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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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| Опубликовано в: : | Boletín de la Sociedad Geológica Mexicana |
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| Главные авторы: | , |
| Формат: | Artigo |
| Язык: | Inglês |
| Опубликовано: |
Sociedad Geológica Mexicana, A.C.
2011
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| Предметы: | |
| Online-ссылка: | https://www.redalyc.org/articulo.oa?id=94321479013 |
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