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New constraints on timing of Hidalgoan (Laramide) deformation in the Parras and La Popa basins, NE Mexico

The Parras and La Popa basins of northeastern Mexico together contain at least three separate types of structures that were active during Maastrichtian through Early Eocene time. These structures include salt diapirs and salt welds, E-W trending anticlines detached within the Campanian Parras shale,...

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Bibliografske podrobnosti
izdano v:Boletín de la Sociedad Geológica Mexicana
Principais autores: Gary G. Gray, Timothy F. Lawton
Format: Artigo
Jezik:Inglês
Izdano: Sociedad Geológica Mexicana, A.C. 2011
Teme:
Online dostop:https://www.redalyc.org/articulo.oa?id=94321479013
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