Investigating the Gravity Signatures of the Margin-Oblique Deep Seated Andean Faults in the Rio Teno Region of the Transitional Southern Volcanic Zone, Chile
In a tectonic regime dominated by North-South oriented convergent stresses, margin oblique lineaments in the main cordillera of the Chilean Andes are theorized to significantly contribute to the dynamic evolution of this mountain belt as hydrothermal and
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| Tipo de recurso: | tesis de maestría |
| Estado: | Versión publicada |
| Fecha de publicación: | 2015 |
| País: | Chile |
| Idioma: | inglés |
| OAI Identifier: | oai:repositorio.anid.cl:10533/235605 |
| Acceso en línea: | https://hdl.handle.net/10533/235605 |
| Access Level: | acceso abierto |
| Palabra clave: | Ciencias Naturales Ciencias de la Tierra y del Medio Ambiente |
| Sumario: | In a tectonic regime dominated by North-South oriented convergent stresses, margin oblique lineaments in the main cordillera of the Chilean Andes are theorized to significantly contribute to the dynamic evolution of this mountain belt as hydrothermal and |
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