{"pageNumber":"6271","pageRowStart":"156750","pageSize":"25","recordCount":184938,"records":[{"id":70175502,"text":"70175502 - 1973 - Time of travel of solutes, field observations of water quality, and suspended-sediment data for stream reaches in the Trinity River Basin, Texas, July 31 to August 14, 1972","interactions":[],"lastModifiedDate":"2016-08-15T14:53:47","indexId":"70175502","displayToPublicDate":"1973-01-01T00:00:00","publicationYear":"1973","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":6,"text":"USGS Unnumbered Series"},"seriesTitle":{"id":375,"text":"Open-File Report","active":false,"publicationSubtype":{"id":6}},"title":"Time of travel of solutes, field observations of water quality, and suspended-sediment data for stream reaches in the Trinity River Basin, Texas, July 31 to August 14, 1972","docAbstract":"<p>No abstract available.</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/70175502","usgsCitation":"Ollman, R., 1973, Time of travel of solutes, field observations of water quality, and suspended-sediment data for stream reaches in the Trinity River Basin, Texas, July 31 to August 14, 1972: Open-File Report, 2 Sheets, https://doi.org/10.3133/70175502.","productDescription":"2 Sheets","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[{"id":583,"text":"Texas Water Science Center","active":true,"usgs":true}],"links":[{"id":326499,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"57b2e7cde4b03bcb0102e993","contributors":{"authors":[{"text":"Ollman, R.H.","contributorId":88806,"corporation":false,"usgs":true,"family":"Ollman","given":"R.H.","email":"","affiliations":[],"preferred":false,"id":645511,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":70011096,"text":"70011096 - 1973 - Excess lead in \"rusty rock\" 66095 and implications for an early lunar differentiation","interactions":[],"lastModifiedDate":"2026-01-23T16:14:56.142458","indexId":"70011096","displayToPublicDate":"1973-01-01T00:00:00","publicationYear":"1973","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":3338,"text":"Science","active":true,"publicationSubtype":{"id":10}},"title":"Excess lead in \"rusty rock\" 66095 and implications for an early lunar differentiation","docAbstract":"<p><span id=\"_mce_caret\" data-mce-bogus=\"1\" data-mce-type=\"format-caret\"><span>Apollo 16 breccia 66095 contains a remarkably high amount of lead (15 parts per million), 85 percent of which is not supported by uranium and thorium in the rock. An acid leach experiment coupled with separate analyses of the whole rock and mineral fractions for uranium, thorium, and lead indicate that the excess lead has a lunar source and was apparently introduced about 4.0 × 10</span><sup>9</sup><span>&nbsp;years ago. The data also suggest that a major lunar crustal differentiation occurred about 4.47 × 10</span><sup>9</sup><span>&nbsp;years ago.</span></span></p>","language":"English","publisher":"American Association for the Advancement of Science","doi":"10.1126/science.182.4115.916","issn":"00368075","usgsCitation":"Nunes, P., and Tatsumoto, M., 1973, Excess lead in \"rusty rock\" 66095 and implications for an early lunar differentiation: Science, v. 182, no. 4115, p. 916-920, https://doi.org/10.1126/science.182.4115.916.","productDescription":"5 p.","startPage":"916","endPage":"920","costCenters":[],"links":[{"id":221422,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"182","issue":"4115","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"505a0da5e4b0c8380cd53111","contributors":{"authors":[{"text":"Nunes, P.D.","contributorId":18487,"corporation":false,"usgs":true,"family":"Nunes","given":"P.D.","email":"","affiliations":[],"preferred":false,"id":360269,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Tatsumoto, M.","contributorId":76798,"corporation":false,"usgs":true,"family":"Tatsumoto","given":"M.","email":"","affiliations":[],"preferred":false,"id":360270,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":70010095,"text":"70010095 - 1973 - Radial particle-size segregation during packing of particulates into cylindrical containers","interactions":[],"lastModifiedDate":"2020-12-30T15:10:51.612357","indexId":"70010095","displayToPublicDate":"1973-01-01T00:00:00","publicationYear":"1973","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":3107,"text":"Powder