Mapping finite-fault earthquake slip using spatial correlation between seismicity and point-source Coulomb failure stress change
Most earthquake energy release arises during fault slip many kilometers below the Earth’s surface. Understanding earthquakes and their hazard requires mapping the geometry and distribution of this slip. Such finite-fault maps are typically derived from surface phenomena, such as seismic and geodeti...
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| Format: | Article |
| Language: | English |
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McGill University
2025-03-01
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| Series: | Seismica |
| Subjects: | |
| Online Access: | https://seismica.library.mcgill.ca/article/view/1412 |
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