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An unzoned mineral that is often zoned at reduced-medium metamorphic grades has possibly knowledgeable large temperature circumstances or was never ever zoned (owing to a simple response record at restricted P-T or to progress solely at substantial-T). Response textures Some metamorphic rocks comprise evidence for incomplete reactions or other textural evidence for Section of the P-T route. An easy illustration could be the partial substitute of andalusite by sillimanite (Fig. 6a) with the polymorphic transformation of andalusite to sillimanite. Textural evidence might also be helpful in situations the place the reactants are completely consumed if The form of one or more reactants are preserved; for instance, pseudomorphs (Figs. 6b-d). An example of a more sophisticated reaction texture includes the formation of coronas , which include a number of shells (rims, moats) of the mineral or minerals all around a central (reactant) period (Fig. 6e). In several scenarios, coronas also require the great-scale intergrowth of minerals inside of a texture often called symplectite (Figs. 6e-f).

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