西藏班公湖-怒江缝合带西段洞错蛇绿岩中的辉长岩锆石U-Pb年代学及地质意义

武勇; 陈松永; 秦明宽; 郭冬发; 郭国林; 张财; 杨经绥

doi:10.3799/dqkx.2018.710

Volume 43 Issue 4

Apr. 2018

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Article Navigation > Earth Science > 2018 > 43(4): 1070-1084

Wu Yong, Chen Songyong, Qin Mingkuan, Guo Dongfa, Guo Guolin, Zhang Cai, Yang Jingsui, 2018. Zircon U-Pb Ages of Dongcuo Ophiolite in Western Bangonghu-Nujiang Suture Zone and Their Geological Significance. Earth Science, 43(4): 1070-1084. doi: 10.3799/dqkx.2018.710

Citation:

Wu Yong, Chen Songyong, Qin Mingkuan, Guo Dongfa, Guo Guolin, Zhang Cai, Yang Jingsui, 2018. Zircon U-Pb Ages of Dongcuo Ophiolite in Western Bangonghu-Nujiang Suture Zone and Their Geological Significance. Earth Science, 43(4): 1070-1084. doi: 10.3799/dqkx.2018.710

Citation:

Wu Yong, Chen Songyong, Qin Mingkuan, Guo Dongfa, Guo Guolin, Zhang Cai, Yang Jingsui, 2018. Zircon U-Pb Ages of Dongcuo Ophiolite in Western Bangonghu-Nujiang Suture Zone and Their Geological Significance. Earth Science, 43(4): 1070-1084. doi: 10.3799/dqkx.2018.710

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Zircon U-Pb Ages of Dongcuo Ophiolite in Western Bangonghu-Nujiang Suture Zone and Their Geological Significance

doi: 10.3799/dqkx.2018.710

1.
CNNC Key Laboratory of Uranium Resources Exploration and Evaluation Technology, Beijing Research Institute of Uranium Geology, Beijing 100029, China
2.
Center for Advanced Research on Mantle(CARMA), Key Laboratory of Deep-Earth Dynamics of Ministry of Land and Resources, Institute of Geology, Chinese Academy of Geological Sciences, Beijing 100037, China
3.
Faculty of Earth Sciences, East China University of Technology, Nanchang 330013, China
4.
Shanxi Museum of Geology, Taiyuan 030024, China

Received Date: 2017-12-20
Publish Date: 2018-04-15

Abstract

Abstract

The Dongcuo ophiolite is located at the western part of Bangong-Nujiang River suture zone, Gaize County. In spite of previous studies on its spacious distribution, tectonic environment and genesis, the key problem remains unresolved. Taking the gabbro of Dongcuo ophiolite as the research object, a detailed study of petrography, geochemistry, petrology and geochronology is carried out to understand the formation of Bangong-Nujiang ocean basin, the tectonic settings of the Dongcuo ophiolite. Compared with N-MORB, the major and trace elements of Dongcuo ophiolite are characterized by high content in Mg^# and low content in K, Na, P, and Ti, the depletion of high field-strength elements (HFSE) of Hf, Zr, Nb and light rare earth element depletion. Geochemistry characteristics of the Dongcuo ophiolite indicate that it is originated from~30% partial melting of depleted spinel lherzolite formed in the tectonic environment of subduction-related island arc or fore arc, belonging to super subduction zone (SSZ) ophiolite. The LA-ICP-MS of zircon U-Pb dating yields the age of 222±4.8 Ma (MSWD=0.5), providing the age constraint on the Dongcuo ophiolite (Late Triassic), and showing that it belongs to the Tethyan system of the Bangong-Nujiang River suture zone, which indicates the intra-oceanic subduction process.
- ophiolite,
- gabbro,
- tectonic environment,
- zircon U-Pb dating,
- Bangong-Nujiang suture zone,
- geochronology

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References(115)

References

Aitchison, J.C., Ali, J.R., Davis, A.M., 2007.When and Where did India and Asia Collide?Journal of Geophysical Research, 112(B5):B05423. https://doi.org/10.1029/2006jb004706

Aldanmaz, E., Pearce, J.A., Thirlwall, M.F., et al., 2000.Petrogenetic Evolution of Late Cenozoic, Post-Collision Volcanism in Western Anatolia, Turkey.Journal of Volcanology and Geothermal Research, 102(1/2):67-95. https://doi.org/10.1016/s0377-0273(00)00182-7

Bao, P.S., Xiao, X.C., Su, L., et al., 2007.Petrological, Geochemical and Chronological Constraints for the Tectonic Setting of the Dongco Ophiolite in Tibet.Science in China (Series D), 31(3):262-268 (in Chinese). doi: 10.1007/s11430-007-0045-5

Bao, P.S., Xiao, X.C., Wang, J., 1996.Geochemistry and Genesis of the Dongcuo Ophiolite in Tibet.Geological Publishing House, Beijing, 190-194 (in Chinese).

