Active faulting and deformation of the Coalinga Anticline as interpreted from three‐dimensional velocity structure and seismicity
- 10 November 1989
- journal article
- Published by American Geophysical Union (AGU) in Journal of Geophysical Research
- Vol. 94 (B11) , 15565-15586
- https://doi.org/10.1029/jb094ib11p15565
Abstract
No abstract availableKeywords
This publication has 19 references indexed in Scilit:
- The Laramide orogeny: Evidence from cocorp deep crustal seismic profiles in the wind river mountains, wyomingPublished by Elsevier ,2003
- Hidden EarthquakesScientific American, 1989
- The style of Late Cenozoic deformation at the eastern front of the California Coast RangesTectonics, 1989
- Empirical relationships among seismic velocity, effective pressure, porosity, and clay content in sandstoneGeophysics, 1989
- Blind thrust systemsGeology, 1988
- New Evidence on the State of Stress of the San Andreas Fault SystemScience, 1987
- Role of Fault Bends in the Initiation and Termination of Earthquake RuptureScience, 1985
- The evolution of a thrust fault system: processes of rupture initiation, propagation and termination in the 1980 El Asnam (Algeria) earthquakeGeophysical Journal International, 1984
- Seismic Potential Revealed by Surface Folding: 1983 Coalinga, California, EarthquakeScience, 1984
- An aftershock study of the El Asnam (Algeria) earthquake of 1980 October 10Geophysical Journal International, 1983