中国青藏高原深部地球物理探测与地球动力学研究(1958—2004)
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摘要
经过半个多世纪的努力,中国学者在青藏高原进行的地壳上地幔地球物理探测工作取得了巨大进展.累计完成长约45000km的深部地球物理探测工作,取得了许多科学数据,为探讨高原地壳上地幔结构、隆升机制和动力学研究奠定了基础.为比较全面反映中国学者多年来的工作成果,作者广泛收集资料,总结了中国学者在青藏高原地壳上地幔地球物理探测工作程度,并按照方法分类绘制了系列工作程度图.文中分别对地壳结构、上地幔的横向不均匀性、岩石圈的电性结构、青藏高原隆升机制、青藏高原地球动力学模型等几个方面所取得的主要成果做了概略的评述.已有资料表明:青藏高原的莫霍面埋深变化较大,且在几条重要缝合带莫霍面两侧都有断错;根据目前的探测结果,高原在20±5km埋深范围内普遍存在壳内低速高导层,速度一般为5.6~5.8km/s,电阻率约为1~10Ω.m,厚度一般为5~10km,但横向分布不连续.低速层与高导层的深度、厚度在趋势上一致,但不十分吻合.天然地震的研究结果表明,组成高原各个地块内部的地震各向异性方向大致相同,各地块的分界处各向异性方向往往有明显的变化;虽然对高原隆升机制还存在不同的看法,但至少认为高原是多期隆升、多种机制共同作用的结果这一点已达成共识.综合已有的地球物理调查成果,结合地质地球化学资料建立的高原地球动力学模型,形象地表达出青藏高原岩石圈的双向挤压变形模式.这些工作为研究青藏高原隆升和变形机制提供有价值的信息.
Chinese geophysicists carried on a series of geophysics research on the crust and upper mantle of Qinghai-Tibet plateau since 1958 and the total investigation length is about 45000km.In order to express the achievements in all aspects,the authors collect materials extensively,summarize the geophysical work on the crust and upper mantle of Qinghai-Tibet plateau,and draw a series of work degree figures according to different methods.This article gives a systematic account of the crustal structure,lateral heterogeneity of the upper mantle,resistivity of the lithosphere,uplifting mechanism of the Qinghai-Tibet plateau,geodynamic model and numerical simulations on lithosphere tectonic stress field.The available data shows that Moho is comparatively deep in this area.From south to north,Moho has different depths and features undulation beneath several main sutures.The results show that there is generally a discontinuous layer of low velocity and high conductivity in the crust of Tibetan plateau,which exists in 20±5km depth generally with a velocity of 5.6～5.8km/s,a low resistivity of 1～10Ω·m and a thickness of 5～10km.The low velocity layer and high conductivity layer are similar but not same in the depth and thickness.The natural earthquake research achievements show similar seismic anisotropy direction in every block on Qinghai-Tibet plateau,but there is obvious change at the boundary of blocks.Though there are different opinions regarding the uplifting history of Qinghai-Tibet plateau,it has been generally acknowledged that the plateau has undergone multi-phase uplift under multiple action mechanisms.On the basis of the results of comprehensive geophysical survey and interpretation and geological information,a geodynamic model was built to demonstrate the deformation mode of the plateau lithosphere.
Chinese geophysicists carried on a series of geophysics research on the crust and upper mantle of Qinghai-Tibet plateau since 1958 and the total investigation length is about 45000km.In order to express the achievements in all aspects,the authors collect materials extensively,summarize the geophysical work on the crust and upper mantle of Qinghai-Tibet plateau,and draw a series of work degree figures according to different methods.This article gives a systematic account of the crustal structure,lateral heterogeneity of the upper mantle,resistivity of the lithosphere,uplifting mechanism of the Qinghai-Tibet plateau,geodynamic model and numerical simulations on lithosphere tectonic stress field.The available data shows that Moho is comparatively deep in this area.From south to north,Moho has different depths and features undulation beneath several main sutures.The results show that there is generally a discontinuous layer of low velocity and high conductivity in the crust of Tibetan plateau,which exists in 20±5km depth generally with a velocity of 5.6～5.8km/s,a low resistivity of 1～10Ω·m and a thickness of 5～10km.The low velocity layer and high conductivity layer are similar but not same in the depth and thickness.The natural earthquake research achievements show similar seismic anisotropy direction in every block on Qinghai-Tibet plateau,but there is obvious change at the boundary of blocks.Though there are different opinions regarding the uplifting history of Qinghai-Tibet plateau,it has been generally acknowledged that the plateau has undergone multi-phase uplift under multiple action mechanisms.On the basis of the results of comprehensive geophysical survey and interpretation and geological information,a geodynamic model was built to demonstrate the deformation mode of the plateau lithosphere.
引文
[1]尹安.喜马拉雅—青藏高原造山带的地质演化———显生宙亚洲大陆增长.地球学报,2001,22(3):193~230Yin A.Geologic evolution of the Himalayan_Tibtan orogen—Phanerozoic growth of Aisa continetal.Acta Geoscientia Sinica(inChinese),2001,22(3):193~230
[2]曾融生,阚荣举.柴达木盆地西部地壳深界面的反射波.地球物理学报,1961,10(1):120~125Zeng R S,Gan R J.Reflected waves from crustal interface in westernChaitamu Basin.Chinese J.Geophys.(Acta Geophysica Sinica)(inChinese),1961,10(1):120~125
[3]中国科学院地球物理研究所.西藏高原当雄-亚东地带地壳与上地幔结构和速度分布的爆炸地震研究.地球物理学报,1981,24(2):155~170Institute of Geophysics,Chinese Academy of Sciences.Explosionseismic study for velocity distribution and structure of the crust andupper mantle from Damxung to Yadong of Xizang plateau.Chinese J.Geophys.(Acta Geophysica Sinica)(in Chinese),1981,24(2):155~170
[4]滕吉文,熊绍柏,尹周勋等.喜马拉雅山北部地区的地壳结构模型和速度分布特征.地球物理学报,1983,26(6):525~540Teng J W,Xiong S B,Yin Z X,et al.Structure of the crust andupper mantle pattern and velocity distributional characteristics in theNorthern Himalayan mountain region.Chinese J.Geophys.(ActaGeophysica Sinica)(in Chinese),1983,26(6):525~540
[5]张中杰,滕吉文,李英康等.藏南地壳速度结构与地壳物质东西向“逃逸”—以佩枯错—普莫雍错宽角反射剖面为例.中国科学(D辑),2002,32(10):793~798Zhang Z J,Teng J W,Li Y K,et al.Crustal velocity structure andeastward escaping of crustal material in the southern Tibet———Anexample revealed by wide_angle seismic profile between Peikucuo andPumoyongcuo.Science in China(Ser.D)(in Chinese),2002,32(10):793~798
[6]滕吉文,尹周勋,熊绍柏.西藏高原北部地区色林错-蓬错-那曲-索县地带地壳结构与速度分布.地球物理学报,1985,28(增刊Ⅰ):28~42Teng J W,Yin Z X,Xiong S B.Crustal structure and velocitydistribution beneath Selin Co_Peng Co_Na Qu_Suo County region inthe Northern Xizang plateau.Chinese J.Geophys.(Acta GeophysicaSinica)(in Chinese),1985,28(Suppl.Ⅰ):28~42
[7]熊绍柏,滕吉文,尹周勋.西藏高原地区的地壳厚度和莫霍界面的起伏.地球物理学报,1985,28(增刊Ⅰ):16~27Xiong S B,Teng J W,Yin Z X.The thickness of the crust andundulation of discontinuity in Xizang(Tibet)plateau.Chinese J.Geophys.(Acta Geophysica Sinica)(in Chinese),1985,28(Suppl.Ⅰ):16~27
[8]卢德源,黄立言,陈纪平等.青藏高原北部沱沱河-格尔木地区地壳和上地幔的结构模型和速度分布特征.见:西藏地球物理文集.北京:地质出版社.1990.51~62Lu D Y,Huang L Y,Chen J P,et al.Structural model and velocitydispersion characteristics of the crust and upper mantle in Tuotuohe_Golmud region of north Qinghai_Xizang plateau.In:GeophysicalMemoir on Xizang_Qinghai Plateau.Beijing:Geological PublishingHouse,1990.51~62
[9]徐新忠,齐雄飞,杨长来等.青海花石峡-甘肃阿克赛人工爆破地震测深成果.见:中国地球物理学会编.中国地球物理学会年刊,北京:地震出版社,1993.80Xu X Z,Qi X F,Yang C L,et al.Results of man_made explosionseismic sounding from Huashixia(in Qinghai)to Aksay(in Gansu).In:Chinese Geophysical Society eds.Annual of the ChineseGeophysical Society in 1993.Beijing:Seismological Press,1993.80
