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An unzoned mineral that is typically zoned at reduced-medium metamorphic grades has both expert high temperature circumstances or was never zoned (owing to a straightforward response heritage at confined P-T or to growth entirely at large-T). Response textures Some metamorphic rocks include proof for incomplete reactions or other textural proof for part of the P-T path. A simple example could be the partial alternative of andalusite by sillimanite (Fig. 6a) with the polymorphic transformation of andalusite to sillimanite. Textural proof might also be handy in scenarios where by the reactants happen to be entirely eaten if the shape of a number of reactants are preserved; by way of example, pseudomorphs (Figs. 6b-d). An illustration of a more advanced response texture requires the formation of coronas , which include a number of shells (rims, moats) of the mineral or minerals all over a central (reactant) period (Fig. 6e). In several scenarios, coronas also contain the great-scale intergrowth of minerals in a texture referred to as symplectite (Figs. 6e-f).

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At the height of metamorphism, the mineral assemblage presumably equilibrated, and no (or small) even more response took place since the rock cooled and decompressed en path to the Earth's surface.

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