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An unzoned mineral that is often zoned at very low-medium metamorphic grades has both experienced superior temperature disorders or was under no circumstances zoned (owing to an easy reaction heritage at confined P-T or to expansion totally at significant-T). Reaction textures Some metamorphic rocks consist of evidence for incomplete reactions or other textural proof for Section of the P-T path. A simple case in point could be the partial alternative of andalusite by sillimanite (Fig. 6a) via the polymorphic transformation of andalusite to sillimanite. Textural evidence may be helpful in instances the place the reactants are already totally eaten if The form of one or more reactants are preserved; for example, pseudomorphs (Figs. 6b-d). An example of a far more intricate reaction texture requires the development of coronas , which here encompass a number of shells (rims, moats) of the mineral or minerals about a central (reactant) stage (Fig. 6e). In several instances, coronas also entail the great-scale intergrowth of minerals in the texture known as symplectite (Figs. 6e-file).

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P-T path condition by by itself doesn't give a exclusive interpretation of tectonic procedure or metamorphic driving forces. Such as, clockwise paths can kind in continental collision belts of subduction zones. Similarly, some subduction zone rocks report clockwise paths and a few history counterclockwise paths. Even so, the integration of P-T route qualities, time/level data, structural information, and various petrologic details can offer considerable information about metamorphic and tectonic procedures.

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