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Using zoning information and facts to reconstruct the A part of the P-T path expert through the zoned mineral is not really straightforward, but a handful of basic components of the relationship of zoning to P-T route might effortlessly be inferred: (a) Garnets with Mn-abundant cores and Mn-poorer rims record development zoning that represents the transform in the decrease-T problems at which the garnet core grew to the higher-T conditions 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 common minerals, so Mn is sequestered in early-formed garnet, depleting the area ecosystem with the increasing garnet in Mn. (b) Minerals that present main factor development zoning most likely didn't working experience incredibly substantial metamorphic temperatures. At substantial temperature (> seven-hundred C) and enough duration, zoning may be check here homogenized as intracrystalline diffusion results in being more practical at reducing compositional variation.

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