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- W615627202 abstract "Antamina, Peru is the largest Cu-Zn skarn deposit in the world. Skarn mineralisation is focused around a multiphase Miocene intrusive complex comprising at least eight distinct phases identified by cross-cutting relationships, including truncated veins, xenoliths and chilled margins. Skarn alteration and mineralisation, as observed in drill core, remain open at depths exceeding 2.2 vertical kilometres. Porphyry intrusions occur as four major phases with subphases (from oldest to youngest): P1 (a, b), P2 (a, b), P3 (a, b) and two dykes of uncertain timing named Oscarina-1 and Oscarina-2. Pla is a hornblende-biotite quartz diorite porphyry with pervasive K-alteration, local endoskarn and 30-40 per cent sheeted quartz veins, all of which obscure original igneous textures. P1b dacite porphyry is a minor unit with 2.2 km) skarn and mineralisation at Antamina." @default.
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- W615627202 date "2015-01-01" @default.
- W615627202 modified "2023-09-27" @default.
- W615627202 title "A model for the intrusive sequence and Cu-Zn skarn formation at the Antamina deposit, Peru" @default.
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