西藏雅鲁藏布江缝合带西段达巴蛇绿岩年代学、地球化学特征及其构造意义

程晨; 夏斌; 郑浩; 袁亚娟; 殷征欣; 陆野; 徐迟; 张霄

doi:10.3799/dqkx.2018.703

Volume 43 Issue 4

Apr. 2018

Turn off MathJax

Article Contents

Article Navigation > Earth Science > 2018 > 43(4): 975-990

Cheng Chen, Xia Bin, Zheng Hao, Yuan Yajuan, Yin Zhengxin, Lu Ye, Xu Chi, Zhang Xiao, 2018. Chronology, Geochemistry and Tectonic Significance of Daba Ophiolites in Western Segment of Yarlung Zangbo Suture Zone, Tibet. Earth Science, 43(4): 975-990. doi: 10.3799/dqkx.2018.703

Citation:

Cheng Chen, Xia Bin, Zheng Hao, Yuan Yajuan, Yin Zhengxin, Lu Ye, Xu Chi, Zhang Xiao, 2018. Chronology, Geochemistry and Tectonic Significance of Daba Ophiolites in Western Segment of Yarlung Zangbo Suture Zone, Tibet. Earth Science, 43(4): 975-990. doi: 10.3799/dqkx.2018.703

Citation:

Cheng Chen, Xia Bin, Zheng Hao, Yuan Yajuan, Yin Zhengxin, Lu Ye, Xu Chi, Zhang Xiao, 2018. Chronology, Geochemistry and Tectonic Significance of Daba Ophiolites in Western Segment of Yarlung Zangbo Suture Zone, Tibet. Earth Science, 43(4): 975-990. doi: 10.3799/dqkx.2018.703

PDF( 3876 KB)

Chronology, Geochemistry and Tectonic Significance of Daba Ophiolites in Western Segment of Yarlung Zangbo Suture Zone, Tibet

doi: 10.3799/dqkx.2018.703

Cheng Chen^{1,2
,},
Xia Bin^{1,2
,
,},
Zheng Hao^1,2,
Yuan Yajuan^1,2,
Yin Zhengxin³,
Lu Ye^1,2,
Xu Chi^1,2,
Zhang Xiao^1,2

1.
School of Marine Sciences, Sun Yat-sen University, Guangzhou 510006, China
2.
Key Laboratory of Offshore Oil Exploration and Development of Guangdong Higher Education Institutes, Guangzhou 510006, China
3.
South China Sea Marine Survey and Technology Center, State Oceanic Administration, Guangzhou 510300, China

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

Abstract

Abstract

The Daba ophiolite is located in the southern sub-belt of the western segment of the Yarlung Zangbo suture zone (YZSZ) and mainly composed of mantle peridotite, mafic dikes and siliceous rocks. Its formation time and tectonic setting are not clear. This is the first report of zircon U-Pb age, petrologic and whole-rock geochemical data from the Daba ophiolite. The major elements of Daba gabbro and dolerite are characterized by high contents in Al, Mg and low contents in Ti, K and P, which belong to subalkaline basalt. The REE distribution patterns are very similar to those of the normal mid-ocean ridge basalt (N-MORB). However, the normalized spider diagram shows significant depletion of Nb, suggesting the influence of fluids from downgoing slab.The dolerites yielded zircon U-Pb ages of 120.0±1.7 Ma, and geochemical features show partial melting from the low degree spinel-bearing mantle source. Combining with previous studies, it is suggested that the intrusion of the mafic rocks into the Daba peridotites may be interpreted as a result of mixing process between MORB-like melts and arc-derived fluids, which may have occurred during the stage of subduction initiation in an extending forearc region.
- Yarlung Zangbo suture zone,
- Daba ophiolite,
- geochemistry,
- zircon U-Pb age,
- tectonic setting

FullText(HTML)

References(78)

References

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 doi: 10.1016/S0377-0273(00)00182-7

Andersen, T., 2002.Correction of Common Pb in U-Pb Analyses That do not Report ²⁰⁴Pb.Chemical Geology, 192(1-2):59-79. https://doi.org/10.1016/S0009-2541(02)00195-X

Bezard, R., Hébert, R., Wang, C.S., et al., 2011.Petrology and Geochemistry of the Xiugugabu Ophiolitic Massif, Western Yarlung Zangbo Suture Zone, Tibet.Lithos, 125(1-2):347-367. https://doi.org/10.1016/j.lithos.2011.02.019

