[1] ZOBACK M L. First-and second-order patterns of stress in the lithosphere：the World Stress Map Project[J]. Journal of Geophysical Research，1992，97(B8)：11 703–11 728.

[2] BARTON C A，ZOBACK M D，BURNS K L. In-situ stress orientation and magnitude at the Fenton geothermal site，New Mexico，determined from wellbore breakouts[J]. Geophysics Research Letter，1988，15(5)：467–470.

[3] ZOBACK M L，HEALY J H.In situ stress measurements to 3.5 km depth in the Cajon Pass scientific research borehole：implications for the mechanics of crustal faulting[J]. Journal of Geophysical Research，1992，97(B4)：5 039–5 057.

[4] VERNIK L，ZOBACK M D. Estimation of maximum horizontal principal stress magnitude from stress-induced well bore breakouts in the Cajon Pass scientific research borehole[J]. Journal of Geophysical Research，1992，97(B4)：5 109–5 119.

[5] TSUKAHARA H，IKEDA R，OMURA K. In-situ stress measurement in an earthquake focal area[J]. Tectonophysics，1996，262(1/4)：281–290.

[6] TSUKAHARA H，IKEDA R，YAMAMOTO K. In situ stress measurements in a borehole close to the Nojima Fault[J]. Island Arc，2001，10(3/4)：261–265.

[7] 李鹏武，崔军文，王连捷，等. 中国大陆科学钻探主孔钻孔崩落与现场应力状态的确定[J]. 岩石学报，2005，21(2)：421–426.(LI Pengwu，CUI Junwen，WANG Lianjie，et al. The determination of in-situ stress from well bore breakouts in the main borehole of the Chinese Continental Scientific Drilling[J]. Acta Petrologica Sinica，2005，21(2)：421–426.(in Chinese ))

[8] 李  宏，安其美，谢富仁. 福建沿海边缘陆域的原地应力测量研究[J]. 地震学报，2005，27(5)：508–514.(LI Hong，AN Qimei，XIE Furen. Study on in-situ stress measurement around coastal Marginal land in Fujian[J]. Acta Seismologica Sinica，2005，27(5)：508–514.(in Chinese))

[9] REYNOLDS S D，MILDREN S D，HILLIS R R，et al. Constraining stress magnitudes using petroleum exploration data in the Cooper Eromanga Basins，Australia[J]. Tectnophysics，2006，415(1/4)：123–140.

[10] WU H，MA K，ZOBACK M，et al. Stress orientations of Taiwan Chelungpu-fault drilling project(TCDP) hole——a as observed from geophysical logs[J]. Geophysics Research Letter，2007，34，L01303，doi：10.1029/2006GL028050.

[11] 谢富仁，李  宏. 利用断层滑动资料确定鲜水河断裂带现代构造应力的方向和大小[J]. 地震学报，1995，17(2)：164–171.(XIE Furen，LI Hong. Using fault slip data to determine the direction and level of tectonic stress in Xianshui River fault zone[J]. Acta Seismologica Sinica，1995，17(2)：164–171.(in Chinese ))

[12] PLENEFISCH T，BONJER K P. The stress field in the Rhine Graben area inferred from earthquake focal mechanisms and estimation of frictional parameters[J]. Tectonophysics，1997，275(1/3)：71–97.

[13] 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[J]. 地震学报，2002，24(3)：268–276.(ZHAO Jiantao，CUI Xiaofeng，XIE Furen. Preliminary analysis of the tectonic stress intensity in the source region of Tangshan earthquake[J]. Acta Seismologica Sinica，2002，24(3)：268–276.(in Chinese))

[14] SPUDICH P. On the inference of absolute stress levels from seismic radiation[J]. Tectonophysics，1992，211(1/4)：99–106.

[15] SPUDICH P，GUATTERI M，OTSUKI K，et al. Use os fault striations and dislocation models to infer tectonic shear stress during the 1995 Hyogo-ken Nanbu(Kobe) earthquake[J]. Bulletin of the Seismological Society of America，1998，88(2)：413–427.

