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Crystals which have various locations with various compositions are zoned . A quite common zoning pattern consists of a distinction in composition of the mineral's center (Main) compared to its rim, and concentric rings of various compositions organized amongst the Main along with the rim (Fig. five). Minerals that normally clearly show this kind of zoning in the most important or trace components are garnet, plagioclase, zircon, and tourmaline (Fig. five). Of those, garnet and plagioclase are relevant to reports of metamorphic P-T paths, and zircon is applicable to dedication with the timing of petrologic occasions.
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