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Making use of zoning details to reconstruct the Portion of the P-T route knowledgeable by the zoned mineral is just not straightforward, but a handful of standard components of the connection of zoning to P-T path may simply be inferred: (a) Garnets with Mn-prosperous cores and Mn-poorer rims file expansion zoning that signifies the transform from the reduced-T ailments at which the garnet Main grew to the higher-T ailments at which the garnet rim grew (i.e., prograde metamorphism involving expanding temperature and stress). Mn is preferentially partitioned into garnet relative to most other widespread minerals, so Mn is sequestered in early-fashioned garnet, depleting the neighborhood environment of the escalating garnet in Mn. (b) Minerals that present big ingredient development zoning in all probability did not working experience pretty higher metamorphic temperatures. At large temperature (> seven-hundred C) and enough length, zoning could be homogenized as intracrystalline diffusion turns into more practical at eradicating compositional variation.
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