Oxygen-isotope composition of ground water and secondary minerals in Columbia Plateau basalts: Implications for the paleohydrology of the Pasco Basin
P.P. Hearn Jr., W.C. Steinkampf, D. G. Horton, G.C. Solomon, L. D. White, J.R. Evans
1989, Geology (17) 606-610
Concentrations of 18O and deuterium in ground waters beneath the Hanford Reservation, Washington State, suggest that the meteoric waters recharging the basalt aquifers have been progressively depleted in these isotopes since at least Pleistocene time. This conclusion is supported by oxygen-isotope analyses of low-temperature...
Trace metal associations in the water column of South San Francisco Bay, California
J.S. Kuwabara, Cecily C.Y. Chang, J. E. Cloern, T. L. Fries, J.A. Davis, S. N. Luoma
1989, Estuarine, Coastal and Shelf Science (28) 307-325
Spatial distributions of copper (Cu), zinc (Zn) and cadmium (Cd) were followed along a longitudinal gradient of dissolved organic carbon (DOC) in South San Francisco Bay (herein referred to as the South Bay). Dissolved Cu, Zn and Cd concentrations ranged from 24 to...
Pockmarks in the floor of Penobscot Bay, Maine
Kathryn M. Scanlon, Harley J. Knebel
1989, Geo-Marine Letters (9) 53-58
Hundreds of depressions (pockmarks) were found within a 40 square kilometer area of the sea floor near the head of Penobscot Bay, Maine. These roughly circular depressions range in diameter from 10 to 300 meters and extend as much as 30 meters below the surrounding sea floor. The pockmarks have...
Uranium-series nuclides in the Golden fault, Colorado, U.S.A.: Dating latest fault displacement and measuring recent uptake of radionuclides by fault-zone materials
Barney J. Szabo, J.N. Rosholt
1989, Applied Geochemistry (4) 177-182
Concentrations and isotopic ratios of U, Th and Ra were measured in a fault zone near Golden, Colorado where major displacement occurred between about 190 and 615 ka. Faulting created new surfaces for leaching and provided the pathways for U-rich ground...
The geology, botany and chemistry of selected peat-forming environments from temperate and tropical latitudes
C. C. Cameron, J.S. Esterle, C.A. Palmer
1989, International Journal of Coal Geology (12) 105-156
Peat has been studied in several geologic settings: (1) glaciated terrain in cold temperate Maine and Minnesota, U.S.A.; (2) an island in the Atlantic Ocean off the coast of Maine, where sea level is rising; (3) the warm temperate U.S. Atlantic...
Introduction to the hydrogeochemical investigations within the International Stripa Project
D. Kirk Nordstrom, T. Olsson, L. Carlsson, P. Fritz
1989, Geochimica et Cosmochimica Acta (53) 1717-1726
The International Stripa Project (1980-1990) has sponsored hydrogeochemical investigations at several subsurface drillholes in the granitic portion of an abandoned iron ore mine, central Sweden. The purpose has been to advance our understanding of geochemical processes in crystalline bedrock that may affect the safety assessment of high-level radioactive waste repositories....
Diapiric transfer of melt in Kilauea Iki lava lake, Hawaii: A quick, efficient process of igneous differentiation
Rosalind Tuthill Helz, H. Kirschenbaum, J.W. Marinenko
1989, Geological Society of America Bulletin (101) 578-594
Kilauea Iki lava lake, formed in 1959, is a large pond of picritic basalt (average MgO content = 15.34% by weight), which has cooled and crystallized as a small, self-roofed magma chamber. Repeated drilling of the upper crust of the lake, down to its molten core, and more recent (1981)...
A note on the occurrence of allocrioceras billinghursti Klinger, 1976 (Cretaceous Ammonoidea) in the Middle Turonian of the Western Interior of the United States
W. A. Cobban, W. J. Kennedy
1989, Cretaceous Research (10) 173-175
No abstract available....
