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Page 4847, results 121151 - 121175

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Publication Extents

Not all publications have extents, not all extents are completely accurate
Evolution of geothermal fluids deduced from chemistry plots: Yellowstone National Park (U.S.A.)
E. Mazor, J. M. Thompson
1982, Journal of Volcanology and Geothermal Research (12) 351-360
Large amounts of chemical data, obtained in geothermal fields, may readily be sorted-out by the aid of a simple set of graphs that provide a clear over-all picture and facilitate the understanding of geochemical processes taking place. As a case study, data from several hundred samples of the thermal springs...
The 57Fe Mössbauer parameters of pyrite and marcasite with different provenances
B.J. Evans, R. G. Johnson, F. E. Senftle, C. B. Cecil, F. Dulong
1982, Geochimica et Cosmochimica Acta (46) 761-775
Eighteen pyrite and twelve marcasite samples which have different provenances have been investigated to determine the systematics of the influence of mineralogical and geological factors on the 57Fe Mössbauer spectra at 298 K. The following results have been obtained: there is no ambiguity in distinguishing single phase pyrite from single...
Upper crustal structure of the Mount Hood, Oregon, region as revealed by time term analysis
W.M. Kohler, J. H. Healy, S.S. Wegener
1982, Journal of Geophysical Research Solid Earth (87) 339-355
Seismic refraction data with a dense areal distribution were collected to study the seismic structure of Mount Hood and the surrounding region. This area is typical of Cascade volcanoes and is geologically quite complex. The prime goals of this project were to search for velocity variations in the upper crustal...
Late Eocene- Oligocene magnetostratigraphy and biostratigraphy at South Atlantic DSDP site 522
R.Z. Poore, L. Tauxe, S.F. Percival Jr., John L. LaBrecque
1982, Geology (10) 508-511
Upper Eocene to lowest Miocene sediments recovered at Deep Sea Drilling Project (DSDP) Site 522 in the South Atlantic Ocean allow direct calibration of magnetostratigraphy and calcareous plankton biostratigraphy. The results from Site 522 show that the Eocene/Oligocene boundary occurs in the reversed...
Notes. Characterization of plutonium in ground water near the idaho chemical processing plant
Jess M. Cleveland, Terry F. Rees
1982, Environmental Science and Technology (16) 437-439
Plutonium is present in very low concentrations in ground water near the disposal well at the Idaho Chemical Processing Plant but was not detected in waters at greater distances. Because of the absence of strong complexing agents, the plutonium is present as an uncomplexed (perhaps hydrolyzed) tetravalent species, which is...
Stability studies of surficial sediments in the Wilmington-Lindenkohl Canyons area, eastern U.S. margin
G. Almagor, R.H. Bennett, B.A. Mc Gregor, L.E. Shephard
1982, Geo-Marine Letters (2) 129-134
Stability analysis, based on infinite slope analysis and geotechnical data from a suite of 34 cores collected from the continental slope between Wilmington and Lindenkohl Canyons, indicates that the Quaternary surficial silty clay sediments on gentle slopes are stable; that sediment stability on steeper slopes (14??-19??) is marginal; and that...
Contemporary block tectonics: California and Nevada
D.P. Hill
1982, Journal of Geophysical Research Solid Earth (87) 5433-5450
Well-determined fault plane solution and the gross pattern of late-Cenozoic faulting in California and Nevada show a systematic relation between the orientation of fault planes and slip directions. In general, normal faults have northerly strikes, reverse faults have easterly strikes, and dextral and sinstral strike slip faults have northwesterly and...
Stolzite from Tsumeb.
E.E. Foord, N. M. Conklin
1982, Mineralogical Record (13) 149-150
The world's largest known crystal of stolzite (1.3 X 1.3 X 2.5 cm) is described. It is associated with tennantite and quartz, and is from the Tsumeb mine, Tsumeb, Namibia. Forms present include (001), (111), (101), (122), and (212). Spectrographic analyses indicate a nearly end-member composition with Mo, Fe, Ba,...
Evaluation of 0.46- to 2.36-mu m multispectral scanner images of the east Tintic mining district, Utah, for mapping hydrothermally altered rocks
L. C. Rowan, A.B. Kahle
1982, Economic Geology (77) 441-452
Airborne multispectral scanner images recorded in the 0.46- to 2.36-mu m region for the East Tintic mining district, Utah, were evaluated to determine their usefulness for distinguishing six types of hydrothermally altered rocks from a wide range of sedimentary and igneous rock types. Limestone, dolomite, and argillaceous rocks were of...
Exotic terranes of western California
M.O. McWilliams, D. G. Howell
1982, Nature (297) 215-217
Numerous distinct geological terranes compose the North American Cordillera1; there may be as many as 50 terranes in California alone2. Critical to deciphering the history of Cordilleran tectonic assembly is an understanding of the displacement history of individual terranes. It is therefore important to know: (1) whether a terrane has...
Velocity and bottom-stress measurements in the bottom boundary layer, outer Norton Sound, Alaska.
