西藏甲鲁朗地区叶巴组火山岩成因及其对新特提斯洋俯冲的约束
|
摘要
西藏冈底斯岩浆弧叶巴组火山岩对于新特提斯洋俯冲时限的制约存在着重要的意义.通过对甲鲁朗地区叶巴组凝灰岩的LA-ICP-MS锆石U-Pb年龄和岩石地球化学组成的研究,锆石测年获得3件凝灰岩样品~(206)Pb/~(238)U年龄加权平均值分别为207.8±1.6 Ma、204.8±1.7 Ma和209.3±3.4 Ma,结合古生物化石证据,表明其形成于晚三叠世;凝灰岩样品富集轻稀土元素和大离子亲石元素(Rb、K、Th、U、Pb),亏损重稀土元素和高场强元素(Nb、Ta、Ti、P),同时亏损Sr元素,Eu负异常较明显.岩石地球化学特征表明叶巴组中酸性岩可能为壳幔混染成因.综合前人研究成果,认为叶巴组形成于新特提斯洋俯冲环境下的大陆边缘弧,新特提斯洋的俯冲从晚三叠世就已经开始.本研究为叶巴组的形成时代以及动力学背景提供了新的制约.
The volcanic rocks of the Yeba Formation on the Gangdese magmatic arc,Tibet are of importance for limiting the initiation of the Neo-Tethyan oceanic slab subduction.This paper reports LA-ICP-MS zircon U-Pb ages and whole-rock geochemistry compositions of the tuffs from the Yeba Formation in Jialulang area.LA-ICP-MS U-Pb isotopic dating of the tuffs obtained~(206)Pb/~(238)U age weighted average values are 207.8±1.6 Ma,204.8±1.7 Ma and 209.3±3.4 Ma,based on this analysis above and the evidence of fossil organism as well,the tuffs of the Yeba Formation were formed in the Late Triassic.The tuffs exhibit LREE and LILE(Rb,K,Th,U,Pb)enrichment and HREE and HFSE(Nb,Ta,Ti,P)depletion,depletion of Sr as well,with negative Eu anomaly.Combining with geochemical characteristics,it has been suggested a mixing source from crust and depleted mantle for the intermediate-acid rocks from the Yeba Formation.Based on the previous studies,it is indicated that the volcanic rocks of the Yeba Formation were formed in the active continental margin arc setting with the subduction of the NeoTethyan oceanic slab,the initiation of the subduction occurred at Late Triassic.This study provides new constraints for the ages and dynamic settings of the Yeba Formation.
The volcanic rocks of the Yeba Formation on the Gangdese magmatic arc,Tibet are of importance for limiting the initiation of the Neo-Tethyan oceanic slab subduction.This paper reports LA-ICP-MS zircon U-Pb ages and whole-rock geochemistry compositions of the tuffs from the Yeba Formation in Jialulang area.LA-ICP-MS U-Pb isotopic dating of the tuffs obtained~(206)Pb/~(238)U age weighted average values are 207.8±1.6 Ma,204.8±1.7 Ma and 209.3±3.4 Ma,based on this analysis above and the evidence of fossil organism as well,the tuffs of the Yeba Formation were formed in the Late Triassic.The tuffs exhibit LREE and LILE(Rb,K,Th,U,Pb)enrichment and HREE and HFSE(Nb,Ta,Ti,P)depletion,depletion of Sr as well,with negative Eu anomaly.Combining with geochemical characteristics,it has been suggested a mixing source from crust and depleted mantle for the intermediate-acid rocks from the Yeba Formation.Based on the previous studies,it is indicated that the volcanic rocks of the Yeba Formation were formed in the active continental margin arc setting with the subduction of the NeoTethyan oceanic slab,the initiation of the subduction occurred at Late Triassic.This study provides new constraints for the ages and dynamic settings of the Yeba Formation.
引文
Andersen,T.,2002.Correction of Common Lead in U-Pb Analyses that do not Report204Pb.Chemical Geology,192(1-2):59-79.https://doi.org/10.1016/s0009-2541(02)00195-x
Atherton,M.P.,Petford,N.,1993.Generation ofSodium-Rich Magmas from Newly Underplated Basaltic Crust.Nature,362(6416):144-146.https://doi.org/10.1038/362144a0
Bacon,C.R.,Druitt,T.H.,1988.Compositional Evolution of the Zoned Cal-Calkaline Magma Chamber of Mount Mazama,Crater Lake,Oregon.Contributions to Mineralogy and Petrology,98(2):224-256.https://doi.org/10.1007/bf00402114
Chen,W.,Ma,C.Q.,Bian,Q.J.,et al.,2009.Evidences from Geochemistry and Zircon U-Pb Geochronology of Volcanic Rocks of Yeba Formation in Demingding Area,the East of Middle Gangdise,Tibet.Geological Science and Technology Information,28(3):31-40(in Chinese with English abstract).
Chu,M.F.,Chung,S.L.,Song,B.,et al.,2006.Zircon U-Pb and Hf Isotope Constraints on the Mesozoic Tectonics and Crustal Evolution of Southern Tibet.Geology,34(9):745.https://doi.org/10.1130/g22725.1
Condie,K.C.,Bowling,G.P.,Allen,P.,1986.Origin of Granites in an Archean High-Grade Terrane,Southern India.Contributions to Mineralogy and Petrology,92(1):93-103.https://doi.org/10.1007/bf00373967
Dong,X.,Zhang,Z.M.,2013.Genesis and Tectonic Significance of the Early Jurassic Magmatic Rocks from the Southern Lhasa Terrane.Acta Petrologica Sinica,29(6):1933-1948(in Chinese with Englishabstract).
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).
Fitton,J.G.,James,D.,Kempton,P.D.,et al.,1988.The Role of Lithospheric Mantle in the Generation of Late Cenozoic Basic Magmas in the Western United States.Journal of Petrology,Special_Volume,(1):331-349.https://doi.org/10.1093/petrology/special_volume.1.331
Geng,Q.R.,Pan,G.T.,Jin,Z.M.,et al.,2005.Geochemistry and Genesis of the Yeba Volcanic Rocks in the Gangdise Magmatic Arc,Tibet.Earth Science,30(6):747-760(in Chinese with English abstract).
Geng,Q.R.,Pan,G.T.,Wang,L.Q.,et al.,2006.Isotopic Geochronology of the Volcanic Rocks from the Yeba Formation in the Gangdise Zone,Xizang.Sedimentary Geology and Tethyan Geology,26(1):1-7(in Chinese with English abstract).
