Terranes and suture zones in east central Alaska
M. Churkin Jr., H.L. Foster, R. M. Chapman, F. R. Weber
1982, Journal of Geophysical Research B: Solid Earth (87) 3718-3730
East central Alaska, with its 17 terranes, forms a part of the mosaic of allochthonous terranes that join the North American and Siberian plates. These terranes range from continental and continental margin, such as the Tatonduk with its thick well-bedded succession of marine shelf rocks, to seamount, arc, and ocean...
Uranium-lead isotopic ages from the Sierra Nevada Batholith, California
J. Chen
1982, Journal of Geophysical Research B: Solid Earth (87) 4761-4784
This study provides new information on the timing and distribution of Mesozoic magmatic events in the Sierra Nevada batholithic complex chiefly between 36° and 37°N. latitude. U-Pb ages have been determined for 133 zircon and 7 sphene separates from 82 samples of granitoid rocks. Granitoid rocks in this area range...
The occurrence of the Complexiopollis-Atlantopollis zone (Palynomorphs) in the Eagle Ford Group (Upper Cretaceous) of Texas
Raymond A. Christopher
1982, Journal of Paleontology (56) 525-541
The Lower and lower Upper Cretaceous palynological zones defined in the Atlantic Coastal Plain Province and which occur in the eastern Gulf Coastal Plain Province are characterized by a paucity of marine invertebrate fossils. As a result, correlation of these zones with European and provincial stages, as well as with...
Representation of multiaquifer well effects in three-dimensional ground-water flow simulation
Gordon D. Bennett, Angelo L. Kontis, Steven P. Larson
1982, Groundwater (20) 334-341
The presence of multiaquifer or multilayer wells changes the nature of the equations which must be solved in a three-dimensional ground-water flow simulation and, in effect, alters the stencil of computation. A method has been devised which takes this change into consideration by allowing simulation of the hydraulic effects of...
Time-predictable bimodal volcanism in the Coso Range, California
Charles R. Bacon
1982, Geology (10) 65-69
The bimodal Pleistocene part of the Coso volcanic field has erupted rhyolite and basalt at constant long-term rates during the past ∼0.5 m.y. Both basalt and high-silica rhyolite were erupted in several independent, geologically brief episodes. The interval between eruptions of rhyolite was proportional to the volume of the preceding...
A 40-foot static cone penetrometer
R.M. Beard, H.J. Lee
1982, Conference Paper
The Navy needs a lightweight device for testing seafloor soils to sub bottom depths of 12 meters in water depths to 60 meters. To meet this need a quasistatic cone penetration device that uses water jetting to reduce friction on the cone rod has been developed. This device is called...
The use of vertical seismic profiles in seismic investigations of the earth
Alfred H. Balch, Myung W. Lee, J. J. Miller, Robert T. Ryder
1982, Geophysics (47) 906-918
During the past 8 years, the U.S. Geological Survey has conducted an extensive investigation on the use of vertical seismic profiles (VSP) in a variety of seismic exploration applications. Seismic sources used were surface air guns, vibrators, explosives, marine air guns, and downhole air guns. Source offsets have ranged from...
Geologic hazards in Navarin Basin Province, Northern Bering Sea
Paul R. Carlson, Herman A. Karl, Jeffrey M. Fischer, Brian D. Edwards
1982, Conference Paper, Proceedings- Offshore Technology Conference
Navarin Basin, scheduled for leasing in 1984 (OCS sale 83), may contain vast accumulations of oil and gas. Several geologic and oceanographic processes that may be active in and around Navarin Basin province could be hazardous to commercial development. These potential hazards include submarine slides; sea-floor instability resulting from disturbance...
On the distribution of species occurrence
Martin A. Buzas, Carl F. Koch, Stephen J. Culver, Norman F. Sohl
1982, Paleobiology (8) 143-150
The distribution of species abundance (number of individuals per species) is well documented. The distribution of species occurrence (number of localities per species), however, has received little attention. This study investigates the distribution of species occurrence for five large data sets. For modern benthic foraminifera, species occurrence is examined from...
