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An unzoned mineral that is often zoned at reduced-medium metamorphic grades has both expert large temperature circumstances or was hardly ever zoned (owing to a straightforward reaction history at restricted P-T or to advancement solely at higher-T). Response textures Some metamorphic rocks incorporate proof for incomplete reactions or other textural evidence for Section of the P-T path. A simple instance may be the partial alternative of andalusite by sillimanite (Fig. 6a) with the polymorphic transformation of andalusite to sillimanite. Textural proof may additionally be handy in conditions where by the reactants have been absolutely eaten if The form of a number of reactants are preserved; such as, pseudomorphs (Figs. 6b-d). An illustration of a far more complex reaction texture involves the formation of coronas , which consist of one or more shells (rims, moats) of a mineral or minerals around a central (reactant) phase (Fig. 6e). In several cases, coronas also contain the great-scale intergrowth of minerals in a texture known as symplectite (Figs. 6e-f).

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