As a result, While subduction zone rocks can abide by several paths all through subduction and exhumation, deciding the particular path that a certain exhumed subduction zone rock followed is significant for comprehending subduction dynamics.
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In Determine 3, kyanite inclusions manifest in garnet within a rock here which includes only sillimanite from the matrix, indicating that the rock was previously while in the kyanite balance discipline but that P-T ailments modified. In the event the matrix from the rock (including the garnet rim) equilibrated, the rock was within the silliminate stability field (Fig. four).
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