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Utilizing zoning data to reconstruct the Section of the P-T path professional with the zoned mineral just isn't simple, but some standard elements of the connection of zoning to P-T route could very easily be inferred: (a) Garnets with Mn-wealthy cores and Mn-poorer rims report growth zoning that signifies the alter with the lessen-T situations at which the garnet Main grew to the upper-T circumstances at which the garnet rim grew (i.e., prograde metamorphism involving escalating temperature and stress). Mn is preferentially partitioned into garnet relative to most other popular minerals, so Mn is sequestered in early-formed garnet, depleting the nearby natural environment of the expanding garnet in Mn. (b) Minerals that demonstrate main element growth zoning almost certainly didn't practical experience really large metamorphic temperatures. At substantial temperature (> seven hundred C) and enough period, zoning can be homogenized as intracrystalline diffusion gets more effective at eradicating compositional variation.

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