大陆中洋壳俯冲增生杂岩带特征与识别的重大科学意义
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摘要
大洋或弧后洋盆俯冲增生是大陆地壳增长的主导地质作用.重建大陆中消亡的洋地层岩石组合序列是当代大陆动力学和地学研究的重大前沿.洋壳消减杂岩带的厘定是洋板块地质构造重建乃至全球大地构造研究之纲,是理解区域大地构造形成演化及动力学的核心.俯冲增生杂岩带的基本特征:(1)俯冲增生杂岩带物质组成的共性是:以强烈构造变形洋底沉积的硅质岩-硅泥质岩-粉砂岩、凝灰岩;弧-沟浊积岩等为基质;以洋岛-海山灰岩-玄武岩及塌积砾岩,洋内弧残留岩块,超镁铁质蛇绿岩、绿片岩、蓝片岩等为岩块.(2)变形样式:同斜倒转冲断叠瓦构造、增生柱前缘重力滑动构造以及泥质岩的底辟构造;增生楔前缘变形和增生形式受控于大洋或弧后洋盆的规模和洋壳的俯冲速度,也取决于陆缘碎屑供给量及洋底沉积厚度和岩性.(3)宽度和厚度:厚常达几千米,宽达几十公里至数百公里,延长上千公里,是洋壳俯冲消亡过程洋盆地层系统及陆缘沉积物加积的结果.(4)形成机制:是大陆碰撞前大洋(或弧后洋盆)岩石圈俯冲消减的产物.结合带中的早期俯冲增生杂岩带往往卷入晚期的构造混杂作用.
Oceanic subduction-accretion or back-arc oceanic subduction-accretion is the dominant geological process of continental crustal growth.Reconstructing the gradual extinction oceanic rock assemblage sequence of continent is a frontier of contemporary continental dynamics and geosciences.The determination of the oceanic crust subduction complex belt is the core of the reconstruction for the oceanic geological structure and the research of the global geotectonics,which is the core of the understanding for the evolution and dynamics of the regional geotectonics.Basic characteristics of the subduction accretion belt include:(1)the commonality of the material composition of the subduction accretionary complex:the pelagic siliceous rock,siliceous mudstone,siltstone,arc-trench turbidite as matrix,in highly tectonic deformation.Stratigraphic sequences of oceanic islands and seamounts are comprised of limestone and basalt,slided conglomerate,residual rock of intra-arc;ultramafic serpentine rocks,greenschists,and blueschists as mass.(2)Deformation style:synclinal overturned thrust imbricated structure,the gravity sliding structure of the accretionary prim front and the diapir structure of the argillaceous rock.The deformation and accretion form of the accretionary wedge front are controlled by the scale of oceanic crust or back-arc oceanic basina,and the subduction speed also depends on the amount of continent margin debris and the sediment thickness and lithology of ocean floor.(3)Width and thickness:the thickness is often several kilometers,the width is from several tens of kilometers to hundreds of kilometers,and the extension is thousands of kilometers.It is the result of the accumulation of oceanic basin system and continental margin sediments during the subduction of oceanic crust.(4)Formation mechanism:it is the product of the subduction of the lithosphere before the collision of the continent or back-arc oceanic basin.The early subduction accretionary belts in the jointing belt are often involved in late tectonic mélange.
Oceanic subduction-accretion or back-arc oceanic subduction-accretion is the dominant geological process of continental crustal growth.Reconstructing the gradual extinction oceanic rock assemblage sequence of continent is a frontier of contemporary continental dynamics and geosciences.The determination of the oceanic crust subduction complex belt is the core of the reconstruction for the oceanic geological structure and the research of the global geotectonics,which is the core of the understanding for the evolution and dynamics of the regional geotectonics.Basic characteristics of the subduction accretion belt include:(1)the commonality of the material composition of the subduction accretionary complex:the pelagic siliceous rock,siliceous mudstone,siltstone,arc-trench turbidite as matrix,in highly tectonic deformation.Stratigraphic sequences of oceanic islands and seamounts are comprised of limestone and basalt,slided conglomerate,residual rock of intra-arc;ultramafic serpentine rocks,greenschists,and blueschists as mass.(2)Deformation style:synclinal overturned thrust imbricated structure,the gravity sliding structure of the accretionary prim front and the diapir structure of the argillaceous rock.The deformation and accretion form of the accretionary wedge front are controlled by the scale of oceanic crust or back-arc oceanic basina,and the subduction speed also depends on the amount of continent margin debris and the sediment thickness and lithology of ocean floor.(3)Width and thickness:the thickness is often several kilometers,the width is from several tens of kilometers to hundreds of kilometers,and the extension is thousands of kilometers.It is the result of the accumulation of oceanic basin system and continental margin sediments during the subduction of oceanic crust.(4)Formation mechanism:it is the product of the subduction of the lithosphere before the collision of the continent or back-arc oceanic basin.The early subduction accretionary belts in the jointing belt are often involved in late tectonic mélange.
引文
Brown,D.,Ryan,P.D.,2011.Arc-Continent Collision.Springer,New York.
Deng,J.F.,Feng,Y.F.,Di,Y.J.,et al.,2015.The Instructions of Intrusion Tectonic Map in China(1∶2 500 000).Geological Publishing House,Beijing(in Chinese).
Deng,J.F.,Feng,Y.F.,Di,Y.J.,et al.,2017.Intrusive Tectonic of China.Geological Publishing House,Beijing(in Chinese).
Deng,X.G.,Ding,L.,Liu,X.H.,et al.,2000.40 Ar/39 Ar Chronology for Gongrnarco Glaucophane Schist from Central Qiangtang,Tibet.Chinese Science Bulletin,45(21):2322-2326(in Chinese).
Deng,X.G.,Ding,L.,Liu,X.H.,et al.,2002.Geochemical Characteristics of the Blueschists and Its Tectonic Significance in the Central Qiangtang Area,Tibet.Acta Petrologica Sinica,18(4):517-525(in Chinese with English abstract).
Feng,Y.M.,Zhang,Y.,2018.Introduction and Commentary on Ocean Plate Stratigrapgy.Geological Bulletin of China,37(4):523-531(in Chinese with English abstract).
Gao,J.,Qian,Q.,Long,L.L.,et al.,2009.Accretionary Orogenic Process of Western Tianshan,China.Geological Bulletin of China,28(12):1804-1816(in Chinese with English abstract).
Geng,Q.R.,Pan,G.T.,Wang,L.Q.,et al.,2011.Tethyan Evolution and Metallogenic Geological Background of the Bangong Co-Nujiang Belt and the Qiangtang Massif in Tibet.Geological Bulletin of China,30(8):1261-1274(in Chinese with English abstract).
Greenly,E.,1919.The Geology of Anglesey.Memoir of the Geological Survey of the U.K.,2:980.
Guo,L.Z.,Shi,Y.S.,Ma,R.S.,1983.On the Formation and Evolution of the Mesozoic-Cenozoic Active Continental Margin and Island Arc Tectonics of the Western Pacific Ocean.Acta Geologica Sinica,57(1):11-21(in Chinese with English abstract).
Hamilton,W.B.,1978.Tectonic Map of the Indonesian Region(1∶5 000 000).USGS Map I-875-D.
Hou,Z.Q.,Wang,E.Q.,2008.Metallogenesis of the Indo-Asian Collisional Orogen:New Advances.Acta Geoscientica Sinica,29(3):275-292(in Chinese with English abstract).
Hou,Z.Q.,Zhong,D.L.,Deng,W.M.,et al.,2005.A Tectonic Model for Porphyry Copper-Molybdenum-Gold Deposits in the Eastern Indo-Asian Collision Zone.In:Porter,T.M.,ed.,Super Porphyry Copper&Gold Deposits-A Global Perspective.PGC Publishing,Adelaide,423-440.
Hsü,K.J.,1968.Principles of Mélanges and Their Bearing on the Franciscan-Knoxville Paradox.Geological Society of America Bulletin,79(8):1063-1074.https://doi.org/10.1130/0016-7606(1968)79[1063:pomatb]2.0.co;2
Hsü,K.J.,Pan,G.T.,?eng?r,A.M.C.,et al.,1995.Tectonic Evolution of the Tibetan Plateau:A Working Hypothesis Based on the Archipelago Model of Orogenesis.International Geology Review,37:473-508.
Hu,P.Y.,Li,C.,Wu,Y.W.,et al.,2014.Opening of the Longmu Co-Shuanghu-Lancangjiang Ocean:Constraints from Plagiogranites.Chinese Science Bulletin,59(20):1992-2003(in Chinese).
Huang,J.Q.,Chen,B.W.,1987.Evolution of the Tethys Sea from China and Its Adjacent Areas.Geological Publishing House,Beijing(in Chinese).
Huang,J.Q.,Chen,G.M.,Chen,B.W.,1984.Preliminary Analysis of the Tethy-Himalayan Tectonic Domain.Acta Geologica Sinica,58(1):1-17(in Chinese with English abstract).
Isozaki,Y.,Maruyama,S.,Furuoka,F.,1990.Accreted Oceanic Materials in Japan.Tectonophysics,181(1-4):179-205.https://doi.org/10.1016/0040-1951(90)90016-2
Jian,P.,Liu,D.Y.,Kr9ner,A.,et al.,2010.Evolution of a Permian Intraoceanic Arc-Trench System in the Solonker Suture Zone,Central Asian Orogenic Belt,China and Mongolia.Lithos,118(1-2):169-190.https://doi.org/10.1016/j.lithos.2010.04.014
Jiang,Q.Y.,Li,C.,Su,L.,et al.,2015.Carboniferous Arc Magmatism in the Qiangtang Area,Northern Tibet:Zircon U-Pb Ages,Geochemical and Lu-Hf Isotopic Characteristics,and Tectonic Implications.Journal of Asian Earth Sciences,100:132-144.https://doi.org/10.1016/j.jseaes.2015.01.012
Jiang,Q.Y.,Li,C.,Xie,C.M.,et al.,2014.Geochemistry and LA-ICP-MS Zircon U-Pb Age of Volcanic Rocks of Wangguoshan Formation in the Gangmar Co Area of Qiangtang,Tibet.Geological Bulletin of China,33(11):1702-1714(in Chinese with English abstract).