Technology","active":true,"publicationSubtype":{"id":10}},"title":"Radial particle-size segregation during packing of particulates into cylindrical containers","docAbstract":"<p>In a series of experiments, soil materials were placed in long cylindrical containers, using various packing procedures. Soil columns produced by deposition and simultaneous vibratory compaction were dense and axially uniform, but showed significant radial segregation of particle sizes. Similar results were obtained with deposition and simultaneous impact-type compaction when the impacts resulted in significant container “bouncing”. The latter procedure, modified to minimize “bouncing” produced dense, uniform soil columns, showing little radial particle-size segregation. Other procedures tested (deposition alone and deposition followed by compaction) did not result in radial segregation, but produced columns showing either relatively low or axially nonuniform densities.</p><p>Current data suggest that radial particle-size segregation is mainly due to vibration-induced particle circulation in which particles of various sizes have different circulation rates and paths.</p>","language":"English","publisher":"Elsevier","doi":"10.1016/0032-5910(73)80079-8","issn":"00325910","usgsCitation":"Ripple, C., James, R., and Rubin, J., 1973, Radial particle-size segregation during packing of particulates into cylindrical containers: Powder Technology, v. 8, no. 3-4, p. 165-175, https://doi.org/10.1016/0032-5910(73)80079-8.","productDescription":"11 p.","startPage":"165","endPage":"175","numberOfPages":"11","costCenters":[],"links":[{"id":219666,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"8","issue":"3-4","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"505a9390e4b0c8380cd80ed4","contributors":{"authors":[{"text":"Ripple, C.D.","contributorId":11586,"corporation":false,"usgs":true,"family":"Ripple","given":"C.D.","email":"","affiliations":[],"preferred":false,"id":357883,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"James, R.V.","contributorId":106634,"corporation":false,"usgs":true,"family":"James","given":"R.V.","email":"","affiliations":[],"preferred":false,"id":357885,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Rubin, J.","contributorId":26433,"corporation":false,"usgs":true,"family":"Rubin","given":"J.","email":"","affiliations":[],"preferred":false,"id":357884,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":70010057,"text":"70010057 - 1973 - Paleomagnetism of some Precambrian basaltic flows and red beds, Eastern Grand Canyon, Arizona","interactions":[],"lastModifiedDate":"2020-12-30T14:55:57.529015","indexId":"70010057","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":"Paleomagnetism of some Precambrian basaltic flows and red beds, Eastern Grand Canyon, Arizona","docAbstract":"<div id=\"abstracts\" class=\"Abstracts u-font-serif\"><div id=\"ab1\" class=\"abstract author\" lang=\"en\"><div id=\"aep-abstract-sec-id4\"><p>Lava flows and red sandstone beds near the middle of the Upper Precambrian Grand Canyon Series exhibit stable remanent magnetization. The beds are about 1000 m stratigraphically above rocks of the Grand Canyon Series for which paleomagnetic poles have been reported. All specimens were subjected to stepwise thermal (200°–700°C) or alternating field (25–5000 Oe) demagnetization for the determination of characteristic magnetization. The pole for two flows and an intercalated sandstone bed of the Cardenas Lavas of Ford, Breed and Mitchell (upper Unkar Group), is at 174.6W, 0.4N (<i>N</i><span>&nbsp;</span>= 10,<span>&nbsp;</span><i>K</i><span>&nbsp;</span>= 50, α<sub>95</sub><span>&nbsp;</span>= 6.9°). The pole for a weathered zone developed across the Cardenas Lavas is at 167.8W, 49.4N (<i>N</i><span>&nbsp;</span>= 5,<span>&nbsp;</span><i>K</i><span>&nbsp;</span>= 79, α<sub>95</sub><span>&nbsp;</span>= 8.6°). The pole for directly overlying sandstone of the Nankoweap Formation of Maxson is at 174.4E, 12.5N (<i>N</i><span>&nbsp;</span>= 6,<span>&nbsp;</span><i>K</i><span>&nbsp;</span>= 105, α<sub>95</sub><span>&nbsp;</span>= 6.6°). These poles lie on or near, and appear to follow, part of an apparent polar wandering path recently proposed for the Precambrian of North America by Spall. If the fit is not accidental, little or no rotation has occurred between north-central Arizona and parts of the North American continent used to define the proposed path.