西藏定结高压基性麻粒岩(退变榴辉岩)的变质<i>P-T</i>轨迹及构造意义

丁自耕; 仝来喜; 刘小汉; 刘兆; 周学君

doi:10.3799/dqkx.2018.013

Volume 43 Issue 1

Jan. 2018

Turn off MathJax

Article Contents

Article Navigation > Earth Science > 2018 > 43(1): 220-235

Ding Zigeng, Tong Laixi, Liu Xiaohan, Liu Zhao, Zhou Xuejun, 2018. Metamorphic P-T Path of High-Pressure Mafic Granulite (Retrograded Eclogite) from Dinggye of Tibet and Its Tectonic Implication. Earth Science, 43(1): 220-235. doi: 10.3799/dqkx.2018.013

Citation:

Ding Zigeng, Tong Laixi, Liu Xiaohan, Liu Zhao, Zhou Xuejun, 2018. Metamorphic P-T Path of High-Pressure Mafic Granulite (Retrograded Eclogite) from Dinggye of Tibet and Its Tectonic Implication. Earth Science, 43(1): 220-235. doi: 10.3799/dqkx.2018.013

Citation:

PDF( 4151 KB)

Metamorphic P-T Path of High-Pressure Mafic Granulite (Retrograded Eclogite) from Dinggye of Tibet and Its Tectonic Implication

doi: 10.3799/dqkx.2018.013

Ding Zigeng^{1,2
,},
Tong Laixi^{1
,
,},
Liu Xiaohan³,
Liu Zhao^1,2,
Zhou Xuejun³

1.
State Key Laboratory of Isotope Geochemistry, Guangzhou Institute of Geochemistry, Chinese Academy of Sciences, Guangzhou 510640, China
2.
University of Chinese Academy of Sciences, Beijing 100049, China
3.
Institute of Tibetan Plateau Research, Chinese Academy of Sciences, Beijing 100085, China

Received Date: 2017-08-01
Publish Date: 2018-01-15

Abstract

Abstract

Dinggye is located in the central part of the Greater Himalayan crystalline complex (GHC) in southern Tibet. It is essential to investigate the metamorphic P-T path of granulite in this area to better understand the collision and uplifting process of the Tibetan plateau. The petrological study of the high-pressure mafic granulite (retrograded eclogite) from the region indicates four stages:(1) peak eclogite facies mineral assemblage (M₁) consists of garnet (core)+omphacite (psedomorph)+quartz+rutile; (2) high-pressure granulite facies mineral assemblage (M₂) comprises garnet (mantle)+clinopyroxene+plagioclase+ilmenite+amphibole+biotite; (3) medium-pressure granulite facies assemblage (M₃) is composed of garnet (rim)+orthopyroxene+plagioclase+biotite; (4) amphibolite facies mineral assemblage (M₄) consists of amphibole+plagioclase. Using the THERMOCALC program, the thermodynamic modeling in the NCFMASHTO system has been undertaken for the high-pressure mafic granulite. Combined with the conventional thermobarometers and the average P-T estimates, the P-T conditions of the different metamorphic stages are estimated to be 786-826℃, 0.78-0.96 GPa (M₂); 798-850℃, 0.71-0.75 GPa (M₃); and 610-666℃, 0.51-0.60 GPa (M₄), respectively, indicating a post-peak clockwise P-T path characterized by nearly isothermal decompression. Combined with geological data available, we propose that the high-pressure mafic granulite (retrograded eclogite) of the Dinggye formed during the Himalayan collisional orogeny, and underwent a post-peak tectonic uplift process of nearly isothermal decompression.
- high-pressure mafic granulite,
- P-T path,
- collisional orogenesis,
- Greater Himalaya,
- Dinggye,
- petrology

FullText(HTML)

References(86)

References

Anderson, J.L., Smith, D.R., 1995.The Effects of Temperature and F(O₂) on the Al-in-Hornblende Barometer.American Mineralogist, 80(5-6):549-559. https://doi.org/10.2138/am-1995-5-615

Bézos, A., Humler, E., 2005.The Fe³⁺/∑Fe Ratios of MORB Glasses and Their Implications for Mantle Melting.Geochimica et Cosmochimica Acta, 69(3):711-725. https://doi.org/10.1016/j.gca.2004.07.026

