{"pageNumber":"5058","pageRowStart":"126425","pageSize":"25","recordCount":165579,"records":[{"id":70012242,"text":"70012242 - 1980 - Elastic moduli of rock glasses under pressure to 8 kilobars and geophysical implications","interactions":[],"lastModifiedDate":"2024-07-16T16:56:57.73129","indexId":"70012242","displayToPublicDate":"1980-01-01T00:00:00","publicationYear":"1980","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":6453,"text":"Journal of Geophysical Research Solid Earth","active":true,"publicationSubtype":{"id":10}},"title":"Elastic moduli of rock glasses under pressure to 8 kilobars and geophysical implications","docAbstract":"Shear and longitudinal velocities were measured by the ultrasonic phase comparison method as a function of pressure to 8 kbar on synthetic glasses of basalt, andesite, rhyolite, and quartz composition and on natural obsidian. Velocities of most of the glasses decrease anomalously with pressure, but increasingly more-normal behavior occurs with decrease in SiO2 content. The pressure derivatives of rigidity and bulk modulus increase linearly, from −3.39 to −0.26 and from −5.91 to +2.09, respectively, with decrease in SiO2 content from 100 to 49%. The change from negative to positive in the pressure derivatives of both moduli and observed at Poisson's ratio of about 0.25 is consistent with the Smyth model for the anomalous elastic behavior of glass. If the temperature in the upper mantle is about 1500°C, tholeiitic basalt would be molten in accordance with the partial melt explanation for the low-velocity zone; at 1300°C and below, basalt would be in the glassy state, especially if more felsic than tholeiite. At a temperature of 1370°C and at 30 kbar, reasonable values for the upper mantle at 100 km depth, the basalt glass of this study would have a viscosity of about 1013 P. On the basis of the theory of viscoelasticity the glass would support shear wave propagation at frequencies above 0.1 Hz. Under such conditions of PT, 10 to 30% basalt glass in a matrix either of eclogite or olivine would reduce the seismic velocities by 3 to 9% and could also account for the values observed in the low-velocity zone.
","language":"English","publisher":"American Geophysical Union","doi":"10.1029/JB085iB11p06461","issn":"01480227","usgsCitation":"Meister, R., Robertson, E., Werke, R., and Raspet, R., 1980, Elastic moduli of rock glasses under pressure to 8 kilobars and geophysical implications: Journal of Geophysical Research Solid Earth, v. 85, no. B11, p. 6461-6470, https://doi.org/10.1029/JB085iB11p06461.","productDescription":"10 p.","startPage":"6461","endPage":"6470","numberOfPages":"10","costCenters":[],"links":[{"id":221875,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"85","issue":"B11","noUsgsAuthors":false,"publicationDate":"2012-09-20","publicationStatus":"PW","scienceBaseUri":"505a0881e4b0c8380cd51b51","contributors":{"authors":[{"text":"Meister, R.","contributorId":96003,"corporation":false,"usgs":true,"family":"Meister","given":"R.","email":"","affiliations":[],"preferred":false,"id":363072,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Robertson, E.C.","contributorId":43365,"corporation":false,"usgs":true,"family":"Robertson","given":"E.C.","email":"","affiliations":[],"preferred":false,"id":363069,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Werke, R.W.","contributorId":88879,"corporation":false,"usgs":true,"family":"Werke","given":"R.W.","email":"","affiliations":[],"preferred":false,"id":363071,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Raspet, R.","contributorId":77656,"corporation":false,"usgs":true,"family":"Raspet","given":"R.","affiliations":[],"preferred":false,"id":363070,"contributorType":{"id":1,"text":"Authors"},"rank":4}]}}
,{"id":70012180,"text":"70012180 - 1980 - Dissolution and analysis of amorphous silica in marine sediments","interactions":[],"lastModifiedDate":"2024-05-23T00:50:43.596469","indexId":"70012180","displayToPublicDate":"1980-01-01T00:00:00","publicationYear":"1980","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":2450,"text":"Journal of Sedimentary Petrology","active":true,"publicationSubtype":{"id":10}},"title":"Dissolution and analysis of amorphous silica in marine sediments","docAbstract":"The analytical estimation of amorphous silica in selected Atlantic and Antarctic Ocean sediments, the U.S.G.S. standard marine mud (MAG-1), A.A.P.G. clays, and samples from cultures of a marine diatom, Hemidiscus, has been examined. Quantitative recovery of sedimentary amorphous silica was achieved by reacting 2 M Na 2 CO 3 with a sample for 4 hours at 90 degrees -100 degrees C; where necessary, aluminum analysis is used to correct for the extraction of non-amorphous silica. Oceanic sediments having an amorphous SiO 2 /clay ratio of 1.0 or more can be analyzed by a single extraction with 2 M Na 2 CO 3 , without correction for non-amorphous additions. Marine sediments having an amorphous SiO 2 /clay ratio of from 1.0 to 0.25 can be corrected for inputs of clay-derived silica using an aluminum determination and an empirical correction factor. Sediments with amorphous SiO 2 /clay ratios of less than 0.25, samples containing non-silica-bearing aluminous materials such as gibbsite, or materials having low absolute levels of amorphous silica require successive leaches to accurately correct for silica inputs from non-amorphous sources. Our values for amorphous silica-rich circum-Antarctic sediments are equal to or greater than literature values, whereas our values for a set of amorphous silica-poor sediments from a transect of the North Atlantic at 11 degrees N, after appropriate correction for silica released from clays, are significantly lower than previous estimates from the same region.
The rhythmic Touchet Beds in the Walla Walla and lower Yakima valleys resulted from many separate backfloodings by hydraulically ponded glacial Lake Missoula water. At least once this episodic lake briefly contained half the ![\"\"](\"https://www.journals.uchicago.edu/na101/home/literatum/publisher/uchicago/journals/content/jg/1980/i30063875/628553/20180625/images/eqs/eq-00001.gif\")
of water that catastrophically drained the largest glacial Lakes Missoula. Evidence that the Touchet Beds rhythmites originated from brief backfloodings includes up-valley thinning and fining of locally derived bedload, upvalley paleocurrents, and upvalley transport of erratics derived from Cordilleran ice. Evidence that a lengthy nonflood environment followed the emplacement of each of about 40 Touchet Beds rhythmite includes inferred eolian and slopewash sediment overlying many rhythmites, uncontaminated Mount St. Helens \"set S\" tephra couplet atop one rhythmite as much as 220 m below the maximum level of backflooding, filled semiconsolidated rodent burrows throughout the 30 m of the thickest section, and dispersed skeletons of mammals. The lack of weathering or soil within the Touchet Beds suggests that all rhythmites are late Wisconsin. Bottom sediment of glacial Lake Missoula in Montana consists of rhythmites each interpreted as the record of a gradually deepening lake. Forty superposed rhythmites record about 40 late-Wisconsin fillings and emptyings of glacial Lake Missoula. The complementary records of about 40 separate glacial Lakes Missoula and about 40 great floods in southern Washington and in the Willamette Valley, Oregon indicate that the Missoula floods were great jokulhlaups. The last several floods were smaller than earlier ones because the controlling dam of Cordilleran ice thinned during deglaciation.
