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Crystals which have various locations with diverse compositions are zoned . A quite common zoning sample will involve a difference in composition of a mineral's Centre (Main) when compared to its rim, and concentric rings of different compositions arranged amongst the Main plus the rim (Fig. five). Minerals that ordinarily show this type of zoning in the main or trace components are garnet, plagioclase, zircon, and tourmaline (Fig. 5). Of these, garnet and plagioclase are pertinent to scientific studies of metamorphic P-T paths, and zircon is appropriate check here to perseverance with the timing of petrologic gatherings.
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