地震动态应力触发研究进展
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摘要
本文从以下几方面阐述了近几年来地震动态应力触发的研究进展:地震动态应力触发问题的提出;地震动态应力触发存在的证据(包括地震频度图中探寻被触发震群和独立地震、数字滤波后新发现的被触发地震和形变仪器记录的同震变化和应力阶跃等);地震动态触发的研究现状和机理等。还提出了目前动态应力触发研究中存在的问题,并对其近期的发展进行了展望。
The research progress of seismic dynamic stress triggering in recent years from several aspects is expounded: How the problems are put forward.The exist evidences of dynamic stress triggering,including seek triggered earthquake swarm or single earthquake in seismic frequency map,find new triggered earthquake by digital filter,and co-seism change and stress step recorded by strain instrument;current situation of the research;triggering mechanism and so on.Meanwhile some problems in the research are given up,and the development of seismic dynamic tress triggering research in recent future is look ahead.
The research progress of seismic dynamic stress triggering in recent years from several aspects is expounded: How the problems are put forward.The exist evidences of dynamic stress triggering,including seek triggered earthquake swarm or single earthquake in seismic frequency map,find new triggered earthquake by digital filter,and co-seism change and stress step recorded by strain instrument;current situation of the research;triggering mechanism and so on.Meanwhile some problems in the research are given up,and the development of seismic dynamic tress triggering research in recent future is look ahead.
引文
[1]王海涛,王琼,赵翠萍.2003年2月24日新疆巴楚—伽师MS6.8地震的应力触发作用研究[J].西北地震学报,2006,28(40):335-340.
[2]万永革,沈正康,甘卫军,等.东昆仑活动断裂带大地震之间的弹性应力触发研究[J].西北地震学报,2003,25(1):1-7.
[3]张国民,张晓东,刘杰,等.印尼苏门答腊8.7级大震对中国陆区的影响[J].地震,2005,25(4):15-25.
[4]Kilb D,Gomberg J,Bodin P.Triggering of earthquake aftershocksby dynamic stresses[J].Nature,2000,408:570-574.
[5]Hill D P,Reasenberg P A,Michael A,et al.Seismicity remotelytriggered by the magnitude 7.3 Landers,California,earthquake[J].Science,1993,260:1617-1623.
[6]Cotton F,Coutant O.Dynamic stress variations due to shear faul-ting in a plane-layered medium[J].Geophys.J.Int.,1997,128:676-688.
[7]Harris R A.Introduction to special section:Stress triggers,stressshadows,and implications for seismic hazard[J].J.phys.Res.,1998,103:24347-24358.
[8]Brodsky E E,Karakostas V,Kanamori H.A new observation ofdynamically triggered regional seismicity:earthquakes in Greecefollowing the August,1999,Izmit,Turkey earthquake[J].Geo-phys.Res.Lett.,2000,27:2741-2744.
[9]Mohamad R,Darkal A N,Seber D,et al.Remote earthquake trig-gering along the Dead Sea Fault in Syria following the 1995 Gulf ofAqaba earthquake(MS=7.3)[J].Seismol.Res.Lett.,2000,71:47-52.
[10]Gomberg J,Reasenberg P A,Bodin P,et al..Earthquakes trig-gering by seismic waves following the Landera and Hector Mineearthquakes[J].Nature,2001,411:462-465.
[11]Hill D P,Reasenberg P A,Michael A,et a1..Seismicity re-motely triggered by the magnitude 7.3 Landers,Califomia earth-quake[J].Science,1993,260:1617-1623.
[12]Anderson J G,Brune J N,Louie J N.et al..Seismicity in thewestern Great Basin apparently triggered by the Landers,Califor-nia,earthquake,28 June 1992[J].Bull.Seismol.Soc.America,1994,84:863-891.
[13]Bodin P,Gomberg J.Triggered seismicity and deformation be-tween the Landers,California and Little Skull mountain,Nevada,earthquakes[J].Bull.Seismol.Soc.America,1994,84:835-843.
[14]Gomberg J,Davis S.Stress/strain changes and triggered seismic-ity at The Geysers,California[J].J.Geophys.Res.,1996,101:733-749.
[15]Arnadottir T,Geirsson H,Einarsson P.Coseismic stress changesand crustalde formation on the Reykjanes Peninsula due to trig-gered earthquakes on 17 June 2000[J].J.Geophys.Res.,2004,109,doi:10.1029/2004JB003130.
