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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Vydáno v:	Boletín de la Sociedad Geológica Mexicana
Hlavní autoři:	Antoni Camprubí, Elena Centeno-García, Gustavo Tolson, Berlaine Ortega, Alexander Iriondo, Fanis Abdullin, Daniel Bolaños, José L. Portugal-Reyna, Mario A. Ramos-Arias
Médium:	Artigo
Jazyk:	Inglês
Vydáno:	Sociedad Geológica Mexicana, A.C. 2018
Témata:	Ciencias de la Tierra
On-line přístup:	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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