蛇绿混杂岩就位机制及其大地构造意义新解:基于残余洋盆型蛇绿混杂岩构造解析的启示
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摘要
蛇绿岩代表了古洋壳的残余,通常被作为识别古汇聚板块边界的重要标志之一.但是,通过对西准噶尔造山带和松潘-甘孜造山带内出露的蛇绿混杂岩的大比例尺填图和构造解析,揭示出并非所有的蛇绿混杂岩带都具有缝合带的大地构造意义.综合前人研究结果,将蛇绿混杂岩划分为缝合带型和非缝合带型2种类型.非缝合带型蛇绿混杂岩带的分布与残余洋盆在闭合过程中的构造过程密切相关.在残余洋盆被巨厚层的碎屑岩填充之后,作为残余盆地基底的大洋岩石圈物质在区域挤压应力作用下,可通过多种形式构造就位于上覆碎屑沉积地层之中,形成具有弥散性分布特点的残余洋盆型蛇绿混杂岩系统.而缝合带型蛇绿混杂岩的就位过程可划分为3种方式,分别是俯冲就位、仰冲就位和碰撞就位.这些不同类型的蛇绿混杂岩带在板块汇聚后的再造山过程中,早期的构造变形会被叠加改造甚至导致蛇绿混杂岩的重新就位,使其分布形式复杂化.因此,正确识别和厘定不同构造过程形成的蛇绿混杂岩带及其对应的大地构造背景,对研究洋陆转换过程和造山带的演化至关重要.
Ophiolites represent on-land fragments of paleo-oceanic crust and have been recognized as one of the key markers of suture zones.Here,we provide new insights into the emplacement of ophiolitic mélanges based on detailed geological mapping and structural analysis in the West Junggar and Songpan-Ganzi orogens.The results show that some ophiolitic mélange belts cannot be regarded as suture zones.The distribution of these ophiolitic mélange belts are usually associated with the structural processes during the closure of remnant oceanic basins.After the remnant oceanic basin is filled with thick clastic deposit,the oceanic lithosphere material as the base of the remnant basin can be injected into the overlying sedimentary strata through various faultings under the regional compressive stress,forming the remnant oceanic basin-type ophiolitic mélange system with dispersive distribution characteristics.Combining with previous researches,the emplacement mechanism of suture-zone type ophiolitic mélanges can be divided into three categories:subduction type,obduction type,and collision type.These different types of ophiolitic mélange belts will be superimposed and even re-emplaced by the tectonic processes of post-plate convergence,complicating their distribution.Therefore,identifying the ophiolitic mélanges formed in different tectonic processes and their backgrounds is of importance for understanding the process of ocean-continental transition and the tectonic evolution of orogenic belts.
Ophiolites represent on-land fragments of paleo-oceanic crust and have been recognized as one of the key markers of suture zones.Here,we provide new insights into the emplacement of ophiolitic mélanges based on detailed geological mapping and structural analysis in the West Junggar and Songpan-Ganzi orogens.The results show that some ophiolitic mélange belts cannot be regarded as suture zones.The distribution of these ophiolitic mélange belts are usually associated with the structural processes during the closure of remnant oceanic basins.After the remnant oceanic basin is filled with thick clastic deposit,the oceanic lithosphere material as the base of the remnant basin can be injected into the overlying sedimentary strata through various faultings under the regional compressive stress,forming the remnant oceanic basin-type ophiolitic mélange system with dispersive distribution characteristics.Combining with previous researches,the emplacement mechanism of suture-zone type ophiolitic mélanges can be divided into three categories:subduction type,obduction type,and collision type.These different types of ophiolitic mélange belts will be superimposed and even re-emplaced by the tectonic processes of post-plate convergence,complicating their distribution.Therefore,identifying the ophiolitic mélanges formed in different tectonic processes and their backgrounds is of importance for understanding the process of ocean-continental transition and the tectonic evolution of orogenic belts.
引文
Agard,P.,Yamato,P.,Jolivet,L.,et al.,2009.Exhumation of Oceanic Blueschists and Eclogites in Subduction Zones:Timing and Mechanisms.Earth-Science Reviews,92(1-2):53-79.https://doi.org/10.1016/j.earscirev.2008.11.002
Ben-Avraham,Z.,Nur,A.,Jones,D.,1982.The Emplacement of Ophiolites by Collision.Journal of Geophysical Research,87(B5):3861.https://doi.org/10.1029/jb087ib05p03861
Bruguier,O.,Lancelot,J.R.,Malavieille,J.,1997.U-Pb Dating on Single Detrital Zircon Grains from the Triassic Songpan-Ganze Flysch(Central China):Provenance and Tectonic Correlations.Earth and Planetary Science Letters,152(1-4):217-231.https://doi.org/10.1016/s0012-821x(97)00138-6
Buckman,S.,Aitchison,J.C.,2004.Tectonic Evolution of Paleozoic Terranes in West Junggar,Xinjiang,NW China.In:Malpas,J.,Fletcher,C.J.N.,Aitchison,J.C.,eds.,Aspects of the Tectonic Evolution of China.Geological Society,London,Special Publications,226:101-129.
Cawood,P.A.,Kr9ner,A.,Collins,W.J.,et al.,2009.Earth Accretionary Orogens through Earth History.In:Cawood,P.A.,Kr9ner,A.,eds.,Earth Accretionary Systems in Space and Time.Geological Society,London,Special Publications,318:1-36.
Chen,B.,Arakawa,Y.,2005.Elemental and Nd-Sr Isotopic Geochemistry of Granitoids from the West Junggar Foldbelt(NW China),with Implications for Phanerozoic Continental Growth.Geochimica et Cosmochimica Acta,69(22):5387-5388.https://doi.org/10.1016/j.gca.2005.06.012
Chen,S.,Guo,Z.J.,2010.Time Constraints,Tectonic Setting of Dalabute Ophiolitic Complex and Its Significance for Late Paleozoic Tectonic Evolution in West Junggar.Acta Petrologica Sinica,26(8):2336-2344(in Chinese with English Abstract).
Chen,S.,Guo,Z.J.,Pe-Piper,G.,et al.,2013.Late Paleozoic Peperites in West Junggar,China,and How They Constrain Regional Tectonic and Palaeoenvironmental Setting.Gondwana Research,23(2):666-681.https://doi.org/10.1016/j.gr.2012.04.012
Chen,S.,Pe-Piper,G.,Piper,D.J.W.,et al.,2014.Ophiolitic Mélanges in Crustal-Scale Fault Zones:Implications for the Late Palaeozoic Tectonic Evolution in West Junggar,China.Tectonics,33(12):2419-2443.https://doi.org/10.1002/2013tc003488
Cheng,C.,Xia,B.,Zheng,H.,et al.,2018.Chronology,Geochemistry and Tectonic Significance of Daba Ophiolites in Western Segment of Yarlung Zangbo Suture Zone,Tibet.Earth Science,43(4):975-990(in Chinese with English abstract).
