They record a history of sinistral motion under medium to high metamorphic conditions followed by a diachronous reversal in shear sense and a change to brittle deformation during the Oligocene on the TPF and MPF, and the Miocene on the ASRR
They recorda history of sinistral motion under medium to high metamorphicconditions followed by a diachronous reversal in shear sense anda change to brittle deformation during the Oligocene on the TPF andMPF, and the Miocene on the ASRR