作者: A. ISSAR , E. ROSENTHAL , Y. ECKSTEIN , R. BOGOCH
DOI: 10.1080/02626667109493772
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摘要: Abstract The chemical composition of formation waters tapped in oil wells and emerging as hot springs along the Suez coast Sinai was examined. A scheme is proposed for geochemical evolution these their relation to geological history area. thermal regime investigated area characterized by high gradient foci located immediate proximity major faults. Fe—mineralization, dolomitization concentrations heavy metals were observed on eastern shore Gulf Suez. have equivalent ionic ratios similar those brines found three Deeps Red Sea (Degens Ross, 1969). mineralization phenomena also show a resemblance Deeps.