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Using zoning facts to reconstruct the A part of the P-T route knowledgeable by the zoned mineral is just not simple, but a handful of basic components of the relationship of zoning to P-T path may possibly easily be inferred: (a) Garnets with Mn-abundant cores and Mn-poorer rims document advancement zoning that represents the improve from your lower-T problems at which the garnet core grew to the upper-T situations at which the garnet rim grew (i.e., prograde metamorphism involving expanding temperature and strain). Mn is preferentially partitioned into garnet relative to most other popular minerals, so Mn is sequestered in early-shaped garnet, depleting the area surroundings from the rising garnet in Mn. (b) Minerals that display big element expansion zoning probably didn't knowledge very substantial metamorphic temperatures. At superior temperature (> seven hundred C) and enough duration, zoning could possibly be homogenized as intracrystalline diffusion becomes simpler at doing away with compositional variation.

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