[1] Allen C, Gillespie A, Yuan H, et al. Red river and associated faults, Yunnan Province, China: Quarternary geology, slip rate and seismic hazard[J]. Geol Soc Am Bull, 1984, 95: 786-700. [2] Jarrard, R D. Terrane motion by strike-slip faulting of forearc slivers[J]. Geology, 1986, 14: 780-783. [3] Harris R D. Introduction to special section: Stress triggers, stress shadows, and implications for seismic hazard[J]. J Geophys Res, 1998, 103: 24347-24358. [4] Reasenberg P A, Simpson R W. Response of regional seismicity to the static stress change produced by the Loma Prieta earthquake[J]. Science, 1992, 255: 1687-1690. [5] Hardebeck J L, Nazareth J J, Hauksson E. The static stress change triggering model: Constraints from two southern California aftershock sequences[J]. J Geophys Res, 1998, 98: 4461-4472. [6] Toda S. Stress transferred by the 1995 MW=6.9 Kobe, Japan, shock: Effect on aftershocks and future earthquake probabilities[J]. J Geophys Res, 1998, 103: 24543-24565. [7] 刘桂萍, 傅征祥. 1976年7月28日唐山7.8级地震触发的区域地震活动和静应力场变化[J]. 地震学报, 2000, 22(1): 17-26. [8] 刘桂萍, 傅征祥. 1973年炉霍大地震(MS=7.6)最大余震(MS=6.3)的库仑破裂应力触发[J]. 中国地震, 18(2): 175-182. [9] 郝平, 傅征祥, 田勤俭, 等. 昆仑山口西8.1级地震强余震库仑破裂应力触发研究[J]. 地震学报, 2004, 26(1): 30-37. [10] Hill D P, Reasenberg P A, Michael A, et al. Seismicity remotely triggered by the magnitude 7.3 Landers, California, earthquake[J]. Science, 1993, 260: 1617-1623. [11] Cotton F, Coutant O. Dynamic stress variations due to shear faults in a plane-layered medium[J]. Geophy J Int, 1997, 128: 676-688. [12] Vidale J E, Agnew D, Johnston M, et al. Absence of earthquake correlation with each tides: An indications of high preseismic fault stress rate[J]. J Geophys Res, 1998, 103(B10): 24567-24572. [13] Jaeger J C, Cook N G W. Fundamentals of Rock Mechanics[M]. New York: Methuen, 1969: 513. [14] 万永革, 吴忠良, 周公威, 等. 几次复杂地震中不同破裂事件之间的“应力触发”问题[J]. 地震学报, 2000, 22(6): 568-576. [15] Stein R S, King G C P, Lin J. Change in failure stress on the southern San Andreas fault system caused by the 1992 magnitude=7.4 Landers earthquake[J]. Science, 1992, 258: 1328-1332. [16] King G C P, Stein R S, Lin J. Static stress changes and the triggering of earthquakes[J]. Bull Seism Soc Amer, 1994, 84: 935-953. [17] Okada Y. Internal deformation due to shear and tensile faults in a half-space[J]. Bull Seism Soc Amer, 1992, 82: 1018-1040. [18] Wells D L, Coppersmith K J. New empirical Relationships among magnitude, rupture length, rupture width, rupture area, and surface displacement[J]. Bull Seism Soc Amer, 1994, 84: 974-1002. [19] Kanamori H. The energy release in great earthquakes[J]. J Geophys Res, 1977, 82: 2981-2987. [20] Hanks T C, Kanamori H. A moment magnitude scale[J]. J Geophys Res, 1979, 84(B5): 2348-2350. [21] Dreger D S. Empirical Green's function study of the January 17, 1994 Northridge, California earthquake[J]. Geophys Res Lett, 1994, 21: 2633-2636. [22] Kanamori H. The radiated energy of the 2004 Sumatra-Andaman earthquake[M]. Radiated Energy and the Physics of Earthquake Faulting, R. Abercrombie, A. McGarr, H. Kanamori, and G. Di Toro (Editors), 2006, American Geophysical Monograph (in press). [23] Lin J, Stein R S. Stress triggering in thrust and subduction earthquakes, and stress interaction between the southern San Andreas and nearby thrust and strike-slip faults[J]. J Geophys Res, 2004, B02303, doi: 10.1029/2003JB002607. [24] Toda S, Stein R S, Richards-Dinger K, et al. Forecasting the evolution of seismicity in southern California: Animations built on earthquake stress transfer[J]. J Geophys Res, 2005, B05S16, doi:10.1029/2004JB003415. |