Abstract
The high sulfur content and the low concentrations of PGE (0.47 g/t, evaluation by Río Narcea Recursos, SA) of the Aguablanca mineralization indicate that this deposit belongs, according to the classification of Naldrett (Magmatic sulfide deposit: Geology, geochemistry and exploration. Springer, Berlin, p 728, 2004), to those magmatic sulfide deposits valuable due to their primary Ni and Cu contents with PGE recovered as by-products.
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Piña, R. (2019). Ore-Forming Processes in the Aguablanca Ore Deposit. In: The Ni-Cu-(PGE) Aguablanca Ore Deposit (SW Spain). SpringerBriefs in World Mineral Deposits. Springer, Cham. https://doi.org/10.1007/978-3-319-93154-8_5
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