An unzoned mineral that is usually zoned at small-medium metamorphic grades has either skilled large temperature ailments or was never zoned (owing to a simple reaction historical past at constrained P-T or to expansion completely at substantial-T). Reaction textures Some metamorphic rocks have evidence for incomplete reactions or other textural evidence for Section of the P-T path. An easy case in point would be the partial substitution of andalusite by sillimanite (Fig. 6a) by the polymorphic transformation of andalusite to sillimanite. Textural evidence could also be useful in conditions exactly where the reactants have already been entirely eaten if The form of one or more reactants are preserved; for instance, pseudomorphs (Figs. 6b-d). An example of a far å°åŒ—ç¡¬ç¢Ÿæ•‘æ´ more sophisticated reaction texture includes the formation of coronas , which encompass a number of shells (rims, moats) of a mineral or minerals around a central (reactant) period (Fig. 6e). In many scenarios, coronas also entail the fine-scale intergrowth of minerals in the texture referred to as symplectite (Figs. 6e-file).
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