Jin,Z.M.,GreenⅡ,H.W.,Borch,R.S.,et al.,1993.Mantle Xenolith and Mark of Geothermal from Back-Arc in Eastern China.Science in China(Series B:Chemistry),23(4):410-416(in Chinese).
Kapp,P.,Yin,A.,Manning,C.E.,et al.,2000.BlueschistBearing Metamorphic Core Complexes in the Qiangtang Block Reveal Deep Crustal Structure of Northern Tibet.Geology,28(1):19-22.https://doi.org/10.1130/0091-7613(2000)028<0019:bbmcci>2.3.co;2
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
Karig,D.E.,1983.Temporal Relationships between Back-Arc Basin Formation and Arc Volcanism with Special Reference to the Philippinesea.Geophysical Monograph Series,27:318-325.
Kroner,A.,2015.The Central Asian Orogenic Belt.Bornttaeger Science Publishers,Suttgart.
Kusky,T.M.,Windley,B.F.,Safonova,I.,et al.,2013.Recognition of Ocean Plate Stratigraphy in Accretionary Orogens through Earth History:A Record of 3.8Billion Years of Sea Floor Spreading,Subduction,and Accretion.Gondwana Research,24(2):501-547.https://doi.org/10.1016/j.gr.2013.01.004
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):155-166(in Chinese with English abstract).
Li,C.,Cheng,L.R.,Zhang,Y.C.,et al.,2004.Discovery of Ordovician-Devonian Strata in the South of the Qiangtang Area,Tibet.Geological Bulletin of China,23(5-6):602-604(in Chinese with English abstract).
Li,C.,Dong,Y.S.,Zhai,Q.G.,et al.,2008.Discovery of Eopaleozoic Ophiolite in the Qiangtang of Tibet Plateau:Evidence from SHRIMP U-Pb Dating and Its Tectonic Implications.Acta Petrologica Sinica,24(1):31-36(in Chinese with English abstract).
Li,C.,Huang,X.P,Zhai,Q.G.,et al.,2006.The Longmu CoShuanghu-Jitang Plate Suture and the Northern Boundary of Gondwanaland in the Qinghai-Tibet Plateau.Earth Science Frontiers,13(4):136-147(in Chinese with English abstract).
Li,C.,Xie,Y.W.,Dong,Y.S.,et al.,2009.Discussion on the Age of Jitang Group around Leiwuqi Area,Eastern Tibet,China and Primary Understanding.Geological Bulletin of China,28(9):1178-1180(in Chinese with English abstract).
Li,C.Y.,Wang,Q.,Liu,X.Y.,et al.,1982.The Instructions of Asian Tectonic Map in China(1∶800 000).Geological Publishing House,Beijing(in Chinese).
Li,C.Y.,Wang,Q.,Liu,X.Y.,et al.,1984.Tectonic Evolution of Asia.Bulletin of the Chinese Academy of Geological Sciences,10:3-11(in Chinese with English abstract).
Li,J.L.,1992.Collision Orogenic Belt Geotectonic Facies.Modern Geology(Part I).Nanjing University Press,Nanjing(in Chinese).
Li,J.Y.,Zhang,J.,Wang,F.G.,et al.,2015.The Instructions of Deformation Tectonic Map in China(1∶2 500 000).Geological Publishing House,Beijing(in Chinese).
Li,J.Y.,Zhang,J.,Zhao,X.X.,et al.,2016.Mantle Subduction and Uplift of Intracontinental Mountains:A Case Study from the Chinese Tianshan Mountains within Eurasia.Scientific Reports,6:28831.
Li,S.Z.,Suo,Y.H.,Guo,L.L.,et al.,2017.Principles of Submarine Tectonics.Science Press,Beijing(in Chinese).
Li,S.Z.,Yang,Z.,Zhao,S.J.,et al.,2016.Global Early Paleozoic Orogens(Ⅰ):Collision-Type Orogeny.Journal of Jilin University(Earth Science Edition),46(4):945-967(in Chinese with English abstract).
Liu,B.P.,Feng,Q.L.,Fang,N.Q.,et al.,1993.Tectonic Evolution of Palaeo-Tethys Poly-Island-Ocean in Changning-Menglian and Langcangjiang Belts,Southwestern Yunnan,China.Earth Science,18(5):529-539,671(in Chinese with English abstract).
Liu,Z.Q.,Pan,G.T.,Zheng,H.X.,1983.A Preliminary Study on the North Boundary and the Evolution of Gondwana and Tethys in Light of the New Data on Qinghai-Xizang(Tibet)Plateau.In:Geological Anthology of QinghaiTibet Plateau(12):“Three Rivers”Tectonic Geology.Geological Publishing House,Beijing(in Chinese).
Lu,S.N.,Hao,G.J.,Wang,H.C.,et al.,2015.The Instructions of Metamorphite Tectonic Map in China(1∶2 500 000).Geological Publishing House,Beijing(in Chinese).
Lu,S.N.,Hao,G.J.,Wang,H.C.,et al.,2017.Metamorphite Tectonic of China.Geological Publishing House,Beijing(in Chinese).
McCall,G.J.H.,Kidd,R.G.W.,1982.The Makran,Southeastern Iran:The Anatomy of a Convergent Plate Margin Active from Cretaceous to Present.Geological Society,London,Special Publications,10(1):387-397.https://doi.org/10.1144/gsl.sp.1982.010.01.26
Mo,X.X.,2011.Magmatism and Evolution of the Tibetan Plateau.Geological Journal of China Universities,17(3):351-367(in Chinese with English abstract).
Mo,X.X.,Pan,G.T.,2006.From the Tethys to the Formation of the Qinghai-Tibet Plateau:Constrained by Tectono-Magmatic Events.EarthScienceFrontiers,13(6):43-51(in Chinese with English abstract).
Mo,X.X.,Zhao,Z.D.,Deng,J.F.,et al.,2003.Response of Volcanism to the India-Asia Collision.Earth Science Frontiers,10(3):135-148(in Chinese with English abstract).
Myhill,R.,2011.Constraints on the Evolution of the Mesohellenic Ophiolite from Subophiolitic Metamorphic Rocks.The Geological Society of America,Special Paper,480:75-94.
Ogawa,Y.,1985.Variety of Subduction and Accretion Processes in Cretaceous to Recent Plate Boundaries around Southwest and Central Japan.Tectonophysics,112(1-4):493-518.https://doi.org/10.1016/0040-1951(85)90192-1
Ogawa,Y.,Taniguchi,H.,1987.Ophiolitic Mélange in Forearc Area and Formation of the Mineoka Belt:Kyushu University,Japan.Science Reports,Geology,15:1-23.
Pan,G.T.,Chen,Z.L.,Li,X.L.,et al.,1997.Tectonic Formation Evolution of East Tethys Geology.Geological Publishing House,Beijing(in Chinese).
Pan,G.T.,Lu,S.N.,Xiao,Q.H.,et al.,2016.Division of Tectonic Stages and Tectonic Evolution in China.Earth Science Frontiers,23(6):1-23(in Chinese with English abstract).
Pan,G.T.,Wang,L.Q.,Li,R.S.,et al.,2012.Tectonic Evolution of the Qinghai-Tibet Plateau.Journal of Asian Earth Sciences,53:3-14.https://doi.org/10.1016/j.jseaes.2011.12.018
Pan,G.T.,Wang,L.Q.,Zhang,W.P.,et al.,2013.The Instructions of Tectonic Map in Qinghai-Tibet Plateau and Its Adjacent Areas(1∶1 500 000).Geological Publishing House,Beijing(in Chinese).
Pan,G.T.,Wang,L.Q.,Zhu,D.C.,2004.Thoughts on Some Important Scientific Problems in Regional Geological Survey of the Qinghai-Tibet Plateau.Geological Bulletin of China,23(1):12-19(in Chinese with English abstract).
Pan,G.T.,Xian,Q.H.,Yin,F.G.,et al.,2015.The Instructions of Tectonic Map in China(1∶2 500 000).Geological Publishing House,Beijing(in Chinese).
Pan,G.T.,Xiao,Q.H.,Lu,S.N.,et al.,2008.Definition,Classification,Characteristics and Diagnostic Indications of Tectonic Facies.Geological Bulletin of China,27(10):1613-1637(in Chinese with English abstract).
Pan,G.T.,Zheng,H.X.,Xu,Y.R.,et al.,1983.A Priliminary Study of Bangongco-Nujiang Suture.Geological Publishing House,Beijing(in Chinese).
Peng,X.J.,Hu,C.C.,1993.Tectonic Evolution of the Sanjiang Belt in Eastern Tibet.Regional Geology of China,(2):140-148(in Chinese with English abstract).
Ren,J.S.,Xiao,L.W.,2004.Lifting the Mysterious Veil of the Tectonics of the Qinghai-Tibet Plateau by 1∶250 000Geological Mapping.Geological Bulletin of China,23(1):1-11(in Chinese with English abstract).
Revan,M.K.,Gen9,Y.,Maslennikov,V.V.,et al.,2014.Mineralogy and Trace-Element Geochemistry of Sulfide Minerals in Hydrothermal Chimneys from the Upper-Cretaceous VMSDeposits of the Eastern Pontide Orogenic Belt(NE Turkey).Ore Geology Reviews,63:129-149.https://doi.org/10.1016/j.oregeorev.2014.05.006
Reymond,M.C.,1975.Mechanism of Brittle Fracture of Rock during Uniaxial Compression in Laboratory and in a Quarry by an Acoustic Emission Technique.International Journal of Rock Mechanics and Mining Sciences&Geomechanics Abstracts,12(7):89.https://doi.org/10.1016/0148-9062(75)90377-0
Robertson,A.H.F.,1994.Role of the Tectonic Facies Concept in Orogenic Analysis and Its Application to Tethys in the Eastern Mediterranean Region.Earth-Science Reviews,37(3-4):139-213.https://doi.org/10.1016/0012-8252(94)90028-0
Safonova,I.,Kojima,S.,Nakae,S.,et al.,2014.Oceanic Island Basalts in Accretionary Complexes of SW Japan:Tectonic and Petrogenetic Implications.Journal of Asian Earth Sciences,113(SI):508-523.https://dx.doi.org/10.1016/j.jseaes.2014.09.015
Saleeby,J.B.,2011.Geochemical Mapping of the KingsKaweah Ophiolite Belt,California-Evidence for Progressive Mélange Formation in a Large Offset Transform-Subduction Initiation Environment.The Geological Society of America,480:31-73.
