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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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Morphological properties of moat-drift systems around the world
To facilitate a comprehensive study of moat-drift systems, we analysed moats from different locations around the world. We measured the following morphological parameters:... -
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... -
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... -
Sinking velocity of silt and sand from IODP Core 339-U1389A-25X
This dataset has no description
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Isotope analysis from IODP Core 339-U1389A-25X
A further 48 samples were analysed for their organic carbon (TOC), CaCO~3~ and stable isotopic contents, using Elemental Analyser - Isotope Ratio Mass Spectrometry (EA-IRMS).... -
Carbonate free bulk analysis from IODP Core 339-U1389A-25X
Grain-size statistical parameters were calculated using Gradistat software (Blott and Pye, 2001) and based on the geometric graphical method (Folk and Ward, 1957). The same... -
Bulk analysis from IODP Core 339-U1389A-25X
Grain-size statistical parameters were calculated using Gradistat software (Blott and Pye, 2001) and based on the geometric graphical method (Folk and Ward, 1957). The same... -
Sinking velocity of silt and sand from IODP Core 339-U1389A-11H
This dataset has no description
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Isotope analysis from IODP Core 339-U1389A-11H
A further 48 samples were analysed for their organic carbon (TOC), CaCO~3~ and stable isotopic contents, using Elemental Analyser - Isotope Ratio Mass Spectrometry (EA-IRMS).... -
Carbonate free grain size analysis from IODP Core 339-U1389A-11H
A total of 96 samples were analysed for bulk grain size from the two selected sequences, using a Malvern Mastersizer laser micro-granulometer (Malvern Panalytical) at the... -
Grain size analysis from IODP Core 339-U1389A-11H
A total of 96 samples were analysed for bulk grain size from the two selected sequences, using a Malvern Mastersizer laser micro-granulometer (Malvern Panalytical) at the... -
Carbonate free bulk analysis from IODP Core 339-U1389A-11H
Grain-size statistical parameters were calculated using Gradistat software (Blott and Pye, 2001) and based on the geometric graphical method (Folk and Ward, 1957). The same... -
Bulk analysis from IODP Core 339-U1389A-11H
Grain-size statistical parameters were calculated using Gradistat software (Blott and Pye, 2001) and based on the geometric graphical method (Folk and Ward, 1957). The same... -
Geostatistical analyses of IODP Hole 339-U1389D
Shipboard core description and thickness measurements were used as base for the current data. These were verified and, where necessary, minor corrections made during re-logging...