Soft-sediment deformation structures associated with slumps and mass transport deposits
(MTDs) are generally considered to form at the surface when unlithified sediment moves …

The offshore area of the Otway Basin (south‐eastern Australia) is dominated by
multibranched canyons where mass‐transport complexes are widely distributed. This study …

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 …

Both submarine landslides and submarine canyons can transfer large amounts of
terrigenous quantities from the continental shelf to the deep sea. In some cases, they can …

Submarine landslides can generate complicated patterns of seafloor relief that influence
subsequent flow behaviour and sediment dispersal patterns. In subsurface studies, the term …

Emplacement of submarine landslides, or mass‐transport deposits, can radically reshape
the physiography of continental margins, and strongly influence subsequent sedimentary …

Core descriptions provide an essential element of ground truth to subsurface reservoir
characterizations, but adequate core characterization and interpretation require a significant …

The classic fill‐and‐spill model is widely applied to interpret topographic controls on
depositional architecture and facies distributions in slope successions with complicated …

Abstract The most important North Sea Jurassic–lowermost Cretaceous lithostratigraphic
units, as developed in the UK, Norway and Danish sectors, are summarized in this chapter …

Sediment remobilization of seafloor strata is linked to the early stages of sediment burial,
diagenesis and fluid migration in different geological settings. It can impact the depositional …