Reinterpretation of the boundary between the Cosumnes and Logtown Ridge Formations, Amador County, California
Robert V. Sharp, Wendell A. Duffield
1973, Geological Society of America Bulletin (84) 3969-3976
Recent detailed geologic mapping in the Sierran foothills reveals that rocks previously included in the Jurassic Amador Group must be redefined. The term “Amador Group” was applied by Taliaferro and Clark to a section of epiclastic metasedimentary rocks (the Cosumnes Formation) and the seemingly conformable overlying metavolcanic rocks (the Logtown...
Interstitial water studies on small core samples, Leg 15
Fred L. Sayles, Frank T. Manheim, Lee S. Waterman
1973, Initial reports of the Deep Sea Drilling Project (15) 783-804
Analyses of pore fluids from reducing environments demonstrate that reduction of SO4 is accompanied by large increases in alkalinity and strong depletion of Ca and Mg. The data are compatible with a model of replacement of Fe3+ in clay lattices by Mg from the interstitial solutions and the precipitation of...
Resistivity, self‐potential, and induced‐polarization surveys of a vapor‐dominated geothermal system
A.A.R. Zohdy, L. A. Anderson, L.J. Patrick Muffler
1973, Geophysics (38) 1130-1144
The Mud Volcano area in Yellowstone National Park provides an example of a vapor‐dominated geothermal system. A test well drilled to a depth of about 347 ft penetrated the vapor‐dominated reservoir at a depth of less than 300 ft. Subsequently, 16 vertical electrical soundings (VES) of the Schlumberger type were...
Zircon fission-track ages of Pearlette family ash beds in Meade County, Kansas
C. W. Naeser, Glen A. Izett, Ray E. Wilcox
1973, Geology (1) 187-189
Pearlette family volcanic ash beds at two faunally important late Cenozoic localities near Meade, Meade County, Kansas, are very similar in chemical and mineralogic composition, yet their zircon microphenocrysts have markedly different fission-track ages. Zircon microphenocrysts from type B Pearlette volcanic ash underlying sediments that contain the Borchers local fauna...
Annealing history limits for inhomogeneous, native gold grains as determined from Au-Ag diffusion rates
Gerald K. Czamanske, George A. Desborough, Fraser E. Goff
1973, Economic Geology (68) 1275-1288
Quantitative study of intrinsic inhomogeneities in native gold grains from three deposits in the western United States has revealed concentration profiles that represent the integrated sum of natural diffusion plus original chemical heterogeneity. By assuming that measured natural concentration gradients result solely from diffusion, upper limits may be placed on...
Geologic factors affecting compaction of deposits in a land-subsidence area
William B. Bull
1973, Geological Society of America Bulletin (84) 3783-3802
In the west-central San Joaquin Valley, California, pumping of ground water has changed water levels, thereby increasing the stresses that tend to compact alluvium by as much as 50 percent and creating a large area of intense land subsidence.The estimated 1943–1960 specific unit compaction (compaction during a time period, per...
Stress of formalin treatment in juvenile spring chinook salmon (Oncorhynchus tshawytscha) and steelhead trout (Salmo gairdneri>)
Gary Wedemeyer, W. T. Yasutake
1973, Journal of the Fisheries Research Board of Canada (31) 179-184
The physiological stress of 200 ppm formalin treatments at 10 C is more severe in the juvenile steelhead trout (Salmo gairdneri) than in the spring chinook salmon (Oncorhynchus tshawytscha). In the steelhead, a marked hypochloremia follows a 1-hr treatment and recovery requires about 24 hr. During longer treatments, hypercholesterolemia together with reduced...
Westward tidal lag as the driving force of plate tectonics
George W. Moore
1973, Geology (1) 99-100
As spreading at known interarc basins occurs to the west of westward-dipping subduction zones, and movement of the lower plates is also to the west, it is suggested that all plates move chiefly westward. Rates of motion are equal to a net difference between eastward and westward transport on semidiurnal...
