Physics
Scientific paper
Dec 2008
adsabs.harvard.edu/cgi-bin/nph-data_query?bibcode=2008georl..3523305p&link_type=abstract
Geophysical Research Letters, Volume 35, Issue 23, CiteID L23305
Physics
15
Seismology: Earthquake Interaction, Forecasting, And Prediction (1217, 1242), Seismology: Transform Faults, Tectonophysics: Dynamics And Mechanics Of Faulting (8004)
Scientific paper
We show clear evidence of non-volcanic tremor triggered by 2002 Mw7.8 Denali Fault earthquake near Parkfield. Triggered tremor is identified as bursts of high-frequency (~2-8 Hz), non-impulsive seismic energy whose envelope is coherent among many stations and has the same periodicity as the passing surface waves. The tremor originates from at least three hypocenters near the San Andreas fault with differing frictional regimes, two in the creeping section and the other where the San Andreas is transitional between creeping and locked. All the sources originate below the seismogenic zone, suggesting that transitional frictional properties are necessary conditions for tremor generation. Tremor is excited by the Love waves when the San Andreas is sheared in a right-lateral sense, encouraging slip, and is absent when the San Andreas is sheared in a left-lateral sense, consistent with a simple frictional response to the driving stress.
Bodin Paul
Creager Kenneth C.
Gomberg Joan
Peng Zhigang
Rubinstein Justin L.
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