A direct correlation among indoor Rn, soil gas Rn and geology in the Reading Prong near Boyertown, Pennsylvania
G.M. Reimer, L.C.S. Gundersen
1989, Health Physics (57) 155-160
We feel that this study suggests a relationship among geology, soil gas Rn and the potential for indoor Rn accumulation in this portion of the Reading Prong. There are deviations from a perfect correlation but these are related to inhomogeneities in the geologic environment and perhaps variations in construction techniques...
Spatial and temporal variability in South San Francisco Bay (USA). I. Horizontal distributions of salinity, suspended sediments, and phytoplankton biomass and productivity
T.M. Powell, J. E. Cloern, L.M. Huzzey
1989, Estuarine, Coastal and Shelf Science (28) 583-597
The horizontal pattern of mesoscale (1–4 km) variability in salinity was a poor predictor of mesoscale patterns in chlorophyll a, suspended particulate matter, and daily primary productivity in the South San Francisco Bay estuary during spring 1987. The tidally-averaged salinity distribution varied over weekly time scales, reflecting inputs of freshwater as...
A thrust-ridge paleodepositional model for the Upper Freeport coal bed and associated clastic facies, Upper Potomac coal field, Appalachian basin, U.S.A.
Edward S. Belt, P.C. Lyons
1989, International Journal of Coal Geology (12) 293-328
A blind-thrust-ridge model is proposed to explain the lack of coarse clastic material in the vast minable Upper Freeport coal bed (UF). This coal bed contains only fine elastic partings and is overlain by regionally extensive, closely spaced channel-belt deposits in...
Surface faulting: A preliminary view
R. V. Sharp
1989, Earthquake Spectra (5) 13-22
This description of surface faulting near Spitak, Armenia, is based on a field inspection made December 22-26, 1988. The surface rupture west of Spitak, displacement of the ground surface, pre-earthquake surface expressions of the fault, and photolineaments in landsat images are described and surface faulting is compared to aftershocks. It...
Lagoonal deposits in the Upper Cretaceous Rock Springs Formation (Mesaverde Group), southwest Wyoming
M.A. Kirschbaum
1989, Marine Geology (88) 349-364
Most paleogeographic reconstructions of the Rock Springs Formation show shorelines having lobate to arcuate deltas. These shorelines are oriented NE-SW, with the sea to the southeast. Brackish-water bodies are usually shown in interdistributary areas or associated with abandoned delta lobes, and are open to the sea. In this study,...
Sea-floor observations in the tongue of the ocean, Bahamas: An Argo/SeaMARC survey
W. C. Schwab, E. Uchupi, Richard D. Ballard, T.K. Dettweiler
1989, Geo-Marine Letters (9) 171-178
SeaMARC side-scan sonographs and Argo video and photographic data suggest that the recent sedimentary environment of the floor of the Tongue of the Ocean is controlled by an interplay of turbidity current flow from the south, sediment spill-over from the carbonate platform to the east (windward side), and rock falls...
Changes in floral diversities, floral turnover rates, and climates in Campanian and Maastrichtian time, North Slope of Alaska
N. O. Frederiksen
1989, Cretaceous Research (10) 249-266
One-hundred-and-ten angiosperm pollen taxa have been found in upper Campanian to Masstrichtian rocks of the Colville River region, North Slope of Alaska. These are the highest paleolatitude Campanian and Maastrichtian floras known from North America. Total angiosperm pollen diversity rose during the Campanian and declined toward the end of the...
A record of Appalachian denudation in postrift Mesozoic and Cenozoic sedimentary deposits of the U.S. Middle Atlantic continental margin
C. W. Poag, W. D. Sevon
1989, Geomorphology (2) 119-157
The complex interplay between source-terrain uplift, basin subsidence, paleoclimatic shifts, and sea-level change, left an extensive sedimentary record in the contiguous offshore basins of the U.S. middle Atlantic margin (Salisbury Embayment, Baltimore Canyon Trough, and Hatteras Basin). Isopach maps of 23 postrift...
Simulation of calcite dissolution and porosity changes in saltwater mixing zones in coastal aquifers
Ward E. Sanford, Leonard F. Konikow
1989, Water Resources Research (25) 655-667
Thermodynamic models of aqueous solutions have indicated that the mixing of seawater and calcite-saturated fresh groundwater can produce a water that is undersaturated with respect to calcite. Mixing of such waters in coastal carbonate aquifers could lead to significant amounts of limestone dissolution. The potential for such dissolution in coastal...
