Abstract:The thermal fluids vented over Eskisehir province have been investigated for their origin and to estimate the geothermal potential of the area. Thermal waters as well as bubbling and dissolved gases were collected and analysed for their chemical and isotopic features. Their isotopic composition varies in the range from -11.5 to -7.7 ‰ for δO, -84 and -57 ‰ for δH, and 0-7.2 TU for tritium. The gases (bubbling and dissolved) are mostly N-dominated with a significant amount of CO. The helium isotopic ratios are … Show more
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