</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)90064-2","issn":"0012821X","usgsCitation":"Elston, D.P., and Robert, S.G., 1973, Paleomagnetism of some Precambrian basaltic flows and red beds, Eastern Grand Canyon, Arizona: Earth and Planetary Science Letters, v. 18, no. 2, p. 253-265, https://doi.org/10.1016/0012-821X(73)90064-2.","productDescription":"13 p.","startPage":"253","endPage":"265","numberOfPages":"13","costCenters":[],"links":[{"id":218842,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United States","state":"Arizona","otherGeospatial":"Eastern Grand Canyon","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -112.445068359375,\n              35.64836915737426\n            ],\n            [\n              -111.29699707031249,\n              35.64836915737426\n            ],\n            [\n              -111.29699707031249,\n              36.43454191900892\n            ],\n            [\n              -112.445068359375,\n              36.43454191900892\n            ],\n            [\n              -112.445068359375,\n              35.64836915737426\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","volume":"18","issue":"2","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"505a7427e4b0c8380cd77493","contributors":{"authors":[{"text":"Elston, D. P.","contributorId":96334,"corporation":false,"usgs":true,"family":"Elston","given":"D.","email":"","middleInitial":"P.","affiliations":[],"preferred":false,"id":357790,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Robert, Scott G.","contributorId":73744,"corporation":false,"usgs":true,"family":"Robert","given":"Scott","email":"","middleInitial":"G.","affiliations":[],"preferred":false,"id":357789,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":70010069,"text":"70010069 - 1973 - Imaging characteristics of photogrammetric camera systems","interactions":[],"lastModifiedDate":"2020-12-30T15:03:22.230034","indexId":"70010069","displayToPublicDate":"1973-01-01T00:00:00","publicationYear":"1973","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":3050,"text":"Photogrammetria","active":true,"publicationSubtype":{"id":10}},"title":"Imaging characteristics of photogrammetric camera systems","docAbstract":"<p>In view of the current interest in high-altitude and space photographic systems for photogrammetric mapping, the United States Geological Survey (U.S.G.S.) undertook a comprehensive research project designed to explore the practical aspects of applying the latest image quality evaluation techniques to the analysis of such systems. The project had two direct objectives: (1) to evaluate the imaging characteristics of current U.S.G.S. photogrammetric camera systems; and (2) to develop methodologies for predicting the imaging capabilities of photogrammetric camera systems, comparing conventional systems with new or different types of systems, and analyzing the image quality of photographs. Image quality was judged in terms of a number of evaluation factors including response functions, resolving power, and the detectability and measurability of small detail.</p><p>The limiting capabilities of the U.S.G.S. 6-inch and 12-inch focal length camera systems were established by analyzing laboratory and aerial photographs in terms of these evaluation factors. In the process, the contributing effects of relevant parameters such as lens aberrations, lens aperture, shutter function, image motion, film type, and target contrast procedures for analyzing image quality and predicting and comparing performance capabilities.