{"pageNumber":"6266","pageRowStart":"156625","pageSize":"25","recordCount":184938,"records":[{"id":70010125,"text":"70010125 - 1973 - U-Th-Pb measurements of Luna 20 soil","interactions":[],"lastModifiedDate":"2021-01-06T14:22:44.31134","indexId":"70010125","displayToPublicDate":"1973-01-01T00:00:00","publicationYear":"1973","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1759,"text":"Geochimica et Cosmochimica Acta","active":true,"publicationSubtype":{"id":10}},"title":"U-Th-Pb measurements of Luna 20 soil","docAbstract":"<div id=\"abstracts\" class=\"Abstracts u-font-serif\"><div id=\"aep-abstract-id4\" class=\"abstract author\"><div id=\"aep-abstract-sec-id5\"><p>The concentrations of uranium, thorium and lead and the lead isotopic composition of Luna 20 soil were determined. The data indicate that the Luna 20 soil is mainly a mixture of highland anorthosites and low-K basalt, but little KREEP basalt. The U-Th-Pb systematics are discussed in comparison with other lunar soils, especially with Apollo 16 soils which were collected from a ‘typical’ highland region. The data fit well in the Apollo 16 soil array on a U-Pb evolution diagram, and they exhibit excess lead relative to uranium. This relationship appears to be a characteristic of highland localities. Considering the previous observations of lunar samples, we infer that lead enrichment in the soil relative to uranium occurred between 3.2 and 3.9 b.y. ago and that the soil was disturbed by ‘third events’ about 2.0 b.y. ago. A lunar evolution model is discussed.</p></div></div></div>","language":"English","publisher":"Elsevier","doi":"10.1016/0016-7037(73)90202-0","issn":"00167037","usgsCitation":"Tatsumoto, M., 1973, U-Th-Pb measurements of Luna 20 soil: Geochimica et Cosmochimica Acta, v. 37, no. 4, p. 1079-1086, https://doi.org/10.1016/0016-7037(73)90202-0.","productDescription":"8 p.","startPage":"1079","endPage":"1086","numberOfPages":"8","costCenters":[],"links":[{"id":218929,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"37","issue":"4","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"505bb9dde4b08c986b327e75","contributors":{"authors":[{"text":"Tatsumoto, M.","contributorId":76798,"corporation":false,"usgs":true,"family":"Tatsumoto","given":"M.","email":"","affiliations":[],"preferred":false,"id":358023,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":70010973,"text":"70010973 - 1973 - Simultaneous flow of water and solutes through geological membranes-I. Experimental investigation","interactions":[],"lastModifiedDate":"2020-12-29T14:05:30.568856","indexId":"70010973","displayToPublicDate":"1973-01-01T00:00:00","publicationYear":"1973","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1759,"text":"Geochimica et Cosmochimica Acta","active":true,"publicationSubtype":{"id":10}},"title":"Simultaneous flow of water and solutes through geological membranes-I. Experimental investigation","docAbstract":"<div id=\"abstracts\" class=\"Abstracts u-font-serif\"><div id=\"aep-abstract-id4\" class=\"abstract author\"><div id=\"aep-abstract-sec-id5\"><p>The relative retardation by geological membranes of cations and anions generally present in subsurface waters was investigated using a high pressure and high temperature ‘filtration cell’. The solutions were forced through different clays and a disaggregated shale subjected to compaction pressures up to 9500 psi and to temperatures from 20 to 70°C.</p><p>The overall efficiences measured increased with increase of exchange capacity of the material used and with decrease in concentration of the input solution. The efficiency of a given membrane increased with increasing compaction pressure but decreased slightly at higher temperatures for solutions of the same ionic concentration.</p><p>The results further show that geological membranes are specific for different dissolved species. The retardation sequences varied depending on the material used and on experimental conditions. The sequences for monovalent and divalent cations at laboratory temperatures were generally as follows: Li &lt; Na &lt; NH<sub>3</sub><span>&nbsp;</span>&lt; K &lt; Rb &lt; Cs Mg &lt; Ca &lt; Sr &lt; Ba.</p><p>The sequences for anions at room temperature were variable, but at 70°C, the sequence was: HCO<sub>3</sub><span>&nbsp;</span>&lt; I &lt; B &lt; SO<sub>4</sub><span>&nbsp;</span>&lt; Cl &lt; Br.</p><p>Monovalent cations contrary to some field data were generally retarded with respect to divalent cations. The differences in the filtration ratios among the divalent cations were smaller than those between the monovalent cations. The passage rate of B, HCO<sub>3</sub>, I and NH<sub>3</sub><span>&nbsp;</span>was greatly increased at 70°C.</p></div></div></div><ul id=\"issue-navigation\" class=\"issue-navigation u-margin-s-bottom u-bg-grey1\"></ul>","language":"English","publisher":"Elsevier","doi":"10.1016/0016-7037(73)90267-6","issn":"00167037","usgsCitation":"Kharaka, Y., and Berry, F., 1973, Simultaneous flow of water and solutes through geological membranes-I. Experimental investigation: Geochimica et Cosmochimica Acta, v. 37, no. 12, p. 2577-2603, https://doi.org/10.1016/0016-7037(73)90267-6.","productDescription":"27 p.","startPage":"2577","endPage":"2603","numberOfPages":"27","costCenters":[],"links":[{"id":221209,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"37","issue":"12","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"505b90d3e4b08c986b31968e","contributors":{"authors":[{"text":"Kharaka, Y.K.","contributorId":23568,"corporation":false,"usgs":true,"family":"Kharaka","given":"Y.K.","email":"","affiliations":[],"preferred":false,"id":360003,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Berry, F.A.P.","contributorId":57594,"corporation":false,"usgs":true,"family":"Berry","given":"F.A.P.","email":"","affiliations":[],"preferred":false,"id":360004,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":70010022,"text":"70010022 - 1973 - Absolute stress measurements at the rangely anticline, Northwestern Colorado. Discussion of R. V. De La Cruz and C. B. Raleigh's","interactions":[],"lastModifiedDate":"2013-01-18T13:36:33","indexId":"70010022","displayToPublicDate":"1973-01-01T00:00:00","publicationYear":"1973","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":2071,"text":"International Journal of Rock Mechanics and Mining Sciences & Geomechanics Abstracts","active":true,"publicationSubtype":{"id":10}},"title":"Absolute stress measurements at the rangely anticline, Northwestern Colorado. Discussion of R. V. De La Cruz and C. B. Raleigh's","docAbstract":"[No abstract available]","largerWorkType":{"id":2,"text":"Article"},"largerWorkTitle":"International Journal of Rock Mechanics and Mining Sciences & Geomechanics Abstracts","largerWorkSubtype":{"id":10,"text":"Journal Article"},"language":"English","publisher":"Elsevier","doi":"10.1016/0148-9062(73)90018-1","issn":"01489062","usgsCitation":"Nichols, T.C., and Farrow, R., 1973, Absolute stress measurements at the rangely anticline, Northwestern Colorado. Discussion of R. V. De La Cruz and C. B. Raleigh's: International Journal of Rock Mechanics and Mining Sciences & Geomechanics Abstracts, v. 10, no. 6, p. 751-755, https://doi.org/10.1016/0148-9062(73)90018-1.","productDescription":"p.751-755","startPage":"751","endPage":"755","numberOfPages":"5","costCenters":[],"links":[{"id":265956,"type":{"id":10,"text":"Digital Object Identifier"},"url":"https://dx.doi.org/10.1016/0148-9062(73)90018-1"},{"id":219345,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"10","issue":"6","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"5059e64ce4b0c8380cd4731a","contributors":{"authors":[{"text":"Nichols, T. C. Jr.","contributorId":95482,"corporation":false,"usgs":true,"family":"Nichols","given":"T.","suffix":"Jr.","email":"","middleInitial":"C.","affiliations":[],"preferred":false,"id":357709,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Farrow, R.A.","contributorId":60636,"corporation":false,"usgs":true,"family":"Farrow","given":"R.A.","affiliations":[],"preferred":false,"id":357708,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":70010146,"text":"70010146 - 1973 - Solubility and occurrence of lead in surface water","interactions":[],"lastModifiedDate":"2025-01-07T16:11:33.867111","indexId":"70010146","displayToPublicDate":"1973-01-01T00:00:00","publicationYear":"1973","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":2136,"text":"Journal - American Water Works Association","active":true,"publicationSubtype":{"id":10}},"title":"Solubility and occurrence of lead in surface water","docAbstract":"<p><span>The data in this article suggest methods of reducing the lead content of drinking water at the water-treatment plant.