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Page 5970, results 149226 - 149250

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Publication Extents

Not all publications have extents, not all extents are completely accurate
Supergene iron ores of minas Gerais, Brazil
J. V.N. Dorr II
1964, Economic Geology (59) 1203-1240
The iron ores of Minas Gerais, Brazil, fall into two categories: (1) hypogene hematite ore averaging 66 percent or more Fe, and (2) lower-grade supergene ores. Most ore now extracted is high-grade hypogene ore; lower-grade supergene ores will be of much future value. All supergene ores formed by weathering of itabirite, a metamorphosed oxide-facies iron formation averaging about 38 percent Fe and 44 percent Si02. The Caue Itabirite crops out for...
Rigid plastic collars for marking geese
R.M. Ballou, F.W. Martin
1964, Journal of Wildlife Management (28) 846-847
Rigid plastic collars of one to three colors proved useful for recognition of individual Canada geese (Branta canadensis). The collars did not seem to affect the behavior of the geese, and there was little mortality caused by their use. In good light, bright colors are visible through a 20-power spotting...
Problems of the geographic and stratigraphic distribution of American Middle Eocene larger Foraminifera
W. Storrs Cole, Esther English Richards Applin
1964, Bulletins of American Paleontology (47) 1-48
Larger Foraminifera from the middle Eocene of Florida and southern Georgia are discussed, including 2 new species, and their geographic and stratigraphic distribution, not only in the U. S., but also at selected localities in the Caribbean region, is analyzed. Several species not previously reported from the U. S. are...
The international hydrological decade
R. L. Nace
1964, Eos, Transactions, American Geophysical Union (45) 413-421
Work toward establishing a program of international cooperative studies in scientific hydrology began about 4 years ago, and the IHD (International Hydrological Decade) will begin under international auspices in January 1965. This program will be highly important for hydrology and hydrologists, and it should contribute greatly to human welfare in the future. Fortuitously, the opening year...
Geohydrologic analogies between the Jordan Valleys of Utah and the holy land
Edward Bradley
1964, International Association of Scientific Hydrology - Bulletin (9) 12-23
The biblical Jordan River Valley, which extends from Lake Tiberias (the Sea of Galilee) to the Dead Sea, is decidedly similar to the Jordan River Valley of Utah, which joins Lake Utah and Great Salt Lake. Both Jordan Rivers drain relatively large fresh-water lakes and also are major sources of discharge into large salty lakes that have no outlets to the ocean.The...
Experimental determination of the reaction chalcopyrite + sulfur = pyrite + bornite from 350 to 500° C
P. B. Barton Jr., P. Toulmin III
1964, Economic Geology (59) 747-752
The fugacity of sulfur along the curve representing the univariant equilibrium assemblage, chalcopyrite + bornite + pyrite + vapor, has been determined by the electrum tarnish method (1). The conditions of the equilibrium may be expressed by the equation (TP) - /°s 2 (T, 1 atm) = -50,730 + 56.95T (cal.) (350 - 500° C) (T in °K). With gentle curvature, the line...
Officer's cave, a pseudokarst feature in altered tuff and volcanic ash of the John Day formation in eastern Oregon
Garald G. Parker, Lynn M. Shown, Karl W. Ratzlaff
1964, Geological Society of America Bulletin (75) 393-402
Officer's Cave is the uppermost of four rapidly eroding cave levels constituting a cavern complex about 700 feet long developed chiefly in clay and silt. Its outer room is 35 feet by 43.5 feet by 100 feet and slopes about 45° east into the western end of a narrow linear hill called Officer's Cave Ridge. Dry valleys, blind valleys, hanging valleys, sinkholes, pipes,...
Pre-tertiary orogenic and plutonic intrusive activity in central and northeastern Oregon
T. P. Thayer, C. E. Brown
1964, Geological Society of America Bulletin (75) 1255-1261
Pre-Tertiary rocks of the Blue Mountain region of central and northeastern Oregon comprise three major sedimentary and volcanic sequences and two distinct intrusive magma series. The ages of the sedimentary-volcanic sequences are Paleozoic, Late Triassic-Late Jurassic, and middle Cretaceous (Albian to Cenomanian), respectively. The earlier intrusive magma series ranges in composition from peridotite to albite granite and was emplaced during the major...
