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of other minerals. For example, garnets commonly include inclusions of minerals that were present inside the rock matrix as being the garnet grew, but which were not wholly removed by metamorphic reactions all through progressive metamorphism.

Crystals that have unique areas with distinctive Click Here compositions are zoned . A quite common zoning pattern requires a variation in composition of a mineral's Heart (core) compared to its rim, and concentric rings of different compositions organized amongst the core and the rim (Fig. 5). Minerals that typically demonstrate this type of zoning in the main or trace elements are garnet, plagioclase, zircon, and tourmaline (Fig. five). Of those, garnet and plagioclase are suitable to studies of metamorphic P-T paths, and zircon is pertinent to perseverance of your timing of petrologic activities.

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