Shen,S.Y.,Feng,Q.L.,Liu,B.P.,et al.,2002.Study on Ocean Ridge,Ocean Island Volcanic Rocks of Changning-Menglian Belt.Geological Science and Technology Information,21(3):13-17(in Chinese with English abstract).
Sillitoe,R.H.,2013.Metallogenic and Regulatory Inequalities around the Northern Pacific Rim:Implications for Discovery.Society of Economic Geologists,Inc.,Special Publication,17:1-16.
Silver,E.A.,Beutner,E.C.,1980.Mélanges.Geology,8:32-34.
Simandjuntak,T.O.,Barber,A.J.,1996.Contrasting Tectonic Styles in the Neogene Orogenic Belts of Indonesia.Geological Society,London,Special Publications,106(1):185-201.https://doi.org/10.1144/gsl.sp.1996.106.01.12
Sun,X.M.,Shi,G.Y.,Xiong,D.X.,et al.,2007.Platinum Group Elements Geochemistry and Re-Os Isotopic Compositions of Daping Gold Deposit in Ailaoshan Gold Belt,Yunnan Province,China and Their Metallogenic Implications.Acta Geologica Sinica,81(3):394-404(in Chinese with English abstract).
von Huene,R.,Scholl,D.W.,1991.Observations at Convergent Margins Concerning Sediment Subduction,Subduction Erosion,and the Growth of Continental Crust.Reviews of Geophysics,29(3):279.https://doi.org/10.1029/91rg00969
Wakabayashi,J.,Dilek,Y.,2011.Mélanges:Processes of Formation and Societal Significance.The Geological Society of America,Special Paper,480(4):279.
Wakita,K.,2012.Mappable Features of Mélanges Derived from Ocean Plate Stratigraphy in the Jurassic Accretionary Complexes of Mino and Chichibu Terranes in Southwest Japan.Tectonophysics,568-569:74-85.
Wang,B.D.,Wang,L.Q.,Pan,G.T.,et al.,2013.U-Pb Zircon Dating of Early Paleozoic Gabbro from the Nantinghe Ophiolite in the Changning-Menglian Suture Zone and Its Geological Implication.Chinese Science Bulletin,58(4):344-354(in Chinese).
Wang,B.D.,Wang,L.Q.,Xu,J.F.,et al.,2015.The Discovery of High-Pressure Granulite at Shelama in Dongco Area along the Bangongco-Nujiang River Suture Zone and Its Tectonic Significance.Geological Bulletin of China,34(9):1605-1616(in Chinese with English abstract).
Wang,H.Z.,1985.Atlas of the Palaeogeography of China.SinoMaps Press,Beijing(in Chinese).
Wang,H.Z.,Yang,S.N.,Liu,B.P.,et al.,1990.TectonoPalaeogeography and Palaeobiogeography of China and Adjacent Regions.China University of Geosciences Press,Wuhan(in Chinese).
Wang,L.Q.,Pan,G.T.,Li,C.,et al.,2008.SHRIMP U-Pb Zircon Dating of Eopaleozoic Cumulate in Guoganjianian Mt.from Central Qiangtang Area of Northern TibetConsidering the Evolvement of Proto-and PaleoTethys.Geological Bulletin of China,27(12):2045-2056(in Chinese with English abstract).
Wang,L.Q.,Pan,G.T.,Li,D.M.,et al.,1999.The SpatioTemporal Framework and Geological Evolution of the Jinshajiang Arc-Basin Systems.Acta Geologica Sinica,73(3):206-218(in Chinese with English abstract).
Wang,S.D.,Zhang,K.X.,Song,B.W.,et al.,2018.Geochronology and Geochemistry of the Niujuanzi Ophiolitic Mélange,Gansu Province,NW China:Implications for Tectonic Evolution of the Beishan Orogenic College.International Journal of Earth Sciences,107(1):269-289.
Wang,Y.,Jin,Z.M.,Shi,F.,2013.Characteristics of Hydroxyl in Lherzolite from Different Geological Setting.Earth Science,38(3):489-500(in Chinese with English abstract).
Windley,B.F.,1984.The Evolution Continents.John Wiley&Sons,Inc.,Chichester.
Wu,G.Y.,2006.Bitu Ophiolite in the Zogang Area,Eastern Tibet:Geological Records of Paleo-Tethyan Major Oceanic Basin.Geological Bulletin of China,25(6):685-693(in Chinese with English abstract).
Wu,H.Q.,Feng,Y.M.,Song,S.G.,1993.Metamorphic and Deformation of Blueschist Belts and Their Tectonic Implications,North Qilian Mountains,China.Journal of Metamorphic Geology,11(4):523-536.
Wu,Y.W.,Li,C.,Xie,C.M.,et al.,2013.Petrology,Geochemistry and Tectonic Significance of the Metamorphic Peridotites from Longmuco-Shuanghu Ophiolitic Mélange Belt,Tibet.Acta Geologica Sinica,87(2):426-439.
Xing,G.F.,Feng,Y.M.,Jin,G.D.,et al.,2015.The Instructions of Volcanic Tectonic Map in China(1∶2 500 000).Geological Publishing House,Beijing(in Chinese).
Xing,G.F.,Feng,Y.M.,Yu,M.G.,et al.,2017.The Volcanic Tectonic of China.Geological Publishing House,Beijing(in Chinese).
Xu,J.H.,Sun,S.,Wang,Q.C.,et al.,1998.Tectonic Facies of China(1∶4 000 000).Science Press,Beijing(in Chinese).
Yakubchuk,A.,Degtyarev,K.,Maslennikov,V.,et al.,2012.Tectonomagmatic Settings,Architecture,and Metallogeny of the Central Asian Copper Province.In:Hedenquist,J.W.,ed.,Geology and Genesis of the Major Copper Deposits and Districts of the World:A Tribute to Richard H.Sillitoe.Society of Economic Geologists,16:403-432.
Yin,H.F.,Zhang,K.X.,Wang,G.C.,et al.,1998.Method of Non-Wilson and Non-Smith Strata-Theory and Method of Orogenic Belt.Regional Geology of China,(Suppl.):1-9(in Chinese).
Zhai,M.G.,2013.The Main Old Lands in China and Assembly of Chinese Unified Continent.Science in China(Series D:Earth Sciences),43(10):1583-1606(in Chinese).
Zhai,Q.G.,Jahn,B.M.,Zhang,R.Y.,et al.,2011.Triassic Subduction of the Paleo-Tethys in Northern Tibet,China:Evidence from the Geochemical and Isotopic Characteristics of Eclogites and Blueschists of the Qiangtang Block.Journal of Asian Earth Sciences,42(6):1356-1370.
Zhai,Q.G.,Li,C.,2007.Zircon SHRIMP Dating of Volcanic Rock from the Nadigangri Formation in Juhuashan,Qiangtang,Northern Tibet and Its Geological Significance.Acta Geologica Sinica,81(6):795-800(in Chinese with English abstract).
Zhai,Q.G.,Li,C.,Cheng,L.R.,et al.,2004.Geological Features of Permian Ophiolite in the Jiaomuri Area,Qiangtang,Tibet,and Its Tectonic Significance.Geological Bulletin of China,23(12):1228-1230(in Chinese with English abstract).
Zhai,Q.G.,Li,C.,Wang,J.,et al.,2009.Petrology,Mineralogy and 40 Ar/39 Ar Chronology for Rongma Blueschist from Central Qiangtang,Northern Tibet.Acta Petrologica Sinica,25(9):2281-2288(in Chinese with English abstract).
Zhai,Q.G.,Wang,J.,Li,C.,et al.,2010.SHRIMP U-Pb Dating and Hf Isotopic Analyses of Middle Ordovician Meta-Cumulate Gabbro in Central Qiangtang,Northern Tibetan Plateau.Science in China(Series D:Earth Sciences),40(5):565-573(in Chinese).
Zhang,G.W.,Zhang,B.R.,Yuan,X.C.,et al.,2001.Qinling Orogenic Belt and Continental Dynamics.Science Press,Beijing(in Chinese).
Zhang,J.,Deng,J.F.,Xiao,Q.H.,et al.,2012.New Advances in the Study of Ophiolites.Geological Bulletin of China,31(1):1-12(in Chinese with English abstract).
Zhang,K.X.,He,W.H.,Luo,M.S.,et al.,2017.Evolution of Sedimentary Formation and Tectonics in China.Geological Publishing House,Beijing(in Chinese).
Zhang,K.X.,He,W.H.,Xu,Y.D.,et al.,2014.Subdivision and Identification of Sedimentary Tectonic Facies.Earth Science,39(8):915-928(in Chinese with English abstract).https://doi.org/10.3799/dqkx.2014.086
Zhang,K.X.,He,W.H.,Xu,Y.D.,et al.,2015.The Instructions of Sedimentary Tectonic Map in China(1∶2 500 000).Geological Publishing House,Beijing(in Chinese).
Zhang,K.X.,He,W.H.,Xu,Y.D.,et al.,2016.Palaeogeographic Distribution and Tectonic Evolution of OPS in China.Earth Science Frontiers,23(6):24-30(in Chinese with English abstract).