Bhadra, S., Bhattacharya, A., 2007.The Barometer Tremolite+Tschermakite+2 Albite=2 Pargasite+8 Quartz:Constraints from Experimental Data at Unit Silica Activity, with Application to Garnet-Free Natural Assemblages.American Mineralogist, 92(4):491-502. https://doi.org/10.2138/am.2007.2067

Bohlen, S.R., 1987.Pressure-Temperature-Time Paths and a Tectonic Model for the Evolution of Granulites.The Journal of Geology, 95(5):617-632. doi: 10.1086/629159

Chakungal, J., Dostal, J., Grujic, D., et al., 2010.Provenance of the Greater Himalayan Sequence:Evidence from Mafic Granulites and Amphibolites in NW Bhutan.Tectonophysics, 480(1-4):198-212. https://doi.org/10.1016/j.tecto.2009.10.014

Chen, X.Y., Tong, L.X., Zhang, C.L., et al., 2015.Retrograde Garnet Amphibolite from Eclogite of the Zhejiang Longyou Area:New Evidence of the Caledonian Orogenic Event in the Cathaysia Block.Chinese Science Bulletin, 60(13):1207-1217 (in Chinese with English abstract). doi: 10.1360/N972015-00094

Coleman, R.G., Lee, D.E., Beatty, L.B., et al., 1965.Eclogites and Eclogites:Their Differences and Similarities.Geological Society of America Bulletin, 76(5):483-508. https://doi.org/10.1130/0016-7606(1965)76[483:EAETDA]2.0.CO;2

Corrie, S.L., Kohn, M.J., Vervoort, J.D., 2010.Young Eclogite from the Greater Himalayan Sequence, Arun Valley, Eastern Nepal:P-T-t Path and Tectonic Implications.Earth & Planetary Science Letters, 289(3-4):406-416. https://doi.org/10.1016/j.epsl.2009.11.029

Cottrell, E., Kelley, K.A., 2011.The Oxidation State of Fe in MORB Glasses and the Oxygen Fugacity of the Upper Mantle.Earth and Planetary Science Letters, 305(3-4):270-282. https://doi.org/10.1016/j.epsl.2011.03.014

Daczko, N.R., Halpin, J.A., 2009.Evidence for Melt Migration Enhancing Recrystallization of Metastable Assemblages in Mafic Lower Crust, Fiordland, New Zealand.Journal of Metamorphic Geology, 27(2):167-185. https://doi.org/10.1111/j.1525-1314.2009.00811.x

Diener, J.F.A., Powell, R., White, R.W., et al., 2007.A New Thermodynamic Model for Clino-and Orthoamphiboles in the System Na₂O-CaO-FeO-MgO-Al₂O₃-SiO₂-H₂O-O.Journal of Metamorphic Geology, 25(6):631-656. https://doi.org/10.1111/j.1525-1314.2007.00720.x

Ding, L., Zhong, D.L., 1999.Metamorphic Characteristic and Geotectonic Implication of the High-Pressure Granulites from Namjagbarwa, Eastern Tibet.Science in China (Series D), 29(5):385-397 (in Chinese).

Eckert, J.O., Newton, R., Kleppa, O., 1991.The H of Reaction and Recalibration of Garnet-Pyroxene-Plagioclase-Quartz Geobarometers in the CMAS System by Solution Calorimetry.American Mineralogist, 76(1-2):148-160. https://pubs.geoscienceworld.org/ammin/article-lookup/76/1-2/148

England, P.C., Thompson, A.B., 1984.Pressure-Temperature-Time Paths of Regional Metamorphism I.Heat Transfer during the Evolution of Regions of Thickened Continental Crust.Journal of Petrology, 25(4):894-928. https://doi.org/10.1093/petrology/25.4.894

Green, E., Holland, T., Powell, R., 2007.An Order-Disorder Model for Omphacitic Pyroxenes in the System Jadeite-Diopside-Hedenbergite-Acmite, with Applications to Eclogitic Rocks.American Mineralogist, 92(7):1181-1189. https://doi.org/10.2138/am.2007.2401

Groppo, C., Lombardo, B., Rolfo, F., et al., 2007.Clockwise Exhumation Path of Granulitized Eclogites from the Ama Drime Range (Eastern Himalayas).Journal of Metamorphic Geology, 25(1):51-75. https://doi.org/10.1111/j.1525-1314.2006.00678.x