Gorton,M.P.,Schandl,E.S.,2000.From Continents to Island Arcs:A Geochemical Index of Tectonic Setting for Arc-Related and Within-Plate Felsic to Intermediate Volcanic Rocks.The Canadian Mineralogist,38(5):1065-1073.https://doi.org/10.2113/gscanmin.38.5.1065
Gou,J.,1994.A New Knowledge on the Attributes of Yeba Formation in Lhasa Area.Tibetan Geology,(11):1-6(in Chinese with English abstract).
Guo,L.,Zhang,H.F.,Harris,N.,et al.,2013.Late Cretaceous(~81 Ma)High-Temperature Metamorphism in the Southeastern Lhasa Terrane:Implication for the NeoTethys Ocean Ridge Subduction.Tectonophysics,608:112-126.https://doi.org/10.1016/j.tecto.2013.10.007
Gutscher,M.A.,Maury,R.,Eissen,J.P.,et al.,2000.Can Slab Melting be Caused by Flat Subduction?.Geology,28(6):535-538.https://doi.org/10.1130/0091-7613(2000)28<535:csmbcb>2.0.co;2
He,Z.H.,Yang,D.M.,Zheng,C.Q.,et al.,2006.Isotopic Dating of the Mamba Granitoid in the Gangdise Tectonic Belt and Its Constraint on the Subduction Time of the Neotethys.Geological Review,52(1):100-106(in Chinese with English abstract).
Hu,P.Y.,Zhai,Q.G.,Wang,J.,et al.,2018.Precambrian Origin of the North Lhasa Terrane,Tibetan Plateau:Constraint from Early Cryogenian Back-Arc Magmatism.Precambrian Research,313:51-67.https://doi.org/10.1016/j.precamres.2018.05.014
Huang,F.,Xu,J.F.,Chen,J.L.,et al.,2015.Early Jurassic Volcanic Rocks from the Yeba Formation and Sangri Group:Products of Continental Marginal Arc and IntraOceanic Arc during the Subduction of Neo-Tethys Ocean?.Acta Petrologica Sinica,31(7):2089-2098(in Chinese with English abstract).
Kelemen,P.B.,Hangh?j,K.,Greene,A.R.,2007.One View of the Geochemistry of Subduction-Related Magmatic Arcs,with an Emphasis on Primitive Andesite and Lower Crust.Treatise on Geochemistry,3:593-660.https://doi.org/10.1016/B0-08-043751-6/03035-8
Leat,P.T.,Thompson,R.N.,Morrison,M.A.,et al.,1988.Compositionally-Diverse Miocene-Recent RiftRelated Magmatism in Northwest Colorado:Partial Melting,and Mixing of Mafic Magmas from 3 Different Asthenospheric and Lithospheric Mantle Sources.Journal of Petrology,Special Volume(1):351-377.https://doi.org/10.1093/petrology/special_volume.1.351
Li,H.Q.,Xu,Z.Q.,Yang,J.S.,et al.,2011.Syn-Collisional Exhumation of Sumdo Eclogite in the Lhasa Terrane,Tibet:Evidences from Structural Deformation and40Ar-39Ar Geochronology.Earth Science Frontiers,18(3):66-78(in Chinese with English abstract).
Liu,Z.C.,Ding,L.,Zhang,L.Y.,et al.,2018.Sequence and Petrogenesis of the Jurassic Volcanic Rocks(Yeba Formation)in the Gangdese Arc,Southern Tibet:Implications for the Neo-Tethyan Subduction.Lithos,312-313:72-88.https://doi.org/10.1016/j.lithos.2018.04.026
Ma,X.X.,Xu,Z.Q.,Chen,X.J.,et al.,2017.The Origin and Tectonic Significance of the Volcanic Rocks of the Yeba Formation in the Gangdese Magmatic Belt,South Tibet.Journal of Earth Science,28(2):265-282.https://doi.org/10.1007/s12583-016-0925-8
Maniar,P.D.,Piccoli,P.M.,1989.Tectonic Discrimination of Granitoids.Geological Society of America Bulletin,101(5):635-643.https://doi.org/10.1130/0016-7606(1989)101<0635:tdog>2.3.co;2
McCarron,J.J.,Smellie,J.L.,1998.Tectonic Implications of Fore-Arc Magmatism and Generation of High-Magnesian Andesites:Alexander Island,Antarctica.Journal of the Geological Society,155(2):269-280.https://doi.org/10.1144/gsjgs.155.2.0269
Miyashiro,A.,1974.Volcanic Rock Series in Island Arcs and Active Continental Margins.American Journal of Science,274(4):321-355.https://doi.org/10.2475/ajs.274.4.321
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 Universities,11(3):281-290(in Chinese with English abstract).
Mo,X.X.,Niu,Y.L.,Dong,G.C.,et al.,2008.Contribution of Syncollisional Felsic Magmatism to Continental Crust Growth:A Case Study of the Paleogene Linzizong Volcanic Succession in Southern Tibet.Chemical Geology,250(1-4):49-67.https://doi.org/10.1016/j.chemgeo.2008.02.003
Murphy,M.A.,Yin,A.,Harrison,T.M.,et al.,1997.Did the Indo-Asian Collision Alone Create the Tibetan Plateau?.Geology,25(8):719.https://doi.org/10.1130/0091-7613(1997)025<0719:dtiaca>2.3.co;2
Müller,D.,Rock,N.M.S.,Groves,D.I.,1992.Geochemical Discrimination between Shoshonitic and Potassic Volcanic Rocks in Different Tectonic Settings:A Pilot Study.Mineralogy and Petrology,46(4):259-289.https://doi.org/10.1007/bf01173568
Pan,F.B.,Zhang,H.F.,Xu,W.C.,et al.,2016.U-Pb Zircon Dating,Geochemical and Sr-Nd-Hf Isotopic Compositions of Mafic Intrusive Rocks in the Motuo,SE Tibet Constrain on Their Petrogenesis and Tectonic Implication.Lithos,245:133-146.https://doi.org/10.1016/j.lithos.2015.05.011
Pan,G.T.,Mo,X.X.,Hou,Z.Q.,et al.,2006.SpatialTemporal Framework of the Gangdese Orogenic Belt and Its Evolution.Acta Petrologica Sinica,22(3):521-533(in Chinese with English abstract).
