Campanian-Maastrichtian paleogeography and reservoir distribution in the Upper Magdalena Valley of Colombia.

G. Veloza-Fajardo; M. de Freitas; M. Mantilla

doi:10.3997/2214-4609-pdb.111.191

Campanian-Maastrichtian paleogeography and reservoir distribution in the Upper Magdalena Valley of Colombia.
By G. Veloza-Fajardo, M. de Freitas and M. Mantilla
Publisher: European Association of Geoscientists & Engineers
Source: Conference Proceedings, 9th Simposio Bolivariano - Exploracion Petrolera en las Cuencas Subandinas, Sep 2006, cp-111-00136
DOI: https://doi.org/10.3997/2214-4609-pdb.111.191

Abstract

Integration of stratigraphic, structural, petrologic, seismic, well interpretation and biostratigraphic data<br>allow for a new interpretation for the Upper Cretaceous sequence of the Upper Magdalena<br>Valley. Thickness changes among similar depositional environments and between the Neiva<br>and Girardot Sub-basins (from 130-1300 ft respectively) allow us to constrain Maastrichtian<br>deformation, previous to Andean deformation.

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2006-09-24

2025-01-24

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Campanian-Maastrichtian paleogeography and reservoir distribution in the Upper Magdalena Valley of Colombia.

Abstract

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