Results 211 to 220 of about 6,266 (245)
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Pockmarks in the floor of Penobscot Bay, Maine
Geo-Marine Letters, 1989Hundreds of depressions (pockmarks) were found within a 40 square kilometer area of the sea floor near the head of Penobscot Bay, Maine. These roughly circular depressions range in diameter from 10 to 300 meters and extend as much as 30 meters below the surrounding sea floor.
Kathryn M. Scanlon, Harley J. Knebel
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Characteristics of pockmarks in the Norwegian Trench
Marine Geology, 1981A 3 km wide corridor across the Norwegian Trench was surveyed in detail with high-resolution, side-scan sonar and subbottom profiler (boomer) in order to study pockmarks. The pockmarks in the Norwegian Trench are dish-shaped depressions found in the soft, silty clays.
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Late Miocene Pockmarks in the Danish Central Graben - Origin and Significance
68th EAGE Conference and Exhibition incorporating SPE EUROPEC 2006, 2006Late Miocene pockmarks have been identified and mapped in 3D seismic surveys covering large parts of the Danish Central Graben. The upper Miocene succession comprises a thick westward progradational wedge of clay, silt and sand grade siliciclastic sediments. The majority of the pockmarks are located in the clay prone toesets.
Andresen, Katrine +2 more
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Discovery of pockmarks in the Zengmu Basin, southern South China Sea and the implication
Journal of Oceanology and Limnology, 2023Yanlin Wang +6 more
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Can subaerial pockmarks exist?
2010A new possible example of subaerial pockmark is shown. Recently, a question has been put foreward (Castellarin et al. 2006) as to whether the natural degassing of the Po plain sedimentary succession could originate morphological features such as marine pockmarcks (at least from the functional standpoint) in the present continental domain and, therefore,
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Shallow Gas Hydrates Associated to Pockmarks in the Northern Congo Deep-Sea Fan, SW Africa
World Atlas of Submarine Gas Hydrates in Continental Margins, 2022T. Pape, G. Bohrmann
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