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 …

A census of 83 Infralittoral Prograding Wedges (IPWs) was carried out in the Central-Eastern
Tyrrhenian Sea, to learn more about their morpho-bathymetric variability and test their …

Understanding how subaqueous sediment gravity flows (SSGF) evolve in time and space,
and how their deposits vary spatially, is a key research focus for gravity flow sedimentology …

Lacustrine shallow-water deltas exhibit highly variable morphologies, owing to their high
sensitivity to changes in the upstream and downstream boundary conditions, where a small …

We know less about subglacial meltwater flow properties in distributed inefficient and semi-
efficient systems in comparison to those of ice marginal eskers and proglacial environments …

Detailed facies and sequence stratigraphic analysis of an Aptian shallow-marine succession
illustrates the evolution of sedimentary environments and their benthic faunal associations in …

Submarine channel mouth settings are hardly preserved in the stratigraphic record.
Although they are still poorly known with respect to other segments of turbidite systems …

Fan deltas of the Lower Cretaceous area in Saihantala sag, Erlian Basin have been
identified as major petroleum exploration opportunities. The sedimentary evolution is …

Distinguishing between shallow‐water delta and fluvial fan deposits in the subsurface of
lacustrine basins is challenging due to their similar depositional characteristics and …

Pleistocene kame deltas are known mainly from glaciomarginal environments, whereas
there are fewer examples of deltas where kames formed within decaying ice sheets. In this …