Timescales and Processes of Au and Cu Fertile Magmatic-Hydrothermal Reservoir Accumulation in Continental Arcs

Wiemer, Daniel, Hagemann, Steffen G., Kemp, Anthony I., Thebaud, Nicholas, Ireland, Trevor, and Villanes, Carlos (2021) Timescales and Processes of Au and Cu Fertile Magmatic-Hydrothermal Reservoir Accumulation in Continental Arcs. In: [Presented at the SEG 100 Conference]. 4154. From: SEG 100 Conference: Celebrating a Century of Discovery, 14-17 Spetember 2021, Whistler, Canada.

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Abstract

Continental arc systems are loci of world-class Cu-Au porphyry and intrusion-related orogenic Au vein deposits. The subduction environment facilitates high magma and fluid fluxes, acting as a heat engine and promoting metal transport. How and when, during the lifetime of an accretionary orogen, Cu and Au fertile magmas are generated and ore-producing fluids are expelled, remains elusive.

We present combined structural, geochemical, and zircon trace element, U/Pb and Lu/Hf isotopic data from the Carboniferous Eastern Andean Cordillera, northern Perú. Our geochemical data demonstrate that primitive, mantle-derived calc-alkaline diorite magmas are hydrous, oxidized, and enriched in metals (Cu, Au), but lack evidence for crustal assimilation. Field relationships indicate repeated intrusion of these fertile magmas into mid-crustal levels. Hornblende-dominated crystallization and fractionation led to successive batch segregation of granodiorite melt upon diorite recharge. Petrographic observations attest to hornblende textural breakdown during magmatic recharge, providing a mechanism for ore-fluid expulsion in the plutonic realm.

Item ID: 83434
Item Type: Conference Item (Abstract / Summary)
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Date Deposited: 27 Aug 2024 00:58
FoR Codes: 37 EARTH SCIENCES > 3705 Geology > 370502 Geochronology @ 50%
37 EARTH SCIENCES > 3705 Geology > 370508 Resource geoscience @ 50%
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