Clinoforms are inclined and normally basinward-dipping horizons developed over a range
of spatial and temporal scales in both siliciclastic and carbonatic systems. The study of …

Abstract Development of the rift-type North Croatian Basin located in the south-western
Neogene Pannonian Basin System and belonging to the Central Paratethys realm, was …

The architecture of sedimentary basins reflects the relationship between accommodation
space and sediment supply, their rates and localization being variable during basin …

The basin of giant Lake Pannon in Central Europe was filled by forward accretion of
sediment packages during the Late Miocene and Early Pliocene. Successive positions of the …

The large number and distribution of rollback systems in Mediterranean orogens infer the
possibility of interacting extensional back‐arc deformation driven by different slabs. The …

This special issue dealing with the recent advances on modern and ancient clinoform‐
stratified sedimentary successions arises from a European Geoscience Union (EGU) …

Sažetak Upper Miocene to Pliocene (Pannonian) sediments of the Pannonian Basin System
accumulated in the brackish Lake Pannon and the fluvial feeder systems, between 11.6-2.6 …

To track the evolution and formation of one of the major sub-basins of the Pannonian back-
arc basin system, we re-evaluate pre-rift, syn-rift, post-rift, and inversion stages of the …

This study proposes a concept and presents a workflow to examine potential reasons for low
injectivity of sandstone aquifers. Injection related problems are a major challenge for the …

Clinoforms and clinothems are important and common architectural elements in the
sedimentary record of many basins worldwide. The influence that they exert on …