引文
[1]邓起东,张培震,冉勇康,等.中国活动构造基本特征[J].中国科学(D辑),2002,32(12):1020-1030.Deng Q D,Zhang P Z,Ran Y K,et al.Basic characteristics ofactive tectonics of China[J].Science in China Series D:EarthSciences,2003,46(4):356-372.
[2]张培震,邓起东,张国民,等.中国大陆的强震活动与活动地块[J].中国科学(D辑),2003,33(增刊):12-20.Zhang P Z,Deng Q D,Zhang G M,et al.Active tectonicblocks and strong earthquakes in the continent of China[J].Science in China(Series D),2003,46(Suppl.):13-24.
[3]张岳桥,杨农,施炜,等.青藏高原东缘新构造及其对汶川地震的控制作用[J].地质学报,2008,82(12):1668-1678.Zhang Y Q,Yang N,Shi W,et al.Neotectonics of easternTibet and its control on the Wenchuan earthquake[J].ActaGeologica Sinica(in Chinese),2008,82(12):1668-1678.
[4]张培震.青藏高原东缘川西地区的现今构造变形、应变分配与深部动力过程[J].中国科学(D辑):地球科学,2008,38(9):1041-1056.Zhang P Z.Present structural deformation,strain distributionand the deep dynamic process of eastern edge of Qinghai-Tibetplateau of western Sichuan region[J].Science in China SeriesD-Earth Sciences(in Chinese),2008,38(9):1041-1056.
[5]韦伟,孙若昧,石耀霖.青藏高原东南缘地震层析成像及汶川地震成因探讨[J].中国科学:地球科学,2010,40(7):831-839.Wei W,Sun R,Shi Y L.P-wave tomographic images beneathsoutheastern Tibet:Investigating the mechanism of the 2008Wenchuan earthquake[J].Science China-Earth Sciences,2010,53(9):1252-1259.
[6]许志琴,李海兵,吴忠良.汶川地震和科学钻探[J].地质学报,2008,82(12):1613-1621.Xu Z Q,Li H B,Wu Z L.Wenchuan earthquake and scientificdrilling[J].Acta Geologica Sinica(in Chinese),2008,82(12):1613-1621.
[7]石耀霖,曹建玲.库仑应力计算及应用过程中若干问题的讨论——以汶川地震为例[J].地球物理学报,2010,53(1):102-110.Shi Y L,Cao J L.Some aspects in static stress changecalculation——on case study on Wenchuan earthquake[J].Chinese J.Geophys.(in Chinese),2010,53(1):102-110.
[8]郭启良,王成虎,马洪生,等.汶川MS8.0级大震前后的水压致裂原地应力测量[J].地球物理学报,2009,52(5):1395-1401.Guo Q L,Wang C H,Ma H S,et al.In-site hydro-fracturestress measurement before and after the Wenchuan MS8.0earthquake of China[J].Chinese J.Geophys.(in Chinese),2009,52(5):1395-1401.
[9]Luo G,Liu M.Stress evolution and fault interactions beforeand after the 2008 Great Wenchuan earthquake[J].Tectonophysics,2010,491(1-4):127-140.
[10]Heidbach O,Reinecker J,Tingay M,et al.Plate boundaryforces are not enough:Second-and third-order stress patternshighlighted in the World Stress Map database[J].Tectonics,2007,26,TC6014,doi:10.1029/2007TC002133.
[11]Liu M,Yang Y Q,Shen Z K,et al.Active tectonics andintracontinental earthquakes in China:the kinematics andgeodynamics[C].//Stein S,Mazzotti S,eds.ContinentalIntraplate Earthquakes:Science Hazard and Policy Issues:Geological Society of America Special Paper 425,2007:299-318.
[12]刘峡,马瑾,傅容珊,等.华北地区现今地壳运动动力学初步研究[J].地球物理学报,2010,53(6):1418-1427.Liu X,Ma J,Fu R S,et al.Primary study on the dynamicsof the present-day crustal motion in North China Region[J].Chinese J.Geophys.(in Chinese),2010,53(6):1418-1427.
