.61 0.064926 0.011818 0.405260 0.078972 0.052105 0.002988 0.29 772.2 385.0 345.5 57.1 327.4 18.3 94%

E148-35 0.13 0.00 2.07 0.054019 0.007363 0.402682 0.066217 0.051557 0.001426 0.17 372.3 311.1 343.6 47.9 324.1 8.7 94%

E148-40 0.03 0.00 0.67 0.074398 0.017214 0.405623 0.065627 0.051423 0.003013 0.36 1053.7 481.5 345.7 47.4 323.2 18.5 93%

E148-04 0.13 0.00 1.99 0.065360 0.006375 0.461527 0.043822 0.052687 0.001977 0.40 787.0 212.0 385.3 30.4 331.0 12.1 84%

E148-14 0.03 0.00 0.43 0.135338 0.028045 0.760605 0.111369 0.052768 0.003980 0.52 2168.2 368.5 574.4 64.2 331.5 24.4 46%

E148-15 0.14 0.00 2.08 0.071744 0.008305 0.535928 0.066903 0.053061 0.001830 0.28 988.9 237.0 435.7 44.2 333.3 11.2 73%

E148-19 0.09 0.00 1.21 0.076897 0.012176 0.627848 0.147741 0.051891 0.002381 0.20 1120.4 320.4 494.8 92.2 326.1 14.6 58%

E148-21 0.09 0.00 1.34 0.067666 0.009265 0.545564 0.118479 0.051513 0.002420 0.22 857.4 287.0 442.1 77.8 323.8 14.8 69%

E148-28 0.03 0.00 0.25 0.068626 0.014434 0.537687 0.142235 0.058764 0.003535 0.23 887.0 441.6 436.9 93.9 368.1 21.5 82%

E148-32 0.08 0.00 1.08 0.088432 0.009579 0.657340 0.070433 0.054594 0.001868 0.32 1391.7 209.3 513.0 43.2 342.7 11.4 60%

E148-34 0.08 0.00 1.24 0.063519 0.009473 0.469795 0.078079 0.052890 0.002920 0.33 725.6 320.3 391.0 53.9 332.2 17.9 83%

E199-13 0.69 0.00 0.92 0.057690 0.009065 0.392850 0.060876 0.053619 0.002492 0.30 516.7 350.0 336.4 44.4 336.7 15.3 99%

E199-01 0.71 0.17 12.26 0.051074 0.004711 0.373764 0.041076 0.051484 0.000839 0.15 242.7 212.9 322.4 30.4 323.6 5.1 99%

E199-04 0.10 0.00 12.34 0.054439 0.005779 0.373995 0.047488 0.050073 0.001325 0.21 390.8 240.7 322.6 35.1 315.0 8.1 97%

E199-05 0.37 0.00 2.28 0.055666 0.006683 0.373698 0.048379 0.051586 0.001467 0.22 438.9 270.3 322.4 35.8 324.2 9.0 99%

E199-08 0.11 0.00 6.10 0.053200 0.006558 0.385018 0.052456 0.052386 0.001009 0.14 344.5 281.4 330.7 38.5 329.2 6.2 99%

E199-09 0.12 0.00 6.39 0.050455 0.004579 0.379927 0.046241 0.052203 0.001178 0.19 216.7 196.3 327.0 34.0 328.0 7.2 99%

E199-11 0.06 0.00 1.85 0.054641 0.006489 0.379292 0.047054 0.051795 0.001396 0.22 398.2 268.5 326.5 34.6 325.5 8.6 99%

E199-12 0.03 0.00 17.52 0.056385 0.006081 0.379214 0.041010 0.050311 0.000740 0.14 477.8 245.3 326.5 30.2 316.4 4.5 96%

E199-14 0.12 0.00 0.53 0.061140 0.013812 0.383058 0.075753 0.053010 0.002783 0.27 642.6 534.2 329.3 55.6 333.0 17.0 98%

E199-15 0.17 0.00 1.90 0.059271 0.008664 0.379093 0.048026 0.051601 0.001974 0.30 576.0 316.5 326.4 35.4 324.3 12.1 99%

E199-16 0.15 0.00 3.06 0.055176 0.005910 0.366822 0.039242 0.050819 0.001312 0.24 420.4 240.7 317.3 29.2 319.5 8.1 99%

E199-17 0.18 0.00 2.56 0.061844 0.008145 0.383508 0.039159 0.050347 0.001359 0.26 733.3 280.5 329.6 28.7 316.7 8.3 95%

E199-18 0.40 0.00 2.90 0.055398 0.005920 0.375579 0.037368 0.051908 0.001442 0.28 427.8 238.9 323.8 27.6 326.2 8.8 99%

E199-19 0.73 0.00 6.95 0.051229 0.005852 0.375240 0.056644 0.051092 0.001093 0.14 250.1 244.4 323.5 41.8 321.2 6.7 99%

E199-21 0.53 0.00 9.04 0.051580 0.004298 0.380332 0.036606 0.052251 0.000830 0.17 333.4 195.3 327.3 26.9 328.3 5.1 99%

