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Pegmatites, uranium deposits

Intrusive Deposits. Deposits included in the intmsive deposit type are those associated with intmsive or anatectic rocks of different chemical composition, eg, alaskite, granite, monzonite, peralkaline syenite, carbonatite, and pegmatite. Examples include the uranium occurrences in the porphyry copper deposits such as Bingham Canyon and Twin Butte in the United States, the Rossing Deposit in Namibia, and Ilimaussaq deposit in Greenland, Palabora in South Africa, and the deposits in the Bancroft area, Canada (15). [Pg.184]

Brannerite is the third most important reduced uranium mineral in that it occurs in many different types of deposits and is the chief uranium producer in the conglomerates of Blind River-Elliot Lake, Ontario, Canada. Although it has been found in pegmatites, hydrothermal and sedimentary deposits, it is always associated with uraninite and probably forms through reactions with uraninite and titanium phases that are also present. [Pg.47]


See other pages where Pegmatites, uranium deposits is mentioned: [Pg.93]    [Pg.98]    [Pg.93]    [Pg.98]    [Pg.314]    [Pg.461]    [Pg.314]    [Pg.499]    [Pg.356]    [Pg.56]    [Pg.89]    [Pg.89]    [Pg.94]    [Pg.98]    [Pg.124]    [Pg.313]    [Pg.44]    [Pg.72]    [Pg.313]    [Pg.1690]    [Pg.2820]    [Pg.600]    [Pg.498]    [Pg.2656]    [Pg.43]    [Pg.48]    [Pg.91]    [Pg.97]    [Pg.122]    [Pg.122]    [Pg.122]    [Pg.123]    [Pg.124]    [Pg.176]    [Pg.300]    [Pg.378]   
See also in sourсe #XX -- [ Pg.43 , Pg.47 , Pg.48 , Pg.55 , Pg.59 , Pg.91 , Pg.94 , Pg.96 , Pg.98 , Pg.123 ]




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