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For many rocks, the one part of the P-T route recorded from the mineral assemblage and texture of the rock would be the 'peak' of metamorphism -- the conditions from the thermal highest (i.e., the utmost temperature plus the tension at the maximum temperature). In case the rock experienced a sedimentary or volcanic protolith, it is possible to infer that the rock started on the floor, arrived at peak disorders at some temperature and depth inside the Earth, and returned to the area (the place the rock was gathered).

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Using zoning information to reconstruct the Section of the P-T path skilled because of the zoned mineral isn't easy, but a number of basic aspects of the connection of zoning to P-T route may well quickly be inferred: (a) Garnets with Mn-prosperous cores and Mn-poorer rims history development zoning that signifies the change through the decreased-T disorders at which the garnet core grew to the higher-T situations at which the garnet rim grew (i.e., prograde metamorphism involving rising temperature and force). Mn is preferentially partitioned into garnet relative to most other common minerals, so Mn is sequestered in early-fashioned garnet, depleting the community setting of your growing garnet in Mn. (b) Minerals that display main factor expansion zoning probably did not practical experience quite significant metamorphic temperatures. At significant temperature (> seven-hundred C) and enough length, zoning read more may very well be homogenized as intracrystalline diffusion results in being more practical at doing away with compositional variation.

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