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    Tian Kan, Zheng Youye, Gao Shunbao, Jiang Junsheng, Xu Jing, Zhang Yongchao, 2019. Petrogenesis and Geological Implications of Late Cretaceous Intrusion from Bangbule Pb-Zn-Cu Deposit, Western Gangdese, Tibet. Earth Science, 44(6): 1905-1922. doi: 10.3799/dqkx.2018.349
    Citation: Tian Kan, Zheng Youye, Gao Shunbao, Jiang Junsheng, Xu Jing, Zhang Yongchao, 2019. Petrogenesis and Geological Implications of Late Cretaceous Intrusion from Bangbule Pb-Zn-Cu Deposit, Western Gangdese, Tibet. Earth Science, 44(6): 1905-1922. doi: 10.3799/dqkx.2018.349

    Petrogenesis and Geological Implications of Late Cretaceous Intrusion from Bangbule Pb-Zn-Cu Deposit, Western Gangdese, Tibet

    doi: 10.3799/dqkx.2018.349
    • Received Date: 2018-07-16
    • Publish Date: 2019-06-15
    • The Bangbule deposit is located in the western part of the Nyainqing Tanggula Pb-Zn-Ag polymetallic metallogenic belt, which is a newly discovered large skarn Pb-Zn-Cu polymetallic deposit in 2010. The magmatic activity in the mining area is relatively simple, with the development of gray-light gray quartz porphyry, which is mainly composed of stock and dyke, and is closely related to the skarn Pb-Zn-Cu mineralization in space and time. In this paper, based on the detailed field basic geological field work and microscopic observation, we study the geochemistry, zircon U-Pb dating, whole rock Sr-Nd-Pb and zircon Hf isotopes of quartz porphyry. The results showed that the LA-ICP-MS U-Pb age of quartz porphyry is 77.2 ±0.8 Ma and 77.3 ±0.7 Ma, which occurred in the Late Cretaceous. The contents of SiO2 in quartz porphyry vary from 72.78% to 77.12%, the contents of K2O are 3.80%~5.55%, and the A/CNK is 0.88-1.18, which showing high-K calc-alkaline, metaluminous and high differentiation I-type granite characteristics. Total REE contents are between 146.89×10-6 and 247.89×10-6, which is characterized by relative enrichment of light rare earth and depletion of heavy rare earth. It has obvious anomalies such as Sr, Eu, Nb, Ta and P, suggesting that the magma experienced an important crystallization differentiation process. The εHf(t) of quartz porphyry is concentrated in the range of -7.92 to -5.73, and the corresponding crustal model is 1 651-1 121 Ma. The (87Sr/86Sr)i and the εNd(t) are 0.714 8-0.725 8 and -9.01 to -7.32, respectively, with the corresponding second Nd model ages (tDM2) of 1 612-1 477 Ma. The lead isotopes show that 206Pb/204Pb, 207Pb/204Pb and 208Pb/204Pb are 18.686-18.781, 15.699-15.762 and 39.131-39.344, respectively. In summary, the Bangbule quartz porphyry may have been formed by the magma derived from partial melting of the Mesoproterozoic Lhasa block during the extension environment in the post collision after Bangong -Nujiang south subduction. The discovery of the Late Cretaceous quartz porphyry in the Bangbule deposit shows that there is no absolute eruption in the Gangdese belt (80-70 Ma), which suggesting the continuity of the regional magmatic activity.

