Results 211 to 220 of about 6,266 (245)
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Pockmarks in the floor of Penobscot Bay, Maine

Geo-Marine Letters, 1989
Hundreds 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
openaire   +1 more source

Characteristics of pockmarks in the Norwegian Trench

Marine Geology, 1981
A 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.
openaire   +1 more source

Late Miocene Pockmarks in the Danish Central Graben - Origin and Significance

68th EAGE Conference and Exhibition incorporating SPE EUROPEC 2006, 2006
Late 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
openaire   +3 more sources

Discovery of pockmarks in the Zengmu Basin, southern South China Sea and the implication

Journal of Oceanology and Limnology, 2023
Yanlin Wang   +6 more
semanticscholar   +1 more source

Sedimentary characteristics and genetic mechanism of the giant ancient pockmarks in the Qiongdongnan Basin, northern South China Sea

Acta Oceanologica Sinica, 2023
Peng Xiong   +9 more
semanticscholar   +1 more source

Formation mechanism of deep-sea giant pockmarks: A case study of the Reed Basin in the South China Sea

Geomorphology, 2023
Ziyin Wu   +7 more
semanticscholar   +1 more source

Pockmarked

JAMA Dermatology, 2016
Walter H C, Burgdorf, Leonard J, Hoenig
openaire   +2 more sources

Can subaerial pockmarks exist?

2010
A 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,
openaire   +1 more source

Shallow Gas Hydrates Associated to Pockmarks in the Northern Congo Deep-Sea Fan, SW Africa

World Atlas of Submarine Gas Hydrates in Continental Margins, 2022
T. Pape, G. Bohrmann
semanticscholar   +1 more source

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