南羌塘增生过程的中-晚三叠世岩浆记录:藏北玛依岗日-角木日地区基性岩墙
|
摘要
古特提斯洋向北俯冲形成增生杂岩,它们向南增生构成了南羌塘增生地体,且增生期内发育的岩浆岩可以用来研究南羌塘的增生过程。在南羌塘增生杂岩带内,由北向南,发育有玛依岗日(MG)辉长岩墙、角木日(JM)辉长辉绿岩墙。锆石U-Pb测年结果显示,两者分别形成于237. 1±2. 3Ma和230. 7±1. 8Ma,为南羌塘增生期内岩浆岩。它们的岩石地球化学特征均介于OIB与E-MORB之间,富集Ti、Nb,以及LREE和LILE。Nd-Pb同位素结果显示两者均起源于富集地幔源区。Sm/YbLa/Yb图解显示,两者均起源于尖晶石-石榴石二辉橄榄岩源区,相对于JM辉长辉绿岩MG辉长岩部分熔融程度较高。两者Mg#和Ni、Cr特征表明,MG辉长岩分异程度高于JM辉长辉绿岩。Th/Nb-La/Nb图解显示,相对于JM辉长辉绿岩MG辉长岩经历了一定程度的地壳混染。综合研究认为,MG辉长岩和JM辉长辉绿岩为古特提斯洋壳俯冲过程中软流圈上涌的两次岩浆活动的产物,并受俯冲洋壳和地幔楔影响。MG辉长岩和JM辉长辉绿岩记录了南羌塘的增生过程,它们为相关研究提供了岩浆岩证据。
The northward subduction of Paleo-Tethys Ocean( PTO) formed the accretionary complex,which constructed the South Qiangtang accretionary terrane( SQAT). Therefore,the magmatic rocks formed during the accretionary period can be used to study the accretionary processes of SQAT. From north to south,the Mayigangri( MG) gabbro and the Jiaomuri( JM) gabbro-diabase are developed and outcropped in the accretionary complex belt of SQAT. Zircon SHRIMP U-Pb dating results show that the MG gabbro and the JM gabbro-diabase formed at 237. 1 ± 2. 3 Ma and 230. 7 ± 1. 8 Ma respectively,developed in the accretionary period of SQAT. Their characteristics of whole rock geochemical data are between those of OIB and E-MORB. Both of rocks contain high Ti and Nb contents,and are enriched in LREE and LILE. The Nd-Pb isotopic data indicate that both of them were derived from enriched mantle.Furthermore,the Sm/Yb-La/Yb diagram shows that both of them were derived from spinel-garnet lherzolite,while the MG gabbro magma was generated by higher degree of partial melting of source mantle than the JM gabbro-diabase. In addition,their Mg#as well as the contents of Cr and Ni suggested that the MG gabbro experienced higher degree of fractionation than the JM gabbro-diabase. On the other hand,the Th/Nb-La/Nb diagram shows that the MG gabbro underwent a certain degree of crustal contamination compared with the JM gabbro-diabase. Comprehensively,both of the MG gabbro and the JM gabbro-diabase were the products of twice magmatic events caused by the upwelling of asthenosphere during the oceanic crust subduction of PTO. Meanwhile,both of them were influenced by the subduction slab and mantle wedge. Consequently,the MG gabbro and the JM gabbro-diabase recorded the accretionary processes of SQAT,and thus provide magmatic evidence for relevant research.
The northward subduction of Paleo-Tethys Ocean( PTO) formed the accretionary complex,which constructed the South Qiangtang accretionary terrane( SQAT). Therefore,the magmatic rocks formed during the accretionary period can be used to study the accretionary processes of SQAT. From north to south,the Mayigangri( MG) gabbro and the Jiaomuri( JM) gabbro-diabase are developed and outcropped in the accretionary complex belt of SQAT. Zircon SHRIMP U-Pb dating results show that the MG gabbro and the JM gabbro-diabase formed at 237. 1 ± 2. 3 Ma and 230. 7 ± 1. 8 Ma respectively,developed in the accretionary period of SQAT. Their characteristics of whole rock geochemical data are between those of OIB and E-MORB. Both of rocks contain high Ti and Nb contents,and are enriched in LREE and LILE. The Nd-Pb isotopic data indicate that both of them were derived from enriched mantle.Furthermore,the Sm/Yb-La/Yb diagram shows that both of them were derived from spinel-garnet lherzolite,while the MG gabbro magma was generated by higher degree of partial melting of source mantle than the JM gabbro-diabase. In addition,their Mg#as well as the contents of Cr and Ni suggested that the MG gabbro experienced higher degree of fractionation than the JM gabbro-diabase. On the other hand,the Th/Nb-La/Nb diagram shows that the MG gabbro underwent a certain degree of crustal contamination compared with the JM gabbro-diabase. Comprehensively,both of the MG gabbro and the JM gabbro-diabase were the products of twice magmatic events caused by the upwelling of asthenosphere during the oceanic crust subduction of PTO. Meanwhile,both of them were influenced by the subduction slab and mantle wedge. Consequently,the MG gabbro and the JM gabbro-diabase recorded the accretionary processes of SQAT,and thus provide magmatic evidence for relevant research.
