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Page 1512, results 37776 - 37800

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Not all publications have extents, not all extents are completely accurate
U-Pb zircon geochronology and geological evolution of the Halaban- Al Amar region of the eastern Arabian Shield, Kingdom of Saudi Arabia.
J. S. Stacey, D. B. Stoeser, W.R. Greenwood, L. B. Fischer
1984, Journal of the Geological Society (141) 1043-1055
U-Pb zircon model ages for eleven major units from the Halaban-Al Amar region of the eastern Arabian Shield indicate three stages of evolution: (1) plate convergence, (2) plate collision, and (3) post-orogenic intracratonic activity.Convergence occurred between the western Afif and eastern Ar Rayn plates that were separated by oceanic crust....
The impact of uncertainties in hydrologic measurement on phosphorus budgets and empirical models for two Colorado reservoirs.
James W. LaBaugh, T. C. Winter
1984, Limnology and Oceanography (29) 322-339
Water budgets and related chemical budgets of aquatic ecosystems commonly are interpreted without reference to uncertainties resulting from errors of measurement. The importance of such uncertainties in the use and interpretation of the phosphorus budgets of two Colorado reservoirs was determined....
Geology of El Chichon volcano, Chiapas, Mexico
W. A. Duffield, R.I. Tilling, R. Canul
1984, Journal of Volcanology and Geothermal Research (20) 117-132
The (pre-1982) 850-m-high andesitic stratovolcano El Chicho??n, active during Pleistocene and Holocene time, is located in rugged, densely forested terrain in northcentral Chiapas, Me??xico. The nearest neighboring Holocene volcanoes are 275 km and 200 km to the southeast and northwest, respectively. El Chicho??n is built on Tertiary siltstone and sandstone,...
Spilled oil and infaunal activity - Modification of burrowing behavior and redistribution of oil
H.E. Clifton, K.A. Kvenvolden, J. B. Rapp
1984, Marine Environmental Research (11) 111-136
A series of experiments in Willapa Bay, Washington, indicates the degree to which the presence of spilled oil modifies the burrowing behavior of infauna and the extent to which the animals redistribute oil into intertidal sediment. Small amounts of North Slope crude oil introduced at low tide directly into burrow...
Proton and metal ion binding to natural organic polyelectrolytes—II. Preliminary investigation with a peat and a humic acid
J.A. Marinsky, M.M. Reddy
1984, Organic Geochemistry (7) 215-221
We summarize here experimental studies of proton and metal ion binding to a peat and a humic acid. Data analysis is based on a unified physico-chemical model for reaction of simple ions with polyelectrolytes employing a modified Henderson-Hasselbalch equation. Peat exhibited an apparent intrinsic acid dissociation constant of 10−4.05, and...
Transitional paleointensities from Kauai, Hawaii, and geomagnetic reversal models
Scott W. Bogue, Robert S. Coe
1984, Journal of Geophysical Research (89) 10341-10354
Previously presented paleointensity results from an R-N transition zone in Kauai, Hawaii, show that field intensity dropped from 0. 431 Oe to 0. 101 Oe while the field remained within 30 degree of the reversed axial dipole direction. A recovery in intensity and the main directional change followed this presumably...
Deglaciation and postglacial timberline in the San Juan Mountains, Colorado
P. E. Carrara, W.N. Mode, M. Rubin, S.W. Robinson
1984, Quaternary Research (21) 42-55
Lake Emma, which no longer exists because of a mining accident, was a tarn in a south-facing cirque near the headwaters of the Animas River in the San Juan Mountains of southwestern Colorado. During the Pinedale glaciation, this area was covered by a large transection glacier centered over the Lake...
Interactions of solutes and streambed sediment: 1. An experimental analysis of cation and anion transport in a mountain stream
Kenneth E. Bencala, Vance C. Kennedy, Gary W. Zellweger, Alan P. Jackman, Ronald J. Avanzino
1984, Water Resources Research (20) 1797-1803
An experimental injection was performed to study the transport of stream water solutes under conditions of significant interaction with streambed sediments in a mountain pool-and-riffle stream. Experiments were conducted in Little Lost Man Creek, Humboldt County, California, in a period of low flow duringwhich only a part of the bank-full...