","language":"English","publisher":"University of Chicago Press","doi":"10.1086/628553","issn":"00221376","usgsCitation":"Waitt, R.B., 1980, About forty last-glacial Lake Missoula jokulhlaups through southern Washington: Journal of Geology, v. 88, no. 6, p. 653-679, https://doi.org/10.1086/628553.","productDescription":"27 p.","startPage":"653","endPage":"679","numberOfPages":"27","costCenters":[],"links":[{"id":222051,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"88","issue":"6","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"5059e644e4b0c8380cd472d5","contributors":{"authors":[{"text":"Waitt, R. B. Jr.","contributorId":48558,"corporation":false,"usgs":true,"family":"Waitt","given":"R.","suffix":"Jr.","email":"","middleInitial":"B.","affiliations":[],"preferred":false,"id":362762,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":70012181,"text":"70012181 - 1980 - Evaluation of multispectral middle infrared aircraft images for lithologic mapping in the East Tintic Mountains, Utah","interactions":[],"lastModifiedDate":"2024-02-01T23:13:00.365141","indexId":"70012181","displayToPublicDate":"1980-01-01T00:00:00","publicationYear":"1980","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1796,"text":"Geology","active":true,"publicationSubtype":{"id":10}},"title":"Evaluation of multispectral middle infrared aircraft images for lithologic mapping in the East Tintic Mountains, Utah","docAbstract":"Six channels of multispectral middle infrared (8 to 14 μrn) aircraft scanner data were acquired over the East Tintic mining district, Utah. This area has high relief and moderate vegetation and consists mainly of Tertiary silicic igneous rocks and Paleozoic quartzite and carbonate rocks that have been locally hydro thermally altered. These digital-image data were computer processed to create a color-composite image based on principal component transformations. Color differences in this image are related to the spectral differences in the surface material and allow discrimination of several rock types, depending primarily on their silica content. When combined with a visible and near infrared color-composite image from a previous flight, with limited field checking, it is possible to discriminate quartzite, carbonate rocks, quartz latitic and quartz monzonitic rocks, latitic and monzonitic rocks, silicified altered rocks, argillized altered rocks, and vegetation.
The northern part of the Yucatan Peninsula is a relatively flat, low-lying carbonate terrane with no geomorphic expressions of stream channels. It is estimated that mean annual recharge to the groundwater system is 150 mm. For the 65,500 km2 study area, mean annual discharge (equivalent to recharge) is 9.8 × 109 m3, or 8.6 × 106 m3 for each 1 km of the 1,100-km-long coastline. In the interior of the peninsula, the recharging water annually dissolves about 37.5 t (metric tons) of calcite per 1 km2. When the groundwater has become saturated with calcite, little additional water-rock interaction occurs until the active mixing (dispersion) zone is reached near the coastline.
Theoretical calculations and laboratory experiments have shown that when two waters, each calcite saturated and with different salinities, are mixed, the resulting solution generally becomes undersaturated with calcite and, therefore, is capable of dissolving additional calcite. On the basis of our study of the Xel Ha lagoon on the east coast of Yucatan, we calculate that as much as 1.2 mmol/L additional calcite can be dissolved in the brackish groundwater zone of dispersion. This indicates that if the total solution potential of the amount of water discharging at Xel Ha has focused within the lagoon area, the lagoon could be chemically incised in less than 3,000 yr. We postulate that chemical mass wasting by dissolution in the zone of groundwater mixing is an important geomorphic process in coastal areas of limestone terranes.
","language":"English","publisher":"GeoScienceWorld","doi":"10.1130/0091-7613(1980)8<222:CMOTNY>2.0.CO;2","issn":"00917613","usgsCitation":"Hanshaw, B., and Back, W., 1980, Chemical mass-wasting of the northern Yucatan Peninsula by groundwater dissolution: Geology, v. 8, no. 5, p. 222-224, https://doi.org/10.1130/0091-7613(1980)8<222:CMOTNY>2.0.CO;2.","productDescription":"3 p. ","startPage":"222","endPage":"224","numberOfPages":"3","costCenters":[],"links":[{"id":221996,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"Mexico ","otherGeospatial":"Yucatan Peninsula","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"type\": \"Polygon\",\n \"coordinates\": [\n [\n [\n -91.62597656249999,\n 18.114529138838503\n ],\n [\n -86.429443359375,\n 18.114529138838503\n ],\n [\n -86.429443359375,\n 22.471954507739227\n ],\n [\n -91.62597656249999,\n 22.471954507739227\n ],\n [\n -91.62597656249999,\n 18.114529138838503\n ]\n ]\n ]\n }\n }\n ]\n}","volume":"8","issue":"5","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"5059f57fe4b0c8380cd4c272","contributors":{"authors":[{"text":"Hanshaw, B.B.","contributorId":25928,"corporation":false,"usgs":true,"family":"Hanshaw","given":"B.B.","email":"","affiliations":[],"preferred":false,"id":362942,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Back, W.","contributorId":33839,"corporation":false,"usgs":true,"family":"Back","given":"W.","email":"","affiliations":[],"preferred":false,"id":362943,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":70010384,"text":"70010384 - 1980 - Thallium identification in selected atmospheric deposition samples","interactions":[],"lastModifiedDate":"2023-02-09T17:51:22.970427","indexId":"70010384","displayToPublicDate":"1980-01-01T00:00:00","publicationYear":"1980","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":924,"text":"Atmospheric Environment","active":true,"publicationSubtype":{"id":10}},"title":"Thallium identification in selected atmospheric deposition samples","docAbstract":"No abstract available.
","language":"English","publisher":"Elsevier","doi":"10.1016/0004-6981(80)90152-3","issn":"00046981","usgsCitation":"Bonelli, J.E., Taylor, H.E., Schroder, L., and Skogerboe, R., 1980, Thallium identification in selected atmospheric deposition samples: Atmospheric Environment, v. 14, no. 7, p. 867-870, https://doi.org/10.1016/0004-6981(80)90152-3.","productDescription":"4 p.","startPage":"867","endPage":"870","costCenters":[],"links":[{"id":218797,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United States","state":"New York, 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E.","contributorId":35064,"corporation":false,"usgs":true,"family":"Bonelli","given":"J.","email":"","middleInitial":"E.","affiliations":[],"preferred":false,"id":358797,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Taylor, Howard E. hetaylor@usgs.gov","contributorId":1551,"corporation":false,"usgs":true,"family":"Taylor","given":"Howard","email":"hetaylor@usgs.gov","middleInitial":"E.","affiliations":[{"id":5044,"text":"National Research Program - Central Branch","active":true,"usgs":true}],"preferred":true,"id":358795,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Schroder, L.J.","contributorId":31767,"corporation":false,"usgs":true,"family":"Schroder","given":"L.J.","email":"","affiliations":[{"id":595,"text":"U.S. Geological Survey","active":false,"usgs":true}],"preferred":false,"id":358796,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Skogerboe, R.K.","contributorId":7348,"corporation":false,"usgs":true,"family":"Skogerboe","given":"R.K.","email":"","affiliations":[],"preferred":false,"id":358794,"contributorType":{"id":1,"text":"Authors"},"rank":4}]}}