       

    • Amelin, Y., Lee, D.C., Halliday, A.N., et al., 1999.Nature of the Earth's Earliest Crust from Hafnium Isotopes in Sin-gle Detrital Zircons.Nature, 399(6733):252-255. doi: 10.1038/20426
      Blichert-Toft, J., Albarède, F., 1997.The Lu-Hf Isotope Geo-chemistry of Chondrites and the Evolution of the Mantle-Crust System.Earth and Planetary Science Letters, 148(1-2):243-258. https://doi.org/10.1016/s0012-821x(97)00040-x
      Cao, S.H., Li, D.W., Yu, Z.Z., et al., 2007.Metallogenic and Geological Characteristics of the Nixiong Superlarge Magnetite Deposit in Gangdese, Tibet. Geotectonica et Metallogenia, 31(3):328-334(in Chinese with English abstract). http://www.wanfangdata.com.cn/details/detail.do?_type=perio&id=ddgzyckx200703009
      Chappell, B.W., White, A.J.R., 1992.I-and S-Type Granites in the Lachlan Fold Belt. The Geological Society of America, 272:1-26. doi: 10.1130/SPE272
      Chappell, B.W., White, A.J.R., 2001.Two Contrasting Gran-ite Types:25 Years Later. Australian Journal of Earth Sciences, 48(4):489-499. doi: 10.1046/j.1440-0952.2001.00882.x
      Chen, W., Ma, C.Q., Bian, Q.J., et al., 2010.Subduction-Relat-ed Late Cretaceous Granitoids in Demingding Area, East of Middle Gangdese, Tibet:Evidence from Zircon U-Pb Geochronology and Geochemistry.Journal of Miner-al and Petrology. 30(1):83-92(in Chinese with English abstract).
      Chu, N.C., Taylor, R.N., Chavagnac, V., et al., 2002.Hf Iso-tope Ratio Analysis Using Multi-Collector Inductively Coupled Plasma Mass Spectrometry:An Evaluation of Isobaric Interference Corrections. Journal of Analytical Atomic Spectrometry, 17(12):1567-1574. doi: 10.1039/b206707b
      Collins, W.J., Beams, S.D., White, A.J.R., et al., 1982.Nature and Origin of A-Type Granites with Particular Reference to Southeastern Australia. Contributions to Mineralogy and Petrology, 80(2):189-200. doi: 10.1007/BF00374895
      Ding, L., Kapp, P., Zhong, D., et al., 2003. Cenozoic Volca-nism in Tibet:Evidence for a Transition from Oceanic to Continental Subduction. Journal of Petrology, 44(10):1833-1865. doi: 10.1093/petrology/egg061
      Ding, L., Zhao, Y.Y., Yang, Y.Q., et al., 2012.LA-ICP-MS Zircon U-Pb Dating and Geochemical Characteristics of Ore-Bearing Granite in Skarn-Type Iron Polymetallic Deposits of Duoba Area, Baingoin County, Tibet, and Their Significance.Acta Petrologica et Mineralogica, 31(4):479-496(in Chinese with English abstract). http://www.wanfangdata.com.cn/details/detail.do?_type=perio&id=yskwxzz201204002
      Ding, P. F., Wei, Q. R., Wang, C., et al., 2014. Chronology, Geochemical Characteristics and Tectonic Settings of the Late Yanshanian Granitoids in Zexue Area, Tibet.Geological Science and Technology Information, 33(4):37-45, 59(in Chinese with English abstract). http://www.wanfangdata.com.cn/details/detail.do?_type=perio&id=dzkjqb201404007
      Dong, Y.H., Xu, J.F., Zeng, Q.G., et al., 2006.Is There a Neo-Tethys' Subduction Record Earlier than Arc Volcanic Rocks in the Sangri Group? Acta Petrologica Sinica, 22(3):661-668.(in Chinese with English abstract).
      Du, D. D., Qu, X. M., Wang, G. H., et al., 2011. Bidirectional Subduction of the Middle Tethys Oceanic Basin in the West Segment of Bangonghu-Nujiang Suture, Tibet:Evi-dence from Zircon U-Pb LA-ICP-MS Dating and Petro-geochemistry of Arc Granites. Acta Petrologica Sinica, 27(7):1993-2002(in Chinese with English abstract).
