引文
[1]CHINNERY M A.The stress changes that accompanystrike-slip faulting[J].Bull Seism Soc Amer,1963,53(1):921-932.
[2]SMITH S W,Van de Lindt W.Strain adjustments associ-ated with earthquakes in southern California[J].BullSeism Soc Amer,1969,59(4):1 569-1 589.
[3]RYBICHI K.Analysis of aftershocks on the basis of dis-location theory[J].Phys Earth Planet Inter,1973,7(4):409-422.
[4]陈运泰,林邦慧,林中洋,等.根据地面形变的观测研究1966年邢台地震的震源过程[J].地球物理学报,1975,18(3):164-182.
[5]罗灼礼.震源应力场、形变场和倾斜场[J].地震学报,1980,2(2):169-185.
[6]DAS S,SCHOLZ C.Off-fault aftershock clusters causedby shear stress increase[J].Bull Seism Soc Amer,1981,71(5):1 669-1 675.
[7]KATO T,RYBICKI K,KASAHARA K.Mechanical inter-action between neighboring active faults-An applicationto the Altera fault,central Japan[J].Tectonophysics,1987,144:181-188.
[8]HUDNUT K W,SEEBER L,PACHECO J.Cross-faulttriggering in the November 1987 Superstition Hills earth-quake sequence,southern California[J].Geophys ResLett,1989,16:199-202.
[9]HARRIS R A,SIMPSON R W.Changes in static stresson southern California faults after the 1992 Landersearthquake[J].Nature,1992,360:251-254.
[10]OKADA Y.Internal deformation due to shear and ten-sile faults in a half-space[J].BSSA,1992,82(2):1 018-1 040.
[11]STEIN R S,KING G C P,LIN J.Change in failurestress on the southern San Andreas fault system causedby the 1992 magnitude=7.4 Landers earthquake[J].Science,1992,258:1 328-1 332.
[12]KING G C P,STEIN R S,LIN J.Static stress changesand the triggering of earthquakes[J].BSSA,1994,84(3):935-953.
[13]GROSS S,KISSLINGER C.Estimating tectonic stressrate and state with Landers aftershocks[J].JGR,1997,102:7 603-7 612.
[14]刘桂萍,傅征祥.日本1995年1月17日兵库县南部7.2级地震触发的区域地震活动[J].地震学报,1999,21(3):250-257.
[15]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.
[16]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,2002,18(2):175-182.
[17]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.
[18]郝平,傅征祥,田勤俭,等.1970年通海7.7级大地震强余震触发[J].地震,2004,24(2):38-46.
[19]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.
[20]郝平,田勤俭,傅征祥,等.2000年1月15日姚安6.5级地震较强余震的应力触发[J].地震研究,2004,27(3):246-251.
[21]HARRIS R A.Introduction to special section:Stress trig-gers,Stress shadows,and implications for seismic haz-ard[J].J Geophys Res,1998,103(B10):24 347-24 358.
[22]REASENBERG P A,SIMPSON R W.Response of re-gional seismicity to the static stress change produced bythe Loma Prieta earthquake[J].Science,1992,255:1 687-1 690.
[23]SIMPSON R W,REASENBERG P A.Earthquake-in-duced static stress changes on central California faults[A]//Simpson R W.The Loma Prieta,CaliforniaEarthquake of October 17,1989-Tectonic processesand models[C].US Geol Surv Prof Pap,1994,1550-F,F55-F89.
[24]RICE J R.Fault stress states,pore pressure distribu-tion,and the weakness of the San Andreas fault[A]//Evans B Wong T F.Fault Mechanics and TransportProperties of Rock[C].London:Academic Press,1992,475-503.
[25]龙锋,张永久,闻学泽,等.2008年8月30日攀枝花-会理6.1级地震序列ML≥4.0事件的震源机制解[J].地球物理学报,2010,53(12):2852-2860.
[26]唐荣昌.四川活动断裂与地震[M].北京:地震出版社,1993:1-368.
[27]李世成,张潜,郑定昌,等.攀枝花Ms6.1地震余震强震动流动观测[J].地震研究,2009,32(S):449-455.
[28]环文林,常向东,黄纬琼.地震危险性分析中的综合概率法[M].北京:地震出版社,1990:9-41.
[29]李忠华,苏有锦,蔡明军,等.云南地区震源破裂长度与震级的经验公式[J].西北地震学报,1999,21(3):331-333.
[30]丁国瑜,田勤俭,孔凡臣,等.活断层分段——原则、方法及应用[M].北京:地震出版社,1993.
[31]BODRI B,IIZUKAS.On the correlation between Earthtidal and microseismic activity[J].Phys Earth PlanetInter,1989,55(12):126-134.
[32]STEIN R S,KING G C P,LIN J.Stress triggering of the1994 M=6.7 Northridge,California earthquake by itspredecessors[J].Science,1994,265:1 432-1 435.
[33]JAUME S C,SYKES L R.Changes in state of stress onthe southern San Andreas Fault resulting from the Cali-fornia earthquake sequence of April to June 1992[J].Science,1992,258:1 325-1 328.
[34]张国民,傅征祥,桂燮泰,等.地震预报引论[M].北京:科学出版社,2001:372.
[35]DENG J,GURNIS M,KANAMORI H,et al.Viscoelas-tic flow in the lower crust after the 1992 Landers,Cali-fornia,earthquake[J].Science,1998,282:1 689-1 692.
[36]FREED A M,LIN J.Delayed triggering of the 1999 Hec-tor Mine earthquake by viscoelastic stress transfer[J].Nature,2001,411:180-183.