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Publication Extents

Not all publications have extents, not all extents are completely accurate
Referees and the publications crisis
Frank T. Manheim
1973, Eos, Earth and Space Science News (54) 532-537
Routine refereeing by peers of manuscripts submitted to scholarly journals is a logical and effective device that can obviate ‘crankiness, irrelevance and gross incompetence’ [Ziman, 1970a] on the one hand and minimize editorial arbitrariness on the other. As reviewed by Zuckerman and Merton [1971], the device has historical roots that extend back...
Fordilla troyensis Barrande: The oldest known pelecypod
J. Pojeta Jr., B. Runnegar, J. Kriz
1973, Science (180) 866-868
Specimens of the small bivalved animal Fordilla troyensis Barrande from New York State show that this fossil is the oldest known pelecypod mollusk and not a conchostracan arthropod. This finding extends the range of the class Pelecypoda backward in time from the Early Ordovician (about 495 million years ago)...
Lonar Lake, India: An impact crater in basalt
K. Fredriksson, A. Dube, D.J. Milton, M.S. Balasundaram
1973, Science (180) 862-864
Discovery of shock-metamorphosed material establishes the impact origin of Lonar Crater. Coarse breccia with shatter coning and microbreccia with moderately shocked fragments containing maskelynite were found in drill holes through the crater floor. Trenches on the rim yield strongly shocked fragments in which plagioclase has melted and vesiculated, and bombs...
Obsidian hydration dates glacial loading?
I. Friedman, K. L. Pierce, J. D. Obradovich, W.D. Long
1973, Science (180) 733-734
Three different groups of hydration rinds have been measured on thin sections of obsidian from Obsidian Cliff, Yellowstone National Park, Wyoming . The average thickness of the thickest (oldest) group of hydration rinds is 16.3 micrometers and can be related to the original emplacement of the flow 176,000 years ago...
Isotopic and paleontologic evidence for correlating three volcanic sequences in the Maine coastal volcanic belt
Douglas G. Brookins, Jean M. Berdan, David B. Stewart
1973, Geological Society of America Bulletin (84) 1619-1628
The correlation of the Castine Volcanics, the Thorofare Andesite–Vinalhaven Rhyolite sequence, and the Cranberry Island Series of Shaler (1889), suggested by their similar lithologies, appearance, and structural histories, is supported by the results of Rb-Sr whole-rock isotopic analyses and by the faunal assemblages from old and new fossil localities in...
Pebble segregation and bed lenticularity in wave-worked versus alluvial gravel
H. Edward Clifton
1973, Sedimentology (20) 173-187
Two aspects of bedding may permit visual discrimination between wave-worked and alluvial gravel. Pebbles in gravel worked by waves tend to be better segregated into discrete beds than those in alluvial deposits, and bedding in wave-worked gravel tends to be more laterally regular, or less lenticular, than that in stream...
Petrology of the Vulcan Peak alpine-type peridotite, southwestern Oregon
Glen R. Himmelberg, Robert Ahlberg Loney
1973, Geological Society of America Bulletin (84) 1585-1600
The alpine-type peridotite in the area of Vulcan Peak, Oregon, is part of the larger Josephine ultramafic complex in the Klamath Mountains geologic province. Partially serpentinized, foliated harzburgite with 15 to 30 percent orthopyroxene makes up approximately 90 percent of the body. The remaining 10 percent is dunite that occurs...
Territorial behavior, pesticides, and the population ecology of red-shouldered hawks in central Maryland, 1943-1971
Charles J. Henny, F. C. Schmid, Elwood M. Martin, L. L. Hood
1973, Ecology (54) 545-554
A breeding population of red—shouldered hawks (Buteo lineatus) along the Patuxent River in central Maryland was studied during the interval 1943—71. Numbers of breeding pairs remained unchanged or increased on the PWRC (Patuxent Wildlife Research Center) and an adjoining area where habibat was not altered. A reduction in breeding pairs...
Energy and plane waves in linear viscoelastic media
Roger D. Borcherdt
1973, Journal of Geophysical Research (78) 2442-2453
The mathematical framework for describing plane waves in elastic and linear anelastic media is presented. Theoretical results suggest that the nature of plane waves in anelastic materials is distinctly different from the nature of plane waves in elastic materials. In elastic media the only type of inhomogeneous plane wave (P or S)...
Antarctic icebergs as a fresh water resource
W.F. Weeks, W. J. Campbell
1973, Polar Record (16) 661-665
In a recent study (Weeks and Campbell, in press), we made a rather complete examination of the idea that icebergs could advantageously be used as a source of fresh water. The origin of the general idea of transporting icebergs is obscure; it may date from the 1850's when ice was...
Hydrologic changes after clear-cut logging in a small Oregon coastal watershed
D.D. Harris
1973, Journal of Research of the U.S. Geological Survey (1) 487-491
Preliminary graphical analysis indicates that clear-cut logging of a small Oregon watershed has significantly altered certain hydrologic characteristics. After logging, moderate increases were noted in annual runoff, but no significant changes were detected in either peak or minimum flow rates. Both the annual sediment yields and the maximum monthly water temperatures increased greatly after logging; sediment...
Solubility of cryolite at 25° C and 1 atmosphere pressure
C. E. Roberson, J.D. Hem
1973, Journal of Research of the U.S. Geological Survey (1) 483-485
For natural cryolite from Greenland the activity product for the reaction (in water),Na3 Al F6 c --> 3Na+ + Al3+ + 6F-,was found to be 10-34.3 +/- 0.1. This is in good agreement with earlier work in which equilibrium was approached from supersaturation....