      Foley, S. F., Barth, M. G., Jenner, G. A., 2000. Rutile/Melt Partition Coefficients for Trace Elements and an Assess-ment of the Influence of Rutile on the Trace Element Characteristics of Subduction Zone Magmas.Geochimica et Cosmochimica Acta, 64(5):933-938. https://doi.org/10.1016/s0016-7037(99)00355-5
      Gao, S.B., Zheng, Y.Y., Xie, M.C., et al., 2011.Geodynamic Setting and Mineralizational Implication of the Xueru In-trusion in Ban' ge, Tibet.Earth Science, 36(4):729-739(in Chinese with English abstract). https://doi.org/10.3799/dqkx.2011.073
      Gao, Y.F., Hou, Z.Q., Wei, R.H., 2003.Neogene Porphyries from Gangdese:Petrological, Geochemical Characteris-tics and Geodynamic Significances.Acta Petrologica Si-nica, 19(3):418-428(in Chinese with English abstract). http://en.cnki.com.cn/Article_en/CJFDTOTAL-YSXB200303004.htm
      Gariépy, C., Allègre, C. J., Xu, R. H., 1985. The Pb-Isotope Geochemistry of Granitoids from the Himalaya-Tibet Collision Zone:Implications for Crustal Evolution.Earth and Planetary Science Letters, 74(2-3):220-234. https://doi.org/10.1016/0012-821x(85)90023-8
      Griffin, W. L., Pearson, N. J., Belousova, E., et al., 2000. The Hf Isotope Composition of Cratonic Mantle:LAM-MC-ICPMS Analysis of Zircon Megacrysts in Kimberlites.Geochimica et Cosmochimica Acta, 64(1):133-147. https://doi.org/10.1016/s0016-7037(99)00343-9
      Guan, J.L., Geng, Q.R., Wang, G.Z., et al., 2014.Geochemi-cal, Zircon U-Pb Dating and Hf Isotope Compositions Studies of the Granite in Ritu County-Lameila Pass Ar-ea, North Gangdse, Tibe.Acta Petrologica Sinica, 30(6):1666-1684(in Chinese with English abstract).
      Guynn, J.H., Kapp, P., Pullen, A., et al., 2006.Tibetan Base-ment Rocks near Amdo Reveal "Missing" Mesozoic Tectonism along the Bangong Suture, Central Tibet.Ge-ology, 34(6):505. https://doi.org/10.1130/g22453.1
      He, Z.H., Yang, D.M., Wang, T.W., et al., 2005.SHRIMP U-Pb Dating of Zircons from Two-Mica Granite in Baga Area in Gangdise Belt.Journal of Jilin University (Earth Science Edition), 35(3):302-307(in Chinese with Eng-lish abstract). http://www.wanfangdata.com.cn/details/detail.do?_type=perio&id=cckjdxxb200503005
      Hou, Z.Q., Duan, L.F., Lu, Y.J., et al., 2015.Lithospheric Ar-chitecture of the Lhasa Terrane and Its Control on Ore Deposits in the Himalayan-Tibetan Orogen. Economic Geology, 110(6):1541-1575. https://doi.org/10.2113/econgeo.110.6.1541
      Hou, Z.Q., Yang, Z.S., Xu, W.Y., et al., 2006.Metallogenesis in Tibetan Collisional Orogenic Belt:Ⅰ.Mineralization in Main Collisional Orogenic Setting. Mineral Deposits, 25(4):337-358(in Chinese with English abstract).
      Huang, J.Q., Chen, B.W., 1993.Geological Evolution of Teth-ys Sea Around China and It Adjacent Areas. Geological Publishing House, Beijing(in Chinese).