Chen, Y.L., Zhang, K.Z., Yang, Z.M., et al., 2006.Discovery of a Complete Ophiolite Section in the Jueweng Area, Nagqu County, in the Central Segment of the Bangong Co-Nujiang Junction Zone, Qinghai-Tibet Plateau.Geological Bulletin of China, 25(6):694-699 (in Chinese with English abstract). http://en.cnki.com.cn/Article_en/CJFDTOTAL-ZQYD200606007.htm

Cherniak, D.J., Watson, E.B., 2001.Pb Diffusion in Zircon.Chemical Geology, 172(1/2):5-24. https://doi.org/10.1016/s0009-2541(00)00233-3

Coleman, R.G, 1977.Ophiolites.Springer-Verlag, Berlin, 37(3):298-307.

Dewey, J.F., Shackleton, R.M., Chengfa, C., et al., 1988.The Tectonic Evolution of the Tibetan Plateau.Philosophical Transactions of the Royal Society A:Mathematical, Physical and Engineering Sciences, 327(1594):379-413. https://doi.org/10.1098/rsta.1988.0135

Dilek, Y., 2003.Ophiolite Concept and Its Evolution.Geological Society of America Papers, 373:1-16. https://doi.org/10.1130/0-8137-2373-6.1

Dilek, Y., Furnes, H., 2014.Ophiolite and Their Origins.Elements, 10(2):93-100. https://doi.org/10.2113/gselements.10.2.93

Dilek, Y., Furnes, H., Shallo, M., 2007.Suprasubduction Zone Ophiolite Formation along the Periphery of Mesozoic Gondwana.Gondwana Research, 11(4):453-475. https://doi.org/10.1016/j.gr.2007.01.005

Elliott, T., Plank, T., Zindler, A., et al., 1997.Element Transport from Slab to Volcanic Front at the Mariana Arc.Journal of Geophysical Research:Solid Earth, 102(B7):14991-15019. https://doi.org/10.1029/97jb00788

Fu, J.J., Ding, L., Xu, Q., et al., 2015.Zircon U-Pb Geochronology and Hf Isotopic Composition of the Cretaceous Volcanic Rocks and Constraint of the Collision Age of Banggong-Nujiang Suture Zone in Dongco Area, Gaize, Tibet.Chinese Journal of Geology, 50(1):182-202 (in Chinese with English abstract). http://www.dzkx.org/EN/abstract/abstract11139.shtml

He, Z.H., Yang, D.M., Wang, T.W., 2006.Age, Geochemistry and Its Tectonic Significance of Kaimeng Ophiolites in Jiali Fault Belt, Tibet.Acta Petrologica Sinica, 22(2):653-660 (in Chinese with English abstract). http://en.cnki.com.cn/Article_en/CJFDTOTAL-KWYS200601012.htm

Hofmann, A.W., 1988.Chemical Differentiation of the Earth:The Relationship between Mantle, Continental Crust, and Oceanic Crust.Earth and Planetary Science Letters, 90(3):297-314. https://doi.org/10.1016/0012-821x(88)90132-x

Huang, Q.S., Shi, R.D., Ding, B.H., et al., 2012.Re-Os Isotopic Evidence of MOR-Type Ophiolite from the Bangong Co for the Opening of Bangong-Nujiang Tethys Ocean.Acta Petrologica et Mineralogica, 31(4):465-478 (in Chinese with English abstract). https://www.researchgate.net/publication/284761968_Re-Os_isotopic_evidence_of_MOR-type_ophiolite_from_the_Bangong_Co_for_the_opening_of_Bangong-Nujiang_Tethys_Ocean

Huang, Q.T., Li, J.F., Xia, B., et al., 2015.Petrology, Geochemistry, Chronology and Geological Significance of Jiang Tso Ophiolite in Middle Segment of Banggonghu-Nujiang Suture Zone, Tibet.Earth Science, 40(1):35-48 (in Chinese with English abstract). http://en.cnki.com.cn/Article_en/CJFDTotal-DQKX201501003.htm

Kang, Z.Q., Xu, J.F., Wang, B.D., et al., 2010.Qushenla Formation Volcanic Rocks in North Lhasa Block:Products of Bangong Co-Nujiang Tethy's Southward Subduction.Acta Petrologica Sinica, 26(10):3106-3116 (in Chinese with English abstract). https://www.researchgate.net/publication/283768751_Qushenla_Formation_volcanic_rocks_in_north_Lhasa_block_Products_of_Bangong_Co-Nujiang_Tethy's_southward_subduction

