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Utilizing zoning info to reconstruct the part of the P-T route knowledgeable by the zoned mineral just isn't uncomplicated, but a few common facets of the relationship of zoning to P-T path may easily be inferred: (a) Garnets with Mn-rich cores and Mn-poorer rims record expansion zoning that represents the transform with the reduced-T conditions at which the garnet core grew to the higher-T disorders at which the garnet rim grew (i.e., prograde metamorphism involving expanding temperature and pressure). Mn is preferentially partitioned into garnet relative to most other widespread minerals, so Mn is sequestered in early-shaped garnet, depleting the area atmosphere with the expanding garnet in Mn. (b) Minerals that exhibit significant aspect development zoning in all probability did not practical experience extremely high metamorphic temperatures. At substantial temperature (> seven-hundred C) and adequate duration, zoning can be homogenized as intracrystalline diffusion gets to be simpler at eliminating compositional variation.
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