Considerations To Know About 台中硬碟救援

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paths The idealized view of P-T paths is that mineral assemblages equilibrate at each phase of The trail with the onset of metamorphism to the peak of metamorphism, at which the final assemblage is locked in. This view ignores kinetic things relevant to the energetics of nucleation and growth of minerals, Whilst these components might be important for some metamorphic phases and reactions. For instance, the existence of coexisting andalusite and sillimanite (Fig. 6a) in a Discover More rock that equilibrated at P-T ailments corresponding to The soundness industry of sillimanite illustrates that the sluggish kinetics with the andalusite-to-sillimanite transformation allowed andalusite to persist metastably exterior its steadiness area. It can be crucial to recognize the impact of deformation on metamorphic reactions, and the extent to which deformation (strain Electrical power) may well help reactions.

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