</p>","language":"English","publisher":"Elsevier","doi":"10.1016/0031-8663(73)90006-9","issn":"00318663","usgsCitation":"Welch, R., and Halliday, J., 1973, Imaging characteristics of photogrammetric camera systems: Photogrammetria, v. 29, no. 1, p. 1-43, https://doi.org/10.1016/0031-8663(73)90006-9.","productDescription":"43 p.","startPage":"1","endPage":"43","numberOfPages":"43","costCenters":[],"links":[{"id":219282,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"29","issue":"1","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"505a3880e4b0c8380cd615ba","contributors":{"authors":[{"text":"Welch, R.","contributorId":6996,"corporation":false,"usgs":true,"family":"Welch","given":"R.","email":"","affiliations":[],"preferred":false,"id":357824,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Halliday, J.","contributorId":63160,"corporation":false,"usgs":true,"family":"Halliday","given":"J.","email":"","affiliations":[],"preferred":false,"id":357825,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":70010056,"text":"70010056 - 1973 - Galerkin finite-element simulation of a geothermal reservoir","interactions":[],"lastModifiedDate":"2020-12-30T14:45:23.526129","indexId":"70010056","displayToPublicDate":"1973-01-01T00:00:00","publicationYear":"1973","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1828,"text":"Geothermics","active":true,"publicationSubtype":{"id":10}},"title":"Galerkin finite-element simulation of a geothermal reservoir","docAbstract":"<div id=\"abstracts\" class=\"Abstracts u-font-serif\"><div id=\"aep-abstract-id3\" class=\"abstract author\"><div id=\"aep-abstract-sec-id4\"><p>The equations describing fluid flow and energy transport in a porous medium can be used to formulate a mathematical model capable of simulating the transient response of a hot-water geothermal reservoir. The resulting equations can be solved accurately and efficiently using a numerical scheme which combines the finite element approach with the Galerkin method of approximation. Application of this numerical model to the Wairakei geothermal field demonstrates that hot-water geothermal fields can be simulated using numerical techniques currently available and under development.</p></div></div></div><ul id=\"issue-navigation\" class=\"issue-navigation u-margin-s-bottom u-bg-grey1\"></ul>","language":"English","publisher":"Elsevier","doi":"10.1016/0375-6505(73)90011-4","issn":"03756505","usgsCitation":"Mercer, J., and Pinder, G., 1973, Galerkin finite-element simulation of a geothermal reservoir: Geothermics, v. 2, no. 3-4, p. 81-89, https://doi.org/10.1016/0375-6505(73)90011-4.","productDescription":"9 p.","startPage":"81","endPage":"89","numberOfPages":"9","costCenters":[],"links":[{"id":218841,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"2","issue":"3-4","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"505a14aae4b0c8380cd54ae1","contributors":{"authors":[{"text":"Mercer, J.W. Jr.","contributorId":25691,"corporation":false,"usgs":true,"family":"Mercer","given":"J.W.","suffix":"Jr.","email":"","affiliations":[],"preferred":false,"id":357787,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Pinder, G.F.","contributorId":104618,"corporation":false,"usgs":true,"family":"Pinder","given":"G.F.","affiliations":[],"preferred":false,"id":357788,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":1013582,"text":"1013582 - 1973 - Changes in the visual pigments of trout","interactions":[],"lastModifiedDate":"2023-11-17T00:36:38.202645","indexId":"1013582","displayToPublicDate":"1973-01-01T00:00:00","publicationYear":"1973","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1176,"text":"Canadian Journal of Zoology","active":true,"publicationSubtype":{"id":10}},"title":"Changes in the visual pigments of trout","docAbstract":"<div>The proportions of two visual pigments (rhodopsin and porphyropsin) were examined in four species of trout under experimental and natural conditions. Brook trout (<i>Salvelinus fontinalis</i>), rainbow trout (<i>Salmo gairdneri</i>), and brown trout (<i>Salmo trutta</i>) have different relative proportions of visual pigments in their retinae. The visual pigment balance in wild cutthroat trout (<i>Salmo clarki</i>) is related to forest canopy (access to light) and season. The brown trout have a more red-sensitive and less labile pair of visual pigments than brook or rainbow trout, which respond to photic conditions by increasing the proportion of porphyropsin (in light) and increasing rhodopsin (in darkness). The brown trout have a high percentage of porphyropsin, regardless of experimental conditions. This result does not reflect an inability to form rhodopsin but rather may relate to a consistently high proportion of 3-dehydroretinol in the pigment epithelium. The possible advantages and mechanisms of environmental control of trout visual pigment absorbance, as currently understood, are discussed.