5 Essential Elements For 台北硬碟救援

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paths The idealized check out of P-T paths is the fact that mineral assemblages equilibrate at every phase of The trail from your onset of metamorphism to the peak of metamorphism, at which the ultimate assemblage is locked in. This see ignores kinetic factors connected to the energetics of nucleation and expansion of minerals, Despite the fact that these aspects might be crucial for some metamorphic phases and reactions. For example, the existence of coexisting andalusite and sillimanite (Fig. 6a) in a very rock that equilibrated at P-T problems equivalent to the stability area of sillimanite illustrates that the sluggish kinetics of your andalusite-to-sillimanite transformation authorized andalusite to persist metastably outdoors its Discover More stability industry. It is crucial to acknowledge the impact of deformation on metamorphic reactions, as well as the extent to which deformation (strain Electrical power) may possibly help reactions.

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