[16] GUATTERI M，SPUDICH P. Coseismic temporal changes of slip direction：the effect of absolute stress on dynamic rupture[J]. Bulletin of the Seismological Society of America，1998，88(3)：777–789.

[17] WESSON R L，BOYD O S. Stress before and after the 2002 Denali fault earthquake[J]. Geophysics Research Letter，2007，34，L07303，doi：10.1029/2007GL029189.

[18] 万永革，沈正康，兰从欣. 根据走滑大地震前后应力轴偏转和应力降求取偏应力量值的研究[J]. 地球物理学报，2006，49(3)：838–844.(WAN Yongge，SHEN Zhengkang，LAN Congxin. Deviatoric stress level estimation according to principle axes rotation of stress field before and after large strike-slip type earthquake and stress drop[J]. Chinese Journal of Geophysics，2006，49(3)：838–844.(in Chinese))

[19] 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[J]. 地震学报，2006，28(5)：472–477.(WAN Yongge. Study on determination of stress level by seismic stress drops and the stress axis deflections before and after large earthquakes[J]. Acta Seismologica Sinica，2006，28(5)：472–477.(in Chinese))

[20] 华  卫，刘  杰，郑斯华，等. 2003年云南大姚6.2，6.1级地震序列特征分析及地震触发研究[J]. 中国地震，2006，22(1)：10–23. (HUA Wei，LIU Jie，ZHENG Sihua，et al. The characteristic analysis and seismic triggering study of the Dayao M6.2 and M6.1 earthquake sequences in 2003[J]. Earthquake Research in China，2006，22(1)：10–23.(in Chinese))

[21] 俞春泉，陶  开，崔效锋，等. 用格点尝试法求解P波初动震源机制解及解的质量评价[J]. 地球物理学报，2009，52(5)：1 402–1 411. (YU Chunquan，TAO Kai，CUI Xiaofeng，et al. P-wave first-motion focal mechanism solutions and their quality evaluation[J]. Chinese Journal of Geophysics，2009，52(5)：1 402–1 411.(in Chinese))

[22] 许忠淮，阎  明，赵仲和. 由多个小地震推断的华北地区构造应力场的方向[J]. 地震学报，1983，5(3)：268–279.(XU Zhonghuai，YAN Ming，ZHAO Zhonghe. Evaluation of the direction of tectonic stress in north China from recorded data of a large number of small earthquakes[J]. Acta Seismologica Sinica，1983，5(3)：268–279.(in Chinese))

[23] KNOPOFF L. Energy release in earthquakes[J]. Geophysical Journal Royal Astronomical Society，1958，(1)：44–52.

[24] 秦嘉政，叶建庆，蔡绍平，等. 云南大姚地震近源数字地震观测与现代新参数报告[M]. 北京：地震出版社，2005：39–384.(QIN Jiazheng，YE Jianqing，CAI Shaoping，et al. Yunnan Dayao earthquake digital seismic observation and modern new parameter report[M]. Beijing：Earthquake Press，2005：39–384.(in Chinese))

[25] DZIEWONSKI A M，ANDERSON D L. Preliminary reference earth model(PREM)[J]. Physics of the Earth and Planet Interiors，1981，25(4)：297–356.

[26] 万永革，沈正康，刁桂苓，等. 利用小震分布和区域应力场确定大震断层面参数方法及其在唐山地震序列中的应用[J]. 地球物理学报，2008，51(3)：793–804.(WAN Yongge，SHEN Zhengkang，DIAO Guiling，et al. An algorithm of fault parameter determination using distribution of small earthquakes and parameters of regional stress field and its application to Tangshan earthquake sequence[J]. Chinese Journal of Geophysics，2008，51(3)：793–804.(in Chinese)).

[27] 陈运泰，顾浩鼎. 震源理论[M]. 北京：高等教育出版社，1990：1–256.(CHEN Yuntai，GU Haoding. Theory of seismic source[M]. Beijing：Higher Education Press，1990：1–256.(in Chinese)