Volume 39 Issue 6
Jun.  2014
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Xu Jing, Zheng Youye, Sun Xiang, Jiang Junsheng, Geng Ruirui, Shen Yahui, 2014. Mineralogical Characteristics of Zhibula Skarn-Type Cu Deposit in Tibet and Their Geological Significance. Earth Science, 39(6): 654-670, 768. doi: 10.3799/dqkx.2014.062
Citation: Xu Jing, Zheng Youye, Sun Xiang, Jiang Junsheng, Geng Ruirui, Shen Yahui, 2014. Mineralogical Characteristics of Zhibula Skarn-Type Cu Deposit in Tibet and Their Geological Significance. Earth Science, 39(6): 654-670, 768. doi: 10.3799/dqkx.2014.062
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Mineralogical Characteristics of Zhibula Skarn-Type Cu Deposit in Tibet and Their Geological Significance

doi: 10.3799/dqkx.2014.062
  • 1.

    Faculty of Earth Resources, China University of Geosciences, Wuhan 430074, China

  • 2.

    Geological Survey, China University of Geosciences, Wuhan 430074, China

  • 3.

    State Key Laboratory of Geological Processes and Mineral Resources, China University of Geosciences, Beijing 100083, China

  • Received Date: 2013-09-25
  • Publish Date: 2014-06-15
    Abstract
  • The Zhibula skarn-type Cu deposit is located about 2 km away from the south of Qulong super-large porphyry Cu-Mo deposit in Gangdese metallogenic belt, Tibet. The skarn and ore body are mainly distributed as layer-stratoid in the tuff and marble of Yeba Group in Lower Jurassic, which show zoning characteristics: tuff-garnert tuff-garnet skarn-pyroxene skarn-(wollastonite) marble. From early to late stages, or from tuff to marble, the colors of garnets change from dark brownish red to brownish red, followed by green(brown), and pale brownish yellow These garnets are mainly grossular and andradite. The end members of pyroxenes are dominated by diopside, with minor johannsenite. Garnets near tuff have higher Al, Ti contents, whereas those nearthe marble have relatively more enriched Fe, Mn contents. Garnets show distinctive light and dark oscillatory-zoning. Light zoning is distinctively enriched withcalcium-iron components, and dark zoning is enriched with calcium-aluminum components. These garnets generally show increasing calcium-iron components and relatively reducing calcium-aluminum components from the core to outer zones. The Zhibula layer-stratoid skarn-type ore body are developed due to thedeep buriedore-bearinghy drothermal migration with differential magmatic crystallization along the interface, or migration along fractured rock bands driven by temperature and pressure differences. In addition, selective metasomatic alteration between tuff and marble or crystalline limestone contributed to the formation of this ore deposits. Therefore, this ore deposit belongs to the magmatic hydrothermal contact metasomatic type rather than stratabound or exhalative forming layer skarn-type, and has the same forming mechanism with Qulong porphyry Cu-Mo deposit.

