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An unzoned mineral that is often zoned at low-medium metamorphic grades has both expert superior temperature conditions or was by no means zoned (owing to an easy reaction historical past at minimal P-T or to advancement entirely at high-T). Reaction textures Some metamorphic rocks include evidence for incomplete reactions or other textural evidence for Portion of the P-T route. An easy case in point will be the partial alternative of andalusite by sillimanite (Fig. 6a) because of the polymorphic transformation of andalusite to sillimanite. Textural proof may also be helpful in instances in which the reactants have already been fully eaten if The form of a number of reactants are preserved; such as, pseudomorphs (Figs. 6b-d). An illustration of a far more complex reaction texture entails the development of coronas , which consist of one or more shells (rims, moats) of a mineral or minerals all over a central (reactant) period (Fig. 6e). In lots of situations, coronas also entail the fantastic-scale intergrowth of minerals inside a texture often called symplectite (Figs. 6e-file).

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of other minerals. By way of example, garnets typically include inclusions of minerals that were existing from the rock matrix since the garnet grew, but that were not totally removed by metamorphic reactions through progressive metamorphism.

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