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Using zoning facts to reconstruct the Portion of the P-T path seasoned by the zoned mineral will not be straightforward, but a few standard aspects of the connection of zoning to P-T path may well effortlessly be inferred: (a) Garnets with Mn-loaded cores and Mn-poorer rims file growth zoning that signifies the change through the reduce-T situations at which the garnet Main grew to the upper-T conditions at which the garnet rim grew (i.e., prograde metamorphism involving growing temperature and strain). Mn is preferentially partitioned into garnet relative to most other prevalent minerals, so Mn is sequestered in early-fashioned garnet, depleting the area atmosphere in the increasing garnet in Mn. (b) Minerals that exhibit important element development zoning almost certainly didn't working experience incredibly superior metamorphic temperatures. At high temperature (> 700 C) and enough length, zoning may be homogenized as intracrystalline diffusion results in being simpler at eradicating compositional variation.

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