The smart Trick of 台北硬碟救援 That Nobody is Discussing

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paths The idealized view of P-T paths is mineral assemblages equilibrate at each individual stage of The trail from your onset of metamorphism to the height of metamorphism, at which the final assemblage is locked in. This look at ignores kinetic factors connected with the energetics of nucleation and advancement of minerals, Though these things could be vital for some metamorphic phases and reactions. By way of example, the existence of coexisting andalusite and sillimanite (Fig. 6a) within a rock that equilibrated Click Here at P-T ailments corresponding to The steadiness field of sillimanite illustrates the sluggish kinetics with the andalusite-to-sillimanite transformation allowed andalusite to persist metastably exterior its steadiness area. It is crucial to recognize the affect of deformation on metamorphic reactions, as well as extent to which deformation (strain Strength) may perhaps help reactions.

in comparison to the ailments of the height of metamorphism depict disequilibrium. Normally, nonetheless, the evidence for disequilibrium can be very useful mainly because it can be employed to reconstruct P-T route segments.

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