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HOLOCENE SLIP RATES ALONG THE OWENS VALLEY FAULT, CALIFORNIA:IMPLICATIONS FOR THE RECENT EVOLUTION OF THE EASTERNCALIFORNIA SHEAR ZONE (2001)
It is completed new paleoseismic studies along the Owens Valley fault to determine the age of pre-1872 earthquakes, to better bracket Holocene slip rates, and to understand better the role of the Owens Valley fault in accommodating right-lateral shear within the Eastern California Shear Zone.
Reference:
Geology; September 2001; v. 29; no. 9; p. 819�822
Geology; September 2001; v. 29; no. 9; p. 819�822
Organization:
Department of Geological Sciences, Central Washington University, Ellensburg, Washington 98926, USA, andInstitute for Crustal Studies, University of California, Santa Barbara, California 93106, USA
USA, California
Department of Geological Sciences, Central Washington University, Ellensburg, Washington 98926, USA, andInstitute for Crustal Studies, University of California, Santa Barbara, California 93106, USA
USA, California
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