台北硬碟救援 Fundamentals Explained

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paths The idealized watch of P-T paths is that mineral assemblages equilibrate at every single phase of the path with the onset of metamorphism to Continue the peak of metamorphism, at which the ultimate assemblage is locked in. This check out ignores kinetic things associated with the energetics of nucleation and growth of minerals, Despite the fact that these factors could be essential for many metamorphic phases and reactions. For example, the presence of coexisting andalusite and sillimanite (Fig. 6a) inside a rock that equilibrated at P-T ailments corresponding to The soundness area of sillimanite illustrates the sluggish kinetics of the andalusite-to-sillimanite transformation permitted andalusite to persist metastably outside its balance subject. It is necessary to acknowledge the influence of deformation on metamorphic reactions, along with the extent to which deformation (pressure Electricity) may guide reactions.

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