华北-西伯利亚板块对接带早白垩纪的裂解:来自西拉木伦断裂带中性岩墙群的锆石U-Pb年龄及地球化学证据
摘要
在内蒙古林西县西拉木伦断裂带内发育规模较大的中性岩墙群,岩墙多呈NE3°～5°近直立侵入.对岩石进行了锆石LA-ICP-MS U-Pb定年和详细的岩石地球化学特征研究.锆石LA-ICP-MS U-Pb年龄为132.2±2.2Ma,岩石侵位于早白垩世.岩石地球化学特征显示岩石具有高钾钙碱性系列-钾玄岩系列的过渡特征,形成于板内拉张环境,岩浆源区具有壳幔混源的特征,是早期俯冲洋壳遭受幔源岩浆底侵作用的结果.岩墙的产状受左旋剪切机制控制,该机制可能主要与太平洋板块相对亚洲板块的向北运动有关.
A large scale of intermediate dykes developed in Xar Moron fault belt in Linxi county,Inner-Mongolia,with NE3° to 5° angle of strike and nearly vertical trend.LA-ICP-MS zircon U-Pb dating method and whole rock geochemistry test were applied.It is indicated that the intermediate dykes emplaced in Lower Cretaceous with LA-ICP-MS zircon U-Pb age of 132.2±2.2 Ma.The whole rock geochemistry of the dykes reveals transition characteristics between high potassium calc-alkaline series and shoshonite series.They formed in intraplate extensional background and sourced from crust-mantle magmatic mixing,which result from the mantle magma underplating below the early subducted oceanic crust.The strike of the dykes was chronically controlled by a sinistral shear mechanism in the area,which might be related to the northward movement of Pacific plate to Asian plate.
A large scale of intermediate dykes developed in Xar Moron fault belt in Linxi county,Inner-Mongolia,with NE3° to 5° angle of strike and nearly vertical trend.LA-ICP-MS zircon U-Pb dating method and whole rock geochemistry test were applied.It is indicated that the intermediate dykes emplaced in Lower Cretaceous with LA-ICP-MS zircon U-Pb age of 132.2±2.2 Ma.The whole rock geochemistry of the dykes reveals transition characteristics between high potassium calc-alkaline series and shoshonite series.They formed in intraplate extensional background and sourced from crust-mantle magmatic mixing,which result from the mantle magma underplating below the early subducted oceanic crust.The strike of the dykes was chronically controlled by a sinistral shear mechanism in the area,which might be related to the northward movement of Pacific plate to Asian plate.
引文
Andersen,T.,2002.Correction of commonleadin U-Pb ana-lyses that do not report204Pb.Chemical Geology,192(1-2):59-79.doi:10.1016/S0009-2541(02)00195-X
Badarch,G.,Cuningham,W.D.,Windley,B.F.,2002.Anewterrane subdivision for Mongolia:i mplications forthe Phanerozoic crustal growth of Central Asia.Journalof Asian Earth Sciences,21(1):87-110.doi:10.1016/S1367-9120(02)00017-2
Chen,B.,Jahn,B.M.,Wilde,S.,et al.,2000.Two contras-ting Paleozoic magmatic belts in northern Inner Mongo-lia,China:petrogenesis and tectonic i mplications.Tectonophysics,328(1-2):157-182.doi:10.1016/S0040-1951(00)00182-7
Deng,J.F.,Su,S.G.,Liu,C.,et al.,2006.Discussion on thelithospheric thinning of the North China craton:delami-nation-or thermal erosion and chemical metasomatism-Earth Science Frontiers,13(2):105-119(in Chinesewith English abstract).
Deng,J.F.,Zhao,H.L.,Mo,X.X.,et al.,1996.Continentalroots-plume tectonics of China:key to the continentaldynamics.Geological Publishing House,Beijing,30-39(in Chinese).
Fukao,Y.,Obayashi,M.,Inoue,H.,et al.,1992.Subductingslabs stagnant in the mantle transition zone.Journal ofGeophysical Research,97:4809-4822.doi:10.1029/91JB02749
Halls,H.C.,1982.The i mportance and potential of maficdyke swarms in studies of geodynamic processes.Geo-sciences Canada,9:145-154.
Hong,D.W.,Wang,S.G.,Xie,X.L.,et al.,2000.Genesisof positiveεNd(t)granitoids in the Da Hinggan MTS-Mongolia oroganic belt and continental crustal growth.Earth Science Frontiers,7(2):441-456(in Chinesewith English abstract).
Hu,S.X.,Zhao,Y.Y.,Hu,Z.H.,et al.,1994.Evolutionand development of tectonics and magmatismat the ac-tive continental margin of the East China(E106°)dur-ing Mesozoic and Cenozoic.Acta Petrologica Sinica,10(4):370-381(in Chinese with English abstract).
Irvine,T.N.,Baragar,W.R.A.,1971.Aguide to the chemi-cal classification of the common volcanic rocks.Canadi-an Journal of Earth Sciences,8:523-548.
