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Ar-Ar ages of iceberg-rafted debris from Scotia Sea IODP Site 382-U1538
Ar-Ar ages of 58 individual hornblendes and micas picked from a discrete iceberg-rafted layer deposited ~1.2 Ma at IODP U1538. The layer was recovered 310.79–310.82 meters below... -
CRONUS Input of all samples from the detrital river sediment in central Cuba
Input data table for the online calculator described by Balco et al. (2008) (hess.ess.washington.edu) and subsequently updated. Note: This table is set up so that you can open... -
(Appendix 5) Major element composition of brucite, iowaite, chlorite and serp...
This dataset has no description
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(Appendix 4) Average trace element concentrations in relict olivine, orthopyr...
This dataset has no description
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(Appendix A) Major element composition of serpentine, brucite, Fe- and Cl-ric...
Sample S021 = 84-566C-6-1,9-12 piece 1, 117.3 to 117.6 mbsf. -
(Table 3) Chemical and mineralogical composition of the deposits
Mineralogy: + + = abundant, + = present, t = trace, - = not detected -
(Table 2) Selected analyses for garnet pyroxenite and amphibolite samples fro...
Garnet pyroxenite samples = W216, W218, W240, W242A and garnet amphibolite samples = W232, W251, W334. -
Siderite C-O-Fe isotope compositions, pore water geochemistry and bulk sedime...
Siderite C-O-Fe isotope compositions, pore water geochemistry and bulk sediment measurements covering the 100 m-long core from drill site TDP-1A in ferruginous Lake Towuti,... -
(Table 5) U/Pb dating on monazite and zircon from leucogranite results (Rennes)
This dataset has no description
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(Table 1) Age analysis at DSDP Hole 57-439
Correction factors used are (39Ar/37Ar)Ca = 0.0039, (36Ar/37Ar)Ca = 0.00029, (40Ar/39Ar)K = 0.031. Errors given in the apparent ages indicate 1 sigma. Empty cells = no data. -
(Table 1) Helium and argon within fluid inclusions in precipitates from subsu...
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(Table S3) Argon geochemistry of minerals from Hawaiian-Emperor seamounts
Position of the seamounts are estimated. The parameter J, a measure of the extent of conversion of 39K to 39Ar, was determined for each sample by analyzing co-irradiated Fish... -
(Table 1) Isotopic composition of noble gases from metasediments
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(Table 1) U and Th isotope analyses of pyrite and anhydrite of ODP Site 158-957
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... -
(Table 2) Chalcopyrite and Sphalerite geochemistry of the Ermioni Volcanogeni...
All percentages in wt%. -
(Table 2) Pukeonake plagioclase, clinopyroxene, orthopyroxene, olivine and ox...
Oxygen isotope compositions determined by laser fluorination (see main text for analytical methods). Numbering of minerals denotes similar crystals. Values of 0.00 are below... -
(Table 1) Pukeonake whole rock, glass and glass inclusion compositions
Matrix glasses and glass inclusion major elements were measured by electron microprobe, whole rock major elements were determined by XRF and whole rock trace element analyses... -
Seawater carbonate chemistry and carbon isotope values (delta 13C) in the mus...
Ocean acidification (OA) and global warming present future challenges for shell producing organisms such as mussels through reduction in the carbonate available to produce... -
(Table 1, page 67) Chemical analyses and XRD determined mineralogy of mangane...
The uptake of Ni and Co in the hydrous Mn oxide or the amorphous Fe-oxide phases of ferromanganese deposits in the oceans was studied by electron-microprobe analyses of 17... -
δ44Ca stable isotopes of Dharamjali speleothem DHAR-1A (Table X1)
This dataset has no description