An unzoned mineral that is often zoned at small-medium metamorphic grades has either skilled superior temperature circumstances or was in no way zoned (owing to an easy response heritage at limited P-T or to growth completely at large-T). Response textures Some metamorphic rocks incorporate proof for incomplete reactions or other textural evidence for Section of the P-T route. A straightforward illustration is the partial alternative of andalusite by sillimanite (Fig. 6a) with the polymorphic transformation of andalusite to sillimanite. Textural proof might also be helpful in circumstances where by the reactants have been completely eaten if the shape of one or more reactants are preserved; one example is, pseudomorphs (Figs. 6b-d). An example of a far more sophisticated reaction texture will involve the formation of coronas , which include a number of shells (rims, moats) of the mineral or minerals around a central (reactant) phase (Fig. 6e). In lots of scenarios, coronas also contain the great-scale intergrowth of minerals inside of a texture referred to as symplectite (Figs. 6e-file).
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