2019
DOI: 10.1016/j.gexplo.2019.03.004
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Origin of Miocene halite from Tuz Gölü basin in Central Anatolia, Turkey: Evidences from the pure halite and fluid inclusion geochemistry

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Cited by 7 publications
(1 citation statement)
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“…Tuz Lake constitutes the Main Zone (a water body with a depth of about 70 cm in the spring) and a separate area of the lake, designated as the Deep Zone (a water body with a depth exceeding 100 cm in the spring), is found in the mid-east part of the main area of the lake [ 20 , 21 ]. In addition, on the shore of Tuz Lake, there are several salterns that are the major source for salt production in Turkey, estimated to meet 70% of the salt needs of this country [ 22 , 23 ]. Kayacik saltern, Kaldirim saltern, and Yavsan saltern are located in the mid-east, north-east, and western parts of the lake, respectively ( Figure 1 ).…”
Section: Introductionmentioning
confidence: 99%
“…Tuz Lake constitutes the Main Zone (a water body with a depth of about 70 cm in the spring) and a separate area of the lake, designated as the Deep Zone (a water body with a depth exceeding 100 cm in the spring), is found in the mid-east part of the main area of the lake [ 20 , 21 ]. In addition, on the shore of Tuz Lake, there are several salterns that are the major source for salt production in Turkey, estimated to meet 70% of the salt needs of this country [ 22 , 23 ]. Kayacik saltern, Kaldirim saltern, and Yavsan saltern are located in the mid-east, north-east, and western parts of the lake, respectively ( Figure 1 ).…”
Section: Introductionmentioning
confidence: 99%