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An unzoned mineral that is usually zoned at lower-medium metamorphic grades has both expert superior temperature circumstances or was under no circumstances zoned (owing to a simple reaction heritage at confined P-T or to advancement solely at large-T). Reaction textures Some metamorphic rocks contain evidence for incomplete reactions or other textural proof for part of the P-T route. A simple instance could be the partial substitute of andalusite by sillimanite (Fig. 6a) via the polymorphic transformation of andalusite to sillimanite. Textural evidence may also be beneficial in conditions wherever the reactants have been entirely eaten if The form of one or more reactants are preserved; one example is, pseudomorphs (Figs. 6b-d). An illustration of a more complex reaction texture includes the formation of coronas , which consist of one or more shells (rims, moats) of the mineral or minerals around a central (reactant) section (Fig. 6e). In lots of scenarios, coronas also contain the wonderful-scale intergrowth of minerals inside a texture often called symplectite (Figs. 6e-f).

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For a few rocks, the only real Section of the P-T path recorded in the mineral assemblage and texture of your rock may be the 'peak' of metamorphism -- the problems from the thermal highest (i.e., the utmost temperature plus the strain at the utmost temperature). When the rock experienced a sedimentary or volcanic protolith, you may infer the rock begun in the floor, arrived at peak ailments at some temperature and depth while in the Earth, and returned for the floor (the place the rock was collected).

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