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Crystals that have different areas with distinctive compositions are zoned . A very common zoning sample requires a big difference in composition of the mineral's Middle (Main) in comparison to its rim, and concentric rings of various compositions arranged read more between the core and also the rim (Fig. 5). Minerals that ordinarily clearly show this sort of zoning in the most important or trace aspects are garnet, plagioclase, zircon, and tourmaline (Fig. 5). Of these, garnet and plagioclase are relevant to experiments of metamorphic P-T paths, and zircon is suitable to resolve with the timing of petrologic functions.
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