Black, L.P., Kamo, S.L., Allen, C.M., et al., 2003.TEMORA 1:A New Zircon Standard for Phanerozoic U-Pb Geochronology.Chemical Geology, 200(1-2):155-170.https://doi.org/10.1016/s0009-2541(03)00165-7 doi: 10.1016/S0009-2541(03)00165-7

Butler, J.P., Beaumont, C., 2017.Subduction Zone Decoupling/Retreat Modeling Explains South Tibet (Xigaze) and Other Supra-Subduction Zone Ophiolites and Their UHP Mineral Phases.Earth and Planetary Science Letters, 463:101-117. https://doi.org/10.1016/j.epsl.2017.01.025

Cabanis, B., Lecolle, M., 1989.Le Diagramme La/10-Y/15-Nb/8:Un Outilpour La Discrimination des Séries Volcaniques et La Mise Enévidence Des Processus de Mélange et/ou de Contamination Crustale.Comptes Rendus de l'Académie des Sciences, Série Ⅱ, 309:2023-2029.

Coleman, R.G., 1977.Ophiolites:Ancient Oceanic Lithosphere.Springer-Verlag, Berlin. https://linkinghub.elsevier.com/retrieve/pii/0012825279901132

Compston, W., Williams, I.S., Kirschvink, J.L., et al., 1992.Zircon U-Pb Ages for the Early Cambrian Time-Scale.Journal of the Geological Society, 149(2):171-184. https://doi.org/10.1144/gsjgs.149.2.0171

Dai, J.G., Wang, C.S., Polat, A., et al., 2013.Rapid Forearc Spreading between 130 and 120 Ma:Evidence from Geochronology and Geochemistry of the Xigaze Ophiolite, Southern Tibet.Lithos, 172-173:1-16. https://doi.org/10.1016/j.lithos.2013.03.011

Dai, J.G., Wang, C.S., Hébert, R., et al., 2011.Late Devonian OIB Alkaline Gabbro in the Yarlung Zangbo Suture Zone:Remnants of the Paleo-Tethys?Gondwana Research, 19(1):232-243. https://doi.org/10.1016/j.gr.2010.05.015

Dilek, Y., Furnes, H., 2011.Ophiolite Genesis and Global Tectonics:Geochemical and Tectonic Fingerprinting of Ancient Oceanic Lithosphere.Geological Society of America Bulletin, 123(3-4):387-411.https://doi.org/10.1130/b30446.1 doi: 10.1130/B30446.1

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

Furnes, H., Dilek, Y., 2017.Geochemical Characterization and Petrogenesis of Intermediate to Silicic Rocks in Ophiolites:A Global Synthesis.Earth-Science Reviews, 166:1-37. https://doi.org/10.1016/j.earscirev.2017.01.001

Gribble, R.F., Stern, R.J., Newman, S., et al., 1998.Chemical and Isotopic Composition of Lavas from the Northern Mariana Trough:Implications for Magma Genesis in Back-Arc Basins.Journal of Petrology, 39(1):125-154. https://doi.org/10.1093/petroj/39.1.125

Guilmette, C., Hébert, R., Dostal, J., et al., 2012.Discovery of a Dismembered Metamorphic Sole in the Saga Ophiolitic Mélange, South Tibet:Assessing an Early Cretaceous Disruption of the Neo-Tethyan Supra-Subduction Zone and Consequences on Basin Closing.Gondwana Research, 22(2):398-414. https://doi.org/10.1016/j.gr.2011.10.012

Hébert, R., Bezard, R., Guilmette, C., et al., 2012.The Indus-Yarlung Zangbo Ophiolites from Nanga Parbat to Namche Barwa Syntaxes, Southern Tibet:First Synthesis of Petrology, Geochemistry, and Geochronology with Incidences on Geodynamic Reconstructions of Neo-Tethys.Gondwana Research, 22(2):377-397. https://doi.org/10.1016/j.gr.2011.10.013

Hellebrand, E., 2002.Garnet-Field Melting and Late-Stage Refertilization in 'Residual' Abyssal Peridotites from the Central Indian Ridge.Journal of Petrology, 43(12):2305-2338. https://doi.org/10.1093/petrology/43.12.2305

Huang, G.C., Xu, D.M., Lei, Y.J., et al., 2010.Characteristics and Geological Implications of Chert Associated with Ophiolite in Southwestern Tibet.Geology in China, 37(1):101-109 (in Chinese with English abstract). http://or.nsfc.gov.cn/bitstream/00001903-5/266436/1/1000014593461.pdf

Leng, Q.F., Tang, J.X., Zheng, W.B., et al., 2016.Geochronology, Geochemistry and Zircon Hf Isotopic Compositions of the Ore-Bearing Porphyry in the Lakang'e Porphyry Cu-Mo Deposit, Tibet.Earth Science, 41(6):999-1015 (in Chinese with English abstract).

