Spatial migration of earthquakes within seismic clusters in Southern California: Evidence for fluid diffusion
Seismicity within many earthquake swarms is observed to migrate slowly with time, which may reflect event triggering due to slow fault slip or fluid flow. We search for this behavior in Southern California by applying a weighted least squares method to quantify event migration within 69 previously o...
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Veröffentlicht in: | Journal of Geophysical Research: Solid Earth 2012-04, Vol.117 (B4), p.n/a |
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Format: | Artikel |
Sprache: | eng |
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