5 Simple Statements About 台中硬碟救援 Explained

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paths The idealized watch of P-T paths is always that mineral assemblages equilibrate at each and every stage of The trail within the onset of metamorphism to the height of metamorphism, at which the final assemblage is locked in. This view ignores kinetic factors connected to the energetics of nucleation and expansion of minerals, Though these elements may be significant for a few metamorphic phases and reactions. For instance, the presence of coexisting andalusite and sillimanite (Fig. 6a) inside of a rock that equilibrated at P-T problems akin to the stability industry of sillimanite illustrates the sluggish kinetics from the andalusite-to-sillimanite transformation authorized andalusite to persist metastably exterior its balance field. It can be crucial to Discover More acknowledge the influence of deformation on metamorphic reactions, and the extent to which deformation (pressure Strength) might guide reactions.

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