An unzoned mineral that is usually zoned at lower-medium metamorphic grades has both professional higher temperature situations or was never zoned (owing to a straightforward reaction history at minimal P-T or to development entirely at superior-T). Reaction textures Some metamorphic rocks contain proof for incomplete reactions or other textural proof for part of the P-T path. A simple instance may be the partial substitute of andalusite by sillimanite (Fig. 6a) because of the polymorphic transformation of andalusite to sillimanite. Textural proof may be practical in conditions where the reactants happen to be totally consumed if the shape of one or more reactants are preserved; as an example, pseudomorphs (Figs. 6b-d). An example of a more sophisticated reaction texture requires the formation of coronas , which consist of a number of shells (rims, moats) of the mineral or minerals all-around a central (reactant) section (Fig. 6e). In several cases, coronas also involve the fine-scale intergrowth of minerals inside a texture referred to as symplectite (Figs. 6e-f).
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