Metamorphic facies indicated by vein minerals in basal beds of the Great Valley sequence, northern California
Edgar H. Bailey, David L. Jones
1973, Journal of Research of the U.S. Geological Survey (1) 383-385
A reexamination of reported blueschist mineral localities in the basal strata of the Great Valley sequence revealed only prehnite-pumpellyite facies minerals. Franciscan graywacke thrust below the Great Valley rocks contains lawsonite-quartz blueschist assemblages. At a common pressure of about 4 kb, the Franciscan blueschists formed at lower temperatures than the overlying Great Valley prehnite-bearing rocks, lending...
Lower Jurassic ammonite from the south-central Sierra Nevada, California
David L. Jones, James G. Moore
1973, Journal of Research of the U.S. Geological Survey (1) 453-458
A Lower Jurassic ammonite has been found in metasiltstone of the Boyden Cave roof pendant, south-central Sierra Nevada, Calif. Although too poorly preserved to permit positive generic and specific identification, its general shape, coiling, and ornamentation are characteristic of Early Jurassic forms. Strata associated with the fossiliferous rocks in the pendant include quartzite, andalusite hornfels, and...
Current slope-stability studies in the San Francisco Bay region
Tor H. Nilsen, Earl E. Brabb
1973, Journal of Research of the U.S. Geological Survey (1) 431-437
An extensive program of slope-stability studies is presently underway in the San Francisco Bay region, California. Work to date has resulted in the publication of estimates of landslide damage, an estimated-landslide-abundance map of the region, new slope maps prepared by photomechanical processes, photointerpretive maps of landslide, colluvial, and other surficial deposits, and maps of relative slope...
Boron-bearing potassium feldspar of authigenic origin in closed-basin deposits
Richard A. Sheppard, Arthur J. 3rd Gude 3rd
1973, Journal of Research of the U.S. Geological Survey (1) 377-382
Silicic vitric tuffs in saline, alkaline lacustrine deposits are commonly altered to a variety of zeolites and potassium feldspar. The tuffs generally show a lateral gradation, in a basinward direction, of fresh glass to zeolites and then to potassium feldspar. Zeolites were formed early in diagenesis by reaction of the glass with the interstitial water....
Potential shale-oil resources of a stratigraphic sequence above the Mahogany Zone, Green River Formation, Piceance Creek Basin, Colorado
John R. Donnell, Janet K. Pitman
1973, Journal of Research of the U.S. Geological Survey (1) 467-473
In the southern part of the Piceance Creek basin the upper part of the Green River Formation above the Mahogany zone contains beds of rich oil shale which may be economically recoverable by a surface-mining operation. Four units within this sequence were evaluated for thickness, distribution, oil yield, and potential shale-oil resources. In the area...
Identification of a lithium-bearing smectite from Spor Mountain, Utah
Harry C. Starkey, Wayne Mountjoy
1973, Journal of Research of the U.S. Geological Survey (1) 415-419
Chemical analyses, X-ray diffraction data, and cation exchange determinations are given for a lithium-bearing smectite. The X-ray data and Greene-Kelly's lithium test indicate the presence of both dioctahedral and trioctahedral phases. The exchange determinations indicate that the lithium is in the structure of the clay, and the chemical data are intermediate between those for hectorite...
Application of the source-area concept of storm runoff to a small Arizona watershed
F.E. Arteaga, S. E. Rantz
1973, Journal of Research of the U.S. Geological Survey (1) 493-498
An attempt to demonstrate the source-area concept of storm runoff by analysis of the rainfall-runoff relation for the watershed of Queen Creek tributary in south-central Arizona was moderately successful. The demonstration was somewhat marred by the necessity to make several simplifying assumptions to eliminate some of the many basin variables of unknown magnitude. The percentage...
Spectrochemical computer analysis - instrumentation
A.W. Helz
1973, Journal of Research of the U.S. Geological Survey (1) 475-482
A microphotometer is described for making magnetic tape recordings of spectra 480 mm long from 102- by 508-mm photographic plates. Transmission readings are recorded at a rate exceeding 1,300 per second for every 5.08 um of length of the spectrum, A two-linecadmium fiducial line system and a developing tank for 102- by 508-mm...
Potassium, thorium, and uranium contents of upper Cenozoic basalts of the southern Rocky Mountain region, and their relation to the Rio Grande depression
Peter W. Lipman, Carl M. Bunker, Charles A Bush
1973, Journal of Research of the U.S. Geological Survey (1) 387-401
Late Cenozoic basaltic volcanism in southern Colorado and northern New Mexico was most intense near the Rio Grande rift depression but extended onto stable platforms to the west (Colorado Plateau) and to the east (High Plains). Tholeiitic rocks are largely confined to the Rio Grande depression, and the basalts become increasingly alkalic with distance from...
A Precambrian diamictite below the base of the Stillwater Complex, southwestern Montana
Randolph Koski, Norman J. Page
1973, Journal of Research of the U.S. Geological Survey (1) 403-414
The metasedimentary rocks of Precambrian age below the base of the Stillwater Complex, southwestern Montana, contain a metamorphosed diamictite similar to diamictite in strata of late Precambrian and Early Cambrian age in Canada and the Western United States. The diamictite consists of a quartz-cordierite matrix containing an average 10-15 percent of rock fragments diverse in...