引文
[1]England P,Houseman G.Extension during continentalconvergence,with application to the Tibetan plateau.J.Geophys.Res.,1989,94(B12):17561-17579.
[2]Tapponnier P,Xu Z Q,Francoise R,et al.Oblique stepwiserise and growth of the Tibet plateau.Science,2001,294(5547):1671-1677,doi:10.1126/science.105978.
[3]Meyer B,Tapponnier P,Bourjot L,et al.Crustal thickeningin Gansu-Qinghai,lithospheric mantle subduction,andoblique,strike-slip controlled growth of the Tibet plateau.Geophys.J.Int.,1998,135(1):1-47.
[4]Yue Y J,Liou J G.Two-stage evolution model for the AltynTagh fault,China.Geology,1999,27(3):227-230,doi:10.1030/0091-7613.
[5]Fu B H,Awata Y.Displacement and timing of left-lateralfaulting in the Kunlun Fault Zone,northern Tibet,inferredfrom geologic and geomorphic features.J.Asian Earth Sci.,2007,29(2-3):253-265.
[6]Zheng D W,Zhang P Z,Wan J L,et al.Rapid exhumationat~8 Ma on the Liupan Shan thrust fault from apatitefission-track thermochronology:Implications for growth ofthe northeastern Tibetan Plateau margin.Earth Planet.Sci.Lett.,2006,248(1-2):198-208,doi:10.1016/j.epsl.2006.05.023.
[7]Li C Y,Zhang P Z,Yin J H,et al.Late Quaternary left-lateral slip rate of the Haiyuan fault,northeastern margin ofthe Tibetan Plateau.Tectonics,2009,28(5):TC5010,doi:10.1029/2008TC002302.
[8]Zheng D W,Clark M K,Zhang P Z,et al.Erosion,faultinitiation and topographic growth of the North Qilian Shan(Northern Tibetan Plateau).Geosphere,2010,6(6):937-941,doi:10.1130/GES00523.1.
[9]Wittlinger G,Masson F,Poupinet G,et al.Seismictomography of northern Tibet and Kunlun:Evidence forcrustal blocks and mantle velocity contrasts.Earth Planet.Sci.Lett.,1995,139(1-2):263-279.
[10]丁志峰,何正勤,吴建平等.青藏高原地震波三维速度结构的研究.中国地震,2001,17(2):202-209.Ding Z F,He Z Q,Wu J P,et al.Research on the 3-Dseismic velocity structures in Qinghai-Xizang plateau.EarthquakeResearch in China(in Chinese),2001,17(2):202-209.
[11]Huang Z X,Su W,Peng Y J,et al.Rayleigh wavetomography of China and adjacent regions.J.Geophys.Res.,2003,108(B2):2073,doi:10.1029/2001JB001696.
[12]Huang J L,Zhao D P.High-resolution mantle tomography ofChina and surrounding regions.J.Geophys.Res.,2006,111(B9):B09305,doi:10.1029/2005JB004066.
[13]Chen Y,Badal J,Hu J F.Love and Rayleigh wavetomography of the Qinghai-Tibet Plateau and surroundingareas.Pure Appl.Geophys.,2010,167(10):1171-1203.
[14]Kind R,Yuan X,Saul J,et al.Seismic images of crust andupper mantle beneath Tibet:Evidence for Eurasia platesubduction.Science,2002,298(5596):1219-1221.
[15]Wittlinger G,Farra V,Vergen J.Lithospheric and uppermantle stratifications beneath Tibet:New insight from Spconversions.Geophys.Res.Lett.,2004,31:L19615,doi:10.1029/2004GL020955.
[16]Zhao J,Yuan X,Liu H,et al.The boundary between theIndian and Asian tectonic plates below Tibet.Proc.Natl.Acad.Sci.,2010,107:11229-11233.
[17]Zhao W J,Kumar P,Mechie J,et al.Tibetan plateoverriding the Asian plate in central and northern Tibet.Nature Geoscience,2011,4:870-873,doi:10.1038/NGEO1309.