Choulet,F.,Faure,M.,Cluzel,D.,et al.,2012.From Oblique Accretion to Transpression in the Evolution of the Altaid Collage:New Insights from West Junggar,Northwestern China.Gondwana Research,21(2-3):530-547.https://doi.org/10.1016/j.gr.2011.07.015
Coleman,R.G.,1971.Plate Tectonic Emplacement of Upper Mantle Peridotites along Continental Edges.Journal of Geophysical Research,76(5):1212-1222.https://doi.org/10.1029/jb076i005p01212
Dai,J.G.,Wang,C.S.,Polat,A.,et al.,2013.Rapid Forearc Spreading between 130and 120Ma:Evidence from Geochronology and Geochemistry of the Xigaze Ophiolite,Southern Tibet.Lithos,172-173:1-16.https://doi.org/10.1016/j.lithos.2013.03.011
Dewey,J.F.,1976.Ophiolite Obduction.Tectonophysics,31(1-2):93-120.https://doi.org/10.1016/0040-1951(76)90169-4
Dewey,J.F.,1977.Suture Zone Complexities:A Review.Tectonophysics,40(1-2):53-67.https://doi.org/10.1016/0040-1951(77)90029-4
Dilek,Y.,Furnes,H.,2009.Structure and Geochemistry of Tethyan Ophiolites and Their Petrogenesis in Subduction Rollback Systems.Lithos,113(1-2):1-20.https://doi.org/10.1016/j.lithos.2009.04.022
Dilek,Y.,Furnes,H.,2011.Ophiolite Genesis and Global Tectonics:Geochemical and Tectonic Fingerprinting of Ancient Oceanic Lithosphere.Geological Society of America Bulletin,123(3-4):387-411.https://doi.org/10.1130/b30446.1
Dilek,Y.,Furnes,H.,2014.Ophiolites and Their Origins.Elements,10(2):93-100.https://doi.org/10.2113/gselements.10.2.93
Dong,Y.P.,He,D.F.,Sun,S.S.,et al.,2018.Subduction and Accretionary Tectonics of the East Kunlun Orogen,Western Segment of the Central China Orogenic System.Earth-Science Reviews,186:231-261.https://doi.org/10.1016/j.earscirev.2017.12.006
Federico,L.,Crispini,L.,Scambelluri,M.,et al.,2007.Ophiolite Mélange Zone Records Exhumation in a Fossil Subduction Channel.Geology,35(6):499.https://doi.org/10.1130/g23190a.1
Fu,C.L.,Yan,Z.,Wang,Z.Q.,et al.,2018.Lajishankou Ophiolite Complex:Implications for Paleozoic Multiple Accretionary and Collisional Events in the South Qilian Belt.Tectonics,37(5):1321-1346.https://doi.org/10.1029/2017tc004740
Gao,R.,Xiao,L.,Pirajno,F.,et al.,2014.CarboniferousPermian Extensive Magmatism in the West Junggar,Xinjiang,Northwestern China:Its Geochemistry,Geochronology,and Petrogenesis.Lithos,204:125-143.https://doi.org/10.1016/j.lithos.2014.05.028
Gealey,W.K.,1977.Ophiolite Obduction and Geologic Evolution of the Oman Mountains and Adjacent Areas.Geological Society of America Bulletin,88(8):1183-1191.https://doi.org/10.1130/0016-7606(1977)88<1183:ooageo>2.0.co;2
Gong,Y.M.,Zong,R.W.,2015.Paleozoic Stratigraphic Regionalization and Paleogeographical Evolution in Western Junggar,Northwestern China.Earth Science,40(3):461-484(in Chinese with English abstract).
Han,B.F.,Ji,J.Q.,Song,B.,et al.,2006.Late Paleozoic Vertical Growth of Continental Crust around the Junggar Basin,Xinjiang,China(PartⅠ):Timing of PostCollisional Plutonism.Acta Petrologica Sinica,22(5):1077-1086(in Chinese with English abstract).
Hébert,R.,Bezard,R.,Guilmette,C.,et al.,2012.The IndusYarlung Zangbo Ophiolites from Nanga Parbat to Namche Barwa Syntaxes,Southern Tibet:First Synthesis of Petrology,Geochemistry,and Geochronology with Incidences on Geodynamic Reconstructions of NeoTethys.Gondwana Research,22(2):377-397.https://doi.org/10.1016/j.gr.2011.10.013
Hou,Q.L.,2018.Higher Structural Geology.Science Press,Beijing,130-150(in Chinese).
Hsu,K.J.,1988.Relict Back-Arc Basins:Principles of Recognition and Possible New Examples from China.In:Kleinspehn,K.L.,Paola,C.,eds.,New Perspectives in Basin Analysis.Springer-Verlag,New York,245-263.
Ingersoll,R.,Graham,S.A.,Dickinson,W.R.,1995.Remnant Ocean Basins.In:Busby,C.J.,Ingersoll,R.V.,eds.,Tectonics of Sedimentary Basins.Blackwell Science Inc.,Cambridge,363-391.
Ingersoll,R.,Dickinson,W.R.,Graham,S.A.,2003.RemnantOcean Submarine Fans:Largest Sedimentary Systems on Earth.Geological Society of America,Special Paper,370:191-208.
Kaplanis,A.,Koukouvelas,I.,Xypolias,P.,et al.,2013.Kinematics and Ophiolite Obduction in the Gerania and Helicon Mountains,Central Greece.Tectonophysics,595-596:215-234.https://doi.org/10.1016/j.tecto.2012.07.014
Klemd,R.,Gao,J.,Li,J.L.,et al.,2015.Metamorphic Evolution of(Ultra)-High-Pressure Subduction-Related Transient Crust in the South Tianshan Orogen(Central Asian Orogenic Belt):Geodynamic Implications.Gondwana Research,28(1):1-25.https://doi.org/10.1016/j.gr.2014.11.008
Klemd,R.,John,T.,Scherer,E.E.,et al.,2011.Changes in Dip of Subducted Slabs at Depth:Petrological and Geochronological Evidence from HP-UHP Rocks(Tianshan,NW-China).Earth and Planetary Science Letters,310(1-2):9-20.https://doi.org/10.1016/j.epsl.2011.07.022
Li,D.,He,D.F.,Qi,X.F.,et al.,2015.How was the Carboniferous Balkhash-West Junggar Remnant Ocean Filled and Closed?Insights from the Well Tacan-1 Strata in the Tacheng Basin,NW China.Gondwana Research,27(1):342-362.https://doi.org/10.1016/j.gr.2013.10.003
Li,D.,He,D.F.,Tang,Y.,2016a.Reconstructing Multiple Arc-Basin Systems in the Altai-Junggar Area(NW China):Implications for the Architecture and Evolution of the Western Central Asian Orogenic Belt.Journal of Asian Earth Sciences,121:84-107.https://doi.org/10.1016/j.jseaes.2016.02.010
Li,J.L.,Gao,J.,Wang,X.S.,2016b.A Subduction Channel Model for Exhumation of Oceanic-Type High-Pressure to Ultrahigh-Pressure Eclogite-Facies Metamorphic Rocks in SW Tianshan,China.Science China Earth Sciences,59(12):2339-2354.https://doi.org/10.1007/s11430-016-5103-7
Li,J.L.,Klemd,R.,Gao,J.,et al.,2016c.Poly-Cyclic Metamorphic Evolution of Eclogite:Evidence for Multistage Burial-Exhumation Cycling in a Subduction Channel.Journal of Petrology,57(1):119-146.https://doi.org/10.1093/petrology/egw002
Li,J.H.,Cheng,H.Y.,Zhao,X.,et al.,2009.Tectonic Evolution of Remnant Oceanic Basin and Its Implication for Hydrocarbon.Earth Science Frontiers,16(4):40-51(in Chinese with English abstract).
