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An unzoned mineral that is usually zoned at lower-medium metamorphic grades has both professional high temperature ailments or was by no means zoned (owing to an easy reaction historical past at minimal P-T or to advancement entirely at high-T). Reaction textures Some metamorphic rocks have evidence for incomplete reactions or other textural evidence for Section of the P-T route. A straightforward illustration is definitely the partial substitution of andalusite by sillimanite (Fig. 6a) by the polymorphic transformation of andalusite to sillimanite. Textural evidence might also be helpful in circumstances in which the reactants are already absolutely eaten if The form of a number of reactants are preserved; one example is, pseudomorphs (Figs. 6b-d). An illustration of a more complex response texture entails the formation of coronas , which consist of a number of shells (rims, moats) of a mineral or minerals all over a central (reactant) stage (Fig. 6e). In several circumstances, coronas also contain the good-scale intergrowth of minerals within a texture known as symplectite (Figs. 6e-f).

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P-T path condition by by itself won't supply a unique interpretation of tectonic system or metamorphic driving forces. One example is, clockwise paths can variety in continental collision belts of subduction zones. Similarly, some subduction zone rocks file clockwise paths plus some document counterclockwise paths. Having said that, The combination of P-T path features, time/fee information and facts, structural info, as well as other petrologic information and facts can provide major details about metamorphic and tectonic procedures.

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