Ancient fluvial valley systems are long recognized as important features in the stratigraphic
record, but emerged as a specific focus of attention with publication of first-generation …

Recent development of fluvial facies models has been due to improved description of
natural river and floodplain processes and deposits using:(1) ground-penetrating radar …

A primary objective in exploration for and development of fluvial reservoirs is determining
the thickness and width of sandstone-conglomerate bodies (mainly channel-belt deposits) …

A quantitative, three‐dimensional depositional model of gravelly, braided rivers has been
developed based largely on the deposits of the Sagavanirktok River in northern Alaska …

The 30 to 155 m thick Early Permian (Artinskian) Warchha Sandstone of the Salt Range,
Pakistan is a conglomerate, sandstone and claystone succession within which seven …

Classical models developed for ancient fluvial point bars are based on the assumption that
meander bends invariably increase their radius as meander-bend apices migrate in a …

ABSTRACT Detailed three‐dimensional (3‐D) observations of sandy point‐bar deposits
from the River South Esk in Scotland were made using very closely spaced (metres) …

Abstract The Castlegate Sandstone is part of the Upper Cretaceous (Campanian-
Maastrichtian) Mesaverde Group, a clastic wedge that prograded eastward from the Sevier …

Fluvial deposits of the Cretaceous Chubut Group, San Jorge Basin, Argentina, were studied
in outcrop to provide analogs for adjacent subsurface hydrocarbon-bearing strata. Outcrops …

The geometry of heterogeneities within fluvial channel-belt deposits is predicted using an
existing model of flow and sediment transport in river channel-meander bends. The thickest …