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Sediment and geochemistry of bi-gradational contourite sequences from the Gul...
The contourite depositional systems at the Gulf of Cadiz during IODP 339 are characterised by the repetition of bi-gradational sequences. These sequences are of an average... -
Thickness, age and layers data of sediments at IODP Site U1386, U1387, and U1389
The bi-gradational sequence is recognised as a defining feature of contourite deposition. The present research questions are: In what pattern these bi-gradational sequences are... -
Sediment echosounder processed data (Atlas Parasound P70 echosounder working ...
The main objectives of the study are to characterize the sedimentary structures observed in the area where internal waves interact with the seafloor and to identify the... -
Vessel-mounted ADCP current measurements from offshore Namibia during RV METE...
The main objectives of the study are to characterize the sedimentary structures observed in the area where internal waves interact with the seafloor and to identify the... -
Interaction of a deep-sea current with a blind submarine canyon (Mar del Plat...
The Mar del Plata (MdP) Canyon at the Argentine continental margin is incorporated into a major contourite depositional system, built by the incursion of southern-sourced water... -
Mineral quantification of sediment cores GeoB2703-5, GeoB6812-1, GeoB13861-1,...
Results are weight % if not stated differently values smaller than 1 wt.% can only be seen as traces of the mineral. -
X-ray diffraction analysis of turbidite sediment cores GeoB2703-5, GeoB6812-1...
This dataset has no description
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Grain size analysis of turbidite sediment cores GeoB2703-5, GeoB6812-1, GeoB1...
This dataset has no description
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Age and turbidite of sediment cores GeoB13861-1,GeoB13823-2, and GeoB13824-1
(Ts = sandy turbidite; Tm = muddy turbidite). -
Age and magnetic susceptibility of sediment core GeoB13861-1
This dataset has no description
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Mass flux, major components and the Lead 210 concentration of sediment collec...
To monitor particle fluxes and near bottom hydrographic variability a modified version of the benthic Bottom Boundary (BOBO) lander was deployed at 57 29.09 N, 27 54.53 W on the... -
Current speed and acoustic backscatter data measured with a Bottom Boundary (...
To monitor particle fluxes and near bottom hydrographic variability a modified version of the benthic Bottom Boundary (BOBO) lander was deployed at 57° 29.09 N, 27° 54.53 W on...