[16]Wen KL,Beresnev I A,Cheng S.Moderate-magnitude seismici-ty remotely triggered in the Taiwan Region by large earthquakesaround the Philippine Sea Plate[J].Bull.Seismol.Soc.Ameri-ca,1996,86:843-847.
[17]Prejean S G,Hill D P,Brodsky E E,et al..Remotely triggeredseismicity on the United States west coast following theMW7.9Denali Fault earthquake[J].Bull.Seismol.Soc.America,2004,94:S348-S359.
[18]Harrington R M,Brodsky E E.The absence of remotely triggeredseismicity in Japan[J].Bull.Seismol.Soc.America,2006,96:871-878.
[19]Miyazawa M,Mori J.Detection of triggered deep low-frequencyevents from the 2003 Takachi-oki earthquake[J].Geophys.Res.Lett.,2005,32:L10307.
[20]Harrington R M,Brodsky E E.The absence of remotely triggeredseismicity in Japan[J].Bull.Seismol.Soc.America,2006,96:871-878.
[21]李纲,刘杰,郭铁栓.印尼8.7、8.5级巨震对云南地区地震活动的远震触发分析[J].地震,2005,25(4):49-57.
[22]马寅生,史大年,安美建,等.苏门答腊地震对柴达木地方震的触发作用[J].地质力学学报,2005,11(2):110-115.
[23]焦明若,王海燕,李芳,等.印尼8.7级地震对辽宁地区的影响[J].东北地震研究,2005,21(4):1-9.
[24]Ukawa M,Fujita E,Kumagai T.Remote triggering of microe-arthquakes at the Iwo-Jima volcano[J].Journal of Geography,2002,111:277-286.
[25]West M,Sanchez J J,Mcnutt S R.Periodically triggered seis-micity at Mount Wrangell,Alaska,after the Sumatra earthquake[J].Science,2005,308:1144-1146.
[26]Tibi R,Wiens D A,Inoue H.Remote triggering of deep earth-quakes in the 2002 Tonga sequence[J].Nature,2003,424:921-925.
[27]Aagaard B T,Anderson,Hudnut K W.Dynamic rupture model-ing of the transition from thrust to strike-slip motion in the 2002Denali Fault earthquake[J].Bull.Seismol.Soc.America,2004,94:S190-S201.
[28]Gomberg J,Bodin P,Reasenberg P A.Observing earthquakestriggered in the near field by dynamic deformations[J].Bull.Seismol.Soc America,2003,93:118-138.
[29]Gomberg J,Bodin P,Larson K,et al..Earthquakes nucleated bytransient deformations caused by theM=7.9 Denali,Alaska,earthquake[J].Nature,2004,427:621-624.
[30]Gomberg J,Johnson P.Dynamic triggering of earthquakes[J].Nature,2005,437:830.
[31]Hill D P,Johnston MJ,Langbein J O,et al..Response of LongValley Caldera to theMW=7.3 Landers,California,earthquake[J].Journal of Geophysical Research,1995,100:12985-13005.
[32]Ziv A.On the role of multiple interactions in remote aftershocktriggering:the Landers and the Hector Mine case studies[J].Bull.Seismol.Soc.America,2006,96:80-89.
[33]Singh S K,Anderson J G,Rodriguez M.Triggered seismicity inthe Valley of Mexico from major Mexican earthquakes[J].Geofiscia International,1998,37:3-15.
[34]Mohamad R,Darkal A N,Seber D,et al..Remote earthquaketriggering along the Dead Sea Fault in Syria following the 1995Gulf of Aqaba earthquake(MS=7.3)[J].Seismol.Res.Lett.,2000,71:47-52.
[35]Hill D P,Pollitz F,Newhall C.Earthquake-volcano interac-tions[J].Physics Today,2002,55:41-47.
[36]Brodsky E,Sturtevant B,Kanamori H.Earthquakes,volcan-ones,and rectified diffusion[J].J.Geophys.Res.,1998,103:23827-3838.
[37]Linde A T,ladwin M T,ohnston M J S,et al..A slow earth-quake sequence on the San Andreas fault[J],Nature,1996,383:65-68.
[38]Hill D P,Johnston M J S,Langbein J O,et al..Response ofLong Valley Caldera to theMW=7.3 Landers,California,earth-quake[J].Journal of Geophysical Research,1995,100:12985-13005.
