Using Comb-Layered Textures in Porphyry Ore Deposits to Sample Pristine Magmatic Fluids

摘要

Comb-layered textures preserve the cyclic accumulation and release of volatiles inside magmas that are temporally associated with large Cu-Au-Mo-rich porphyry ore deposits. Fluid inclusions in these textures sample pristine magmatic fluid. Microanalysis of this fluid helps constrain the physical models that operate at melt-fluid interface and in the broader magma system responsible for ore deposit formation.