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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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| Gepubliceerd in: | Boletín de la Sociedad Geológica Mexicana |
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| Hoofdauteurs: | , |
| Formaat: | Artigo |
| Taal: | Espanhol |
| Gepubliceerd in: |
Sociedad Geológica Mexicana, A.C.
2008
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| Onderwerpen: | |
| Online toegang: | https://www.redalyc.org/articulo.oa?id=94316033004 |
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