引文
[1]Chen P,Jordan T H,Zhao L.Finite-Moment Tensor of the3September 2002 Yorba Linda Earthquake.Bull.Seism.Soc.Amer.,2005,95(3):1170-1180.
[2]Wallace T,Helmberger D.Determining source parameters ofmoderate-size earthquakes from regional waveforms.Phys.Earth Planet.Inter.,1982,30(2-3):185-196.
[3]许忠淮,汪素云,黄雨蕊等.由大量的地震资料推断的我国大陆构造应力场.地球物理学报,1989,32(6):636-647.Xu Z H,Wang S Y,Huang Y R,et al.The tectonic stressfield of Chinese continent deduced from a great number ofearthquakes.Chinese J.Geophys.(in Chinese),1989,32(6):636-647.
[4]郑勇,马宏生吕坚等.汶川地震强余震(Ms≥5.6)的震源机制解及其与发震构造的关系.中国科学(D辑),2009,39(4):413-426.Zheng Y,Ma H S,LüJ,et al.Relations between sourcemechanisms and seismogenic structures of Wenchuan earthquake′sstrong aftershocks.Sci.China Ser.D-Earth Sci.,(in Chinese),2009,53(1):54-63.
[5]Nakano H.Notes on the nature of the forces which give riseto the earthquake motions.Seismol.Bull.Centr.Meteorol.Obs.Japan,1923,1:92.
[6]Hardebeck J L,Shearer P M.A new method for determiningfirstmotion focal mechanisms.Bull.Seism.Soc.Amer.,2002,92(6):2264-2276.
[7]胡幸平,俞春泉,陶开等.利用P波初动资料求解汶川地震及其强余震震源机制解.地球物理学报,2008,51(6):1711-1718.Hu X P,Yu C Q,Tao K,et al.Focal mechanism solutionsof Wenchuan earthquake and its strong aftershocks obtainedfrom initial P wave polarity analysis.Chinese J.Geophys.(in Chinese),2008,51(6):1711-1718.
[8]Hardebeck J L,Shearer P M.Using S/P amplitude ratios toconstrain the focal mechanisms of small earthquakes.Bull.Seism.Soc.Amer.,2003,93(6):2434-2444.
[9]Julian B R,Foulger G R.Earthquake mechanisms fromlinear-programming inversion of seismic-wave amplitude.Bull.Seism.Soc.Amer.,1996,86(4):972-980.
[10]Dreger D,Helmberger D.Determination of source parameters atregional distances with three-component sparse network data.J.Geophys.Res,1993,98(B5):8107-8125.
[11]吴建平,明跃红,张恒荣等.2002年夏季长白山天池火山区的地震活动研究.地球物理学报,2005,48(3):621-628.Wu J P,Ming Y H,Zhang H R,et al.Seismic activity at theChangbaishan Tianchi volcano in the summer of 2002.Chinese J.Geophys.(in Chinese),2005,48(3):621-628.
[12]Nábělek J,Xia G.Moment-tensor analysis using regionaldata:Application to the 25 March,Scotts Mills,Oregon,Earthquake.Geophys.Res.Lett.,1993,22(1):13-16.
[13]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.
[14]Kanamori H,Given J W.Use of long-period surface wavesfor rapid determination of earthquake-source parameters.Phys.Earth Planet.Inter.,1981,27(1):8-31.
[15]Kanamori H,Rivera L.Source inversion of W phase:speeding up seismic tsunami warning.Geophys.J.Int.,2008,175(1):222-238.
[16]Zhao L S,Helmberger D.Source estimation from broadbandregional seismograms.Bull.Seism.Soc.Amer.,1994,84:91-104.
[17]Geiger L.Probability method for the determination ofearthquake epicenters from the arrival time only.Bull.St.Louis Univ.,1912,8:60-71.
[18]Douglas A.Joint epicenter determination.Nature,1967,215(5096):47-48.
[19]Spence W.Relative epicenter determination using P-wavearrival-time differences.Bull.Seism.Soc.Am.,1980,70(1):171-183.
[20]Zhan Z,Wei S,Ni S,et al.Earthquake centroid locationsusing calibration from ambient seismic noise.Bull.Seisml.Soc.Am.,2011,101(3):1438-1445.
[21]Xie J,Zeng X F,Chen W W,et al.Comparison of groundtruth location of earthquake from InSAR and from ambientseismic noise:A case study of the 1998Zhangbei earthquake.Earthq.Sci.,2011,24(2):239-247.
[22]Uski M,Hyvonena T,Korjaa A,et al.Focal mechanisms ofthree earthquakes in Finland and their relation to surfacefaults.Tectonophysics,2003,363(1-2):141-157.
[23]Saikia C K.A method for path calibration using regional andteleseismic broadband seismograms:application to the 21May 1997Jabalpur,India earthquake(Mw5 8).Curr.Sci.,2000,79(9-10):1301-1315.
[24]Bent A L,Perry H K C.Depths of eastern Canadianearthquakes from regional data.Seism.Res.Lett.,2002,73(2):273-284.
