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An unzoned mineral that is usually zoned at very low-medium metamorphic grades has possibly professional large temperature disorders or was never zoned (owing to a simple reaction historical past at minimal P-T or to expansion entirely at significant-T). Reaction textures Some metamorphic rocks contain evidence for incomplete reactions or other textural evidence for Portion of the P-T path. A straightforward illustration is the partial replacement of andalusite by sillimanite (Fig. 6a) by the polymorphic transformation of andalusite to sillimanite. Textural proof can also be valuable in scenarios where the reactants have already been completely eaten if The form of one or more reactants are preserved; such as, pseudomorphs (Figs. 6b-d). An illustration of a more advanced response texture includes the formation of coronas , which consist of a number of shells (rims, moats) of the mineral or minerals about a central (reactant) phase (Fig. 6e). In several cases, coronas also entail the fine-scale intergrowth of minerals inside of a texture often called symplectite (Figs. 6e-f).

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of other minerals. As an example, garnets generally include inclusions of minerals that were existing from the rock matrix because the garnet grew, but that were not completely eliminated by metamorphic reactions for the duration of progressive metamorphism.

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