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(Table 2a) TOC and trace metal concentrations in ODP Hole 161-974C
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(Table 1a) Trace metal concentrations in sequential digests of ODP Hole 161-974C
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(Table 3) Distribution of chemical elements in ferromanganese crusts from the...
This dataset has no description
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(Table 1) Age and U and Th isotopes in bottom sediments from Core VER-99-1-St...
Relative errors are shown for 1 sigma based on 10 measurements. Extracts have been recovered by 8% (0.7 M) water solution of NH4HCO3. -
(Table 1) Isotope ratios of Lesser Antilles lavas
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(Appendix C3) Rare earth element concentration in ODP Hole 129-802A sediments
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(Appendix C2) Rare earth element concentration in ODP Site 129-801 sediments
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(Appendix C1) Rare earth element concentration in ODP Hole 129-800A sediments
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(Table 2) Major and trace element chemical composition of igneous rocks of OD...
This dataset has no description
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(Table 7) Uranium contents in DSDP Leg 42 Black Sea bottom sediments before a...
This dataset has no description
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(Table 6) Uranium contents in New Euxinian to recent bottom sediments of the ...
This dataset has no description
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(Table 3) Uranium contents in Black Sea bottom sediments from DSDP Leg 42 holes
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(Table 2) Whole-rock major and trace element compositions of granite samples ...
This dataset has no description
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(Table 33a) Composition of Atlantic Ocean bottom sediments and uranium concen...
This dataset has no description
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(Table 33b) Composition of Pacific Ocean bottom sediments and uranium concent...
This dataset has no description
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(Table 33c) Composition of Black Sea bottom sediments and uranium concentrati...
This dataset has no description
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(Table 28) Uranium in sediment cores from the Aral Sea
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Debris bulk oxide and trace elemental composition from glaciers in Norway, Ne...
Expected accuracy 98%. -
Snow and ice trace elemental abundances from glaciers in Norway, Nepal and Ne...
0 = below detection limit; expected accuracy 90%. -
Sedimentation and accumulation rates of opal, carbonate and organic carbon an...
Note that MARtoc, MARcaco3, and MARopal (mg/cm2/y) are not 230Th fluxes, but are estimated as: MAR = f * LSR * DBD (where DBD = dry bulk density; LSR = linear sedimentation...