The paradox of the Loma Prieta Earthquake: Why did rupture terminate at depth?
- 10 November 1993
- journal article
- Published by American Geophysical Union (AGU) in Journal of Geophysical Research
- Vol. 98 (B11) , 19859-19867
- https://doi.org/10.1029/93jb02166
Abstract
No abstract availableThis publication has 23 references indexed in Scilit:
- Nucleation and growth of dip‐slip faults in a stable cratonJournal of Geophysical Research, 1992
- Variations in Strength and Slip Rate Along the San Andreas Fault SystemScience, 1992
- Geodynamic aspects of the Loma Prieta EarthquakeGeophysical Research Letters, 1990
- Evolution of the Northern Santa Cruz Mountains by Advection of Crust Past a San Andreas Fault BendScience, 1990
- Hidden EarthquakesScientific American, 1989
- Can natural faults propagate under Mode II conditions?Tectonics, 1988
- New Evidence on the State of Stress of the San Andreas Fault SystemScience, 1987
- Why large earthquakes do not nucleate at shallow depthsNature, 1983
- Preseismic rupture progression and great earthquake instabilities at plate boundariesJournal of Geophysical Research, 1983
- Stress Analysis of CracksPublished by ASTM International ,1965