</span></p>","language":"English","publisher":"American Water Works Association","doi":"10.1002/j.1551-8833.1973.tb01896.x","issn":"0003150X","usgsCitation":"Hem, J., and Durum, W.H., 1973, Solubility and occurrence of lead in surface water: Journal - American Water Works Association, v. 65, no. 8, p. 562-568, https://doi.org/10.1002/j.1551-8833.1973.tb01896.x.","productDescription":"7 p.","startPage":"562","endPage":"568","numberOfPages":"7","costCenters":[],"links":[{"id":219352,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"65","issue":"8","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"505b9241e4b08c986b319db7","contributors":{"authors":[{"text":"Hem, J.D.","contributorId":54576,"corporation":false,"usgs":true,"family":"Hem","given":"J.D.","affiliations":[],"preferred":false,"id":358117,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Durum, W. H.","contributorId":78311,"corporation":false,"usgs":true,"family":"Durum","given":"W.","email":"","middleInitial":"H.","affiliations":[],"preferred":false,"id":358118,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":70010230,"text":"70010230 - 1973 - More on noble gases in Yellowstone National Park hot waters","interactions":[],"lastModifiedDate":"2020-12-29T14:42:26.27664","indexId":"70010230","displayToPublicDate":"1973-01-01T00:00:00","publicationYear":"1973","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1759,"text":"Geochimica et Cosmochimica Acta","active":true,"publicationSubtype":{"id":10}},"title":"More on noble gases in Yellowstone National Park hot waters","docAbstract":"<div id=\"abstracts\" class=\"Abstracts u-font-serif\"><div id=\"aep-abstract-id5\" class=\"abstract author\"><div id=\"aep-abstract-sec-id6\"><p>Water and gas samples from research wells in hydrothermal areas of Yellowstone National Park, U.S.A., have been mass spectrometrically analyzed for their rare gas contents and isotopic composition. In agreement with previous findings, the rare gases have been found to originate from infiltrating run-off water, saturated with air at 10 to 20°C. The atmospheric rare gas retention values found for the water varied between 3 and 87 per cent. The fine structure of the Ar, Kr and Xe abundance pattern in the water reveals fraotionational enrichment of the heavier gases due to partial outgassing of the waters. Radiogenic He and Ar have been detected. No positive evidence for magmatic water contribution has been found. Nevertheless, additions of magmatic waters free of rare gas can not be excluded, but if present the proportion is significantly less than 13 to 36 per cent.</p></div></div></div>","language":"English","publisher":"Elsevier","doi":"10.1016/0016-7037(73)90215-9","issn":"00167037","usgsCitation":"Mazor, E., and Fournier, R., 1973, More on noble gases in Yellowstone National Park hot waters: Geochimica et Cosmochimica Acta, v. 37, no. 3, p. 515-525, https://doi.org/10.1016/0016-7037(73)90215-9.","productDescription":"11 p.","startPage":"515","endPage":"525","numberOfPages":"11","costCenters":[],"links":[{"id":219359,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United States","state":"Wyoming","otherGeospatial":"Yellowstone National Park","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -111.15966796875,\n              43.068887774169625\n            ],\n            [\n              -108.56689453125,\n              43.068887774169625\n            ],\n            [\n              -108.56689453125,\n              45.042478050891546\n            ],\n            [\n              -111.15966796875,\n              45.042478050891546\n            ],\n            [\n              -111.15966796875,\n              43.068887774169625\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","volume":"37","issue":"3","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"505a5e28e4b0c8380cd7082d","contributors":{"authors":[{"text":"Mazor, E.","contributorId":18104,"corporation":false,"usgs":true,"family":"Mazor","given":"E.","email":"","affiliations":[],"preferred":false,"id":358372,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Fournier, R.O.","contributorId":73584,"corporation":false,"usgs":true,"family":"Fournier","given":"R.O.","email":"","affiliations":[],"preferred":false,"id":358373,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":70010123,"text":"70010123 - 1973 - Tertiary plate tectonics and high-pressure metamorphism in New Caledonia","interactions":[],"lastModifiedDate":"2020-12-30T20:31:49.041071","indexId":"70010123","displayToPublicDate":"1973-01-01T00:00:00","publicationYear":"1973","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":3525,"text":"Tectonophysics","active":true,"publicationSubtype":{"id":10}},"title":"Tertiary plate tectonics and high-pressure metamorphism in New Caledonia","docAbstract":"<p>The sialic basement of New Caledonia is a Permian-Jurassic greywacke sequence which was folded and metamorphosed to prehnite-pumpellyite or low-grade greenschist facies by the Late Jurassic. Succeeding Cretaceous-Eocene sediments unconformably overlie this basement and extend outwards onto oceanic crust. Tertiary tectonism occurred in three distinct phases.</p><dl class=\"list\"><dt class=\"list-label\">1. During the Late Eocene a nappe of peridotite was obducted onto southern New Caledonia from northeast to southwest, but without causing significant metamorphism in the underlying sialic rocks.</dt><dt class=\"list-label\">2. Oligocene compressive thrust tectonics in the northern part of the island accompanied a major east-west subduction zone, at least 30 km wide, which is identified by an imbricate system of tectonically intruded melanges and by development of lawsonite-bearing assemblages in adjacent country rocks; this high-pressure mineralogy constituted a primary metamorphism for the Cretaceous-Eocene sedimentary pile, but was overprinted on the Mesozoic prehnite-pumpellyite metagreywackes.</dt><dt class=\"list-label\">3. Post-Oligocene transcurrent faulting along a northwest-southeast line (the&nbsp;<i>sillon</i>) parallel to the west coast caused at least 150 km of dextral offset of the southwest frontal margin of the Eocene ultramafic nappe.</dt></dl><p>At the present time, the tectonics of the southwest Pacific are related to a series of opposite facing subduction (Benioff) zones connected by transform faults extending from New Britain-Solomon Islands south through the New Hebrides to New Zealand and marking the boundary between the Australian and Pacific plates. Available geologic data from this region suggest that a similar geometry existed during the Tertiary and that the microcontinents of New Guinea, New Caledonia and New Zealand all lay along the former plate boundary which has since migrated north and east by a complex process of sea-floor spreading behind the active island arcs.</p>","language":"English","publisher":"Elsevier","doi":"10.1016/0040-1951(73)90046-2","issn":"00401951","usgsCitation":"Brothers, R., and Blake, M., 1973, Tertiary plate tectonics and high-pressure metamorphism in New Caledonia: Tectonophysics, v. 17, no. 4, p. 337-358, https://doi.org/10.1016/0040-1951(73)90046-2.","productDescription":"22 p.","startPage":"337","endPage":"358","costCenters":[{"id":312,"text":"Geology, Minerals, Energy, and Geophysics Science Center","active":true,"usgs":true}],"links":[{"id":218927,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"17","issue":"4","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"505ba57fe4b08c986b320ab3","contributors":{"authors":[{"text":"Brothers, R.N.","contributorId":90866,"corporation":false,"usgs":true,"family":"Brothers","given":"R.N.","email":"","affiliations":[],"preferred":false,"id":358020,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Blake, M.C. Jr.","contributorId":27094,"corporation":false,"usgs":true,"family":"Blake","given":"M.C.","suffix":"Jr.","affiliations":[],"preferred":false,"id":358019,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":70010160,"text":"70010160 - 1973 - Polyphenyl fluorides","interactions":[],"lastModifiedDate":"2013-03-14T12:51:04","indexId":"70010160","displayToPublicDate":"1973-01-01T00:00:00","publicationYear":"1973","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":2292,"text":"Journal of Fluorine Chemistry","active":true,"publicationSubtype":{"id":10}},"title":"Polyphenyl fluorides","docAbstract":"Studies related to the chemistry of aromatic fluorine compounds have been carried out at the Illinois State Geological Survey since 1933. In our reference collection we have several compounds that have not previously been described. This communication records data on 18 biphenyl, three terphenyl and some benzene fluorinated derivatives that were obtained as by-products and/or by specific synthesis. ?? 