Accumulation of organic matter in Cretaceous oxygen-deficient depositional environments in the central Pacific Ocean
W.E. Dean, George E. Claypool, J. Thide
1984, Organic Geochemistry (7) 39-51
Complete records of organic-carbon-rich Cretaceous strata were continuouslycored on the flanks of the Mid-Pacific Mountains and southern Hess Rise in the central North Pacific Ocean during DSDP Leg 62. Organic-carbon-rich laminated silicified limestones were deposited in the western Mid-Pacific Mountains during the early Aptian, a time when that region was...
ASSESSMENT OF HIGH-TEMPERATURE GEOTHERMAL RESOURCES IN HYDROTHERMAL CONVECTION SYSTEMS IN THE UNITED STATES.
Manuel Nathenson
1984, Conference Paper, Proceedings of the Intersociety Energy Conversion Engineering Conference
The amount of thermal energy in high-temperature geothermal systems (>150 degree C) in the United States has been calculated by estimating the temperature, area, and thickness of each identified system. These data, along with a general model for recoverability of geothermal energy and a calculation that takes account of the...
Numerical simulation of phytoplankton productivity in partially mixed estuaries
D. H. Peterson, J.F. Festa
1984, Estuarine, Coastal and Shelf Science (19) 563-589
A two-dimensional steady-state model of light-driven phytoplankton productivity and biomass in partially mixed estuaries has been developed. Effects of variations in river flow, suspended sediment concentration, phytoplankton sinking, self-shading and growth rates on distributions of phytoplankton biomass and productivity are investigated.Numerical simulation experiments show that biomass and productivity are particularly...
Simulation of ground-water flow in a mined watershed in eastern Ohio
J. S. Weiss, A. C. Razem
1984, Groundwater (22) 549-560
A 43-acre watershed in Muskingum County, Ohio, was studied to determine the hydrologic consequences of strip mining for coal. A quantitative description of the effects on the ground-water flow components of the hydrologic system has been obtained using digital models.The premining watershed was characterized by...
Distribution of trace elements in coal from the Powhatan No. 6 mine, Ohio
C.A. Palmer, R.H. Filby
1984, Fuel (63) 318-328
Size and density separates of low-temperature-ashed coal from the Powhatan No. 6 mine, Ohio, have been used to determine the mode of occurrence of 28 minor and trace elements in coal. The size distribution of the major minerals has been determined, and correlations of trace elements with major minerals have...
Copper and cobalt in aquatic mosses and stream sediments from the Idaho Cobalt Belt
J. A. Erdman, P.J. Modreski
1984, Journal of Geochemical Exploration (20) 75-84
Samples of stream sediments and aquatic mosses were collected from nine sites across several mineralized zones at the southeasternmost extension of the Idaho Cobalt Belt. Because the steepness of the terrain and the attendant high flow rate of the streams made it difficult to obtain adequate sediment samples, mosses were...
Mineral resources of the Atlantic Exclusive Economic Zone
William P. Dillon
1984, Conference Paper, Oceans Conference Record (IEEE)
Potential mineral resources of the Atlantic Exclusive Economic Zone (including the Gulf of Mexico and US Caribbean areas) include petroleum, sand and gravel, phosphorite, placer deposits of heavy mineral sands, ferromanganese nodules, and fresh water. Although major efforts have been made to search for petroleum, the oil and gas resources...
Eyewitness account of the 1931 great earthquake at Hawke’s Bay, New Zealand
H. Spall
1984, Earthquake Information Bulletin (USGS) (16) 12-20
No part of New Zealand is far from a known earthquake origin. The magnitude 7.9 earthquake of 1931 at Hawke's Bay, North Island, on February 3, 1931, was the most serious event recorded in New Zealand hsitory. It was responsible for 256 deaths. The Modified Mercalli intensity reached XI in...