[39]Pollitz F F,Johnston M J.Direct test of static stress versus dy-namic stress triggering of aftershocks[J].Geophys.Res.Lett.,2006,33:1029GL026764.
[40]Spudich P,Steck L K,Hellweg M,et al..Transient stresses atParkfield,California,produced by theMS7.4 Landers earthquakeof June 28,1992:Observations from the UPSAR dense seismo-graph array[J].J.Geophys.Res.,1995,100:675-690.
[41]Stein R S,Barka A A,Dieterich J H.Progressive failure on theNorth Anatolian fault since 1939 by earthquake stress triggering[J].Geophys.J.Int.,1997,128:594-604.
[42]Nalbant S S,Hubert A,King G C P.Stress coupling betweenearthquakes in northwest Turkey and the north Aegean Sea[J].J.Geophys.Res.,1998,103:24469-24486.
[2]万永革,沈正康,甘卫军,等.东昆仑活动断裂带大地震之间的弹性应力触发研究[J].西北地震学报,2003,25(1):1-7.
[3]张国民,张晓东,刘杰,等.印尼苏门答腊8.7级大震对中国陆区的影响[J].地震,2005,25(4):15-25.
[4]Kilb D,Gomberg J,Bodin P.Triggering of earthquake aftershocksby dynamic stresses[J].Nature,2000,408:570-574.
[5]Hill D P,Reasenberg P A,Michael A,et al.Seismicity remotelytriggered by the magnitude 7.3 Landers,California,earthquake[J].Science,1993,260:1617-1623.
[6]Cotton F,Coutant O.Dynamic stress variations due to shear faul-ting in a plane-layered medium[J].Geophys.J.Int.,1997,128:676-688.
[7]Harris R A.Introduction to special section:Stress triggers,stressshadows,and implications for seismic hazard[J].J.phys.Res.,1998,103:24347-24358.
[8]Brodsky E E,Karakostas V,Kanamori H.A new observation ofdynamically triggered regional seismicity:earthquakes in Greecefollowing the August,1999,Izmit,Turkey earthquake[J].Geo-phys.Res.Lett.,2000,27:2741-2744.
[9]Mohamad R,Darkal A N,Seber D,et al.Remote earthquake trig-gering along the Dead Sea Fault in Syria following the 1995 Gulf ofAqaba earthquake(MS=7.3)[J].Seismol.Res.Lett.,2000,71:47-52.
[10]Gomberg J,Reasenberg P A,Bodin P,et al..Earthquakes trig-gering by seismic waves following the Landera and Hector Mineearthquakes[J].Nature,2001,411:462-465.
[11]Hill D P,Reasenberg P A,Michael A,et a1..Seismicity re-motely triggered by the magnitude 7.3 Landers,Califomia earth-quake[J].Science,1993,260:1617-1623.
[12]Anderson J G,Brune J N,Louie J N.et al..Seismicity in thewestern Great Basin apparently triggered by the Landers,Califor-nia,earthquake,28 June 1992[J].Bull.Seismol.Soc.America,1994,84:863-891.
[13]Bodin P,Gomberg J.Triggered seismicity and deformation be-tween the Landers,California and Little Skull mountain,Nevada,earthquakes[J].Bull.Seismol.Soc.America,1994,84:835-843.
[14]Gomberg J,Davis S.Stress/strain changes and triggered seismic-ity at The Geysers,California[J].J.Geophys.Res.,1996,101:733-749.
[15]Arnadottir T,Geirsson H,Einarsson P.Coseismic stress changesand crustalde formation on the Reykjanes Peninsula due to trig-gered earthquakes on 17 June 2000[J].J.Geophys.Res.,2004,109,doi:10.1029/2004JB003130.
[16]Wen KL,Beresnev I A,Cheng S.Moderate-magnitude seismici-ty remotely triggered in the Taiwan Region by large earthquakesaround the Philippine Sea Plate[J].Bull.Seismol.Soc.Ameri-ca,1996,86:843-847.
[17]Prejean S G,Hill D P,Brodsky E E,et al..Remotely triggeredseismicity on the United States west coast following theMW7.9Denali Fault earthquake[J].Bull.Seismol.Soc.America,2004,94:S348-S359.
[18]Harrington R M,Brodsky E E.The absence of remotely triggeredseismicity in Japan[J].Bull.Seismol.Soc.America,2006,96:871-878.
[19]Miyazawa M,Mori J.Detection of triggered deep low-frequencyevents from the 2003 Takachi-oki earthquake[J].Geophys.Res.Lett.,2005,32:L10307.