E199-23 0.80 0.00 14.23 0.052660 0.005760 0.375035 0.041118 0.051349 0.000817 0.15 322.3 251.8 323.4 30.4 322.8 5.0 99%

E199-24 0.14 0.00 2.22 0.051659 0.005223 0.383463 0.043127 0.052829 0.001744 0.29 333.4 233.3 329.6 31.7 331.9 10.7 99%

 17

E199-25 0.23 0.00 3.63 0.049153 0.006962 0.381408 0.071289 0.052351 0.001640 0.17 153.8 303.7 328.1 52.4 328.9 10.0 99%

E199-26 0.16 0.00 2.75 0.055709 0.010937 0.386529 0.081022 0.051587 0.002050 0.19 442.6 385.1 331.8 59.3 324.3 12.6 97%

E199-27 0.08 0.00 1.32 0.055508 0.006952 0.385916 0.053493 0.052559 0.002212 0.30 431.5 286.1 331.4 39.2 330.2 13.6 99%

E199-28 0.71 0.00 11.57 0.051438 0.008004 0.372401 0.066346 0.050578 0.001089 0.12 261.2 322.2 321.4 49.1 318.1 6.7 98%

E199-29 0.16 0.00 2.30 0.051657 0.005948 0.379227 0.058990 0.051845 0.001816 0.23 333.4 188.9 326.5 43.4 325.8 11.1 99%

E199-30 0.06 0.00 0.74 0.063490 0.010446 0.383945 0.054744 0.050629 0.003084 0.43 724.1 353.7 329.9 40.2 318.4 18.9 96%

E199-31 0.10 0.00 1.37 0.050010 0.007342 0.379389 0.064844 0.052340 0.002277 0.25 194.5 311.1 326.6 47.7 328.9 13.9 99%

E199-32 0.32 0.00 5.32 0.051120 0.006506 0.362507 0.052861 0.049966 0.001018 0.14 255.6 261.1 314.1 39.4 314.3 6.2 99%

E199-33 0.37 0.00 6.28 0.049574 0.008315 0.377702 0.076742 0.051991 0.001485 0.14 176.0 348.1 325.3 56.6 326.7 9.1 99%

E199-34 0.58 0.00 9.91 0.050276 0.007608 0.375189 0.068310 0.051248 0.001017 0.11 209.3 314.8 323.5 50.4 322.2 6.2 99%

E199-35 0.04 0.00 0.69 0.052490 0.008360 0.373735 0.059784 0.053750 0.002794 0.33 305.6 329.6 322.4 44.2 337.5 17.1 95%

E199-36 0.12 0.00 1.95 0.053374 0.007323 0.372953 0.057424 0.050909 0.001782 0.23 346.4 113.9 321.8 42.5 320.1 10.9 99%

E199-38 0.15 0.00 2.42 0.054469 0.004468 0.373453 0.030926 0.051456 0.001504 0.35 390.8 185.2 322.2 22.9 323.5 9.2 99%

E199-39 0.14 0.00 2.11 0.049551 0.007201 0.375436 0.071513 0.051525 0.001872 0.19 172.3 311.1 323.7 52.8 323.9 11.5 99%

E199-40 0.27 0.00 3.91 0.046622 0.007778 0.387539 0.092439 0.053607 0.002149 0.17 31.6 355.5 332.6 67.6 336.6 13.1 98%

E199-20 0.20 0.00 13.61 0.048320 0.003769 0.345967 0.028844 0.050780 0.001027 0.24 122.3 177.8 301.7 21.8 319.3 6.3 94%

E199-02 0.15 0.00 3.25 0.058180 0.004714 0.420613 0.036039 0.053229 0.001220 0.27 600.0 177.8 356.5 25.8 334.3 7.5 93%

E199-07 0.38 0.00 1.69 0.057696 0.008774 0.397952 0.070277 0.050144 0.001869 0.21 516.7 338.8 340.2 51.0 315.4 11.5 92%

E199-10 0.97 0.00 1.59 0.058140 0.006325 0.414259 0.046221 0.052785 0.002439 0.41 600.0 245.3 351.9 33.2 331.6 14.9 94%

E199-22 0.07 0.00 0.64 0.135065 0.019793 0.964576 0.107626 0.059771 0.003424 0.51 2165.1 457.9 685.7 55.6 374.2 20.8 41%

ALT-1-06 0.39 0.01 6.48 0.053762 0.005473 0.382642 0.045173 0.051074 0.001231 0.20 361.2 226.8 329.0 33.2 321.1 7.6 97%

ALT-1-08 0.06 0.00 0.86 0.059147 0.009471 0.390053 0.058661 0.051657 0.002454 0.32 572.3 349.0 334.4 42.8 324.7 15.0 97%

ALT-1-09 0.58 0.00 9.98 0.049892 0.006781 0.371012 0.066007 0.050376 0.001118 0.12 190.8 288.9 320.4 48.9 316.8 6.9 98%

ALT-1-11 0.32 0.00 5.07 0.053229 0.005732 0.380877 0.047899 0.050739 0.001055 0.17 338.9 244.4 327.7 35.2 319.1 6.5 97%

