台北硬碟救援 - An Overview

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In Determine 3, kyanite inclusions happen in garnet in a very rock which includes only sillimanite inside the matrix, indicating that the rock was Formerly inside the kyanite security field but that P-T conditions improved. In the event the matrix on the rock (including the garnet rim) equilibrated, the rock was in the silliminate steadiness subject (Fig. 4).

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paths The idealized look at of P-T paths is always that mineral assemblages equilibrate at each and every stage of the path within the onset of metamorphism to the height of metamorphism, at which the final assemblage is locked in. This see ignores kinetic factors connected to the energetics of nucleation and expansion of minerals, Despite the fact that these aspects might be important for many metamorphic phases and reactions. One example is, the presence of coexisting andalusite and sillimanite (Fig. 6a) inside a rock that equilibrated at P-T conditions similar to The soundness discipline of sillimanite illustrates that the sluggish kinetics of your andalusite-to-sillimanite transformation authorized andalusite to persist Clicking Here metastably exterior its balance field. It can be crucial to acknowledge the affect of deformation on metamorphic reactions, and the extent to which deformation (pressure Strength) might assist reactions.

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