Zhang,K.X.,Lin,Q.X.,Zhu,Y.H.,et al.,2004.New Paleotological Evidence on Time Determination of the East Part of the Eastern Kunlun Melange and Its Tectonic Significance.Science in China(Series D:Earth Sciences),47(10):865-873.
Zhang,K.X.,Xu,Y.D.,He,W.H.,et al.,2018.Oceanic and Continental Blocks Distribution during Neoproterozoic Early Qingbaikouan Period(1 000-820 Ma)in China.Earth Science,43(11):3837-3852(in Chinese with English abstract).
Zhang,K.X.,Yin,H.F.,Zhu,Y.H.,et al.,2001.Geological Survey Theory,Method and Practice of Mélange Zone in Orogenic Belt.China University of Geosciences Press,Wuhan(in Chinese).
Zhang,Q.,Li,D.Z.,Zhang,K.W.,1985.Preliminary Study on Tongchangjie Ophiolite Melange from Yun County,Yunnan Province.Acta Petrologica Sinica,1(3):1-14(in Chinese with English abstract).
Zhang,W.B.,Ye,J.H.,2017.Geological Characteristics,OreForming Processes and Prospecting Potential of Cu-Au Deposits in the Circum-Pacific Metallogenic Domain.GeologicalBulletinofChina,36(1):1-15(in Chinese with English abstract).
Zhang,W.P.,Wang,L.Q.,Qiangba,Z.X.,et al.,2010.Discovery and P-T Path of High-Pressure Granulite in Tongka Area of Tibet and Its Tectonic Significance.Acta Petrologica Sinica,26(6):1915-1924(in Chinese with English abstract).
Zhao,G.C.,Wang,Y.J.,Huang,B.C.,et al.,2018.Geological Reconstructions of the East Asian Blocks:From the Breakup of Rodinia to the Assembly of Pangea.EarthScience Reviews,186:262-286.https://doi.org/10.1016/j.earscirev.2018.10.003
Zhu,Q.W.,Zhang,S.Q.,Tan,J.,1998.Geochemical Evidence of Volcanic Rocks for Determining the South Lancangjiang Suture Zone.Acta Petrologica et Mineralogica,17(4):296-307(in Chinese with English abstract).
邓晋福,冯艳芳,狄永军,等,2015.中国侵入岩大地构造图说明书(1∶2 500 000).北京:地质出版社.
邓晋福,冯艳芳,狄永军,等,2017.中国侵入岩大地构造.北京:地质出版社.
邓希光,丁林,刘小汉,等,2000.青藏高原羌塘中部冈玛日地区蓝闪石片岩及其40 Ar/39 Ar年代学.科学通报,45(21):2322-2326.
邓希光,丁林,刘小汉,等,2002.青藏高原羌塘中部蓝片岩的地球化学特征及其构造意义.岩石学报,18(4):517-525.
冯益民,张越,2018.大洋板块地层(OPS)简介及评述.地质通报,37(4):523-531.
高俊,钱青,龙灵利,2009.西天山的增生造山过程.地质通报,28(12):1804-1816.
耿全如,潘桂棠,王立全,等,2011.班公湖-怒江带、羌塘地块特提斯演化与成矿地质背景.地质通报,30(8):1261-1274.
郭令智,施央申,马瑞士,1983.西太平洋中、新生代活动大陆边缘和岛弧构造的形成及演化.地质学报,57(1):11-21.
侯增谦,王二七,2008.印度-亚洲大陆碰撞成矿作用主要研究进展.地球学报,29(3):275-292.
胡培远,李才,吴彦旺,等,2014.龙木错-双湖-澜沧江洋的打开时限:来自斜长花岗岩的制约.科学通报,59(20):1992-2003.
黄汲清,陈炳蔚,1987.中国及邻区特提斯海的演化.北京:地质出版社,71-74.
黄汲清,陈国铭,陈炳蔚,1984.特提斯-喜马拉雅构造域初步分析.地质学报,58(1):1-17.
江庆源,李才,解超明,等,2014.藏北羌塘冈玛错地区望果山组火山岩地球化学特征及LA-ICP-MS锆石U-Pb年龄.地质通报,33(11):1702-1714.
金振民,Green,H.W.,Borch,R.S.,等,1993.幔源包体和中国东部现代弧后地热标志.中国科学(B辑:化学),23(4):410-416.
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):155-166.
李才,程立人,张以春,等,2004.西藏羌塘南部发现奥陶纪-泥盆纪地层.地质通报,23(5-6):602-604.
李才,董永胜,翟庆国,等,2008.青藏高原羌塘中部早古生代蛇绿岩-堆晶辉长岩SHRIMP U-Pb定年及其构造意义.岩石学报,24(1):31-36.
李才,黄小鹏,翟庆国,等,2006.龙木错-双湖-吉塘板块缝合带与青藏高原冈瓦纳北界.地学前缘,13(4):136-147.
李才,谢尧武,董永胜,等,2009.藏东类乌齐一带吉塘岩群时代讨论及初步认识.地质通报,28(9):1178-1180.
李春昱,王荃,刘雪亚,等,1982.亚洲大地构造图(1∶800万)及说明书.北京:地质出版社.
李春昱,王荃,刘雪亚,等,1984.亚洲大地构造的演化.中国地质科学院院报,10:3-11.
李继亮,1992.碰撞造山带大地构造相.现代地质学文集(上).南京:南京大学出版社.
李锦轶,张进,王方国,等,2015.中国大型变形构造图说明书(1∶2 500 000).北京:地质出版社.
李三忠,索艳慧,郭玲莉,2017.海底构造原理.北京:科学出版社.
李三忠,杨朝,赵淑娟,等,2016.全球早古生代造山带(Ⅰ):碰撞型造山.吉林大学学报(地球科学版),46(4):945-967.
刘本培,冯庆来,方念乔,等,1993.滇西南昌宁-孟连带和澜沧江带古特提斯多岛洋构造演化.地球科学,18(5):529-539,671.
刘增乾,潘桂棠,郑海翔,1983.从地质新资料试论冈瓦纳北界及青藏高原地区特提斯的演变.见:青藏高原地质文集(12):“三江”构造地质.北京:地质出版社.
陆松年,郝国杰,王惠初,等,2015.中国变质岩大地构造图说明书(1∶2 500 000).北京:地质出版社.
陆松年,郝国杰,王惠初,等,2017.中国变质岩大地构造.北京:地质出版社.
莫宣学,2011.岩浆作用与青藏高原演化.高校地质学报,17(3):351-367.
莫宣学,潘桂棠,2006.从特提斯到青藏高原形成:构造-岩浆事件的约束.地学前缘,13(6):43-51.
莫宣学,赵志丹,邓晋福,等,2003.印度-亚洲大陆主碰撞过程的火山作用响应.地学前缘,10(3):135-148.
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.
潘桂棠,陆松年,肖庆辉,等,2016.中国大地构造阶段划分和演化.地学前缘,23(6):1-23.
潘桂棠,王立全,张万平,等,2013.青藏高原及邻区大地构造图及说明书(1∶1 500 000).北京:地质出版社.
潘桂棠,王立全,朱弟成,2004.青藏高原区域地质调查中几个重大科学问题的思考.地质通报,23(1):12-19.
潘桂棠,肖庆辉,陆松年,等,2008.大地构造相的定义、划分、特征及其鉴别标志.地质通报,27(10):1613-1637.
潘桂棠,肖庆辉,尹福光,等,2015.中国大地构造图说明书(1∶2 500 000).北京:地质出版社.
潘桂棠,郑海祥,徐耀荣,等,1983.初论班公湖-怒江结合带.北京:地质出版社.
彭兴阶,胡长寿,1993.藏东三江带的古构造演化.中国区域地质,(2):140-147.
任纪舜,肖黎薇,2004.1∶25万地质填图进一步揭开了青藏高原大地构造的神秘面纱.地质通报,23(1):1-11.
沈上越,冯庆来,刘本培,等,2002.昌宁-孟连带洋脊、洋岛型火山岩研究.地质科技情报,21(3):13-17.
孙晓明,石贵勇,熊德信,等,2007.云南哀牢山金矿带大坪金矿铂族元素(PGE)和Re-Os同位素地球化学及其矿床成因意义.地质学报,81(3):394-404.
王保弟,王立全,潘桂棠,等,2013.昌宁-孟连结合带南汀河早古生代辉长岩锆石年代学及地质意义.科学通报,58(4):344-354.
王保弟,王立全,许继峰,等,2015.班公湖-怒江结合带洞错地区舍拉玛高压麻粒岩的发现及其地质意义.地质通报,34(9):1605-1616.
王鸿祯,1985.中国古地理图集.北京:地图出版社.
王鸿祯,杨森楠,刘本培,等,1990.中国及邻区构造古地理与生物古地理.武汉:中国地质大学出版社.
王立全,潘桂棠,李才,等,2008.藏北羌塘中部果干加年山早古生代堆晶辉长岩的锆石SHRIMP U-Pb年龄---兼论原-古特提斯洋的演化.地质通报,27(12):2045-2056.
王立全,潘桂棠,李定谋,等,1999.金沙江弧-盆系时空结构及地史演化.地质学报,73(3):206-218.
汪洋,金振民,史峰,2013.不同大地构造背景橄榄岩结构水特征.地球科学,38(3):489-500.
吴根耀,2006.藏东左贡地区碧土蛇绿岩:古特提斯主洋盆的地质记录.地质通报,25(6):685-693.
邢光福,冯益民,靳国栋,等,2015.中国火山岩大地构造图说明书(1∶2 500 000).北京:地质出版社.
邢光福,冯益民,余明刚,等,2017.中国火山岩大地构造.北京:地质出版社.
许靖华,孙枢,王清晨,等,1998.中国大地构造相图(1∶4 000 000).北京:科学出版社.
殷鸿福,张克信,王国灿,等,1998.非威尔逊旋回与非史密斯方法---中国造山带研究理论与方法.中国区域地质,(增刊):1-9.
翟明国,2013.中国主要古陆与联合大陆的形成---综述与展望.中国科学(D辑:地球科学),43(10):1583-1606.
