Age and nature of the basement in northeastern Washington and northern Idaho: isotopic evidence from Mesozoic and Cenozoic granitoids
M.J. Whitehouse, J. S. Stacey, F. K. Miller
1992, Journal of Geology (100) 691-701
K-feldspar Pb and whole rock Nd isotopic analyses from 25 Mesozoic and Cenozoic plutonic rocks and two gneisses from NE Washington and northern Idaho are used to elucidate the age and nature of the concealed cratonic basement. The plutons form two highly...
Relationship between inferred redox potential of the depositional environment and geochemistry of the Upper Pennsylvanian (Missourian) Stark Shale Member of the Dennis Limestone, Wabaunsee County, Kansas, U.S.A.
J. R. Hatch, J.S. Leventhal
1992, Chemical Geology (99) 65-82
Analyses of 21 samples collected from a core of the 52.8-cm-thick Stark Shale Member of the Dennis Limestone in Wabaunsee County, Kansas, demonstrate four cycles with two-orders-of-magnitude variations in contents of Cd, Mo, P, V and Zn, and order-of-magnitude variations in contents of organic carbon, Cr, Ni, Se and U....
A systematic approach to modelling the dynamic linkage of climate, physical catchment descriptors and hydrologic response components
A.J. Jakeman, G.M. Hornberger, I.G. Littlewood, P.G. Whitehead, J. W. Harvey, K.E. Bencala
1992, Mathematics and Computers in Simulation (33) 359-366
No abstract available....
Effects of acidic deposition on the erosion of carbonate stone - experimental results from the U.S. National Acid Precipitation Assessment Program (NAPAP)
P. A. Baedecker, M.M. Reddy, K.J. Reimann, C.A. Sciammarella
1992, Conference Paper, Atmospheric Environment - Part B Urban Atmosphere
One of the goals of NAPAP-sponsored research on the effects of acidic deposition on carbonate stone has been to quantify the incremental effects of wet and dry deposition of hydrogen ion, sulfur dioxide and nitrogen oxides on stone erosion. Test briquettes and slabs of freshly quarried Indiana limestone and Vermont...
The effect of rock type, grain size, sorting, permeability, and moisture on measurements of radon in soil gas: A comparison of two measurement techniques
L.C.S. Gundersen
1992, Conference Paper, Journal of Radioanalytical and Nuclear Chemistry
Soil surveys of radon conducted in the Coastal Plain of New Jersey, Alabama and Texas indicate that soil composition and grain size exert the strongest control on the concentration of radon measured. Soil-gas radon was measured in-situ using two techniques; one developed by G. Michael REIMER of the U.S. Geological...
Small scale heterogeneity of Phanerozoic lower crust: evidence from isotopic and geochemical systematics of mid-Cretaceous granulite gneisses, San Gabriel Mountains, southern California
A. P. Barth, J. L. Wooden, D. J. May
1992, Contributions to Mineralogy and Petrology (109) 394-407
An elongate belt of mid-Cretaceous, compositionally banded gneisses and granulites is exposed in Cucamonga terrane, in the southeastern foothills of the San Gabriel Mountains of southern California. Banded gneisses include mafic granulites of two geochemical types: type 1 rocks are similar to high Al arc basalts and andesites but have...
Manganese carbonate mineralization in the Molango district, Mexico
P.M. Okita
1992, Economic Geology (87) 1345-1366
The Molango manganese deposit in Mexico is by far the largest known Mn deposit in North America. Mn carbonate mineralization is hosted by a finely laminated Upper Jurassic marine sedimentary sequence that forms the base of the Chipoco facies of the Taman Formation (Kimmeridgian). Manganese enrichment occurs over a total...
Origin of stratiform sediment-hosted manganese carbonate ore deposits: Examples from Molango, Mexico, and TaoJiang, China
P.M. Okita, Wayne C. Shanks III
1992, Chemical Geology (99) 139-163
Carbonate and sulfide minerals from the Molango, Mexico, and TaoJiang, China, Mn deposits display similar and distinctive ??34S and ??13C patterns in intervals of manganese carbonate mineralization. ??13C-values for Mn-bearing carbonate range from -17.8 to +0.5??? (PDB), with the most negative values occurring in high-grade ore zones that are composed...