Kapp, P., Yin, A., Manning, C.E., et al., 2003.Tectonic Evolution of the Early Mesozoic Blueschist-Bearing Qiangtang Metamorphic Belt, Central Tibet.Tectonics, 22(4):1043. https://doi.org/10.1029/2002tc001383

Lai, S.C., Liu, C.Y., 2003.Geochemistry and Genesis of the Island-Arc Ophiolite in Anduo Area, Tibetan Plateau.Acta Petrologica Sinica, 19(4):675-682 (in Chinese with English abstract). http://en.cnki.com.cn/Article_en/CJFDTOTAL-YSXB200304007.htm

Lee, J.K.W., Williams, I.S., Ellis, D.J., 1997.Pb, U and Th Diffusion in Natural Zircon.Nature, 390(6656):159-162. https://doi.org/10.1038/36554

Li, C., 1987.The Longmucuo-Shuanghu-Lancangjiang Plate Suture and the North Boundary of Distribution of Gondwana Facies Permo-Carboniferous System in Northern Xizang, China.Journal of Changchun College of Geology, 17(2):155-167 (in Chinese with English abstract). http://en.cnki.com.cn/Article_en/CJFDTOTAL-CCDZ198702003.htm

Li, J.F., Xia, B., Wang, R., et al., 2013.Mineralogical Characteristics of the Dong Tso Ophiolite and Its Tectonic Implications.Geotectonica et Metallogenia, 37(2):308-318 (in Chinese with English abstract). http://en.cnki.com.cn/Article_en/CJFDTotal-DGYK201302015.htm

Liu, W.B., Qian, Q., Yue, G.L., et al., 2002.The Geochemical Characteristics of Fore-Arc Ophiolite from Dingqing Area, Tibet.Acta Petrologica Sinica, 18(3):392-400 (in Chinese with English abstract). http://en.cnki.com.cn/Article_en/CJFDTOTAL-YSXB200203014.htm

Liu, Y.S., Hu, Z.C., Zong, K.Q., et al., 2010.Reappraisement and Refinement of Zircon U-Pb Isotope and Trace Element Analyses by LA-ICP-MS.Chinese Science Bulletin, 55(15):1535-1546. https://doi.org/10.1007/s11434-010-3052-4

Ludwig, K. R., 2009. ISOPLOT 3. 70: A Geochronological Toolkit for Microsoft Excel. Berkeley Geochronology Center, California.

Mi, W.T., Zhu, L.D., Li, Z.W., et al., 2012.Geochemical Characteristics of Gabbro and Diabase in the Shemalagou Ophiolite in Tibet.Xinjiang Geology, 30(4):465-470 (in Chinese with English abstract). http://en.cnki.com.cn/Article_en/CJFDTotal-XJDI201204018.htm

Moores, E.M., 2003.A Personal History of the Ophiolite Concept.Geological Society of America Special Papers, 373:17-29. https://doi.org/10.1130/0-8137-2373-6.17

Nimaciren, Xie, Y.W., 2005.Discovery of Middle Triassic Strata in the Nagqu Area, Northern Tibet, China, and Its Geological Implications.Geological Bulletin of China, 24(12):1141-1149 (in Chinese with English abstract). http://en.cnki.com.cn/Article_en/CJFDTotal-ZQYD200512010.htm

Pan, G.T., 1997.Geological Tectonic Evolution in the Eastern Tethys.Geological Publishing House, Beijing (in Chinese).

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 Geophysics.Earth Science Frontiers, 11(4):371-382 (in Chinese with English abstract). http://industry.wanfangdata.com.cn/dl/Detail/Periodical?id=Periodical_dxqy200404004

Pearce, J.A., 2008.Geochemical Fingerprinting of Oceanic Basalts with Applications to Ophiolite Classification and the Search for Archean Oceanic Crust.Lithos, 100(1/2/3/4):14-48. https://doi.org/10.1016/j.lithos.2007.06.016

Pearce, J.A., 2014.Immobile Element Fingerprinting of Ophiolites.Elements, 10(2):101-108.doi.:10.2113/gselements.10.2.101 doi: 10.2113/gselements.10.2.101

Pearce, J.A., Cann, J.R., 1973.Tectonic Setting of Basic Volcanic Rocks Determined Using Trace Element Analyses.Earth and Planetary Science Letters, 19(2):290-300. https://doi.org/10.1016/0012-821x(73)90129-5

Pearce, J.A., Parkinson, I.J., 1993.Trace Element Models for Mantle Melting:Application to Volcanic Arc Petrogenesis.Geological Society, London, Special Publications, 76(1):373-403. https://doi.org/10.1144/gsl.sp.1993.076.01.19

