新疆东天山小石头泉地区琼库都克银多金属矿床成矿流体特征及其地质意义

于明杰; 王玉往; 毛启贵; 王京彬; 张锐; 程奋维; 付王伟; 于明杰; 王玉往; 毛启贵; 王京彬; 张锐; 程奋维; 付王伟

doi:10.3799/dqkx.2018.290

[1]

Bethke, P.M., Rye, R.O., Stoffregen, R.E., et al., 2005.Evolution of the Magmatic-Hydrothermal Acid-Sulfate System at Summitville, Colorado:Integration of Geological, Stable-Isotope, and Fluid-Inclusion Evidence.Chemical Geology, 215(1-4):281-315. https://doi.org/10.1016/j.chemgeo.2004.06.041

[2]

Brown, P.E., Hagemann, S.G., 1995.MacFlinCor and Its Application to Fluids in Archean Lode-Gold Deposits.Geochimica et Cosmochimica Acta, 59(19):3943-3952. https://doi.org/10.1016/0016-7037(95)00254-w

[3]

Cao, F.G., Tu, Q.J., Zhang, X.M., et al., 2006.Preliminary Determination of the Early Paleozoic Magmatic Arc in the Karlik Mountains, East Tianshan, Xinjiang, China-Evidence from Zircon SHRIMP U-Pb Dating of Granite Bodies in the Tashuihe Area.Geological Bulletin of China, 25(8):923-927 (in Chinese with English abstract). https://www.researchgate.net/publication/285742843_Preliminary_determination_of_the_Early_Paleozoic_magmatic_arc_in_the_Karlik_Mountains_East_Tianshan_Xinjiang_China-Evidence_from_zircon_SHRIMP_U-Pb_dating_of_granite_bodies_in_the_Tashuihe_area

[4]

Chen, Y.J., Pirajno, F., Wu, G., et al., 2012.Epithermal Deposits in North Xinjiang, NW China.International Journal of Earth Sciences, 101(4):889-917. https://doi.org/10.1007/s00531-011-0689-4

[5]

Cooke, D.R., McPhail, D.C., 2001.Epithermal Au-Ag-Te Mineralization, Acupan, Baguio District, Philippines:Numerical Simulations of Mineral Deposition.Economic Geology, 96(1):109-131. https://doi.org/10.2113/gsecongeo.96.1.109

[6]

Cooke, D.R., Simmons, S.F., 2000.Characteristics and Genesis of Epithermal Gold Deposits.Reviws in Economic Geology, 13(12):221-244. http://d.old.wanfangdata.com.cn/Periodical/huangj201302004

[7]

Ding, Y.X., 1994.The Geological Characteristics and Prospecting in the District Ⅰ Tongshan Ore Deposit, the Xinjiang Uygur Autonomous Region.Geologcal Exploration for Non-Ferrous Metals, 3(2):77-82 (in Chinese with English abstract). http://en.cnki.com.cn/Article_en/CJFDTOTAL-KCYD200506010.htm

[8]

Fang, T.H., Qin, K.Z., Wang, S.L., et al., 2002.Geological Characteristics and Exploration Prospect of Copper and Multi-Metal Deposits in Xiaoshitouquan District, Eastern Xinjiang.Xinjiang Geology, 20(4):371-374 (in Chinese with English abstract). https://www.sciencedirect.com/science/article/pii/S0169136813002023

[9]

Gemmell, J.B., Sharpe, R., Jonasson, I.R., et al., 2004.Sulfur Isotope Evidence for Magmatic Contributions to Submarine and Subaerial Gold Mineralization:Conical Seamount and the Ladolam Gold Deposit, Papua New Guinea.Economic Geology, 99(8):1711-1725. https://doi.org/10.2113/gsecongeo.99.8.1711

[10]

Guo, D.Y., 1995.Metallogenic Geologic Setting of the Xiaoshitouquan District in the Eastern Xinjiang.Geological Exploration for Non-Ferrous Metals, 4(4):212-218 (in Chinese). http://www.wanfangdata.com.cn/details/detail.do?_type=perio&id=QK199500587184

[11]

