Geochronology and Tectonic Setting of the Lamasu Cu Deposit in Northern Xinjiang: Evidence from In-situ LA-ICP-MS Garnet U-Pb Dating

doi:10.19657/j.geoscience.1000-8527.2023.003

Abstract

Abstract:

Garnet, as a typical altered mineral in skarn deposits, is suggested to be an important mineral for obtaining accurate ore-forming age. There are abundant skarn Cu deposits in the Chinese Western Tianshan, yet the actual skarn Cu ore-forming ages remain controversial. This limits sufficient understanding of skarn Cu ore genesis and metallogenic dynamic background in the Chinese Western Tianshan. To obtain accurate metallogenic age of skarn Cu deposits in the Chinese Western Tianshan, we selected garnet from the Lamasu Cu deposit for systematic geochemical and geochronological study by Electron Probe X-ray Micro-Analyzer (EPMA) and LA-ICP-MS U-Pb dating. According to the hand-specimen and petrographic characteristics of the garnet minerals, the Lamasu deposit has three types of garnets, including red-brown, light-brown and yellow-green garnets. These garnets belong to the andradite-grossularite series, and occur as andradite (56.96%-85.09%) with minor grossularite (14.33%-43.85%). Three types of garnets yielded LA-ICP-MS U-Pb weighted average ages of (389.1±2.0) to (387.0±2.3) Ma, indicating that the Lamasu Cu mineralization occurred during the Middle Devonian subduction of the northern Tianshan oceanic crust.

Key words: LA-ICP-MS U-Pb dating, garnet, skarn, Lamasu, Xinjiang

CLC Number:

WANG Xiaotong, LIU Jun, YANG Yan, HE Juncheng. Geochronology and Tectonic Setting of the Lamasu Cu Deposit in Northern Xinjiang: Evidence from In-situ LA-ICP-MS Garnet U-Pb Dating[J]. Geoscience, 2023, 37(03): 645-661.

