A silentMw4.7 slip event of October 2006 on the Superstition Hills fault, southern California

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A silent Mw 4.7 slip event of October 2006 on the Superstition Hills fault, southern California

[1] During October 2006, the 20-km-long Superstition Hills fault (SHF) in the Salton Trough, southern California, slipped aseismically, producing a maximum offset of 27 mm, as recorded by a creepmeter. We investigate this creep event as well as the spatial and temporal variations in slip history since 1992 using ERS-1/2 and Envisat satellite data. During a 15-year period, steady creep is punctu...

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Evidence for Prehistoric Earthquakes on the Superstition Hills Fault from Offset Geomorphic Features by Scott

Offset geomorphic features along the Superstition Hills fault show evidence for at least one slip event prior to the 1987 surface rupture, and possibly as many as four to five earlier prehistoric earthquakes. We documented several geomorphic features that appeared offset by multiple events by making detailed topographic maps. Offset features were abundant along reaches of the fault with high to...

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Slip-Parallel Seismic Lineations on the Northern Hayward Fault, California

A high-resolution relative earthquake location procedure is used to image the fine-scale seismicity structure of the northern Hayward fault, California. The seismicity defines a narrow, near-vertical fault zone containing horizontal alignments of hypocenters extending along the fault zone. The lineations persist over the 15-year observation interval, implying the localization of conditions on t...

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Constraints on fault slip rates of the southern California plate boundary from GPS velocity and stress inversions

Thorsten W. Becker,1,∗ Jeanne L. Hardebeck2 and Greg Anderson3 1Cecil H. and Ida M. Green Institute of Geophysics and Planetary Physics, Scripps Institution of Oceanography, University of California, San Diego 9500 Gilman Drive, La Jolla CA 92093, USA 2United States Geological Survey, 345 Middlefield Road, MS 977, Menlo Park, CA 94025, USA 3UNAVCO, Inc., 6350 Nautilus Drive, Boulder, CO 80301, USA

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Stratigraphic record of Pleistocene initiation and slip on the Coyote Creek fault, Lower Coyote Creek, southern California

The Coyote Creek fault is a major strand of the San Jacinto fault zone in southern California. Pleistocene sediments and sedimentary rocks exposed in the lower Coyote Creek area preserve a record of surface deformation, stream reorganization, and erosion that resulted from initiation and slip on the Coyote Badlands strand of the Coyote Creek fault. A well-exposed section of conglomerate and san...

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ژورنال

عنوان ژورنال: Journal of Geophysical Research

سال: 2009

ISSN: 0148-0227

DOI: 10.1029/2008jb006135