1973.","largerWorkType":{"id":2,"text":"Article"},"largerWorkTitle":"Journal of Fluorine Chemistry","largerWorkSubtype":{"id":10,"text":"Journal Article"},"language":"English","publisher":"Elsevier","doi":"10.1016/S0022-1139(00)82864-X","issn":"00221139","usgsCitation":"Dickerson, D.R., Finger, G.C., and Shiley, R., 1973, Polyphenyl fluorides: Journal of Fluorine Chemistry, v. 3, no. 1, p. 113-116, https://doi.org/10.1016/S0022-1139(00)82864-X.","startPage":"113","endPage":"116","numberOfPages":"4","costCenters":[],"links":[{"id":269323,"type":{"id":10,"text":"Digital Object Identifier"},"url":"https://dx.doi.org/10.1016/S0022-1139(00)82864-X"},{"id":219511,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"3","issue":"1","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"505a7d09e4b0c8380cd79cff","contributors":{"authors":[{"text":"Dickerson, D. R.","contributorId":66837,"corporation":false,"usgs":true,"family":"Dickerson","given":"D.","email":"","middleInitial":"R.","affiliations":[],"preferred":false,"id":358159,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Finger, G. C.","contributorId":89277,"corporation":false,"usgs":true,"family":"Finger","given":"G.","email":"","middleInitial":"C.","affiliations":[],"preferred":false,"id":358160,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Shiley, R.H.","contributorId":44282,"corporation":false,"usgs":true,"family":"Shiley","given":"R.H.","email":"","affiliations":[],"preferred":false,"id":358158,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":70010229,"text":"70010229 - 1973 - The sorption of silver by poorly crystallized manganese oxides","interactions":[],"lastModifiedDate":"2020-12-29T14:29:23.591245","indexId":"70010229","displayToPublicDate":"1973-01-01T00:00:00","publicationYear":"1973","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1759,"text":"Geochimica et Cosmochimica Acta","active":true,"publicationSubtype":{"id":10}},"title":"The sorption of silver by poorly crystallized manganese oxides","docAbstract":"<p>The sorption of silver by poorly crystallized manganese oxides was studied using synthesized samples of three members of the manganous manganite (birnessite) group, of different chemical composition and crystallinity, and a poorly organized γ-MnO<sub>2</sub>. All four oxides sorbed significant quantities of silver. The manganous manganites showed the greatest sorption (up to 0.5 moles silver/mole MnO<sub><i>x</i></sub><span>&nbsp;</span>at pH 7) while the γ-MnO<sub>2</sub><span>&nbsp;</span>showed the least (0.3 moles silver/ mole MnO<sub><i>x</i></sub><span>&nbsp;</span>at pH 7). Sorption of silver was adequately described by the Langmuir equation over a considerable concentration range. The relationship failed at low pH values and high equilibrium silver concentrations. The sorption capacity showed a direct relationship with pH. However, the rate of increase of sorption capacity decreased at the higher pH values.</p><p>Silver sorption maxima. were not directly related to surface area but appeared to vary with the amount of occluded sodium and potassium present in the manganese oxide. The important processes involved in the uptake of silver by the four poorly crystallized manganese oxides ara considered to be surface exchange for manganese, potassium and sodium as well as exchange for structural manganese, potassium and sodium.</p>","language":"English","publisher":"Elsevier","doi":"10.1016/0016-7037(73)90222-6","issn":"00167037","usgsCitation":"Anderson, B., Jenne, E., and Chao, T.T., 1973, The sorption of silver by poorly crystallized manganese oxides: Geochimica et Cosmochimica Acta, v. 37, no. 3, p. 611-622, https://doi.org/10.1016/0016-7037(73)90222-6.","productDescription":"12 p.","startPage":"611","endPage":"622","numberOfPages":"12","costCenters":[],"links":[{"id":219358,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"37","issue":"3","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"505bb046e4b08c986b324d58","contributors":{"authors":[{"text":"Anderson, B.J.","contributorId":70914,"corporation":false,"usgs":true,"family":"Anderson","given":"B.J.","email":"","affiliations":[],"preferred":false,"id":358371,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Jenne, E. A.","contributorId":45716,"corporation":false,"usgs":true,"family":"Jenne","given":"E. A.","affiliations":[],"preferred":false,"id":358370,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Chao, T. T.","contributorId":31900,"corporation":false,"usgs":true,"family":"Chao","given":"T.","email":"","middleInitial":"T.","affiliations":[],"preferred":false,"id":358369,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":70010228,"text":"70010228 - 1973 - Inorganic chemical investigation by x-ray fluorescence analysis: The Viking Mars Lander","interactions":[],"lastModifiedDate":"2025-02-28T16:52:00.529379","indexId":"70010228","displayToPublicDate":"1973-01-01T00:00:00","publicationYear":"1973","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1963,"text":"Icarus","active":true,"publicationSubtype":{"id":10}},"title":"Inorganic chemical investigation by x-ray fluorescence analysis: The Viking Mars Lander","docAbstract":"<div class=\"u-margin-s-bottom\">The inorganic chemical investigation added in August 1972 to the Viking Lander scientific package will utilize an energy-dispersive X-ray fluorescence spectrometer in which four sealed, gas-filled proportional counters will detect X-rays emitted from samples of the Martian surface materials irradiated by X-rays from radioisotope sources (<sup>55</sup>Fe and<span>&nbsp;</span><sup>109</sup>Cd). The output of the proportional counters will be subjected to pulse-height analysis by an on-board step-scanning single-channel analyzer with adjustable counting periods. The data will be returned to Earth, via the Viking Orbiter relay system, and the spectra constructed, calibrated, and interpreted here. The instrument is inside the Lander body, and samples are to be delivered to it by the Viking Lander Surface Sampler. Calibration standards are an integral part of the instrument.</div><div class=\"u-margin-s-bottom\">The results of the investigation will characterize the surface materials of Mars as to elemental composition with accuracies ranging from a few tens of parts per million (at the trace-element level) to a few percent (for major elements) depending on the element in question. Elements of atomic number 11 or less are determined only as a group, though useful estimates of their individual abundances maybe achieved by indirect means. The expected radiation environment will not seriously hamper the measurements. Based on the results, inferences can be drawn regarding (1) the surface mineralogy and lithology; (2) the nature of weathering processes, past and present, and the question of equilibrium between the atmosphere and the surface; and (3) the extent and type of differentiation that the planet has undergone.</div><div class=\"u-margin-s-bottom\">The Inorganic Chemical Investigation supports and is supported by most other Viking Science investigations.