Evidence for episodic hydrothermal activity in the Red Sea from the composition and formation of hydrothermal sediments, Thetis Deep
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Cited by (17)
Chemical characteristics of modern deep-sea metalliferous sediments in closed versus open basins, with emphasis on rare-earth elements and Nd isotopes
2021, Earth-Science ReviewsCitation Excerpt :To our knowledge, no REE data have been reported as yet for the sediments of the Bannock, Tyro and Urania Basins. In the Thetis Deep of the Red Sea (location in Fig. 1a), up to several metres of Mn-oxide-rich or Fe-oxyhydroxide-rich sediments are present (Bignell et al., 1976; Scholten et al., 1991). In core 1037, the upper 1 m of metalliferous sediments, which consists mainly of Fe-oxyhydroxides, has strong positive Eu anomalies (Butuzova and Lyapunov, 1995; Pierret et al., 2010).
Comment on "Formation of Thetis Deep metal-rich sediments in the absence of brines, Red Sea" by Pierret et al. (2010)
2011, Journal of Geochemical ExplorationReply to the comment of Mitchell et al. (2010) on "Formation of Thetis Deep metal-rich sediments in the absence of brines, Red Sea" by Pierret et al. (2010)
2011, Journal of Geochemical ExplorationFormation of Thetis Deep metal-rich sediments in the absence of brines, Red Sea
2010, Journal of Geochemical ExplorationIsotopic indicators of deformation in the Red Sea
2006, Journal of Structural GeologyChemical and isotopic (<inf>87</inf>Sr/<inf>86</inf>Sr, δD) contraints to the formation processes of red-sea brimes
2001, Geochimica et Cosmochimica Acta
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