ALT-1-12 0.04 0.00 0.60 0.060391 0.011222 0.376246 0.056880 0.051982 0.002724 0.35 616.7 404.6 324.3 42.0 326.7 16.7 99%

ALT-1-15 0.28 0.00 4.51 0.049969 0.005822 0.386622 0.055848 0.052824 0.001284 0.17 194.5 248.1 331.9 40.9 331.8 7.9 99%

ALT-1-16 0.95 0.00 15.26 0.049817 0.007833 0.374573 0.073997 0.051322 0.001428 0.14 187.1 329.6 323.0 54.7 322.6 8.8 99%

ALT-1-21 0.13 0.00 1.92 0.050287 0.006175 0.369297 0.050373 0.052495 0.001888 0.26 209.3 268.5 319.1 37.4 329.8 11.6 96%

ALT-1-22 0.03 0.00 0.45 0.060464 0.009974 0.372811 0.055305 0.051346 0.002991 0.39 620.4 362.9 321.7 40.9 322.8 18.3 99%

ALT-1-23 0.35 0.01 5.69 0.051327 0.004140 0.371484 0.034530 0.052117 0.000921 0.19 253.8 187.0 320.8 25.6 327.5 5.6 97%

ALT-1-24 0.49 0.00 7.79 0.053187 0.004035 0.383376 0.032909 0.051787 0.000812 0.18 344.5 174.1 329.5 24.2 325.5 5.0 98%

ALT-1-25 0.06 0.00 0.98 0.059223 0.016692 0.384099 0.091231 0.052164 0.003427 0.28 576.0 518.5 330.0 66.9 327.8 21.0 99%

 18

ALT-1-26 0.24 0.00 4.03 0.052960 0.004853 0.378420 0.038260 0.051545 0.001215 0.23 327.8 209.2 325.9 28.2 324.0 7.5 99%

ALT-1-31 0.06 0.00 1.04 0.054394 0.007564 0.376298 0.055835 0.050891 0.001866 0.25 387.1 316.6 324.3 41.2 320.0 11.4 98%

ALT-1-33 0.87 0.01 14.93 0.051617 0.003110 0.368869 0.026497 0.050777 0.000736 0.20 333.4 171.3 318.8 19.7 319.3 4.5 99%

ALT-1-34 0.85 0.00 15.51 0.054698 0.005558 0.378153 0.041946 0.049290 0.000728 0.13 398.2 229.6 325.7 30.9 310.2 4.5 95%

ALT-1-35 0.27 0.00 4.69 0.054208 0.004018 0.385677 0.026830 0.052212 0.001384 0.38 388.9 163.9 331.2 19.7 328.1 8.5 99%

ALT-1-38 0.13 0.00 2.18 0.053740 0.004507 0.380184 0.030294 0.052373 0.001502 0.36 361.2 186.1 327.2 22.3 329.1 9.2 99%

ALT-1-39 0.43 0.00 7.57 0.051672 0.004543 0.357581 0.026624 0.050879 0.000876 0.23 333.4 201.8 310.4 19.9 319.9 5.4 96%

ALT-1-40 0.03 0.00 0.41 0.058065 0.010294 0.372537 0.062745 0.052418 0.003169 0.36 531.5 396.3 321.5 46.4 329.3 19.4 97%

ALT-1-04 0.20 0.00 3.09 0.057647 0.008380 0.398063 0.058852 0.050287 0.001400 0.19 516.7 323.0 340.2 42.7 316.3 8.6 92%

ALT-1-10 0.68 0.00 11.02 0.059334 0.010611 0.410082 0.074412 0.050561 0.001156 0.13 588.9 363.9 348.9 53.6 318.0 7.1 90%

ALT-1-18 0.32 0.00 4.89 0.056819 0.008241 0.453405 0.090404 0.051339 0.001520 0.15 483.4 324.0 379.7 63.2 322.7 9.3 83%

ALT-1-20 0.01 0.00 0.23 0.128379 0.050722 0.406439 0.075170 0.052295 0.005051 0.52 2075.6 758.3 346.3 54.3 328.6 30.9 94%

ALT-1-05 0.59 0.03 8.94 0.064108 0.006430 0.450615 0.048161 0.050477 0.001013 0.19 746.3 213.7 377.7 33.7 317.4 6.2 82%

ALT-1-07 0.93 0.09 14.42 0.065776 0.004269 0.456269 0.028798 0.050932 0.000881 0.27 798.2 137.0 381.7 20.1 320.2 5.4 82%

ALT-1-13 0.06 0.00 0.78 0.066816 0.009573 0.502102 0.092720 0.050893 0.002355 0.25 831.5 301.8 413.1 62.7 320.0 14.4 74%

ALT-1-27 0.11 0.00 1.27 0.126386 0.010570 0.984797 0.084972 0.057557 0.002053 0.41 2050.0 148.1 696.1 43.5 360.8 12.5 36%

ALT-1-28 0.85 0.13 11.39 0.072195 0.003265 0.549254 0.024423 0.055043 0.000876 0.36 990.7 91.2 444.5 16.0 345.4 5.4 74%

ALT-1-32 0.07 0.01 0.83 0.113096 0.010729 0.791017 0.063425 0.054010 0.002155 0.50 1850.0 167.6 591.7 36.0 339.1 13.2 45%

