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 …

The Rifian Corridor was one of the Mediterranean–Atlantic seaways that progressively
restricted and caused the Messinian Salinity Crisis (MSC). Many key questions concerning the …

Observations in sedimentary basins affected by deformation show that the fault-induced
depositional accommodation, at various spatial and temporal scales, is closely linked to basin …

Miocene evolution of the Carpathian-Pannonian region was influenced by four important
geotectonic events. The Oligocene-Early Miocene collision of the Alpine Carpathian chain with …

Fluvial morphology is affected by a wide range of forcing factors, which can be external,
such as faulting and changes in climate, or internal, such as variations in rock hardness or …

Turbiditic flysch units of the Rajang Group form a large crescentic belt of deformed strata in
central Borneo. Unfortunately, our understanding of its bed type characteristics and …

Along-fault lithological heterogeneity is observed in all fault zones that cross-cut compositional
layering. Numerical modelling studies on fault rupture nucleation, propagation and arrest …

After a rapid multiphase evolution and a transition from passive to active rifting during late
Early Miocene to Pliocene times, the Pannonian Basin has been subjected to compressional …

We provide lithological, sedimentological and micropalaeontological descriptions of 39
sections and boreholes crossing the upper Miocene deposits of the Rifian Corridor. These …

Formation and evolution of back-arc basins is related to the evolution of subduction zones,
resulting geometries being dependent on the interplay between the velocity of retreating …