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Crystals which have diverse areas with diverse compositions are zoned . A quite common zoning sample will involve a difference in composition of a mineral's Heart (Main) when compared to its rim, and concentric rings of various compositions organized concerning the Main and also the rim (Fig. 5). Minerals that normally demonstrate this sort of zoning in the most important or trace components are garnet, plagioclase, zircon, and tourmaline (Fig. 5). Of these, garnet and plagioclase are pertinent to reports of metamorphic P-T paths, and zircon is appropriate to perseverance with the timing of petrologic activities.
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