引文
Abratis M and W9rner G.2001.Ridge collision,slab-window formation,and the flux of Pacific asthenosphere into the Caribbean realm.Geology,29(2):127-130
Bédard JH.1999.Petrogenesis of boninites from the Betts Cove ophiolite,Newfoundland,Canada:Identification of subducted source components.Journal of Petrology,40(12):1853-1889
Bickford ME.1988.The formation of continental crust:Part 1.A review of some principles;Part 2.An application to the Proterozoic evolution of southern North America.GSA Bulletin,100(9):1375-1391
Castillo PR.2008.Origin of the adakite-high-Nb basalt association and its implications for postsubduction magmatism in Baja California,Mexico.GSA Bulletin,120(3-4):451-462
Chen F,Hegner E and Todt W.2000.Zircon ages and Nd isotopic and chemical compositions of orthogneisses from the Black Forest,Germany:Evidence for a Cambrian magmatic arc.International Journal of Earth Sciences,88(4):791-802
Chen FK,Li XH,Wang XL,Li QL and Siebel W.2007.Zircon age and Nd-Hf isotopic composition of the Yunnan Tethyan belt,southwestern China.International Journal of Earth Sciences,96(6):1179-1194
Chen SS,Shi RD,Yi GD and Zou HB.2016.Middle Triassic volcanic rocks in the Northern Qiangtang(Central Tibet):Geochronology,petrogenesis,and tectonic implications.Tectonophysics,666:90-102
Condie KC.1993.Chemical composition and evolution of the upper continental crust:Contrasting results from surface samples and shales.Chemical Geology,104(1-4):1-37
Dan W,Wang Q,White WM,Zhang XZ,Tang GJ,Jiang ZQ,Hao LLand Ou Q.2018.Rapid formation of eclogites during a nearly closed ocean:Revisiting the Pianshishan eclogite in Qiangtang,central Tibetan Plateau.Chemical Geology,477:112-122
Davis D,Suppe J and Dahlen FA.1983.Mechanics of fold-and-thrust belts and accretionary wedges.Journal of Geophysical Research:Solid Earth,88(B2):1153-1172
Deng WM,Yin JX and Guo ZP.1996.Basic-ultrabasic and volcanic rocks in Chagbu-Shuanghu area of northern Xizang(Tibet),China.Science in China(Series D),39(4):359-368
Dilek Y and Furnes H.2011.Ophiolite genesis and global tectonics:Geochemical and tectonic fingerprinting of ancient oceanic lithosphere.GSA Bulletin,123(3-4):387-411
Dilek Y and Furnes H.2014.Ophiolites and their origins.Elements,10(2):93-100
Elliot T.2003.Tracers of the slab.In:Eiler J(ed.).Inside the Subduction Factory.Washington:American Geophysical Union,23-45
Frey FA,Green DH and Roy SD.1978.Integrated models of basalt petrogenesis:A study of quartz tholeiites to olivine melilitites from South Eastern Australia:Utilizing geochemical and experimental petrological data.Journal of Petrology,19(3):463-513
Furukawa Y.2011.Simple flow models of accretionary prisms:Predictions for coexisting arc-normal compression and extension,and implications for locked zones on the interplate megathrust.Tectonophysics,505(1-4):57-67
Gorring ML and Kay SM.2001.Mantle processes and sources of Neogene slab window magmas from southern Patagonia,Argentina.Journal of Petrology,42(6):1067-1094
Hoffman PF.1988.United plates of America,the birth of a craton:Early Proterozoic assembly and growth of Laurentia.Annual Review of Earth and Planetary Sciences,16:543-603
Hofmann AW.1997.Mantle geochemistry:The message from oceanic volcanism.Nature,385(6613):219-229
Kapp P,Yin A,Manning CE,Harrison TM,Taylor MH and Ding L.2003.Tectonic evolution of the Early Mesozoic blueschist-bearing Qiangtang metamorphic belt,central Tibet.Tectonics,22(4):1043
Keto LS and Jacobsen SB.1987.Nd and Sr isotopic variations of Early Paleozoic oceans.Earth and Planetary Science Letters,84(1):27-41
Li C.1987.The Longmucuo-Shuanghu-Lancangjiang plate suture and the north boundary of distribution of Gondwana facies PermianCarboniferous system in northern Xizang,China.Journal of Changchun University of Earth Science,17(2):155-166(in Chinese)
Li C,Zhai QG,Dong YS,Yu JJ and Huang XP.2007.Establishment of the Upper Triassic Wanghuling Formation at Guoganjianian mountain,central Qiangtang,Qinghai-Tibet Plateau,and its significance.Geological Bulletin of China,26(8):1003-1008(in Chinese with English abstract)
Li C,Zhai GY,Wang LQ,Yin FG and Mao XC.2009.An important window for understanding the Qinghai-Tibet Plateau:A review on research progress in recent years of Qiangtang area,Tibet,China.Geological Bulletin of China,28(9):1169-1177(in Chinese with English abstract)
Li D,Wang GH,Gao JH,Yuan GL,Zhou J,Fang DR,Zhang L,Gong YD and Zhao HC.2018.The continental subduction in the evolution of central Qiangtang mélange belt and its tectonic significance.International Geology Review,doi:10.1080/00206814.2018.1499450
Li JC,Zhao ZB,Zheng YL,Yuan GL,Liang X,Wang GH and Liu X.2015.The magmatite evidences in southern Qiangtang for paleoTethys ocean subducting collision:Gangtang-Co granites in Rongma,Tibet.Acta Petrologica Sinica,31(7):2078-2088(in Chinese with English abstract)
Li JL.2004.Basic characteristics of accretion-type orogens.Geological Bulletin of China,23(9-10):947-951(in Chinese with English abstract)
Li LG,Liang X,Wang GH,Wang XL,Gao X,Jiao PW and Huang ZG.2018.Discovery of the middle-late Triassic carbonatite formation in the central Qiangtang accretionary complex,North Tibet and its tectonic significance.Acta Geologica Sinica,92(4):828-844(in Chinese with English abstract)
Li PW,Gao R,Cui JW and Guan Y.2005.Paleomagnetic results from the Three Rivers Region,SW China:Implications for the collisional and accretionary history.Acta Geoscientica Sinica,26(5):387-404(in Chinese with English abstract)
Li PW,Gao R,Guan Y and Li QS.2009.Paleomagnetic constraints on the closure time of Paleo-Tethys:Implications for the tectonic setting of formation of Triassic Songpan-Ganzi flysch complex.Acta Geoscientica Sinica,30(1):39-50(in Chinese with English abstract)
