General P, type-I S, and type-II S waves in anelastic solids; inhomogeneous wave fields in low-loss solids
Roger D. Borcherdt, Leif Wennerberg
1985, Bulletin of the Seismological Society of America (75) 1729-1763
The physical characteristics for general plane-wave radiation fields in an arbitrary linear viscoelastic solid are derived. Expressions for the characteristics of inhomogeneous wave fields, derived in terms of those for homogeneous fields, are utilized to specify the characteristics and a set of reference curves for general P and S wave fields in arbitrary viscoelastic...
Active tectonic and magmatic processes beneath Long Valley Caldera, eastern California: An overview
D.P. Hill, R. A. Bailey, A.S. Ryall
1985, Journal of Geophysical Research Solid Earth (90) 11111-11120
Geological, chronological, and structural studies of the Long Valley-Mono/Inyo Craters area document a long history of related volcanic eruptions and earthquakes controlled by regional extensional tectonics of the Basin and Range province. This activity has persisted for hundreds of thousands of years and is likely to continue. The Long Valley...
Simulated fissioning of uranium and testing of the fission-track dating method
V.E. McGee, N.M. Johnson, C. W. Naeser
1985, Nuclear Tracks and Radiation Measurements (1982) (10) 365-379
A computer program (FTD-SIM) faithfully simulates the fissioning of 238U with time and 235U with neutron dose. The simulation is based on first principles of physics where the fissioning of 238U with the flux of time is described by Ns = ??f 238Ut and the fissioning of 235U with the...
Wavelike movement of bedload sediment, East Fork River, Wyoming
R.H. Meade
1985, Environmental Geology and Water Sciences (7) 215-225
Bedload is moved down the East Fork River in distinct wavelike pulses that have the form of composite dune fields The moving material consists mostly of coarse sand and fine gravel The wavelengths of the pulses are about 500-600 m, a distance that is predetermined by the pattern of stoage...
The transverse and oblique cylindrical equal-area projection of the ellipsoid.
J.P. Snyder
1985, Annals of the Association of American Geographers (75) 431-442
The formulas for the ellipsoidal projection are derived for both forward and inverse computations and consist of modifying the formulas obtained by using the authalic sphere so that the scale along the central line of the projection is constant. Fourier series are used to eliminate recurring numerical integration and other...
EFFECTS OF LITHOLOGY ON TELEVIEWER-LOG QUALITY AND FRACTURE INTERPRETATION.
Frederick L. Paillet, W.S. Keys, A.E. Hess
1985, Conference Paper, Transactions of the SPWLA Annual Logging Symposium (Society of Professional Well Log Analysts)
Representative televiewer logs illustrating natural fractures in such common rock types as granite, gabbro, basalt, schist, sandstone, limestone and shale are presented in addition to photographs of the same fractures in core samples. These examples demonstrate the many difficulties in recognizing fractures on televiewer logs compared to fractures in logs...
SAS program for quantitative stratigraphic correlation by principal components
M.E. Hohn
1985, Computers & Geosciences (11) 471-477
A SAS program is presented which constructs a composite section of stratigraphic events through principal components analysis. The variables in the analysis are stratigraphic sections and the observational units are range limits of taxa. The program standardizes data in each section, extracts eigenvectors, estimates missing range limits, and computes the...
Electronic spectra of Fe3+ oxides and oxide hydroxides in the near IR to near UV.
David M. Sherman, T.D. Waite
1985, American Mineralogist (70) 1262-1269
Optical absorption and diffuse reflectance spectra of several Fe2O3 and FeOOH polymorphs (hematite, maghemite, goethite, lepidocrocite) in the near-IR to near-UV spectral regions (2000-200 nm) are presented. The spectra consist primarily of Fe3+ ligand field and ligand-to-metal charge-transfer transitions.-J.A.Z....
Solid state recording current meter conversion
Ralph T. Cheng, Lichen Wang
1985, Conference Paper, Oceans Conference Record (IEEE)
The authors describe the conversion of an Endeco-174 current meter to a solid-state recording current meter. A removable solid-state module was designed to fit in the space originally occupied by an 8-track tape cartridge. The module contains a CPU and 128 kilobytes of nonvolatile CMOS memory. The solid-state module communicates...
Hydrogeologic comparison of an acidic-lake basin with a neutral-lake basin in the West-Central Adirondack Mountains, New York
N.E. Peters, Peter S. Murdoch
1985, Water, Air, & Soil Pollution (26) 387-402
Two small headwater lake basins that receive similar amounts of acidic atmospheric deposition have significantly different lake outflow pH values; pH at Panther Lake (neutral) ranges from about 4.7 to 7; that at Woods Lake (acidic) ranges from about 4.3 to 5. A hydrologic analysis, which included monthly water budgets,...
FINDINGS OF A SYMPOSIUM ON COAL QUALITY.
Stanley P. Schweinfurth, Susan Garbini
1985, Conference Paper
The U. S. Geological Survey (USGS) has been doing research on coal quality for almost a century. Most of the work of the USGS regarding coal went into efforts to assess the quantity of coal in the United States, not the quality. On April 9-11, 1985, the U. S. Geological...
The Dunbar Gneiss-granitoid dome: Implications for early Proterozoic tectonic evolution of northern Wisconsin
P.K. Sims, Z. E. Peterman, K. J. Schulz
1985, Geological Society of America Bulletin (96) 1101-1112
The Dunbar dome in northeastern Wisconsin is a critical structural feature in the early Proterozoic Penokean orogen. It provides exposures of gneisses (Dunbar Gneiss) that structurally underlie the voluminous metavolcanic rocks of northeastern Wisconsin, and exposures of abundant granitoid rocks ranging from tonalite...
