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The trajectory and shape of your P-T route, the charges of metamorphic processes, as well as length of metamorphism certainly are a operate from the supply of warmth as well as the mechanisms of burial and unroofing (if pressure transform is included).
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Crystals which have different regions with distinctive compositions are zoned . A very common zoning sample entails a variance in composition of the mineral's Middle (Main) in comparison to its rim, and concentric rings of different compositions arranged between the core along with the rim (Fig. five). Minerals that commonly display this sort of zoning in the major or trace components are garnet, plagioclase, zircon, and tourmaline (Fig. five). Of these, garnet and plagioclase are appropriate to research of metamorphic P-T paths, and zircon is applicable to willpower of your timing of petrologic Click This Link activities.
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