     

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  • Atkinson, W.W., Einaudi, M.T., 1978. Skarn Formation and Mineralization in the Contact Aureole at Carr Fork, Bingham, Utah. Economic Geology, 73(7): 1326-1365. doi: 10.2113/gsecongeo.73.7.1326
    Baker, T., Van Achterberg, E., Ryan, C.R., et al., 2004. Composition and Evolution of Ore Fluids in a Magmatic-Hydrothermal Skarn Deposit. Geology, 32(2): 117-120. doi: 10.1130/G19950.1
    Berman, R.G., Brown, T.H., Greenwood, H.J., 1985. Heat Capacity of Minerals in the System Na2O-K2O-CaO-MgO-FeO-Fe2O3-Al2O3-SiO2-TiO2-H2O-O2. Contributions to Mineralogy and Petrology, 89(2-3): 168-183. doi: 10.1007/BF00379451
    Calagari, A.A., Hosseinzadeh, G., 2006. The Mineralogy of Copper-Bearing Skarn to the East of the Sungun-Chay River, East-Azarbaidjan, Iran. Journal of Asian Earth Sciences, 28(4-6): 423-438. doi: 10.1016/j.jseaes.2005.11.009
    Canet, C., González, P.E., Camprubí, A., et al., 2011. The Zn-Pb-Ag Skarns of Zacatepec, Northeastern Oaxaca, Mexico: A Study of Mineral Assemblages and Ore-Forming Fluids. Ore Geology Reviews, 39(4): 277-290. doi: 10.1016/j.oregeorev.2011.03.007
    Chang, Y.F., Liu, X.G., 1983. On Strata-Bound Skarn Deposits. Mineral Deposits, 2(1): 11-20 (in Chinese with English abstract). http://en.cnki.com.cn/Article_en/CJFDTOTAL-KCDZ198301001.htm
    Chang, Z.S., Meinert, L.D., 2004. The Magmatic-Hydrothermal Transition—Evidence from Quartz Phenocryst Textures and Endoskarn Abundance in Cu-Zn Skarns at the Empire Mine, Idaho, USA. Chemical Geology, 210(1-4): 149-171. doi: 10.1016/j.chemgeo.2004.06.018
    Chen, L., Qing, K.Z., Li, G.M., et al., 2012. Geological and Skarn Mineral Characteristics of Nuri Cu-W-Mo Deposit in Southeast Gangdese, Tibet. Mineral Deposits, 31(3): 417-437 (in Chinese with English abstract). http://www.researchgate.net/publication/285319845_Geological_and_skarn_mineral_characteristics_of_Nuri_Cu-W-Mo_deposit_in_southern_Gangdese_Tibet
    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. doi: 10.1130/0091-7613120013029<0479:OIATEZ>2.0.CO;2
    Deer, W.A., Howie, R.A., Zussman, J., 1992. An Introduction to the Rock-Forming Minerals. Longman Group Ltd., New York, 696.
    Du, G.S., Yao, P., Pan, F.Z., et al., 1998. Sedimentation-Exhalation Skarn and Ore-Formation—Example by Jiama Copper-Polymetallic Deposits, Xizang (Tibet). Sichuan Science and Technology Press, Chengdu, 40-136 (in Chinese with English abstract).
    Du, Y.L., 2013. Ore-Controlling Factors and Metallogenic Model of Strata Bound Skarn Deposits in Tongling Area, Anhui Province (Dissertation). China University of Geosciences, Beijing (in Chinese with English abstract).
    Einaudi, M.T., Burt, D.M., 1982. Introduction, Terminology, Classification, and Composition of Skarn Deposits. Economic Geology, 77(4): 745-754. doi: 10.2113/gsecongeo.77.4.745
    Einaudi, M.T., Meinert, L.D., Newberry, R.J., 1981. Skarn Deposits. Economic Geology, 75: 317-391.
    Geng, Q.R., Pan, G.T., Jin, Z.M., et al., 2005. Geochemistry and Genesis of the Yeba Volcanic Rocks in the Gangdise Magmatic Arc, Tibet. Earth Science—Journal of China University of Geosciences, 30(6): 747-760 (in Chinese with English abstract). http://d.old.wanfangdata.com.cn/Periodical_dqkx-e200504001.aspx
    Gu, X.X., Dong, S.Y., Liu, L., et al., 2008. Ore-Forming Conditions and Significance of Unconformity in the Mineralization of the Yi'nan Au-Cu-Fe Deposit, Shandong, China. Bulletin of Mineralogy, Petrology and Geochemistry, 27(3): 254-268 (in Chinese with English abstract). http://dialnet.unirioja.es/servlet/articulo?codigo=265509
    Harris, N.B., Einaudi, M.T., 1982. Skarn Deposits in the Yerington District, Nevada; Metasomatic Skarn Evolution near Ludwig. Economic Geology, 77(4): 877-898. doi: 10.2113/gsecongeo.77.4.877
    Hezarkhani, A., Williams-Jones, A.E., Gammons, C.H., 1999. Factors Controlling Copper Solubility and Chalcopyrite Deposition in the Sungun Porphyry Copper Deposit, Iran. Mineralium Deposita, 34(8): 770-783. doi: 10.1007/s001260050237
    Holten, T., Jamtveit, B., Meakin, P., 2000. Noise and Oscillatory Zoning of Minerals. Geochimica et Cosmochimica Acta, 64(11): 1893-1904. doi: 10.1016/s0016-7037199100444-5
    Huang, H.S., 1994. Advances in Skarn Deposits. Earth Science Frontiers, 1(3-4): 105-111 (in Chinese with English abstract).
