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An unzoned mineral that is often zoned at small-medium metamorphic grades has both seasoned significant temperature situations or was never ever zoned (owing to a straightforward reaction historical past at constrained P-T or to progress totally at significant-T). Response textures Some metamorphic rocks incorporate proof for incomplete reactions or other textural evidence for Portion of the P-T path. A simple example will be the partial substitution of andalusite by sillimanite (Fig. 6a) via the polymorphic transformation of andalusite to sillimanite. Textural evidence might also be handy in circumstances where the reactants happen to be entirely consumed if The form of a number of reactants are preserved; by way of example, pseudomorphs (Figs. 6b-d). An illustration of a far more complicated reaction texture includes the development of coronas , which consist of a number of shells (rims, moats) of a mineral or minerals Check This Out all over a central (reactant) phase (Fig. 6e). In many conditions, coronas also involve the high-quality-scale intergrowth of minerals inside a texture often known as symplectite (Figs. 6e-f).

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