Analogues, especially outcrop analogues, have played a central role in improving
understanding of subsurface reservoir architectures. Analogues provide important …

Steep-fronted Gilbert-type deltas are common features of tectonically active settings, as well
as of physiographic settings where accommodation is dictated by landforms with steeply …

Existing facies models of tide‐dominated deltas largely omit fine‐grained, mud‐rich
successions. Sedimentary facies and sequence stratigraphic analysis of the exceptionally …

Although several studies have considered the sedimentary facies of the Upper Triassic
Yanchang Formation in terms of their hydrocarbon potential in the petroliferous Ordos Basin …

Shallow-water deltas remain enigmatic in terms of placing the observed facies within a
coherent process-based depositional model. Here we report tank experiments on mouth-bar …

Piggyback basins often display asymmetric sedimentary successions influenced by both
regional and local syn-depositional tectonic structures. There are few examples where a …

The first sandstone unit of the Esdolomada Member of the Roda Formation (hereafter
referred to as 'Esdolomada 1') was formed by a laterally‐migrating, shelf tidal bar. This …

The Sibari Plain (northeastern Calabria) shows a well-developed stair of late Quaternary
marine/coastal terraces resulting from the interaction between sea level fluctuations and …

Aggradation, progradation and retrogradation are the main patterns that define the large-
scale architecture of Gilbert-type deltas. These patterns are governed by the ratio between …

This study focuses on facies analysis and depositional architecture of the Arente shelf-type
delta, located at the southernmost margin of the Pleistocene Crati Basin (northern Calabria …