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Crystals that have unique locations with unique compositions are zoned . A quite common zoning pattern includes a distinction in composition of the mineral's center (Main) in comparison to its rim, and concentric rings of various compositions arranged involving the core along with the website rim (Fig. 5). Minerals that generally show this sort of zoning in the foremost or trace factors are garnet, plagioclase, zircon, and tourmaline (Fig. five). Of these, garnet and plagioclase are suitable to research of metamorphic P-T paths, and zircon is appropriate to determination in the timing of petrologic situations.
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