Dataset - B2FIND

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 4) Average trace element concentrations in relict olivine, orthopyr...

This dataset has no description

(Table 3) Chemical and mineralogical composition of the deposits

Mineralogy: + + = abundant, + = present, t = trace, - = not detected

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

(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...

This dataset has no description

(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

This dataset has no description

(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...

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...