Jahn,B.M.,Capdevila,R.,Liu,D.,et al.,2004.Sources ofPhanerozoic granitoids in the transect Bayanhongor-Ul-aan Baatar,Mongolia:geochemical and Nd isotopic evi-dence,and i mplications for Phanerozoic crustal growth.Journal of Asian Earth Sciences,23(5):629-653.doi:10.1016/S1367-9120(03)00125-1
Khain,E.V.,Bibikova,E.V.,Kr ner,A.,et al.,2002.Themost ancient ophiolite of the Central Asian fold belt:U-Pb and Pb-Pb zircon ages for the Dunzhugur com-plex,eastern Sayan,Siberia,and geodynamic i mplica-tions.Earth and Planetary Science Letters,199(3-4):311-325.doi:10.1016/S0012-821X(02)00587-3
Khain,E.V.,Bibikova,E.V.,Salnikova,E.B.,et al.,2003.The Palaeo-Asian oceaninthe Neoproterozoic and EarlyPalaeozoic:new geochronologic data and palaeotectonicreconstructions.Precambrian Research,122(1-4):329-358.doi:10.1016/S0301-9268(02)00218-8
Li,P.W.,Gao,R.,Guan,Y.,et al.,2006.Palaeomagnetieconstraints on the final closure ti me of Solonker-Linxisuture.Journal of Jilin University(Earth Science E-dition),36(5):744-758(in Chinese with English ab-stract).
Li,Y.L.,Zhou,H.W.,Ge,M.C.,et al.,2007.Characteris-tics and genesis of migmatites within the northern ofShuangjing micro-plateinthe West Lamulunfault zone,Inner Mongolia.J.Mineral.Petrol.,27(4):22-29(inChinese with English abstract).
Li,Y.L.,Zhou,H.W.,Ge,M.C.,et al.,2008.LA-ICP-MSzircon U-Pb dating of migmatite from north ofShuangjing schist in Linxi,Inner Mongolia.J.Mineral.Petrol.,28(2):10-16(in Chinese with English ab-stract).
Li,Y.L.,Zhou,H.W.,Zhong,Z.Q.,et al.,2009.Collisionprocesses of North China and Siberian Plates:evidencefrom LA-ICP-MS zircon U-Pb age on deformed granitein Xar Moron suture zone.Earth Science—Journal ofChina University of Geosciences,34(6):931-938(inChinese with English abstract).
Lu,F.X.,Sang,L.K.,2002.Petrology.Geological Publish-ing House,Beijing,42-45(in Chinese).
Ludwig,K.R.,1991.Isoplot—a plotting and regression pro-gramfor radiogenic-isotope data.US Geological SurveyOpen-File Report,39:91-445.
Ma,Z.J.,Wang,G.Q.,1999.Strip-shaped tectonic divisionof contemporary lithospheric structure of eastern Chi-na.Geological Journal of China Universities,5(1):7-16(in Chinese with English abstract).
MacDonald,G.A.,Katsura,T.,1964.Chemical compositionof Hawaiian lavas.Journal of Petrology,5(1):82-133.doi:10.1093/petrology/5.1.82
McCulloch,M.T.,Gamble,J.A.,1989.Depleted source forvolcanic arc basalts:constraints from basalts of Kema-dec-Taupo volcanic zone based on trace elements,iso-topes and subduction chemical geodynamica.In:Conti-nental magmatism,Inter.Volcanic.Conf.Abstr.,NewMexico Bur.Miner.Resour.Bull.,131-180.
Miao,L.C.,Fan,W.M.,Liu,D.Y.,et al.,2008.Geochro-nology and geochemistry of the Hegenshan ophiolitecomplex:i mplications for late-stage tectonic evolution ofthe Inner Mongolia-Daxinganling orogenic belt,China.Journal of Asian Earth Sciences,32(5-6):348-370.doi:10.1016/j.jseaes.2007.11.005
Morrison,G.W.,1980.Characteristics and tectonic setting ofshoshonite rock association.Lithos,13(1):97-108.doi:10.1016/0024-4937(80)90067-5
Mller,D.,Groves,D.I.,1995.Potassic igneous rocks andassociated gold-copper mineralization.Springer Verlag,Berlin,1-144.
Pearce,J.A.,Gorman,B.E.,Birkett,T.C.,1975.The Ti O2-K2O-P2O5diagram,a method of discri mination betweenocean and non-ocean basalts.Earth and Planetary Sci-ence Letters,24:419-426.
Pearce,N.J.G.,Perkins,W.T.,Westgate,J.A.,et al.,1997.A compilation of new and published major andtrace element data for NIST SRM610and NIST SRM612glass reference materials.Geostandardand Geoana-lytical Research,21(1):115-144.doi:10.1111/j.1751-908X.1997.tb00538.x
Pearce,T.H.,Gorman,B.E.,Birkett,T.C.,1977.The rela-tionship between major element chemistry and tectonicenviroment of basic and intermediate volcanic rocks.Earth and Planetary Science Letters,36(1):121-132.doi:10.1016/0012-821X(77)90193-5
Ren,J.S.,Niu,B.G.,He,Z.J.,et al.,1997.Tectonic frame-work and geodynamic evolution of eastern China.Geo-logical Research,29(30):43-55(in Chinese with Eng-lish abstract).
Ren,J.S.,Wang,Z.X.,Chen,B.W.,et a1.,1999.The tec-tonics of China froma global view—a guide to the tec-tonic map of China and adjacent regions.GeologicalPublishing House,Beijing,32-33(in Chinese).
Seng r,A.M.C.,Natal in,B.A.,Burt man,V.S.,1993.Evolution of the Altaid tectonic collage and Palaeozoiccrustal growth in Eurasia.Nature,364:299-307.doi:10.1038/364299a0
Shang,Q.H.,2004.Occurrences of Permian radiolarians incentral and eastern Nei Mongol(Inner Mongolia)andtheir geological significance to the northern China oro-gen.Chinese Science Bulletin,49(24):2613-2619.doi:10.1360/04wd0069
Shao,J.A.,Gai,F.Y.,Zhang,L.Q.,1998.Coupling of man-tle-upwelling and shearing-Mesozoic dyke-swarms inDa-Hinggan mountains,Northeast China.Episodes,21:99-103.