Li, J.F., Xia, B., Liu, L.W., et al., 2008.SHRIMP U-Pb Zircon Dating of Diabase in the La'nga Co Ophiolite, Burang, Tibet, China, and Its Geological Significance.Geological Bulletin of China, 27(10):1739-1743 (in Chinese with English abstract).

Li, S.G., 1993.Ba-Nb-Th-La Diagrams Used to Identify Tectonic Environments of Ophiolite.Acta Petrologica Sinica, 9(2):146-157 (in Chinese with English abstract). http://www.ysxb.ac.cn/ysxb/ch/reader/view_abstract.aspx?pcid=3C5CA5E51F7D0F8A&jid=2013B5467E3054B1614CEC199353FCED&aid=77C0020DB5762141F511C9EAA2EFB584&yid=D418FDC97F7C2EBA&vid=9CF7A0430CBB2DFD&iid=0B39A22176CE99FB&eid=0B4F496D54044D86

Liu, C.Z., Wu, F.Y., Wilde, S.A., et al., 2010.Anorthitic Plagioclase and Pargasitic Amphibole in Mantle Peridotites from the Yungbwa Ophiolite (Southwestern Tibetan Plateau) Formed by Hydrous Melt Metasomatism.Lithos, 114(3-4):413-422. https://doi.org/10.1016/j.lithos.2009.10.008

Liu, F., Yang, J.S., Lian, D.Y., et al., 2015a.The Genesis and Tectonic Significance of Mafic Dikes in the Western Part of the Yarlung Zangbo Suture Zone, Tibet.Acta Geoscientica Sinica, 36(4):441-454 (in Chinese with English abstract).

Liu, F., Yang, J.S., Lian, D.Y., et al., 2015b.Genesis and Characteristics of the Western Part of the Yarlung Zangbo Ophiolites, Tibet.Acta Petrologica Sinica, 31(12):3609-3628 (in Chinese with English abstract).

Liu, Q., Deng, Y.B., Xiang, S.Y., et al., 2017.Early Ordovician Tectono-Thermal Event in Zhongba Terrane and Its Geological Significance.Earth Science, 42(6):881-890 (in Chinese with English abstract). doi: 10.1139/e11-076

Liu, Z., Li, Y., Xiong, F.H., et al., 2011.Petrology and Geochronology of MOR Gabbro in the Purang Ophiolite of Western Tibet, China.Acta Petrologica Sinica, 27(11):3269-3279 (in Chinese with English abstract).

Ludwing, K.R., 2003.Isoplot:A Geochronological Toolkit for Microsoft Excel.Berkeley Geochronology Center, Special Publication, Berkeley. https://searchworks.stanford.edu/view/6739593

Luhr, J.F., Haldar, D., 2006.Barren Island Volcano (NE Indian Ocean):Island-Arc High-Alumina Basalts Produced by Troctolite Contamination.Journal of Volcanology and Geothermal Research, 149(3-4):177-212. https://doi.org/10.1016/j.jvolgeores.2005.06.003

Meschede, M., 1986.A Method of Discriminating between Different Types of Mid-Ocean Ridge Basalts and Continental Tholeiites with the Nb-Zr-Y Diagram.Chemical Geology, 56(3-4):207-218. https://doi.org/10.1016/0009-2541(86)90004-5

Moores, E.M., Kellogg, L.H., Dilek, Y., 2000.Tethyan Ophiolites, Mantle Convection, and Tectonic "Historical Contingency":A Resolution of the "Ophiolite Conundrum".In:Dilek, Y., Moores, E.M., Elthon, D., et al., Ophiolites and Oceanic Crust:New Insights from Field Studies and the Ocean Drilling Program.Geological Society of America Special Paper, 349:3-12. https://pubs.geoscienceworld.org/books/book/501/chapter/3800505/Tethyan-ophiolites-mantle-convection-and-tectonic