ALT-1-36 0.03 0.00 0.47 0.087569 0.018590 0.568011 0.128842 0.051525 0.003494 0.30 1373.2 450.9 456.7 83.4 323.9 21.4 65%

ALT-2-10 0.28 0.00 4.62 0.055445 0.007315 0.382372 0.039299 0.050828 0.001273 0.24 431.5 298.1 328.8 28.9 319.6 7.8 97%

ALT-2-13 1.99 0.00 36.49 0.051894 0.003845 0.370512 0.023823 0.051539 0.000730 0.22 279.7 170.4 320.0 17.7 324.0 4.5 98%

ALT-2-14 0.63 0.04 11.38 0.052482 0.003211 0.376581 0.021454 0.051535 0.000839 0.29 305.6 138.9 324.5 15.8 323.9 5.1 99%

ALT-2-15 0.96 0.00 17.43 0.052274 0.003924 0.379769 0.028064 0.052001 0.000770 0.20 298.2 172.2 326.9 20.7 326.8 4.7 99%

ALT-2-16 1.81 0.00 31.62 0.052239 0.005656 0.383594 0.039582 0.052401 0.001005 0.19 294.5 248.1 329.7 29.0 329.2 6.2 99%

ALT-2-18 0.55 0.00 9.98 0.052065 0.004282 0.383919 0.037071 0.051840 0.001218 0.24 287.1 188.9 329.9 27.2 325.8 7.5 98%

ALT-2-20 0.35 0.00 5.33 0.053495 0.005637 0.388591 0.041554 0.052223 0.001404 0.25 350.1 236.1 333.3 30.4 328.2 8.6 98%

ALT-2-22 0.78 0.00 13.12 0.054071 0.005859 0.387942 0.050350 0.051322 0.000829 0.12 372.3 250.9 332.9 36.8 322.6 5.1 96%

ALT-2-25 0.47 0.00 7.89 0.055042 0.006468 0.387114 0.051205 0.051683 0.001150 0.17 413.0 264.8 332.3 37.5 324.8 7.1 97%

ALT-2-28 0.23 0.00 3.86 0.055277 0.006906 0.391563 0.052273 0.050983 0.001387 0.20 433.4 281.4 335.5 38.1 320.6 8.5 95%

ALT-2-32 0.54 0.00 8.85 0.052367 0.002888 0.379870 0.019180 0.051662 0.000828 0.32 301.9 130.5 326.9 14.1 324.7 5.1 99%

ALT-2-35 2.27 0.06 36.67 0.053085 0.005420 0.387078 0.038674 0.051426 0.000939 0.18 331.5 233.3 332.2 28.3 323.3 5.8 97%

ALT-2-37 1.60 0.00 27.71 0.052217 0.005483 0.374486 0.041443 0.050863 0.000849 0.15 294.5 240.7 323.0 30.6 319.8 5.2 99%

 19

ALT-2-38 0.35 0.02 5.67 0.053983 0.003923 0.388816 0.031854 0.051008 0.001004 0.24 368.6 164.8 333.5 23.3 320.7 6.2 96%

ALT-2-39 1.62 0.07 28.75 0.054052 0.005587 0.371661 0.032295 0.050167 0.000644 0.15 372.3 235.2 320.9 23.9 315.5 4.0 98%

ALT-2-40 1.67 0.00 29.06 0.052430 0.004598 0.371469 0.034316 0.050802 0.000659 0.14 305.6 200.0 320.7 25.4 319.4 4.0 99%

ALT-2-26 0.39 0.00 6.11 0.063823 0.008708 0.430362 0.061245 0.050329 0.001270 0.18 744.5 297.2 363.4 43.5 316.5 7.8 86%

ALT-2-27 0.24 0.00 4.09 0.056183 0.007224 0.396633 0.055757 0.051253 0.001106 0.15 461.2 287.8 339.2 40.5 322.2 6.8 94%

ALT-2-21 1.95 0.06 28.14 0.073503 0.004496 0.525568 0.035942 0.052251 0.000740 0.21 1027.8 124.1 428.9 23.9 328.3 4.5 73%

