Abstract
Uranium deposits have been identified in the Kyzylkum region in central Uzbekistan and the Karamazar region in eastern Uzbekistan (> Fig. 7.1). The former contains sandstone-type U mineralization in sedimentary basins as well as carbonaceous (or black) shale-related stockwork-type mineralization in basement uplifts. Volcanic vein-stockwork-type deposits are typical for the Karamazar region.
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Aleksandrov 1922; Barsukov et al. 1972; Vlasov et al. 1966; Volfson (chief ed) 1978; Bain 1950; Boitsov AV pers. commun.; Chervinsky 1925; Fazlullin et al. 2002; Fersman 1927, 1930; Gorlov et al. 2005; IAEA 1995, 2007; Ischukova et al. 2002; Karimov et al. 1996; Kazansky 1955, 1970; Kazansky and Laverov 1977; Kislyakov and Shchetochkin 2000; Kohl 1954; Komischau 1927; Kotlyar 1968; Kuchersky 1997; Laverov 1972; Laverov et al. 1985, 1992a–c, 1993; Mashkovtsev et al. 1979; Mashkovtsev and Naumov 1999; Melnikov et al. 1996; Minerals Yearbook 1946, 1949; OECD-NEA/IAEA 1993–2005; Perevozchikov 2000; Shcherbakov 1924; Shchetochkin and Kislyakov 1993; Shimkin 1949; Smorchkov 1966; Venatovsky 1993.
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Dahlkamp, F.J. (2009). Uzbekistan. In: Dahlkamp, F.J. (eds) Uranium Deposits of the World. Springer, Berlin, Heidelberg. https://doi.org/10.1007/978-3-540-78558-3_15
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DOI: https://doi.org/10.1007/978-3-540-78558-3_15
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