东天山卡拉塔格西二区铁铜矿床地质地球化学特征及成因

陈磊; 王京彬; 邓小华; 吴湘滨; 邹海洋; 张会琼; 毛启贵; 孙燕; 陈磊; 王京彬; 邓小华; 吴湘滨; 邹海洋; 张会琼; 毛启贵; 孙燕

doi:10.3799/dqkx.2018.157

[1]

Bodnar, R.J., Burnham, C.W., Sterner, S.M., 1985.Synthetic Fluid Inclusions in Natural Quartz.Ⅲ.Determination of Phase Equilibrium Properties in the System H₂O-NaCl to 1000℃ and 1500 bars.Geochimica et Cosmochimica Acta, 49(9):1861-1873. https://doi.org/10.1016/0016-7037(85)90081-x

[2]

Chen, G.Y., Sun, D.S., Yin, H.A., 1987.Genesis Mineralogy and Prospecting Mineralogy.Chongqing Publishing House, Chongqing (in Chinese).

[3]

Chen, L., Wang, J.B., Bagas, L., et al., 2017.Significance of Adakites in Petrogenesis of Early Silurian Magmatism at the Yudai Copper Deposit in the Kalatag District, NW China.Ore Geology Reviews, 91:780-794. https://doi.org/10.1016/j.oregeorev.2017.08.022

[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]

Crowe, D.E., Riciputi, L.R., Bezenek, S., et al., 2001.Oxygen Isotope and Trace Element Zoning in Hydrothermal Garnets:Windows into Large-Scale Fluid-Flow Behavior.Geology, 29(6):479-482.https://doi.org/10.1130/0091-7613(2001)029<0479:oiatez>2.0.co; 2 doi: 10.1130/0091-7613(2001)029<0479:oiatez>2.0.co;2

[6]

Dai, A.F., 2015.Study on the Geological Characteristics and the Genesis of Bailing Mountain Iron Deposit in Eastern Tianshan, Xinjiang Province (Dissertation).Chang'an University, Xi'an, 1-68 (in Chinese with English abstract).

[7]

Deer, W.A., Howie, R.A., Iussman, J., 1962.Rock-Forming Minerals:Sheet Silicates.Longman, London, 270.

[8]

Deng, X.H., Wang, J.B., Pirajno, F., et al., 2016.Re-Os Dating of Chalcopyrite from Selected Mineral Deposits in the Kalatag District in the Eastern Tianshan Orogen, China.Ore Geology Reviews, 77:72-81. https://doi.org/10.1016/j.oregeorev.2016.01.014

[9]

Deng, X.H., Wang, J.B., Santosh, M., et al., 2017.Early Paleozoic Volcanic Rocks with VMS Mineralization from Eastern Tianshan Orogen: Implication for Tectonic Evolution.Geological Journal, Online.https://doi.org/10.1002/gj.3046.

[10]

Deng, X.H., Wang, J.B., Wang, Y.W., et al., 2014.Geological Characteristics of the Hongshi Cu-Au Deposit, Eastern Tianshan, Xinjiang and Discussion of the Deposit Genesis.Mineral Exploration, 5(2):159-168 (in Chinese with English abstract).

[11]

Driesner, T., Heinrich, C.A., 2007.The System H₂O-NaCl.Part I:Correlation Formulae for Phase Relations in Temperature-Pressure-Composition Space from 0 to 1000℃, 0 to 5000bar, and 0 to 1 X_NaCl.Geochimca et Cosmochimica Acta, 71:4880-4901. https://doi.org/10.1016/j.gca.2006.01.033

[12]

Dupuis, C., Beaudoin, G., 2011.Discriminant Diagrams for Iron Oxide Trace Element Fingerprinting of Mineral Deposit Types.Mineralium Deposita, 46(4):319-335. https://doi.org/10.1007/s00126-011-0334-y

[13]

Fournier, R.O., 1999.Hydrothermal Processes Related to Movement of Fluid from Plastic into Brittle Rock in the Magmatic-Epithermal Environment.Economic Geology, 94(8):1193-1211. https://doi.org/10.2113/gsecongeo.94.8.1193

[14]

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

[15]

Hedenquist, J.W., Arribas, A., Reynolds, T.J., 1998.Evolution of an Intrusion-Centered Hydrothermal System; Far Southeast-Lepanto Porphyry and Epithermal Cu-Au Deposits, Philippines.Economic Geology, 93(4):373-404. https://doi.org/10.2113/gsecongeo.93.4.373

[16]

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

[17]

Jiang, H.J., Chen, H.Y., Han, J.S., et al., 2016.Mineralogy of the Shaquanzi Fe-Cu Deposit, Eastern Tianshan and Its Metallogenic Implications.Geochimica, 45(4):329-355 (in Chinese with English abstract).

[18]

Lei, R.X., Wu, C.Z., Qu, X., et al., 2014.Geochronology, Geochemistry and Zircon Hf Isotope Compositions of the Ore-Bearing Gneiss Granite of the Tianhudong Iron-Molybdenum Ore Deposit in the Central Tianshan, West China:Implications for the Early Paleozoic Tectonic Evolution of Central Tianshan.Journal of Jilin University (Earth Science Edition), 44(5):1540-1552 (in Chinese with English abstract).

