W.B. Allen
1952, Open-File Report 52-3
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Publication Extents
Not all publications have extents, not all extents are completely accurateIrwin Remson
1952, Open-File Report 52-125
Joseph D. Meyers, R. C. Newcomb
1952, Open-File Report 52-99
H. C. Riggs
1952, Open-File Report 52-126
R.N. Doolittle
1952, Open-File Report 52-34
L.C. Halpenny
1952, Open-File Report 52-69
D.R. Coates
1952, Open-File Report 52-24
Raymond L. Nace
1952, Open-File Report 52-106
Vincent Ellis McKelvey, L.E. Smith, R.A. Hoppin, F.C. Armstrong
1952, Trace Elements Investigations 184
As part of a comprehensive investigation of the phosphate deposits of the western field begun in 1947, the U. S. Geological Survey has measured and sampled the Permian Phosphoria formation at many localities in Wyoming and adjacent states. Because these data will not be fully synthesized for many years,...
Roger Warren Swanson, M. R. Klepper, W.R. Lowell, F.S. Honkala, E. R. Cressman, D.A. Bostwick, O.A. Payne, E. T. Ruppel
1952, Trace Elements Investigations 186
The U. S. Geological Survey has recently measured and sampled the Phosphoria formation at many localities in Montana and other western states. These data will not be fully synthesized and analyzed for several years, but segments of the data, accompanied by little or no interpretation, will be published as...
Vincent Ellis McKelvey, L.E. Smith, D.M. Kinney, J. W. Huddle, G.F. Hosford, R.S. Sears, D.P. Sprouse, M.D. Steward
1952, Trace Elements Investigations 185
As part of a comprehensive investigation of the phosphate deposits of the western field begun in 1947, the U. S. Geological survey has measured an sampled the full thickness of the Permian Phosphoria formation and its partial correlative, the Park City formation, at many localities in Utah and other western...
Harry C. Granger, Herman L. Bauer Jr., Tom G. Lovering, Elliot Gillerman
1952, Trace Elements Investigations 156
The known uranium deposits of Grant county, N. Mex., are principally in the White Signal and Black Hawk districts. Both districts are within a northwesterly-trending belt of pre-Cambrian rocks, composed chiefly of granite with included gneisses, schists, and quartzites. Younger dikes and stocks intrude the pre-Cambrian complex....
J.D. Strobell Jr.
1952, Trace Elements Memorandum 428
No abstract available....
William R. Thurston
1952, Trace Elements Investigations 139
The Front Range of Colorado is composed chiefly of schists of the pre-Cambrian Idaho Springs formation which have been intruded by a variety of granitic batholiths. In the Crystal Mountain district the Mount Olympus granite, a satellite of the Longs Peak batholith, forms sills and essentially concordant multiple intrusions in...
J.D. Strobell Jr.
1952, Trace Elements Memorandum 415
No abstract available....
Vincent Ellis McKelvey, D.F. Davidson, F. W. O’Malley, L.E. Smith, F.C. Armstrong, R.P. Sheldon
1952, Trace Elements Investigations 183
The Permian Phosphoria formation of the western states contains one of the world's largest reserves of phosphate. Although previous investigations (see especially Mansfield, 1927), including reconnaissance geologic mapping and sampling, established the location of most of the important deposits and their quality of scattered localities, they were not sufficiently detailed...
W. P. Brosge, Hillard N. Reiser
1952, Geological Investigations, Naval Petroleum Reserve No. 4, Alaska 32
No abstract available....
Clifford A. Kaye
1952, Geological Society of America Bulletin (63)
No abstract available. ...
Paul Livingston Applin
1952, Geological Society of America Bulletin (63) 1159-1164
Mesozoic sedimentary rocks are present throughout Florida and the Coastal Plain of Georgia, but chiefly in the subsurface in an area of approximately 93,500 square miles. The Mesozoic rocks in this area belong, for the most part, to the Gulf and Comanche series of the Cretaceous system. Rocks tentatively classified...
Robert R. Coats
1952, Geological Society of America Bulletin (63) 485-514
Samples of 17 volcanic rocks of Tertiary and Quaternary age from Adak and Kanaga islands have been chemically analyzed and studied microscopically. Spectrograms have been made of 10 of them. The rocks from Adak represent one center of possibly older Tertiary age and two centers of younger Tertiary or Quaternary age. The rocks from Kanaga Island represent both a shield volcano of possibly Tertiary age, partly destroyed by the formation of a caldera, and a young cone of Quaternary age that...
Charles Storrow Denny
1952, Geological Society of America Bulletin (63) 883-922
Reconnaissance field work along the Alaska Highway in northern British Columbia and southeastern Yukon furnishes preliminary data on the later Quaternary history of the region, and on the processes and results of intensive frost action. Extensive erosion surfaces were developed prior to glaciation, such as the Alberta Plateau of northeastern British Columbia and the Yukon Plateau in southern Yukon. In the region from Dawson Creek to Fort Nelson, British Columbia, the drift is dominantly...
William P. Brosge, J. Thomas Dutro Jr., Marvin D. Mangus, Hillard N. Reiser
1952, Geological Investigations, Naval Petroleum Reserve No. 4, Alaska 42
No abstract available....
Robert L. Detterman, Robert Samuel Bickel
1952, Geological Investigations, Naval Petroleum Reserve No. 4, Alaska 41
No abstract available....
H. T. Morris, T. S. Lovering
1952, Economic Geology (47) 685-716
Part I, T. S. Lovering. Preliminary work in the Tintic district, Utah, determined the relative distance of migration of ore metals in moist carbonate and silicic wall rocks near ore, and in ground water having a very sluggish circulation through mineralized ground. The analyses of efflorescences in the Tintic Standard mine openings at suitable localities indicated that under the conditions existing during the past 25 years lead has not...
Clyde T. Hardy, S. Muessig
1952, Geological Society of America Bulletin (63) 1109-1116
The Fish Lake Plateau, nearly centrally located among the High Plateaus of Utah, exhibits glacial and other geomorphic features of regional significance. The plateau is divided into two areas by Fish Lake and the wide valley of Sevenmile Creek. The Fish Lake trough is a structural basin; Sevenmile Valley may be largely erosional. Volcanic rocks of Tertiary age underlie most of the plateau;...