Influence of the shape of the friction law and fault finiteness on the duration of initiation

被引:41
作者
Ionescu, IR
Campillo, M
机构
[1] Univ Savoie, Math Lab, Chambery, France
[2] Univ Grenoble 1, Observ Grenoble, Lab Geophys Interne, F-38041 Grenoble, France
[3] Ist Informat & Math Appl, Lab Modelisat & Calcul, Grenoble, France
[4] Inst Univ France, Paris, France
关键词
D O I
10.1029/1998JB900090
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 consider the two-dimensional (2-D) elastic problem of slip instability under slip dependent friction. This paper concentrates on the parameters that determine the duration of the initiation phase, that is, the delay between an initial small perturbation of the system at the metastable equilibrium and the onset of dynamic rupture propagation. We first consider the case of a homogeneous fault (i.e., with infinite length) with a slip dependent friction with varying weakening rate. We show that different laws associated with the same values of stress drop and critical slip lead to a broad range of initiation duration. The duration is mainly governed by the slope of the friction law at the origin. We interpret these results using the analytical solution proposed by Campillo and Ionescu [1997] for the case of a constant weakening rate. These late results suggest a definition of a characteristic length associated with the rate of weakening at the origin. When the region of slip is limited to a finite weak patch, we found that the duration of initiation varies rapidly when the fault length is of the order of the characteristic length. Under these conditions the initiation duration increases extremely rapidly with decreasing fault length up to about 100 s in the numerical experiments we carried out. These results suggest that very simple elastic models with slip dependent friction and realistic values of the parameters could explain a broad range of delay of the onset of rupture propagation.
引用
收藏
页码:3013 / 3024
页数:12
相关论文
共 13 条
[1]   Correlation and prediction of synthesis gas solubility in n-paraffin systems [J].
Campanella, EA .
CHEMICAL ENGINEERING & TECHNOLOGY, 1997, 20 (06) :371-377
[3]   EARTHQUAKE NUCLEATION ON FAULTS WITH RATE-DEPENDENT AND STATE-DEPENDENT STRENGTH [J].
DIETERICH, JH .
TECTONOPHYSICS, 1992, 211 (1-4) :115-134
[4]  
DIETERICH JH, 1986, EARTHQUAKE SOURCE ME, V37, P37
[5]   SEISMIC EVIDENCE FOR AN EARTHQUAKE NUCLEATION PHASE [J].
ELLSWORTH, WL ;
BEROZA, GC .
SCIENCE, 1995, 268 (5212) :851-855
[7]   SLOW INITIAL PHASE OF THE P-WAVE VELOCITY PULSE GENERATED BY MICROEARTHQUAKES [J].
IIO, Y .
GEOPHYSICAL RESEARCH LETTERS, 1992, 19 (05) :477-480
[8]   On the contact problem with slip displacement dependent friction in elastostatics [J].
Ionescu, IR ;
Paumier, JC .
INTERNATIONAL JOURNAL OF ENGINEERING SCIENCE, 1996, 34 (04) :471-491
[9]   SLIP-DEPENDENT FRICTION LAW AND NUCLEATION PROCESSES IN EARTHQUAKE RUPTURE [J].
MATSUURA, M ;
KATAOKA, H ;
SHIBAZAKI, B .
TECTONOPHYSICS, 1992, 211 (1-4) :135-148
[10]   A constitutive law for the shear failure of rock under lithospheric conditions [J].
Ohnaka, M ;
Akatsu, M ;
Mochizuki, H ;
Odedra, A ;
Tagashira, F ;
Yamamoto, Y .
TECTONOPHYSICS, 1997, 277 (1-3) :1-27