[18]高锐,王海燕,王成善等.青藏高原东北缘岩石圈缩短变形——深地震反射剖面再处理提供的证据.地球学报,2011,32(5):513-520.Gao R,Wang H Y,Wang C S,et al.Lithosphericdeformation shortening of the northeastern Tibetan plateau:Evidence from reprocessing of deep seismic reflection data.Acta Geoscientica Sinica(in Chinese),2011,32(5):513-520.
[19]Tian X B,Zhang Z J.Crustal thickness and Vp/Vsratiosfrom the northeastern Tibetan Plateau:Evidence of internalcrustal deformation.Gondwana Research,2012,submitted.
[20]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(2):431-438.Chang L J,Wang C Y,Ding Z F,et al.Seismic anisotropy ofupper mantle in the northeastern margin of the Tibetanplateau.Chinese J.Geophys.(in Chinese),2008,51(2):431-438.
[21]王琼,高原,石玉涛等.青藏高原东北缘上地幔各向异性.地球物理学报,2013,待刊.Wang Q,Gao Y,Shi Y T,et al.Seismic anisotropy in theuppermost mantle beneath the northeastern margin ofQinghai-Tibet plateau.Chinese J.Geophys.(in Chinese),2013,in press.
[22]Kumar P,Yuang X H,Kind R,et al.Imaging the collidingIndian and Asian lithospheric plates beneath Tibet.J.Geophys.Res.,2006,111(B6):B06308,doi:10.1029/2005JB003930.
[23]Kumar P,Yuan X H,Kumar M R,et al.The rapid drift ofthe Indian tectonic plate.Nature,2007,449(7164):894-897,doi:10.1038/nature06214.
[24]Wilson D C,Angus D A,Ni J F,et al.Constraints on theinterpretation of S-to-P receiver functions.Geophys.J.Int.,2006,165(3):969-980.
[25]Yuan X H,Kind R,Li X Q,et al.The S receiver functions:synthetics and data example.Geophys.J.Int.,2006,165(2):555-564.
[26]Tian X B,Zhang J L,Si S K,et al.SKS splittingmeasurements with horizontal component misalignment.Geophys.J.Int.,2011,185(1):329-340,doi:10.1111/j.1365-246X.2011.04936.x.
[27]Kiefer J."Conditional Confidence Statements and ConfidenceEstimators(with discussion)".Journal of the AmericanStatistical Association,1977,72:789-827.
[28]Wolfe C J,Silver P G.Seismic anisotropy of oceanic uppermantle:shear wave splitting methodologies and observations.J.Geophys.Res.,1998,103(B1):749-771.
[29]Silver P G,Chan W W.Shear wave splitting andsubcontinental mantle deformation.J.Geophys.Res.,1991,96(B10):16429-16454.
[30]Bowman J R,Ando M.Shear-wave splitting in the upper-mantle wedge above the Tonga subduction zone.Geophys.J.Roy.Astr.Soc.,1987,88(1):25-41.
[31]Vergne J,Wittlinger G,Hui Q,et al.Seismic evidence forstepwise thickening of the crust across the NE Tibetanplateau.Earth Planet.Sci.Lett.,2002,203(1):25-33.
[32]GalvéA,Hirn A,Jiang M,et al.Modes of raisingnortheastern Tibet probed by explosion seismology.Ear.Plan.Sci.Lett.,2002,203(1):35-43.
[33]Li S G,Mooney W D,Fan J C.Crustal structure of mainlandChina from deep seismic sounding data.Tectonophysics,2006,420(1-2):239-252.
[34]Liu M G,Mooney W D,Li S D,et al.Crustal structure ofthe northeastern margin of the Tibetan plateau from theSongpan-Ganzi terrane to the Ordos basin.Tectonophysics,2006,420(1-2):253-266.
[35]高锐,王海燕,马永生等.松潘地块若尔盖盆地与西秦岭造山带岩石圈尺度的构造关系——深地震反射剖面探测成果.地球学报,2006,27(5):411-418.Gao R,Wang H Y,Ma Y S,et al.Tectonic relationshipsbetween the Zoigêbasin of the Song-Pan block and the westQinling orogen at lithosphere scale:Results of deep seismicreflection profiling.Acta Geoscientica Sinica(in Chinese),2006,27(5):411-418.
