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of other minerals. As an example, garnets typically include inclusions of minerals that were existing inside the rock matrix because the garnet grew, but that were not wholly removed by metamorphic reactions for the duration of progressive metamorphism.

Crystals that have distinct regions with distinct compositions are zoned . A quite common zoning sample includes a variance in composition of a mineral's Centre (Main) in comparison with its rim, and concentric rings of various compositions arranged between the Main along with the rim (Fig. 5). Minerals that generally clearly show such a zoning in the main or trace components are garnet, plagioclase, zircon, and tourmaline (Fig. 5). Of these, garnet and Check This Out plagioclase are appropriate to research of metamorphic P-T paths, and zircon is suitable to determination on the timing of petrologic situations.

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