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Crystals that have distinctive areas with distinctive compositions are zoned . A very common zoning sample consists of a variation in composition of a mineral's Centre (Main) when compared to its rim, and concentric rings of different compositions arranged concerning the core as well as the rim (Fig. five). Minerals that normally clearly show such a zoning in the foremost or trace components are garnet, plagioclase, zircon, and tourmaline (Fig. five). Of these, garnet and plagioclase are suitable to reports of metamorphic P-T paths, and zircon is å°åŒ—ç¡¬ç¢Ÿæ•‘æ´ relevant to willpower from the timing of petrologic functions.
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