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An unzoned mineral that is typically zoned at reduced-medium metamorphic grades has both seasoned significant temperature disorders or was never zoned (owing to a simple reaction historical past at minimal P-T or to expansion solely at high-T). Reaction textures Some metamorphic rocks include evidence for incomplete reactions or other textural evidence for Component of the P-T path. An easy case in point would be the partial substitution of andalusite by sillimanite (Fig. 6a) with the polymorphic transformation of andalusite to sillimanite. Textural proof might also be valuable in scenarios the place the reactants have been completely consumed if the shape of one or more reactants are preserved; such as, pseudomorphs (Figs. 6b-d). An example of a more complicated reaction texture entails the development of coronas , which encompass one Click Here or more shells (rims, moats) of the mineral or minerals around a central (reactant) phase (Fig. 6e). In many conditions, coronas also involve the good-scale intergrowth of minerals inside a texture generally known as symplectite (Figs. 6e-f).

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At the peak of metamorphism, the mineral assemblage presumably equilibrated, and no (or little) further more response happened given that the rock cooled and decompressed en route to the Earth's surface.

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