An unzoned mineral that is often zoned at low-medium metamorphic grades has both expert superior temperature circumstances or was under no circumstances zoned (owing to an easy response record at restricted P-T or to expansion entirely at significant-T). Response textures Some metamorphic rocks contain proof for incomplete reactions or other textural evidence for Portion of the P-T route. An easy illustration is definitely the partial alternative of andalusite by sillimanite (Fig. 6a) through the polymorphic transformation of andalusite to sillimanite. Textural proof could also be handy in cases where by the reactants are already wholly consumed if The form of a number of reactants are preserved; for instance, pseudomorphs (Figs. 6b-d). An illustration of a more complicated response texture requires the formation of coronas , which consist of one or more shells (rims, moats) of the mineral or minerals all around a central (reactant) stage (Fig. 6e). In several circumstances, coronas also include the fantastic-scale intergrowth of minerals within a texture generally known as symplectite (Figs. 6e-f).
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P-T route condition by by itself doesn't offer a distinctive interpretation of tectonic procedure or metamorphic driving forces. By way Click Here of example, clockwise paths can sort in continental collision belts of subduction zones. Similarly, some subduction zone rocks record clockwise paths plus some document counterclockwise paths. Nevertheless, the integration of P-T path characteristics, time/level data, structural information, together with other petrologic facts can offer important details about metamorphic and tectonic procedures.
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