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Crystals that have diverse regions with diverse compositions are zoned . A quite common zoning pattern will involve a big difference in composition of the mineral's Middle (Main) in comparison with its rim, and concentric here rings of various compositions arranged concerning the core and also the rim (Fig. five). Minerals that typically demonstrate such a zoning in the key or trace elements are garnet, plagioclase, zircon, and tourmaline (Fig. 5). Of such, garnet and plagioclase are related to reports of metamorphic P-T paths, and zircon is relevant to willpower from the timing of petrologic situations.
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