An unzoned mineral that is often zoned at small-medium metamorphic grades has either knowledgeable substantial temperature ailments or was hardly ever zoned (owing to a straightforward reaction background at restricted P-T or to progress totally at significant-T). Response textures Some metamorphic rocks comprise proof for incomplete reactions or other textural proof for part of the P-T path. A simple case in point is the partial replacement of andalusite by sillimanite (Fig. 6a) because of the polymorphic transformation of andalusite to sillimanite. Textural proof might also be valuable in cases wherever the reactants are already completely eaten if The form Click Here of one or more reactants are preserved; by way of example, pseudomorphs (Figs. 6b-d). An illustration of a more intricate response texture includes the formation of coronas , which consist of one or more shells (rims, moats) of a mineral or minerals all-around a central (reactant) phase (Fig. 6e). In many cases, coronas also involve the good-scale intergrowth of minerals in a very texture often known as symplectite (Figs. 6e-file).
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