Figures/Tables 9

References 80

[1]	薛春纪, 赵晓波, 张国震, 等. 西天山金铜多金属重要成矿类型、成矿环境及找矿潜力[J]. 中国地质, 2015, 42(3): 381-410.
[2]	薛春纪, 赵晓波, 莫宣学, 等. 西天山巨型金铜铅锌成矿带构造成矿演化和找矿方向[J]. 地质学报, 2014, 88(12): 2490-2531.
[3]	ROBB L J. Introduction to ore-forming processes[M]. Malden: Blackwell Publication, 2005: 113-117.
[4]	TANG G J, WANG Q, WYMAN D A, et al. Geochronology and geochemistry of Late Paleozoic magmatic rocks in the Lamasu-Dabate area, northwestern Tianshan(west China): Evidence for a tectonic transition from arc to post-collisional setting[J]. Lithos, 2010, 119(3/4): 393-411. DOI URL
[5]	张东阳, 张招崇, 薛春纪, 等. 西天山喇嘛苏铜矿成矿斑岩的岩石学、地球化学特征及成因探讨[J]. 岩石学报, 2010, 26(3): 680-694.
[6]	LIU J, MAO J W, LAI C K, et al. Contrasting geochemical signatures between fertile and barren granites and multi-isotope (Sr-Nd-Pb-S-He) study in the Lamasu-Saibo deposit, NW China: Implications for petrogenesis and ore genesis[J]. Ore Geology Reviews, 2022, 149: 105114. DOI URL
[7]	杨军臣, 崔彬, 李天福. 新疆博乐喇嘛苏铜矿床地质特征和成因研究[J]. 地质论评, 1998, 44(1): 23-30.
[8]	王核, 彭省临, 赖健清. 论新疆喇嘛苏铜矿床的多因复成成矿作用[J]. 大地构造与成矿学, 2001, 25(2): 149-154.
[9]	廖启林, 赖健清. 新疆北部喇嘛苏铜矿区有关岩石的稀土元素地球化学[J]. 地质找矿论丛, 2002, 17(3): 145-151.
[10]	李华芹, 陈富文, 等. 中国新疆区域成矿作用年代学[M]. 北京: 地质出版社, 2004: 202-205.
[11]	ZHANG Z H, WANG Z L, WANG L S, et al. Metallogenic epoch and ore-forming environment of the Lamasu skarn-porphyritic Cu-Zn deposit, western Tianshan, Xinjiang, NW China[J]. Acta Geologica Sinica, 2008, 82(4): 731-740. DOI URL
[12]	唐功建, 王强, 赵振华, 等. 西天山喇嘛苏成矿斑岩年代学、地球化学特征与成因初探[J]. 矿物岩石地球化学通报, 2008, 27(增): 269-271.
[13]	石海岗. 新疆西天山喇嘛苏铜矿床成矿流体研究[D]. 北京: 中国地质大学(北京), 2011.
[14]	ZHU M T, WU G, XIE H J, et al. Geochronology and fluid inclusion studies of the Lailisigaoer and Lamasu porphyry-skarn Cu-Mo deposits in Northwestern Tianshan, China[J]. Journal of Asian Earth Sciences, 2012, 49: 116-130. DOI URL
[15]	解洪晶, 武广, 朱明田, 等. 西天山喇嘛苏岩体年代学、地球化学及成矿意义[J]. 地学前缘, 2013, 20(1): 190-205.
[16]	ZHAN X Z, YUE J H, CHEN C, et al. Granite zircon U-Pb geochronology and geochemistry and the geological significance of the Saibo copper deposit in the western Tianshan Mountains, Xinjiang Province, China[J]. Ore Geology Reviews, 2018, 99: 58-74. DOI URL
[17]	FERNANDO G W A R, HAUZENBERGER C A, BAUMGARTNER L P, et al. Modeling of retrograde diffusion zoning in garnet: Evidence for slow cooling of granulites from the Highland Complex of Sri Lanka[J]. Mineralogy and Petrology, 2003, 78(1/2): 53-71. DOI URL
[18]	KIM H S. Deformation-induced garnet zoning[J]. Gondwana Research, 2006, 10(3/4): 379-388. DOI URL
[19]	GASPAR M, KNAACK C, MEINERT L D, et al. REE in skarn systems: A LA-ICP-MS study of garnets from the Crown Jewel gold deposit[J]. Geochimica et Cosmochimica Acta, 2008, 72(1): 185-205. DOI URL
[20]	MARTIN L A J, BALLÈVRE M, BOULVAIS P, et al. Garnet re-equilibration by coupled dissolution-reprecipitation: Evidence from textural, major element and oxygen isotope zoning of ‘cloudy’ garnet[J]. Journal of Metamorphic Geology, 2011, 29(2):213-231. DOI URL
[21]	ZHAI D G, LIU L L, ZHANG H Y, et al. Origin of oscillatory zoned garnets from the Xieertala Fe-Zn skarn deposit, northern China: In situ LA-ICP-MS evidence[J]. Lithos, 2014, 190/191: 279-291. DOI URL
[22]	边晓龙, 张静, 王佳琳, 等. 滇西北红山矽卡岩型铜矿床石榴子石原位成分及其地质意义[J]. 岩石学报, 2019, 35(5): 1463-1477.
[23]	TANG Y W, GAO J F, LAN T G, et al. In situ low-U garnet U-Pb dating by LA-SF-ICP-MS and its application in constraining the origin of Anji skarn system combined with Ar-Ar dating and Pb isotopes[J]. Ore Geology Reviews, 2021, 130: 103970. DOI URL
[24]	GEVEDON M, SEMAN S, BARNES J D, et al. Unraveling histories of hydrothermal systems via U-Pb laser ablation dating of skarn garnet[J]. Earth and Planetary Science Letters, 2018, 498: 237-246. DOI URL
[25]	WAFFORN S, SEMAN S, KYLE J R, et al. Andradite garnet U-Pb geochronology of the big gossan skarn, ertsberg-grasberg mining district, Indonesia[J]. Economic Geology, 2018, 113(3): 769-778. DOI URL
[26]	LI N, YANG F Q, ZHANG Z X, et al. Geochemistry and chronology of the biotite granite in the Xiaobaishitou W-(Mo) depo-sit, eastern Tianshan, China: Petrogenesis and tectonic implications[J]. Ore Geology Reviews, 2019, 107: 999-1019. DOI URL
[27]	DUAN Z, GLEESON S A, GAO W S, et al. Garnet U-Pb dating of the Yinan Au-Cu skarn deposit, Luxi District, North China Craton: Implications for district-wide coeval Au-Cu and Fe skarn mineralization[J]. Ore Geology Reviews, 2020, 118: 103310. DOI URL
[28]	刘益, 孔志岗, 陈港, 等. 滇东南官房钨矿床石榴子石原位LA-SF-ICP-MS U-Pb定年及地质意义[J]. 岩石学报, 2021, 37(3): 847-864.
[29]	高俊, 钱青, 龙灵利, 等. 西天山的增生造山过程[J]. 地质通报, 2009, 28(12): 1804-1816.
[30]	JIANG Z S, WANG D C, ZHANG Z H, et al. Application of in situ titanite U-Pb geochronology to volcanic-hosted magnetite deposit: New constraints on the timing and genesis of the Zhibo deposit, Western Tianshan, NW China[J]. Ore Geology Reviews, 2018, 95: 325-341. DOI URL
[31]	朱明田, 武广, 解洪晶, 等. 新疆西天山科克赛岩体年代学、地球化学及地质意义[J]. 岩石学报, 2011, 27(10): 3041-3054.
[32]	ZHANG D Y, ZHANG Z C, ENCARNACIÓN J, et al. Petrogenesis of the Kekesai composite intrusion, western Tianshan, NW China: Implications for tectonic evolution during Late Paleozoic time[J]. Lithos, 2012, 146/147: 65-79. DOI URL
[33]	LIU C, XUE C J, CHI G X, et al. Geology, geochronology and geochemistry of the Dabate Cu-Mo deposit, northern Chinese Tien Shan: Implications for spatial separation of copper and molybdenum mineralization[J]. Ore Geology Reviews, 2018, 92: 542-557. DOI URL
[34]	解洪晶. 西北天山晚古生代中酸性侵入岩成因及意义[D]. 北京: 中国科学院大学, 2012.
[35]	ZHANG W, LENG C B, ZHANG X C, et al. Petrogenesis of the Seleteguole granitoids from Jinhe County in Xinjiang (West China): Implications for the tectonic transformation of Northwest Tianshan[J]. Lithos, 2016, 256/257: 148-164. DOI URL
[36]	朱明田, 武广, 解洪晶, 等. 新疆西天山莱历斯高尔斑岩型铜钼矿床辉钼矿Re-Os同位素年龄及流体包裹体研究[J]. 岩石学报, 2010, 26(12): 3667-3682.
[37]	解洪晶, 武广, 朱明田, 等. 西北天山莱历斯高尔岩体年代学、地球化学及其成因[J]. 地质科学, 2013, 48(3): 827-846.
[38]	张东阳, 张招崇, 艾羽, 等. 西天山莱历斯高尔一带铜(钼)矿成矿斑岩年代学、地球化学及其意义[J]. 岩石学报, 2009, 25(6): 1319-1331.
[39]	薛春纪, 陈波, 贾志业, 等. 新疆西天山莱历斯高尔-3571斑岩铜钼矿田地质地球化学和成矿年代[J]. 地学前缘, 2011, 18(1): 149-165.
[40]	陈波. 新疆西天山莱历斯高尔—肯登高尔铜钼铅锌矿集区成矿作用研究[D]. 西安: 长安大学, 2011.
[41]	贾志业, 薛春纪, 屈文俊, 等. 新疆肯登高尔铜钼矿地质和S、Pb、O、H同位素组成及Re-Os测年[J]. 矿床地质, 2011, 30(1): 74-86.
