An unzoned mineral that is typically zoned at minimal-medium metamorphic grades has both expert superior temperature situations or was never zoned (owing to a simple response history at confined P-T or to progress fully at large-T). Reaction textures Some metamorphic rocks comprise proof for incomplete reactions or other textural evidence for Element of the P-T route. A simple case in point would be the partial replacement of andalusite by sillimanite (Fig. 6a) via the polymorphic transformation of andalusite to sillimanite. Textural evidence could also be helpful in cases where the reactants have been totally consumed if The form of one or more reactants are preserved; for example, pseudomorphs (Figs. 6b-d). An example of a more intricate response texture includes the development of coronas , which encompass a number of shells (rims, moats) Clicking Here of the mineral or minerals all-around a central (reactant) section (Fig. 6e). In several scenarios, coronas also contain the great-scale intergrowth of minerals inside of a texture known as symplectite (Figs. 6e-f).
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