Grujic, D., Warren, C.J., Wooden, J.L., 2011.Rapid Synconvergent Exhumation of Miocene-Aged Lower Orogenic Crust in the Eastern Himalaya.Lithosphere, 3(5):346-366. https://doi.org/10.1130/L154.1

Guilmette, C., Indares, A., Hébert, R., 2011.High-Pressure Anatectic Paragneisses from the Namche Barwa, Eastern Himalayan Syntaxis:Textural Evidence for Partial Melting, Phase Equilibria Modeling and Tectonic Implications.Lithos, 124(1-2):66-81. https://doi.org/10.1016/j.lithos.2010.09.003

Harley, S.L., 1989.The Origins of Granulites:A Metamorphic Perspective.Geological Magazine, 126(3):215-247. https://doi.org/10.1017/s0016756800022330

Hodges, K.V., 2000.Tectonics of the Himalaya and Southern Tibet from Two Perspectives.Geological Society of America Bulletin, 112(3):324-350.https://doi.org/10.1130/0016-7606(2000)112<0324:TOTHAS>2.3.CO;2 doi: 10.1130/0016-7606(2000)112<0324:TOTHAS>2.3.CO;2

Holland, T., Blundy, J., 1994.Non-Ideal Interactions in Calcic Amphiboles and Their Bearing on Amphibole-Plagioclase Thermometry.Contributions to Mineralogy and Petrology, 116(4):433-447. https://doi.org/10.1007/BF00310910

Holland, T., Powell, R., 2003.Activity-Composition Relations for Phases in Petrological Calculations:An Asymmetric Multicomponent Formulation.Contributions to Mineralogy and Petrology, 145(4):492-501. https://doi.org/10.1007/s00410-003-0464-z

Holland, T.J.B., Powell, R., 1998.An Internally Consistent Thermodynamic Data Set for Phases of Petrological Interest.Journal of Metamorphic Geology, 16(3):309-343. https://doi.org/10.1111/j.1525-1314.1998.00140.x

Jessup, M.J., Cottle, J.M., 2010.Progression from South-Directed Extrusion to Orogen-Parallel Extension in the Southern Margin of the Tibetan Plateau, Mount Everest Region, Tibet.The Journal of Geology, 118(5):467-486. https://doi.org/10.1086/655011

Jessup, M.J., Newell, D.L., Cottle, J.M., et al., 2008.Orogen-Parallel Extension and Exhumation Enhanced by Denudation in the Trans-Himalayan Arun River Gorge, Ama Drime Massif, Tibet-Nepal.Geology, 36(7):587-590. https://doi.org/10.1130/G24722A.1

Ji, J.Q., Zhong, D.L., Song, B., et al., 2004.Metamorphism, Geochemistry and U-Pb Zircon SHRIMP Geochronology of the High-Pressure Granulites in the Central Greater Himalayas.Acta Petrologica Sinica, 20(5):1283-1300 (in Chinese with English abstract).

Kali, E., Leloup, P.H., Arnaud, N., et al., 2010.Exhumation History of the Deepest Central Himalayan Rocks, Ama Drime Range:Key Pressure-Temperature-Deformation-Time Constraints on Orogenic Models.Tectonics, 29(2):TC2014. https://doi.org/10.1029/2009TC002551

Kellet, D.A., Cottle, J.M., Smit, M., 2014.Eocene Deep Crust at Ama Drime, Tibet:Early Evolution of the Himalayan Orogen.Lithosphere, 6(4):220-229. https://doi.org/10.1130/L350.1

Kohn, M.J., 2014.Himalayan Metamorphism and Its Tectonic Implications.Annual Review of Earth and Planetary Sciences, 42(1):381-419. https://doi.org/10.1146/annurev-earth-060313-055005

Lal, R.K., 1993.Internally Consistent Recalibrations of Mineral Equilibria for Geothermobarometry Involving Gar-net-Orthopyroxene-Plagioclase-Quartz Assemblages and Their Application to the South Indian Granulites.Journal of Metamorphic Geology, 11(6):855-866. https://doi.org/10.1111/j.1525-1314.1993.tb00195.x

Langille, J.M., Jessup, M.J., Cottle, J.M., et al., 2010.Kinematic Evolution of the Ama Drime Detachment:Insights into Orogen-Parallel Extension and Exhumation of the Ama Drime Massif, Tibet-Nepal.Journal of Structural Geology, 32(7):900-919. https://doi.org/10.1016/j.jsg.2010.04.005

