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Chemically zoned garnet growth and coeval modification of this zoning through diffusion are calculated during prograde metamorphic heating to temperatures of up to 850°C. This permits quantification of how the preservation or elimination of zoning profiles in garnet crystals of a given size is sensitive to the specific burial and heating (P–T) path followed, and the integrated duration spent at hi...

Preservation of Garnet Growth Zoning and the Duration of Prograde Metamorphism