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Geologic structure of the northern margin of the Chihuahua trough: Evidence for controlled deformation during Laramide Orogeny

In this article we studied the northern part of the Laramide foreland of the Chihuahua Trough. The purpose of this work is twofold; fi rst we studied whether the deformation involves or not the basement along crustal faults (thin- or thick- skinned deformation), andsecond, we studied the nature of t...

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Bibliografske podrobnosti
izdano v:Boletín de la Sociedad Geológica Mexicana
Main Authors: Dana Carciumaru, Roberto Ortega
Format: Artigo
Jezik:Espanhol
Izdano: Sociedad Geológica Mexicana, A.C. 2008
Teme:
Online dostop:https://www.redalyc.org/articulo.oa?id=94316033004
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