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Utilizing zoning facts to reconstruct the A part of the P-T route professional by the zoned mineral is not really simple, but some typical aspects of the relationship of zoning to P-T route may possibly easily be inferred: (a) Garnets with Mn-abundant cores and Mn-poorer rims document development zoning that signifies the modify within the decreased-T circumstances at which the garnet Main grew to the higher-T circumstances at which the garnet rim grew (i.e., prograde metamorphism involving raising temperature and strain). Mn is preferentially partitioned into garnet relative to most other popular minerals, so Mn is sequestered in early-formed garnet, depleting the local ecosystem in the escalating garnet in Mn. (b) Minerals that show major aspect development zoning probably didn't working experience really high metamorphic temperatures. At higher temperature (> 700 C) and enough duration, zoning could possibly be homogenized as intracrystalline diffusion becomes simpler at eliminating compositional variation.
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