Li,L.,Wang,G.C.,Yan,W.B.,et al.,2015.Characteristics of Cleavages with Different Directions in Houshan Area of Karamay,Xinjiang,NW China and Their Geodynamic Background.Earth Science,40(3):521-534(in Chinese with English abstract).
Li,Y.J.,Xu,Q.,Liu,J.,et al.,2016.Redefinition and Geological Significance of Jiamuhe Formation in Hala’alate Mountain of West Junggar,Xinjiang.Earth Science,41(9):1479-1488(in Chinese with English abstract).
Liu,B.,Han,B.F.,Chen,J.F.,et al.,2017a.Closure Time of the Junggar-Balkhash Ocean:Constraints from Late Paleozoic Volcano-Sedimentary Sequences in the Barleik Mountains,West Junggar,NW China.Tectonics,36(12):2823-2845.https://doi.org/10.1002/2017tc004606
Liu,Y.M.,Wang,M.,Li,C.,et al.,2017b.Cretaceous Structures in the Duolong Region of Central Tibet:Evidence for an Accretionary Wedge and Closure of the BangongNujiang Neo-Tethys Ocean.Gondwana Research,48:110-123.https://doi.org/10.1016/j.gr.2017.04.026
Liu,F.,Yang,J.S.,Lian,D.Y.,et al.,2015.The Genesis and Tectonic Significance of Mafic Dikes in the Western Part of the Yarlung Zangbo Suture Zone,Tibet.Acta Geoscientica Sinica,36(4):441-454(in Chinese with English abstract).
Ma,C.,Zhao,G.P.,Xiao,W.J.,et al.,2011.Emplacement of Ophiolites:Mechanisms and Timing.Chinese Journal of Geology(Scientia Geologica Sinica),46(3):865-874(in Chinese with English abstract).
Mattei,M.,Cifelli,F.,Alimohammadian,H.,et al.,2017.Oroclinal Bending in the Alborz Mountains(Northern Iran):New Constraints on the Age of South Caspian Subduction and Extrusion Tectonics.Gondwana Research,42:13-28.https://doi.org/10.1016/j.gr.2016.10.003
Metcalf,R.V.,Shervais,J.W.,2008.Suprasubduction-Zone Ophiolites:Is There Really an Ophiolite Conundrum?Geological Society of America,Special Paper,438:191-222.
Miyashiro,A.,1975.Classification,Characteristics,and Origin of Ophiolites.The Journal of Geology,83(2):249-281.https://doi.org/10.1086/628085
Moores,E.M.,1982.Origin and Emplacement of Ophiolites.Reviews of Geophysics,20(4):735-760.https://doi.org/10.1029/rg020i004p00735
Pearce,J.A.,Lippard,S.J.,Roberts,S.,1984.Characteristics and Tectonic Significance of Supra-Subduction Zone Ophiolites.Geological Society,London,Special Publications,16(1):77-94.https://doi.org/10.1144/gsl.sp.1984.016.01.06
Pei,X.Z.,Li,R.B.,Li,Z.C.,et al.,2018.Composition Feature and Formation Process of Buqingshan Composite Accretionary Mélange Belt in Southern Margin of East Kunlun Orogen.Earth Science,43(12):4498-4520(in Chinese with English abstract).
Robertson,A.,2004.Development of Concepts Concerning the Genesis and Emplacement of Tethyan Ophiolites in the Eastern Mediterranean and Oman Regions.EarthScience Reviews,66(3-4):331-387.https://doi.org/10.1016/j.earscirev.2004.01.005
Robertson,A.H.F.,2002.Overview of the Genesis and Emplacement of Mesozoic Ophiolites in the Eastern Mediterranean Tethyan Region.Lithos,65(1-2):1-67.https://doi.org/10.1016/s0024-4937(02)00160-3
She,Z.B.,Ma,C.Q.,Mason,R.,et al.,2006.Provenance of the Triassic Songpan-Ganzi Flysch,West China.Chemical Geology,231(1-2):159-175.https://doi.org/10.1016/j.chemgeo.2006.01.001
Tang,Y.,Zhang,Y.P.,Tong,L.L.,2018.Mesozoic-Cenozoic Evolution of the Zoige Depression in the Songpan-Ganzi Flysch Basin,Eastern Tibetan Plateau:Constraints from Detrital Zircon U-Pb Ages and Fission-Track Ages of the Triassic Sedimentary Sequence.Journal of Asian Earth Sciences,151:285-300.https://doi.org/10.1016/j.jseaes.2017.10.021
Wakabayashi,J.,2011.Mélanges of the Franciscan Complex,California:Diverse Structural Settings,Evidence for Sedimentary Mixing,and Their Connection to Subduction Processes.In:Wakabayashi,J.,Dilek,Y.,eds.,Mélanges:Processes of Formation and Societal Significance.Geological Society of America,Special Paper,480:117-141.
Wakabayashi,J.,Dilek,Y.,2003.What Constitutes‘Emplacement’of an Ophiolite?:Mechanisms and Relationship to Subduction Initiation and Formation of Metamorphic Soles.Geological Society,London,Special Publications,218(1):427-447.https://doi.org/10.1144/gsl.sp.2003.218.01.22
Wang,G.C.,Jia,C.X.,Zhu,Y.H.,et al.,2004.New Results and Major Progress in Regional Geological Survey of the Alag Lake Sheet.Geological Bulletin,23(5-6):549-554(in Chinese with English abstract).
Wang,G.C.,Wintsch,R.P.,Garver,J.I.,et al.,2009.Provenance and Thermal History of the Bayan Har Group in the Western-Central Songpan-Ganzi-Bayan Har Terrane:Implications for Tectonic Evolution of the Northern Tibetan Plateau.Island Arc,18(3):444-466.https://doi.org/10.1111/j.1440-1738.2009.00666.x
Xiao,W.J.,Huang,B.C.,Han,C.M.,et al.,2010.A Review of the Western Part of the Altaids:A Key to Understanding the Architecture of Accretionary Orogens.Gondwana Research,18(2-3):253-273.https://doi.org/10.1016/j.gr.2010.01.007
Xiao,X.C.,1995.Discussion on the Classification of Ophiolites by Spreading Rate.Acta Petrologica Sinica,11(Suppl.):10-23(in Chinese with English abstract).
