Using field observations and geochronology to constrain the age of magmatic-hydrothermal activity at the Antamina deposit, Peru

Antamina is the largest skarn in the world with a resource of ~2,968 Mt averaging 0.89% Cu, 0.77% Zn, 11 g/t Ag and 0.02% Mo (Glencore, 2015). The Antamina skarn surrounds an intrusive complex consisting of 4 porphyry centers comprised of at least 10 phases emplaced between 10.96 ± 0.03 Ma and 10.23 ± 0.07 Ma (U-Pb zircon; this study). Major phases in each porphyry center include: P1 (early), P2 (inter-mineral), and P3 (late). P1 is related to skarn formation; P2 and P3 cross-cut skarns and do not contain skarn alteration. Re-Os molybdenite ages reveal an early mineralization stage in skarns (10.58 ± 0.07 Ma to 10.39 ± 0.05 Ma) and a late stage in P2 and P3 (10.05 ± 0.06 Ma to 9.68 ± 0.05 Ma). Zircon and molybdenite ages generally decrease from NE to SW along the axis of the deposit, and record ~1.5 Ma of magmatic-hydrothermal activity