[10]崔作舟,李秋生,吴朝东等.格尔木-额济纳旗地学断面的地壳结构与深部构造.地球物理学报,1995,38(增刊Ⅱ):15~28Cui Z Z,Li Q S,Wu C D,et al.The crustal and deep tectonics inGolmud_Ejin Qi GGT.Chinese J.Geophys.(in Chinese),1995,38(Suppl.Ⅱ):15~28
[11]熊绍柏,刘宏兵.青藏高原西部的地壳结构.科学通报,1997,42(12):1309~1312Xiong S B,Liu H B.Crustal structure in the west Tibetan plateau.Chinese Science Bulletin(in Chinese),1997,42(12):1309~1312
[12]孔祥儒,王谦身,熊绍柏.青藏高原西部综合地球物理剖面和岩石圈结构与动力学.科学通报,1999,44(12):1257~1265Kong X R,Wang Q S,Xiong S B.The study of comprehensivegeophysical profile and lithosphere structure and dynamic in westTibet.Chinese Science Bulletin(in Chinese),1999,44(12):1257~1265
[13]李秋生,卢德源,高锐等.新疆地学断面(泉水沟—独山子)深地震测深成果综合研究.地球学报,2001,22(6):534~540Li Q S,Lu D Y,Gao R,et al.An integrated study of deep seismicsounding profile along Xinjiang Global Geoscience Transect(Quanshuigou_Dushanzi).Acta Geoscientia Sinica(in Chinese),2001,22(6):534~540
[14]Zhao W J,Mechie J,Brown L D,et al.Crustal structure of centralTibet as derived from INDEPTH wide_angle seismic data.GeophysicalJournal International,2001,145:486~498
[15]王有学,钱辉.青海东部地壳速度结构特征研究.地学前缘,2000,7(4):568~579Wang Y X,Qian H.Study of crustal velocity structure in the eastQinghai.Earth Science Fronties(in Chinese),2000,7(4):568~579
[16]赖晓玲,李松林,张先康.玛沁—兰州—靖边剖面壳幔复杂性的研究.地球物理学进展,2001,16(2):65~72Lai X L,Li S L,Zhang X K.A study on the complexity at the crust_upper mantle transition zone along Maqin_Lanzhou_Jingbian deepseismic sounding(DSS)profile.Progress in Geophysics(inChinese),2001,16(2):65~72
[17]李松林,张先康,张成科.玛沁—兰州—靖边地震测深剖面地壳速度结构的初步研究.地球物理学报,2002,45(2):210~217Li S L,Zhang X K,Zhang C K.A preliminary study on the crustalvelocity structure of Maqin_Lanzhou_Jingbian by means of deepseismic sounding profile.Chinese J.Geophys.(in Chinese),2002,45(2):210~217
[18]Zhang Z J,Wang G J.P_wave structure along 1100km long wide_angle seismic profile in the eastern Tibet.AGU,Japan.2002
[19]王椿镛,吴建平,楼海.川西藏东地区的地壳P波速度结构.中国科学(D辑),2003,33(增):181~189Wang C Y,Wu J P,Lou H.Crustal P_wave velocity structure in thewest Sichuan and east Tibet region.Science in China(Series D)(inChinese),2003,33(Suppl.):181~189
[20]赵俊猛,张先康,王尚旭等.准噶尔盆地、天山造山带、塔里木盆地、阿尔金造山带、柴达木盆地和昆仑造山带(北缘)岩石圈结构及其动力学研究.见:中国地球物理学会编.中国地球物理学会年刊.昆明:云南科技出版社,2001.13Zhao J M,Zhang X K,Wang S X,et al.The lithospheric structureand dynamic process of the Junggar Basin,the Tianshan OrogenicBelt,the Tarim Basin,the Altun Orogenic Belt,the Qaidam Basin andthe Kunlun Orogenic Belt(northern margin).In:ChineseGeophysical Society eds.Annual of the Chinese Geophysical Society.Kunming:Yunnan Science&Technology Press,2001.13
[21]赵俊猛,张先康,邓宏钊等.拜城—大柴旦剖面的上地壳Q值结构.地球物理学报,2003,46(4):503~509Zhao J M,Zhang X K,Deng H Z,et al.Qvalue structure of theupper crust along the profile from Baicheng to Da Qaidam.ChineseJ.Geophys.(in Chinese),2003,46(4):503~509
[22]Wang C Y,Han W B,Wu J P,et al.Crustal structure beneath theSongpan_Garze orogenic belt.Acta Seimologica Sinica,2003,16(3):237~250
[23]Zhao W J,Nelson K D,Project INDEPTH Team.Deep seismicreflection evidence for continental underthrusting beneath southernTibet.Nature,1993,366(9):557~559
[24]Zhao W J,Nelson K D,Meissner.Advances of INDEPTH_A deepprofiling study in Tibet and the Himalayas.Episodes,1997,20(4):266~272
[25]吴宣志,吴春玲,卢杰等.利用深地震反射剖面研究北祁连-河西走廊地壳细结构.地球物理学报,1995,38(增Ⅱ):29~35Wu X Z,Wu C L,Lu J,et al.Research on the fine crustal structureof the northern Qilian_Hexi Corridor by deep seismic reflection.Chinese J.Geophys.(in Chinese):1995,38(Suppl.Ⅱ):29~35
[26]高锐,黄东定,卢德源等.横过西昆仑造山带与塔里木盆地结合带的深地震反射剖面.科学通报,2000,45(17):1874~1879Gao R,Huang D D,Lu D Y,et al.Deep seismic reflection profileacross the contact zone of the West Kunlun orogenic belt and theTarim basin.Chinese Science Bulletin(in Chinese),2000,45(17):1874~1879
[27]高锐,肖序常,刘训等.新疆地学断面深地震反射剖面揭示的西昆仑-塔里木结合带岩石圈细结构.地球学报,2001,22(6):547~552Gao R,Xiao X C,Liu X,et al.Detail lithospheric structure of thecontact zone of West Kunlun_Tarim revealed by the deep seismicreflection profile along Xinjiang geotransect.Acta Geoscientia Sinica(in Chinese),2001,22(6):547~552
[28]高锐,李鹏武,李秋生等.青藏高原北缘碰撞变形的深部过程———深地震探测成果之启示.中国科学(D辑),2001,31(增):66~71Gao R,Li P W,Li Q S,et al.Deep process of the collision anddeformation in northern Tibetan Plateau—implications from deepseismic sounding results.Science in China(Series D)(in Chinese),2001,31(Suppl.):66~71
[29]Gao R,Ma Y S,Zhu X,et al.The lithospheric structures of theSongpan block in the northeastern Tibetan plateau_revelation frominvestigation of the deep seismic profile,GEOLOGIE ALPINE,20thHimalayan_Karakoruam_Tibet Workshop Special ExtendedAbstracts,Aussois,France,2005,44,58
[30]姜枚,吕庆田,薛光琦.中、法两国联合进行青藏高原天然地震探测地壳结构的研究.地球物理学报,1994,37(3):412~413Jiang M,Lu Q T,Xue G Q.Researches on the crustal structure ofthe Tibetan Plateau by means of seismic experiment jointly by Chineseand French geophysics.Chinses J.Geophys.(in Chinese),1994,37(3):412~413
[31]许志琴,杨经绥,姜枚.青藏高原北部的碰撞造山及深部动力学—中法地学合作研究新进展.地球学报,2001,22(1):5~10Xu Z Q,Yang J S,Jiang M.Collision_orogeny of the northernQinghai_Tibet plateau and its deep dynamics.Acta Geoscientia Sinica(in Chinese),2001,22(1):5~10
[32]Kao H,Gao R,Rau Ruey_Juin,et al.Seismic image of the Tarimbasin and its collision with Tibet.Geology,2001,29(7):575~578
[33]管烨,高弘,高锐等.新疆塔里木-西昆仑宽频地震观测实验研究.地球学报,2001,22(6):559~562Guan Y,Gao H,Gao R,et al.Broadband seismic observationalexperiments from Tarim basin to Kunlun mountains.Acta GeoscientiaSinica(in Chinese),2001,22(6):559~562
[34]丁志峰,曾融生.青藏高原横波分裂的观测研究.地球物理学报,1996,39(2):211~220Ding Z F,Zeng R S.Observation and study of shear wave anisotropyin Tibetan Plateau.Chinese J.Geophys.(in Chinese),1996,39(2):211~220
[35]曾融生,丁志峰,吴庆举.喜马拉雅-祁连山地壳构造与大陆-大陆碰撞过程.地球物理学报,1998,41(1):49~60Zeng R S,Ding Z F,Wu Q J.The crustal structure from Himalayasto Qilian and its implications for continent_continent collision process.Chinese J.Geophys.(in Chinese),1998,41(1):49~60
[36]吕庆田,姜枚,马开义.三维走时反演与青藏高原南部深部构造.地震学报,1996,18(4):451~459LüQ T,Jiang M,Ma K Y.3_D travel time tomography inversion andthe deep structure of the southern Tibet.Acta Seismologica Sinica(inChinese),1996,18(4):451~459
[37]姜枚,吕庆田,史大年.用天然地震探测青藏高原中部地壳、上地幔结构.地球物理学报,1996,39(4):470~482Jiang M,LüQ T,Shi D N.The study on the structure of crustal andupper mantle with natural earthquakes in central Tibetan Plateau.Chinese J.Geophys.(in Chinese),1996,39(4):470~482
[38]Kind R,Yuan X,Saul J,et al.Seismic Images of crust and uppermantle beneath Tibet:evidence for Eurasian plate subduction.Science,2002,298:1219~1221
[39]董英君,薛光琦,马开义.阿尔金断裂系及邻区剪切波各向异性研究.地球物理学进展,1999,14(4):58~65Dong Y J,Xue G Q,Ma K Y.Studies on shear wave anisotropybeneath Altyn fault system and its adjacent area.Progress inGeophysics(in Chinese),1999,14(4):58~65
[40]史大年,姜枚,马开义等.阿尔金断裂带地壳和上地幔结构的P波层析成像.地球物理学报,1999,42(3):341~350Shi D N,Jiang M,Ma K Y,et al.Crust and upper mantletomographic structure across the Altyn fault zone using teleseismic P_waves.Chinese J.Geophys.(in Chinese),1999,42(3):341~350