</div>","language":"English","publisher":"Canadian Science Publishing","doi":"10.1139/z73-137","usgsCitation":"Allen, D., McFarland, W., Munz, F., and Poston, H.A., 1973, Changes in the visual pigments of trout: Canadian Journal of Zoology, v. 51, no. 9, p. 901-914, https://doi.org/10.1139/z73-137.","productDescription":"14 p.","startPage":"901","endPage":"914","numberOfPages":"14","costCenters":[{"id":365,"text":"Leetown Science Center","active":true,"usgs":true}],"links":[{"id":131899,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"51","issue":"9","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e49e5e4b07f02db5e696f","contributors":{"authors":[{"text":"Allen, D.M.","contributorId":51696,"corporation":false,"usgs":true,"family":"Allen","given":"D.M.","email":"","affiliations":[],"preferred":false,"id":318786,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"McFarland, W.N.","contributorId":16796,"corporation":false,"usgs":true,"family":"McFarland","given":"W.N.","email":"","affiliations":[],"preferred":false,"id":318783,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Munz, F.W.","contributorId":40939,"corporation":false,"usgs":true,"family":"Munz","given":"F.W.","email":"","affiliations":[],"preferred":false,"id":318785,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Poston, H. A.","contributorId":21893,"corporation":false,"usgs":true,"family":"Poston","given":"H.","email":"","middleInitial":"A.","affiliations":[],"preferred":false,"id":318784,"contributorType":{"id":1,"text":"Authors"},"rank":4}]}}
,{"id":70010071,"text":"70010071 - 1973 - Age of Kōko Seamount, Emperor Seamount chain","interactions":[],"lastModifiedDate":"2022-11-22T15:46:30.038285","indexId":"70010071","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":"Age of Kōko Seamount, Emperor Seamount chain","docAbstract":"<p><span>K—</span><span>Ar ages obtained by the conventional isotope-dilution and the&nbsp;</span><sup>40</sup><span>Ar/</span><sup>39</sup><span>Ar techniques on two sanidine trachytes, four basalts, and a phonolite dredged from the top of Kōko Seamount, 300 km north of the Hawaiian-Emperor bend, show that the seamount is 46.4 ± 1.1 my old. These data indicate that the volcanoes in the Hawaiian-Emperor chain continue to increase in age to the west and north beyond Midway Atoll, as predicted by the melting-spot hypothesis for the origin of the chain, and that the rate of volcanic migration along the chain was nonlinear between the time of formation of the island of Hawaii and Kōko Seamount.</span></p>","language":"English","publisher":"Elsevier","doi":"10.1016/0012-821X(73)90209-4","usgsCitation":"Clague, D.A., and Dalrymple, G.B., 1973, Age of Kōko Seamount, Emperor Seamount chain: Earth and Planetary Science Letters, v. 17, no. 2, p. 411-415, https://doi.org/10.1016/0012-821X(73)90209-4.","productDescription":"5 p.","startPage":"411","endPage":"415","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[],"links":[{"id":219284,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"otherGeospatial":"Kōko Seamount","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"coordinates\": [\n          [\n            [\n              167.74029001240342,\n              39.315224155809034\n            ],\n            [\n              167.74029001240342,\n              31.05570696777248\n            ],\n            [\n              173.4998876510632,\n              31.05570696777248\n            ],\n            [\n              173.4998876510632,\n              39.315224155809034\n            ],\n            [\n              167.74029001240342,\n              39.315224155809034\n            ]\n          ]\n        ],\n        \"type\": \"Polygon\"\n      }\n    }\n  ]\n}","volume":"17","issue":"2","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"5059e8ede4b0c8380cd47fa2","contributors":{"authors":[{"text":"Clague, David