Considerations To Know About 台中硬碟救援



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paths The idealized watch of P-T paths is the fact mineral assemblages equilibrate at every phase of The trail within the onset of metamorphism to the height of metamorphism, at which the ultimate assemblage is locked in. This perspective ignores kinetic components relevant to the energetics of nucleation and expansion of minerals, Whilst these things may very well be significant for many metamorphic phases and reactions. By way of example, the existence of coexisting andalusite and sillimanite (Fig. 6a) in the rock that equilibrated at P-T problems akin to the stability area of sillimanite illustrates that the sluggish kinetics of your andalusite-to-sillimanite here transformation authorized andalusite to persist metastably exterior its security discipline. It is vital to recognize the influence of deformation on metamorphic reactions, as well as extent to which deformation (strain Electricity) may aid reactions.

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