,{"id":70010385,"text":"70010385 - 1980 - The age curves of sulfur and oxygen isotopes in marine sulfate and their mutual interpretation","interactions":[],"lastModifiedDate":"2014-08-19T11:33:04","indexId":"70010385","displayToPublicDate":"1980-01-01T00:00:00","publicationYear":"1980","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1213,"text":"Chemical Geology","active":true,"publicationSubtype":{"id":10}},"title":"The age curves of sulfur and oxygen isotopes in marine sulfate and their mutual interpretation","docAbstract":"Three hundred new samples of marine evaporite sulfate, of world-wide distribution, were analyzed for δ34S, and 60 of these also for δ18O in the sulfate ion. Detailed δ34S age curves for Tertiary—Cretaceous, Permian—Pennsylvanian, Devonian, Cambrian and Proterozoic times document large variations in δ34S. A summary curve forδ18O also shows definite variations, some at different times than δ34S, and always smaller. The measured δ34S and δ18O correspond to variations in these isotopes in sulfate of the world ocean surface. The variations of δ18O are controlled by input and output fluxes of sulfur in the ocean, three of which are the same that control δ34S: deposition and erosion of sulfate, and deposition of sulfide. Erosion of sulfide differs in its effect on the S and O systems. δ18O in the sulfate does not seem to be measurably affected by equilibration with either seawater or with subsurface waters after crystallization. In principle, the simultaneous application of both δ34S and δ18O age curves should help reduce the number of assumptions in calculations of the cycles of sulfur and oxygen through geological time, and a new model involving symmetrical fluxes is introduced here to take advantage of the oxygen data. However, all previously published models as well as this one lead to anomalies, such as unreasonable calcium or oxygen depletions in the ocean—atmosphere system. In addition, most models are incapable of reproducing the sharp rises of the δ34S curve in the late Proterozoic, the Devonian and the Triassic which would be the result of unreasonably fast net sulfide deposition. This fast depletion could result from an ocean that has not always been mixed (as previously assumed in all model calculations).","largerWorkType":{"id":2,"text":"Article"},"largerWorkTitle":"Chemical Geology","largerWorkSubtype":{"id":10,"text":"Journal Article"},"language":"English","publisher":"Elsevier","publisherLocation":"New York, NY","doi":"10.1016/0009-2541(80)90047-9","issn":"00092541","usgsCitation":"Claypool, G.E., Holser, W.T., Kaplan, I.R., Sakai, H., and Zak, I., 1980, The age curves of sulfur and oxygen isotopes in marine sulfate and their mutual interpretation: Chemical Geology, v. 28, no. C, p. 199-260, https://doi.org/10.1016/0009-2541(80)90047-9.","productDescription":"62 p.","startPage":"199","endPage":"260","numberOfPages":"62","costCenters":[],"links":[{"id":218864,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"},{"id":266126,"type":{"id":10,"text":"Digital Object Identifier"},"url":"https://dx.doi.org/10.1016/0009-2541(80)90047-9"}],"volume":"28","issue":"C","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"505ba9ade4b08c986b32241d","contributors":{"authors":[{"text":"Claypool, George E.","contributorId":76312,"corporation":false,"usgs":true,"family":"Claypool","given":"George","email":"","middleInitial":"E.","affiliations":[],"preferred":false,"id":358802,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Holser, William T.","contributorId":12131,"corporation":false,"usgs":true,"family":"Holser","given":"William","email":"","middleInitial":"T.","affiliations":[],"preferred":false,"id":358799,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Kaplan, Isaac R.","contributorId":8218,"corporation":false,"usgs":true,"family":"Kaplan","given":"Isaac","email":"","middleInitial":"R.","affiliations":[],"preferred":false,"id":358798,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Sakai, Hitoshi","contributorId":30639,"corporation":false,"usgs":true,"family":"Sakai","given":"Hitoshi","email":"","affiliations":[],"preferred":false,"id":358800,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"Zak, Israel","contributorId":48697,"corporation":false,"usgs":true,"family":"Zak","given":"Israel","email":"","affiliations":[],"preferred":false,"id":358801,"contributorType":{"id":1,"text":"Authors"},"rank":5}]}}
,{"id":70012184,"text":"70012184 - 1980 - The distribution and mobility of uranium in glassy and zeolitized tuff, Keg Mountain area, Utah, U.S.A.","interactions":[],"lastModifiedDate":"2013-01-21T12:34:59","indexId":"70012184","displayToPublicDate":"1980-01-01T00:00:00","publicationYear":"1980","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1213,"text":"Chemical Geology","active":true,"publicationSubtype":{"id":10}},"title":"The distribution and mobility of uranium in glassy and zeolitized tuff, Keg Mountain area, Utah, U.S.A.","docAbstract":"The distribution and mobility of uranium in a diagenetically altered, 8 Ma old tuff in the Keg Mountain area, Utah, are modelled in this study. The modelling represents an improvement over similar earlier studies in that it: (1) considers a large number of samples (76) collected with good geologic control and exhibiting a wide range of alteration; (2) includes radiometric data for Th, K and RaeU (radium equivalent uranium) as well as U; (3) considers mineralogic and trace-element data for the same samples; and (4) analyzes the mineral and chemical covariation by multivariate statistical methods. The variation of U in the tuff is controlled mainly by its primary abundance in glass and by the relative abundance of non-uraniferous detritus and uraniferous accessory minerals. Alteration of glass to zeolite, even though extensive, caused no large or systematic change in the bulk concentration of U in the tuff. Some redistribution of U during diagenesis is indicated by association of U with minor alteration products such as opal and hydrous Fe-Mn oxide minerals. Isotopic studies indicate that the zeolitized tuff has been open to migration of U decay products during the last 0.8 Ma. The tuff of Keg Mountain has not lost a statistically detectable fraction of its original U, even though it has a high (??? 9 ppm) trace U content and has been extensively altered to zeolite. Similar studies in a variety of geological environments are required in order to identify the particular combination of conditions most favorable for liberation and migration of U from tuffs. ?? 1980.","largerWorkType":{"id":2,"text":"Article"},"largerWorkTitle":"Chemical Geology","largerWorkSubtype":{"id":10,"text":"Journal Article"},"language":"English","publisher":"Elsevier","doi":"10.1016/0009-2541(80)90010-8","issn":"00092541","usgsCitation":"Zielinski, R.A., Lindsey, D.A., and Rosholt, J., 1980, The distribution and mobility of uranium in glassy and zeolitized tuff, Keg Mountain area, Utah, U.S.A.: Chemical Geology, v. 29, no. 1-4, p. 139-162, https://doi.org/10.1016/0009-2541(80)90010-8.","startPage":"139","endPage":"162","numberOfPages":"24","costCenters":[],"links":[{"id":221997,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"},{"id":266129,"type":{"id":10,"text":"Digital Object Identifier"},"url":"https://dx.doi.org/10.1016/0009-2541(80)90010-8"}],"volume":"29","issue":"1-4","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"505baacce4b08c986b322a0a","contributors":{"authors":[{"text":"Zielinski, R. A. 0000-0002-4047-5129","orcid":"https://orcid.org/0000-0002-4047-5129","contributorId":106930,"corporation":false,"usgs":true,"family":"Zielinski","given":"R.","email":"","middleInitial":"A.","affiliations":[{"id":164,"text":"Central Energy Resources Science