台北硬碟救援 Can Be Fun For Anyone

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For a few rocks, the only Component of the P-T route recorded during the mineral assemblage and texture with the rock would be the 'peak' of metamorphism -- the conditions of your thermal optimum (i.e., the utmost temperature and also the pressure at the utmost temperature). If your rock experienced a sedimentary or volcanic protolith, it is possible to infer which the rock commenced for the floor, attained peak problems at some temperature and depth while in the Earth, and returned to your floor (in which the rock was collected).

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您說的情況，資料可以回復。我們的收費價格在我們網站有明確報價，可以開發票，沒有問題�?資料救援中心

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compared to the problems of the height of metamorphism represent 台中硬碟救援 disequilibrium. Generally, even so, the proof for disequilibrium can be very helpful since it may be used to reconstruct P-T route segments.