Constraints on the Origin of the Balıkesir Thermal Waters (Turkey) from Stable Isotope (\delta^{18}O, \deltaD, \delta^{13}C, \delta^{34}S) and Major-Trace Element Compositions

Turkish Journal of Earth Sciences

HALİM MUTLU¹ 

关键词: water-rock interaction;    stable isotope compositions;    major-trace element geochemistry;    Balıkesir thermal waters;    Turkey;   

学科分类：地球科学(综合)

来源: Scientific and Technical Research Council of Turkey - TUBITAK

【 摘 要 】

The Balıkesir thermal waters in northwestern Turkey have discharge temperatures in the range of 31.8-98.5 ºC, near neutral pH values of 6.40 to 8.40 and TDS contents between 327 and 2578 mg/l. Samples display variable chemical compositions changing from high-temperature Na_2SO_4-NaHCO_3 waters to warmer CaHCO_3 waters. Trace element concentrations of the waters show significant variation. Comparison between the concentrations of alkaline earth metals in waters and carbonate deposits reveals mobile behavior for Mg and Ba. The ratio of strontium to calcium concentrations in solid and liquid phases was found to be almost the same. Li/Cs and B/Cl ratios of waters and carbonates are similar suggesting the operation of a simple rock leaching process. Mineral equilibrium calculations imply that the CO_2 concentration has a great effect on the chemistry of the thermal waters and that most fluid compositions are controlled by rock dissolution rather than equilibration. The chemical geothermometers applied to the Balıkesir thermal waters yield a maximum reservoir temperature of 200 °C. The \delta^{18}O-\deltaD compositions clearly indicate a meteoric origin for the waters. \delta^{34}S contents of sulfate in thermal waters range from -5.5 to +25.2%o. Sulfur isotope compositions of some waters correspond to those of non-marine evaporates while sulfur in others is derived from sulfate reduction. The \delta^{13}C ratio for dissolved inorganic carbonate in the waters lies between -17.7 and +0.7%o. There are also multiple sources of carbon. In high-temperature waters carbon is thought to originate from the dissolution of marine carbonates, an interpretation supported by carbon isotope compositions of marine carbonate rocks in the region. Carbon in low-temperature waters is derived from an organic source.

【 授权许可】

Unknown