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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| Publicat a: | Boletín de la Sociedad Geológica Mexicana |
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| Autors principals: | , |
| Format: | Artigo |
| Idioma: | Espanhol |
| Publicat: |
Sociedad Geológica Mexicana, A.C.
2008
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| Matèries: | |
| Accés en línia: | https://www.redalyc.org/articulo.oa?id=94316033004 |
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