    Jamtveit, B., 1991. Oscillatory Zonation Patterns in Hydrothermal Grossular-Andradite Garnet; Nonlinear Dynamics in Regions of Immiscibility. American Mineralogist, 76(7-8): 1319-1327. http://petrology.oxfordjournals.org/cgi/ijlink?linkType=ABST&journalCode=gsammin&resid=76/7-8/1319
    Jamtveit, B., Wogelius, R.A., Fraser, D.G., 1993. Zonation Patterns of Skarn Garnets: Records of Hydrothermal System Evolution. Geology, 21(2): 113-116. doi: 10.1130/0091-7613(1993)021<0113:ZPOSGR>2.3.CO;2
    Jiang, H.Z., Zeng, H.L., Wu, Z.S., 2011. Geological Characteristics and Prospecting Prediction in Deep Area of Layered Skarn Cu-W-Mo Deposit in Shannan Nuri Ore District, Tibet. Geology and Exploration, 47(1): 71-77 (in Chinese with English abstract).
    Li, G.M., Rui, Z.Y., Wang, G.M., et al., 2005. Molybdenite Re-Os Dating of Jiama and Zhibula Polymetallic Copper Deposits in Gangdese Metallogenic Belt of Tibet and Its Significance. Mineral Deposits, 24(5): 481-489 (in Chinese with English abstract). http://en.cnki.com.cn/Article_en/CJFDTOTAL-KCDZ200505002.htm
    Liang, X.J., 1994. Garnets of Garossular-Andradite Series: Their Characteristics and Metaomatic Mechanism. Acta Petrologica et Mieralogica, 13(4): 342-352 (in Chinese with English abstract). http://en.cnki.com.cn/Article_en/CJFDTOTAL-YSKW404.007.htm
    Lin, X.D., 1987. A Skarn Genesis—Magmatic Genesis. Geological Science and Technology Information, 6(2): 92-94 (in Chinese).
    Lu, H.Z., Liu, Y.M., Wang, C.L., et al., 2003. Mineralization and Fluid Inclusion Study of the Shizhuyuan W-Sn-Bi-Mo-F Skarn Deposit, Hunan Province, China. Economic Geology, 98(5): 955-974. doi: 10.2113/gsecongeo.98.5.955
    Lu, Y.F., Chen, K.X., Zhan, M.G., 1999. Geochemical Evidence of Exhalative-Sedimentary Ore-Bearing Skarns in Yangla Copper Mineralization Concentrated Area, Deqin County, Northwestern Yunnan Province. Earth Science—Journal of China University of Geosciences, 24(3): 298-303 (in Chinese with English abstract). http://en.cnki.com.cn/Article_en/CJFDTOTAL-DQKX903.017.htm
    Maher, K.C., 2010. Skarn Alteration and Mineralization at Coroccohuayco, Tintaya District, Peru. Economic Geology, 105(2): 263-283. doi: 10.2113/gsecongeo.105.2.263
    Meinert, L.D., 1992. Skarns and Skarn Deposits. Geoscience Canada, 19(4): 145-162. http://pdf.eurekamag.com/023/023604119.pdf
    Meinert, L.D., 1997. Application of Skarn Deposit Zonation Models to Mineral Exploration. Exploration and Mining Geology, 6(2): 185-208. http://www.researchgate.net/profile/Lawrence_Meinert/publication/262450785_Meinert_L.D._1997_Application_of_skarn_deposit_zonation_models_to_mineral_exploration_Exploration_and_Mining_Geology_v._6_p._185-208/links/0c960537bcd7f4e811000000.pdf
    Meinert, L.D., Dipple, G.M., Nicolescu, S., 2005. World Skarn Deposits. Economic Geology, 100 th Anniversary Volume, 299-336.
