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https://hdl.handle.net/11499/39596| Title: | Hydrogeochemical investigation of ortakci hot and mineralized spring (Buharkent-Aydın) | Other Titles: | Ortakçı (Buharkent-Aydın) sıcak ve mineralli su kaynağının hidrojeokimyasal incelemesi | Authors: | Kaya, M Gokgoz, A |
Keywords: | Water chemistry; Chemical equilibrium; Geothermometer | Publisher: | PAMUKKALE UNIV | Abstract: | The temperature and discharge of the Ortakci hot and mineralized water are 48.1 degrees C and 2.4 l/s, respectively. The spring has being formed as a result of ascending geothermal fluid due to the tectonic activity of the region. The geothermal fluid within joints has not been reached to chemical equilibrium with host rock which consists of gneiss, quartzite and schist. Ortakci thermal water is the type of Na-SO4-HCO3 and subsurface temperature calculated using chemical geothermometers is about 80 degrees C. | URI: | https://hdl.handle.net/11499/39596 | ISSN: | 1300-7009 |
| Appears in Collections: | Mühendislik Fakültesi Koleksiyonu TR Dizin İndeksli Yayınlar Koleksiyonu / TR Dizin Indexed Publications Collection WoS İndeksli Yayınlar Koleksiyonu / WoS Indexed Publications Collection |
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| File | Size | Format | |
|---|---|---|---|
| ff148402-2ef7-49ca-b146-5f7aa53e95b9.pdf | 570.31 kB | Adobe PDF | View/Open |
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