[41]钱辉,姜枚,薛光琦等.天然地震接收函数揭示的青藏高原东部地壳结构.地震学报,2001,23(1):103~108Qian H,Jiang M,Xue G Q,et al.Crustal structure of eastern Tibetinferred from natural earthquake receiver function analysis.ActaSeismological Sinica(in Chinese),2001,23(1):103~108
[42]Frederik T,Ni J,INDEPTH_ⅢSeismic Team.Seismic imaging ofthe down_welling Indian lithosphere beneath central Tibet.Science,2003,300,1424~1427
[43]薛光琦,姜枚,宿和平.利用层析成像研究青藏高原叶城-狮泉河地区深部构造.中国科学(D辑),2004,34(4):329~334Xue G Q,Jiang M,Su H P.A study on deep structure of Yecheng_Shiquanhe region on Tibetan plateau by tomographic imaging.Sciencein China(Series D)(in Chinese),2004,34(4):329~334
[44]郭飚,刘启元,陈九辉等.青藏高原东北缘—鄂尔多斯地壳上地幔地震层析成像研究.地球物理学报,2004,47(5):790~797Guo B,Liu Q Y,Chen J H,et al.Seismic tomographic imaging ofthe crust and upper mantle beneath the Northeastern edge of theQinghai_Xizang plateau and the Ordos area.Chinese J.Geophys.(in Chinese),2004,47(5):790~797
[45]Pelkum S,Monsalve G,Sheehan A,et al.Imaging the Indiansubcontinent beneath the Himalayas.Nature,2005,435:1222~1225
[46]谭捍东,魏文博,Martyn Unsworth等.西藏高原南部雅鲁藏布江缝合带地区地壳电性结构研究.地球物理学报,2004,47(4):685~690Tan H D,Wei W B,Martyn Unsworth,et al.Crustal electricalconductivity structure beneath the Yarlung Zangbo Jiang suture in thesouthern Xizang plateau.Chinese J.Geophys.(in Chinese),2004,47(4):685~690
[47]范文科,袁学诚.羊八井至洛扎南北向剖面磁大地电流测深初步成果.见:李光岑,Mercier J L编.中法喜马拉雅考察成果1980.北京:地质出版社,1984.413~419Pham Van Ngoc,Yuan X C.Execution of a long MT profile of NSdirection from Yangbajing to Lhozag:First results.In:Li G C,Mercier J L eds.Sino_French Cooperative Investigation in Himalyas(in Chinese).Beijing:Geological Publishing House,1984.413~419
[48]袁学诚,李立,金国元等.西藏洛扎-那曲一带地壳和上地幔的磁大地电流测深研究.见:西藏地球物理文集,北京:地质出版社,1990.63~71Yuan X C,Li L,Jin G Y,et al.Magnetotelluroc investigations inLhozang_area,Tibet.In:Geophysical Memoir on Xizang_QinghaiPlateau(in Chinese).Beijing:Geological Publishing House,1990.63~71
[49]郭新峰,张元丑,程庆云等.青藏高原亚东-格尔木地学断面岩石圈电性研究.中国地质科学院院报,1990,21:191~202Guo X F,Zhang Y C,Cheng Q Y,et al.Magnetotelluric studiesalong Yadong_Golmud geosciences transect in Qinghai_Xizangplateau.Bulletin of The Chinese Academy of Geological Sciences(inChinese),1990,21:191~202
[50]朱仁学,胡祥云.格尔木-额济纳旗地学断面岩石圈电性结构的研究.地球物理学报,1995,38(增刊Ⅱ):46~57Zhu R X,Hu X Y.Study on the resistivity structure of thelithosphere along the Golmod_Ejin Qi geoscience transect.Chinese J.Geophys.(in Chinese),1995,38(Suppl.Ⅱ):46~57
[51]Wei W B,Unsworth M,Jones A,et al.Detection of widespreadfluids in the Tibetan crust by magnetotelluric studies.Science,2001,292:716~718
[52]马晓冰,孔祥儒,于晟.青藏高原西部大地电磁测深探测结果.科学通报,1997,42(11):1185~1187Ma X B,Kong X R,Yu S.Magnetotelluric sounding in westernTibet.Chinese Science Bulletin(in Chinese),1997,42(11):1185~1187
[53]孙洁,晋光文,白登海等.青藏高原东缘地壳、上地幔电性结构探测及其构造意义.中国科学(D辑),2003,33(增):173~180Sun J,Jin G W,Bai D H,et al.Electrical structure of the crust andupper mantle and tectonics sense on the edge of the East Tibet.Science in China(Series D)(in Chinese),2003,33(Suppl.):173~180
[54]李立,金国元.西藏岩石圈电性和热状态.地质矿产部地球物理地球化学勘查研究所所刊,1986,2:121~128Li L,Jin G Y.The electrical characteristic and thermal state of thelithosphere in area of Xizang(Tibet)autonomous region.Bulletin ofthe Institute of Geophysical&Geochemical Exploration,Ministry ofGeology and Mineral Resources(in Chinese),1986,2:121~128
[55]Yuan X C,Xu X Z.Global geoscience transect(GGT)acrossEurasia_Chinese part(from Altay to Taiwan).Abstracts of 30thInternational Geological Congress,1996,1:141
[56]秦国卿,陈九辉,刘大建等.昆仑山脉和喀喇昆仑山脉地区的地壳上地慢电性结构特征.地球物理学报,1994,37(2):193~199Qin G Q,Chen J H,Liu D J,et al.The characteristics of theelectrical structure of the crust and upper mantle in the region of theKunlun and the Karakorum mountains.Chinese J.Geophys.(ActaGeophysica Sinica)(in Chinese),1994,37(2):193~199
[57]Chen L S,John R Booker,Alan G Jones,et al.Electricallyconductive crust in southern Tibet from INDEPTH magnetoelluricsurveying.Science,1996,274:1694~1696
[58]马晓冰,孔祥儒,刘宏兵等.青藏高原东部大地电磁测深探测结果.中国科学(D辑),2001,31(增):72~76Ma X B,Kong X R,Liu H B,et al.Magnetotelluric soundingresults in eastern Tibetan Plateau.Science in China(Series D)(inChinese),2001,31(Suppl.):72~76
[59]孟令顺,申江胜,齐立等.西藏羊八井-聂拉木地区的重力工作及其初步解释.石油物探,1984,23(2):1~21Meng L S,Shen J S,Qi L,et al.The preliminary interpretation ofthe gravity profile of well Yang No.8_Nielamu,Tibet.GeophysicalProspecting For Petroleum(in Chinese),1984,23(2):1~21
[60]孟令顺,高锐,周富祥等.利用重力异常研究亚东-格尔木地壳构造.中国地质科学院院报,1990,21:149~161Meng L S,Gao R,Zhou F X,et al.Intepretation of the crustalstructure in Yadong_Golmud area using gravity anomalies.Bulletin ofThe Chinese Academy ofGeological Sciences(in Chinese),1990,21:149~161
[61]孟令顺,姜喜荣,张风华等.新疆叶城-西藏狮泉河重力剖面与地壳结构.地球物理学报,1990,33(6):670~677Meng L S,Jiang X R,Zhang F H,et al.Gravity profile and thecrustal structure of Yecheng_Shiquanhe.Chinese J.Geophys.(ActaGeophysica Sinica)(in Chinese),1990,33(6):670~677
[62]孟令顺.地壳的重力构造.见:中国地质科学院岩石圈研究中心编.青藏高原岩石圈结构构造和形成演化.中华人民共和国地质矿产部地质专报,第20号.北京:地质出版社,1996.83~93Meng L S.Gravity structure of crust in Tibet.In:The LithosphereResearch Center of Chinese Academy of Geology Science,Institute ofGeology Science of Ministry of Geology and Mineral Resources eds.Lithospheric Structure and Tectonics in Tibet and Its Formation andEvolution.People’s Republic of China Ministry of Geology andMineral Resources.Geological Tectonics,NO.20.Beijing:Geological Publishing House,1996.83~93
[63]孟令顺,齐立,高锐等.横过阿尔金山的重力测量及初步解释.长春科技大学学报,1998,28(3):345~350Meng L S,Qi L,Gao R,et al.Gravity survey and isostatic messagealong the profile of Aergan(in Xinjiang)-Laomangya(in Qinghai).Journal of Changchun University of Science and Technology(inChinese),1998,28(3):345~350
[64]孟令顺,管烨,齐立等.格尔木-额济纳旗地学断面及其邻区重力场与深部地壳构造.地球物理学报,1995,38(增刊Ⅱ):36~45Meng L S,Guan Y,Qi L,et al.Gravity field and deep crustalstructure in Golmud_Ejin Qi geoscience transection and nearby area.Chinese J.Geophys.(in Chinese),1995,38(Suppl.Ⅱ):36~45
[65]王谦身,武传真,江为为.青藏高原西部吉隆-鲁谷地区的重力场与地壳构造.科学通报,1997,42(8):858~862Wang Q S,Wu C Z,Jiang W W.Gravity field and crustal structureof Jilong_Lugu region in western Tibet.Chinese Science Bulletin(inChinese),1997,42(8):858~862
[66]王谦身,安玉林.青藏高原东部玛多—沙马地区的重力场与深部构造.地球物理学进展,2001,16(4):4~10Wang Q S,An Y L.Gravity field and deep structure of Madoi_Shamaregion in eastern Qinghai_Xizang(Tibetan)plateau.Process inGeophysics(in Chinese),2001,16(4):4~10
[67]余钦范,孙运生,楼海等.亚东格尔木地学断面的磁结构.中国地质科学院院报,1990,21:183~190Yu Q F,Sun Y S,Lou H,et al.The magnetic structure ofgeoscience transect from Yadong to Golmud.Bulletin of The ChineseAcademy of Geological Sciences(in Chinese),1990,21:183~190
[68]余钦范,楼海,胡中栋.格尔木-额济纳旗地学断面岩石圈结构的磁场分析.地球物理学报,1995,38(增刊Ⅱ):58~Yu Q F,Lou H,Hu Z D.Magnetic data interpretation of the crustalstructure of the geoscience transection from Golmud to Ejin Qi.Chinese J.Geophys.(in Chinese),1995,38(Suppl.Ⅱ):58~70
[69]孙鸿烈,郑度主编.青藏高原形成、演化与发展.广州:广东科技出版社,1998.21~23Sun H L,Zheng D.Formation,Evolution and Development ofQinghai_Xizang Plateau(in Chinese).Guangzhou:GuangdongScience&Technology Press,1988.
