Quantitative kinematic of a frictional viscous low-angle normal fault on Kea (Western Cyclades, Greece)

Lithospheric extension during the Miocene is well documented in the Aegean. Within the Central and Western Cyclades extension has been documented in detail by the formation of Metamorphic Core Complexes and movement along low-angle normal faults (LANFs). Focusing on a hitherto unrecognised main low-angled fault geometry outcropping on northern Kea, this work presents pervasive evidence of top-to-south kinematics.