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Crystals that have different regions with unique compositions are zoned . A very common zoning pattern consists of a difference in composition of a mineral's center (Main) in comparison to its rim, and concentric rings of various compositions organized concerning the Main along with the rim (Fig. five). Minerals that generally Click This Link display this sort of zoning in the major or trace aspects are garnet, plagioclase, zircon, and tourmaline (Fig. five). Of these, garnet and plagioclase are suitable to experiments of metamorphic P-T paths, and zircon is related to willpower of the timing of petrologic activities.
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