Copper, lead, and zinc occurrences in Alaska
Edward Huntington Cobb
1960, Mineral Investigations Resource Map 9
Geologic interpretation of magnetic data in the Copper River basin, Alaska
Gordon E. Andreasen, Arthur Grantz, Isidore Zietz
1960, Open-File Report 60-10
Geology and mineral deposits of the St. Regis-Superior area, Mineral County, Montana
Arthur B. Campbell
1960, Bulletin 1082-I
The St. Regis-Superior area occupies about 300 square miles in northwestern Montana and includes parts of the Squaw Peak Range and Coeur d'Alerie Mountains of the northern Rocky Mountains physiographic province. Nearly 50,000 feet of metasedimentary rocks of the Precambrian Belt series, chiefly varieties of quartzite and argillite, underlies most...
Geology and fluorspar deposits, Northgate district, Colorado
Thomas A. Steven
1960, Bulletin 1082-F
The fluorspar deposits in the Northgate district, Jackson County, Colo., are among the largest in Western United States. The mines were operated intermittently during the 1920's and again during World War II, but production during these early periods of operation was not large. Mining was begun on a larger scale...
Scheelite in the precambrian gneisses of Colorado
O.L. Tweto
1960, Economic Geology (55) 1406-1428
Scheelite of Precambrian age has been found at several localities in Colorado and Wyoming in recent years. Most of it is disseminated in regionally metamorphosed rocks, principally in calc-silicate gneiss, but also in amphibolite. Small amounts are found in pegmatites and in gold-or copper-quartz veins of Precambrian age. The scheelite in most of the deposits contains molybdenum, and much of...
Iron-ore resources of the United States including Alaska and Puerto Rico, 1955
Martha S. Carr, Carl E. Dutton
1959, Bulletin 1082-C
The importance of iron ore, the basic raw material of steel, as a fundamental mineral, resource is shown by the fact that about 100 million long tons of steel is used annually in the economy of the United States, as compared with a combined total of about 5 million long...
Copper, lead and zinc in Alaska
Edward Huntington Cobb
1959, Open-File Report 59-22
No abstract available. ...
Geology of the Garo uranium-vanadium-copper deposit, Park County, Colorado
Verl R. Wilmarth
1959, Bulletin 1087-A
Geology and uranium-vanadium deposits of the slick rock district, San Miguel and Dolores counties, Colorado
D. R. Shawe, Norbert L. Archbold, G. C. Simmons
1959, Economic Geology (54) 395-415
Sedimentary rocks known in the Slick Rock district in southwestern Colorado range in age from Devonian (?) to Cretaceous, and aggregate about 13,000 feet in maximum thickness. Important uranium-vanadium production has come from deposits in the Salt Wash member of the Morrison formation of Late Jurassic age.The sedimentary rocks are gently folded in...
Plastic standards for geochemical prospecting
D. B. Hawkins, F. C. Canney, F. N. Ward
1959, Economic Geology (54) 738-744
Plastic standards for use in geochemical prospecting have been prepared by impregnating a clear thermosetting resin with different amounts of a stable dye or colored metal complex. The colored plastic is molded or subsequently milled into convenient shapes to form standards that are less bulky and more stable than the...
Amygdule mineral zoning in the Portage Lake lava series, Michigan copper district
R.E. Stoiber, Edward S. Davidson
1959, Economic Geology (54) 1444-1460
No abstract available....
Some phase relations in the hydrothermally altered rocks of porphyry copper deposits
Saville Cyrus Creasey
1959, Economic Geology (54) 351-373
The application of ACF and AKF diagrams to the hydrothermal alteration in porphyry Cu deposits aids in the recognition of the critical components, and the characteristic mineral phases permit the distinction of one alteration facies from another. The somewhat meager chemical and mineralogical data suggest...
Aeromagnetic map of the Copper River basin, Alaska
Gordon E. Andreasen, W.J. Dempsey, J. R. Henderson Jr., F. P. Gilbert
1958, Geophysical Investigations Map 156
Geology and ore deposits of the east Shasta copper-zinc district, Shasta County, California
John Patrick Albers
1958, Open-File Report 58-1
No abstract available....