ZW-1-02 0.48 0.00 9.28 0.052461 0.008489 0.356047 0.055767 0.049070 0.003497 0.46 305.6 333.3 309.3 41.8 308.8 21.5 99%

ZW-1-05 0.15 0.00 2.85 0.054648 0.015084 0.367678 0.037709 0.050246 0.002196 0.43 398.2 522.2 317.9 28.0 316.0 13.5 99%

ZW-1-08 0.40 0.00 7.53 0.052008 0.009324 0.368990 0.028997 0.051590 0.001558 0.38 287.1 362.9 318.9 21.5 324.3 9.6 98%

ZW-1-09 0.76 0.00 14.56 0.052382 0.007348 0.373098 0.031781 0.051384 0.001776 0.41 301.9 292.6 321.9 23.5 323.0 10.9 99%

ZW-1-11 0.16 0.00 3.21 0.061138 0.014556 0.372520 0.055147 0.050184 0.002943 0.40 642.6 529.6 321.5 40.8 315.6 18.1 98%

ZW-1-12 0.57 0.00 11.04 0.054385 0.006090 0.377190 0.026870 0.050127 0.001307 0.37 387.1 249.0 325.0 19.8 315.3 8.0 96%

ZW-1-13 0.44 0.00 8.14 0.053425 0.009350 0.388567 0.048886 0.052685 0.001889 0.28 346.4 355.5 333.3 35.7 331.0 11.6 99%

ZW-1-15 0.29 0.00 5.51 0.052032 0.008572 0.377374 0.039034 0.052285 0.002972 0.55 287.1 346.3 325.1 28.8 328.5 18.2 98%

ZW-1-16 0.22 0.00 4.33 0.053916 0.008173 0.377843 0.037429 0.051192 0.001905 0.38 368.6 307.4 325.4 27.6 321.8 11.7 98%

ZW-1-17 0.31 0.00 5.96 0.052665 0.008322 0.380715 0.044803 0.052329 0.001819 0.30 322.3 316.6 327.6 32.9 328.8 11.1 99%

ZW-1-19 0.48 0.00 9.37 0.051039 0.006712 0.374645 0.044884 0.051877 0.001789 0.29 242.7 277.8 323.1 33.2 326.0 11.0 99%

ZW-1-20 0.17 0.00 3.40 0.052166 0.006011 0.380486 0.040250 0.051894 0.001781 0.32 300.1 297.2 327.4 29.6 326.1 10.9 99%

ZW-1-22 0.15 0.00 2.86 0.054964 0.019906 0.363082 0.123955 0.050879 0.004993 0.29 409.3 655.5 314.5 92.3 319.9 30.6 98%

ZW-1-29 0.05 0.00 0.88 0.056608 0.009171 0.369051 0.066252 0.050294 0.003104 0.34 476.0 360.1 318.9 49.1 316.3 19.1 99%

ZW-1-30 0.47 0.00 9.06 0.052394 0.007339 0.366122 0.052152 0.051068 0.002304 0.32 301.9 292.6 316.8 38.8 321.1 14.1 98%

ZW-1-33 0.41 0.00 7.31 0.055100 0.006478 0.396003 0.031517 0.053242 0.002662 0.63 416.7 266.6 338.7 22.9 334.4 16.3 98%

ZW-1-39 0.31 0.00 5.63 0.052753 0.006417 0.375215 0.034864 0.051506 0.001596 0.33 316.7 277.7 323.5 25.7 323.8 9.8 99%

ZW-1-01 0.56 0.04 9.13 0.057020 0.008799 0.425045 0.074198 0.053652 0.002094 0.22 500.0 545.3 359.7 52.9 336.9 12.8 93%

ZW-1-04 0.52 0.00 9.94 0.048311 0.011074 0.340464 0.025074 0.051224 0.001658 0.44 122.3 466.6 297.5 19.0 322.0 10.2 92%

ZW-1-06 0.37 0.00 6.89 0.062897 0.016693 0.443902 0.041692 0.051173 0.002031 0.42 705.6 588.8 373.0 29.3 321.7 12.5 85%

ZW-1-21 0.71 0.02 12.95 0.059375 0.003525 0.436805 0.022258 0.052259 0.001204 0.45 588.9 125.0 368.0 15.7 328.4 7.4 88%

ZW-1-23 0.63 0.00 11.41 0.047246 0.004157 0.364392 0.030336 0.054562 0.002081 0.46 61.2 196.3 315.5 22.6 342.5 12.7 91%

ZW-1-24 0.07 0.00 1.18 0.066275 0.009701 0.476941 0.052043 0.054614 0.003423 0.57 816.7 309.2 396.0 35.8 342.8 20.9 85%

ZW-1-38 0.31 0.01 5.56 0.046861 0.005833 0.332014 0.036004 0.051252 0.002965 0.53 42.7 274.0 291.1 27.4 322.2 18.2 89%

 20

ZW-1-03 0.18 0.01 2.89 0.078415 0.015429 0.574477 0.056524 0.053417 0.001887 0.36 1166.7 398.1 460.9 36.5 335.5 11.5 68%

ZW-1-07 0.51 0.03 7.71 0.109556 0.024270 0.825151 0.069606 0.054353 0.001779 0.39 1792.3 414.0 610.9 38.7 341.2 10.9 43%

ZW-1-14 0.47 0.20 6.18 0.117188 0.018316 0.966055 0.116226 0.056984 0.001908 0.28 1913.9 284.7 686.4 60.0 357.3 11.6 36%

ZW-1-18 0.68 0.23 9.89 0.102210 0.009580 0.828217 0.049678 0.057473 0.001414 0.41 1664.8 174.1 612.6 27.6 360.2 8.6 48%