Shao,J.A.,Liu,F.T.,Chen,H.,2001a.Relationship be-tween Mesozoic magmatismand subductionin Da Hing-gan-Yanshan area.Acta Geologica Sinica,75(1):56-63(in Chinese with English abstract).
Shao,J.A.,Zhang,L.Q.,2002.Mesozoic dyke swarms inthe north of North China.Acta Petrologica Sinica,18(3):312-318(in Chinese with English abstract).
Shao,J.A.,Zhang,L.Q.,Wei,C.J.,et al.,2001b.Composi-tion and features of the Mesozoic bi modal dike swarmin Nankou area,Beijing.Acta Geologica Sinica,75(2):205-212(in Chinese with English abstract).
Song,B.,Zhang,Y.H.,Wan,Y.S.,et al.,2002.Mountmaking and procedure of the SHRI MP dating.Geolog-ical Review,48(Suppl.):26-30(in Chinese with Eng-lish abstract).
Sun,D.Y.,Wu,F.Y.,Zhang,Y.B.,et al.,2004.The finalclosing ti me of the west Lamulun River-Changchun-Yanji plate suture zone—evidence from the Dayushangranitic pluton,Jilin Province.Journal of Jilin Univer-sity(Earth Science Edition),34(2):174-181(in Chi-nese with English abstract).
Sun,S.S.,McDonough,W.F.,1989.Chemical and isotopicsystematics of oceanic basalts:i mplications for mantlecomposition and processes.In:Saundern,A.D.,Norry,M.J.,eds.,Magmatismin the ocean basins.GeologicalSociety of London,Special Publications,42:313-345.doi:10.1144/GSL.SP.1989.042.01.19
Tang,K.D.,1990.Tectonic development of Paleozoic fold-belts at the north margin of the Sino-Korean craton.Tectonics,9:249-260.
The Second Regional Geological Survey Teamof Inner Mon-golia Autonomous Region,1997.1∶50000regional ge-ological surveys report on Shuangjing region(in Chi-nese).
Wang,Y.L.,Zhang,C.J.,Xiu,S.Z.,2001.Th/Hf-Ta/Hf i-dentification of tectonic setting of basalts.Acta Petro-logica Sinica,17(3):413-421(in Chinese with Eng-lish abstract).
Wiedenbeck,M.,Alle,P.,Corfu,F.,et al.,1995.Three nat-ural zircon standards for U-Th-Pb,Lu-Hf,trace elementand REE analyses.Geostand.Newsl.,19(1):1-23.doi:10.1111/j.1751-908X.1995.tb00147.x
Wu,F.Y.,Ge,W.C.,Sun,D.Y.,et al.,2003.Discussionson thelithospheric thinningin eastern China.Earth Sci-ence Frontiers,10(3):51-60(in Chinese with Englishabstract).
Wu,F.Y.,Sun,D.Y.,Lin,Q.,et al.,1999.Petrogenesis ofthe Phanerozoic granites and crustal growth in North-east China.Acta Petrologica Sinica,15(2):181-189(in Chinese with English abstract).
Wu,G.Y.,2002.The Yanshanian orogeny and Late Mesozo-ic activationin China continent.Chinese Journal of Ge-ology,37(4):453-461(in Chinese with English ab-stract).
Wu,L.R.,1985.Mesozoic granitoids in East China.ActaPetrologia Sinica,1(1):1-9(in Chinese with Englishabstract).
Xiao,W.J.,Windley,B.F.,Hao,J.,et al.,2003.Accretionleading to collision and the Permian Solonker suture,In-ner Mongolia,China:termination of the Central Asianorogenic belt.Tectonics,22:1484-1505.doi:10.1029/2002TC001484.
Xu,Y.G.,2001.Thermo-tectonic destruction of the Archae-an lithospheric keel beneath the Sino-Korean craton inChina:evidence,ti ming and mechanism.Physics andChemistry of the Earth,Part A:Solid Earth and Ge-odesy,26(9-10):747-757.doi:10.1016/S1464-1895(01)00124-7
Xu,Y.G.,2006.Using basalts geochemistry to constrainMesozoic-Cenozoic evolution of the lithosphere beneathNorth China Craton.Earth Science Frontiers,13(2):93-104(in Chinese with English abstract).
Zhai,M.G.,Meng,Q.R.,Liu,J.M.,et al.,2004.Geologicalfeatures of Mesozoic tectonic regi meinversionin easternNorth China and i mplication for geodynamics.EarthScience Frontiers,11(3):285-297(in Chinese withEnglish abstract).
Zhai,M.G.,Yang,J.H.,Liu,W.J.,2001.Large clusters ofgold deposits and large-scale metallogenesis in the Jia-odong Peninsula,eastern China.Science in China(Se-ries D),44(8):758-768.doi:10.1007/BF02907205
Zhai,M.G.,Zhu,R.X.,Liu,J.M.,et al.,2004.Ti me rangeof Mesozoic tectonic regi me inversion in eastern NorthChina block.Science in China(Series D),47(2):151-159.doi:10.1360/02ydo416
Zhang,C.L.,Zhou,D.W.,Jin,H.L.,et al.,1999.Study onthe Sr,Nd,Pb and Oisotopes of basic dyke swarms inthe Wudang block and basic volcanics of the YaolingheGroup.Acta Petrologica Sinica,15(3):430-437(inChinese with English abstract).
Zhang,H.R.,1998.Yanshan event.Acta Goeologica Sinica,72(2):103-111(in Chinese with English abstract).