    Oyman, T., 2010. Geochemistry, Mineralogy and Genesis of the Ayazmant Fe-Cu Skarn Deposit in Ayvalik (Balikesir), Turkey. Ore Geology Reviews, 37(3-4): 175-201. doi: 10.1016/j.oregeorev.2010.03.002
    Pan, G.T., Chen, Z.L., Li, X.Z., et al., 1997. Geological Formation and Evolution of Eastern Tethys. Geological Publishing House, Beijing (in Chinese).
    Qiu, R.L., 1988. A Study of Garnets and Their Zonal Structure in the Tongshan Skarn Type Copper Ore Deposit, Guichi County. Acta Petrologica et Mineralogica, 7(3): 244-252 (in Chinese with English abstract). http://en.cnki.com.cn/Article_en/CJFDTOTAL-YSKW198803007.htm
    Rui, Z.Y., Li, Y.Q., Wang, L.S., et al., 2003. Approach to Ore-Forming Conditions in Light of Ore Fluid Inclusions. Mineral Deposits, 22(1): 13-23 (in Chinese with English abstract). http://www.researchgate.net/publication/288907189_Approach_to_ore-forming_conditions_in_light_of_ore_fluid_inclusions
    Seward, T.M., Barnes, H.L., 1997. Metal Transport by Hydrothermal Ore Fluids. Geochemistry of Hydrothermal Ore Deposits, 3: 435-486. http://ci.nii.ac.jp/naid/10008463258
    She, H.Q., Feng, C.Y., Zhang, D.Q., et al., 2005. Characteristics and Metallogenic Potential of Skarn Copper-Lead-Zinc Polymetallic Deposits in Central Eastern Gangdese. Mineral Deposits, 24(5): 508-520 (in Chinese with English abstract). http://www.researchgate.net/publication/306218076_Characteristics_and_metallogenic_potential_of_skarn_copper-lead-zinc_polymetallic_deposits_in_central_eastern_Gangdese
    Smith, M.P., Henderson, P., Jeffries, T.E.R., et al., 2004. The Rare Earth Elements and Uranium in Garnets from the Beinn an Dubhaich Aureole, Skye, Scotland, UK: Constraints on Processes in a Dynamic Hydrothermal System. Journal of Petrology, 45(3): 457-484. doi: 10.1093/petrology/egg087
    Wang, C.Y., Li, X.F., Xiao, R., et al., 2012. Elements Mobilization of Mineralized Porphyry Rocks during Hydrothermal Alteration at Zhushahong Porphyry Copper Deposit, Dexing District, South China. Acta Petrologica Sinica, 28(12): 3869-3886 (in Chinese with English abstract). http://www.researchgate.net/publication/284503741_Elements_mobilization_of_mineralized_porphyry_rocks_during_hydrothermal_alteration_at_Zhushahong_porphyry_copper_deposit_Dexing_district_South_China
    Wang, S.X., Zhang, X.C., Leng, C.B., et al., 2008. Stable Isotopic Compositions of the Hongshan Skarn Copper Deposit in the Zhongdian Area and Its Implication for the Copper Mineralization Process. Acta Petrologica Sinica, 24(3): 480-488 (in Chinese with English abstract). http://en.cnki.com.cn/Article_en/CJFDTOTAL-YSXB200803008.htm
    Wilkinson, J.J., Crowther, H.L., Coles, B.J., 2011. Chemical Mass Transfer during Hydrothermal Alteration of Controls of Seafloor Subsidence, Sedimentation and Zn-Pb Mineralization in the Irish Carboniferous. Chemical Geology, 289(1): 55-75. doi: 10.1016/j.chemgeo.2011.07.008
    Wu, S., Zheng, Y.Y., Sun, X., et al., 2014. Origin of the Miocene Porphyries and Their Mafic Microgranular Enclaves from Dabu Porphyry Cu-Mo Deposit, Southern Tibet: Implications for Magma Mixing/Mingling and Mineralization. International Geology Review, 56(5): 571-595. doi: 10.1080/00206814.2014.880074.
