台中硬碟救援 - An Overview

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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，

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paths The idealized perspective of P-T paths is the fact mineral assemblages equilibrate at each individual stage of The trail within the onset of metamorphism to the peak of metamorphism, at which the final assemblage is locked in. This see ignores kinetic factors connected to the energetics of nucleation and advancement of minerals, Even though these factors may very well be vital for many metamorphic phases and reactions. For example, the presence of coexisting andalusite and sillimanite (Fig. 6a) inside of a rock that equilibrated at P-T situations similar to the stability industry of sillimanite illustrates that the sluggish kinetics with the andalusite-to-sillimanite transformation permitted andalusite to persist metastably outside the house its stability discipline. It is Continue necessary to recognize the affect of deformation on metamorphic reactions, along with the extent to which deformation (pressure Electrical power) may guide reactions.

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