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Page 5862, results 146526 - 146550

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Not all publications have extents, not all extents are completely accurate
The geochronology of foraminiferal ooze deposits in the "Southern Ocean"
Charles W. Holmes, J.K. Osmond, H.G. Goodell
1968, Earth and Planetary Science Letters (4) 368-374
Many cores raised from the Drake Passage are characterized by alternating zones of foraminiferal ooze and sandysilt. Cores raised from the East Pacific Rise are foraminiferal ooze or alternating siliceous and carbonate ooze. The uranium and thorium concentrations and isotopic ratios in foraminifers separated from these cores were measured by...
The relationship between specific capacity and aquifer transmissibility in the Houston Area, Texas
R.K. Gabrysch
1968, Groundwater (6) 9-14
Water well drillers gather information essential to recovery tests as part of normal procedure. Added effort could yield additional valuable information. More care in measurement of water levels both before and after a period of pumping can be used with ground‐water formulae to determine approximate well efficiency. A relationship exists between the ability of...
Estimating cost of ground‐water withdrawal for river basin planning
Este F. Hollyday, Paul R. Seaber
1968, Groundwater (6) 15-23
Comparative costs of ground water were needed for comprehensive planning of water resources development in the Susquehanna River basin in order to appraise the feasibility of alternative sources of water supply. Log‐normal plots on logarithmic‐probability paper that represented specific capacities adjusted to 180 days of pumping were used to estimate well yields and costs of obtaining the ground water from each of 65 potential aquifers....
Television observations from Surveyor 3
Eugene Merle Shoemaker, R. M. Batson, H. E. Holt, E. C. Morris, J. J. Rennilson, E. A. Whitaker
1968, Journal of Geophysical Research (73) 3989-4043
A total of 6315 pictures were taken by the television camera on Surveyor 3 after the lunar landing. These pictures have provided much new information about the location of the landing site on the moon, the detailed topographic and geologic characteristics of the lunar surface, and the appearance of the...
Lunar theory and processes
D. E. Gault, R. J. Collins, T. Gold, J. Green, G. P. Kuiper, H. Masursky, J. O'Keefe, R. Phinney, Eugene Merle Shoemaker
1968, Journal of Geophysical Research (73) 4115-4131
Despite the fact that the Surveyor 3 landed in a crater, the general appearance of the terrain is remarkably similar to that revealed by Surveyor 1. Evidence of the transport of material down the crater wall was observed. Some picture degradation occurred, apparently as a result of...
European Cretaceous flints on the coast of North America
K.O. Emery, C. A. Kaye, D.H. Loring, D.J.G. Nota
1968, Science (160) 1225-1228
Flint pebbles and nodules from the Upper Cretaceous chalks of Europe occur offshore and at many seaports along the Atlantic coast of North America, where they were brought as ship's ballast. Isolated pieces imported from Europe as gunflints also are present....
Argon-40: Excess in submarine pillow basalts from Kilauea Volcano, Hawaii
G. Brent Dalrymple, James G. Moore
1968, Science (161) 1132-1135
Submarine pillow basalts from Kilauea Volcano contain excess radiogenic argon-40 and give anomalously high potassium-argon ages. Glassy rims of pillows show a systematic increase in radiogenic argon-40 with depth, and a pillow from a depth of 2590 meters shows a decrease in radiogenic argon-40 inward from the pillow rim. The...
Hypogene veins of gibbsite, pyrolusite, and lithiophorite in Nye County, Nevada
Donnel Foster Hewett, Henry Rowland Cornwall, Richard C. Erd
1968, Economic Geology (63) 360-371
Gibbsite, lithiophorite, pyrolusite, and goethite, plus discrete mixtures of gibbsite and lithiophorite and of gibbsite and iron oxide, occur as replacement veins in limestone. Minor accessories are barite, alunite, opal. Minerals of wall-rock alteration are garnet, idocrase, K-feldspar, prehnite, sericite, and quartz. These silicates formed at higher temperature than the...
Environment of ore deposition at the Mex-Tex deposits, Hansonburg District, New Mexico, from studies of fluid inclusions
E. Roedder, A. V. Heyl, J.P. Creel
1968, Economic Geology (63)-336
These deposits, in Pennsylvanian limestone and shale, contain barite, fluorite, low-silver galena with "J-type" lead, and quartz, and only minor amounts of other minerals. Mineralization occurs in veins, in blankets of bedded, rhythmically banded "coontail" ore, and in vuggy, coarsely crystalline open-space fillings in tectonic and solution channels in limestone adjacent to...
The synthesis of ferroselite from an aqueous solution at low temperature
C. G. Warren
1968, Economic Geology (63) 418-419
Ferroselite, FeSe 2, is commonly associated with sandstone-type uranium deposits. Although it has been previously synthesized, the conditions of synthesis were not applicable to the natural system, and the literature did not provide any information on the formation of natural ferroselite. The U. S. Geological Survey's Ambrosia Lake study, however, was concerned with the...
