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Working with zoning info to reconstruct the part of the P-T route skilled because of the zoned mineral isn't straightforward, but a number of normal aspects of the relationship of zoning to P-T route may possibly conveniently be inferred: (a) Garnets with Mn-abundant cores and Mn-poorer rims history expansion zoning that represents the change in the reduced-T conditions at which the garnet Main grew to the higher-T situations at which the garnet rim grew (i.e., prograde metamorphism involving increasing temperature and force). Mn is preferentially partitioned into garnet relative to most other frequent minerals, so Mn is sequestered in early-fashioned garnet, depleting the neighborhood ecosystem in the escalating garnet in Mn. (b) Minerals that present important factor advancement zoning almost certainly didn't expertise pretty large metamorphic temperatures. At superior temperature (> 700 C) and enough duration, zoning could possibly be homogenized as intracrystalline diffusion becomes simpler at doing away with compositional variation.
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