[42]	WANG G N, GU X X, ZHANG Y M, et al. Ore genesis and hydrothermal evolution of the Kendenggao’er copper-molybdenum deposit, western Tianshan: Evidence from isotopes (S, Pb, H, O) and fluid inclusions[J]. Ore Geology Reviews, 2018, 100: 294-316. DOI URL
[43]	LIU R, CHEN G W. The 109 porphyry Cu deposit in the western Tianshan orogenic belt, NW China: An example of Cu mineralization in a reduced magmatic-hydrothermal system in an extensional setting[J]. Ore Geology Reviews, 2019, 112: 102989. DOI URL
[44]	高景刚, 李文渊, 薛春纪, 等. 新疆哈勒尕提铜铁矿床的成矿年代学研究[J]. 矿床地质, 2014, 33(2): 386-396.
[45]	田宁. 西北天山阔库确科—哈勒尕提一带晚古生代岩浆作用与铁铜多金属成矿[D]. 武汉: 中国地质大学(武汉), 2016.
[46]	赵振华, 熊小林, 王强, 等. 新疆西天山莫斯早特石英钠长斑岩铜矿床——一个与埃达克质岩石有关的铜矿实例[J]. 岩石学报, 2004, 20(2): 249-258.
[47]	顾枫华, 章永梅, 彭义伟, 等. 新疆西天山阔库确科铁铜矿区成矿岩体地球化学、年代学特征及其地质意义[J]. 矿物学报, 2017, 37(增): 196-217.
[48]	顾雪祥, 章永梅, 王新利, 等. 新疆西天山可克萨拉—艾木斯呆依铁铜矿床成岩成矿年代学及其地质意义[J]. 地学前缘, 2013, 20(6): 195-209.
[49]	薛春纪, 王洪刚, 赵晓波, 等. 新疆西天山吐拉苏金矿集区克峡希小岩体群及其铜矿找矿前景[J]. 地学前缘, 2013, 20(6): 180-194.
[50]	WANG B, FAURE M, SHU L S, et al. Paleozoic tectonic evolution of the Yili Block, western Chinese Tianshan[J]. Bulletin De La Société Géologique De France, 2008, 179(5): 483-490. DOI URL
[51]	XIAO W J, SANTOSH M. The western Central Asian Orogenic Belt: A window to accretionary orogenesis and continental growth[J]. Gondwana Research, 2014, 25(4): 1429-1444. DOI URL
[52]	ZHU Y F, GUO X A, SONG B A, et al. Petrology, Sr-Nd-Hf isotopic geochemistry and zircon chronology of the Late Palaeozoic volcanic rocks in the southwestern Tianshan Mountains, Xinjiang, NW China[J]. Journal of the Geological Society, 2009, 166(6): 1085-1099. DOI URL
[53]	ZHONG L L, WANG B, ALEXEIEV D V, et al. Paleozoic multi-stage accretionary evolution of the SW Chinese Tianshan: New constraints from plutonic complex in the Nalati Range[J]. Gondwana Research, 2017, 45: 254-274. DOI URL
[54]	ZHU X Y, WANG B, CLUZEL D, et al. Early Neoproterozoic gneissic granitoids in the southern Yili Block (NW China): Constraints on microcontinent provenance and assembly in the SW Central Asian Orogenic Belt[J]. Precambrian Research, 2019, 325: 111-131. DOI URL
[55]	ZHU X Y, WANG B, SUN Z C, et al. Detrital zircon ages of the Mesoproterozoic metasedimentary rocks in the southern Yili Block: Implications for tectonic affinities of the microcontinents in SW Central Asian Orogenic Belt[J]. Precambrian Research, 2020, 350: 105926. DOI URL
[56]	SUN M J, CAI K D, SUN M, et al. Devonian arc-related granitoids in the Northwestern Chinese Tianshan, Central Asian Orogenic Belt: Implications for the bending of the Kazakhstan Orocline[J]. International Geology Review, 2020, 63(8): 992-1010. DOI URL
[57]	新疆维吾尔自治区地质矿产局. 新疆维吾尔自治区区域地质志[M]. 北京: 地质出版社, 1993: 1-941.
[58]	HUANG H, WANG T, TONG Y, et al. Rejuvenation of ancient micro-continents during accretionary orogenesis: Insights from the Yili Block and adjacent regions of the SW Central Asian Orogenic Belt[J]. Earth-Science Reviews, 2020, 208: 103255. DOI URL
[59]	陈有炘, 裴先治, 王盟, 等. 伊犁地块北缘别珍套山中泥盆统汗吉尕组物源特征及其地质意义[J]. 地球科学与环境学报, 2021, 43(3): 469-486.
[60]	新疆赛博矿业有限公司. 新疆博乐市喇嘛苏外围铜矿勘探工作报告(2015年度)[R]. 乌鲁木齐: 新疆赛博矿业有限公司, 2015.
[61]	展新忠. 新疆赛博铜矿床成矿作用及找矿勘查研究[D]. 徐州: 中国矿业大学, 2019.
[62]	SEMAN S, STOCKLI D F, MCLEAN N M. U-Pb geochronology of grossular-andradite garnet[J]. Chemical Geology, 2017, 460: 106-116. DOI URL
[63]	LUDWIG K R. User’s Manual for Isoplot 3.00: A Geochronological Toolkit for Microsoft Excel[M]. Berkeley: Berkeley Geochronology Center, 2003.
[64]	CHANG Z S, SHU Q H, MEINERT L D. Skarn deposits of China[J]. Economic Geology, 2019, 22: 189-234. DOI URL
[65]	MEZGER K, HANSON G N, BOHLEN S R. U-Pb systematics of garnet: dating the growth of garnet in the late Archean Pikwitonei granulite domain at Cauchon and Natawahunan Lakes, Manitoba, Canada[J]. Contributions to Mineralogy and Petrology, 1989, 101(2): 136-148. DOI URL
[66]	CADDICK M J, KONOPÁSEK J, THOMPSON A B. Preservation of garnet growth zoning and the duration of prograde metamorphism[J]. Journal of Petrology, 2010, 51(11): 2327-2347. DOI URL
[67]	BAGHBAN S, HOSSEINZADEH M R, MOAYYED M, et al. Chemical composition and evolution of the garnets in the Astamal Fe-LREE distal skarn deposit, Qara-Dagh-Sabalan metallogenic belt, Lesser Caucasus, NW Iran[J]. Ore Geology Reviews, 2016, 78: 166-175. DOI URL
[68]	DENG X D, LI J W, LUO T, et al. Dating magmatic and hydrothermal processes using andradite-rich garnet U-Pb geochronometry[J]. Contributions to Mineralogy and Petrology, 2017, 172(9): 71. DOI URL
[69]	WINDLEY B F, ALEXEIEV D, XIAO W J, et al. Tectonic models for accretion of the Central Asian Orogenic Belt[J]. Journal of the Geological Society, 2007, 164(1): 31-47. DOI URL
[70]	BISKE Y S, SELTMANN R. Paleozoic Tian-Shan as a transitional region between the Rheic and Urals-Turkestan Oceans[J]. Gondwana Research, 2010, 17(2/3): 602-613. DOI URL
[71]	顾雪祥, 章永梅, 彭义伟, 等. 西天山博罗科努成矿带与侵入岩有关的铁铜钼多金属成矿系统:成岩成矿地球化学与构造-岩浆演化[J]. 地学前缘, 2014, 21(5): 156-175. DOI
[72]	王强, 赵振华, 许继峰, 等. 天山北部石炭纪埃达克岩-高镁安山岩-富Nb岛弧玄武质岩:对中亚造山带显生宙地壳增生与铜金成矿的意义[J]. 岩石学报, 2006, 22(1): 11-30.
[73]	徐学义, 马中平, 夏祖春, 等. 天山中西段古生代花岗岩TIMS法锆石U-Pb同位素定年及岩石地球化学特征研究[J]. 西北地质, 2006, 39(1): 50-75.
[74]	徐学义, 夏林圻, 马中平, 等. 北天山巴音沟蛇绿岩斜长花岗岩SHRIMP锆石U-Pb年龄及蛇绿岩成因研究[J]. 岩石学报, 2006, 22(1): 83-94.
[75]	WANG B, SHU L S, CLUZEL D, et al. Geochemical constraints on Carboniferous volcanic rocks of the Yili Block (Xinjiang, NW China): Implication for the tectonic evolution of Western Tian-shan[J]. Journal of Asian Earth Sciences, 2007, 29(1): 148-159. DOI URL
[76]	胡霭琴, 韦刚健, 张积斌, 等. 西天山温泉地区早古生代斜长角闪岩的锆石SHRIMP U-Pb年龄及其地质意义[J]. 岩石学报, 2008, 24(12): 2731-2740.
[77]	ZHAO Z H, XIONG X L, WANG Q, et al. Underplating-related adakites in Xinjiang Tianshan, China[J]. Lithos, 2008, 102(1/2): 374-391. DOI URL
[78]	WANG B, CLUZEL D, SHU L S, et al. Evolution of calc-alkaline to alkaline magmatism through Carboniferous convergence to Permian transcurrent tectonics, western Chinese Tianshan[J]. International Journal of Earth Sciences, 2009, 98(6): 1275-1298. DOI URL
[79]	徐学义, 马中平, 夏林圻, 等. 北天山巴音沟蛇绿岩形成时代的精确厘定及意义[J]. 地球科学与环境学报, 2005, 27(2): 17-20.
[80]	ZHAO Z H, XIONG X L, WANG Q, et al. Late Paleozoic underplating in North Xinjiang: Evidence from shoshonites and adakites[J]. Gondwana Research, 2009, 16(2): 216-226. DOI URL