Basement depths from widely spaced aeromagnetic profiles in Kansas and Nebraska
Joel S. Watkins
1964, Geophysics (29) 80-86
Profiles of the basement surface in western Kansas and Nebraska were constructed by drawing smooth curves through the shallowest depths estimated from aeromagnetic anomalies along six widely spaced traverses. Ratios of inferred-depth-to-basement to true depth along the traverses ranges from 0.7 to 1.0. Clusters of shallow depth estimates commonly yield an average estimate within 15 percent of the true depth....
Magnetic disturbances preceding the 1964 Alaska earthquake
George W. Moore
1964, Nature (203) 508-509
THROUGH a fortunate circumstance, a recording magnetometer was operating in the city of Kodiak, 30 km north-west of the surface trace of a fault zone along which movement occurred at the time when the earthquake occurred in Alaska on March 27, 1964. Fortunately, too, the instrument...
Veins of hypogene manganese oxide minerals in the southwestern United States
D. F. Hewett
1964, Economic Geology (59) 1429-1472
Characteristic minerals are psilomelane, hollandite, cryptomelane, and coronadite, more rarely ramsdellite and pyrolusite. Host rocks are Mn-deficient; 80 percent of examples are middle to late Tertiary layered volcanics. Though deposits are shallow, mostly mined to only 100-200 feet (maximum 500 feet), a hypogene origin is...
Chemical aspects of hydrothermal alteration with emphasis on hydrogen metasomatism
J.J. Hemley, W. R. Jones
1964, Economic Geology (59) 538-569
The ratio of cation to hydrogen-ion concentration is used as a basis for coordinating many observed varieties of silicate rock alteration. Low ratios drive alteration from feldspar through sericite, montmorillonite, or paragonite, toward kaolinite or pyrophyllite. Principal controls of ratio are reactions with wall rock,...
Nickeliferous laterites in southwestern Oregon and northwestern California
Preston E. Hotz
1964, Economic Geology (59) 355-396
Deposits of ferruginous nickeliferous lateritic soils formed by weathering in place of ultramafic rocks occur at several places in northwestern California and southwestern Oregon, mostly in the Klamath Mountains province. Most of the deposits have been derived from relatively fresh peridotite, although at least one...
Deep geothermal brine near Salton Sea, California
Donald E. White
1964, Bulletin Volcanologique (27) 369-370
A well drilled for geothermal power near Salton Sea in Imperial Valley, Calif., is 5,232 feet deep; it is the deepest well in the world (1962) in a high-temperature hot spring area. In the lower half of the hole temperatures are too high to measure with available equipment, but are...
Oriented lakes and lineaments of northeastern Bolivia
George Plafker
1964, GSA Bulletin (75) 503-522
Strongly oriented lineaments, defined by lake shores and stream and vegetation alignments, are distributed throughout more than 45,000 square miles of the Beni basin in northeastern Bolivia. The area in which these features occur is a flat, poorly drained, lake-studded plain. It is underlain by flat-lying, poorly consolidated, continental clastic...
Barchan-dune movement in Imperial Valley, California
Joseph Long, Robert Sharp
1964, GSA Bulletin (75) 149-156
The movement of 47 barchan dunes on the west side of Salton Sea, California, ranged from 325 to 925 feet over the 7 years between 1956 and 1963, an average of 82 feet per year. During the 15 years between 1941 and 1956, the movement...
Plastic adhesive tape for color-marking birds
Don P. Fankhauser
1964, Journal of Wildlife Management (28) 594-594
Colored plastic adhesive tape wrapped around the tarsus has been used successfully for color-marking birds and has proved to be easy to put on, adaptable, permanent, and colorfast....
Thorne Cave, northeastern Utah: Geology
Harold E. Malde, Asher P. Schick
1964, American Antiquity (30) 60-73
Geologic interest in Thorne Cave stems from its link with valley alluvium along Cliff Creek, which accumulated to a height of 48 ft., continued to build up another 13 ft. while men lived here, and then reached 30 ft. higher-sealing in the signs of man. Mineralogic study shows that ground water then circulated...