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Utilizing zoning details to reconstruct the Component of the P-T route experienced through the zoned mineral is just not uncomplicated, but a few common facets of the connection of zoning to P-T route may perhaps easily be inferred: (a) Garnets with Mn-wealthy cores and Mn-poorer rims file expansion zoning that signifies the improve from the reduce-T situations at which the garnet Main grew to the upper-T disorders at which the garnet rim grew (i.e., prograde metamorphism involving increasing temperature and stress). Mn is preferentially partitioned into garnet relative to most other frequent minerals, so Mn is sequestered in early-shaped garnet, depleting the community ecosystem of your growing garnet in Mn. (b) Minerals that display main factor expansion zoning in all probability didn't working experience very higher metamorphic temperatures. At higher temperature (> seven hundred C) and adequate length, zoning could possibly be homogenized more info as intracrystalline diffusion will become more practical at doing away with compositional variation.

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