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Sulphur, sulphate oxygen and strontium isotopic composition of Cenozoic Turkish evaporates

Palmer, Martin R., Helvaci, Cahit and Fallick, Anthony E. (2004) Sulphur, sulphate oxygen and strontium isotopic composition of Cenozoic Turkish evaporates Chemical Geology, 209, (3-4), pp. 341-356. (doi:10.1016/j.chemgeo.2004.06.027).

Record type: Article


Sulphur (?34S) and strontium isotope (87Sr/86Sr) ratios have been measured in 37 sulphate minerals (gypsum, celestite and thenardite) and 4 sulphide samples (?34S only) from 9 Cenozoic marine and nonmarine evaporites located in Anatolia, Turkey. Oxygen isotope (?18Osulphate) ratios were also measured in 25 gypsum and 1 anhydrite sample from these deposits. These data have been used to determine the origin of dissolved sulphate in the brines that precipitated these minerals. They show that seawater was the dominant source of sulphate and Sr in the marine evaporites, but that perturbations from contemporaneous seawater Sr and sulphur isotope compositions result from recycling of older evaporites and sulphate reduction. Although continental geothermal fluids played an important role in supplying the dissolved salts that formed the nonmarine evaporites, the ?18Osulphate, ?34S and Sr isotope compositions of many of these nonmarine evaporites are indistinguishable from the marine evaporites. As well as suggesting that recycling of marine evaporites was important for controlling the composition of the nonmarine evaporites, it also suggests that ?18Osulphate, ?34S and Sr isotope compositions are not unequivocal tracers in distinguishing between these two types of evaporite. For the Turkish evaporites considered here, the major difference between marine and nonmarine evaporites that contain similar ?34S–?18Osulphate–87Sr/86Sr relationships is that the latter contain high concentrations of boron that reflect a geothermal contribution to the deposits.

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Published date: 27 September 2004
Keywords: turkey, evaporites, strontium, oxygen, sulphur isotopes


Local EPrints ID: 12713
ISSN: 0009-2541
PURE UUID: 1fb72e51-c29b-4983-ae44-e300e73d0e8f

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Date deposited: 02 Dec 2004
Last modified: 17 Jul 2017 17:02

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Author: Cahit Helvaci
Author: Anthony E. Fallick

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