引文
[1]Nettles M,Ekstrom G,Koss H C.Centroid-moment-tensoranalysis of the 2011 Tohoku earthquake and its largerforeshocks and aftershocks.Earth Planets Space,2011,99(1-9):1-8.
[2]Dziewonski A M,Chou T A,Woodhouse J H.Determinationof earthquake source parameters from waveform data forstudies of global and regional seismicity.J.Geophys.Res.,1981,86(B4):2825-2852.
[3]Arvidsson R,Ekstrom G.Global CMT analysis of moderateearthquake,Mw≥4.5,using intermediate-period surfacewaves.Bull.Seism.Soc.Am.,1998,88(4):1003-1013.
[4]Ekstrom G,Dziewoński A M,Maternovskaya N N,et al.Global seismicity of 2003:centroid-moment-tensor solutionsfor 1087earthquakes.Phys.Earth Planet.Inter.,2005,148(2-4):327-351.
[5]Hayes G P,Earle P S,Benz H M,et al.88Hours:The U.S.geological survey national earthquake information centerresponse to the 11 March 2011 Mw9.0Tohoku earthquake.Seismol.Res.Lett.,2011,82(4):481-493.
[6]Sipkin S A.Estimation of earthquake source parameters bythe inversion of waveform data:synthetic waveforms.Phys.Earth Planet.Inter.,1982,30(2-3):242-259.
[7]Sipkin S A.Estimation of earthquake source parameters bythe inversion of waveform data:Global seismicity,1981—1983.Bull.Seism.Soc.Am.,1986,76(6):1515-1541.
[8]Sipkin S A.Rapid determination of global moment-tensorsolutions.Geophys.Res.Lett.,1994,21(16):1667-1670.
[9]Duputel Z,Rivera L,Kanamori H,et al.Real-time W phaseinversion during the 2011off the Pacific coast of Tohokuearthquake.Earth Planets Space,2011,63(7):535-539.
[10]W Phase source inversion results 3/11/2011(Mw9.0),Tohoku-oki,Japan.http://eost.u-strasbg.fr/wphase/tohoku_oki_2011/UPDATED.
[11]Shao G F,Li X Y,Ji C,et al.Focal mechanism and sliphistory of the 2011 Mw9.1off the Pacific coast of Tohokuearthquake,constrained with teleseismic body and surfacewaves.Earth Planets Space,2011,63(7):559-564.
[12]Hayes G P.Rapid source characterization of the 2011 Mw9.0off the Pacific coast of Tohoku earthquake.Earth PlanetsSpace,2011,63(7):529-534.
[13]陈运泰.地震参数:数字地震学在地震预测中的应用.北京:地震出版社,2003.Chen Y T.Parameters of Earthquake-Application of DigitalSeismology in Earthquake Prediction(in Chinese).Beijing:Seismological Press,2003.
[14]Stein S,Okal E A.Seismology:Speed and size of theSumatra earthquake.Nature,2005,434(7033):581-582.
[15]Ammon C J,Ji C,Thio H K,et al.Rupture process of the2004 Sumatra-Andaman earthquake.Science,2005,308(5725):1133-1139.
[16]Lay T,Kanamori H,Ammon C J,et al.The great Sumatra-Andaman earthquake of 26December 2004.Science,2005,308(5725):1127-1133.
[17]Giardini D,Li X D,Woodhouse J H.Three-dimensionalstructure of the Earth from splitting in free-oscillationspectra.Nature,1987,325(6103):405-411.
[18]Laske G,Masters G.Limits on differential rotation of theinner core from an analysis of the Earth′s free oscillations.Nature,1999,402(6757):66-69.
[19]Ishii M,Tromp J.Normal-mode and free-air gravityconstraints on lateral variations in velocity and density ofEarth′s mantle.Science,1999,285(5431):1231-1236.
[20]Hu X G,Liu L T,Sun H P,et al.Wavelet filter analysis ofsplitting and coupling of seismic normal modes below 1.5mHz with superconducting gravimeters after the December26,2004Sumatra earthquake.Science in China Series D:Earth Sciences,2006,49(12):1259-1269.
[21]Hu X G,Liu L T,Hinderer J,et al.Wavelet filter analysisof local atmospheric pressure effects on gravity variations.J.Geodesy,2005,79(8):447-459.
[22]Hu X G,Liu L T,Hinderer J,et al.Wavelet filter analysisof atmospheric pressure effects in the long-period seismicmode band.Phys.Earth Planet.Inter.,2006,154(1):70-84.
[23]Aki K,Richards P G.Quantitative Seismology:Theory andMethods.San Francisco:W.H.Freeman,1980.
[24]Helffrich G R.How good are routinely determined focalmechanisms?Empirical statistics based on a comparison ofHarvard,USGS and ERI moment tensors.Geophys.J.Int.,1997,131(3):741-750.
[25]Kanamori H,Rivera L.Source inversion of W-phase:Speeding up seismic tsunami warning.Geophys.J.Int.,2008,175(1):222-238.
[26]Dziewonski A M,Anderson D L.Preliminary reference Earthmodel.Phys.Earth Planet.Inter.,1981,25(4):297-356.
[27]Kedar S,Watada S,Tanimoto T.The 1989Macquarie Ridgeearthquake:Seismic moment estimation from long-period freeoscillations.J.Geophys.Res.,1994,99(B9):17893-17907.
[28]Park J,Song T A,Tromp J,et al.Earth′s free oscillationsexcited by the 26 December 2004 Sumatra-Andamanearthquake.Science,2005,308(5725):1139-1144.
[29]Lambotte S,Rivera L,Hinderer J.Rupture length andduration of the 2004 Aceh-Sumatra earthquake from thephases of the Earth′s gravest free oscillations.Geophys.Res.Lett.,2006,33:L03307,doi:10.1029/2005GL024090.
[30]Shapiro N M,Ritzwoller M H.Monte-Carlo inversion for aglobal shear-velocity model of the crust and upper mantle.Geophys.J.Int.,2002,151(1):88-105.
[31]Tsai V C,Hayes G P,Duputel Z.Constraints on the long-period moment-dip tradeoff for the Tohoku earthquake.Geophys.Res.Lett.,2011,38:L00G17,doi:10.1029/2011GL049129.
[32]Banerjee P,Pollitz F F,Bürgmann R.The size and durationof the Sumatra-Andaman earthquake from far-field staticoffsets.Science,2005,308(5729):1769-1772.
[33]Pollitz F F,Bürgmann R,Banerjee P.Geodetic slip model ofthe 2011 M9.0Tohoku earthquake.Geophys.Res.Lett.,2011,38:L00G08,doi:10.1029/2011GL048632.
[34]Ammon C J,Lay T,Kanamori H,et al.A rupture model ofthe 2011off the Pacific coast of Tohoku earthquake.EarthPlanets Space,2011,63(7):693-696.