Center","active":true,"usgs":true}],"preferred":false,"id":362946,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Lindsey, D. A.","contributorId":49814,"corporation":false,"usgs":true,"family":"Lindsey","given":"D.","email":"","middleInitial":"A.","affiliations":[],"preferred":false,"id":362945,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Rosholt, J.N.","contributorId":37749,"corporation":false,"usgs":true,"family":"Rosholt","given":"J.N.","email":"","affiliations":[],"preferred":false,"id":362944,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":70012174,"text":"70012174 - 1980 - Circular current loops, magnetic dipoles and spherical harmonic analysis.","interactions":[],"lastModifiedDate":"2013-03-14T12:43:03","indexId":"70012174","displayToPublicDate":"1980-01-01T00:00:00","publicationYear":"1980","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":2310,"text":"Journal of Geomagnetism & Geoelectricity","active":true,"publicationSubtype":{"id":10}},"title":"Circular current loops, magnetic dipoles and spherical harmonic analysis.","docAbstract":"Spherical harmonic analysis (SHA) is the most used method of describing the Earth's magnetic field, even though spherical harmonic coefficients (SHC) almost completely defy interpretation in terms of real sources. Some moderately successful efforts have been made to represent the field in terms of dipoles placed in the core in an effort to have the model come closer to representing real sources. Dipole sources are only a first approximation to the real sources which are thought to be a very complicated network of electrical currents in the core of the Earth. -Author","largerWorkType":{"id":2,"text":"Article"},"largerWorkTitle":"Journal of Geomagnetism & Geoelectricity","largerWorkSubtype":{"id":10,"text":"Journal Article"},"language":"English","doi":"10.5636/jgg.32.357","issn":"00221392","usgsCitation":"Alldredge, L., 1980, Circular current loops, magnetic dipoles and spherical harmonic analysis.: Journal of Geomagnetism & Geoelectricity, v. 32, no. 6, p. 357-364, https://doi.org/10.5636/jgg.32.357.","startPage":"357","endPage":"364","numberOfPages":"8","costCenters":[],"links":[{"id":480594,"rank":1,"type":{"id":40,"text":"Open Access Publisher Index Page"},"url":"https://doi.org/10.5636/jgg.32.357","text":"Publisher Index Page"},{"id":269317,"type":{"id":10,"text":"Digital Object Identifier"},"url":"https://dx.doi.org/10.5636/jgg.32.357"},{"id":221872,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"32","issue":"6","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"5059f602e4b0c8380cd4c548","contributors":{"authors":[{"text":"Alldredge, L.R.","contributorId":53457,"corporation":false,"usgs":true,"family":"Alldredge","given":"L.R.","email":"","affiliations":[],"preferred":false,"id":362925,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":70012185,"text":"70012185 - 1980 - Geology and biology of Oceanographer submarine canyon.","interactions":[],"lastModifiedDate":"2012-03-12T17:19:04","indexId":"70012185","displayToPublicDate":"1980-01-01T00:00:00","publicationYear":"1980","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":2667,"text":"Marine Geology","active":true,"publicationSubtype":{"id":10}},"title":"Geology and biology of Oceanographer submarine canyon.","docAbstract":"Santonian beds more than 100 m thick are the oldest rocks collected from the canyon. Quaternary silty clay veneers the canyon walls in many places and is commonly burrowed by benthic organisms that cause extensive erosion of the canyon walls, especially in the depth zone (100-1300 m) inhabited by the crabs Geryon and Cancer. Bioerosion is minimal on high, near-vertical cliffs of sedimentary rock, in areas of continual sediment movement, and where the sea floor is paved by gravel. A thin layer of rippled, unconsolidated silt and sand is commonly present on the canyon walls and in the axis. Shelf sediments are transported from Georges Bank over the E rim and in the Canyon by the SW drift and storm currents; tidal currents and internal waves move the sediment downcanyon along the walls and axis.- from Authors","largerWorkType":{"id":2,"text":"Article"},"largerWorkTitle":"Marine Geology","largerWorkSubtype":{"id":10,"text":"Journal Article"},"language":"English","doi":"10.1016/0025-3227(80)90004-3","issn":"00253227","usgsCitation":"Valentine, P.C., Uzmann, J., and Cooper, R., 1980, Geology and biology of Oceanographer submarine canyon.: Marine Geology, v. 38, no. 4, p. 283-312, https://doi.org/10.1016/0025-3227(80)90004-3.","startPage":"283","endPage":"312","numberOfPages":"30","costCenters":[],"links":[{"id":222056,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"},{"id":205189,"rank":9999,"type":{"id":10,"text":"Digital Object Identifier"},"url":"https://dx.doi.org/10.1016/0025-3227(80)90004-3"}],"volume":"38","issue":"4","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"505a22a3e4b0c8380cd57209","contributors":{"authors":[{"text":"Valentine, P. C.","contributorId":46505,"corporation":false,"usgs":true,"family":"Valentine","given":"P.","email":"","middleInitial":"C.","affiliations":[],"preferred":false,"id":362949,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Uzmann, J. R.","contributorId":38647,"corporation":false,"usgs":true,"family":"Uzmann","given":"J. R.","affiliations":[],"preferred":false,"id":362948,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Cooper, R.A.","contributorId":29509,"corporation":false,"usgs":true,"family":"Cooper","given":"R.A.","email":"","affiliations":[],"preferred":false,"id":362947,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":70012186,"text":"70012186 - 1980 - Stress measurements at depth in the vicinity of the San Andreas fault. Implications for the magnitude of shear stress at depth","interactions":[],"lastModifiedDate":"2024-07-17T14:02:08.413139","indexId":"70012186","displayToPublicDate":"1980-01-01T00:00:00","publicationYear":"1980","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":6453,"text":"Journal of Geophysical Research Solid Earth","active":true,"publicationSubtype":{"id":10}},"title":"Stress measurements at depth in the vicinity of the San Andreas fault. Implications for the magnitude of shear stress at depth","docAbstract":"Using the hydraulic fracturing technique, we have made a systematic series of in situ stress measurements in wells drilled near the San Andreas fault. In an attempt to provide constraints for the magnitude of shear stress on the San Andreas fault at depth we have measured both the variation of stress with distance from the fault in relatively shallow (∼230 m) wells and the variation of stress with depth in a ∼1-km-deep well located 4 km from the fault. The shallow wells are located along profiles roughly perpendicular to the fault in the western Mojave desert near Palmdale and in central California where the fault is creeping. In both areas the direction of maximum compression was found to be approximately 45° from the local trend of the San Andreas. The two stress profiles show very similar results: (1) shear stress (on planes parallel to the San Andreas) increases with distance from the fault, more markedly in the western Mojave, (2) the far-field shear stress at ∼200 m depth is ∼50 bars, and (3) the horizontal principal stresses as well as shear stress increase with depth more rapidly in the wells farthest from the fault. The ∼1-km-deep well, also located in the western Mojave desert, shows increases of both horizontal principal stresses and shear stress with depth. Shear stress increases from about 25 bars at 150–300 m to about 80 bars at 750–850 m. Although this rapid increase of shear stress with depth suggests that the mean shear stress on the fault at seismogenic depths exceeds several hundred bars, the principal stresses increase with depth in a steplike manner. As this may be a near-surface effect, extrapolation of the measurements to much greater depths may not be warranted.