Li RB,Pei XZ,Li ZC,Pei L,Chen GC,Liu CJ,Chen YX and Liu ZQ.2014.Geochemical characteristics of Gerizhuotuo OIB and its tectonic significance in Buqingshan tectonic mélange belt,southern margin of East Kunlun Orogen.Earth Science Frontiers,21(1):183-195(in Chinese with English abstract)
Li YJ,Wu HR and Li HS.1997.Discovery of radioarians in the Amugang and Chasang groups and Lugu Formation in northern Tibet and some related geological problems.Geological Review,43(3):250-256(in Chinese with English abstract)
Liang X,Wang GH,Yuan GL and Liu Y.2012.Structural sequence and geochronology of the Qomo Ri accretionary complex,Central Qiangtang,Tibet:Implications for the Late Triassic subduction of the Paleo-Tethys Ocean.Gondwana Research,22(2):470-481
Liang X,Wang GH,Yuan GL and Che XC.2015.Mesozoic and Cenozoic deformations in the Raggyorcaka area,Tibet:Implications for the tectonic evolution of the North Qiangtang terrane.Journal of the Geological Society,172(5):614-623
Liang X,Wang GH,Yang B,Ran H,Zheng YL,Du JX and Li LG.2017.Stepwise exhumation of the Triassic Lanling high-pressure metamorphic belt in Central Qiangtang,Tibet:Insights from a coupled study of metamorphism,deformation,and geochronology.Tectonics,36(4):652-670,doi:10.1002/2016TC004455
Liu WB,Qian Q,Yue GL,Li QS,Zhang Q and Zhou MF.2002.The Geochemical characteristics of fore-arc ophiolite from Dingqing area,Tibet.Acta Petrologica Sinica,18(3):392-400(in Chinese with English abstract)
Ludwig KR.2003.User’s Manual for isoplot/ex version 3.00:Ageochronological toolkit for Microsoft excel.Berkeley:Berkeley Geochronology Center,Special Publication,1-70
Ma L,Li ZX,Li Y,Liu H,Wu CS,Wei HW and Deng Q.2016.Zircon U-Pb age,geochemical characteristics and geological significance of Shanzixingshan Basalt in Shuanghu,Northern Tibet.Geoscience,30(4):748-759(in Chinese with English abstract)
Mao XC,Wang GH,Liang X,Zhang F,Liu Y,Liu JP,Zheng YL and Niu WC.2015.Practice and exploration of 1∶50000 geological mapping in accretionary complex belt:An example from Qomo Ri area of Central Qiangtang,Tibet.Earth Science Frontiers,22(3):382-393(in Chinese with English abstract)
Metcalfe I.2013.Gondwana dispersion and Asian accretion:Tectonic and palaeogeographic evolution of eastern Tethys.Journal of Asian Earth Sciences,66:1-33
Miyashiro A.1974.Volcanic rock series in island arcs and active continental margins.American Journal of Science,274(4):321-355
Mo XX and Pan GT.2006.From the Tethys to the formation of the Qinghai-Tibet Plateau:Constrained by tectono-magmatic events.Earth Science Frontiers,13(6):43-51(in Chinese with English abstract)
Moore JC and Silver EA.1987.Continental margin tectonics:Submarine accretionary prisms.Reviews of Geophysics,25(6):1305-1312
Pan GT,Mo XX,Hou ZQ,Zhu DC,Wang LQ,Li GM,Zhao ZD,Geng QR and Liao ZL.2006.Spatial-temporal framework of the Gangdese orogenic belt and its evolution.Acta Petrologica Sinica,22(3):521-533(in Chinese with English Abstract)
Pan GT,Wang LQ,Li RS,Yuan SH,Ji WH,Yin FG,Zhang WP and Wang BD.2012.Tectonic evolution of the Qinghai-Tibet Plateau.Journal of Asian Earth Sciences,53:3-14
Pearce JA and Cann JR.1971.Ophiolite origin investigated by discriminant analysis using Ti,Zr and Y.Earth and Planetary Science Letters,12(3):339-349
Pearce JA and Cann JR.1973.Tectonic setting of basic volcanic rocks determined using trace element analyses.Earth and Planetary Science Letters,19(2):290-300
Pearce JA and Norry MJ.1979.Petrogenetic implications of Ti,Zr,Y,and Nb variations in volcanic rocks.Contributions to Mineralogy and Petrology,69(1):33-47
Pearce JA.1983.Role of the sub-continental lithosphere in magma genesis at active continental margins.In:Hawkesworth CJ and Norry MJ(eds.).Continental Basalts and Mantle Xenoliths.Nantwich,Cheshire:Shiva Publications,230-249
Pearce JA.2003.Supra-subduction zone ophiolites:The search for modern analogues.In:Dilek Y and Newcomb S(eds.).Ophiolite Concept and the Evolution of Geological Thought.Colorado:Geological Society of America,373:269-293
Pearce JA.2014.Immobile element fingerprinting of ophiolites.Elements,10(2):101-108
Pullen A,Kapp P,Gehrels GE,Vervoort JD and Ding L.2008.Triassic continental subduction in central Tibet and Mediterranean-style closure of the Paleo-tethys Ocean.Geology,36(5):351-354
Reymer A and Schubert G.1984.Phanerozoic addition rates to the continental crust and crustal growth.Tectonics,3(1):63-77
Rogers G,Saunders AD,Terrell DJ,Verma SP and Marriner GF.1985.Geochemistry of Holocene volcanic rocks associated with ridge subduction in Baja California,Mexico.Nature,315(6018):389-392
Sang M,Xiao WJ,Orozbaev R,Bakirov A,Sakiev K,Pak N,Ivleva E,Zhou KF,Ao SJ,Qiao QQ and Zhang ZX.2018.Structural styles and zircon ages of the South Tianshan accretionary complex,Atbashi Ridge,Kyrgyzstan:Insights for the anatomy of ocean plate stratigraphy and accretionary processes.Journal of Asian Earth Sciences,153:9-41
Shervais JW.1982.Ti-V plots and the petrogenesis of modern and ophiolitic lavas.Earth and Planetary Science Letters,59(1):101-118
Song B.2015.SHRIMP zircon U-Pb age measurement:Sample preparation,measurement,data processing and explanation.Geological Bulletin of China,34(10):1777-1788(in Chinese with English abstract)
Song DF,Xiao WJ,Han CM and Tian ZH.2013.Geochronological and geochemical study of gneiss-schist complexes and associated granitoids,Beishan Orogen,southern Altaids.International Geology Review,55(14):1705-1727
Stacey JS and Kramers JD.1975.Approximation of terrestrial lead isotope evolution by a two-stage model.Earth and Planetary Science Letters,26(2):207-221
