Submarine lobe-fringe deposits form heterolithic successions that may include a high
proportion of hybrid beds. The identification of lobe-fringe successions aids interpretation of …

Sedimentary facies in the distal parts of deep‐marine lobes can diverge significantly from
those predicted by classical turbidite models, and sedimentological processes in these …

This study reviews the thickness statistics of non-channelized turbidites from four tertiary
basins of Central-Northern Apennines (Italy), where bed geometry and sedimentary …

This study documents the character and occurrence of hybrid event beds (HEBs) deposited
across a range of deep‐water sub‐environments in the Cretaceous–Palaeocene Gottero …

Flutes and tool marks are commonly observed sedimentary structures on the bases of
sandstones in deep‐water successions. These sole structures are universally used as …

Inherited rift topography controls the sediment routing, timing of sand supply, and
sedimentary linkage of early post‐rift depocentres. Exhumed examples of early post‐rift …

The outer parts of deep-water fans, and the basin plains into which they pass, are often
described as areas where erosion is negligible and turbidite systems have net aggradation …

This paper presents a model of facies distribution within a set of early Cretaceous, deep‐
lacustrine, partially confined turbidite fans (Sea Lion Fan, Sea Lion North Fan and Otter Fan) …

Hybrid event beds are texturally and compositionally‐diverse deposits preserved within
deepwater settings. They are deposited by flows exhibiting 'mixed behaviour', forming …

Channel‐lobe transition zones are dynamic areas located between deepwater channels
and lobes. Presented here is a rare example of an exhumed channel‐lobe transition zone …