Contribution of mantle components within juvenile lower-crust to collisional zone porphyry Cu systems in Tibet
Abstract
Most porphyry Cu–Mo–Au deposits are found in magmatic arcs worldwide, and are associated with hydrous, high-fO2, calc-alkaline magmas, derived from a mantle wedge that was metasomatized by the fluids from a subducted oceanic slab. Recently, such deposits have been documented as occurring widely in collisional settings, where they are associated with potassic magmas generated during the collisional process, but the genesis of the fertile magmas...
Paper Details
Title
Contribution of mantle components within juvenile lower-crust to collisional zone porphyry Cu systems in Tibet
Published Date
May 13, 2012
Journal
Volume
48
Issue
2
Pages
173 - 192
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