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Radiogenic isotopic record of Pliocene speleotherms from Coves d'Artá, Mallorca
These final results assume an initial δ234U of 750 ‰. -
(Tabel 2) U-series ages, isotope concentrations and ratios of sediment cores ...
U-series datings were performed on fragments of the two cold-water coral species Lophelia pertusa and Enallopsammia profunda.1 Th corrected ages.* discarded. -
(Table S4) 230Th/U-dating of coral BON-39-A
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(Table 1) U-series ages and epsilon-Nd values obtained for cold-water coral s...
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(Table 2) Age determination based on U-series analysis on Lophelia pertusa fr...
This dataset has no description
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(Table A1) Open-system age model and Uranium/Thorium analyses of coral sample...
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(Table 2) U and Th concentrations, isotopic activity ratios, and ages of cora...
This dataset has no description
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(Table 3) Uranium and thorium contents and determined activity ratios from ME...
This dataset has no description
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(Table 2) Age determination of Desmophyllum dianthus samples
This dataset has no description
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(Table 1) Uranium-Thorium datings from corals of Hainan Island, South China Sea
All isotopic ratios are activity ratios. Errors are quoted as 2 sigma. Half lives used in the calculation are as follows: 230Th, 77381 ± 590 (2s); 234U, 244600 ± 490 (2s);... -
(Table 1) Th and U isotope ratios of sediments from ODP Site 166-1009
U and Th blanks are <1‰ of the measured sample and are corrected for. Raw ages and delta234U values are adjusted to account for initial 230Th to give the corrected numbers in... -
(Table 1) Th and U isotope ratios of sediments from ODP Site 166-1008
U and Th blanks are <1‰ of the measured sample and are corrected for. Raw ages and delta234U values are adjusted to account for initial 230Th to give the corrected numbers in... -
(Table 1) TIMS U and Th concentrations and isotope ratios of ODP Leg 166 sites
AGE is the corrected age -
(Table 1) Uranium and thorium mass spectrometric results for stalagmite 1s
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(Table 1) Details on the Uranium/Thorium age determinations carried out on co...
Cold-water corals are widely distributed along the Atlantic continental margin with varying growth patterns in relation to their specific environment. Here, we investigate the... -
(Table 1) U and Th isotope analyses of pyrite and anhydrite of ODP Site 158-9...
Hydrothermal circulation at oceanic spreading ridges causes sea water to penetrate to depths of 2 to 3 km in the oceanic crust where it is heated to ~400 °C before venting at...