      Irvine, T.N., Baragar, W.R.A.F., 1971.A Guide to the Chemi-cal Classification of the Common Volcanic Rocks.Cana-dian Journal of Earth Sciences, 8(5):523-548. doi: 10.1139/e71-055
      Ji, W.Q., Wu, F.Y., Chung, S.L., et al., 2009a.Zircon U-Pb Geochronology and Hf Isotopic Constraints on Petrogen-esis of the Gangdese Batholith, Southern Tibet. Chemi-cal Geology, 262(3-4):229-245. https://doi.org/10.1016/j.chemgeo.2009.01.020
      Ji, W. Q., Wu, F. Y., Liu, C. Z., et al., 2009b. Geochronology and Petrogenesis of Granitic Rocks in Gangdese Batho-lith, Southern Tibet. Science in China (Series D), 52(9):1240-1261. https://doi.org/10.1007/s11430-009-0131-y
      Ji, W.Q., Wu, F.Y., Chung, S.L., et al., 2014.The Gangdese Magmatic Constraints on a Latest Cretaceous Litho-spheric Delamination of the Lhasa Terrane, Southern Ti-bet. Lithos, 210-211:168-180. https://doi.org/10.1016/j.lithos.2014.10.001
      Jia, J. C., Wen, C. S., Wang, G. H., et al., 2005. Geochemical Characteristics and Geodynamic Significance of the Linzizong Group Volcanic Rocks in the Gangdise Area.Geology in China, 32(3):396-404(in Chinese with Eng-lish abstract). http://www.wanfangdata.com.cn/details/detail.do?_type=perio&id=zgdizhi200503007
      Jiang, J.H., Wang, R.J., Qu, X.M., et al., 2011.Crustal Exten-sion of the Bangong Lake Arc Zone, Western Tibetan Plateau, after the Closure of the Tethys Oceanic Basin. Earth Science, 36(6):1021-1026(in Chinese with Eng-lish abstract).
      Kapp, P., Murphy, M. A., Yin, A., et al., 2003. Mesozoic and Cenozoic Tectonic Evolution of the Shiquanhe Area of Western Tibet. Tectonics, 22(4):1029. https://doi.org/10.1029/2001tc001332
      Kelemen, P. B., Hanghøj, K., Greene, A. R., 2007. One View of the Geochemistry of Subduction-Related Magmatic Arcs, with an Emphasis on Primitive Andesite and Low-er Crust.Treatise on Geochemistry, 3:1-70. https://www.sciencedirect.com/science/article/pii/B0080437516030358
      Keto, L. S., Jacobsen, S. B., 1987. Nd and Sr Isotopic Varia-tions of Early Paleozoic Oceans. Earth and Planetary Science Letters, 84(1):27-41. https://doi.org/10.1016/0012-821x(87)90173-7
      Li, T.D., 2002.New Progress in the Geoscience Study of the Qinghai-Tibet Plateau.Geological Bulletin of China, 21(7):370-376(in Chinese with English abstract). http://www.wanfangdata.com.cn/details/detail.do?_type=perio&id=zgqydz200207002
      Li, X. S., Zhao, Y. Y., Wang, J. P., et al., 2013. Geochemical Characteristics, Chronology and Significance of Gengnai Skarn-Type Iron Polymetallic Deposit, Tibet.Acta Geo-logica Sinica, 87(11):1679-1693(in Chinese with Eng-lish abstract). http://www.wanfangdata.com.cn/details/detail.do?_type=perio&id=dizhixb201311004
      Liu, J. B., Na, X. H., Zhang, Z., et al., 2012. Dating and Geo-chemistry of the Late Cretaceous Granitoids near Menba Area in Gangdise Belt and Their Tectonic Setting.Glob-al Geology, 31(4):638-647(in Chinese with English ab-stract). http://en.cnki.com.cn/Article_en/CJFDTOTAL-SJDZ201204004.htm
      Liu, Y.S., Hu, Z.C., Zong, K.Q., et al., 2010.Reappraisement and Refinement of Zircon U-Pb Isotope and Trace Ele-ment Analyses by LA-ICP-MS. Chinese Science Bulle-tin, 55(15):1535-1546. https://doi.org/10.1007/s11434-010-3052-4