Solution properties of almandine-pyrope garnet as determined by phase equilibrium experiments
A.M. Koziol, S.R. Bohlen
1992, American Mineralogist (77) 765-773
The thermodynamic mixing properties of almandine-pyrope garnet were derived from phase equilibrium experiments at temperatures of 900 and 1000??C and pressures from 8 to 14 kbar. Almandine has essentially ideal behavior in almandine-pyrope garnet over the composition range Alm89-Alm61 at the above experimental conditions. In all experimental products a systematic...
Desk-top model buildings for dynamic earthquake response demonstrations
A. Gerald Brady
1992, Conference Paper, NIST Special Publication
Models of buildings that illustrate dynamic resonance behavior when excited by hand are designed and built. Two types of buildings are considered, one with columns stronger than floors, the other with columns weaker than floors. Combinations and variations of these two types are possible. Floor masses and column stiffnesses are...
Arrival times and temporal moments of breakthrough curves for an imperfectly stratified aquifer
R.L. Naff
1992, Water Resources Research (28) 53-68
Using concepts developed in an earlier study, a solution in Laplace transform space is obtained for transport of resident concentration in an imperfectly but yet highly stratified porous medium. The flow field, into which an instantaneous pulse of tracer is injected, is taken to be steady and mean uniform parallel...
Late Pleistocene equilibrium-line reconstructions in the northern Peruvian Andes
D. T. Rodbell
1992, Boreas (21) 43-52
ELA reconstructions using the toe-to-headwall-altitude ratio method for paleoglaciers in the Cordilleras Blanca and Oriental, northern Peruvian Andes indicate that ELAs during the last glacial maximum (LGM; marine isotope stage 2)) were c.4300 m in the Cordillera Blanca, c.3900-3600 m on the west side of the Cordillera Oriental, and c.3200...
Differential tolerance of Sulfolobus strains to transition metals
K.W. Miller, Risanico S. Sass, J.B. Risatti
1992, FEMS Microbiology Letters (93) 69-73
Sulfolobus acidocaldarius strains 98-3 and B12, and S. solfataricus ATCC 35091 were evaluated for tolerance to Cd, Co, Cu, Ni, Zn and Mg. The tolerance of strains 98-3 and ATCC 35091 to these metals was Mg > Zn > Cd > Cu ??? Co > Ni. For B12, however, the...
Code to generate random identifiers and select QA/QC samples
Edward Mehnert
1992, Groundwater (30) 437-439
SAMPLID is a PC-based, FORTH AN-77 code which generates unique numbers for identification of samples, selection of QA/QC samples, and generation of labels. These procedures are tedious, but using a computer code such as SAMPLID can increase efficiency and reduce or eliminate errors and bias....
Volcán Quizapu, Chilean Andes
Wes Hildreth, Robert E. Drake
1992, Bulletin of Volcanology (54) 93-125
Quizapu is a flank vent of the basalt-to-rhyodacite Holocene stratocone, Cerro Azul, and lies at the focus of a complex Quaternary volcanic field on the Andean volcanic front. The Quizapu vent originated in 1846 when 5 km3 of hornblende-dacite magma erupted effusively with little accompanying tephra....
Ground water chemistry and geochemical modeling of water-rock interactions at the Osamu Utsumi mine and the Morro do Ferro analogue study sites, Poços de Caldas, Minas Gerais, Brazil
D. Kirk Nordstrom, R.H. McNutt, I. Puigdomenech, John A.T. Smellie, M. Wolf
1992, Journal of Geochemical Exploration (45) 249-287
Surface and ground waters, collected over a period of three years from the Osamu Utsumi uranium mine and the Morro do Ferro thorium/rare-earth element (Th/REE) deposits, were analyzed and interpreted to identify the major hydrogeochemical processes. These results provided information on the current geochemical evolution of ground...
Toward digital geologic map standards: a progress report
George E. Ulrech, Mitchell W. Reynolds, Richard B. Taylor
1992, Conference Paper, ASTM Special Technical Publication
Establishing modern scientific and technical standards for geologic maps and their derivative map products is vital to both producers and users of such maps as we move into an age of digital cartography. Application of earth-science data in complex geographic information systems, acceleration of geologic map production, and reduction of...
