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Table 3 Chronology of the different shear zones, faults and folds in the Simplon region

From: The 3D interplay between folding and faulting in a syn-orogenic extensional system: the Simplon Fault Zone in the Central Alps (Switzerland and Italy)

  1. Note that the peak of Barrovian metamorphism in this region is considered to be ca. 30 Ma (Vance and O’Nions 1992)