矿床名称	类型	金属量	品位	赋矿围岩	金属矿物	年龄(Ma)	参考文献
科克赛	斑岩型 Cu-Mo	27 kt Cu	0.2%~ 0.5% Cu	二长花岗斑岩、粉砂岩、砂岩	Cpy+Py+Po+Mo+Sph+Gal	锆石U-Pb:301.9±1.8	[31-32]
喇嘛苏	矽卡岩型Cu	0.6 Mt Cu	0.3%~ 6.3% Cu	花岗闪长斑岩、碳酸盐岩地层	Po+Mag+Cpy+Py+Sph+Mo	锆石U-Pb:(366.0±3.0)~(390.5±7.7) 石榴子石U-Pb:(389.4±2.0) ~(387.1±2.3)	[4,11,14?-16], 本次工作
达巴特	斑岩型 Cu-Mo	52 kt Cu, 5.6 t Mo	0.67% Cu	流纹斑岩、花岗斑岩、凝灰岩、砂岩	Cpy+Asp+Bo+Sph+Mo	锆石U-Pb:297.3±8.0 辉钼矿Re-Os:299.6±3.2	[33]
恰尔巴赫特	斑岩型 Cu-Mo	n/a	n/a	闪长岩、花岗闪长岩	Cpy+Mo+Cc+Py	锆石U-Pb:368.0±5.0、354.0±4.0	[34]
色勒特果勒	矽卡岩型 Cu-Mo	14 kt Cu, 357 t Mo	0.12%~ 2.02%Cu, 0.01%~ 0.1% Mo	闪长(玢)岩	Cpy+Bo+Mo+Cc+Py+Po	锆石U-Pb:301.8±2.9、302.4±2.6 辉钼矿Re-Os:301.0±2.0	[35]
莱历斯高尔	斑岩型 Cu-Mo	2 kt Cu 707 t Mo	2%Cu, 0.01%~ 0.2% Mo	花岗闪长斑岩、砂岩、粉砂岩	Mo+Py+Po+ Cpy	锆石U-Pb:374.0±4.0 辉钼矿Re-Os:372.5±5.0	[36-37]
3571	斑岩型Cu	2 kt Cu	n/a	花岗闪长斑岩	Cpy+Py+Po	锆石U-Pb:350.0±0.7、354.0±0.7	[38-39]
肯登高尔	矽卡岩型 Cu-Mo	19 kt Cu, 1 kt Mo	0.6%~ 1.2% Cu, 0.04%~ 0.3% Mo	花岗闪长岩、灰岩、粉砂岩	Cpy+Mo+Py+Bo+Po	锆石U-Pb:313.0±4.0、316.3±3.5 辉钼矿Re-Os:313.9±2.5	[40?-42]
109	斑岩型Cu	6.4 kt Cu	0.8% Cu	钠长斑岩	Cpy+Bo+Py	锆石U-Pb:300.0±4.0	[43]
哈勒尕提	矽卡岩型 Cu-Fe	n/a	n/a	二长花岗岩、碳酸盐岩地层	Cpy+Bo+Cc+Mag+Mo	锆石U-Pb:367.3±2.2、 368.0±2.0 辉钼矿Re-Os:370.1±2.4	[44-45]
莫斯早特	斑岩型Cu	n/a	n/a	钠长斑岩	Cpy+Bo+Cpy+Py	云母Ar-Ar:268.0±5.0	[46]
阔库确科	矽卡岩型Cu	n/a	n/a	花岗岩	Mag+Hem+ Cpy+Gal+Sph	锆石U-Pb:362.3±2.8	[47]
可克萨拉	矽卡岩型 Fe-Cu	n/a	n/a	二长花岗岩	Mag+Cpy+Py	辉钼矿Re-Os:288.3±1.5	[48]
克峡希	斑岩型Cu	51 kt Cu	0.48% Cu	闪长(玢)岩、花岗闪长岩	Cpy+Py+Sph+Gal	锆石U-Pb:357.2±3.0、356.4±2.2、350.8±3.8、348.0±2.2	[49]

