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...

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Autores:
Tipo de recurso:
Fecha de publicación:
2013
Institución:
Universidad del Rosario
Repositorio:
Repositorio EdocUR - U. Rosario
Idioma:
eng
OAI Identifier:
oai:repository.urosario.edu.co:10336/25877
Acceso en línea:
https://doi.org/10.1002/2013GL058109
https://repository.urosario.edu.co/handle/10336/25877
Palabra clave:
Earthquake
Intermediate depth
Fracture energy
Efficiency
Source scaling
Thermal runaway
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