D.A. Cacchione, D.E. Drake, P. Wiberg
1982, Geologie en Mijnbouw (61) 71-78
We have used long-term measurements of near-bottom velocities at four heights above the sea floor in Norton Sound, Alaska, to compute hourly values of shear velocity u., roughness and bottom-drag coefficient. Maximum sediment resuspension and transport, predicted for periods when the computed value of u. exceeds a critical level, occur...
The chemical and isotopic record of rock-water interaction in the Sherman Granite, Wyoming and Colorado
R. A. Zielinski, Z. E. Peterman, J. S. Stuckless, J.N. Rosholt, Ignatius T. Nkomo
1982, Contributions to Mineralogy and Petrology (78) 209-219
Chemical, isotopic, radiographic, and rock-leaching data are combined to describe the effects of rock-water interactions in core samples of petrographically fresh, 1.43 b.y.-old Sherman Granite. The data serve to identify sensitive indicators of incipient alteration and to estimate the degree, pathways, and timing of element mobilization. Unfractured core samples of...
Multi-element analysis of manganese nodules by atomic absorption spectrometry without chemical separation
Jean S. Kane, J. M. Harnly
1982, Analytica Chimica Acta (139) 297-305
Five manganese nodules, including the USGS reference nodules A-1 and P-1, were analyzed for Co, Cu, Fe, K, Mg, Mn, Na, Ni and Zn without prior chemical separation by using a simultaneous multi-element atomic absorption spectrometer with an air—cetylene flame. The nodules were prepared in three digestion matrices. One of...
Morphology, distribution, and development of submarine canyons on the United States Atlantic continental slope between Hudson and Baltimore Canyons
David C. Twichell, David G. Roberts
1982, Geology (10) 408-412
The distribution and morphology of submarine canyons off the eastern United States between Hudson and Baltimore Canyons have been mapped by long-range sidescan sonar. In this area canyons are numerous, and their spacing correlates with overall slope gradient; they are absent where the gradient is less than 3°, are 2...
Depositional setting and diagenetic evolution of some Tertiary unconventional reservoir rocks, Uinta Basin, Utah
Janet K. Pitman, T. D. Fouch, M. B. Goldhaber
1982, American Association of Petroleum Geologists Bulletin (66) 1581-1596
The Douglas Creek Member of the Tertiary Green River Formation underlies much of the Uinta basin, Utah, and contains large volumes of oil and gas trapped in a complex of fractured low-permeability sandstone reservoirs. In the southeastern part of the basin at Pariette Bench, the Eocene Douglas Creek Member is...
Rapid intrusion of magma into wet rock: Groundwater flow due to pore pressure increases
P.T. Delaney
1982, Journal of Geophysical Research Solid Earth (87) 7739-7756
Analytical and numerical solutions are developed to simulate the pressurization, expansion, and flow of groundwater contained within saturated, intact host rocks subject to sudden heating from the planar surface of an igneous intrusion. For most rocks, water diffuses more rapidly than heat, assuring that groundwater is not heated along a...
Environmental implications of test-to-substrate attachment among some modern sublittoral foraminifera
C. Wylie Poag
1982, Geological Society of America Bulletin (93) 252-268
Topographic highs on the outer continental shelf of New Jersey are sites for the concentration of three species of attached calcareous benthic foraminifera. Elphidium subarcticum Cushman, normally considered a vagrant species, cements itself by an organic film to one or more quartz grains. Webbinella concave (Williamson) attaches to quartz grains...
Automated standardization technique for an inductively-coupled plasma emission spectrometer
John R. Garbarino, Howard E. Taylor
1982, Analytica Chimica Acta (134) 153-165
The manifold assembly subsystem described permits real-time computer-controlled standardization and quality control of a commercial inductively-coupled plasma atomic emission spectrometer. The manifold assembly consists of a branch-structured glass manifold, a series of microcomputer-controlled solenoid valves, and a reservoir for each standard. Automated standardization involves selective actuation of each solenoid valve...
Glass frit nebulizer for atomic spectrometry
L. R. Layman
1982, Analytical Chemistry (54) 638-642
The nebuilizatlon of sample solutions Is a critical step In most flame or plasma atomic spectrometrlc methods. A novel nebulzatlon technique, based on a porous glass frit, has been Investigated. Basic operating parameters and characteristics have been studied to determine how thte new nebulizer may be applied to atomic spectrometrlc...
Genetic relations among basic lavas and ultramafic nodules: Evidence from oxygen isotope compositions
T.K. Kyser, J. R. O’Neil, I. S. E. Carmichael
1982, Contributions to Mineralogy and Petrology (81) 88-102
??18O values of unaltered basic lavas range from 4.9 to 8.3 but different types of basalts are usually restricted to narrow and distinct ranges of isotopic composition. The average ??18O values for Hawaiian tholeiites, mid-ocean ridge tholeiites, and alkali basalts are 5.4, 5.7, and 6.2 permil, respectively. Potassic lavas and...