Effects of prestress state and rupture velocity on dynamic fault branching

被引:202
作者
Kame, N
Rice, JR
Dmowska, R
机构
[1] Harvard Univ, Dept Earth & Planetary Sci, Cambridge, MA 02138 USA
[2] Harvard Univ, Div Engn & Appl Sci, Cambridge, MA 02138 USA
关键词
branching; fault; rupture propagation; boundary integral equation method (BIEM); fracture;
D O I
10.1029/2002JB002189
中图分类号
P3 [地球物理学]; P59 [地球化学];
学科分类号
0708 ; 070902 ;
摘要
[1] We consider a mode II rupture which propagates along a planar main fault and encounters an intersection with a branching fault. Using an elastodynamic boundary integral equation formulation, allowing the failure path to be dynamically self-chosen, we study the following questions: Does the rupture initiate along the branch? Does it continue? Is the extensional or compressional side most favored for branching? Does rupture continue on the main fault too? Failure is described by a slip-weakening law for which the strength at any amount of slip is proportional to normal stress. Our results show that dynamic stresses around the rupture tip, which increase with rupture velocity at locations off the main fault plane relative to those on it, could initiate rupture on a branching fault. As suggested by prior work, whether branched rupture can be continued to a larger scale depends on principal stress directions in the prestress state and on rupture velocity. The most favored side for branching rupture switches from the extensional to the compressional side as we consider progressively shallower angles of the direction of maximum compressive prestress with the main fault. Simultaneous rupturing on both faults can be activated when the branching angle is wide but is usually difficult for a narrow branching angle due to strong stress interactions between faults. However, it can be also be activated by enhanced dynamic stressing when the rupture velocity is very near the Rayleigh velocity. Natural examples seem consistent with the simulations that we present.
引用
收藏
页数:21
相关论文
共 31 条
[1]   RUPTURE VELOCITY OF PLANE STRAIN SHEAR CRACKS [J].
ANDREWS, DJ .
JOURNAL OF GEOPHYSICAL RESEARCH, 1976, 81 (32) :5679-5687
[2]   Selectivity of spontaneous rupture propagation on a branched fault [J].
Aochi, H ;
Fukuyama, E ;
Matsu'ura, M .
GEOPHYSICAL RESEARCH LETTERS, 2000, 27 (22) :3635-3638
[3]   Effect of normal stress during rupture propagation along nonplanar faults [J].
Aochi, H ;
Madariaga, R ;
Fukuyama, E .
JOURNAL OF GEOPHYSICAL RESEARCH-SOLID EARTH, 2002, 107 (B2)
[4]   Three-dimensional nonplanar simulation of the 1992 Landers earthquake [J].
Aochi, H ;
Fukuyama, E .
JOURNAL OF GEOPHYSICAL RESEARCH-SOLID EARTH, 2002, 107 (B2)
[5]   Spontaneous rupture propagation on a non-planar fault in 3-D elastic medium [J].
Aochi, H ;
Fukuyama, E ;
Matsu'ura, M .
PURE AND APPLIED GEOPHYSICS, 2000, 157 (11-12) :2003-2027
[6]   A FAULTING MODEL FOR THE 1979 IMPERIAL-VALLEY EARTHQUAKE [J].
ARCHULETA, RJ .
JOURNAL OF GEOPHYSICAL RESEARCH, 1984, 89 (NB6) :4559-4585
[7]  
Broberg K. B., 1999, Cracks and Fracture
[8]   Pore pressure and poroelasticity effects in Coulomb stress analysis of earthquake interactions [J].
Cocco, M ;
Rice, JR .
JOURNAL OF GEOPHYSICAL RESEARCH-SOLID EARTH, 2002, 107 (B2)
[9]   DYNAMIC FAULTING UNDER RATE-DEPENDENT FRICTION [J].
COCHARD, A ;
MADARIAGA, R .
PURE AND APPLIED GEOPHYSICS, 1994, 142 (3-4) :419-445
[10]   SEISMICITY AND GEOMETRY OF A 110-KM-LONG BLIND THRUST-FAULT .1. THE 1985 KETTLEMAN HILLS, CALIFORNIA, EARTHQUAKE [J].
EKSTROM, G ;
STEIN, RS ;
EATON, JP ;
EBERHARTPHILLIPS, D .
JOURNAL OF GEOPHYSICAL RESEARCH-SOLID EARTH, 1992, 97 (B4) :4843-4864