Sun SS and Mc Donough WF.1989.Chemical and isotopic systematics of oceanic basalts:Implications for mantle composition and processes.In:Saunders AD and Norry MJ(eds.).Magmatism in the Ocean Basins.Geological Society,London,Special Publication,42(1):313-345
Takami M and Itaya T.1996.Episodic accretion and metamorphism of Jurassic accretionary complex based on biostratigraphy and K-Ar geochronology in the western part of the Mino-Tanba Belt,Southwest Japan.Island Arc,5(3):321-336
von Huene R and Scholl DW.1991.Observations at convergent margins concerning sediment subduction,subduction erosion,and the growth of continental crust.Reviews of Geophysics,29(3):279-316
Wang GH,Han FL,Yang YJ,Li YQ and Cui JL.2009.Discovery and geologic significance of Late Paleozoic accretionary complexes in central Qiangtang,northern Tibet,China.Geological Bulletin of China,28(9):1181-1187(in Chinese with English abstract)
Wang Q,Xu SC,Wei RZ,Yang YS,Tian ZY,Dong AG,Yang WB and Wei YF.2006.Characteristics and tectonic setting of volcanic rocks of the Permian Zhanjin Formation in the Tuoheping Co area,northern Qiangtang,Qinghai-Tibet Plateau.Geological Bulletin of China,25(1-2):146-155(in Chinese with English abstract)
Wang Q,Wyman DA,Xu JF,Wan YS,Li CF,Zi F,Jiang ZQ,Qiu HN,Chu ZY,Zhao ZH and Dong YH.2008.Triassic Nb-enriched basalts,magnesian andesites,and adakites of the Qiangtang terrane(Central Tibet):Evidence for metasomatism by slab-derived melts in the mantle wedge.Contributions to Mineralogy and Petrology,155(4):473-490
Wendl RF,Altherr R,Neumann ER and Baldridge WS.2006.APetrology,geochemistry,isotopes.Developments in Geotectonics,25:47-60
White WM.1993.238U/204Pb in MORB and open system evolution of the depleted mantle.Earth and Planetary Science Letters,115(1-4):211-226
Winchester JA and Floyd PA.1977.Geochemical discrimination of different magma series and their differentiation products using immobile elements.Chemical Geology,20:325-343
Workman RK and Hart SR.2005.Major and trace element composition of the depleted MORB mantle(DMM).Earth and Planetary Science Letters,231(1-2):53-72
Wu H,Xu W,Li C,Sun SL and Jiang QY.2018.Partial melting of subducted Southern Qiangtang crust in northern Tibet:Evidence from the geochemistry and geochronology of the Riwanchaka granodiorite porphyry in Central Qiangtang.International Geology Review,1-16
Wu YB and Zheng YF.2004.Genesis of zircon and its constraints on interpretation of U-Pb age.Chinese Science Bulletin,49(15):1554-1569
Wu YW.2013.The evolution record of Longmuco-Shuanghu-Lancang ocean:Cambrian-Permian ophiolites.Ph.D.Dissertation.Changchun:Jilin University,1-162(in Chinese with English summary)
Xiao WJ,Zhang LC,Qin KZ,Sun S and Li JL.2004.Paleozoic accretionary and collisional tectonics of the Eastern Tianshan(China):Implications for the continental growth of central Asia.American Journal of Science,304(4):370-395
Xu JF,Chen FR,Yu XY,Niu HC and Zheng ZP.2001.Kuerti ophiolite in Altay area of North Xinjiang:Magmatism of an ancient back-arc basin.Acta Petrologica et Mineralogica,20(3):344-352(in Chinese with English abstract)
Xu W,Li C,Wang M,Fan JJ,Wu H and Li X.2017.Subduction of a spreading ridge within the Bangong Co-Nujiang Tethys Ocean:Evidence from Early Cretaceous mafic dykes in the Duolong porphyry Cu-Au deposit,western Tibet.Gondwana Research,41:128-141
Xu ZQ,Yang JS,Li HB,Ji SC,Zhang ZM and Liu Y.2011.On the tectonics of the India-Asia collision.Acta Geologica Sinica,85(1):1-33(in Chinese with English abstract)
Yin A and Harrison TM.2000.Geologic evolution of the HimalayanTibetan orogen.Annual Review of Earth and Planetary Sciences,28(1):211-280
Zeng LS,Gao LE,Guo CL,Hou KJ and Wang Q.2017.Early Cretaceous forearc extension of the Gangdese continental arc,southern Tibet.Acta Petrologica Sinica,33(8):2377-2394(in Chinese with English abstract)
Zhai QG,Li C and Huang XP.2006.Geochemistry of Permian basalt in the Jiaomuri area,central Qiangtang,Tibet,China,and its tectonic significance.Geological Bulletin of China,25(12):1419-1427(in Chinese with English abstract)
Zhai QG,Zhang RY,Jahn BM,Li C,Song SG and Wang J.2011a.Triassic eclogites from central Qiangtang,northern Tibet,China:Petrology,geochronology and metamorphic P-T path.Lithos,125(1-2):173-189
Zhai QG,Jahn BM,Zhang RY,Wang J and Su L.2011b.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 QG,Jahn BM,Su L,Wang J,Mo XX,Lee HY,Wang KL and Tang SH.2013a.Triassic arc magmatism in the Qiangtang area,northern Tibet:Zircon U-Pb ages,geochemical and Sr-Nd-Hf isotopic characteristics,and tectonic implications.Journal of Asian Earth Sciences,63:162-178
Zhai QG,Jahn BM,Su L,Ernst RE,Wang KL,Zhang RY,Wang J and Tang SH.2013b.SHRIMP zircon U-Pb geochronology,geochemistry and Sr-Nd-Hf isotopic compositions of a mafic dyke swarm in the Qiangtang terrane,northern Tibet and geodynamic implications.Lithos,174:28-43
Zhang KJ,Tang XC,Wang Y and Zhang YX.2011.Geochronology,geochemistry,and Nd isotopes of Early Mesozoic bimodal volcanism in northern Tibet,western China:Constraints on the exhumation of the central Qiangtang metamorphic belt.Lithos,121(1-4):167-175
Zhang YX,Jin X,Zhang KJ,Sun WD,Liu JM,Zhou XY and Yan LL.2018.Newly discovered Late Triassic Baqing eclogite in central Tibet indicates an anticlockwise West-East Qiangtang collision.Scientific Reports,8:966
Zhao JH and Zhou MF.2009.Secular evolution of the Neoproterozoic lithospheric mantle underneath the northern margin of the Yangtze Block,South China.Lithos,107(3-4),152-168
Zhao ZH.2016.Principles of Trace Element Geochemistry.2ndEdition.Beijing:Science Press,1-534(in Chinese)
