Geochronology of Mexican mineral deposits. VII: the Peña Colorada magmatic-hydrothermal iron oxide deposits (IOCG “clan”), Colima
The Peña Colorada mineralized area contains several iron oxide-apatite (IOA) deposits around the arguably richest known iron resource in Mexico. The Lower Cretaceous volcano-sedimentary host rock sequence has been subjected to several episodes of hydrothermal alteration, each accompanied by a distin...
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| Udgivet i: | Boletín de la Sociedad Geológica Mexicana |
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| Principais autores: | , , , , , , , , |
| Format: | Artigo |
| Sprog: | Inglês |
| Udgivet: |
Sociedad Geológica Mexicana, A.C.
2018
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| Fag: | |
| Online adgang: | https://www.redalyc.org/articulo.oa?id=94358881004 https://www.redalyc.org/journal/943/94358881004/ https://www.redalyc.org/journal/943/94358881004/html/ https://www.redalyc.org/journal/943/94358881004/94358881004.epub https://www.redalyc.org/journal/943/94358881004/movil |
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