[36]高锐,熊小松,李秋生等.由地震探测揭示的青藏高原莫霍面深度.地球学报,2009,30(6):761-773.Gao R,Xiong X S,Li Q S,et al.The Moho depth ofQinghai-Tibet plateau revealed by seismic detection.ActaGeoscientia Sinica(in Chinese),2009,30(6):761-773.
[37]王海燕,高锐,马永生等.若尔盖与西秦岭地震反射岩石圈结构和盆山耦合.地球物理学报,2007,50(2):472-481.Wang H Y,Gao R,Ma Y S,et al.Basin-range coupling andlithosphere structure between the Zoigêand the west Qinling.ChineseJ.Geophys.(in Chinese),2007,50(2):472-481.
[38]滕吉文,白登海,杨辉等.2008年汶川Ms8.0地震发生的深层过程和动力学响应.地球物理学报,2008,51(5):1385-1402.Teng J W,Bai D H,Yang H,et al.Deep processes anddynamic responses associated with the Wenchuan Ms8.0earthquake of 2008.Chinese J.Geophys.(in Chinese),2008,51(5):1385-1402.
[39]Zhang Z J,Klemperer S,Bai Z M,et al.Crustal structure ofthe Paleozoic Kunlun orogeny from an active-source seismicprofile between Moba and Guide in East Tibet,China.Gond.Res.,2010,19(4):994-1007,doi:10.1016/j.gr.2010.09.008.
[40]Kennett B L N,Engdahl E R.Traveltimes for globalearthquake location and phase identification.Geophys.J.Int.,1991,105(2):429-465.
[41]Zhao G C,Sun M,Wilde S A,et al.Late Archean toPaleoproterozoic evolution of the North China Craton:Keyissues revisited.Precambrian Res.,2005,136(2):177-202.
[42]Tian Y,Zhao D P,Sun R M,et al.Seismic imaging of thecrust and upper mantle beneath the North China Craton.Physics of the Earth and Planetary Interiors,2009,172(3-4):169-182.
[43]陈凌,危自根,程骋.从华北克拉通中、西部结构的区域差异性探讨克拉通破坏.地学前缘,2010,17(1):212-228.Chen L,Wei Z G,Cheng C.Significant structural variationsin the Central and Western North China craton and itsimplications for the craton destruction.Earth ScienceFrontiers(in Chinese),2010,17(1):212-228.
[44]Tian X B,Teng J W,Zhang H S,et al.Structure of crustand upper mantle beneath the Ordos Block and the YinshanMountains revealed by receiver function analysis.Physics ofthe Earth and Planetary Interiors,2011,184(3-4):186-193.
[45]王萍,王增光.阿拉善活动块体的划分及归宿.地震,1997,17(1):103-112.Wang P,Wang Z G.Division of the Alxa block and itsattribution.Earthquake(in Chinese),1997,17(1):103-112.
[46]马杏垣.中国及邻近海域岩石圈动力学图(1∶400万).北京:地质出版社,1986.Ma X Y.Lithospheric Dynamics Map of China and AdjacentAreas(in Chinese).Beijing:Geological Publishing House,1986
[47]葛肖虹,刘俊来.被肢解的“西域克拉通”.岩石学报,2000,16(1):59-66.Ge X H,Liu J L.Broken“Western China Craton”.ActaPetrologica Sinica(in Chinese),2000,16(1):59-66.
[48]葛肖虹,任收麦,刘永江等.中国西部的大陆构造格架.岩石学报,2001,22(5):1-5.Ge X H,Ren S M,Liu Y J,et al.Continental tectonicframework of west China.Acta Petrologica Sinica(inChinese),2001,22(5):1-5.
[49]葛肖虹,马文璞,刘俊来等.对中国大陆构造格架的讨论.中国地质,2009,36(5):949-965.Ge X H,Ma W P,Liu J L,et al.A discussion on thetectonic framework of Chinese mainland.Geology in China(in Chinese),2009,36(5):949-965.
[50]Kirby E,Harkins N,Wang E Q,et al.Slip rate gradientsalong the eastern Kunlun fault.Tectonics,2007,26(2),doi:10.1029/2006TC002033.
