1887

Abstract

Subsidence analysis is a common technique used by the oil industry for definition of the thermal maturity of<br>source rocks. Here, we performed subsidence analysis via 1D and 2D backstripping to reconstruct the geometry<br>of a foreland basin (Llanos Basin) that resulted from flexural deformation associated to the growth of an<br>orogenic belt (Eastern Cordillera). Examples from two regional cross sections illustrate this foreland basin -<br>orogenic belt coupled evolution.

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/content/papers/10.3997/2214-4609-pdb.111.125
2006-09-24
2021-10-27
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http://instance.metastore.ingenta.com/content/papers/10.3997/2214-4609-pdb.111.125
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