Pati?o Douce,A.E.,Johnston,A.D.,1991.Phase Equilibria and Melt Productivity in the Pelitic System:Implications for the Origin of Peraluminous Granitoids and Aluminous Granulites.Contributions to Mineralogy and Petrology,107(2):202-218.https://doi.org/10.1007/bf00310707
Pearce,J.A.,1982.Trace Element Characteristics of Lavas from Destructive Plate Boundaries.Andesites:Orogenic Andesites and Related Rocks.John Wiley and Sons,New York,525-548.
Pearce,J.A.,Harris,N.B.W.,Tindle,A.G.,1984.Trace Element Discrimination Diagrams for the Tectonic Interpretation of Granitic Rocks.Journal of Petrology,25(4):956-983.https://doi.org/10.1093/petrology/25.4.956
Pearce,J.A.,Mei,H.J.,1988.Volcanic Rocks of the 1985Tibet Geotraverse:Lhasa to Golmud.Philosophical Transactions of the Royal Society A:Mathmatical,Physical and Engineering Science,327(1594):169-201.https://doi.org/10.1098/rsta.1988.0125
Pei,S.W.,1999.Early and Middle Jurassic Bivalve Fauna in Volcanic Rocks of Tibetan Lhasa Block and Its Paleobiogeography.Geoscience,13(3):291-297(in Chinese with English abstract).
Plank,T.,2005.Constraints from Thorium/Lanthanum on Sediment Recycling at Subduction Zones and the Evolution of the Continents.Journal of Petrology,46(5):921-944.https://doi.org/10.1093/petrology/egi005
Qiu,J.S.,Wang,R.Q.,Zhao,J.L,et al.,2015.Petrogenesis of the Early Jurassic Gabbro-Granite Complex in the Middle Segment of the Gangdese Belt and Its Implications for Tectonic Evolution of Neo-Tethys:A Case Study of the Dongga Pluton in Xi’gaze.Acta Petrologica Sinica,31(12):3569-3580(in Chinese with English abstract).
Rudnick,R.L.,Gao,S.,2003.Composition of the Contiental Crust.Treatise on Geochemistry,3:1-64
Salters,V.J.M.,Stracke,A.,2004.Composition of the Depleted Mantle.Geochemistry,Geophysics,Geosystems,5(5):1-27.https://doi.org/10.1029/2003gc000597
Schiano,P.,Monzier,M.,Eissen,J.P.,et al.,2010.Simple Mixing as the Major Control of the Evolution of Volcanic Suites in the Ecuadorian Andes.Contributions to Mineralogy and Petrology,160(2):297-312.https://doi.org/10.1007/s00410-009-0478-2
Shinjo,R.,Kato,Y.,2000.Geochemical Constraints on the Origin of Bimodal Magmatism at the Okinawa Trough,an Incipient Back-Arc Basin.Lithos,54(3-4):117-137.https://doi.org/10.1016/s0024-4937(00)00034-7
Sisson,T.W.,1994.Hornblende-Melt Trace-Element Partitioning Measured by Ion Microprobe.Chemical Geology,117(1-4):331-344.https://doi.org/10.1016/0009-2541(94)90135-x
Song,S.G.,Niu,Y.L.,Wei,C.J.,et al.,2010.Metamorphism,Anatexis,Zircon Ages and Tectonic Evolution of the Gongshan Block in the Northern Indochina Continent-An Eastern Extension of the Lhasa Block.Lithos,120(3-4):327-346.https://doi.org/10.1016/j.lithos.2010.08.021
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
Tafti,R.,Lang,J.R.,Mortensen,J.K.,et al.,2014.Geology and Geochronology of the Xietongmen(Xiongcun)Cu-Au Porphyry District,Southern Tibet,China.Economic Geology,109(7):1967-2001.https://doi.org/10.2113/econgeo.109.7.1967
Taylor,S.R.,McLennan,S.M.,1995.The Geochemical Evolution of the Continental Crust.Reviews of Geophysics,33(2):241-265.https://doi.org/10.1029/95rg00262
Tepper,J.H.,Nelson,B.K.,Bergantz,G.W.,et al.,1993.Petrology of the Chilliwack Batholith,North Cascades,Washington:Generation of Calc-Alkaline Granitoids by Melting of Mafic Lower Crust with Variable Water Fugacity.Contributions to Mineralogy and Petrology,113(3):333-351.https://doi.org/10.1007/bf00286926
Wang,C.,Ding,L.,Zhang,L.Y.,et al.,2016.Petrogenesis of Middle-Late Triassic Volcanic Rocks from the Gangdese Belt,Southern Lhasa Terrane:Implications for Early Subduction of Neo-Tethyan Oceanic Lithosphere.Lithos,262:320-333.https://doi.org/10.1016/j.lithos.2016.07.021
Wang,Q.,Zhu,D.C.,Cawood,P.A.,et al.,2015.Eocene Magmatic Processes and Crustal Thickening in Southern Tibet:Insights from Strongly Fractionated Ca.43 Ma Granites in the Western Gangdese Batholith.Lithos,239:128-141.https://doi.org/10.1016/j.lithos.2015.10.003
Wei,Y.Q.,Zhao,Z.D.,Niu,Y.L.,et al.,2017.Geochronology and Geochemistry of the Early Jurassic Yeba Formation Volcanic Rocks in Southern Tibet:Initiation of Back-Arc Rifting and Crustal Accretion in the Southern Lhasa Terrane.Lithos,278-281:477-490.https://doi.org/10.1016/j.lithos.2017.02.013
Wilson,M.,1993.Magmatism and the Geodynamics of Basin Formation.Sedimentary Geology,86(1-2):5-29.https://doi.org/10.1016/0037-0738(93)90131-n
Wu,F.Y.,Ji,W.Q.,Liu,C.Z.,et al.,2010.Detrital Zircon U-Pb and Hf Isotopic Data from the Xigaze ForeArc Basin:Constraints on Transhimalayan Magmatic Evolution in Southern Tibet.Chemical Geology,271(1-2):13-25.https://doi.org/10.1016/j.chemgeo.2009.12.007
Wu,Y.,Chen,S.Y.,Qin,M.K.,et al.,2018.Zircon U-Pb Ages of Dongcuo Ophiolite in Western Bangonghu-Nujiang Suture Zone and Their Geological Significance.Earth Science,43(4):1070-1084(in Chinese with English abstract).https://doi.org/10.3799/dqkx.2018.710
Wu,Y.W.,Li,C.,Xu,M.J.,et al.,2017.Zircon U-Pb Age,Geochemical Data:Constraints on the Origin and Tectonic Evolution of the Metamafic Rocks from Longmuco-Shuanghu-Lancang Suture Zone,Tibet.Journal of Earth Science,28(3):422-432.https://doi.org/10.1007/s12583-017-0730-z
Xiong,Q.W.,Chen,J.L.,Xu,J.F.,et al.,2015.LA-ICP-MSZircon U-Pb Geochronology,Geochemical Characteristics and Genetic Study ofYeba Formation Lavas in Demingding Area,Southern Tibet.Geological Bulletin of China,34(9):1645-1655(in Chinese with English abstract).