翟庆国,李才,2007.藏北羌塘菊花山那底岗日组火山岩锆石SHRIMP定年及其意义.地质学报,81(6):795-800.
翟庆国,李才,程立人,等,2004.西藏羌塘角木日地区二叠纪蛇绿岩的地质特征及意义.地质通报,23(12):1228-1230.
翟庆国,李才,王军,等,2009.藏北羌塘中部绒玛地区蓝片岩岩石学、矿物学和40 Ar/39 Ar年代学.岩石学报,25(9):2281-2288.
翟庆国,王军,李才,等,2010.青藏高原羌塘中部中奥陶世变质堆晶辉长岩锆石SHRIMP年代学及Hf同位素特征.中国科学(D辑:地球科学),40(5):565-573.
张国伟,张本仁,袁学诚,等,2001.秦岭造山带与大陆动力学.北京:科学出版社.
张进,邓晋福,肖庆辉,等,2012.蛇绿岩研究的最新进展.地质通报,31(1):1-12.
张克信,何卫红,骆满生,等,2017.中国沉积岩建造与沉积大地构造演化.北京:地质出版社.
张克信,何卫红,徐亚东,等,2014.沉积大地构造相划分与鉴别.地球科学,39(8):915-928.
张克信,何卫红,徐亚东,等,2015.中国沉积大地构造图说明书(1∶2 500 000).北京:地质出版社.
张克信,何卫红,徐亚东,等,2016.中国洋板块地层分布及构造演化.地学前缘,23(6):24-30.
张克信,徐亚东,何卫红,等,2018.中国新元古代青白口纪早期(1 000~820 Ma)洋陆分布.地球科学,43(11):3837-3852.
张克信,殷鸿福,朱云海,等,2001.造山带混杂岩区地质填图理论、方法与实践---以东昆仑造山带为例.武汉:中国地质大学出版社.
张旗,李达周,张魁武,1985.云南省云县铜厂街蛇绿混杂岩的初步研究.岩石学报,1(3):1-14.
张伟波,叶锦华,2017.环太平洋成矿域主要铜-金矿床地质特征、成矿作用及找矿潜力.地质通报,36(1):1-15.
张万平,王立全,强巴扎西,等,2010.西藏同卡地区高压麻粒岩的发现、PT轨迹及其大地构造意义.岩石学报,26(6):1915-1924.
朱勤文,张双全,谭劲,1998.确定南澜沧江缝合带的火山岩地球化学证据.岩石矿物学杂志,17(4):296-307.
Deng,J.F.,Feng,Y.F.,Di,Y.J.,et al.,2015.The Instructions of Intrusion Tectonic Map in China(1∶2 500 000).Geological Publishing House,Beijing(in Chinese).
Deng,J.F.,Feng,Y.F.,Di,Y.J.,et al.,2017.Intrusive Tectonic of China.Geological Publishing House,Beijing(in Chinese).
Deng,X.G.,Ding,L.,Liu,X.H.,et al.,2000.40 Ar/39 Ar Chronology for Gongrnarco Glaucophane Schist from Central Qiangtang,Tibet.Chinese Science Bulletin,45(21):2322-2326(in Chinese).
Deng,X.G.,Ding,L.,Liu,X.H.,et al.,2002.Geochemical Characteristics of the Blueschists and Its Tectonic Significance in the Central Qiangtang Area,Tibet.Acta Petrologica Sinica,18(4):517-525(in Chinese with English abstract).
Feng,Y.M.,Zhang,Y.,2018.Introduction and Commentary on Ocean Plate Stratigrapgy.Geological Bulletin of China,37(4):523-531(in Chinese with English abstract).
Gao,J.,Qian,Q.,Long,L.L.,et al.,2009.Accretionary Orogenic Process of Western Tianshan,China.Geological Bulletin of China,28(12):1804-1816(in Chinese with English abstract).
Geng,Q.R.,Pan,G.T.,Wang,L.Q.,et al.,2011.Tethyan Evolution and Metallogenic Geological Background of the Bangong Co-Nujiang Belt and the Qiangtang Massif in Tibet.Geological Bulletin of China,30(8):1261-1274(in Chinese with English abstract).
Greenly,E.,1919.The Geology of Anglesey.Memoir of the Geological Survey of the U.K.,2:980.
Guo,L.Z.,Shi,Y.S.,Ma,R.S.,1983.On the Formation and Evolution of the Mesozoic-Cenozoic Active Continental Margin and Island Arc Tectonics of the Western Pacific Ocean.Acta Geologica Sinica,57(1):11-21(in Chinese with English abstract).
Hamilton,W.B.,1978.Tectonic Map of the Indonesian Region(1∶5 000 000).USGS Map I-875-D.
Hou,Z.Q.,Wang,E.Q.,2008.Metallogenesis of the Indo-Asian Collisional Orogen:New Advances.Acta Geoscientica Sinica,29(3):275-292(in Chinese with English abstract).
Hou,Z.Q.,Zhong,D.L.,Deng,W.M.,et al.,2005.A Tectonic Model for Porphyry Copper-Molybdenum-Gold Deposits in the Eastern Indo-Asian Collision Zone.In:Porter,T.M.,ed.,Super Porphyry Copper&Gold Deposits-A Global Perspective.PGC Publishing,Adelaide,423-440.
Hsü,K.J.,1968.Principles of Mélanges and Their Bearing on the Franciscan-Knoxville Paradox.Geological Society of America Bulletin,79(8):1063-1074.https://doi.org/10.1130/0016-7606(1968)79[1063:pomatb]2.0.co;2
Hsü,K.J.,Pan,G.T.,?eng?r,A.M.C.,et al.,1995.Tectonic Evolution of the Tibetan Plateau:A Working Hypothesis Based on the Archipelago Model of Orogenesis.International Geology Review,37:473-508.
Hu,P.Y.,Li,C.,Wu,Y.W.,et al.,2014.Opening of the Longmu Co-Shuanghu-Lancangjiang Ocean:Constraints from Plagiogranites.Chinese Science Bulletin,59(20):1992-2003(in Chinese).
Huang,J.Q.,Chen,B.W.,1987.Evolution of the Tethys Sea from China and Its Adjacent Areas.Geological Publishing House,Beijing(in Chinese).
Huang,J.Q.,Chen,G.M.,Chen,B.W.,1984.Preliminary Analysis of the Tethy-Himalayan Tectonic Domain.Acta Geologica Sinica,58(1):1-17(in Chinese with English abstract).
Isozaki,Y.,Maruyama,S.,Furuoka,F.,1990.Accreted Oceanic Materials in Japan.Tectonophysics,181(1-4):179-205.https://doi.org/10.1016/0040-1951(90)90016-2
Jian,P.,Liu,D.Y.,Kr9ner,A.,et al.,2010.Evolution of a Permian Intraoceanic Arc-Trench System in the Solonker Suture Zone,Central Asian Orogenic Belt,China and Mongolia.Lithos,118(1-2):169-190.https://doi.org/10.1016/j.lithos.2010.04.014
Jiang,Q.Y.,Li,C.,Su,L.,et al.,2015.Carboniferous Arc Magmatism in the Qiangtang Area,Northern Tibet:Zircon U-Pb Ages,Geochemical and Lu-Hf Isotopic Characteristics,and Tectonic Implications.Journal of Asian Earth Sciences,100:132-144.https://doi.org/10.1016/j.jseaes.2015.01.012
Jiang,Q.Y.,Li,C.,Xie,C.M.,et al.,2014.Geochemistry and LA-ICP-MS Zircon U-Pb Age of Volcanic Rocks of Wangguoshan Formation in the Gangmar Co Area of Qiangtang,Tibet.Geological Bulletin of China,33(11):1702-1714(in Chinese with English abstract).
Jin,Z.M.,GreenⅡ,H.W.,Borch,R.S.,et al.,1993.Mantle Xenolith and Mark of Geothermal from Back-Arc in Eastern China.Science in China(Series B:Chemistry),23(4):410-416(in Chinese).
Kapp,P.,Yin,A.,Manning,C.E.,et al.,2000.BlueschistBearing Metamorphic Core Complexes in the Qiangtang Block Reveal Deep Crustal Structure of Northern Tibet.Geology,28(1):19-22.https://doi.org/10.1130/0091-7613(2000)028<0019:bbmcci>2.3.co;2
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
Karig,D.E.,1983.Temporal Relationships between Back-Arc Basin Formation and Arc Volcanism with Special Reference to the Philippinesea.Geophysical Monograph Series,27:318-325.
Kroner,A.,2015.The Central Asian Orogenic Belt.Bornttaeger Science Publishers,Suttgart.
Kusky,T.M.,Windley,B.F.,Safonova,I.,et al.,2013.Recognition of Ocean Plate Stratigraphy in Accretionary Orogens through Earth History:A Record of 3.8Billion Years of Sea Floor Spreading,Subduction,and Accretion.Gondwana Research,24(2):501-547.https://doi.org/10.1016/j.gr.2013.01.004
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):155-166(in Chinese with English abstract).
Li,C.,Cheng,L.R.,Zhang,Y.C.,et al.,2004.Discovery of Ordovician-Devonian Strata in the South of the Qiangtang Area,Tibet.Geological Bulletin of China,23(5-6):602-604(in Chinese with English abstract).
Li,C.,Dong,Y.S.,Zhai,Q.G.,et al.,2008.Discovery of Eopaleozoic Ophiolite in the Qiangtang of Tibet Plateau:Evidence from SHRIMP U-Pb Dating and Its Tectonic Implications.Acta Petrologica Sinica,24(1):31-36(in Chinese with English abstract).
Li,C.,Huang,X.P,Zhai,Q.G.,et al.,2006.The Longmu CoShuanghu-Jitang Plate Suture and the Northern Boundary of Gondwanaland in the Qinghai-Tibet Plateau.Earth Science Frontiers,13(4):136-147(in Chinese with English abstract).
