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Working with zoning information to reconstruct the part of the P-T route professional via the zoned mineral is not really uncomplicated, but a handful of typical areas of the connection of zoning to P-T route may possibly very easily be inferred: (a) Garnets with Mn-prosperous cores and Mn-poorer rims record progress zoning that signifies the transform from your decrease-T situations at which the garnet Main grew to the upper-T situations at which the garnet rim grew (i.e., prograde metamorphism involving increasing temperature and tension). Mn is preferentially partitioned into garnet relative to most other widespread minerals, so Mn is sequestered in early-formed garnet, depleting the neighborhood environment with the increasing garnet in Mn. (b) Minerals that display main element expansion zoning in all probability did not working experience quite substantial metamorphic temperatures. At superior temperature (> 700 C) and sufficient length, zoning could possibly be homogenized as intracrystalline diffusion becomes more practical at getting rid of compositional variation.
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