Xu,Z.Q.,Yang,J.S.,Li,H.B.,et al.,2007.The Tibetan Plateau:Formed by Orogeny.Geological Publishing House,Beijing(in Chinese).
Yang,J.S.,Xu,Z.Q.,Geng,Q.R.,et al.,2006.A Possible New HP/UHP(?)Metamorphic Belt in China:Discovery of Eclogite in the Lasha Terrane,Tibet.Acta Geologica Sinica,80(12):1787-1792(in Chinese with English abstract).
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
Yin,J.R.,Cai,H.W.,Zhou,Z.G.,2006.Study of Marine Triassic/Jurassic Boundary Stratigraphy and the Latest Triassic Mass Extinction in Tibet.Earth Science Frontiers,13(4):244-254(in Chinese with English abstract).
Yin,J.R.,Grant-Mackie,J.A.,2005.Late Triassic-Jurassic Bivalves from Volcanic Sediments of the Lhasa Block,Tibet.New Zealand Journal of Geology and Geophysics,48(3):555-577.https://doi.org/10.1080/00288306.2005.9515133
Zeng,Y.C.,Xu,J.F.,Chen,J.L.,et al.,2018.Geochronological and Geochemical Constraints on the Origin of the Yunzhug Ophiolite in the Shiquanhe-Yunzhug-Namu Tso Ophiolite Belt,Lhasa Terrane,Tibetan Plateau.Lithos,300-301:250-260.https://doi.org/10.1016/j.lithos.2017.11.025
Zeng,Z.C.,Liu,D.M.,Zeren,Z.X.,et al.,2009.Geochemistry and Tectonic Setting of Lavas in the Yeba Formation in the Eastern Part of the Gangdise Belt.Journal of Jilin University(Earth Science Edition),39(3):435-445(in Chinese with English abstract).
Zhang,H.F.,Xu,W.C.,Guo,J.Q.,et al.,2007.Zircon U-Pb and Hf Isotopic Composition of Deformed Granite in the Southern Margin of the Gangdise Belt,Tibet:Evidence for Early Jurassic Subduction of Neo-Tethyan Oceanic Slab.Acta Petrologica Sinica,23(6):1347-1353(in Chinese with English abstract).
Zhou,S.,2002.Study on the Geochronology of Several Key Regions of Gangdese Magmatic and Yarlung Zangpo Ophiolite Belts,Tibet(Dissertation).China University of Geosciences,Beijing(in Chinese with English abstract).
Zhu,D.C.,Pan,G.T.,Chung,S.L.,et al.,2008.SHRIMP Zircon Age and Geochemical Constraints on the Origin of Lower Jurassic Volcanic Rocks from the Yeba Formation,Southern Gangdese,South Tibet.International Geology Review,50(5):442-471.https://doi.org/10.2747/0020-6814.50.5.442
Zhu,D.C.,Pan,G.T.,Wang,L.Q.,et al.,2008a.Spatial-Temporal Distribution and Tectonic Setting of Jurassic Magmatism in the Gangdise Belt,Tibet,China.Geological Bulletin of China,27(4):458-468(in Chinese with English abstract).
Zhu,D.C.,Pan,G.T.,Wang,L.Q.,et al.,2008b.TempoSpatial Variations of Mesozoic Magmatic Rocks in the Gangdise Belt,Tibet,China,with a Discussion of Geodynamic Setting-Related Issues.Geological Bulletin of China,27(9):1535-1550(in Chinese with English abstract).
Zhu,D.C.,Zhao,Z.D.,Niu,Y.L.,et al.,2011.The Lhasa Terrane: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,J.,Du,Y.S.,Liu,Z.X.,et al.,2005.Mesozoic Radiolarian Chert from the Middle Sector of the Yarlung-Zangbo Suture Zone,Tibet and Its Tectonic Implications.Science in China(Series D),35(12):1131-1139(in Chinese).
Zorpi,M.J.,Coulon,C.,Orsini,J.B.,1991.Hybridization between Felsic and Mafic Magmas in Calc-Alkaline Granitoids―A Case Study in Northern Sardinia,Italy.Chemical Geology,92(1-3):45-86.https://doi.org/10.1016/0009-2541(91)90049-w
陈炜,马昌前,边秋娟,等,2009.西藏得明顶地区叶巴组火山岩地球化学特征和同位素U-Pb年龄证据.地质科技情报,28(3):31-40.
董昕,张泽明,2013.拉萨地体南部早侏罗世岩浆岩的成因和构造意义.岩石学报,29(6):1933-1948.
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.
耿全如,潘桂棠,金振民,等,2005.西藏冈底斯带叶巴组火山岩地球化学及成因.地球科学,30(6):747-760.
耿全如,潘桂棠,王立全,等,2006.西藏冈底斯带叶巴组火山岩同位素地质年代.沉积与特提斯地质,26(1):1-7.
苟金,1994.对拉萨地区叶巴组时代归属的新认识.西藏地质,(11):1-6.
和钟铧,杨德明,郑常青,等,2006.冈底斯带门巴花岗岩同位素测年及其对新特提斯洋俯冲时代的约束.地质论评,52(1):100-106.
黄丰,许继峰,陈建林,等,2015.早侏罗世叶巴组与桑日群火山岩:特提斯洋俯冲过程中的陆缘弧与洋内弧?.岩石学报,31(7):2089-2098.
李化启,许志琴,杨经绥,等,2011.拉萨地体内松多榴辉岩的同碰撞折返:来自构造变形和40Ar-39Ar年代学的证据.地学前缘,18(3):66-78.
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.
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.
裴树文,1999.拉萨地块火山岩系内早-中侏罗世双壳类动物群及其古生物地理.现代地质,13(3):291-297.
邱检生,王睿强,赵姣龙,等,2015.冈底斯中段早侏罗世辉长岩-花岗岩杂岩体成因及其对新特提斯构造演化的启示:以日喀则东嘎岩体为例.岩石学报,31(12):3569-3580.