Geology and ore deposits of the Jerome area, Yavapai County, Arizona
C.A. Anderson, S.C. Creasey
1958, Professional Paper 308
The Jerome area, in central Arizona, includes the Mingus Mountain quadrangle and parts of the adjacent Clarkdale, Mayer, and Mount Union quadrangles. The largest copper mines in the area at Jerome are the United Verde Extension and the United Verde. The United Verde Extension, closed in 1938 and the United...
Copper and uranium deposits of the Coyote district, Mora County, New Mexico
C.M. Tschanz, D.C. Laub, G.W. Fuller
1958, Bulletin 1030-L
Geology of the Copper King uranium mine, Larimer County, Colorado
P.K. Sims, George Phair, Robert Hadley Moench
1958, Bulletin 1032-D
Nickel-gold ore of the mackinaw mine, Snohomish County, Washington
C. Milton, D.J. Milton
1958, Economic Geology (53) 426-447
The Mackinaw mine ore is of an unusual or unique type, consisting chiefly of niccolite, maucherite, pentlandite, chalcopyrite, cubanite, and magnetite in an altered peridotite. Valleriite, gold and sphalerite are minor primary minerals; chalcocite and violarite or bravoite are supergene minerals. Pyrrhotite and pyrite are absent. From the textural relations...
Some natural variations in the relative abundance of copper isotopes
E. C. Walker, F. Cuttitta, F. E. Senftle
1958, Geochimica et Cosmochimica Acta (15) 183-194
The relative isotopic abundance of copper has been measured in a number of minerals and a few plant materials. Suites of samples from Michigan and the Colorado Plateau have been examined in more detail to determine if local variations due to isotopic exchange or diffusion could be found. The relative...
Spectrochemical method for the determination of selenium
C. L. Waring, H.W. Worthing, K.V. Hazel
1958, Analytical Chemistry (30) 1504-1506
Selenium can be determined in pyrite, chalcocite, and marcasite by a simple and rapid spectrochemical method that requires no complicated arrangement of spectrographic equipment or chemical pretreatment of samples. Advantage is taken of the new short wave length radiation plates (Eastman) and the addition of copper oxide to enhance the...
Apparatus and technique for multiple tests by the confined-spot method of colorimetric analysis: Application to field estimation of nickel and copper
J. H. McCarthy Jr., R.E. Stevens
1958, Analytical Chemistry (30) 535-538
The confined-spot method of colorimetric analysis is generally applicable to the semiquantitative estimation of traces of ions in solution that form colored precipitates or otherwise alter material on a confined area of reagent paper. For precise results, the rate of flow of test solutions through the reagent paper must be...
Some natural variations in the relative abundance of copper isotopes
Edward C. Walker, Frank Cuttitta, F. E. Senftle
1957, Trace Elements Investigations 696
Geology of possible petroleum provinces in Alaska
Don John Miller, Thomas G. Payne, George Gryc
1957, Open-File Report 57-72
The history of petroleum exploration in Alaska and the geology of possible petroleum provinces in Alaska are reviewed. Maps showing Alaska's major Mesozoic and Tertiary tectonic elements, possible petroleum provinces, and indications of petrol, are included in this report. Annotated references in Geological Survey publications relating to petroleum and oil...
Volumetric determination of uranium: Titanous sulfate as reductant before oxidimetric titration
J.S. Wahlberg, D. L. Skinner, L. F. Rader Jr.
1957, Analytical Chemistry (29) 954-957
Need for a more rapid volumetric method for the routine determination of uranium in uranium-rich materials has led to the development of a method that uses titanous sulfate as a reductant before oxidimetric titration. Separation of the hydrogen sulfide group is not necessary. Interfering elements precipitated by cupferron are removed...
Minor elements in Keweenawan lavas, Michigan
H. R. Cornwall, H. J. Rose Jr.
1957, Geochimica et Cosmochimica Acta (12) 209-224
The distribution of minor elements in three basaltic flows of the Keweenawan series, of Michigan, is related to differentiation in the flows. Thus, nickel is most abundant in the early differentiates; nickel, chromium, and barium are generally deficient in the pegmatites, which formed late; whereas copper, vanadium, yttrium, and other...