Zhang,Y.T.,Zhang,L.C.,Ying,J.F.,et al.,2006.Geo-chemistry of Zhalantun dyke swarmin North Da Hing-gan mountain andits geological i mplication.Acta Petro-logica Sinica,22(11):2733-2742(in Chinese withEnglish abstract).
Zhao,D.P.,2004.Global tomographic i mages of mantle plumesand subducting slabs:insight into deep Earth dynamics.Physics ofthe Earth and Planetary Interiors,146(1-2):3-34.doi:10.1016/j.pepi.2003.07.032
Zhao,Y.,1990.The Mesozoic orogenies and tectonic evolu-tion of the Yanshan area.Geological Review,36(1):1-13(in Chinese with English abstract).
Zheng,J.P.,O Reilly,S.Y.,Griffin,W.L.,et al.,2001.Relict refractory mantle beneath the eastern North China block:significance for lithosphere evolution.Lithos,57(1):43-66.doi:10.1016/S0024-4937(00)00073-6
Zheng,Y.D.,Davis,G.A.,Wang,C.,et al.,2000.MajorMesozoic tectonic events in the Yanshan belt and theplate tectonic setting.Acta Geologica Sinica,74(4):289-302(in Chinese with English abstract).
Zhou,X.H.,2006.Major transformation of subcontinentallithosphere beneath eastern China in the Cenozoic-Mes-ozoic:review and prospect.Earth Science Frontiers,13(2):50-64(in Chinese with English abstract).
Zhou,X.H.,2009.Major transformation of subcontinentallithosphere beneath North China in Cenozoic-Mesozoic:revisited.Geological Journal of China Universities,15(1):1-18(in Chinese with English abstract).
邓晋福,苏尚国,刘翠,等,2006.关于华北克拉通燕山期岩石圈减薄的机制与过程的讨论:是拆沉,还是热侵蚀和化学交代-地学前缘,13(2):105-119.
邓晋福,赵海玲,莫宣学,等,1996.中国大陆根-柱构造:大陆动力学的钥匙.北京:地质出版社,30-39.
洪大卫,王式洸,谢锡林,等,2000.兴蒙造山带正εNd(t)值花岗岩的成因和大陆地壳生长.地学前缘,7(2):441-456.
胡受奚,赵乙英,胡志宏,等,1994.中国东部中-新生代活动大陆边缘构造——岩浆作用演化和发展.岩石学报,10(4):370-381.
李朋武,高锐,管烨,等,2006.内蒙古中部索伦-林西缝合带封闭时代的古地磁分析.吉林大学学报(地球科学版),36(5):744-758.
李益龙,周汉文,葛梦春,等,2007.西拉木伦断裂带双井微地块北缘混合岩的基本特征及其成因机制讨论.矿物岩石,27(4):22-29.
李益龙,周汉文,葛梦春,等,2008.内蒙古林西县双井片岩北缘混合岩LA-ICPMS锆石U-Pb年龄.矿物岩石,28(2):10-16.
李益龙,周汉文,钟增球,等,2009.华北与西伯利亚板块的对接过程:来自西拉木伦缝合带变形花岗岩锆石的LA-ICPMS U-Pb年龄证据.地球科学——中国地质大学学报,34(6):931-938.
路凤香,桑隆康,2002.岩石学.北京:地质出版社,42-45.
马宗晋,王国权,1999.中国大陆东部现今岩石圈结构的板条构造分区.高校地质学报,5(1):7-16.
内蒙古第二区域地质调查队,1997.双井地区1∶5万区域地质调查报告.
任纪舜,牛宝贵,和政军,等,1997.中国东部的构造格局和动力学演化.地学研究,29(30):43-55.
任纪舜,王作勋,陈炳蔚,等,1999.从全球看中国大地构造——中国及邻区大地构造图简要说明.北京:地质出版社,32-33.
尚庆华,2004.北方造山带内蒙古中、东部地区二叠纪放射虫的发现及意义.科学通报,49(24):2574-2579.
邵济安,刘福田,陈辉,等,2001a.大兴安岭-燕山晚中生代岩浆活动与俯冲作用关系.地质学报,75(1):56-63.
邵济安,张履桥,2002.华北北部中生代岩墙群.岩石学报,18(3):312-318.
邵济安,张履桥,魏春景,等,2001b.北京南口中生代双峰式岩墙群的组成及其特征.地质学报,75(2):205-212.
宋彪,张玉海,万渝生,等,2002.锆石SHRI MP样品靶制作、年龄测定及有关现象讨论.地质论评,48(增刊):26-30.
孙德有,吴福元,张艳斌,等,2004.西拉木伦河-长春-延吉板块缝合带的最后闭合时间——来自吉林大玉山花岗岩体的证据.吉林大学学报(地球科学版),34(2):174-181.
汪云亮,张成江,修淑芝,2001.玄武岩类形成的大地构造环境的Th/Hf-Ta/Hf图解判别.岩石学报,17(3):413-421.
吴福元,葛文春,孙德有,等,2003.中国东部岩石圈减薄研究中的几个问题.地学前缘,10(3):51-60.
吴福元,孙德有,林强,等,1999.东北地区显生宙花岗岩的成因与地壳增生.岩石学报,15(2):181-189.
吴根耀,2002.燕山运动和中国大陆晚中生代的活化.地质科学,37(4):453-461.
吴利仁,1985.中国东部中生代花岗岩类.岩石学报,1(1):1-9.
徐义刚,2006.用玄武岩组成反演中-新生代华北岩石圈的演化.地学前缘,13(2):93-104.
翟明国,孟庆任,刘建明,等,2004.华北东部中生代构造体制转折峰期的主要地质效应和形成动力学探讨.地学前缘,11(3):285-297.
