引文
[1]李钦祖.华北地壳应力场的基本特征.地球物理学报,1980,23(4):376~387Li Q Z.The basic character of crustal stress field in north China.Chinese J.Geophys.(in Chinese),1980,23(4):376~387
[2]李钦祖,靳雅敏,于新昌.华北地区的震源机制与地壳应力场.地震学报,1982,4(1):55~61Li QZ,Jin Y M,Yu XC.Focal mechanisms and crustal stressfield in north China.Acta Seismologica Sinica(in Chinese),1982,4(1):55~61
[3]崔效锋,谢富仁.1976年唐山地震前后华北地区现代构造应力场的时空变化特征.中国地震,2001,17(3):280~288Cui X F,Xie F R.The space-time variations of present tectonic stress field in North China before and after1976Tangshanearthquake.Earthquake Research in China(in Chinese),2001,17(3):280~288
[4]郭良迁.断层活动应力轴的确定及首都圈应力场.东北地震研究,1998,14(3):50~57Guo L Q.Determinatingstress axis of fault activity and stressfield of Capital Circle.Seismological Research of Northeast China(in Chinese),1998,14(3):50~57
[5]徐锡伟,吴卫民,张先康等.首都圈地区地壳最新构造变动与地震.科学出版社,2002Xu X W,Wu W M,Zhang X K,et al.New Changing of Crustal Tectonic and Earthquakes in Capital Circal(in Chinese).Science Press,2002
[6]Crampin S.Seismic wave propagation through a crack solid:polarization as a possible dilatancy diagnostic.Geophys.J.R.Astr.Soc.,1978,53(3):467~496
[7]Crampin S.Geological and industrial implications of extensive—dilatancy anisotropy.Nature,1987,328:491~496
[8]姚陈,王培德,陈运泰.卢龙地区S波偏振与上地壳裂隙各向异性.地球物理学报,1992,35(3):305~315Yao C,Wang P D,Chen Y T.Shear-wave polarization and crack induced anisotropyof upper crustin Lulong,north China.Chinese J.Geophys.(in Chinese),1992,35(3):305~315
[9]高原,郑斯华,孙勇.唐山地区剪切波分裂和地壳裂隙各向异性.地震学报,1995,17(3):283~293Gao Y,Zheng S H,Sun Y.Crack-induced anisotropy in the crust fromshear wave splitting observedin Tangshanregion,North China.Acta Seismologica Sinica(in Chinese),1995,17(3):283~293
[10]雷军,王培德,姚陈等.云南剑川近场横波特征及其与构造的关系.地球物理学报,1997,40(6):791~801Lei J,Wang P D,Yao C,et al.The near-field shear wave splitting and its relation with structure in Jianchuan,Yunnan province.Chinese J.Geophys.(in Chinese),1997,40(6):791~801
[11]赖院根,刘启元,陈九辉等.新疆伽师强震群区的横波分裂与应力场特征.地球物理学报,2002,45(1):83~92Lai Y G,Liu Q Y,Chen J H,et al.Features of the shear-wave splitting and stress field in the Xinjiang-Jishi strong earthquake region.Chinese J.Geophys.(in Chinese),2002,45(1):83~92
[12]高文学,马瑾.首都圈地震地质环境与地震灾害.地震出版社,1993Gao W X,Ma J.Seismo-Geological Background and Earthquake Hazardin Beijing Area.Beijing:Seismological Press,1993
[13]徐杰,宋长青,楚全芝.张家口-蓬莱断裂带地震构造序列的初步探讨.地震地质,1998,20(2):146~154Xu J,Song C Q,Chu QZ.Preliminary study onthe seismo-tectonic characters of the Zhangjiakou-Penglai fault zone.Seismology and Geology(in Chinese),1998,20(2):146~154
[14]Liu E,Crampin S.Effects of the internal shear wave window:comparison with anisotropyinduced splitting.Geophys.J.R.Astr.Soc.,1990,95:11275~11282
[15]Evans R.Effects of the free surface on shear-wave trains.Geophys.J.R.Astr.Soc.,1984,76(1):165~172
[16]Booth D C,Crampin S.Shear-wave polarizations on a curved wavefront at anisotropic free-surface.Geophys.J.R.Astr.Soc.,1985,83(1):31~45
[17]Chen TC,Booth D C,Crampin S.Shear-wave polarization near the North Anatolian Fault-III,observations of temporal changes.Geophys.J.R.Astr.Soc.,1987,91(2):287~311
[18]Bowman R J,Ando M.Shear-wave splitting in the upper mantle wedge above the Tonga subduction zone.Geophys.J.R.Astr.Soc.,1987,88(1):25~41
[19]Melosh H J,Raefsky A.A simple and efficient method for introducingfaults intofinite element computations.BSSA,1981,71(5):1391~1400
[20]宋惠珍,兰印刚,徐鹏飞等.1303年洪洞8级地震震源过程研究.地震地质,1995,17(1):13~24Song HZ,Lan YG,Xu PF,et al.Analysis of Hongdong1303M8earthquake processes.Seismology and Geology(in Chinese),1995,17(1):13~24
[21]刘洁,宋惠珍.低速体与深浅断裂共同孕震过程的数值模拟初步研究.地震地质,2002,24(3):355~367LiuJ,Song HZ.Anumerical simulation of seismogenic process of lowvelocity body and deep and shallowactive faults.Seismologyand Geology(in Chinese),2002,24(3):355~367
[22]刘洁,宋惠珍.用数值模拟方法评估华北北部地震危险性.地震地质,1999,21(3):221~228LiuJ,Song HZ.Estimation of earthquake risk for northern North China by numerical modeling.Seismology and Geology(in Chinese),1999,21(3):221~228
[23]刘昌铨,刘明军,嘉世旭.利用华北北部深部地球物理资料数值模拟地壳应力场.地震学报,1998,20(3):240~249Liu C Q,Liu MJ,Jia S X.Simulationthe North China crustal stress fields using geophysical data.Acta Seismologica Sinica(in Chinese)1998,20(3):240~249
[24]陈连旺,陆远忠,张杰等.华北地区三维构造应力场.地震学报,1999,21(2):140~149Chen L W,Lu Y Z,Zhang J,et al.3_D tectonic stress fields of North China.Acta Seismologica Sinica(in Chinese),1999,21(2):140~149
[25]邓起东,张裕明,许桂林,范福田.中国构造应力场特征及其与板块运动的关系.地震地质,1979,1(1):11~22Deng QD,Zhang Y M,Xu G L,Fan F T.On the tectonic stress fieldin China and its relation to plate movement.Seismology and Geology(in Chinese),1979,1(1):11~22
[26]刘洁,宋惠珍,巫映祥,刘贵梅.倾斜断层深部不均匀滑动的反演计算.地震地质,1995,17(1):25~31LiuJ,Song HZ,Wu Y X,Liu G M.Inversion of deep slip of inclined-fault from geodetic data.Seismology and Geology(in Chinese),1995,17(1):25~31