Li,C.,Xie,Y.W.,Dong,Y.S.,et al.,2009.Discussion on the Age of Jitang Group around Leiwuqi Area,Eastern Tibet,China and Primary Understanding.Geological Bulletin of China,28(9):1178-1180(in Chinese with English abstract).
Li,C.Y.,Wang,Q.,Liu,X.Y.,et al.,1982.The Instructions of Asian Tectonic Map in China(1∶800 000).Geological Publishing House,Beijing(in Chinese).
Li,C.Y.,Wang,Q.,Liu,X.Y.,et al.,1984.Tectonic Evolution of Asia.Bulletin of the Chinese Academy of Geological Sciences,10:3-11(in Chinese with English abstract).
Li,J.L.,1992.Collision Orogenic Belt Geotectonic Facies.Modern Geology(Part I).Nanjing University Press,Nanjing(in Chinese).
Li,J.Y.,Zhang,J.,Wang,F.G.,et al.,2015.The Instructions of Deformation Tectonic Map in China(1∶2 500 000).Geological Publishing House,Beijing(in Chinese).
Li,J.Y.,Zhang,J.,Zhao,X.X.,et al.,2016.Mantle Subduction and Uplift of Intracontinental Mountains:A Case Study from the Chinese Tianshan Mountains within Eurasia.Scientific Reports,6:28831.
Li,S.Z.,Suo,Y.H.,Guo,L.L.,et al.,2017.Principles of Submarine Tectonics.Science Press,Beijing(in Chinese).
Li,S.Z.,Yang,Z.,Zhao,S.J.,et al.,2016.Global Early Paleozoic Orogens(Ⅰ):Collision-Type Orogeny.Journal of Jilin University(Earth Science Edition),46(4):945-967(in Chinese with English abstract).
Liu,B.P.,Feng,Q.L.,Fang,N.Q.,et al.,1993.Tectonic Evolution of Palaeo-Tethys Poly-Island-Ocean in Changning-Menglian and Langcangjiang Belts,Southwestern Yunnan,China.Earth Science,18(5):529-539,671(in Chinese with English abstract).
Liu,Z.Q.,Pan,G.T.,Zheng,H.X.,1983.A Preliminary Study on the North Boundary and the Evolution of Gondwana and Tethys in Light of the New Data on Qinghai-Xizang(Tibet)Plateau.In:Geological Anthology of QinghaiTibet Plateau(12):“Three Rivers”Tectonic Geology.Geological Publishing House,Beijing(in Chinese).
Lu,S.N.,Hao,G.J.,Wang,H.C.,et al.,2015.The Instructions of Metamorphite Tectonic Map in China(1∶2 500 000).Geological Publishing House,Beijing(in Chinese).
Lu,S.N.,Hao,G.J.,Wang,H.C.,et al.,2017.Metamorphite Tectonic of China.Geological Publishing House,Beijing(in Chinese).
McCall,G.J.H.,Kidd,R.G.W.,1982.The Makran,Southeastern Iran:The Anatomy of a Convergent Plate Margin Active from Cretaceous to Present.Geological Society,London,Special Publications,10(1):387-397.https://doi.org/10.1144/gsl.sp.1982.010.01.26
Mo,X.X.,2011.Magmatism and Evolution of the Tibetan Plateau.Geological Journal of China Universities,17(3):351-367(in Chinese with English abstract).
Mo,X.X.,Pan,G.T.,2006.From the Tethys to the Formation of the Qinghai-Tibet Plateau:Constrained by Tectono-Magmatic Events.EarthScienceFrontiers,13(6):43-51(in Chinese with English abstract).
Mo,X.X.,Zhao,Z.D.,Deng,J.F.,et al.,2003.Response of Volcanism to the India-Asia Collision.Earth Science Frontiers,10(3):135-148(in Chinese with English abstract).
Myhill,R.,2011.Constraints on the Evolution of the Mesohellenic Ophiolite from Subophiolitic Metamorphic Rocks.The Geological Society of America,Special Paper,480:75-94.
Ogawa,Y.,1985.Variety of Subduction and Accretion Processes in Cretaceous to Recent Plate Boundaries around Southwest and Central Japan.Tectonophysics,112(1-4):493-518.https://doi.org/10.1016/0040-1951(85)90192-1
Ogawa,Y.,Taniguchi,H.,1987.Ophiolitic Mélange in Forearc Area and Formation of the Mineoka Belt:Kyushu University,Japan.Science Reports,Geology,15:1-23.
Pan,G.T.,Chen,Z.L.,Li,X.L.,et al.,1997.Tectonic Formation Evolution of East Tethys Geology.Geological Publishing House,Beijing(in Chinese).
Pan,G.T.,Lu,S.N.,Xiao,Q.H.,et al.,2016.Division of Tectonic Stages and Tectonic Evolution in China.Earth Science Frontiers,23(6):1-23(in Chinese with English abstract).
Pan,G.T.,Wang,L.Q.,Li,R.S.,et al.,2012.Tectonic Evolution of the Qinghai-Tibet Plateau.Journal of Asian Earth Sciences,53:3-14.https://doi.org/10.1016/j.jseaes.2011.12.018
Pan,G.T.,Wang,L.Q.,Zhang,W.P.,et al.,2013.The Instructions of Tectonic Map in Qinghai-Tibet Plateau and Its Adjacent Areas(1∶1 500 000).Geological Publishing House,Beijing(in Chinese).
Pan,G.T.,Wang,L.Q.,Zhu,D.C.,2004.Thoughts on Some Important Scientific Problems in Regional Geological Survey of the Qinghai-Tibet Plateau.Geological Bulletin of China,23(1):12-19(in Chinese with English abstract).
Pan,G.T.,Xian,Q.H.,Yin,F.G.,et al.,2015.The Instructions of Tectonic Map in China(1∶2 500 000).Geological Publishing House,Beijing(in Chinese).
Pan,G.T.,Xiao,Q.H.,Lu,S.N.,et al.,2008.Definition,Classification,Characteristics and Diagnostic Indications of Tectonic Facies.Geological Bulletin of China,27(10):1613-1637(in Chinese with English abstract).
Pan,G.T.,Zheng,H.X.,Xu,Y.R.,et al.,1983.A Priliminary Study of Bangongco-Nujiang Suture.Geological Publishing House,Beijing(in Chinese).
Peng,X.J.,Hu,C.C.,1993.Tectonic Evolution of the Sanjiang Belt in Eastern Tibet.Regional Geology of China,(2):140-148(in Chinese with English abstract).
Ren,J.S.,Xiao,L.W.,2004.Lifting the Mysterious Veil of the Tectonics of the Qinghai-Tibet Plateau by 1∶250 000Geological Mapping.Geological Bulletin of China,23(1):1-11(in Chinese with English abstract).
Revan,M.K.,Gen9,Y.,Maslennikov,V.V.,et al.,2014.Mineralogy and Trace-Element Geochemistry of Sulfide Minerals in Hydrothermal Chimneys from the Upper-Cretaceous VMSDeposits of the Eastern Pontide Orogenic Belt(NE Turkey).Ore Geology Reviews,63:129-149.https://doi.org/10.1016/j.oregeorev.2014.05.006
Reymond,M.C.,1975.Mechanism of Brittle Fracture of Rock during Uniaxial Compression in Laboratory and in a Quarry by an Acoustic Emission Technique.International Journal of Rock Mechanics and Mining Sciences&Geomechanics Abstracts,12(7):89.https://doi.org/10.1016/0148-9062(75)90377-0
Robertson,A.H.F.,1994.Role of the Tectonic Facies Concept in Orogenic Analysis and Its Application to Tethys in the Eastern Mediterranean Region.Earth-Science Reviews,37(3-4):139-213.https://doi.org/10.1016/0012-8252(94)90028-0
Safonova,I.,Kojima,S.,Nakae,S.,et al.,2014.Oceanic Island Basalts in Accretionary Complexes of SW Japan:Tectonic and Petrogenetic Implications.Journal of Asian Earth Sciences,113(SI):508-523.https://dx.doi.org/10.1016/j.jseaes.2014.09.015
Saleeby,J.B.,2011.Geochemical Mapping of the KingsKaweah Ophiolite Belt,California-Evidence for Progressive Mélange Formation in a Large Offset Transform-Subduction Initiation Environment.The Geological Society of America,480:31-73.
Shen,S.Y.,Feng,Q.L.,Liu,B.P.,et al.,2002.Study on Ocean Ridge,Ocean Island Volcanic Rocks of Changning-Menglian Belt.Geological Science and Technology Information,21(3):13-17(in Chinese with English abstract).
Sillitoe,R.H.,2013.Metallogenic and Regulatory Inequalities around the Northern Pacific Rim:Implications for Discovery.Society of Economic Geologists,Inc.,Special Publication,17:1-16.
Silver,E.A.,Beutner,E.C.,1980.Mélanges.Geology,8:32-34.
Simandjuntak,T.O.,Barber,A.J.,1996.Contrasting Tectonic Styles in the Neogene Orogenic Belts of Indonesia.Geological Society,London,Special Publications,106(1):185-201.https://doi.org/10.1144/gsl.sp.1996.106.01.12
Sun,X.M.,Shi,G.Y.,Xiong,D.X.,et al.,2007.Platinum Group Elements Geochemistry and Re-Os Isotopic Compositions of Daping Gold Deposit in Ailaoshan Gold Belt,Yunnan Province,China and Their Metallogenic Implications.Acta Geologica Sinica,81(3):394-404(in Chinese with English abstract).
von Huene,R.,Scholl,D.W.,1991.Observations at Convergent Margins Concerning Sediment Subduction,Subduction Erosion,and the Growth of Continental Crust.Reviews of Geophysics,29(3):279.https://doi.org/10.1029/91rg00969
Wakabayashi,J.,Dilek,Y.,2011.Mélanges:Processes of Formation and Societal Significance.The Geological Society of America,Special Paper,480(4):279.