武勇,陈松永,秦明宽,等,2018.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.地球科学,43(4):1070-1084.
熊秋伟,陈建林,许继峰,等,2015.拉萨地块南部得明顶地区叶巴组火山岩LA-ICP-MS锆石U-Pb年龄、地球化学特征及其成因.地质通报,34(9):1645-1655.
许志琴,杨经绥,李海兵,等,2007.造山的高原--青藏高原的地体拼合、碰撞造山及隆升机制.北京:地质出版社
杨经绥,许志琴,耿全如,等,2006.中国境内可能存在一条新的高压/超高压(?)变质带--青藏高原拉萨地体中发现榴辉岩带.地质学报,80(12):1787-1792.
阴家润,蔡华伟,周志广,等,2006.西藏海相三叠系-侏罗系界线及晚三叠世生物绝灭事件研究.地学前缘,13(4),244-254.
曾忠诚,刘德民,泽仁扎西,等,2009.西藏冈底斯东段叶巴组火山岩地球化学特征及其地质构造意义.吉林大学学报(地球科学版),39(3):435-445.
张宏飞,徐旺春,郭建秋,等,2007.冈底斯南缘变形花岗岩错石U-Pb年龄和Hf同位素组成:新特提斯洋早侏罗世俯冲作用的证据.岩石学报,23(6):1347-1353.
周肃,2002.西藏冈底斯岩浆岩带及雅鲁藏布蛇绿岩带关键地段同位素年代学研究(博士学位论文).北京:中国地质大学.
朱弟成,潘桂棠,王立全,等,2008a.西藏冈底斯带侏罗纪岩浆作用的时空分布及构造环境.地质通报,27(4):458-468.
朱弟成,潘桂棠,王立全,等,2008b.西藏冈底斯带中生代岩浆岩的时空分布和相关问题的讨论.地质通报,27(9):1535-1550.
朱杰,杜远生,刘早学,等,2005.西藏雅鲁藏布江缝合带中段中生代放射虫硅质岩成因及其大地构造意义.中国科学(D辑),35(12):1131-1139.
Atherton,M.P.,Petford,N.,1993.Generation ofSodium-Rich Magmas from Newly Underplated Basaltic Crust.Nature,362(6416):144-146.https://doi.org/10.1038/362144a0
Bacon,C.R.,Druitt,T.H.,1988.Compositional Evolution of the Zoned Cal-Calkaline Magma Chamber of Mount Mazama,Crater Lake,Oregon.Contributions to Mineralogy and Petrology,98(2):224-256.https://doi.org/10.1007/bf00402114
Chen,W.,Ma,C.Q.,Bian,Q.J.,et al.,2009.Evidences from Geochemistry and Zircon U-Pb Geochronology of Volcanic Rocks of Yeba Formation in Demingding Area,the East of Middle Gangdise,Tibet.Geological Science and Technology Information,28(3):31-40(in Chinese with English abstract).
Chu,M.F.,Chung,S.L.,Song,B.,et al.,2006.Zircon U-Pb and Hf Isotope Constraints on the Mesozoic Tectonics and Crustal Evolution of Southern Tibet.Geology,34(9):745.https://doi.org/10.1130/g22725.1
Condie,K.C.,Bowling,G.P.,Allen,P.,1986.Origin of Granites in an Archean High-Grade Terrane,Southern India.Contributions to Mineralogy and Petrology,92(1):93-103.https://doi.org/10.1007/bf00373967
Dong,X.,Zhang,Z.M.,2013.Genesis and Tectonic Significance of the Early Jurassic Magmatic Rocks from the Southern Lhasa Terrane.Acta Petrologica Sinica,29(6):1933-1948(in Chinese with Englishabstract).
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).
Fitton,J.G.,James,D.,Kempton,P.D.,et al.,1988.The Role of Lithospheric Mantle in the Generation of Late Cenozoic Basic Magmas in the Western United States.Journal of Petrology,Special_Volume,(1):331-349.https://doi.org/10.1093/petrology/special_volume.1.331
Geng,Q.R.,Pan,G.T.,Jin,Z.M.,et al.,2005.Geochemistry and Genesis of the Yeba Volcanic Rocks in the Gangdise Magmatic Arc,Tibet.Earth Science,30(6):747-760(in Chinese with English abstract).
Geng,Q.R.,Pan,G.T.,Wang,L.Q.,et al.,2006.Isotopic Geochronology of the Volcanic Rocks from the Yeba Formation in the Gangdise Zone,Xizang.Sedimentary Geology and Tethyan Geology,26(1):1-7(in Chinese with English abstract).
Gorton,M.P.,Schandl,E.S.,2000.From Continents to Island Arcs:A Geochemical Index of Tectonic Setting for Arc-Related and Within-Plate Felsic to Intermediate Volcanic Rocks.The Canadian Mineralogist,38(5):1065-1073.https://doi.org/10.2113/gscanmin.38.5.1065
Gou,J.,1994.A New Knowledge on the Attributes of Yeba Formation in Lhasa Area.Tibetan Geology,(11):1-6(in Chinese with English abstract).
Guo,L.,Zhang,H.F.,Harris,N.,et al.,2013.Late Cretaceous(~81 Ma)High-Temperature Metamorphism in the Southeastern Lhasa Terrane:Implication for the NeoTethys Ocean Ridge Subduction.Tectonophysics,608:112-126.https://doi.org/10.1016/j.tecto.2013.10.007
Gutscher,M.A.,Maury,R.,Eissen,J.P.,et al.,2000.Can Slab Melting be Caused by Flat Subduction?.Geology,28(6):535-538.https://doi.org/10.1130/0091-7613(2000)28<535:csmbcb>2.0.co;2
He,Z.H.,Yang,D.M.,Zheng,C.Q.,et al.,2006.Isotopic Dating of the Mamba Granitoid in the Gangdise Tectonic Belt and Its Constraint on the Subduction Time of the Neotethys.Geological Review,52(1):100-106(in Chinese with English abstract).
Hu,P.Y.,Zhai,Q.G.,Wang,J.,et al.,2018.Precambrian Origin of the North Lhasa Terrane,Tibetan Plateau:Constraint from Early Cryogenian Back-Arc Magmatism.Precambrian Research,313:51-67.https://doi.org/10.1016/j.precamres.2018.05.014
Huang,F.,Xu,J.F.,Chen,J.L.,et al.,2015.Early Jurassic Volcanic Rocks from the Yeba Formation and Sangri Group:Products of Continental Marginal Arc and IntraOceanic Arc during the Subduction of Neo-Tethys Ocean?.Acta Petrologica Sinica,31(7):2089-2098(in Chinese with English abstract).
