引文
[1]张培震,甘卫军,沈正康等.中国大陆现今构造作用的地块运动和连续变形耦合模型.地质学报,2005,79(6):748-756.Zhang P Z,Gan W J,Shen Z K,et al.A coupling model ofrigid-block movement and continuous deformation:patterns of the present-day deformation of China′s continent and its vicinity.Acta Geological Sinica(in Chinese),2005,79(6):748-756.
[2]Yin A,Harrison T M.Geologic evolution of the Himalayan-Tibetan orogen.Annual Review of Earth and Planetary Sciences,2000,28(1):211-280.
[3]高原,滕吉文.中国大陆地壳与上地幔地震各向异性研究.地球物理学进展,2005,20(1):180-185.Gao Y,Teng J W.Studies on seismic anisotropy in the crust and mantle on Chinese mainland.ProgressinGeophysics(in Chinese),2005,20(1):180-185.
[4]Crampin S,Peacock S.A review of shear-wave splitting in the compliant crack critical anisotropic Earth.Wave Motion,2005,41(1):59-77.
[5]Meissner R,Mooney W D,Artemieva I.Seismic anisotropy and mantle creep in young orogens.Geophysical Journal International,2002,149(1):1-14.
[6]Silver P G,Chan W W.Shear Wave Splitting and Sub continental Mantle Deformation.J.Geophys.Res,1991,96(10):16429-16454.
[7]Gao S S,Liu K H,Abdelsalam M G.Seismic anisotropy beneath the Afar Depression and adjacent areas:Implications for mantle flow.J.Geophys.Res,2010,115:B12330.
[8]郑斯华,高原.中国大陆岩石层的方位各向异性.地震学报,1994,16(2):131-140.Zheng S H,Gao Y.Azimuthal anisotropy beneath lithosphere in the continent of China.Acta Seimologica Sinica,1994,16(2):131-140.
[9]Mcnamara D E,Owens T J,Silver P G,et al.Shear wave anisotropy beneath the Tibetan Plateau.Journal of Geophysical Research,1994,99(B7):13613-13655.
[10]Holt W E,Chamot Rooke N,Le Pichon X,et al.Velocity field in Asia inferred from Quarternary fault slip rates and Global Positioning System observations.Journal of Geophysical Research,2000,105(B8):19-185.
[11]Shapiro N M,Ritzwoller M H,Molnar P,et al.Thinning and flow of Tibetan crust constrained by seismic anisotropy.Science,2004,305(5681):233-236.
[12]Sherrington H F,Zandt G,Frederiksen A.Crustal fabric in the Tibetan Plateau based on waveform inversions for seismic anisotropy parameters.Journal of Geophysical Research,2004,109(B2):B2312.
[13]Ozacar A A,Zandt G.Crustal seismic anisotropy in central Tibet:Implications for deformational style and flow in the crust.Geophysical Research Letters,2004,31(23):L23601.
[14]Hirn A,Jiang M,Sapin M,et al.Seismic anisotropy as an indicator of mantle flow beneath the Himalayas and Tibet.Nature,1995,375(6532):571-574.
[15]Flesch L M,Holt W E,Silver P G,et al.Constraining the extent of crust-mantle coupling in central Asia using GPS,geologic,and shear wave splitting data.Earth and PlanetaryScience Letters,2005,238(1-2):248-268.
[16]崔笃信,王庆良,胡亚轩等.青藏高原东北缘岩石圈变形及其机理.地球物理学报,2009,52(6):1490-1499.Cui D X,Wang Q L,Hu Y X,et al.Lithsophere deformation and deformation mechanism in northeastern margin of Qinghai Tibet Plateau.Chinese J.Geophys,(in Chinese),2009,52(6):1490-1499.
[17]常利军,王椿镛,丁志峰等.青藏高原东北缘上地幔各向异性研究.地球物理学报,2008,51(02):431-438.Chang L J,Wang C Y,Ding Z F,et al.Seismic anisotropy of upper mantle in the northern margin of the Tibetan Plateau.Chinese J.Geophys.(in Chinese),2008,51(02):431-438.
[18]张辉,高原,石玉涛等.基于地壳介质各向异性分析青藏高原东北缘构造应力特征.地球物理学报,2012,55(1):95-104.Zhang H,Gao Y,Shi Y T,et al.Tectonic stress analysis based on the crustal seismic anisotropy in the northeastern margin of Tibetan plateau.Chinese J.Geophys.,(in Chinese).2012,55(1):95-104.
