Consequently, Even though subduction zone rocks can observe several paths during subduction and exhumation, pinpointing the precise path that a selected exhumed subduction zone rock followed is essential for comprehending subduction dynamics.
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The trajectory and form with the P-T path, the charges of metamorphic processes, plus the duration of metamorphism absolutely are a operate of the source of warmth and also the mechanisms of burial and unroofing (if tension alter is included).
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of other minerals. For instance, garnets commonly comprise inclusions of minerals that were current inside the rock matrix as the garnet grew, but which were not totally eradicated by metamorphic reactions during progressive metamorphism.
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