Evidence for multiple mechanisms of crustal contamination of magma from compositionally zoned plutons and associated ultramafic intrusions of the Alaska Range
P.W. Reiners, B.K. Nelson, S.W. Nelson
1996, Journal of Petrology (37) 261-292
Models of continental crustal magmagenesis commonly invoke the interaction of mafic mantle-derived magma and continental crust to explain geochemical and petrologic characteristics of crustal volcanic and plutonic rocks. This interaction and the specific mechanisms of crustal contamination associated with it are poorly understood. An excellent opportunity to study the...
Near bottom velocity measurements in San Francisco Bay, California
Jeffrey W. Gartner, Ralph T. Cheng
Anon, editor(s)
1996, Conference Paper, Oceans Conference Record (IEEE)
The ability to accurately measure long-term time-series of tidal currents in bays and estuaries is critical in estuarine hydrodynamic studies. Accurate measurements of tidal currents near the air-water interface and in the bottom boundary layer remain difficult in spite of the significant advances in technology for measuring tidal currents which...
A digital photogrammetric method for measuring horizontal surficial movements on the slumgullion earthflow, Hinsdale county, Colorado
P. S. Powers, M. Chiarle, W. Z. Savage
1996, Computers & Geosciences (22) 651-663
The traditional approach to making aerial photographic measurements uses analog or analytic photogrammetric equipment. We have developed a digital method for making measurements from aerial photographs which uses geographic information system (GIS) software, and primarily DOS-based personal computers. This method, which is based on the concept that a direct visual...
Earthquake mechanisms from linear-programming inversion of seismic-wave amplitude ratios
B.R. Julian, G.R. Foulger
1996, Bulletin of the Seismological Society of America (86) 972-980
The amplitudes of radiated seismic waves contain far more information about earthquake source mechanisms than do first-motion polarities, but amplitudes are severely distorted by the effects of heterogeneity in the Earth. This distortion can be reduced greatly by using the ratios of amplitudes...
A resource evaluation of the Bakken Formation (Upper Devonian and Lower Mississippian) continuous oil accumulation, Williston Basin, North Dakota and Montana
J. W. Schmoker
1996, Mountain Geologist (33) 1-10
The Upper Devonian and Lower Mississippian Bakken Formation in the United States portion of the Williston Basin is both the source and the reservoir for a continuous oil accumulation - in effect a single very large field - underlying approximately 17,800 mi2 (46,100 km2) of North Dakota and Montana. Within...
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...
Role of stress triggering in earthquake migration on the North Anatolian fault
R.S. Stein, James H. Dieterich, A.A. Barka
1996, Physics and Chemistry of the Earth (21) 225-230
Ten M???6.7 earthquakes ruptured 1,000 km of the North Anatolian fault (Turkey) during 1939-92, providing an unsurpassed opportunity to study how one large shock sets up the next. Calculations of the change in Coulomb failure stress reveal that 9 out of 10 ruptures were brought closer to failure by the...
Crustal shear-wave splitting from local earthquakes in the Hengill triple junction, southwest Iceland
J.R. Evans, G.R. Foulger, B.R. Julian, A.D. Miller
1996, Geophysical Research Letters (23) 455-458
The Hengill region in SW Iceland is an unstable ridge-ridge-transform triple junction between an active and a waning segment of the mid-Atlantic spreading center and a transform that is transgressing southward. The triple junction contains active and extinct spreading segments and a widespread geothermal area. We...
Climatic control of nitrate loss from forested watersheds in the northeast United States
M.J. Mitchell, C. T. Driscoll, J. S. Kahl, G.E. Likens, Peter S. Murdoch, L.H. Pardo
1996, Environmental Science & Technology (30) 2609-2612
Increased losses of nitrate from watersheds may accelerate the depletion of nutrient cations and affect the acidification and trophic status of surface waters. Patterns of nitrate concentrations and losses were evaluated in four forested watersheds (East Bear Brook Watershed, Lead Mountain, ME; Watershed 6, Hubbard Brook Experimental Forest, White Mountains,...
Cyanazine, atrazine, and their metabolites as geochemical indicators of contaminant transport in the Mississippi River
M. T. Meyer, E.M. Thurman, D. A. Goolsby
1996, ACS Symposium Series (630) 288-302
The geochemical transport of cyanazine and its metabolite cyanazine amide (CAM) was compared to atrazine and its metabolite deethylatrazine (DEA) at three sites in the Mississippi River basin during 1992 and six sites during 1993. The floods of 1993 caused an uninterrupted exponential decline in herbicide concentrations; whereas, in 1992...
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...
Effects of winter atmospheric circulation on temporal and spatial variability in annual streamflow in the western United States
G. J. McCabe Jr.
1996, Hydrological Sciences Journal (41) 873-887
Winter mean 700-hectoPascal (hPa) height anomalies, representing the average atmospheric circulation during the snow season, are compared with annual streamflow measured at 140 streamgauges in the western United States. Correlation and anomaly pattern analyses are used to identify relationships between winter mean atmospheric circulation and temporal and spatial variability in...
