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Page 6343, results 158551 - 158575

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Publication Extents

Not all publications have extents, not all extents are completely accurate
The geologic setting of the Luna 16 landing site
J.F. McCauley, D. H. Scott
1972, Earth and Planetary Science Letters (13) 225-232
The Luna 16 landing site is similar in its geologic setting to Apollos 11 and 12. All three sites are located on basaltic mare fill which occurs mostly within multi-ring basins formed by impact earlier in the moon's history. A regolith developed...
Site distribution of iron in staurolite
Eric Dowty
1972, Earth and Planetary Science Letters (15) 72-74
The Mössbauer spectrum of staurolite does not necessarily indicate that ferrous iron is distributed over both the tetrahedral Fe site and one or more of the octahedral sites, as previously thought. Two doublets are present in the spectrum, but their quadrupole spliting...
Studies of quaternary saline lakes-I. Hydrogen isotope fractionation in saline minerals
S. Matsuo, I. Friedman, G.I. Smith
1972, Geochimica et Cosmochimica Acta (36) 427-435
Borax, gaylussite, nahcolite and trona were synthesized in aqueous solution at temperatures ranging from 8° to 35°C. Except for borax, deuterium was always depleted in these hydrated minerals relative to the solutions from which they were crystallized. In borax, no significant fractionation was found. The fractionation factor of <span id="MathJax-Element-1-Frame"...
Prospects for earthquake prediction and control
J. H. Healy, W.H.K. Lee, L. C. Pakiser, C.B. Raleigh, M.D. Wood
1972, Tectonophysics (14) 319-332
The San Andreas fault is viewed, according to the concepts of seafloor spreading and plate tectonics, as a transform fault that separates the Pacific and North American plates and along which relative movements of 2 to 6 cm/year have been taking place. The resulting strain can be released by creep,...
Biscalitheca suzanneana, N. Sp., from the uppermost Pennsylvanian of Texas
S.H. Mamay
1972, Review of Palaeobotany and Palynology (14) 141-147
Biscalitheca suzanneana, n. sp., is described from specimens found in an uppermost Pennsylvanian deposit in north-central Texas. The genus was identified primarily on the basis of impressions of the unique sporangial annuli. The occurrence establishes for Biscalitheca a stratigraphic range equivalent to nearly the entire...
Fish viruses: Histopathologic changes associated with experimental channel catfish virus disease
K. Wolf, R. L. Herman, C. P. Carlson
1972, Journal of the Fisheries Research Board of Canada (29) 149-150
A histologic examination was carried out on fry with experimentally induced channel catfish virus disease (CCVD). The infection produced a hemorrhagic and necrotic disease with the target organs being the kidneys, liver, digestive tract, and skeletal muscle. The results agree with symptoms of the disease and with published data on...
Electron microprobe evaluation of terrestrial basalts for whole-rock K-Ar dating
E. A. Mankinen, G. Brent Dalrymple
1972, Earth and Planetary Science Letters (17) 89-94
Four basalt samples for whole-rock K-Ar dating were analyzed with an electron microprobe to locate potassium concentrations. Highest concentrations of potassium were found in those mineral phases which were the last to crystallize. The two reliable samples had potassium concentrated in fine-grained...
Oil development and conservation in Arctic America
J. C. Reed
1972, Biological Conservation (4) 369-371
As in his earlier article to which reference is made, the author stresses the need for more background information and a much greater research effort before problems of environmental protection from oil developments in northern Alaska can be effectively tackled. Meanwhile, there...
Lunar "dunite", "pyroxenite" and "anorthosite"
H. G. Wilshire, E.D. Jackson
1972, Earth and Planetary Science Letters (16) 396-400
Monomineralic aggregates of olivine, clinopyroxene, orthopyroxene and plagioclase with granoblastic textures are widespread minor constituents of Apollo 14 breccias. Recrystallization is commonly incomplete within these aggregates, leaving relict material that clearly indicates single-mineral-grain sources for the aggregates. The aggregates are not, therefore, properly characterized by igneous rock names, nor can...
Fecundity of the sea lamprey (Petromyzon marinus) in Lake Superior
Patrick J. Manion
1972, Transactions of the American Fisheries Society (101) 718-720
An infectious agent, which appears to be a virus (RJV) has been isolated from the liver of a wild raccoon which has led to a highly fatal type of disease characterized by conjunctivitis and an elevated serum bilirubin frequently accompanied by jaundice on inoculation of raccoons. Ferrets also appear to...
Exposure times necessary for antimycin and rotenone to eliminate certain freshwater fish
P.A. Gilderhus
1972, Journal of the Fisheries Research Board of Canada (29) 199-202
In laboratory flowing-water troughs exposure required to induce 100% mortality, regardless of time to death for antimycin and rotenone against selected freshwater fish species was determined. Carp and white suckers required shorter exposures to antimycin (6 hr) than to rotenone (18–24 hr) at field-use concentrations of 5 and 50 ppb respectively. Bullheads were...
Downstream migration of recently transformed sea lampreys before and after treatment of a Lake Michigan tributary with a lampricide
John W. Hodges
1972, Journal of the Fisheries Research Board of Canada (29) 1237-1240
After the Pere Marquette River was treated with a lampricide in May 1964, the number of recently transformed sea lampreys (Petromyzon marinus) collected in the water-intake structure of a chemical plant near the mouth of the stream dropped 99.5%, from 13,913 (average for 1962-63 and 1963-64) to 76 (average for...
H. W. Murdy, 1924-1971
H.K. Nelson
1972, Journal of Wildlife Management (36) 681-681
Abstract has not been submitted...
Ground-water outflow from Chino Basin, Upper Santa Ana Valley, southern California
James J. French
1972, Water Supply Paper 1999-G
Ground-water outflow from Chino basin was calculated ,by a direct method using the equation Q = PIA, in which Q is the quantity of ground-water outflow, P is the average coefficient of permeability of the sediments through which the flow occurs, I is the average hydraulic gradient, and A is...