Saline waters and residual brines in the Shiraz-Sarvistan basin,Iran |
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| Authors: | I Zak JR Gat |
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| Institution: | 1. Department of Geology, The Hebrew University, Jerusalem Israel;2. Isotope Department, Weizmann Institute of Science, Rehovot Israel |
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| Abstract: | Origin of saline waters in the Shiraz-Sarvistan area, Iran, is determined by a combined isotopic (18O and D) and chemical characterization. Four types are recognized: (a) fresh water of the anticlinal carbonatic aquifer; (b) fresh and brackish runoff in the synclinal basins; (c) salt springs originating through dissolution of rock salt by type (a) fresh water; and (d) residual brines formed in synclinal closed drainage basins, through evaporation of former water types and loss of the relatively less-soluble salts. |
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