矿床名称	类型	金属量	品位	赋矿围岩	金属矿物	年龄(Ma)	参考文献
科克赛	斑岩型 Cu-Mo	27 kt Cu	0.2%~ 0.5% Cu	二长花岗斑岩、粉砂岩、砂岩	Cpy+Py+Po+Mo+Sph+Gal	锆石U-Pb:301.9±1.8	[31-32]
喇嘛苏	矽卡岩型Cu	0.6 Mt Cu	0.3%~ 6.3% Cu	花岗闪长斑岩、碳酸盐岩地层	Po+Mag+Cpy+Py+Sph+Mo	锆石U-Pb:(366.0±3.0)~(390.5±7.7) 石榴子石U-Pb:(389.4±2.0) ~(387.1±2.3)	[4,11,14?-16], 本次工作
达巴特	斑岩型 Cu-Mo	52 kt Cu, 5.6 t Mo	0.67% Cu	流纹斑岩、花岗斑岩、凝灰岩、砂岩	Cpy+Asp+Bo+Sph+Mo	锆石U-Pb:297.3±8.0 辉钼矿Re-Os:299.6±3.2	[33]
恰尔巴赫特	斑岩型 Cu-Mo	n/a	n/a	闪长岩、花岗闪长岩	Cpy+Mo+Cc+Py	锆石U-Pb:368.0±5.0、354.0±4.0	[34]
色勒特果勒	矽卡岩型 Cu-Mo	14 kt Cu, 357 t Mo	0.12%~ 2.02%Cu, 0.01%~ 0.1% Mo	闪长(玢)岩	Cpy+Bo+Mo+Cc+Py+Po	锆石U-Pb:301.8±2.9、302.4±2.6 辉钼矿Re-Os:301.0±2.0	[35]
莱历斯高尔	斑岩型 Cu-Mo	2 kt Cu 707 t Mo	2%Cu, 0.01%~ 0.2% Mo	花岗闪长斑岩、砂岩、粉砂岩	Mo+Py+Po+ Cpy	锆石U-Pb:374.0±4.0 辉钼矿Re-Os:372.5±5.0	[36-37]
3571	斑岩型Cu	2 kt Cu	n/a	花岗闪长斑岩	Cpy+Py+Po	锆石U-Pb:350.0±0.7、354.0±0.7	[38-39]
肯登高尔	矽卡岩型 Cu-Mo	19 kt Cu, 1 kt Mo	0.6%~ 1.2% Cu, 0.04%~ 0.3% Mo	花岗闪长岩、灰岩、粉砂岩	Cpy+Mo+Py+Bo+Po	锆石U-Pb:313.0±4.0、316.3±3.5 辉钼矿Re-Os:313.9±2.5	[40?-42]
109	斑岩型Cu	6.4 kt Cu	0.8% Cu	钠长斑岩	Cpy+Bo+Py	锆石U-Pb:300.0±4.0	[43]
哈勒尕提	矽卡岩型 Cu-Fe	n/a	n/a	二长花岗岩、碳酸盐岩地层	Cpy+Bo+Cc+Mag+Mo	锆石U-Pb:367.3±2.2、 368.0±2.0 辉钼矿Re-Os:370.1±2.4	[44-45]
莫斯早特	斑岩型Cu	n/a	n/a	钠长斑岩	Cpy+Bo+Cpy+Py	云母Ar-Ar:268.0±5.0	[46]
阔库确科	矽卡岩型Cu	n/a	n/a	花岗岩	Mag+Hem+ Cpy+Gal+Sph	锆石U-Pb:362.3±2.8	[47]
可克萨拉	矽卡岩型 Fe-Cu	n/a	n/a	二长花岗岩	Mag+Cpy+Py	辉钼矿Re-Os:288.3±1.5	[48]
克峡希	斑岩型Cu	51 kt Cu	0.48% Cu	闪长(玢)岩、花岗闪长岩	Cpy+Py+Sph+Gal	锆石U-Pb:357.2±3.0、356.4±2.2、350.8±3.8、348.0±2.2	[49]

