Incipient Pulverization at Shallow Burial Depths Along the San Jacinto Fault, Southern California

Author:

Whearty James J.1,Rockwell Thomas K.1,Girty Gary H.1

Affiliation:

1. Department of Geological Sciences; San Diego State University; San Diego California USA

Publisher

John Wiley & Sons, Inc.

Reference36 articles.

1. Trace-element comparison of clasts in Eocene conglomerates, southwestern California and northwestern Mexico;Abbott;J. Geol.,1978

2. Sonora, Mexico, source for the Eocene Poway Conglomerate of southern California;Abbott;Geol.,1989

3. Anderson , K. 2010 Chemical and physical changes within the damage and pulverized zones of the Mojave segment of the San Andreas fault: Implications for the origin of pink potassium feldspar grains San Diego State Univ. Dept. of Geol. Sci

4. Stable, rapid rate of slip since inception of the San Jacinto fault, California;Blisniuk;Geophysical Research Letters,2013

5. Late quaternary slip rate gradient defined using high-resolution topography and 10Be dating of offset landforms on the southern San Jacinto fault zone, California;Blisniuk;J. Geophys. Res.,2010

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