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(Table 1) Geochemistry of ODP Hole 128-798B
Because of heterogeneity, average values of sediment composition can be difficult to establish accurately in fine-grained rocks. As a result, derived values (such as biogenic... -
(Table 1) Sediment chemistry and Sulphur isotope ratios of ODP Site 127-795
Sixty sediment samples collected every 10 m from Holes 795A and 795B in the northern Japan Sea were analyzed for 27 major and trace elements using instrumental neutron... -
(Table 1) Chemical and isotopic composition of pore fluids in cores TGC-1 and...
The role of sediment diagenesis in the marine cycles of Li and B is poorly understood. Because Li and B are easily mobilized during burial and are consumed in authigenic clay... -
Major- and trace-element analyses of cherts, porcellanites, oozes, and clays ...
Analyses of 42 Cretaceous rock samples from Deep Sea Drilling Project (DSDP) Leg 32, in the northern Pacific, show that chert and porcellanite are enriched in Fe, Mn, P, Cu, Ba,... -
(Table 1) Data of direct potentiometric determinations of bromides in seawate...
A new method is presented for on board determination of bromide concentrations in seawater with use of a bromide ion-selective electrode with (accuracy of +/-3 %). The activity... -
(Table 1) Chemical composition of interstitial waters from the area of gas hy...
Distributions of halogens (Cl, Br and I) in interstitial waters from sediments containing methane hydrate and in water of the hydrate itself are presented. High concentrations... -
(Table 2) Composition of rain water collected over the Indian Ocean in 1967
Analytical data on the basic salt composition in evaporation products of sea (ocean) water and of rain water falling on the central area of the Indian Ocean are examined. Both... -
(Table 1) Pore water halogen concentrations in ODP Holes 169-1033B and 169-1034B
The entire suite of halogens was measured in the pore fluids of Hole 1033B and 1034B from Saanich Inlet: ODP Leg 169S. The fast sedimentation rates and large amount of organic... -
Concentrations of heavy and precious metals in animals from hydrothermal vent...
A series of samples of inhabitants of hydrothermal vents were collected during the 12-th cruise ofR/V Akademik Mstislav Keldysh in Guaymas Basin (the Gulf of California) and the... -
X-ray fluorescence (XRF) data of sediment core GeoB8903-1
This dataset has no description
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Major and trace element abundance in sediment samples from ODP Hole 121-758B ...
Major and trace element analyses of 30 sediment samples from ODP Core 758B across the Brunhes-Matuyama geomagnetic polarity reversal and the Australasian microtektite-bearing... -
(Table 1) Chemical composition of Mediterranean halite from DSDP Hole 13-134
Bromine content of a 15 cm halite core from Deep Sea Drilling Project Leg XIII Hole 134 was analyzed at 1.5 cm intervals. The Br varies from 140 to 254 ppm, and three maxima... -
(Appendix 1) Element concentrations in sediment and basalt samples from DSDP ...
The geochemistry of the REE (rare earth elements) in oceanic sediments is discussed, based mainly on samples from DSDP Holes 530A and 530B, Leg 75, and Hole 525A, Leg 74. The... -
Chemical composition of hydrothermal fluids at station MSM04/3-282-ROV-2
Inductively Coupled Plasma Mass Spectrometry: dilution factor = 25; Matrix = 0.5M HNO3. Inductively Coupled Plasma Optical Emission Spectrometry: dilution factor = 10; Matrix =... -
Chemical composition of hydrothermal fluids at station MSM04/3-275-ROV-7
Inductively Coupled Plasma Mass Spectrometry: dilution factor = 25; Matrix = 0.5M HNO3. Inductively Coupled Plasma Optical Emission Spectrometry: dilution factor = 10; Matrix =... -
Chemical composition of hydrothermal fluids at station MSM04/3-275-ROV-5
Inductively Coupled Plasma Mass Spectrometry: dilution factor = 25; Matrix = 0.5M HNO3. Inductively Coupled Plasma Optical Emission Spectrometry: dilution factor = 10; Matrix =... -
Chemical composition of hydrothermal fluids at station MSM04/3-271-ROV-4
Inductively Coupled Plasma Mass Spectrometry: dilution factor = 25; Matrix = 0.5M HNO3. Inductively Coupled Plasma Optical Emission Spectrometry: dilution factor = 10; Matrix =... -
Chemical composition of hydrothermal fluids at station MSM04/3-271-ROV-18
Inductively Coupled Plasma Mass Spectrometry: dilution factor = 25; Matrix = 0.5M HNO3. Inductively Coupled Plasma Optical Emission Spectrometry: dilution factor = 10; Matrix =... -
Chemical composition of hydrothermal fluids at station MSM04/3-271-ROV-11
Inductively Coupled Plasma Mass Spectrometry: dilution factor = 25; Matrix = 0.5M HNO3. Inductively Coupled Plasma Optical Emission Spectrometry: dilution factor = 10; Matrix =... -
Chemical composition of hydrothermal fluids at station MSM04/3-263-ROV-8
Inductively Coupled Plasma Mass Spectrometry: dilution factor = 25; Matrix = 0.5M HNO3. Inductively Coupled Plasma Optical Emission Spectrometry: dilution factor = 10; Matrix =...