样号	TiO₂	CaO	K₂O	P₂O₅	NiO	Na₂O	MgO	SiO₂	Al₂O₃	MnO	FeO	Cr₂O₃	Total	Ura	And	Pyr	Spe	Gro
XS-54-1.1	0.14	35.46	0	0	0.01	0	0.19	36.77	6.81	0.12	19.43	0.02	98.95	0.05	63.49	0.73	0.27	35.46
XS-54-1.2	0.01	34.13	0.01	0.03	0	0.06	0.06	35.90	2.64	0.08	24.92	0.05	97.90	0.15	85.09	0.24	0.19	14.33
XS-54-1.3	0	34.93	0	0.04	0.01	0.02	0.04	36.55	6.19	0.13	20.91	0	98.82	0	69.77	0.17	0.28	29.77
XS-54-1.4	0	34.36	0.04	0.02	0	0.06	0.13	36.43	5.62	0.11	21.49	0.01	98.27	0.04	72.69	0.51	0.24	26.52
XS-54-1.5	0.02	34.52	0	0.03	0	0.03	0.04	36.37	6.13	0.15	20.84	0.02	98.15	0.07	70.32	0.18	0.33	29.10
XS-54-1.6	0.01	34.32	0	0	0	0.02	0.02	36.27	6.71	0.20	20.55	0.03	98.14	0.11	68.05	0.10	0.45	30.54
XS-54-1.7	0	35.03	0	0.03	0.03	0	0.02	35.94	4.53	0.13	23.18	0.01	98.90	0.04	77.17	0.08	0.30	22.40
XS-54-1.8	0	34.25	0.02	0.03	0	0.01	0.01	36.39	5.16	0.16	22.41	0	98.42	0	75.35	0.02	0.35	23.85
XS-54-1.9	0.02	33.78	0.02	0.04	0.01	0	0.03	37.04	5.90	0.18	21.68	0	98.70	0	71.72	0.11	0.42	26.41
XS-54-1.10	0.02	34.56	0.01	0	0	0.02	0.03	36.80	6.16	0.17	21.08	0.01	98.87	0.04	70.74	0.11	0.40	28.57
XS-54-1.11	0.01	33.99	0.01	0.01	0.03	0.03	0.05	35.95	3.12	0.16	24.83	0	98.17	0	84.96	0.22	0.37	14.44
XS-54-1.12	0	33.73	0	0	0	0.02	0.05	36.33	3.71	0.15	24.31	0	98.31	0	82.08	0.20	0.36	16.58
XS-54-1.13	0	34.20	0.01	0.01	0	0.03	0.01	36.73	6.33	0.18	20.74	0.01	98.23	0.02	69.72	0.03	0.41	29.38
XS-54-1.14	0.03	34.18	0	0	0.02	0.01	0.03	36.60	5.54	0.14	21.73	0	98.26	0	73.45	0.10	0.31	25.83
XS-54-1.15	0.06	34.70	0	0	0.02	0	0.03	36.30	6.75	0.17	20.13	0.01	98.16	0.03	67.58	0.12	0.39	31.88
样号	TiO₂	CaO	K₂O	P₂O₅	NiO	Na₂O	MgO	SiO₂	Al₂O₃	MnO	FeO	Cr₂O₃	Total	Ura	And	Pyr	Spe	Gro
XS-38-1.1	0.58	34.98	0.04	0.04	0	0.02	0.73	36.44	7.36	0.28	17.62	0.01	98.10	0.04	56.96	2.79	0.60	39.61
XS-38-1.2	0.49	33.73	0.02	0	0	0.05	0.60	35.45	8.33	0.26	16.49	2.75	98.15	8.61	52.46	2.35	0.57	34.51
XS-38-1.3	0.19	35.02	0.01	0.01	0.02	0	0.66	37.50	8.35	0.35	17.29	0	99.41	0.01	55.88	2.55	0.77	40.79
XS-38-1.4	0.07	35.08	0	0.02	0.04	0	0.62	37.98	8.04	0.36	17.95	0.02	100.16	0.05	58.02	2.37	0.77	38.78
XS-38-1.5	0.03	34.69	0	0.01	0	0.01	0.54	36.66	7.14	0.39	18.89	0.06	98.40	0.20	61.88	2.10	0.86	34.97
XS-38-1.6	0	35.15	0.01	0.01	0	0.01	0.52	37.51	9.78	0.32	16.48	0.01	99.79	0.04	53.41	2.01	0.70	43.85
XS-38-1.7	0.04	35.17	0.02	0.04	0	0.02	0.36	37.35	7.35	0.17	18.84	0.02	99.37	0.06	61.64	1.39	0.36	36.55
XS-38-1.8	0	35.07	0	0.02	0	0.07	0.28	37.73	6.75	0.20	19.67	0.01	99.79	0.02	64.67	1.07	0.45	33.79
XS-38-1.9	0	35.09	0.01	0.03	0	0.03	0.40	37.59	7.01	0.19	19.11	0	99.46	0	62.52	1.55	0.41	35.51
XS-38-1.10	0.05	34.99	0	0	0	0.02	0.26	37.19	6.24	0.20	20.03	0	98.98	0	66.07	1.01	0.44	32.48
XS-38-1.11	0.13	34.95	0	0.06	0.02	0.03	0.21	36.87	5.87	0.22	20.67	0.04	99.05	0.13	68.31	0.82	0.50	30.24
XS-38-1.12	0.01	34.82	0.01	0.02	0.01	0.01	0.23	36.41	4.59	0.18	22.54	0.03	98.87	0.10	74.80	0.91	0.40	23.79
样号	TiO₂	CaO	K₂O	P₂O₅	NiO	Na₂O	MgO	SiO₂	Al₂O₃	MnO	FeO	Cr₂O₃	Total	Ura	And	Pyr	Spe	Gro
XS-62-1.1	0.27	34.54	0	0	0	0.02	0.18	36.94	6.91	0.22	19.35	0.03	98.45	0.09	64.79	0.70	0.50	33.92
XS-62-1.2	0.38	34.58	0.02	0.01	0	0.01	0.35	36.61	7.42	0.25	18.48	0.01	98.13	0.02	61.35	1.37	0.57	36.68
XS-62-1.3	0.17	34.37	0.02	0.03	0.02	0.01	0.09	36.54	4.95	0.19	22.17	0	98.53	0	74.95	0.34	0.43	24.28
XS-62-1.4	0.33	34.90	0	0.03	0	0.03	0.24	36.89	6.08	0.15	20.08	0	98.74	0	66.49	0.94	0.34	32.24
XS-62-1.5	0.15	34.65	0.01	0	0	0	0.27	36.84	5.35	0.14	21.03	0.02	98.47	0.07	70.09	1.06	0.32	28.46
XS-62-1.6	0.50	34.57	0.01	0.04	0	0.04	0.28	36.52	6.12	0.18	20.09	0	98.35	0.01	67.02	1.11	0.41	31.46
XS-62-1.7	0.29	34.90	0	0.02	0.03	0	0.29	36.62	6.25	0.18	19.69	0.01	98.28	0.04	65.04	1.12	0.40	33.40
XS-62-1.8	0.36	34.87	0	0	0	0	0.25	37.05	6.67	0.21	19.52	0.01	98.93	0.04	64.61	0.97	0.46	33.92
XS-62-1.9	0.23	35.02	0.03	0.03	0.03	0	0.32	36.54	6.38	0.20	19.60	0	98.37	0	64.40	1.25	0.44	33.91
XS-62-1.10	0.31	34.61	0.01	0.01	0.01	0.01	0.25	36.67	6.00	0.18	20.03	0	98.08	0	66.79	1.01	0.41	31.79
XS-62-1.11	0.38	34.63	0.01	0.01	0.01	0.05	0.30	36.47	5.90	0.16	20.09	0.01	98.02	0.03	66.88	1.18	0.37	31.54
XS-62-1.12	0.36	34.63	0.01	0.03	0.03	0.02	0.24	36.30	5.31	0.21	20.95	0	98.09	0	69.83	0.95	0.47	28.75
XS-62-1.13	0.31	34.99	0.01	0.02	0	0	0.23	36.83	5.36	0.20	21.21	0	99.16	0	70.01	0.92	0.44	28.63
XS-62-1.14	0.19	34.68	0.02	0	0	0.01	0.17	36.61	6.39	0.24	19.97	0.01	98.29	0.03	66.59	0.69	0.54	32.15
XS-62-1.15	0.14	34.68	0	0.03	0	0	0.13	36.66	5.75	0.18	20.91	0	98.49	0	69.94	0.53	0.41	29.12

