-
- Robert M. Nadeau
- Berkeley Seismological Laboratory, 211 McCone Hall, University of California, Berkeley, CA 94720–4760, USA.
-
- Thomas V. McEvilly
- Berkeley Seismological Laboratory, 211 McCone Hall, University of California, Berkeley, CA 94720–4760, USA.
書誌事項
- 公開日
- 2004-01-09
- DOI
-
- 10.1126/science.1090353
- 公開者
- American Association for the Advancement of Science (AAAS)
この論文をさがす
説明
<jats:p>Deep fault slip information from characteristically repeating microearthquakes reveals previously unrecognized patterns of extensive, large-amplitude, long-duration, quasiperiodic repetition of aseismic events along much of a 175-kilometer segment of the central San Andreas fault.Pulsing occurs both in conjunction with and independent of transient slip from larger earthquakes.It extends to depths of ∼10 to 11 kilometers but may be deeper, and it may be related to similar phenomena occurring in subduction zones.Over much of the study area, pulse onset periods also show a higher probability of larger earthquakes, which may provide useful information for earthquake forecasting.</jats:p>
収録刊行物
-
- Science
-
Science 303 (5655), 220-222, 2004-01-09
American Association for the Advancement of Science (AAAS)
