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 …

Deltas are discrete shoreline protuberances formed where a river enters a standing body of
water and supplies sediments more rapidly than they can be redistributed by basinal …

Using modern and ancient examples we show that river-dominated deltas formed in shallow
basins have multiple coeval terminal distributary channels at different scales. Sediment …

Despite the historical assumption that the bulk of marine “shelf” mud is deposited by gradual
fallout from suspension in quiet water, recent studies of modern muddy shelves and their …

Analyses of deltaic facies successions highlight recurring ichnological patterns that reflect a
variety of physicochemical stresses imposed upon infaunal organisms by the interaction of …

Although delta-building processes and the resultant facies and facies associations have
been studied for over a century, there remains a lack of well-documented facies architectural …

Facies analysis of the Upper Cretaceous (Turonian) Ferron Sandstone in the western Henry
Mountains of south-central Utah, USA, indicates sediment accumulation in a series of flood …

Facies architectural analysis of a river-dominated deltaic parasequence in the Turonian
Ferron Sandstone Member, near Factory Butte, Utah, was conducted to determine the …

Source-to-sink interpretations of genetic equivalency between fluvial feeder systems and
basin accumulations infer that the sediment and water mass collected and transferred by …