Sulfate in plagiogranites from the Troodos ophiolite, Cyprus.

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  • Kawahata Hodaka
    Marine Geology Department, Geological Survey of Japan and Graduate School of Science, Tohoku University
  • Kusakabe Minoru
    Institute for study of the Earth Interior, Okayama University
  • Scott Steven D.
    Department of Geology, University of Tronto

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  • Sulfate in plagiogranites from the Troo

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Plagiogranites occur locally in the interface between the sheeted dike complex and the uppermost level of gabbros, containing a high proportion of sulfate with a δ34S value of 13.0‰ on average. Strontium and sulfur isotopic compositions of the plagiogranites suggest that magmatic or magmatic-hydrothermal sulfate constitutes the major fraction of the sulfate in the plagiogranites with high δ34S values and that seawater-derived Sr might have been incorporated in the latest stage of crystallization.

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