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| DOI | 10.1016/J.TECTO.2016.05.016 | ||||
| Año | 2016 | ||||
| Tipo | artículo de investigación |
Citas Totales
Autores Afiliación Chile
Instituciones Chile
% Participación
Internacional
Autores
Afiliación Extranjera
Instituciones
Extranjeras
Deformation driven by oblique subduction is partially partitioned into strike-slip and shortening components. The trench-parallel component is mostly accommodated by NS-striking right-lateral faults of the LOFS. Trench-perpendicular shortening is accommodated by sinistral-reverse ATF and dextral-reverse NNE-striking faults. We conclude that the SVZ records a deformation history coeval with magma/fluid migration. (C) 2016 Elsevier B.V. All rights reserved.
| Ord. | Autor | Género | Institución - País |
|---|---|---|---|
| 1 | PEREZ-FLORES, PAMELA VIVIANA | Mujer |
Pontificia Universidad Católica de Chile - Chile
Comision Nacional de Investigacion Cientifica y Tecnologica - Chile Centro de Excelencia en Geotermia de Los Andes - Chile |
| 2 | CEMBRANO-PERASSO, JOSE MIGUEL | Hombre |
Pontificia Universidad Católica de Chile - Chile
Comision Nacional de Investigacion Cientifica y Tecnologica - Chile Centro de Excelencia en Geotermia de Los Andes - Chile |
| 3 | Sanchez-Alfaro, Pablo A. | Hombre |
Comision Nacional de Investigacion Cientifica y Tecnologica - Chile
Universidad de Chile - Chile Centro de Excelencia en Geotermia de Los Andes - Chile |
| 4 | VELOSO-ESPINOSA, EUGENIO ANDRES | Hombre |
Pontificia Universidad Católica de Chile - Chile
Comision Nacional de Investigacion Cientifica y Tecnologica - Chile Centro de Excelencia en Geotermia de Los Andes - Chile |
| 5 | ARANCIBIA-HERNANDEZ, GLORIA CECILIA | Mujer |
Pontificia Universidad Católica de Chile - Chile
Comision Nacional de Investigacion Cientifica y Tecnologica - Chile Centro de Excelencia en Geotermia de Los Andes - Chile |
| 6 | Roquer, Tomas | Hombre |
Pontificia Universidad Católica de Chile - Chile
Comision Nacional de Investigacion Cientifica y Tecnologica - Chile Centro de Excelencia en Geotermia de Los Andes - Chile |
| Fuente |
|---|
| FONDECYT |
| Comisión Nacional de Investigación Científica y Tecnológica |
| Comisión Nacional de Investigación CientÃfica y Tecnológica |
| African Mathematics Millennium Science Initiative |
| Millennium Science Initiative Grant |
| Andean Geothermal Center of Excellence (CEGA) FONDAP/CONICYT Project |
| CONICYT - Beca Doctorado Nacional |
| Agradecimiento |
|---|
| We are grateful to Julie Rowland, Diego Morata, Martin Reich and Gerd Sielfeld for fruitful discussions on the interplay among tectonics, volcanism and hydrothermal fluid flow over the last years. Special thanks to the generous help of Martin Lizama during and after fieldwork, and to Felipe Astudillo and Juan Ignacio Sanchez who also helped in the fieldwork. We sincerely thank Associated Editor Rob Covers and reviewers Elena Druguet and Ozgur Karaoglu for their constructive comments on the manuscript. We also thank Tom Mitchell for hosting PPF at the UCL Rock Preparation Laboratory and Jim Davy for his help with thin sections preparation and SEM analysis. Thanks are also due to our colleagues Daniele Tardani, Rodrigo Gomila, Pablo Iturrieta, Ashley Stanton-Yonge and Felipe Aron; all of them shared their enthusiasm and ideas with us. This paper is a contribution to the Andean Geothermal Center of Excellence (CEGA) FONDAP/CONICYT Project 15090013 and FONDECYT Projects 1130030 (GA) and 1141139 (JC). Perez-Flores's PhD studies are funded by CONICYT - Beca Doctorado Nacional 21120519. Sanchez, P acknowledges support given by Millennium Science Initiative grant NC130065. |
| We are grateful to Julie Rowland, Diego Morata, Martin Reich and Gerd Sielfeld for fruitful discussions on the interplay among tectonics, volcanism and hydrothermal fluid flow over the last years. Special thanks to the generous help of Martin Lizama during and after fieldwork, and to Felipe Astudillo and Juan Ignacio Sanchez who also helped in the fieldwork. We sincerely thank Associated Editor Rob Govers and reviewers Elena Druguet and Ozgur Karaoglu for their constructive comments on the manuscript. We also thank Tom Mitchell for hosting PPF at the UCL Rock Preparation Laboratory and Jim Davy for his help with thin sections preparation and SEM analysis. Thanks are also due to our colleagues Daniele Tardani, Rodrigo Gomila, Pablo Iturrieta, Ashley Stanton-Yonge and Felipe Aron; all of them shared their enthusiasm and ideas with us. This paper is a contribution to the Andean Geothermal Center of Excellence (CEGA) FONDAP/CONICYT Project 15090013 and FONDECYT Projects 1130030 (GA) and 1141139 (JC). Perez-Flores's PhD studies are funded by CONICYT — Beca Doctorado Nacional 21120519 . Sanchez, P acknowledges support given by Millennium Science Initiative grant NC130065 . |