Results 71 to 80 of about 2,201 (156)
Journal of Marine Science and EngineeringPockmarks are globally distributed geomorphic features exhibiting diverse morphologies. Their geometric characteristics are commonly quantified by the radius-to-depth ratio.
Zhengrong Zhang +6 more
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, 2020 A Remotely Operated Vehicle (RB600, Eprons Latvia) was used to survey the giant pockmarks. The ROV was equipped with a 360° sonar (SeaPrince, Tritech) and registered video material in VHS and HD quality. A light CTD probe (DCX-22-CTD, Keller Switzerland)
Wirth, Stefanie B +2 more
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GeosciencesFluid seepages and seabed pockmarks are widely observed on continental margins worldwide in hydrate- and non-hydrate-bearing sediment. Subsurface gas chimneys connecting seafloor pockmarks to underlying gas reservoirs are commonly revealed by seismic ...
Zheng Su +3 more
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Геологія і корисні копалини Світового океану, 2019 The article considers the existing models of pokmark formation, processes and structures that form them. Special attention is paid to the regularities of their development in the Black Sea, shape, size and features that are of interest for further study ...
E.N. Rybak, L.V. Stupina
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Мінеральні ресурси України, 2019 Based on an analytical review of factual materials, the article discusses the peculiarities of the distribution of gas hydrates in the development zones of mud volcanism of the Mediterranean, Black and Caspian seas, which are direct indications of ...
Ad. A. Aliyev +2 more
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Alternatives for Hydrocarbon Exploration Offshore Southern Cuba
Revista Cubana de Ingeniería, 2014 Today oil and gas exploration has integrated to the geology and geophysics studies, new technologiesas data from remote sensing that helps to detect interesting aspects for research. Cuban southernpetroleum province has a low exploration level. The study
Isabel Morales Carrillo +3 more
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Deep and shallow structures of large pockmarks in the Turkish shelf, Eastern Black Sea
, 2003 Circular and elongated pockmarks are present between 180- and 300-m water depths in the Eastern Black Sea shelf. The circular pockmarks have diameters of 50-120 m and the elongated pockmarks are 150-200 m wide with crater depths of 10-25 m.
DONDURUR, DERMAN +2 more
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Scotland's pockmarks: understanding their formation and relationship to buried carbon in fjordic systems [PDF]
, 2021 Pockmarks are concave seabed depressions formed by the venting of sub-seabed fluids into the water column. These fluids can contain greenhouse gases such as methane and carbon dioxide, formed by the microbial breakdown of organic carbon, thus creating a ...
Audsley, Allan
core
Journal of Marine Science and EngineeringFerdinandea Island, part of a shallow-water submarine volcanic field, emerged in the Sicily Channel between Italy and Tunisia in July 1831 and was eroded below sea level within months; its submerged remnant forms the shallowest water depth region of ...
Daniele Spatola +5 more
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Pockmarks in Passamaquoddy Bay, New Brunswick, Canada
, 2016 Pockmarks are seafloor depressions associated with fluid escape (Judd & Hovland 2007). They proliferate in the muddy seafloors of coastal Gulf of Maine and Bay of Fundy, where they are associated with shallow natural gas likely of biogenic origin (Ussler
Brothers, L. L. +6 more
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