    Wu, Y.C., 1992. On Magmatic Skarn—A New Type of Skarn. Geology of Anhui, 2(1): 12-26 (in Chinese with English abstract). http://en.cnki.com.cn/Article_en/CJFDTOTAL-AHDZ199201002.htm
    Xia, Y.F., 1999. Geological Characteristics and Ore-Forming Condition of Stratabound Skarn-Type Ore Deposits in Tongling District. Mineral Resources and Geology, 13(6): 338-342 (in Chinese with English abstract). http://en.cnki.com.cn/Article_en/CJFDTOTAL-KCYD199906013.htm
    Xiao, B., Qin, K.Z., Li. G.M., et al., 2011. Distributions and Characters of Zhibula-Langmujiaguo Skarn Cu Deposits Environing the Qulong Porphyry Cu-Mo Deposit and Their Implications for Ore-Search towards to the Deep Subsurface. Geology and Exploration, 47(1): 43-53 (in Chinese with English abstract). http://en.cnki.com.cn/Article_en/CJFDTOTAL-DZKT201101007.htm
    Yan, X.Y., Huang, S.F., Du, A.D., 2010. Re-Os Ages of Large Tungsten, Copper and Molybdenum Deposit in the Zetang Orefield, Gangdisê and Marginal Strike-Slip Transforming Metallogenesis. Acta Geologica Sinica, 84(3): 398-406 (in Chinese with English abstract).
    Yang, Z.S., Hou, Z.Q., Meng, Y.F., et al., 2004. Spatial-Temporal Structures of Hercynian Exhalative-Sedimentary Fluid System in Tonglin Ore Concentration Area, Anhui Province. Mineral Deposits, 23(3): 281-297 (in Chinese with English abstract). http://en.cnki.com.cn/Article_en/CJFDTOTAL-KCDZ200403002.htm
    Yao, P., Zheng, M.H., Peng, Y.M., et al., 2002. Sources of Ore-Forming Materials and Genesis of the Jiama Copper and Polymetallic Deposit in Gangdise Island-Arc Belt, Xizang. Geological Review, 48(5): 468-479 (in Chinese with English abstract). http://en.cnki.com.cn/Article_en/CJFDTOTAL-DZLP200205003.htm
    Yin, J.W., Lee, H.K., Chio, K.K., et al., 2000. Characteristics of Garnet in Shizhuyuan Skarn Deposit, Hunan Province. Earth Science—Journal of China University of Geosciences, 25(2): 163-171 (in Chinese with English abstract). http://www.researchgate.net/publication/284193935_Characteristics_of_garnet_in_Shizhuyuan_skarn_deposit_Hunan_Province
    Zeng, Q.D., Liu, J.M., Jia, C.S., et al., 2007. Sedimentary Exhalative Origin of the Baiyinnuoer Zinc-Lead Deposit, Chifeng, Inner Mongolia: Geological and Sulfur Isotope Evidence. Journal of Jilin University (Earth Science Edition), 37(4): 659-667 (in Chinese with English abstract). http://www.researchgate.net/publication/312662823_Sedimentary_exhalative_origin_of_the_Baiyinnuoer_zinc-lead_deposit_Chifeng_Inner_Mongolia_Geological_and_sulfur_isotope_evidence
    Zhai, Y.S., Lin, X.D., Chi, S.C., et al., 1980. Discussion on the Yangtze River Iron Ore Deposit Types and Mineralization Series. Geology and Exploration, 3: 9-14 (in Chinese).
    Zhai, Y.S., Yao, S.Z., Cai, K.Q., 2011. Mineral Deposits. Geological Publishing House, Beijing, 96-122 (in Chinese).
