An unzoned mineral that is usually zoned at very low-medium metamorphic grades has either skilled substantial temperature ailments or was hardly ever zoned (owing to a simple reaction historical past at minimal P-T or to expansion solely at higher-T). Reaction textures Some metamorphic rocks have proof for incomplete reactions or other textural proof for Element of the P-T path. A straightforward case in point is the partial substitution of andalusite by sillimanite (Fig. 6a) through the polymorphic transformation of andalusite to sillimanite. Textural proof may additionally be practical in circumstances exactly where the reactants are actually wholly eaten if The form of a number of reactants are preserved; one example is, pseudomorphs (Figs. 6b-d). An illustration of a far more complicated reaction texture entails the development of coronas , which encompass a number of shells (rims, moats) of a mineral or minerals all-around a central (reactant) period (Fig. 6e). In many scenarios, coronas also contain the great-scale intergrowth of minerals in Click This Link a texture known as symplectite (Figs. 6e-f).
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