5 Essential Elements For 台北硬碟救援

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For many rocks, the only real Portion of the P-T path recorded inside the mineral assemblage and texture of your rock could be the 'peak' of metamorphism -- the ailments from the thermal maximum (i.e., the most temperature plus the force at the most temperature). When the rock experienced a sedimentary or volcanic protolith, you may infer the rock started within the surface area, reached peak circumstances at some temperature and depth during the Earth, and returned on the floor (the place the rock was collected).

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Applying zoning information and facts to reconstruct the part of the P-T route experienced because of the zoned mineral is not easy, but several standard facets of the relationship of zoning to P-T path may perhaps effortlessly be inferred: (a) Garnets with Mn-loaded cores and Mn-poorer rims history expansion zoning that signifies the transform within the lower-T conditions at which the garnet core grew to the upper-T problems at which the garnet rim grew (i.e., prograde metamorphism involving raising temperature and tension). Mn is preferentially partitioned into garnet relative to most other common minerals, so Mn is sequestered in early-fashioned garnet, depleting the local setting in the escalating garnet in Mn. (b) Minerals that present major factor growth zoning possibly did not practical experience extremely higher metamorphic temperatures. At higher temperature (> seven hundred C) and ample period, zoning might be homogenized as intracrystalline diffusion turns into more effective at eradicating compositional variation.

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