[20]Harrington R M,Brodsky E E.The absence of remotely triggeredseismicity in Japan[J].Bull.Seismol.Soc.America,2006,96:871-878.
[21]李纲,刘杰,郭铁栓.印尼8.7、8.5级巨震对云南地区地震活动的远震触发分析[J].地震,2005,25(4):49-57.
[22]马寅生,史大年,安美建,等.苏门答腊地震对柴达木地方震的触发作用[J].地质力学学报,2005,11(2):110-115.
[23]焦明若,王海燕,李芳,等.印尼8.7级地震对辽宁地区的影响[J].东北地震研究,2005,21(4):1-9.
[24]Ukawa M,Fujita E,Kumagai T.Remote triggering of microe-arthquakes at the Iwo-Jima volcano[J].Journal of Geography,2002,111:277-286.
[25]West M,Sanchez J J,Mcnutt S R.Periodically triggered seis-micity at Mount Wrangell,Alaska,after the Sumatra earthquake[J].Science,2005,308:1144-1146.
[26]Tibi R,Wiens D A,Inoue H.Remote triggering of deep earth-quakes in the 2002 Tonga sequence[J].Nature,2003,424:921-925.
[27]Aagaard B T,Anderson,Hudnut K W.Dynamic rupture model-ing of the transition from thrust to strike-slip motion in the 2002Denali Fault earthquake[J].Bull.Seismol.Soc.America,2004,94:S190-S201.
[28]Gomberg J,Bodin P,Reasenberg P A.Observing earthquakestriggered in the near field by dynamic deformations[J].Bull.Seismol.Soc America,2003,93:118-138.
[29]Gomberg J,Bodin P,Larson K,et al..Earthquakes nucleated bytransient deformations caused by theM=7.9 Denali,Alaska,earthquake[J].Nature,2004,427:621-624.
[30]Gomberg J,Johnson P.Dynamic triggering of earthquakes[J].Nature,2005,437:830.
[31]Hill D P,Johnston MJ,Langbein J O,et al..Response of LongValley Caldera to theMW=7.3 Landers,California,earthquake[J].Journal of Geophysical Research,1995,100:12985-13005.
[32]Ziv A.On the role of multiple interactions in remote aftershocktriggering:the Landers and the Hector Mine case studies[J].Bull.Seismol.Soc.America,2006,96:80-89.
[33]Singh S K,Anderson J G,Rodriguez M.Triggered seismicity inthe Valley of Mexico from major Mexican earthquakes[J].Geofiscia International,1998,37:3-15.
[34]Mohamad R,Darkal A N,Seber D,et al..Remote earthquaketriggering along the Dead Sea Fault in Syria following the 1995Gulf of Aqaba earthquake(MS=7.3)[J].Seismol.Res.Lett.,2000,71:47-52.
[35]Hill D P,Pollitz F,Newhall C.Earthquake-volcano interac-tions[J].Physics Today,2002,55:41-47.
[36]Brodsky E,Sturtevant B,Kanamori H.Earthquakes,volcan-ones,and rectified diffusion[J].J.Geophys.Res.,1998,103:23827-3838.
[37]Linde A T,ladwin M T,ohnston M J S,et al..A slow earth-quake sequence on the San Andreas fault[J],Nature,1996,383:65-68.
[38]Hill D P,Johnston M J S,Langbein J O,et al..Response ofLong Valley Caldera to theMW=7.3 Landers,California,earth-quake[J].Journal of Geophysical Research,1995,100:12985-13005.
[39]Pollitz F F,Johnston M J.Direct test of static stress versus dy-namic stress triggering of aftershocks[J].Geophys.Res.Lett.,2006,33:1029GL026764.
[40]Spudich P,Steck L K,Hellweg M,et al..Transient stresses atParkfield,California,produced by theMS7.4 Landers earthquakeof June 28,1992:Observations from the UPSAR dense seismo-graph array[J].J.Geophys.Res.,1995,100:675-690.
[41]Stein R S,Barka A A,Dieterich J H.Progressive failure on theNorth Anatolian fault since 1939 by earthquake stress triggering[J].Geophys.J.Int.,1997,128:594-604.
[42]Nalbant S S,Hubert A,King G C P.Stress coupling betweenearthquakes in northwest Turkey and the north Aegean Sea[J].J.Geophys.Res.,1998,103:24469-24486.
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