Initial SE-dipping slow subduction of the Ligurian–Tethys lithosphere beneath Africa from
Late Cretaceous to middle Oligocene twisting to a later faster E-dipping subduction of the …

The lower boundary of the lithospheric plates has remained as an enigmatic boundary for
seismologists, since it is relatively poorly observed by seismic means. There is traditionally a …

We map the lithospheric structure under the westernmost Mediterranean convergent setting
interpreting P-receiver functions obtained from a dense seismic network. No orogenic root …

Modes of mantle delamination in collision zones are discussed in the light of 2D numerical
modeling. Freely evolving thermomechanical models take into account phase changes in …

We use a thin-shell approximation for the lithosphere to model the neotectonics of the Gulf of
Cadiz, SW Iberia margin and the westernmost Mediterranean, in the eastern segment of the …

The westernmost Mediterranean has developed into its present day tectonic configuration as
a result of complex interactions between late stage subduction of the Neo-Tethys Ocean …

Inconsistencies between observations from long and short period seismic waves and
geochemical data mean craton formation and evolution remains enigmatic. Specifically …

We study the crustal and lithospheric mantle structure under central Betics in the
westernmost Mediterranean region by migrating P-receiver functions along a dense seismic …

We make use of the S‐to‐P receiver function technique beneath Colombia and neighboring
regions to make a first‐order approximation of the depth of the Lithosphere‐Asthenosphere …

Tomographic studies of the mantle of southern California (USA) commonly found evidence
for seismically high speed material, known as the Isabella anomaly, extending from near the …