ZW-1-25 0.03 0.00 0.44 0.071301 0.011498 0.490726 0.071191 0.053089 0.003321 0.43 966.4 333.3 405.4 48.5 333.5 20.3 80%

ZW-1-26 0.14 0.01 2.09 0.096164 0.010849 0.681663 0.065627 0.054505 0.002095 0.40 1550.9 213.0 527.8 39.6 342.1 12.8 57%

ZW-1-28 0.12 0.03 1.75 0.102786 0.011412 0.775570 0.078349 0.056252 0.002110 0.37 1675.9 239.4 583.0 44.8 352.8 12.9 50%

ZW-1-32 0.40 0.02 5.98 0.087769 0.004968 0.668535 0.035863 0.055395 0.001239 0.42 1377.5 109.3 519.8 21.8 347.6 7.6 60%

ZW-1-34 0.07 0.01 1.19 0.047076 0.007642 0.343747 0.045080 0.056073 0.003010 0.41 53.8 412.9 300.0 34.1 351.7 18.4 84%

ZW-1-35 0.73 0.05 12.20 0.067373 0.003630 0.495907 0.024506 0.052825 0.001077 0.41 850.0 116.8 408.9 16.6 331.8 6.6 79%

ZW-1-36 0.24 0.01 3.94 0.073585 0.005592 0.538840 0.040659 0.052484 0.001607 0.41 1031.5 149.1 437.7 26.8 329.8 9.8 71%

ZW-1-2-2 0.76 0.01 14.63 0.052276 0.004202 0.374300 0.029524 0.051808 0.001188 0.29 298.2 185.2 322.8 21.8 325.6 7.3 99%

ZW-1-2-4 0.83 0.00 16.16 0.053228 0.004356 0.370569 0.026479 0.051116 0.001102 0.30 338.9 189.8 320.1 19.6 321.4 6.8 99%

ZW-1-2-9 0.93 0.02 16.50 0.055622 0.005811 0.389291 0.027937 0.051310 0.001228 0.33 438.9 233.3 333.9 20.4 322.6 7.5 96%

ZW-1-2-10 0.98 0.00 19.13 0.052715 0.004169 0.372498 0.024118 0.050878 0.001140 0.35 316.7 181.5 321.5 17.8 319.9 7.0 99%

ZW-1-2-14 0.96 0.00 18.63 0.049865 0.005978 0.360885 0.040146 0.050987 0.001550 0.27 187.1 268.5 312.9 30.0 320.6 9.5 97%

ZW-1-2-16 1.26 0.00 23.71 0.052314 0.003447 0.373452 0.021255 0.050769 0.000909 0.31 298.2 150.0 322.2 15.7 319.2 5.6 99%

ZW-1-2-17 0.43 0.00 8.11 0.051484 0.006177 0.364015 0.043055 0.050569 0.002135 0.36 261.2 255.5 315.2 32.1 318.0 13.1 99%

ZW-1-2-20 2.02 0.01 37.22 0.051312 0.005717 0.363281 0.036151 0.051270 0.001325 0.26 253.8 246.3 314.7 26.9 322.3 8.1 97%

ZW-1-2-22 0.56 0.00 10.37 0.052941 0.003599 0.374579 0.024535 0.051403 0.001100 0.33 327.8 153.7 323.0 18.1 323.1 6.7 99%

ZW-1-2-23 0.36 0.00 6.86 0.054434 0.006640 0.370871 0.038009 0.051725 0.001526 0.29 390.8 271.3 320.3 28.2 325.1 9.4 98%

ZW-1-2-25 0.73 0.00 14.16 0.050927 0.003031 0.365390 0.021274 0.051633 0.000996 0.33 239.0 137.0 316.2 15.8 324.5 6.1 97%

ZW-1-2-26 1.25 0.00 24.59 0.056436 0.004200 0.387194 0.024034 0.050359 0.001242 0.40 477.8 166.6 332.3 17.6 316.7 7.6 95%

ZW-1-2-27 0.31 0.00 6.03 0.051837 0.005423 0.369666 0.035599 0.050652 0.001264 0.26 279.7 240.7 319.4 26.4 318.5 7.8 99%

ZW-1-2-29 0.56 0.00 10.96 0.055499 0.004317 0.382572 0.028485 0.050243 0.001215 0.32 431.5 174.1 328.9 20.9 316.0 7.5 95%

ZW-1-2-30 1.37 0.01 26.06 0.054277 0.003496 0.381107 0.022252 0.050540 0.001127 0.38 383.4 144.4 327.9 16.4 317.8 6.9 96%

ZW-1-2-32 0.52 0.00 3.31 0.060936 0.013870 0.382762 0.068511 0.053482 0.002768 0.29 636.7 505.5 329.1 50.3 335.9 16.9 97%

ZW-1-2-33 0.70 0.01 9.85 0.054241 0.004522 0.382034 0.027606 0.051432 0.001255 0.34 388.9 188.9 328.5 20.3 323.3 7.7 98%

ZW-1-2-36 0.58 0.01 13.83 0.052069 0.004383 0.368194 0.023935 0.050787 0.001173 0.36 287.1 197.2 318.3 17.8 319.4 7.2 99%

ZW-1-2-1 0.55 0.00 11.34 0.049805 0.003763 0.349209 0.025593 0.051312 0.001717 0.46 187.1 166.6 304.1 19.3 322.6 10.5 94%

 21

ZW-1-2-3 0.48 0.00 10.89 0.046800 0.004328 0.329523 0.029214 0.050781 0.001363 0.30 39.0 216.6 289.2 22.3 319.3 8.4 90%

ZW-1-2-5 0.11 0.01 8.46 0.091635 0.011067 0.601268 0.054032 0.051308 0.001762 0.38 1461.1 231.5 478.0 34.3 322.5 10.8 61%

