An unzoned mineral that is often zoned at small-medium metamorphic grades has both seasoned significant temperature disorders or was never zoned (owing to a simple response historical past at confined P-T or to development entirely at large-T). Response textures Some metamorphic rocks have evidence for incomplete reactions or other textural proof for A part of the P-T path. An easy case in point could be the partial alternative of andalusite by sillimanite (Fig. 6a) via the polymorphic transformation of andalusite to sillimanite. Textural proof may also be practical in cases where the reactants have already been entirely consumed if the shape of one or more reactants are preserved; as an example, pseudomorphs (Figs. 6b-d). An illustration of a far more advanced reaction texture requires the formation of coronas , which include one or more shells (rims, moats) of a mineral or minerals around a central (reactant) period (Fig. 6e). In several conditions, coronas also contain the great-scale intergrowth of minerals in a texture referred to as symplectite (Figs. 6e-f).
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