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An unzoned mineral that is typically zoned at very low-medium metamorphic grades has possibly seasoned large temperature disorders or was hardly ever zoned (owing to a simple response heritage at limited P-T or to development totally at higher-T). Reaction textures Some metamorphic rocks contain proof for incomplete reactions or other textural proof for Component of the P-T route. A straightforward case in point may be the partial substitution of andalusite by sillimanite (Fig. 6a) through the polymorphic transformation of andalusite to sillimanite. Textural proof might also be helpful in scenarios the place the reactants happen to be wholly eaten if The form of a number of reactants are preserved; such as, pseudomorphs (Figs. 6b-d). An illustration of a far more intricate reaction texture requires the formation of coronas , which encompass one or more shells (rims, moats) of the mineral or minerals all-around a central (reactant) stage (Fig. 6e). In several circumstances, coronas also Do you agree involve the wonderful-scale intergrowth of minerals within a texture often called symplectite (Figs. 6e-file).

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