The smart Trick of 台中硬碟救援 That No One is Discussing

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paths The idealized view of P-T paths is mineral assemblages equilibrate at just about every phase of The trail from your onset of metamorphism to the height of metamorphism, at which the ultimate assemblage is locked in. This check out ignores kinetic variables related to the energetics of nucleation and progress of minerals, Even though these things could possibly be critical for many metamorphic phases and reactions. For instance, the existence of coexisting andalusite and sillimanite (Fig. 6a) inside of a rock that equilibrated at P-T conditions similar to The steadiness discipline of sillimanite illustrates that the sluggish kinetics in the andalusite-to-sillimanite transformation authorized andalusite to persist metastably outside the house its stability field. It is crucial to acknowledge the influence of deformation on metamorphic reactions, along with the extent to which Discover More deformation (strain Power) might guide reactions.

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