Earth-surface processes operate across erosionally dominated landscapes and deliver
sediment to depositional systems that can be preserved over a range of timescales. The …

Alluvial and fluvial fans are the most widespread depositional landforms bordering the
margins of long-lived highland regions and actively subsiding continental basins, across a …

Climate, tectonics, and life influence the flux and caliber of sediment transported across
Earth's surface. These environmental conditions can leave behind imprints in the Earth's …

Sediment archives in the terrestrial and marine realm are regularly analyzed to infer
changes in climate, tectonic, or anthropogenic boundary conditions of the past. However …

Source-to-sink paleogeography in a time-constrained sequence stratigraphic framework has
been reconstructed for the non-marine to marine transitional Lo**ian strata (Late Permian) …

Production, transport, and deposition of siliciclastic sediments takes place across changing
altitudes, physical processes, environments, and controls en route from source to sink …

The study of drainage network response to uplift is important not only for understanding river
system dynamics and associated channel properties and fluvial landforms, but also for …

The stratigraphies of foreland basins have been related to orogeny, where continent–
continent collision causes the construction of topography and the downwar** of the …

The volumes, rates and grain size distributions of sediment supplied from hillslopes
represent the initial input of sediment delivered from upland areas and propagated through …

Catchments provide water and sediment to downstream sedimentary systems, and these
form individual source-to-sink systems. Source-to-sink systems comprise adjacent linked …