Hall, D.L., Sterner, S.M., Bodnar, R.J., 1988.Freezing Point Depression of NaCl-KCl-H₂O Solutions.Economic Geology, 83(1):197-202. https://doi.org/10.2113/gsecongeo.83.1.197

[12]

Hedenquist, J.W., Arribas, A., Gonzalez-Urien, E., 2000.Exploration for Epithermal Gold Deposits.Reviews in Economic Geology, 13(2):45-77. http://d.old.wanfangdata.com.cn/OAPaper/oai_doaj-articles_58360456a1dfa1c33a61d3ec372c2316

[13]

Hedenquist, J.W., Lowenstern, J.B., 1994.The Role of Magmas in the Formation of Hydrothermal Ore Deposits.Nature, 370(6490):519-527. https://doi.org/10.1038/370519a0

[14]

Heinrich, C.A., 2005.The Physical and Chemical Evolution of Low-Salinity Magmatic Fluids at the Porphyry to Epithermal Transition:A Thermodynamic Study.Mineralium Deposita, 39(8):864-889. https://doi.org/10.1007/s00126-004-0461-9

[15]

Heinrich, C.A., 2007.Fluid-Fluid Interactions in Magmatic-Hydrothermal Ore Formation.Reviews in Mineralogy and Geochemistry, 65(1):363-387. https://doi.org/10.2138/rmg.2007.65.11

[16]

Ji, Y.S., 1994.Primary Halo Geochemical Characteristics of the District Ⅰ Tongshan in Xiaoshitouquan.Mineral Resources and Geology, 43(8):373-379 (in Chinese). https://www.mindat.org/show.php?id=46605&ld=1

[17]

Jin, L.Y., Zhang, J., Zhu, Z.X., et al., 2013.The Geologic Character and Tectonic Significance of Paleozoic Volcanic Rocks in the Harlik Mountains, Xinjiang.Xinjiang Geology, 31(3):173-179 (in Chinese with English abstract). doi: 10.1029/JB087iB05p03709/full

[18]

Lu, H.Z., Fan, H.R, Ni, P., et al., 2004.Fluid Inclusion.Science Press, Beijing, 406-419 (in Chinese).

[19]

Lu, H.Z., Li, B.L., Wei, J.X., 1990.Fluid Inclusion Geochemistry.Geological Publishing House, Beijing (in Chinese).

[20]

Mo, J.P., Sha, Y.K., Wang, X.D., et al., 2001.Study on Geological and Geochemical Characteristics and Genesis of Tongshan Copper Polymetallic Deposit, Xingjiang.Mineral Resources and Geology, 15(3):162-166 (in Chinese with English abstract). https://www.sciencedirect.com/science/article/pii/S0169136817306388

[21]

Nesbitt, B.E., 1996.Applications of Oxygen and Hydrogen Isotopes to Exploration for Hydrothermal Mineralization.SEG Newsletter, 27:1-13. https://www.sciencedirect.com/science/article/pii/S1872579107600414

[22]

Ohmoto, H., 1986.Stable Isotope Geochemistry of Ore Deposits.Reviews in Mineralogy and Geochemistry, 16(1):491-559. http://d.old.wanfangdata.com.cn/Periodical/kwysdqhxtb201801010

[23]

Qin, K.Z., Peng, X.M., San, J.Z., et al., 2003.Types of Major Ore Deposits, Division of Metallogenic Belts in Eastern Tianshan, and Discrimination of Potential Prospects of Cu, Au, Ni Mineralization.Xinjiang Geology, 21(2):143-150 (in Chinese with English abstract). doi: 10.1007%2Fs00531-004-0383-x

[24]

Roedder, E., 1979.In Physics and Chemistry of the Earth.Pergamas Press, Oxford, 9-35.

[25]

Roedder, E., 1984.Fluid Inclusions.In: Ribbe, P.H., ed., Reviews in Mineralogy.Mineralogical Society of America, Washington D.C..

