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The rising garnets surrounded these relict minerals as being the garnets grew, and also the relict minerals are preserved as mineralogical proof of an previously stage in the metamorphic background from the rock.
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Crystals that have unique regions with diverse compositions are zoned . A quite common zoning sample will involve a difference in composition of a mineral's center (Main) as compared to its rim, and concentric rings of different compositions arranged between the Main and also the rim (Fig. 5). Minerals that usually present this type of zoning in the major or trace factors are garnet, plagioclase, zircon, and tourmaline (Fig. five). Of these, garnet and plagioclase are suitable to experiments of metamorphic P-T paths, and zircon is suitable to resolve with the timing of petrologic activities.
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