[19]

Li, H.M., Ding, J.H., Li, L.X., et al., 2014.The Genesis of the Skarn and the Genetic Type of the Yamansu Iron Deposit, Eastern Tianshan, Xinjiang.Acta Geologica Sinica, 88(12):2477-2489 (in Chinese with English abstract).

[20]

Ma, X.H., Chen, B., Wang, C., et al., 2015.Early Paleozoic Subduction of the Paleo-Asian Ocean:Zircon U-Pb Geochronological, Geochemical and Sr-Nd Isotopic Evidence from the Harlik Pluton, Xinjiang.Acta Petrologica Sinica, 31(1):89-104 (in Chinese with English abstract). http://d.old.wanfangdata.com.cn/Periodical/ysxb98201501007

[21]

Mao, Q.G., Yu, M.J., Xiao, W.J., et al., 2018.Skarn-Mineralized Porphyry Adakites in the Harlik Arc at Kalatage, E.Tianshan (NW China):Slab Melting in the Devonian-Early Carboniferous in the Southern Central Asian Orogenic Belt.Journal of Asian Earth Sciences, 153:365-378. https://doi.org/10.1016/j.jseaes.2017.03.021

[22]

Meinert, L.D., Dipple, G.M., Nicolescu, S., 2005.World Skarn Deposits.Economic Geology, 100:299-336. http://d.old.wanfangdata.com.cn/NSTLQK/NSTL_QKJJ026240992/

[23]

Meinert, L.D., 1992.Skarns and Skarn Deposits.Geoscience Canada, 19(4):145-162. http://d.old.wanfangdata.com.cn/Periodical/hbjzkjxyxb200901022

[24]

Pirajno, F., Seltmann, R., Yang, Y.Q., 2011.A Review of Mineral Systems and Associated Tectonic Settings of Northern Xinjiang, NW China.Geoscience Frontiers, 2(2):157-185. https://doi.org/10.1016/j.gsf.2011.03.006

[25]

Qin, K.Z., Fang, T.H., Wang, S.L., et al., 2002.Plate Tectonics Division, Evolution and Metallogenic Settings in Eastern Tianshan Mountains, NW-China.Xinjiang Geology, 20(4):302-308 (in Chinese with English abstract).

[26]

Sato, K., 1980.Tungsten Skarn Deposit of the Fujigatani Mine, Southwest Japan.Economic Geology, 75(7):1066-1082. https://doi.org/10.2113/gsecongeo.75.7.1066

[27]

Schwartz, M.O., Melcher, F., 2004.The Falémé Iron District, Senegal.Economic Geology, 99(5):917-939. https://doi.org/10.2113/gsecongeo.99.5.917

[28]

Çengör, A.M.C., Natal'in, B.A., Burtman, V.S., 1993.Evolution of the Altaid Tectonic Collage and Palaeozoic Crustal Growth in Eurasia.Nature, 364(6435):299-307. https://doi.org/10.1038/364299a0

[29]

Shi, Y., Wang, Y.W., Wang, J.B., 2017.Olivine Composition of Erhongwa Complex, East Tianshan, and Its Implications to CuNi-VTiFe Composite Mineralization.Earth Science, 42(3):325-338 (in Chinese with English abstract). https://doi.org/10.3799/dqkx.2017.025

[30]

Stefano, B., 1999.Applying X-Ray Geothermometer Diffraction to a Chlorite.Clays and Clay Minerals, 47(1):54-63. https://doi.org/10.1346/CCMN.1999.0470106

[31]

Sun, J.G., Li, H.Y., Liu, X.H., et al., 2015.Characteristics of Chlorite from the Tongkuangyu Copper Deposit in Shanxi Province and Their Geological Implications.Bulletin of Mineralogy, Petrology and Geochemistry, 34(6):1142-1154 (in Chinese with English abstract). http://www.wanfangdata.com.cn/details/detail.do?_type=perio&id=kwysdqhxtb201506009

[32]

Wan, D.F., Fan, T.Y., Tian, S.H., et al., 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

[33]

Wang, J., Sun, F.Y., Yu, L., et al., 2017.Fluid Inclusions and H-O-S-Pb Isotope Systematics of the Galonggema Cu Deposit in Yushu, Qinghai Province, China.Earth Science, 42(6):941-956 (in Chinese with English abstract). https://doi.org/10.3799/dqkx.2017.074

[34]

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).

[35]

Xu, J.H., Zhang, X.F., 1994.Mineralogic, Isotopic, and Fluid Inclusion Study of the Qinglongshan Iron Skarn Deposit at the South Margin of the Binjiang Granite, South Anhui, China.Proceedings of the Ninth Quadrennial IAGOD Symposium, Beijing.