</div>","language":"English","publisher":"Elsevier","doi":"10.1016/0019-1035(73)90048-1","issn":"00191035","usgsCitation":"Toulmin, P., Baird, A.K., Clark, B.C., Keil, K., and Rose, H.J., 1973, Inorganic chemical investigation by x-ray fluorescence analysis: The Viking Mars Lander: Icarus, v. 20, no. 2, p. 153-178, https://doi.org/10.1016/0019-1035(73)90048-1.","productDescription":"26 p.","startPage":"153","endPage":"178","numberOfPages":"26","costCenters":[],"links":[{"id":219294,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"20","issue":"2","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"505a3c08e4b0c8380cd629f4","contributors":{"authors":[{"text":"Toulmin, P. III","contributorId":81244,"corporation":false,"usgs":true,"family":"Toulmin","given":"P.","suffix":"III","email":"","affiliations":[],"preferred":false,"id":358368,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Baird, A. K.","contributorId":65148,"corporation":false,"usgs":true,"family":"Baird","given":"A.","email":"","middleInitial":"K.","affiliations":[],"preferred":false,"id":358366,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Clark, B. C.","contributorId":39918,"corporation":false,"usgs":true,"family":"Clark","given":"B.","middleInitial":"C.","affiliations":[],"preferred":false,"id":358364,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Keil, Klaus","contributorId":55955,"corporation":false,"usgs":true,"family":"Keil","given":"Klaus","email":"","affiliations":[],"preferred":false,"id":358365,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"Rose, H. J. Jr.","contributorId":79465,"corporation":false,"usgs":true,"family":"Rose","given":"H.","suffix":"Jr.","email":"","middleInitial":"J.","affiliations":[],"preferred":false,"id":358367,"contributorType":{"id":1,"text":"Authors"},"rank":5}]}}
,{"id":70010111,"text":"70010111 - 1973 - Can American oil refineries yield vanadium?","interactions":[],"lastModifiedDate":"2012-03-12T17:18:23","indexId":"70010111","displayToPublicDate":"1973-01-01T00:00:00","publicationYear":"1973","noYear":false,"publicationType":{"id":24,"text":"Conference Paper"},"publicationSubtype":{"id":19,"text":"Conference Paper"},"title":"Can American oil refineries yield vanadium?","docAbstract":"[No abstract available]","largerWorkTitle":"Preprints","language":"English","issn":"05693799","usgsCitation":"Fischer, R.P., 1973, Can American oil refineries yield vanadium?, <i>in</i> Preprints, v. 18, no. 4, p. 620-622.","startPage":"620","endPage":"622","numberOfPages":"3","costCenters":[],"links":[{"id":218704,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"18","issue":"4","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"5059f331e4b0c8380cd4b654","contributors":{"authors":[{"text":"Fischer, R. P.","contributorId":89958,"corporation":false,"usgs":true,"family":"Fischer","given":"R.","email":"","middleInitial":"P.","affiliations":[],"preferred":false,"id":357941,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":70010157,"text":"70010157 - 1973 - Extraction and concentration of organic solutes from water","interactions":[],"lastModifiedDate":"2023-03-17T16:43:19.525112","indexId":"70010157","displayToPublicDate":"1973-01-01T00:00:00","publicationYear":"1973","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":761,"text":"Analytical Chemistry","active":true,"publicationSubtype":{"id":10}},"title":"Extraction and concentration of organic solutes from water","docAbstract":"<p>A continuous extraction apparatus is described. It extracts and simultaneously concentrates organic solutes from water. Any immiscible solvent can be used in this apparatus if the solute will partition between the solvent and water. A concentration factor of up to 10<sup>5</sup> is obtained with this technique. The dipole moment difference between the solute and solvent is demonstrated to be an index of the extraction efficiency. Optimum extraction of a given molecular species may be obtained by use of this index.</p>","language":"English","publisher":"ACS Publications","doi":"10.1021/ac60323a020","usgsCitation":"Goldberg, M.C., DeLong, L.L., and Sinclair, M., 1973, Extraction and concentration of organic solutes from water: Analytical Chemistry, v. 45, no. 1, p. 89-93, https://doi.org/10.1021/ac60323a020.","productDescription":"5 p.","startPage":"89","endPage":"93","numberOfPages":"5","costCenters":[],"links":[{"id":219434,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"45","issue":"1","noUsgsAuthors":false,"publicationDate":"2002-05-01","publicationStatus":"PW","scienceBaseUri":"505a0e5ce4b0c8380cd533f2","contributors":{"authors":[{"text":"Goldberg, Marvin C.","contributorId":26066,"corporation":false,"usgs":true,"family":"Goldberg","given":"Marvin","email":"","middleInitial":"C.","affiliations":[],"preferred":false,"id":358152,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"DeLong, Lewis L.","contributorId":91146,"corporation":false,"usgs":true,"family":"DeLong","given":"Lewis","email":"","middleInitial":"L.","affiliations":[],"preferred":false,"id":358150,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Sinclair, Mark","contributorId":91027,"corporation":false,"usgs":true,"family":"Sinclair","given":"Mark","email":"","affiliations":[],"preferred":false,"id":358151,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":70010113,"text":"70010113 - 1973 - Isotopic composition of oil-field brines from Kettleman North Dome, California, and their geologic implications","interactions":[],"lastModifiedDate":"2020-12-30T15:25:29.654987","indexId":"70010113","displayToPublicDate":"1973-01-01T00:00:00","publicationYear":"1973","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1759,"text":"Geochimica et Cosmochimica Acta","active":true,"publicationSubtype":{"id":10}},"title":"Isotopic composition of oil-field brines from Kettleman North Dome, California, and their geologic implications","docAbstract":"<p>Deuterium and O<sup>18</sup><span>&nbsp;</span>analyses were made on 25 formation-water samples from Miocene (Temblor Formation) and Eocene (McAdams Formation) reservoir rocks at Kettleman North Dome oil field, California, and on three surface water samples from Reef Ridge located about three miles to the west of the field. The<span>&nbsp;</span><i>δO</i><sup>18</sup><span>&nbsp;</span>values obtained generally increase with depth and most probably are due to temperature controlled exchange reactions with carbonate cement and dissolved carbonate species. The δD values obtained seem to be controlled primarily by the membrane behavior of shales modifying the assumed original values. The contribution of isotopic exchange between water and clays cannot be evaluated at present.</p><p>The isotopic data support the conclusions based on a detailed study of geology, hydrodynamics, and formation water geochemistry (<span class=\"small-caps\">Kharaka</span>, 1971) which indicate that:</p><p>1. The Temblor Formation waters are probably meteoric in origin concentrated chemically and isotopically by shale membranes, and 2. The McAdams Formation waters were most probably obtained by squeezing the original interstitial marine connate waters of deposition from the underlying Mesozoic sediments.</p>","language":"English","publisher":"Elsevier","doi":"10.1016/0016-7037(73)90148-8","issn":"00167037","usgsCitation":"Kharaka, Y., Berry, F., and Friedman, I., 1973, Isotopic composition of oil-field brines from Kettleman North Dome, California, and their geologic implications: Geochimica et Cosmochimica Acta, v. 37, no. 8, p. 1899-1908, https://doi.org/10.1016/0016-7037(73)90148-8.","productDescription":"10 p.","startPage":"1899","endPage":"1908","numberOfPages":"10","costCenters":[],"links":[{"id":381758,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United States","state":"California","otherGeospatial":"Kettleman North Dome","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -119.58892822265626,\n              35.980228800645676\n            ],\n            [\n              -119.41177368164061,\n              35.980228800645676\n            ],\n            [\n              -119.41177368164061,\n              36.094609063015085\n            ],\n            [\n              -119.58892822265626,\n              36.094609063015085\n            ],\n            [\n              -119.58892822265626,\n              35.980228800645676\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","volume":"37","issue":"8","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"505a3fa3e4b0c8380cd646aa","contributors":{"authors":[{"text":"Kharaka, Y.K.","contributorId":23568,"corporation":false,"usgs":true,"family":"Kharaka","given":"Y.K.","email":"","affiliations":[],"preferred":false,"id":357954,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Berry, F.A.F.","contributorId":15755,"corporation":false,"usgs":true,"family":"Berry","given":"F.A.F.","email":"","affiliations":[],"preferred":false,"id":357953,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Friedman, I.","contributorId":95596,"corporation":false,"usgs":true,"family":"Friedman","given":"I.","email":"","affiliations":[],"preferred":false,"id":357955,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":37402,"text":"ssrw167 - 1973 - Sex determination of eagles, owls, and herons by analyzing plasma steroid hormones","interactions":[],"lastModifiedDate":"2020-03-20T06:57:58","indexId":"ssrw167","displayToPublicDate":"1973-01-01T00:00:00","publicationYear":"1973","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":1,"text":"Federal Government Series"},"seriesTitle":{"id":83,"text":"Special Scientific Report  - Wildlife","active":false,"publicationSubtype":{"id":1}},"seriesNumber":"167","title":"Sex determination of eagles, owls, and herons by analyzing plasma steroid hormones","docAbstract":"<p>No abstract available.