The 5-Second Trick For 台北硬碟救援

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paths The idealized see of P-T paths is that mineral assemblages equilibrate at just about every phase of the path in the onset of metamorphism to the height of metamorphism, at which the ultimate assemblage is locked in. This look at ignores kinetic aspects related to the energetics of nucleation and advancement of minerals, Despite the fact that these components can be essential for many metamorphic phases and reactions. Such as, the presence of coexisting andalusite and sillimanite (Fig. 6a) in the rock that equilibrated at P-T conditions akin to the stability industry of sillimanite illustrates the get more info sluggish kinetics on the andalusite-to-sillimanite transformation permitted andalusite to persist metastably outside its steadiness subject. It is vital to recognize the impact of deformation on metamorphic reactions, along with the extent to which deformation (pressure Power) may support reactions.

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