An unzoned mineral that is typically zoned at low-medium metamorphic grades has either knowledgeable substantial temperature conditions or was by no means zoned (owing to a simple response historical past at minimal P-T or to development fully at higher-T). Reaction textures Some metamorphic rocks comprise proof for incomplete reactions or other textural proof for Portion of the P-T route. An easy example is the partial substitution of andalusite by sillimanite (Fig. 6a) through the polymorphic transformation of andalusite to sillimanite. Textural evidence may be practical in situations exactly where the reactants are absolutely consumed if The form of one or more reactants are preserved; such as, pseudomorphs (Figs. 6b-d). An example of a more complicated response texture includes the formation of coronas , which include one or more shells (rims, moats) of a mineral or minerals all-around a central (reactant) stage (Fig. 6e). In several conditions, coronas also involve the high-quality-scale intergrowth of minerals inside a texture referred to as symplectite (Figs. 6e-file).
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