Le Fort, P., 1975.Himalayas:The Collided Range.Present Knowledge of the Continental Arc.American Journal of Science, 275:1-44. http://www.oalib.com/references/7070282

Leake, B.E., Woolley, A.R., Brich, W.D., et al., 2004.Nomenclature of Amphiboles:Additions and Revisions to the International Mineralogical Association's Amphibole Nomenclature.Mineralogical Magazine, 68(1):209-215. https://doi.org/10.1180/0026461046810182

Leloup, P.H., Mahéo, G., Arnaud, N., et al., 2010.The South Tibet Detachment Shear Zone in the Dinggye Area:Time Constraints on Extrusion Models of the Himalayas.Earth and Planetary Science Letters, 292(1-2):1-16. https://doi.org/10.1016/j.epsl.2009.12.035

Li, D.W., Liao, Q.A., Yuan, Y.M., et al., 2002.Discovery and Significance of Basic Granulites in the Complexes in the Middle Himalaya.Earth Science, 27(1):80, 96 (in Chinese). doi: 10.1007/s11430-011-4250-x

Li, D.W., Liao, Q.A., Yuan, Y.M., et al., 2003.U-Pb Zircon Ages of Rimana Granulites in the Middle Himalaya.Chinese Science Bulletin, 48(20):2176-2179 (in Chinese). doi: 10.1007/BF03182846

Liao, Q.A., Li, D.W., Yi, S.H., et al., 2003.Petrologic and Geologic Significance of Garnet Pyroxenite and Mafic Granulites from High Himalayan Region, Tibet.Earth Science, 28(6):627-633 (in Chinese with English abstract).

Liu, D.M., Li, D.W., Yang, W.R., 2003.Study of Mylonite and Deformation of Ductile Shear Zone, Dingjie Area.Earth Science Frontiers, 10(2):479-486 (in Chinese with English abstract). https://www.sciencedirect.com/science/article/pii/0191814180900486

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). https://doi.org/10.3799/dqkx.2017.076

Liu, S.W., Zhang, J.J., Shu, G.M., et al., 2005.Mineral Chemistry, P-T-t Paths and Exhumation Processes of Mafic Granulites in Dinggye, Southern Tibet.Science in China (Series D), 35(9):810-820 (in Chinese).

Liu, X.H., Ju, Y.T., Wei, L.J., et al., 2009.An Alternative Tectonic Model for the Yarlung Zangbo Suture Zone.Science in China (Series D), 39(4):448-463 (in Chinese). doi: 10.1007/s11430-009-0177-x

Liu, Y., Zhong, D.L., 1998.Petrology of High-Pressure Granulites from Eastern Himalaya:Implications to Tectonic Significance.Scientia Geologica Sinica, 33(3):267-281 (in Chinese with English abstract). https://www.researchgate.net/publication/230028123_Petrology_of_high-pressure_granulites_from_the_eastern_Himalayan_syntaxis

Lombardo, B., Rolfo, F., 2000.Two Contrasting Eclogite Types in the Himalayas:Implications for the Himalayan Orogeny.Journal of Geodynamics, 30(1-2):37-60. https://doi.org/10.1016/S0264-3707(99)00026-5

Lombardo, B., Rolfo.F., Compagnoni, R., 2000.Glaucophane and Barroisite Eclogites from the Upper KaghanNappe:Implications for the Metamorphic History of the NW Himalaya.Geological Society, London, Special Publications, 170(1):411-430. https://doi.org/10.1144/GSL.SP.2000.170.01.22

Mottram, C.M., Parrish, R.R., Regis, D., et al., 2015.Using U-Th-Pb Petrochronology to Determine Rates of Ductile Thrusting:Time Windows into the Main Central Thrust, Sikkim Himalaya.Tectonics, 34(7):1355-1374. https://doi.org/10.1002/2014TC003743

Mukherjee, B., Sachan, H.K., Ahmad, T., 2005.A New Occurrence of Microdiamond from Indus Suture Zone, Himalata:A Possible Origin.In:Memoire, H.S., ed., Special Extended Abstract Volume.Géologie Alpine, 44:136. https://www.researchgate.net/publication/278300924_New_occurrence_of_microdiamond_from_indus_suture_Zone_Himalaya_possible_origin_Geologie_alpine_abs_2005_No_44p_35