</p>","language":"English","publisher":"U.S. Fish and Wildlife Service","usgsCitation":"Dieter, M.P., 1973, Sex determination of eagles, owls, and herons by analyzing plasma steroid hormones: Special Scientific Report  - Wildlife 167, iv, 13 p.","productDescription":"iv, 13 p.","costCenters":[{"id":531,"text":"Patuxent Wildlife Research Center","active":true,"usgs":true}],"links":[{"id":166215,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e49fbe4b07f02db5f4aa1","contributors":{"authors":[{"text":"Dieter, Michael P.","contributorId":80547,"corporation":false,"usgs":true,"family":"Dieter","given":"Michael","email":"","middleInitial":"P.","affiliations":[],"preferred":false,"id":218010,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":70010280,"text":"70010280 - 1973 - An empirical NaKCa geothermometer for natural waters","interactions":[],"lastModifiedDate":"2020-12-29T15:04:56.671286","indexId":"70010280","displayToPublicDate":"1973-01-01T00:00:00","publicationYear":"1973","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1759,"text":"Geochimica et Cosmochimica Acta","active":true,"publicationSubtype":{"id":10}},"title":"An empirical NaKCa geothermometer for natural waters","docAbstract":"<p>An empirical method of estimating the last temperature of water-rock interaction has been devised. It is based upon molar Na, K and Ca concentrations in natural waters from temperature environments ranging from 4 to 340°C. The data for most geothermal waters cluster near a straight line when plotted as the function<span>&nbsp;</span><span class=\"math\"><span id=\"MathJax-Element-1-Frame\" class=\"MathJax_SVG\" data-mathml=\"<math xmlns=&quot;http://www.w3.org/1998/Math/MathML&quot;><mtext>log (</mtext><mtext>Na</mtext><mtext>K</mtext><mtext>) + &amp;#x3B2; log [ &amp;#x221A;</mtext><mtext>(Ca)</mtext><mtext>Na</mtext><mtext>]</mtext></math>\"><span class=\"MJX_Assistive_MathML\">log (NaK) + β log [ √(Ca)Na]</span></span></span><span>&nbsp;</span>vs reciprocal of absolute temperature, where β is either<span>&nbsp;</span><span class=\"math\"><span id=\"MathJax-Element-2-Frame\" class=\"MathJax_SVG\" data-mathml=\"<math xmlns=&quot;http://www.w3.org/1998/Math/MathML&quot;><mtext>1</mtext><mtext>3</mtext></math>\"><span class=\"MJX_Assistive_MathML\">13</span></span></span><span>&nbsp;</span>or<span>&nbsp;</span><span class=\"math\"><span id=\"MathJax-Element-3-Frame\" class=\"MathJax_SVG\" data-mathml=\"<math xmlns=&quot;http://www.w3.org/1998/Math/MathML&quot;><mtext>4</mtext><mtext>3</mtext></math>\"><span class=\"MJX_Assistive_MathML\">43</span></span></span><span>&nbsp;</span>depending upon whether the water equilibrated above or below 100°C. For most waters tested, the method gives better results than the<span>&nbsp;</span><span class=\"math\"><span id=\"MathJax-Element-4-Frame\" class=\"MathJax_SVG\" data-mathml=\"<math xmlns=&quot;http://www.w3.org/1998/Math/MathML&quot;><mtext>Na</mtext><mtext>K</mtext></math>\"><span class=\"MJX_Assistive_MathML\">NaK</span></span></span><span>&nbsp;</span>methods suggested by other workers. The ratio<span>&nbsp;</span><span class=\"math\"><span id=\"MathJax-Element-5-Frame\" class=\"MathJax_SVG\" data-mathml=\"<math xmlns=&quot;http://www.w3.org/1998/Math/MathML&quot;><mtext>Na</mtext><mtext>K</mtext></math>\"><span class=\"MJX_Assistive_MathML\">NaK</span></span></span><span>&nbsp;</span>should not be used to estimate temperature if<span>&nbsp;</span><span class=\"math\"><span id=\"MathJax-Element-6-Frame\" class=\"MathJax_SVG\" data-mathml=\"<math xmlns=&quot;http://www.w3.org/1998/Math/MathML&quot;><mtext>&amp;#x221A; (</mtext><mtext>M</mtext><msub><mi></mi><mn>Ca</mn></msub><mtext>)</mtext><mtext>M</mtext><msub><mi></mi><mn>Na</mn></msub></math>\"><span class=\"MJX_Assistive_MathML\">√ (MCa)MNa</span></span></span><span>&nbsp;</span>is greater than 1. The<span>&nbsp;</span><span class=\"math\"><span id=\"MathJax-Element-7-Frame\" class=\"MathJax_SVG\" data-mathml=\"<math xmlns=&quot;http://www.w3.org/1998/Math/MathML&quot;><mtext>Na</mtext><mtext>K</mtext></math>\"><span class=\"MJX_Assistive_MathML\">NaK</span></span></span><span>&nbsp;</span>values of such waters generally yield calculated temperatures much higher than the actual temperature at which water interacted with the rock.</p><p>A comparison of the composition of boiling hot-spring water with that obtained from a nearby well (170°C) in Yellowstone Park shows that continued water-rock reactions may occur during ascent of water even though that ascent is so rapid that little or no heat is lost to the country rock, i.e. the water cools adiabatically. As a result of such continued reaction, waters which dissolve additional Ca as they ascend from the aquifer to the surface will yield estimated aquifer temperatures that are too low. On the other hand, waters initially having enough Ca to deposit calcium carbonate during ascent may yield estimated aquifer temperatures that are too high if aqueous Na and K are prevented from further reaction with country rock owing to armoring by calcite or silica minerals.</p><p>The Na-K-Ca geothermometer is of particular interest to those prospecting for geothermal energy. The method also may be of use in interpreting compositions of fluid inclusions.</p>","language":"English","publisher":"Elsevier","doi":"10.1016/0016-7037(73)90060-4","issn":"00167037","usgsCitation":"Fournier, R., and Truesdell, A., 1973, An empirical NaKCa geothermometer for natural waters: Geochimica et Cosmochimica Acta, v. 37, no. 5, p. 1255-1275, https://doi.org/10.1016/0016-7037(73)90060-4.","productDescription":"21 p.","startPage":"1255","endPage":"1275","numberOfPages":"21","costCenters":[],"links":[{"id":219060,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United States","state":"Wyoming","otherGeospatial":"Yellowstone National Park","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -111.15966796875,\n              43.068887774169625\n            ],\n            [\n              -108.56689453125,\n              43.068887774169625\n            ],\n            [\n              -108.56689453125,\n              45.042478050891546\n            ],\n            [\n              -111.15966796875,\n              45.042478050891546\n            ],\n            [\n              -111.15966796875,\n              43.068887774169625\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","volume":"37","issue":"5","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"5059ea33e4b0c8380cd486d4","contributors":{"authors":[{"text":"Fournier, R.O.","contributorId":73584,"corporation":false,"usgs":true,"family":"Fournier","given":"R.O.","email":"","affiliations":[],"preferred":false,"id":358512,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Truesdell, A.H.","contributorId":52566,"corporation":false,"usgs":false,"family":"Truesdell","given":"A.H.","email":"","affiliations":[{"id":6672,"text":"former: USGS Southwest Biological Science Center, Colorado Plateau Research Station, Flagstaff, AZ. Current address:  TN-SCORE, Univ of Tennessee, Knoxville, TN, e-mail: jennen@gmail.com","active":true,"usgs":false}],"preferred":false,"id":358511,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":85560,"text":"85560 - 1973 - The use of fish bioassays to determine the rate of deactivation of