Age and correlation of the Windermere Group in northeastern Washington
F. K. Miller, E.H. McKee, R. G. Yates
1973, Geological Society of America Bulletin (84) 3723-3729
Greenstone of basaltic composition forms the middle part of the Windermere System in southern British Columbia and the correlative Windermere Group in northeastern Washington. The greenstone, together with the rest of the Windermere in this region, is highly sheared, altered, and metamorphosed, except for a small exposed mass of relatively...
What about ground water?
Ralph C. Heath
1973, Groundwater (11) 50-51
No abstract available....
Variations in Sr, Rb, K, Na, and Initial Sr87/Sr86 in Mesozoic Granitic Rocks and Intruded Wall Rocks in Central California
Ronald Wayne Kistler, Zell E. Peterman
1973, Geological Society of America Bulletin (84) 3489-3512
Initial Sr87/Sr86 of granitic rocks which are exposed north of the Garlock fault in California, and which represent the entire 130-m.y. time span of emplacement during the Mesozoic, ranges mainly from 0.7031 to 0.7082, with one value of 0.7094. A systematic areal variation, independent of age, exists for initial Sr87/Sr86 in these...
Critically refracted waves in a spherically symmetric radially heterogeneous Earth model
David P. Hill
1973, Geophysical Journal of the Royal Astronomical Society (34) 149-177
A theoretical analysis of acoustic waves refracted by a spherical boundary across which velocity and density increase abruptly and below which velocity and density may either increase or decrease continuously with depth is formulated in terms of waves generated at a harmonic point source and scattered by a radially...
Precambrian iron-formations of the United States
R. W. Bayley, H. L. James
1973, Economic Geology (68) 934-959
No abstract available....
Variations in lead-isotopic compositions in Mesozoic granitic rocks of California: A preliminary investigation
Bruce R. Doe, Maryse Delevaux
1973, Geological Society of America Bulletin (84) 3513-3526
Six alkali feldspar and two whole-rock samples of granitic rocks from the Sierra Nevada batholith and adjacent Klamath Mountains were analyzed for their lead-isotope compositions. The samples represented each of three 87Sr/86Sr groupings (< 0.704, 0.704 to 0.706, and > 0.706) for granitic rocks north of the Garlock fault in California....
Nodal tidal cycle of 18.6 yr.: Its importance in sea-level curves of the east coast of the United States and its value in explaining long-term sea-level changes
Clifford A. Kaye, Gary W. Stuckey
1973, Geology (1) 141-144
The 18.6-yr cycle of the Moon's nodes dominates the annual means of high water, low water, and range at Boston and at other East Coast harbors. The maxima and minima of the high-water and range curves agree closely with the 180° and 0° long. yr, respectively, of the Moon's ascending...
Microprobe analyses of sericite, chlorite, and epidote from Jerome, Arizona
J. Thomas Nash
1973, Journal of Research of the U.S. Geological Survey (1) 673-678
Volcanic rocks in the vicinity of the massive sulfide deposits at the United Verde mine, Jerome, Ariz., have been modified in several periods of hydrothermal alteration and greenschist metamorphism. Chlorite, 2M, mica (sericite), and epidote are characteristic alteration products. Microprobe analyses for sericite, chlorite, and epidote are recalculated to structural formulas by the method employing oxygen...
Determination of the association and dissociation of humic acid fractions by small angle X-ray scattering
D.J. Pinckney, R.L. Wershaw
1973, Journal of Research of the U.S. Geological Survey (1) 701-707
A procedure has been devised for the fractionation of humic acid samples from different environments. This procedure involves fractionation of the sample by adsorption chromatography on a Sephadex G-50 column followed by chromatography on either a G-25 or a G-100 column. The fractions of the solutions are then examined by small angle X-ray scattering. Three...
