The 5-Second Trick For 台北硬碟救援

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### ### 本輸入法表格(輕鬆輸入法大型詞庫版) 乃根據《輕鬆資訊「輕鬆輸入法大詞庫」公眾授權書》的規定，

### 可以修改、複製及散佈本輸入法表格，唯本輸入法表格卻不包含任何擔保。

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paths The idealized check out of P-T paths is always that mineral assemblages equilibrate at just about every phase of The trail from the onset of metamorphism to the peak of metamorphism, Discover More Here at which the final assemblage is locked in. This check out ignores kinetic elements connected to the energetics of nucleation and expansion of minerals, Despite the fact that these aspects might be important for many metamorphic phases and reactions. By way of example, the presence of coexisting andalusite and sillimanite (Fig. 6a) inside of a rock that equilibrated at P-T ailments akin to the stability industry of sillimanite illustrates the sluggish kinetics in the andalusite-to-sillimanite transformation allowed andalusite to persist metastably exterior its balance subject. It is necessary to recognize the impact of deformation on metamorphic reactions, plus the extent to which deformation (strain energy) may perhaps aid reactions.

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