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Crystals which have unique locations with various compositions are more info zoned . A quite common zoning sample involves a variance in composition of the mineral's Middle (Main) in comparison with its rim, and concentric rings of various compositions arranged involving the Main along with the rim (Fig. five). Minerals that ordinarily show this sort of zoning in the key or trace elements are garnet, plagioclase, zircon, and tourmaline (Fig. five). Of these, garnet and plagioclase are related to studies of metamorphic P-T paths, and zircon is suitable to resolve from the timing of petrologic activities.
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