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An unzoned mineral that is often zoned at low-medium metamorphic grades has either knowledgeable substantial temperature problems or was hardly ever zoned (owing to a straightforward response history at limited P-T or to development totally at substantial-T). Response textures Some metamorphic rocks consist of proof for incomplete reactions or other textural proof for part of the P-T path. A simple example may be the partial substitute of andalusite by sillimanite (Fig. 6a) with the polymorphic transformation of andalusite to sillimanite. Textural proof may be handy in conditions where by the reactants have been entirely consumed if the shape of a number of reactants are preserved; one example is, pseudomorphs (Figs. 6b-d). An illustration of a far more complex response texture involves the formation of coronas , which encompass a number of shells (rims, moats) of the mineral or minerals around a central (reactant) phase (Fig. 6e). In many instances, Do you agree coronas also entail the great-scale intergrowth of minerals in the texture generally known as symplectite (Figs. 6e-f).
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