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Making use of zoning information to reconstruct the Component of the P-T path expert with the zoned mineral is not simple, but a few typical aspects of the relationship of zoning to P-T path may possibly simply be inferred: (a) Garnets with Mn-abundant cores and Mn-poorer rims history growth zoning that represents the modify with the reduce-T disorders at which the garnet core grew to the upper-T situations at which the garnet rim grew (i.e., prograde metamorphism involving increasing temperature and strain). Mn is preferentially partitioned into garnet relative to most other common minerals, so Mn is sequestered in early-shaped garnet, depleting the local setting of the rising garnet in Mn. (b) Minerals that show big element progress zoning probably didn't experience really superior metamorphic temperatures. At large temperature (> seven-hundred C) and adequate period, zoning might be homogenized as intracrystalline diffusion will become more effective at reducing compositional variation.
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