Seismic quiescence at Parkfield due to detachment faulting

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Abstract

On the San Andreas fault near Parkfield, California, rates of seismicity1,2 and geodetic line shortening3,4have been lower since 1986 than before. Wyss et al.1,3interpret the rate decreases as precursors to an imminent moderate earthquake (magnitude M = 5.5−6) and estimate the earthquake time to be March 1991 ± 1 yr. The earthquake was previously predicted to occur in 1988 ± 5 yr based on five of six similar earthquakes which occurred at intervals 22 yr, the last one in 19665. Here I present a model that attributes the rate changes to the initiation of slip on a subhorizontal detachment fault under the pending rupture area. In this model, the slip starts late in the seismic cycle, and diminishes the loading rate on the nearby San Andreas, thus acting as a buffer.

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Publication type Article
Publication Subtype Journal Article
Title Seismic quiescence at Parkfield due to detachment faulting
Series title Nature
DOI 10.1038/349058a0
Volume 349
Issue 6304
Year Published 1991
Language English
Publisher Springer Nature
Description 4 p.
First page 58
Last page 61
Country United States
State California
City Parkfield
Other Geospatial San Andreas fault
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