Sketch of the geodynamic evolution of the Italian region. Dashed

Sketch of the geodynamic evolution of the Italian region. Dashed lines

Geodynamic evolution of southwestern North America since the Late Eocene

Complex trans-ridge normal faults controlling large earthquakes

Jurassic mountain building and Mesozoic-Cenozoic geodynamic evolution of the Northern Calcareous Alps as proven in the Berchtesgaden Alps (Germany)

Neogene and Quaternary rollback evolution of the Tyrrhenian Sea, the Apennines, and the Sicilian Maghrebides - Rosenbaum - 2004 - Tectonics - Wiley Online Library

Location of the study area, in the Lucania Apennines, Southern Italy.

Minerals, Free Full-Text

Geological map of the investigated area (dashed line). 1: pre-Tortonian

Tectonic sketch map of the western Alps. The dashed grey rectangle

Sketch map of the Central Mediterranean. Black lines show the path of

New insights on the active degassing system of the Lipari–Vulcano complex (South Italy) inferred from Local Earthquake Tomography

Geodynamic evolution of the central and western Mediterranean: Tectonics vs. igneous petrology constraints - ScienceDirect

Sketch of the geodynamic evolution of the Italian region. Dashed lines

Remote Sensing, Free Full-Text

SE - Present-day geodynamics of the Western Alps: new insights from earthquake mechanisms