Self-affine asperity model for earthquakes

被引:42
作者
DeRubeis, V
Hallgass, R
Loreto, V
Paladin, G
Pietronero, L
Tosi, P
机构
[1] UNIV ROMA LA SAPIENZA, DIPARTIMENTO FIS, I-00185 ROME, ITALY
[2] UNIV AQUILA, DIPARTIMENTO FIS, I-67100 COPPITO, ITALY
关键词
D O I
10.1103/PhysRevLett.76.2599
中图分类号
O4 [物理学];
学科分类号
0702 ;
摘要
A model for fault dynamics consisting of two rough and rigid Brownian profiles that slide one over the other is introduced. An earthquake occurs when there is an intersection between the two profiles. The energy released is proportional to the overlap interval. Our model exhibits some specific features which follow from the fractal geometry of the fault: (1) nonuniversality of the exponent of the Gutenberg-Richter law for the magnitude distribution, (2) presence of local stress accumulation before a large seismic event, and (3) nontrivial space-time clustering of the epicenters.
引用
收藏
页码:2599 / 2602
页数:4
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