pesticides","interactions":[],"lastModifiedDate":"2012-02-02T00:15:15","indexId":"85560","displayToPublicDate":"1973-01-01T00:00:00","publicationYear":"1973","noYear":false,"publicationType":{"id":5,"text":"Book chapter"},"publicationSubtype":{"id":24,"text":"Book Chapter"},"title":"The use of fish bioassays to determine the rate of deactivation of pesticides","docAbstract":"Abstract not submitted to date","largerWorkType":{"id":4,"text":"Book"},"largerWorkTitle":"Bioassay techniques and environmental chemistry","largerWorkSubtype":{"id":4,"text":"Other Government Series"},"language":"English","publisher":"Ann Arbor Science Publishers Inc.","publisherLocation":"Ann Arbor, MI","usgsCitation":"Marking, L.L., and Walker, C., 1973, The use of fish bioassays to determine the rate of deactivation of pesticides, chap. <i>of</i> Bioassay techniques and environmental chemistry, 357-366.","productDescription":"357-366","costCenters":[{"id":606,"text":"Upper Midwest Environmental Sciences Center","active":true,"usgs":true}],"links":[{"id":201423,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a5fe4b07f02db634977","contributors":{"editors":[{"text":"Glass, G.E.","contributorId":37853,"corporation":false,"usgs":true,"family":"Glass","given":"G.E.","email":"","affiliations":[],"preferred":false,"id":504524,"contributorType":{"id":2,"text":"Editors"},"rank":1}],"authors":[{"text":"Marking, L. L.","contributorId":90661,"corporation":false,"usgs":true,"family":"Marking","given":"L.","middleInitial":"L.","affiliations":[],"preferred":false,"id":296078,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Walker, C.R.","contributorId":69097,"corporation":false,"usgs":true,"family":"Walker","given":"C.R.","email":"","affiliations":[],"preferred":false,"id":296077,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":70010936,"text":"70010936 - 1973 - 87Sr/86Sr ratios in basalts from islands in the Indian Ocean","interactions":[],"lastModifiedDate":"2023-12-14T00:56:28.669484","indexId":"70010936","displayToPublicDate":"1973-01-01T00:00:00","publicationYear":"1973","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1427,"text":"Earth and Planetary Science Letters","active":true,"publicationSubtype":{"id":10}},"title":"87Sr/86Sr ratios in basalts from islands in the Indian Ocean","docAbstract":"<div id=\"abstracts\" class=\"Abstracts u-font-serif text-s\"><div id=\"ab1\" class=\"abstract author\" lang=\"en\"><div id=\"aep-abstract-sec-id8\"><p><sup>87</sup>Sr/<sup>86</sup>Sr ratios of basalts from islands in the Indian Ocean (0.7040) are higher than those of basalts dredged from the Mid-Indian Ocean Ridge (0.7034). The sources of the island basalts have apparently not been in equilibrium with the source of the ridge basalts for roughly 10<sup>9</sup><span>&nbsp;</span>years. Both ridge and island basalts in the Indian Ocean are higher in<sup>87</sup>Sr/<sup>86</sup>Sr than are rocks from similar settings in the eastern Pacific.</p></div></div></div><ul id=\"issue-navigation\" class=\"issue-navigation u-margin-s-bottom u-bg-grey1\"></ul>","language":"English","publisher":"Elsevier","doi":"10.1016/0012-821X(73)90222-7","issn":"0012821X","usgsCitation":"Hedge, C., Watkins, N., Hildreth, R., and Doering, W.P., 1973, 87Sr/86Sr ratios in basalts from islands in the Indian Ocean: Earth and Planetary Science Letters, v. 21, no. 1, p. 29-34, https://doi.org/10.1016/0012-821X(73)90222-7.","productDescription":"6 p.","startPage":"29","endPage":"34","numberOfPages":"6","costCenters":[],"links":[{"id":220738,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"21","issue":"1","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"5059e26ee4b0c8380cd45b95","contributors":{"authors":[{"text":"Hedge, C. E.","contributorId":73611,"corporation":false,"usgs":true,"family":"Hedge","given":"C. E.","affiliations":[],"preferred":false,"id":359935,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Watkins, N.D.","contributorId":77662,"corporation":false,"usgs":true,"family":"Watkins","given":"N.D.","email":"","affiliations":[],"preferred":false,"id":359936,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Hildreth, R.A.","contributorId":29111,"corporation":false,"usgs":true,"family":"Hildreth","given":"R.A.","email":"","affiliations":[],"preferred":false,"id":359934,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Doering, W. P.","contributorId":7270,"corporation":false,"usgs":true,"family":"Doering","given":"W.","email":"","middleInitial":"P.","affiliations":[],"preferred":false,"id":359933,"contributorType":{"id":1,"text":"Authors"},"rank":4}]}}
,{"id":70161842,"text":"70161842 - 1973 - Nutritional factors in the biochemical pathology of Corynebacterial kidney disease in the coho salmon (Oncorhynchus kisutch)","interactions":[],"lastModifiedDate":"2016-01-06T16:06:49","indexId":"70161842","displayToPublicDate":"1973-01-01T00:00:00","publicationYear":"1973","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":2543,"text":"Journal of the Fisheries Research Board of Canada","active":true,"publicationSubtype":{"id":10}},"title":"Nutritional factors in the biochemical pathology of Corynebacterial kidney disease in the coho salmon (Oncorhynchus kisutch)","docAbstract":"<p><span>The influence of diet ingredient on the morbidity and biochemical pathogenesis of corynebacterial kidney disease was investigated using juvenile coho salmon (</span><i>Oncorhynchus kisutch</i><span>) fed the Abernathy dry ration made up with either corn gluten or cottonseed meal (isoprotein, isocaloric substitution). Evaluation of incidence of infection, pituitary activation and aspects of carbohydrate metabolism, acid-base balance, renal function, and hematopoietic activity showed that the actual disease incidence was about the same for both diets but the nonspecific stress of infection was more severe in fish fed the corn gluten.Discriminant function calculations combining four physiological parameters gave a probability of 0.86 for successfully diagnosing infected fish on the basis of these blood chemistry tests.</span></p>","language":"English","publisher":"NRC Research Press","doi":"10.1139/f73-052","usgsCitation":"Wedemeyer, G.A., and Ross, A.J., 1973, Nutritional factors in the biochemical pathology of Corynebacterial kidney disease in the coho salmon (Oncorhynchus kisutch): Journal of the Fisheries Research Board of Canada, v. 30, no. 2, p. 296-298, https://doi.org/10.1139/f73-052.","productDescription":"3 p.","startPage":"296","endPage":"298","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[{"id":654,"text":"Western Fisheries Research Center","active":true,"usgs":true}],"links":[{"id":313984,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"30","issue":"2","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"568e491fe4b0e7a44bc41a15","contributors":{"authors":[{"text":"Wedemeyer, Gary A.","contributorId":30668,"corporation":false,"usgs":true,"family":"Wedemeyer","given":"Gary","email":"","middleInitial":"A.","affiliations":[],"preferred":false,"id":587904,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Ross, A. J.","contributorId":105267,"corporation":false,"usgs":true,"family":"Ross","given":"A.","email":"","middleInitial":"J.","affiliations":[],"preferred":false,"id":587905,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":70161843,"text":"70161843 - 1973 - Some physiological aspects of sublethal heat stress in the juvenile steelhead trout (Salmo gairdneri) and coho salmon (Oncorhynchus kisutch)","interactions":[],"lastModifiedDate":"2016-01-06T16:10:11","indexId":"70161843","displayToPublicDate":"1973-01-01T00:00:00","publicationYear":"1973","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":2543,"text":"Journal of the Fisheries Research Board of Canada","active":true,"publicationSubtype":{"id":10}},"title":"Some physiological aspects of sublethal heat stress in the juvenile steelhead trout (Salmo gairdneri) and coho salmon (Oncorhynchus kisutch)","docAbstract":"<p><span>A rapid (3&ensp;min) but sublethal temperature increase from 10 to 20 imposed a greater stress on juvenile coho salmon (</span><i>Oncorhynchus kisutch</i><span>) than on juvenile steelhead trout (</span><i>Salmo gairdneri</i><span>). Both species suffered hyperglycemia, hypocholesterolemia, increased blood hemoglobin, and decreased blood sugar regulatory precision, but the steelhead recovered more quickly. Acid&ndash;base equilibrium was essentially unaffected, and only the coho suffered any significant interrenal vitamin C depletion. Vitamin C normalization required about 24&ensp;hr.