Möller, C., 1998.Decompressed Eclogites in the Sveconorwegian (-Grenvillian) Orogen of SW Sweden:Petrology and Tectonic Implications.Journal of Metamorphic Geology, 16(5):641-656. https://doi.org/10.1111/j.1525-1314.1998.00160.x

O'Brien, P.J., Zotov, N., Law, R., et al., 2001.Coesite in Himalayan Eclogite and Implications for Models of India-Asia Collision.Geology, 29(5):435-438.https://doi.org/10.1130/0091-7613(2001)029<0435:CIHEAI>2.0.CO;2 doi: 10.1130/0091-7613(2001)029<0435:CIHEAI>2.0.CO;2

Pan, Y., Kidd, W.S.F., 1992.Nyainqentanglha Shear Zone:A Late Miocene Extensional Detachment in the Southern Tibetan Plateau.Geology, 20(9):775-778.https://doi.org/10.1130/0091-7613(1992)020<0775:NSZALM>2.3.CO;2 doi: 10.1130/0091-7613(1992)020<0775:NSZALM>2.3.CO;2

Pitra, P., Ballèvre, M., Ruffet, G., 2010.Inverted Metamorphic Field Gradient towards a Variscan Suture Zone (Champtoceaux Complex, Armorican Massif, France).Journal of Metamorphic Geology, 28(2):183-208. https://doi.org/10.1111/j.1525-1314.2009.00862.x

Powell, R., Holland, T., Worley, B., 1998.Calculating Phase Diagrams Involving Solid Solutions via Non-Linear Equations, with Examples Using THERMOCALC.Journal of Metamorphic Geology, 16(4):577-588. https://doi.org/10.1111/j.1525-1314.1998.00157.x

Ravna, K., 2000.The Garnet-Clinopyroxene Fe²⁺-Mg Geothermometer:An Updated Calibration.Journal of Metamorphic Geology, 18(2):211-219. https://doi.org/10.1046/j.1525-1314.2000.00247.x

Rolfo, F., McClelland, W., Lombardo, B., 2005.Geochronological Constraints on the Age of the Eclogite-Facies Metamorphism in the Eastern Himalaya.In:Memoire, H.S., ed., Special Extended Abstract Volume.Géologie Alpine, 44:170.

Wang, Y.H., Zhang, L.F., Zhang, J.J., et al., 2017.The Youngest Eclogite in Central Himalaya:P-T Path, U-Pb Zircon Age and Its Tectonic Implication.Gondwana Research, 41:188-206. https://doi.org/10.1016/j.gr.2015.10.013

Wei, C.J., 2011.Approaches and Advancement of the Study of Metamorphic P-T-t Paths.Earth Science Frontiers, 18(2):1-16 (in Chinese with English abstract). https://www.sciencedirect.com/science/article/pii/S0037073804002362

White, R.W., Powell, R., Clarke, G.L., 2002.The Interpretation of Reaction Textures in Fe-Rich Metapelitic Granulites of the Musgrave Block, Central Australia:Constraints from Mineral Equilibria Calculations in the System K₂O-FeO-MgO-Al₂O₃-SiO₂-H₂O-TiO₂-Fe₂O₃.Journal of Metamorphic Geology, 20(1):41-55. https://doi.org/10.1046/j.0263-4929.2001.00349.x

White, R.W., Powell, R., Holland, T.J.B., 2007.Progress Relating to Calculation of Partial Melting Equilibria for Metapelites.Journal of Metamorphic Geology, 25(5):511-527. https://doi.org/10.1111/j.1525-1314.2007.00711.x

White, R.W., Powell, R., Holland, T.J.B., et al., 2000.The Effect of TiO₂ and Fe₂O₃ on Metapelitic Assemblages at Greenschist and Amphibolite Facies Conditions:Mineral Equilibria Calculations in the System K₂O-FeO-MgO-Al₂O₃-SiO₂-H₂O-TiO₂-Fe₂O₃.Journal of Metamorphic Geology, 18(5):497-511. doi: 10.1046/j.1525-1314.2000.00269.x

Xiao, W.J., Ao, S.J., Yang, L., et al., 2017.Anatomy of Composition and Nature of Plate Convergence:Insights for Alternative Thoughts for Terminal India-Eurasia Collision.Science in China (Series D), 47(6):631-656 (in Chinese). doi: 10.1007/s11430-016-9043-3