Water-level changes in the Ogallala aquifer, northwestern Oklahoma.
J.S. Havens
1985, Oklahoma Geology Notes (45) 205-210
The Ogallala aquifer, that part of the High Plains aquifer in Oklahoma, is part of a regional aquifer system that underlies parts of Colorado, Kansas, Nebraska, New Mexico, Oklahoma, South Dakota, Texas, and Wyoming. In 1978 the US Geological Survey began a 5- year study of the High Plains regional...
Unit hydrograph approximations assuming linear flow through topologically random channel networks
Brent M. Troutman, Michael R. Karlinger
1985, Water Resources Research (21) 743-754
The instantaneous unit Hydrograph (IUH) of a drainage basin is derived in terms of fundamental basin characteristics (Z, α, β), where α parameterizes the link (channel segment) length distribution, and β is a vector of hydraulic parameters, Z is one of three basin topological properties, N, (N, D), or (N, M), where N is magnitude (number of...
Wave energy saturation on a natural beach of variable slope
A. H. Sallenger Jr., R.A. Holman
1985, Journal of Geophysical Research - Oceans (90) 11939-11944
Time series of flow were measured across the inner surf zone during a storm. These data were used to quantify the dependence of wave height (transformed from measured flow) and velocity on local slope and depth. Similar to previous studies, as incident waves broke and propagated into the surf zone,...
Airfall tuff in the Browns Park Formation, northwestern Colorado and northeastern Utah.
S. J. Luft
1985, Mountain Geologist (22) 110-127
Bedded airfall tuffs, mainly rhyolitic in composition and locally very thick, occur throughout the Browns Park Formation (upper Oligocene to upper Miocene) in northwestern Colorado and northeasternmost Utah. They have received only cursory attention other than for the purpose of radiometric dating. The present writer began study of the tuffs...
Geochemical mass-balance relationships for selected ions in precipitation and stream water, Catoctin Mountains, Maryland
B. G. Katz, O.P. Bricker, M.M. Kennedy
1985, American Journal of Science (285) 951-962
Results of a study of input/output mass balances for major ions based on the chemical composition of precipitation and stream-water, geochemical reactions with different loading rates of hydrogen ion, and watershed processes influencing the chemical character of stream-waters in two small watershed areas are reported with a view to predicting...
Terrestrial vs. marine depositional model—A new assessment of subsurface Lower Pennsylvanian rocks of southwestern Virginia
C. L. Rice
1985, Geology (13) 786-789
A reinterpretation of the origin of subsurface rocks in southwestern Virginia and southeastern Kentucky suggests that, contrary to commonly accepted ideas, the Mississippian-Pennsylvanian Systemic boundary is an unconformity and the Lower Pennsylvanian quartz arenite sequences were deposited in a fluvial environment. Because Pennsylvanian...
Latest Mississippian (Namurian A) nonmarine ostracodes from West Virginia and Virginia
I. G. Sohn
1985, Journal of Paleontology (59) 446-460
Nonmarine ostracodes occur as partly exfoliated carapaces and internal molds at the base of the Bramwell Member of the Bluestone Formation, which represents the uppermost Mississippian (Namurian A), stratigraphic subdivision in West Virginia and Virginia. These specimens are important in that they permit the determination of a variety of adductor-muscle-attachment...
Uranium-series dating of fossil corals from marine sediments of southeastern United States Atlantic Coastal Plain
Barney J. Szabo
1985, Geological Society of America Bulletin (96) 398-406
Extensive low-lying marine deposits border the southeastern United States Atlantic Coastal Plain. Some units are fossiliferous and contain corals as isolated fragments in sediments of a detrital character. These corals are subject to alteration processes such that suites of related samples must be...
Adjustment of geochemical background by robust multivariate statistics
D. Zhou
1985, Journal of Geochemical Exploration (24) 207-222
Conventional analyses of exploration geochemical data assume that the background is a constant or slowly changing value, equivalent to a plane or a smoothly curved surface. However, it is better to regard the geochemical background as a rugged surface, varying with changes in geology and environment. This rugged surface can...
A uniform technique for flood frequency analysis.
W.O. Thomas Jr.
1985, Journal of Water Resources Planning and Management (111) 321-337
This uniform technique consisted of fitting the logarithms of annual peak discharges to a Pearson Type III distribution using the method of moments. The objective was to adopt a consistent approach for the estimation of floodflow frequencies that could be used in computing average annual flood losses for project evaluation....
Fish recruitment and movement in a flood control reservoir and tailwater
K.E. Jacobs, W.D. Swink, J.M. Nestler, L.T. Curtis
1985, Report
Abstract not submitted to date...
Contaminant trends in lake trout (Salvelinus namaycush) of the upper Great Lakes
David S. DeVault, Wayne A. Willford, Robert J. Hesselberg
1985, Report
Contaminant body burdens in lake trout from the Upper Great Lakes have been monitored since 1970 on Lake Michigan and since 1977 and 1978 on Lakes Superior and Huron by USEPA, Great Lakes National Program Office and USFWS, Great Lakes Fishery Laboratory. Analysis of the Lake Michigan data shows that mean...
Solubility relations in the system sodium chloride-ferrous chloride-water between 25 and 70.degree.C at 1 atm
I.-M. Chou, L.D. Phan
1985, Journal of Chemical and Engineering Data (30) 216-218
Solubility relations in the ternary system NaCl-FeCl2-H2O have been determined by the visual polythermal method at 1 atm from 20 to 85??C along six composition lines. These she composition lines are defined by mixing FeCl2??4H2O with six aqueous NaCl solutions containing 5, 10, 11, 15, 20, and 25 wt %...
