Abstract Campi Flegrei caldera (Southern Italy) is a densely inhabited area and suffered
several unrest episodes in the last centuries. The dynamic of the caldera is highly debated …

Subduction-transform edge propagators are lithospheric tears bounding slabs and back-arc
basins. The volcanism at these edges is enigmatic because it is lacking comprehensive …

The evolution and state of geological structure at Earth's surface is best understood with an
accurate characterization of the subsurface. Here we present seismic tomographic images of …

In southern Mexico, tears of the Cocos plate, slab windows, and signatures of the transform
margins have been invoked to justify the peculiar geometry of the subducting plate and the …

Based on multidisciplinary data, including seismological and geodetic observations, as well
as seismic reflection profiles and gravity maps, we analysed the pattern of crustal …

The evolution of the Sicily Channel Rift Zone (SCRZ) is thought to accommodate the
regional tectonic stresses of the Calabrian subduction system. Much of the observations we …

The Ionian subduction in the central Mediterranean, just 200 km wide, is one of the
narrowest in the world. Its evolution has involved a progressive disruption of the subducting …

Dense GPS observations can help Earth scientists to capture the surface imprint of mantle
toroidal flow at slab edges. We document this process in the Calabrian subduction system …

The results of an integrated stratigraphic, structural, geophysical, and geochemical study
reveal the presence of a crustal discontinuity in western Sicily that, at present, runs roughly …

Sicily Channel is a portion of Mediterranean Sea, between Sicily (Southern Italy) and
Tunisia, representing a part of the foreland Apennine-Maghrebian thrust belt. The seismicity …