翟明国,杨进辉,刘文军,2001.胶东大型黄金矿集区及大规模成矿作用.中国科学(D辑),31(7):545-552.
翟明国,朱日祥,刘建明,等,2003.华北东部中生代构造体制转折的关键时限.中国科学(D辑),33(10):913-920.
张成立,周鼎武,金海龙,等,1999.武当地块基性岩墙群及耀岭河群基性火山岩的Sr、Nd、Pb、O同位素研究.岩石学报,15(3):430-437.
张宏仁,1998.燕山事件.地质学报,72(2):103-111.
张玉涛,张连昌,英基丰,等,2006.大兴安岭北部扎兰屯脉岩群的地球化学特征及其地质意义.岩石学报,22(11):2733-2742.
赵越,1990.燕山地区中生代造山运动及构造演化.地质论评,36(1):1-13.
郑亚东,Davis,G.A.,王琮,等,2000.燕山带中生代主要构造事件与板块构造背景问题.地质学报,74(4):289-302.
周新华,2006.中国东部中、新生代岩石圈转型与减薄研究若干问题.地学前缘,13(2):50-64.
周新华,2009.华北中-新生代大陆岩石圈转型的研究现状与方向——兼评“岩石圈减薄”和“克拉通破坏”.高校地质学报,15(1):1-18.
Badarch,G.,Cuningham,W.D.,Windley,B.F.,2002.Anewterrane subdivision for Mongolia:i mplications forthe Phanerozoic crustal growth of Central Asia.Journalof Asian Earth Sciences,21(1):87-110.doi:10.1016/S1367-9120(02)00017-2
Chen,B.,Jahn,B.M.,Wilde,S.,et al.,2000.Two contras-ting Paleozoic magmatic belts in northern Inner Mongo-lia,China:petrogenesis and tectonic i mplications.Tectonophysics,328(1-2):157-182.doi:10.1016/S0040-1951(00)00182-7
Deng,J.F.,Su,S.G.,Liu,C.,et al.,2006.Discussion on thelithospheric thinning of the North China craton:delami-nation-or thermal erosion and chemical metasomatism-Earth Science Frontiers,13(2):105-119(in Chinesewith English abstract).
Deng,J.F.,Zhao,H.L.,Mo,X.X.,et al.,1996.Continentalroots-plume tectonics of China:key to the continentaldynamics.Geological Publishing House,Beijing,30-39(in Chinese).
Fukao,Y.,Obayashi,M.,Inoue,H.,et al.,1992.Subductingslabs stagnant in the mantle transition zone.Journal ofGeophysical Research,97:4809-4822.doi:10.1029/91JB02749
Halls,H.C.,1982.The i mportance and potential of maficdyke swarms in studies of geodynamic processes.Geo-sciences Canada,9:145-154.
Hong,D.W.,Wang,S.G.,Xie,X.L.,et al.,2000.Genesisof positiveεNd(t)granitoids in the Da Hinggan MTS-Mongolia oroganic belt and continental crustal growth.Earth Science Frontiers,7(2):441-456(in Chinesewith English abstract).
Hu,S.X.,Zhao,Y.Y.,Hu,Z.H.,et al.,1994.Evolutionand development of tectonics and magmatismat the ac-tive continental margin of the East China(E106°)dur-ing Mesozoic and Cenozoic.Acta Petrologica Sinica,10(4):370-381(in Chinese with English abstract).
Irvine,T.N.,Baragar,W.R.A.,1971.Aguide to the chemi-cal classification of the common volcanic rocks.Canadi-an Journal of Earth Sciences,8:523-548.
Jahn,B.M.,Capdevila,R.,Liu,D.,et al.,2004.Sources ofPhanerozoic granitoids in the transect Bayanhongor-Ul-aan Baatar,Mongolia:geochemical and Nd isotopic evi-dence,and i mplications for Phanerozoic crustal growth.Journal of Asian Earth Sciences,23(5):629-653.doi:10.1016/S1367-9120(03)00125-1
Khain,E.V.,Bibikova,E.V.,Kr ner,A.,et al.,2002.Themost ancient ophiolite of the Central Asian fold belt:U-Pb and Pb-Pb zircon ages for the Dunzhugur com-plex,eastern Sayan,Siberia,and geodynamic i mplica-tions.Earth and Planetary Science Letters,199(3-4):311-325.doi:10.1016/S0012-821X(02)00587-3
Khain,E.V.,Bibikova,E.V.,Salnikova,E.B.,et al.,2003.The Palaeo-Asian oceaninthe Neoproterozoic and EarlyPalaeozoic:new geochronologic data and palaeotectonicreconstructions.Precambrian Research,122(1-4):329-358.doi:10.1016/S0301-9268(02)00218-8
Li,P.W.,Gao,R.,Guan,Y.,et al.,2006.Palaeomagnetieconstraints on the final closure ti me of Solonker-Linxisuture.Journal of Jilin University(Earth Science E-dition),36(5):744-758(in Chinese with English ab-stract).
Li,Y.L.,Zhou,H.W.,Ge,M.C.,et al.,2007.Characteris-tics and genesis of migmatites within the northern ofShuangjing micro-plateinthe West Lamulunfault zone,Inner Mongolia.J.Mineral.Petrol.,27(4):22-29(inChinese with English abstract).
Li,Y.L.,Zhou,H.W.,Ge,M.C.,et al.,2008.LA-ICP-MSzircon U-Pb dating of migmatite from north ofShuangjing schist in Linxi,Inner Mongolia.J.Mineral.Petrol.,28(2):10-16(in Chinese with English ab-stract).
