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Working with zoning info to reconstruct the Element of the P-T path knowledgeable from the zoned mineral will not be easy, but a number of typical aspects of the relationship of zoning to P-T path may quickly be inferred: (a) Garnets with Mn-wealthy cores and Mn-poorer rims history progress zoning that represents the transform from your lessen-T disorders at which the garnet core grew to the upper-T problems at which the garnet rim grew (i.e., prograde metamorphism involving growing temperature and tension). Mn is preferentially partitioned into garnet relative to most other frequent minerals, so Mn is sequestered in early-fashioned garnet, depleting the neighborhood environment on the expanding garnet in Mn. (b) Minerals that exhibit main ingredient progress zoning probably did not working experience quite high metamorphic temperatures. At substantial temperature (> 700 C) and enough duration, zoning could possibly be homogenized as intracrystalline diffusion becomes simpler at eliminating compositional variation.
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