A condition for super-shear rupture propagation in a heterogeneous stress field

被引:35
作者
Fukuyama, E [1 ]
Olsen, KB
机构
[1] Natl Res Inst Earth Sci & Disaster Prevent, Tsukuba, Ibaraki 3050006, Japan
[2] Univ Calif Santa Barbara, Inst Crustal Studies, Santa Barbara, CA 93106 USA
基金
美国国家科学基金会;
关键词
rupture velocity; in-plain crack; super-shear rupture; boundary integral equation method;
D O I
10.1007/s00024-002-8722-y
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
We have used numerical simulations with the boundary integral equation method to investigate a mechanism to excite super-shear rupture velocities in a homogeneous stress field including an asperity of increased initial stress. When the rupture, with the slip-weakening distance selected to generate sub-Rayleigh speed, encounters the asperity it either accelerates to super-shear velocities or maintains the sub-Rayleigh speed, dependent on the size and amplitude of the asperity. Three classes of rupture propagation are identified: the velocity (a) for the most narrow asperities increases slowly towards the Rayleigh wave speed, (b) for intermediate width of the asperities jumps to super-shear values for a short distance but then decreases to sub-Rayleigh wave speeds, and (c) for the widest asperities jumps to supershear values and pertains to values between the S- and P-wave velocities. The transitions between the three classes of rupture propagation are characterized by very narrow (critical) ranges of rupture resistance. If the size of the initial asperity is smaller than critical, it becomes difficult for rupture to propagate with super-shear velocities even if the initial stress level is high. Our results suggest that stress variation along the rupture path helps homogenize the rupture velocity and propagate with sub-Rayleigh wave speeds.
引用
收藏
页码:2047 / 2056
页数:10
相关论文
共 13 条
[1]   RUPTURE VELOCITY OF PLANE STRAIN SHEAR CRACKS [J].
ANDREWS, DJ .
JOURNAL OF GEOPHYSICAL RESEARCH, 1976, 81 (32) :5679-5687
[2]  
ANDREWS DJ, 1985, B SEISMOL SOC AM, V75, P1
[3]   A FAULTING MODEL FOR THE 1979 IMPERIAL-VALLEY EARTHQUAKE [J].
ARCHULETA, RJ .
JOURNAL OF GEOPHYSICAL RESEARCH, 1984, 89 (NB6) :4559-4585
[4]   Seismic imaging of the 1999 Izmit (Turkey) rupture inferred from the near-fault recordings [J].
Bouchon, M ;
Toksöz, N ;
Karabulut, H ;
Bouin, MP ;
Dietrich, M ;
Aktar, M ;
Edie, M .
GEOPHYSICAL RESEARCH LETTERS, 2000, 27 (18) :3013-3016
[5]   ADMISSIBLE SPEEDS FOR PLANE-STRAIN SELF-SIMILAR SHEAR CRACKS WITH FRICTION BUT LACKING COHESION [J].
BURRIDGE, R .
GEOPHYSICAL JOURNAL OF THE ROYAL ASTRONOMICAL SOCIETY, 1973, 35 (04) :439-455
[6]   Dynamic propagation and interaction of a rupture front on a planar fault [J].
Fukuyama, E ;
Madariaga, R .
PURE AND APPLIED GEOPHYSICS, 2000, 157 (11-12) :1959-1979
[7]  
FUKUYAMA E, 1995, B SEISMOL SOC AM, V85, P614
[8]  
Fukuyama E, 1998, B SEISMOL SOC AM, V88, P1
[9]   COHESIVE FORCE ACROSS TIP OF A LONGITUDINAL-SHEAR CRACK AND GRIFFITHS SPECIFIC SURFACE-ENERGY [J].
IDA, Y .
JOURNAL OF GEOPHYSICAL RESEARCH, 1972, 77 (20) :3796-+
[10]  
Madariaga R, 2000, PROBLEMS IN GEOPHYSICS FOR THE NEW MILLENNIUM, P89