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Crystals which have unique locations with diverse compositions are zoned . A very common zoning sample requires a variation in composition of the mineral's Centre (Main) compared to its rim, and concentric rings of different compositions arranged among the core as well as the Do you agree rim (Fig. five). Minerals that typically display such a zoning in the main or trace components are garnet, plagioclase, zircon, and tourmaline (Fig. five). Of those, garnet and plagioclase are applicable to studies of metamorphic P-T paths, and zircon is suitable to willpower of your timing of petrologic events.
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