Baturin, Gleb N; Kochenov, A V; Trimonis, Egidius S (1969): Chemical composition of bottom sediments from the Discovery Deep, Red Sea rift zone. PANGAEA, https://doi.org/10.1594/PANGAEA.753310, Supplement to: Baturin, GN et al. (1969): Composition and origin of iron-ore sediments and hot brines in the Red Sea. Oceanology, 9, 360-368
Always quote above citation when using data! You can download the citation in several formats below.
Hot brines in depressions of the central Red Sea contain thousands of times more iron, manganese and other metals than . After removal of salts, approximately half of sediments from these depressions consists of iron hydroxides and they are enriched in zinc, copper, lead and molybdenum. Hydrothermal deposits with the same complex of metals, located along the coast of the Red Sea, are correlated with faults and may be due to occurrences of Tertiary volcanism. Brines of similar composition are known in the Cheleken Peninsula. Certain geological and geochemical data indicate that such brines are of relatively deep origin.
Latitude: 21.000000 * Longitude: 38.000000