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Sediment structure and deposition rates of sediment core PG2303 1
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Sediment structure and deposition rates of sediment core YC18 HB GCO1
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Sediment structure and deposition rates of sediment core YC18 PB SCO1
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(Table 1-2 and 3, page 282-284) 10Be, U, Th, 226Ra and 210Pb analyses for lay...
From 1983 until 1989 NOAA-NCEI compiled the NOAA-MMS Marine Minerals Geochemical Database from journal articles, technical reports and unpublished sources from other... -
Physical oceanography, river water fraction, 226Ra, and 228Ra measured on wat...
Water temperature and salinity taken from Markus Frank (1996) -
Export production by 234Th, including 210Po and 210Pb measured on water bottl...
This dataset has no description
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Geochemical glass data for the contribution: Identifying fluid-fluxed versus ...
File contains, campaigns, events, locations, major and trace elements, H2O, radiogenic and short-lived isotopes of new data along with respective analytical facility for the... -
Radiochemical data for a manganese nodule sample from the MN7601-PLEIADES cam...
Using radiochemical methods, the authors have measured the distribution of uranium, thorium, radium, polonium and protactinium isotopes from the top and bottom sides of the a... -
Distribution of radioisotopes in polymetallic nodules from the CCZ collected ...
This dataset comprises gamma spectrometric measurements of radioisotopes in samples from polymetallic nodules, which were collected in the framework of the European... -
Radium isotopes and 228Th in water column samples collected on POLARSTERN exp...
Radium isotopes are produced by decay of an isotope of thorium, a highly particle reactive element. Radium is relatively soluble in seawater such that once a thorium isotope in... -
Radium isotopes and 228Th in surface water samples collected on POLARSTERN ex...
Radium isotopes are produced by decay of an isotope of thorium, a highly particle reactive element. Radium is relatively soluble in seawater such that once a thorium isotope in... -
Radium isotopes and 228Th in water column samples collected on POLARSTERN exp...
Radium isotopes are produced by decay of an isotope of thorium, a highly particle reactive element. Radium is relatively soluble in seawater such that once a thorium isotope in... -
Radium isotopes and 228Th in surface water samples collected on POLARSTERN ex...
228Ra is strongly enriched in shelf waters and its half-life (5.8 years) is well suited to study the fate of shelf-derived water in the central Arctic. During PS78 (TRANSARC I)... -
Mineralogical and geochemical characterisation of iron-sulfur deposits from t...
In this dataset, seven inactive massive sulfide chimneys, collected in the Manus Basin (Bismarck Sea, Papua New Guinea, SW Pacific) during SONNE cruise SO216 in 2011, are... -
(Tables 1,2 and 3, pages 853-854) Isotopic data for the solid-phase of three ...
Determination of radium, thorium, uranium isotopes, and 210Pb in sediments and sediment pore waters from North Equatorial Pacific deep-sea clay-silicous oozes shows that the... -
Madrepora oculata and Lophelia pertusa mass and 210Pb-226Ra chronology, Røst ...
Here we show the use of the 210Pb-226Ra excess method to determine the growth rate of corals from one of the world's largest known cold-water coral reef, the Røst Reef off... -
(Table 4) Radionuclide activity in sediment core BL12-10 from the El Bibane L...
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Radionuclides in surface water on cruise ANT-XVII/4
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Radionuclides and silicate measured on water bottle samples during POLARSTERN...
In this thesis the distribution of 210Po and 210Pb in the upper 600 m of the Antarctic Circumpolar Current and the Weddell Sea was investigated along north-south transects in... -
(Table II) Results of the 210Pb and 137Cs analyses from sediment core POS175/1_9
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