    Zhang, S.Z., Ling, Q.C., 1993. Characteristics of Skarn Copper Deposit: An Example from Dongshizishan Copper Deposit in Tongling County, Anhui Province. Earth Science—Journal of China University of Geosciences, 18(6): 801-809 (in Chinese with English abstract). http://en.cnki.com.cn/Article_en/CJFDTOTAL-DQKX199306017.htm
    Zhang, Z.Y., Du, Y.S., Zhang, J., et al., 2013. Alteration, Mineralization, and Genesis of the Zoned Tongshan Skarn-Type Copper Deposit, Anhui, China. Ore Geology Reviews, 53: 489-501. doi: 10.1016/j.oregeorev.2013.02.009
    Zhao, B., Barton, M.D., 1987. Compositional Characteristics of Garnets and Pyroxenes in Contact-Metasomatic Skarn Deposits and Their Relationship to Metallizaition. Acta Mineralogica Sinica, 7(1): 1-8 (in Chinese with English abstract). http://en.cnki.com.cn/Article_en/CJFDTOTAL-KWXB198701000.htm
    Zhao, J.S., Xia, B., Qiu, X.L., et al., 2008. Finding of Melt Inclusion in Garnet from Skarn of Shilu Iron Deposit, Hainan Provinee. Acta Petrologica Sinica, 24(1): 149-160 (in Chinese with English abstract). http://www.irgrid.ac.cn/handle/1471x/51472?mode=full&submit_simple=Show+full+item+record
    Zhao, Y.M., Dong, Y.G., Li, D.X., et al., 2003. Geology, Mineralogy, Geochemistry, and Zonation of the Bajiazi Dolostone-Hosted Zn-Pb-Ag Skarn Deposit, Liaoning Province, China. Ore Geology Reviews, 23(3): 153-182. http://ci.nii.ac.jp/naid/10030175201
    Zhao, Y.M., Lin, W.W., Bi, C.S., et al., 1990. China Skarn Deposits. Geological Publishing House, Beijing (in Chinese with English abstract).
    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://en.cnki.com.cn/Article_en/CJFDTOTAL-KCDZ704.003.htm
    Zheng, Y.Y., Gao, S.B., Zhang, D.Q., et al., 2006. Ore-Forming Fluid Controlling Mineralization in Qulong Super-Large Porphyry Copper Deposit, Tibet. Earth Science—Journal of China University of Geosciences, 31(3): 349-354 (in Chinese with English abstract). http://www.researchgate.net/publication/296736571_Ore-forming_fluid_controlling_mineralization_in_Qulong_super-large_porphyry_copper_deposit_Tibet
    Zheng, Y.Y., Sun, X., Gao, S.B., et al., 2014. Multiple Mineralization Events at the Jiru Porphyry Copper Deposit, Southern Tibet: Implications for Eocene and Miocene Magma Sources and Resource Potential. Journal of Asian Earth Sciences, 79(Part B): 842-857. doi: 10.1016/j.jseaes.2013.03.029
    Zheng, Y.Y., Xue, Y.X., Cheng, L.J., et al., 2004. Finding, Characteristics and Significances of Qulong Superlarge Porphyry Copper (Molybdenum) Deposit, Tibet. Earth Science—Journal of China University of Geosciences, 29(1): 103-108 (in Chinese with English abstract). http://www.researchgate.net/publication/285272629_Finding_characteristics_and_significances_of_Qulong_superlarge_porphyry_copper_molybdenum_deposit_Tibet
    Zhou, T.F., Yuan, F., Yue, S.C., et al., 2002. Water/Rock Interaction during Formation of Skarn-Type Deposits in Yueshan Orefield, Anhui Province. Mineral Deposits, 21(1): 1-9 (in Chinese with English abstract). http://www.researchgate.net/publication/288031557_Water-rock_interaction_during_formation_of_skarn-type_deposits_in_Yueshan_orefield_Anhui_Province
    常印佛, 刘学圭, 1983. 关于层控式矽卡岩型矿床——以安徽省内下扬子坳陷中一些矿床为例. 矿床地质, 2(1): 11-20. https://www.cnki.com.cn/Article/CJFDTOTAL-KCDZ198301001.htm
    陈雷, 秦克章, 李光明, 等, 2012. 西藏冈底斯南缘努日铜钨钼矿床地质特征与矽卡岩矿物学研究. 矿床地质, 31(3): 417-437. doi: 10.3969/j.issn.0258-7106.2012.03.002
    杜光树, 姚鹏, 潘凤雏, 等, 1998. 喷流成因矽卡岩与成矿——以西藏甲马铜多金属矿床为例. 成都: 四川科学技术出版社, 40-136.
    杜轶伦, 2013. 安徽铜陵地区层控矽卡岩型矿床控矿因素及成矿模型研究(博士学位论文). 北京: 中国地质大学.