[25]Bock G,Grfinthal G,Wylegalla K.The 1985/86 WesternBohemia earthquakes:Modelling source parameters withsynthetic seismograms.Tectonophysics,1996,261(1-3):139-146.
[26]高立新,刘芳,赵蒙生等.用sPn震相计算震源深度的初步分析与应用.西北地震学报,2007,29(3):213-244.Gao L X,Liu F,Zhao M S,et al.Primary analysis on theseismic source depth determination using sPn phase and itsapplication.Northwestern Seismological Journal(in Chinese),2007,29(3):213-244.
[27]房明山,杜安陆,董孝平等.用sPn震相测定近震震源深度.地震地磁观测与研究,1995,16(5):13-18.Fang M S,Du A L,Dong X P,et al.Determination of focaldepth with the sPn phase(in Chinese).Seismol GeomagObser Res.(in Chinese),1995,16(5):13-18.
[28]Engdahl E R,van der Hilst R,Buland R.Global teleseismicearthquake relocation with improved travel times andprocedures for depth determination.Bull.Seism.Soc.Am.,1998,88(3):722-743.
[29]Keilis-Borok V I,Yanovskaya T B.Dependence of thespectrum of surface waves on the depth of the focus withinthe Earth′S crust.Bull.Acad.Sci.USSR.Geophys.Set.,(English Transl.),1962,11:1532-1539.
[30]Tsai Y B,Aki K.Simultaneous determination of the seismicmoment and attenuation of seismic surface waves.Bull.Seism.Soc.Am.,1969,59(1):275-287.
[31]陈纬苍.2010-03-04高雄甲仙地震灾情评估报告.https://conf.ncree.org.tw/download%5CA0990322-高雄甲仙地震_災情評估-Mr.Chen.pdf.Chen W C.Condition of disaster reporting of 2010-03-04Kaohsiung Earthquake[R/OL](in Chinese).https://conf.ncree.org.tw/download%5CA0990322-高雄甲仙地震_災情評估-Mr.Chen.pdf.
[32]Zhu L,Helmberger D V.Advancement in source estimationtechniques using broadband regional seismograms.Bull.Seism.Soc.Am.,1996,86(5):1634-1641.
[33]Zhu L,Rivera L A.A note on the dynamic and staticdisplacements from a point source in multilayered media.Geophysical Journal International,2002,148(3):619-627.
[34]Kikuchi M,Kanamori H.Inversion of complex body waves.Bulletin of the Seismological Society of America,1982,72(2):491-506.
[35]Langston C A.Structure under Mount rainier,Washington,Inferred From Teleseismic Body Waves.J.Geophys.Res.,1979,84(B9):4749-4762.
[36]Baag C E,Langston C A.A WKBJ spectral method forcomputation of SV synthetic seismograms in a cylindricallysymmetric medium.Geophysical Journal of the RoyalAstronomical Society,1985,80(2):387-417.
[37]http://igppweb.ucsd.edu/-gabi/rem.html
[38]http://geophysics.ou.edu/solid_earth/prem.html
[39]Wells D L,Coppersmith K J.New empirical relationshipsamong magnitude,rupture length,rupture width,rupturearea,and surface displacement.Bulletin of the SeismologicalSociety of America,1994,84(4):974-1002.
[40]Langston C A.Depth of faulting during the 1968Meckering,Australia,earthquake sequence determined from waveformanalysis of local seismograms.Journal of GeophysicalResearch,1987,92(B11):11561-11 574.
[41]Fan G,Wallace T.The determination of source parametersfor small earthquakes from a single,very broadband seismicstation.Geophys.Res.Lett.,1991,18(8):1385-1388.
[42]Fan G,Wallace T.Focal mechanism of a recent event in SouthAfrica:a study using a sparse very broadband network.International Journal of Rock Mechanics and MiningSciences and Geomechanics Abstracts,1996,33(7):295A-295A.
[43]Bowers D.The October 30,1994,Seismic disturbance inSouth Africa:Earthquake or large rock burst?J.Geophys.Res.,1997,102(B5):9843-9857.
[44]韦生吉,倪四道,崇加军等.2003年8月16日赤峰地震:一个可能发生在下地壳的地震?地球物理学报,2009,52(1):111-119.Wei S J,Ni S D,Chong J J,et al.The 16 August 2003Chifeng earthquake:Is it a lower crust earthquake?ChineseJ.Geophys.(in Chinese),2009,52(1):111-119.
[45]Efron B.Bootstrap methods:Another look at the jackknife.The Annals of Statistics,1979,7(1):1-26.
[46]Wang S Y,Xu Z H,Pei S P.Velocity structure ofuppermost mantle beneath North China from Pn tomographyand its implications.Science in China Series D:EarthSciences.,2003,46(2):130-140.
[47]裴顺平,刘杰,马宏生等.川滇地区横波Q值动态变化.地球物理学报,2010,53(7):1639-1652.Pei S P,Liu J,Ma H S,et al.Dynamic variation of S-waveQvalue beneath Sichuan-Yunnan,China.Chinese J.Geophys.(in Chinese),2010,53(7):1639-1652.