Magma-poor rifted margins consistently show extreme crustal thinning accompanied by
normal faulting, the serpentinization of the mantle beneath crust thinned to less than 8±2 km …

The deep structure of the West African continental margin between 5° S and 8° S was
investigated using vertical reflection and wide-angle reflection/refraction techniques, during …

The tectonic history of the Western Mediterranean region during the Oligocene and Early
Miocene is illustrated through a series of plate reconstructions, from chron C13n to chron …

The Ligurian basin, western Mediterranean Sea, has opened from late Oligocene to early
Miocene times, behind the Apulian subduction zone and partly within the western Alpine …

The TRANSMED Atlas, consisting of a CD-ROM and a book, provides an updated overview
of the geological and geophysical characteristics of the Mediterranean region by integrating …

Taking benefit of the AlpArray temporary network and permanent networks in W‐Europe, we
construct a 3‐D onshore‐offshore velocity model of the crust and upper mantle using …

Deep seismic profiles and subsidence history of the Gulf of Lion margin reveal an intense
stretching of the distal margin and strong postrift subsidence, despite weak extension of the …

We focus on the northern Ligurian margin, at the geological junction of the subalpine
domain and the Ligurian oceanic basin, in order (1) to identify the location of the southern …

In this work we investigate the crustal and tectonic structures of the Central Tyrrhenian back‐
arc basin combining refraction and wide‐angle reflection seismic (WAS), gravity, and …

The origin of the Algerian margin remains one of the key questions still discussed in the
Western Mediterranean sea, due to the imprecise nature and kinematics of the associated …