[19]郑秀芬,欧阳飚,张东宁等.“国家数字测震台网数据备份中心”技术系统建设及其对汶川大地震研究的数据支撑.地球物理学报,2009,52(5):1412-1417.Zheng X F,Ouyang B,Zhang D N,et al.The role played and opportunities provided by IGP DMC of China National Seismic Network in Wenchuan.Bull.Seismol.Soc.Am.,2010,100(5B):2866-2872.
[20]Gao S S,Liu K H.Significant seismic anisotropy beneath the southern Lhasa Terrane,Tibetan Plateau.Geochem.Geophys.Geosyst,2009,10(2):1-19.
[21]Liu K H,Gao S S,Gao Y,et al.Shear wave splitting and mantle flow associated with the deflected Pacific slab beneath northeast Asia.J.Geophys.Res.,2008,113(B1):1-15.
[22]Zhang Z J,Li Y K,Lu D Y,et al.Velocity and anisotropy structure of the crust in the Dabieshan organic belt from wide-angle seismic data.Physics of the Earth and Planetary Interiors,2000,122(1-2):115-131.
[23]Zhang Z J,Teng J W,Badal J,et al.Construction of regional and local seismic anisotropic structures from wide-angle seismic data:crustal deformation in the southeast of China.Journal of Seismology,2009,3(3):16-20.
[24]石玉涛,高原,吴晶.剪切波分裂分析系统SAM(2007)———区域地震台网资料应用实例.中国地震,2008,24(4):354-361.Shi Y T,Gao Y,Wu J,et al.Systematic analysis method of shear-wave splitting SAM(2007):examples of application in the regional seismograph networks.Earthquake Reaearch in China(in Chinese),2008,24(4):354-361.
[25]高原,石玉涛,梁维等.剪切波分裂分析系统SAM(2007)———软件系统.中国地震,2008,24(4):345-353.Gao Y,Shi Y T,Liang W,et al.Systematic analysis method of shear-wave splitting SAM(2007):software system.Earthquake Research in China(in Chinese),2008,24(4):345-353.
[26]Crampin S.Seismic-wave propagation through a cracked solid:polarization as a possible dilatancy diagnostic.Geophysical Journal of the Royal Astronomical Society,1978,53(3):467-496.
[27]高原,吴晶,易桂喜等.从壳幔地震各向异性初探华北地区壳幔耦合关系.科学通报,2010,55(29):2837-2843.Gao Y,Wu J,Yi G X,et al.Crust-mantle coupling in North China:Preliminary analysis from seismic anisotropy.Chinese Sci Bull,2010,55:3599-3605.
[28]Gan W,Zhang P,Shen Z K,et al.Present-day crustal motion within the Tibetan Plateau inferred from GPS measurements.J.Geophys.Res.,2007,112:B8416.
[29]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土地幔特征.地球学报,2001,22(2):111-116.Jiang M,Xu Z Q,Hirn A,et al.Teleseismic anisotropy and corresponding features of the upper mantle in Tibet plateau and its neighboring areas.Acta Geoscientia Sinica(in Chinese),2001,22(2):111-116.
[30]常利军,王椿镛,丁志峰.鄂尔多斯块体及周缘上地幔各向异性研究.中国科学(D辑:地球科学),2011,41(5):686-699.Chang L J,Wang C Y,Ding Z F.Upper mantle anisotropy in the Ordos Block and its margins.Sci China Earth Sci.,2011,54:888-900.
[31]李永华,吴庆举,冯强强等.青海地区S波分裂研究.地球物理学报,2010,53(6):1374-1383.Li Y H,Wu Q J,Feng Q Q,et al.Seismic anisotropy beneath Qinghai province revealed by shear wave splitting.Chinese J.Geophys.,(in Chinese).2010,53(6):1374-1383.
[32]Li Y H,Wu Q J,Jiang L J,et al.Complex seismic anisotropic structure beneath the central Tien Shan revealed by shear wave splitting analyses.Geophysical Journal International,2010,181(3):1678-1686.
[33]胡亚轩,崔笃信,季灵运等.鄂尔多斯块体及其周缘上地幔各向异性分析研究.地球物理学报,2011,54(6):1549-1558.Hu Y X,Cui D X,Ji L Y,et al.Seismic anisotropy of upper mantle in Ordos block and adjacent regions.Chinese J.Geophys.(in Chinese),2011,54(6):1549-1558.
[34]Li S,Mooney W D,Fan J.Crustal structure of mainland China from deep seismic sounding data.Tectonophysics,2006,420(1-2):239-252.
[35]An M J,Shi Y.Lithospheric thickness of the Chinese continent.Physics of the Earth and Planetary Interiors,2006,159(3-4):257-266.
