A Rusty Record of Weathering and Groundwater Movement in the Hyperarid Central Andes
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DOI: 10.1029/2021gc009759
Abstract: The Central Andes of northern Chile host many large porphyry copper deposits (PCDs)—hydrothermally generated, sulfide-bearing orebodies centered on felsic to intermediate igneous intrusions (Richards, 2013). Initially formed at depths of ∼1–4 km (Sillitoe, 2010), many… read more here.
Keywords: movement; water; aridity induced; central andes ... See more keywords