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A few common methods for inferring P-T route segments are: Mineral inclusions Some minerals comprise inclusions

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Using zoning information to reconstruct the part of the P-T route professional via the zoned mineral is not really very simple, but a few general components of the connection of zoning to P-T route may perhaps conveniently be inferred: (a) Garnets with Mn-loaded cores and Mn-poorer rims history advancement zoning that signifies the transform through the decrease-T problems at which the garnet Main grew to the higher-T circumstances at which the garnet rim grew (i.e., prograde metamorphism involving growing temperature and pressure). Mn is preferentially partitioned into garnet relative to most other popular minerals, so Mn is sequestered in early-fashioned garnet, depleting the community natural environment with the increasing garnet in Mn. (b) Minerals that present main component growth zoning probably didn't practical experience quite large metamorphic temperatures. At large temperature (> 700 C) and sufficient period, zoning may very well be homogenized as intracrystalline diffusion will become simpler at removing compositional variation.

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