      Ludwig, K. R., 2003. Isoplot 3.0:A Geochronological Toolkit for Microsoft Excel:Berkeley.Geochronology Center Spe-cial Publication 4:1-70. doi: 10.1016-j.immuni.2011.10.010/
      Lv, L.N., Zhao, Y.Y., Song, L., et al., 2011.Characteristics of C, Si, O, S and Pb Isotopes of the Fe-Rich and Cu(Au) Deposits in the Western Bangong-Nujiang Metallogenic Belt, Tibet, and their Geological Significance.Acta Geo-logica Sinica, 85(8):1291-1304(in Chinese with English abstract). http://www.wanfangdata.com.cn/details/detail.do?_type=perio&id=dizhixb201108005
      Middlemost, E.A.K., 1986.Magmas and Magmatic Rocks:An Introduction to Igneous Petrology. Mineralogical Maga-zine, 50(355):185-186. https://www.researchgate.net/publication/236367046_Magmas_and_Magmatic_Rocks_an_introduction_to_igneous_petrology
      Middlemost, E.A.K., 1994.Naming Materials in the Magma/Igneous Rock System.Earth-Science Reviews, 37(3-4):215-224. doi: 10.1016/0012-8252(94)90029-9
      Miller, C., Schuster, R., Klötzli, U., et al., 1999. Post-Colli-sional Potassic and Ultrapotassic Magmatism in SW Ti-bet:Geochemical and Sr-Nd-Pb-O Isotopic Constraints for Mantle Source Characteristics and Petrogenesis.Journal of Petrology, 40(9):1399-1424. doi: 10.1093/petroj/40.9.1399
      Mo, X. X., Dong, G. C., Zhao, Z. D., et al., 2005. Spatial and Temporal Distribution and Characteristics of Granitoids in the Gangdese, Tibet and Implication for Crustal Growth and Evolution.Geological Journal of China Uni-versities, 11(3):281-290(in Chinese with an English ab-stract). http://www.wanfangdata.com.cn/details/detail.do?_type=perio&id=gxdzxb200503001
      Mo, X. X., Zhao, Z. D., Deng, J. F., et al., 2003. Response of Volcanism to the India-Asia Collision. Earth Science Frontiers, 10(3):135-148 (in Chinese with English ab-stract).
      Pan, G.T., Mo, X.X., Hou, Z.Q., et al., 2006.Spatial-Tempo-ral Framework of the Gangdese Orogenic Belt and Its Evolution. Acta Petrologica Sinica, 22(3):521-533(in Chinese with English abstract).
      Pan, G. T., Zhu, D. C., Wang, L. Q., et al., 2004. Bangong Lake-Nu River Suture Zone-The Northern Boundary of Gondwanaland:Evidence from Geology and Geophys-ics. Earth Science Frontiers, 11(4):371-382(in Chinese with English abstract). http://en.cnki.com.cn/Article_en/CJFDTOTAL-DXQY200404005.htm
      Pan, G.T., Wang, L.Q., Li, R.S., et al., 2012.Tectonic Evolu-tion of the Qinghai-Tibet Plateau.Journal of Asian Earth Sciences, 53:3-14. https://doi.org/10.1016/j.jseaes.2011.12.018
      Peccerillo, A., Taylor, S. R., 1976. Geochemistry of Eocene Calc-Alkaline Volcanic Rocks from the Kastamonu Ar-ea, Northern Turkey. Contributions to Mineralogy and Petrology, 58(1):63-81. doi: 10.1007/BF00384745
      Qu, X.M., Hou, Z.Q., Huang, W., 2001.Is Gangdese Porphy-ry Copper Belt the Second "Yulong" Copper Belt? Min-eral Deposits, 20(4):355-366 (in Chinese with English abstract). http://en.cnki.com.cn/Article_en/CJFDTotal-KCDZ200104009.htm
      Qu, X. M., Wang, R. J., Dai, J. J., et al., 2012. Discovery of Xiongmei Porphyry Copper Deposit in Middle Segment of Bangonghu-Nujiang Suture Zone and Its Significance.Mineral Deposits, 31(1):1-12(in Chinese with English abstract) http://www.wanfangdata.com.cn/details/detail.do?_type=perio&id=kcdz201201001
