Dyke swarms are common on Earth and other planetary bodies, comprising arrays of dykes
that can extend laterally for tens to thousands of kilometres. The vast extent of such dyke …

Pockmarks are geohazards that can impact offshore developments, and an understanding of
their formation assists in determination of their physical characteristics and in the prediction …

Lateral spread and submarine creep are processes that occur near the headwalls of both
terrestrial landslides and submarine mass‐transport complexes (MTCs). Both submarine …

A detailed tectono-stratigraphic analysis of the Mesozoic through Present-day structures and
sedimentary sequences has been carried-out on a very large merged 3-D seismic survey …

Understanding how normal faults grow is key to determining the tectono‐stratigraphic
evolution of rifts. According to recent studies, normal faults tend to grow in two temporally …

Fluid escape pipes are vertical pathways of focused flow venting from a variety of deep
overpressure sources. These geological features are typical of many sedimentary basins …

Pit craters are quasi‐circular depressions observed on rocky and icy planetary bodies, as
well as numerous asteroids. Pit craters are thought to form by overburden collapse into a …

Mass transport deposits have long been known on the Exmouth Plateau, offshore NW
Australia, identified in 2D and 3D industry seismic lines. The expedition SO257 in 2017 …

Submarine mass wasting plays a fundamental role in transporting substantial volumes of
sediments basinward including gigantic slide blocks. However, the understanding of …

The syn‐rift architecture of extensional basins records deposition from and interactions
between footwall‐, hangingwall‐, and axially‐derived systems. However, the exact controls …