","language":"English","publisher":"American Geophysical Union","doi":"10.1029/JB085iB11p06157","issn":"01480227","usgsCitation":"Zobach, M., Tsukahara, H., and Hickman, S., 1980, Stress measurements at depth in the vicinity of the San Andreas fault. Implications for the magnitude of shear stress at depth: Journal of Geophysical Research Solid Earth, v. 85, no. B11, p. 6157-6173, https://doi.org/10.1029/JB085iB11p06157.","productDescription":"17 p.","startPage":"6157","endPage":"6173","numberOfPages":"17","costCenters":[],"links":[{"id":222057,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"85","issue":"B11","noUsgsAuthors":false,"publicationDate":"2012-09-20","publicationStatus":"PW","scienceBaseUri":"505b9b5fe4b08c986b31ce2e","contributors":{"authors":[{"text":"Zobach, M.D.","contributorId":20218,"corporation":false,"usgs":true,"family":"Zobach","given":"M.D.","email":"","affiliations":[],"preferred":false,"id":362951,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Tsukahara, H.","contributorId":16280,"corporation":false,"usgs":true,"family":"Tsukahara","given":"H.","email":"","affiliations":[],"preferred":false,"id":362950,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Hickman, S.","contributorId":79995,"corporation":false,"usgs":true,"family":"Hickman","given":"S.","email":"","affiliations":[],"preferred":false,"id":362952,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":70012189,"text":"70012189 - 1980 - Leg 67: the Deep Sea Drilling Project Mid-America Trench transect off Guatemala.","interactions":[],"lastModifiedDate":"2018-01-08T12:53:33","indexId":"70012189","displayToPublicDate":"1980-01-01T00:00:00","publicationYear":"1980","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1786,"text":"Geological Society of America Bulletin","active":true,"publicationSubtype":{"id":10}},"title":"Leg 67: the Deep Sea Drilling Project Mid-America Trench transect off Guatemala.","docAbstract":"Drilling on the Cocos plate recovered a basal chalk sequence deposited during early and mid-Miocene time, a short interval of abyssal red clay, and an upper sequence of late Miocene and younger sediment deposited within an area influenced by a terrigenous source. In the trench, a mud and sand fill less than 400,000 yr old overlies the oceanic sequence. The entire section shows no evidence of compressive deformation. In contrast, the section cored on the trench's landward slope 3 km from the trench axis is affected by tectonism. The section contains a Cretaceous to Pliocene claystone sequence capped by Pliocene to Quaternary hemipelagic slope deposits.- from Authors","largerWorkType":{"id":2,"text":"Article"},"largerWorkTitle":"Geological Society of America Bulletin","largerWorkSubtype":{"id":10,"text":"Journal Article"},"language":"English","publisher":"Geological Society of America","doi":"10.1130/0016-7606(1980)91<421:LTDSDP>2.0.CO;2","usgsCitation":"von Huene, R.E., 1980, Leg 67: the Deep Sea Drilling Project Mid-America Trench transect off Guatemala.: Geological Society of America Bulletin, v. 91, no. 7 pt 1, p. 421-432, https://doi.org/10.1130/0016-7606(1980)91<421:LTDSDP>2.0.CO;2.","startPage":"421","endPage":"432","numberOfPages":"12","costCenters":[],"links":[{"id":222060,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"},{"id":268124,"type":{"id":10,"text":"Digital Object Identifier"},"url":"https://dx.doi.org/10.1130/0016-7606(1980)91<421:LTDSDP>2.0.CO;2"}],"volume":"91","issue":"7 pt 1","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"505a463be4b0c8380cd675d2","contributors":{"authors":[{"text":"von Huene, Roland E. 0000-0003-1301-3866 rvonhuene@usgs.gov","orcid":"https://orcid.org/0000-0003-1301-3866","contributorId":191070,"corporation":false,"usgs":true,"family":"von Huene","given":"Roland","email":"rvonhuene@usgs.gov","middleInitial":"E.","affiliations":[{"id":237,"text":"Earthquake Science Center","active":true,"usgs":true},{"id":7065,"text":"USGS emeritus","active":true,"usgs":false}],"preferred":false,"id":362958,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":70012190,"text":"70012190 - 1980 - Tertiary climates and floristic relationships at high latitudes in the northern hemisphere","interactions":[],"lastModifiedDate":"2013-02-19T16:22:06","indexId":"70012190","displayToPublicDate":"1980-01-01T00:00:00","publicationYear":"1980","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":2996,"text":"Palaeogeography, Palaeoclimatology, Palaeoecology","printIssn":"0031-0182","active":true,"publicationSubtype":{"id":10}},"title":"Tertiary climates and floristic relationships at high latitudes in the northern hemisphere","docAbstract":"During the Paleocene and Eocene, climates were characterized by a low mean annual range of temperature (a maximum of 10-15??C), a moderate to high mean annual temperature (10-20??C), and abundant precipitation; strong broad-leaved evergreen vegetation extended to almost lat. 60??N during the Paleocene and to well above 61??N during the Eocene. Poleward of the broad-leaved evergreen forests were forests that were broad-leaved deciduous; these deciduous forests, however, were unlike extant broad-leaved deciduous forests in general floristic composition and physiognomy. Coniferous forests probably occupied the northernmost latitudes. At the end of the Eocene, a major climatic deterioration resulted in a high (> 30??C) mean annual range of temperature and a low mean annual temperature (< 10??C). Vegetation represented temperate broad-leaved deciduous and coniferous forests. The Oligocene and Neogene climatic trends represent a decrease in both mean annual range of temperature and mean annual temperature. Tundra vegetation did not appear until late in the Neogene. The present distribution of broad-leaved evergreens concomitant with the principles of plant physiology indicates that present winter light conditions at high latitudes could not support broad-leaved evergreen forest. A possible solution to the problem is to increase winter light by lessening the inclination of the earth's rotational axis. ?? 1980.","largerWorkType":{"id":2,"text":"Article"},"largerWorkTitle":"Palaeogeography, Palaeoclimatology, Palaeoecology","largerWorkSubtype":{"id":10,"text":"Journal Article"},"language":"English","publisher":"Elsevier","doi":"10.1016/0031-0182(80)90063-2","issn":"00310182","usgsCitation":"Wolfe, J.A., 1980, Tertiary climates and floristic relationships at high latitudes in the northern hemisphere: Palaeogeography, Palaeoclimatology, Palaeoecology, v. 30, no. C, p. 313-323, https://doi.org/10.1016/0031-0182(80)90063-2.","startPage":"313","endPage":"323","numberOfPages":"11","costCenters":[],"links":[{"id":267791,"type":{"id":10,"text":"Digital Object Identifier"},"url":"https://dx.doi.org/10.1016/0031-0182(80)90063-2"},{"id":222120,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"30","issue":"C","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"505ba56fe4b08c986b320a50","contributors":{"authors":[{"text":"Wolfe, J. A.","contributorId":14026,"corporation":false,"usgs":true,"family":"Wolfe","given":"J.","email":"","middleInitial":"A.","affiliations":[],"preferred":false,"id":362959,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":70012171,"text":"70012171 - 1980 - Distribution of modern benthic foraminifers on the New Jersey Outer Continental Shelf","interactions":[],"lastModifiedDate":"2019-12-04T06:43:07","indexId":"70012171","displayToPublicDate":"1980-01-01T00:00:00","publicationYear":"1980","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":2673,"text":"Marine Micropaleontology","active":true,"publicationSubtype":{"id":10}},"title":"Distribution of modern benthic foraminifers on the New Jersey Outer Continental Shelf","docAbstract":"We used samples from 21 stations within a 600 km2 area of the New Jersey Outer Continental Shelf to assess the effects of a hydrodynamic environment on the distribution and redistribution of benthic foraminifers. These samples show that, although the predominant genera (Elphidium, Cibicides, and Saccammina) are the same as those reported by other investigators for this region, the environmental factors that control the generic distribution are more complex than were previously postulated. Generic distribution patterns derived from this study are correlated with the bottom topography and sediment distribution as well as the temperature, salinity, and dissolved oxygen concentrations of the bottom waters. The six predominant species observed in the samples (and their phenotypic variants) are cryophilic forms known to occur in the Virginian and Nova Scotian biogeographic provinces and in Arctic waters. Species distribution patterns also correlate well with bottom topography and hydrographic factors, but may be modified by seasonal fluctuations in test production and by redistribution of dead tests. At most stations, specimens of Elphidium subarcticum were attached to quartz grains. This phenomenon, which has not been reported before, probably is an adaptation to a high-energy environment. The distribution pattern of Elphidium subarcticum along with those of the sessile species Webbinella concava and Vasiglobulina n.sp. corroborate sedimentological evidence that the accumulation of modern sediments in the area is negligible.
