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The trajectory and condition on the P-T route, the rates of metamorphic procedures, plus the length of metamorphism really are a perform of the supply of heat and also the mechanisms of burial and unroofing (if tension adjust is concerned).

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Employing zoning facts to reconstruct the part of the P-T path seasoned via the zoned mineral is not straightforward, but some typical aspects of the relationship of zoning to P-T route may well easily be inferred: (a) Garnets with Mn-wealthy cores and Mn-poorer rims file expansion zoning that represents the modify through the decreased-T disorders at which the garnet core grew to the higher-T problems 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 popular minerals, so Mn is sequestered in early-formed garnet, depleting the neighborhood atmosphere with the developing garnet in Mn. (b) Minerals that clearly show main ingredient growth zoning likely did not working experience really superior metamorphic temperatures. At large temperature (> seven-hundred C) and adequate period, zoning might be homogenized as intracrystalline diffusion results in being more effective at eradicating compositional variation.

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