Modeling of ancient climate from deuterium content of water in volcanic glass
I. Friedman, J. Gleason, R. Wilcox, A. Warden
1992, Quaternary International (13-14) 201-203
The explosive nature of the eruptions that produced rhyolitic tephras resulted in the ash being distributed over large areas. This ash, within a few thousand years after deposition, incorporated relatively large amounts of environmental water (up to 3.5%) into the glass structure. This hydration water is shown to retain its...
Garnet/high-silica rhyolite trace element partition coefficients measured by ion microprobe
Thomas W. Sisson, Charles R. Bacon
1992, Geochimica et Cosmochimica Acta (56) 2133-2136
Garnet/liquid trace element partition coefficients have been measured in situ by ion microprobe in a rhyolite from Monache Mountain, California. Partition coefficients are reported for La, Ce, Nd, Sm, Dy, Er, Yb, Sc, Ti, V, Cr, Sr, Y, and Zr. The in situ analyses avoid the problem of contamination of...
Simultaneous parameter estimation and contaminant source characterization for coupled groundwater flow and contaminant transport modelling
B.J. Wagner
1992, Journal of Hydrology (135) 275-303
Parameter estimation and contaminant source characterization are key steps in the development of a coupled groundwater flow and contaminant transport simulation model. Here a methodologyfor simultaneous model parameter estimation and source characterization is presented. The parameter estimation/source characterization inverse model combines groundwater flow and contaminant transport simulation with non-linear maximum...
Increased concentrations of potassium in heartwood of trees in response to groundwater contamination
D.A. Vroblesky, T.M. Yanosky, F.R. Siegel
1992, Environmental Geology and Water Sciences (19) 71-74
The wood of tuliptrees (Liriodendron tulipifera L.) growing above groundwater contamination from a hazardous-waste landfill in Maryland contained elevated concentrations of potassium (K). The groundwater contamination also contained elevated concentrations of dissolved K, as well as arsenic (As), cadmium (Cd), chloride (Cl), iron (Fe), manganese (Mn), zinc (Zn), and organic...
Moment tensors of ten witwatersrand mine tremors
Art McGarr
1992, Pure and Applied Geophysics PAGEOPH (139) 781-800
Ground motions, recorded both underground and on the surface in two of the South African Gold mining districts, were inverted to determine complete moment tensors for 10 mining-induced tremors in the magnitude range 1.9 to 3.3. The resulting moment tensors fall into two separate categories. Seven of the events involve...
Geochemical heterogeneity in a sand and gravel aquifer: Effect of sediment mineralogy and particle size on the sorption of chlorobenzenes
L.B. Barber II, E.M. Thurman, D.R. Runnells
McCalady Donald L., editor(s)
1992, Conference Paper, Journal of Contaminant Hydrology
The effect of particle size, mineralogy and sediment organic carbon (SOC) on solution of tetrachlorobenzene and pentachlorobenzene was evaluated using batch-isotherm experiments on sediment particle-size and mineralogical fractions from a sand and gravel aquifer, Cape Cod, Massachusetts. Concentration of SOC and sorption of chlorobenzenes increase with decreasing particle size. For...
Effect of membrane filtration artifacts on dissolved trace element concentrations
Arthur J. Horowitz, Kent A. Elrick, Mark R. Colberg
1992, Water Research (26) 763-763
Among environment scientists, the current and almost universally accepted definition of dissolved constituents is an operational one; only those materials which pass through a 0.45-??m membrane filter are considered to be dissolved. Detailed laboratory and field studies on Fe and Al indicate that a number of factors associated with filtration,...
Consumption of freons CFC-11 and CFC-12 by anaerobic sediments and soils
Derek R. Lovley, J.C. Woodward
1992, Environmental Science & Technology (26) 925-929
A variety of anaerobic sediments and soils consumed CFC-11 (CFCl3) and CFC-12 (CF2Cl2). An aerobic soil did not. Active microbial metabolism was required for CFC-12 uptake in all of the sediments examined. CFC-11 uptake was faster in the presence of microbial activity, but reduced components in the sediments also resulted...