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Working with zoning data to reconstruct the A part of the P-T route expert through the zoned mineral just isn't straightforward, but a handful of standard elements of the connection of zoning to P-T route may easily be inferred: (a) Garnets with Mn-rich cores and Mn-poorer rims history development zoning that signifies the transform within the lessen-T disorders at which the garnet core grew to the higher-T ailments at which the garnet rim grew (i.e., prograde metamorphism involving raising temperature and stress). Mn is preferentially partitioned into garnet relative to most other prevalent minerals, so Mn is sequestered in early-fashioned garnet, depleting the regional atmosphere in the rising garnet in Mn. (b) Minerals that present important component expansion zoning almost certainly did not encounter pretty superior metamorphic temperatures. At substantial temperature (> 700 C) and ample length, zoning can be click here homogenized as intracrystalline diffusion will become simpler at eliminating compositional variation.
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