Wakita,K.,2012.Mappable Features of Mélanges Derived from Ocean Plate Stratigraphy in the Jurassic Accretionary Complexes of Mino and Chichibu Terranes in Southwest Japan.Tectonophysics,568-569:74-85.
Wang,B.D.,Wang,L.Q.,Pan,G.T.,et al.,2013.U-Pb Zircon Dating of Early Paleozoic Gabbro from the Nantinghe Ophiolite in the Changning-Menglian Suture Zone and Its Geological Implication.Chinese Science Bulletin,58(4):344-354(in Chinese).
Wang,B.D.,Wang,L.Q.,Xu,J.F.,et al.,2015.The Discovery of High-Pressure Granulite at Shelama in Dongco Area along the Bangongco-Nujiang River Suture Zone and Its Tectonic Significance.Geological Bulletin of China,34(9):1605-1616(in Chinese with English abstract).
Wang,H.Z.,1985.Atlas of the Palaeogeography of China.SinoMaps Press,Beijing(in Chinese).
Wang,H.Z.,Yang,S.N.,Liu,B.P.,et al.,1990.TectonoPalaeogeography and Palaeobiogeography of China and Adjacent Regions.China University of Geosciences Press,Wuhan(in Chinese).
Wang,L.Q.,Pan,G.T.,Li,C.,et al.,2008.SHRIMP U-Pb Zircon Dating of Eopaleozoic Cumulate in Guoganjianian Mt.from Central Qiangtang Area of Northern TibetConsidering the Evolvement of Proto-and PaleoTethys.Geological Bulletin of China,27(12):2045-2056(in Chinese with English abstract).
Wang,L.Q.,Pan,G.T.,Li,D.M.,et al.,1999.The SpatioTemporal Framework and Geological Evolution of the Jinshajiang Arc-Basin Systems.Acta Geologica Sinica,73(3):206-218(in Chinese with English abstract).
Wang,S.D.,Zhang,K.X.,Song,B.W.,et al.,2018.Geochronology and Geochemistry of the Niujuanzi Ophiolitic Mélange,Gansu Province,NW China:Implications for Tectonic Evolution of the Beishan Orogenic College.International Journal of Earth Sciences,107(1):269-289.
Wang,Y.,Jin,Z.M.,Shi,F.,2013.Characteristics of Hydroxyl in Lherzolite from Different Geological Setting.Earth Science,38(3):489-500(in Chinese with English abstract).
Windley,B.F.,1984.The Evolution Continents.John Wiley&Sons,Inc.,Chichester.
Wu,G.Y.,2006.Bitu Ophiolite in the Zogang Area,Eastern Tibet:Geological Records of Paleo-Tethyan Major Oceanic Basin.Geological Bulletin of China,25(6):685-693(in Chinese with English abstract).
Wu,H.Q.,Feng,Y.M.,Song,S.G.,1993.Metamorphic and Deformation of Blueschist Belts and Their Tectonic Implications,North Qilian Mountains,China.Journal of Metamorphic Geology,11(4):523-536.
Wu,Y.W.,Li,C.,Xie,C.M.,et al.,2013.Petrology,Geochemistry and Tectonic Significance of the Metamorphic Peridotites from Longmuco-Shuanghu Ophiolitic Mélange Belt,Tibet.Acta Geologica Sinica,87(2):426-439.
Xing,G.F.,Feng,Y.M.,Jin,G.D.,et al.,2015.The Instructions of Volcanic Tectonic Map in China(1∶2 500 000).Geological Publishing House,Beijing(in Chinese).
Xing,G.F.,Feng,Y.M.,Yu,M.G.,et al.,2017.The Volcanic Tectonic of China.Geological Publishing House,Beijing(in Chinese).
Xu,J.H.,Sun,S.,Wang,Q.C.,et al.,1998.Tectonic Facies of China(1∶4 000 000).Science Press,Beijing(in Chinese).
Yakubchuk,A.,Degtyarev,K.,Maslennikov,V.,et al.,2012.Tectonomagmatic Settings,Architecture,and Metallogeny of the Central Asian Copper Province.In:Hedenquist,J.W.,ed.,Geology and Genesis of the Major Copper Deposits and Districts of the World:A Tribute to Richard H.Sillitoe.Society of Economic Geologists,16:403-432.
Yin,H.F.,Zhang,K.X.,Wang,G.C.,et al.,1998.Method of Non-Wilson and Non-Smith Strata-Theory and Method of Orogenic Belt.Regional Geology of China,(Suppl.):1-9(in Chinese).
Zhai,M.G.,2013.The Main Old Lands in China and Assembly of Chinese Unified Continent.Science in China(Series D:Earth Sciences),43(10):1583-1606(in Chinese).
Zhai,Q.G.,Jahn,B.M.,Zhang,R.Y.,et al.,2011.Triassic Subduction of the Paleo-Tethys in Northern Tibet,China:Evidence from the Geochemical and Isotopic Characteristics of Eclogites and Blueschists of the Qiangtang Block.Journal of Asian Earth Sciences,42(6):1356-1370.
Zhai,Q.G.,Li,C.,2007.Zircon SHRIMP Dating of Volcanic Rock from the Nadigangri Formation in Juhuashan,Qiangtang,Northern Tibet and Its Geological Significance.Acta Geologica Sinica,81(6):795-800(in Chinese with English abstract).
Zhai,Q.G.,Li,C.,Cheng,L.R.,et al.,2004.Geological Features of Permian Ophiolite in the Jiaomuri Area,Qiangtang,Tibet,and Its Tectonic Significance.Geological Bulletin of China,23(12):1228-1230(in Chinese with English abstract).
Zhai,Q.G.,Li,C.,Wang,J.,et al.,2009.Petrology,Mineralogy and 40 Ar/39 Ar Chronology for Rongma Blueschist from Central Qiangtang,Northern Tibet.Acta Petrologica Sinica,25(9):2281-2288(in Chinese with English abstract).
Zhai,Q.G.,Wang,J.,Li,C.,et al.,2010.SHRIMP U-Pb Dating and Hf Isotopic Analyses of Middle Ordovician Meta-Cumulate Gabbro in Central Qiangtang,Northern Tibetan Plateau.Science in China(Series D:Earth Sciences),40(5):565-573(in Chinese).
Zhang,G.W.,Zhang,B.R.,Yuan,X.C.,et al.,2001.Qinling Orogenic Belt and Continental Dynamics.Science Press,Beijing(in Chinese).
Zhang,J.,Deng,J.F.,Xiao,Q.H.,et al.,2012.New Advances in the Study of Ophiolites.Geological Bulletin of China,31(1):1-12(in Chinese with English abstract).
Zhang,K.X.,He,W.H.,Luo,M.S.,et al.,2017.Evolution of Sedimentary Formation and Tectonics in China.Geological Publishing House,Beijing(in Chinese).
Zhang,K.X.,He,W.H.,Xu,Y.D.,et al.,2014.Subdivision and Identification of Sedimentary Tectonic Facies.Earth Science,39(8):915-928(in Chinese with English abstract).https://doi.org/10.3799/dqkx.2014.086
Zhang,K.X.,He,W.H.,Xu,Y.D.,et al.,2015.The Instructions of Sedimentary Tectonic Map in China(1∶2 500 000).Geological Publishing House,Beijing(in Chinese).
Zhang,K.X.,He,W.H.,Xu,Y.D.,et al.,2016.Palaeogeographic Distribution and Tectonic Evolution of OPS in China.Earth Science Frontiers,23(6):24-30(in Chinese with English abstract).
Zhang,K.X.,Lin,Q.X.,Zhu,Y.H.,et al.,2004.New Paleotological Evidence on Time Determination of the East Part of the Eastern Kunlun Melange and Its Tectonic Significance.Science in China(Series D:Earth Sciences),47(10):865-873.
Zhang,K.X.,Xu,Y.D.,He,W.H.,et al.,2018.Oceanic and Continental Blocks Distribution during Neoproterozoic Early Qingbaikouan Period(1 000-820 Ma)in China.Earth Science,43(11):3837-3852(in Chinese with English abstract).
Zhang,K.X.,Yin,H.F.,Zhu,Y.H.,et al.,2001.Geological Survey Theory,Method and Practice of Mélange Zone in Orogenic Belt.China University of Geosciences Press,Wuhan(in Chinese).
Zhang,Q.,Li,D.Z.,Zhang,K.W.,1985.Preliminary Study on Tongchangjie Ophiolite Melange from Yun County,Yunnan Province.Acta Petrologica Sinica,1(3):1-14(in Chinese with English abstract).
Zhang,W.B.,Ye,J.H.,2017.Geological Characteristics,OreForming Processes and Prospecting Potential of Cu-Au Deposits in the Circum-Pacific Metallogenic Domain.GeologicalBulletinofChina,36(1):1-15(in Chinese with English abstract).
Zhang,W.P.,Wang,L.Q.,Qiangba,Z.X.,et al.,2010.Discovery and P-T Path of High-Pressure Granulite in Tongka Area of Tibet and Its Tectonic Significance.Acta Petrologica Sinica,26(6):1915-1924(in Chinese with English abstract).
Zhao,G.C.,Wang,Y.J.,Huang,B.C.,et al.,2018.Geological Reconstructions of the East Asian Blocks:From the Breakup of Rodinia to the Assembly of Pangea.EarthScience Reviews,186:262-286.https://doi.org/10.1016/j.earscirev.2018.10.003
Zhu,Q.W.,Zhang,S.Q.,Tan,J.,1998.Geochemical Evidence of Volcanic Rocks for Determining the South Lancangjiang Suture Zone.Acta Petrologica et Mineralogica,17(4):296-307(in Chinese with English abstract).
邓晋福,冯艳芳,狄永军,等,2015.中国侵入岩大地构造图说明书(1∶2 500 000).北京:地质出版社.
邓晋福,冯艳芳,狄永军,等,2017.中国侵入岩大地构造.北京:地质出版社.
邓希光,丁林,刘小汉,等,2000.青藏高原羌塘中部冈玛日地区蓝闪石片岩及其40 Ar/39 Ar年代学.科学通报,45(21):2322-2326.