样号	TiO₂	CaO	K₂O	P₂O₅	NiO	Na₂O	MgO	SiO₂	Al₂O₃	MnO	FeO	Cr₂O₃	Total	Ura	And	Pyr	Spe	Gro
XS-54-1.1	0.14	35.46	0	0	0.01	0	0.19	36.77	6.81	0.12	19.43	0.02	98.95	0.05	63.49	0.73	0.27	35.46
XS-54-1.2	0.01	34.13	0.01	0.03	0	0.06	0.06	35.90	2.64	0.08	24.92	0.05	97.90	0.15	85.09	0.24	0.19	14.33
XS-54-1.3	0	34.93	0	0.04	0.01	0.02	0.04	36.55	6.19	0.13	20.91	0	98.82	0	69.77	0.17	0.28	29.77
XS-54-1.4	0	34.36	0.04	0.02	0	0.06	0.13	36.43	5.62	0.11	21.49	0.01	98.27	0.04	72.69	0.51	0.24	26.52
XS-54-1.5	0.02	34.52	0	0.03	0	0.03	0.04	36.37	6.13	0.15	20.84	0.02	98.15	0.07	70.32	0.18	0.33	29.10
XS-54-1.6	0.01	34.32	0	0	0	0.02	0.02	36.27	6.71	0.20	20.55	0.03	98.14	0.11	68.05	0.10	0.45	30.54
XS-54-1.7	0	35.03	0	0.03	0.03	0	0.02	35.94	4.53	0.13	23.18	0.01	98.90	0.04	77.17	0.08	0.30	22.40
XS-54-1.8	0	34.25	0.02	0.03	0	0.01	0.01	36.39	5.16	0.16	22.41	0	98.42	0	75.35	0.02	0.35	23.85
XS-54-1.9	0.02	33.78	0.02	0.04	0.01	0	0.03	37.04	5.90	0.18	21.68	0	98.70	0	71.72	0.11	0.42	26.41
XS-54-1.10	0.02	34.56	0.01	0	0	0.02	0.03	36.80	6.16	0.17	21.08	0.01	98.87	0.04	70.74	0.11	0.40	28.57
XS-54-1.11	0.01	33.99	0.01	0.01	0.03	0.03	0.05	35.95	3.12	0.16	24.83	0	98.17	0	84.96	0.22	0.37	14.44
XS-54-1.12	0	33.73	0	0	0	0.02	0.05	36.33	3.71	0.15	24.31	0	98.31	0	82.08	0.20	0.36	16.58
XS-54-1.13	0	34.20	0.01	0.01	0	0.03	0.01	36.73	6.33	0.18	20.74	0.01	98.23	0.02	69.72	0.03	0.41	29.38
XS-54-1.14	0.03	34.18	0	0	0.02	0.01	0.03	36.60	5.54	0.14	21.73	0	98.26	0	73.45	0.10	0.31	25.83
XS-54-1.15	0.06	34.70	0	0	0.02	0	0.03	36.30	6.75	0.17	20.13	0.01	98.16	0.03	67.58	0.12	0.39	31.88
样号	TiO₂	CaO	K₂O	P₂O₅	NiO	Na₂O	MgO	SiO₂	Al₂O₃	MnO	FeO	Cr₂O₃	Total	Ura	And	Pyr	Spe	Gro
XS-38-1.1	0.58	34.98	0.04	0.04	0	0.02	0.73	36.44	7.36	0.28	17.62	0.01	98.10	0.04	56.96	2.79	0.60	39.61
XS-38-1.2	0.49	33.73	0.02	0	0	0.05	0.60	35.45	8.33	0.26	16.49	2.75	98.15	8.61	52.46	2.35	0.57	34.51
XS-38-1.3	0.19	35.02	0.01	0.01	0.02	0	0.66	37.50	8.35	0.35	17.29	0	99.41	0.01	55.88	2.55	0.77	40.79
XS-38-1.4	0.07	35.08	0	0.02	0.04	0	0.62	37.98	8.04	0.36	17.95	0.02	100.16	0.05	58.02	2.37	0.77	38.78
XS-38-1.5	0.03	34.69	0	0.01	0	0.01	0.54	36.66	7.14	0.39	18.89	0.06	98.40	0.20	61.88	2.10	0.86	34.97
XS-38-1.6	0	35.15	0.01	0.01	0	0.01	0.52	37.51	9.78	0.32	16.48	0.01	99.79	0.04	53.41	2.01	0.70	43.85
XS-38-1.7	0.04	35.17	0.02	0.04	0	0.02	0.36	37.35	7.35	0.17	18.84	0.02	99.37	0.06	61.64	1.39	0.36	36.55
XS-38-1.8	0	35.07	0	0.02	0	0.07	0.28	37.73	6.75	0.20	19.67	0.01	99.79	0.02	64.67	1.07	0.45	33.79
XS-38-1.9	0	35.09	0.01	0.03	0	0.03	0.40	37.59	7.01	0.19	19.11	0	99.46	0	62.52	1.55	0.41	35.51
XS-38-1.10	0.05	34.99	0	0	0	0.02	0.26	37.19	6.24	0.20	20.03	0	98.98	0	66.07	1.01	0.44	32.48
XS-38-1.11	0.13	34.95	0	0.06	0.02	0.03	0.21	36.87	5.87	0.22	20.67	0.04	99.05	0.13	68.31	0.82	0.50	30.24
XS-38-1.12	0.01	34.82	0.01	0.02	0.01	0.01	0.23	36.41	4.59	0.18	22.54	0.03	98.87	0.10	74.80	0.91	0.40	23.79
样号	TiO₂	CaO	K₂O	P₂O₅	NiO	Na₂O	MgO	SiO₂	Al₂O₃	MnO	FeO	Cr₂O₃	Total	Ura	And	Pyr	Spe	Gro
XS-62-1.1	0.27	34.54	0	0	0	0.02	0.18	36.94	6.91	0.22	19.35	0.03	98.45	0.09	64.79	0.70	0.50	33.92
XS-62-1.2	0.38	34.58	0.02	0.01	0	0.01	0.35	36.61	7.42	0.25	18.48	0.01	98.13	0.02	61.35	1.37	0.57	36.68
XS-62-1.3	0.17	34.37	0.02	0.03	0.02	0.01	0.09	36.54	4.95	0.19	22.17	0	98.53	0	74.95	0.34	0.43	24.28
XS-62-1.4	0.33	34.90	0	0.03	0	0.03	0.24	36.89	6.08	0.15	20.08	0	98.74	0	66.49	0.94	0.34	32.24
XS-62-1.5	0.15	34.65	0.01	0	0	0	0.27	36.84	5.35	0.14	21.03	0.02	98.47	0.07	70.09	1.06	0.32	28.46
XS-62-1.6	0.50	34.57	0.01	0.04	0	0.04	0.28	36.52	6.12	0.18	20.09	0	98.35	0.01	67.02	1.11	0.41	31.46
XS-62-1.7	0.29	34.90	0	0.02	0.03	0	0.29	36.62	6.25	0.18	19.69	0.01	98.28	0.04	65.04	1.12	0.40	33.40
XS-62-1.8	0.36	34.87	0	0	0	0	0.25	37.05	6.67	0.21	19.52	0.01	98.93	0.04	64.61	0.97	0.46	33.92
XS-62-1.9	0.23	35.02	0.03	0.03	0.03	0	0.32	36.54	6.38	0.20	19.60	0	98.37	0	64.40	1.25	0.44	33.91
XS-62-1.10	0.31	34.61	0.01	0.01	0.01	0.01	0.25	36.67	6.00	0.18	20.03	0	98.08	0	66.79	1.01	0.41	31.79
XS-62-1.11	0.38	34.63	0.01	0.01	0.01	0.05	0.30	36.47	5.90	0.16	20.09	0.01	98.02	0.03	66.88	1.18	0.37	31.54
XS-62-1.12	0.36	34.63	0.01	0.03	0.03	0.02	0.24	36.30	5.31	0.21	20.95	0	98.09	0	69.83	0.95	0.47	28.75
XS-62-1.13	0.31	34.99	0.01	0.02	0	0	0.23	36.83	5.36	0.20	21.21	0	99.16	0	70.01	0.92	0.44	28.63
XS-62-1.14	0.19	34.68	0.02	0	0	0.01	0.17	36.61	6.39	0.24	19.97	0.01	98.29	0.03	66.59	0.69	0.54	32.15
XS-62-1.15	0.14	34.68	0	0.03	0	0	0.13	36.66	5.75	0.18	20.91	0	98.49	0	69.94	0.53	0.41	29.12

