台中硬碟救援 Fundamentals Explained

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paths The idealized check out of P-T paths is usually that mineral assemblages equilibrate at each phase of the path in the onset of metamorphism to the height of metamorphism, at which the ultimate assemblage is locked in. This check out ignores kinetic elements related to the energetics of nucleation and advancement of minerals, Despite the fact that these aspects might be vital for a few metamorphic phases and reactions. As an example, the presence of coexisting andalusite and sillimanite (Fig. 6a) inside of a rock that equilibrated at P-T situations comparable to The soundness field of sillimanite illustrates which the sluggish kinetics on the andalusite-to-sillimanite transformation allowed andalusite to persist metastably outside the house its security area. It is important to acknowledge the affect of deformation on metamorphic reactions, and the extent to which deformation (pressure Vitality) might guide reactions.

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