ZW-1-2-6 0.92 0.00 1.93 0.068330 0.009874 0.509424 0.069679 0.053346 0.002557 0.35 879.6 303.7 418.1 46.9 335.0 15.6 77%

ZW-1-2-7 0.50 0.02 17.53 0.060307 0.005462 0.423220 0.031637 0.050805 0.001328 0.35 613.0 196.3 358.4 22.6 319.5 8.1 88%

ZW-1-2-8 0.95 0.02 7.18 0.119399 0.011688 0.914755 0.078644 0.056075 0.001781 0.37 1947.2 175.9 659.6 41.7 351.7 10.9 39%

ZW-1-2-11 1.02 0.07 16.74 0.067973 0.005340 0.502924 0.032011 0.052768 0.001259 0.37 877.8 169.4 413.7 21.6 331.5 7.7 77%

ZW-1-2-12 0.13 0.05 16.81 0.069664 0.006075 0.538995 0.037057 0.055208 0.001357 0.36 918.2 180.1 437.8 24.5 346.4 8.3 76%

ZW-1-2-13 1.63 0.01 1.92 0.097248 0.011434 0.778634 0.078841 0.058906 0.002663 0.45 1572.2 188.7 584.7 45.0 369.0 16.2 54%

ZW-1-2-15 1.52 0.00 32.43 0.046061 0.003314 0.322996 0.018479 0.049810 0.001054 0.37 400.1 -235.2 284.2 14.2 313.4 6.5 90%

ZW-1-2-18 0.16 0.00 29.42 0.039623 0.002903 0.281438 0.018981 0.051026 0.001246 0.36 251.8 15.0 320.8 7.6 75% ZW-1-2-19 0.58 0.00 3.10 0.049528 0.006455 0.320880 0.029193 0.051228 0.002299 0.49 172.3 277.7 282.6 22.4 322.1 14.1 86%

ZW-1-2-21 1.23 0.00 11.26 0.041314 0.002655 0.290016 0.016714 0.051426 0.001138 0.38 258.6 13.2 323.3 7.0 77% ZW-1-2-24 0.56 0.13 13.21 0.172759 0.008771 1.498856 0.067134 0.062559 0.001099 0.39 2584.3 117.6 929.9 27.3 391.2 6.7 18%

ZW-1-2-28 1.23 0.03 8.71 0.109712 0.007263 0.796932 0.041753 0.053769 0.001239 0.44 1794.8 121.0 595.1 23.6 337.6 7.6 44%

ZW-1-2-31 0.19 0.40 17.73 0.128260 0.006475 0.952263 0.041850 0.053437 0.000965 0.41 2075.9 88.7 679.3 21.8 335.6 5.9 32%

ZW-1-2-34 1.24 0.02 20.03 0.076463 0.005613 0.574608 0.030300 0.053847 0.001177 0.41 1107.1 146.8 461.0 19.5 338.1 7.2 69%

ZW-1-2-35 0.37 0.01 6.91 0.069240 0.008117 0.494423 0.055832 0.051210 0.002223 0.38 905.6 244.4 407.9 37.9 321.9 13.6 76%

