An Unbiased View of 台北硬碟救援

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of the metamorphic rock is the list of all P-T disorders skilled by a rock throughout its metamorphic record (Figure 1).

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paths The idealized see of P-T paths is mineral assemblages equilibrate at every single phase of The trail from the onset of metamorphism to the peak of metamorphism, at which the final assemblage is locked in. This view ignores kinetic elements linked to the energetics of nucleation and development of minerals, Despite the fact that these components could possibly be important for many metamorphic phases and reactions. As an example, the presence Check This Out of coexisting andalusite and sillimanite (Fig. 6a) within a rock that equilibrated at P-T disorders akin to The steadiness subject of sillimanite illustrates that the sluggish kinetics with the andalusite-to-sillimanite transformation authorized andalusite to persist metastably outside the house its steadiness field. It's important to recognize the affect of deformation on metamorphic reactions, along with the extent to which deformation (pressure Electrical power) may perhaps assist reactions.

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