El Pilar: A Particular Case in the Porphyry Copper Deposits in Mexico
El Pilar is a porphyry copper deposit located in the northern part of the state of Sonora, Mexico, at ~15 km from the border with USA, and about (40 km) from the town of Cananea, inside the most favorable part of the porphyry copper belt of the southwestern North America. Its features are relatively...
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2022
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oai:http:--epistemus.unison.mx:article-2002023-06-14T01:03:40Z El Pilar: A Particular Case in the Porphyry Copper Deposits in Mexico El Pilar: un caso particular en los depósitos de tipo pórfido de cobre en México Aguilar Austria, Silja Valencia-Moreno, Martín ore deposits porphyry copper exotic yacimientos minerales pórfidos de cobre exótico El Pilar is a porphyry copper deposit located in the northern part of the state of Sonora, Mexico, at ~15 km from the border with USA, and about (40 km) from the town of Cananea, inside the most favorable part of the porphyry copper belt of the southwestern North America. Its features are relatively atypical when compared with the rest of the deposits in Mexico, considering the most accepted porphyry copper model. The El Pilar is an exotic copper deposit hosted in Miocene gravels, that filled basins generated during the Basin and Range extensional event. The primary sulfide mineralization is poorly exposed and is associated with a magmatic breccia, linked with the emplacement of a monzonitic pluton dated by U-Pb zircon at ~75 Ma. The age of the mineralization was obtained by Re-Os molybdenite dating in ~73.9 Ma, and the estimated resources are of 0.36Mt copper. El Pilar es un yacimiento de tipo pórfido de cobre ubicado en el estado de Sonora, México, a 15 km de la frontera con E.U.A., y 40 km de la ciudad de Cananea, dentro de la zona más favorable del cinturón de pórfidos de cobre del suroeste de Norteamérica. Sus características son relativamente atípicas en comparación con el resto de los depósitos en México, considerando el modelo más aceptado de un pórfido de cobre. El Pilar es un yacimiento de cobre exótico hospedado en gravas del Mioceno, que rellenaron cuencas generadas durante el evento extensional Basin and Range. La mineralización de sulfuros hipogéncos aflora poco y está asociada con una brecha magmática ligada al emplazamiento de un plutón monzonítico fechado por U-Pb en zircones en ~75 Ma. La edad del depósito obtenida por Re-Os en molibdenita es de ~73.9 Ma, y las reservas se estiman en 0.36 Mt de cobre. Universida de Sonora 2022-05-16 info:eu-repo/semantics/article info:eu-repo/semantics/publishedVersion CienTecYSoc CienTecYSoc application/pdf application/pdf text/xml https://epistemus.unison.mx/index.php/epistemus/article/view/200 10.36790/epistemus.v16i32.200 EPISTEMUS; Vol. 16 No. 32 (2022): Issue 32; 86-92 EPISTEMUS; Vol. 16 Núm. 32 (2022): Revista No. 32; 86-92 2007-8196 2007-4530 spa https://epistemus.unison.mx/index.php/epistemus/article/view/200/297 https://epistemus.unison.mx/index.php/epistemus/article/view/200/234 https://epistemus.unison.mx/index.php/epistemus/article/view/200/260 Derechos de autor 2022 EPISTEMUS https://creativecommons.org/licenses/by-nc-sa/4.0 |
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Epistemus |
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language |
spa |
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Online |
author |
Aguilar Austria, Silja Valencia-Moreno, Martín |
spellingShingle |
Aguilar Austria, Silja Valencia-Moreno, Martín El Pilar: A Particular Case in the Porphyry Copper Deposits in Mexico |
author_facet |
Aguilar Austria, Silja Valencia-Moreno, Martín |
author_sort |
Aguilar Austria, Silja |
title |
El Pilar: A Particular Case in the Porphyry Copper Deposits in Mexico |
title_short |
El Pilar: A Particular Case in the Porphyry Copper Deposits in Mexico |
title_full |
El Pilar: A Particular Case in the Porphyry Copper Deposits in Mexico |
title_fullStr |
El Pilar: A Particular Case in the Porphyry Copper Deposits in Mexico |
title_full_unstemmed |
El Pilar: A Particular Case in the Porphyry Copper Deposits in Mexico |
title_sort |
el pilar: a particular case in the porphyry copper deposits in mexico |
description |
El Pilar is a porphyry copper deposit located in the northern part of the state of Sonora, Mexico, at ~15 km from the border with USA, and about (40 km) from the town of Cananea, inside the most favorable part of the porphyry copper belt of the southwestern North America. Its features are relatively atypical when compared with the rest of the deposits in Mexico, considering the most accepted porphyry copper model. The El Pilar is an exotic copper deposit hosted in Miocene gravels, that filled basins generated during the Basin and Range extensional event. The primary sulfide mineralization is poorly exposed and is associated with a magmatic breccia, linked with the emplacement of a monzonitic pluton dated by U-Pb zircon at ~75 Ma. The age of the mineralization was obtained by Re-Os molybdenite dating in ~73.9 Ma, and the estimated resources are of 0.36Mt copper. |
publisher |
Universida de Sonora |
publishDate |
2022 |
url |
https://epistemus.unison.mx/index.php/epistemus/article/view/200 |
work_keys_str_mv |
AT aguilaraustriasilja elpilaraparticularcaseintheporphyrycopperdepositsinmexico AT valenciamorenomartin elpilaraparticularcaseintheporphyrycopperdepositsinmexico AT aguilaraustriasilja elpilaruncasoparticularenlosdepositosdetipoporfidodecobreenmexico AT valenciamorenomartin elpilaruncasoparticularenlosdepositosdetipoporfidodecobreenmexico |
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