[51]Gan W J,Zhang P Z,Shen Z K,et al.Present-day crustalmotion within the Tibetan Plateau inferred from GPSmeasurements.J.Geophys.Res.,2007,112(B8),doi:10.1029/2005JB004120.
[52]高锐,李朋武,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:地球科学),2001,31(增刊):66-71.Gao R,Li P W,Li Q S,et al.Deep process of the collisionand deformation on the northern margin of the TibetanPlateau:Revelation from investigation of the deep seismicprofiles.Science in China(Series D),2001,44(S1):71-78.
[53]宋仲和,安昌强,陈国英等.中国西部三维速度结构及其各向异性.地球物理学报,1991,34(6):694-707.Song Z H,An C Q,Chen G Y,et al.Study on 3Dvelocitystructure and anisotropy beneath the west China from theLove wave dispersion.Acta Geophysica Sinica(Chinese J.Geophys.)(in Chinese),1991,34(6):694-707.
[54]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):46-57.Zhu R X,Hu X Y.Study on the resistivity structure of thelithosphere along the Golmud-Ejin Qi geoscience transect.Acta Geophysica Sinica(Chinese J.Geophys.)(in Chinese),1995,38(S2),46-57.
[55]Meng Q R,Hu J M,Yang F Z.Timing and magnitude ofdisplacement on the Altyn Tagh fault:constraints fromstratigraphic correlation of adjoining Tarim and Qaidambasins,NW China.Terra Nova,2001,13(2):86-91,doi:10.1046/j.1365-3121.2001.00320.x.
[56]王良书,李成,杨春.塔里木盆地岩石层热结构特征.地球物理学报,1996,39(6):794-803.Wang L S,Li C,Yang C.The lithospheric thermal structurebeneath Tarim basin,Western China.Acta GeophysicaSinica(Chinese J.Geophys.)(in Chinese),1996,39(6):794-803.
[57]Xu Y,Liu F T,Liu J H,et al.Crust and upper mantlestructure beneath western China from P wave travel timetomography.J.Geophys.Res.,2002,107(B10):ESE4-1-ESE4-15,doi:1029/2001JB000402.
[58]Basu A R,Wang J W,Huang W K,et al.Major element,REE,and Pb,Nd and Sr isotopic geochemistry of Cenozoicvolcanic rocks of eastern China:Implications for their originfrom suboceanic-type mantle reservoirs.Earth Planet.Sci.Lett.,1991,105(1-3):149-169.
[59]Flower M,Tamaki K,Hoang N.Mantle extrusion:A modelfor dispersed volcanism and DUPAL-like asthenosphere inEast Asia and the western Pacific.∥Flower M F J ed.Mantle Dynamic and Plate Interaction in East Asia.Washington:AGU.Geodyn.Ser.,1998,27:67-88.
[60]Liu M,Cui X,Liu,F.Cenozoic rifting and volcanism ineastern China:A mantle dynamic link to the indo-AsiancollisionTectonophysics,2004,393(1-4):29-42.
[61]Brandon C,Romanowicz B.A‘‘no-lid’’zone in the centralChang-Thang platform of Tibet:Evidence from pure pathphase velocity measurements of long period Rayleigh waves.J.Geophys.Res.,1986,91(B6):6547-6564.
[62]McNamara D E,Owens T J,Walter W R.Observations ofregional phase propagation across the Tibetan Plateau.J.Geophys.Res.,1995,100(B11):22215-22229.
[63]Owens T J,Zandt G.Implications of crustal propertyvariations for models of Tibetan plateau evolution.Nature,1997,387(6628):37-43.
[64]Rodgers A J,Schwartz S Y.Lithospheric structure of theQiangtang Terrane,northern Tibetan Plateau,from completeregional waveform modeling:Evidence for partial melt.J.Geophys.Res.,1998,103(B4):7137-7152.
[65]Su B X,Zhang H F,Sakyi P A,et al.Compositionallystratified lithosphere and carbonatite metasomatism recordedin mantle xenoliths from the Western Qinling(CentralChina).Lithos.,2010,116(1-2):111-128.
