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Crystals which have various areas with various compositions are zoned . A very common zoning pattern consists of a change in composition of the mineral's Centre (Main) as compared to its rim, and concentric rings of various Click Here compositions organized among the core along with the rim (Fig. 5). Minerals that generally present this kind of zoning in the major or trace features are garnet, plagioclase, zircon, and tourmaline (Fig. five). Of these, garnet and plagioclase are relevant to experiments of metamorphic P-T paths, and zircon is suitable to dedication from the timing of petrologic events.

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