Three-dimensional crustal structure of the southern Sierra Nevada from seismic fan profiles and gravity modeling
M.M. Fliedner, S. Ruppert, P.E. Malin, S. K. Park, G. Jiracek, R. A. Phinney, J.B. Saleeby, B. Wernicke, R. Clayton, Rebecca Hylton Keller, K. Miller, C. Jones, J.H. Luetgert, Walter D. Mooney, H. Oliver, S.L. Klemperer, G. A. Thompson
1996, Geology (24) 367-370
Traveltime data from the 1993 Southern Sierra Nevada Continental Dynamics seismic refraction experiment reveal low crustal velocities in the southern Sierra Nevada and Basin and Range province of California (6.0 to 6.6 km/s), as well as low upper mantle velocities (7.6 to 7.8 km/s). The crust thickens from southeast to...
Metasomatic tourmalinite formation along basement-cover decollements, Orobic Alps, Italy
J. F. Slack, C.W. Passchier, J.S. Zhang
1996, Schweizerische Mineralogische und Petrographische Mitteilungen (76) 193-207
Cryptocrystalline tourmalinites that occur discontinuously for ???30 km along basement-cover de??collements of the Orohic Alps (Italy) formed by the metasomatism of aluminous cataclasites derived from Permian conglomerates and/or feldspathic sandstones. Using Al as an immobile element monitor, calculations show that the majority of tourmalinites in the region formed through the...
Kinetic determinations of trace element bioaccumulation in the mussel Mytilus edulis
W.-X. Wang, N.S. Fisher, S. N. Luoma
1996, Marine Ecology Progress Series (140) 91-113
Laboratory experiments employing radiotracer methodology were conducted to determine the assimilation efficiencies from ingested natural seston, the influx rates from the dissolved phase and the efflux rates of 6 trace elements (Ag, Am, Cd, Co, Se and Zn) in the mussel Mytilus edulis. A kinetic model was then employed to...
Hydrogeologic controls on the groundwater interactions with an acidic lake in karst terrain, Lake Barco, Florida
T. M. Lee
1996, Water Resources Research (32) 831-844
Transient groundwater interactions and lake stage were simulated for Lake Barco, an acidic seepage lake in the mantled karst of north central Florida. Karst subsidence features affected groundwater flow patterns in the basin and groundwater fluxes to and from the lake. Subsidence features peripheral to the lake intercepted potential groundwater...
Three-dimensional models of deformation near strike-slip faults
Uri S. ten Brink, Rafael Katzman, J. Lin
1996, Journal of Geophysical Research B: Solid Earth (101) 16205-16220
We use three-dimensional elastic models to help guide the kinematic interpretation of crustal deformation associated with strike-slip faults. Deformation of the brittle upper crust in the vicinity of strike-slip fault systems is modeled with the assumption that upper crustal deformation is driven by the relative plate motion in the upper...
Modern benthic foraminifer distribution in the Amerasian Basin, Arctic Ocean
S. E. Ishman, K.M. Foley
1996, Micropaleontology (42) 206-220
A total of 38 box cores were collected from the Amerasian Basin, Arctic Ocean during the U.S. Geological Survey 1992 (PI92-AR) and 1993 (PI93-AR) Arctic Cruises aboard the U.S. Coast Guard Icebreaker Polar Star. In addition, the cruises collected geophysical data, piston cores and hydrographic data to address the geologic...
Slip history of the 1995 Kobe, Japan, earthquake determined from strong motion, teleseismic, and geodetic data
D.J. Wald
1996, Journal of Physics of the Earth (44) 489-503
Near-source ground motions, teleseismic body waveforms, and geodetic displacements produced by the 1995 Kobe, Japan, earthquake have been used to determine the spatial and temporal dislocation pattern on the faulting surfaces. A linear, least-squares approach was used to invert the data sets both independently and in unison in order to...
The alteration of rhyolite in CO2 charged water at 200 and 350°C: The unreactivity of CO2 at higher temperature
James L. Bischoff, Robert J. Rosenbauer
1996, Geochimica et Cosmochimica Acta (60) 3859-3867
Geochemical and hydrologic modeling indicates that geothermal waters in the T > 270°C reservoirs beneath Yellowstone National Park have HCO3 ≪ Cl and contrast with waters in reservoirs at lower temperatures which attain HCO3 about equal to Cl. Experiments reacting rhyolite with 0.5 molal solutions of CO2 at 200°...
