Holocene offset and seismicity along the panamint valley fault zone, western basin-and-range province, California |
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Authors: | Roger SU Smith |
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Abstract: | Holocene right-slip along the central segment of the Panamint Valley totals 20 m and dip-slip is somewhat less. The most recent offset, about 2 m right-slip, probably occurred at least several hundred years ago. If a comparable amount of slip occurred during earlier earthquakes, mean seismic recurrence intervals would have been about 700–2500 years during the Holocene. |
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