[13]朱守彪,张培震,石耀霖.华北盆地强震孕育的动力学机制研究[J].地球物理学报,2010,53(6):1409-1417.Zhu S B,Zhang P Z,Shi Y L.A study on the mechanisms ofstrong earthquake occurrence in the North China Basin[J].Chinese J.Geophys.(in Chinese),2010,53(6):1409-1417.
[14]酆少英,高锐,龙长兴,等.银川地堑地壳挤压应力场:深地震反射剖面[J].地球物理学报,2011,54(3):692-697.Feng S Y,Gao R,Long C X,et al.The compressive stressfield of Yinchuan garben:Deep seismic reflection profile[J].Chinese J.Geophys.(in Chinese),2011,54(3):692-697.
[15]Zoback M L.First-and second-order patterns of stress in thelithosphere:the world stress map project[J].J.Geophys.Res.,1992,97(B8):11703-11728.
[16]Flesch L M,Haines A J,Holt W E.Dynamics of the India-Eurasia collision zone[J].J.Geophys.Res.,2001,106(B8):16435-16460.
[17]朱守彪,石耀霖.青藏高原地形扩展力以及下地壳对上地壳的拖曳力的遗传有限单元法反演[J].北京大学学报(自然科学版),2005,41(2):225-234.Zhu S B,Shi Y L.Genetic algorithm-finite element inversionof topographic spreading forces and drag forces of lower crustto upper crust in Tibetan plateau[J].Acta ScientiarumNaturalium Universitatis Pekinensis(in Chinese),2005,41(2):225-234.
[18]谢富仁,祝景忠,梁海庆,等.中国西南地区现代构造应力场基本特征[J].地震学报,1993,15(4):407-417.Xie F R,Zhu J Z,Liang H Q,et al.The present basiccharacter of tectonic stress of the southwest China[J].ActaSeismologica Sinica(in Chinese),1993,15(4):407-417.
[19]柳畅,朱伯靖,石耀霖.粘弹性数值模拟龙门山断裂带应力积累及大震复发周期[J].地质学报,2012,86(1):157-169.Liu C,Zhu B J,Shi Y L.Stress accumulation of theLongmenshan fault and recurrence interval of Wenchuanearthquake based on viscoelasticity simulation[J].ActaGeologica Sinica(in Chinese),2012,86(1):157-169.
[20]熊熊,滕吉文.青藏高原东缘地壳运动与深部过程的研究[J].地球物理学报,2002,45(4):507-515.Xiong X,Teng J W.Study on crustal movement and deepprocess in eastern Qinghai-Xizang plateau[J].Chinese J.Geophys.(in Chinese),2002,45(4):507-515.
[21]马杏垣.中国岩石圈动力学地图集[M].北京:中国地图出版社,1989:1-68.Ma X Y.Dynamics atlas of Chinese lithosphere(in Chinese)[M].Beijing:Sino Maps Press,1989:1-68.
[22]Huang Z W,Su Y,Peng Y J,et al.Rayleigh wave tomographyof China and adjacent regions[J].J.Geophys.Res.,2003,108(B2):2073,doi:10.1029/2001JB001696.
[23]徐锡伟,张培震,闻学泽,等.川西及其邻近地区活动构造基本特征与强震复发模型[J].地震地质,2005,27(3):446-461.Xu X W,Zhang P Z,Wen X Z,et al.Features of activetectonics and recurrence behaviors of strong earthquakes inthe western Sichuan province and its adjacent regions[J].Seismology and Geology(in Chinese),2005,27(3):447-461.
[24]Wen X Z,Ma S L,Xu X W,et al.Historical pattern andbehavior of earthquake ruptures along the eastern boundaryof the Sichuan-Yunnan faulted-block,southwestern China[J].Phys.Earth Planet Int.,2008,168(1-2):16-36.
[25]Shen Z K,LüJ N,Wang M,et al.Contemporary crustaldeformation around the southeast borderland of the TibetanPlateau[J].J.Geophys.Res.,2005,110:B11409,doi:10.1029/2004JB003421.
[26]Molnar P.Continental tectonics in the aftermath of plate tectonics[J].Nature,1988,335(6186):131-137.
[27]Royden L H,Burchfiel B C,King R W,eta l.Surface deformationand lower crustal flow in eastern Tibet[J].Science,1997,276(5313):788-790.
