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

The source-to-sink (S2S) concept is focused on quantification of the various components of
siliciclastic sedimentary systems from initial source sediment production areas, through the …

Turbidity currents, and other types of submarine sediment density flow, redistribute more
sediment across the surface of the Earth than any other sediment flow process, yet their …

Linear rates of sediment aggradation and fluvial incision are inverse functions of
measurement interval, a generic consequence of unsteadiness in the underlying processes …

Abstract The Barrow Group was deposited in the Northern Carnarvon Basin from the latest
Tithonian to the Late Valanginian. This moderately deep-water shelf-margin is composed …

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

Deciphering depositional age from deposits that accumulate in deep-water slope settings
can enhance understanding of shelf-margin evolutionary timing, as well as controlling …

Abstract The Thar Desert is a major sediment depocenter located in southwestern Asia and
bordering the Indus drainage system to its east. It is unclear where the sediment that built the …

Sediment supply to the ocean influences basin-margin growth and reflects upstream
landscape evolution, including patterns of sediment routing, denudation, and tectono …

Sediment production and its subsequent preservation in the marine stratigraphic record
offshore of large rivers are linked by complex sediment-transfer systems. To interpret the …