Clinoforms are ubiquitous depositional surfaces in sedimentary systems. The quintessential
shape, with a flat or gentle topset, sloping foreset, and gentle to flat bottomset, is …

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

Abstract The Greater Barents Sea Basin (GBSB) in Arctic Russia and Norway is an
intracratonic basin that accommodated an enormous amount of sediment during the …

Triassic strata in the Greater Barents Sea Basin are important records of geodynamic activity
in the surrounding catchments and sediment transport in the Arctic basins. This study is the …

Many modern deltas exhibit a compound geometry that consists of a shoreline clinoform and
a larger subaqueous clinoform connected through a subaqueous platform. Despite the …

Opening of the Arctic Ocean has been the subject of much debate, and the placement of
terranes in the Early Mesozoic remains a crucial part of this important discussion. Several …

The Barents Sea region of Arctic Norway preserves a thick succession of marine and deltaic
Triassic strata that yield an abundant and diverse association of terrestrial and marine …

Abstract The East Barents Megabasin (EBM) is a system of sedimentary basins in the
Russian sector of the Barents Sea. A large amount of new seismic data has been acquired …

Process-physics-based, coupled hydrodynamic–morphodynamic delta models are
constructed to understand preserved facies heterogeneities that can influence subsurface …

The upper Palaeozoic basins of central-western Argentina include continuous fossiliferous
successions spanning the Carboniferous-Permian interval. The palynostratigraphic …