An integrated view of the methane system in the pockmarks at Vestnesa Ridge, 79 N

G Panieri, S Bünz, DJ Fornari, J Escartin, P Serov… - Marine Geology, 2017 - Elsevier
Abstract The Vestnesa Ridge is a NW-SE trending,~ 100 km-long, 1–2 km-thick contourite
sediment section located in the Arctic Ocean, west of Svalbard, at 79° N. Pockmarks align …

Seismic characteristics of fluid escape pipes in sedimentary basins: Implications for pipe genesis

J Cartwright, C Santamarina - Marine and Petroleum Geology, 2015 - Elsevier
Fluid escape pipes were first documented from 3D seismic data over a decade ago, and
have subsequently been identified in many petroliferous basins worldwide. They are …

[HTML][HTML] Sedimentation record of a complete glacial-interglacial cycle: Down-slope deposits, contourites and plumites of the North Sea trough mouth fan

AM Garcia, B Bellwald, S Planke, I Anell… - Quaternary Science …, 2024 - Elsevier
Trough mouth fans (TMFs) are major submarine depocentres that form in front of ice streams
advancing onto the continental shelf, and they provide extensive records of past glaciations …

High-resolution P-Cable 3D seismic imaging of gas chimney structures in gas hydrated sediments of an Arctic sediment drift

CJ Petersen, S Bünz, S Hustoft, J Mienert… - Marine and Petroleum …, 2010 - Elsevier
The newly developed P-Cable 3D seismic system allows for high-resolution seismic imaging
to characterize upper geosphere geological features focusing on geofluid expressions (gas …

Unit-pockmarks and their potential significance for predicting fluid flow

M Hovland, R Heggland, MH De Vries… - Marine and Petroleum …, 2010 - Elsevier
Unit-pockmarks were recognized as more-or-less insignificant features on the seafloor in the
early 1980s. However, this investigation, at four different regions in Norwegian waters …

Repeated fluid expulsion through sub-seabed chimneys offshore Norway in response to glacial cycles

A Plaza-Faverola, S Bünz, J Mienert - Earth and Planetary Science Letters, 2011 - Elsevier
Focused fluid flow through sub-seabed sediments is a common phenomenon on continental
margins worldwide. However, the governing controls and timing of this fluid release have …

Three‐dimensional seismic analysis of the morphology and spatial distribution of chimneys beneath the Nyegga pockmark field, offshore mid‐Norway

S Hustoft, S Bünz, J Mienert - Basin Research, 2010 - earthdoc.org
ABSTRACT Three‐dimensional (3D) seismic data analysis has identified 415 seismic
chimneys in the Nyegga area, on the mid‐Norwegian continental margin. The majority of the …

Resolving hydromechanical coupling in two and three dimensions: spontaneous channelling of porous fluids owing to decompaction weakening

L Räss, T Duretz… - Geophysical Journal …, 2019 - academic.oup.com
Fingering, veining, channelling and focussing of porous fluids are widely observed
phenomena in the Earth's interior, driving a range of geo-processes across all scales. While …

Sea-level change and free gas occurrence influencing a submarine landslide and pockmark formation and distribution in deepwater Nigeria

V Riboulot, A Cattaneo, N Sultan, S Garziglia… - Earth and Planetary …, 2013 - Elsevier
A series of pockmarks observed at the seabed matches well the perimeter of a large
submarine landslide, called NG1, located on the outer shelf and continental slope of the …

Gas hydrate and associated free gas in the Dongsha Area of northern South China Sea

L Li, X Lei, X Zhang, Z Sha - Marine and Petroleum Geology, 2013 - Elsevier
A large ongoing cold seep, named Jiulong Methane Reef, was discovered in the Dongsha
Area of northern South China Sea (SCS) in 2004. To understand links among seafloor …