[26]

Scott, A.M., Watanabe, Y., 1998."Extreme Boiling"Model for Variable Salinity of the Hokko Low-Sulfidation Epithermal Au Prospect, Southwestern Hokkaido, Japan.Mineralium Deposita, 33(6):568-578. https://doi.org/10.1007/s001260050173

[27]

Sharp, Z.D., Gibbons, J.A., Maltsev, O., et al., 2016.A Calibration of the Triple Oxygen Isotope Fractionation in the SiO₂-H₂O System and Applications to Natural Samples.Geochimica et Cosmochimica Acta, 186:105-119. https://doi.org/10.1016/j.gca.2016.04.047

[28]

Sheppard, S.M.F., 1986.Characterization and Isotopic Variations in Natural Waters.Reviews in Mineralogy, 16:165-183. http://www.wanfangdata.com.cn/details/detail.do?_type=perio&id=JJ0232683584

[29]

Sillitoe, R.H., 1997.Characteristics and Controls of the Largest Porphyry Copper-Gold and Epithermal Gold Deposits in the Circcum-Pacific Region.Australian Journal of Earth Sciences, 44(3):373-388. https://doi.org/10.1080/08120099708728318

[30]

Sun, W.D., Arculus, R.J., Kamenetsky, V.S., et al., 2004.Release of Gold-Bearing Fluids in Convergent Margin Magmas Prompted by Magnetite Crystallization.Nature, 431(7011):975-978. https://doi.org/10.1038/nature02972

[31]

Taylor, H.P., 1979.Oxygen and Hydrogen Isotope Relationships in Hydrothermal Mineral Deposits.In: Barnes, H.L., ed., Geochemistry of Hydrothermal Ore Deposits.John Wiley & Sons, New York.

[32]

Taylor, H.P., 1997.Oxygen and Hydrogen Isotope Relationships in Hydrothermal Mineral Deposits.In: Barnes, H.L., ed., Geochemistry of Hydrothermal Ore Deposits.John Wiley & Sons, New York.

[33]

Turner, W., Richards, J., Nesbitt, B., et al., 2001.Proterozoic Low-Sulfidation Epithermal Au-Ag Mineralization in the Mallery Lake Area, Nunavut, Canada.Mineralium Deposita, 36(5):442-457. https://doi.org/10.1007/s001260100181

[34]

Wan, B., Zhang, L.C., Xu, X.W., et al., 2006.Geochemical Characteristics of Volcanic, Sub-Volcanic Rocks in Xiaoshitouquan Copper Polymetallic Deposit, Eastern Tianshan, and Its Metallogenic Setting.Acta Petrologica Sinica, 22(11):2711-2718 (in Chinese with English abstract). https://www.researchgate.net/publication/285986099_Geochemical_characteristics_of_volcanic_sub-volcanic_rock_in_Xiaoshitouquan_copper_polymetallic_deposit_eastern_Tianshan_and_its_metallogenic_setting

[35]

Wan, D.F., Fan, T.Y., Tian, S.H., 2005.The Chromium Analytical Technique for Hydrogen Isotopes.Acta Geoscientica Sinica, 26(Suppl.):35-38 (in Chinese with English abstract). http://www.wanfangdata.com.cn/details/detail.do?_type=perio&id=dqxb2005z1014

[36]

Wang, J.B., Wang, Y.W., He, Z.J., 2006.Ore Deposits as a Guide to the Tectonic Evolution in the East Tianshan Mountains, NW China.Geology in China, 33(3):461-469 (in Chinese with English abstract).

[37]

Wang, L.J., Peng, Z.G., Zhu, X.Y., et al., 2009.Source and Evolution of Ore Fluid of the Xitieshan Sedimentary Exhaleative Lead Zinc System, Qinghai Province:Evidence from Fluid Inclusion and Isotope Geochemistry.Acta Petrologica Sinica, 25(11):3007-3015 (in Chinese with English abstract). https://www.researchgate.net/publication/279655485_Source_and_evolution_of_ore-fluid_of_the_Xitieshan_sedimentary-exhalative_lead-zinc_system_Qinghai_province_Evidence_from_fluid_inclusion_and_isotope_geochemistry

[38]

Wang, X.D., 1994.Analysis of volcanogenic mineralization of Tongshan Copper Polymetallic Deposits.Mineral Resources and Geology, 8(5):383-387 (in Chinese). https://www.sciencedirect.com/science/article/pii/S0169136813000528

