Organic matter burial in the deep-sea fan sediments is an important component of the long-
term carbon cycle. Although there is increasing recognition of the importance of organic …

The underpinning problems of deep-water facies still remain unresolved.(1) The Tb, Tc, and
Td divisions of the turbidite facies model, with traction structures, are an integral part of the …

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

Hybrid event beds comprising both clean and mud‐rich sandstone are important
components of many deep‐water systems and reflect the passage of turbulent sediment …

Deposits of sediment gravity flows in the Aberystwyth Grits Group (Silurian, west Wales,
United Kingdom) display evidence that sole marks are suitable for reconstructing …

The fringe of fine‐grained deep‐marine systems often exhibits complex sedimentary facies
and facies associations, because the presence of clay promotes the development of …

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

Hybrid event beds comprising clay‐poor and clay‐rich sandstone are abundant in
Maastrichtian‐aged sandstones of the Springar Formation in the north‐west Vøring Basin …