Research Article| June 01, 2008 Elevated shear zone loading rate during an earthquake cluster in eastern California Michael Oskin; Michael Oskin * 1Department of Geological Sciences, University of North Carolina at Chapel Hill, Chapel Hill, North Carolina 27599, USA *E-mail: oskin@email.unc.edu. Search for other works by this author on: GSW Google Scholar Lesley Perg; Lesley Perg 2Department of Geology and Geophysics, University of Minnesota, Minneapolis, Minnesota 55455, USA Search for other works by this author on: GSW Google Scholar Eitan Shelef; Eitan Shelef 3Department of Geological Sciences, University of North Carolina at Chapel Hill, Chapel Hill, North Carolina 27599, USA Search for other works by this author on: GSW Google Scholar Michael Strane; Michael Strane 3Department of Geological Sciences, University of North Carolina at Chapel Hill, Chapel Hill, North Carolina 27599, USA Search for other works by this author on: GSW Google Scholar Emily Gurney; Emily Gurney 3Department of Geological Sciences, University of North Carolina at Chapel Hill, Chapel Hill, North Carolina 27599, USA Search for other works by this author on: GSW Google Scholar Brad Singer; Brad Singer 4Department of Geology and Geophysics, University of Wisconsin, Madison, Wisconsin 53706, USA Search for other works by this author on: GSW Google Scholar Xifan Zhang Xifan Zhang 4Department of Geology and Geophysics, University of Wisconsin, Madison, Wisconsin 53706, USA Search for other works by this author on: GSW Google Scholar Geology (2008) 36 (6): 507–510. https://doi.org/10.1130/G24814A.1 Article history received: 25 Jan 2008 rev-recd: 27 Feb 2008 accepted: 03 Mar 2008 first online: 02 Mar 2017 Cite View This Citation Add to Citation Manager Share Icon Share MailTo Twitter LinkedIn Tools Icon Tools Get Permissions Search Site Citation Michael Oskin, Lesley Perg, Eitan Shelef, Michael Strane, Emily Gurney, Brad Singer, Xifan Zhang; Elevated shear zone loading rate during an earthquake cluster in eastern California. Geology 2008;; 36 (6): 507–510. doi: https://doi.org/10.1130/G24814A.1 Download citation file: Ris (Zotero) Refmanager EasyBib Bookends Mendeley Papers EndNote RefWorks BibTex toolbar search Search Dropdown Menu toolbar search search input Search input auto suggest filter your search All ContentBy SocietyGeology Search Advanced Search Abstract We compare geodetic velocity to geologic fault slip rates to show that tectonic loading was doubled across the eastern California shear zone (ECSZ) during a cluster of major earthquake activity. New slip rates are presented for six dextral faults that compose the ECSZ in the central Mojave Desert. These rates were determined from displaced alluvial fans dated with cosmogenic 10Be and from a displaced lava flow dated with 40Ar/39Ar. We find that the sum geologic Mojave ECSZ slip rate, ≤6.2 ± 1.9 mm/yr, is only half the present-day geodetically measured velocity of 12 ± 2 mm/yr. These rates account for cumulative fault slip and geodetic observations that span the 60-km-wide shear zone; therefore this difference cannot be attributed to postseismic relaxation. Redistribution of tectonic loading over the earthquake cycle at a regional scale suggests that earthquake clustering may be enhanced via feedback with weakening of ductile shear zones. You do not have access to this content, please speak to your institutional administrator if you feel you should have access.
Read full abstract