Geochronology of Mexican mineral deposits. V: the Peñón Blanco epithermal deposit Durango
The low sulfidation epithermal deposits of the San Juan de Mogotes mineralized area in the Peñón Blanco district, central-eastern Durango, were dated in this study at 31.29 ± 0.08 Ma (adularia from crustiform veins, 40 Ar/ 39 Ar plateau age). Therefore, these deposits belong to the most productiv...
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| Vydáno v: | Boletín de la Sociedad Geológica Mexicana |
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| Hlavní autoři: | , , |
| Médium: | Artigo |
| Jazyk: | Inglês |
| Vydáno: |
Sociedad Geológica Mexicana, A.C.
2016
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| Témata: | |
| On-line přístup: | https://www.redalyc.org/articulo.oa?id=94346152013 https://www.redalyc.org/journal/943/94346152013/ https://www.redalyc.org/journal/943/94346152013/html/ https://www.redalyc.org/journal/943/94346152013/94346152013.epub https://www.redalyc.org/journal/943/94346152013/movil |
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