An unzoned mineral that is typically zoned at very low-medium metamorphic grades has either seasoned high temperature circumstances or was in no way zoned (owing to a straightforward response record at restricted P-T or to development totally at substantial-T). Reaction textures Some metamorphic rocks comprise proof for incomplete reactions or other textural proof for part of the P-T path. A simple illustration would be the partial substitute of andalusite by sillimanite (Fig. 6a) with the polymorphic transformation of andalusite to sillimanite. Textural evidence may be useful in instances where by the reactants are entirely consumed if The form of a number of reactants are preserved; for instance, pseudomorphs (Figs. 6b-d). An illustration of a far more advanced response texture entails the formation of coronas , which consist of a number of shells (rims, moats) of the mineral or minerals close to a central (reactant) phase (Fig. 6e). In lots of conditions, coronas also contain the fine-scale intergrowth of minerals inside of a texture often called symplectite (Figs. 6e-file).
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