Cutoffs, which include neck and chute cutoffs, are the results of the fluvial processes that
fundamentally influence evolution of meandering rivers. A neck cutoff happens when the two …

Many of the world's alluvial rivers are characterised by single or multiple channels that are
often sinuous and that migrate to produce a mosaicked floodplain landscape of truncated …

Only about 10% of geologic time is imprinted in sedimentary strata and the rest is hidden in
non-depositional or erosional surfaces called unconformities. Stratigraphic unconfor-mities …

An orthogonal 2D training image is constructed from the geological analysis results of well
logs and sedimentary facies; the 2D probabilities in three directions are obtained through …

The fluvial–tidal transition (FTT) is a complex depositional zone, where fluvial flow is
modified by tides as rivers approach a receiving marine basin. Variations in the relative …

Tight sandstones of the late Permian Willespie Formation constitute an important reservoir
rock in the Whicher Range gas field of the Perth Basin. The sandstones under the effect of …

An extensive subsurface dataset from the Lower Cretaceous McMurray Formation of
northeastern Alberta, Canada, is leveraged to provide new insights into the Aptian drainage …

Regionally extensive parasequences in the upper McMurray Formation, Grouse
Paleovalley, north‐east Alberta, Canada, preserve a shift in depositional processes in a …

High‐frequency incised valley systems and subaerial exposure surfaces are prevalent in
Aptian‐aged units, having been documented in numerous basins around the world. In light …

Low-accommodation foreland basins have been of recent interest because their
stratigraphic architectures provide insight into the interaction of tectonic subsidence and …