An unzoned mineral that is typically zoned at reduced-medium metamorphic grades has either professional significant temperature problems or was in no way zoned (owing to a simple response record at limited P-T or to growth completely at large-T). Response textures Some metamorphic rocks comprise proof for incomplete reactions or other textural evidence for A part of the P-T route. A simple example may be the partial substitution of andalusite by sillimanite (Fig. 6a) by the polymorphic transformation of andalusite to sillimanite. Textural evidence might also be helpful in circumstances the place the reactants are already absolutely eaten if The form of a number of reactants are preserved; such as, pseudomorphs (Figs. 6b-d). An illustration of a å°ä¸ç¡¬ç¢Ÿæ•‘æ´ far more elaborate response texture will involve the formation of coronas , which encompass a number of shells (rims, moats) of a mineral or minerals close to a central (reactant) stage (Fig. 6e). In lots of scenarios, coronas also require the fantastic-scale intergrowth of minerals within a texture known as symplectite (Figs. 6e-f).
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