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Behavior of the southernmost San Andreas fault during the past 300 years

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Behavior of the southernmost San Andreas fault during the past 300 years

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dc.contributor.author Sieh, Kerry
dc.contributor.author Williams, Patrick L.
dc.date.accessioned 2012-09-11T01:20:24Z
dc.date.available 2012-09-11T01:20:24Z
dc.date.copyright 1990
dc.date.issued 2012-09-11
dc.identifier.citation Sieh, K., & Williams, P. L. (1990). Behavior of the southernmost San Andreas fault during the past 300 years. Journal of Geophysical Research, 95(B5), 6629–6645.
dc.identifier.issn 0148–0227
dc.identifier.uri http://hdl.handle.net/10220/8487
dc.description.abstract Surficial creep occurs at low rates along the Coachella Valley segment of the San Andreas fault, which has not produced a large earthquake during the period of historical record. Geodetic data indicate, however, that the crust adjacent to this segment of the San Andreas fault is accumulating strain at a high rate. Furthermore, neotectonic and paleoseismic data indicate that the fault does produce very large earthquakes every two to three centuries. In view of its long-term behavior, the occurrence of creep along the surficial trace of the fault in the Coachella Valley is of particular interest. Along two short reaches of the San Andreas fault in the Coachella Valley, measurements of offset geological deposits and man-made structures and from alignment arrays and creep meters show that slip rates of 2–4 mm/yr near Indio and near the Salton Sea have persisted for the past three centuries. This slow aseismic surficial creep is not a transient precursor to seismic failure of this segment of the fault. We suggest that the Coachella Valley segment of the San Andreas fault creeps in its upper few kilometers. This behavior may be due to tectonically induced high pore pressures in the coarse sediments that abut the fault.
dc.language.iso en
dc.relation.ispartofseries Journal of geophysical research
dc.rights © 1990 American Geophysical Union. This paper was published in Journal of Geophysical Research and is made available as an electronic reprint (preprint) with permission of American Geophysical Union. The paper can be found at the following official URL: http://dx.doi.org/10.1029/JB095iB05p06629. One print or electronic copy may be made for personal use only. Systematic or multiple reproduction, distribution to multiple locations via electronic or other means, duplication of any material in this paper for a fee or for commercial purposes, or modification of the content of the paper is prohibited and is subject to penalties under law.
dc.subject DRNTU::Science::Geology::Volcanoes and earthquakes.
dc.title Behavior of the southernmost San Andreas fault during the past 300 years
dc.type Journal Article
dc.identifier.doi http://dx.doi.org/10.1029/JB095iB05p06629
dc.description.version Published version

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