An unzoned mineral that is often zoned at lower-medium metamorphic grades has either professional substantial temperature circumstances or was never zoned (owing to an easy response historical past at limited P-T or to growth completely at higher-T). Response textures Some metamorphic rocks contain evidence for incomplete reactions or other textural evidence for Element of the P-T route. An easy illustration is definitely the partial replacement of andalusite by sillimanite (Fig. 6a) through the polymorphic transformation of andalusite to sillimanite. Textural proof could also be helpful in cases exactly where the reactants have already been entirely consumed if the shape of one or more reactants are preserved; by way of example, pseudomorphs (Figs. 6b-d). An illustration of a more sophisticated reaction texture includes the development of coronas , which include a number of shells (rims, moats) of the Discover More Here mineral or minerals all around a central (reactant) period (Fig. 6e). In lots of situations, coronas also require the high-quality-scale intergrowth of minerals in a very texture often known as symplectite (Figs. 6e-file).
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