Helium and carbon isotope composition of gas discharges in the Simav Geothermal Field, Turkey: Implications for the heat source

• 3He/4He and CO2/3He ratios of fluids in the Simav geothermal field were reported.
• Mantle He contributions were calculated up to 19.4% in the total helium contents.
• Mantle derived CO2 contributions were calculated up to 32%.
• 3He/enthalpy ratios were computed between 0.016 and 0.275 × 10−12 cm3 STP/J.
• The maximum magmatic heat contribution in the field has been estimated as ∼55%.

Helium and 13C(CO2) isotope compositions of gas discharges are used in conjunction with 3He/enthalpy ratios to identify major heat sources of the Simav Geothermal Field, located on one of the major active graben system in western Anatolia (Turkey). The air-corrected 3He/4He ratios, δ13C(CO2) values, and CO2/3He ratios of gas samples collected at the wellheads range from 1.36 RA to 1.57 RA (where RA is the atmospheric 3He/4He ratio), −1.47‰ VPDB to −4.01‰ VPDB, and 4.66 × 109 to 11.4 × 109, respectively. The air-corrected helium ratios indicate a dominant crustal source for helium with significant mantle-derived helium contributions (up to 19.4%) to the total helium contents. Additionally, the combined CO2/3He ratios and δ13C (CO2) values reveal that while the principal CO2 contribution was from decomposition of marine carbonates, mantle-derived CO2 contributions to the total CO2 contents of the geothermal fluids can reach up to ∼32%. The 3He/enthalpy ratios were calculated in range from 0.016 × 10−12 cm3 STP/J to 0.275 × 10−12 cm3 STP/J, and are generally comparable to the theoretical 3He/heat production ratio of the upper mantle. On the basis of 3He/enthalpy ratios, the maximum magmatic heat contribution in the field was estimated as ∼55% which is consistent with the average surface heat flow estimates for western Anatolia implying that at least half of the heat input to the overall heat budget of the Simav Geothermal System originating from a magmatic source. Finally, because there is no evidence of any active or recent volcanism in the region, mantle volatiles and magmatic heat contribution were attributed to the extension-related mantle melt generation providing mantle heat and volatile input beneath the crust.