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The expanding garnets surrounded these relict minerals as the garnets grew, and the relict minerals are preserved as mineralogical evidence of an earlier stage in the metamorphic record of your rock.
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In Figure three, kyanite inclusions take place in garnet in a rock which includes only sillimanite inside the matrix, indicating which the rock was Earlier during the kyanite security subject but that P-T situations improved. If the matrix in the rock (such as the garnet rim) equilibrated, the rock was in the silliminate security field (Fig. four).
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Therefore, the shape of The trail, combined with time information, provides details about the driving forces
paths The idealized watch of P-T paths is usually that mineral assemblages equilibrate at each individual phase of The trail from the onset of metamorphism to the height of metamorphism, at which the ultimate assemblage is locked in. This watch ignores kinetic aspects connected with the energetics of nucleation and expansion of minerals, although these components may very well be important for some metamorphic phases and reactions. As an example, the existence of coexisting andalusite and sillimanite (Fig. 6a) in a rock that equilibrated at P-T problems corresponding to The steadiness industry of sillimanite illustrates the sluggish kinetics of the andalusite-to-sillimanite transformation authorized andalusite to persist metastably outdoors its stability area. It is crucial to acknowledge the affect of deformation on metamorphic reactions, Click Here as well as extent to which deformation (strain Vitality) may possibly support reactions.
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