Preliminary evaluations of regional ground-water quality in relation to land use
D. Cain, D.R. Helsel, S.E. Ragone
1989, Ground Water (27) 230-244
Preliminary results from New York, New Jersey, Connecticut, Florida, Nebraska, and Colorado indicate that regional ground-water quality has been affected by human activities. The frequencies of detection of volatile organic compounds and some trace elements were larger in ground water underlying urban or industrial areas in comparison to undeveloped areas....
Comparison of geoelectrical/tectonic models for suture zones in the western U.S.A. and eastern Europe: are black shales a possible source of high conductivities?
W. D. Stanley
1989, Physics of the Earth and Planetary Interiors (53) 228-238
Large-scale geoelectrical anomalies have been mapped with geomagnetic depth sounding (GDS) and magnetotelluric (MT) surveys in the Carpathian Mountains region. These anomalies are associated with the zone of closure between stable Europe and a complex of microplates in front of the converging African plate. The zone of closure, or suture...
A comparison of instrumental dewatering methods for the separation and concentration of suspended sediment for subsequent trace element analysis
A. J. Horowitz, K. A. Elrick, R.C. Hooper
1989, Hydrological Processes (3) 163-184
A comparison involving both field and laboratory trials was performed to evaluate the utility of two continuous-flow centrifuges and a tangential-flow filtration system for dewatering suspended sediments for subsequent trace element analysis. Although recovery efficiencies for the various devices differ, the analytical results from the...
Determination of sensible heat flux over sparse canopy using thermal infrared data
William P. Kustas, B. J. Choudhury, M. S. Moran, R. J. Reginato, R. D. Jackson, L. W. Gay, H. L. Weaver
1989, Agricultural and Forest Meteorology (44) 197-216
Surface temperatures, Ts, were estimated for a natural vegetative surface in Owens Valley, California, with infrared thermometric observations collected from an aircraft. The region is quite arid and is composed primarily of bushes (∼30%) and bare soil (∼70%). Application of the bulk transfer equation for the estimation of sensible heat, H, gave...
Processing and attenuation of noise in deep seismic-reflection data from the Gulf of Maine
D. R. Hutchinson, Myung W. Lee
1989, Marine Geophysical Research (11) 51-67
The U.S. Geological Survey deep crustal studies reflection profile across the Gulf of Maine off southeastern New England was affected by three sources of noise: side-scattered noise, multiples, and 20-Hz whale sounds. The special processing most effective in minimizing this noise consisted of a combination of frequency-wavenumber (F-K) filtering, predictive...
The separation of the Hartland Formation and Ravenswood Granodiorite from the Fordham Gneiss at Cameron's Line in the New York City area
C.A. Baskerville, D.G. Mose
1989, Northeastern Geology (11) 22-28
Recent study of the rocks in City Water Tunnel Number 3 between Roosevelt Island and beneath 34th Street and the 63rd Street subway-rail tunnels at 41st Avenue in Long Island City, as well as study of drill core from other sites in western Queens, establishes that this area of New...
Chemical hydrogeology in natural and contaminated environments
W. Back, M.J. Baedecker
1989, Journal of Hydrology (106) 1-28
Chemical hydrogeology, including organic and inorganic aspects, has contributed to an increased understanding of groundwater flow systems, geologic processes, and stressed environments. Most of the basic principles of inorganic-chemical hydrogeology were first established by investigations of organic-free, regional-scale systems for which simplifying assumptions could be made. The problems of groundwater...
Basin-scale relations via conditioning
B.M. Troutman, M.R. Karlinger, D.P. Guertin
1989, Stochastic Hydrology and Hydraulics (3) 111-133
A rainfall-runoff model is used in conjunction with a probabilistic description of the input to this model to obtain simple regression-like relations for basin runoff in terms of basin and storm characteristics. These relations, similar to those sought in regionalization studies, are computed by evaluating the conditional distribution of model...