Les formations eruptives hercyniennes de la cordillere orientale de colombie
The magmatisme of the Oriental Cordillera of Colombia has been put on evidence. This magmatisme is characterized by association of granites, microgranites and rhyolites. These igneous rocks are evidently the result of a reactivation of the ancient basement and are post or a-tectonic.
- Autores:
-
Radelli, Luigi
- Tipo de recurso:
- Article of journal
- Fecha de publicación:
- 1962
- Institución:
- Universidad Nacional de Colombia
- Repositorio:
- Universidad Nacional de Colombia
- Idioma:
- spa
- OAI Identifier:
- oai:repositorio.unal.edu.co:unal/41119
- Acceso en línea:
- https://repositorio.unal.edu.co/handle/unal/41119
http://bdigital.unal.edu.co/31216/
- Palabra clave:
- Geología
Ciencias de la tierra
Geociencias
Magmatismo hercínico
zócalo antiguo
granitos
microgranitos
riolitas
Geología
ciencias de la tierra
Geociencias
Magmatismo hercínico
zócalo antiguo
granitos
microgranitos
riolitas
- Rights
- openAccess
- License
- Atribución-NoComercial 4.0 Internacional
| Summary: | The magmatisme of the Oriental Cordillera of Colombia has been put on evidence. This magmatisme is characterized by association of granites, microgranites and rhyolites. These igneous rocks are evidently the result of a reactivation of the ancient basement and are post or a-tectonic. |
|---|