[70]刘宏兵,孔祥儒,马晓冰等.青藏高原东南地区地壳物性结构特征.中国科学(D辑),2001,31(增):61~71Liu H B,Kong X R,Ma X B,et al.Crustal structure characteristicof the southeast Tibet.Science in China(Series D)(in Chinese),2001,31(Suppl.):61~71
[71]沈显杰,张文仁,杨淑贞等.青藏高原南北地体壳幔热结构差异的大地热流证据.中国地质科学院院报,1990,21:203~214Shen X J,Zhang W R,Yang S Z,et al.Heat flow evidence for thedifferentiated crust_mantle thermal structures of the Qinghai_Xizangplateau.Bulletin of the Chinese Academy of Geological Sciences(inChinese),1990,21:203~214
[72]沈显杰,杨淑贞,沈继英.格尔木-额济纳旗地学断面热流研究与分析.地球物理学报,1995,38(增刊Ⅱ):86~97Shen X J,Yang S Z,Shen J Y.Heat flow study and analysis alongthe Golmud_Ejin Qi geotransect.Chinese J.Geophys.(ActaGeophysica Sinica)(in Chinese),1995,38(Suppl.Ⅱ):86~97
[73]Wittlinger G,Vergne J,Tapponnier P,et al.Teleseismic imaging ofsubducting lithosphere and Moho offsets beneath western Tibet.Earthand Planetary Science Letter,2004,221:117~130
[74]Hirn A,Lepine J C,Jobert T G,et al.Crust structure andvariability of the Himalayan border of Tibet.Nature,1984,307(5946):23~25
[75]李秋生,彭苏萍,高锐.青藏高原莫霍面的研究进展.地质论评,2004,50(6):598~612Li Q S,Peng S P,Gao R.A review on the Moho discontinuitybeneath the Tibetan plateau.Geological Review(in Chinese),2004,50(6):598~612
[76]高恩源,徐中信,王香泾等.喜马拉雅山北麓—雅鲁藏布江地区人工爆炸地震测深地壳结构.见:中国地质科学院主编.西藏地球物理文集.北京:地质出版社,1990.1~14Gao E Y,Xu Z X,Wang X J,et al.Structure of the crust andvelocity distributional characteristics in the unit between Himalayamountain and the Yaluzangbo river.In:Geophysical Memoir onXizang_Qinghai Plateau(in Chinese).China Academy of GeologyScience eds.Beijing:Geological Publishing House,1990.1~14
[77]黄立言,卢德源,李小鹏等.藏北色林湖—蓬错—雅安多地带的深部地震测深.见:西藏地球物理文集.北京:地质出版社,1990.25~37Huang L Y,Lu D Y,Li X P,et al.Deep seismic sounding ofSelincuo Lake_Pengcuo Lake_Yangamdo in the north of the Xizang(Tibet).In:Geophysical Memoir on Xizang_Qinghai Plateau(inChinese).Beijing:Geological Publishing House,1990.25~37
[78]张中杰,李英康,王光杰等.藏北地壳东西向结构与“下凹”莫霍面———来自宽角反射剖面的启示.中国科学(D辑),2001,31(11):881~888Zhang Z J,Li Y K,Wang G J,et al.E—W crustal structure underthe northern Tibet and“down—bowing”Moho under the northernTibet revealed by wide_angle seismic profile.Science in China(Series D)(in Chinese),2001,31(11):881~888
[79]曾融生,丁志峰,吴庆举.青藏高原岩石圈构造及动力学过程研究.地球物理学报,1994,37(增):99~116Zeng R S,Ding Z F,Wu Q J.A review on the lithosphericstructures in Tibetan plateau and constraints for dynamics.Chinese J.Geophys.(Acta Geophysica Sinica)(in Chinese),1994,37(Suppl.):99~116
[80]Ross A,Brown L,Passakorn P,et al.Deep reflection surveying incentral Tibet:lower_crustal layering and crustal flow.GeophysicalJournal International,2004,156:115~128
[81]李秋生,彭苏萍,高锐等.东昆仑大地震的深部构造.地球学报,2004,25(1):11~16Li Q S,Peng S P,Gao R,et al.Deep tectonic background of the8.1Ms earthquake in the east Kunlun.Acta Geoscientica Sinica(inChinese),2004,25(1):11~16
[82]Kind R,Yuan X,Saul J,et al.Seismic images of crust and uppermantle beneath Tibet:evidence for Eurasian plate subduction.Science,2002,298:1219~1221
[83]吴庆举,曾融生.用宽频带远震接收函数研究青藏高原的地壳结构.地球物理学报,1998,41(5):669~679Wu Q J,Zeng R S.The crustal stucture of Qinghai_Xizang plateauinferred from broadband teleseismic waveform.Chinese J.Geophys.(Acta Geophysica Sinica)(in Chinese),1998,41(5):669~679
[84]Zhu L P,Helmberger D V.Moho offset across the northern margin ofthe Tibetan plateau.Science,1998,281:1170~1172
[85]Zhang Z J,Klemperer S L.West_east variation in crustal thickness innorthern Lhasa block,central Tibet,from deep seismic soundingdata.J.Geophys.Res.,2005,110(B9),B09403,doi:10.1029/2004JB003139
[86]李秋生,彭苏萍,高锐等.青藏高原北部巴颜喀拉构造带基底隆起的地震学证据.地质通报,2003,22(10):782~788Li Q S,Peng S P,Gao R,et al.Seismic evidence of the basementuplift in the Bayan Har tectonic belt,Qinghai,and its tectonicsignificance.Geological Bulletin of China(in Chinese),2003,22(10):782~788
[87]王椿镛,韩渭宾,吴建平等.松潘—甘孜造山带地壳速度结构.地震学报,2003,25(3):229~241Wang C Y,Han W B,Wu J P,et al.Crustal structure beneath theSongpan_Garze orogenic belt.Acta Seismologica Sinica(in Chinese),2003,25(3),229~241
[88]高锐,吴功建.青藏高原亚东-格尔木地学断面地球物理综合解释模型与现今地球动力学过程.长春地质学院学报,1995,25(3):241~250Gao R,Wu G J.Geophysical model and geodynamic process ofYadong_Ge’ermu geoscience transect in Qinghai_Tibet plateau.Journal of Changchun University of Earth Sciences(in Chinese),1995,25(3):241~250
[89]Nelson K D,Zhao W J,Brown L D,et al.Partially molten middlecrust beneath Southern Tibet:Synthesis of project INDEPTH results.Science,1996,274:1684~1688
[90]Kind R,Ni J,Zhao W J,et al.Evidence from earthquake data for apartially molten crustal layer in Southern Tibet.Science,1996,274:1692~1694
[91]王式,卢德源,黄立言等.西藏高原南北走向的地壳结构模型和速度分布特征.见:西藏地球物理文集.北京:地质出版社,1990.38~47Wang S,Lu D Y,Huang L Y,et al.Velocity distributioncharacteristics and N_S variation of the depth of the earth’s crust inthe Xizang(Tibet)plateau.In:Geophysical Memoir on Xizang_Qinghai Plateau(in Chinese).Beijing:Geological Publishing House,1990.38~47
[92]Spratt J E,Jones A G,Nelson K D,et al.Crustal structure of theIndia_Asia collision zone,southern Tibet,from INDEPTH MTinvestigations.Physics of the Earth and Planetary Interiors,2005,150(1_3):227~237
[93]崔作舟,尹周勋,高恩元等.青藏高原地壳结构构造及其与地震的关系.中国地质科学院院报,1990,21:215~226Cui Z Z,Yin Z X,Gao E Y,et al.The structure and tectonics ofthe crust and their relation with earthquakes in the Qinghai_Xizangplateau.Bulletin of The Chinese Academy of Geological Sciences(inChinese),1990,21:215~226
[94]吴功建,高锐,余钦范等.青藏高原“亚东-格尔木地学断面”综合地球物理调查与研究.地球物理学报,1991,34(5):552~562Wu G J,Gao R,Yu Q F,et al.Intergrated investigations of theQinghai_Tibet plateau along the Yadong_Golmud geoscience transect.Chinese J.Geophys.(Acta Geophysica Sinica)(in Chinese),1991,34(5):552~562
[95]McNamara D E,Owens T J,Walter W R.Observations of theregional phase propagation across the Tibetan Plateau.Journal ofGeophysical Research,1995,100(22):22215~22229
[96]滕吉文等.柴达木东盆地的深层地震反射波和地壳构造.地球物理学报,1974,17(2):121~134Teng J W,et al.Deep reflected waves and the structure of the earthcrust of the eastern part of Qaidam basin.Chinese J.Geophys.(Acta Geophysica Sinica)(in Chinese),1974,17(2):121~134
[97]宋仲和,安昌强,王椿镛等.青藏高原及南北带上地幔P波速度结构.地球物理学报,1985,28(增):148~160Song Z H,An C Q,Wang C Y,et al.The P wave velocity of uppermantle beneath Qinghai_Tibet plateau and north_south seismic zone.Chinese J.Geophys.(Acta Geophysica Sinica)(in Chinese),1985,28(Suppl.):148~160
[98]庄真,傅竹武,吕梓玲等.青藏高原及邻近地区地壳与上地幔剪切波三维速度结构.地球物理学报,1992,35(6):694~709Zhuang Z,Fu Z W,LüZ L,et al.3_D shear velocity model of crustand upper mantle beneath the Tibetan plateau and its adjacentregions.Chinese J.Geophys.(Acta Geophysica Sinica)(inChinese),1992,35(6):694~709
[99]陈国英,曾融生.用地震面波频散研究喜马拉雅山与西藏高原岩石圈构造的差异.地球物理学报,1985,28(Suppl.):161~173Chen G Y,Zeng R S.The difference of lithospheric structurebetween Himalayan mountain and Tibetan plateau from surface wavedispersion.Chinese J.Geophys.(Acta Geophysica Sinica)(inChinese),1985,28(Suppl.):161~173
[100]吴建平,明跃红,叶太兰等.体波波形反演对青藏高原上地幔速度结构的研究.地球物理学报,1998,41(增):15~25Wu J P,Ming Y H,Ye T L,et al.Upper mantle velocity structurein the Qinghai_Xizang Plateau from inversion of body waveforms.Chinese J.Geophys.(Acta Geophysica Sinica)(in Chinese),1998,41(Suppl.):15~25
[101]McNamara D E,Owens T J,Silver P G,et al.Shear wave anisotropybeneath the Tibetan plateau.Journal of Geophysical Research,1994,99(B7):13655~13665
[102]Hirn A,Jiang M,Sapin M,et al.Seismic anisotropy as an indicatorof mantle flow beneath the Himalayas and Tibet.Nature,1995,375:571~574
[103]姜枚,许志琴,Hirn A等.青藏高原及其部分邻区地震各向异性和上地幔特征.地球学报,2001,22(2):111~116Jiang M,Xu Z Q,Hirn A,et al.Seismic anisotropy and uppermantle characteristic of Tibetan plateau and its partial adjacent area.Acta Geoscientica Sinica.(in Chinese),2001,22(2):111~116