Pearce, J.A., Stern, R.J., 2006.Origin of Back-Arc Basin Magmas:Trace Element and Isotope Perspectives, Back-Arc Spreading Systems:Geological, Biological, Chemical, and Physical Interactions.Geophys.Monogr.Ser.AGU, Washington, DC, 63-86. https://doi.org/10.1029/166GM06

Qiangba, Z.X., Xie, Y.W., Wu, Y.W., et al., 2009.Zircon SIMS U-Pb Dating and Its Significance of Cumulate Gabbro from Dengqen Ophiolite, Eastern Tibet, China.Geological Bulletin of China, 28(9):1253-1258 (in Chinese with English abstract). http://en.cnki.com.cn/Article_en/CJFDTotal-ZQYD200909014.htm

Qiu, R.Z., Deng, J.F., Zhou, S., et al., 2005.Ophiolite Types in Western Qinghai Tibetan Plateau-Evidences from Petrology and Geochemistry.Earth Science Frontiers, 12(2):277-291 (in Chinese with English abstract). http://en.cnki.com.cn/Article_en/CJFDTOTAL-DXQY200502011.htm

Qiu, R.Z., Xiao, R., Zhou, S., et al., 2002.Geochronology and Nd and Sr Isotope Characteristics of Gabbro Dikes from the Shemalagou Area in the Middle Sector of the Bangonco-Nujiang Ophiolite Belt, North Tibet.Geological Review, 48(Suppl.):64-68 (in Chinese with English abstract). http://en.cnki.com.cn/Article_en/CJFDTOTAL-DZLP2002S1012.htm

Qiu, R.Z., Zhou, S., Deng, J.F., et al., 2004.Dating of Gabbro in the Shemalagou Ophiolite in the Western Segment of the Bangong Co-Nujiang Ophiolite Belt, Tibet-With a Discussion of the Age of the Bangong Co-Nujiang Ophiolite Belt.Geology in China, 31(3):262-268 (in Chinese with English abstract). http://en.cnki.com.cn/Article_en/CJFDTOTAL-DIZI200403003.htm

Qu, X.M., Wang, R.J., Xin, H.B., et al., 2009.Geochronology and Geochemistry of Igneous Rocks Related to the Subduction of the Tethys Oceanic Plate along the Bangong Lake Arc Zone, the Western Tibetan Plateau.Geochimica, 38(6):523-535 (in Chinese with English abstract). http://or.nsfc.gov.cn/bitstream/00001903-5/269773/1/1000014453093.doc

Qu, X.M., Xin, H.B., Xu, W.Y., et al., 2007.Petrogenesis of the Ore-Hosting Volcanic Rocks and Their Contribution to Mineralization in Xiongcun Superlarge Cu-Au Deposit, Tibet.Acta Geologica Sinica, 81(7):964-971 (in Chinese with English abstract). http://en.cnki.com.cn/Article_en/CJFDTotal-DZXE200707011.htm

Qu, X.M., Xin, H.B., Zhao, Y.Y., 2010.Opening Time of Bangong Lake Middle Tethys Oceanic Basin of the Tibet Plateau:Constraints from Petro-Geochemistry and Zircon U-Pb LA-ICP-MS Dating of Mafic Ophiolites.Earth Science Frontiers, 17(3):53-63 (in Chinese with English abstract). http://en.cnki.com.cn/Article_en/CJFDTotal-DXQY201003007.htm

Shervais, J.W., 1982.Ti-V Plots and the Petrogenesis of Modern and Ophiolitic Lavas.Earth and Plantary Science Letters, 59(1):101-118. doi: 10.1016/0012-821X(82)90120-0

Shi, R.D., 2007.The Age of Bangonghu SSZ-Type Ophiolite and Restrict of the Ban-Nu Ocean.Chinese Science Bulletin, 52(2):223-227 (in Chinese).

Shi, R.D., Griffin, W.L., O'Reilly, S.Y., et al., 2012.Melt/Mantle Mixing Produces Podiform Chromite Deposits in Ophiolites:Implications of Re-Os Systematics in the Dongqiao Neo-Tethyan Ophiolite, Northern Tibet.Gondwana Research, 21:194-206. doi: 10.1016/j.gr.2011.05.011

Sun, L.X., Bai, Z.D., Xu, D.B., et al., 2011.Geological Characteristics and Zircon U-Pb SHRIMP Dating of the Plagiogranite in Amduo Ophiolites, Tibet.Geological Survey and Research, 34(1):10-15 (in Chinese with English abstract). http://or.nsfc.gov.cn/bitstream/00001903-5/266436/1/1000014593461.pdf

