An unzoned mineral that is often zoned at minimal-medium metamorphic grades has either knowledgeable significant temperature situations or was hardly ever zoned (owing to an easy response history at restricted P-T or to progress totally at substantial-T). Response textures Some metamorphic rocks consist of proof for incomplete reactions or other textural proof for part of the P-T path. A simple example will be the partial substitute of andalusite by sillimanite (Fig. 6a) with the polymorphic transformation of andalusite to sillimanite. Textural proof may additionally be handy in scenarios where by the reactants have been completely consumed if the shape of one or more reactants are preserved; for instance, pseudomorphs (Figs. 6b-d). An example of a more complicated reaction texture entails the formation of coronas , which consist of one or more shells (rims, moats) of a mineral or minerals about a central (reactant) phase (Fig. 6e). In many instances, coronas also include the good-scale intergrowth of minerals inside a texture called symplectite (Figs. 6e-f).
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