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Working with zoning information to reconstruct the part of the P-T path seasoned via the zoned mineral is just not uncomplicated, but several general components of the relationship of zoning to P-T path could effortlessly be inferred: (a) Garnets with Mn-wealthy cores and Mn-poorer rims history growth zoning that represents the improve with the decreased-T disorders at which the garnet Main grew to the upper-T situations 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-shaped garnet, depleting the nearby natural environment of your increasing garnet in Mn. (b) Minerals that show major element expansion zoning most likely didn't practical experience really superior metamorphic temperatures. At significant temperature (> 700 C) and ample period, zoning might website be homogenized as intracrystalline diffusion gets simpler at doing away with compositional variation.

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