Nicolas, A., Girardeau, J., Marcoux, J., et al., 1981.The Xigaze Ophiolite (Tibet):A Peculiar Oceanic Lithosphere.Nature, 294(5840):414-417. https://doi.org/10.1038/294414a0

Pan, G.T., Chen, Z.L., Li, X.Z., et al., 1997.Geological and Tectonic Evolution in the Eastern Tethys.Geological Publishing House, Beijing (in Chinese). doi: 10.1002/tect.20013

Pearce, J.A., 2008.Geochemical Fingerprinting of Oceanic Basalts with Applications to Ophiolite Classification and the Search for Archean Oceanic Crust.Lithos, 100(1-4):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. https://doi.org/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 doi: 10.1016/0012-821X(73)90129-5

Pearce, N.J.G., Perkins, W.T., Westgate, J.A., et al., 1997.A Compilation of New and Published Major and Trace Element Data for NIST SRM 610 and NIST SRM 612 Glass Reference Materials.Geostandards and Geoanalytical Research, 21(1):115-144.https://doi.org/10.1111/j.1751-908x.1997.tb00538.x doi: 10.1111/ggr.1997.21.issue-1

Qi, L., Grégoire, D.C., 2000.Determination of Trace Elements in Twenty Six Chinese Geochemistry Reference Materials by Inductively Coupled Plasma-Mass Spectrometry.Geostandards and Geoanalytical Research, 24(1):51-63.https://doi.org/10.1111/j.1751-908x.2000.tb00586.x doi: 10.1111/ggr.2000.24.issue-1

Reagan, M.K., Ishizuka, O., Stern, R.J., et al., 2010.Fore-Arc Basalts and Subduction Initiation in the Izu-Bonin-Mariana System.Geochemistry, Geophysics, Geosystems, 11(3):427-428.https://doi.org/10.1029/2009gc002871 doi: 10.1029/2009GC002871/references

Saccani, E., 2015.A New Method of Discriminating Different Types of Post-Archean Ophiolitic Basalts and Their Tectonic Significance Using Th-Nb and Ce-Dy-Yb Systematics.Geoscience Frontiers, 6(4):481-501. https://doi.org/10.1016/j.gsf.2014.03.006

Saccani, E., Principi, G., Garfagnoli, F., et al., 2008.Corsica Ophiolites:Geochemistry and Petrogenesis of Basaltic and Metabasaltic Rocks.Ofioliti, 33:187-207. https://www.researchgate.net/profile/Emilio_Saccani/publication/282643330_Corsica_ophiolites_Geochemistry_and_petrogenesis_of_basaltic_and_metabasaltic_rocks/links/5615194208aed47facefab85.pdf?origin=publication_detail

Schilling, J.G., Zajac, M., Evans, R., et al., 1983.Petrologic and Geochemical Variations along the Mid-Atlantic Ridge from 29 Degrees N to 73 Degrees N.American Journal of Science, 283(6):510-586. https://doi.org/10.2475/ajs.283.6.510

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

Simon, L.H., Nigel, M.K., 2007.Zircon:Tiny but Timely.Elements, 3(1):13-18. https://doi.org/10.2113/gselements.3.1.13

Singer, B.S., Jicha, B.R., Harper, M.A., et al., 2008.Eruptive History, Geochronology, and Magmatic Evolution of the Puyehue-Cordon Caulle Volcanic Complex, Chile.Geological Society of America Bulletin, 120(5-6):599-618.https://doi.org/10.1130/b26276.1 doi: 10.1130/B26276.1

Stern, R.J., Reagan, M., Ishizuka, O., et al., 2012.To Understand Subduction Initiation, Study Forearc Crust:To Understand Forearc Crust, Study Ophiolites.Lithosphere, 4(6):469-483.https://doi.org/10.1130/l183.1 doi: 10.1130/L183.1

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 doi: 10.1144/GSL.SP.1989.042.01.19

Tian, L.Y., Castillo, P.R., Hawkins, J.W., et al., 2008.Major and Trace Element and Sr-Nd Isotope Signatures of Lavas from the Central Lau Basin:Implications for the Nature and Influence of Subduction Components in the Back-Arc Mantle.Journal of Volcanology and Geothermal Research, 178(4):657-670. https://doi.org/10.1016/j.jvolgeores.2008.06.039

Wilkinson, J.F.G., 1982.The Genesis of Mid-Ocean Ridge Basalt.Earth-Science Reviews, 18(1):1-57. https://doi.org/10.1016/0012-8252(82)90002-2

