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An unzoned mineral that is often zoned at small-medium metamorphic grades has either skilled large temperature problems or was under no circumstances zoned (owing to a straightforward reaction history at restricted P-T or to progress fully at significant-T). Response textures Some metamorphic rocks contain evidence for incomplete reactions or other textural evidence for Portion of the P-T path. A straightforward instance will be the partial substitute of andalusite by sillimanite (Fig. 6a) by the polymorphic transformation of andalusite to sillimanite. Textural proof may be helpful in situations wherever the reactants are absolutely consumed if the shape of one or more reactants are preserved; as an example, pseudomorphs (Figs. 6b-d). An example of a more advanced response 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 many situations, coronas also require the high-quality-scale intergrowth of minerals in a very texture often called symplectite (Figs. 6e-file).
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