引文
[1] 崔效峰,谢富仁,张红艳.川滇地区现代构造应力场分区及动力学意义.地震学报,2006,28(5) :451~461CuiX F,Xie F R,Zhang H Y.Recent tectonic stress field zoning in Sichuan-Yunnan region and its dynamic interest.Acta Seismologica Sinica (in Chinese),2006,28(5) :451 ~461
[2] 刁桂苓,王海涛,高国英等.伽师强震系列应力场的转向过程.地球物理学报,2005,48(5) :1062~1068Diao G L,Wang H T,Gao G Y,et al.A deflection process for the stress field of the Jiashi strong earthquake sequence.Chinese J.Geophys.(in Chinese),2005,48(5) :1062~ 1068
[3] 许忠淮,汪素云,黄雨蕊等.由多个小震推断的青甘和川滇地区地壳应力场的方向特征.地球物理学报,1987,30(5) : 476~486Xu Z H,Wang S Y,Huang Y R,et al.Directions of mean stress axes in southwestern China deduced from microearthquake data.Chinese J.Geophys.(in Chinese),1987,30(5) :476~486
[4] Yukutake Y,Iio Y,Katao H,et al.Estimation of the stress field in the region of the 2000 Western Tottori Earthquake:Using numerous aftershock focal mechanisms.J.Geophys.Res.,2007,112,B09306,doi:10. 1029/2005JB004250
[5] Zoback M L.Stress field constraints on intraplate seismicity in eastern north America.J.Geophys.Res.,1992,97:11761~ 11782
[6] 谢富仁,祝景忠,梁海庆等.中国西南地区现代构造应力场基本特征.地震学报,1993,15(4) :407~417Xie F R,Zhu J Z,Liang H Q,et al.Characteristics of modern tectonic stress field in southwestern China.Acta Seismologica Sinica (in Chinese),1993,15(4) :407 ~417
[7] 许忠淮.用滑动方向拟合法反演唐山余震区的平均应力场.地震学报,1985,7(4) :349~361Xu Z H.Mean stress field in Tangshan aftershock area obtained from focal mechanism data by fitting slip directions.Acta Seismologica Sinica (in Chinese),1985,7(4) :349~361
[8] Angelier J.Tectonic analysis of fault slip data sets.J.Geophys.Res.,1984,89(B7) I:5836~5848
[9] Etchcopar A,Vasseur G,Daignieres M.An inverse problem in microtectoaics for the determination of stress tensors from fault striation analysis.Struct.,1981,3(1) :51~55
[10] 李方全.套芯法、水压致裂法原地应力测量、钻孔崩落及震源 机制解分析所得结果的比较.地震学报,1992,14(2) :149~155Li F Q.A comprison of crustal stress measurement result with overcoring method,hydraulic fracturing technique,borehole breakout and focal mechanism solutions analysis.Acta Seismologica Sinica (in Chinese),1992,14(2) :149 ~155
[11] 赵建涛,崔效锋,谢富仁.唐山地震震源区构造应力场强度的初步分析.地震学报,2002,24(3) :268~276Zhao J T,Cui X F,Xie F R.Preliminary analysis of the tectonic stress inten-sity in the source region of Tangshanearthquake.Acta Seismologica Sinica (in Chinese),2002,24(3) :268~276
[12] 徐纪人,赵志新.深井地震:地球物理长期观测与研究--现代地球科学的新进展.地质论评,2004,50(5) :537~553Xu J R,Zhao Z X.Seismic:Geophysic long term observe and study on deep drills:advances of mordern geosciences.Geological Review (in Chinese),2004,50(5) :537~553
[13] Zoback M D,Apel R,Eaumgartner J,et al.Upper-crustal strength inferred from stress measurements to 6 km depth inthe KTB borehole.Nature,1993,365:633~635
[14] 万永革.根据大地震前后应力轴偏转和应力降求取应力量值的研究.地震学报,2006,28(5) :472~477Wan Y G.Study on determination of stress level by seismic stress drops and the stress axis deflections before and after large earthquakes.Acta Seismologica Sinica (in Chinese),2006,28(5) :472~477
[15] Wesson R L,Boyd O S.Stress before and after the 2002 Denali fault earthquake.Geophys.Res.Lett.,2007,34:L07303,doi:10. 1029/2007GL029189
[16] 万永革,沈正康,曾跃华等.青藏高原东北部的库仑应力积累演化对大地震发生的影响.地震学报,2007,29(2) :115~ 129Wan Y G,Shen Z K,Zeng Y H,et al.Evolution of cumulative coulomb failure stress in northeastern Qinghai-Xizang (Tibetan) Plateau and its effect on l.arge earthquake occurrence.Acta Seismologica Sinica (in Chinese),2007,29(2) :115~129
[17] 万永革,沈正康,尚 丹.2005年10月巴基斯坦Mw7. 6地震对余震的触发研究.中国地震,2006,22(3) :277~286Wan Y G,Shen Z K,Shang D.Study on triggering effect of the October,2005 Pakistan Mw7. 6 earthquake on its aftershocks.Earthquake Research in China (in Chinese),2006,22(3) :277~286
[18] Deng J,Sykes L R.Stress evolution in southern California and triggering of moderate-,small-,and micro-size earthquakes.J.Geophys.Res.,1997,102:2441~2443
[19] Kagan Y Y,Jackson D D,Liu Z.Stress and earthquakes in southern California,1850 ~ 2004. J.Geophys.Res.,2005. 110:B05S14,doi:10. 1029/2004JB003313