[36]

Zhang, L.C., Wang, Y.T., Chen, X.F., et al., 2013.Mineralogy, Mineral Chemistry and Genesis of the Hongyuntan Iron Deposit in East Tianshan Mountians, Xinjiang.Acta Petrologica et Mineralogica, 32(4):431-449 (in Chinese with English abstract).

[37]

Zhao, Y.M., Zhang, Y.N., Lin, W.W., 1997.Characteristics of Pyroxenes and Pyroxenoids in Skarn Deposits of China and Their Relationship with Metallization.Mineral Deposits, 16(4):318-329 (in Chinese with English abstract). http://www.wanfangdata.com.cn/details/detail.do?_type=perio&id=QK199700781576

[38]

Zheng, R.Q., 2015.Geological Characteristics and Genesis of Hongyuntan Iron Deposit in the Eastern Tianshan, Xinjiang (Dissertation).China University of Geosciences, Beijing (in Chinese with English abstract).

[39]

Zheng, Y.F., 1993.Calculation of Oxygen Isotope Fractionation in Anhydrous Silicate Minerals.Geochimica et Cosmochimica Acta, 57(5):1079-1091. https://doi.org/10.1016/0016-7037(93)90042-U

[40]

Zhu, Y.F., An, F., Feng, W.Y., et al., 2016.Geological Evolution and Huge Ore-Forming Belts in the Core Part of the Central Asian Metallogenic Region.Journal of Earth Science, 27(3):491-506. https://doi.org/10.1007/s12583-016-0673-7

[41]

陈光远, 孙岱生, 殷辉安, 1987.成因矿物学与找矿矿物学.重庆:重庆出版社.

[42]

戴安峰, 2015.新疆东天山百灵山铁矿地质特征及其成因探究(硕士学位论文).西安: 长安大学, 1-68.

[43]

邓小华, 王京彬, 王玉往, 等, 2014.东天山卡拉塔格红石铜矿地质特征及矿床成因初步探讨.矿产勘查, 5(2):159-168. doi: 10.3969/j.issn.1674-7801.2014.02.007

[44]

江宏君, 陈华勇, 韩金生, 等, 2016.东天山沙泉子铁铜矿床矿物学特征及其成矿意义.地球化学, 45(4):329-355. doi: 10.3969/j.issn.0379-1726.2016.04.001

[45]

雷如雄, 吴昌志, 屈迅, 等, 2014.中天山天湖东铁钼矿含矿片麻状花岗岩年代学、地球化学和锆石Hf同位素——对于中天山早古生代构造演化的启示.吉林大学学报(地球科学版), 44(5):1540-1552. http://d.old.wanfangdata.com.cn/Periodical/cckjdxxb201405014

[46]

李厚民, 丁建华, 李立兴, 等, 2014.东天山雅满苏铁矿床矽卡岩成因及矿床成因类型.地质学报, 88(12):2477-2489. http://d.old.wanfangdata.com.cn/Periodical/dizhixb201412024

[47]

马星华, 陈斌, 王超, 等, 2015.早古生代古亚洲洋俯冲作用:来自新疆哈尔里克侵入岩的锆石U-Pb年代学、岩石地球化学和Sr-Nd同位素证据.岩石学报, 31(1):89-104. http://d.old.wanfangdata.com.cn/Periodical/ysxb98201501007

[48]

秦克章, 方同辉, 王书来, 等, 2002.东天山板块构造分区、演化与成矿地质背景研究.新疆地质, 20(4):302-308. doi: 10.3969/j.issn.1000-8845.2002.04.002

[49]

石煜, 王玉往, 王京彬, 等, 2017.东天山二红洼岩体橄榄石成分对CuNi-VTiFe复合矿化的启示.地球科学, 42(3):325-338. http://www.earth-science.net/WebPage/Article.aspx?id=3546

[50]

孙军刚, 李洪英, 刘晓煌, 等, 2015.山西铜矿峪铜矿床绿泥石特征及其地质意义.矿物岩石地球化学通报, 34(6):1142-1154. doi: 10.3969/j.issn.1007-2802.2015.06.007

[51]

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

[52]

王键, 孙丰月, 禹禄, 等, 2017.青海玉树尕龙格玛VMS型矿床流体包裹体及H-O-S-Pb同位素特征.地球科学, 42(6):941-956. http://www.earth-science.net/WebPage/Article.aspx?id=3589

[53]

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

[54]

张立成, 王义天, 陈雪峰, 等, 2013.东天山红云滩铁矿床矿物学、矿物化学特征及矿床成因探讨.岩石矿物学杂志, 32(4):431-449. doi: 10.3969/j.issn.1000-6524.2013.04.003

[55]

赵一鸣, 张轶男, 林文蔚, 1997.我国夕卡岩矿床中的辉石和似辉石特征及其与金属矿化的关系.矿床地质, 16(4):318-329. http://www.wanfangdata.com.cn/details/detail.do?_type=perio&id=QK199700781576

[56]

郑仁乔, 2015.新疆东天山红云滩铁矿床地质特征与矿床成因研究(硕士学位论文).北京: 中国地质大学.