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Employing zoning info to reconstruct the Element of the P-T path experienced with the zoned mineral isn't uncomplicated, but a couple of typical facets of the connection of zoning to P-T path may simply be inferred: (a) Garnets with Mn-rich cores and Mn-poorer rims report development zoning that signifies the alter within the reduced-T disorders at which the garnet core grew to the upper-T problems 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 typical minerals, so Mn is sequestered in early-fashioned garnet, depleting the nearby natural environment in the escalating garnet in Mn. (b) Minerals that present important component advancement zoning almost certainly didn't encounter quite high metamorphic temperatures. At high temperature (> seven-hundred C) and enough length, zoning might be homogenized as intracrystalline diffusion gets to be more practical at eliminating compositional variation.
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