LEADER 02116oam  2200565   450 
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035   $a(EXLCZ)995470000002460266
100   $a20141123d1984      ua             0
101 0 $aeng
135   $aurmn|||||||||
181   $ctxt$2rdacontent
182   $cc$2rdamedia
183   $acr$2rdacarrier
200 10$aGeophysical interpretation of the gneiss terrane of northern Washington and southern British Columbia, and its implications for uranium exploration /$fby John W. Cady and Kenneth F. Fox, Jr
210  1$aWashington :$cUnited States Department of the Interior, Geological Survey,$d1984.
215   $a1 online resource (iii, 29 pages) $cillustrations, maps +$e1 plate
225 1 $aGeological Survey professional paper ;$v1260
300   $aTitle from title screen (viewed October 14, 2014).
300   $a"Gravity highs suggest that gneiss domes of the Omineca crystalline belt are the surface expression of a zone of dense infrastructure."
320   $aIncludes bibliographical references (pages 26-29).
606   $aGneiss$zWashington (State)
606   $aGneiss$zBritish Columbia
606   $aUranium ores$zWashington (State)
606   $aUranium ores$zBritish Columbia
606   $aGneiss$2fast
606   $aUranium ores$2fast
607   $aBritish Columbia$2fast
607   $aWashington (State)$2fast
615  0$aGneiss
615  0$aGneiss
615  0$aUranium ores
615  0$aUranium ores
615  7$aGneiss.
615  7$aUranium ores.
700   $aCady$b John W.$01387171
702   $aFox$b Kenneth F.
712 02$aGeological Survey (U.S.),
801  0$bCOP
801  1$bCOP
801  2$bOCLCO
801  2$bOCLCF
801  2$bGPO
906   $aBOOK
912   $a9910706921503321
996   $aGeophysical interpretation of the gneiss terrane of northern Washington and southern British Columbia, and its implications for uranium exploration$93436712
997   $aUNINA