C. E. Dobbin, Charles Edgar Erdmann
1955, Oil and Gas Investigation Map 178-B
No abstract available....
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Publication Extents
Not all publications have extents, not all extents are completely accurateP. P. Orkild
1955, IMAP 79
Herbert Mordecai Ezekiel
1955, Trace Elements Memorandum 864
The wet ashing of oils and aspbaltenes by sulfUric acid, percbloric acid, and nitric-sulfuric acid techniques is discussed and compared. A simple sulfuric acid=nitric acid technique which has been found to be satisfactory for these substances is described....
Gerald Martin Richmond
1955, Open-File Report 55-150
George E. Becraft
1955, Trace Elements Memorandum 944
Uranium minerals and radioactivity anomalies occur in many silver-lead veins and chalcedony veins and vein zones in the Boulder batholith of southwestern Montanao Pitchblende has been identified in a few silver-lead veins. These veins occupy shear zones along which there is no evidence of large-scale lateral displacement. The wall rock...
Ernest Dobrovolny
1955, Open-File Report 55-42
1955, Trace Elements Investigations 590
This report is a statement of progress during the six-months period from June 1 to November 30, 1955 on investigations of radioactive materials in the United States and Alaska, undertaken by the U.S. Geological Survey under the sponsorship of the U.S. Atomic Energy Commission. During the period the Geological Survey's program...
J. V. B. Wells
1955, Water Supply Paper 1316
No abstract available....
Robert Berman
1955, Trace Elements Investigations 569
Five samples of purple fluorite found in association with radioactive, materials, and a synthetic colorless control sample were studied and compared. Before and after heating, observations were made on specific gravity, index of refraction, unit-cell size, breadth of X-ray diffraction lines, and fluorescence. The purple samples became colorless on heating...
F. S. Grimaldi, Mary H. Fletcher
1955, Trace Elements Investigations 571
Thoron is popularly used for the spectrophotometric determination of thorium. An undesirable feature of its use is the high sensitivity of the reagent toward zirconium. This study describes the use of tartaric acid as a masking reagent for zirconium. Three tartaric acid-thoron systems, developed for the determination of thorium, differ...
K. S. Muir
1955, Open-File Report 55-117
The investigation of the ground-water resources of Santa Barbara County was continued (luring 1954 in cooperation with the Santa Barbara County Wallet Agency. Monthly water-level measurements were made in 182 wells in 6 of which automatic water-level recorders were operated. Earlier measurements covering the period 1941 through 1952 have been...
Edward J. Webber
1955, Open-File Report 55-190
Allen O. Taylor, James Farl Powers
1955, Trace Elements Memorandum 874-A
The Moonlight mine and Granite Foint claims are on the western flank of the Double H Mountains between the Kings River and Quinn, River valleys in northern Humboldt County, Nev. Uranium minerals at the Moonlight mine occur in a vein in intensely altered Tertiary volcanic rocks. The knovm uranium mineralization...
Frank W. Trainer
1955, Open-File Report 55-182
T. W. Robinson
1955, Open-File Report 55-152
Jack E. Sceva, Duane E. Wegner
1955, Open-File Report 55-160
Location and Extent of Area The area covered by this report (fig. 1) includes the part of Pierce County, ~ash. that lies west of the foothills of the Cascade Mountains and east of the main waterway of Puget Sound, and extends from the county line on the north to the Nisqually...
Elmer H. Baltz Jr.
1955, Trace Elements Memorandum 915
Coal and carbonaceous shale of the Dakota formation of Cretaceous age were examined for radioactivity in the Colorado Plateau of southwestern Colorado and northwestern New l1exico during the summer of 1953. Older and younger sedimentary rocks and some igneous rocks also were examined, but in less detail, Weak radioactivity was...
George E. Becraft
1955, Trace Elements Memorandum 917
Anomalous radioactivity and a yellow secondary uranium mineral tentatively identified as carnotite have been found in Tertiary sedimentary rocks about 3 miles northeast of Winston, Mont. The uranium is in tuffs and tuffaceous shales and particularly in beds rich in organic matter. Carnotite(?) was identified from three localities, principally coating...
Frank C. Armstrong
1955, Trace Elements Memorandum 918
The Last Chance group> Brown Bear and Shady Tree claims in Beaverhead County, Mont., were explored for thorium under a Defense Minerals Exploration Administration Contract in 1951 and 1952. The project was undertaken to explore northwest-trending moderately to steep dipping, thorite-bearing quartz-barite-hematite veins. The veins are wall-rock replacements and fissure fillings...
Irving A. Breger, Richard T. Moore
1955, Trace Elements Memorandum 942
An aqueous solution of uranyl sulfate containing a suspension of subbituminous coal has been heated at 210 C for three days. Examination of the coal at the end of the experiment showed it to contain 31.8 percent uranium recognizable as uraninite by a sharp, strong X-ray diffraction pattern. A similar...
Konrad Bates Krauskopf
1955, Trace Elements Investigations 509
Carl Houston Roach, Mary E. Thompson
1955, Trace Elements Investigations 512
Albert F. Trites Jr., R. T. Chew III, Tom Gray Lovering
1955, Trace Elements Investigations 514
Theodore Botinelly, Richard Philip Fischer
1955, Trace Elements Investigations 516
Donald Parker Elston, Theodore Botinelly
1955, Trace Elements Investigations 518