      Sun, S. S., McDonough, W. F., 1989. Chemical and Isotopic Systematics of Oceanic Basalts:Implications for Mantle Composition and Processes. Geological Society, London, Special Publications, 42(1):313-345. https://doi.org/10.1144/gsl.sp.1989.042.01.19
      Taylor, S. R., Rudnick, R. L., McLennan, S. M., et al., 1986. Rare Earth Element Patterns in Archean High-Grade Metasediments and Their Tectonic Significance.Geochimica et Cosmochimica Acta, 50(10):2267-2279. doi: 10.1016/0016-7037(86)90081-5
      Wang, J.P., Zhao, Y.Y., Cui, Y.B., et al., 2012.LA-ICP-MS Zircon U-Pb Dating of Important Skarn Type Iron (Cop-per) Polymetallic Deposits in Baingoin County of Tibet and Geochemical Characteristics of Granites. Geological Bulletin of China, 31(9):1435-1450(in Chinese with English abstract). http://en.cnki.com.cn/Article_en/CJFDTOTAL-ZQYD201209008.htm
      Wang, L.Y., Zheng, Y.Y., Gao, S.B., et al., 2014.The Upper Cretaceous Magmatism from Gangzai Pluton in Middle-Gangdese, Jiwa, Tibet and Its Tectonic Significance.Journal of Central South University(Science and Tech-nology), 45(8):2740-2751(in Chinese with English ab-stract). http://www.wanfangdata.com.cn/details/detail.do?_type=perio&id=zngydxxb201408027
      Yu, Y. S., Yang, Z. S., Dai, P. Y., et al. 2015. Geochronology and Genesis of the Magmatism in the Ri' a Copper Polymetallic Deposit of the Nixiong Orefield, Coqen, Ti-bet. Geology in China, 42(1):118-133(in Chinese with English abstract). http://en.cnki.com.cn/Article_en/CJFDTotal-DIZI201501009.htm
      Zhang, X.Q., Zhu, D.C., Zhao, Z.D., et al., 2010.Petrogenesis of the Nixiong Pluton in Coqen, Tibet and Its Potential Significance for the Nixiong Fe-Rich Mineralization.Ac-ta Petrologica Sinica, 26(6):1793-1804(in Chinese with English abstract). http://www.wanfangdata.com.cn/details/detail.do?_type=perio&id=ysxb98201006014
      Zhao, T.P., Zhou, M.F., Zhao, J.H., et al., 2008.Geochronolo-gy and Geochemistry of the ca. 80 Ma Rutog Granitic Pluton, Northwestern Tibet:Implications for the Tecton-ic Evolution of the Lhasa Terrane.Geological Magazine, 145(6):845-857.
      Zhao, Z. D., Mo, X. X., Dong, G. C., et al., 2007. Pb Isotopic Geochemistry of Tibetan Plateau and Its Implications.Geoscience, 21(2):265-274(in Chinese with English ab-stract). http://d.old.wanfangdata.com.cn/Periodical/dqkx-e201603007
      Zhu, D. C., Zhao, Z. D., Niu, Y. L., et al., 2012. Cambrian Bi-modal Volcanism in the Lhasa Terrane, Southern Tibet:Record of an Early Paleozoic Andean-Type Magmatic Arc in the Australian Proto-Tethyan Margin. Chemical Geology, 328:290-308. https://doi.org/10.1016/j.chemgeo.2011.12.024
      Zhu, D.C., Li, S.M., Cawood, P.A., et al., 2016.Assembly of the Lhasa and Qiangtang Terranes in Central Tibet by Divergent Double Subduction.Lithos, 245:7-17. https://doi.org/10.1016/j.lithos.2015.06.023
      Zhu, D.C., Mo, X.X., Wang, L.Q., et al., 2008.Hotspot-Ridge Interaction for the Evolution of Neo-Tethys:Insights from the Late Jurassic-Early Cretaceous Magmatism in South Tibet. Acta Petrological Sinica, 24(2):225-237(in Chinese with English abstract).