Winchester, J.A., Floyd, P.A., 1976.Geochemical Magma Type Discrimination:Application to Altered and Metamorphosed Basic Igneous Rocks.Earth and Planetary Science Letters, 28(3):459-469.https://doi.org/10.1016/0012-821x(76)90207-7 doi: 10.1016/0012-821X(76)90207-7

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, F.Y., Liu, C.Z., Zhang, L.L., et al., 2014.Yarlung Zangbo Ophiolite:A Critical Updated View.Acta Petrologica Sinica, 30(2):293-325 (in Chinese with English abstract). http://en.cnki.com.cn/Article_en/CJFDTOTAL-YSXB201402001.htm

Xia, B., Li, J.F., Liu, L.W., et al., 2008.SHRIMP U-Pb Dating for Diabase in Sangsang Ophiolite, Xizang, China:Geochronological Constraint for Development of Eastern Tethys Basin.Geochimica, 37(4):399-403 (in Chinese with English abstract). http://en.cnki.com.cn/Article_en/CJFDTOTAL-DZLP200602012.htm

Xiong, Q., Griffin, W.L., Zheng, J.P., et al., 2016.Southward Trench Migration at 130-120 Ma Caused Accretion of the Neo-Tethyan Forearc Lithosphere in Tibetan Ophiolites.Earth and Planetary Science Letters, 438:57-65. https://doi.org/10.1016/j.epsl.2016.01.014

Xiong, F.H., Yang, J.S., Liang, F.H., et al., 2011.Zircon U-Pb Ages of the Dongbo Ophiolite in the Western Yarlung Zangbo Suture Zone and Their Geological Significance.Acta Petrologica Sinica, 27(11):3223-3238 (in Chinese with English abstract). http://en.cnki.com.cn/Article_en/CJFDTOTAL-YSXB201111006.htm

Xu, Z.Q., Yang, J.S., Hou, Z.Q., et al., 2016.The Progress in the Study of Continental Dynamics of the Tibetan Plateau.Geology in China, 43(1):1-42 (in Chinese with English abstract).

Yang, J.S., Dobrzhinetskaya, L., Bai, W.J., et al., 2007.Diamond-and Coesite-Bearing Chromitites from the Luobusa Ophiolite, Tibet.Geology, 35(10):875.https://doi.org/10.1130/g23766a.1 doi: 10.1130/G23766A.1

Yin, A., Harrison, T.M., 2000.Geologic Evolution of the Himalayan-Tibetan Orogen.Annual Review of Earth and Planetary Sciences, 28(1):211-280. https://doi.org/10.1146/annurev.earth.28.1.211

Yuan, H.L., Gao, S., Liu, X.M., et al., 2004.Accurate U-Pb Age and Trace Element Determinations of Zircon by Laser Ablation-Inductively Coupled Plasma-Mass Spectrometry.Geostandards and Geoanalytical Research, 28(3):353-370.https://doi.org/10.1111/j.1751-908x.2004.tb00755.x doi: 10.1111/ggr.2004.28.issue-3

Zhang, K.J., Xia, B., Zhang, Y.X., et al., 2014.Central Tibetan Meso-Tethyan Oceanic Plateau.Lithos, 210-211:278-288. https://doi.org/10.1016/j.lithos.2014.09.004

Zhang, K.J., Zhang, Y.X., Tang, X.C., et al., 2012.Late Mesozoic Tectonic Evolution and Growth of the Tibetan Plateau Prior to the Indo-Asian Collision.Earth-Science Reviews, 114(3-4):236-249. https://doi.org/10.1016/j.earscirev.2012.06.001

Zhang, Q., Zhou, G.Q., 2001.The Ophilite of China.Science Press, Beijing (in Chinese).

Zhang, Z., Song, J.L., Tang, J.X., et al., 2017.Petrogenesis, Diagenesis and Mineralization Ages of Galale Cu-Au Deposit, Tibet:Zircon U-Pb Age, Hf Isotopic Composition and Molybdenite Re-Os Dating.Earth Science, 42(6):862-880 (in Chinese with English abstract).

