台北硬碟救援 - An Overview

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paths The idealized look at of P-T paths is mineral assemblages equilibrate at every stage of The trail from the onset of metamorphism to the peak of metamorphism, at which the ultimate assemblage is locked in. This watch ignores kinetic aspects relevant to the energetics of nucleation and expansion of minerals, While these elements could be crucial for some metamorphic phases and reactions. One example is, the existence of coexisting andalusite and sillimanite (Fig. 6a) inside a rock that equilibrated at P-T situations akin to The soundness subject of sillimanite illustrates which the sluggish kinetics Discover More Here on the andalusite-to-sillimanite transformation permitted andalusite to persist metastably outside its steadiness subject. It is important to acknowledge the affect of deformation on metamorphic reactions, and also the extent to which deformation (pressure Strength) might help reactions.

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