Why large earthquakes do not nucleate at shallow depths
- 1 October 1983
- journal article
- letter
- Published by Springer Nature in Nature
- Vol. 305 (5935), 621-623
- https://doi.org/10.1038/305621a0
Abstract
No abstract availableKeywords
This publication has 11 references indexed in Scilit:
- Implications of an elastic analysis of in situ stress measurements near the San Andreas FaultJournal of Geophysical Research, 1982
- Three-dimensional spontaneous rupture propagation and implications for the earthquake source mechanismGeophysical Journal International, 1981
- A numerical method for determination of source time functions for general three-dimensional rupture propagationGeophysical Journal International, 1980
- Friction of rocksPure and Applied Geophysics, 1978
- A numerical study of two-dimensional spontaneous rupture propagationGeophysical Journal International, 1977
- The faulting mechanism of the San Fernando EarthquakeJournal of Geophysical Research, 1974
- Possible criteria for predicting earthquake locations and their application to major plate boundaries of the Pacific and the CaribbeanJournal of Geophysical Research, 1973
- Detailed studies of frictional sliding of granite and implications for the earthquake mechanismJournal of Geophysical Research, 1972
- Dynamic Shear Cracks with Friction as Models for Shallow Focus EarthquakesGeophysical Journal International, 1971
- Static and kinetic friction of granite at high normal stressInternational Journal of Rock Mechanics and Mining Sciences, 1970