KP-1-03 0.30 0.00 5.62 0.051882 0.003705 0.360136 0.024859 0.049985 0.001047 0.30 279.7 162.9 312.3 18.6 314.4 6.4 99%

KP-1-04 0.30 0.00 5.59 0.053150 0.003961 0.371698 0.027789 0.050678 0.001059 0.28 344.5 163.9 320.9 20.6 318.7 6.5 99%

KP-1-05 0.28 0.01 5.06 0.053065 0.003678 0.384442 0.026176 0.052558 0.001156 0.32 331.5 159.2 330.3 19.2 330.2 7.1 99%

KP-1-07 0.30 0.00 5.44 0.050129 0.004521 0.357888 0.036761 0.050321 0.000988 0.19 211.2 187.0 310.6 27.5 316.5 6.1 98%

KP-1-08 0.30 0.00 5.40 0.050983 0.005047 0.357810 0.039486 0.049336 0.000881 0.16 239.0 214.8 310.6 29.5 310.4 5.4 99%

KP-1-10 0.03 0.00 0.56 0.058191 0.009704 0.375899 0.043718 0.051700 0.004030 0.67 600.0 370.3 324.0 32.3 325.0 24.7 99%

KP-1-12 0.21 0.00 3.73 0.049596 0.004592 0.357520 0.036686 0.050713 0.001090 0.21 176.0 212.9 310.4 27.4 318.9 6.7 97%

KP-1-13 0.33 0.00 5.90 0.050537 0.004079 0.365136 0.031193 0.051529 0.001110 0.25 220.4 188.9 316.0 23.2 323.9 6.8 97%

KP-1-14 0.33 0.00 6.23 0.052817 0.003299 0.362874 0.022257 0.049627 0.000773 0.25 320.4 142.6 314.4 16.6 312.2 4.7 99%

KP-1-15 0.36 0.00 6.19 0.052632 0.004600 0.394510 0.039554 0.053505 0.000902 0.17 322.3 200.0 337.7 28.8 336.0 5.5 99%

KP-1-16 0.36 0.00 6.64 0.050393 0.003519 0.355146 0.024737 0.051029 0.000851 0.24 213.0 162.9 308.6 18.5 320.8 5.2 96%

KP-1-17 0.37 0.00 6.70 0.051439 0.003642 0.366038 0.028999 0.050918 0.001022 0.25 261.2 158.3 316.7 21.6 320.2 6.3 98%

 22

KP-1-18 0.09 0.00 1.54 0.055530 0.007017 0.376134 0.039496 0.051199 0.001916 0.36 435.2 285.1 324.2 29.2 321.9 11.7 99%

KP-1-21 0.41 0.00 7.22 0.050133 0.003610 0.366275 0.026709 0.051771 0.000984 0.26 211.2 163.9 316.9 19.9 325.4 6.0 97%

KP-1-27 0.48 0.00 8.74 0.052300 0.003431 0.373202 0.025096 0.050624 0.000773 0.32 298.2 150.0 322.0 18.6 318.3 4.7 98%

KP-1-30 0.17 0.00 3.00 0.051733 0.006110 0.358711 0.046638 0.049032 0.001732 0.27 272.3 251.8 311.3 34.9 308.6 10.6 99%

KP-1-31 0.08 0.00 1.40 0.054640 0.008524 0.384228 0.055253 0.052730 0.002726 0.36 398.2 161.1 330.1 40.6 331.3 16.7 99%

KP-1-32 0.46 0.00 7.90 0.051186 0.006155 0.372015 0.053814 0.050594 0.001093 0.15 250.1 255.5 321.1 39.8 318.2 6.7 99%

KP-1-33 0.04 0.00 0.63 0.051649 0.006253 0.380354 0.044193 0.053981 0.003417 0.54 333.4 194.4 327.3 32.5 338.9 20.9 96%

KP-1-34 0.37 0.00 6.26 0.052859 0.004046 0.378291 0.028783 0.051724 0.001121 0.28 324.1 174.1 325.8 21.2 325.1 6.9 99%

KP-1-35 0.47 0.00 7.84 0.050516 0.006002 0.380691 0.059393 0.051423 0.001307 0.16 220.4 251.8 327.5 43.7 323.3 8.0 98%

KP-1-37 0.07 0.00 1.30 0.055273 0.009093 0.362670 0.053853 0.050324 0.002418 0.32 433.4 374.0 314.2 40.1 316.5 14.8 99%

KP-1-39 0.17 0.00 2.87 0.052533 0.007230 0.370353 0.054173 0.050533 0.001093 0.15 309.3 285.2 319.9 40.2 317.8 6.7 99%

KP-1-40 0.12 0.00 1.92 0.050948 0.006552 0.370519 0.052032 0.051496 0.001801 0.25 239.0 270.3 320.0 38.6 323.7 11.0 98%

KP-1-02 0.05 0.00 0.90 0.069738 0.013742 0.467167 0.069600 0.054417 0.003010 0.37 920.4 413.4 389.2 48.2 341.6 18.4 86%

KP-1-09 0.15 0.00 2.37 0.060992 0.005253 0.413446 0.031138 0.050354 0.001724 0.45 638.9 185.2 351.4 22.4 316.7 10.6 89%

KP-1-20 0.26 0.00 4.50 0.054369 0.006538 0.404505 0.059512 0.051209 0.001153 0.15 387.1 267.6 344.9 43.1 321.9 7.1 93%

KP-1-23 0.13 0.00 1.88 0.064504 0.013394 0.442268 0.084944 0.053003 0.002245 0.22 766.7 444.3 371.9 59.9 332.9 13.7 88%

KP-1-28 0.28 0.00 4.55 0.054197 0.007013 0.436637 0.073553 0.053919 0.001233 0.23 388.9 299.0 367.9 52.0 338.5 7.5 91%

KP-1-29 0.15 0.00 2.31 0.054483 0.006733 0.440215 0.068697 0.055477 0.001780 0.14 390.8 284.2 370.4 48.5 348.1 10.9 93%

KP-1-11 0.06 0.00 0.76 0.083759 0.018838 0.911288 0.320973 0.051437 0.003763 0.21 1287.0 450.0 657.7 #### 323.3 23.1 31%

KP-1-22 0.01 0.00 0.13 0.241155 0.051023 1.458658 0.241107 0.055392 0.006382 0.70 3127.5 342.9 913.5 99.9 347.5 39.0 10%

KP-1-24 0.50 0.00 8.94 0.066092 0.002825 0.476174 0.022440 0.050640 0.000775 0.62 809.3 89.7 395.4 15.4 318.5 4.8 78%

KP-1-25 0.03 0.02 0.47 0.157390 0.020388 1.085187 0.105962 0.054273 0.003280 0.21 2428.1 220.8 746.2 51.6 340.7 20.1 25%

KP-1-36 0.12 0.00 1.74 0.056406 0.010682 0.490256 0.125656 0.053825 0.002249 0.16 477.8 362.6 405.1 85.8 338.0 13.8 81%

KP-1-38 0.10 0.00 1.65 0.058407 0.008140 0.397230 0.068553 0.049106 0.001911 0.23 546.3 313.9 339.6 49.9 309.0 11.7 90%