[104]董英君,薛光琦,马开义.阿尔金断裂系及邻区剪切波各向异性研究.地球物理学进展,1999,14(4):58~65Dong Y J,Xue G Q,Ma K Y.Studies on shear wave anisotropybeneath Altyn fault system and its adjacent area.Progress inGeophysics(in Chinese),1999,14(4):58~65
[105]高锐.青藏高原岩石圈结构与地球动力学的30个为什么.地质论评,1997,43(5):460~464Gao R.Thirty problems of the lithospheric structure and geodynamicsin the Qinghai_Xizang plateau.Geological Review(in Chinese),1997,43(5):460~464
[106]潘裕生.青藏高原的形成和隆升.地学前缘,1999,6(3):153~163Pan Y S.Formation and uplifting of the Qinghai_Tibet plateau.EarthScience Frontiers(in Chinese),1999,6(3):153~163
[107]常承法,潘裕生,郑锡谰等.青藏高原地质构造.北京:科学出版社,1982Chang C F,Pan Y S,Zheng X L,et al.The Geological Tectonics ofQinghai-Xizang(Tibet)Plateau.Beijing:Science Press,1982
[108]滕吉文,张中杰,杨顶辉等.青藏高原地体划分的地球物理标志研究.地球物理学报,1996,39(5):629~641Teng J W,Zhang Z J,Yang D H,et al.The study of geophysicalcriterion for dividing terranes in Qinghai_Xizang Plateau.Chinese J.Geophys.(Acta Geophysica Sinica)(in Chinese),1996,39(5):629~641
[109]Murphy M A,Yin A,Harrison T M,et al.Did the Indo_Asiancollision alone create the Tibetan plateau?Geology,1997,25(8):719~722
[110]李廷栋.青藏高原隆升的过程和机制.地球学报,1995,(1):1~9Li T D.The uplifting process and mechanism of the Qinghai_Tibetplateau.Acta Geoscientia Sinica(in Chinese),1995,(1):1~9
[111]钟大赉,丁林.青藏高原的隆起过程及其机制探讨.中国科学(D辑),1996,26(4):289~295Zhong D L,Ding L.Research on the uplift process and mechanism ofthe Tibetan plateau.Science in China(Series D)(in Chinese),1996,26(4):289~295
[112]许志琴,姜枚,杨经绥等.青藏高原的地幔结构:地幔羽、地幔剪切带及岩石圈俯冲板片的拆沉.地学前缘,2004,11(4):329~343Xu Z Q,Jiang M,Yang J S,et al.Mantle structure of Qinghai-Tibet plateau:Mantle plume,mantle shear zone and delamination oflithospheric slab.Earth Science Frontiers(in Chinese),2004,11(4):329~343
[113]滕吉文,张中杰,王光杰等.喜马拉雅碰撞造山带的深层动力过程与陆-陆碰撞新模型.地球物理学报,1999,42(4):481~494Teng J W,Zhang Z J,Wang G J,et al.The deep internal dynamicalprocesses and new model of continental-continental collision inHimalayan collision orogenic zone.Chinese J.Geophys.(inChinese),1999,42(4):481~494
[114]高锐.青藏高原岩石圈变形与陆壳运动.见:中国地球物理学会年刊,北京:地震出版社,1990.121Gao R.Lithospheric deformation and crustal movement in Tibet.In:Chinese Geophysical Society eds.Annual of the Chinese GeophysicalSociety 1990.Beijing:Seismological Press,1990.121
[115]高锐,成湘洲,丁谦.格尔木-额济纳旗地学断面地球动力学模型初探.地球物理学报,1995,38(Suppl.):3~14Gao R,Cheng X Z,Ding Q.Preliminary geodynamic model ofGolmud_Ejin Qi geoscience transect.Chinese J.Geophys.(ActaGeophysica Sinica)(in Chinese),1995,38(Suppl.):3~14
[116]Bird P.Initiation of intracontinental subduction in the Himalaya.J.Geophys.Res.,1978,83:1975~1987
[117]Kosarev G,Kind R,Sobolev S V,et al.Seismic evidence for adetached Indian lithospheric mantle beneath Tibet.Science,1999,283:1306~1309
[118]Tilmann F,Ni J,INDEPTH Seismic Team.Seismic imaging of thedown_welling Indian lithosphere beneath central Tibet.Science,2003,300:1424~1427
[119]吴庆举,曾融生,赵文津.喜马拉雅-青藏高原的上地幔倾斜构造与陆-陆碰撞过程.中国科学(D辑),2004,34(10):919~925Wu Q J,Zeng R S,Zhao W J.Dipping structure of upper mantleand continent_continent collision in Himalayas_Tibet Plateau.Sciencein China(Series D)(in Chinese),2004,34(10):919~925
[120]曾融生,丁志峰,吴庆举等.喜马拉雅及南藏的地壳俯冲带—地震学证据.地球物理学报,2000,43(6):780~797Zeng R S,Ding Z F,Wu Q J,et al.Seismological evidence for themultiple income crustal subductions in Himalayas and southern Tibet.Chinese J.Geophys.(in Chinese),2000,43(6):780~797
[121]曾融生,吴庆举,丁志峰等.印度-欧亚碰撞与洋-陆碰撞的差异.地震学报,2006(待刊)Zeng R S,Wu Q J,Ding Z F,et al.Differences of India_Eurasianplate collision and ocean_continent collision.Acta Seismologica Sinica(in Chinese),2006(in press)
[2]曾融生,阚荣举.柴达木盆地西部地壳深界面的反射波.地球物理学报,1961,10(1):120~125Zeng R S,Gan R J.Reflected waves from crustal interface in westernChaitamu Basin.Chinese J.Geophys.(Acta Geophysica Sinica)(inChinese),1961,10(1):120~125
[3]中国科学院地球物理研究所.西藏高原当雄-亚东地带地壳与上地幔结构和速度分布的爆炸地震研究.地球物理学报,1981,24(2):155~170Institute of Geophysics,Chinese Academy of Sciences.Explosionseismic study for velocity distribution and structure of the crust andupper mantle from Damxung to Yadong of Xizang plateau.Chinese J.Geophys.(Acta Geophysica Sinica)(in Chinese),1981,24(2):155~170
[4]滕吉文,熊绍柏,尹周勋等.喜马拉雅山北部地区的地壳结构模型和速度分布特征.地球物理学报,1983,26(6):525~540Teng J W,Xiong S B,Yin Z X,et al.Structure of the crust andupper mantle pattern and velocity distributional characteristics in theNorthern Himalayan mountain region.Chinese J.Geophys.(ActaGeophysica Sinica)(in Chinese),1983,26(6):525~540
[5]张中杰,滕吉文,李英康等.藏南地壳速度结构与地壳物质东西向“逃逸”—以佩枯错—普莫雍错宽角反射剖面为例.中国科学(D辑),2002,32(10):793~798Zhang Z J,Teng J W,Li Y K,et al.Crustal velocity structure andeastward escaping of crustal material in the southern Tibet———Anexample revealed by wide_angle seismic profile between Peikucuo andPumoyongcuo.Science in China(Ser.D)(in Chinese),2002,32(10):793~798
[6]滕吉文,尹周勋,熊绍柏.西藏高原北部地区色林错-蓬错-那曲-索县地带地壳结构与速度分布.地球物理学报,1985,28(增刊Ⅰ):28~42Teng J W,Yin Z X,Xiong S B.Crustal structure and velocitydistribution beneath Selin Co_Peng Co_Na Qu_Suo County region inthe Northern Xizang plateau.Chinese J.Geophys.(Acta GeophysicaSinica)(in Chinese),1985,28(Suppl.Ⅰ):28~42
[7]熊绍柏,滕吉文,尹周勋.西藏高原地区的地壳厚度和莫霍界面的起伏.地球物理学报,1985,28(增刊Ⅰ):16~27Xiong S B,Teng J W,Yin Z X.The thickness of the crust andundulation of discontinuity in Xizang(Tibet)plateau.Chinese J.Geophys.(Acta Geophysica Sinica)(in Chinese),1985,28(Suppl.Ⅰ):16~27
[8]卢德源,黄立言,陈纪平等.青藏高原北部沱沱河-格尔木地区地壳和上地幔的结构模型和速度分布特征.见:西藏地球物理文集.北京:地质出版社.1990.51~62Lu D Y,Huang L Y,Chen J P,et al.Structural model and velocitydispersion characteristics of the crust and upper mantle in Tuotuohe_Golmud region of north Qinghai_Xizang plateau.In:GeophysicalMemoir on Xizang_Qinghai Plateau.Beijing:Geological PublishingHouse,1990.51~62
[9]徐新忠,齐雄飞,杨长来等.青海花石峡-甘肃阿克赛人工爆破地震测深成果.见:中国地球物理学会编.中国地球物理学会年刊,北京:地震出版社,1993.80Xu X Z,Qi X F,Yang C L,et al.Results of man_made explosionseismic sounding from Huashixia(in Qinghai)to Aksay(in Gansu).In:Chinese Geophysical Society eds.Annual of the ChineseGeophysical Society in 1993.Beijing:Seismological Press,1993.80
[10]崔作舟,李秋生,吴朝东等.格尔木-额济纳旗地学断面的地壳结构与深部构造.地球物理学报,1995,38(增刊Ⅱ):15~28Cui Z Z,Li Q S,Wu C D,et al.The crustal and deep tectonics inGolmud_Ejin Qi GGT.Chinese J.Geophys.(in Chinese),1995,38(Suppl.Ⅱ):15~28
[11]熊绍柏,刘宏兵.青藏高原西部的地壳结构.科学通报,1997,42(12):1309~1312Xiong S B,Liu H B.Crustal structure in the west Tibetan plateau.Chinese Science Bulletin(in Chinese),1997,42(12):1309~1312
[12]孔祥儒,王谦身,熊绍柏.青藏高原西部综合地球物理剖面和岩石圈结构与动力学.科学通报,1999,44(12):1257~1265Kong X R,Wang Q S,Xiong S B.The study of comprehensivegeophysical profile and lithosphere structure and dynamic in westTibet.Chinese Science Bulletin(in Chinese),1999,44(12):1257~1265
[13]李秋生,卢德源,高锐等.新疆地学断面(泉水沟—独山子)深地震测深成果综合研究.地球学报,2001,22(6):534~540Li Q S,Lu D Y,Gao R,et al.An integrated study of deep seismicsounding profile along Xinjiang Global Geoscience Transect(Quanshuigou_Dushanzi).Acta Geoscientia Sinica(in Chinese),2001,22(6):534~540
[14]Zhao W J,Mechie J,Brown L D,et al.Crustal structure of centralTibet as derived from INDEPTH wide_angle seismic data.GeophysicalJournal International,2001,145:486~498
[15]王有学,钱辉.青海东部地壳速度结构特征研究.地学前缘,2000,7(4):568~579Wang Y X,Qian H.Study of crustal velocity structure in the eastQinghai.Earth Science Fronties(in Chinese),2000,7(4):568~579
[16]赖晓玲,李松林,张先康.玛沁—兰州—靖边剖面壳幔复杂性的研究.地球物理学进展,2001,16(2):65~72Lai X L,Li S L,Zhang X K.A study on the complexity at the crust_upper mantle transition zone along Maqin_Lanzhou_Jingbian deepseismic sounding(DSS)profile.Progress in Geophysics(inChinese),2001,16(2):65~72
[17]李松林,张先康,张成科.玛沁—兰州—靖边地震测深剖面地壳速度结构的初步研究.地球物理学报,2002,45(2):210~217Li S L,Zhang X K,Zhang C K.A preliminary study on the crustalvelocity structure of Maqin_Lanzhou_Jingbian by means of deepseismic sounding profile.Chinese J.Geophys.(in Chinese),2002,45(2):210~217
[18]Zhang Z J,Wang G J.P_wave structure along 1100km long wide_angle seismic profile in the eastern Tibet.AGU,Japan.2002
