Results 161 to 170 of about 2,782 (220)

Variations in deep-sea methane seepage linked to millennial-scale changes in bottom water temperatures ~ 50-6 ka, NW Svalbard margin. [PDF]

Sci Rep
Rasmussen TL, El Bani Altuna N, Thomsen E.   +2 more
europepmc   +1 more source

An extensive pockmark field on the upper Atlantic margin of Southeast Brazil: spatial analysis and its relationship with salt diapirism. [PDF]

Heliyon, 2017
de Mahiques MM, Schattner U, Lazar M, Sumida PY, Souza LA.   +4 more
europepmc   +1 more source

Only 5 southern Greenland shelf edge glaciations since the early Pliocene. [PDF]

Sci Rep, 2013
Nielsen T, Kuijpers A.
europepmc   +1 more source

A comprehensive sediment dynamics study of a major mud belt system on the inner shelf along an energetic coast. [PDF]

Sci Rep, 2018
Liu JT, Hsu RT, Yang RJ, Wang YP, Wu H, Du X, Li A, Chien SC, Lee J, Yang S, Zhu J, Su CC, Chang Y, Huh CA.   +13 more
europepmc   +1 more source

Morphometry of Concepcion Bank: Evidence of Geological and Biological Processes on a Large Volcanic Seamount of the Canary Islands Seamount Province. [PDF]

PLoS One, 2016
Rivera J, Canals M, Lastras G, Hermida N, Amblas D, Arrese B, Martín-Sosa P, Acosta J.   +7 more
europepmc   +1 more source

Spatial and temporal evolution of the Le Danois Contourite Depositional System, Southern Bay of Biscay [PDF]

, 2012
Van de Putte, S., Van Rooij, D.
core  

Deep sea sediment types on the North Atlantic sea floor

, 1977
Kidd, Robert Benjamin.
core  

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Seismic features diagnostic of contourite drifts

Marine Geology, 1999
Abstract The sedimentary construction of oceanic margins is most often carried out by the combined action of gravitational processes and processes related to bottom (contour) currents. One of the major difficulties encountered in the interpretation of seismic profiles crossing such margins is the differentiation of these two types of deposit ...
Dorrik A V Stow, Patrice Imbert
exaly   +2 more sources

The Lofoten contourite drift off Norway

Marine Geology, 1999
Abstract Based on high-resolution and multichannel seismic data, a contourite drift, the Lofoten Drift, has been identified below ca. 1000 m water depth on the continental slope off Norway. The Lofoten Drift has a maximum thickness of about 360 m. Correlation to published seismic stratigraphy implies a Neogene age.
Jan Sverre Laberg
exaly   +2 more sources

Contourites in the Fram Strait

Sedimentary Geology, 1993
Abstract Multichannel seismic reflection profiles from the Fram Strait show many features that can be attributed to bottom-current influence on the sediments, by comparison with well-known contourite sequences elsewhere. A greater than 2 km thick contourite drift with a smooth internal reflection pattern is observed northwest of Svalbard.
Ola Eiken, Karl Hinz
openaire   +1 more source