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

Vavra, G., Schmid, R., Gebauer, D., 1999.Internal Morphology, Habit and U-Th-Pb Microanalysis of Amphibolite-to-Granulite Facies Zircons:Geochronology of the Ivrea Zone (Southern Alps).Contributions to Mineralogy and Petrology, 134(4):380-404. https://doi.org/10.1007/s004100050492

Wang, B.D., Wang, L.Q., Chung, S.L., et al., 2016.Evolution of the Bangong-Nujiang Tethyan Ocean:Insights from the Geochronology and Geochemistry of Mafic Rocks within Ophiolites.Lithos, 245:18-33. https://doi.org/10.13039/100007834

Wang, W.L., Aitchison, J.C., Lo, C.H., et al., 2008.Geochemistry and Geochronology of the Amphibolite Blocks in Ophiolite Melanges along Bangong-Nujiang Suture, Central Tibet.Joural of Asian Earth Sciences, 33(1-2):122-138. doi: 10.1016/j.jseaes.2007.10.022

Wang, X.B., Bao, P.S., Deng, W.M., et al., 1987.Tibet Ophiolite.Geological Publishing House, Beijing (in Chinese).

Wei, S.G., Song, Y., Tang, J.X., et al., 2016.Geochemistry and Geochronology of Intra-Oceanic Subduction of the Bangong-Nujiang Tethyan Ocean during Late Permian (ca.252Ma).Geological Review, 62(Suppl.):194-196 (in Chinese with English abstract).

Wei, Z.Q., Xia, B., Xu, L.F., et al., 2009.Geochemistry and Tectonic Setting of Western Pung Co Lake Ophiolite, Xizang (Tibet).Geological Review, 55(6):785-794 (in Chinese with English abstract). http://en.cnki.com.cn/Article_en/CJFDTotal-DZLP200906004.htm

Wei, Z.Q., Xia, B., Zhou, G.Q., et al., 2007.Geochemical Characteristics and Its Origin for Mid-Ocean Ridge Superposing Oceanic Island of Chongbe Ophiolite Mélange, Dingqing, Xizang (Tibet).Geological Review, 53(2):187-197 (in Chinese with English abstract). http://en.cnki.com.cn/Article_en/CJFDTOTAL-DZLP200702007.htm

Wilson, M., 1989.Igneous Petrogenesis.Journal of Geology, 12:348-356. https://doi.org/10.1007/978-94-010-9388-0

Winchester, J.A., Floyd, P.A., 1977.Geochemical Discrimination of Different Magma Series and Their Differentiation Products Using Immobile Elements.Chemical Geology, 20:325-343. https://doi.org/10.1016/0009-2541(77)90057-2

Wu, Z.H., Ye, P.S., Yin, C.Y., et al., 2013.The Early Cenozoic Gerze Thrust System in Northern Tibet.Acta Geoscientica Sinica, 34(1):31-37 (in Chinese with English abstract). http://en.cnki.com.cn/Article_en/CJFDTotal-DQXB201301006.htm

Xia, B, Xu, L.F., Wei, Z.Q., et al., 2008.SHRIMP Zircon Dating of Gabbro from the Donqiao Ophiolite in Tibet and Its Geological Implications.Acta Geologica Sinica, 82(4):528-531 (in Chinese with English abstract). http://en.cnki.com.cn/Article_en/CJFDTOTAL-DZXE200804010.htm

Xia, B., Zhong, F.T., 1991.Geochemical Characteristics and Genetic Significance of Ophiolite from Dong Tso, Tibet.Geology of Tibet, (2):73-87 (in Chinese).

Xu, Y.G., Menzies, M.A., Thirlwall, M.F., et al., 2001.Exotic Lithosphere Mantle beneath the Western Yangtze Craton:Petrogenetic Links to Tibet Using Highly Magnesian Ultrapotassic Rocks.Geology, 29(9):863.https://doi.org/10.1130/0091-7613(2001)029<0863:elmbtw>2.0.co;2 doi: 10.1130/0091-7613(2001)029<0863:elmbtw>2.0.co;2

Xu, Z.Q., Li, H.B., Yang, J.S., 2006.An Orogenic Plateau-The Orogenic Collage and Orogenic Types of the Qinghai Tibet Plateau.Earth Science Frontiers, 13(4):1-17(in Chinese with English abstract). http://en.cnki.com.cn/Article_en/CJFDTotal-DXQY200604001.htm

Yang, J.S., Bai, W.J., Fang, Q.S., et al., 2004.Coesite Discovered from the Podiform Chromitite in the Luobusha Ophiolite, Tibet.Earth Science, 29(6):651-660 (in Chinese with English abstract). http://en.cnki.com.cn/Article_en/CJFDTotal-DQKX200406002.htm

