The Ultimate Guide To 台中硬碟救援

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paths The idealized perspective of P-T paths is mineral assemblages equilibrate at each individual stage of The trail in the onset of metamorphism to the height of metamorphism, at which the ultimate assemblage is locked in. This perspective ignores kinetic elements website relevant to the energetics of nucleation and development of minerals, While these factors could possibly be vital for many metamorphic phases and reactions. For instance, the existence of coexisting andalusite and sillimanite (Fig. 6a) in a rock that equilibrated at P-T situations similar to the stability area of sillimanite illustrates the sluggish kinetics of the andalusite-to-sillimanite transformation allowed andalusite to persist metastably exterior its stability discipline. It can be crucial to acknowledge the influence of deformation on metamorphic reactions, as well as the extent to which deformation (pressure energy) could guide reactions.

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