Using remote sensing and GIS techniques to estimate discharge and recharge. fluxes for the Death Valley regional groundwater flow system, USA
F. A. D’Agnese, C.C. Faunt, Turner A. Keith
1996, IAHS-AISH Publication 503-511
The recharge and discharge components of the Death Valley regional groundwater flow system were defined by remote sensing and GIS techniques that integrated disparate data types to develop a spatially complex representation of near-surface hydrological processes. Image classification methods were applied to multispectral satellite data to produce a vegetation map....
Shallow subsurface geology of part of the Savannah River alluvial valley in the upper Coastal Plain of Georgia and South Carolina
D.C. Leeth, D.D. Nagle
1996, Southeastern Geology (36) 1-14
The depth to which Coastal Plain rivers incise underlying formations is an important control on local and regional hydrologic flow systems. In order to clarify these stream/aquifer relations, a better understanding of the shallow subsurface geology of the Savannah River was necessary. To accomplish this, three drillhole transects were completed...
Block and shear-zone architecture of the Minnesota River Valley subprovince: Implications for late Archean accretionary tectonics
D. L. Southwick, V.W. Chandler
1996, Canadian Journal of Earth Sciences (33) 831-847
The Minnesota River Valley subprovince of the Superior Province is an Archean gneiss terrane composed internally of four crustal blocks bounded by three zones of east-northeast-trending linear geophysical anomalies. Two of the block-bounding zones are verified regional-scale shears. The geological nature of the third boundary has not been established. Potential-field...
Kinematics of the Eastern California shear zone: Evidence for slip transfer from Owens and Saline Valley fault zones to Fish Lake Valley fault zone
M.C. Reheis, T.H. Dixon
1996, Geology (24) 339-342
Late Quaternary slip rates and satellite-based geodetic data for the western Great Basin constrain regional fault-slip distribution and evolution. The geologic slip rate on the Fish Lake Valley fault zone (the northwest extension of the Furnace Creek fault zone) increases northward from about...
Implications of fault constitutive properties for earthquake prediction
James H. Dieterich, B. Kilgore
1996, Conference Paper, Proceedings of the National Academy of Sciences of the United States of America
The rate- and state-dependent constitutive formulation for fault slip characterizes an exceptional variety of materials over a wide range of sliding conditions. This formulation provides a unified representation of diverse sliding phenomena including slip weakening over a characteristic sliding distance D(c), apparent fracture energy at a rupture front, time- dependent...
Semivariogram modeling by weighted least squares
X. Jian, Ricardo A. Olea, Y.-S. Yu
1996, Computers & Geosciences (22) 387-397
Permissible semivariogram models are fundamental for geostatistical estimation and simulation of attributes having a continuous spatiotemporal variation. The usual practice is to fit those models manually to experimental semivariograms. Fitting by weighted least squares produces comparable results to fitting manually in less time, systematically, and provides an Akaike information criterion...
Granular-flow rheology: Role of shear-rate number in transition regime
Chiu-Lan Chen, C. #NAME? Ling
1996, Journal of Engineering Mechanics (122) 469-479
This paper examines the rationale behind the semiempirical formulation of a generalized viscoplastic fluid (GVF) model in the light of the Reiner-Rivlin constitutive theory and the viscoplastic theory, thereby identifying the parameters that control the rheology of granular flow. The shear-rate number ( N ) proves to be among the most significant...
Groundwater inflow measurements in wetland systems
Randy J. Hunt, David P. Krabbenhoft, Mary P. Anderson
1996, Water Resources Research (32) 495-507
Our current understanding of wetlands is insufficient to assess the effects of past and future wetland loss. While knowledge of wetland hydrology is crucial, groundwater flows are often neglected or uncertain. In this paper, groundwater inflows were estimated in wetlands in southwestern Wisconsin using traditional Darcy's law calculations and three...
Reactive solute transport in acidic streams
R. E. Broshears
1996, Water, Air, & Soil Pollution (90) 195-204
Spatial and temporal profiles of Ph and concentrations of toxic metals in streams affected by acid mine drainage are the result of the interplay of physical and biogeochemical processes. This paper describes a reactive solute transport model that provides a physically and thermodynamically quantitative interpretation of these profiles. The model...
