The basins and orogens of the Mediterranean region ultimately result from the opening of
oceans during the early break-up of Pangea since the Triassic, and their subsequent …

Deep crustal and mantle rocks are exhumed in core complex mode of extension in three
types of structures: metamorphic core complexes, oceanic core complexes and magma poor …

Slab retreat, slab tearing and interactions of slabs are first-order drivers of the deformation of
the overriding lithosphere. An independent description of the tectonic evolution of the back …

Many countries have made pledges to reduce CO 2 emissions over the upcoming decades
to meet the Paris Agreement targets of limiting warming to no> 1.5° C, aiming for net zero by …

Abstract The Western Alboran Basin (WAB) formation has always been the subject of debate
and considered either as a back-arc or a forearc basin. Stratigraphic analyses of high …

Water plays an important role in geological processes. Providing constraints on what may
influence the distribution of aqueous fluids is thus crucial to understanding how water …

Mesozoic lithological successions of the Alborán domain record two rifting events. An initial
Triassic rifting stage is characterized by thick stratigraphic successions showing typical …

Abstract The long-term Pressure-Temperature-time-deformation (PTtd) evolution of the
internal zones of orogens results from complex interactions between the subducting …

Many relics of passive margin are found in mountain belts sometimes together with pristine
exhume mantle. The reasons why these structures are preserved from tectonic reworking …

We study the structure of the Llevant ranges in Mallorca with special emphasis on the
Cenozoic extensional evolution of the island, which we integrate in a new geodynamic …