Clinoforms are inclined and normally basinward-dipping horizons developed over a range
of spatial and temporal scales in both siliciclastic and carbonatic systems. The study of …

Clinoforms are ubiquitous deltaic, shallow-marine and continental-margin depositional
morphologies, occurring over a range of spatial scales (1–10 4 m in height). Up to four types …

Sea level has been estimated for the last 108 million years through backstripping of
corehole data from the New Jersey and Delaware Coastal Plains. Inherent errors due to this …

Shoreline and shelf‐edge trajectories describe the migration through time of sedimentary
systems, using geomorphological breaks‐in‐slope that are associated with key changes in …

Quantitative modelling of the filling of sedimentary basins was begun in earnest in the
1960s. Dozens of themes and variations have been proposed since then, and have yielded …

▪ Abstract Accumulation rates of terrestrial sediment have increased in the past few million
years both on and adjacent to continents, although not everywhere. Apparently, erosion has …

The Yinggehai–Song Hong basin is one of the world's largest pull‐apart basins, lying along
the trace of the Red River fault zone in the South China Sea. South of Hainan Island this …

The Gargano subaqueous delta formed on the eastern and southeastern sides of the
Gargano promontory, in the western Adriatic. This subaqueous deposit represents the …

Emphasis on the association between relative sea-level lowstand and the formation of
sandy deep-water fans has tended to downplay the significance of high sediment supply …

The persistence of topography within ancient orogens remains one of the outstanding
questions in landscape evolution. In the eastern North American Appalachians, this question …