Detecting remotely triggered temporal changes around the Parkfield section of the San Andreas fault
Author:
Publisher
Earthquake Science
Subject
Geology,Geophysics,Geotechnical Engineering and Engineering Geology
Link
http://link.springer.com/content/pdf/10.1007/s11589-010-0748-0
Reference81 articles.
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2. Bakun W H (1984). Seismic moments, local magnitudes, and coda-duration magnitudes for earthquakes in central California. Bull Seismol Soc Am74: 439–458.
3. Bakun W H and Lindh A G (1985). The Parkfield, California, earthquake prediction experiment. Science229: 619–624.
4. Brenguier F, Shapiro N M, Campillo M, Ferrazzini V, Duputel Z, Coutant O and Nercessian A (2008a). Towards forecasting volcanic eruptions using seismic noise. Nature Geoscience1: 126–130, doi:10.1038/ngeo104.
5. Brenguier F, Campillo M, Hadziioannou C, Shapiro N M, Nadeau R M and Larose E (2008b). Postseismic relaxation along the San Andreas fault at Parkfield from continuous seismological observations. Science321: 1 478–1 481.
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