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XRF-Scanning elemental data 30kV of IODP Site 363-U1483
We performed high-resolution X-ray fluorescence (XRF) core scanning with the 2nd Generation Avaatech XRF Core Scanner at the Institute of Geosciences,... -
X-ray fluorescence (XRF) data of sediment core GeoB24351-1, 30 kV run
X-Ray fluorescence (XRF) scans were carried out for core GeoB24351-1 (Gelendzhik MV; 0-284 cm) in 10 mm steps downcore on the split core surface of the archive half with the XRF... -
X-ray fluorescence (XRF) data of sediment core GeoB24351-1, 50 kV run
X-Ray fluorescence (XRF) scans were carried out for core GeoB24351-1 (Gelendzhik MV; 0-284 cm) in 10 mm steps downcore on the split core surface of the archive half with the XRF... -
Pore water geochemistry of sediment core GeoB24352-1
The samples are retrieved from sediment core GeoB24352-1 (Heraklion MV; 0-272 cm) in the Olimpi mud volcano field, located south of Crete at the Mediterranean Ridge accretionary... -
Pore water geochemistry of sediment core GeoB24346-2
The samples are retrieved from sediment core GeoB24346-2 (Milano MV; 0-274 cm) in the Olimpi mud volcano field, located south of Crete at the Mediterranean Ridge accretionary... -
Pore water geochemistry of sediment core GeoB24348-2
The samples are retrieved from sediment core GeoB24348-2 (Brine pool; 0-537 cm) in the Olimpi mud volcano field, located south of Crete at the Mediterranean Ridge accretionary... -
Pore water geochemistry of sediment core GeoB24351-1
The samples are retrieved from sediment core GeoB24351-1 (Gelendzhik MV; 0-284 cm) in the Olimpi mud volcano field, located south of Crete at the Mediterranean Ridge... -
Pore water geochemistry of sediment core GeoB24343-1
The samples are retrieved from sediment core GeoB24343-1 (Monza MV; 0-318 cm) in the Olimpi mud volcano field, located south of Crete at the Mediterranean Ridge accretionary... -
Pore water geochemistry of sediment core GeoB24324-2
The samples are retrieved from sediment core GeoB24324-2 (Brine Pool; 0-445 cm) in the Olimpi mud volcano field, located south of Crete at the Mediterranean Ridge accretionary... -
Pore water geochemistry of sediment core GeoB24311-1
The samples are retrieved from sediment core GeoB24311-1 (Bergamo MV; 0-356 cm) in the Olimpi mud volcano field, located south of Crete at the Mediterranean Ridge accretionary... -
Pore water geochemistry of sediment core GeoB24310-1
The samples are retrieved from sediment core GeoB24310-1 (Napoli MV; 0-280 cm) in the Olimpi mud volcano field, located south of Crete at the Mediterranean Ridge accretionary... -
XRF data sheet: Weiße Elster overbank silt-clay deposition (SC40 core, Salsit...
We used stationary XRF spectrometry for analysing elemental composition of Holocene floodplain sediments from a recovered core form the Weiße Elster floodplain. For XRF sample... -
XRF data sheet: overbank silt-clay deposition sampling (4*4 km grid, Weiße El...
We used stationary XRF spectrometry for analysing elemental composition of bank and streambed samples from Weiße Elster sub-basins (refined grids of 44 km). For XRF sample... -
XRF element data of fluvial deposits from the Weiße Elster catchment
We used stationary XRF spectrometry for analysing elemental composition of bank and streambed samples from Weiße Elster sub-basins (111 grids of 8*8 km). For XRF sample... -
Inter-comparison of ICP and XRF-scanning results by four different XRF-labs (...
Four discrete samples were freeze-dried and powdered and pressed into disc-shaped pellets about 2 cm in diameter from nearby Core MD01-2407 on the Oki Ridge (37°04'N, 134°42'E,... -
Inter-comparison of XRF core scanning results from IODP Site 346-U1424 and 34...
Over the course of four years (2014 to 2017), the set of seven u-channels was shipped around the world to seven labs with XRF scanners including, in no particular order, the... -
Raw values of boundary layer Br2 measurements at Neumayer III station, Antarc...
From January 2016 until August 2018, an automated Long-Path Differential Optical Absorption Spectroscopy (LP-DOAS) instrument was operated at the German research station... -
Porewater analyses of sediment core M157_41-13
Fe2+ was analysed photometrically (Hach Lange DR 5000 photometer) at 565 nm following the method of Collins et al. (1959). 1 mL of acidified sample (20 L of 1% ascorbic acid)... -
Porewater analyses of sediment core M157_41-03
Fe2+ was analysed photometrically (Hach Lange DR 5000 photometer) at 565 nm following the method of Collins et al. (1959). 1 mL of acidified sample (20 L of 1% ascorbic acid)... -
XRF analysis data from sediment core MD18-3532, eastern Taiwan, over the past...
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