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An unzoned mineral that is usually zoned at very low-medium metamorphic grades has either professional substantial temperature ailments or was never ever zoned (owing to a simple response background at limited P-T or to progress completely at superior-T). Response textures Some metamorphic rocks have evidence for incomplete reactions or other textural proof for Portion of the P-T path. A straightforward instance could be the partial substitute of andalusite by sillimanite (Fig. 6a) by the polymorphic transformation of andalusite to sillimanite. Textural proof might also be handy in circumstances where the reactants are already completely eaten if The form of a number of reactants are preserved; for example, pseudomorphs (Figs. 6b-d). An illustration of a far more intricate response texture includes the formation of coronas , which include one or more shells (rims, moats) of a mineral or minerals all-around a central (reactant) period (Fig. 6e). In many situations, coronas also involve the wonderful-scale intergrowth of minerals inside a texture often called symplectite (Figs. 6e-file).

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The trajectory and condition of the P-T path, the prices of metamorphic processes, plus the period of metamorphism are a operate of the supply of warmth and also the mechanisms of burial and unroofing (if pressure improve is included).

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P-T path shape by by itself will not provide a one of a kind interpretation of tectonic system or metamorphic driving forces. One example is, clockwise paths can type in continental collision belts of subduction zones. In the same way, some subduction zone rocks report clockwise paths and a few history counterclockwise paths. On the other hand, the integration of P-T route qualities, time/price facts, structural information, along read more with other petrologic details can provide sizeable specifics of metamorphic and tectonic processes.

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