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Using zoning information and facts to reconstruct the A part of the P-T route knowledgeable via the zoned mineral isn't uncomplicated, but a handful of common aspects of the connection of zoning to P-T path may possibly easily be inferred: (a) Garnets with Mn-abundant cores and Mn-poorer rims report advancement zoning that represents the alter from your reduced-T ailments at which the garnet Main grew to the higher-T circumstances at which the garnet rim grew (i.e., prograde metamorphism involving expanding temperature and pressure). Mn is preferentially partitioned into garnet relative to most other typical minerals, so Mn is sequestered in early-shaped garnet, depleting the area ecosystem on the growing garnet in Mn. (b) Minerals that present major aspect development zoning probably did not working experience really significant metamorphic temperatures. At higher temperature (> seven-hundred C) and ample duration, zoning could be homogenized as intracrystalline diffusion results in being more practical at removing compositional variation.

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