Geochemical signature of the Kizildere geothermal field, western Anatolia, Turkey
INTERNATIONAL GEOLOGY REVIEW, cilt.44, sa.2, ss.153-163, 2002 (SCI-Expanded, Scopus)
- Yayın Türü: Makale / Tam Makale
- Cilt numarası: 44 Sayı: 2
- Basım Tarihi: 2002
- Doi Numarası: 10.2747/0020-6814.44.2.153
- Dergi Adı: INTERNATIONAL GEOLOGY REVIEW
- Derginin Tarandığı İndeksler: Science Citation Index Expanded (SCI-EXPANDED), Scopus
- Sayfa Sayıları: ss.153-163
- Süleyman Demirel Üniversitesi Adresli: Evet
Özet
The Kizildere thermal waters are located in the northern part of the Buyuk Menderes rift zone. The Paleozoic metamorphic rocks form the basement of the studied area and are discordantly overlain by Pliocene elastic sediments. The thermal waters are associated with NE-SW- and NW-SE-oriented faults, representing a compressional event that followed extensional formation of the rift zone. The hydrothermal alteration includes phyllic, argillic, silicic, hematitized, and carbonatized alteration zones.