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An unzoned mineral that is usually zoned at reduced-medium metamorphic grades has both knowledgeable high temperature ailments or was never zoned (owing to an easy reaction heritage at constrained P-T or to development entirely at high-T). Reaction textures Some metamorphic rocks comprise proof for incomplete reactions or other textural evidence for Portion of the P-T route. A straightforward instance will be the partial alternative of andalusite by sillimanite (Fig. 6a) by the polymorphic transformation of andalusite to sillimanite. Textural evidence could also be beneficial in circumstances where the reactants are fully eaten if the shape of a number of reactants are preserved; for instance, pseudomorphs (Figs. 6b-d). An example of a more complicated reaction texture entails the development of coronas , which include one or more shells (rims, moats) of the mineral or minerals close to a central (reactant) period (Fig. 6e). In lots of conditions, coronas also require the high-quality-scale intergrowth of minerals in a very texture known as symplectite (Figs. 6e-f).

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At the height of metamorphism, the mineral assemblage presumably equilibrated, and no (or minor) additional response passed off since the rock cooled and decompressed en route to the Earth's area.

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