An unzoned mineral that is typically zoned at small-medium metamorphic grades has both experienced significant temperature conditions or was hardly ever zoned (owing to an easy reaction heritage at restricted P-T or to advancement totally at high-T). Response textures Some metamorphic rocks contain evidence for incomplete reactions or other textural proof for Portion of the P-T route. A simple instance could be the partial alternative of andalusite by sillimanite (Fig. 6a) from the polymorphic transformation of andalusite to sillimanite. Textural proof might also be handy in circumstances where the reactants are absolutely eaten if the shape of a number of reactants are preserved; as an example, pseudomorphs (Figs. 6b-d). An illustration of a more complex response texture involves the development of coronas , which encompass one or more shells (rims, moats) of the mineral or minerals close to a central (reactant) section (Fig. 6e). In lots of conditions, coronas also include the great-scale intergrowth of minerals within a texture often called symplectite (Figs. 6e-f).
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The growing garnets surrounded these relict minerals as the garnets grew, as well as relict minerals are preserved as mineralogical proof of the before phase while in the metamorphic historical past in the rock.
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