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Using zoning details to reconstruct the Portion of the P-T route expert through the zoned mineral isn't easy, but a couple of normal elements of the connection of zoning to P-T route may possibly conveniently be inferred: (a) Garnets with Mn-rich cores and Mn-poorer rims history advancement zoning that signifies the modify from the reduced-T situations at which the garnet Main grew to the higher-T situations at which the garnet rim grew (i.e., prograde metamorphism involving growing temperature and tension). Mn is preferentially partitioned into garnet relative to most other typical minerals, so Mn is sequestered in early-shaped garnet, depleting the nearby ecosystem on the increasing garnet in Mn. (b) Minerals that exhibit significant ingredient growth zoning almost certainly didn't encounter pretty high metamorphic temperatures. At significant temperature (> seven Continued hundred C) and enough period, zoning could be homogenized as intracrystalline diffusion gets to be simpler at eliminating compositional variation.
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