Xu,Q.Q.,Ji,J.Q.,Zhao,L.,et al.,2013.Tectonic Evolution and Continental Crust Growth of Northern Xinjiang in Northwestern China:Remnant Ocean Model.EarthScience Reviews,126:178-205.https://doi.org/10.1016/j.earscirev.2013.08.005
Xu,X.,Zhou,K.F.,Wang,Y.,2010.Study on Extinction of the Remnant Oceanic Basin and Tectonic Setting of West Junggar during Late Paleozoic.Acta Petrologica Sinica,26(11):3206-3214(in Chinese with English abstract).
Xu,Y.X.,Yang,B.,Zhang,S.,et al.,2016.Magnetotelluric Imaging of a Fossil Paleozoic Intraoceanic Subduction Zone in Western Junggar,NW China.Journal of Geophysical Research(Solid Earth),121(6):4103-4117.https://doi.org/10.1002/2015jb012394
Xu,Z.Q.,Dilek,Y.,Yang,J.S.,et al.,2015.Crustal Structure of the Indus-Tsangpo Suture Zone and Its Ophiolites in Southern Tibet.Gondwana Research,27(2):507-524.https://doi.org/10.1016/j.gr.2014.08.001
Yan,W.B.,Wang,G.C.,Li,L.,et al.,2015.Deformation Analyses and Their Geological Implications of Carboniferous-Permian Tectonic Transformation Period in Northwest Margin of Junggar Basin.Earth Science,40(3):504-520(in Chinese with English abstract).
Yang,G.,Li,Y.,Santosh,M.,et al.,2013.Geochronology and Geochemistry of Basalts from the Karamay Ophiolitic Melange in West Junggar(NW China):Implications for Devonian-Carboniferous Intra-Oceanic Accretionary Tectonics of the Southern Altaids.Geological Society of America Bulletin,125(3-4):401-419.https://doi.org/10.1130/b30650.1
Yang,G.X.,Li,Y.J.,Gu,P.Y.,et al.,2012a.Geochronological and Geochemical Study of the Darbut Ophiolitic Complex in the West Junggar(NW China):Implications for Petrogenesis and Tectonic Evolution.Gondwana Research,21(4):1037-1049.https://doi.org/10.1016/j.gr.2011.07.029
Yang,G.X.,Li,Y.J.,Santosh,M.,et al.,2012b.Geochronology and Geochemistry of Basaltic Rocks from the Sartuohai Ophiolitic Mélange,NW China:Implications for a Devonian Mantle Plume within the Junggar Ocean.Journal of Asian Earth Sciences,59:141-155.https://doi.org/10.1016/j.jseaes.2012.07.020
Yang,G.X.,Li,Y.J.,Xiao,W.J.,et al.,2015.OIB-Type Rocks within West Junggar Ophiolitic Mélanges:Evidence for the Accretion of Seamounts.Earth-Science Reviews,150:477-496.https://doi.org/10.1016/j.earscirev.2015.09.002
Yuan,C.,Zhou,M.F.,Sun,M.,et al.,2010.Triassic Granitoids in the Eastern Songpan-Ganzi Fold Belt,SW China:Magmatic Response to Geodynamics of the Deep Lithosphere.Earth and Planetary Science Letters,290(3-4):481-492.https://doi.org/10.1016/j.epsl.2010.01.005
Zhang,L.,Wang,G.C.,Gao,R.,et al.,2015.U-Pb Chronology of Detrital Zircons from the Carboniferous Sequences and Its Geological Implications in West Junggar.Geotectonica et Metallogenia,39(4):704-717(in Chinese with English abstract).
Zhang,P.,Wang,G.C.,Li,Y.T.,et al.,2017.Emplacement Mechanism of the Akebasitao Pluton:Implications for Regional Tectonic Evolution of West Junggar,NW China.Acta Geologica Sinica(English Edition),91(3):857-874.https://doi.org/10.1111/1755-6724.13314
Zhang,P.,Wang,G.C.,Polat,A.,et al.,2018a.Emplacement of the Ophiolitic Mélanges in the West Karamay Area:Implications for the Late Paleozoic Tectonic Evolution of West Junggar,Northwestern China.Tectonophysics,747-748:259-280.https://doi.org/10.1016/j.tecto.2018.08.019
Zhang,P.,Wang,G.C.,Polat,A.,et al.,2018b.Geochemistry of Mafic Rocks and Cherts in the Darbut and Karamay Ophiolitic Mélanges in West Junggar,Northwestern China:Evidence for a Late Silurian to Devonian BackArc Basin System.Tectonophysics,745:395-411.https://doi.org/10.1016/j.tecto.2018.08.018
Zhang,P.,Wang,G.C.,Xiao,L.,et al.,2015.Three-Dimensional Configuration Analysis and Its Geological Significance of Akebasitao Pluton in West Junggar.Earth Science,40(6):941-952(in Chinese with English abstract).
Zhang,Q.,1990.Classification of Ophiolites.Scientia Geologica Sinica,(1):54-60(in Chinese with English abstract).
Zhang,X.T.,Wang,B.Z.,Yu,J.,et al.,2005.Sedimentary Characteristics of the Bayan Har Remnant Ocean Basin,Northwestern China.Geological Bulletin of China,24(7):613-620(in Chinese with English abstract).
Zhu,Y.H.,Pan,Y.M.,Zhang,K.X.,et al.,2000.Emplacement Mechanisms of Ophiolites and Their Characteristics.Geological Science and Technology Information,19(1):16-18(in Chinese with English abstract).
Zong,R.W.,Gong,Y.M.,Wang,G.C.,2014.Carboniferous Stratal Sequence and Its Palaeogeographical Evolution in Southern Western Junggar,NW China.Earth Science Frontiers,21(2):216-233(in Chinese with English abstract).
陈石,郭召杰,2010.达尔布特蛇绿岩带的时限和属性以及对西准噶尔晚古生代构造演化的讨论.岩石学报,26(8):2336-2344.
程晨,夏斌,郑浩,等,2018.西藏雅鲁藏布江缝合带西段达巴蛇绿岩年代学、地球化学特征及其构造意义.地球科学,43(4):975-990.
龚一鸣,纵瑞文,2015.西准噶尔古生代地层区划及古地理演化.地球科学,40(3):461-484.
韩宝福,季建清,宋彪,等,2006.新疆准噶尔晚古生代陆壳垂向生长(Ⅰ)---后碰撞深成岩浆活动的时限.岩石学报,22(5):1077-1086.
侯泉林,2018.高等构造地质学.北京:科学出版社,130-150.
李江海,程海艳,赵星,等,2009.残余洋盆的大地构造演化及其油气意义.地学前缘,16(4):40-51.
李理,王国灿,晏文博,等,2015.西准噶尔克拉玛依后山地区不同方向劈理特征及其动力学背景.地球科学,40(3):521-534.