邓希光,丁林,刘小汉,等,2002.青藏高原羌塘中部蓝片岩的地球化学特征及其构造意义.岩石学报,18(4):517-525.
冯益民,张越,2018.大洋板块地层(OPS)简介及评述.地质通报,37(4):523-531.
高俊,钱青,龙灵利,2009.西天山的增生造山过程.地质通报,28(12):1804-1816.
耿全如,潘桂棠,王立全,等,2011.班公湖-怒江带、羌塘地块特提斯演化与成矿地质背景.地质通报,30(8):1261-1274.
郭令智,施央申,马瑞士,1983.西太平洋中、新生代活动大陆边缘和岛弧构造的形成及演化.地质学报,57(1):11-21.
侯增谦,王二七,2008.印度-亚洲大陆碰撞成矿作用主要研究进展.地球学报,29(3):275-292.
胡培远,李才,吴彦旺,等,2014.龙木错-双湖-澜沧江洋的打开时限:来自斜长花岗岩的制约.科学通报,59(20):1992-2003.
黄汲清,陈炳蔚,1987.中国及邻区特提斯海的演化.北京:地质出版社,71-74.
黄汲清,陈国铭,陈炳蔚,1984.特提斯-喜马拉雅构造域初步分析.地质学报,58(1):1-17.
江庆源,李才,解超明,等,2014.藏北羌塘冈玛错地区望果山组火山岩地球化学特征及LA-ICP-MS锆石U-Pb年龄.地质通报,33(11):1702-1714.
金振民,Green,H.W.,Borch,R.S.,等,1993.幔源包体和中国东部现代弧后地热标志.中国科学(B辑:化学),23(4):410-416.
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):155-166.
李才,程立人,张以春,等,2004.西藏羌塘南部发现奥陶纪-泥盆纪地层.地质通报,23(5-6):602-604.
李才,董永胜,翟庆国,等,2008.青藏高原羌塘中部早古生代蛇绿岩-堆晶辉长岩SHRIMP U-Pb定年及其构造意义.岩石学报,24(1):31-36.
李才,黄小鹏,翟庆国,等,2006.龙木错-双湖-吉塘板块缝合带与青藏高原冈瓦纳北界.地学前缘,13(4):136-147.
李才,谢尧武,董永胜,等,2009.藏东类乌齐一带吉塘岩群时代讨论及初步认识.地质通报,28(9):1178-1180.
李春昱,王荃,刘雪亚,等,1982.亚洲大地构造图(1∶800万)及说明书.北京:地质出版社.
李春昱,王荃,刘雪亚,等,1984.亚洲大地构造的演化.中国地质科学院院报,10:3-11.
李继亮,1992.碰撞造山带大地构造相.现代地质学文集(上).南京:南京大学出版社.
李锦轶,张进,王方国,等,2015.中国大型变形构造图说明书(1∶2 500 000).北京:地质出版社.
李三忠,索艳慧,郭玲莉,2017.海底构造原理.北京:科学出版社.
李三忠,杨朝,赵淑娟,等,2016.全球早古生代造山带(Ⅰ):碰撞型造山.吉林大学学报(地球科学版),46(4):945-967.
刘本培,冯庆来,方念乔,等,1993.滇西南昌宁-孟连带和澜沧江带古特提斯多岛洋构造演化.地球科学,18(5):529-539,671.
刘增乾,潘桂棠,郑海翔,1983.从地质新资料试论冈瓦纳北界及青藏高原地区特提斯的演变.见:青藏高原地质文集(12):“三江”构造地质.北京:地质出版社.
陆松年,郝国杰,王惠初,等,2015.中国变质岩大地构造图说明书(1∶2 500 000).北京:地质出版社.
陆松年,郝国杰,王惠初,等,2017.中国变质岩大地构造.北京:地质出版社.
莫宣学,2011.岩浆作用与青藏高原演化.高校地质学报,17(3):351-367.
莫宣学,潘桂棠,2006.从特提斯到青藏高原形成:构造-岩浆事件的约束.地学前缘,13(6):43-51.
莫宣学,赵志丹,邓晋福,等,2003.印度-亚洲大陆主碰撞过程的火山作用响应.地学前缘,10(3):135-148.
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.
潘桂棠,陆松年,肖庆辉,等,2016.中国大地构造阶段划分和演化.地学前缘,23(6):1-23.
潘桂棠,王立全,张万平,等,2013.青藏高原及邻区大地构造图及说明书(1∶1 500 000).北京:地质出版社.
潘桂棠,王立全,朱弟成,2004.青藏高原区域地质调查中几个重大科学问题的思考.地质通报,23(1):12-19.
潘桂棠,肖庆辉,陆松年,等,2008.大地构造相的定义、划分、特征及其鉴别标志.地质通报,27(10):1613-1637.
潘桂棠,肖庆辉,尹福光,等,2015.中国大地构造图说明书(1∶2 500 000).北京:地质出版社.
潘桂棠,郑海祥,徐耀荣,等,1983.初论班公湖-怒江结合带.北京:地质出版社.
彭兴阶,胡长寿,1993.藏东三江带的古构造演化.中国区域地质,(2):140-147.
任纪舜,肖黎薇,2004.1∶25万地质填图进一步揭开了青藏高原大地构造的神秘面纱.地质通报,23(1):1-11.
沈上越,冯庆来,刘本培,等,2002.昌宁-孟连带洋脊、洋岛型火山岩研究.地质科技情报,21(3):13-17.
孙晓明,石贵勇,熊德信,等,2007.云南哀牢山金矿带大坪金矿铂族元素(PGE)和Re-Os同位素地球化学及其矿床成因意义.地质学报,81(3):394-404.
王保弟,王立全,潘桂棠,等,2013.昌宁-孟连结合带南汀河早古生代辉长岩锆石年代学及地质意义.科学通报,58(4):344-354.
王保弟,王立全,许继峰,等,2015.班公湖-怒江结合带洞错地区舍拉玛高压麻粒岩的发现及其地质意义.地质通报,34(9):1605-1616.
王鸿祯,1985.中国古地理图集.北京:地图出版社.
王鸿祯,杨森楠,刘本培,等,1990.中国及邻区构造古地理与生物古地理.武汉:中国地质大学出版社.
王立全,潘桂棠,李才,等,2008.藏北羌塘中部果干加年山早古生代堆晶辉长岩的锆石SHRIMP U-Pb年龄---兼论原-古特提斯洋的演化.地质通报,27(12):2045-2056.
王立全,潘桂棠,李定谋,等,1999.金沙江弧-盆系时空结构及地史演化.地质学报,73(3):206-218.
汪洋,金振民,史峰,2013.不同大地构造背景橄榄岩结构水特征.地球科学,38(3):489-500.
吴根耀,2006.藏东左贡地区碧土蛇绿岩:古特提斯主洋盆的地质记录.地质通报,25(6):685-693.
邢光福,冯益民,靳国栋,等,2015.中国火山岩大地构造图说明书(1∶2 500 000).北京:地质出版社.
邢光福,冯益民,余明刚,等,2017.中国火山岩大地构造.北京:地质出版社.
许靖华,孙枢,王清晨,等,1998.中国大地构造相图(1∶4 000 000).北京:科学出版社.
殷鸿福,张克信,王国灿,等,1998.非威尔逊旋回与非史密斯方法---中国造山带研究理论与方法.中国区域地质,(增刊):1-9.
翟明国,2013.中国主要古陆与联合大陆的形成---综述与展望.中国科学(D辑:地球科学),43(10):1583-1606.
翟庆国,李才,2007.藏北羌塘菊花山那底岗日组火山岩锆石SHRIMP定年及其意义.地质学报,81(6):795-800.
翟庆国,李才,程立人,等,2004.西藏羌塘角木日地区二叠纪蛇绿岩的地质特征及意义.地质通报,23(12):1228-1230.
翟庆国,李才,王军,等,2009.藏北羌塘中部绒玛地区蓝片岩岩石学、矿物学和40 Ar/39 Ar年代学.岩石学报,25(9):2281-2288.
翟庆国,王军,李才,等,2010.青藏高原羌塘中部中奥陶世变质堆晶辉长岩锆石SHRIMP年代学及Hf同位素特征.中国科学(D辑:地球科学),40(5):565-573.
张国伟,张本仁,袁学诚,等,2001.秦岭造山带与大陆动力学.北京:科学出版社.
张进,邓晋福,肖庆辉,等,2012.蛇绿岩研究的最新进展.地质通报,31(1):1-12.
张克信,何卫红,骆满生,等,2017.中国沉积岩建造与沉积大地构造演化.北京:地质出版社.
张克信,何卫红,徐亚东,等,2014.沉积大地构造相划分与鉴别.地球科学,39(8):915-928.
张克信,何卫红,徐亚东,等,2015.中国沉积大地构造图说明书(1∶2 500 000).北京:地质出版社.
张克信,何卫红,徐亚东,等,2016.中国洋板块地层分布及构造演化.地学前缘,23(6):24-30.
张克信,徐亚东,何卫红,等,2018.中国新元古代青白口纪早期(1 000~820 Ma)洋陆分布.地球科学,43(11):3837-3852.
张克信,殷鸿福,朱云海,等,2001.造山带混杂岩区地质填图理论、方法与实践---以东昆仑造山带为例.武汉:中国地质大学出版社.
张旗,李达周,张魁武,1985.云南省云县铜厂街蛇绿混杂岩的初步研究.岩石学报,1(3):1-14.
张伟波,叶锦华,2017.环太平洋成矿域主要铜-金矿床地质特征、成矿作用及找矿潜力.地质通报,36(1):1-15.
张万平,王立全,强巴扎西,等,2010.西藏同卡地区高压麻粒岩的发现、PT轨迹及其大地构造意义.岩石学报,26(6):1915-1924.
朱勤文,张双全,谭劲,1998.确定南澜沧江缝合带的火山岩地球化学证据.岩石矿物学杂志,17(4):296-307.
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