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An unzoned mineral that is usually zoned at lower-medium metamorphic grades has possibly professional superior temperature conditions or was by no means zoned (owing to a straightforward reaction heritage at constrained P-T or to expansion solely at superior-T). Reaction textures Some metamorphic rocks incorporate proof for incomplete reactions or other textural proof for Element of the P-T route. A straightforward case in point is the partial substitute of andalusite by sillimanite (Fig. 6a) through the polymorphic transformation of andalusite to sillimanite. Textural evidence may additionally be handy in conditions exactly where the reactants are actually completely consumed if the shape of one or more reactants are preserved; for example, pseudomorphs (Figs. 6b-d). An example of a far more Click Here advanced reaction texture consists of the development of coronas , which encompass one or more shells (rims, moats) of the mineral or minerals all around a central (reactant) period (Fig. 6e). In lots of circumstances, coronas also include the fantastic-scale intergrowth of minerals within a texture called symplectite (Figs. 6e-f).

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