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Volumn 46, Issue 12, 1992, Pages 7445-7449

Dynamical model of an earthquake fault with localization

Author keywords

[No Author keywords available]

Indexed keywords

EID: 0000400971 PISSN: 10502947 EISSN: None Source Type: Journal
DOI: 10.1103/PhysRevA.46.7445 Document Type: Article

Times cited : (59)

References (33)

2
- 35949011191
- Properties of earthquakes generated by fault dynamics
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- Carlson, J.¹ Langer, J.S.²

3
- 3543014842
- (1989) Phys. Rev. A , vol.40 , pp. 6470
- Carlson, J.¹ Langer, J.S.²

7
- 0024932740
- Earthquakes as a self-organized critical phenomenon
- (1989) Journal of Geophysical Research , vol.94 , pp. 15635
- Bak, P.¹ Tang, C.²

8
- 45549119532
- (1988) Phys. Lett. A , vol.131 , pp. 244
- Takayasu, H.¹ Matsuzaki, M.²

10
- 0025209563
- (1990) J. Geophys. Res. , vol.95 , pp. 6853
- Ito, K.¹ Matsuzaki, M.²

13
- 0001349398
- ibid.
- (1991) Phys. Rev. A , vol.43 , pp. 625
- Chen, K.¹ Bak, P.² Obukhov, S.P.³

14
- 0042212553
- (1991) Phys. Rev. Lett. , vol.66 , pp. 2669
- Feder, H.J.S.¹ Feder, J.²

16
- 0026304624
- Fractal features of the earthquake phenomenon and a simple mechanical model
- (1991) Journal of Geophysical Research , vol.96 , pp. 19925
- Matsuzaki, M.¹ Takayasu, H.²

18
- 0000790963
- Analysis of the theory of extremes as applied to earthquake problems
- (1977) Journal of Geophysical Research , vol.82 , pp. 5647
- Knopoff, L.¹ Kagan, Y.Y.²

26
- 3743095406
- ibid.
- (1978) Pure Appl. Geophys. , vol.116 , pp. 964
- Nur, A.¹

27
- 0023488624
- (1987) J. Geophys. Res. , vol.92 , pp. 345
- Okubo, P.G.¹ Aki, K.²

29
- 84927302769
- Many of the static models in [3] make use of stress-absorbing edge conditions, which do not allow for the inward diffusion of stress into the lattice from the parts of the fault outside it. The free edge as in [2] is a reflector of stress and hence, by virtue of imaging, simulates an infinite fault with correlations, as does our assumption of periodic boundary conditions. More important is the question whether ``runaways,'' i.e., events whose lengths are equal to the lattice size, can appear on either the finite or the (imaged) infinite lattice. By the imaging argument, runaways create an undesirable, infinitely long fracture.

30
- 0000084693
- (1991) Phys. Rev. Lett. , vol.67 , pp. 1043
- Langer, J.S.¹ Tang, C.²

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