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Page 1444, results 36076 - 36100

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A climatic-limnologic model of diatom succession for paleolimnological interpretation of varved sediments at Elk Lake, Minnesota
Bradbury J. Platt
1988, Journal of Paleolimnology (1) 115-131
Sediment traps placed in the profundal region of Elk Lake, north central Minnesota during the 1979 spring and 1983-84 fall and spring seasons monitored seasonal diatom production for two climatically distinctive periods. The spring of 1979 was one of the coldest and wettest on record. Ice out at Elk Lake...
Regional assessment of pumpage in southeastern Virginia
Pixie A. Hamilton
1988, Conference Paper
A U.S. Geological Survey investigation was conducted, in cooperation with the Virginia Water Control Board, to analyze the hydrogeology and groundwater flow system in the Coastal Plain physiographic province of southeastern Virginia, and to assess the continued reliability of groundwater as a freshwater resource. To provide a more detailed analysis...
The growth of geological structures by repeated earthquakes 1. Conceptual framework
G.C.P. King, R.S. Stein, J. B. Rundle
1988, Journal of Geophysical Research Solid Earth (93) 13307-13318
In many places, earthquakes with similar characteristics have been shown to recur. If this is common, then relatively small deformations associated with individual earthquake cycles should accumulate over time to create geological structures. Following this paradigm, we show that existing models developed to describe leveling line changes associated with the...
Detection of tannins in modern and fossil barks and in plant residues by high-resolution solid-state 13C nuclear magnetic resonance
M. A. Wilson, Patrick G. Hatcher
1988, Organic Geochemistry (12) 539-546
Bark samples isolated from brown coal deposits in Victoria, Australia, and buried wood from Rhizophora mangle have been studies by high-resolution solid-state nuclear magnetic resonance (NMR) techniques. Dipolar dephasing 13C NMR appears to be a useful method of detecting the presence of tannins in geochemical samples including barks, buried woods, peats and leaf...
Depositional models for two Tertiary coal-bearing sequences in the Powder River Basin, Wyoming, USA
Peter D. Warwick, Ronald W. Stanton
1988, Journal of the Geological Society (145) 613-620
Depositional controls on peat-forming environments which produce thick (>10m) coal beds can be inferred from relationships between coal bed geometry, maceral composition and associated lithologies. Study of these relationships within sedimentary sequences associated with the Wyodak-Anderson (Palaeocene) and the Felix (Eocene) sub-bituminous coal beds in the Powder River Basin,...
Mineral and whole-rock compositions of seawater-dominated hydrothermal alteration at the Arctic volcanogenic massive sulfide prospect, Alaska
J.M. Schmidt
1988, Economic Geology (83) 822-842
The Arctic volcanogenic massive sulfide prospect, located in the Ambler mineral district of northwestern Alaska, includes three types of hydrothermally altered rocks overlying, underlying, and interlayered with semimassive sulfide mineralization. Hydrothermal alteration of wall rocks and deposition of sulfide and gangue minerals were contemporaneous with Late Devonian or Early Mississippian...
Statistical Methods and Sampling Design for Estimating Step Trends in Surface-Water Quality
Robert M. Hirsch
1988, Water Resources Bulletin (24) 493-503
This paper addresses two components of the problem of estimating the magnitude of step trends in surface water quality. The first is finding a robust estimator appropriate to the data characteristics expected in water-quality time series. The J. L. Hodges-E. L. Lehmann class of estimators is found to be robust...
Three-dimensional gravity modeling of the geologic structure of Long Valley caldera
S. F. Carle
1988, Journal of Geophysical Research Solid Earth (93) 13237-13250
A 48-mGal gravity low coincides with Long Valley caldera and is mainly attributed to low-density caldera fill. Gravity measurements by Unocal Geothermal have been integrated with U.S. Geological Survey data, vastly improving gravity station coverage throughout the caldera. A strong regional gravity trend is mainly attributed to isostasy. A “best...
