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Crystals which have various locations with distinct compositions are zoned . A quite common zoning pattern consists of a difference in composition of a mineral's Centre (core) when compared to its rim, and concentric rings of different compositions organized in between the core and also the rim (Fig. five). Minerals that generally demonstrate this type of zoning in the key or trace factors are garnet, plagioclase, zircon, and tourmaline (Fig. five). Of these, garnet and plagioclase are applicable to experiments of metamorphic P-T paths, and zircon is suitable to determination on the timing of petrologic gatherings.
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