Problems of underground storage of wastes
Raymond L. Nace
1973, Journal of Research of the U.S. Geological Survey (1) 719-723
Problems of underground storage of waste involve geology in its broadest sense, including hydrology, geochemistry, and geophysics. Wastes may be solid, liquid, or gaseous, and they may be chemically toxic or noxious, esthetically offensive, or radioactive. Some wastes require only temporary containment, whereas others must be isolated for indefinitely long periods. The means and locale...
Loss of volatiles during fountaining and flowage of basaltic lava at Kilauea Volcano, Hawaii
Donald A. Swanson, Brent P. Fabbi
1973, Journal of Research of the U.S. Geological Survey (1) 649-658
The amount of water and sulfur in pumice erupted during periods of vigorous activity during the 1969-71 Mauna Ulu eruption varied inversely with fountain height because of degassing during the fountaining. The pumice lost about 0.05 wt percent water and 0.003 wt percent sulfur during fountaining to heights of 400-540 m. Analyses suggest that the...
Flow characteristics of a subsurface-controlled recharge basin on Long Island, New York
Robert C. Prill, Donald B. Aaronson
1973, Journal of Research of the U.S. Geological Survey (1) 735-744
Ponding studies at the Woodbury recharge basin on Long Island, N.Y., show that the principal zones controlling infiltration are a surface-loam stratum and an intermediate gravelly, sandy loam stratum. The saturated hydraulic conductivities of these strata are 0.90 and 0.1 ft per day, respectively. The surface loam acts as the principal zone controlling infiltration until...
Fluorescent spectroscopy, a technique for characterizing surface films
Marvin C. Goldberg, David H. Devonald III
1973, Journal of Research of the U.S. Geological Survey (1) 709-717
A relationship is established between fluorescent spectra obtained by using a light path through the liquid solution and the fluorescent spectra obtained by a direct reading of surface reflection (remote sensing). A brief review of quantum fundamentals provides the necessary information to conclude that "see-through" and reflectance spectra are identical in wavelength response. Many floating...
Archaeocycas and Phasmatocycas - new genera of Permian cycads
Sergius H. Mamay
1973, Journal of Research of the U.S. Geological Survey (1) 687-689
The generic names Archaeocycas and Phasmatocycas are introduced for two previously announced but unnamed new genera of Early Permian plants; these taxa are regarded as early stages in the cycadean lineage. The names arc formalized with diagnoses, illustrations, and type designations....
Sr87/Sr86, K, Na, Rb, and Sr in some eclogites and associated basalts from California and southwestern Oregon
E. D. Ghent, Z. E. Peterman, R. G. Coleman
1973, Journal of Research of the U.S. Geological Survey (1) 643-647
Six samples of group C eclogites from California and southwestern Oregon have initial Sr87/Sr86 ratios in the range of 0.7028 to 0.7051; Rb contents from less than 1 to 53.4 ppm; and Sr contents from 147 to 270 ppm. These data and major-element compositions suggest that the eclogites were derived from basalts older than but...
Effects of migratory waterfowl on water quality at the Montezuma National Wildlife Refuge, Seneca County, New York
Mark A. Have
1973, Journal of Research of the U.S. Geological Survey (1) 725-734
This study was done in response to the shellfish industry's concern that bacteria in effluent from the national wildlife refuges along the northeast coast of the United States may be adversely affecting the harvest of shellfish. A line graph shows inconsistent relationships between bird population at the Montezuma refuge and total coliform, fecal coliform, and...
Radioelement distribution in the basement complex of the Yukon-Tanana upland, Eielson deep test hole, Alaska
C. M. Bunker, C. A. Bush, R. B. Forbes
1973, Journal of Research of the U.S. Geological Survey (1) 659-663
Uranium, thorium, and potassium contents were determined in 94 samples of drill cuttings from a 9,774-foot-deep exploratory hole drilled entirely in crystalline schists of the basement complex of the Yukon-Tanana Upland. The data indicate two distinctively different rock types and reflect differences in the calcite content of the rock. Zones of anomalously high concentrations of...