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) …
C Pellegrini, A Asioli, KM Bohacs, TM Drexler… - Marine and Petroleum …, 2018 - Elsevier
Although facies and stratal geometries of continental margin successions can be defined in detail based on subsurface and outcrop studies, most studies lack the high-resolution age …
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 …
Aggradational deltaic successions are uncommon in the stratigraphic record since deltas are progradational by nature. However, deltaic coastlines fed by multiple small distributaries …
Abstract The South China Sea continental margin in the Qiongdongnan Basin (QDNB) area has incrementally prograded since 10.5 Ma generating a margin sediment prism more than …
In recent years it has become clear that many shallow‐marine heterolithic and mudstone‐ dominated successions are deposited as mud belts forming part of subaqueous deltas that …
The influence of bottom currents and tectonic activity on shelf sedimentary processes and sand distribution remains poorly constrained. A growing body of research highlights the …
Process-physics-based, coupled hydrodynamic–morphodynamic delta models are constructed to understand preserved facies heterogeneities that can influence subsurface …