[39]

Wang, X.W., Xu, X.Y., Ma, Z.P., et al., 2015.Geochemistry and Tectonic Setting of the Early Carboniferous Volcanic Rocks in the Eastern Section of the Bogda Orogenic Belt in Xinjiang.Geology and Exploration, 51(1):108-122 (in Chinese with English abstract). http://d.old.wanfangdata.com.cn/Periodical/dzykt201501012

[40]

Wilkinson, J.J., 2001.Fluid Inclusions in Hydrothermal Ore Deposits.Lithos, 55(1-4):229-272. https://doi.org/10.1016/s0024-4937(00)00047-5

[41]

Williams-Jones, A.E., Heinrich, C.A., 2005.Vapor Transport of Metals and the Formation of Magmatic-Hydrothermal Ore Deposit.Economic Geology, 100(7):1287-1312. https://doi.org/10.2113/100.7.1287

[42]

Xiong, S.F., Yao, S.Z., Gong, Y.J., et al., 2016.Ore-Forming Fluid and Thermochemical Sulfate Reduction in the Wusihe Lead-Zinc Deposit, Sichuan Province, China.Earth Science, 41(1):105-120 (in Chinese with English abstract). https://doi.org/10.3799/dqkx.2016.008

[43]

Zhang, D.H., 1992.Aqueous Phase Composition Characteristic of Mineral Fluid Inclusions and Its Significance in Oregenesis.Earth Science, 17(6):677-688 (in Chinese with English abstract). http://en.cnki.com.cn/Article_en/CJFDTOTAL-HJDZ200001004.htm

[44]

Zhang, L.G., 1985.The Application of the Stable Isotope to Geology, the Hydrothermal Mineralization of Metal Activation and It's Prospecting.Shannxi Science and Technology Press, Xi'an (in Chinese).

[45]

Zhang, R., Mao, Q.G., Yu, M.J., et al., 2017.Geochemical Characteristics and Zircon U-Pb Ages of the Magmatite in the Qiongdukuke Ag-Pb-Zn Polymetallic Deposit of Xinjiang.Geology and Exploration, 53(2):270-282 (in Chinese with English abstract). doi: 10.1007/s11707-007-0008-3

[46]

Zheng, Y.F., Chen, J.F., 2000.Stable Isotope Geochemistry.Science Press, Beijing (in Chinese).

[47]

Zhou, X.B., Li, J.F., Wang, K.Y., et al., 2016.Geochemical Characteristics of Ore-Forming Fluid in Huanggoushan Gold Deposit, Jilin Province.Earth Science, 41(1):121-130 (in Chinese with English abstract). https://doi.org/10.3799/dqkx.2016.009

[48]

Zhu, H.P., Wang, L.J., 2001.Determining Gaseous Composition of Fluid Inclusions with Quadrupole Mass Spectrometer.Science in China (Series D), 31(7):586-590 (in Chinese). http://www.wanfangdata.com.cn/details/detail.do?_type=perio&id=zgkx-ed200202001

[49]

曹福根, 涂其军, 张晓梅, 等, 2006.哈尔里克山早古生代岩浆弧的初步确定——来自塔水河一带花岗质岩体锆石SHRIMP U-Pb测年的证据.地质通报, 25(8): 923-927. doi: 10.3969/j.issn.1671-2552.2006.08.004

[50]

丁玉学, 1994.论新疆铜山Ⅰ区地质特征及找矿方向.有色金属矿产与勘查, 3(2): 77-82. http://d.old.wanfangdata.com.cn/Conference/186422

[51]

方同辉, 秦克章, 王书来, 等, 2002.新疆小石头泉铜多金属矿床地质特征、找矿前景.新疆地质, 20(4): 371-374. doi: 10.3969/j.issn.1000-8845.2002.04.017

[52]

郭德英, 1995.浅析新疆东部小石头泉地区成矿地质条件.有色金属矿产与勘查, 4(4): 212-218. http://www.wanfangdata.com.cn/details/detail.do?_type=perio&id=QK199500587184

[53]

吉蕴生, 1994.小石头泉铜山Ⅰ区原生晕地球化学特征的研究.矿产与地质, 43(8): 373-379. http://www.wanfangdata.com.cn/details/detail.do?_type=perio&id=QK199400287124

[54]

靳刘圆, 张济, 朱志新, 等, 2013.哈尔里克山古生代火山岩地质特征及构造意义.新疆地质, 31(3): 173-179. doi: 10.3969/j.issn.1000-8845.2013.03.007

[55]

卢焕章, 范宏瑞, 倪培, 等, 2004.流体包裹体.北京:科学出版社, 406-419.

