Comment to "Porphyry-related high-sulfidation mineralization early in Central American Arc Development: Cerro Quema deposit, Azuero Peninsula, Panama" by Perelló et al., (2020)
The Cerro Quema Au-Cu deposit is hosted by a dacite dome complex of the Río Quema Formation, a Late Campanian-Maastrichtian volcano-sedimentary sequence of the Panamanian magmatic arc. Its formational age is constrained at ~49 Ma by field evidences, crosscutting relationships and 40Ar/39Ar geochrono...
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| Опубликовано в:: | Boletín de la Sociedad Geológica Mexicana |
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| Главный автор: | |
| Формат: | Artigo |
| Язык: | Inglês |
| Опубликовано: |
Sociedad Geológica Mexicana, A.C.
2021
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| Предметы: | |
| Online-ссылка: | https://www.redalyc.org/articulo.oa?id=94370810018 https://www.redalyc.org/journal/943/94370810018/ https://www.redalyc.org/journal/943/94370810018/html/ https://www.redalyc.org/journal/943/94370810018/94370810018.epub https://www.redalyc.org/journal/943/94370810018/movil |
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