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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... -
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... -
Geostatistical analyses of IODP Hole 339-U1389B
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... -
Geostatistical analyses of IODP Hole 339-U1389A
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... -
Geostatistical analyses of IODP Hole 339-U1387B
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... -
Geostatistical analyses of IODP Hole 339-U1387A
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... -
Geostatistical analyses of IODP Hole 339-U1386B
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... -
Geostatistical analyses of IODP Hole 339-U1386A
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... -
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... -
Geostatistical analyses of IODP Hole 339-U1389C
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... -
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... -
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. -
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:... -
X-ray fluorescence (XRF) measurements of sediment core GeoB22722-5
XRF Core Scanner data were collected at the split core surface of the archive half with a XRF Core Scanner II (AVAATECH Serial No. 2) at the MARUM - University of Bremen.... -
Total organic carbon, carbonate and total sulphur content of sediment core Ge...
Total organic carbon (TOC), carbonate and sulphur content was determined at the Faculty of Geosciences, University of Bremen, using a Leco CS744. Sample preparation involved... -
Terrigenous grain-size measurements of sediment core GeoB22722-5
Measurements were performed with a Beckman Coulter Laser diffraction particle size analyzer LS 13 320 at MARUM laboratories (University of Bremen). Samples were pretreated with... -
Bulk grain-size measurements of sediment core GeoB22722-5
Measurements were performed with a Beckman Coulter Laser diffraction particle size analyzer LS 13 320 at MARUM laboratories (University of Bremen). Samples were pretreated with... -
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... -
Sinking velocity of silt and sand from IODP Core 339-U1389A-25X
This dataset has no description