Yang, J.S., Xu, X.Z., Rong, H., et al., 2013.Deep Mineral in Ophiolitic Mantle Peridotites:Discovery and Progress.Bulletin of Mineralogy, Petrology and Geochemistry, 32(2):159-170 (in Chinese with English abstract). http://www.geojournals.cn/dzxb/ch/reader/view_abstract.aspx?file_no=dzxbcn2013z10011&flag=1

Ye, P.S., Wu, Z.H., Hu, D.G., et al., 2004.Geochemical Characteristics and Tectonic Setting of Ophiolite of Dongqiao, Tibet.Geoscience, 18(3):309-315 (in Chinese with English abstract). http://en.cnki.com.cn/Article_en/CJFDTOTAL-XDDZ200403007.htm

You, Z.P., 1997.⁴⁰Ar-³⁹Ar Chronology of Dingqing Ophiolite, Tibet.Geology of Tibet, (2):24-30 (in Chinese with English abstract).

Zhang, Y. X., 2007. Tectonic Evolution of the Middle-Western Bangong-Nujiang Suture, Tibet (Dissertation). Chinese Academy of Sciences, Guangzhou (in Chinese with English abstract).

Zheng, Y.Y., Xu, R.K., He, L.X., et al., 2004.The Shiquan River Ophiolite Mélange Zone in Xizang:The Delineation and Significance of a New Archipelagic Arc-Basin System.Sedimentary Geology and Tetyan Geology, 24(1):13-20 (in Chinese with English abstract). http://en.cnki.com.cn/Article_en/CJFDTotal-TTSD200401001.htm

Zheng, Y.Y., Xu, R.K., Ma, G.T., et al., 2006.Ages of Generation and Subduction of Shiquan River Ophiolite:Restriction from SHRIMP Zircon Dating.Acta Petrologica Sinica, 22(4):895-904 (in Chinese with English abstract). http://www.oalib.com/paper/1473585

Zhong, Y, Liu., W.L, Xia, B., et al., 2017.Geochemistry and Geochronology of the Mesozoic Lanong Ophiolitic Melange, Northern Tibet:Implications for Petrogenesis and Tectonic Evolution.Lithos, 292:111-131. https://doi.org/10.1016/j.lithos.2017.09.003

Zhou, G.Q., 2008.Ophiolite:Some Key Aspects Regarding Its Definition and Classification.Journal of Nanjing University (Natural Sciences), 44(1):1-24 (in Chinese with English abstract). http://en.cnki.com.cn/Article_en/CJFDTOTAL-NJDZ200801002.htm

Zhou, M.F., Malpas, J.G., Robinson, P.T., et al., 1997.The Dynamothermal Aureole of the Donqiao Ophiolite (Northern Tibet).Canadian Journal of Earth Science., 34(1):59-65. doi: 10.1139/e17-005

Zhu, D.C., Pan, G.T., Mo, X.X., et al., 2006.Late Jurassic-Early Cretaceous Geodynamic Setting in Middle-Northern Gangdese:New Insights from Volcanic Rocks.Acta Petrologica Sinica, 22(3):534-546 (in Chinese with English abstract). http://www.oalib.com/paper/1472180

鲍佩声, 肖序常, 苏梨, 等, 2007.西藏洞错蛇绿岩的构造环境:岩石学、地球化学和年代学制约.中国科学(D辑), 31(3):262-268. http://www.cqvip.com/Main/Detail.aspx?id=24393545

鲍佩声, 肖序常, 王军, 等, 1996.西藏洞错蛇绿岩的地球化学及其生因.北京:地质出版社, 190-194.

陈玉禄, 张宽忠, 杨志民, 等, 2006.青藏高原班公湖-怒江结合带中段那曲县觉翁地区发现完整的蛇绿岩剖面.地质通报, 25(6):694-699. http://www.wanfangdata.com.cn/details/detail.do?_type=perio&id=zgqydz200606007

付佳俊, 丁林, 许强, 等, 2015.西藏改则洞错地区白垩纪火山岩锆石U-Pb年代学、Hf同位素组成及对班公-怒江洋俯冲闭合的制约.地质科学, 50(1):182-202. http://www.dzkx.org/cn/abstract/abstract11139.shtml

和钟铧, 杨德明, 王天武, 等, 2006.西藏嘉黎断裂带凯蒙蛇绿岩的年代学、地球化学特征及其大地构造意义.岩石学报, 22(2):653-660. http://www.ysxb.ac.cn/ysxb/ch/reader/view_abstract.aspx?file_no=20060370

