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Strain-softening instability model for the san fernando earthquake

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Abstract

Changes in the ground elevation observed before and immediately after the 1971 San Fernando, California, earthquake are consistent with a theoretical model in which fault zone rocks are strain-softening after peak stress. The model implies that the slip rate of the fault increased to about 0.1 meter per year near the focus before the earthquake.
Publication type Article
Publication Subtype Journal Article
Title Strain-softening instability model for the san fernando earthquake
Series title Science
Volume 203
Issue 4383
Year Published 1979
Language English
Larger Work Type Article
Larger Work Subtype Journal Article
Larger Work Title Science
First page 907
Last page 910
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