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In Figure three, kyanite inclusions occur in garnet in the rock which includes only sillimanite inside the matrix, indicating the rock was Earlier from the kyanite stability area but that P-T situations changed. In the event the matrix of the rock (such as the garnet rim) equilibrated, the rock was inside the silliminate balance field (Fig. 4).
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P-T route condition by alone does not give a distinctive interpretation of tectonic procedure or metamorphic driving forces. Such as, clockwise paths can variety in continental collision belts of subduction zones. In the same way, some subduction zone rocks file clockwise paths plus some report counterclockwise paths. Nevertheless, the integration of P-T path features, time/price facts, structural data, and other petrologic facts can offer significant details about metamorphic and tectonic processes.
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