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Applying zoning info to reconstruct the part of the P-T path knowledgeable with the zoned mineral just isn't uncomplicated, but some normal components of the connection of zoning to P-T route might effortlessly be inferred: (a) Garnets with Mn-rich cores and Mn-poorer rims record advancement zoning that signifies the transform with the reduce-T disorders at which the garnet Main grew to the upper-T ailments at which the garnet rim grew (i.e., prograde metamorphism involving raising temperature and tension). Mn is preferentially partitioned into garnet relative to most other prevalent minerals, so Mn is sequestered in early-formed garnet, depleting the nearby atmosphere from the growing garnet in Mn. (b) Minerals that show important component development zoning possibly did not working experience extremely large metamorphic temperatures. At large temperature (> seven-hundred C) and adequate length, zoning might be homogenized as intracrystalline diffusion gets more practical at getting rid of compositional variation.
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