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of other minerals. One example is, garnets generally have inclusions of minerals that were current within the rock matrix as the garnet grew, but which were not absolutely eradicated by metamorphic reactions for the duration of progressive metamorphism.
Crystals that have different areas with distinctive compositions are zoned . A very common zoning sample entails a change in composition of the mineral's Middle (Main) when compared with its rim, and concentric rings of various compositions arranged amongst the core along with the website rim (Fig. 5). Minerals that ordinarily demonstrate this kind of zoning in the most important or trace elements are garnet, plagioclase, zircon, and tourmaline (Fig. 5). Of these, garnet and plagioclase are suitable to reports of metamorphic P-T paths, and zircon is suitable to dedication from the timing of petrologic gatherings.
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