    耿全如, 潘桂棠, 金振民, 等, 2005. 西藏冈底斯带叶巴组火山岩地球化学及成因. 地球科学——中国地质大学学报, 30(6): 747-760. https://www.cnki.com.cn/Article/CJFDTOTAL-DQKX200506010.htm
    顾雪祥, 董树义, 刘丽, 等, 2008. 山东沂南金-铜-铁矿床成矿条件分析—兼论不整合面的控矿作用. 矿物岩石地球化学通报, 27(3): 254-268. doi: 10.3969/j.issn.1007-2802.2008.03.007
    黄华盛, 1994. 矽卡岩矿床的研究现状. 地学前缘, 1(3-4): 105-111. https://www.cnki.com.cn/Article/CJFDTOTAL-DXQY403.014.htm
    江化寨, 曾海良, 吴志山, 2011. 西藏山南努日矿区层矽卡岩型铜钨钼矿床地质特征及深部找矿预测. 地质与勘探, 47(1): 71-77. doi: 10.3969/j.issn.1001-1986.2011.01.017
    李光明, 芮宗瑶, 王高明, 等, 2005. 西藏冈底斯成矿带甲马和知不拉铜多金属矿床的Re-Os同位素年龄及其意义. 矿床地质, 24(5): 481-489. doi: 10.3969/j.issn.0258-7106.2005.05.002
    梁祥济, 1994. 钙铝-钙铁系列石榴子石的特征及其交代机理. 岩石矿物学杂志, 13(4): 342-352. https://www.cnki.com.cn/Article/CJFDTOTAL-YSKW404.007.htm
    林新多, 1987. 矽卡岩的一种成因——岩浆成因. 地质科技情报, 6(2): 92-94. https://www.cnki.com.cn/Article/CJFDTOTAL-DZKQ198702021.htm
    路远发, 陈开旭, 战明国, 1999. 羊拉地区含矿矽卡岩成因的地球化学证据. 地球科学——中国地质大学学报, 24(3): 298-303. https://www.cnki.com.cn/Article/CJFDTOTAL-DQKX903.017.htm
    潘桂棠, 陈智梁, 李兴振, 等, 1997. 东特提斯地质构造形成演化. 北京: 地质出版社.
    邱瑞龙, 1988. 安徽贵池铜山矽卡岩铜矿石榴石及其环带研究. 岩石矿物学杂志, 7(3): 244-252. https://www.cnki.com.cn/Article/CJFDTOTAL-YSKW198803007.htm
    芮宗瑶, 李荫清, 王龙生, 等, 2003. 从流体包裹体研究探讨金属矿床成矿条件. 矿床地质, 22(1): 13-23. doi: 10.3969/j.issn.0258-7106.2003.01.002
    佘宏全, 丰成友, 张德全, 等, 2005. 西藏冈底斯中东段矽卡岩铜-铅-锌多金属矿床特征及成矿远景分析. 矿床地质, 24(5): 508-520. doi: 10.3969/j.issn.0258-7106.2005.05.005
    王翠云, 李晓峰, 肖荣, 等, 2012. 德兴朱砂红斑岩铜矿热液蚀变作用及元素地球化学迁移规律. 岩石学报, 28(12): 3869-3886. https://www.cnki.com.cn/Article/CJFDTOTAL-YSXB201212007.htm
    王守旭, 张兴春, 冷成彪, 等, 2008. 中甸红山矽卡岩铜矿稳定同位素特征及其对成矿过程的指示. 岩石学报, 24(3): 480-488. https://www.cnki.com.cn/Article/CJFDTOTAL-YSXB200803008.htm
    吴言昌, 1992. 论岩浆矽卡岩——一种新类型矽卡岩. 安徽地质, 2(1): 12-26. https://www.cnki.com.cn/Article/CJFDTOTAL-AHDZ199201002.htm
    夏元法, 1999. 铜陵地区层控矽卡岩型矿床地质特征和成矿条件. 矿产与地质, 13(6): 338-342. doi: 10.3969/j.issn.1001-5663.1999.06.005