","language":"English","publisher":"Elsevier","doi":"10.1016/0377-8398(80)90006-7","issn":"03778398","usgsCitation":"Poag, C.W., Knebel, H., and Todd, R., 1980, Distribution of modern benthic foraminifers on the New Jersey Outer Continental Shelf: Marine Micropaleontology, v. 5, no. C, p. 43-69, https://doi.org/10.1016/0377-8398(80)90006-7.","productDescription":"27 p. ","startPage":"43","endPage":"69","numberOfPages":"27","costCenters":[],"links":[{"id":221869,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United States","state":"New Jersey 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Jersey\",\"nation\":\"USA \"}}]}","volume":"5","issue":"C","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"505a02e5e4b0c8380cd50252","contributors":{"authors":[{"text":"Poag, C. Wylie","contributorId":52714,"corporation":false,"usgs":true,"family":"Poag","given":"C.","email":"","middleInitial":"Wylie","affiliations":[],"preferred":false,"id":362919,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Knebel, H.J.","contributorId":79092,"corporation":false,"usgs":true,"family":"Knebel","given":"H.J.","affiliations":[],"preferred":false,"id":362921,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Todd, R.","contributorId":77654,"corporation":false,"usgs":true,"family":"Todd","given":"R.","email":"","affiliations":[],"preferred":false,"id":362920,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":70012194,"text":"70012194 - 1980 - Influence of San Gabriel submarine canyon on narrow-shelf sediment dynamics, southern California","interactions":[],"lastModifiedDate":"2014-11-14T13:59:14","indexId":"70012194","displayToPublicDate":"1980-01-01T00:00:00","publicationYear":"1980","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":2667,"text":"Marine Geology","active":true,"publicationSubtype":{"id":10}},"title":"Influence of San Gabriel submarine canyon on narrow-shelf sediment dynamics, southern California","docAbstract":"Variations in the concentration of total suspended particulate matter (TSM) collected 1 m above bottom, changes in vertical profiles of light transmission, and substrate textural patterns reveal a corridor for preferential sediment transport on San Pedro continental shelf, California. During the winter, this corridor, designated the preferential transport corridor (PTC), is defined by higher concentrations of TSM relative to the rest of the shelf and extends for 10-15 km from the inner shelf to the head of San Gabriel Submarine Canyon. Vertical profiles of light transmission within the PTC suggest density stratification throughout the water column and apparent mixing in the upper 15-20 m of water column on either side of the PTC. The PTC is not as fully developed during the summer. Excursions in isopleths of substrate textural variables perpendicular to isobaths in the PTC suggest that although the PTC is seasonally episodic, it recurs regularly over a longer period.
\n
\nA conceptual model attributes the PTC to modification of shelf circulation patterns by San Gabriel Canyon. Surface waves diverge over the canyon head resulting in differential wave set up at the shore face. This forces back turbid nearshore water for a distance of a few kilometers toward the canyon. At some point on the shelf, seaward nearshore flow overlaps offshore currents generated or modified by internal waves focused onto the shelf by the canyon and/or turbulent eddies produced by flow separation in currents moving across the canyon axis. At times, these subtle processes overprint tidal and wind-driven currents and thereby create the PTC. The model suggests that canyons heading several kilometers from shore can have a regulatory effect on narrow-shelf sediment dynamics.
","language":"English","publisher":"Elsevier","doi":"10.1016/0025-3227(80)90141-3","issn":"00253227","usgsCitation":"Karl, H.A., 1980, Influence of San Gabriel submarine canyon on narrow-shelf sediment dynamics, southern California: Marine Geology, v. 34, no. 1-2, p. 61-78, https://doi.org/10.1016/0025-3227(80)90141-3.","productDescription":"18 p.","startPage":"61","endPage":"78","numberOfPages":"18","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[{"id":186,"text":"Coastal and Marine Geology Program","active":true,"usgs":true}],"links":[{"id":222184,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United States","state":"California","otherGeospatial":"San Gabriel Submarine Canyon","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"type\": \"Polygon\",\n \"coordinates\": [\n [\n [\n -118.31520080566406,\n 33.535671379525546\n ],\n [\n -118.31520080566406,\n 33.79854997801964\n ],\n [\n -117.91831970214842,\n 33.79854997801964\n ],\n [\n -117.91831970214842,\n 33.535671379525546\n ],\n [\n -118.31520080566406,\n 33.535671379525546\n ]\n ]\n ]\n }\n }\n ]\n}","volume":"34","issue":"1-2","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"505a3b05e4b0c8380cd62179","contributors":{"authors":[{"text":"Karl, Herman A.","contributorId":80649,"corporation":false,"usgs":true,"family":"Karl","given":"Herman","email":"","middleInitial":"A.","affiliations":[],"preferred":false,"id":362966,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":70012196,"text":"70012196 - 1980 - Comparison of bed form variance spectra within a meander bend during flood and average discharge","interactions":[],"lastModifiedDate":"2024-05-23T00:48:57.127749","indexId":"70012196","displayToPublicDate":"1980-01-01T00:00:00","publicationYear":"1980","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":2450,"text":"Journal of Sedimentary Petrology","active":true,"publicationSubtype":{"id":10}},"title":"Comparison of bed form variance spectra within a meander bend during flood and average discharge","docAbstract":"Time series analysis of streambed elevation in a meander bend along the Congaree River was used to determine the changes in bed form population succeeding a 16-year flood event. Bed forms observed during the flood event had a significantly greater total height variance than bed forms observed at the same location one week later. Variance spectra were computed for a 595 m longitudinal profile. The data indicate that: a) the bed form variance for the flood record is significantly greater for all wavelengths from 5 to 30 m; b) no well-demarcated bed form classes were present during the survey times, pointing to the possible existence of a continuum of bed form sizes rather than well-defined classes; and c) bed forms produced by the flood discharge were rapidly altered as the stage returned toward average level.
Emission spectra of the cations of 2,5- and 3,5-difluorophenol, of 2,3,4- and 2,4,5-trifluorophenol, of 2,3,5,6-tetrafluorophenol and of 2,3,4,5,6-pentafluorophenol have been obtained in the gas phase using low-energy electron beam excitation. The band systems are assigned to the B̃(π−1) → X̃(π−1) electronic transitions of these cations by reference to photoelectron spectroscopic data. The He(Iα) photoelectron spectra and the ionisation energies of ten fluoro-substituted phenols are reported. The symmetries of the four lowest electronic states of these cations are inferred from the radiative decay studies. The lifetimes of the lowest vibrational levels of the B̃(π−1) state of the six fluoro-substituted phenol cations above have also been measured.