李永军,徐倩,刘佳,等,2016.新疆西准噶尔哈山地区佳木河组的重新厘定及地质意义.地球科学,41(9):1479-1488.
刘飞,杨经绥,连东洋,等,2015.雅鲁藏布江缝合带西段北亚带的基性岩成因和构造意义.地球学报,36(4):441-454.
马冲,赵桂萍,肖文交,等,2011.蛇绿岩就位机制及时限.地质科学,46(3):865-874.
裴先治,李瑞保,李佐臣,等,2018.东昆仑南缘布青山复合增生型构造混杂岩带组成特征及其形成演化过程.地球科学,43(12):4498-4520.
王国灿,贾春兴,朱云海,等,2004.阿拉克湖幅地质调查新成果及主要进展.地质通报,23(5-6):549-554.
肖序常,1995.从扩张速率试论蛇绿岩的类型划分.岩石学报,11(增刊):10-23.
徐新,周可法,王煜,2010.西准噶尔晚古生代残余洋盆消亡时间与构造背景研究.岩石学报,26(11):3206-3214.
晏文博,王国灿,李理,等,2015.准噶尔西北缘石炭-二叠纪构造转换期变形分析及其地质意义.地球科学,40(3):504-520.
张雷,王国灿,高睿,等,2015.新疆西准噶尔石炭系碎屑锆石U-Pb年代学及其地质意义.大地构造与成矿学,39(4):704-717.
张攀,王国灿,肖龙,等,2015.西准噶尔阿克巴斯陶岩体三维形态及其地质意义.地球科学,40(6):941-952.
张旗,1990.蛇绿岩的分类.地质科学,(1):54-60.
张雪亭,王秉璋,俞建,等,2005.巴颜喀拉残留洋盆的沉积特征.地质通报,24(7):613-620.
朱云海,潘元明,张克信,等,2000.蛇绿岩就位机制研究.地质科技情报,19(1):16-18.
纵瑞文,龚一鸣,王国灿,2014.西准噶尔南部石炭纪地层层序及古地理演化.地学前缘,21(2):216-233.
Ben-Avraham,Z.,Nur,A.,Jones,D.,1982.The Emplacement of Ophiolites by Collision.Journal of Geophysical Research,87(B5):3861.https://doi.org/10.1029/jb087ib05p03861
Bruguier,O.,Lancelot,J.R.,Malavieille,J.,1997.U-Pb Dating on Single Detrital Zircon Grains from the Triassic Songpan-Ganze Flysch(Central China):Provenance and Tectonic Correlations.Earth and Planetary Science Letters,152(1-4):217-231.https://doi.org/10.1016/s0012-821x(97)00138-6
Buckman,S.,Aitchison,J.C.,2004.Tectonic Evolution of Paleozoic Terranes in West Junggar,Xinjiang,NW China.In:Malpas,J.,Fletcher,C.J.N.,Aitchison,J.C.,eds.,Aspects of the Tectonic Evolution of China.Geological Society,London,Special Publications,226:101-129.
Cawood,P.A.,Kr9ner,A.,Collins,W.J.,et al.,2009.Earth Accretionary Orogens through Earth History.In:Cawood,P.A.,Kr9ner,A.,eds.,Earth Accretionary Systems in Space and Time.Geological Society,London,Special Publications,318:1-36.
Chen,B.,Arakawa,Y.,2005.Elemental and Nd-Sr Isotopic Geochemistry of Granitoids from the West Junggar Foldbelt(NW China),with Implications for Phanerozoic Continental Growth.Geochimica et Cosmochimica Acta,69(22):5387-5388.https://doi.org/10.1016/j.gca.2005.06.012
Chen,S.,Guo,Z.J.,2010.Time Constraints,Tectonic Setting of Dalabute Ophiolitic Complex and Its Significance for Late Paleozoic Tectonic Evolution in West Junggar.Acta Petrologica Sinica,26(8):2336-2344(in Chinese with English Abstract).
Chen,S.,Guo,Z.J.,Pe-Piper,G.,et al.,2013.Late Paleozoic Peperites in West Junggar,China,and How They Constrain Regional Tectonic and Palaeoenvironmental Setting.Gondwana Research,23(2):666-681.https://doi.org/10.1016/j.gr.2012.04.012
Chen,S.,Pe-Piper,G.,Piper,D.J.W.,et al.,2014.Ophiolitic Mélanges in Crustal-Scale Fault Zones:Implications for the Late Palaeozoic Tectonic Evolution in West Junggar,China.Tectonics,33(12):2419-2443.https://doi.org/10.1002/2013tc003488
Cheng,C.,Xia,B.,Zheng,H.,et al.,2018.Chronology,Geochemistry and Tectonic Significance of Daba Ophiolites in Western Segment of Yarlung Zangbo Suture Zone,Tibet.Earth Science,43(4):975-990(in Chinese with English abstract).
Choulet,F.,Faure,M.,Cluzel,D.,et al.,2012.From Oblique Accretion to Transpression in the Evolution of the Altaid Collage:New Insights from West Junggar,Northwestern China.Gondwana Research,21(2-3):530-547.https://doi.org/10.1016/j.gr.2011.07.015
Coleman,R.G.,1971.Plate Tectonic Emplacement of Upper Mantle Peridotites along Continental Edges.Journal of Geophysical Research,76(5):1212-1222.https://doi.org/10.1029/jb076i005p01212
Dai,J.G.,Wang,C.S.,Polat,A.,et al.,2013.Rapid Forearc Spreading between 130and 120Ma:Evidence from Geochronology and Geochemistry of the Xigaze Ophiolite,Southern Tibet.Lithos,172-173:1-16.https://doi.org/10.1016/j.lithos.2013.03.011
Dewey,J.F.,1976.Ophiolite Obduction.Tectonophysics,31(1-2):93-120.https://doi.org/10.1016/0040-1951(76)90169-4
Dewey,J.F.,1977.Suture Zone Complexities:A Review.Tectonophysics,40(1-2):53-67.https://doi.org/10.1016/0040-1951(77)90029-4
Dilek,Y.,Furnes,H.,2009.Structure and Geochemistry of Tethyan Ophiolites and Their Petrogenesis in Subduction Rollback Systems.Lithos,113(1-2):1-20.https://doi.org/10.1016/j.lithos.2009.04.022
Dilek,Y.,Furnes,H.,2011.Ophiolite Genesis and Global Tectonics:Geochemical and Tectonic Fingerprinting of Ancient Oceanic Lithosphere.Geological Society of America Bulletin,123(3-4):387-411.https://doi.org/10.1130/b30446.1
Dilek,Y.,Furnes,H.,2014.Ophiolites and Their Origins.Elements,10(2):93-100.https://doi.org/10.2113/gselements.10.2.93
Dong,Y.P.,He,D.F.,Sun,S.S.,et al.,2018.Subduction and Accretionary Tectonics of the East Kunlun Orogen,Western Segment of the Central China Orogenic System.Earth-Science Reviews,186:231-261.https://doi.org/10.1016/j.earscirev.2017.12.006
Federico,L.,Crispini,L.,Scambelluri,M.,et al.,2007.Ophiolite Mélange Zone Records Exhumation in a Fossil Subduction Channel.Geology,35(6):499.https://doi.org/10.1130/g23190a.1
Fu,C.L.,Yan,Z.,Wang,Z.Q.,et al.,2018.Lajishankou Ophiolite Complex:Implications for Paleozoic Multiple Accretionary and Collisional Events in the South Qilian Belt.Tectonics,37(5):1321-1346.https://doi.org/10.1029/2017tc004740
Gao,R.,Xiao,L.,Pirajno,F.,et al.,2014.CarboniferousPermian Extensive Magmatism in the West Junggar,Xinjiang,Northwestern China:Its Geochemistry,Geochronology,and Petrogenesis.Lithos,204:125-143.https://doi.org/10.1016/j.lithos.2014.05.028
Gealey,W.K.,1977.Ophiolite Obduction and Geologic Evolution of the Oman Mountains and Adjacent Areas.Geological Society of America Bulletin,88(8):1183-1191.https://doi.org/10.1130/0016-7606(1977)88<1183:ooageo>2.0.co;2
Gong,Y.M.,Zong,R.W.,2015.Paleozoic Stratigraphic Regionalization and Paleogeographical Evolution in Western Junggar,Northwestern China.Earth Science,40(3):461-484(in Chinese with English abstract).
