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...
محفوظ في:
المؤلفون الرئيسيون: | Lindsey, Eric Ostrom, Mallick, Rishav, Hubbard, Judith, Bradley, Kyle, Almeida, Rafael V., Moore, James Daniel Paul, Bürgmann, Roland, Hill, Emma M. |
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مؤلفون آخرون: | Asian School of the Environment |
التنسيق: | مقال |
اللغة: | English |
منشور في: |
2022
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الموضوعات: | |
الوصول للمادة أونلاين: | https://hdl.handle.net/10356/157059 |
الوسوم: |
إضافة وسم
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المؤسسة: | Nanyang Technological University |
اللغة: | English |
مواد مشابهة
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Implications of the diffuse deformation of the Indian Ocean lithosphere for slip partitioning of oblique plate convergence in Sumatra
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