</span></p>","language":"English","publisher":"NRC Research Press","doi":"10.1139/f73-138","usgsCitation":"Wedemeyer, G., 1973, Some physiological aspects of sublethal heat stress in the juvenile steelhead trout (Salmo gairdneri) and coho salmon (Oncorhynchus kisutch): Journal of the Fisheries Research Board of Canada, v. 30, no. 6, p. 831-834, https://doi.org/10.1139/f73-138.","productDescription":"4 p.","startPage":"831","endPage":"834","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[{"id":654,"text":"Western Fisheries Research Center","active":true,"usgs":true}],"links":[{"id":313985,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"30","issue":"6","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"568e492ee4b0e7a44bc41a89","contributors":{"authors":[{"text":"Wedemeyer, Gary gwedemeyer@usgs.gov","contributorId":5504,"corporation":false,"usgs":true,"family":"Wedemeyer","given":"Gary","email":"gwedemeyer@usgs.gov","affiliations":[],"preferred":true,"id":587906,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":70009773,"text":"70009773 - 1973 - Point of zero charge of weathered forsterite","interactions":[],"lastModifiedDate":"2020-12-29T19:44:51.597727","indexId":"70009773","displayToPublicDate":"1973-01-01T00:00:00","publicationYear":"1973","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":"Point of zero charge of weathered forsterite","docAbstract":"<div id=\"abstracts\" class=\"Abstracts u-font-serif\"><div id=\"aep-abstract-id4\" class=\"abstract author\"><div id=\"aep-abstract-sec-id5\"><p id=\"simple-para.0010\">The point of zero charge of forsterite shifts from an estimated 8.9 for the unaltered mineral to 8.4 and 8.0, respectively, after being weathered artificially for 1 h and 4 h. These results corroborate the presence of magnesium-deficient surfaces on the weathered minerals, also indicated by chemical analyses of the solutions. H<sup>+</sup><span>&nbsp;</span>and OH<sup>−</sup><span>&nbsp;</span>are shown to be potential-determining ions in this system</p></div></div></div><ul id=\"issue-navigation\" class=\"issue-navigation u-margin-s-bottom u-bg-grey1\"></ul>","language":"English","publisher":"Elsevier","doi":"10.1016/0009-2541(73)90112-5","issn":"00092541","usgsCitation":"Luce, R., and Parks, G.A., 1973, Point of zero charge of weathered forsterite: Chemical Geology, v. 12, no. 2, p. 147-153, https://doi.org/10.1016/0009-2541(73)90112-5.","productDescription":"7 p.","startPage":"147","endPage":"153","numberOfPages":"7","costCenters":[],"links":[{"id":219491,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"12","issue":"2","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"505a7cb3e4b0c8380cd79b24","contributors":{"authors":[{"text":"Luce, R.W.","contributorId":39862,"corporation":false,"usgs":true,"family":"Luce","given":"R.W.","email":"","affiliations":[],"preferred":false,"id":357107,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Parks, George A.","contributorId":41433,"corporation":false,"usgs":true,"family":"Parks","given":"George","email":"","middleInitial":"A.","affiliations":[],"preferred":false,"id":357108,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":58357,"text":"mf518 - 1973 - Faults and earthquakes in the Monterey Bay region, California","interactions":[],"lastModifiedDate":"2022-12-30T17:49:45.434807","indexId":"mf518","displayToPublicDate":"1973-01-01T00:00:00","publicationYear":"1973","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":325,"text":"Miscellaneous Field Studies Map","code":"MF","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"518","title":"Faults and earthquakes in the Monterey Bay region, California","docAbstract":"<p>No abstract available.</p>","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Reston, VA","doi":"10.3133/mf518","usgsCitation":"Greene, H., Lee, W., McCulloch, D.S., and Brabb, E.E., 1973, Faults and earthquakes in the Monterey Bay region, California: U.S. Geological Survey Miscellaneous Field Studies Map 518, Report: 14 p.; 4 Plates: 24.40 × 28.62 inches, https://doi.org/10.3133/mf518.","productDescription":"Report: 14 p.; 4 Plates: 24.40 × 28.62 inches","costCenters":[],"links":[{"id":410297,"rank":7,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_3612.htm","linkFileType":{"id":5,"text":"html"}},{"id":272395,"rank":6,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/mf/0518/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":272396,"rank":5,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/mf/0518/report-thumb.jpg"},{"id":272394,"rank":4,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/mf/0518/plate-4.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":272392,"rank":2,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/mf/0518/plate-2.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":272393,"rank":3,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/mf/0518/plate-3.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":184986,"rank":1,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/mf/0518/plate-1.pdf"}],"scale":"200000","country":"United States","state":"California","otherGeospatial":"Monterey Bay region","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -122.25,36.25 ], [ -122.25,37.25 ], [ -121.25,37.25 ], [ -121.25,36.25 ], [ -122.25,36.25 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e49fee4b07f02db5f72a6","contributors":{"authors":[{"text":"Greene, H. G.","contributorId":149765,"corporation":false,"usgs":false,"family":"Greene","given":"H. G.","affiliations":[{"id":17819,"text":"MLML Center for Habitat Studies","active":true,"usgs":false}],"preferred":false,"id":258859,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Lee, W.H.K.","contributorId":35303,"corporation":false,"usgs":true,"family":"Lee","given":"W.H.K.","affiliations":[],"preferred":false,"id":258858,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"McCulloch, D. S.","contributorId":78315,"corporation":false,"usgs":true,"family":"McCulloch","given":"D.","email":"","middleInitial":"S.","affiliations":[],"preferred":false,"id":258861,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Brabb, E. E.","contributorId":43780,"corporation":false,"usgs":true,"family":"Brabb","given":"E.","middleInitial":"E.","affiliations":[],"preferred":false,"id":258860,"contributorType":{"id":1,"text":"Authors"},"rank":4}]}}
,{"id":70174173,"text":"70174173 - 1973 - Floods in Iowa: Technical manual for estimating their magnitude and frequency","interactions":[],"lastModifiedDate":"2025-07-29T18:14:39.097091","indexId":"70174173","displayToPublicDate":"1973-01-01T00:00:00","publicationYear":"1973","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":2,"text":"State or Local Government Series"},"seriesTitle":{"id":5108,"text":"Iowa Natural Resources Council Bulletin","active":true,"publicationSubtype":{"id":2}},"seriesNumber":"11","title":"Floods in Iowa: Technical manual for estimating their magnitude and frequency","docAbstract":"<p>No abstract available.</p>","language":"English","publisher":"Iowa Natural Resources Council","usgsCitation":"Lara, O.G., 1973, Floods in Iowa: Technical manual for estimating their magnitude and frequency: Iowa Natural Resources Council Bulletin 11, 56 p.","productDescription":"56 p.","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[{"id":351,"text":"Iowa Water Science Center","active":true,"usgs":true}],"links":[{"id":493122,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/unnumbered/70174173/IA-NRC_bull11.pdf","text":"Report","size":"3.9 MB","linkFileType":{"id":1,"text":"pdf"}},{"id":324498,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"57739fb0e4b07657d1a90cc8","contributors":{"authors":[{"text":"Lara, Oscar G.","contributorId":19555,"corporation":false,"usgs":true,"family":"Lara","given":"Oscar","email":"","middleInitial":"G.","affiliations":[],"preferred":false,"id":641028,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":70009774,"text":"70009774 - 1973 - The selenium content of U.S.G.S. standard rocks","interactions":[],"lastModifiedDate":"2020-12-29T19:47:52.513022","indexId":"70009774","displayToPublicDate":"1973-01-01T00:00:00","publicationYear":"1973","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 selenium content of U.S.G.S. standard rocks","docAbstract":"<div id=\"abstracts\" class=\"Abstracts u-font-serif\"><div id=\"aep-abstract-id5\" class=\"abstract author\"><div id=\"aep-abstract-sec-id6\"><p id=\"simple-para.0010\">Selenium was determined in duplicate portions from three bottles of six U.S.G.S. standard rocks by a spect rofluorimetric procedure. The following averages, as p.p.m. Se, were obtained: PCC-1, 0.031; GSP-1, 0.088; BCR-1, 0.12; SCo-1, 0.91; MAG-1, 1.3; and SGR-1, 3.7. One-way analysis of variance of the several sets of data showed no significant differences in the selenium content among bottles of any specific rock; these samples may be accepted as homogeneous for their selenium contents by this analytical method.