Ostwald ripening and interparticle-diffraction effects for illite crystals
D. D. Eberl, J. Srodon
1988, American Mineralogist (73) 1335-1345
The Warren-Averbach method, an X-ray diffraction (XRD) method used to measure mean particle thickness and particle-thickness distribution, is used to restudy sericite from the Silverton caldera. Apparent particle-thickness distributions indicate that the clays may have undergone Ostwald ripening and that this process has modified the K-Ar ages of the samples....
Near-infrared reflectance spectra of mixtures of kaolin-group minerals: Use in clay mineral studies
James K. Crowley, Norma Vergo
1988, Clays and Clay Minerals (36) 310-316
Near-infrared (NIR) reflectance spectra for mixtures of ordered kaolinite and ordered dickite have been found to simulate the spectral response of disordered kaolinite. The amount of octahedral vacancy disorder in nine disordered kaolinite samples was estimated by comparing the sample spectra to the spectra of reference mixtures. The resulting estimates...
Liquid hydrocarbons probable under Ross Sea
A. K. Cooper, F.J. Davey, K. Hinz
1988, Oil & Gas Journal (86) 118-124
Thick glacial strata, which have no source-rock potential, cover the Ross Sea. If these strata persist to great depths, then hydrocarbon-generation prospects will be poor. Deeply buried strata within Ross Sea rift-grabens, if like other Gondwana rift-deposits, could have good potential for hydrocarbon generation. Current hydrocarbon assessments of the Ross...
Gravity model studies of Newberry Volcano, Oregon
M. E. Gettings, A. Griscom
1988, Journal of Geophysical Research Solid Earth (93) 10109-10118
Newberry Volcano, a large Quaternary volcano located about 60 km east of the axis of the High Cascades volcanoes in central Oregon, has a coincident positive residual gravity anomaly of about 12 mGals. Model calculations of the gravity anomaly field suggest that the volcano is underlain by an intrusive complex...
Mineralization, alteration, and hydrothermal metamorphism of the ophiolite-hosted Turner-Albright sulfide deposit, southwestern Oregon
R.A. Zierenberg, Wayne C. Shanks III, W.E. Seyfried Jr., R.A. Koski, M.D. Strickler
1988, Journal of Geophysical Research Solid Earth (93) 4657-4674
The Turner-Albright sulfide deposit, part of the Josephine ophiolite, formed on and below the seafloor during Late Jurassic volcanism at a back arc spreading center. Ore fluids were probably localized by faults which were active on the seafloor at the time of sulfide deposition. The uppermost massive sulfide formed on...
The chemical evolution of a travertine-depositing stream: Geochemical processes and mass transfer reactions
Michelle M. Lorah, Janet S. Herman
1988, Water Resources Research (24) 1541-1552
This field study focuses on quantitatively defining the chemical changes occurring in Falling Spring Creek, a travertine-depositing stream located in Alleghany County, Virginia. The processes of CO2outgassing and calcite precipitation or dissolution control the chemical evolution of the stream. The observed chemical composition of the water was used with the...
Age and petrology of alkalic postshield and rejuvenated-stage lava from Kauai, Hawaii
D.A. Clague, G. B. Dalrymple
1988, Contributions to Mineralogy and Petrology (99) 202-218
At the top of the Waimea Canyon Basalt on the island of Kauai, rare flows of alkalic postshield-stage hawaiite and mugearite overlie tholeiitic flows of the shield stage. These postshield-stage flows are 3.92 Ma and provide a younger limit for the age of the tholeiitic shield stage. The younger Koloa...
Spatial variation of crustal coda Q in California
W.S. Philips, W.H.K. Lee, J.T. Newberry
1988, Pure and Applied Geophysics PAGEOPH (128) 251-260
Coda wave data from California microearthquakes were studied in order to delineate regional fluctuations of apparent crustal attenuation in the band 1.5 to 24 Hz. Apparent attenuation was estimated using a single back scattering model of coda waves. The coda wave data were restricted to ???30 s following the origin...