Han,B.F.,Ji,J.Q.,Song,B.,et al.,2006.Late Paleozoic Vertical Growth of Continental Crust around the Junggar Basin,Xinjiang,China(PartⅠ):Timing of PostCollisional Plutonism.Acta Petrologica Sinica,22(5):1077-1086(in Chinese with English abstract).
Hébert,R.,Bezard,R.,Guilmette,C.,et al.,2012.The IndusYarlung Zangbo Ophiolites from Nanga Parbat to Namche Barwa Syntaxes,Southern Tibet:First Synthesis of Petrology,Geochemistry,and Geochronology with Incidences on Geodynamic Reconstructions of NeoTethys.Gondwana Research,22(2):377-397.https://doi.org/10.1016/j.gr.2011.10.013
Hou,Q.L.,2018.Higher Structural Geology.Science Press,Beijing,130-150(in Chinese).
Hsu,K.J.,1988.Relict Back-Arc Basins:Principles of Recognition and Possible New Examples from China.In:Kleinspehn,K.L.,Paola,C.,eds.,New Perspectives in Basin Analysis.Springer-Verlag,New York,245-263.
Ingersoll,R.,Graham,S.A.,Dickinson,W.R.,1995.Remnant Ocean Basins.In:Busby,C.J.,Ingersoll,R.V.,eds.,Tectonics of Sedimentary Basins.Blackwell Science Inc.,Cambridge,363-391.
Ingersoll,R.,Dickinson,W.R.,Graham,S.A.,2003.RemnantOcean Submarine Fans:Largest Sedimentary Systems on Earth.Geological Society of America,Special Paper,370:191-208.
Kaplanis,A.,Koukouvelas,I.,Xypolias,P.,et al.,2013.Kinematics and Ophiolite Obduction in the Gerania and Helicon Mountains,Central Greece.Tectonophysics,595-596:215-234.https://doi.org/10.1016/j.tecto.2012.07.014
Klemd,R.,Gao,J.,Li,J.L.,et al.,2015.Metamorphic Evolution of(Ultra)-High-Pressure Subduction-Related Transient Crust in the South Tianshan Orogen(Central Asian Orogenic Belt):Geodynamic Implications.Gondwana Research,28(1):1-25.https://doi.org/10.1016/j.gr.2014.11.008
Klemd,R.,John,T.,Scherer,E.E.,et al.,2011.Changes in Dip of Subducted Slabs at Depth:Petrological and Geochronological Evidence from HP-UHP Rocks(Tianshan,NW-China).Earth and Planetary Science Letters,310(1-2):9-20.https://doi.org/10.1016/j.epsl.2011.07.022
Li,D.,He,D.F.,Qi,X.F.,et al.,2015.How was the Carboniferous Balkhash-West Junggar Remnant Ocean Filled and Closed?Insights from the Well Tacan-1 Strata in the Tacheng Basin,NW China.Gondwana Research,27(1):342-362.https://doi.org/10.1016/j.gr.2013.10.003
Li,D.,He,D.F.,Tang,Y.,2016a.Reconstructing Multiple Arc-Basin Systems in the Altai-Junggar Area(NW China):Implications for the Architecture and Evolution of the Western Central Asian Orogenic Belt.Journal of Asian Earth Sciences,121:84-107.https://doi.org/10.1016/j.jseaes.2016.02.010
Li,J.L.,Gao,J.,Wang,X.S.,2016b.A Subduction Channel Model for Exhumation of Oceanic-Type High-Pressure to Ultrahigh-Pressure Eclogite-Facies Metamorphic Rocks in SW Tianshan,China.Science China Earth Sciences,59(12):2339-2354.https://doi.org/10.1007/s11430-016-5103-7
Li,J.L.,Klemd,R.,Gao,J.,et al.,2016c.Poly-Cyclic Metamorphic Evolution of Eclogite:Evidence for Multistage Burial-Exhumation Cycling in a Subduction Channel.Journal of Petrology,57(1):119-146.https://doi.org/10.1093/petrology/egw002
Li,J.H.,Cheng,H.Y.,Zhao,X.,et al.,2009.Tectonic Evolution of Remnant Oceanic Basin and Its Implication for Hydrocarbon.Earth Science Frontiers,16(4):40-51(in Chinese with English abstract).
Li,L.,Wang,G.C.,Yan,W.B.,et al.,2015.Characteristics of Cleavages with Different Directions in Houshan Area of Karamay,Xinjiang,NW China and Their Geodynamic Background.Earth Science,40(3):521-534(in Chinese with English abstract).
Li,Y.J.,Xu,Q.,Liu,J.,et al.,2016.Redefinition and Geological Significance of Jiamuhe Formation in Hala’alate Mountain of West Junggar,Xinjiang.Earth Science,41(9):1479-1488(in Chinese with English abstract).
Liu,B.,Han,B.F.,Chen,J.F.,et al.,2017a.Closure Time of the Junggar-Balkhash Ocean:Constraints from Late Paleozoic Volcano-Sedimentary Sequences in the Barleik Mountains,West Junggar,NW China.Tectonics,36(12):2823-2845.https://doi.org/10.1002/2017tc004606
Liu,Y.M.,Wang,M.,Li,C.,et al.,2017b.Cretaceous Structures in the Duolong Region of Central Tibet:Evidence for an Accretionary Wedge and Closure of the BangongNujiang Neo-Tethys Ocean.Gondwana Research,48:110-123.https://doi.org/10.1016/j.gr.2017.04.026
Liu,F.,Yang,J.S.,Lian,D.Y.,et al.,2015.The Genesis and Tectonic Significance of Mafic Dikes in the Western Part of the Yarlung Zangbo Suture Zone,Tibet.Acta Geoscientica Sinica,36(4):441-454(in Chinese with English abstract).
