ARE EARTHQUAKES AN EXAMPLE OF DETERMINISTIC CHAOS

被引:111
作者
HUANG, J
TURCOTTE, DL
机构
[1] Department of Geological Sciences, Cornell University, Ithaca, New York
关键词
D O I
10.1029/GL017i003p00223
中图分类号
P [天文学、地球科学];
学科分类号
07 ;
摘要
We use a simple mass‐spring model to systematically examine the dynamical behavior introduced by fault zone heterogeneities. The model consists of two sliding blocks coupled to each other and to a constant velocity driver by elastic springs. The state of this system can be characterized by the positions of the two blocks relative to the driver. A simple static/dynamic friction law is used. When the system is symmetric, we observe cyclic behavior. For an asymmetric system where the fractional forces for the two blocks are not equal, the solutions exhibit deterministic chaos. Chaotic windows occur repeatedly between regions of limit cycles on bifurcation diagrams. Our model behavior is similar to that of the one‐dimensional logistic map. In many examples of deterministic chaos, chaotic behavior of a low order system implies chaos in similar higher order systems. Thus, our results provide substantial evidence that earthquakes are an example of deterministic chaos. Copyright 1990 by the American Geophysical Union.
引用
收藏
页码:223 / 226
页数:4
相关论文
共 17 条
[1]  
Aki K., 1981, EARTHQUAKE PRED RES, DOI DOI 10.1029/ME004P0566
[2]  
[Anonymous], 1981, MECH BEHAV CRUSTAL R, DOI DOI 10.1029/GM024P0103
[3]  
BURRIDGE R, 1967, B SEISMOL SOC AM, V57, P341
[4]  
BYERLEE JD, 1978, PURE APPL GEOPHYS, V116, P616
[5]   SEISMICITY SIMULATION WITH A RATE-DEPENDENT AND STATE-DEPENDENT FRICTION LAW [J].
CAO, TQ ;
AKI, K .
PURE AND APPLIED GEOPHYSICS, 1986, 124 (03) :487-513
[6]  
CAO TQ, 1984, PURE APPL GEOPHYS, V122, P10, DOI 10.1007/BF00879646
[7]   PROPERTIES OF EARTHQUAKES GENERATED BY FAULT DYNAMICS [J].
CARLSON, JM ;
LANGER, JS .
PHYSICAL REVIEW LETTERS, 1989, 62 (22) :2632-2635
[8]   COMPUTER-SIMULATION OF EARTHQUAKES [J].
COHEN, SC .
JOURNAL OF GEOPHYSICAL RESEARCH, 1977, 82 (26) :3781-3796
[9]  
Dieterich J. H., 1980, SOLID EARTH GEOPHYS, V42, P21
[10]   TIME-DEPENDENT FRICTION AS A POSSIBLE MECHANISM FOR AFTERSHOCKS [J].
DIETERICH, JH .
JOURNAL OF GEOPHYSICAL RESEARCH, 1972, 77 (20) :3771-+