An unzoned mineral that is usually zoned at very low-medium metamorphic grades has possibly seasoned superior temperature problems or was under no circumstances zoned (owing to a straightforward reaction historical past at restricted P-T or to growth fully at higher-T). Reaction textures Some metamorphic rocks contain evidence for incomplete reactions or other textural proof for part of the P-T route. A straightforward illustration may be the partial substitute of andalusite by sillimanite (Fig. 6a) because of the polymorphic transformation of andalusite to sillimanite. Textural proof can also be practical in situations the place the reactants are fully eaten if the shape Continue of one or more reactants are preserved; such as, pseudomorphs (Figs. 6b-d). An example of a more elaborate response texture requires the formation of coronas , which consist of a number of shells (rims, moats) of a mineral or minerals about a central (reactant) section (Fig. 6e). In several scenarios, coronas also involve the high-quality-scale intergrowth of minerals in the texture often called symplectite (Figs. 6e-f).
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