Page 60 - Introduction to Mineral Exploration
P. 60

3: MINERAL DEPOSIT GEOLOGY AND MODELS  43


                 TABLE 3.1 (continued)

                 Element             Cox & Singer                    Eckstrand
                 Texture and structure  Breccias, veins, and disseminations.
                                     Uranium minerals coarse and
                                     colloform. Latest veins have open
                                     space filling textures
                 Alteration          Multistage chloritization dominant.
                                     Local sercitization, hematization,
                                     kaolinization, and dolomitization.
                                     Vein silicification in alteration
                                     envelope. Alteration enriched in
                                     Mg, F, REE, and various metals.
                                     Alkalis depleted
                 Ore controls        Fracture porosity controlled ore  1 At or near unconformity between
                                     distribution in metamorphics.   Helikian sandstone and Archaean
                                     Unconformity acted as disruption in  basement
                                     fluid flow but not necessarily ore locus  2 Intersection of unconformity with
                                                                     reactivated basement faults
                                                                     3 Associated with graphitic basement
                                                                     rocks and gray and/or multicolored shale
                                                                     and sandstone cover
                                                                     4 Intense clay, chlorite, and sericite
                                                                     alteration of basement and cover rocks
                                                                     5 Basement rocks with higher than
                                                                     average U content
                 Weathering          Various secondary U minerals
                 Geochemical and     Increase in U, Mg, P, and locally Ni,
                 geophysical         Cu, Pb, Zn, Co, As; decrease in SiO 2 .
                 Signature (Cox &    Locally Au with Ag, Te, Ni, Pd, Re,
                 Singer)             Mo, Hg, REE, and Rb. Anomalous
                                     radioactivity. Graphitic schists in
                                     some deposits are strong EM
                                     conductors
                 Genetic model                                       Combinations of:
                                                                     1 Preconcentration of U during deposition
                                                                     of Aphebian sediments and their anatexis
                                                                     2 Concentration in lateritic regolith
                                                                     (Helikian)
                                                                     3 Mobilization by heated oxidized
                                                                     solutions and precipitation in reducing
                                                                     environment at unconformity and fault
                                                                     locus
                                                                     4 Additional cycles of mobilization and
                                                                     precipitation leading to redistribution of
                                                                     uranium
                 Examples            Rabbit Lake, Saskatchewan Cluff  Key Lake, Rabbit Lake, Cluff Lake,
                                     Lake Saskatchewan               Canada. Jabiluka I and II, Ranger, N.T.,
                                                                     Australia
                 Importance                                          Canada: 35% of current U production but
                                                                     50% of reserves
                                                                     World: 15% of reserves
                 Typical grade       see Fig. 3.12                   Canada: small to 5 Mt of 0.3–3% U.
                 and tonnage                                         Australia: maximum 200,000 t of
                                                                     contained U but grade lower than Canada
   55   56   57   58   59   60   61   62   63   64   65