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Page 6190, results 154726 - 154750

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Publication Extents

Not all publications have extents, not all extents are completely accurate
Geochemistry of sphalerite from the Star Mine, Coeur d'Alene district, Idaho
V.C. Fryklund, Janet D. Fletcher
1956, Economic Geology (51) 223-247
Forty sphalerite samples from the Star mine, Coeur d'Alene district, Idaho, and 19 sphalerite samples from other Coeur d'Alene mines have been quantitatively analyzed by spectrographic methods for Fe, Cu, Pb, Cd, Ga, Ge, In, Mn, Co, and Hg. The samples from the Star vein were collected over a strike...
Uranium deposits of the northern part of the Boulder Batholith, Montana
G.E. Becraft
1956, Economic Geology (51) 362-374
Uranium minerals and radioactivity anomalies occur in many silverlead veins and chalcedony veins and vein zones in the Boulder batholith of southwestern Montana. Pitchblende has been identified in a few silverlead veins. These silver-lead veins occupy shear zones along which there is no evidence of large-scale lateral displacement. The wall...
A petrographic study of Gila Polychrome 
E.B. Danson, R.M. Wallace
1956, American Antiquity (22) 180-183
Gila Polychrome pottery has been recognized since the time of the earliest archaeological work in the Southwest. Cushing, in 1887–88, recognized in the polychromes at Los Muertos and other Classic period sites of the Hohokam area the pottery type we now call Gila Polychrome. As more of the Southwest became...
Discussion of “The displacement of calibration curves for electrical soil‐moisture units”
F. R. Dreibelbis, Irwin Remson, G. S. Fox
1956, Eos, Transactions, American Geophysical Union (37) 497-499
This paper seems to leave unanswered a number of questions pertaining to calibration of soil‐moisture units. In Remson and Fox's discussion of results they list five facts that are shown by the calibration.The first three deal with the second drying curve being different than the first, and subsequent dryings being...
Application of the modified Einstein procedure for computation of total sediment load
K. B. Schroeder, C. H. Hembree
1956, Eos, Transactions, American Geophysical Union (37) 197-212
A method that enables good estimates to be made of total sediment load has been tested with data from several western streams. The method, which uses both theoretical and empirical formulas, combines a modification of Einstein's procedure for computing bed‐material load and the usually available data from suspended‐sediment measurements. Basic...
Non-pegmatitic resources of beryllium in United States
Lawrence Allen Warner, W.T. Holser, V.R. Wilmarth, E.N. Cameron
1956, Trace Elements Investigations 137
During the period from 1948 to 1950 the U.S. Geological Survey conducted a program of field and laboratory research w determine the mode of occurrence of beryllium in non-pegmatitic rocks and mineral deposits as part of the Beryllium Program of the Division of Raw Materials of the U.S. Atomic Energy Commission. Approximately 23...
Some limitations on the possible composition of the ore-forming fluid
Paul B. Barton Jr.
1956, Trace Elements Investigations 633
The activity rations of various important anions (S, CO3, SO4, OH, F, and Cl) in hydrothermal solutions at the time of deposition are evaluated using a simple thermodynamic technique. The rations are interpreted in the light of the mineralogy of ore deposits and limites are placed on the variability of...
Volumetric determination of uranium using titanous sulfate as reductant before oxidimetric titration
James S. Wahlberg, Dwight L. Skinner, Lewis F. Rader
1956, Trace Elements Investigations 614
A new method for determining uranium in samples containing 0.05 percent or more U3O8, using titanous sulfate as reducing agent, is much shorter, faster, and has fewer interferences than conventional methods using reductor columns. The sample is dissolved with sulfuric, nitric, perchloric, and hydrofluoric acids. Elements that would otherwise form insoluble...
Radiometric traverse along the Yukon River from Fort Yukon to Ruby, Alaska, 1949
Max G. White, John M. Stevens, John J. Matzko
1956, Trace Elements Memorandum 357
In 1949, a radiometric traverse was made of rocks exposed along the banks of and near the Yukon River about Fort Yukon to Ruby, Alaska. Granitic rocks of Tertiary age and of Devonian or Carboniferous age and sandstone beds of Cretaceous age gave the highest readings obtained in the...
Bird banding
U.S. Branch of Wildlife Research
1956, Wildlife Leaflet 373
No abstract available....