      Zhu, D.C., Zhao, Z.D., Niu, Y.L., et al., 2011.The Lhasa Ter-rane:Record of a Microcontinent and Its Histories of Drift and Growth. Earth and Planetary Science Letters, 301(1-2):241-255. https://doi.org/10.1016/j.epsl.2010.11.005
      Zhu, D. C., Zhao, Z. D., Pan, G. T., et al., 2009. Early Creta-ceous Subduction-Related Adakite-Like Rocks of the Gangdese Belt, Southern Tibet:Products of Slab Melting and Subsequent Melt-Peridotite Interaction? Journal of Asian Earth Sciences, 34(3):298-309. doi: 10.1016/j.jseaes.2008.05.003
      曹圣华, 李德威, 余忠珍, 等, 2007.西藏冈底斯尼雄超大型富铁矿的成矿地质特征.大地构造与成矿学, 31(3):328-334. doi: 10.3969/j.issn.1001-1552.2007.03.009
      陈炜, 马昌前, 边秋绢, 等, 2010.西藏冈底斯带中段以东得明顶地区晚白垩世花岗岩类锆石U-Pb年代学和地球化学证据.矿物岩石, 30(1):83-92. http://d.old.wanfangdata.com.cn/Periodical/kwys201001014
      定立, 赵元艺, 杨永强, 等, 2012.西藏班戈县多巴区矽卡岩型铁多金属矿床含矿花岗岩LA-ICP-MS锆石U-Pb定年、地球化学及意义.岩石矿物学杂志, 31(4):479-496. doi: 10.3969/j.issn.1000-6524.2012.04.002
      丁鹏飞, 魏启荣, 王程, 等, 2014.西藏则学地区俄穷瓦二长岩体的年代学、岩石地球化学特征及构造环境分析.地质科技情报, 33(4):37-45, 59. doi: 10.3969/j.issn.1009-6248.2014.04.005
      董彦辉, 许继峰, 曾庆高, 等, 2006.存在比桑日群弧火山岩更早的新特提斯洋俯冲记录么?岩石学报, 22(3):661-668. http://d.old.wanfangdata.com.cn/Periodical/ysxb98200603015
      杜德道, 曲晓明, 王根厚, 等, 2011.西藏班公湖-怒江缝合带西段中特提斯洋盆的双向俯冲:来自岛弧型花岗岩锆石U-Pb年龄和元素地球化学的证据.岩石学报, 27(7):1993-2002. http://d.old.wanfangdata.com.cn/Periodical/ysxb98201107008
      高顺宝, 郑有业, 谢名臣, 等, 2011.西藏班戈地区雪如岩体的形成环境及成矿意义.地球科学, 36(4):729-739. https://doi.org/10.3799/dqkx.2011.073
      高永丰, 侯增谦, 魏瑞华, 等, 2003.冈底斯晚第三纪斑岩的岩石学、地球化学及其地球动力学意义.岩石学报, 19(3):418-428. http://d.old.wanfangdata.com.cn/Periodical/ysxb98200303005
      关俊雷, 耿全如, 王国芝, 等, 2014.北冈底斯带日土县-拉梅拉山口花岗岩体的岩石地球化学特征、锆石U-Pb测年及Hf同位素组成.岩石学报, 30(6):1666-1684. http://d.old.wanfangdata.com.cn/Periodical/ysxb98201406010
      和钟铧, 杨德明, 王天武, 等, 2005.冈底斯带巴嘎区二云母花岗岩SHRIMP锆石U-Pb定年.吉林大学学报(地球科学版), 35(3):302-307. http://d.old.wanfangdata.com.cn/Periodical/cckjdxxb200503005
      侯增谦, 杨竹森, 徐文艺, 等, 2006.青藏高原碰撞造山带:I.主碰撞造山成矿作用.矿床地质, 25(4):337-358. http://d.old.wanfangdata.com.cn/Periodical/kcdz200604001
      黄汲清, 陈炳蔚, 1993.中国及邻区特提斯海的演化.北京:地质出版社.
