Metamorphism and deformation in the El Fuerte region: their role in the tectonic evolution of NW Mexico
The Río Fuerte Formation, cropping out in Sinaloa state of northwestern Mexico, has been ascribed to the Middle to Late Ordovician based on its fossil content. U-Pb detrital zircon study in a rock sample of this unit yielded peaks at 521 Ma, 605 Ma and 881 Ma. Relative-age probability plots in the r...
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| Udgivet i: | Revista Mexicana de Ciencias Geológicas |
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| Principais autores: | , , , , |
| Format: | Artigo |
| Sprog: | Inglês |
| Udgivet: |
Universidad Nacional Autónoma de México
2011
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| Online adgang: | https://www.redalyc.org/articulo.oa?id=57220090002 |
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