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Geochemistry by ICP in pore waters of sediment cores from James Cook cruise J...
Geochemical data for major and minor cations in pore waters obtained on ICP-MS (ThermoScientific X-Series 2) and ICP-OES (Thermo Scientific ICAP 6500 Duo). Quality-controlled... -
Paleomagnetism in sediment core JC138-52GC from James Cook cruise JC138
Paleomagnetic data as mean deconvolute relative paleomagnetic intensity (after applying the deconvolution optimization with the UDECON software) in 52GC, as well as comparison... -
Stable oxygen isotopes in sediment cores from James Cook cruise JC138
Stable oxygen isotopes for the cores JC138-27GC, JC138-28GC, JC138-29GC, JC138-38GC, JC138-49GC and JC138-52GC, measured on a Kiel IV Carbonate device coupled to a MAT253... -
Calcium carbonate by coulometry in sediment cores from James Cook cruise JC138
Calcium carbonate concentrations measured on CM5015 coulometer at the SEAPORT laboratories (University of Southampton) for the cores JC138-27GC, JC138-28GC, JC138-29GC,... -
Chemostratigraphy of sediment core JC138-52GC
The chemostratigraphy of sediment core JC138-52GC was analysed with the ITRAX core-scanning X-ray fluorescence system (Cox Analytical Systems) at BOSCORF. The ITRAX produced a... -
Chemostratigraphy of sediment core JC138-49GC
The chemostratigraphy of sediment core JC138-49GC was analysed with the ITRAX core-scanning X-ray fluorescence system (Cox Analytical Systems) at BOSCORF. The ITRAX produced a... -
Chemostratigraphy of sediment core JC138-39GC
The chemostratigraphy of sediment core JC138-39GC was analysed with the ITRAX core-scanning X-ray fluorescence system (Cox Analytical Systems) at BOSCORF. The ITRAX produced a... -
Chemostratigraphy of sediment core JC138-38GC
The chemostratigraphy of sediment core JC138-38GC was analysed with the ITRAX core-scanning X-ray fluorescence system (Cox Analytical Systems) at BOSCORF. The ITRAX produced a... -
Chemostratigraphy of sediment core JC138-28GC
The chemostratigraphy of sediment core JC138-28GC was analysed with the ITRAX core-scanning X-ray fluorescence system (Cox Analytical Systems) at BOSCORF. The ITRAX produced a... -
Chemostratigraphy of sediment core JC138-27GC
The chemostratigraphy of sediment core JC138-27GC was analysed with the ITRAX core-scanning X-ray fluorescence system (Cox Analytical Systems) at BOSCORF. The ITRAX produced a... -
Chemostratigraphy of sediment core JC138-16GC
The chemostratigraphy of sediment core JC138-16GC was analysed with the ITRAX core-scanning X-ray fluorescence system (Cox Analytical Systems) at BOSCORF. The ITRAX produced a... -
Chemostratigraphy of sediment core JC138-031RD
The chemostratigraphy of sediment core JC138-31RD was analysed with the ITRAX core-scanning X-ray fluorescence system (Cox Analytical Systems) at BOSCORF. The ITRAX produced a... -
Chemostratigraphy of sediment core JC138-29GC
The chemostratigraphy of sediment core JC138-29GC was analysed with the ITRAX core-scanning X-ray fluorescence system (Cox Analytical Systems) at BOSCORF. The ITRAX produced a... -
Chemostratigraphy of sediment core JC138-022RD
The chemostratigraphy of sediment core JC138-22RD was analysed with the ITRAX core-scanning X-ray fluorescence system (Cox Analytical Systems) at BOSCORF. The ITRAX produced a... -
Density and porosity of sediment cores from James Cook cruise JC138
Porosity and bulk density were calculated from known volume and weight of sediments before and after drying at 50°C or freeze-drying. Large imprecision of the porosity and... -
Grain sizes of sediment cores from James Cook cruise JC138
Grain size was measured on 5 carbonate ooze samples and 18 hydrothermal sediment samples with the Malvern Masterize Particle Size Analyser. The instrument measured 5 aliquots of... -
Porewater geochemistry of sediments from ROV push cores during Pourquoi Pas ?...
Deep-sea sediment samples were taken from the (wider) Kairei hydrothermal field area (25°S, 70°E) as well as a remote site (26°S, 71°E) in the Indian Ocean during the INDEX... -
Solid phase geochemistry of sediments from ROV push cores during Pourquoi Pas...
Deep-sea sediment samples were taken from the (wider) Kairei hydrothermal field area (25°S, 70°E) as well as a remote site (26°S, 71°E) in the Indian Ocean during the INDEX...