[en] The study area is located at southwest part of Konya (Central Anatolia). The basement formation of the area is Caltepe, deposited from Early Cambrian through Middle Cambrian. Seydisehir Formation which is composed of alternating slate, sandstone and metasandstone overlies conformably the overthrown Caltepe Formation and is Upper Cambrian-Lower Ordovician in age. Seydisehir Formation is conformably underlined by Tarasci Limestone, Neogene in age. Alluvium is Quaternary-Present in age. The hot and mineralized waters are located in the study area around Ilicatepe and Kavakkoy village having temperature range between 31 deg. C and 46 deg. C, flow rate between 1.42 and 5.0 L/s and total dissolved solids between 2,218-3,500 mg/L. Aquifers of these waters are the porous limestone and dolomitic limestone of the Caltepe Formation. The travertine cones occur as a result of water activity. The groundwaters are classified according to the AIH standards are Ca, Na, HCO₃, and B bearing hot and mineralized water. The oxygen and hydrogen isotope compositions of geothermal waters reveal meteoric origin. They have more negative δ¹⁸O and δ²H values and lower ³H contents compared to cold waters. The geothermal water aquifers are recharged from higher altitudes and they are hardly affected by recent precipitations. (author)

[en] Konya has important potential amound of hot and mineral waters in Inner Anatolia Region. Hot springs surrounding Konya are located in nort at Cihanbeyli region and in east at Karapinar-Eregli region and in west at Beysehir-Seydisehir-Ilgin region. Each thermal spring has geological, hydrogeological and physicochemical properties differs from another. Hot and mineral waters around Cihanbeyli have temperature range from 17,5 to 29 degrees, their discharge is 1,2 lt/sn. Total mineralisation of these springs range from 4587 to 5139,5 mg/lt. Thermal springs around Karapynar- Ereoli region have temperature between 18-28 degree, discharge between 0,45-2 lt/sn and total mineralisation between 5207-35449 mg/lt. The temperatures and discharges of hot and mineral waters of Beypehir-Seydisehir-Ilgin region are suitable for thermal tourism. They are important geothermal resources in Konya. The water temperature range from 27 to 41degrees, discharge range from 15 to 50 lt/sn and classified as low mineralised. Aquifers of these springs are Paleosoic marbles and their characteristics have been controlled by fault dynamics. The thermal waters of nort-Konya are classified as 'F-Na-HCO₃ hot and mineral waters'according to AIH. The thermal water of Karapynar is classified as 'S-Na-HCO₃ hot and mineral water', and the water of Eregli is classified as 'I-F-Na-Cl hot and mineral water'. Chemical properties of the thermal waters of west-Konya are ^Aquatherm^. The whole thermal waters classified according to Piper diagramme; the northest grouped in region 6, the eastern grouped in region 7, the western grouped in regions 5, 6, 9. The thermal waters have 'Rav waters' properties according to Giggenbach diagramme. The reservuar rock temperature is calculated due to geothermometers as 250 degrees, and water depths are ranging from 500 to 1000 m. The waters heating from volcanism and geothermal gradient. It is necassary to increase the thermal waters temperatures and discharges with drillings to use in thermal tourism. The springs should have been prevented from contamination by applying conservation zones surroundings them

[en] The study area is located at southwest part of Konya (Central Anatolia). The basement formation of the area is Caltepe, deposited from Early Cambrian through Middle Cambrian. Seydisehir Formation which is composed of alternating slate, sandstone and metasandstone overlies conformably the overthrown Caltepe Formation and is Upper Cambrian-Lower Ordovician in age. Seydisehir Formation is conformably underlined by Neocene in age Tarasci Limestone. Alluvium is Quaternary-Present in age. The hot and mineralized waters located in the study area around Ilicatepe and Kavakkoy villages have a temperature range between 31 deg. C and 46 deg. C, flow rate between 1.42 and 5 L/s and a total dissolved mineral between 2218-3500 mg/L. Aquifer of these waters are the porous limestone and dolomitic limestone of the Qaltepe formation. The travertine cones occur as a result of water activity. The waters classified according to the AIH standards are Ca, Na, HCO₃, and B bearing hot and mineralized water. The oxygen and hydrogen isotope compositions of geothermal waters reveal meteoric origin. They have more negative δ¹⁸O and δ²H values, and lower ³H contents compared to cold waters. The geothermal water aquifers are recharged from higher altitudes and are hardly affected by recent precipitations. (author)

[en] Konya region (Turkey) has three important geothermal subregion. These are Cihanbeyli, Beysehir-Seydisehir-Ilgin and Ismil-Eregli subregions. Geothermal waters in the region have temperature between 19.8-51 deg. C, discharge between 0.1-130 L/s and total mineralization range from 852 to 5110 mg/L. The isotopic analysis evaluated according to ¹⁸O/²H, ¹⁸O/TU, Cl/TU, pH/EC and Giggenbach diagrams. The geothermal water aquifers are recharged from higher altitudes and they are hardly affected by recent precipitations and these waters reveal meteoric origin. They have more negative δ¹⁸O and δ²H values and lower ³H contents compared to cold waters. The reservoir rock temperature is 250 deg. C, and water depths are ranging from 500 to 1000 m. The waters are heated from volcanism and geothermal gradient. (author)

[en] Konya region (Turkey) has three important geothermal subregion. These are Cihanbeyli, Beysehir-Seydisehir-Ilgin and Ismil-Eregli subregions. Geothermal waters in the region have temperature between 19.8-51 deg. C, discharge between 0.1-130 L/s and total mineralization range from 852 to 5110 mg/L. The isotopic analysis evaluated according to ¹⁸O/²H, ¹⁸O/TU, Cl/TU, pH/EC and Giggenbach diagrams. The geothermal water aquifers are recharged from higher altitudes and they are hardly affected by recent precipitations and these waters reveal meteoric origin. They have more negative δ¹⁸O and δ²H values and lower ³H contents compared to cold waters. The reservoir rock temperature is 250 deg. C, and water depths are ranging from 500 to 1000 m. The waters heat from volcanism and geothermal gradient. (author)