Geophysical investigation of Pleistocene volcanism and tectonics offshore Capo Vaticano (Calabria, southeastern Tyrrhenian Sea)

- Geophysical data image a Pleistocene volcanic ridge offshore Capo Vaticano.
- Inverse 3D magnetic modeling reveals the volcano plumbing system at depth.
- The volcanic ridge formed at the intersection of a NW- and NE-trending normal fault.
- High-angle, NE-trending, SE-dipping normal fault formed during Pleistocene.
- The structural pattern controlled the pathways of ascending magma through time.