High-frequency identification of non-volcanic tremor triggered by regional earthquakes

Details High-frequency identification of non-volcanic tremor triggered by regional earthquakes High-frequency identification of non-volcanic tremor triggered by regional earthquakes

Aug 2010

adsabs.harvard.edu/cgi-bin/nph-data_query?bibcode=2010georl..3716309g&link_type=abstract

Geophysical Research Letters, Volume 37, Issue 16, CiteID L16309

Physics

3

Seismology: Earthquake Interaction, Forecasting, And Prediction (1217, 1242), Seismology: Transform Faults, Tectonophysics: Dynamics And Mechanics Of Faulting (8004), Seismology: Seismicity And Tectonics (1207, 1217, 1240, 1242)

Scientific paper

Subsequent to the discovery of ambient “non-volcanic” tremor activity along the Parkfield-Cholame section of the San Andreas fault in central California, triggered tremors associated with the surface waves of large teleseismic earthquakes have been recognized. However, no evidence of triggered tremors from regional earthquakes has previously been found either here or in other tremor regions. By systematically filtering seismograms to higher frequencies (i.e., above 20 Hz) associated with 99 regional M5+ earthquakes since 2001, we identify four regional earthquakes that have triggered tremors in central California. Significant high-frequency energy is also observed in previously identified teleseismically triggered and ambient tremors, suggesting a common mechanism. We find that long-period and large-amplitude surface waves from both regional and teleseismic events have a greater potential of triggering tremor in the same region, and that the inferred minimum triggering dynamic stress is ˜1 kPa.

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