Zheng, H., Huang, Q.T., Kapsiotis, A., et al., 2017.Early Cretaceous Ophiolites of the Yarlung Zangbo Suture Zone:Insights from Dolerites and Peridotites from the Baer Upper Mantle Suite, SW Tibet (China).International Geology Review, 59(11):1471-1489. https://doi.org/10.1080/00206814.2016.1276867

黄圭成, 徐德明, 雷义均, 等, 2010.西藏西南部与蛇绿岩伴生的硅质岩特征及地质意义.中国地质, 37(1):101-109. http://kns.cnki.net/KCMS/detail/detail.aspx?filename=dizi201001014&dbname=CJFD&dbcode=CJFQ

冷秋锋, 唐菊兴, 郑文宝, 等, 2016.西藏拉抗俄斑岩Cu-Mo矿床含矿斑岩地球化学、锆石U-Pb年代学及Hf同位素组成.地球科学, 41(6):999-1015. http://www.earth-science.net/WebPage/Article.aspx?id=3312

李建峰, 夏斌, 刘立文, 等, 2008.西藏普兰地区拉昂错蛇绿岩中辉绿岩的锆石SHRIMP U-Pb年龄及其地质意义.地质通报, 27(10):1739-1743. doi: 10.3969/j.issn.1671-2552.2008.10.016

李曙光, 1993.蛇绿岩生成构造环境的Ba-Th-Nb-La判别图.岩石学报, 9(2):146-157. http://www.ysxb.ac.cn/ysxb/ch/reader/view_abstract.aspx?pcid=3C5CA5E51F7D0F8A&jid=2013B5467E3054B1614CEC199353FCED&aid=77C0020DB5762141F511C9EAA2EFB584&yid=D418FDC97F7C2EBA&vid=9CF7A0430CBB2DFD&iid=0B39A22176CE99FB&eid=0B4F496D54044D86

刘飞, 杨经绥, 连东洋, 等, 2015a.雅鲁藏布江缝合带西段北亚带的基性岩成因和构造意义.地球学报, 36(4):441-454. http://www.cqvip.com/QK/98325X/201504/665698151.html

刘飞, 杨经绥, 连东洋, 等, 2015b.西藏雅鲁藏布江缝合带西段南北亚带蛇绿岩的成因探讨.岩石学报, 31(12):3609-3628. http://kns.cnki.net/KCMS/detail/detail.aspx?filename=ysxb201512008&dbname=CJFD&dbcode=CJFQ

刘强, 邓玉彪, 向树元, 等, 2017.藏南仲巴地体早奥陶世构造-热事件及其地质意义.地球科学, 42(6):881-890. http://www.earth-science.net/WebPage/Article.aspx?id=3585

刘钊, 李源, 熊发挥, 等, 2011.西藏西部普兰蛇绿岩中的MOR型辉长岩:岩石学和年代学.岩石学报, 27(11):3269-3279. http://kns.cnki.net/KCMS/detail/detail.aspx?filename=ysxb201111009&dbname=CJFD&dbcode=CJFQ

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.

吴福元, 刘传周, 张亮亮, 等, 2014.雅鲁藏布蛇绿岩—事实与臆想.岩石学报, 30(2):293-325. http://www.ysxb.ac.cn/ysxb/ch/reader/create_pdf.aspx?file_no=20140201&journal_id=ysxb&year_id=2014

夏斌, 李建峰, 刘立文, 等, 2008.西藏桑桑蛇绿岩辉绿岩SHRIMP锆石U-Pb年龄:对特提斯洋盆发育的年代学制约.地球化学, 37(4):399-403. http://kns.cnki.net/KCMS/detail/detail.aspx?filename=dqhx200804012&dbname=CJFD&dbcode=CJFQ

熊发挥, 杨经绥, 梁凤华, 等, 2011.西藏雅鲁藏布江缝合带西段东波蛇绿岩中锆石U-Pb定年及地质意义.岩石学报, 27(11):3223-3238. http://kns.cnki.net/KCMS/detail/detail.aspx?filename=ysxb201111006&dbname=CJFD&dbcode=CJFQ

许志琴, 杨经绥, 侯增谦, 等, 2016.青藏高原大陆动力学研究若干进展.中国地质, 43(1):1-42. http://www.wanfangdata.com.cn/details/detail.do?_type=perio&id=zgdizhi201601001

张旗, 周国庆, 2001.中国蛇绿岩.北京:科学出版社.

张志, 宋俊龙, 唐菊兴, 等, 2017.西藏嘎拉勒铜金矿床的成岩成矿时代与岩石成因:锆石U-Pb年龄、Hf同位素组成及辉钼矿Re-Os定年.地球科学, 42(6):862-880. http://www.earth-science.net/WebPage/Article.aspx?id=3584

Relative Articles

Supplements(0)

Cited By

Proportional views