[56]

卢焕章, 李秉伦, 魏家秀, 1990.包裹体地球化学.北京:地质出版社.

[57]

莫江平, 依沙克, 王旭东, 等, 2001.新疆铜山铜多金属矿床地质地球化学特征及成因研究.矿产与地质, 15(3): 162-166. doi: 10.3969/j.issn.1001-5663.2001.03.003

[58]

秦克章, 彭晓明, 三金柱, 等, 2003.东天山主要矿床类型、成矿区带划分与成矿远景区优选.新疆地质, 21(2):143-150. doi: 10.3969/j.issn.1000-8845.2003.02.001

[59]

万博, 张连昌, 徐兴旺, 等, 2006.东天山小石头泉铜多金属矿区火山岩-次火山岩地球化学与成矿构造背景.岩石学报, 22(11):2711-2718. http://d.old.wanfangdata.com.cn/Periodical/ysxb98200611009

[60]

万德芳, 樊天义, 田世洪, 2005.用金属铬法分析微量水和有机质氢同位素组成.地球学报, 26(增刊):35-38. http://d.old.wanfangdata.com.cn/Periodical/dqxb2005z1014

[61]

王京彬, 王玉往, 何志军, 2006.东天山大地构造演化的成矿示踪.中国地质, 33(3):461-469. doi: 10.3969/j.issn.1000-3657.2006.03.002

[62]

王莉娟, 彭志刚, 祝新友, 等, 2009.青海省锡铁山Sedex型铅锌矿床成矿流体来源及演化:流体包裹体及同位素地球化学证据.岩石学报, 25(11):3007-3015. http://d.old.wanfangdata.com.cn/Periodical/ysxb98200911029

[63]

王旭东, 1994.铜山铜多金属矿床火山成矿作用浅析.矿产与地质, 8(5):383-387. http://www.wanfangdata.com.cn/details/detail.do?_type=perio&id=QK199400287126

[64]

汪晓伟, 徐学义, 马中平, 等, 2015.博格达造山带东段早石炭世火山岩地球化学特征及构造属性.地质与勘探, 51(1):108-122. http://d.old.wanfangdata.com.cn/Periodical/dzykt201501012

[65]

熊索菲, 姚书振, 宫勇军, 等, 2016.四川乌斯河铅锌矿床成矿流体特征及TSR作用初探.地球科学, 41(1):105-120. http://earth-science.net/WebPage/Article.aspx?id=3224

[66]

张德会, 1992.矿物包裹体液相成分特征及其矿床成因意义.地球科学, 17(6):677-688. http://www.wanfangdata.com.cn/details/detail.do?_type=perio&id=QK000000260153

[67]

张理刚, 1985.稳定同位素在地质科学中的应用.西安:陕西科学技术出版社.

[68]

张锐, 毛启贵, 于明杰, 等, 2017.新疆琼库都克Ag-Pb-Zn多金属矿区岩浆岩地球化学特征及锆石U-Pb年龄研究.地质与勘探, 53(2):270-282. http://d.old.wanfangdata.com.cn/Periodical/dzykt201702007

[69]

郑永飞, 陈江峰, 2000.稳定同位素地球化学.北京:科学出版社.

[70]

周向斌, 李剑锋, 王可勇, 等, 2016.吉林荒沟山金矿床成矿流体特征.地球科学, 41(1):121-130. http://earth-science.net/WebPage/Article.aspx?id=3225

[71]

朱和平, 王莉娟, 2001.四极质谱测定流体包裹体中的气相成分.中国科学(D辑), 31(7):586-590. http://d.old.wanfangdata.com.cn/Periodical/zgkx-cd200107008