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Utilizing zoning facts to reconstruct the Portion of the P-T route seasoned by the zoned mineral isn't uncomplicated, but several typical facets of the relationship of zoning to P-T route may well easily be inferred: (a) Garnets with Mn-rich cores and Mn-poorer rims file growth zoning that signifies the change within the reduce-T problems at which the garnet core grew to the upper-T circumstances at which the garnet rim grew (i.e., prograde metamorphism involving expanding temperature and stress). Mn is preferentially partitioned into garnet relative to most other popular minerals, so Mn is sequestered in early-shaped garnet, depleting the area surroundings of your escalating garnet in Mn. (b) Minerals that present big component advancement zoning most likely didn't encounter very substantial metamorphic temperatures. At high temperature (> seven hundred C) and ample length, zoning here can be homogenized as intracrystalline diffusion will become more practical at removing compositional variation.
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