[66]An M J,Shi Y L.Lithospheric thickness of the Chinesecontinent.Phys.Earth Planet.Inter.,2006,159(3-4):257-266.
[67]Hu J F,Xu X Q,Yang H Y,et al.S receiver functionanalysis of the crustal and lithospheric structures beneatheastern Tibet.Ear.Plan.Sci.Lett.,2011,306(1-2):77-85,doi:10.1016/j.epsl.2011.03.034.
[68]Zhang Z J,Yuan X H,Chen Y,et al.Seismic signature ofthe collision between the east Tibetan escape flow and theSichuan Basin.Earth and Planet.Sci.Let.,2010,292(3-4):254-264.
[69]McNamara D E,Owens T J,Silver P G.Shear waveanisotropy beneath the Tibetan plateau.J.Geophys.Res.,1994,99(B7):13655-13665.
[70]Wang C Y,Flesch L M,Silver P G,et al.Evidence formechanically coupled lithosphere in central Asia and resultingimplications.Geology,2008,36(5):363-366,doi:10.1130/G24450A.
[71]Silver P G,Chan W W.Implications for continental structureand evolution from seismic anisotropy.Nature,1988,335(6185):34-39.
[72]Christensen N I.The magnitude,symmetry and origin ofupper mantle anisotropy based on fabric analyses of ultramafictectonites.Geophys.J.R.Astron.Soc.,1984,76(1):89-111.
[73]Nicolas A,Christensen N I.Formation of anisotropy in uppermantle peridotites-a review.∥Fuchs K,Froideveaux C,eds.Composition,Structure and Dynamics of the Lithosphere-Asthenosphere System.Washington:American GeophysicalUnion.Geodyn.Ser.,1987,16:111-123.
[74]Zhang S Q,Karato S I.Lattice preferred orientation ofolivine aggregates deformed in simple shear.Nature,1995,415(6534):777-780.
[75]Long M D,Silver P G.Shear wave splitting and mantleanisotropy:measurements,interpretations,and new directions.Surv.Geophys.,2009,30(4-5):407-461.
[76]滕吉文.强烈地震孕育与发生的地点、时间及强度预测的思考与探讨.地球物理学报,2010,53(8):1749-1766.Teng J W.Ponder and research on the genesis and occurrenceof strong earthquakes and the prediction of their place,timeand intensity.Chinese J.Geophys.(in Chinese),2010,53(8):1749-1766.
[77]孙若昧,刘福田,刘建华.四川地区的地震层析成像.地球物理学报,1991,34(6):708-716.Sun R M,Liu F T,Liu J H.Seismic tomography of Sichuan.Acta Geophysica Sinica(Chinese J.Geophys.)(in Chinese),1991,34(6):708-716.
[78]张雪梅,孙若昧,滕吉文.青藏高原及其邻区地壳、岩石圈和软流层厚度研究.科学通报,2007,52(3):332-338.Zhang X M,Sun R M,Teng J W.Study on crustal,lithospheric and asthenospheric thickness beneath theQinghai-Tibet plateau and its adjacent areas.Chinese ScienceBulletin,2007,52(6):797-804.
[79]雷建设,赵大鹏,苏金蓉等.龙门山断裂带地壳精细结构与汶川地震发震机理.地球物理学报,2009,52(2):339-345.Lei J S,Zhao D P,Su J R,et al.Fine seismic structureunder the Longmenshan fault zone and the mechanism of thelarge Wenchuan earthquake.Chinese J.Geophys.(in Chinese),2009,52(2):339-345.
[80]Clark M K,Royden L H.Topographic ooze:Building theeastern margin of Tibet by lower crustal flow.Geology,2000,28(8):703-706.
[81]Cook K L,Royden L H.The role of crustal strengthvariations in shaping orogenic plateaus,with application toTibet.J.Geophys.Res.,2008,113(B8):B08407,doi:10.1029/2007JB005457.
[82]Huang Z C,Xu M J,Wang L S,et al.Shear wave splittingin the southern margin of the Ordos Block,north China.Geophys.Res.Lett.,2008,35(19):l19301,doi:10.1029/2008GL035188.