Sulfate in plagiogranites from the Troodos ophiolite, Cyprus
Hodaka Kawahata, Minoru Kusakabe, Steven D. Scott
Geochemical Journal, Vol. 31, No. 2, P. 119-124, 1997
ABSTRACT
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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