Isotopic composition of various forms of sulfur in barite crusts from the Red Sea rift
| Cobertura |
LATITUDE: 21.371700 * LONGITUDE: 38.076700 * MINIMUM ELEVATION: -2060.0 m * MAXIMUM ELEVATION: -2020.0 m |
|---|---|
| Data(s) |
03/02/1988
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| Resumo |
Barite crusts were formed by an intermittent hydrothermal vent with output temperature from 85 to 465°C. Principal sources of supply of sulfate sulfur are sea water, evaporites, and tholeiitic basalts of the Red Sea rift. Sulfides and sulfates were formed in conditions of isotope disequilibrium with respect to sulfur because rate of precipitation of sulfur compounds from hydrothermal solution was high compared with rate of isotope exchange. |
| Formato |
text/tab-separated-values, 81 data points |
| Identificador |
https://doi.pangaea.de/10.1594/PANGAEA.756823 doi:10.1594/PANGAEA.756823 |
| Idioma(s) |
en |
| Publicador |
PANGAEA |
| Direitos |
CC-BY: Creative Commons Attribution 3.0 Unported Access constraints: unrestricted |
| Fonte |
Supplement to: Strizhov, Valentin P; Sval'nov, Vyacheslav N; Nikolaev, Sergey D; Zhabina, Nina N; Gurina, NV (1988): Isotope composition of sulfur in barite crusts of the Red Sea. Oceanology, 28(1), 83-85 |
| Palavras-Chave | #Archive of Ocean Data; ARCOD; Calculated; delta 34S, sulphate; delta 34S, sulphide; Dredge; DRG; Mass spectrometry; PIKAR; PS-407; Red Sea; Sample code/label; Sample type; Sulphides; Sulphur, elemental; Sulphur bound in Sulphate; Temperature, calculated; Wet chemistry |
| Tipo |
Dataset |