","language":"English","publisher":"Elsevier","doi":"10.1016/0368-2048(80)80031-4","issn":"03682048","usgsCitation":"Maier, J.P., Marthaler, O., Mohraz, M., and Shiley, R., 1980, Emission spectra of the cations of some fluoro-substituted phenols in the gaseous phase: Journal of Electron Spectroscopy and Related Phenomena, v. 19, no. 1, p. 11-20, https://doi.org/10.1016/0368-2048(80)80031-4.","productDescription":"10 p.","startPage":"11","endPage":"20","numberOfPages":"10","costCenters":[],"links":[{"id":222244,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"19","issue":"1","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"505a08fce4b0c8380cd51d48","contributors":{"authors":[{"text":"Maier, John Paul","contributorId":61166,"corporation":false,"usgs":true,"family":"Maier","given":"John","email":"","middleInitial":"Paul","affiliations":[],"preferred":false,"id":362976,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Marthaler, O.","contributorId":89663,"corporation":false,"usgs":true,"family":"Marthaler","given":"O.","email":"","affiliations":[],"preferred":false,"id":362977,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Mohraz, Manijeh","contributorId":26444,"corporation":false,"usgs":true,"family":"Mohraz","given":"Manijeh","email":"","affiliations":[],"preferred":false,"id":362974,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Shiley, R.H.","contributorId":44282,"corporation":false,"usgs":true,"family":"Shiley","given":"R.H.","email":"","affiliations":[],"preferred":false,"id":362975,"contributorType":{"id":1,"text":"Authors"},"rank":4}]}}
,{"id":65107,"text":"i1124 - 1980 - Geologic map of the Parker NW, Parker, and parts of the Whipple Mountains SW and Whipple Wash quadrangles, California and Arizona","interactions":[],"lastModifiedDate":"2023-08-02T16:09:13.367681","indexId":"i1124","displayToPublicDate":"1980-01-01T00:00:00","publicationYear":"1980","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":320,"text":"IMAP","code":"I","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"1124","title":"Geologic map of the Parker NW, Parker, and parts of the Whipple Mountains SW and Whipple Wash quadrangles, California and Arizona","docAbstract":"No abstract available.
","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/i1124","usgsCitation":"Dickey, D., Carr, W.J., and Bull, W., 1980, Geologic map of the Parker NW, Parker, and parts of the Whipple Mountains SW and Whipple Wash quadrangles, California and Arizona: U.S. Geological Survey IMAP 1124, 1 Plate: 70.75 x 51.74 inches, https://doi.org/10.3133/i1124.","productDescription":"1 Plate: 70.75 x 51.74 inches","costCenters":[],"links":[{"id":188962,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":419508,"rank":3,"type":{"id":30,"text":"Data Release"},"url":"https://doi.org/10.5066/P9F29ZMI","text":"USGS data release","description":"USGS data release","linkHelpText":"Digital database for the geologic map of the Parker NW, Parker, and parts of the Whipple Mountains SW and Whipple Wash quadrangles, California and Arizona"},{"id":101919,"rank":2,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_234.htm","linkFileType":{"id":5,"text":"html"}}],"scale":"24000","datum":"National Geodetic Vertical Datum 1929","country":"United States","state":"Arizona, California","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -114.5,34.1175 ], [ -114.5,34.284166666666664 ], [ -114.25,34.284166666666664 ], [ -114.25,34.1175 ], [ -114.5,34.1175 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4af4e4b07f02db691fc3","contributors":{"authors":[{"text":"Dickey, D.D.","contributorId":15612,"corporation":false,"usgs":true,"family":"Dickey","given":"D.D.","email":"","affiliations":[],"preferred":false,"id":272669,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Carr, W. J.","contributorId":9245,"corporation":false,"usgs":true,"family":"Carr","given":"W.","email":"","middleInitial":"J.","affiliations":[],"preferred":false,"id":272668,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Bull, W.B.","contributorId":96731,"corporation":false,"usgs":true,"family":"Bull","given":"W.B.","email":"","affiliations":[],"preferred":false,"id":272670,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":64774,"text":"i1254A - 1980 - Map showing water circulation and rates of sedimentation in the Port Isabel 1 degree by 2 degrees quadrangle, Texas","interactions":[],"lastModifiedDate":"2023-08-29T18:31:13.927695","indexId":"i1254A","displayToPublicDate":"1980-01-01T00:00:00","publicationYear":"1980","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":320,"text":"IMAP","code":"I","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"1254","subseriesTitle":"MGA","chapter":"A","title":"Map showing water circulation and rates of sedimentation in the Port Isabel 1 degree by 2 degrees quadrangle, Texas","docAbstract":"No abstract available.
","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/i1254A","usgsCitation":"Berryhill, H.L., and Trippet, A., 1980, Map showing water circulation and rates of sedimentation in the Port Isabel 1 degree by 2 degrees quadrangle, Texas: U.S. Geological Survey IMAP 1254, Report: 1 p.; 1 Plate: 46.83 x 24.80 inches, https://doi.org/10.3133/i1254A.","productDescription":"Report: 1 p.; 1 Plate: 46.83 x 24.80 inches","costCenters":[],"links":[{"id":255197,"rank":3,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/imap/1254a/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":255198,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/imap/1254a/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":420252,"rank":4,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_9078.htm","linkFileType":{"id":5,"text":"html"}},{"id":255199,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/imap/1254a/report-thumb.jpg"}],"scale":"250000","country":"United States","state":"Texas","otherGeospatial":"Port Isabel 1 degree x 2 degrees quadrangle","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"type\": \"Polygon\",\n \"coordinates\": [\n [\n [\n -97.5,\n 28\n ],\n [\n -97.5,\n 27\n ],\n [\n -96,\n 27\n ],\n [\n -96,\n 28\n ],\n [\n -97.5,\n 28\n ]\n ]\n ]\n }\n }\n ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a6fe4b07f02db640e0a","contributors":{"authors":[{"text":"Berryhill, H. L. Jr.","contributorId":35361,"corporation":false,"usgs":true,"family":"Berryhill","given":"H.","suffix":"Jr.","email":"","middleInitial":"L.","affiliations":[],"preferred":false,"id":272129,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Trippet, A. R.","contributorId":105377,"corporation":false,"usgs":true,"family":"Trippet","given":"A. R.","affiliations":[],"preferred":false,"id":272130,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":8043,"text":"ofr8078 - 1980 - Intrusive rocks and plutonic belts of southeastern Alaska, U.S.A.","interactions":[{"subject":{"id":8043,"text":"ofr8078 - 1980 - Intrusive rocks and plutonic belts of southeastern Alaska, U.S.A.","indexId":"ofr8078","publicationYear":"1980","noYear":false,"title":"Intrusive rocks and plutonic belts of southeastern Alaska, U.S.A."},"predicate":"SUPERSEDED_BY","object":{"id":70209349,"text":"70209349 - 1983 - Intrusive rocks and plutonic belts of southeastern Alaska, U.S.A","indexId":"70209349","publicationYear":"1983","noYear":false,"title":"Intrusive rocks and plutonic belts of southeastern Alaska, U.S.A"},"id":1}],"supersededBy":{"id":70209349,"text":"70209349 - 1983 - Intrusive rocks and plutonic belts of southeastern Alaska, U.S.A","indexId":"70209349","publicationYear":"1983","noYear":false,"title":"Intrusive rocks and plutonic belts of southeastern Alaska, U.S.A"},"lastModifiedDate":"2022-12-09T20:54:28.56421","indexId":"ofr8078","displayToPublicDate":"1980-01-01T00:00:00","publicationYear":"1980","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":330,"text":"Open-File Report","code":"OFR","onlineIssn":"2331-1258","printIssn":"0196-1497","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"80-78","title":"Intrusive rocks and plutonic belts of southeastern Alaska, U.S.A.","docAbstract":"No abstract available.
