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Crystals which have different regions with distinct compositions are zoned . A quite common zoning sample involves here a change in composition of a mineral's center (core) in comparison to its rim, and concentric rings of different compositions arranged among the core and also the rim (Fig. 5). Minerals that usually show such a zoning in the foremost or trace aspects are garnet, plagioclase, zircon, and tourmaline (Fig. 5). Of these, garnet and plagioclase are relevant to research of metamorphic P-T paths, and zircon is related to dedication from the timing of petrologic events.
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