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Working with zoning info to reconstruct the Element of the P-T path professional via the zoned mineral just isn't simple, but some common components of the relationship of zoning to P-T path could effortlessly be inferred: (a) Garnets with Mn-prosperous cores and Mn-poorer rims file progress zoning that represents the modify with the reduce-T ailments at which the garnet core grew to the upper-T situations at which the garnet rim grew (i.e., prograde metamorphism involving rising temperature and tension). Mn is preferentially partitioned into garnet relative to most other common minerals, so Mn is sequestered in early-formed garnet, depleting the regional atmosphere on the growing garnet in Mn. (b) Minerals that exhibit major aspect advancement zoning probably did not encounter really superior metamorphic temperatures. At substantial temperature (> seven hundred C) and adequate length, zoning can be homogenized å°ä¸ç¡¬ç¢Ÿæ•‘æ´ as intracrystalline diffusion results in being simpler at eradicating compositional variation.
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