Li,Y.L.,Zhou,H.W.,Zhong,Z.Q.,et al.,2009.Collisionprocesses of North China and Siberian Plates:evidencefrom LA-ICP-MS zircon U-Pb age on deformed granitein Xar Moron suture zone.Earth Science—Journal ofChina University of Geosciences,34(6):931-938(inChinese with English abstract).
Lu,F.X.,Sang,L.K.,2002.Petrology.Geological Publish-ing House,Beijing,42-45(in Chinese).
Ludwig,K.R.,1991.Isoplot—a plotting and regression pro-gramfor radiogenic-isotope data.US Geological SurveyOpen-File Report,39:91-445.
Ma,Z.J.,Wang,G.Q.,1999.Strip-shaped tectonic divisionof contemporary lithospheric structure of eastern Chi-na.Geological Journal of China Universities,5(1):7-16(in Chinese with English abstract).
MacDonald,G.A.,Katsura,T.,1964.Chemical compositionof Hawaiian lavas.Journal of Petrology,5(1):82-133.doi:10.1093/petrology/5.1.82
McCulloch,M.T.,Gamble,J.A.,1989.Depleted source forvolcanic arc basalts:constraints from basalts of Kema-dec-Taupo volcanic zone based on trace elements,iso-topes and subduction chemical geodynamica.In:Conti-nental magmatism,Inter.Volcanic.Conf.Abstr.,NewMexico Bur.Miner.Resour.Bull.,131-180.
Miao,L.C.,Fan,W.M.,Liu,D.Y.,et al.,2008.Geochro-nology and geochemistry of the Hegenshan ophiolitecomplex:i mplications for late-stage tectonic evolution ofthe Inner Mongolia-Daxinganling orogenic belt,China.Journal of Asian Earth Sciences,32(5-6):348-370.doi:10.1016/j.jseaes.2007.11.005
Morrison,G.W.,1980.Characteristics and tectonic setting ofshoshonite rock association.Lithos,13(1):97-108.doi:10.1016/0024-4937(80)90067-5
Mller,D.,Groves,D.I.,1995.Potassic igneous rocks andassociated gold-copper mineralization.Springer Verlag,Berlin,1-144.
Pearce,J.A.,Gorman,B.E.,Birkett,T.C.,1975.The Ti O2-K2O-P2O5diagram,a method of discri mination betweenocean and non-ocean basalts.Earth and Planetary Sci-ence Letters,24:419-426.
Pearce,N.J.G.,Perkins,W.T.,Westgate,J.A.,et al.,1997.A compilation of new and published major andtrace element data for NIST SRM610and NIST SRM612glass reference materials.Geostandardand Geoana-lytical Research,21(1):115-144.doi:10.1111/j.1751-908X.1997.tb00538.x
Pearce,T.H.,Gorman,B.E.,Birkett,T.C.,1977.The rela-tionship between major element chemistry and tectonicenviroment of basic and intermediate volcanic rocks.Earth and Planetary Science Letters,36(1):121-132.doi:10.1016/0012-821X(77)90193-5
Ren,J.S.,Niu,B.G.,He,Z.J.,et al.,1997.Tectonic frame-work and geodynamic evolution of eastern China.Geo-logical Research,29(30):43-55(in Chinese with Eng-lish abstract).
Ren,J.S.,Wang,Z.X.,Chen,B.W.,et a1.,1999.The tec-tonics of China froma global view—a guide to the tec-tonic map of China and adjacent regions.GeologicalPublishing House,Beijing,32-33(in Chinese).
Seng r,A.M.C.,Natal in,B.A.,Burt man,V.S.,1993.Evolution of the Altaid tectonic collage and Palaeozoiccrustal growth in Eurasia.Nature,364:299-307.doi:10.1038/364299a0
Shang,Q.H.,2004.Occurrences of Permian radiolarians incentral and eastern Nei Mongol(Inner Mongolia)andtheir geological significance to the northern China oro-gen.Chinese Science Bulletin,49(24):2613-2619.doi:10.1360/04wd0069
Shao,J.A.,Gai,F.Y.,Zhang,L.Q.,1998.Coupling of man-tle-upwelling and shearing-Mesozoic dyke-swarms inDa-Hinggan mountains,Northeast China.Episodes,21:99-103.
Shao,J.A.,Liu,F.T.,Chen,H.,2001a.Relationship be-tween Mesozoic magmatismand subductionin Da Hing-gan-Yanshan area.Acta Geologica Sinica,75(1):56-63(in Chinese with English abstract).
Shao,J.A.,Zhang,L.Q.,2002.Mesozoic dyke swarms inthe north of North China.Acta Petrologica Sinica,18(3):312-318(in Chinese with English abstract).
Shao,J.A.,Zhang,L.Q.,Wei,C.J.,et al.,2001b.Composi-tion and features of the Mesozoic bi modal dike swarmin Nankou area,Beijing.Acta Geologica Sinica,75(2):205-212(in Chinese with English abstract).
Song,B.,Zhang,Y.H.,Wan,Y.S.,et al.,2002.Mountmaking and procedure of the SHRI MP dating.Geolog-ical Review,48(Suppl.):26-30(in Chinese with Eng-lish abstract).
Sun,D.Y.,Wu,F.Y.,Zhang,Y.B.,et al.,2004.The finalclosing ti me of the west Lamulun River-Changchun-Yanji plate suture zone—evidence from the Dayushangranitic pluton,Jilin Province.Journal of Jilin Univer-sity(Earth Science Edition),34(2):174-181(in Chi-nese with English abstract).
