Masthead Logo Smith ScholarWorks Geosciences: Faculty Publications Geosciences 3-2012 Geodetic Constraints on San Francisco Bay Area Fault Slip Rates and Potential Seismogenic Asperities on the Partially Creeping Hayward Fault Eileen L. Evans Harvard University John P. Loveless Harvard University,
[email protected] Brendan J. Meade Harvard University Follow this and additional works at: https://scholarworks.smith.edu/geo_facpubs Part of the Geology Commons Recommended Citation Evans, Eileen L.; Loveless, John P.; and Meade, Brendan J., "Geodetic Constraints on San Francisco Bay Area Fault Slip Rates and Potential Seismogenic Asperities on the Partially Creeping Hayward Fault" (2012). Geosciences: Faculty Publications, Smith College, Northampton, MA. https://scholarworks.smith.edu/geo_facpubs/21 This Article has been accepted for inclusion in Geosciences: Faculty Publications by an authorized administrator of Smith ScholarWorks. For more information, please contact
[email protected] JOURNAL OF GEOPHYSICAL RESEARCH, VOL. 117, B03410, doi:10.1029/2011JB008398, 2012 Geodetic constraints on San Francisco Bay Area fault slip rates and potential seismogenic asperities on the partially creeping Hayward fault Eileen L. Evans,1 John P. Loveless,1,2 and Brendan J. Meade1 Received 28 March 2011; revised 17 November 2011; accepted 31 January 2012; published 31 March 2012. [1] The Hayward fault in the San Francisco Bay Area (SFBA) is sometimes considered unusual among continental faults for exhibiting significant aseismic creep during the interseismic phase of the seismic cycle while also generating sufficient elastic strain to produce major earthquakes. Imaging the spatial variation in interseismic fault creep on the Hayward fault is complicated because of the interseismic strain accumulation associated with nearby faults in the SFBA, where the relative motion between the Pacific plate and the Sierra block is partitioned across closely spaced subparallel faults.