引文
[1]Yin A,Harrison T M.Geologic evolution of the Hi malayan-Tibetan orogen.Annu.Earth Planet Sci.,2000,28:211~280
[2]Hirn A,Nercessian A,Sapin M,et al.Lhasa block andbordering sutures,a continuation of a 500 km Moho traversethrough Tibet.Nature,1984,307(5946):25~27
[3]Zhao W,Nelson K D,Indepth Team.Deep seismic reflectionevidence for continental underthrusting beneath Tibet.Nature,1993,366:557~559
[4]Hirn A,Lepine J C,Jobert G,et al.Crustal structur andvariability of the Hi malayan border of Tibet.Nature,1984,307(5946):23~25
[5]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 andvelocity distribution beneath Selin Co-Peng Co-Na Qu-SuoCounty region in the Northern Xizang plateau.Chinese J.Geophys.(Acta Geophysica Sinica)(in Chinese),1985,28(Suppl.Ⅰ):28~42
[6]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 velocitystructure and eastward escaping of crustal material in thesouthern Tibet-An example revealed by wide-angle seismicprofile between Peikucuo and Pumoyongcuo.Sciencein China(Ser.D)(in Chinese),2002,32(10):793~798
[7]Pelkum S,Monsalve G,Sheehan A,et al.I maging theIndian subcontinent beneath the Hi malayas.Nature,2005,435:1222~1225
[8]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 crustand undulation of discontinuity in Xizang(Tibet)plateau.Chinese J.Geophys.(Acta Geophysica Sinica)(in Chinese),1985,28(Suppl.Ⅰ):16~27
[9]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,1990,1:25~37Huang L Y,Lu D Y,Li X P,et al.Deep seismic sounding ofSelincuo Lake-Pengcuo Lake-Yangamdo in the north of theXizang(Tibet).In:Geophysical Memoir on Xizang-QinghaiPlateau(in Chinese).Beijing:Geological Publishing House,1990,1:25~37
[10]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-Wcrustal structureunder the northern Tibet and“down-bowing”Moho underthe northern Tibet revealed by wide-angle seismic profile.Sciencein China(Series D)(in Chinese),2001,31(11):881~888
[11]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 QJ.Areviewon the lithosphericstructures in Tibetan plateau and constraints for dynamics.Chinese J.Geophys.(Acta Geophysica Sinica)(in Chinese),1994,37(Suppl.):99~116
[12]Ross A,Brown L,Passakorn P,et al.Deep reflectionsurveying in central Tibet:lower-crustal layering and crustalflow.Geophysical Journal International,2004,156:115~128
[13]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 crustand upper mantle pattern and velocity distributionalcharacteristics in the Northern Hi malayan mountain region.Chinese J.Geophys.(Acta Geophysica Sinica)(in Chinese),1983,26(6):525~540
[14]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 crustand undulation of discontinuity in Xizang(Tibet)plateau.Chinese J.Geophys.(Acta Geophysica Sinica)(in Chinese),1985,28(Suppl.Ⅰ):16~27
[15]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 crustand velocity distributional characteristics in the unit betweenHi malaya mountain and the Yaluzangbo river.In:Geophysical Memoir on Xizang-Qinghai Plateau(in Chinese).China Academy of Geology Science eds.Beijing:GeologicalPublishing House,1990.1~14
[16]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 Tibetanplateau.Chinese Science Bulletin(in Chinese),1997,42(12):1309~1312
[17]Zhang Z J,Wang G J.P-wave structure along 1100kmlongwide angle seismic profilein the eastern Tibet.AGU,Japan.2002
[18]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.Areviewon the Moho discontinuitybeneath the Tibetan plateau.Geological Review(inChinese),2004,50(6):598~612
[19]Zhao L S,Sen M K,Stoffa P,et al.Application of very fastsi mulated annealing to the determination of the crustal structurebeneath Tibet.Geophys.J.Int.,1996,125:355~370
[20]周莹.接收台站精细地壳结构的波形反演[硕士论文].北京:中国科学院地球物理研究所,1999Zhou Y.Waveforminverse for fine crustal structure beneathseismicstation[M.A.thesis](in Chinese).Beijing:Instituteof Geophysics,Chinese Academy of Sciences.1999
[21]王卫民,姚振兴.用转换函数方法研究台湾地区三维深部结构.地球物理学报,2003,46(5),628~632Wang W M,Yao Z X.A study on the 3D crustal structurebeneath Tai wan by teleseismic transform function method.Chinese J.Geophys.(in Chinese),2003,46(5):628~632
[22]高星,王卫民,姚振兴.中国及邻近地区地壳结构.地球物理学报,2005,48(3):591~601Gao X,Wang W M,Yao Z X.Crustal structure of Chinamainland and its adjacent regions.Chinese J.Geophys.(inChinese),2005,48(3):591~601
[23]高星,郭志,王卫民等.用转换函数方法研究腾冲—临沧地区地壳结构.地球物理学报,2008,51(2):451~459Gao X,Guo Z,Wang W M,et al.Crust structure beeathTenchong-Lincang,region,Yunnan province revealed byTransform function.Chinese J.Geophys.(in Chinese),2008,51(2):451~459
[24]Zhao W,Nelson K D,Indepth Team.Deep seismic reflectionevidence for continental underthrusting beneath Tibet.Nature,1993,366:557~559