Oxygen and hydrogen isotope ratios of interstitial waters from ODP Leg 116 samples

DOI

The oxygen and hydrogen isotope compositions of pore waters are controlled by several processes: (1) hyperfiltration-osmotic effects, (2) carbonate deposition, (3) reaction with volcanic ash, and (4) mixing with water that has reacted with basaltic basement. These data are useful to supplement information obtained from shipboard chemical analyses.

Supplement to: Boulègue, Jacques; Bariac, T (1990): Oxygen and hydrogen isotope ratios of interstitial waters from an intraplate deformation area: Bengal Fan, Leg 116. In: Cochran, JR; Stow, DAV; et al. (eds.), Proceedings of the Ocean Drilling Program, Scientific Results, College Station, TX (Ocean Drilling Program), 116, 127-133

Identifier
DOI https://doi.org/10.1594/PANGAEA.756541
Related Identifier IsSupplementTo https://doi.org/10.2973/odp.proc.sr.116.133.1990
Metadata Access https://ws.pangaea.de/oai/provider?verb=GetRecord&metadataPrefix=datacite4&identifier=oai:pangaea.de:doi:10.1594/PANGAEA.756541
Provenance
Creator Boulègue, Jacques; Bariac, T
Publisher PANGAEA
Publication Year 1990
Rights Creative Commons Attribution 3.0 Unported; https://creativecommons.org/licenses/by/3.0/
OpenAccess true
Representation
Resource Type Supplementary Publication Series of Datasets; Collection
Format application/zip
Size 3 datasets
Discipline Earth System Research
Spatial Coverage (81.390W, -1.021S, 81.401E, -0.930N); South Indian Ridge, South Indian Ocean
Temporal Coverage Begin 1987-07-10T00:00:00Z
Temporal Coverage End 1987-08-02T00:00:00Z