Xu, Z.Q., Wang, Q., Pêcher, A., et al., 2013.Orogen-Parallel Ductile Extension and Extrusion of the Greater Himalaya in the Late Oligocene and Miocene.Tectonics, 32(2):191-215. https://doi.org/10.1002/tect.20021

Yin, A., 2006.Cenozoic Tectonic Evolution of the Himalayan Orogen as Constrained by along-Strike Variation of Structural Geometry, Exhumation History, and Foreland Sedimentation.Earth-Science Reviews, 76(1):1-131. https://doi.org/10.1016/j.earscirev.2006.08.005

Yu, J.J., Zeng, L.S., Liu, J., et al., 2011.Early Miocene Leucogranites in Dinggye Area, Southern Tibet:Formation Mechanism and Tectonic Implications.Acta Petrologica Sinica, 27(7):1961-1972 (in Chinese with English abstract). http://www.irgrid.ac.cn/password-login;jsessionid=E73DBB84A6B710BEEF8327921CA5133E

Zhang, J.J., Guo, L., Ding, L., 2002.Structural Characteristics of Middle and Southern Xainza-Dinggye Normal Fault System and Its Relationship to Southern Tibetan Detachment System.Chinese Science Bulletin, 47(10):738-743 (in Chinese).

Zhang, Z.M., Dong, X., He, Z.Y., et al., 2013.Indian and Asian Continental Collision Viewed from HP and UHP Metamorphism of the Himalaya Orogen.Acta Petrologica Sinica, 29(5):1713-1726 (in Chinese with English abstract). http://www.ysxb.ac.cn/ysxb/ch/reader/view_abstract.aspx?file_no=20130518

Zhang, Z.M., Zhao, G., Santosh, M., et al., 2010.Two Stages of Granulite Facies Metamorphism in the Eastern Himalayan Syntaxis, South Tibet:Petrology, Zircon Geochronology and Implications for the Subduction of Neo-Tethys and the Indian Continent beneath Asia.Journal of Metamorphic Geology, 28(7):719-733. https://doi.org/10.1111/j.1525-1314.2010.00885.x

Zhang, Z.M., Zheng, L.L., Wang, J.L., et al., 2007.Garnet Pyroxenite in the Namjagbarwa Group-Complex in the Eastern Himalayan Tectonic Syntaxis, Tibet, China:Evidence for Subduction of the Indian Continent beneath the Eurasian Plate at 80-100km Depth.Geological Bulletin of China, 26(1):1-12 (in Chinese with English abstract).

Zhao, G., Cawood, P.A., Wilde, S.A., et al., 2001.High-Pressure Granulites (Retrograded Eclogites) from the Hengshan Complex, North China Craton:Petrology and Tectonic Implications.Journal of Petrology, 42(6):1141-1170. https://doi.org/10.1093/petrology/42.6.1141

Zhou, X., Tong, L.X., Liu, X.H., et al., 2014.Metamorphism Evolution of Mafic Granulite from the Larsemann Hills, East Antarctica.Acta Petrologica Sinica, 30(6):1731-1747 (in Chinese with English abstract). https://www.researchgate.net/publication/266383599_Metamorphism_evolution_of_mafic_granulite_from_the_Larsemann_Hills_East_Antarctica

陈相艳, 仝来喜, 张传林, 等, 2015.浙江龙游石榴石角闪岩(退变榴辉岩):华夏加里东期碰撞造山事件的新证据.科学通报, 60(13):1207-1217. http://www.oalib.com/paper/4267633

丁林, 钟大赉, 1999.西藏南迦巴瓦峰地区高压麻粒岩相变质作用特征及其构造地质意义.中国科学(D辑), 29(5):385-397. http://d.old.wanfangdata.com.cn/Periodical/zgkx-cd199905001

季建清, 钟大赉, 宋彪, 等, 2004.喜马拉雅中段高压麻粒岩变质作用、地球化学与年代学.岩石学报, 20(5):1283-1300. https://www.researchgate.net/profile/Li_Wangchao/publication/277559493_Metamorphism_and_anatexis_of_the_Himalayan_orogen_Petrology_and_geochronology_of_HP_pelitic_granulites_from_the_Yadong_area_Southern_Tibet/links/556d358d08aefcb861d7ec4c.pdf?inViewer=0&pdfJsDownload=0&origin=publication_detail

