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 …

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

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

An overview of quantitative approaches to analysis and modelling of sediment generation
and provenance is presented, with an emphasis on major framework components as …

The basic parameters that control stratal architecture in depositional sequences are
sediment flux, rate of change of sediment accommodation (ie, eustasy and sea-floor …

Deciphering the role slope topography plays in partitioning sediment on siliciclastic
continental slope and base‐of‐slope systems helps our understanding of slope depositional …

Experimental work suggests that the rate of upstream-to-downstream loss of sediment from
an active depositional system to permanent storage exerts a fundamental control on …

The study of source‐to‐sink systems relates long‐term variations in sediment flux to
morphogenic evolution of erosional–depositional systems. These variations are caused by …

A new approach is recommended for estimating the catchment size and paleohydrology of
ancient rivers from analysis of their sedimentary record. Estimates of drainage area have …

Integrated, multi-method provenance studies of siliciclastic sedimentary deposits are
increasingly used to reconstruct the history of source-to-sink transport, paleogeography, and …