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Crystals that have unique locations with distinctive compositions are zoned . A very common zoning pattern requires a big difference in composition of the mineral's Heart (Main) as compared to its rim, and concentric rings of various compositions organized between the core as well as the rim (Fig. 5). Minerals that generally exhibit such a zoning in the foremost or trace elements are garnet, plagioclase, zircon, and tourmaline (Fig. 5). Of these, garnet and plagioclase are relevant to research of metamorphic P-T paths, and zircon is related to Check Out Your URL willpower on the timing of petrologic functions.
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