THERMAL-INERTIA MAPPING IN VEGETATED TERRAIN FROM HEAT CAPACITY MAPPING MISSION SATELLITE DATA.
Ken Watson, Susanne Hummer-Miller
1984, Conference Paper
Thermal-inertia data, derived from the Heat Capacity Mapping Mission (HCMM) satellite, were analyzed in areas of varying amounts of vegetation cover. Thermal differences which appear to correlate with lithologic differences have been observed previously in areas of substantial vegetation cover. However, the energy exchange occurring within the canopy is much...
Uranium mineralization in response to regional metamorphism at Lilljuthatten, Sweden
J. S. Stuckless, B. Troeng
1984, Economic Geology (79) 509-528
Analyses of six mineralized and five nonmineralized whole-rock drill core samples from the uranium deposit at Lilljuthatten yield a lead-lead isochron age of 420 + or - 1 m.y. This age corresponds to the last stage of the Caledonian Orogeny. None of the isotopic systems examined have completely retained the...
Economics and appraisal of conventional oil and gas resources in the western Gulf of Mexico
Emil Attanasi, John L. Haynes
1984, Journal of Petroleum Technology (36) 2171-2180
The oil and gas industry frequently appraises undiscovered oil and gas resources on a regional basis to decide whether to start or continue exploration programs. The appraisals are of little value unless conditioned by estimates of the costs of finding and producing the resources. This paper presents an economic appraisal...
Submersible pressure outflow cell for measurement of soil water retention and diffusivity from 5 to 95 degrees C
Jim Constantz, W.N. Herkelrath
1984, Soil Science Society of America Journal (48) 7-10
A technique was developed to measure water content in soil as a function of capillary pressure from 5 to 95°C. To overcome problems encountered at high temperature, a modified Tempe pressure cell containing a soil sample is suspended in a constant-temperature water bath. The cell's porous plate is in direct...
Magmatic epidote and its petrologic significance
E-An Zen, J. M. Hammarstrom
1984, Geology (12) 515-518
Epidote is a major magmatic mineral in tonalite and granodiorite in a belt coextensive with the Mesozoic accreted terranes between northern California and southeastern Alaska. Textural and chemical evidence indicates that epidote crystallized as a relatively late but magmatic mineral that formed through...
Chemical equilibration of the Earth's core and upper mantle
R. Brett
1984, Geochimica et Cosmochimica Acta (48) 1183-1188
The oxygen fugacity (fO2) of the Earth's upper mantle appears to lie somewhat above that of the iron-wüstite buffer, its fO2 is assumed to have been similar to the present value at the time of core formation. In the upper mantle, the Fe-rich liquid protocore that would form under such conditions...
Pegmatite/wallrock interactions, Black Hills, South Dakota: Progressive boron metasomatism adjacent to the Tip Top pegmatite
C.K. Shearer, J. J. Papike, S.B. Simon, J.C. Laul, R.P. Christian
1984, Geochimica et Cosmochimica Acta (48) 2563-2579
Interaction between country rock and fluids derived from the Tip Top pegmatite has resulted in a series of boron enriched assemblages. Between unaltered quartz-mica schist to the pegmatite contact is a succession of four mineral assemblages:1.(1) Quartz-Biotite-Potassium Feldspar assemblage (Q-B-K), which consists essentially of the original metamorphic...
Magnetic properties of the Bay of Islands ophiolite suite and implications for the magnetization of oceanic crust
B. Ann Swift, H. Paul Johnson
1984, Journal of Geophysical Research B: Solid Earth (89) 3291-3308
Rock magnetic properties, opaque mineralogy, and degree of metamorphism were determined for 101 unoriented samples from the North Arm and Blow-Me-Down massifs of the Bay of Islands ophiolite complex, Newfoundland. The weathered and metamorphosed extrusive basalt samples have a weak, secondary magnetization arising from oxidation and exsolution of ilmenite of...