Remotely triggered microearthquakes and tremor in central California following the 2010 Mw 8.8 Chile earthquake
Version of Record online: 31 DEC 2010
Copyright 2010 by the American Geophysical Union.
Geophysical Research Letters
Volume 37, Issue 24, December 2010
How to Cite
2010), Remotely triggered microearthquakes and tremor in central California following the 2010 Mw 8.8 Chile earthquake, Geophys. Res. Lett., 37, L24312, doi:10.1029/2010GL045462., , , and (
- Issue online: 31 DEC 2010
- Version of Record online: 31 DEC 2010
- Manuscript Accepted: 2 NOV 2010
- Manuscript Revised: 28 OCT 2010
- Manuscript Received: 13 SEP 2010
Auxiliary material for this article contains supplementary text, eight figures, and their figure captions.
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|grl27602-sup-0001-readme.txt||plain text document||16K||readme.txt|
|grl27602-sup-0002-txts01.pdf||PDF document||15194K||Text S1. Supplementary text and figures in PDF format.|
|grl27602-sup-0003-fs01.pdf||PDF document||1301K||Figure S1. Magnitudes versus occurrence times for all earthquakes occurred around the Coso region since 1997.|
|grl27602-sup-0004-fs02.pdf||PDF document||1362K||Figure S2. A record section of the 2–8 Hz band-pass-filtered vertical seismograms showing regionally triggered earthquakes and locally triggered tremor by the 2010 Mw8.8 Chile earthquake in the Parkfield region, and the broadband three-component velocity seismograms recorded at station PKD.|
|grl27602-sup-0005-fs03.pdf||PDF document||2340K||Figure S3. A record section of 2–16 Hz band-pass-filtered vertical seismograms showing the moveout of the Ml 3.5 earthquake near Coso.|
|grl27602-sup-0006-fs04.pdf||PDF document||36K||Figure S4. A zoom-in plot of Figure S1 showing locally triggered tremor modulated with the Rayleigh waves of the 2010 Mw8.8 Chile earthquake.|
|grl27602-sup-0007-fs05.pdf||PDF document||32K||Figure S5. Triggering potential for 200-second Love and Rayleigh waves in terms of the dynamic Coulomb-failure stress.|
|grl27602-sup-0008-fs06.pdf||PDF document||38K||Figure S6. Influence of variations in the coefficient of friction on the Love and Rayleigh wave triggering potentials as a function of incidence angle on the San Andreas Fault computed for a depth of 25 km as in Figure 4.|
|grl27602-sup-0009-fs07.pdf||PDF document||106K||Figure S7. A zoom-in plot of Figure 3a showing the relationship between the teleseismic body waves of the Chile mainshock and the local earthquakes near Coso.|
|grl27602-sup-0010-fs08.pdf||PDF document||105K||Figure S8. A zoom-in plot showing the relationships among the Love waves of the Chile mainshock, the regional seismic signals from the Ml 3.5 earthquake near Coso, and high-frequency local tremor signals.|
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