Physics
Scientific paper
Jun 2001
adsabs.harvard.edu/cgi-bin/nph-data_query?bibcode=2001georl..28.2265l&link_type=abstract
Geophysical Research Letters, Volume 28, Issue 11, p. 2265-2268
Physics
17
Geodesy And Gravity: Crustal Movements-Interplate, Geodesy And Gravity: Seismic Deformations, Seismology: Seismic Hazard Assessment And Prediction, Tectonophysics: Continental Neotectonics
Scientific paper
We present results from over 30 yr of precise surveys of creep along the Hayward fault. Along most of the fault, spatial variability in long-term creep rates is well determined by these data and can help constrain 3D-models of the depth of the creeping zone. However, creep at the south end of the fault stopped completely for more than 6 years after the M7 1989 Loma Prieta Earthquake (LPEQ), perhaps delayed by stress drop imposed by this event. With a decade of detailed data before LPEQ and a decade after it, we report that creep response to that event does indeed indicate the expected deficit in creep.
Galehouse Jon S.
Lienkaemper James J.
Simpson Robert W.
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