动态88小时:美国地质调查局国家地震信息中心对2011年3月11日M_W9.0日本地震的响应
|
摘要
<正>引言2011年3月11日日本本州岛东海岸附近海域发生的M9.0地震(Tohoku earth-quake,以下称"东日本大地震"———译者注)及其引发的海啸造成数以万计的人员死亡,造成的财产损失可能超过1万亿美元,这是有历史记录以来最严重的自然灾害之一。美
引文
[1]Butler R,Lay T,Creager K,et al.The Global Seismographic Network surpasses its design goal.Eos,Transactions,American Geophysical Union,2004,85(23);doi:10.1029/2004EO230001
[2]Kanamori H,Rivera L.Sourceinversion of Wphase:Speeding up seismic tsunami warning.GeophysicalJournal International,2008,175:222-238
[3]Hayes G P,Rivera L,Kanamori H.Source inversion of the Wphase:Real-ti me i mplementation and ex-tension to low magnitudes.Seismological Research Letters,2009,80:817-822;doi:810.1785/gssrl.1780.1785.1817
[4]Duputel Z,Rivera L,Kanamori H,et al.W-phase fast source inversion for moderate to large earth-quakes(MW6.5,1990—2010).Submitted to Geophysical Journal International,2011
[5]Ji C,Wald DJ,Hel mberger D V.Source description of the 1999 Hector Mine,California,earthquake,part I:Wavelet domaininversion theory and resolution analysis.Bulletin of the Seismological Society ofAmerica,2002,92:1192-1207
[6]Buland R P,Guy M,Kragness D,et al.Comprehensive seismic monitoring for emergency response andhazard assessment:Recent developments at the USGS National Earthquake Information Center.Eos,Transactions,American Geophysical Union,2009,90(52),Fall Meeting Supplement,Abstract S11B-1696
[7]Tsuboi S,Abe K,Takano K,et al.Rapid determination ofMWfrom broadband P waveforms.Bulletinof the Seismological Society of America,1995,85:606-613
[8]Allen TI,Wald DJ.Evaluation of Ground-Motion Modeling Techniques for Usein Global Shake Map:ACritique of Instrumental Ground-Motion Prediction Equations,Peak Ground Motion to Macroseismic In-tensity Conversions,and Macroseismic Intensity Predictions in Different Tectonic Settings.USGS Open-File Report 2009-1047,2009,114 pp
[9]Wald DJ,Lin K-W,Quitoriano V.Quantifying and Qualifying USGS Shake Map Uncertainty.USGSOpen-File Report 2008-1238,2008,26 pp
[10]Polet J,Thio H K.Rapid characterization of a centroid moment tensor and waveheight predictions a-round the north Pacific for the 2011 Tohoku earthquake.Earth,Planets and Space(forthcoming)
[11]Hayes G P,Wald DJ,Keranen K.Advancing techniques to constrain the geometry of the seismic rup-ture plane on subduction interfaces a priori:Higher-order functional fits.Geochemistry,Geophysics,Geosystems,2009,10;doi:10.1029/2009GC002633
[12]Kanamori H,Given J W.Use of long-period surface waves for rapid determination of earthquake sourceparameters.Physics of the Earth and Planetary Interiors,1981,27:8-31
[13]Dziewonski A M,Anderson D L.Preli minary Reference Earth Model(PREM).Physics of the Earth andPlanetary Interiors,1981,25:297-356
[14]Hayes G P.Rapid source characterization of the 03-11-2011MW9.0 Tohoku Earthquake.Earth,Planetsand Space(forthcoming)
[15]Wessel P,Smith W HF.Free software helps map and display data.Eos,Transactions,American Geo-physical Union,1991,72:445-446(原文中致谢———译者注)
[2]Kanamori H,Rivera L.Sourceinversion of Wphase:Speeding up seismic tsunami warning.GeophysicalJournal International,2008,175:222-238
[3]Hayes G P,Rivera L,Kanamori H.Source inversion of the Wphase:Real-ti me i mplementation and ex-tension to low magnitudes.Seismological Research Letters,2009,80:817-822;doi:810.1785/gssrl.1780.1785.1817
[4]Duputel Z,Rivera L,Kanamori H,et al.W-phase fast source inversion for moderate to large earth-quakes(MW6.5,1990—2010).Submitted to Geophysical Journal International,2011
[5]Ji C,Wald DJ,Hel mberger D V.Source description of the 1999 Hector Mine,California,earthquake,part I:Wavelet domaininversion theory and resolution analysis.Bulletin of the Seismological Society ofAmerica,2002,92:1192-1207
[6]Buland R P,Guy M,Kragness D,et al.Comprehensive seismic monitoring for emergency response andhazard assessment:Recent developments at the USGS National Earthquake Information Center.Eos,Transactions,American Geophysical Union,2009,90(52),Fall Meeting Supplement,Abstract S11B-1696
[7]Tsuboi S,Abe K,Takano K,et al.Rapid determination ofMWfrom broadband P waveforms.Bulletinof the Seismological Society of America,1995,85:606-613
[8]Allen TI,Wald DJ.Evaluation of Ground-Motion Modeling Techniques for Usein Global Shake Map:ACritique of Instrumental Ground-Motion Prediction Equations,Peak Ground Motion to Macroseismic In-tensity Conversions,and Macroseismic Intensity Predictions in Different Tectonic Settings.USGS Open-File Report 2009-1047,2009,114 pp
[9]Wald DJ,Lin K-W,Quitoriano V.Quantifying and Qualifying USGS Shake Map Uncertainty.USGSOpen-File Report 2008-1238,2008,26 pp
[10]Polet J,Thio H K.Rapid characterization of a centroid moment tensor and waveheight predictions a-round the north Pacific for the 2011 Tohoku earthquake.Earth,Planets and Space(forthcoming)
[11]Hayes G P,Wald DJ,Keranen K.Advancing techniques to constrain the geometry of the seismic rup-ture plane on subduction interfaces a priori:Higher-order functional fits.Geochemistry,Geophysics,Geosystems,2009,10;doi:10.1029/2009GC002633
[12]Kanamori H,Given J W.Use of long-period surface waves for rapid determination of earthquake sourceparameters.Physics of the Earth and Planetary Interiors,1981,27:8-31
[13]Dziewonski A M,Anderson D L.Preli minary Reference Earth Model(PREM).Physics of the Earth andPlanetary Interiors,1981,25:297-356
[14]Hayes G P.Rapid source characterization of the 03-11-2011MW9.0 Tohoku Earthquake.Earth,Planetsand Space(forthcoming)
[15]Wessel P,Smith W HF.Free software helps map and display data.Eos,Transactions,American Geo-physical Union,1991,72:445-446(原文中致谢———译者注)
版权所有：© 2023 中国地质图书馆 中国地质调查局地学文献中心