Zhu DC,Pan GT,Mo XX,Liao ZL,Jiang XS,Wang LQ and Zhao ZD.2005.Geochemistry and petrogenesis of the Sangxiu Formation basalts in the central segment of Tethyan Himalaya.Geochimica,34(1):7-19(in Chinese with English abstract)
Zhu DC,Pan GT,Mo XX,Wang LQ,Zhao ZD,Liao ZL,Geng QR and Dong GC.2006.Identification for the Mesozoic OIB-type basalts in central Qinghai-Tibetan Plateau:Geochronology,geochemistry and their tectonic setting.Acta Geologica Sinica,80(9):1312-1328(in Chinese with English abstract)
Zhu GQ,Cheng XG,Yang SF and Chen HL.1997.Two types of basic models for continental crust accretion and their comparison.Geological Journal of China Universities,3(4):411-418(in Chinese with English abstract)
Zindler A and Hart S.1986.Chemical geodynamics.Annual review of earth and planetary sciences,14(1):493-571
邓万明,尹集祥,呙中平.1996.羌塘茶布-双湖地区基性超基性岩和火山岩研究.中国科学(D辑),26(4):296-301
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,翟庆国,董永胜,于介江,黄小鹏.2007.青藏高原羌塘中部果干加年山上三叠统望湖岭组的建立及意义.地质通报,26(8):1003-1008
李才,翟刚毅,王立全,尹福光,毛晓长.2009.认识青藏高原的重要窗口---羌塘地区近年来研究进展评述(代序).地质通报,28(9):1169-1177
李静超,赵中宝,郑艺龙,袁国礼,梁晓,王根厚,刘曦.2015.古特提斯洋俯冲碰撞在南羌塘的岩浆岩证据:西藏荣玛乡冈塘错花岗岩.岩石学报,31(7):2078-2088
李继亮.2004.增生型造山带的基本特征.地质通报,23(9-10):947-951
李林贵,梁晓,王根厚,王训练,高曦,焦鹏伟,黄祖根.2018.西藏羌塘增生杂岩带内中-晚三叠世碳酸盐岩地层的发现及大地构造意义.地质学报,92(4):828-844
李朋武,高锐,崔军文,管烨.2005.西藏和云南三江地区特提斯洋盆演化历史的古地磁分析.地球学报,26(5):387-404
李朋武,高锐,管烨,李秋生.2009.古特提斯洋的闭合时代的古地磁分析:松潘复理石杂岩形成的构造背景.地球学报,30(1):39-50
李瑞保,裴先治,李佐臣,裴磊,陈国超,刘成军,陈有炘,刘战庆.2014.东昆仑南缘布青山构造混杂带哥日卓托洋岛玄武岩地球化学特征及构造意义.地学前缘,21(1):183-195
李曰俊,吴浩若.1997.藏北阿木岗群,查叠群和鲁谷组放射虫的发现及有关问题讨论.地质论评,43(3):250-256
刘文斌,钱青,岳国利,李秋生,张旗,周美付.2002.西藏丁青弧前蛇绿岩的地球化学特征.岩石学报,18(3):392-400
马龙,李忠雄,李勇,刘函,吴成书,卫红伟,邓奇.2016.藏北双湖山字形山玄武岩锆石U-Pb年龄、地球化学特征及其地质意义.现代地质,30(4):748-759
毛晓长,王根厚,梁晓,张锋,刘洋,刘军平,郑艺龙,牛文超.2015.增生杂岩带1∶5万地质填图的实践与探索:以西藏羌塘中部角木日地区为例.地学前缘,22(3):382-393
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
潘桂棠,莫宣学,侯增谦,朱弟成,王立全,李光明,赵志丹,耿全如,廖忠礼.2006.冈底斯造山带的时空结构及演化.岩石学报,22(3):521-533
宋彪.2015.用SHRIMP测定锆石U-Pb年龄的工作方法.地质通报,34(10):1777-1788
王根厚,韩芳林,杨运军,李元庆,崔江利.2009.藏北羌塘中部晚古生代增生杂岩的发现及其地质意义.地质通报,28(9):1181-1187
王权,续世朝,魏荣珠,杨月生,田志勇,董挨管,杨五宝,魏云峰.2006.青藏高原羌塘北部托和平错一带二叠系展金组火山岩的特征及构造环境.地质通报,25(1-2):146-155
吴元保,郑永飞.2004.锆石成因矿物学研究及其对U-Pb年龄解释的制约.科学通报,49(16):1589-1604
吴彦旺.2013.龙木错-双湖-澜沧江洋历史记录---寒武纪-二叠纪的蛇绿岩.博士学位论文.长春:吉林大学,1-162
许继峰,陈繁荣,于学元,牛贺才,郑作平.2001.新疆北部阿尔泰地区库尔提蛇绿岩:古弧后盆地系统的产物.岩石矿物学杂志,20(3):344-352
许志琴,杨经绥,李海兵,嵇少丞,张泽明,刘焰.2011.印度-亚洲碰撞大地构造.地质学报,85(1):1-33
曾令森,高利娥,郭春丽,侯可军,王倩.2017.西藏南部冈底斯大陆弧早白垩纪弧前伸展作用.岩石学报,33(8):2377-2394
翟庆国,李才,黄小鹏.2006.西藏羌塘中部角木日地区二叠纪玄武岩的地球化学特征及其构造意义.地质通报,25(12):1419-1427
赵振华.2016.微量元素地球化学原理.第2版.北京:科学出版社,1-534
朱弟成,潘桂棠,莫宣学,廖忠礼,江新胜,王立全,赵志丹.2005.特提斯喜马拉雅带中段桑秀组玄武岩的地球化学和岩石成因.地球化学,34(1):7-19
朱弟成,潘桂棠,莫宣学,王立全,赵志丹,廖忠礼,耿全如,董国臣.2006.青藏高原中部中生代OIB型玄武岩的识别:年代学、地球化学及其构造环境.地质学报,80(9):1312-1328
竺国强,程晓敢,杨树锋,陈汉林.1997.试论陆壳增生的两种基本模式及其对比.高校地质学报,3(4):411-418
Bédard JH.1999.Petrogenesis of boninites from the Betts Cove ophiolite,Newfoundland,Canada:Identification of subducted source components.Journal of Petrology,40(12):1853-1889
Bickford ME.1988.The formation of continental crust:Part 1.A review of some principles;Part 2.An application to the Proterozoic evolution of southern North America.GSA Bulletin,100(9):1375-1391
Castillo PR.2008.Origin of the adakite-high-Nb basalt association and its implications for postsubduction magmatism in Baja California,Mexico.GSA Bulletin,120(3-4):451-462
Chen F,Hegner E and Todt W.2000.Zircon ages and Nd isotopic and chemical compositions of orthogneisses from the Black Forest,Germany:Evidence for a Cambrian magmatic arc.International Journal of Earth Sciences,88(4):791-802
Chen FK,Li XH,Wang XL,Li QL and Siebel W.2007.Zircon age and Nd-Hf isotopic composition of the Yunnan Tethyan belt,southwestern China.International Journal of Earth Sciences,96(6):1179-1194
Chen SS,Shi RD,Yi GD and Zou HB.2016.Middle Triassic volcanic rocks in the Northern Qiangtang(Central Tibet):Geochronology,petrogenesis,and tectonic implications.Tectonophysics,666:90-102
Condie KC.1993.Chemical composition and evolution of the upper continental crust:Contrasting results from surface samples and shales.Chemical Geology,104(1-4):1-37
Dan W,Wang Q,White WM,Zhang XZ,Tang GJ,Jiang ZQ,Hao LLand Ou Q.2018.Rapid formation of eclogites during a nearly closed ocean:Revisiting the Pianshishan eclogite in Qiangtang,central Tibetan Plateau.Chemical Geology,477:112-122
Davis D,Suppe J and Dahlen FA.1983.Mechanics of fold-and-thrust belts and accretionary wedges.Journal of Geophysical Research:Solid Earth,88(B2):1153-1172
Deng WM,Yin JX and Guo ZP.1996.Basic-ultrabasic and volcanic rocks in Chagbu-Shuanghu area of northern Xizang(Tibet),China.Science in China(Series D),39(4):359-368
Dilek Y and Furnes H.2011.Ophiolite genesis and global tectonics:Geochemical and tectonic fingerprinting of ancient oceanic lithosphere.GSA Bulletin,123(3-4):387-411
Dilek Y and Furnes H.2014.Ophiolites and their origins.Elements,10(2):93-100
Elliot T.2003.Tracers of the slab.In:Eiler J(ed.).Inside the Subduction Factory.Washington:American Geophysical Union,23-45
Frey FA,Green DH and Roy SD.1978.Integrated models of basalt petrogenesis:A study of quartz tholeiites to olivine melilitites from South Eastern Australia:Utilizing geochemical and experimental petrological data.Journal of Petrology,19(3):463-513
Furukawa Y.2011.Simple flow models of accretionary prisms:Predictions for coexisting arc-normal compression and extension,and implications for locked zones on the interplate megathrust.Tectonophysics,505(1-4):57-67
Gorring ML and Kay SM.2001.Mantle processes and sources of Neogene slab window magmas from southern Patagonia,Argentina.Journal of Petrology,42(6):1067-1094
