| Article ID | Journal | Published Year | Pages | File Type |
|---|---|---|---|---|
| 5478701 | Geothermics | 2017 | 19 Pages |
Abstract
Hydrogeochemical properties of the field show that surface temperature of fluid ranges from 30 to 34 °C. Geothermal fluids in Gülbahçe have high salinity (EC > 34 mS/cm) and low enthalpy. Piper and Schoeller diagrams indicate that geothermal fluid is in the NaCl facies. Chemical geothermometers suggest that the reservoir temperature is around 53-136 °C. The isotopic data (oxygen-18, deuterium and tritium) suggest that geothermal fluids are formed by local recharge and deep circulation of sea water.
Keywords
Related Topics
Physical Sciences and Engineering
Earth and Planetary Sciences
Geochemistry and Petrology
Authors
Taygun Uzelli, Alper Baba, Gamze Gül Mungan, R. Kadir Dirik, Hasan Sözbilir,