</p></div></div></div><ul id=\"issue-navigation\" class=\"issue-navigation u-margin-s-bottom u-bg-grey1\"></ul>","language":"English","publisher":"Elsevier","doi":"10.1016/0009-2541(73)90030-2","issn":"00092541","usgsCitation":"Schnepfe, M., and Flanagan, F., 1973, The selenium content of U.S.G.S. standard rocks: Chemical Geology, v. 12, no. 1, p. 77-80, https://doi.org/10.1016/0009-2541(73)90030-2.","productDescription":"4 p.","startPage":"77","endPage":"80","numberOfPages":"4","costCenters":[],"links":[{"id":219567,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"12","issue":"1","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"505bb00be4b08c986b324bbf","contributors":{"authors":[{"text":"Schnepfe, M. M.","contributorId":93622,"corporation":false,"usgs":true,"family":"Schnepfe","given":"M. M.","affiliations":[],"preferred":false,"id":357110,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Flanagan, F.J.","contributorId":50139,"corporation":false,"usgs":true,"family":"Flanagan","given":"F.J.","email":"","affiliations":[],"preferred":false,"id":357109,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":41925,"text":"ofr73291 - 1973 - Aeromagnetic map of northern Frederick County, Maryland, and parts of adjacent counties in Maryland and Pennsylvania","interactions":[],"lastModifiedDate":"2022-12-14T20:57:37.664247","indexId":"ofr73291","displayToPublicDate":"1973-01-01T00:00:00","publicationYear":"1973","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":"73-291","title":"Aeromagnetic map of northern Frederick County, Maryland, and parts of adjacent counties in Maryland and Pennsylvania","docAbstract":"<p>No abstract available.</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr73291","usgsCitation":"Water Resources Division, U.S. Geological Survey, 1973, Aeromagnetic map of northern Frederick County, Maryland, and parts of adjacent counties in Maryland and Pennsylvania: U.S. Geological Survey Open-File Report 73-291, 1 Plate: 43.00 × 41.00 inches, https://doi.org/10.3133/ofr73291.","productDescription":"1 Plate: 43.00 × 41.00 inches","costCenters":[],"links":[{"id":136687,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":410496,"rank":3,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_68260.htm","linkFileType":{"id":5,"text":"html"}},{"id":98723,"rank":1,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1973/0291/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}}],"scale":"62500","country":"United States","state":"Maryland, Pennsylvania","county":"Frederick County","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"coordinates\": [\n          [\n            [\n              -77,\n              39.75\n            ],\n            [\n              -77.75,\n              39.75\n            ],\n            [\n              -77.75,\n              39.3756\n            ],\n            [\n              -77,\n              39.3756\n            ],\n            [\n              -77,\n              39.75\n            ]\n          ]\n        ],\n        \"type\": \"Polygon\"\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4affe4b07f02db697ce7","contributors":{"authors":[{"text":"Water Resources Division, U.S. Geological Survey","contributorId":128075,"corporation":true,"usgs":false,"organization":"Water Resources Division, U.S. Geological Survey","id":530706,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":2000036,"text":"2000036 - 1973 - Lamprey control in the United States","interactions":[],"lastModifiedDate":"2023-04-07T15:19:26.060294","indexId":"2000036","displayToPublicDate":"1973-01-01T00:00:00","publicationYear":"1973","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":3,"text":"Organization Series"},"seriesTitle":{"id":156,"text":"Annual Report","active":false,"publicationSubtype":{"id":3}},"seriesNumber":"1971","title":"Lamprey control in the United States","docAbstract":"<p>No abstract available.</p>","largerWorkType":{"id":18,"text":"Report"},"largerWorkTitle":"Annual report of the Great Lakes Fishery Commission 1971","largerWorkSubtype":{"id":3,"text":"Organization Series"},"language":"English","publisher":"Great Lakes Fishery Commission","usgsCitation":"Smith, B.R., and Braem, R.A., 1973, Lamprey control in the United States: Annual Report 1971, 13 p.","productDescription":"13 p.","startPage":"29","endPage":"41","numberOfPages":"13","costCenters":[{"id":324,"text":"Great Lakes Science Center","active":true,"usgs":true}],"links":[{"id":198948,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b32e4b07f02db6b4211","contributors":{"authors":[{"text":"Smith, Bernard R.","contributorId":38924,"corporation":false,"usgs":true,"family":"Smith","given":"Bernard","email":"","middleInitial":"R.","affiliations":[],"preferred":false,"id":324964,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Braem, Robert A.","contributorId":34858,"corporation":false,"usgs":true,"family":"Braem","given":"Robert","email":"","middleInitial":"A.","affiliations":[],"preferred":false,"id":324963,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":1001622,"text":"1001622 - 1973 - Red-winged blackbirds nesting near Great Slave Lake, N.W.T","interactions":[],"lastModifiedDate":"2023-09-21T14:44:27.787391","indexId":"1001622","displayToPublicDate":"1973-01-01T00:00:00","publicationYear":"1973","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1063,"text":"Blue Jay","active":true,"publicationSubtype":{"id":10}},"title":"Red-winged blackbirds nesting near Great Slave Lake, N.W.T","docAbstract":"<p>No abstract available.</p>","language":"English","publisher":"Nature Saskatchewan","doi":"10.29173/bluejay4157","usgsCitation":"Krapu, G., 1973, Red-winged blackbirds nesting near Great Slave Lake, N.W.T: Blue Jay, v. 31, no. 3, p. 147-149, https://doi.org/10.29173/bluejay4157.","productDescription":"3 p.","startPage":"147","endPage":"149","costCenters":[{"id":480,"text":"Northern Prairie Wildlife Research Center","active":true,"usgs":true}],"links":[{"id":480664,"rank":2,"type":{"id":40,"text":"Open Access Publisher Index Page"},"url":"https://doi.org/10.29173/bluejay4157","text":"Publisher Index Page"},{"id":130526,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"Canada","state":"Northwest Territories","otherGeospatial":"Great Slave Lake","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"coordinates\": [\n          [\n            [\n              -108.46634810500355,\n              63.13976004970118\n            ],\n            [\n              -118.08698043345574,\n              63.13976004970118\n            ],\n            [\n              -118.08698043345574,\n              60.61830047095037\n            ],\n            [\n              -108.46634810500355,\n              60.61830047095037\n            ],\n            [\n              -108.46634810500355,\n              63.13976004970118\n            ]\n          ]\n        ],\n        \"type\": \"Polygon\"\n      }\n    }\n  ]\n}","volume":"31","issue":"3","noUsgsAuthors":false,"publicationDate":"1970-01-01","publicationStatus":"PW","scienceBaseUri":"4f4e4a60e4b07f02db635327","contributors":{"authors":[{"text":"Krapu, Gary 0000-0001-8482-6130 gkrapu@usgs.gov","orcid":"https://orcid.org/0000-0001-8482-6130","contributorId":168791,"corporation":false,"usgs":true,"family":"Krapu","given":"Gary","email":"gkrapu@usgs.gov","affiliations":[{"id":480,"text":"Northern Prairie Wildlife Research Center","active":true,"usgs":true}],"preferred":true,"id":311364,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
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