Kelemen,P.B.,Hangh?j,K.,Greene,A.R.,2007.One View of the Geochemistry of Subduction-Related Magmatic Arcs,with an Emphasis on Primitive Andesite and Lower Crust.Treatise on Geochemistry,3:593-660.https://doi.org/10.1016/B0-08-043751-6/03035-8
Leat,P.T.,Thompson,R.N.,Morrison,M.A.,et al.,1988.Compositionally-Diverse Miocene-Recent RiftRelated Magmatism in Northwest Colorado:Partial Melting,and Mixing of Mafic Magmas from 3 Different Asthenospheric and Lithospheric Mantle Sources.Journal of Petrology,Special Volume(1):351-377.https://doi.org/10.1093/petrology/special_volume.1.351
Li,H.Q.,Xu,Z.Q.,Yang,J.S.,et al.,2011.Syn-Collisional Exhumation of Sumdo Eclogite in the Lhasa Terrane,Tibet:Evidences from Structural Deformation and40Ar-39Ar Geochronology.Earth Science Frontiers,18(3):66-78(in Chinese with English abstract).
Liu,Z.C.,Ding,L.,Zhang,L.Y.,et al.,2018.Sequence and Petrogenesis of the Jurassic Volcanic Rocks(Yeba Formation)in the Gangdese Arc,Southern Tibet:Implications for the Neo-Tethyan Subduction.Lithos,312-313:72-88.https://doi.org/10.1016/j.lithos.2018.04.026
Ma,X.X.,Xu,Z.Q.,Chen,X.J.,et al.,2017.The Origin and Tectonic Significance of the Volcanic Rocks of the Yeba Formation in the Gangdese Magmatic Belt,South Tibet.Journal of Earth Science,28(2):265-282.https://doi.org/10.1007/s12583-016-0925-8
Maniar,P.D.,Piccoli,P.M.,1989.Tectonic Discrimination of Granitoids.Geological Society of America Bulletin,101(5):635-643.https://doi.org/10.1130/0016-7606(1989)101<0635:tdog>2.3.co;2
McCarron,J.J.,Smellie,J.L.,1998.Tectonic Implications of Fore-Arc Magmatism and Generation of High-Magnesian Andesites:Alexander Island,Antarctica.Journal of the Geological Society,155(2):269-280.https://doi.org/10.1144/gsjgs.155.2.0269
Miyashiro,A.,1974.Volcanic Rock Series in Island Arcs and Active Continental Margins.American Journal of Science,274(4):321-355.https://doi.org/10.2475/ajs.274.4.321
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 Universities,11(3):281-290(in Chinese with English abstract).
Mo,X.X.,Niu,Y.L.,Dong,G.C.,et al.,2008.Contribution of Syncollisional Felsic Magmatism to Continental Crust Growth:A Case Study of the Paleogene Linzizong Volcanic Succession in Southern Tibet.Chemical Geology,250(1-4):49-67.https://doi.org/10.1016/j.chemgeo.2008.02.003
Murphy,M.A.,Yin,A.,Harrison,T.M.,et al.,1997.Did the Indo-Asian Collision Alone Create the Tibetan Plateau?.Geology,25(8):719.https://doi.org/10.1130/0091-7613(1997)025<0719:dtiaca>2.3.co;2
Müller,D.,Rock,N.M.S.,Groves,D.I.,1992.Geochemical Discrimination between Shoshonitic and Potassic Volcanic Rocks in Different Tectonic Settings:A Pilot Study.Mineralogy and Petrology,46(4):259-289.https://doi.org/10.1007/bf01173568
Pan,F.B.,Zhang,H.F.,Xu,W.C.,et al.,2016.U-Pb Zircon Dating,Geochemical and Sr-Nd-Hf Isotopic Compositions of Mafic Intrusive Rocks in the Motuo,SE Tibet Constrain on Their Petrogenesis and Tectonic Implication.Lithos,245:133-146.https://doi.org/10.1016/j.lithos.2015.05.011
Pan,G.T.,Mo,X.X.,Hou,Z.Q.,et al.,2006.SpatialTemporal Framework of the Gangdese Orogenic Belt and Its Evolution.Acta Petrologica Sinica,22(3):521-533(in Chinese with English abstract).
Pati?o Douce,A.E.,Johnston,A.D.,1991.Phase Equilibria and Melt Productivity in the Pelitic System:Implications for the Origin of Peraluminous Granitoids and Aluminous Granulites.Contributions to Mineralogy and Petrology,107(2):202-218.https://doi.org/10.1007/bf00310707
Pearce,J.A.,1982.Trace Element Characteristics of Lavas from Destructive Plate Boundaries.Andesites:Orogenic Andesites and Related Rocks.John Wiley and Sons,New York,525-548.
Pearce,J.A.,Harris,N.B.W.,Tindle,A.G.,1984.Trace Element Discrimination Diagrams for the Tectonic Interpretation of Granitic Rocks.Journal of Petrology,25(4):956-983.https://doi.org/10.1093/petrology/25.4.956
Pearce,J.A.,Mei,H.J.,1988.Volcanic Rocks of the 1985Tibet Geotraverse:Lhasa to Golmud.Philosophical Transactions of the Royal Society A:Mathmatical,Physical and Engineering Science,327(1594):169-201.https://doi.org/10.1098/rsta.1988.0125
Pei,S.W.,1999.Early and Middle Jurassic Bivalve Fauna in Volcanic Rocks of Tibetan Lhasa Block and Its Paleobiogeography.Geoscience,13(3):291-297(in Chinese with English abstract).
Plank,T.,2005.Constraints from Thorium/Lanthanum on Sediment Recycling at Subduction Zones and the Evolution of the Continents.Journal of Petrology,46(5):921-944.https://doi.org/10.1093/petrology/egi005
Qiu,J.S.,Wang,R.Q.,Zhao,J.L,et al.,2015.Petrogenesis of the Early Jurassic Gabbro-Granite Complex in the Middle Segment of the Gangdese Belt and Its Implications for Tectonic Evolution of Neo-Tethys:A Case Study of the Dongga Pluton in Xi’gaze.Acta Petrologica Sinica,31(12):3569-3580(in Chinese with English abstract).