Limestone characterization to model damage from acidic precipitation: Effect of pore structure on mass transfer
S.D. Leith, M.M. Reddy, W.F. Irez, M.J. Heymans
1996, Environmental Science & Technology (30) 2202-2210
The pore structure of Salem limestone is investigated, and conclusions regarding the effect of the pore geometry on modeling moisture and contaminant transport are discussed based on thin section petrography, scanning electron microscopy, mercury intrusion porosimetry, and nitrogen adsorption analyses. These investigations are compared to and shown to compliment permeability...
Settlement patterns reflected in assemblages from the Pleistocene/Holocene transition of North Central China
D.B. Madsen, R. G. Elston, R. L. Bettinger, C. Xu, K. Zhong
1996, Journal of Archaeological Science (23) 217-231
Survey along the margins of the Helan Mountains in the Ningxia Hui and Nei Mongol Autonomous Regions discloses variability in the distribution and assemblage composition among 47 archaeological localities, and suggests a reduction in hunter-gatherer residential mobility through time. Late Palaeolithic tool assemblages are less frequent, smaller, and relatively uniform...
Raman spectroscopic characterization of gas mixtures. II. Quantitative composition and pressure determination of the CO2-CH4 system
J. C. Seitz, J. D. Pasteris, I.-M. Chou
1996, American Journal of Science (296) 577-600
Raman spectral parameters were determined for the v1 band of CH4 and the v1 and 2v2 bands (Fermi diad) of CO2 in pure CO2 and CO2-CH4 mixtures at pressures up to 700 bars and room temperature. Peak position, area, height, and width were investigated as functions of pressure and composition....
Global distribution of plant-extractable water capacity of soil
K.A. Dunne, C.J. Willmott
1996, International Journal of Climatology (16) 841-859
Plant-extractable water capacity of soil is the amount of water that can be extracted from the soil to fulfill evapotranspiration demands. It is often assumed to be spatially invariant in large-scale computations of the soil-water balance. Empirical evidence, however, suggests that this assumption is incorrect. In this paper, we estimate...
Interpreting the ASTM 'content standard for digital geospatial metadata'
Douglas D. Nebert
1996, Conference Paper, ASTM Special Technical Publication
ASTM and the Federal Geographic Data Committee have developed a content standard for spatial metadata to facilitate documentation, discovery, and retrieval of digital spatial data using vendor-independent terminology. Spatial metadata elements are identifiable quality and content characteristics of a data set that can be tied to a geographic location or...
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...
Quiescent-phase evolution of a surge-type glacier: Black Rapids Glacier, Alaska, U.S.A.
T.A. Heinrichs, L.R. Mayo, K.A. Echelmeyer, W.D. Harrison
1996, Journal of Glaciology (42) 110-122
Black Rapids Glacier, a surge-type glacier in the Alaska Range, most recently surged in 1936–37 and is currently in its quiescent phase. Mass balance, ice velocity and thickness change have been measured at three to ten sites from 1972 to 1994. The annual speed has undergone cyclical...
Observations and analysis of self-similar branching topology in glacier networks
D.B. Bahr, S.D. Peckham
1996, Journal of Geophysical Research B: Solid Earth (101) 25511-25521
Glaciers, like rivers, have a branching structure which can be characterized by topological trees or networks. Probability distributions of various topological quantities in the networks are shown to satisfy the criterion for self-similarity, a symmetry structure which might be used to simplify future models of glacier dynamics. Two analytical methods...
Rare, large earthquakes at the laramide deformation front - Colorado (1882) and Wyoming (1984)
W. Spence, C.J. Langer, G. L. Choy
1996, Bulletin of the Seismological Society of America (86) 1804-1819
The largest historical earthquake known in Colorado occurred on 7 November 1882. Knowledge of its size, location, and specific tectonic environment is important for the design of critical structures in the rapidly growing region of the Southern Rocky Mountains. More than one century later, on 18 October 1984, an mb 5.3 earthquake...
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...
Recent volcanism in the Siqueiros transform fault: Picritic basalts and implications for MORB magma genesis
M.R. Perfit, D.J. Fornari, W.I. Ridley, P.D. Kirk, John F. Casey, K.A. Kastens, J.R. Reynolds, M. Edwards, D. Desonie, R. Shuster, S. Paradis
1996, Earth and Planetary Science Letters (141) 91-108
Small constructional volcanic landforms and very fresh-looking lava flows are present along one of the inferred active strike-slip faults that connect two small spreading centers (A and B) in the western portion of the Siqueiros transform domain. The most primitive lavas (picritic and olivine-phyric basalts), exclusively recovered from the young-looking...
Reactive solute transport in an acidic stream: Experimental pH increase and simulation of controls on pH, aluminum, and iron
R. E. Broshears, R.L. Runkel, B. A. Kimball, Diane M. McKnight, K.E. Bencala
1996, Environmental Science & Technology (30) 3016-3024
Solute transport simulations quantitatively constrained hydrologic and geochemical hypotheses about field observations of a pH modification in an acid mine drainage stream. Carbonate chemistry, the formation of solid phases, and buffering interactions with the stream bed were important factors in explaining the behavior of pH, aluminum, and iron. The precipitation...