[19]王椿镛,吴建平,楼海.川西藏东地区的地壳P波速度结构.中国科学(D辑),2003,33(增):181~189Wang C Y,Wu J P,Lou H.Crustal P_wave velocity structure in thewest Sichuan and east Tibet region.Science in China(Series D)(inChinese),2003,33(Suppl.):181~189
[20]赵俊猛,张先康,王尚旭等.准噶尔盆地、天山造山带、塔里木盆地、阿尔金造山带、柴达木盆地和昆仑造山带(北缘)岩石圈结构及其动力学研究.见:中国地球物理学会编.中国地球物理学会年刊.昆明:云南科技出版社,2001.13Zhao J M,Zhang X K,Wang S X,et al.The lithospheric structureand dynamic process of the Junggar Basin,the Tianshan OrogenicBelt,the Tarim Basin,the Altun Orogenic Belt,the Qaidam Basin andthe Kunlun Orogenic Belt(northern margin).In:ChineseGeophysical Society eds.Annual of the Chinese Geophysical Society.Kunming:Yunnan Science&Technology Press,2001.13
[21]赵俊猛,张先康,邓宏钊等.拜城—大柴旦剖面的上地壳Q值结构.地球物理学报,2003,46(4):503~509Zhao J M,Zhang X K,Deng H Z,et al.Qvalue structure of theupper crust along the profile from Baicheng to Da Qaidam.ChineseJ.Geophys.(in Chinese),2003,46(4):503~509
[22]Wang C Y,Han W B,Wu J P,et al.Crustal structure beneath theSongpan_Garze orogenic belt.Acta Seimologica Sinica,2003,16(3):237~250
[23]Zhao W J,Nelson K D,Project INDEPTH Team.Deep seismicreflection evidence for continental underthrusting beneath southernTibet.Nature,1993,366(9):557~559
[24]Zhao W J,Nelson K D,Meissner.Advances of INDEPTH_A deepprofiling study in Tibet and the Himalayas.Episodes,1997,20(4):266~272
[25]吴宣志,吴春玲,卢杰等.利用深地震反射剖面研究北祁连-河西走廊地壳细结构.地球物理学报,1995,38(增Ⅱ):29~35Wu X Z,Wu C L,Lu J,et al.Research on the fine crustal structureof the northern Qilian_Hexi Corridor by deep seismic reflection.Chinese J.Geophys.(in Chinese):1995,38(Suppl.Ⅱ):29~35
[26]高锐,黄东定,卢德源等.横过西昆仑造山带与塔里木盆地结合带的深地震反射剖面.科学通报,2000,45(17):1874~1879Gao R,Huang D D,Lu D Y,et al.Deep seismic reflection profileacross the contact zone of the West Kunlun orogenic belt and theTarim basin.Chinese Science Bulletin(in Chinese),2000,45(17):1874~1879
[27]高锐,肖序常,刘训等.新疆地学断面深地震反射剖面揭示的西昆仑-塔里木结合带岩石圈细结构.地球学报,2001,22(6):547~552Gao R,Xiao X C,Liu X,et al.Detail lithospheric structure of thecontact zone of West Kunlun_Tarim revealed by the deep seismicreflection profile along Xinjiang geotransect.Acta Geoscientia Sinica(in Chinese),2001,22(6):547~552
[28]高锐,李鹏武,李秋生等.青藏高原北缘碰撞变形的深部过程———深地震探测成果之启示.中国科学(D辑),2001,31(增):66~71Gao R,Li P W,Li Q S,et al.Deep process of the collision anddeformation in northern Tibetan Plateau—implications from deepseismic sounding results.Science in China(Series D)(in Chinese),2001,31(Suppl.):66~71
[29]Gao R,Ma Y S,Zhu X,et al.The lithospheric structures of theSongpan block in the northeastern Tibetan plateau_revelation frominvestigation of the deep seismic profile,GEOLOGIE ALPINE,20thHimalayan_Karakoruam_Tibet Workshop Special ExtendedAbstracts,Aussois,France,2005,44,58
[30]姜枚,吕庆田,薛光琦.中、法两国联合进行青藏高原天然地震探测地壳结构的研究.地球物理学报,1994,37(3):412~413Jiang M,Lu Q T,Xue G Q.Researches on the crustal structure ofthe Tibetan Plateau by means of seismic experiment jointly by Chineseand French geophysics.Chinses J.Geophys.(in Chinese),1994,37(3):412~413
[31]许志琴,杨经绥,姜枚.青藏高原北部的碰撞造山及深部动力学—中法地学合作研究新进展.地球学报,2001,22(1):5~10Xu Z Q,Yang J S,Jiang M.Collision_orogeny of the northernQinghai_Tibet plateau and its deep dynamics.Acta Geoscientia Sinica(in Chinese),2001,22(1):5~10
[32]Kao H,Gao R,Rau Ruey_Juin,et al.Seismic image of the Tarimbasin and its collision with Tibet.Geology,2001,29(7):575~578
[33]管烨,高弘,高锐等.新疆塔里木-西昆仑宽频地震观测实验研究.地球学报,2001,22(6):559~562Guan Y,Gao H,Gao R,et al.Broadband seismic observationalexperiments from Tarim basin to Kunlun mountains.Acta GeoscientiaSinica(in Chinese),2001,22(6):559~562
[34]丁志峰,曾融生.青藏高原横波分裂的观测研究.地球物理学报,1996,39(2):211~220Ding Z F,Zeng R S.Observation and study of shear wave anisotropyin Tibetan Plateau.Chinese J.Geophys.(in Chinese),1996,39(2):211~220
[35]曾融生,丁志峰,吴庆举.喜马拉雅-祁连山地壳构造与大陆-大陆碰撞过程.地球物理学报,1998,41(1):49~60Zeng R S,Ding Z F,Wu Q J.The crustal structure from Himalayasto Qilian and its implications for continent_continent collision process.Chinese J.Geophys.(in Chinese),1998,41(1):49~60
[36]吕庆田,姜枚,马开义.三维走时反演与青藏高原南部深部构造.地震学报,1996,18(4):451~459LüQ T,Jiang M,Ma K Y.3_D travel time tomography inversion andthe deep structure of the southern Tibet.Acta Seismologica Sinica(inChinese),1996,18(4):451~459
[37]姜枚,吕庆田,史大年.用天然地震探测青藏高原中部地壳、上地幔结构.地球物理学报,1996,39(4):470~482Jiang M,LüQ T,Shi D N.The study on the structure of crustal andupper mantle with natural earthquakes in central Tibetan Plateau.Chinese J.Geophys.(in Chinese),1996,39(4):470~482
[38]Kind R,Yuan X,Saul J,et al.Seismic Images of crust and uppermantle beneath Tibet:evidence for Eurasian plate subduction.Science,2002,298:1219~1221
[39]董英君,薛光琦,马开义.阿尔金断裂系及邻区剪切波各向异性研究.地球物理学进展,1999,14(4):58~65Dong Y J,Xue G Q,Ma K Y.Studies on shear wave anisotropybeneath Altyn fault system and its adjacent area.Progress inGeophysics(in Chinese),1999,14(4):58~65
[40]史大年,姜枚,马开义等.阿尔金断裂带地壳和上地幔结构的P波层析成像.地球物理学报,1999,42(3):341~350Shi D N,Jiang M,Ma K Y,et al.Crust and upper mantletomographic structure across the Altyn fault zone using teleseismic P_waves.Chinese J.Geophys.(in Chinese),1999,42(3):341~350
[41]钱辉,姜枚,薛光琦等.天然地震接收函数揭示的青藏高原东部地壳结构.地震学报,2001,23(1):103~108Qian H,Jiang M,Xue G Q,et al.Crustal structure of eastern Tibetinferred from natural earthquake receiver function analysis.ActaSeismological Sinica(in Chinese),2001,23(1):103~108
[42]Frederik T,Ni J,INDEPTH_ⅢSeismic Team.Seismic imaging ofthe down_welling Indian lithosphere beneath central Tibet.Science,2003,300,1424~1427
[43]薛光琦,姜枚,宿和平.利用层析成像研究青藏高原叶城-狮泉河地区深部构造.中国科学(D辑),2004,34(4):329~334Xue G Q,Jiang M,Su H P.A study on deep structure of Yecheng_Shiquanhe region on Tibetan plateau by tomographic imaging.Sciencein China(Series D)(in Chinese),2004,34(4):329~334
[44]郭飚,刘启元,陈九辉等.青藏高原东北缘—鄂尔多斯地壳上地幔地震层析成像研究.地球物理学报,2004,47(5):790~797Guo B,Liu Q Y,Chen J H,et al.Seismic tomographic imaging ofthe crust and upper mantle beneath the Northeastern edge of theQinghai_Xizang plateau and the Ordos area.Chinese J.Geophys.(in Chinese),2004,47(5):790~797
[45]Pelkum S,Monsalve G,Sheehan A,et al.Imaging the Indiansubcontinent beneath the Himalayas.Nature,2005,435:1222~1225
[46]谭捍东,魏文博,Martyn Unsworth等.西藏高原南部雅鲁藏布江缝合带地区地壳电性结构研究.地球物理学报,2004,47(4):685~690Tan H D,Wei W B,Martyn Unsworth,et al.Crustal electricalconductivity structure beneath the Yarlung Zangbo Jiang suture in thesouthern Xizang plateau.Chinese J.Geophys.(in Chinese),2004,47(4):685~690
[47]范文科,袁学诚.羊八井至洛扎南北向剖面磁大地电流测深初步成果.见:李光岑,Mercier J L编.中法喜马拉雅考察成果1980.北京:地质出版社,1984.413~419Pham Van Ngoc,Yuan X C.Execution of a long MT profile of NSdirection from Yangbajing to Lhozag:First results.In:Li G C,Mercier J L eds.Sino_French Cooperative Investigation in Himalyas(in Chinese).Beijing:Geological Publishing House,1984.413~419
[48]袁学诚,李立,金国元等.西藏洛扎-那曲一带地壳和上地幔的磁大地电流测深研究.见:西藏地球物理文集,北京:地质出版社,1990.63~71Yuan X C,Li L,Jin G Y,et al.Magnetotelluroc investigations inLhozang_area,Tibet.In:Geophysical Memoir on Xizang_QinghaiPlateau(in Chinese).Beijing:Geological Publishing House,1990.63~71
[49]郭新峰,张元丑,程庆云等.青藏高原亚东-格尔木地学断面岩石圈电性研究.中国地质科学院院报,1990,21:191~202Guo X F,Zhang Y C,Cheng Q Y,et al.Magnetotelluric studiesalong Yadong_Golmud geosciences transect in Qinghai_Xizangplateau.Bulletin of The Chinese Academy of Geological Sciences(inChinese),1990,21:191~202
[50]朱仁学,胡祥云.格尔木-额济纳旗地学断面岩石圈电性结构的研究.地球物理学报,1995,38(增刊Ⅱ):46~57Zhu R X,Hu X Y.Study on the resistivity structure of thelithosphere along the Golmod_Ejin Qi geoscience transect.Chinese J.Geophys.(in Chinese),1995,38(Suppl.Ⅱ):46~57
[51]Wei W B,Unsworth M,Jones A,et al.Detection of widespreadfluids in the Tibetan crust by magnetotelluric studies.Science,2001,292:716~718
[52]马晓冰,孔祥儒,于晟.青藏高原西部大地电磁测深探测结果.科学通报,1997,42(11):1185~1187Ma X B,Kong X R,Yu S.Magnetotelluric sounding in westernTibet.Chinese Science Bulletin(in Chinese),1997,42(11):1185~1187
