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Applying zoning info to reconstruct the Element of the P-T path knowledgeable by the zoned mineral is just not easy, but some typical elements of the relationship of zoning to P-T route may well effortlessly be inferred: (a) Garnets with Mn-abundant cores and Mn-poorer rims report development zoning that represents the improve through the reduce-T problems at which the garnet core grew to the higher-T situations at which the garnet rim grew (i.e., prograde metamorphism involving escalating temperature and force). Mn is preferentially partitioned into garnet relative to most other common minerals, so Mn is sequestered in early-shaped garnet, depleting the area surroundings with the expanding garnet in Mn. (b) Minerals that demonstrate major aspect progress zoning probably didn't experience quite superior metamorphic temperatures. At large temperature (> Click This Link seven-hundred C) and adequate period, zoning might be homogenized as intracrystalline diffusion will become more effective at reducing compositional variation.
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