Structure and morphology of an active conjugate relay zone, Messina Strait, southern Italy

Messina Strait is a narrow fault-bounded marine basin that separates the Calabrian peninsula from Sicily in southern Italy. It sits in a seismically active region where normal fault scarps and raised Quaternary marine terraces record ongoing extension driven by southeastward rollback of the Calabrian subduction zone. A review of published studies and new data shows that normal faults in the Messina Strait region define a conjugate relay zone where displacement is transferred along strike from NW-dipping normal faults in the northeast (southern Calabria) to the SE-dipping Messina-Taormina normal fault in the southwest (offshore eastern Sicily). The narrow marine strait is a graben undergoing active subsidence within the relay zone, where pronounced curvature of normal faults results from large strain gradients and clockwise rotations related to fault interactions. Based on regional fault geometries and published age constraints, we infer that normal faults in southern Calabria migrated northwest while normal faults in NE Sicily migrated southeast during the past ca. 2-2.5 Myr. This pattern has resulted in tectonic narrowing of the strait through time by inward migration of facing normal faults and rapid mantle-driven uplift. Normal faults in Messina Strait define an active conjugate relay zone where strain is transferred along strike between facing normal faults in southern Calabria and northeast Sicily. Stratigraphic and geomorphic data record tectonic narrowing of the strait in the past ca. 2.5 Myr by inward migration of facing normal faults and rapid mantle-driven uplift.image

Automated summary

Messina Strait is a narrow fault-bounded marine basin in southern Italy. It is a seismically active region where normal faults transfer displacement from northeast to southwest. The strait has undergone tectonic narrowing and rapid mantle-driven uplift in the past few million years.