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Evidence for possible horizontal faulting in southern California from earthquake mechanisms

Huang, Weishi and Silver, L. T. and Kanamori, H. (1996) Evidence for possible horizontal faulting in southern California from earthquake mechanisms. Geology, 24 (2). pp. 123-126. ISSN 0091-7613. http://resolver.caltech.edu/CaltechAUTHORS:20130510-154654100

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Abstract

We find that 36 of the 505 fault-plane solutions (M ≥ 3.0, 1981–1990) in southern California have a nodal plane dipping no more than 30 °. With the assumption of the low-angle nodal planes being the fault planes, four cross sections are constructed to show the possible horizontal faults in the middle and upper crust. More than half of these low-angle faults are located within or adjacent to the Transverse Ranges. The focal depths vary from 1 km in the southern end of the Sierra Nevada and the southwestern Mojave Desert to 20 km in the Transverse Ranges. The slip directions are also diverse. In general, east-west extensional movements are dominant in the boundary between the southern Sierra Nevada extending to the San Emigdio Mountains and the western Mojave Desert, whereas north-south compressional movements are dominant in the Transverse Ranges. In the Peninsular Ranges and the Salton Trough, both the slip directions and focal depths vary. These features suggest that seismically active low-angle faults in southern California may exist at different depths and slip in various directions. Our data do not support the existence of a regional-scale seismically active detachment in southern California. Only in the western Transverse Ranges is there some suggestion of a large detachment surface at a depth of about 13 to 14 km.


Item Type:Article
Related URLs:
URLURL TypeDescription
http://dx.doi.org/10.1130/0091-7613(1996)024<0123:EFPHFI>2.3.CO;2DOIArticle
http://geology.geoscienceworld.org/content/24/2/123PublisherArticle
ORCID:
AuthorORCID
Kanamori, H.0000-0001-8219-9428
Additional Information:© 1996 Geological Society of America. Manuscript received May 12, 1995. Revised manuscript received October 10, 1995. Manuscript accepted October 23, 1995. Supported by U.S. Geological Survey grant 14-08-0001-G1774. We thank Tom Parsons and an anonymous reviewer for constructive reviews of the manuscript, and Don Anderson and Joann Stock for helpful discussions. Seismological Laboratory, Division of Geological and Planetary Sciences, California Institute of Technology contribution 5542.
Funders:
Funding AgencyGrant Number
USGS14-08-0001-G1774
Other Numbering System:
Other Numbering System NameOther Numbering System ID
Caltech Division of Geological and Planetary Sciences5542
Record Number:CaltechAUTHORS:20130510-154654100
Persistent URL:http://resolver.caltech.edu/CaltechAUTHORS:20130510-154654100
Official Citation:Weishi Huang, L. T. Silver, and H. Kanamori Evidence for possible horizontal faulting in southern California from earthquake mechanisms Geology, February, 1996, v. 24, p. 123-126, doi:10.1130/0091-7613(1996)024<0123:EFPHFI>2.3.CO;2
Usage Policy:No commercial reproduction, distribution, display or performance rights in this work are provided.
ID Code:38435
Collection:CaltechAUTHORS
Deposited By: Ruth Sustaita
Deposited On:13 May 2013 14:48
Last Modified:09 Jan 2017 01:18

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