1887

Abstract

The Deformation Front of the Eastern Cordillera is defined on its eastern foothills<br>by an asymmetric anticline with steep forelimb (Farallones Anticline at Medina<br>Village) to overturned forelimb (Buenavista Anticline at Villavicencio City). These<br>structures may have transmited strains to the foreland.

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/content/papers/10.3997/2214-4609-pdb.111.176
2006-09-24
2021-11-29
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