Tectonic Role Of Margin-Parallel And Margin-Transverse Faults During Oblique Subduction At The Southern Volcanic Zone Of The Andes
Obliquely convergent subduction margins develop trench-parallel faults shaping the regional architecture of orogenic belts and partitioning interplate deformation. However, transverse faults also are common along most orogenic belts, although have been la
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| Tipo de recurso: | tesis de maestría |
| Estado: | Versión publicada |
| Fecha de publicación: | 2016 |
| País: | Chile |
| Idioma: | inglés |
| OAI Identifier: | oai:repositorio.anid.cl:10533/235600 |
| Acceso en línea: | https://hdl.handle.net/10533/235600 |
| Access Level: | acceso abierto |
| Palabra clave: | Ciencias Naturales Ciencias de la Tierra y del Medio Ambiente |
| Sumario: | Obliquely convergent subduction margins develop trench-parallel faults shaping the regional architecture of orogenic belts and partitioning interplate deformation. However, transverse faults also are common along most orogenic belts, although have been la |
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