Ma,C.,Zhao,G.P.,Xiao,W.J.,et al.,2011.Emplacement of Ophiolites:Mechanisms and Timing.Chinese Journal of Geology(Scientia Geologica Sinica),46(3):865-874(in Chinese with English abstract).
Mattei,M.,Cifelli,F.,Alimohammadian,H.,et al.,2017.Oroclinal Bending in the Alborz Mountains(Northern Iran):New Constraints on the Age of South Caspian Subduction and Extrusion Tectonics.Gondwana Research,42:13-28.https://doi.org/10.1016/j.gr.2016.10.003
Metcalf,R.V.,Shervais,J.W.,2008.Suprasubduction-Zone Ophiolites:Is There Really an Ophiolite Conundrum?Geological Society of America,Special Paper,438:191-222.
Miyashiro,A.,1975.Classification,Characteristics,and Origin of Ophiolites.The Journal of Geology,83(2):249-281.https://doi.org/10.1086/628085
Moores,E.M.,1982.Origin and Emplacement of Ophiolites.Reviews of Geophysics,20(4):735-760.https://doi.org/10.1029/rg020i004p00735
Pearce,J.A.,Lippard,S.J.,Roberts,S.,1984.Characteristics and Tectonic Significance of Supra-Subduction Zone Ophiolites.Geological Society,London,Special Publications,16(1):77-94.https://doi.org/10.1144/gsl.sp.1984.016.01.06
Pei,X.Z.,Li,R.B.,Li,Z.C.,et al.,2018.Composition Feature and Formation Process of Buqingshan Composite Accretionary Mélange Belt in Southern Margin of East Kunlun Orogen.Earth Science,43(12):4498-4520(in Chinese with English abstract).
Robertson,A.,2004.Development of Concepts Concerning the Genesis and Emplacement of Tethyan Ophiolites in the Eastern Mediterranean and Oman Regions.EarthScience Reviews,66(3-4):331-387.https://doi.org/10.1016/j.earscirev.2004.01.005
Robertson,A.H.F.,2002.Overview of the Genesis and Emplacement of Mesozoic Ophiolites in the Eastern Mediterranean Tethyan Region.Lithos,65(1-2):1-67.https://doi.org/10.1016/s0024-4937(02)00160-3
She,Z.B.,Ma,C.Q.,Mason,R.,et al.,2006.Provenance of the Triassic Songpan-Ganzi Flysch,West China.Chemical Geology,231(1-2):159-175.https://doi.org/10.1016/j.chemgeo.2006.01.001
Tang,Y.,Zhang,Y.P.,Tong,L.L.,2018.Mesozoic-Cenozoic Evolution of the Zoige Depression in the Songpan-Ganzi Flysch Basin,Eastern Tibetan Plateau:Constraints from Detrital Zircon U-Pb Ages and Fission-Track Ages of the Triassic Sedimentary Sequence.Journal of Asian Earth Sciences,151:285-300.https://doi.org/10.1016/j.jseaes.2017.10.021
Wakabayashi,J.,2011.Mélanges of the Franciscan Complex,California:Diverse Structural Settings,Evidence for Sedimentary Mixing,and Their Connection to Subduction Processes.In:Wakabayashi,J.,Dilek,Y.,eds.,Mélanges:Processes of Formation and Societal Significance.Geological Society of America,Special Paper,480:117-141.
Wakabayashi,J.,Dilek,Y.,2003.What Constitutes‘Emplacement’of an Ophiolite?:Mechanisms and Relationship to Subduction Initiation and Formation of Metamorphic Soles.Geological Society,London,Special Publications,218(1):427-447.https://doi.org/10.1144/gsl.sp.2003.218.01.22
Wang,G.C.,Jia,C.X.,Zhu,Y.H.,et al.,2004.New Results and Major Progress in Regional Geological Survey of the Alag Lake Sheet.Geological Bulletin,23(5-6):549-554(in Chinese with English abstract).
Wang,G.C.,Wintsch,R.P.,Garver,J.I.,et al.,2009.Provenance and Thermal History of the Bayan Har Group in the Western-Central Songpan-Ganzi-Bayan Har Terrane:Implications for Tectonic Evolution of the Northern Tibetan Plateau.Island Arc,18(3):444-466.https://doi.org/10.1111/j.1440-1738.2009.00666.x
Xiao,W.J.,Huang,B.C.,Han,C.M.,et al.,2010.A Review of the Western Part of the Altaids:A Key to Understanding the Architecture of Accretionary Orogens.Gondwana Research,18(2-3):253-273.https://doi.org/10.1016/j.gr.2010.01.007
Xiao,X.C.,1995.Discussion on the Classification of Ophiolites by Spreading Rate.Acta Petrologica Sinica,11(Suppl.):10-23(in Chinese with English abstract).
Xu,Q.Q.,Ji,J.Q.,Zhao,L.,et al.,2013.Tectonic Evolution and Continental Crust Growth of Northern Xinjiang in Northwestern China:Remnant Ocean Model.EarthScience Reviews,126:178-205.https://doi.org/10.1016/j.earscirev.2013.08.005
Xu,X.,Zhou,K.F.,Wang,Y.,2010.Study on Extinction of the Remnant Oceanic Basin and Tectonic Setting of West Junggar during Late Paleozoic.Acta Petrologica Sinica,26(11):3206-3214(in Chinese with English abstract).
Xu,Y.X.,Yang,B.,Zhang,S.,et al.,2016.Magnetotelluric Imaging of a Fossil Paleozoic Intraoceanic Subduction Zone in Western Junggar,NW China.Journal of Geophysical Research(Solid Earth),121(6):4103-4117.https://doi.org/10.1002/2015jb012394
Xu,Z.Q.,Dilek,Y.,Yang,J.S.,et al.,2015.Crustal Structure of the Indus-Tsangpo Suture Zone and Its Ophiolites in Southern Tibet.Gondwana Research,27(2):507-524.https://doi.org/10.1016/j.gr.2014.08.001
Yan,W.B.,Wang,G.C.,Li,L.,et al.,2015.Deformation Analyses and Their Geological Implications of Carboniferous-Permian Tectonic Transformation Period in Northwest Margin of Junggar Basin.Earth Science,40(3):504-520(in Chinese with English abstract).
