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•  ••  •  •• •• •••• ••• •• ••• •• •••  IntroductIon    Study Area •• •••• • ••• ••  • •••  • •••  •••• •• ••• •••• Water GeOChl!l:llstry  ••    ••••   ••• Mlnenl-Solutlon Equl1lbrh • •• ••• •••• • • •• ••• • .••••  The Use of Pathffnder Eleaents Relate': to the Results of MInerai-Solut ion EquilIbria Approach •••.• •••.  ConclusIons  •  • •• • • •   ..   • •   •• References Cited • •••• • •• •    •  •• ••• • •••• • ••• •• •••• Figure 11 lustratlons l . --Index ... p showIng locatIon of the Beayer basin. Utah • •• ••  Z.--Dlstrlbutlon of uranlta In waters frem the Beayer basIn. Utah ••  • ••  •••• •••• •• • ••• • •••• •• •• •• ••• • 3. --Dfstrlbutlon of calculated redox potential (Ch) of waters frOll the BeaYer basIn. Utah •• •  •• • •• •••• •••• • • ••• 4. · Dfstrlbutlon of satuatlon Indexes for ur.nlnlte of waters fl"OOll the Beaver basin, Utah • • • ••  ••••  ••• 5.--Dfstrlbutlon of satuatlon Indexes for cofffnlte of waters frOll the Beayer basIn. Utah .••• Tables Page 1 1 1 1 3

Application of mineral-solution equilibria to the search for sandstone-type uranium deposits in the Beaver Basin, Utah