[20] Dieterich J H.A constitutive law for rate of earthquake production and its application to earthquake clustering.J.Geophys.Res.,1994,99(B2) :2601~2618
[21] Marsan D.The role of small earthquakes in redistributing crustal elastic stress.Geophys.J.Int.,2005,163:141 ~151
[22] Reasenberg P A,Simpson R W.Response of regional seismicity to the static stress change produced by the Loma Prieta earthquake.Science,1992,255:1687 ~ 1690
[23] King G C,Stein R S,Lin J.Static stress changes and the triggering of earthquakes.Bulletin of the Seismological Society of America,1994,84:935~953
[24] Engdahl E R,Billington S,Kisslinger C.Teleseismically recorded seismicity before and after the May 7,1986,Andreanof Islands,Alaska,earthquake.J.Geophys.Res.,1989,94:15481~ 15498
[25] Tajima,Kanamori H.Global survey of aftershock area expansion patterns.Phys.Earth Planet.Inter.,1985,40:77~134
[26] McCloskey J,Nalbant S S,Steacy S,et al.Structural constraints on the spatial distribution of aftershocks.Geophys.Res.Lett.,2003,30(12) :1610,doi:10. 1029/ 2003GL017225
[27] Gross S J,Kisslinger C.Stress and the spatial distribution of seismicity in the central Aleutians.J.geophys.Res.,1994,99(B8) :15291~15303
[28] Gross S J,Kisslinger C.Estimating tectonic stress rate and state with Landers aftershocks.J.Geophys.Res.,1997,102:7603 ~ 7612
[29] 韩竹军,虢顺民.1996年2月3 日云南丽江7. o级地震发生的构造环境.地震学报,2004,26(4) :410~418Han Z J,Guo S M.Seismotectonic environment of occurring the February 3,1996 Lijiang M7. 0 earthquake,Yunnan Province.Acta Seismologica Sinica (in Chinese),2004,26(4) :410~418
[30] 云南省地震局.一九九六年丽江地震滇西地震预报实验场.北京:地震出版社,1998Earthquake Administration of Yunnan Province.Lijiang Earthquake,Feb.3rd,1996(in Chinese).Beijing:Seismological Press.1998
[31] Okada Y.Internal deformation due to shear faults and tensile in a half space.Bulletin of the Seismological Society of America,1992,82:1018 ~ 1040
[32] gross S J.A model of tectonic stress state and rate using the 1994 northridge earthquake sequence.Bulletin of the Seismilogical Society of America.91(2) :263~275
[33] 陈棋福.中国震例(1995~1996) .北京:地震出版社,2002Chen Q F.Earthquake Cases in China,1995~1996 (in Chinese).Beijing:Seismologial Press,2002
[34] 国家地震局地质研究所、云南省地震局.滇西北地区活动断裂.北京:地震出版社,1986Institute of Geology,CEA,Earthquake Administration of Yunnan Province.Active Faults in Northwestern Yunnan (in Chinese).Beijing:Seismological Press,1986
[35] 朱艾斓,徐锡伟,周永胜等.川西地区小震重新定位及其活动构造意义.地球物理学报,2005,48(3) :629~636Zhu A L,Xu X W,Zhou Y S,et al.Relocation of small earthquakes in western Sichuan,China and its implications for active tectonics.Chinese J.Geoph ys.(in Chinese),2005,48(3) :629~636
[36] 苏有锦,刘祖荫.丽江7. 0级地震震源环境及其破裂过程讨论.地震研究,1997,20(1) :66~71Su Y J,Liu Z Y.Discussion on the source environment and rupture process of the M7. 0 Lijiang earthquake.Journal of Seismological Research (in Chinese),1997,20(1) :66~71
[37] 刘祖荫,苏有锦,秦嘉政等.20世纪云南地震活动.北京:地震出版社,2002Liu Z Y,Su Y J,Qin J Z,et al.Study on Seismicity in Yunnan in the 20th Century (in Chinese).Beijing:Seismological Press,2002
[38] 许力生,陈运泰,S.Fasthof.1996年2月3目云南丽江7. 0 地震震源过程时空复杂性-中国地震学研究进展.北京:地震出版社,1997. 91~105Xu L S,Chen Y T,Fasrhof S.The Temporal and Spatial Complexity of Source Process of Ms7. 0 Earthquake,Feb.3rd,1996,Lijiang,Yunnan:Advances of Seismology Research in China(in Chinese).Beijing:Seismological Press,1997. 91~105
[39] 徐扬.1996年2月3日云南丽江地震震源过程的体波反演.地震学报,1998,20(2) :113~117Xu Y.Bodywave inversion of source process for Feb.3rd,1996,Lijiang earthquake,Yunnan.Acta Seismologica Sinica (in Chinese),1998,20 (2) :113 ~ 117
[40] 苏生瑞,王运生.丽江地震区应力场研究.地质论评,2004,50(1) :57~64Su S R,Wang Y S.A study on the stress field in the region of the Lijiang earthquake.Geological Review (in Chinese),2004,50(1) :57~64
[41] 王绍晋,龙晓帆,罗淑进.丽江地震序列的震源机制,发震应力场和破裂特征.地震研究,1997,20(1) :26~34Wang S J,Long X F,Lou S J.The focal mechanism,seismogenic stress field and rupture characteristics of the Lijiang earthquake sequence.Journal of Seismological Research (in Chinese),1997,20(1) :26~ 34