With the advent of widely available 3D seismic data, numerous workflows focused on
extracting subsurface stratigraphic information have been developed. We present here tools …

In understanding the evolution of siliciclastic systems, Late Quaternary analogs may enable
reliable predictive models of facies-tract architecture. The Po Plain–Adriatic Sea system …

Although facies and stratal geometries of continental margin successions can be defined in
detail based on subsurface and outcrop studies, most studies lack the high-resolution age …

Mass transport deposits can cause marine geohazards and transport sediments to deep-
water areas and act as hydrocarbon reservoirs and seals, which have been extensively …

Free gas is an important trigger of instability on continental slopes, and resulting mass-
wasting strata can potentially form competent seals to hydrocarbon accumulations. This …

Seismic reflection utilizes sound waves transmitted into the subsurface, reflected at rock
boundaries, and recorded at the surface. Interpretation of their travel times and amplitudes …

Submarine slope failures and their products occur at variable scales on continental margins
and island flanks. Here, we review the petrophysics of fine-grained mass-transport deposits …

Recurrent mass transport deposits (MTD) not only act as competent seals trapping fluids, but
their basal shear zones connected by pipes also serve as potential reservoirs for gas …

Submarine landslides have been identified in almost all ocean basins worldwide. The
largest submarine landslides occur on very shallow slopes and can be far larger than any …

Gravity-driven processes are important agents for transporting sediments downslope into
deep-marine environments. The Pliocene to Holocene offshore succession of the …