Sun,S.S.,McDonough,W.F.,1989.Chemical and isotopicsystematics of oceanic basalts:i mplications for mantlecomposition and processes.In:Saundern,A.D.,Norry,M.J.,eds.,Magmatismin the ocean basins.GeologicalSociety of London,Special Publications,42:313-345.doi:10.1144/GSL.SP.1989.042.01.19
Tang,K.D.,1990.Tectonic development of Paleozoic fold-belts at the north margin of the Sino-Korean craton.Tectonics,9:249-260.
The Second Regional Geological Survey Teamof Inner Mon-golia Autonomous Region,1997.1∶50000regional ge-ological surveys report on Shuangjing region(in Chi-nese).
Wang,Y.L.,Zhang,C.J.,Xiu,S.Z.,2001.Th/Hf-Ta/Hf i-dentification of tectonic setting of basalts.Acta Petro-logica Sinica,17(3):413-421(in Chinese with Eng-lish abstract).
Wiedenbeck,M.,Alle,P.,Corfu,F.,et al.,1995.Three nat-ural zircon standards for U-Th-Pb,Lu-Hf,trace elementand REE analyses.Geostand.Newsl.,19(1):1-23.doi:10.1111/j.1751-908X.1995.tb00147.x
Wu,F.Y.,Ge,W.C.,Sun,D.Y.,et al.,2003.Discussionson thelithospheric thinningin eastern China.Earth Sci-ence Frontiers,10(3):51-60(in Chinese with Englishabstract).
Wu,F.Y.,Sun,D.Y.,Lin,Q.,et al.,1999.Petrogenesis ofthe Phanerozoic granites and crustal growth in North-east China.Acta Petrologica Sinica,15(2):181-189(in Chinese with English abstract).
Wu,G.Y.,2002.The Yanshanian orogeny and Late Mesozo-ic activationin China continent.Chinese Journal of Ge-ology,37(4):453-461(in Chinese with English ab-stract).
Wu,L.R.,1985.Mesozoic granitoids in East China.ActaPetrologia Sinica,1(1):1-9(in Chinese with Englishabstract).
Xiao,W.J.,Windley,B.F.,Hao,J.,et al.,2003.Accretionleading to collision and the Permian Solonker suture,In-ner Mongolia,China:termination of the Central Asianorogenic belt.Tectonics,22:1484-1505.doi:10.1029/2002TC001484.
Xu,Y.G.,2001.Thermo-tectonic destruction of the Archae-an lithospheric keel beneath the Sino-Korean craton inChina:evidence,ti ming and mechanism.Physics andChemistry of the Earth,Part A:Solid Earth and Ge-odesy,26(9-10):747-757.doi:10.1016/S1464-1895(01)00124-7
Xu,Y.G.,2006.Using basalts geochemistry to constrainMesozoic-Cenozoic evolution of the lithosphere beneathNorth China Craton.Earth Science Frontiers,13(2):93-104(in Chinese with English abstract).
Zhai,M.G.,Meng,Q.R.,Liu,J.M.,et al.,2004.Geologicalfeatures of Mesozoic tectonic regi meinversionin easternNorth China and i mplication for geodynamics.EarthScience Frontiers,11(3):285-297(in Chinese withEnglish abstract).
Zhai,M.G.,Yang,J.H.,Liu,W.J.,2001.Large clusters ofgold deposits and large-scale metallogenesis in the Jia-odong Peninsula,eastern China.Science in China(Se-ries D),44(8):758-768.doi:10.1007/BF02907205
Zhai,M.G.,Zhu,R.X.,Liu,J.M.,et al.,2004.Ti me rangeof Mesozoic tectonic regi me inversion in eastern NorthChina block.Science in China(Series D),47(2):151-159.doi:10.1360/02ydo416
Zhang,C.L.,Zhou,D.W.,Jin,H.L.,et al.,1999.Study onthe Sr,Nd,Pb and Oisotopes of basic dyke swarms inthe Wudang block and basic volcanics of the YaolingheGroup.Acta Petrologica Sinica,15(3):430-437(inChinese with English abstract).
Zhang,H.R.,1998.Yanshan event.Acta Goeologica Sinica,72(2):103-111(in Chinese with English abstract).
Zhang,Y.T.,Zhang,L.C.,Ying,J.F.,et al.,2006.Geo-chemistry of Zhalantun dyke swarmin North Da Hing-gan mountain andits geological i mplication.Acta Petro-logica Sinica,22(11):2733-2742(in Chinese withEnglish abstract).
Zhao,D.P.,2004.Global tomographic i mages of mantle plumesand subducting slabs:insight into deep Earth dynamics.Physics ofthe Earth and Planetary Interiors,146(1-2):3-34.doi:10.1016/j.pepi.2003.07.032
Zhao,Y.,1990.The Mesozoic orogenies and tectonic evolu-tion of the Yanshan area.Geological Review,36(1):1-13(in Chinese with English abstract).
Zheng,J.P.,O Reilly,S.Y.,Griffin,W.L.,et al.,2001.Relict refractory mantle beneath the eastern North China block:significance for lithosphere evolution.Lithos,57(1):43-66.doi:10.1016/S0024-4937(00)00073-6
Zheng,Y.D.,Davis,G.A.,Wang,C.,et al.,2000.MajorMesozoic tectonic events in the Yanshan belt and theplate tectonic setting.Acta Geologica Sinica,74(4):289-302(in Chinese with English abstract).
Zhou,X.H.,2006.Major transformation of subcontinentallithosphere beneath eastern China in the Cenozoic-Mes-ozoic:review and prospect.Earth Science Frontiers,13(2):50-64(in Chinese with English abstract).