测点编号	U (10^-6)	Th (10^-6)	同位素比值						年龄(Ma)
测点编号	U (10^-6)	Th (10^-6)	²⁰⁷Pb/²⁰⁶Pb	1σ	²⁰⁷Pb/²³⁵U	1σ	²⁰⁶Pb/²³⁸U	1σ	²⁰⁶Pb/²³⁸U	1σ
XS-38-1.01	2.19	3.91	0.10624	0.00480	0.97423	0.04483	0.06701	0.00100	418.1	6.1
XS-38-1.02	2.80	3.03	0.06128	0.00281	0.52662	0.02345	0.06294	0.00074	393.5	4.5
XS-38-1.03	2.75	4.72	0.06566	0.00273	0.55335	0.02293	0.06154	0.00065	385.0	4.0
XS-38-1.04	3.15	5.49	0.06828	0.00245	0.57845	0.02025	0.06212	0.00073	388.5	4.4
XS-38-1.05	3.24	5.02	0.08470	0.00330	0.74906	0.02955	0.06397	0.00069	399.7	4.2
XS-38-1.06	2.44	5.00	0.06519	0.00317	0.57318	0.02722	0.06473	0.00085	404.4	5.1
XS-38-1.07	3.70	7.28	0.05967	0.00287	0.51385	0.02558	0.06206	0.00071	388.2	4.3
XS-38-1.08	2.35	4.53	0.07744	0.00435	0.68068	0.03773	0.06494	0.00091	405.6	5.5
XS-38-1.09	2.48	2.74	0.07557	0.00377	0.66296	0.03280	0.06428	0.00081	401.6	4.9
XS-38-1.10	3.23	4.52	0.05417	0.00229	0.46372	0.02007	0.06204	0.00078	388.0	4.7
XS-38-1.11	1.83	2.77	0.08526	0.00434	0.74076	0.03684	0.06421	0.00103	401.2	6.3
XS-38-1.12	3.31	6.89	0.06030	0.00254	0.51765	0.02181	0.06267	0.00080	391.8	4.8
XS-38-1.13	3.13	6.24	0.06132	0.00282	0.52011	0.02439	0.06128	0.00072	383.4	4.4
XS-38-1.14	1.94	1.19	0.05189	0.00349	0.43832	0.02802	0.06241	0.00112	390.3	6.8
XS-38-1.15	1.62	1.74	0.05419	0.00419	0.46815	0.03577	0.06299	0.00102	393.8	6.2
XS-38-1.16	1.75	1.80	0.06194	0.00377	0.51189	0.02956	0.06213	0.00101	388.6	6.1
XS-38-1.17	1.46	1.45	0.08986	0.00476	0.80177	0.04398	0.06482	0.00101	404.9	6.1
XS-38-1.18	3.19	5.81	0.06305	0.00313	0.53526	0.02502	0.06260	0.00079	391.4	4.8
XS-38-1.19	2.42	2.85	0.09605	0.00409	0.85978	0.03448	0.06646	0.00090	414.8	5.4
XS-38-1.20	3.38	4.55	0.06258	0.00327	0.52593	0.02596	0.06221	0.00084	389.1	5.1
XS-38-1.21	2.25	2.57	0.06831	0.00368	0.60775	0.03253	0.06533	0.00101	407.9	6.1
XS-38-1.22	3.31	4.77	0.05589	0.00222	0.46966	0.01864	0.06153	0.00070	384.9	4.3
XS-38-1.23	2.60	4.06	0.05267	0.00312	0.45368	0.02802	0.06272	0.00091	392.1	5.5
XS-38-1.24	3.72	5.30	0.05884	0.00269	0.49249	0.02175	0.06172	0.00074	386.1	4.5
XS-38-1.25	1.94	1.50	0.07121	0.00404	0.61265	0.03637	0.06285	0.00102	392.9	6.2
XS-38-1.26	1.24	1.75	0.17668	0.00756	1.68913	0.06862	0.07165	0.00130	446.1	7.8
XS-38-1.27	1.20	1.14	0.11446	0.00599	1.02963	0.05306	0.06642	0.00113	414.6	6.8
XS-38-1.28	1.53	2.01	0.07636	0.00448	0.68303	0.03923	0.06459	0.00123	403.5	7.5
XS-38-1.29	2.44	2.83	0.06786	0.00317	0.56899	0.02615	0.06158	0.00086	385.2	5.2
XS-38-1.30	1.22	1.24	0.07836	0.00510	0.67218	0.04258	0.06494	0.00105	405.6	6.4
XS-38-1.31	1.14	1.10	0.05936	0.00445	0.49490	0.03659	0.06230	0.00132	389.6	8.0
XS-38-1.32	1.39	2.56	0.06900	0.00499	0.56854	0.04116	0.06170	0.00129	385.9	7.9
XS-38-1.33	1.41	1.74	0.12310	0.00716	1.14046	0.07416	0.06772	0.00135	422.4	8.1
XS-38-1.34	1.63	2.31	0.09456	0.00497	0.84240	0.04268	0.06550	0.00109	409.0	6.6
XS-38-1.35	1.09	1.06	0.06083	0.00524	0.49798	0.03829	0.06252	0.00118	390.9	7.2
XS-38-1.36	2.26	3.00	0.06973	0.00354	0.58730	0.02807	0.06270	0.00096	392.1	5.8
XS-38-1.37	1.24	1.66	0.06121	0.00391	0.50920	0.03089	0.06290	0.00109	393.3	6.6
XS-38-1.38	1.27	1.65	0.07313	0.00513	0.62032	0.04162	0.06331	0.00123	395.7	7.5
XS-38-1.39	3.34	6.25	0.06098	0.00261	0.51366	0.02136	0.06177	0.00074	386.4	4.5
XS-38-1.40	2.21	2.61	0.09676	0.00428	0.86014	0.03896	0.06470	0.00095	404.1	5.8
XS-54-1.01	1.52	3.49	0.06295	0.00512	0.54913	0.04506	0.06278	0.00125	392.5	7.6
XS-54-1.02	1.48	3.41	0.06639	0.00648	0.52988	0.04653	0.06252	0.00128	390.9	7.8
XS-54-1.03	3.27	8.10	0.05836	0.00456	0.48594	0.03473	0.06225	0.00115	389.3	7.0
XS-54-1.04	3.33	5.34	0.05602	0.00328	0.46072	0.02395	0.06208	0.00088	388.3	5.3
XS-54-1.05	2.23	5.42	0.05689	0.00437	0.47801	0.03590	0.06264	0.00122	391.7	7.4
XS-54-1.06	2.11	4.46	0.05277	0.00568	0.42636	0.04360	0.06283	0.00135	392.8	8.2
XS-54-1.07	1.99	4.83	0.05751	0.00524	0.47738	0.04164	0.06318	0.00141	394.9	8.6
XS-54-1.08	1.98	2.95	0.05224	0.00405	0.45241	0.03341	0.06441	0.00115	402.4	7.0
XS-54-1.09	2.93	5.81	0.06024	0.00303	0.50420	0.02451	0.06216	0.00083	388.7	5.1
XS-54-1.10	2.45	6.05	0.06469	0.00386	0.54619	0.02999	0.06354	0.00098	397.1	5.9
XS-54-1.11	1.46	5.24	0.06358	0.00445	0.56505	0.03880	0.06566	0.00121	409.9	7.3
XS-54-1.12	4.93	2.91	0.05681	0.00388	0.47783	0.03157	0.06199	0.00090	387.7	5.5
XS-54-1.13	1.84	4.79	0.06082	0.00460	0.50035	0.03558	0.06203	0.00120	388.0	7.3
XS-54-1.14	7.02	1.57	0.05569	0.00207	0.47990	0.01857	0.06225	0.00080	389.3	4.8
XS-54-1.15	1.22	3.40	0.06581	0.00685	0.50882	0.05037	0.06243	0.00148	390.4	9.0
XS-54-1.16	2.72	5.19	0.06941	0.00434	0.59009	0.03505	0.06367	0.00103	397.9	6.3
XS-54-1.17	3.59	3.69	0.06013	0.00290	0.50224	0.02349	0.06155	0.00081	385.0	4.9
XS-54-1.18	2.53	7.51	0.04847	0.00419	0.42698	0.04255	0.06336	0.00135	396.0	8.2
XS-54-1.19	3.41	9.53	0.06071	0.00446	0.51259	0.03532	0.06199	0.00107	387.7	6.5
XS-54-1.20	3.22	8.36	0.06067	0.00284	0.51314	0.02324	0.06250	0.00092	390.8	5.6
XS-54-1.21	1.79	5.78	0.08202	0.00507	0.68648	0.04289	0.06293	0.00119	393.4	7.2
XS-54-1.22	2.04	1.91	0.05567	0.00362	0.49172	0.03220	0.06396	0.00113	399.6	6.8
XS-54-1.23	2.29	5.58	0.05767	0.00320	0.49582	0.02742	0.06324	0.00110	395.3	6.6
XS-54-1.24	2.27	5.69	0.05455	0.00390	0.45684	0.03138	0.06235	0.00115	389.9	7.0
XS-54-1.25	3.62	3.23	0.06062	0.00283	0.50671	0.02344	0.06128	0.00086	383.4	5.2
XS-54-1.26	2.36	4.63	0.05907	0.00303	0.49275	0.02523	0.06192	0.00097	387.3	5.9
XS-54-1.27	2.07	4.26	0.05759	0.00397	0.47776	0.03053	0.06219	0.00117	388.9	7.1
XS-54-1.28	2.45	5.93	0.06426	0.00342	0.54446	0.02849	0.06257	0.00095	391.2	5.8
XS-54-1.29	1.80	5.22	0.05363	0.00412	0.44685	0.03485	0.06163	0.00116	385.6	7.0
XS-54-1.30	1.99	4.84	0.07597	0.00451	0.65705	0.03805	0.06372	0.00118	398.2	7.1
XS-54-1.31	2.62	3.85	0.05840	0.00312	0.48407	0.02437	0.06161	0.00089	385.4	5.4
XS-54-1.32	2.68	2.54	0.06000	0.00327	0.50785	0.02670	0.06225	0.00086	389.3	5.2
XS-54-1.33	2.57	5.39	0.05539	0.00318	0.47651	0.02679	0.06278	0.00096	392.5	5.8
XS-54-1.34	2.35	3.29	0.05937	0.00306	0.50877	0.02552	0.06423	0.00095	401.3	5.8
XS-54-1.35	2.39	3.33	0.06459	0.00353	0.57482	0.03093	0.06531	0.00106	407.8	6.4
XS-54-1.36	3.35	3.82	0.05402	0.00249	0.46237	0.02088	0.06290	0.00082	393.2	5.0
XS-54-1.37	1.94	3.54	0.07644	0.00494	0.65284	0.04043	0.06296	0.00118	393.6	7.1
XS-54-1.38	2.71	7.07	0.06277	0.00336	0.52973	0.02739	0.06270	0.00088	392.0	5.4
XS-54-1.39	2.97	6.81	0.05691	0.00295	0.47920	0.02336	0.06263	0.00087	391.6	5.3
XS-54-1.40	2.18	3.13	0.05545	0.00331	0.45842	0.02612	0.06169	0.00096	385.9	5.8
XS-62-1.01	1.07	0.844	0.12666	0.00781	1.15680	0.07238	0.06711	0.00128	418.7	7.7
XS-62-1.02	1.59	1.60	0.06332	0.00398	0.54015	0.03375	0.06189	0.00107	387.1	6.5
XS-62-1.03	3.01	3.05	0.05879	0.00288	0.49456	0.02356	0.06153	0.00078	384.9	4.7
XS-62-1.04	2.83	3.95	0.06634	0.00305	0.56131	0.02488	0.06196	0.00091	387.5	5.5
XS-62-1.05	1.99	4.83	0.21446	0.00878	2.31909	0.10343	0.07828	0.00133	485.9	7.9
XS-62-1.06	2.18	2.97	0.05839	0.00359	0.49896	0.03034	0.06313	0.00108	394.6	6.5
XS-62-1.07	1.88	2.73	0.06590	0.00420	0.54229	0.03140	0.06168	0.00115	385.8	7.0
XS-62-1.08	1.86	1.86	0.08128	0.00508	0.71451	0.04295	0.06426	0.00105	401.5	6.4
XS-62-1.09	1.61	1.75	0.08303	0.00506	0.72110	0.04231	0.06436	0.00106	402.1	6.4
XS-62-1.10	2.26	4.83	0.06103	0.00366	0.50822	0.02856	0.06167	0.00096	385.7	5.8
XS-62-1.11	2.50	4.97	0.05937	0.00309	0.50175	0.02609	0.06178	0.00090	386.4	5.5
XS-62-1.12	1.37	2.30	0.07325	0.00705	0.62411	0.05591	0.06307	0.00139	394.3	8.4
XS-62-1.13	1.42	1.85	0.06364	0.00462	0.53488	0.03834	0.06252	0.00104	390.9	6.3
XS-62-1.14	2.09	2.85	0.06428	0.00538	0.54958	0.04464	0.06259	0.00110	391.3	6.7
XS-62-1.15	2.06	4.19	0.05832	0.00343	0.48790	0.02767	0.06223	0.00099	389.1	6.0
XS-62-1.16	2.39	4.73	0.06432	0.00352	0.55507	0.02988	0.06267	0.00083	391.8	5.0
XS-62-1.17	3.08	3.53	0.05922	0.00299	0.51907	0.02692	0.06332	0.00089	395.8	5.4
XS-62-1.18	1.30	1.36	0.32404	0.0109	4.12568	0.13862	0.09266	0.00174	571.2	10.3
XS-62-1.19	3.06	4.11	0.08861	0.00375	0.78347	0.03545	0.06377	0.00080	398.5	4.8
XS-62-1.20	1.78	2.36	0.06297	0.00399	0.55706	0.03583	0.06463	0.00111	403.8	6.7
XS-62-1.21	2.18	4.17	0.06638	0.00432	0.57582	0.03484	0.06328	0.00090	395.5	5.5
XS-62-1.22	1.76	2.94	0.06663	0.00386	0.56467	0.03118	0.06317	0.00105	394.9	6.4
XS-62-1.23	1.68	2.29	0.08251	0.00612	0.71499	0.05200	0.06413	0.00131	400.7	7.9
XS-62-1.24	2.98	2.82	0.07192	0.00405	0.63278	0.03700	0.06417	0.00098	400.9	5.9
XS-62-1.25	2.13	2.93	0.06245	0.00346	0.52860	0.02956	0.06212	0.00097	388.5	5.9
XS-62-1.26	1.24	1.21	0.07262	0.00532	0.60326	0.04030	0.06260	0.00124	391.4	7.5
XS-62-1.27	0.98	1.16	0.07518	0.00587	0.63310	0.04702	0.06483	0.00134	405.0	8.1
XS-62-1.28	2.17	3.13	0.06577	0.00372	0.55178	0.02977	0.06269	0.00106	392.0	6.4
XS-62-1.29	1.55	2.34	0.06100	0.00411	0.51550	0.03457	0.06294	0.00129	393.5	7.8
XS-62-1.30	1.99	3.22	0.09413	0.00480	0.84323	0.04424	0.06506	0.00098	406.3	5.9
XS-62-1.31	1.87	3.49	0.06415	0.00359	0.54576	0.03123	0.06225	0.00108	389.3	6.6
XS-62-1.32	1.90	3.04	0.07978	0.00426	0.69402	0.03675	0.06425	0.00105	401.4	6.4