Yang,G.,Li,Y.,Santosh,M.,et al.,2013.Geochronology and Geochemistry of Basalts from the Karamay Ophiolitic Melange in West Junggar(NW China):Implications for Devonian-Carboniferous Intra-Oceanic Accretionary Tectonics of the Southern Altaids.Geological Society of America Bulletin,125(3-4):401-419.https://doi.org/10.1130/b30650.1
Yang,G.X.,Li,Y.J.,Gu,P.Y.,et al.,2012a.Geochronological and Geochemical Study of the Darbut Ophiolitic Complex in the West Junggar(NW China):Implications for Petrogenesis and Tectonic Evolution.Gondwana Research,21(4):1037-1049.https://doi.org/10.1016/j.gr.2011.07.029
Yang,G.X.,Li,Y.J.,Santosh,M.,et al.,2012b.Geochronology and Geochemistry of Basaltic Rocks from the Sartuohai Ophiolitic Mélange,NW China:Implications for a Devonian Mantle Plume within the Junggar Ocean.Journal of Asian Earth Sciences,59:141-155.https://doi.org/10.1016/j.jseaes.2012.07.020
Yang,G.X.,Li,Y.J.,Xiao,W.J.,et al.,2015.OIB-Type Rocks within West Junggar Ophiolitic Mélanges:Evidence for the Accretion of Seamounts.Earth-Science Reviews,150:477-496.https://doi.org/10.1016/j.earscirev.2015.09.002
Yuan,C.,Zhou,M.F.,Sun,M.,et al.,2010.Triassic Granitoids in the Eastern Songpan-Ganzi Fold Belt,SW China:Magmatic Response to Geodynamics of the Deep Lithosphere.Earth and Planetary Science Letters,290(3-4):481-492.https://doi.org/10.1016/j.epsl.2010.01.005
Zhang,L.,Wang,G.C.,Gao,R.,et al.,2015.U-Pb Chronology of Detrital Zircons from the Carboniferous Sequences and Its Geological Implications in West Junggar.Geotectonica et Metallogenia,39(4):704-717(in Chinese with English abstract).
Zhang,P.,Wang,G.C.,Li,Y.T.,et al.,2017.Emplacement Mechanism of the Akebasitao Pluton:Implications for Regional Tectonic Evolution of West Junggar,NW China.Acta Geologica Sinica(English Edition),91(3):857-874.https://doi.org/10.1111/1755-6724.13314
Zhang,P.,Wang,G.C.,Polat,A.,et al.,2018a.Emplacement of the Ophiolitic Mélanges in the West Karamay Area:Implications for the Late Paleozoic Tectonic Evolution of West Junggar,Northwestern China.Tectonophysics,747-748:259-280.https://doi.org/10.1016/j.tecto.2018.08.019
Zhang,P.,Wang,G.C.,Polat,A.,et al.,2018b.Geochemistry of Mafic Rocks and Cherts in the Darbut and Karamay Ophiolitic Mélanges in West Junggar,Northwestern China:Evidence for a Late Silurian to Devonian BackArc Basin System.Tectonophysics,745:395-411.https://doi.org/10.1016/j.tecto.2018.08.018
Zhang,P.,Wang,G.C.,Xiao,L.,et al.,2015.Three-Dimensional Configuration Analysis and Its Geological Significance of Akebasitao Pluton in West Junggar.Earth Science,40(6):941-952(in Chinese with English abstract).
Zhang,Q.,1990.Classification of Ophiolites.Scientia Geologica Sinica,(1):54-60(in Chinese with English abstract).
Zhang,X.T.,Wang,B.Z.,Yu,J.,et al.,2005.Sedimentary Characteristics of the Bayan Har Remnant Ocean Basin,Northwestern China.Geological Bulletin of China,24(7):613-620(in Chinese with English abstract).
Zhu,Y.H.,Pan,Y.M.,Zhang,K.X.,et al.,2000.Emplacement Mechanisms of Ophiolites and Their Characteristics.Geological Science and Technology Information,19(1):16-18(in Chinese with English abstract).
Zong,R.W.,Gong,Y.M.,Wang,G.C.,2014.Carboniferous Stratal Sequence and Its Palaeogeographical Evolution in Southern Western Junggar,NW China.Earth Science Frontiers,21(2):216-233(in Chinese with English abstract).
陈石,郭召杰,2010.达尔布特蛇绿岩带的时限和属性以及对西准噶尔晚古生代构造演化的讨论.岩石学报,26(8):2336-2344.
程晨,夏斌,郑浩,等,2018.西藏雅鲁藏布江缝合带西段达巴蛇绿岩年代学、地球化学特征及其构造意义.地球科学,43(4):975-990.
龚一鸣,纵瑞文,2015.西准噶尔古生代地层区划及古地理演化.地球科学,40(3):461-484.
韩宝福,季建清,宋彪,等,2006.新疆准噶尔晚古生代陆壳垂向生长(Ⅰ)---后碰撞深成岩浆活动的时限.岩石学报,22(5):1077-1086.
侯泉林,2018.高等构造地质学.北京:科学出版社,130-150.
李江海,程海艳,赵星,等,2009.残余洋盆的大地构造演化及其油气意义.地学前缘,16(4):40-51.
李理,王国灿,晏文博,等,2015.西准噶尔克拉玛依后山地区不同方向劈理特征及其动力学背景.地球科学,40(3):521-534.
李永军,徐倩,刘佳,等,2016.新疆西准噶尔哈山地区佳木河组的重新厘定及地质意义.地球科学,41(9):1479-1488.
刘飞,杨经绥,连东洋,等,2015.雅鲁藏布江缝合带西段北亚带的基性岩成因和构造意义.地球学报,36(4):441-454.
马冲,赵桂萍,肖文交,等,2011.蛇绿岩就位机制及时限.地质科学,46(3):865-874.
裴先治,李瑞保,李佐臣,等,2018.东昆仑南缘布青山复合增生型构造混杂岩带组成特征及其形成演化过程.地球科学,43(12):4498-4520.
王国灿,贾春兴,朱云海,等,2004.阿拉克湖幅地质调查新成果及主要进展.地质通报,23(5-6):549-554.
肖序常,1995.从扩张速率试论蛇绿岩的类型划分.岩石学报,11(增刊):10-23.
徐新,周可法,王煜,2010.西准噶尔晚古生代残余洋盆消亡时间与构造背景研究.岩石学报,26(11):3206-3214.
晏文博,王国灿,李理,等,2015.准噶尔西北缘石炭-二叠纪构造转换期变形分析及其地质意义.地球科学,40(3):504-520.
张雷,王国灿,高睿,等,2015.新疆西准噶尔石炭系碎屑锆石U-Pb年代学及其地质意义.大地构造与成矿学,39(4):704-717.
张攀,王国灿,肖龙,等,2015.西准噶尔阿克巴斯陶岩体三维形态及其地质意义.地球科学,40(6):941-952.
张旗,1990.蛇绿岩的分类.地质科学,(1):54-60.
张雪亭,王秉璋,俞建,等,2005.巴颜喀拉残留洋盆的沉积特征.地质通报,24(7):613-620.
朱云海,潘元明,张克信,等,2000.蛇绿岩就位机制研究.地质科技情报,19(1):16-18.
纵瑞文,龚一鸣,王国灿,2014.西准噶尔南部石炭纪地层层序及古地理演化.地学前缘,21(2):216-233.
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