An unzoned mineral that is typically zoned at minimal-medium metamorphic grades has both expert superior temperature conditions or was in no way zoned (owing to an easy response heritage at confined P-T or to advancement entirely at higher-T). Reaction textures Some metamorphic rocks have evidence for incomplete reactions or other textural evidence for A part of the P-T path. A simple example may be the partial substitute of andalusite by sillimanite (Fig. 6a) with the polymorphic transformation of andalusite to sillimanite. Textural proof could also be useful in cases exactly where the reactants have already been completely eaten if the shape of a number of reactants are preserved; such as, pseudomorphs (Figs. 6b-d). An illustration of a more complex response texture includes the formation of coronas , which consist of one or more shells (rims, moats) of a mineral or minerals all over a central (reactant) stage (Fig. 6e). In several conditions, coronas also entail the good-scale intergrowth of minerals inside of a texture referred to as symplectite (Figs. 6e-f).
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