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Making use of zoning information to reconstruct the Element of the P-T route expert with the zoned mineral is not very simple, but several general areas of the relationship of zoning to P-T route could easily be inferred: (a) Garnets with Mn-abundant cores and Mn-poorer rims record expansion zoning that represents the change with the reduce-T conditions at which the garnet core grew to the upper-T ailments at which the garnet rim grew (i.e., prograde metamorphism involving raising temperature and stress). Mn is preferentially partitioned into garnet relative to most other common minerals, so Mn is sequestered in early-shaped garnet, depleting the regional surroundings of the increasing garnet in Mn. (b) Minerals that show key component growth zoning likely didn't expertise really higher metamorphic temperatures. At higher temperature (> 700 C) and enough duration, zoning may very well be homogenized as intracrystalline diffusion will become more effective at eradicating compositional variation.

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