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Hot Brines and Recent Heavy Metal Deposits in the Red Sea pp 474–498Cite as

Sulfur Isotope Studies on Red Sea Geothermal Brines and Sediments

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Abstract

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 to +15 per mill, (3) +12 to +2 per mill, (4) <−25 per mill. Sulfate in the brine appears to have been derived from marine evaporites, whereas sulfide originates from two sources. In the Atlantis II Deep, it is derived from a hydrothermal process and introduced with the brine. In the other areas, biological sulfate reduction produces sulfide which precipitates metals from the brine originating in the Atlantis II Deep.

Contribution No. 680, Institute of Geophysics and Planetary Physics.

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Authors and Affiliations

  1. Department of Geology and Institute of Geophysics and Planetary Physics, University of California, Los Angeles, USA

    I. R. Kaplan, R. E. Sweeney & Arie Nissenbaum

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  1. I. R. Kaplan
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  2. R. E. Sweeney
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  3. Arie Nissenbaum
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Editors and Affiliations

  1. Department of Chemistry, Woods Hole Oceanographic Institution, Woods Hole, Massachusetts, USA

    Egon T. Degens

  2. Department of Geology and Geophysics, Woods Hole Oceanographic Institution, Woods Hole, Massachusetts, USA

    David A. Ross

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Kaplan, I.R., Sweeney, R.E., Nissenbaum, A. (1969). Sulfur Isotope Studies on Red Sea Geothermal Brines and Sediments. In: Degens, E.T., Ross, D.A. (eds) Hot Brines and Recent Heavy Metal Deposits in the Red Sea. Springer, Berlin, Heidelberg. https://doi.org/10.1007/978-3-662-28603-6_43

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  • DOI: https://doi.org/10.1007/978-3-662-28603-6_43

  • Publisher Name: Springer, Berlin, Heidelberg

  • Print ISBN: 978-3-662-27120-9

  • Online ISBN: 978-3-662-28603-6

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