Formation of alluvial stratigraphy is controlled by autogenic processes that mix their imprints
with allogenic forcing. In some alluvial successions, sedimentary cycles have been linked to …

We present a parameterisation of fluvio-deltaic drainage network evolution and alluvial
architecture in a basin-scale 2-DH model. The model setup is capable of producing …

In an extended series of papers by M. Leeder, JRL Allen, JS Bridge, J. Alexander, and
others, the depositional stacking patterns of channel-belt deposits were related to tectonic …

Allogenic and autogenic mechanisms both cause changes in the bed elevation of rivers and
thereby influence the characteristics of alluvial stratigraphic records (ASRs). Allogenic …

Alluvial rivers aggrade, incise, and adjust their sediment‐transport rates in response to
changing sediment and water supply. Fluvial landforms, such as river terraces, and …

Modeling is an invaluable tool for studying sedimentary basin filling and for understanding
depositional processes with long recurrence intervals, including channel avulsion …

Various, but related, models have been proposed to explain the architectural arrangement of
channel stacking patterns in avulsion-dominated alluvial sequences. The early models …

Alluvial fan evolution and morphology are often considered to respond primarily to external
forcing (eg, tectonics, climate, and base-level change). Here we present a numerical model …

The quantitative model presented simulates the development of a two‐dimensional alluvial
sedimentary succession beneath a floodplain traversed by a single major river. Several inter …

At the geological time scale, the way in which the erosion of drainage catchments responds
to tectonic uplift and climate changes depends on boundary conditions. In particular …