S34/S32 measurements and trace element analyses were performed on sediment from selected cores from the Red Sea geothermal deposit, the overlying brine and interstitial water. The data show that δS34 falls into four general ranges: (1) >25 per mill, (2) +23...
CITATION STYLE
Kaplan, I. R., Sweeney, R. E., & Nissenbaum, A. (1969). Sulfur Isotope Studies on Red Sea Geothermal Brines and Sediments. In Hot Brines and Recent Heavy Metal Deposits in the Red Sea (pp. 474–498). Springer Berlin Heidelberg. https://doi.org/10.1007/978-3-662-28603-6_43
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