[53]孙洁,晋光文,白登海等.青藏高原东缘地壳、上地幔电性结构探测及其构造意义.中国科学(D辑),2003,33(增):173~180Sun J,Jin G W,Bai D H,et al.Electrical structure of the crust andupper mantle and tectonics sense on the edge of the East Tibet.Science in China(Series D)(in Chinese),2003,33(Suppl.):173~180
[54]李立,金国元.西藏岩石圈电性和热状态.地质矿产部地球物理地球化学勘查研究所所刊,1986,2:121~128Li L,Jin G Y.The electrical characteristic and thermal state of thelithosphere in area of Xizang(Tibet)autonomous region.Bulletin ofthe Institute of Geophysical&Geochemical Exploration,Ministry ofGeology and Mineral Resources(in Chinese),1986,2:121~128
[55]Yuan X C,Xu X Z.Global geoscience transect(GGT)acrossEurasia_Chinese part(from Altay to Taiwan).Abstracts of 30thInternational Geological Congress,1996,1:141
[56]秦国卿,陈九辉,刘大建等.昆仑山脉和喀喇昆仑山脉地区的地壳上地慢电性结构特征.地球物理学报,1994,37(2):193~199Qin G Q,Chen J H,Liu D J,et al.The characteristics of theelectrical structure of the crust and upper mantle in the region of theKunlun and the Karakorum mountains.Chinese J.Geophys.(ActaGeophysica Sinica)(in Chinese),1994,37(2):193~199
[57]Chen L S,John R Booker,Alan G Jones,et al.Electricallyconductive crust in southern Tibet from INDEPTH magnetoelluricsurveying.Science,1996,274:1694~1696
[58]马晓冰,孔祥儒,刘宏兵等.青藏高原东部大地电磁测深探测结果.中国科学(D辑),2001,31(增):72~76Ma X B,Kong X R,Liu H B,et al.Magnetotelluric soundingresults in eastern Tibetan Plateau.Science in China(Series D)(inChinese),2001,31(Suppl.):72~76
[59]孟令顺,申江胜,齐立等.西藏羊八井-聂拉木地区的重力工作及其初步解释.石油物探,1984,23(2):1~21Meng L S,Shen J S,Qi L,et al.The preliminary interpretation ofthe gravity profile of well Yang No.8_Nielamu,Tibet.GeophysicalProspecting For Petroleum(in Chinese),1984,23(2):1~21
[60]孟令顺,高锐,周富祥等.利用重力异常研究亚东-格尔木地壳构造.中国地质科学院院报,1990,21:149~161Meng L S,Gao R,Zhou F X,et al.Intepretation of the crustalstructure in Yadong_Golmud area using gravity anomalies.Bulletin ofThe Chinese Academy ofGeological Sciences(in Chinese),1990,21:149~161
[61]孟令顺,姜喜荣,张风华等.新疆叶城-西藏狮泉河重力剖面与地壳结构.地球物理学报,1990,33(6):670~677Meng L S,Jiang X R,Zhang F H,et al.Gravity profile and thecrustal structure of Yecheng_Shiquanhe.Chinese J.Geophys.(ActaGeophysica Sinica)(in Chinese),1990,33(6):670~677
[62]孟令顺.地壳的重力构造.见:中国地质科学院岩石圈研究中心编.青藏高原岩石圈结构构造和形成演化.中华人民共和国地质矿产部地质专报,第20号.北京:地质出版社,1996.83~93Meng L S.Gravity structure of crust in Tibet.In:The LithosphereResearch Center of Chinese Academy of Geology Science,Institute ofGeology Science of Ministry of Geology and Mineral Resources eds.Lithospheric Structure and Tectonics in Tibet and Its Formation andEvolution.People’s Republic of China Ministry of Geology andMineral Resources.Geological Tectonics,NO.20.Beijing:Geological Publishing House,1996.83~93
[63]孟令顺,齐立,高锐等.横过阿尔金山的重力测量及初步解释.长春科技大学学报,1998,28(3):345~350Meng L S,Qi L,Gao R,et al.Gravity survey and isostatic messagealong the profile of Aergan(in Xinjiang)-Laomangya(in Qinghai).Journal of Changchun University of Science and Technology(inChinese),1998,28(3):345~350
[64]孟令顺,管烨,齐立等.格尔木-额济纳旗地学断面及其邻区重力场与深部地壳构造.地球物理学报,1995,38(增刊Ⅱ):36~45Meng L S,Guan Y,Qi L,et al.Gravity field and deep crustalstructure in Golmud_Ejin Qi geoscience transection and nearby area.Chinese J.Geophys.(in Chinese),1995,38(Suppl.Ⅱ):36~45
[65]王谦身,武传真,江为为.青藏高原西部吉隆-鲁谷地区的重力场与地壳构造.科学通报,1997,42(8):858~862Wang Q S,Wu C Z,Jiang W W.Gravity field and crustal structureof Jilong_Lugu region in western Tibet.Chinese Science Bulletin(inChinese),1997,42(8):858~862
[66]王谦身,安玉林.青藏高原东部玛多—沙马地区的重力场与深部构造.地球物理学进展,2001,16(4):4~10Wang Q S,An Y L.Gravity field and deep structure of Madoi_Shamaregion in eastern Qinghai_Xizang(Tibetan)plateau.Process inGeophysics(in Chinese),2001,16(4):4~10
[67]余钦范,孙运生,楼海等.亚东格尔木地学断面的磁结构.中国地质科学院院报,1990,21:183~190Yu Q F,Sun Y S,Lou H,et al.The magnetic structure ofgeoscience transect from Yadong to Golmud.Bulletin of The ChineseAcademy of Geological Sciences(in Chinese),1990,21:183~190
[68]余钦范,楼海,胡中栋.格尔木-额济纳旗地学断面岩石圈结构的磁场分析.地球物理学报,1995,38(增刊Ⅱ):58~Yu Q F,Lou H,Hu Z D.Magnetic data interpretation of the crustalstructure of the geoscience transection from Golmud to Ejin Qi.Chinese J.Geophys.(in Chinese),1995,38(Suppl.Ⅱ):58~70
[69]孙鸿烈,郑度主编.青藏高原形成、演化与发展.广州:广东科技出版社,1998.21~23Sun H L,Zheng D.Formation,Evolution and Development ofQinghai_Xizang Plateau(in Chinese).Guangzhou:GuangdongScience&Technology Press,1988.
[70]刘宏兵,孔祥儒,马晓冰等.青藏高原东南地区地壳物性结构特征.中国科学(D辑),2001,31(增):61~71Liu H B,Kong X R,Ma X B,et al.Crustal structure characteristicof the southeast Tibet.Science in China(Series D)(in Chinese),2001,31(Suppl.):61~71
[71]沈显杰,张文仁,杨淑贞等.青藏高原南北地体壳幔热结构差异的大地热流证据.中国地质科学院院报,1990,21:203~214Shen X J,Zhang W R,Yang S Z,et al.Heat flow evidence for thedifferentiated crust_mantle thermal structures of the Qinghai_Xizangplateau.Bulletin of the Chinese Academy of Geological Sciences(inChinese),1990,21:203~214
[72]沈显杰,杨淑贞,沈继英.格尔木-额济纳旗地学断面热流研究与分析.地球物理学报,1995,38(增刊Ⅱ):86~97Shen X J,Yang S Z,Shen J Y.Heat flow study and analysis alongthe Golmud_Ejin Qi geotransect.Chinese J.Geophys.(ActaGeophysica Sinica)(in Chinese),1995,38(Suppl.Ⅱ):86~97
[73]Wittlinger G,Vergne J,Tapponnier P,et al.Teleseismic imaging ofsubducting lithosphere and Moho offsets beneath western Tibet.Earthand Planetary Science Letter,2004,221:117~130
[74]Hirn A,Lepine J C,Jobert T G,et al.Crust structure andvariability of the Himalayan border of Tibet.Nature,1984,307(5946):23~25
[75]李秋生,彭苏萍,高锐.青藏高原莫霍面的研究进展.地质论评,2004,50(6):598~612Li Q S,Peng S P,Gao R.A review on the Moho discontinuitybeneath the Tibetan plateau.Geological Review(in Chinese),2004,50(6):598~612
[76]高恩源,徐中信,王香泾等.喜马拉雅山北麓—雅鲁藏布江地区人工爆炸地震测深地壳结构.见:中国地质科学院主编.西藏地球物理文集.北京:地质出版社,1990.1~14Gao E Y,Xu Z X,Wang X J,et al.Structure of the crust andvelocity distributional characteristics in the unit between Himalayamountain and the Yaluzangbo river.In:Geophysical Memoir onXizang_Qinghai Plateau(in Chinese).China Academy of GeologyScience eds.Beijing:Geological Publishing House,1990.1~14
[77]黄立言,卢德源,李小鹏等.藏北色林湖—蓬错—雅安多地带的深部地震测深.见:西藏地球物理文集.北京:地质出版社,1990.25~37Huang L Y,Lu D Y,Li X P,et al.Deep seismic sounding ofSelincuo Lake_Pengcuo Lake_Yangamdo in the north of the Xizang(Tibet).In:Geophysical Memoir on Xizang_Qinghai Plateau(inChinese).Beijing:Geological Publishing House,1990.25~37
[78]张中杰,李英康,王光杰等.藏北地壳东西向结构与“下凹”莫霍面———来自宽角反射剖面的启示.中国科学(D辑),2001,31(11):881~888Zhang Z J,Li Y K,Wang G J,et al.E—W crustal structure underthe northern Tibet and“down—bowing”Moho under the northernTibet revealed by wide_angle seismic profile.Science in China(Series D)(in Chinese),2001,31(11):881~888
[79]曾融生,丁志峰,吴庆举.青藏高原岩石圈构造及动力学过程研究.地球物理学报,1994,37(增):99~116Zeng R S,Ding Z F,Wu Q J.A review on the lithosphericstructures in Tibetan plateau and constraints for dynamics.Chinese J.Geophys.(Acta Geophysica Sinica)(in Chinese),1994,37(Suppl.):99~116
[80]Ross A,Brown L,Passakorn P,et al.Deep reflection surveying incentral Tibet:lower_crustal layering and crustal flow.GeophysicalJournal International,2004,156:115~128
[81]李秋生,彭苏萍,高锐等.东昆仑大地震的深部构造.地球学报,2004,25(1):11~16Li Q S,Peng S P,Gao R,et al.Deep tectonic background of the8.1Ms earthquake in the east Kunlun.Acta Geoscientica Sinica(inChinese),2004,25(1):11~16
[82]Kind R,Yuan X,Saul J,et al.Seismic images of crust and uppermantle beneath Tibet:evidence for Eurasian plate subduction.Science,2002,298:1219~1221
[83]吴庆举,曾融生.用宽频带远震接收函数研究青藏高原的地壳结构.地球物理学报,1998,41(5):669~679Wu Q J,Zeng R S.The crustal stucture of Qinghai_Xizang plateauinferred from broadband teleseismic waveform.Chinese J.Geophys.(Acta Geophysica Sinica)(in Chinese),1998,41(5):669~679
[84]Zhu L P,Helmberger D V.Moho offset across the northern margin ofthe Tibetan plateau.Science,1998,281:1170~1172
[85]Zhang Z J,Klemperer S L.West_east variation in crustal thickness innorthern Lhasa block,central Tibet,from deep seismic soundingdata.J.Geophys.Res.,2005,110(B9),B09403,doi:10.1029/2004JB003139
