Trace-metal content of the Cerro Quema Au-Cu deposit (Azuero Peninsula, Panama): Implications for exploration
Cerro Quema (Azuero Peninsula, Panama) is a high-sulfidation epithermal Au-Cu deposit hosted by a dacite dome complex of the Río Quema Formation (late Campanian to Maastrichtian). High-sulfidation mineralization at Cerro Quema occurs within a lithocap of vuggy quartz and advanced argillic alteration...
Furkejuvvon:
| Publikašuvnnas: | Boletín de la Sociedad Geológica Mexicana |
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| Váldodahkkit: | , , , |
| Materiálatiipa: | Artigo |
| Giella: | Inglês |
| Almmustuhtton: |
Sociedad Geológica Mexicana, A.C.
2018
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| Fáttát: | |
| Liŋkkat: | https://www.redalyc.org/articulo.oa?id=94362562015 https://www.redalyc.org/journal/943/94362562015/ https://www.redalyc.org/journal/943/94362562015/html/ https://www.redalyc.org/journal/943/94362562015/94362562015.epub https://www.redalyc.org/journal/943/94362562015/movil |
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