Rheology heterogeneities on fault surfaces inferred from the time history of afterslip events
Open Access
- 1 February 1994
- journal article
- Published by Oxford University Press (OUP) in Geophysical Journal International
- Vol. 116 (2) , 349-365
Abstract
No abstract availableKeywords
This publication has 16 references indexed in Scilit:
- A crack model of afterslip events on shallow faultsGeophysical Journal International, 1991
- Petrology of pseudotachylytes from the Alpine Fault of New ZealandTectonophysics, 1991
- Anelastic processes and stress transfer from shallow to deep fault regionsTectonophysics, 1990
- A crack model of creep processes on deep sections of faultsGeophysical Journal International, 1987
- Depth of seismicity in the Imperial Valley Region (1977–1983) and its relationship to heat flow, crustal structure and the October 15, 1979, earthquakeJournal of Geophysical Research, 1986
- Quasi-static crack models and the frictional stress threshold criterion for slip arrestGeophysical Journal International, 1985
- Heat flow in southernmost California and the origin of the Salton TroughJournal of Geophysical Research, 1985
- Geophysical and geological evidence for fracturing, water circulation and chemical alteration in granitic rocks adjacent to major strike‐slip faultsJournal of Geophysical Research, 1984
- Time-dependent friction and the mechanics of stick-slipPure and Applied Geophysics, 1978
- Empirical law for fault-creep eventsTectonophysics, 1977