A Comprehensive Analysis of Deformation Data at Parkfield, California: Detection of a Long-term Strain Transient
Abstract
More than a decade of high quality data from geodetic and borehole strain instrumentation in the Parkfield, California area (1985-1997) reveal a significant transient in apparent slip-rate along the San Andreas fault. This transient consists of two components: decreased slip-rate (by 16 ± 5%) during 1991.0 - 1993.0 followed by an increased rate (by 34 ± 6%) from 1993.0 for at least 3 years. The second component was observed by Gwyther et al. (1996) from tensor strain data. This transient is clear in all the deformation data used in this study, including those from 2-color laser geodimeters, borehole strain dilatometers, and creepmeters. Compared with pre-1991 levels, seismicity is greater during this episode, especially for the period of increased slip-rate, during which the four largest earthquakes in the observing period occurred. Since there was also a significant increase in precipitation during the period 1991-1996, we tested for the relative contributions of tectonic and hydrologic subluences to the observed signals. For this purpose we analyzed the geodimeter data, using for each baseline, the decade-long secular change in baseline length as a measure of tectonic sensitivity, and the amplitude of the annual cycle as a measure of hydrologic sensitivity. We found that the anomaly is significantly correlated with tectonic sensitivity at the 95% confidence level, but not with hydrologic sensitivity. From this we conclude that the observed transient is primarily tectonic, and most easily explained by local variations in slip-rate along the San Andreas fault. However, there may still be a hydrologic role in the modulating tectonic activity, through, for example, precipitation-induced variations in pore-pressure within the fault zone or in surface loading. We are presently examining this possibility.
Recommended Citation
P. G. Silver et al., "A Comprehensive Analysis of Deformation Data at Parkfield, California: Detection of a Long-term Strain Transient," American Geophysical Union (AGU), Dec 1997.
Meeting Name
Fall Meeting (1997: Dec. 1, San Francisco, CA)
Department(s)
Geosciences and Geological and Petroleum Engineering
Document Type
Article - Conference proceedings
Document Version
Citation
File Type
text
Language(s)
English
Rights
© 1997 American Geophysical Union (AGU), All rights reserved.
Publication Date
01 Dec 1997