Rudnick,R.L.,Gao,S.,2003.Composition of the Contiental Crust.Treatise on Geochemistry,3:1-64
Salters,V.J.M.,Stracke,A.,2004.Composition of the Depleted Mantle.Geochemistry,Geophysics,Geosystems,5(5):1-27.https://doi.org/10.1029/2003gc000597
Schiano,P.,Monzier,M.,Eissen,J.P.,et al.,2010.Simple Mixing as the Major Control of the Evolution of Volcanic Suites in the Ecuadorian Andes.Contributions to Mineralogy and Petrology,160(2):297-312.https://doi.org/10.1007/s00410-009-0478-2
Shinjo,R.,Kato,Y.,2000.Geochemical Constraints on the Origin of Bimodal Magmatism at the Okinawa Trough,an Incipient Back-Arc Basin.Lithos,54(3-4):117-137.https://doi.org/10.1016/s0024-4937(00)00034-7
Sisson,T.W.,1994.Hornblende-Melt Trace-Element Partitioning Measured by Ion Microprobe.Chemical Geology,117(1-4):331-344.https://doi.org/10.1016/0009-2541(94)90135-x
Song,S.G.,Niu,Y.L.,Wei,C.J.,et al.,2010.Metamorphism,Anatexis,Zircon Ages and Tectonic Evolution of the Gongshan Block in the Northern Indochina Continent-An Eastern Extension of the Lhasa Block.Lithos,120(3-4):327-346.https://doi.org/10.1016/j.lithos.2010.08.021
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
Tafti,R.,Lang,J.R.,Mortensen,J.K.,et al.,2014.Geology and Geochronology of the Xietongmen(Xiongcun)Cu-Au Porphyry District,Southern Tibet,China.Economic Geology,109(7):1967-2001.https://doi.org/10.2113/econgeo.109.7.1967
Taylor,S.R.,McLennan,S.M.,1995.The Geochemical Evolution of the Continental Crust.Reviews of Geophysics,33(2):241-265.https://doi.org/10.1029/95rg00262
Tepper,J.H.,Nelson,B.K.,Bergantz,G.W.,et al.,1993.Petrology of the Chilliwack Batholith,North Cascades,Washington:Generation of Calc-Alkaline Granitoids by Melting of Mafic Lower Crust with Variable Water Fugacity.Contributions to Mineralogy and Petrology,113(3):333-351.https://doi.org/10.1007/bf00286926
Wang,C.,Ding,L.,Zhang,L.Y.,et al.,2016.Petrogenesis of Middle-Late Triassic Volcanic Rocks from the Gangdese Belt,Southern Lhasa Terrane:Implications for Early Subduction of Neo-Tethyan Oceanic Lithosphere.Lithos,262:320-333.https://doi.org/10.1016/j.lithos.2016.07.021
Wang,Q.,Zhu,D.C.,Cawood,P.A.,et al.,2015.Eocene Magmatic Processes and Crustal Thickening in Southern Tibet:Insights from Strongly Fractionated Ca.43 Ma Granites in the Western Gangdese Batholith.Lithos,239:128-141.https://doi.org/10.1016/j.lithos.2015.10.003
Wei,Y.Q.,Zhao,Z.D.,Niu,Y.L.,et al.,2017.Geochronology and Geochemistry of the Early Jurassic Yeba Formation Volcanic Rocks in Southern Tibet:Initiation of Back-Arc Rifting and Crustal Accretion in the Southern Lhasa Terrane.Lithos,278-281:477-490.https://doi.org/10.1016/j.lithos.2017.02.013
Wilson,M.,1993.Magmatism and the Geodynamics of Basin Formation.Sedimentary Geology,86(1-2):5-29.https://doi.org/10.1016/0037-0738(93)90131-n
Wu,F.Y.,Ji,W.Q.,Liu,C.Z.,et al.,2010.Detrital Zircon U-Pb and Hf Isotopic Data from the Xigaze ForeArc Basin:Constraints on Transhimalayan Magmatic Evolution in Southern Tibet.Chemical Geology,271(1-2):13-25.https://doi.org/10.1016/j.chemgeo.2009.12.007
Wu,Y.,Chen,S.Y.,Qin,M.K.,et al.,2018.Zircon U-Pb Ages of Dongcuo Ophiolite in Western Bangonghu-Nujiang Suture Zone and Their Geological Significance.Earth Science,43(4):1070-1084(in Chinese with English abstract).https://doi.org/10.3799/dqkx.2018.710
Wu,Y.W.,Li,C.,Xu,M.J.,et al.,2017.Zircon U-Pb Age,Geochemical Data:Constraints on the Origin and Tectonic Evolution of the Metamafic Rocks from Longmuco-Shuanghu-Lancang Suture Zone,Tibet.Journal of Earth Science,28(3):422-432.https://doi.org/10.1007/s12583-017-0730-z
Xiong,Q.W.,Chen,J.L.,Xu,J.F.,et al.,2015.LA-ICP-MSZircon U-Pb Geochronology,Geochemical Characteristics and Genetic Study ofYeba Formation Lavas in Demingding Area,Southern Tibet.Geological Bulletin of China,34(9):1645-1655(in Chinese with English abstract).
Xu,Z.Q.,Yang,J.S.,Li,H.B.,et al.,2007.The Tibetan Plateau:Formed by Orogeny.Geological Publishing House,Beijing(in Chinese).
Yang,J.S.,Xu,Z.Q.,Geng,Q.R.,et al.,2006.A Possible New HP/UHP(?)Metamorphic Belt in China:Discovery of Eclogite in the Lasha Terrane,Tibet.Acta Geologica Sinica,80(12):1787-1792(in Chinese with English abstract).
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
Yin,J.R.,Cai,H.W.,Zhou,Z.G.,2006.Study of Marine Triassic/Jurassic Boundary Stratigraphy and the Latest Triassic Mass Extinction in Tibet.Earth Science Frontiers,13(4):244-254(in Chinese with English abstract).
Yin,J.R.,Grant-Mackie,J.A.,2005.Late Triassic-Jurassic Bivalves from Volcanic Sediments of the Lhasa Block,Tibet.New Zealand Journal of Geology and Geophysics,48(3):555-577.https://doi.org/10.1080/00288306.2005.9515133
Zeng,Y.C.,Xu,J.F.,Chen,J.L.,et al.,2018.Geochronological and Geochemical Constraints on the Origin of the Yunzhug Ophiolite in the Shiquanhe-Yunzhug-Namu Tso Ophiolite Belt,Lhasa Terrane,Tibetan Plateau.Lithos,300-301:250-260.https://doi.org/10.1016/j.lithos.2017.11.025
Zeng,Z.C.,Liu,D.M.,Zeren,Z.X.,et al.,2009.Geochemistry and Tectonic Setting of Lavas in the Yeba Formation in the Eastern Part of the Gangdise Belt.Journal of Jilin University(Earth Science Edition),39(3):435-445(in Chinese with English abstract).
