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- W1718941172 endingPage "601" @default.
- W1718941172 startingPage "565" @default.
- W1718941172 abstract "In many environments, landslides preserved in the geologic record can be analyzed to determine the likelihood of seismic triggering. If evidence indicates that a seismic origin is likely for a landslide or group of landslides, and if the landslides can be dated, then a paleoearthquake can be inferred and some of its characteristics can be estimated. Such paleoseismic landslide studies thus can help reconstruct the seismic shaking history of a site or region. Paleoseismic landslide studies differ fundamentally from paleoseismic fault studies. While fault studies seek to characterize the movement history of a specific fault, landslide studies characterize the shaking history of a site or region irrespective of the earthquake source. The practical lower-bound earthquake that can be interpreted from paleoseismic landslide investigations is about the magnitude of 5–6. This range is comparable or perhaps slightly lower than that for paleoseismic fault studies." @default.
- W1718941172 created "2016-06-24" @default.
- W1718941172 creator A5022852601 @default.
- W1718941172 date "2009-01-01" @default.
- W1718941172 modified "2023-10-16" @default.
- W1718941172 title "Chapter 8 Using Landslides for Paleoseismic Analysis" @default.
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