1887

Abstract

We use the patterns of growth sedimentation above the frontal and backlimbs of the Dina field structure,<br>located in the western fold and thrust belt of the Upper Magdalena Basin, Colombia, to describe the 3D<br>kinematic evolution of this fault-related fold.

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/content/papers/10.3997/2214-4609-pdb.111.103
2006-09-24
2021-08-02
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http://instance.metastore.ingenta.com/content/papers/10.3997/2214-4609-pdb.111.103
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