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...

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Autores principales: Alfaro, E., Barrera, D.F., Rossello, E.A.
Formato: JOUR
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Acceso en línea:http://hdl.handle.net/20.500.12110/paper_0873948X_v100_n1_p55_Alfaro
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