[36]徐果明,姚华建,朱良保等.中国西部及其邻域地壳上地幔横波速度结构.地球物理学报,2007,50(1):193-208.Xu G M,Yao H J,Zhu L B,et al.Shear wave velocity of the crust and upper mantle in western China and its adjacent area.Chinese J.Geophys.,(in Chinese),2007,50(1):193-208.
[37]Vinnik L P,Makeyeva L I,Milev A,et al.Global patterns of azimuthal anisotropy and deformations in the continental mantle.Geophysical Journal International,1992,111(3):433-447.
[38]Wang C Y,Flesch L M,Silver P G,et al.Evidence for mechanically coupled lithosphere in central Asia and resulting implications.Geology,2008,36(5):363-366.
[39]常利军,王椿镛,丁志峰.云南地区SKS波分裂研究.地球物理学报,2006,49(1):197-204.Chang L J,Wang C Y,Ding Z F.A study of SKS splitting beneath the Yunnan region.Chinese J.Geophys.,(in Chinese),2006,49(1):197-204.
[40]罗艳,黄忠贤,彭艳菊等.中国大陆及邻区SKS波分裂研究.地球物理学报,2004,47(5):812-821.Luo Y,Huang Z X,Peng Y J,et al.A study on SKS wave splitting beneath the China mainland and adjacent regions.Chinese J.Geophys.,(in Chinese).2004,47(5):812-821.
[41]Ding G,Chen J,Tian Q,et al.Active faults and magnitudes of left-lateral displacement along the northern margin of the Tibetan Plateau.Tectonophysics,2004,380(3-4):243-260.
[42]Yin A,Rumelhart P E,Butler R,et al.Tectonic history of the Altyn Tagh fault system in northern Tibet inferred from Cenozoic sedimentation.Geological Society of America Bulletin,2002,114(10):1257-1295.
[43]Matte P,Tapponnier P,Arnaud N,et al.Tectonics of Western Tibet between the Tarim and the Indus.Earth and Planetary Science Letters,1996,142(3-4):311-330.
[44]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):341-350.Shi D N,Jiang M,Ma K Y,et al.Crust and upper mantle tomographic structure across the altyn fault zone using teleseismic P-waves.Chinese J.Geophys.,(in Chinese),1999,42(3):341-350.
[45]许志琴,杨经绥,姜枚等.大陆俯冲作用及青藏高原周缘造山带的崛起.地学前缘,1999,3(6):139-151.Xu Z Q,Yang J S,Jiang M,et al.Continental subduction and uplifting of the organic belts at the margin of the Qinghai-Tibet plateau.Earth Science Frontiers(in Chinese),1999,3(6):139-151.
[46]田勤俭,申旭辉,冯希杰等.渭河盆地断层活动反映的第四纪构造事件初步研究.地震地质,2003,25(1):146-154.Tian Q J,Shen X H,Feng X J,et al.Primary study on quaternary tectonic event based on variation of fault activity in Weihe Basin.Seismology and Geology(in Chinese),2003,25(1):146-154.
[47]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):790-797.Guo B,Liu Q Y,Chen J H,et al.Seismic tomographic imaging of the crust and upper mantle beneath the Northeastern edge of the Qinghai-Xizang plateau and the Ordos area.Chinese J.Geophys.(in Chinese),2004,47(5):790-797.
[48]陈九辉,刘启元,李顺成等.青藏高原东北缘—鄂尔多斯地块地壳上地幔S波速度结构.地球物理学报,2005,48(2):333-342.Chen J H,Liu Q Y,Li S C,et al.Crust and upper mantle S-wave velocity structure across Northeastern Tibetan Plateau and Ordos block.Chinese J.Geophys.,(in Chinese).2005,48(2):333-342.
[49]Lithgow B C,Richards M A.The dynamics of Cenozoic and Mesozoic plate motions.Reviews of Geophysics.,1998,36(1):27-78.
[50]Ricard Y,Richards M,Lithgow Bertelloni C,et al.A geodynamic model of mantle density heterogeneity.Journal of Geophysical Research.,1993,98(B12):21821-21895.
[51]Silver P G.Seismic anisotropy beneath the continents:probing the depths of geology.Annual Review of Earth and Planetary Sciences,1996,24(1):385-432.
[52]王椿镛,吴建平,楼海等.青藏高原东部壳幔速度结构和地幔变形场的研究.地学前缘,2006,13(5):349-359.Wang C Y,Wu J P,Lou H,et al.Study of crustal and upper mantle′s structure and mantle deformation field beneath the eastern Tibetan plateau.Earth Science Frontiers,2006,13(5):349-359.
[53]Gripp A E,Gordon R G.Young tracks of hotspots and current plate velocities.Geophysical Journal International,2002,150(2):321-361.