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Page 6060, results 151476 - 151500

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Publication Extents

Not all publications have extents, not all extents are completely accurate
Lava tree molds of the September 1961 eruption, Kilauea Volcano, Hawaii
James G. Moore, D.H. Richter
1962, GSA Bulletin (73) 1153-1158
Well-developed lava tree molds were formed during the September 1961 eruption along the east rift zone of Kilauea Volcano. The upright molds were produced where fluid lava, flowing through dense tropical forest, became chilled against the larger trees and tree ferns and later drained away. Where the lava ponded temporarily...
Metallic spherules in tektites from Isabela, Philippine Islands
E. C. T. Chao, I. Adler, E.J. Dwornik, J. Littler
1962, Science (135) 97-98
Iron-nickel spherules, as much as 0.5 mm in diameter, have been found completely embedded in some philippinites. The spherules consist mainly of kamacite with unidentified pink inclusions. The meteoritic origin of these spherules seems reasonable, suggesting that the tektites containing them were formed by asteroidal or meteoritic impact....
Metallogenetic provinces of Chile, S. A
F. C. Martinez-Ruiz, G. E. Ericksen
1962, Economic Geology (57) 91-106
The metalliferous deposits of Chile tend to be restricted to well denned metallogenetic provinces, each characterized by a dominant mineral or mineral assemblage. The most important ore deposits are those of copper, iron, silver, gold, and manganese. The primary minerals are few in number and most are simple sulfides and...
Records of wells and ground-water quality in Burlington County, New Jersey
F. Eugene Rush
1962, Report
<This basic-data report is limited to the presentation of selected drillers' logs and their geologic correlations, well data, and chemical analyses of water from wells in Burlington County, N. J. The county lies within the Coastal Plain province; it is underlain by unconsolidated sediments of Quarternary, Tertiary, and Cretaceous...
Generalized structure contour maps of the New Jersey coastal plain
Hoarce G. Richards, F. H. Olmsted, James L. Ruhle
1962, Geologic report (New Jersey) 4
Twelve generalized structural contour maps were prepared from a study of 169 well logs or sample logs of drill cuttings from the Coastal Plain of New Jersey, Delaware, and the E astern Shore of Maryland. The configuration of the tops of the nonmarine Cretaceous deposits (Patuxent , Patapsco, Raritan, and Magothy formations) and...
Physical properties of evaporite minerals
Eugene C. Robertson
1962, Trace Elements Investigations 821
The data in the following tables were abstracted from measurements of physical properties of evaporite minerals or of equivalent synthetic compounds. The compounds considered are the halide and sulfate salts which supposedly precipitated from evaporating ocean water and which form very extensive and thick "rock salt" beds. These beds are...
Diffusion features of uranium-vanadium deposits in Montezuma Canyon, Utah
L.C. Huff, F. G. Lesure
1962, Economic Geology (57) 226-237
Uranium-vanadium deposits in the Salt Wash Member of the Morrison Formation in Montezuma Canyon, San Juan County, Utah, exhibit zoning that is interpreted as a result of metal transport by diffusion. The concentric zones consist of a brown nonmineralized core, an olive-gray mineralized shell, and a gray nonmineralized outer zone. The...
Diatremes and uranium deposits in the Hopi Buttes, Arizona
Eugene Merle Shoemaker, C. H. Roach, F. M. Byers Jr.
A.E.J. Engel, Harold L. James, B. F. Leonard, editor(s)
1962, Book chapter, Petrologic studies: A volume in honor of A. F. Buddington
The Hopi Buttes diatremes erupted in a shallow lake that was filled in as volcanic activity progressed in Pliocene time. At the end of the period of volcanism the landscape included low lava domes capping some of the diatremes, a few flows, and numerous craters of the maar type, surrounded...
Lower temperature terminations of the three-phase region plagioclase-alkali feldspar-liquid
D. B. Stewart, E. H. Roseboom Jr.
1962, Journal of Petrology (3) 280-315
Geological and experimental evidence indicate that the three-phase field, plagioclase-alkalifeldspar-liquid, may terminate in several different ways. The possible terminations have been developed from Schreinemakers' rules governing the disappearance of three-phase fields. In igncous rocks, these different terminations may arise from variations in the relative amounts of additional components in magmas, or from...
Oxygen adsorption and the magnetic susceptibility of ice at low temperatures
F. E. Senftle, A. Thorpe
1962, Nature (194) 673-674
WHEN dealing with the magnetic susceptibility of tumour tissue1, we reported the magnetic susceptibility of ice at various temperatures from 273° K. down to 77° K. Since this publication, the authors have made many susceptibility measurements of ice, using the same equipment, and have obtained similar results, that is, a...
Concentration method for the spectrochemical determination of seventeen minor elements in natural water
W. D. Silvey, R. Brennan
1962, Analytical Chemistry (34) 784-786
A method for the quantitative spectrochemical determination of microgram amounts of 17 minor elements in water is given. The chelating reagents 8-quinolinol, tannic acid, and thionalide are utilized to concentrate traces (1 to 500 μg.) of aluminum, cobalt, chromium, copper, iron, gallium, germanium, manganese, nickel, titanium, vanadium, bismuth, lead, molybdenum,...
Summary of new data on rock samples G-1 and W-1
M. Fleischer, R.E. Stevens
1962, Geochimica et Cosmochimica Acta (26) 525-543
Published and unpublished analyses for major and minor constituents that have become available since April, 1960, are collected for the granite G-1 and diabase W-1. “Best values” are suggested for some of the elements....
Elastic constants of calcite
L. Peselnick, R. A. Robie
1962, Journal of Applied Physics (33) 2889-2892
The recent measurements of the elastic constants of calcite by Reddy and Subrahmanyam (1960) disagree with the values obtained independently by Voigt (1910) and Bhimasenachar (1945). The present authors, using an ultrasonic pulse technique at 3 Mc and 25°C, determined the elastic constants of calcite using the exact equations governing the wave velocities in the single crystal. The results are C11=13.7, C33=8.11, C44=3.50, C12=4.82, C13=5.68, and C14=−2.00,...
Bedrock geology of the Thiel Mountains, Antarctica
A. B. Ford, J.M. Aaron
1962, Science (137) 751-752
Cordierite-bearing, hyper-sthene-quartz monzonite porphyry, the most widespread rock unit, is intruded by biotite granite and porphyritic biotite granite. Sedimentary and metasedimentary rocks, mainly quartzites and argillites, have been metamorphosed locally to hornfels and have been involved in high-angle faulting. Shear zones are common in the plutonic rocks....
K/Na ratio of Cenozoic igneous rocks of the western United States
J.G. Moore
1962, Geochimica et Cosmochimica Acta (26) 101-130
The potassium and sodium content of chemically analysed Cenozoic igneous rocks from about 150 areas of the western United States has been examined. For each area a plot of the molecular proportion K2O(K2O + Na2O)">K2O(K2O + Na2O) [Niggli's k-value] is shown, and the projected k-value determined at 50...
Nordstrandite from Guam
J.C. Hathaway, S.O. Schlanger
1962, Nature (196) 265-266
NORDSTRANDITE (Al2O3·3H2O), previously reported only as a synthetic product1,2, occurs in Miocene limestone on Guam. In south Guam this limestone forms a cap several hundred feet thick, on the Mount Alifan–Mount Lamlan ridge, and overlies late Eocene and early Miocene basalt flows and volcanic conglomerates. The volcanic rocks below the...