    肖波, 秦克章, 李光明, 等, 2011. 冈底斯驱龙斑岩铜-钼矿区外围矽卡岩型铜矿的分布特征及深部找矿意义. 地质与勘探, 47(1): 43-53. https://www.cnki.com.cn/Article/CJFDTOTAL-DZKT201101007.htm
    闫学义, 黄树峰, 杜安道, 2010. 冈底斯泽当大型钨铜钼矿Re-Os年龄及陆缘走滑转换成矿作用. 地质学报, 84(3): 398-406. doi: 10.3969/j.issn.1004-9665.2010.03.017
    杨竹森, 侯增谦, 蒙义峰, 等, 2004. 安徽铜陵矿集区海西期喷流沉积流体系统时空结构. 矿床地质, 23(3): 281-297. doi: 10.3969/j.issn.0258-7106.2004.03.003
    姚鹏, 郑明华, 彭勇民, 等, 2002. 西藏冈底斯岛弧带甲马铜多金属矿床成矿物质来源及成因研究. 地质论评, 48(5): 468-479. doi: 10.3321/j.issn:0371-5736.2002.05.004
    尹京武, 李铉具, 崔庆国, 等, 2000. 湖南省柿竹园矽卡岩矿床中石榴石特征. 地球科学——中国地质大学学报, 25(2): 163-171. https://www.cnki.com.cn/Article/CJFDTOTAL-DQKX200002011.htm
    曾庆栋, 刘建明, 贾长顺, 等, 2007. 内蒙古赤峰市白音诺尔铅锌矿沉积喷流成因: 地质和硫同位素证据. 吉林大学学报(地球科学版), 37(4): 659-667. https://www.cnki.com.cn/Article/CJFDTOTAL-CCDZ200704003.htm
    翟裕生, 林新多, 池三川, 等, 1980. 长江中下游内生铁矿床成因类型及成矿系列探讨. 地质与勘探, 3: 9-14. https://www.cnki.com.cn/Article/CJFDTOTAL-DZKT198003002.htm
    翟裕生, 姚书振, 蔡克勤, 2011. 矿床学. 北京: 地质出版社, 96-122.
    张叔贞, 凌其聪, 1993. 矽卡岩浆型铜矿床特征——以安徽铜陵东狮子山铜矿床为例. 地球科学——中国地质大学学报, 18(6): 801-809. https://www.cnki.com.cn/Article/CJFDTOTAL-DQKX199306017.htm
    赵斌, Barton, M.D., 1987. 接触交代矽卡岩型矿床中石榴子石和辉石成分特点及其与矿化的关系. 矿物学报, 7(1): 1-8. doi: 10.3321/j.issn:1000-4734.1987.01.001
    赵劲松, 夏斌, 邱学林, 等, 2008. 海南岛石碌矽卡岩铁矿石中石榴子石的熔融包裹体及其意义. 岩石学报, 24(1): 149-160. https://www.cnki.com.cn/Article/CJFDTOTAL-YSXB200801013.htm
    赵一鸣, 林文蔚, 毕承思, 等, 1990. 中国矽卡岩矿床. 北京: 地质出版社.
    赵一鸣, 张轶男, 林文蔚, 1997. 我国矽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. https://www.cnki.com.cn/Article/CJFDTOTAL-KCDZ704.003.htm
    郑有业, 高顺宝, 张大权, 等, 2006. 西藏驱龙超大型斑岩铜矿床成矿流体对成矿的控制. 地球科学——中国地质大学学报, 31(3): 349-354. https://www.cnki.com.cn/Article/CJFDTOTAL-DQKX200603009.htm
    郑有业, 薛迎喜, 程力军, 等, 2004. 西藏驱龙超大型斑岩铜(钼)矿床: 发现, 特征及意义. 地球科学——中国地质大学学报, 29(1): 103-108. https://www.cnki.com.cn/Article/CJFDTOTAL-DQKX200401018.htm
    周涛发, 袁峰, 岳书仓, 等, 2002. 安徽月山矿田矽卡岩型矿床形成的水岩作用. 矿床地质, 21(1): 1-9. doi: 10.3969/j.issn.0258-7106.2002.01.001
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