The Yellowstone-Snake River Plain seismic profiling experiment: Crustal structure of the Eastern Snake River Plain
L.W. Braile, R. B. Smith, J. Ansorge, M.R. Baker, M.A. Sparlin, C. Prodehl, M.M. Schilly, J. H. Healy, Mueller, K.H. Olsen
1982, Journal of Geophysical Research B: Solid Earth (87) 2597-2609
Seismic refraction profiles recorded along the eastern Snake River Plain (ESRP) in southeastern Idaho during the 1978 Yellowstone-Snake River Plain cooperative seismic profiling experiment are interpreted to infer the crustal velocity and attenuation (Q-1) structure of the ESRP. Travel-time and synthetic seismogram modeling of a 250 km reversed refraction profile...
The sea slope problem revisited
Robert O. Castle, M.R. Elliott
1982, Journal of Geophysical Research B: Solid Earth (87) 6989-7024
Discrepancies in sea surface topography based on comparisons between the results of steric leveling and repeated geodetic levelings have identified what is known as the ‘sea slope problem.’ This problem is actually twofold: (1) the sea surface relief based on steric leveling differs significantly from that based on geodetic leveling...
Use of packrat middens to determine rates of cliff retreat in the eastern Grand Canyon, Arizona
Kenneth L. Cole, Larry Mayer
1982, Geology (10) 597-599
Packrat midden data can be used to calculate rates of cliff retreat by relating midden age to the distance between cliff face and midden. Regression analysis using 14 radiocarbon-dated packrat deposits from the Mississippian Redwall Limestone in the eastern Grand Canyon suggests that the Redwall has been retreating at an...
Northern East Pacific Rise: Magnetic anomaly and bathymetric framework
Kim D. Klitgord, Jacqueline Mammerickx
1982, Journal of Geophysical Research B: Solid Earth (87) 6725-6750
The oceanic crust in the eastern Pacific between 7°N and 30°N and east of 127°W contains a fairly complete history of the spreading centers associated with the East Pacific Rise since 25 m.y. B.P. (late Oligocene). In this paper, we have summarized the seafloor spreading magnetic-anomaly data and the bathymetric...
Diatom biostratigraphy and paleoecology of the type section of the Luisian Stage, central California
Jack G. Baldauf, John A. Barron
1982, Micropaleontology (28) 84
Diatoms from the type section of the Luisian Stage in central California correlate with the lowermost part of the Denticulopsis lauta Zone through the lower part of subzone "a" of the Denticulopsis hustedtii-D. lauta Zone and are early Middle Miocene in age (about 6.0 to 14.0 Ma), Rocks assigned to...
Source parameters of the 1980 Mammoth Lakes, California, earthquake sequence
Ralph J. Archuleta, Edward Cranswick, Charles Mueller, Paul Spudich
1982, Journal of Geophysical Research B: Solid Earth (87) 4595-4607
From the more than 1500 Mammoth Lakes earthquakes recorded on three-component digital seismographs (Spudich et al., 1981), 150 were used in an analysis of the locations, mechanism, and source parameters. A composite fault plane solution of nine earthquakes 3.9 ≤ M ≤ 5.1 defines a right-lateral strike slip mechanism on...
The Geoid: Effect of compensated topography and uncompensated oceanic trenches
C.G. Chase, Marcia K. McNutt
1982, Geophysical Research Letters (9) 29-32
The geoid is becoming increasingly important in interpretation of global tectonics. Most of the topography of the earth is isostatically compensated, so removal of its effect from the geoid is appropriate before tectonic modeling. The oceanic trenches, however, are dynamically depressed features and cannot be isostatically compensated in the classical...