Climate change and northern prairie wetlands: Simulations of long-term dynamics
Karen A. Poiani, W. Carter Johnson, George A. Swanson, Thomas C. Winter
1996, Limnology and Oceanography (41) 871-881
A mathematical model (WETSIM 2.0) was used to simulate wetland hydrology and vegetation dynamics over a 32-yr period (1961–1992) in a North Dakota prairie wetland. A hydrology component of the model calculated changes in water storage based on precipitation, evapotranspiration, snowpack, surface runoff, and subsurface inflow. A spatially explicit vegetation...
Diagenesis, compaction, and fluid chemistry modeling of a sandstone near a pressure seal: Lower Tuscaloosa Formation, Gulf Coast
Suzanne Weedman, Susan L. Brantley, R. Shiraki, Simon R. Poulson
1996, American Association of Petroleum Geologists Bulletin (80) 1045-1063
Petrographic, isotopic, and fluid-inclusion evidence from normally and overpressured sand-stones of the lower Tuscaloosa Formation (Upper Cretaceous) in the Gulf Coast documents quartz-overgrowth precipitation at 90°C or less, calcite cement precipitation at approximately 100° and 135°C, and prismatic quartz cement precipitation at about 125°C. Textural evidence suggests that carbonate cement...
Genetic characteristics of fluid inclusions in sphalerite from the Silesian-Cracow ores, Poland
A. Kozlowski, D. L. Leach, J.G. Viets
1996, Prace - Panstwowego Instytutu Geologicznego (154) 72-84
Fluid inclusion studies in sphalerite from early-stage Zn-Pb mineralization in the Silesian-Cracow region (southern Poland), yielded homogenization temperatures (Th) from 80 to 158??C. Vertical thermal gradient of the parent fluids was 6 to 10??C, and the ore crystallization temperature ranges varied from <10??C at deep levels to 25??C at shallow...
Upscaled soil-water retention using van Genuchten's function
T.R. Green, J.E. Constantz, D.L. Freyberg
1996, Journal of Hydrologic Engineering (1) 123-130
Soils are often layered at scales smaller than the block size used in numerical and conceptual models of variably saturated flow. Consequently, the small-scale variability in water content within each block must be homogenized (upscaled). Laboratory results have shown that a linear volume average (LVA) of water content at a...
Integrating a geographic information system, a scientific visualization system and an orographic precipitation model
L. Hay, L. Knapp
1996, IAHS-AISH Publication 123-131
Investigating natural, potential, and man-induced impacts on hydrological systems commonly requires complex modelling with overlapping data requirements, and massive amounts of one- to four-dimensional data at multiple scales and formats. Given the complexity of most hydrological studies, the requisite software infrastructure must incorporate many components including simulation modelling, spatial analysis...
Amplitude blanking in seismic profiles from Lake Baikal
Myung W. Lee, Warren F. Agena, D. R. Hutchinson
1996, Marine and Petroleum Geology (13) 549-563
Imaging of the deepest sedimentary section in Lake Baikal using multichannel seismic profiling was hampered by amplitude blanking that is regionally extensive, is associated with water depths greater than about 900 m and occurs at sub-bottom depths of 1-2 km in association with the first water-bottom multiple. Application of a...
Estimation of the potential for atrazine transport in a silt loam soil
D. A. V. Eckhardt, R. J. Wagenet
1996, ACS Symposium Series (630) 101-116
The transport potential of the herbicide atrazine (2-chloro-4-ethyl-6-isopropyl-s-triazine) through a 1-meter-thick root zone of corn (Zea mays L.) in a silty-loam soil in Kansas was estimated for a 22-year period (1972-93) using the one-dimensional water-flow and solute-transport model LEACHM. Results demonstrate that, for this soil, atrazine transport is directly related to...
Experimental investigation and modeling of uranium (VI) transport under variable chemical conditions
M. Kohler, G.P. Curtis, D.B. Kent, J.A. Davis
1996, Water Resources Research (32) 3539-3551
The transport of adsorbing and complexing metal ions in porous media was investigated with a series of batch and column experiments and with reactive solute transport modeling. Pulses of solutions containing U(VI) were pumped through columns filled with quartz grains, and the breakthrough of U(VI) was studied as a function...