应力触发模型研究进展概述
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摘要
对应力触发问题的研究从20世纪60年代至今已近半个世纪。这半个世纪以来,地震专家和学者通过对大量震例的分析和比较,在应力触发问题某些方面的研究逐渐从探索性趋向系统性。主要从静态库仑破裂应力、动态库仑破裂应力和完整库仑破裂应力3方面简要概述其对地震触发的作用。
The study of stress triggering question has already near half century from 60's of 20th century to now.Since the half century,by analyzing and comparing for the large numbers of event cases,the earthquake expert and the scholar studied gradually from exploring to system in some aspects of stress triggering question.In this paper,we summarized mainly and briefly 3 aspects of static coulomb failure stress,dynamic coulomb failure stress and integrated coulomb failure stress to earthquake triggering function.
The study of stress triggering question has already near half century from 60's of 20th century to now.Since the half century,by analyzing and comparing for the large numbers of event cases,the earthquake expert and the scholar studied gradually from exploring to system in some aspects of stress triggering question.In this paper,we summarized mainly and briefly 3 aspects of static coulomb failure stress,dynamic coulomb failure stress and integrated coulomb failure stress to earthquake triggering function.
引文
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[35]Cotton F,Coutant O.Dynamic stress variations due to shear faulting in a plane-layered medium[J].Geophys J Int,1997,128:676-688.
[36]Kilb D,Gomberg J,Bodin P.Tirggeirng of earthquake aftershocks by dynamic stresses[J].Nature,2000,408:570-574.
[37]Gomberg J,Davis S.Stress/strain changes and triggered seismicity at The Geysers,California[J].J Geophys Res,1996,101:733-749.
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[51]曾跃华.1992年兰德斯地震对1997年赫克托矿地震的粘弹性应力触发[J].世界地震译丛,2002,(4):30-34.
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[2]Smith S W,Van de Lindt W.Strain adjustments associated with earthquakes in southern California[J].Bull Seism Soc Amer,1969,59(4):1 569-1 589.
[3]Rybichi K.Analysis of aftershocks on the basis of dislocation theory[J].Phy Earth Planet Inter,1937,7(4):409-422.
[4]陈运泰,林邦慧,林中样,等.根据地面形变的观测研究1966年邢台地震的震源过程[J].地球物理学报,1975,18(3):164-182.
[5]Yamashina K.Induced earthquakes in the Izu Peninsula by Izu-Hanto-Oki earthquake of 1974 Japan[J].Tectonophysics,1978,51:139-154.
[6]黄福明,王延韫.倾斜断层错动产生的应力场[J].地震学报,1980,2(1):1-20.
[7]罗灼礼.震源应力场、形变场和倾斜场[J].地震学报,1980,2(2):169-185.
[8]Jaeger J C,Cook N G W.Fundamental of Rock Mechanics[M].New York:Methuen,1969.
[9]Harris R A.Introduction to special section:Stress triggers,stress shadows,and implications for seismic hazard[J].J Geophys Res,1998,103:24 347-24 358.
[10]Rice J R,Cleary MP.Some basic stress diffusion solutions for fluid-saturated elastic porous media with compressible constituents[J].Rev Geophys,1976,14:227-241.
[11]Roeloffs E A.Fault stability changes induced beneath a reservoir cyclic variations in water level[J].J Geophys Res,1988,93:2 107-2 124.
[12]Green D H,Wang HF.Fluid pressure response to undrained compression in saturated sedimentary rock[J].Geophysics,1986,51:948-956.
[13]Rice J R.Fault stress states,pore pressure distribution,and the weakness of the San Andreas fault.Fault Mechanics and Trans-port Properties of Rock[M].London:Academic press,1992.
[14]陈兵,江在森,车时,等.玛尼7.9级地震对昆仑山口西8.1级地震的触发作用及动力背景初探[J].中国地震,2003,19(1):1-7.
[15]刘桂萍,傅征祥.1976年7月28日唐山7.8级地震触发的区域地震活动和静应力场变化[J].地震学报,2000,22(1):17-26.
[16]刘桂萍,傅征祥.日本1995年1月17日兵库县南部7.2级地震触发的区域地震活动[J].地震学报.1999,21(3):250-257.
[17]Strehlau J.A discussion of the depth extent of rupture in large continental earthquakes[C]//In:Dass,Boat weight JanelScholz Ced.Earthquake Source Mechanis,AGU Geophys mono.37.Washington D.C:American Geophysical Union,131-146.
[18]Otsuka M.Asimulation of earthquake occurrence,5:an interpretation of aftershock phenomena[J].Zisin SerⅡ,1976,29,137-146.
[19]Aki K.Characterization of barriers on and earthquake fault[J].J.Geophys.Res.,1979,84:6 140-6 148.
[20]刘桂萍,傅征祥.1973年炉霍大地震(MS7.6)最大余震(MS6.3)的库仑破裂应力触发[J].中国地震,2002,18(1):175-182.
[21]郝平,傅征祥,田勤俭,等.昆仑山口西8.1级地震强余震库仑破裂应力触发研究[J].地震学报,2004,26(1):30-37.
[22]王海涛,王琼,赵翠萍.2003年2月24日新疆伽师—巴楚MS6.8地震的应力触发研究[J].西北地震学报,2006,28(4):335-340.
