An unzoned mineral that is typically zoned at very low-medium metamorphic grades has either professional substantial temperature conditions or was under no circumstances zoned (owing to a simple response background at confined P-T or to progress entirely at substantial-T). Reaction textures Some metamorphic rocks consist of evidence for incomplete reactions or other textural proof for Portion of the P-T route. An easy case in point would be the partial replacement of andalusite by sillimanite (Fig. 6a) with the polymorphic transformation of andalusite to sillimanite. Textural evidence may additionally be useful in situations exactly where the reactants are totally eaten if the shape of a number of reactants are preserved; for instance, pseudomorphs (Figs. 6b-d). An illustration of a more advanced reaction texture includes the formation of coronas , which include one or more shells (rims, moats) of a mineral or minerals all-around a central (reactant) stage (Fig. 6e). In several circumstances, coronas also contain the fantastic-scale intergrowth Click Here of minerals inside of a texture called symplectite (Figs. 6e-file).
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P-T path form by alone would not provide a special interpretation of tectonic approach or metamorphic driving forces. Such as, clockwise paths can form in continental collision belts of subduction zones. Likewise, some subduction zone rocks file clockwise paths and many history counterclockwise paths. Nevertheless, The combination of P-T route qualities, time/charge information, structural facts, together with other petrologic facts can offer considerable details about metamorphic and tectonic processes.
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