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Page 6046, results 151126 - 151150

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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...
Thorium and rare earths in the United States, exclusive of Alaska and Hawaii
J. C. Olson, J. W. Adams
1962, Mineral Investigations Resource Map 28
The accompanying map shows the location of the principal deposits of thorium and rare-earth minerals in the United States (excluding Alaska and Hawaii). Symbols of different shapes are used to depict deposits of different geologic types, and sizes of symbols denote the relative importance of the deposits. Because of scale...
Behaviour of calcium carbonate in sea water
P. E. Cloud Jr.
1962, Geochimica et Cosmochimica Acta (26) 867-884
Anomalies in the behaviour of calcium carbonate in natural solutions diminish when considered in context. Best values found by traditional oceanographie methods for the apparent solubility product constant K'CaCO3 in sea water at atmospheric pressure are consistent mineralogically—at 36 parts per thousand salinity and T-25°C, K'aragonlte is...
Problem of the thermodynamic status of the mixed-layer minerals
E-An Zen
1962, Geochimica et Cosmochimica Acta (26) 1055-1067
Minerals that show mixed layering, particularly with the component layers in random sequence, pose problems because they may behave thermodynamically as single phases or as polyphase aggregates. Two operational criteria are proposed for their distinction. The first scheme requires two samples of mixed-layer material which differ only in the proportions...
Surface Water Records of Colorado
Water Resources Division U.S. Geological Survey
1962, Water Data Report CO-62-1
The surface-water records for the 1962 water year for gaging stations and miscellaneous sites within the State of Colorado are given in this report. For convenience there are also included records for a few pertinent gaging stations in bordering States. The records were collected and computed by the Water Resources...
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....
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...
Geology and ore deposits of the Globe-Miami district, Arizona
N. P. Peterson
1962, Professional Paper 342
The rocks of the Globe-Miami district range from lower Precambrian to Recent. The oldest formation, the Pinal schist, comprises several varieties of schist formed by dynamic and thermal metamorphism of shale and feldspathic sandstone during the early Precambrian Mazatzal revolution. During the later stages of this revolution, the schist was...