Diachronic Cenozoic wrenching in southwest of the Colombian Basin
We propose a major Eocene tectonic inversion related to an oblique convergence between Farallon (after Cocos plate) and Caribbean plates in the offshore of Colombian Caribbean. Between Eocene- Oligocene occurred an extension and another tectonic inversion since Oligocene to Pleistocene. By structura...
Guardado en:
Autores principales: | Alfaro, E., Barrera, D.F., Rossello, E.A. |
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Formato: | JOUR |
Materias: | |
Acceso en línea: | http://hdl.handle.net/20.500.12110/paper_0873948X_v100_n1_p55_Alfaro |
Aporte de: |
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