Zhou,X.H.,2009.Major transformation of subcontinentallithosphere beneath North China in Cenozoic-Mesozoic:revisited.Geological Journal of China Universities,15(1):1-18(in Chinese with English abstract).
邓晋福,苏尚国,刘翠,等,2006.关于华北克拉通燕山期岩石圈减薄的机制与过程的讨论:是拆沉,还是热侵蚀和化学交代-地学前缘,13(2):105-119.
邓晋福,赵海玲,莫宣学,等,1996.中国大陆根-柱构造:大陆动力学的钥匙.北京:地质出版社,30-39.
洪大卫,王式洸,谢锡林,等,2000.兴蒙造山带正εNd(t)值花岗岩的成因和大陆地壳生长.地学前缘,7(2):441-456.
胡受奚,赵乙英,胡志宏,等,1994.中国东部中-新生代活动大陆边缘构造——岩浆作用演化和发展.岩石学报,10(4):370-381.
李朋武,高锐,管烨,等,2006.内蒙古中部索伦-林西缝合带封闭时代的古地磁分析.吉林大学学报(地球科学版),36(5):744-758.
李益龙,周汉文,葛梦春,等,2007.西拉木伦断裂带双井微地块北缘混合岩的基本特征及其成因机制讨论.矿物岩石,27(4):22-29.
李益龙,周汉文,葛梦春,等,2008.内蒙古林西县双井片岩北缘混合岩LA-ICPMS锆石U-Pb年龄.矿物岩石,28(2):10-16.
李益龙,周汉文,钟增球,等,2009.华北与西伯利亚板块的对接过程:来自西拉木伦缝合带变形花岗岩锆石的LA-ICPMS U-Pb年龄证据.地球科学——中国地质大学学报,34(6):931-938.
路凤香,桑隆康,2002.岩石学.北京:地质出版社,42-45.
马宗晋,王国权,1999.中国大陆东部现今岩石圈结构的板条构造分区.高校地质学报,5(1):7-16.
内蒙古第二区域地质调查队,1997.双井地区1∶5万区域地质调查报告.
任纪舜,牛宝贵,和政军,等,1997.中国东部的构造格局和动力学演化.地学研究,29(30):43-55.
任纪舜,王作勋,陈炳蔚,等,1999.从全球看中国大地构造——中国及邻区大地构造图简要说明.北京:地质出版社,32-33.
尚庆华,2004.北方造山带内蒙古中、东部地区二叠纪放射虫的发现及意义.科学通报,49(24):2574-2579.
邵济安,刘福田,陈辉,等,2001a.大兴安岭-燕山晚中生代岩浆活动与俯冲作用关系.地质学报,75(1):56-63.
邵济安,张履桥,2002.华北北部中生代岩墙群.岩石学报,18(3):312-318.
邵济安,张履桥,魏春景,等,2001b.北京南口中生代双峰式岩墙群的组成及其特征.地质学报,75(2):205-212.
宋彪,张玉海,万渝生,等,2002.锆石SHRI MP样品靶制作、年龄测定及有关现象讨论.地质论评,48(增刊):26-30.
孙德有,吴福元,张艳斌,等,2004.西拉木伦河-长春-延吉板块缝合带的最后闭合时间——来自吉林大玉山花岗岩体的证据.吉林大学学报(地球科学版),34(2):174-181.
汪云亮,张成江,修淑芝,2001.玄武岩类形成的大地构造环境的Th/Hf-Ta/Hf图解判别.岩石学报,17(3):413-421.
吴福元,葛文春,孙德有,等,2003.中国东部岩石圈减薄研究中的几个问题.地学前缘,10(3):51-60.
吴福元,孙德有,林强,等,1999.东北地区显生宙花岗岩的成因与地壳增生.岩石学报,15(2):181-189.
吴根耀,2002.燕山运动和中国大陆晚中生代的活化.地质科学,37(4):453-461.
吴利仁,1985.中国东部中生代花岗岩类.岩石学报,1(1):1-9.
徐义刚,2006.用玄武岩组成反演中-新生代华北岩石圈的演化.地学前缘,13(2):93-104.
翟明国,孟庆任,刘建明,等,2004.华北东部中生代构造体制转折峰期的主要地质效应和形成动力学探讨.地学前缘,11(3):285-297.
翟明国,杨进辉,刘文军,2001.胶东大型黄金矿集区及大规模成矿作用.中国科学(D辑),31(7):545-552.
翟明国,朱日祥,刘建明,等,2003.华北东部中生代构造体制转折的关键时限.中国科学(D辑),33(10):913-920.
张成立,周鼎武,金海龙,等,1999.武当地块基性岩墙群及耀岭河群基性火山岩的Sr、Nd、Pb、O同位素研究.岩石学报,15(3):430-437.
张宏仁,1998.燕山事件.地质学报,72(2):103-111.
张玉涛,张连昌,英基丰,等,2006.大兴安岭北部扎兰屯脉岩群的地球化学特征及其地质意义.岩石学报,22(11):2733-2742.
赵越,1990.燕山地区中生代造山运动及构造演化.地质论评,36(1):1-13.
郑亚东,Davis,G.A.,王琮,等,2000.燕山带中生代主要构造事件与板块构造背景问题.地质学报,74(4):289-302.
周新华,2006.中国东部中、新生代岩石圈转型与减薄研究若干问题.地学前缘,13(2):50-64.
周新华,2009.华北中-新生代大陆岩石圈转型的研究现状与方向——兼评“岩石圈减薄”和“克拉通破坏”.高校地质学报,15(1):1-18.
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