黄启帅, 史仁灯, 丁炳华, 等, 2012.班公湖MOR型蛇绿岩Re-Os同位素特征对班公湖-怒江特提斯洋裂解时间的制约.岩石矿物学杂志, 31(4):465-478. http://www.wanfangdata.com.cn/details/detail.do?_type=perio&id=yskwxzz201204001

黄强太, 李建峰, 夏斌, 等, 2015.西藏班公湖-怒江缝合带中段江错蛇绿岩岩石学、地球化学、年代学及地质意义.地球科学, 40(1):34-48. http://www.earth-science.net/WebPage/Article.aspx?id=3014

康志强, 许继峰, 王宝弟, 等, 2010.拉萨地块北部去申拉组火山岩:班公湖-怒江特提斯洋南向俯冲的产物?岩石学报, 26(10):3106-3116. http://industry.wanfangdata.com.cn/yj/Detail/Periodical?id=Periodical_ysxb98201010022

赖绍聪, 刘池阳, 2003.青藏高原安多岛弧蛇绿岩地球化学及其成因.岩石学报, 19(4):675-682. http://www.wanfangdata.com.cn/details/detail.do?_type=perio&id=ysxb98200304008

李才, 1987.龙木错-双湖-澜沧江板块缝合带与石炭二叠纪冈瓦纳北界.长春地质学院学报, 17(2):155-167. http://www.cqvip.com/QK/91256B/198702/67676890495756554850484851.html

李建峰, 夏斌, 王冉, 等, 2013.洞错地幔橄榄岩、均质辉长岩矿物化学特征及其构造意义.大地构造与成矿学, 37(2):308-318. http://d.wanfangdata.com.cn/Periodical_ddgzyckx201302013.aspx

刘文斌, 钱青, 岳国利, 等, 2002.西藏丁青弧前蛇绿岩的地球化学特征.岩石学报, 18(3):392-400. http://d.old.wanfangdata.com.cn/Periodical/ysxb98200203015

密文天, 朱利东, 李智武, 等, 2012.西藏舍马拉沟蛇绿岩中辉长岩及辉绿岩地球化学特征.新疆地质, 30(4):465-470. http://www.cqvip.com/QK/82738X/201204/44124569.html

尼玛次仁, 谢尧武, 2005.藏北那曲地区中三叠地层的新发现及其地质意义.地质通报, 24(12):1141-1149. doi: 10.3969/j.issn.1671-2552.2005.12.009

潘桂堂, 1997.东特提斯地质构造形成演化.北京:地质出版社.

潘桂堂, 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. http://www.wanfangdata.com.cn/details/detail.do?_type=perio&id=dxqy200404004

强巴扎西, 谢荛武, 吴彦旺, 等, 2009.藏东丁青蛇绿岩中堆晶辉长岩锆石SIMS U-Pb定年及其地质意义.地质通报, 28(9):1253-1258. http://industry.wanfangdata.com.cn/dl/Detail/Periodical?id=Periodical_zgqydz200909013

邱瑞照, 邓晋福, 周肃, 等, 2005.青藏高原西部蛇绿岩类型:岩石学与地球化学证据.地学前缘, 12(2):277-291. http://www.cqvip.com/QK/98600X/2005002/15572659.html

邱瑞照, 肖润, 周肃, 等, 2002.藏北班公湖-怒江带舍玛拉沟蛇绿岩中辉长岩Sm-Nd定年和Sr、Nd同位素研究.地质论评, 48(增刊):64-68. http://www.oalib.com/paper/4892600

邱瑞照, 周肃, 邓晋福, 等, 2004.西藏班公湖-怒江西段舍马拉沟蛇绿岩中辉长岩年龄测定——兼论班公湖-怒江蛇绿岩带形成时代.中国地质, 31(3):262-268. http://geochina.cgs.gov.cn/ch/reader/view_abstract.aspx?file_no=20040304&flag=1

曲晓明, 王瑞江, 辛洪波, 等, 2009.西藏西部与班公湖特提斯洋盆俯冲相关的火成岩年代学和地球化学, 地球化学, 38(6):523-535. http://www.cqvip.com/Main/Detail.aspx?id=31887686

曲晓明, 辛洪波, 徐文艺, 等, 2007.西藏雄村特大型铜金矿床容矿火山岩的成因及其对成矿的贡献.地质学报, 81(7):964-971. http://www.geojournals.cn/dzxb/ch/reader/view_abstract.aspx?file_no=200707112&flag=1

曲晓明, 辛洪波, 赵元艺, 等, 2010.西藏班公湖中特提斯洋盆的打开时间:镁铁质蛇绿岩地球化学与锆石U-Pb LA-ICP-MS定年结果.地学前缘, 17(3):53-63. http://www.earthsciencefrontiers.net.cn/CN/abstract/abstract4083.shtml

史仁灯, 2007.班公湖SSZ型蛇绿岩年龄对班-怒洋时限的制约.科学通报, 52(2):223-227. http://www.oalib.com/paper/4274997

孙立新, 白志达, 徐德斌, 等, 2011.西藏安多蛇绿岩中斜长花岗岩地球化学特征及锆石U-Pb SHRIMP年龄.地质调查与研究, 34(1):10-15. http://www.cqvip.com/QK/71135X/201107/37382939.html

王希斌, 鲍佩声, 邓万明, 等, 1987.西藏蛇绿岩.北京:地质出版社.

