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P-T path shape by by itself would not provide a special interpretation of tectonic approach or metamorphic driving forces. Such as, clockwise paths can form in continental collision belts of subduction zones. Likewise, some subduction zone rocks file clockwise paths plus some record counterclockwise paths. Nevertheless, Discover More The combination of P-T route features, time/rate details, structural data, together with other petrologic information and facts can provide substantial details about metamorphic and tectonic processes.

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Utilizing zoning information and facts to reconstruct the Section of the P-T path expert with the zoned mineral isn't very simple, but several general areas of the relationship of zoning to P-T route may well easily be inferred: (a) Garnets with Mn-abundant cores and Mn-poorer rims document advancement zoning that represents the change with the reduce-T disorders at which the garnet core grew to the upper-T situations at which the garnet rim grew (i.e., prograde metamorphism involving increasing temperature and strain). Mn is preferentially partitioned into garnet relative to most other common minerals, so Mn is sequestered in early-shaped garnet, depleting the area setting of the increasing garnet in Mn. (b) Minerals that clearly show main ingredient progress zoning likely did not knowledge very substantial metamorphic temperatures. At high temperature (> seven hundred C) and ample duration, zoning can be homogenized as intracrystalline diffusion turns into more practical at removing compositional variation.

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