Reforestation with conifers-its effect on streamflow in central New York
Gordon Roundy Ayer
1968, JAWRA (4) 13-24
During the early 1930's, more than 340,000 acres of abandoned farmland in New York State were purchased by the State Conservation Department for the planting, growing, and harvesting of trees. Since then, this land has developed from a heavy cover of weeds and brush into dense coniferous woodlands with trees averaging well over 30...
Tectonic emplacement of the Burro Mountain ultramafic body, Santa Lucia Range, California
Stephen H. Burch
1968, GSA Bulletin (79) 527-544
The Burro Mountain body is a crudely equidimensional block of unusually fresh ultramafic rock. This block, along with numerous smaller and more elongate serpentinite bodies, has been emplaced in a highly sheared Franciscan terrane immediately west of the Nacimiento fault. This fault separates two major structural units: (1) on the...
Gneissic amphibolite at Las Palmas, Puerto Rico, and its significance in the early history of the greater antilles island arc
O. T. Tobisch
1968, Geological Society of America Bulletin (79) 557-574
The basal complex of Puerto Rico consists principally of serpentinite, minor amounts of chert and spilite, and locally small blocks of amphibolite. A detailed structural and metamorphic study of a relatively large block of gneissic amphibolite at Las Palmas reveals that the rock has undergone repeated deformation and regional metamorphism prior to contact metamorphism by intrusive serpentinite. The first event...
Monitoring of changes in quality of ground water
H. E. LeGrand
1968, Groundwater (6) 14-18
Ground water of acceptable quality is commonly interspersed with water of inferior quality. Water of inferior quality may be naturally occurring salty water commonly underlying fresh water, or it may be enclaves of contaminated water from wastes that lie in the fresh-water bodies. Disposal of wastes on and in the...
Aerial estimation of the size of gull breeding colonies
J.A. Kadlec, W.H. Drury
1968, Journal of Wildlife Management (32) 287-293
Counts on photographs and visual estimates of the numbers of territorial gulls are usually reliable indicators of the number of gull nests, but single visual estimates are not adequate to measure the number of nests in individual colonies. To properly interpret gull counts requires that several islands with known numbers...
Ultrastructure of lymphocystis virus
L.O. Zwillinberg, K. Wolf
1968, Journal of Virology (2) 393-399
Lymphocystis virus obtained from bluegills (Lepomis macrochirus) was cultured in the permanent bluegill cell line BF-2 and examined by electron microscopy in ultra-thin sections of cell cultures and in negative-contrast preparations from cells and from centrifuged culture medium. According to negative-contrast preparations, the icosahedral virions have an overall diameter close...
Possible differentiation of natal areas of North American waterfowl by neutron activation analysis
T. Devine, T.J. Peterle
1968, Journal of Wildlife Management (32) 274-279
The possibility of using neutron activation analyses to differentiate sources of North American waterfowl was investigated by irradiating rectrices and wing bones of birds collected in several localities, and comparing the characteristic gamma-ray spectra. Canada goose (Branta canadensis) rectrices from Oregon specimens could be distinguished from those taken in Wisconsin...
Age determination of blue-winged teal
C.W. Dane
1968, Journal of Wildlife Management (32) 267-274
Primary feather length, markings on the greater secondary coverts, and the degree of bill spotting were evaluated as characters for use in the spring to distinguish first-year, blue-winged teal (Anas discors) females from older ones. The length of the 10th primary feather did not prove suitable to separate different aged...
Chapter IX: Lunar theory and processes
D. E. Gault, J. B. Adams, R. J. Collins, G. P. Kuiper, H. Masursky, J. A. O’Keefe, R. A. Phinney, Eugene Merle Shoemaker
1968, Book chapter, Surveyor VII mission report: Part II: Science results
Whereas the previous Surveyor missions were undertaken to examine mare surfaces as potential landing areas for the Apollo Program, the primary objective of the Surveyor VII mission, based on purely scientific motivations, was to explore a contrasting highland region and, specifically, to determine the chemistry of the highland material for...
Exsolution in clinoamphiboles
M. Ross, J. J. Papike, P.W. Weiblen
1968, Science (159) 1099-1102
Ten amphibole specimens from a variety of metamorphic rocks such as talc schists, eclogites, and metamorphosed iron formations contain lamellae of a second amphibole oriented parallel to (1̅01) or (100), or both, of the host. Tremolites, actinolites, and hornblendes commonly have lamellae of a calcium-poor clinoamphibole with P21/m space-group...
Depth control of some concordant intrusions
Melville R. Mudge
1968, Geological Society of America Bulletin (79) 315-332
Analysis of geologic data from 54 localities, mainly in the western United States, shows that concordant igneous masses intruded zones in nearly flat-lying sedimentary rocks where the thickness of cover was 3000 to 7500 feet. The depth of intrusion was apparently affected by a well-defined parting surface (bedding plane or unconformity), static load of the overburden...