[28]Zhang P Z,Shen Z K,Wang M,et al.Continuous deformationof the Tibetan plateau from global positioning system data[J].Geology,2004,32(9):809-812.
[29]Bai D H,Unsworth M J,Meju M A,et al.Crustal deformationof the eastern Tibetan plateau revealed by magnetotelluricimaging[J].Nature Geoscience,2010,3(5):358-362.
[30]Zhang Z J,Wang Y H,Chen Y,et al.Crustal structure acrossLongmenshan fault belt from passive source seismic profiling[J].Geophysical Research Letters,2009,36,L17310,doi:10.1029/2009GL039580.
[31]石耀霖.关于应力触发和应力影概念在地震预报中应用的一些思考[J].地震,2001,(3):1-7.Shi Y L.Stress triggers and stress shadows:How to applythese concepts to earthquake prediction[J].Earthquake(inChinese),2001,(3):1-7.
[32]程佳,刘杰,甘卫军,等.1997年以来巴颜喀拉块体周缘强震之间的黏弹性触发研究[J].地球物理学报,2011,54(8):1997-2010.Cheng J,Liu J,Gan W J,et al.Coulomb stress interactionamong strong earthquakes around the Bayan Har block sincethe Manyi earthquake in 1997[J].Chinese J.Geophys.(inChinese),2011,54(8):1997-2010.
[33]张晁军,曹建玲,石耀霖.从震后形变探讨青藏高原下地壳黏滞系数[J].中国科学(D辑),2008,38(10):1250-1257.Zhang C J,Cao J L,Shi Y L.Study the viscosity of crustusing the post-earthquake deformation[J].Science in ChinaSeries D:Earth Sciences(in Chinese),2008,38(10):1250-1257.
[34]白玉柱,徐锡伟,徐杰,等.2008年汶川地震近断裂区域变形场的空间分布[J].地球物理学报,2011,54(7):1798-1804.Bai Y Z,Xu X W,Xu J,et al.A research on the distributionof deformation fields near the fault of 2008 WenchuanEarthquake[J].Chinese J.Geophys.(in Chinese),2011,54(7):1798-1804.
[35]Turcotte D L.Schubert G.Geodynamics(2nd ed)[M].NewYork:Cambridge University Press,2002.
[36]Byerlee J D.Friction of rocks[J].Pure and Applied Geophysics,1978,116(4-5):615-629.
[37]Townend J,Zoback M D.How faulting keeps the crust strong[J].Geology,2000,28(5):399-402.
[38]Zoback M D,Townend J.Implications of hydrostatic porepressures and high crustal strength for the deformation ofintraplate lithosphere[J].Tectonophysics,2001,336(1-4):19-30.
[39]张国民,马宏生,王辉,等.中国大陆活动地块边界带与强震活动[J].地球物理学报,2005,48(3):602-610.Zhang G M,Ma H S,Wang H,et al.Boundaries betweenactive-tectonic blocks and strong earthquakes in the Chinamainland[J].Chinese J.Geophys.(in Chinese),2005,48(3):602-610.
[40]Zhang Z J,Yuan X H,Chen Y,et al.Seismic signature ofthe collision between the east Tibetan escape flow and theSichuan basin[J].Earth and Planetary Science Letters,2010,292(3-4):254-264.
[41]Zhang Z J,Deng Y F,Teng J W,et al.An overview of thecrustal structure of the Tibetan Plateau after 35years of deepseismic soundings[J].Journal of Asian Earth Sciences,2011a,40(4):977-989.
[42]Zhang Z J,Klemperer S L,Bai Z M,et al.Crustal structureof the Paleozoic Kunlun orogeny from an active-source seismicprofile between Moba and Guide in East Tibet,China[J].Gondwana Research,2011b,19(4):994-1007.
[43]Zhang Z J,Klemperer S L.West-east variation in crustalthickness in northern Lhasa block,central Tibet,from deepseismic sounding data[J].J.Geophys.Res.,2005,110:B09403,doi:10.1029/2004JB003139.
