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The trajectory and condition with the P-T path, the rates of metamorphic procedures, along with the duration of metamorphism really are a functionality with the source of heat plus the mechanisms of burial and unroofing (if strain modify is associated).
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Crystals that have diverse locations with unique compositions are zoned . A quite common zoning pattern includes a variation in composition of the mineral's Middle (core) as compared to its rim, and concentric rings of different compositions organized amongst the core as well Check Out Your URL as rim (Fig. five). Minerals that generally show such a zoning in the key or trace features are garnet, plagioclase, zircon, and tourmaline (Fig. 5). Of such, garnet and plagioclase are related to scientific tests of metamorphic P-T paths, and zircon is relevant to willpower of your timing of petrologic activities.
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