Hydrogeological and isotopic survey of geothermal fields in the Buyuk Menderes graben, Turkey

✍ Scribed by Sakir Simsek

• Publisher: Elsevier Science
• Year: 2003
• Tongue: English
• Weight: 309 KB
• Volume: 32
• Category: Article
• ISSN: 0375-6505
• DOI: 10.1016/s0375-6505(03)00072-5

✦ Synopsis

The main high and low enthalpy geothermal fields in the Buyuk Menderes graben (Western Anatolia) and their reservoir temperatures are as follows: Kizildere (242 C), Germencik (232 C), Aydin-Ilicabasi (101 C), Yılmazkoy (142 C), Salavatli (171 C), Soke (26 C), Denizli -Pamukkale (36 C), Karahayit (59 C), Golemezli (101 C) and Yenice (70 C). The geothermal systems are controlled by active graben faults. The reservoir rocks in the geothermal fields are the limestone and conglomerate units within Neogene sediments and the marble-quartzite units within Paleozoic metamorphic formations. There are clear 18 O shifts from the Mediterranean Meteoric Water Line (MMWL) in the Kizildere, Germencik and Aydin fields, where a good relation between high temperatures and 18 O shift has also been observed, indicating deep circulation and water rock interactions. In the Pamukkale, Karahayit, Golemezli and Yenice fields and in Soke region, low temperatures, small isotope shifts, shallow circulations and mixing with shallow cold water have been noted.