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Crystals which have distinct locations with distinct compositions are zoned . A quite common zoning pattern consists of a distinction in composition of the mineral's Heart (Main) when compared with its rim, and concentric rings of various compositions organized among the core as well as rim (Fig. 5). Minerals that commonly show this sort of zoning in the foremost or trace features are garnet, plagioclase, zircon, and tourmaline (Fig. 5). Of such, garnet and plagioclase are appropriate to studies of metamorphic P-T paths, Continue and zircon is appropriate to resolve in the timing of petrologic gatherings.
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