Zobrazeno 1 - 5
of 5
pro vyhledávání: '"Andrés Fock"'
Autor:
Constanza Fuentes, Daniela Bustamante, Marcelo Farías, Reynaldo Charrier, Felipe Tapia, Daniel Sellés, Francisco Fuentes, Andrés Fock, C. Mark Fanning, Mathieu Benoit, Marcia Muñoz-Gómez
Publikováno v:
Journal of the Geological Society. 177:258-275
Comision Nacional de Investigacion Cientifica y Tecnologica (CONICYT) Fondecyt 11140012 1161806 PAI79160139
Publikováno v:
Andean Geology, Vol 37, Iss 1, Pp 54-77 (2010)
In the El Volcan and Rodeo de los Bueyes areas, Andean Principal Cordillera (east of Santiago; 33°50'S), an Upper Oligocene-Lower Miocene volcanic series belonging to the Abanico Formation (Late Eocene-Early Miocene) is exposed. The rock successions
Externí odkaz:
https://doaj.org/article/b0578be11d084c83a2abc84942e97f99
Publikováno v:
Andean Geology. 37
In the El Volcan and Rodeo de los Bueyes areas, Andean Principal Cordillera (east of Santiago; 33o50'S), an Upper Oligocene-Lower Miocene volcanic series belonging to the Abanico Formation (Late Eocene-Early Miocene) is exposed. The rock successions
Autor:
Diana Comte, Reynaldo Charrier, Claire David, Andrés Tassara, Marcelo Farías, Joseph Martinod, Felipe Tapia, Andrés Fock
Publikováno v:
TECTONICS
Artículos CONICYT
CONICYT Chile
instacron:CONICYT
Artículos CONICYT
CONICYT Chile
instacron:CONICYT
[1] We document a crustal-scale structural model for the central Chile Andes based on seismicity and surface geology, which consists in a major east verging ramp-detachment structure connecting the subduction zone with the cordillera. The ramp rises
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::8c43bbd5a39278135d7b93738162960e
Publikováno v:
ANDEAN GEOLOGY
Artículos CONICYT
CONICYT Chile
instacron:CONICYT
Andean geology v.37 n.1 2010
SciELO Chile
Artículos CONICYT
CONICYT Chile
instacron:CONICYT
Andean geology v.37 n.1 2010
SciELO Chile
In the El Volcan and Rodeo de los Bueyes areas, Andean Principal Cordillera (east of Santiago; 33°50'S), an Upper Oligocene-Lower Miocene volcanic series belonging to the Abanico Formation (Late Eocene-Early Miocene) is exposed. The rock successions