引文
[1]国家地震局震害防御司.中国历史强震目录(公元前23世纪—公元1911年).北京:地震出版社,1995.Disaster Prevention Department of China EarthquakeAdministration.China Historical Earthquake Catalog(23rdCentury BC—1911AD)(in Chinese).Beijing:SeismologicalPress,1995.
[2]Musson R M W,Jeménes M J.Macroseismic estimation ofearthquake parameters.Sixth Framework Programme Report,2008.
[3]Bakun W H,Wentworth C M.Estimating earthquakelocation and magnitude from seismic intensity data.Bull.Seismol.Soc.Am.,1997,89(2):557.
[4]Bakun W H,Cópera A G,Stucchi M.Epistemic uncertaintyin the location and magnitude of earthquakes in Italy frommacroseismic data.Bull.Seismol.Soc.Am.,2011,101(6):2712-2725.
[5]陈培善.震源机制与烈度分布的关系(二).地球物理学报,1977,20(1):9-19.Chen P S.Relation between the seismic source mechanismand the intensity distribution(continued).Chinese J.Geophys.(Acta Geophysica Sinica)(in Chinese),1977,20(1):9-19.
[6]Sirovich L.A simple algorithm for tracing syntheticisoseismals.Bull.Seismol.Soc.Am.,1996,86(4):1019-1027.
[7]Fitzko F,Suhadolc P,Audia A,et al.Constraints on thelocation and mechanism of the 1511 Western-Sloveniaearthquake from active tectonics and modeling ofmacroseismic data.Tectonophysics,2005,404(1-2):77-90.
[8]Nunziata C,Sacco C,Panza G F.Modeling of ground motionat Napoli for the 1688scenario earthquake.Pure.Appl.Geophys.,2010,doi:10.1007/s00024-010-0113-1.
[9]周青云,周仕勇,陈棋福等.正演推算1730年北京西郊地震的发震断层和滑动角.地震研究,2008,31(4):369-376.Zhou Q Y,Zhou S Y,Chen Q F,et al.Forward inference ofthe causative fault and the slip angles of the faults of the 1730western Beijing earthquake.J.Seism.Res.(in Chinese),2008,31(4):369-376.
[10]Ding Z,Romanelli F,Chen Y T,et al.Realistic modeling ofseismic wave ground motion in Beijing city.Pure.Appl.Geophys.,2004,161(5-6):1093-1106,doi:10.1007/s00024-003-2498-6.
[11]Emolo A,Zollo A.Kinematic source parameters for the 1989Loma Prieta earthquake from the nonlinear inversion ofaccelerograms.Bull.Seismol.Soc.Am.,2005,95(3):981-994.
[12]Scherbaum F,Delavaud E,Riggelsen C.Model selection inseismic hazard analysis:An information-theoretic perspective.Bull.Seismol.Soc.Am.,2009,99(6):3234-3247.
[13]Burnham K P,Anderson D R.Model Selection and Multi-model Inference,A Practical Information-Theoretic Approach,2nd ed.New York:Springer-Verlag,2002.
[14]Akaike H.A new look at the statistical model identification.IEEE Trans.Autom.Control,1974,19(6):716-723.
[15]Liu L B,Arcone S A.Propagation of radar pulses from ahorizontal dipole in variable dielectric ground:A numericalapproach.Subsurface Sensing Technologies and Applications,2005,6(1):15-24.
[16]Aki K,Richards P G.Quantitative Seismology,2nd ed.Sausalito,California:University Science Books,2002.
[17]中国地震局监测预报司.一九九八年张北地震.北京:地震出版社,1998:2.Monitoring and Forecasting Department of China EarthquakeAdministration.1998 Zhangbei Earthquake(in Chinese).Beijing:Seismological Press,1998:2.
[18]黄建平,倪四道,傅容珊等.综合近震及远震波形反演2006文安地震(Mw5.1)的震源机制解.地球物理学报,2009,52(1):120-130.Huang J P,Ni S D,Fu R S,et al.Source mechanism of the2006 Mw5.1 Wen′an Earthquake determined from a jointinversion of local and teleseismic broadband waveform data.Chinese J.Geophys.(in Chinese),2009,52(1):120-130.
[19]Ma S,Custódio S,Archuleta R J,et al.Dynamic modelingof the 2004 Mw6.0 Parkfield,California,earthquake.J.Geophys.Res.,2008,113:B02301,doi:10.1029/2007JB005216.
[20]Mendoza C,Hartzell S.Finite-fault analysis of the 2004Parkfield,California,earthquake using pnl waveforms.Bull.Seismol.Soc.Am.,2008,98(6):2746-2755.
[21]Custódio S,Liu P C,Archuleta R J.The 2004 Mw6.0Parkfield,California,earthquake:Inversion of near-sourceground motion using multiple data sets.Geophys.Res.Lett.,2005,32(23):L23312,doi:10.1029/2005GL024417.
[22]McEvilly T V,Bakun W H,Casaday K B.The Parkfield,California,earthquakes of 1966.Bull.Seismol.Soc.Am.,1967,57(6):1221-1244.
[23]Wu F T.Parkfield earthquake of June 28,1966:magnitudeand source mechanism.Bull.Seismol.Soc.Am.,1968,58(2):689-709.
[24]梁富康,于兴河,李先平等.冀中坳陷深县凹陷的生长断层特点及其对沉积的控制作用.中国地质,2011,8(2):263-270.Liang F K,Yu X H,Li X P,et al.Growth faults inShenxian depression and their control over the sedimentation.Geology in China(in Chinese),2011,8(2):263-270.
[25]杨旭升,刘池阳,杨斌谊等.冀中坳陷衡水转换断裂带特征及演化.煤田地质与勘探,2004,32(3):5-8.Yang X S,Liu C Y,Yang B Y,et al.Characteristics andevolution of Hengshui transfer fault zones in Jizhongdepression.Coal Geology&Exploration(in Chinese),2004,32(3):5-8.
[26]龙峰,闻学泽,徐锡伟.华北地区地震活断层的震级-破裂长度、破裂面积的经验关系.地震地质,2006,28(4):511-535.Long F,Wen X Z,Xu X W.Empirical relationships betweenmagnitude and rupture length,and rupture area,forseismogenic active faults in North China.Seismology andGeology(in Chinese),2006,28(4):511-535.
[27]张秀梅.河北省地震资料汇编.北京:地震出版社,1990:324-327.Zhang X M.Hebei Earthquake Material Collection(inChinese).Beijing:Seismological Press,1990:324-327.