韦少港, 宋扬, 唐菊兴, 2016.西藏班公湖-怒江西段特提斯洋晚二叠世(Ca. 252Ma)洋内俯冲的地球化学和年代学证据.地质论评, 62(S1):194-196. http://www.geojournals.cn/georev/ch/reader/view_abstract.aspx?file_no=dzlp201662s094&flag=1

韦振权, 夏斌, 徐力峰, 等, 2009.西藏蓬湖西蛇绿岩地球化学及构造背景研究.地质论评, 55(6):785-794. http://www.cqvip.com/Main/Detail.aspx?id=32209920

韦振权, 夏斌, 周国庆, 等, 2007.西藏丁青宗白蛇绿混杂岩地球化学特征及其洋中脊叠加洋岛的成因.地质论评, 53(2):187-197. http://www.geojournals.cn/georev/ch/reader/view_abstract.aspx?file_no=20070235

吴珍汉, 叶培盛, 殷才云, 等, 2013.藏北改则新生代早期逆冲推覆构造系统.地球学报, 34(1):31-37. doi: 10.3975/cagsb.2013.01.04

夏斌, 徐力峰, 韦振权, 等, 2008.西藏东巧蛇绿岩中辉长岩锆石SHRIMP定年及其地质意义.地质学报, 82(4):528-531. http://d.old.wanfangdata.com.cn/Periodical/dizhixb200804010

夏斌, 钟富泰, 1991.西藏北部洞错蛇绿岩地体的岩石地球化学特征及其成因意义.西藏地质, (2):73-87. http://www.cqvip.com/QK/97137X/199102/631548.html

许志琴, 李海斌, 杨经绥, 等, 2006.造山的高原——青藏高原巨型造山带拼贴体和造山类型.地学前缘, 13(4):1-17. http://www.wanfangdata.com.cn/details/detail.do?_type=perio&id=dxqy200604002

杨经绥, 白文吉, 方青松, 等, 2004.西藏罗布莎豆荚状铬铁矿中发现超高压矿物柯石英.地球科学, 29(6):651-660. http://www.earth-science.net/WebPage/Article.aspx?id=1466

杨经绥, 徐向珍, 戎合, 等, 2013.蛇绿岩地幔橄榄岩中的深部矿物:发现与研究进展.矿物岩石地球化学通报, 32(2):159-170. http://www.wanfangdata.com.cn/details/detail.do?_type=perio&id=kwysdqhxtb201302002

叶培盛, 吴珍汉, 胡道功, 等, 2004.西藏东巧蛇绿岩的地球化学特征及其形成构造环境.现代地质, 18(3):309-315. http://www.cqvip.com/Main/Detail.aspx?id=10277771

游再平, 1997.西藏丁青蛇绿混杂岩⁴⁰Ar-³⁹Ar年代学.西藏地质, (2):24-30. http://www.cqvip.com/QK/97137X/199702/2874879.html

张玉修, 2007. 班公湖-怒江缝合带中西段构造演化(博士学位论文). 广州: 中国科学院研究生院.

郑有业, 许荣科, 何来信, 等, 2004.西藏狮泉河蛇绿混杂岩带——一个新的多岛弧盆系统的厘定及意义.沉积与特提斯地质, 24(1):13-20. http://www.cqvip.com/Main/Detail.aspx?id=9483237

郑有业, 许荣科, 马国桃, 等, 2006.锆石SHRIMP测年对狮泉河蛇绿岩形成和俯冲的时间约束.岩石学报, 22(4):895-904. http://www.ysxb.ac.cn/ysxb/ch/reader/view_abstract.aspx?file_no=20060495&journal_id=ysxb

周国庆, 2008.蛇绿岩研究新进展及其定义和分类的再讨论.南京大学学报(自然科学), 44(1):1-24. https://www.wenkuxiazai.com/doc/a059b8d284254b35eefd345e.html

朱弟成, 潘桂堂, 莫宣学, 等, 2006.冈底斯中北部晚侏罗世-早白垩世地球动力学环境:火山岩约束.岩石学报, 22(3):534-546. http://www.cnki.com.cn/Article/CJFDTOTAL-YSXB200603002.htm

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