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of other minerals. By way of example, garnets frequently contain inclusions of minerals that were current inside the rock matrix given that the garnet grew, but that were not absolutely eliminated by metamorphic reactions through progressive metamorphism.
Crystals that have various regions with distinct compositions are zoned . A quite common zoning sample consists of a difference in composition of a mineral's Middle (core) when compared with its rim, and concentric rings of various compositions organized concerning the core as well as the rim (Fig. 5). Minerals that generally exhibit this sort of zoning in the foremost or trace features are garnet, plagioclase, zircon, and tourmaline (Fig. 5). Of those, garnet and more info plagioclase are appropriate to scientific studies of metamorphic P-T paths, and zircon is pertinent to willpower on the timing of petrologic gatherings.
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