Seismic evidence for thermal runaway during intermediate-depth earthquake rupture
Intermediate-depth earthquakes occur at depths where temperatures and pressures exceed those at which brittle failure is expected. There are two leading candidates for the physical mechanism behind these earthquakes: dehydration embrittlement and self-localizing thermal shear runaway. A complete ene...
| Main Authors: | , , , , , , |
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| Other Authors: | |
| Format: | Article |
| Language: | English |
| Published: |
American Geophysical Union (AGU),
2015-07-28T14:14:29Z.
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| Subjects: | |
| Online Access: | Get fulltext |