Change of apparent segmentation of the San Andreas fault around Parkfield from space geodetic observations across multiple periods
Sequences of earthquakes are commonly represented as a succession of periods of interseismic stress accumulation followed by coseismic and postseismic phases of stress release. Because the recurrence time of large earthquakes is often greater than the available span of space geodetic data, it has be...
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語言: | English |
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2014
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在線閱讀: | https://hdl.handle.net/10356/102071 http://hdl.handle.net/10220/18854 |
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