Research paperStable isotope study of water, gypsum and carbonate samples from the Bannock and Tyro Basins, eastern Mediterranean
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Cited by (12)
Formation of secondary carbonates and native sulphur in sulphate-rich Messinian strata, Sicily
2010, Sedimentary GeologyFluid-sediment interactions at Eastern Mediterranean mud volcanoes: A stable isotope study from ODP Leg 160
2003, Earth and Planetary Science LettersCitation Excerpt :Whereas the simple dissolution of chloride salts by any unsaturated solution would increase the Cl concentration but leave the isotopic values unchanged, a possible contribution of residual brines is expected to cause an enrichment in both 18O and D [17] (Table 2). However, the observed δD values are depleted and a δ18O value of about 2‰ for relict Mediterranean brines [18] is too close to the background value of 1.6‰ for Mediterranean seawater [19] to alter the isotopic composition significantly. Several sedimentary components have δ18O and δD values that differ significantly from the pore water composition and may, therefore, alter its isotopic composition by diagenetic reactions.
The diffusive regime of double-diffusive convection
2003, Progress in OceanographyRelics of evaporated sea water in deep basins of the Eastern Mediterranean
1993, Marine Geology
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