Hoffman PF.1988.United plates of America,the birth of a craton:Early Proterozoic assembly and growth of Laurentia.Annual Review of Earth and Planetary Sciences,16:543-603
Hofmann AW.1997.Mantle geochemistry:The message from oceanic volcanism.Nature,385(6613):219-229
Kapp P,Yin A,Manning CE,Harrison TM,Taylor MH and Ding L.2003.Tectonic evolution of the Early Mesozoic blueschist-bearing Qiangtang metamorphic belt,central Tibet.Tectonics,22(4):1043
Keto LS and Jacobsen SB.1987.Nd and Sr isotopic variations of Early Paleozoic oceans.Earth and Planetary Science Letters,84(1):27-41
Li C.1987.The Longmucuo-Shuanghu-Lancangjiang plate suture and the north boundary of distribution of Gondwana facies PermianCarboniferous system in northern Xizang,China.Journal of Changchun University of Earth Science,17(2):155-166(in Chinese)
Li C,Zhai QG,Dong YS,Yu JJ and Huang XP.2007.Establishment of the Upper Triassic Wanghuling Formation at Guoganjianian mountain,central Qiangtang,Qinghai-Tibet Plateau,and its significance.Geological Bulletin of China,26(8):1003-1008(in Chinese with English abstract)
Li C,Zhai GY,Wang LQ,Yin FG and Mao XC.2009.An important window for understanding the Qinghai-Tibet Plateau:A review on research progress in recent years of Qiangtang area,Tibet,China.Geological Bulletin of China,28(9):1169-1177(in Chinese with English abstract)
Li D,Wang GH,Gao JH,Yuan GL,Zhou J,Fang DR,Zhang L,Gong YD and Zhao HC.2018.The continental subduction in the evolution of central Qiangtang mélange belt and its tectonic significance.International Geology Review,doi:10.1080/00206814.2018.1499450
Li JC,Zhao ZB,Zheng YL,Yuan GL,Liang X,Wang GH and Liu X.2015.The magmatite evidences in southern Qiangtang for paleoTethys ocean subducting collision:Gangtang-Co granites in Rongma,Tibet.Acta Petrologica Sinica,31(7):2078-2088(in Chinese with English abstract)
Li JL.2004.Basic characteristics of accretion-type orogens.Geological Bulletin of China,23(9-10):947-951(in Chinese with English abstract)
Li LG,Liang X,Wang GH,Wang XL,Gao X,Jiao PW and Huang ZG.2018.Discovery of the middle-late Triassic carbonatite formation in the central Qiangtang accretionary complex,North Tibet and its tectonic significance.Acta Geologica Sinica,92(4):828-844(in Chinese with English abstract)
Li PW,Gao R,Cui JW and Guan Y.2005.Paleomagnetic results from the Three Rivers Region,SW China:Implications for the collisional and accretionary history.Acta Geoscientica Sinica,26(5):387-404(in Chinese with English abstract)
Li PW,Gao R,Guan Y and Li QS.2009.Paleomagnetic constraints on the closure time of Paleo-Tethys:Implications for the tectonic setting of formation of Triassic Songpan-Ganzi flysch complex.Acta Geoscientica Sinica,30(1):39-50(in Chinese with English abstract)
Li RB,Pei XZ,Li ZC,Pei L,Chen GC,Liu CJ,Chen YX and Liu ZQ.2014.Geochemical characteristics of Gerizhuotuo OIB and its tectonic significance in Buqingshan tectonic mélange belt,southern margin of East Kunlun Orogen.Earth Science Frontiers,21(1):183-195(in Chinese with English abstract)
Li YJ,Wu HR and Li HS.1997.Discovery of radioarians in the Amugang and Chasang groups and Lugu Formation in northern Tibet and some related geological problems.Geological Review,43(3):250-256(in Chinese with English abstract)
Liang X,Wang GH,Yuan GL and Liu Y.2012.Structural sequence and geochronology of the Qomo Ri accretionary complex,Central Qiangtang,Tibet:Implications for the Late Triassic subduction of the Paleo-Tethys Ocean.Gondwana Research,22(2):470-481
Liang X,Wang GH,Yuan GL and Che XC.2015.Mesozoic and Cenozoic deformations in the Raggyorcaka area,Tibet:Implications for the tectonic evolution of the North Qiangtang terrane.Journal of the Geological Society,172(5):614-623
Liang X,Wang GH,Yang B,Ran H,Zheng YL,Du JX and Li LG.2017.Stepwise exhumation of the Triassic Lanling high-pressure metamorphic belt in Central Qiangtang,Tibet:Insights from a coupled study of metamorphism,deformation,and geochronology.Tectonics,36(4):652-670,doi:10.1002/2016TC004455
Liu WB,Qian Q,Yue GL,Li QS,Zhang Q and Zhou MF.2002.The Geochemical characteristics of fore-arc ophiolite from Dingqing area,Tibet.Acta Petrologica Sinica,18(3):392-400(in Chinese with English abstract)
Ludwig KR.2003.User’s Manual for isoplot/ex version 3.00:Ageochronological toolkit for Microsoft excel.Berkeley:Berkeley Geochronology Center,Special Publication,1-70
Ma L,Li ZX,Li Y,Liu H,Wu CS,Wei HW and Deng Q.2016.Zircon U-Pb age,geochemical characteristics and geological significance of Shanzixingshan Basalt in Shuanghu,Northern Tibet.Geoscience,30(4):748-759(in Chinese with English abstract)
Mao XC,Wang GH,Liang X,Zhang F,Liu Y,Liu JP,Zheng YL and Niu WC.2015.Practice and exploration of 1∶50000 geological mapping in accretionary complex belt:An example from Qomo Ri area of Central Qiangtang,Tibet.Earth Science Frontiers,22(3):382-393(in Chinese with English abstract)
Metcalfe I.2013.Gondwana dispersion and Asian accretion:Tectonic and palaeogeographic evolution of eastern Tethys.Journal of Asian Earth Sciences,66:1-33
Miyashiro A.1974.Volcanic rock series in island arcs and active continental margins.American Journal of Science,274(4):321-355
Mo XX and Pan GT.2006.From the Tethys to the formation of the Qinghai-Tibet Plateau:Constrained by tectono-magmatic events.Earth Science Frontiers,13(6):43-51(in Chinese with English abstract)
Moore JC and Silver EA.1987.Continental margin tectonics:Submarine accretionary prisms.Reviews of Geophysics,25(6):1305-1312
Pan GT,Mo XX,Hou ZQ,Zhu DC,Wang LQ,Li GM,Zhao ZD,Geng QR and Liao ZL.2006.Spatial-temporal framework of the Gangdese orogenic belt and its evolution.Acta Petrologica Sinica,22(3):521-533(in Chinese with English Abstract)
