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 …

In most basins, lateral subsurface petroleum migration occurs over tens or even hundreds of
kilometers between source rock and trap and between accumulations and the surface. In …

A synthesis of backscatter imagery coupled with a large 3D seismic dataset in the Lower
Congo Basin (LCB) reveals a patchy distribution of features interpreted to be associated with …

Cold seeps have been observed with manned submersibles at many sites on the Tokai
margin. Most sites are found on the hanging wall of major thrust faults, within 1–2 km of their …

In situ measurement of fluid flow rates from active margins is an important parameter in
evaluating dissolved mass fluxes and global geochemical balances as well as tectonic …

Abstract Three-dimensional (3D) seismic data, combined with semi-automated mapping in
ArcGIS, were used to analyse the morphology and distribution of 720 pockmarks and 62 …

Cold seeps in deep marine settings emit fluids to the overlying ocean and are often
associated with such seafloor flux indicators as chemosynthetic biota, pockmarks, and …

Geochemical and geophysical evidence indicate that splay faults cutting subduction zone
forearcs are a key hydraulic connection between the plate boundary at depth and the …

Marine cold seeps are windows into different depth levels of the submerged geosphere.
Subduction zones and organic-rich passive margins host most of the world's cold seeps. The …

The subsurface plumbing system of ancient seeps of hydrocarbon-rich gases and fluids is
partially preserved by seep deposits in Miocene rocks of the Coast Ranges and on the …