Classical models developed for ancient fluvial point bars are based on the assumption that
meander bends invariably increase their radius as meander-bend apices migrate in a …

The three-dimensional reconstruction of meander-belt deposits from ancient strata provides
insight into the formative processes of meander-bend evolution and paleogeographic …

Although fundamental types of fluvial meander-bend transformations–expansion,
translation, rotation, and combinations thereof–are widely recognised, the relationship …

Abstract The lower Eocene Willwood Formation of the Bighorn Basin, Wyoming, USA, is an
alluvial succession with a sand content varying around 25%. It has been studied intensively …

The widespread distribution of tidal creeks and channels that undertake meandering
behaviour in modern coasts contrasts with their limited documentation in the fossil record …

Abstract Effects of discharge variability on point-bar sedimentation are not well documented,
although resulting changes in flow patterns are well known. This paper focuses on a …

This paper helps to address the growing need to resolve the severe loss of deltaic lands by
providing a new understanding for shallow‐water digitate delta growth. The integration of …

Vegetation-free fluvial meanders are exceptional on modern Earth, and their abundance in
pre-Silurian rock records is debated. Whether or not landscapes devoid of plant life could …

The depositional facies, sequence stratigraphy, palaeogeography, and coal accumulation in
the fluvio-lacustrine Middle Jurassic Xishanyao Formation in the central Zhunnan (central …

Point bars formed by meandering river systems are an important class of sedimentary
deposit and are of significant economic interest as hydrocarbon reservoirs. Standard point …