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An unzoned mineral that is usually zoned at minimal-medium metamorphic grades has either expert large temperature circumstances or was hardly ever zoned (owing to a straightforward response history at confined P-T or to progress completely at large-T). Reaction textures Some metamorphic rocks consist of evidence for incomplete reactions or other textural evidence for Component of the P-T path. A simple instance is definitely the partial substitution of andalusite by sillimanite (Fig. 6a) because of the polymorphic transformation of andalusite to sillimanite. Textural evidence might also be helpful in instances where by the reactants are already entirely eaten if the shape of one or more reactants are preserved; such Continued as, pseudomorphs (Figs. 6b-d). An example of a more advanced reaction texture will involve the formation of coronas , which encompass a number of shells (rims, moats) of a mineral or minerals all over a central (reactant) stage (Fig. 6e). In several circumstances, coronas also involve the high-quality-scale intergrowth of minerals inside a texture often called symplectite (Figs. 6e-f).

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