Normal upper plate fault reactivation in northern Chile and the subduction earthquake cycle: From geological observations and static Coulomb Failure Stress (CFS) change
The northern Chile subduction zone constitutes a seismic gap where no great interplate earthquakes (Mw > 8.8) have nucleated since 1877. Active normal faulting occurs conspicuously in the Coastal Forearc at the southern end of this gap, between 22.7°S and
| Autores: | , , |
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| Tipo de recurso: | artículo |
| Estado: | Versión publicada |
| Fecha de publicación: | 2015 |
| País: | Chile |
| Idioma: | inglés |
| OAI Identifier: | oai:repositorio.anid.cl:10533/238735 |
| Acceso en línea: | https://hdl.handle.net/10533/238735 |
| Access Level: | acceso abierto |
| Sumario: | The northern Chile subduction zone constitutes a seismic gap where no great interplate earthquakes (Mw > 8.8) have nucleated since 1877. Active normal faulting occurs conspicuously in the Coastal Forearc at the southern end of this gap, between 22.7°S and |
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