Zhang,H.F.,Xu,W.C.,Guo,J.Q.,et al.,2007.Zircon U-Pb and Hf Isotopic Composition of Deformed Granite in the Southern Margin of the Gangdise Belt,Tibet:Evidence for Early Jurassic Subduction of Neo-Tethyan Oceanic Slab.Acta Petrologica Sinica,23(6):1347-1353(in Chinese with English abstract).
Zhou,S.,2002.Study on the Geochronology of Several Key Regions of Gangdese Magmatic and Yarlung Zangpo Ophiolite Belts,Tibet(Dissertation).China University of Geosciences,Beijing(in Chinese with English abstract).
Zhu,D.C.,Pan,G.T.,Chung,S.L.,et al.,2008.SHRIMP Zircon Age and Geochemical Constraints on the Origin of Lower Jurassic Volcanic Rocks from the Yeba Formation,Southern Gangdese,South Tibet.International Geology Review,50(5):442-471.https://doi.org/10.2747/0020-6814.50.5.442
Zhu,D.C.,Pan,G.T.,Wang,L.Q.,et al.,2008a.Spatial-Temporal Distribution and Tectonic Setting of Jurassic Magmatism in the Gangdise Belt,Tibet,China.Geological Bulletin of China,27(4):458-468(in Chinese with English abstract).
Zhu,D.C.,Pan,G.T.,Wang,L.Q.,et al.,2008b.TempoSpatial Variations of Mesozoic Magmatic Rocks in the Gangdise Belt,Tibet,China,with a Discussion of Geodynamic Setting-Related Issues.Geological Bulletin of China,27(9):1535-1550(in Chinese with English abstract).
Zhu,D.C.,Zhao,Z.D.,Niu,Y.L.,et al.,2011.The Lhasa Terrane: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,J.,Du,Y.S.,Liu,Z.X.,et al.,2005.Mesozoic Radiolarian Chert from the Middle Sector of the Yarlung-Zangbo Suture Zone,Tibet and Its Tectonic Implications.Science in China(Series D),35(12):1131-1139(in Chinese).
Zorpi,M.J.,Coulon,C.,Orsini,J.B.,1991.Hybridization between Felsic and Mafic Magmas in Calc-Alkaline Granitoids―A Case Study in Northern Sardinia,Italy.Chemical Geology,92(1-3):45-86.https://doi.org/10.1016/0009-2541(91)90049-w
陈炜,马昌前,边秋娟,等,2009.西藏得明顶地区叶巴组火山岩地球化学特征和同位素U-Pb年龄证据.地质科技情报,28(3):31-40.
董昕,张泽明,2013.拉萨地体南部早侏罗世岩浆岩的成因和构造意义.岩石学报,29(6):1933-1948.
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.
耿全如,潘桂棠,金振民,等,2005.西藏冈底斯带叶巴组火山岩地球化学及成因.地球科学,30(6):747-760.
耿全如,潘桂棠,王立全,等,2006.西藏冈底斯带叶巴组火山岩同位素地质年代.沉积与特提斯地质,26(1):1-7.
苟金,1994.对拉萨地区叶巴组时代归属的新认识.西藏地质,(11):1-6.
和钟铧,杨德明,郑常青,等,2006.冈底斯带门巴花岗岩同位素测年及其对新特提斯洋俯冲时代的约束.地质论评,52(1):100-106.
黄丰,许继峰,陈建林,等,2015.早侏罗世叶巴组与桑日群火山岩:特提斯洋俯冲过程中的陆缘弧与洋内弧?.岩石学报,31(7):2089-2098.
李化启,许志琴,杨经绥,等,2011.拉萨地体内松多榴辉岩的同碰撞折返:来自构造变形和40Ar-39Ar年代学的证据.地学前缘,18(3):66-78.
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.
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.
裴树文,1999.拉萨地块火山岩系内早-中侏罗世双壳类动物群及其古生物地理.现代地质,13(3):291-297.
邱检生,王睿强,赵姣龙,等,2015.冈底斯中段早侏罗世辉长岩-花岗岩杂岩体成因及其对新特提斯构造演化的启示:以日喀则东嘎岩体为例.岩石学报,31(12):3569-3580.
武勇,陈松永,秦明宽,等,2018.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.地球科学,43(4):1070-1084.
熊秋伟,陈建林,许继峰,等,2015.拉萨地块南部得明顶地区叶巴组火山岩LA-ICP-MS锆石U-Pb年龄、地球化学特征及其成因.地质通报,34(9):1645-1655.
许志琴,杨经绥,李海兵,等,2007.造山的高原--青藏高原的地体拼合、碰撞造山及隆升机制.北京:地质出版社
杨经绥,许志琴,耿全如,等,2006.中国境内可能存在一条新的高压/超高压(?)变质带--青藏高原拉萨地体中发现榴辉岩带.地质学报,80(12):1787-1792.
阴家润,蔡华伟,周志广,等,2006.西藏海相三叠系-侏罗系界线及晚三叠世生物绝灭事件研究.地学前缘,13(4),244-254.
曾忠诚,刘德民,泽仁扎西,等,2009.西藏冈底斯东段叶巴组火山岩地球化学特征及其地质构造意义.吉林大学学报(地球科学版),39(3):435-445.
张宏飞,徐旺春,郭建秋,等,2007.冈底斯南缘变形花岗岩错石U-Pb年龄和Hf同位素组成:新特提斯洋早侏罗世俯冲作用的证据.岩石学报,23(6):1347-1353.
周肃,2002.西藏冈底斯岩浆岩带及雅鲁藏布蛇绿岩带关键地段同位素年代学研究(博士学位论文).北京:中国地质大学.
朱弟成,潘桂棠,王立全,等,2008a.西藏冈底斯带侏罗纪岩浆作用的时空分布及构造环境.地质通报,27(4):458-468.
朱弟成,潘桂棠,王立全,等,2008b.西藏冈底斯带中生代岩浆岩的时空分布和相关问题的讨论.地质通报,27(9):1535-1550.
朱杰,杜远生,刘早学,等,2005.西藏雅鲁藏布江缝合带中段中生代放射虫硅质岩成因及其大地构造意义.中国科学(D辑),35(12):1131-1139.