Slip rate deficit and earthquake potential on shallow megathrusts
Most destructive tsunamis are caused by seismic slip on the shallow part of offshore megathrusts. The likelihood of this behaviour is partly determined by the interseismic slip rate deficit, which is often assumed to be low based on frictional studies of shallow fault material. Here we present a new...
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Main Authors: | , , , , , , , |
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格式: | Article |
語言: | English |
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2022
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在線閱讀: | https://hdl.handle.net/10356/157059 |
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機構: | Nanyang Technological University |
語言: | English |