Origin of Miocene halite from Tuz Golu basin in Central Anatolia, Turkey: Evidences from the pure halite and fluid inclusion geochemistry

Karakaya, Muazzez; Bozdag, Ayla; Ercan, Hatice; Karakaya, Necati; Delikan, Arif

doi:10.1016/j.gexplo.2019.03.004

Origin of Miocene halite from Tuz Golu basin in Central Anatolia, Turkey: Evidences from the pure halite and fluid inclusion geochemistry

Atıf İçin Kopyala

Karakaya M. C., Bozdag A., Ercan H. U., Karakaya N., Delikan A.

JOURNAL OF GEOCHEMICAL EXPLORATION, cilt.202, ss.1-12, 2019 (SCI-Expanded)

Yayın Türü: Makale / Tam Makale
Cilt numarası: 202
Basım Tarihi: 2019
Doi Numarası: 10.1016/j.gexplo.2019.03.004
Dergi Adı: JOURNAL OF GEOCHEMICAL EXPLORATION
Derginin Tarandığı İndeksler: Science Citation Index Expanded (SCI-EXPANDED), Scopus
Sayfa Sayıları: ss.1-12
İstanbul Teknik Üniversitesi Adresli: Hayır

Özet

The study area is located in the south of Konya Closed Basin which is the largest Miocene inner basin in Central Anatolia. The aim of this study is to determine the chemical composition of the Miocene halite deposits and depositional environments of Tuz Golu lacustrine basin. For this scope, fluid inclusion analyses (K+, Mg2+, SO42-) of nine pure halites were performed and twenty six pure halite samples have been examined. Additionally, K+, Mg2+, SO42- ion concentrations of the fluid inclusions and pure halite samples were compared to Gulf of Suez (GS), Red Sea (RS) and other Cenozoic seawaters (CS).