Deepwater fold and thrust belts (DWFTBs) are classified into near-field stress-driven Type 1
systems confined to the sedimentary section, and Type 2 systems deformed by either far …

Subsurface sediment remobilization and fluid flow processes and their products are
increasingly being recognized as significant dynamic components of sedimentary basins …

In an active petroleum system the amount of trapped hydrocarbons is the difference between
the volumes charged and the volumes that have leaked or are otherwise destroyed. This …

Fluid flow features such as sandstone intrusions, mud volcano systems and pockmarks
represent well-known geological structures generated due to flow of fluids in the subsurface …

Many structures associated with fluid escape, including mud volcanoes, mud-carbonate
mounds, pockmarks and slides, have been identified and characterized in the Gulf of Cádiz …

We have mapped 18,000+ circular mounds in a portion of southern Acidalia Planitia using
their sizes, shapes, and responses in Nighttime IR. We estimate that 40,000+ of these …

On May 29th 2006 a mud volcano, later to be named 'Lusi', started to form in East Java. It is
still active and has displaced> 30,000 people. The trigger mechanism for this, the world's …

This study examines the use of specific mud volcano features (ie, elongated calderas,
aligned vents and elongated volcanoes) as potential indicators of tectonic stress orientation …

Terra Nova, 24, 255–272, 2012 Abstract Cold seep systems comprise three structural
elements: source, plumbing system, and venting structures or seeping features at or near the …

New high-resolution seismic and swath bathymetry data reveal the detailed structure of nine
mud volcanoes and two large fields of pockmarks at water depths of 400–1100m in the …