02116oam 2200565 450 991070692150332120180426085541.0(CKB)5470000002460266(OCoLC)896810762(OCoLC)995470000002460266(EXLCZ)99547000000246026620141123d1984 ua 0engurmn|||||||||txtrdacontentcrdamediacrrdacarrierGeophysical interpretation of the gneiss terrane of northern Washington and southern British Columbia, and its implications for uranium exploration /by John W. Cady and Kenneth F. Fox, JrWashington :United States Department of the Interior, Geological Survey,1984.1 online resource (iii, 29 pages) illustrations, maps +1 plateGeological Survey professional paper ;1260Title from title screen (viewed October 14, 2014)."Gravity highs suggest that gneiss domes of the Omineca crystalline belt are the surface expression of a zone of dense infrastructure."Includes bibliographical references (pages 26-29).GneissWashington (State)GneissBritish ColumbiaUranium oresWashington (State)Uranium oresBritish ColumbiaGneissfastUranium oresfastBritish ColumbiafastWashington (State)fastGneissGneissUranium oresUranium oresGneiss.Uranium ores.Cady John W.1387171Fox Kenneth F.Geological Survey (U.S.),COPCOPOCLCOOCLCFGPOBOOK9910706921503321Geophysical interpretation of the gneiss terrane of northern Washington and southern British Columbia, and its implications for uranium exploration3436712UNINA