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Crystals which have distinctive regions with various compositions are zoned . A very common zoning sample requires a big difference in composition of a mineral's center (core) compared to its rim, and concentric rings of different compositions organized amongst the core and the rim (Fig. five). Minerals that normally present this kind of zoning in the major or trace elements are garnet, plagioclase, zircon, and tourmaline (Fig. five). Of these, garnet and plagioclase are pertinent Continue to research of metamorphic P-T paths, and zircon is suitable to perseverance on the timing of petrologic gatherings.
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