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Crystals that have distinct areas with diverse compositions are zoned . A quite common zoning sample involves a difference in composition of a mineral's center (core) in comparison with its rim, and concentric rings of different compositions organized amongst the core as well as the rim (Fig. 5). Minerals that normally display this sort of zoning in the major or å°ä¸ç¡¬ç¢Ÿæ•‘æ´ trace factors are garnet, plagioclase, zircon, and tourmaline (Fig. 5). Of such, garnet and plagioclase are pertinent to scientific studies of metamorphic P-T paths, and zircon is appropriate to willpower on the timing of petrologic gatherings.
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