[23]Beroza G C,Zoback MD.Mechanism diversity of the Loma Prieta aftershocks and the mechanics of mainshock-aftershock inter-action[J].Science,1993,259:210-213.
[24]Kilb D,Ellis M,Gomberg J,et al.On the origin of diverse aftershock mechanisms following the 1989 Loma Prieta earthquake[J].Geophy J Int,1997,128:557-570.
[25]Astiz L,Shearer P M,AgnewD.Precise relocations and stress change calculations for the Upland earthquake sequence in south-ern California[J].J Geophys Res,2000,105:2 937-2 935.
[26]王琼,王海涛.伽师强震活动过程的应力触发作用研究[J].中国地震,2007,23(1):35-46.
[27]Parsons T,Dreger D S.Static-stress impact of the 1992 Landers earthquake sequence on nucleation and slip at the site of the1999M=7.1 Hector Mine earthquake,southern California[J].Geophys Res Lett,2000,27:1 949-1 952.
[28]Horikawa H.Earthquake doublet in Kagoshima,Japan:rupture of asperities in a stress shadow[J].Bull Seism Soc Amer,2001,91:112-127.
[29]万永革,吴忠良,周公威,等.几次复杂地震中不同破裂事件之间的“应力触发”问题[J].地震学报,2000,22(6):568-576.
[30]Harris R A.Introduction to special section:Stress triggers,Stress shadows,and implications for seismic hazard[J].J GeophysRes,1998,103:24 347-24 358.
[31]石耀林.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,2001,21(3):1-7.
[32]万永革,吴忠良,周公威,等.地震静态应力触发模型的全球检验[J].地震学报,2002,24(3):302-316.
[33]Simpson R W,Schulz S S,Dietz L D,et al.The response of creeping parts of the San Andreas fault to earthquakes on nearbyfaults:Two examples[J].Pure Appl Geophys,1998,126:665-685.
[34]JauméS C,Sykes LR.Evolution of moderate seismicity in the San Francisco Bay region,1850 to1993:Seismicity changes relat-ed to the occurrence of large and great earthquakes[J].J Geophys Res,1996,101:765-789.
[35]Cotton F,Coutant O.Dynamic stress variations due to shear faulting in a plane-layered medium[J].Geophys J Int,1997,128:676-688.
[36]Kilb D,Gomberg J,Bodin P.Tirggeirng of earthquake aftershocks by dynamic stresses[J].Nature,2000,408:570-574.
[37]Gomberg J,Davis S.Stress/strain changes and triggered seismicity at The Geysers,California[J].J Geophys Res,1996,101:733-749.
[38]Kilb D,Gomberg J,Bodin P.动态应力触发的余震[J].世界地震译丛,2002,(3):18-22.
[39]Nostro C,CCOOC M,Belardinelli ME.Sattic stress changes in extensional regimes:An application to south-central Apennines(Italy)[J].Bull Seism Soc Amer,1997,87:234-248.
[40]Troise C,DeNatale G,Pingue F,et al.Evidence for static stress interaction among earthquakes in south-central Apennines(Italy)[J].Geophys J Int,1998,134:809-817.
[41]Astiz L.Shearer P M,AgnewD.Precise relocations and stress change calculations for the Upland earthquake sequence in south-ern Claifornia[J].J Geophys Res,2000,105:2 937-2 953.
[42]Robinson R,McGinyt P J.The enigma of the Auhtur's Pass,NewZealand,earthquake 2.The aftershock distribution and its rela-tion to regional and induced stress field[J].J Geophys Res,2000,105:16 139-16 150.
[43]郝平,刘杰,韩竹军,等.印尼MS8.7地震对中国大陆3次后续中强地震的动应力触发研究[J].地震,2006,26(3):26-36.
[44]虎雄林,吴小平,杨润海,等.云南武定M6.5地震动态库仑破裂应力变化的数值模拟及其与余震活动的关系[J].地震学报,2008,30(1):26-35.
[45]Ziv A,Rubin AM.Static stress transfer and earthquake triggering:No lower threshold in sight?[J].J Geophys Res,2000,105:13 631-13 642.
[46]Bouchon M,Aki K.Discrete wave-number representation of seismic source wave fields[J].Bull Seism Soc Amer,1977,67:259-277.
[47]Bouchon M.1981.A simple method to calculate Green's functions in elastic layered media[J].Bull Seism Soc Amer,1981,71:959-971.
[48]Bouchon M.A review of the discrete wave-number method[J].Pure Appl Geophys,2003,160(3):445-465.
[49]吴小平,虎雄林,Michel Bouchon,等.云南澜沧—耿马MS7.6地震的完全库仑破裂应力变化与后续地震的动态、静态应力触发[J].中国科学D辑:地球科学,2007,37(6):743-752.
[50]曾跃华.Viscoelastic stress-triggering of the 1999 Hector Mine earthquake by the 1992 Landers earthquake[J].Geophys ResLett,2001,28(15):3 007-3 010.
[51]曾跃华.1992年兰德斯地震对1997年赫克托矿地震的粘弹性应力触发[J].世界地震译丛,2002,(4):30-34.
[52]沈正康,万永革,甘卫军,等.华北地区700年来地壳应力场演化与地震发生研究[J].中国地震,2004,20(3):211-228.
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