Pan GT,Wang LQ,Li RS,Yuan SH,Ji WH,Yin FG,Zhang WP and Wang BD.2012.Tectonic evolution of the Qinghai-Tibet Plateau.Journal of Asian Earth Sciences,53:3-14
Pearce JA and Cann JR.1971.Ophiolite origin investigated by discriminant analysis using Ti,Zr and Y.Earth and Planetary Science Letters,12(3):339-349
Pearce JA and Cann JR.1973.Tectonic setting of basic volcanic rocks determined using trace element analyses.Earth and Planetary Science Letters,19(2):290-300
Pearce JA and Norry MJ.1979.Petrogenetic implications of Ti,Zr,Y,and Nb variations in volcanic rocks.Contributions to Mineralogy and Petrology,69(1):33-47
Pearce JA.1983.Role of the sub-continental lithosphere in magma genesis at active continental margins.In:Hawkesworth CJ and Norry MJ(eds.).Continental Basalts and Mantle Xenoliths.Nantwich,Cheshire:Shiva Publications,230-249
Pearce JA.2003.Supra-subduction zone ophiolites:The search for modern analogues.In:Dilek Y and Newcomb S(eds.).Ophiolite Concept and the Evolution of Geological Thought.Colorado:Geological Society of America,373:269-293
Pearce JA.2014.Immobile element fingerprinting of ophiolites.Elements,10(2):101-108
Pullen A,Kapp P,Gehrels GE,Vervoort JD and Ding L.2008.Triassic continental subduction in central Tibet and Mediterranean-style closure of the Paleo-tethys Ocean.Geology,36(5):351-354
Reymer A and Schubert G.1984.Phanerozoic addition rates to the continental crust and crustal growth.Tectonics,3(1):63-77
Rogers G,Saunders AD,Terrell DJ,Verma SP and Marriner GF.1985.Geochemistry of Holocene volcanic rocks associated with ridge subduction in Baja California,Mexico.Nature,315(6018):389-392
Sang M,Xiao WJ,Orozbaev R,Bakirov A,Sakiev K,Pak N,Ivleva E,Zhou KF,Ao SJ,Qiao QQ and Zhang ZX.2018.Structural styles and zircon ages of the South Tianshan accretionary complex,Atbashi Ridge,Kyrgyzstan:Insights for the anatomy of ocean plate stratigraphy and accretionary processes.Journal of Asian Earth Sciences,153:9-41
Shervais JW.1982.Ti-V plots and the petrogenesis of modern and ophiolitic lavas.Earth and Planetary Science Letters,59(1):101-118
Song B.2015.SHRIMP zircon U-Pb age measurement:Sample preparation,measurement,data processing and explanation.Geological Bulletin of China,34(10):1777-1788(in Chinese with English abstract)
Song DF,Xiao WJ,Han CM and Tian ZH.2013.Geochronological and geochemical study of gneiss-schist complexes and associated granitoids,Beishan Orogen,southern Altaids.International Geology Review,55(14):1705-1727
Stacey JS and Kramers JD.1975.Approximation of terrestrial lead isotope evolution by a two-stage model.Earth and Planetary Science Letters,26(2):207-221
Sun SS and Mc Donough WF.1989.Chemical and isotopic systematics of oceanic basalts:Implications for mantle composition and processes.In:Saunders AD and Norry MJ(eds.).Magmatism in the Ocean Basins.Geological Society,London,Special Publication,42(1):313-345
Takami M and Itaya T.1996.Episodic accretion and metamorphism of Jurassic accretionary complex based on biostratigraphy and K-Ar geochronology in the western part of the Mino-Tanba Belt,Southwest Japan.Island Arc,5(3):321-336
von Huene R and Scholl DW.1991.Observations at convergent margins concerning sediment subduction,subduction erosion,and the growth of continental crust.Reviews of Geophysics,29(3):279-316
Wang GH,Han FL,Yang YJ,Li YQ and Cui JL.2009.Discovery and geologic significance of Late Paleozoic accretionary complexes in central Qiangtang,northern Tibet,China.Geological Bulletin of China,28(9):1181-1187(in Chinese with English abstract)
Wang Q,Xu SC,Wei RZ,Yang YS,Tian ZY,Dong AG,Yang WB and Wei YF.2006.Characteristics and tectonic setting of volcanic rocks of the Permian Zhanjin Formation in the Tuoheping Co area,northern Qiangtang,Qinghai-Tibet Plateau.Geological Bulletin of China,25(1-2):146-155(in Chinese with English abstract)
Wang Q,Wyman DA,Xu JF,Wan YS,Li CF,Zi F,Jiang ZQ,Qiu HN,Chu ZY,Zhao ZH and Dong YH.2008.Triassic Nb-enriched basalts,magnesian andesites,and adakites of the Qiangtang terrane(Central Tibet):Evidence for metasomatism by slab-derived melts in the mantle wedge.Contributions to Mineralogy and Petrology,155(4):473-490
Wendl RF,Altherr R,Neumann ER and Baldridge WS.2006.APetrology,geochemistry,isotopes.Developments in Geotectonics,25:47-60
White WM.1993.238U/204Pb in MORB and open system evolution of the depleted mantle.Earth and Planetary Science Letters,115(1-4):211-226
Winchester JA and Floyd PA.1977.Geochemical discrimination of different magma series and their differentiation products using immobile elements.Chemical Geology,20:325-343
Workman RK and Hart SR.2005.Major and trace element composition of the depleted MORB mantle(DMM).Earth and Planetary Science Letters,231(1-2):53-72
Wu H,Xu W,Li C,Sun SL and Jiang QY.2018.Partial melting of subducted Southern Qiangtang crust in northern Tibet:Evidence from the geochemistry and geochronology of the Riwanchaka granodiorite porphyry in Central Qiangtang.International Geology Review,1-16
Wu YB and Zheng YF.2004.Genesis of zircon and its constraints on interpretation of U-Pb age.Chinese Science Bulletin,49(15):1554-1569
Wu YW.2013.The evolution record of Longmuco-Shuanghu-Lancang ocean:Cambrian-Permian ophiolites.Ph.D.Dissertation.Changchun:Jilin University,1-162(in Chinese with English summary)
Xiao WJ,Zhang LC,Qin KZ,Sun S and Li JL.2004.Paleozoic accretionary and collisional tectonics of the Eastern Tianshan(China):Implications for the continental growth of central Asia.American Journal of Science,304(4):370-395
