An unzoned mineral that is typically zoned at low-medium metamorphic grades has possibly skilled superior temperature problems or was never ever zoned (owing to a simple response background at restricted P-T or to advancement entirely at large-T). Reaction textures Some metamorphic rocks consist of evidence for incomplete reactions or other textural evidence for Component of the P-T path. An easy instance could be the partial replacement of andalusite by sillimanite (Fig. 6a) because of the polymorphic transformation of andalusite to sillimanite. Textural proof can also be practical in circumstances exactly where the reactants are actually fully eaten if The form of a number of reactants are preserved; for instance, pseudomorphs (Figs. 6b-d). An example of å°åŒ—ç¡¬ç¢Ÿæ•‘æ´ a more intricate response texture consists of the development of coronas , which include one or more shells (rims, moats) of a mineral or minerals all around a central (reactant) period (Fig. 6e). In several cases, coronas also require the good-scale intergrowth of minerals inside of a texture often called symplectite (Figs. 6e-file).
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