Effects of three-dimensional velocity structure on the seismicity of the 1984 Morgan Hill, California, aftershock sequence
A.J. Michael
1988, Bulletin of the Seismological Society of America (78) 1199-1221
A three-dimensional velocity model for the area surrounding the 24 April 1984 Morgan Hill earthquake has been developed by simultaneously inverting local earthquake and refraction arrival-time data. This velocity model corresponds well to the surface geology of the region, predominantly showing a low-velocity region associated with the sedimentary sequence to...
The stress heat-flow paradox and thermal results from Cajon Pass
A.H. Lachenbruch, J.H. Sass
1988, Geophysical Research Letters (15) 981-984
Conventional friction models predict a substantial thermal anomaly associated with active traces of strike-slip faults, but no such anomaly is observed from over 100 heat-flow determinations along 1,000 km of the San Andreas fault. The Cajon Pass well is being drilled to bring deep heat-flow and...
Simulation technique for modeling flow on floodplains and in coastal wetlands
Raymond W. Schaffranek, Robert A. Baltzer
1988, Conference Paper
The system design is premised on a proven, areal two-dimensional, finite-difference flow/transport model which is supported by an operational set of computer programs for input data management and model output interpretation. The purposes of the project are (1) to demonstrate the utility of the model for providing useful highway design...
Determining transit losses for water deliveries by use of stream-aquifer models
Russell K. Livingston
1988, Conference Paper
Hydrologic modeling of stream-aquifer interaction commonly has been used to quantify transit losses associated with water deliveries, such as those from reservoir storage. This technique requires estimation of model parameters that include stage-discharge relations, channel-storage coefficient, aquifer transmissivity, and aquifer-storage coefficient. Because data to reliably estimate or calibrate these parameters...
Tectonic evolution of Gorda Ridge inferred from sidescan sonar images
D.G. Masson, D.A. Cacchione, D.E. Drake
1988, Marine Geophysical Research (10) 191-204
Gorda Ridge is the southern segment of the Juan de Fuca Ridge complex, in the north-east Pacific. Along-strike spreading-rate variation on Gorda Ridge and deformation of Gorda Plate are evidence for compression between the Pacific and Gorda Plates. GLORIA sidescan sonographs allow the spreading fabric associated with Gorda Ridge to...
An oxygen isotope and geochemical study of meteoric-hydrothermal systems at Pilot Mountain and selected other localities, Carolina slate belt
T. L. Klein, R.E. Criss
1988, Economic Geology (83) 801-821
Several epigenetic mineral deposits in the Ca1rolina slate belt are intimately related to meteoric-hydrothermal systems of late Precambrian and early Paleozoic age. At Pilot Mountain, low 18 O rocks correlate well with zones of strong silicic alteration and alkali leaching accompanied by high alumina minerals (sericite, pyrophyllite, andalusite + or - topaz)...
Isotopic evidence for organic matter oxidation by manganese reduction in the formation of stratiform manganese carbonate ore
P.M. Okita, J.B. Maynard, E.C. Spiker, E. R. Force
1988, Geochimica et Cosmochimica Acta (52) 2679-2685
Unlike other marine-sedimentary manganese ore deposits, which are largely composed of manganese oxides, the primary ore at Molango (Hidalgo State, Mexico) is exclusively manganese carbonate (rhodochrosite, Mn-calcite, kutnahorite). Stable isotope studies of the carbonates from Molango provide critical new information relevant to the controversy over syngenetic and diagenetic models of...
A statistical method for estimating rates of soil development and ages of geologic deposits: A design for soil-chronosequence studies
P. Switzer, J.W. Harden, R. K. Mark
1988, Mathematical Geology (20) 49-61
A statistical method for estimating rates of soil development in a given region based on calibration from a series of dated soils is used to estimate ages of soils in the same region that are not dated directly. The method is designed specifically to account for sampling procedures and uncertainties...