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The growing garnets surrounded these relict minerals as being the garnets grew, as well as the relict minerals are preserved as mineralogical proof of an before stage during the metamorphic historical past of the rock.
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Crystals which have distinctive regions with distinctive compositions are zoned . A quite common zoning sample will involve a change in composition of the mineral's Heart (Main) in comparison to its rim, and concentric rings of various compositions arranged concerning the core plus Clicking Here the rim (Fig. five). Minerals that generally show this sort of zoning in the major or trace aspects are garnet, plagioclase, zircon, and tourmaline (Fig. five). Of those, garnet and plagioclase are relevant to reports of metamorphic P-T paths, and zircon is related to resolve from the timing of petrologic gatherings.
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