Please use this identifier to cite or link to this item: http://hdl.handle.net/2445/162763
Title: Cerro Quema (Azuero Peninsula, Panama): geology, alteration, mineralization and geochronology of a volcanic dome-hosted high sulfidation Au-Cu deposit.
Author: Corral, Isaac
Cardellach López, Esteve
Corbella i Cordomí, Mercè
Canals i Sabaté, Àngels
Gómez-Gras, David
Griera, A.
Cosca, M. A.
Keywords: Geologia
Panamà
Geocronologia
Jaciments minerals
Geology
Panama
Geochronology
Mineral deposits
Issue Date: 20-Jan-2016
Publisher: Society of Economic Geologists
Abstract: Cerro Quema (Azuero Peninsula, SW Panama) is a high sulfidation epithermal Au-Cu deposit hosted by a dacite dome complex of the Río Quema Formation (Late Campanian to Maastrichtian), a fore-arc basin sequence. Mineral resource estimate (Indicated + Inferred) are 30.86 Mt @ 0.73 g/t Au, containing 728,000 Oz Au (including 76.900 Oz AuEq of Cu ore). Hydrothermal alteration and mineralization are controlled by an E trending regional fault system. Hydrothermal alteration consists of an inner zone of vuggy quartz with locally developed advanced argillic alteration, enclosed by a well-developed zone of argillic alteration, grading to an external halo of propylitic alteration. Mineralization produced dissemination and microveinlets of pyrite and minor chalcopyrite, enargite and tennantite, with traces of sphalerite, crosscut by late stage base metal veins. New 40Ar/39Ar data of igneous rocks combined with biostratigraphic ages of the volcanic sequence indicate a maximum age of Lower Eocene (~55-49 Ma) for the Cerro Quema deposit. It was probably triggered by the emplacement of an underlying porphyry-like intrusion associated with the Valle Rico batholith. The geologic model suggests that in the Azuero Peninsula high sulfidation epithermal mineralization occur in the Cretaceous-Paleogene fore-arc. This consideration should be taken into account when exploring for this deposit type in similar geologic terranes.
Note: Versió postprint del document publicat a: https://doi.org/10.2113/econgeo.111.2.287
It is part of: Economic Geology, 2016, vol. 111, num. 2, p. 287-310
URI: http://hdl.handle.net/2445/162763
Related resource: https://doi.org/10.2113/econgeo.111.2.287
ISSN: 0361-0128
Appears in Collections:Articles publicats en revistes (Mineralogia, Petrologia i Geologia Aplicada)

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