[44]王谦身,滕吉文,张永谦,等.四川中西部地区地壳结构与重力均衡[J].地球物理学报,2009,52(2):579-583.Wang Q S,Teng J W,Zhang Y Q,et al.The crustalstructure and gravity isostasy in the middle western Sichuanarea[J].Chinese J.Geophys.(in Chinese),2009,52(2):579-583.
[45]王谦身,滕吉文,张永谦,等.龙门山断裂系及邻区地壳重力均衡效应与汶川地震[J].地球物理学进展,2008,23(6):1664-1670.Wang Q S,Teng J W,Zhang Y Q,et al.The effect ofcrustal gravity isostasy and Wenchuan earthquake inLongmenshan faults and adjacent area[J].Process inGeophys.(in Chinese),2008,23(6):1664-1670.
[46]Wang C Y,Han W B,Wu J P,et al.Crustal structure beneaththe eastern margin of the Tibetan Plateau and its tectonicimplications[J].J.Geophys.Res.,2007,112,B07307,doi:10.1029/2005JB003873.
[47]赵国泽,陈小斌,王立凤,等.青藏高原东边缘地壳“管流”层的电磁探测证据[J].科学通报,2008,53(3):345-350.Zhao G Z,Chen X B,Wang L F,et al.Evidence of crustal“channel flow”in the eastern margin of Tibetan Plateau fromMT measurements[J].Chinese Science Bulletin,2008,53(12):1887-1893.
[48]Wei W B,Unsworth M,Alan J,et al.Detection of widespreadfluids in the Tibetan crust by magnetotelluric studies[J].Science,2001,292(5517):716-718.
[49]金胜,魏文博,汪硕,等.青藏高原地壳高导层的成因及动力学意义探讨——大地电磁探测提供的证据[J].地球物理学报,2010,53(10):2376-2385.Jin S,Wei W B,Wang S,et al.Discussion of the formationand dynamic signification of the high conductive layer inTibetan crust[J].Chinese J.Geophys.(in Chinese),2010,53(10):2376-2385.
[50]石耀霖,曹建玲.中国大陆岩石圈等效粘滞系数的计算和讨论[J].地学前缘,2008,15(3):82-95.Shi Y L,Cao J L.Effective viscosity of China continentallithosphere[J].Earth Science Frontiers(in Chinese),2008,15(3):82-95.
[51]范桃园,龙长兴,杨振宇,等.中国大陆现今地应力场黏弹性球壳数值模拟综合研究[J].地球物理学报,2012,55(4):1249-1260.Fan T Y,Long C X,Yang Z Y,et al.Comprehensivemodeling on the present crustal stress of China mainland withthe viscoelastic spherical shell[J].Chinese J.Geophys.(inChinese),2012,55(4):1249-1260.
[52]Zoback M D.Reservoir Geomechanics[M].New York:CambridgeUniversity Press,2010:123-139.
[53]李延兴,张静华,周伟,等.南海及周围地区的现今构造运动[J].大地测量与地球动力学,2010,30(3):10-16.Li Y X,Zhang J H,Zhou W,et al.Current tectonicmovement of South China sea and its surrounding areas[J].Journal of Geodesy and Geodynamics(in Chinese),2010,30(3):10-16.
[54]Fan C,Wang G,Wang S F,et al.Structural interpretationof extensional deformation along the Dali fault system,southeastern margin of the Tibetan plateau[J].InternationalGeology Review,2006,48(4):287-310.
[55]Wu Z H,Zhang Y S,Hu D G,et al.Late Quaternarynormal faulting and its kinematic mechanism of easternpiedmont fault of the Haba-Yulong Snow Mountains innorthwestern Yunnan,China[J].Science in China Series D:Earth Sciences,2009,52(10):1470-1484.
[56]Han Z J,Xiang H F,Guo S M.Sinistral shear and extensionof the northern section of Lijiang basin in northwest Yunnanin quaternary[J].Chinese Science Bulletin,2005,50(5):452-459.
[57]王辉,曹建玲,张怀,等.川滇地区下地壳流动对上地壳运动变形影响的数值模拟[J].地震学报,2007,29(6):581-591.Wang H,Cao J L,Zhang H,et al.Numerical simulation ofthe influence of lower crustal flow on the deformation of theSichuan-Yunnan region[J].Acta Seismologica Sinica(inChinese),2007,29(6):581-591.