Volume of organic-rich Devonian shale in the Appalachian Basin: relating "black" to organic-matter content: Geologic notes
Ronald R. Charpentier, James W. Schmoker
1982, American Association of Petroleum Geologists Bulletin (66) 375-378
Some estimates of natural-gas resources in the Devonian shale of the Appalachian basin depend on the volume of organic-rich shale in the basin. A map by L. G. Wallace and W. de Witt showing the thickness and extent of Devonian "black" shale facies in the Appalachian basin is widely used...
Sensitivity of selected geomagnetic properties to truncation level of spherical harmonic expansions
E.R. Benton, Ronald H. Estes, R.A. Langel, L.A. Muth
1982, Geophysical Research Letters (9) 254-257
A two day selection of MAGSAT data is fit by spherical harmonic series truncated at increasing levels NF in the range 2<NF<14 to determine the extent to which the geomagnetic Gauss coefficients depend upon truncation level of the fit. The dependence is found to be concentrated in the range n<NF≲n+4...
Kinematic evolution of the junction of the San Andreas, Garlock, and Big Pine faults, California
Robert G. Bohannon, David G. Howell
1982, Geology (10) 358-363
If the San Andreas fault with about 300 km of right slip, the Carlock fault with about 60 km of left slip, and the Big Pine fault with about 15 km of left slip are considered to have been contemporaneously active, a space problem at their high-angle junctions becomes apparent....
Marine ice-pushed boulder ridge, Beaufort Sea, Alaska
Peter W. Barnes
1982, Arctic (35) 312-316
A steep-faced boulder ridge up to 4m high by 300m long was encountered along the arctic coast east of Prudhoe Bay, Alaska, in the summer of 1979. Marine occurrences of similar ridges are rare. Since ice-push sorts cobble- and boulder-sized material in the construction of a ridge, recent onshore excursions of ice due to wind stress on the fast ice...
Miocene actinommid Radiolaria from the equatorial Pacific
J. R. Blueford
1982, Micropaleontology (28) 189-213
Actinommids (spumellarian Radiolaria) are a group of microfossils in which taxonomy and phylogeny hitherto have been based on features of morphology that change with the growth of individuals. To make Miocene actinommids from the equatorial Pacific useful in biostratigraphy, paleocenography, and paleoecology, ontogenetically invariant morphological features can be analyzed by...
Geologic factors that control mineral matter in coal
C. B. Cecil, R.W. Stanton, F.T. Dulong, J.J. Renton
R.H. Filby, Brett Carpenter, Richard C. Ragaini, editor(s)
1982, Book chapter, Atomic and Nuclear Methods in Fossil Energy Research
Elements other than organically derived and bound C, H, N, O, and S constitute mineral matter in coal. Mineral matter may consist of discrete minerals such as calcite, quartz, clays, and pyrite, and/or organic compounds that contain organically bonded elements such as Ca and CI. Processes that may affect the...
Regional ground-water flow concepts in the United States: Historical perspective
J.D. Bredehoeft, W. Back, B.B. Hanshaw
1982, Special Paper of the Geological Society of America (189) 295-316
A number of important ideas, developed during the past 100 years, form the framework of the present understanding of regional ground-water flow. The most important of these ideas are:Differences in topographic elevation provide the principal driving force for regional flow.Flow through confining layers...
Sedimentation, metamorphism and tectonic accretion of the Franciscan assemblage of northern California
M. Clark Blake Jr., A. S. Jayko, D. G. Howell
1982, Book chapter, Geological Society, London, Special Publications
Net-mortality of Common Murres and Atlantic Puffins in Newfoundland, 1951-81
John F. Piatt, David N. Nettleship, William Threlfall
David N. Nettleship, Gerald A. Sanger, Paul F. Springer, editor(s)
1982, Conference Paper, Marine birds: Their feeding ecology and commercial fisheries relationships
Band recoveries (N = 315) over 26 years (1951-77) and three surveys of seabird bycatch in inshore fishing nets (1972, 1980-81) indicate that there has been a substantial net-mortality of Atlantic Puffins (Fratercula arctica) and Common Murres (Uria aalge) in Newfoundland coastal waters for the past 2 decades. Offshore (e.g....
