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The trajectory and condition of your P-T path, the prices of metamorphic processes, along with the length of metamorphism are a purpose with the supply of heat along with the mechanisms of burial and unroofing (if force improve is involved).
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The duration of The trail from start (onset of metamorphism) to complete (exposure with the rock in the Earth's floor) will vary from rock to rock dependant upon the tectonic background
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Utilizing zoning info to reconstruct the A part of the P-T route expert by the zoned mineral is just not uncomplicated, but a few basic facets of the relationship of zoning to P-T path could effortlessly be inferred: (a) Garnets with Mn-wealthy cores and Mn-poorer rims record growth zoning that signifies the improve with the decreased-T problems at which the garnet core grew to the higher-T circumstances at which the garnet rim grew (i.e., prograde metamorphism involving growing temperature and pressure). Mn is preferentially partitioned into garnet relative to most other popular minerals, so Mn is sequestered in early-fashioned garnet, depleting the community setting on the rising garnet in Mn. (b) Minerals that demonstrate key component development zoning most likely didn't working experience incredibly substantial metamorphic temperatures. At large temperature (> seven hundred C) and adequate duration, zoning may very well be homogenized as intracrystalline diffusion results in being simpler at removing compositional variation.
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