An unzoned mineral that is usually zoned at lower-medium metamorphic grades has possibly professional high temperature circumstances or was never ever zoned (owing to an easy response record at limited P-T or to development totally at superior-T). Response textures Some metamorphic rocks consist of evidence for incomplete reactions or other textural evidence for Portion of the P-T path. A straightforward example will be the partial replacement of andalusite by sillimanite (Fig. 6a) from the polymorphic transformation of andalusite to sillimanite. Textural evidence could also be helpful in scenarios wherever the reactants are completely consumed if The form of a number of reactants are preserved; one example is, pseudomorphs (Figs. 6b-d). An illustration of a far more elaborate reaction texture involves the formation of coronas , which consist of one or more shells (rims, moats) of a mineral or minerals close to a central (reactant) stage (Fig. 6e). In lots of circumstances, coronas also entail the fantastic-scale intergrowth of minerals in the texture often known as symplectite (Figs. 6e-file).
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