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

doi:10.3799/dqkx.2018.290

Volume 43 Issue 9

Sep. 2018

Turn off MathJax

Article Contents

Article Navigation > Earth Science > 2018 > 43(9): 3100-3111, 3125

Yu Mingjie, Wang Yuwang, Mao Qigui, Wang Jingbin, Zhang Rui, Cheng Fenwei, Fu Wangwei, 2018. Characteristics of Ore-Forming Fluids and Their Geological Significance of Qiongkuduke Ag-Polymetallic Deposit in the Xiaoshitouquan Area of Eastern Tianshan Mountains, Xinjiang. Earth Science, 43(9): 3100-3111, 3125. doi: 10.3799/dqkx.2018.290

Citation:

Yu Mingjie, Wang Yuwang, Mao Qigui, Wang Jingbin, Zhang Rui, Cheng Fenwei, Fu Wangwei, 2018. Characteristics of Ore-Forming Fluids and Their Geological Significance of Qiongkuduke Ag-Polymetallic Deposit in the Xiaoshitouquan Area of Eastern Tianshan Mountains, Xinjiang. Earth Science, 43(9): 3100-3111, 3125. doi: 10.3799/dqkx.2018.290

Citation:

Yu Mingjie, Wang Yuwang, Mao Qigui, Wang Jingbin, Zhang Rui, Cheng Fenwei, Fu Wangwei, 2018. Characteristics of Ore-Forming Fluids and Their Geological Significance of Qiongkuduke Ag-Polymetallic Deposit in the Xiaoshitouquan Area of Eastern Tianshan Mountains, Xinjiang. Earth Science, 43(9): 3100-3111, 3125. doi: 10.3799/dqkx.2018.290

PDF( 4611 KB)

Characteristics of Ore-Forming Fluids and Their Geological Significance of Qiongkuduke Ag-Polymetallic Deposit in the Xiaoshitouquan Area of Eastern Tianshan Mountains, Xinjiang

doi: 10.3799/dqkx.2018.290

1.
Beijing Institute of Geology for Mineral Resources, Beijing 100012, China
2.
Institute of Geochemistry, Chinese Academy of Sciences, Guiyang 550081, China
3.
School of Earth Sciences and Resources, China University of Geosciences, Beijing 100083, China
4.
No. 704 Geological Party, Xinjiang Geological Exploration Bureau for Nonferrous Metals, Hami 839005, China
5.
Hami Administration of Work Safety, Hami 839000, China

Received Date: 2018-01-13
Publish Date: 2018-09-15

Abstract

Abstract

Qiongkuduke Ag-polymetallic deposit is located in the central Xiaoshitouquan area, eastern of the Harlik arc. The Qiongkuduke deposit is the largest Ag-polymetallic deposit in the Xiaoshitouquan area. However, the mineralization mechanism of the deposit needs to be further studied. This paper focuses on the study of the homogenization temperature and the hydrogen and oxygen isotopic compositions of the fluid inclusions of the Qiongkuduke deposit based on the previous researches, to discuss the features of ore-forming fluids source. It is found by systematically petrographic observations that fluid inclusions are mainly small, sparse, and aqueous. The homogenization temperature of fluid inclusions ranges from 152 to 280℃ and the salinity ranges from 2.73% to 13.50% NaCleqv in the early stage of mineralization (stage Ⅰ), and the homogenization temperature of fluid inclusions ranges from 131 to 261℃ and the salinity ranges from 0.35% to 9.59% NaCleqv in the main stage of mineralization (stage Ⅱ), indicating that the homogenization temperature and salinity of the ore-forming fluid decrease from the early stage to the main stage of mineralization.The ore-forming fluid belongs to the H₂O-NaCl system with the gas phase mainly composed of H₂O together with minor CO₂ and N₂, while the liquid phase is mainly composed of Na⁺, K⁺, Cl^- together with minor SO₄^2-. The hydrogen and oxygen isotopic compositions of fluid inclusions of the Qiongkuduke deposit show that the δD_H₂O value varies from -89.5‰ to -85.1‰ whereas the δ¹⁸O_H₂O value varies from -8.671‰ to -5.94‰. Combined with the inclusion composition analysis, the ore-forming fluid of the Qiongkuduke deposit is the mixture of magmatic water and atmospheric water. Regarding the regional tectonic setting, geological characteristics of the deposit, the features of ore-forming fluids and the characteristics of isotope analysis, we conclude that the Qiongkuduke Ag-polymetallic deposit belongs to the epithermal deposit.
- geochemistry,
- fluid inclusions,
- hydrogen-oxygen isotope,
- Qiongkuduke Ag-polymetallic deposit,
- eastern Tianshan

FullText(HTML)

References(71)

References

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

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

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

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

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

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

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

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

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

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

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

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

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

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

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

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

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

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

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

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

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

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

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

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

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

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

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

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

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

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

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.

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.

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

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

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

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).

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

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

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

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

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

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

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

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).

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

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

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

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

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

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

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

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

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

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

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

卢焕章, 李秉伦, 魏家秀, 1990.包裹体地球化学.北京:地质出版社.

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

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

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

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

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

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

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

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

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

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

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.

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

郑永飞, 陈江峰, 2000.稳定同位素地球化学.北京:科学出版社.

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

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

Relative Articles

Supplements(0)

Cited By

Proportional views

Proportional views

通讯作者: 陈斌, bchen63@163.com

1.
沈阳化工大学材料科学与工程学院沈阳 110142

Figures(11) / Tables(4)

Get Citation

PDF

XML

Article views (5323) PDF downloads(44)

Characteristics of Ore-Forming Fluids and Their Geological Significance of Qiongkuduke Ag-Polymetallic Deposit in the Xiaoshitouquan Area of Eastern Tianshan Mountains, Xinjiang

doi: 10.3799/dqkx.2018.290

Abstract

References

Proportional views

Catalog

通讯作者: 陈斌, bchen63@163.com

Proportional views

Export File

Citation

Format

Content