REE-Y, Ti, and P Remobilization in Magmatic Rocks by Hydrothermal Alteration during Cu-Au Deposit Formation

作者: M. van Dongen , R. F. Weinberg , A. G. Tomkins

DOI: 10.2113/GSECONGEO.105.4.763

关键词: ApatiteFractionationPorphyry copper depositGeologyHydrothermal circulationRare-earth elementMagmatismTitaniteGeochemistryZircon

摘要: Chondrite-normalized rare earth element (REE) plots of whole-rock geochemical analyses are commonly used to describe the history of magmatic systems. In the particular case of …

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