[86]李秋生,彭苏萍,高锐等.青藏高原北部巴颜喀拉构造带基底隆起的地震学证据.地质通报,2003,22(10):782~788Li Q S,Peng S P,Gao R,et al.Seismic evidence of the basementuplift in the Bayan Har tectonic belt,Qinghai,and its tectonicsignificance.Geological Bulletin of China(in Chinese),2003,22(10):782~788
[87]王椿镛,韩渭宾,吴建平等.松潘—甘孜造山带地壳速度结构.地震学报,2003,25(3):229~241Wang C Y,Han W B,Wu J P,et al.Crustal structure beneath theSongpan_Garze orogenic belt.Acta Seismologica Sinica(in Chinese),2003,25(3),229~241
[88]高锐,吴功建.青藏高原亚东-格尔木地学断面地球物理综合解释模型与现今地球动力学过程.长春地质学院学报,1995,25(3):241~250Gao R,Wu G J.Geophysical model and geodynamic process ofYadong_Ge’ermu geoscience transect in Qinghai_Tibet plateau.Journal of Changchun University of Earth Sciences(in Chinese),1995,25(3):241~250
[89]Nelson K D,Zhao W J,Brown L D,et al.Partially molten middlecrust beneath Southern Tibet:Synthesis of project INDEPTH results.Science,1996,274:1684~1688
[90]Kind R,Ni J,Zhao W J,et al.Evidence from earthquake data for apartially molten crustal layer in Southern Tibet.Science,1996,274:1692~1694
[91]王式,卢德源,黄立言等.西藏高原南北走向的地壳结构模型和速度分布特征.见:西藏地球物理文集.北京:地质出版社,1990.38~47Wang S,Lu D Y,Huang L Y,et al.Velocity distributioncharacteristics and N_S variation of the depth of the earth’s crust inthe Xizang(Tibet)plateau.In:Geophysical Memoir on Xizang_Qinghai Plateau(in Chinese).Beijing:Geological Publishing House,1990.38~47
[92]Spratt J E,Jones A G,Nelson K D,et al.Crustal structure of theIndia_Asia collision zone,southern Tibet,from INDEPTH MTinvestigations.Physics of the Earth and Planetary Interiors,2005,150(1_3):227~237
[93]崔作舟,尹周勋,高恩元等.青藏高原地壳结构构造及其与地震的关系.中国地质科学院院报,1990,21:215~226Cui Z Z,Yin Z X,Gao E Y,et al.The structure and tectonics ofthe crust and their relation with earthquakes in the Qinghai_Xizangplateau.Bulletin of The Chinese Academy of Geological Sciences(inChinese),1990,21:215~226
[94]吴功建,高锐,余钦范等.青藏高原“亚东-格尔木地学断面”综合地球物理调查与研究.地球物理学报,1991,34(5):552~562Wu G J,Gao R,Yu Q F,et al.Intergrated investigations of theQinghai_Tibet plateau along the Yadong_Golmud geoscience transect.Chinese J.Geophys.(Acta Geophysica Sinica)(in Chinese),1991,34(5):552~562
[95]McNamara D E,Owens T J,Walter W R.Observations of theregional phase propagation across the Tibetan Plateau.Journal ofGeophysical Research,1995,100(22):22215~22229
[96]滕吉文等.柴达木东盆地的深层地震反射波和地壳构造.地球物理学报,1974,17(2):121~134Teng J W,et al.Deep reflected waves and the structure of the earthcrust of the eastern part of Qaidam basin.Chinese J.Geophys.(Acta Geophysica Sinica)(in Chinese),1974,17(2):121~134
[97]宋仲和,安昌强,王椿镛等.青藏高原及南北带上地幔P波速度结构.地球物理学报,1985,28(增):148~160Song Z H,An C Q,Wang C Y,et al.The P wave velocity of uppermantle beneath Qinghai_Tibet plateau and north_south seismic zone.Chinese J.Geophys.(Acta Geophysica Sinica)(in Chinese),1985,28(Suppl.):148~160
[98]庄真,傅竹武,吕梓玲等.青藏高原及邻近地区地壳与上地幔剪切波三维速度结构.地球物理学报,1992,35(6):694~709Zhuang Z,Fu Z W,LüZ L,et al.3_D shear velocity model of crustand upper mantle beneath the Tibetan plateau and its adjacentregions.Chinese J.Geophys.(Acta Geophysica Sinica)(inChinese),1992,35(6):694~709
[99]陈国英,曾融生.用地震面波频散研究喜马拉雅山与西藏高原岩石圈构造的差异.地球物理学报,1985,28(Suppl.):161~173Chen G Y,Zeng R S.The difference of lithospheric structurebetween Himalayan mountain and Tibetan plateau from surface wavedispersion.Chinese J.Geophys.(Acta Geophysica Sinica)(inChinese),1985,28(Suppl.):161~173
[100]吴建平,明跃红,叶太兰等.体波波形反演对青藏高原上地幔速度结构的研究.地球物理学报,1998,41(增):15~25Wu J P,Ming Y H,Ye T L,et al.Upper mantle velocity structurein the Qinghai_Xizang Plateau from inversion of body waveforms.Chinese J.Geophys.(Acta Geophysica Sinica)(in Chinese),1998,41(Suppl.):15~25
[101]McNamara D E,Owens T J,Silver P G,et al.Shear wave anisotropybeneath the Tibetan plateau.Journal of Geophysical Research,1994,99(B7):13655~13665
[102]Hirn A,Jiang M,Sapin M,et al.Seismic anisotropy as an indicatorof mantle flow beneath the Himalayas and Tibet.Nature,1995,375:571~574
[103]姜枚,许志琴,Hirn A等.青藏高原及其部分邻区地震各向异性和上地幔特征.地球学报,2001,22(2):111~116Jiang M,Xu Z Q,Hirn A,et al.Seismic anisotropy and uppermantle characteristic of Tibetan plateau and its partial adjacent area.Acta Geoscientica Sinica.(in Chinese),2001,22(2):111~116
[104]董英君,薛光琦,马开义.阿尔金断裂系及邻区剪切波各向异性研究.地球物理学进展,1999,14(4):58~65Dong Y J,Xue G Q,Ma K Y.Studies on shear wave anisotropybeneath Altyn fault system and its adjacent area.Progress inGeophysics(in Chinese),1999,14(4):58~65
[105]高锐.青藏高原岩石圈结构与地球动力学的30个为什么.地质论评,1997,43(5):460~464Gao R.Thirty problems of the lithospheric structure and geodynamicsin the Qinghai_Xizang plateau.Geological Review(in Chinese),1997,43(5):460~464
[106]潘裕生.青藏高原的形成和隆升.地学前缘,1999,6(3):153~163Pan Y S.Formation and uplifting of the Qinghai_Tibet plateau.EarthScience Frontiers(in Chinese),1999,6(3):153~163
[107]常承法,潘裕生,郑锡谰等.青藏高原地质构造.北京:科学出版社,1982Chang C F,Pan Y S,Zheng X L,et al.The Geological Tectonics ofQinghai-Xizang(Tibet)Plateau.Beijing:Science Press,1982
[108]滕吉文,张中杰,杨顶辉等.青藏高原地体划分的地球物理标志研究.地球物理学报,1996,39(5):629~641Teng J W,Zhang Z J,Yang D H,et al.The study of geophysicalcriterion for dividing terranes in Qinghai_Xizang Plateau.Chinese J.Geophys.(Acta Geophysica Sinica)(in Chinese),1996,39(5):629~641
[109]Murphy M A,Yin A,Harrison T M,et al.Did the Indo_Asiancollision alone create the Tibetan plateau?Geology,1997,25(8):719~722
[110]李廷栋.青藏高原隆升的过程和机制.地球学报,1995,(1):1~9Li T D.The uplifting process and mechanism of the Qinghai_Tibetplateau.Acta Geoscientia Sinica(in Chinese),1995,(1):1~9
[111]钟大赉,丁林.青藏高原的隆起过程及其机制探讨.中国科学(D辑),1996,26(4):289~295Zhong D L,Ding L.Research on the uplift process and mechanism ofthe Tibetan plateau.Science in China(Series D)(in Chinese),1996,26(4):289~295
[112]许志琴,姜枚,杨经绥等.青藏高原的地幔结构:地幔羽、地幔剪切带及岩石圈俯冲板片的拆沉.地学前缘,2004,11(4):329~343Xu Z Q,Jiang M,Yang J S,et al.Mantle structure of Qinghai-Tibet plateau:Mantle plume,mantle shear zone and delamination oflithospheric slab.Earth Science Frontiers(in Chinese),2004,11(4):329~343
[113]滕吉文,张中杰,王光杰等.喜马拉雅碰撞造山带的深层动力过程与陆-陆碰撞新模型.地球物理学报,1999,42(4):481~494Teng J W,Zhang Z J,Wang G J,et al.The deep internal dynamicalprocesses and new model of continental-continental collision inHimalayan collision orogenic zone.Chinese J.Geophys.(inChinese),1999,42(4):481~494
[114]高锐.青藏高原岩石圈变形与陆壳运动.见:中国地球物理学会年刊,北京:地震出版社,1990.121Gao R.Lithospheric deformation and crustal movement in Tibet.In:Chinese Geophysical Society eds.Annual of the Chinese GeophysicalSociety 1990.Beijing:Seismological Press,1990.121
[115]高锐,成湘洲,丁谦.格尔木-额济纳旗地学断面地球动力学模型初探.地球物理学报,1995,38(Suppl.):3~14Gao R,Cheng X Z,Ding Q.Preliminary geodynamic model ofGolmud_Ejin Qi geoscience transect.Chinese J.Geophys.(ActaGeophysica Sinica)(in Chinese),1995,38(Suppl.):3~14
[116]Bird P.Initiation of intracontinental subduction in the Himalaya.J.Geophys.Res.,1978,83:1975~1987
[117]Kosarev G,Kind R,Sobolev S V,et al.Seismic evidence for adetached Indian lithospheric mantle beneath Tibet.Science,1999,283:1306~1309
[118]Tilmann F,Ni J,INDEPTH Seismic Team.Seismic imaging of thedown_welling Indian lithosphere beneath central Tibet.Science,2003,300:1424~1427
[119]吴庆举,曾融生,赵文津.喜马拉雅-青藏高原的上地幔倾斜构造与陆-陆碰撞过程.中国科学(D辑),2004,34(10):919~925Wu Q J,Zeng R S,Zhao W J.Dipping structure of upper mantleand continent_continent collision in Himalayas_Tibet Plateau.Sciencein China(Series D)(in Chinese),2004,34(10):919~925
[120]曾融生,丁志峰,吴庆举等.喜马拉雅及南藏的地壳俯冲带—地震学证据.地球物理学报,2000,43(6):780~797Zeng R S,Ding Z F,Wu Q J,et al.Seismological evidence for themultiple income crustal subductions in Himalayas and southern Tibet.Chinese J.Geophys.(in Chinese),2000,43(6):780~797
[121]曾融生,吴庆举,丁志峰等.印度-欧亚碰撞与洋-陆碰撞的差异.地震学报,2006(待刊)Zeng R S,Wu Q J,Ding Z F,et al.Differences of India_Eurasianplate collision and ocean_continent collision.Acta Seismologica Sinica(in Chinese),2006(in press)
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