River delta degradation has been caused by extraction of natural resources, sediment
retention by reservoirs, and sea-level rise. Despite global concerns about these issues …

Understanding controls on sediment distribution in river deltas is paramount to predicting
facies relationships and stratal architecture. Most classifications of deltas have focused on …

The fluvial to marine transition zone (FMTZ) is the area of coastal rivers in which
sedimentation is controlled by the interaction of fluvial and marine processes. This study …

Crevasse subdeltas develop on modern river-dominated delta plains, and may be affected
by the interaction of river currents and marine processes. However, their sedimentology and …

Despite advances in estuarine facies models, ancient bayhead delta deposits are not widely
recognized or utilized, and their facies characteristics are poorly documented …

The seaward end of modern rivers is characterized by the interactions of marine and fluvial
processes, a tract known as the fluvial to marine transition zone, which varies between …

Prediction of sandstone body dimensions within paralic depositional systems is crucial for
the development of predictive 3D reservoir models. Continental-scale paralic reservoir …

Compound deltas, composed of a subaerial delta plain and subaqueous clinoform, are
common termini of large rivers. The transition between clinoform topset and foreset, or …

The interaction of river and marine processes in the fluvial to marine transition zone
fundamentally impacts delta plain morphology and sedimentary dynamics. This study aims …

The stratigraphic architecture of marginal marine successions records the interplay of
autogenic and allogenic processes, and discerning their relative role in governing the …