李德威, 廖群安, 袁晏明, 等, 2002.喜马拉雅造山带中段核部杂岩中基性麻粒岩的发现及构造意义.地球科学, 27(1):80, 96. http://earth-science.net/WebPage/Article.aspx?id=1077

李德威, 廖群安, 袁晏明, 等, 2003.喜马拉雅造山带中段日玛那麻粒岩锆石U-Pb年代学.科学通报, 48(20):2176-2179. doi: 10.3321/j.issn:0023-074X.2003.20.015

廖群安, 李德威, 易顺华, 等, 2003.西藏定结高喜马拉雅石榴辉石岩-镁铁质麻粒岩的岩石特征及其地质意义.地球科学, 28(6):627-633. http://earth-science.net/WebPage/Article.aspx?id=1303

刘德民, 李德威, 杨巍然, 2003.定结地区韧性剪切带变形特征与糜棱岩研究.地学前缘, 10(2):479-486. http://www.docin.com/p-24115591.html

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://earth-science.net/WebPage/Article.aspx?id=3585

刘树文, 张进江, 舒桂明, 等, 2005.藏南定结铁镁质麻粒岩矿物化学、PTt轨迹和折返过程.中国科学(D辑), 35(9):810-820. http://www.wanfangdata.com.cn/details/detail.do?_type=perio&id=zgkx-cd200509002

刘小汉, 琚宜太, 韦利杰, 等, 2009.再论雅鲁藏布江缝合带构造模型.中国科学(D辑), 39(4):448-463. http://kns.cnki.net/KCMS/detail/detail.aspx?filename=jdxk200904008&dbname=CJFD&dbcode=CJFQ

刘焰, 钟大赉, 1998.东喜马拉雅地区高压麻粒岩石学研究及构造意义.地质科学, 33(3):267-281. http://www.wanfangdata.com.cn/details/detail.do?_type=perio&id=zgkx-cd200509002

魏春景, 2011.变质作用P-T-t轨迹的研究方法与进展.地学前缘, 18(2):1-16. doi: 10.1360/N072016-00244

肖文交, 敖松坚, 杨磊, 等, 2017.喜马拉雅汇聚带结构-属性解剖及印度-欧亚大陆最终拼贴格局.中国科学(D辑), 47(6):631-656. http://mall.cnki.net/magazine/Article/JDXK201706001.htm

于俊杰, 曾令森, 刘静, 等, 2011.藏南定结地区早中新世淡色花岗岩的形成机制及其构造动力学意义.岩石学报, 27(7):1961-1972. http://www.ysxb.ac.cn/ysxb/ch/reader/view_abstract.aspx?file_no=20110705&journal_id=ysxb

张进江, 郭磊, 丁林, 2002.申扎-定结正断层体系中, 南段构造特征及其与藏南拆离系的关系.科学通报, 47(10):738-743. doi: 10.3321/j.issn:0023-074X.2002.10.003

张泽明, 董昕, 贺振宇, 等, 2013.喜马拉雅造山带的高压超高压变质作用与印度-亚洲大陆碰撞.岩石学报, 29(5):1713-1726. http://www.ysxb.ac.cn/ysxb/ch/reader/view_abstract.aspx?file_no=20130518

张泽明, 郑来林, 王金丽, 等, 2007.东喜马拉雅构造结南迦巴瓦岩群中的石榴辉石岩-印度大陆向欧亚板块之下俯冲至80~100km深度的证据.地质通报, 26(1):1-12. doi: 10.3969/j.issn.1671-2552.2007.01.002

周信, 仝来喜, 刘小汉, 等, 2014.东南极拉斯曼丘陵镁铁质麻粒岩的变质作用演化.岩石学报, 30(6):1731-1747. http://www.ysxb.ac.cn/ysxb/ch/reader/view_abstract.aspx?file_no=20140615

Relative Articles

Supplements(0)

Cited By

Proportional views

Proportional views

通讯作者: 陈斌, bchen63@163.com

1.
沈阳化工大学材料科学与工程学院沈阳 110142

Figures(7) / Tables(3)

Get Citation

PDF

XML

Article views (4856) PDF downloads(47)

Metamorphic P-T Path of High-Pressure Mafic Granulite (Retrograded Eclogite) from Dinggye of Tibet and Its Tectonic Implication

doi: 10.3799/dqkx.2018.013

Abstract

References

Proportional views

Catalog

通讯作者: 陈斌, bchen63@163.com

Proportional views

Export File

Citation

Format

Content