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Employing zoning facts to reconstruct the Section of the P-T route experienced from the zoned mineral is just not uncomplicated, but a few common elements of the connection of zoning to P-T path may perhaps very easily be inferred: (a) Garnets with Mn-loaded cores and Mn-poorer rims record advancement zoning that represents the modify within the reduced-T ailments at which the garnet Main grew to the upper-T situations at which the garnet rim grew (i.e., prograde metamorphism involving expanding temperature and strain). Mn is preferentially partitioned into garnet relative to most other frequent minerals, so Mn is sequestered in early-formed garnet, depleting the area surroundings of your developing garnet in Mn. (b) Minerals that show key element progress zoning probably didn't experience quite high metamorphic temperatures. At substantial temperature (> 700 C) and enough period, zoning could be homogenized as intracrystalline diffusion results in being more effective at eliminating compositional variation.

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