Coseismic extension from surface cracks reopened by the 2014 Pisagua, northern Chile, earthquake sequence
The A.D. 2014 Pisagua earthquake sequence reactivated ancient surface cracks along the entire rupture length in the northern Chilean forearc. These subtle brittle strain features that are ~50 km above the subduction zone interface in the hyperarid Atacama
| Autores: | , , , |
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| Tipo de recurso: | artículo |
| Estado: | Versión publicada |
| Fecha de publicación: | 2016 |
| País: | Chile |
| Idioma: | inglés |
| OAI Identifier: | oai:repositorio.anid.cl:10533/238821 |
| Acceso en línea: | https://hdl.handle.net/10533/238821 |
| Access Level: | acceso abierto |
| Sumario: | The A.D. 2014 Pisagua earthquake sequence reactivated ancient surface cracks along the entire rupture length in the northern Chilean forearc. These subtle brittle strain features that are ~50 km above the subduction zone interface in the hyperarid Atacama |
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