      贾建称, 温长顺, 王根厚, 等, 2005.冈底斯地区林子宗群火山岩岩石地球化学特征及地球动力学意义.中国地质, 32(3):396-404. doi: 10.3969/j.issn.1000-3657.2005.03.007
      江军华, 王瑞江, 曲晓明, 等, 2011.青藏高原西部班公湖岛弧带特提斯洋盆闭合后的地壳伸展作用.地球科学, 36(6):1021-1026. http://www.earth-science.net/WebPage/Article.aspx?id=2178
      李廷栋, 2002.青藏高原地质科学研究的新进展.地质通报, 21(7):370-376. doi: 10.3969/j.issn.1671-2552.2002.07.002
      李小赛, 赵元艺, 王江朋, 等, 2013.西藏更乃矽卡岩型铁多金属矿床地球化学特征、年代学及意义.地质学报, 87(11):1679-1693. http://d.old.wanfangdata.com.cn/Periodical/dizhixb201311004
      刘建兵, 那晓红, 张忠, 等, 2012.冈底斯带门巴区晚白垩世花岗岩年代学、地球化学及构造背景.世界地质, 31(4):638-647. doi: 10.3969/j.issn.1004-5589.2012.04.003
      吕立娜, 赵元艺, 宋亮, 等, 2011.西藏班公湖-怒江成矿带西段富铁矿与铜(金)矿C、Si、O、S和Pb同位素特征及地质意义.地质学报, 85(8):1291-1304. http://d.old.wanfangdata.com.cn/Periodical/dizhixb201108005
      莫宣学, 董国臣, 赵志丹, 等, 2005.西藏冈底斯带花岗岩的时空分布特征及地壳生长演化信息.高校地质学报, 11(3):281-290. doi: 10.3969/j.issn.1006-7493.2005.03.001
      莫宣学, 赵志丹, 邓晋福, 等, 2003.印度-亚洲大陆主碰撞过程的火山作用响应.地学前缘, 10(3):135-148. doi: 10.3321/j.issn:1005-2321.2003.03.013
      潘桂棠, 莫宣学, 侯增谦, 等, 2006.冈底斯造山带的时空结构及演化.岩石学报, 22(3):521-533. http://d.old.wanfangdata.com.cn/Periodical/ysxb98200603001
      潘桂棠, 朱弟成, 王立全, 等, 2004.班公湖-怒江缝合带作为冈瓦纳大陆北界的地质地球物理证据.地学前缘, 11(4):371-382. doi: 10.3321/j.issn:1005-2321.2004.04.004
      曲晓明, 侯增谦, 黄卫, 2001.冈底斯斑岩铜矿(化)带:西藏第二条"玉龙"铜矿带?矿床地质, 20(4):355-366. doi: 10.3969/j.issn.0258-7106.2001.04.009
      曲晓明, 王瑞江, 代晶晶, 等, 2012.西藏班公湖-怒江缝合带中段雄梅斑岩铜矿的发现及意义.矿床地质, 31(1):1-12. doi: 10.3969/j.issn.0258-7106.2012.01.001
      王江朋, 赵元艺, 崔玉斌, 等, 2012.西藏班戈地区重要矽卡岩型铁(铜)多金属矿床LA-ICP-MS锆石U-Pb测年与花岗岩地球化学特征.地质通报, 31(9):1435-1450. doi: 10.3969/j.issn.1671-2552.2012.09.008
      王力圆, 郑有业, 高顺宝, 等, 2014.西藏吉瓦地区中冈底斯带岗在岩体晚白垩世的岩浆作用及构造意义.中南大学学报(自然科学版), 45(8):2740-2751. http://www.wanfangdata.com.cn/details/detail.do?_type=perio&id=zngydxxb201408027
      于玉帅, 杨竹森, 戴平云, 等, 2015.西藏措勤尼雄矿田日阿铜多金属矿床岩浆活动时代及成因.中国地质, 42(1):118-133. doi: 10.3969/j.issn.1000-3657.2015.01.010
      张晓倩, 朱弟成, 赵志丹, 等, 2010.西藏措勤尼雄岩体的岩石成因及其对富Fe成矿作用的潜在意义.岩石学报, 26(6):1793-1804. http://d.old.wanfangdata.com.cn/Periodical/ysxb98201006014
      赵志丹, 莫宣学, 董国臣, 等, 2007.青藏高原Pb同位素地球化学及其意义.现代地质, 21(2):265-274. doi: 10.3969/j.issn.1000-8527.2007.02.011
      朱弟成, 莫宣学, 王立全, 等, 2008.新特提斯演化的热点与洋脊相互作用:西藏南部晚侏罗世-早白垩世岩浆作用推论.岩石学报, 24(2):225-237. http://d.old.wanfangdata.com.cn/Periodical/ysxb98200802004
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