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Applying zoning info to reconstruct the Portion of the P-T route experienced from the zoned mineral is just not uncomplicated, but a number of normal aspects of the relationship of zoning to P-T route may well simply be inferred: (a) Garnets with Mn-rich cores and Mn-poorer rims history advancement zoning that signifies the transform from the reduce-T problems at which the garnet core grew to the upper-T disorders at which the garnet rim grew (i.e., prograde metamorphism involving escalating temperature and stress). Mn is preferentially partitioned into garnet relative to most other typical minerals, so Mn is sequestered in early-shaped garnet, depleting the regional natural environment on the expanding garnet in Mn. (b) Minerals that clearly show major element growth zoning most likely did not expertise very higher metamorphic temperatures. At large temperature (> seven hundred C) and ample duration, zoning might be homogenized as intracrystalline diffusion turns into more practical at doing away with compositional variation.

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