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Crystals that have diverse regions with unique compositions are zoned . A very common zoning pattern involves a big difference in composition of the mineral's Middle (Main) in comparison with its rim, and concentric rings of various compositions arranged involving the core along with the rim (Fig. 5). Minerals that generally exhibit such a zoning in the Continue foremost or trace features are garnet, plagioclase, zircon, and tourmaline (Fig. five). Of these, garnet and plagioclase are relevant to studies of metamorphic P-T paths, and zircon is related to dedication in the timing of petrologic activities.
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