","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr8078","usgsCitation":"Brew, D.A., and Morrell, R.P., 1980, Intrusive rocks and plutonic belts of southeastern Alaska, U.S.A.: U.S. Geological Survey Open-File Report 80-78, 34 p., https://doi.org/10.3133/ofr8078.","productDescription":"34 p.","costCenters":[],"links":[{"id":111882,"rank":1,"type":{"id":15,"text":"Index Page"},"url":"https://www.dggs.dnr.state.ak.us/pubs/id/11346","linkFileType":{"id":5,"text":"html"}},{"id":140556,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"}],"country":"United States","state":"Alaska","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"coordinates\": [\n [\n [\n -130.91165738230066,\n 54.5052029462494\n ],\n [\n -129.9776219386308,\n 55.523010781731585\n ],\n [\n -130.04554040824726,\n 56.13567819649876\n ],\n [\n -132.17858765960943,\n 57.01857118802178\n ],\n [\n -135.45408909743645,\n 59.83314697994663\n ],\n [\n -137.5306698428756,\n 58.89730477409603\n ],\n [\n -139.14097791234238,\n 60.22893609899762\n ],\n [\n -140.9138146230164,\n 60.21455185866205\n ],\n [\n -141.40765772484477,\n 59.82443600546523\n ],\n [\n -138.00072992473216,\n 58.78217744926826\n ],\n [\n -135.67440967635233,\n 56.881040947208646\n ],\n [\n -134.51737140263486,\n 55.75906000656332\n ],\n [\n -133.5149821776816,\n 54.90536552073422\n ],\n [\n -132.51121257205762,\n 54.605215543264734\n ],\n [\n -130.91165738230066,\n 54.5052029462494\n ]\n ]\n ],\n \"type\": \"Polygon\"\n }\n }\n ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e49bee4b07f02db5d11f5","contributors":{"authors":[{"text":"Brew, David A. dbrew@usgs.gov","contributorId":3244,"corporation":false,"usgs":true,"family":"Brew","given":"David","email":"dbrew@usgs.gov","middleInitial":"A.","affiliations":[],"preferred":true,"id":157041,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Morrell, Robert P.","contributorId":19157,"corporation":false,"usgs":true,"family":"Morrell","given":"Robert","email":"","middleInitial":"P.","affiliations":[],"preferred":false,"id":157042,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":40260,"text":"ofr79163 - 1980 - Coal resource occurrence and coal development potential maps of the Cabin Creek NW quadrangle, Sheridan County, Wyoming, and Powder River County, Montana","interactions":[],"lastModifiedDate":"2023-08-29T21:55:18.398837","indexId":"ofr79163","displayToPublicDate":"1980-01-01T00:00:00","publicationYear":"1980","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":330,"text":"Open-File Report","code":"OFR","onlineIssn":"2331-1258","printIssn":"0196-1497","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"79-163","title":"Coal resource occurrence and coal development potential maps of the Cabin Creek NW quadrangle, Sheridan County, Wyoming, and Powder River County, Montana","docAbstract":"No abstract available.
","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr79163","usgsCitation":"IntraSearch Inc., 1980, Coal resource occurrence and coal development potential maps of the Cabin Creek NW quadrangle, Sheridan County, Wyoming, and Powder River County, Montana: U.S. Geological Survey Open-File Report 79-163, Report: 33 p.; 59 Plates: 23.90 x 30.35 inches or smaller, https://doi.org/10.3133/ofr79163.","productDescription":"Report: 33 p.; 59 Plates: 23.90 x 30.35 inches or 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,{"id":9276,"text":"ofr80218 - 1980 - Geohydrology of southwestern Kansas","interactions":[{"subject":{"id":9276,"text":"ofr80218 - 1980 - Geohydrology of southwestern Kansas","indexId":"ofr80218","publicationYear":"1980","noYear":false,"title":"Geohydrology of southwestern Kansas"},"predicate":"SUPERSEDED_BY","object":{"id":70046183,"text":"70046183 - 1981 - Geohydrology of southwestern Kansas","indexId":"70046183","publicationYear":"1981","noYear":false,"title":"Geohydrology of southwestern Kansas"},"id":1}],"supersededBy":{"id":70046183,"text":"70046183 - 1981 - Geohydrology of southwestern Kansas","indexId":"70046183","publicationYear":"1981","noYear":false,"title":"Geohydrology of southwestern Kansas"},"lastModifiedDate":"2022-07-05T13:52:38.731892","indexId":"ofr80218","displayToPublicDate":"1980-01-01T00:00:00","publicationYear":"1980","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":330,"text":"Open-File Report","code":"OFR","onlineIssn":"2331-1258","printIssn":"0196-1497","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"80-218","title":"Geohydrology of southwestern Kansas","docAbstract":"Southwestern Kansas is one of the principal areas of ground-water development for irrigation in the State, and many reports are available concerning ground-water conditions in the area. The purposes of this investigation were to consolidate and update data, to determine the extent and effects of irrigation development on the ground-water resource, to determine the chemical quality of the ground water in relation to irrigation use, to describe the general operation of the hydrologic system, and to identify problem areas where intensive quantitative studies will be needed by State and local agencies for planning and management of the resource. This study began in 1972 as part of a cooperative program of ground-water investigations between the Kansas Geological Survey and the U.S. Geological Survey. Support in this study was provided by the Division of Water Resources of the Kansas State Board of Agriculture and the Division of Environment of the Kansas Department of Health and Environment.
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,{"id":8641,"text":"ofr8070 - 1980 - Hydrogeologic data for Eureka Springs landfill and adjacent area, north-central Hillsborough County, Florida, 1969-73","interactions":[],"lastModifiedDate":"2022-06-06T18:25:45.900054","indexId":"ofr8070","displayToPublicDate":"1980-01-01T00:00:00","publicationYear":"1980","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":330,"text":"Open-File Report","code":"OFR","onlineIssn":"2331-1258","printIssn":"0196-1497","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"80-70","title":"Hydrogeologic data for Eureka Springs landfill and adjacent area, north-central Hillsborough County, Florida, 1969-73","docAbstract":"Well location and construction data are summarized for 218 wells in the Eureka Springs landfill and adjacent areas in north-central Hillsborough County, FL. Most of the data are for 88 wells within the immediate vicinity of the landfill. Water-quality data are presented for 93 of the wells and 13 surface-water sites. Also presented are water-level data for the surficial and Floridan aquifers for 162 of the wells and lithologic logs for 43 of the wells. (USGS)","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr8070","collaboration":"Prepared in cooperation with Hillsborough County and the City of Tampa, Florida","usgsCitation":"Duerr, A.D., and Stewart, J.W., 1980, Hydrogeologic data for Eureka Springs landfill and adjacent area, north-central Hillsborough County, Florida, 1969-73: U.S. Geological Survey Open-File Report 80-70, iii, 83 p., https://doi.org/10.3133/ofr8070.","productDescription":"iii, 83 p.","costCenters":[],"links":[{"id":401770,"rank":3,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1980/0070/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":400308,"rank":2,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_75185.htm","linkFileType":{"id":5,"text":"html"}},{"id":144107,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1980/0070/report-thumb.jpg"}],"country":"United States","state":"Florida","county":"Hillsborough County","otherGeospatial":"Eureka Springs landfill","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"type\": \"Polygon\",\n \"coordinates\": [\n [\n [\n -82.4,\n 27.9333\n ],\n [\n -82.25,\n 27.9333\n ],\n [\n -82.25,\n 28.0833\n ],\n [\n -82.4,\n 28.0833\n ],\n [\n -82.4,\n 27.9333\n ]\n ]\n ]\n }\n }\n ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a50e4b07f02db628a9d","contributors":{"authors":[{"text":"Duerr, A. D.","contributorId":29821,"corporation":false,"usgs":true,"family":"Duerr","given":"A.","email":"","middleInitial":"D.","affiliations":[],"preferred":false,"id":158073,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Stewart, Joseph William","contributorId":48185,"corporation":false,"usgs":true,"family":"Stewart","given":"Joseph","email":"","middleInitial":"William","affiliations":[],"preferred":false,"id":158074,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
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