5 Simple Statements About 台中硬碟救援 Explained

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The trajectory and shape of your P-T path, the fees of metamorphic processes, as well as the duration of metamorphism can be a purpose of your source of warmth along with the mechanisms of burial and unroofing (if pressure alter is included).

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Employing zoning information and facts to reconstruct the Portion of the P-T route knowledgeable via the zoned mineral isn't straightforward, but a couple of standard components of the relationship of zoning to P-T route may perhaps conveniently be inferred: (a) Garnets with Mn-abundant cores and Mn-poorer rims history progress zoning that represents the modify through the reduced-T situations at which the garnet Main grew to the higher-T ailments at which the garnet rim grew (i.e., prograde metamorphism involving expanding 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 setting of your expanding garnet in Mn. (b) Minerals that demonstrate important ingredient development zoning almost certainly did not working experience very significant metamorphic temperatures. At superior temperature (> seven-hundred C) and enough duration, zoning may be homogenized as intracrystalline diffusion results in being more effective at doing away with compositional variation.

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