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Shinkolobwe mine

Uraninite, or pitchblende as it is more commonly known, is the form in which uranium was first discovered, at Joachimsthal, Czechoslovakia. Later, very rich deposits of massive uraninite were discovered at the Shinkolobwe mine in the Belgian Congo (Zaire) and were the principal source of uranium for the Manhattan Project. Leaner ores containing finely divided... [Pg.232]

An example of veins with complex mineralogy is the mined-out uranium deposit at Shinkolobwe, Zaire, at the northwest end of the African Copperbelt. It occurs in a faulted transported fold in metamorphosed dolomitic shales of the middle Proterozoic Mine Series of the Roan Group.Uraninite and uranophane mineralization (about 620m.y. ago) was followed by several later mineralizations in which pyrite, molybdenite, monazite, selenium, Co-Ni sulphides and selenides and copper minerals were formed. It is believed that this orebody was formed by redistribution of metals originally deposited in marine sedimentary rocks." The uranium, originally weathered from granites and deposited in the marine sediments, was in low... [Pg.133]


See other pages where Shinkolobwe mine is mentioned: [Pg.427]    [Pg.500]    [Pg.123]    [Pg.33]    [Pg.305]    [Pg.427]    [Pg.500]    [Pg.123]    [Pg.33]    [Pg.305]    [Pg.249]    [Pg.309]   
See also in sourсe #XX -- [ Pg.305 , Pg.309 ]




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