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Consequently, While subduction zone rocks can adhere to many paths in the course of subduction and exhumation, determining the particular route that a certain exhumed subduction zone rock adopted is vital for understanding subduction dynamics.

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In Figure three, kyanite inclusions arise in garnet within a rock that has only sillimanite in the matrix, indicating which the rock was Earlier inside the kyanite balance field but that P-T disorders transformed. Once the matrix from the rock (such as the garnet rim) equilibrated, the rock was from the silliminate stability discipline (Fig. 4).

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