Published January 1, 2018
| Version v1
Journal article
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Origin, evolution and geothermometry of the thermal waters in the Golemezli Geothermal Field, Denizli Basin (SW Anatolia, Turkey)
Creators
- 1. Pamukkale Univ, Dept Geol Engn, TR-20070 Denizli, Turkey
- 2. Univ Bari, Dept Earth & Geoenvironm Sci, I-70125 Bari, Italy
- 3. CNR, IGG, Inst Geosci & Earth Resources, Via G La Pira 4, I-50121 Florence, Italy
- 4. Univ Perugia, Dept Phys & Geol, I-06123 Perugia, Italy
- 5. Univ Siena, Dept Phys Earth & Environm Sci, I-53100 Siena, Italy
- 6. Nat Sources & Cultural Heritage Directorate, Denizli Governorship, TR-20070 Denizli, Turkey
Description
The Golemezli Geothermal Field (GGF) is one of the best known geothermal fields in western Anatolia (Turkey). The exploited fluids are of meteoric origin, mixed with deep magmatic fluids, which interacted with the metamorphic rocks of the Menderes Massif. The geothermal fluids are channeled along Quaternary faults belonging to the main normal faults system delimiting the northern side of the Denizli Basin and their associated transfer zones. In this study, hydrochemical and isotopic analyses of the thermal and cold waters allow us to determine water-rock interactions, fluid paths and mixing processes.
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