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The trajectory and form from the P-T path, the fees of metamorphic processes, along with the duration of metamorphism certainly are a operate with the source of heat along with the mechanisms of burial and unroofing (if force alter is included).

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Crystals that have distinctive areas with distinctive compositions are zoned . here A very common zoning sample entails a difference in composition of a mineral's Centre (core) when compared to its rim, and concentric rings of different compositions organized in between the Main and the rim (Fig. five). Minerals that usually show such a zoning in the key or trace factors are garnet, plagioclase, zircon, and tourmaline (Fig. five). Of these, garnet and plagioclase are relevant to experiments of metamorphic P-T paths, and zircon is applicable to resolve with the timing of petrologic functions.

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