Xu JF,Chen FR,Yu XY,Niu HC and Zheng ZP.2001.Kuerti ophiolite in Altay area of North Xinjiang:Magmatism of an ancient back-arc basin.Acta Petrologica et Mineralogica,20(3):344-352(in Chinese with English abstract)
Xu W,Li C,Wang M,Fan JJ,Wu H and Li X.2017.Subduction of a spreading ridge within the Bangong Co-Nujiang Tethys Ocean:Evidence from Early Cretaceous mafic dykes in the Duolong porphyry Cu-Au deposit,western Tibet.Gondwana Research,41:128-141
Xu ZQ,Yang JS,Li HB,Ji SC,Zhang ZM and Liu Y.2011.On the tectonics of the India-Asia collision.Acta Geologica Sinica,85(1):1-33(in Chinese with English abstract)
Yin A and Harrison TM.2000.Geologic evolution of the HimalayanTibetan orogen.Annual Review of Earth and Planetary Sciences,28(1):211-280
Zeng LS,Gao LE,Guo CL,Hou KJ and Wang Q.2017.Early Cretaceous forearc extension of the Gangdese continental arc,southern Tibet.Acta Petrologica Sinica,33(8):2377-2394(in Chinese with English abstract)
Zhai QG,Li C and Huang XP.2006.Geochemistry of Permian basalt in the Jiaomuri area,central Qiangtang,Tibet,China,and its tectonic significance.Geological Bulletin of China,25(12):1419-1427(in Chinese with English abstract)
Zhai QG,Zhang RY,Jahn BM,Li C,Song SG and Wang J.2011a.Triassic eclogites from central Qiangtang,northern Tibet,China:Petrology,geochronology and metamorphic P-T path.Lithos,125(1-2):173-189
Zhai QG,Jahn BM,Zhang RY,Wang J and Su L.2011b.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 QG,Jahn BM,Su L,Wang J,Mo XX,Lee HY,Wang KL and Tang SH.2013a.Triassic arc magmatism in the Qiangtang area,northern Tibet:Zircon U-Pb ages,geochemical and Sr-Nd-Hf isotopic characteristics,and tectonic implications.Journal of Asian Earth Sciences,63:162-178
Zhai QG,Jahn BM,Su L,Ernst RE,Wang KL,Zhang RY,Wang J and Tang SH.2013b.SHRIMP zircon U-Pb geochronology,geochemistry and Sr-Nd-Hf isotopic compositions of a mafic dyke swarm in the Qiangtang terrane,northern Tibet and geodynamic implications.Lithos,174:28-43
Zhang KJ,Tang XC,Wang Y and Zhang YX.2011.Geochronology,geochemistry,and Nd isotopes of Early Mesozoic bimodal volcanism in northern Tibet,western China:Constraints on the exhumation of the central Qiangtang metamorphic belt.Lithos,121(1-4):167-175
Zhang YX,Jin X,Zhang KJ,Sun WD,Liu JM,Zhou XY and Yan LL.2018.Newly discovered Late Triassic Baqing eclogite in central Tibet indicates an anticlockwise West-East Qiangtang collision.Scientific Reports,8:966
Zhao JH and Zhou MF.2009.Secular evolution of the Neoproterozoic lithospheric mantle underneath the northern margin of the Yangtze Block,South China.Lithos,107(3-4),152-168
Zhao ZH.2016.Principles of Trace Element Geochemistry.2ndEdition.Beijing:Science Press,1-534(in Chinese)
Zhu DC,Pan GT,Mo XX,Liao ZL,Jiang XS,Wang LQ and Zhao ZD.2005.Geochemistry and petrogenesis of the Sangxiu Formation basalts in the central segment of Tethyan Himalaya.Geochimica,34(1):7-19(in Chinese with English abstract)
Zhu DC,Pan GT,Mo XX,Wang LQ,Zhao ZD,Liao ZL,Geng QR and Dong GC.2006.Identification for the Mesozoic OIB-type basalts in central Qinghai-Tibetan Plateau:Geochronology,geochemistry and their tectonic setting.Acta Geologica Sinica,80(9):1312-1328(in Chinese with English abstract)
Zhu GQ,Cheng XG,Yang SF and Chen HL.1997.Two types of basic models for continental crust accretion and their comparison.Geological Journal of China Universities,3(4):411-418(in Chinese with English abstract)
Zindler A and Hart S.1986.Chemical geodynamics.Annual review of earth and planetary sciences,14(1):493-571
邓万明,尹集祥,呙中平.1996.羌塘茶布-双湖地区基性超基性岩和火山岩研究.中国科学(D辑),26(4):296-301
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,翟庆国,董永胜,于介江,黄小鹏.2007.青藏高原羌塘中部果干加年山上三叠统望湖岭组的建立及意义.地质通报,26(8):1003-1008
李才,翟刚毅,王立全,尹福光,毛晓长.2009.认识青藏高原的重要窗口---羌塘地区近年来研究进展评述(代序).地质通报,28(9):1169-1177
李静超,赵中宝,郑艺龙,袁国礼,梁晓,王根厚,刘曦.2015.古特提斯洋俯冲碰撞在南羌塘的岩浆岩证据:西藏荣玛乡冈塘错花岗岩.岩石学报,31(7):2078-2088
李继亮.2004.增生型造山带的基本特征.地质通报,23(9-10):947-951
李林贵,梁晓,王根厚,王训练,高曦,焦鹏伟,黄祖根.2018.西藏羌塘增生杂岩带内中-晚三叠世碳酸盐岩地层的发现及大地构造意义.地质学报,92(4):828-844
李朋武,高锐,崔军文,管烨.2005.西藏和云南三江地区特提斯洋盆演化历史的古地磁分析.地球学报,26(5):387-404
李朋武,高锐,管烨,李秋生.2009.古特提斯洋的闭合时代的古地磁分析:松潘复理石杂岩形成的构造背景.地球学报,30(1):39-50
李瑞保,裴先治,李佐臣,裴磊,陈国超,刘成军,陈有炘,刘战庆.2014.东昆仑南缘布青山构造混杂带哥日卓托洋岛玄武岩地球化学特征及构造意义.地学前缘,21(1):183-195
李曰俊,吴浩若.1997.藏北阿木岗群,查叠群和鲁谷组放射虫的发现及有关问题讨论.地质论评,43(3):250-256
刘文斌,钱青,岳国利,李秋生,张旗,周美付.2002.西藏丁青弧前蛇绿岩的地球化学特征.岩石学报,18(3):392-400
马龙,李忠雄,李勇,刘函,吴成书,卫红伟,邓奇.2016.藏北双湖山字形山玄武岩锆石U-Pb年龄、地球化学特征及其地质意义.现代地质,30(4):748-759
毛晓长,王根厚,梁晓,张锋,刘洋,刘军平,郑艺龙,牛文超.2015.增生杂岩带1∶5万地质填图的实践与探索:以西藏羌塘中部角木日地区为例.地学前缘,22(3):382-393
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
潘桂棠,莫宣学,侯增谦,朱弟成,王立全,李光明,赵志丹,耿全如,廖忠礼.2006.冈底斯造山带的时空结构及演化.岩石学报,22(3):521-533
宋彪.2015.用SHRIMP测定锆石U-Pb年龄的工作方法.地质通报,34(10):1777-1788
王根厚,韩芳林,杨运军,李元庆,崔江利.2009.藏北羌塘中部晚古生代增生杂岩的发现及其地质意义.地质通报,28(9):1181-1187
王权,续世朝,魏荣珠,杨月生,田志勇,董挨管,杨五宝,魏云峰.2006.青藏高原羌塘北部托和平错一带二叠系展金组火山岩的特征及构造环境.地质通报,25(1-2):146-155
吴元保,郑永飞.2004.锆石成因矿物学研究及其对U-Pb年龄解释的制约.科学通报,49(16):1589-1604
吴彦旺.2013.龙木错-双湖-澜沧江洋历史记录---寒武纪-二叠纪的蛇绿岩.博士学位论文.长春:吉林大学,1-162
许继峰,陈繁荣,于学元,牛贺才,郑作平.2001.新疆北部阿尔泰地区库尔提蛇绿岩:古弧后盆地系统的产物.岩石矿物学杂志,20(3):344-352
许志琴,杨经绥,李海兵,嵇少丞,张泽明,刘焰.2011.印度-亚洲碰撞大地构造.地质学报,85(1):1-33
曾令森,高利娥,郭春丽,侯可军,王倩.2017.西藏南部冈底斯大陆弧早白垩纪弧前伸展作用.岩石学报,33(8):2377-2394
翟庆国,李才,黄小鹏.2006.西藏羌塘中部角木日地区二叠纪玄武岩的地球化学特征及其构造意义.地质通报,25(12):1419-1427
赵振华.2016.微量元素地球化学原理.第2版.北京:科学出版社,1-534
朱弟成,潘桂棠,莫宣学,廖忠礼,江新胜,王立全,赵志丹.2005.特提斯喜马拉雅带中段桑秀组玄武岩的地球化学和岩石成因.地球化学,34(1):7-19
朱弟成,潘桂棠,莫宣学,王立全,赵志丹,廖忠礼,耿全如,董国臣.2006.青藏高原中部中生代OIB型玄武岩的识别:年代学、地球化学及其构造环境.地质学报,80(9):1312-1328
竺国强,程晓敢,杨树锋,陈汉林.1997.试论陆壳增生的两种基本模式及其对比.高校地质学报,3(4):411-418
© 2004-2018 中国地质图书馆版权所有 京ICP备05064691号 京公网安备11010802017129号 地址：北京市海淀区学院路29号 邮编：100083 电话：办公室：(+86 10)66554848；文献借阅、咨询服务、科技查新：66554700 |