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This study illustrates the origin of Quaternary brines and groundwater salinization processes at Laizhou Bay using hydrochemical and δ2H, δ18O, δ11B and δ37Cl data. The characteristics of the major ionic components of these brines demonstrated that brines originated from evaporated seawater. The δ2H and δ18O values of brines showed that seawater underwent strong evaporation and that these brines underwent...
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