| Article ID | Journal | Published Year | Pages | File Type |
|---|---|---|---|---|
| 5782034 | Marine and Petroleum Geology | 2017 | 35 Pages |
Abstract
Regarding the processes after entrapment, in all of the basins, the biodegradation effects were observed in varying degrees. These processes are dominant toward more quiescent regions, beyond the areas with more tectonic activity, far from the foothills of the Eastern Cordillera. Instead, close to the Eastern Cordillera are more common the paleobiodegradation processes due to reburial of younger molasses. The effects of mixing or refreshing are remarkable close to the Eastern Cordillera foothills in Llanos, Middle Magdalena Valley, and Upper Magdalena Valley basins.
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Authors
A. Rangel, J.F. Osorno, J.C. Ramirez, J. De Bedout, J.L. González, J.M. Pabón,