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- W156408033 startingPage "267" @default.
- W156408033 abstract "Paleoseimology utilizes aspects of tectonic geomorphology, sedimentology, and stratigraphy to determine the location, timing, and displacement of past earthquakes. Most studies concentrate on providing data on Late Quaternary earthquakes to extend the historical seismic record. Earthquake recurrence models utilize paleoseismic data to help in earthquake hazard assessment. Recent methodological developments, including remote sensing, geodesy, fault trenching, and numerical dating, have helped accelerate knowledge and study of past earthquakes. Paleoseismic studies include on-fault and off-fault studies. The former involves mapping active fault traces and fault trenching. Off-fault studies mainly include studying and examining uplift of marine terraces, paleoliquefaction features, earthquake-triggered landslides, and tsunami deposits. Seismic hazard analysis is concerned with the long-term forecast of large earthquake and/or determining or estimating the amount of ground motion likely during a future earthquake. Effective seismic hazard mapping includes developing ground acceleration maps based on high-resolution, detailed geomorphic and Quaternary geologic mapping. Notable future challenges for paleoseismology include reconstructing the timing and magnitude of past earthquakes beyond a few tens of thousands of years to enhance understanding of the nature of earthquakes with long recurrence intervals, improving models for earthquake cycles, and applying paleoseismic knowledge for effective seismic hazard mitigation." @default.
- W156408033 created "2016-06-24" @default.
- W156408033 creator A5001972788 @default.
- W156408033 creator A5087510114 @default.
- W156408033 date "2013-01-01" @default.
- W156408033 modified "2023-09-30" @default.
- W156408033 title "5.12 Paleoseismology" @default.
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