Interactions between Temperature and Pore-Fluid Pressure during Earthquake Faulting and a Mechanism for Partial or Total Stress Relief
- 1 May 1973
- journal article
- Published by Springer Nature in Nature Physical Science
- Vol. 243 (126), 66-68
- https://doi.org/10.1038/physci243066a0
Abstract
No abstract availableKeywords
This publication has 7 references indexed in Scilit:
- Melting on Fault Planes During Large EarthquakesGeophysical Journal International, 1972
- Tectonic stress and the spectra of seismic shear waves from earthquakesJournal of Geophysical Research, 1970
- Heat flow, stress, and rate of slip along the San Andreas Fault, CaliforniaJournal of Geophysical Research, 1969
- Permeability of granite under high pressureJournal of Geophysical Research, 1968
- Stick-Slip as a Mechanism for EarthquakesScience, 1966
- ROLE OF FLUID PRESSURE IN MECHANICS OF OVERTHRUST FAULTINGGSA Bulletin, 1959
- On the Mechanics of FaultingGeological Magazine, 1942