A.","contributorId":77105,"corporation":false,"usgs":false,"family":"Clague","given":"David","email":"","middleInitial":"A.","affiliations":[],"preferred":false,"id":357828,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Dalrymple, G. Brent","contributorId":54564,"corporation":false,"usgs":true,"family":"Dalrymple","given":"G.","email":"","middleInitial":"Brent","affiliations":[],"preferred":false,"id":357829,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":70010293,"text":"70010293 - 1973 - Effect of sea water interaction on strontium isotope composition of deep-sea basalts","interactions":[],"lastModifiedDate":"2020-12-29T15:14:13.871125","indexId":"70010293","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":"Effect of sea water interaction on strontium isotope composition of deep-sea basalts","docAbstract":"<div id=\"abstracts\" class=\"Abstracts u-font-serif\"><div id=\"ab1\" class=\"abstract author\" lang=\"en\"><div id=\"aep-abstract-sec-id8\"><p>Analyses of rim-to-interior samples of fresh tholeiitic pillow basalts, deuterically altered holocrystalline basalts, and older, weathered tholeiitic basalts from the deep sea indicate that<span>&nbsp;</span><sup>87</sup>Sr/<sup>86</sup>Sr ratios of the older basalts are raised by low temperature interaction with strontium dissolved in sea water.<span>&nbsp;</span><sup>87</sup>Sr/<sup>86</sup>Sr correlates positively with H<sub>2</sub>O in these basalts; however, there is little detectable modification of the strontium isotope composition in rocks with H<sub>2</sub>O contents less than 1%. The isotope changes appear to be a function of relatively long-term, low-temperature weathering, rather than high-temperature or deuteric alteration. Strontium abundance and isotopic data for these rocks suggest that strontium content is only slightly modified by interaction with sea water, and it is a relatively insensitive indicator of marine alteration. Average Rb-Sr parameters for samples of apparently unaltered basalt are: Rb= 1.11ppm; Sr= 132ppm;<span>&nbsp;</span><sup>87</sup>Sr/<sup>86</sup>Sr= 0.70247.</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)90112-X","issn":"0012821X","usgsCitation":"Julius, D.E., Hedge, C., and Dymond, J., 1973, Effect of sea water interaction on strontium isotope composition of deep-sea basalts: Earth and Planetary Science Letters, v. 19, no. 2, p. 177-183, https://doi.org/10.1016/0012-821X(73)90112-X.","productDescription":"7 p.","startPage":"177","endPage":"183","numberOfPages":"7","costCenters":[],"links":[{"id":219224,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"19","issue":"2","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"505a0604e4b0c8380cd510a0","contributors":{"authors":[{"text":"Julius, Dasch E.","contributorId":85318,"corporation":false,"usgs":true,"family":"Julius","given":"Dasch","email":"","middleInitial":"E.","affiliations":[],"preferred":false,"id":358538,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Hedge, C. E.","contributorId":73611,"corporation":false,"usgs":true,"family":"Hedge","given":"C. E.","affiliations":[],"preferred":false,"id":358537,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Dymond, J.","contributorId":98461,"corporation":false,"usgs":true,"family":"Dymond","given":"J.","email":"","affiliations":[],"preferred":false,"id":358539,"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":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":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":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":70185774,"text":"70185774 - 1973 - River channel change with time : An example","interactions":[],"lastModifiedDate":"2017-03-29T08:58:28","indexId":"70185774","displayToPublicDate":"1973-01-01T00:00:00","publicationYear":"1973","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":"River channel change with time : An example","docAbstract":"<p><span>Monumented channel cross sections were resurveyed over a period of 20 yrs (1953 to 1972) to determine the amount and kind of change of channel area and position on a 3.7-sq-mi basin, Watts Branch near Rockville, Maryland. For the first 12 yrs, the channel progressively but slowly became smaller as urbanization of the basin gradually proceeded. After 1966, a threshold of change apparently was passed and, probably as a result of an increased rate of land alteration upstream, large amounts of sediment were deposited within the channel and overbank. The number of floods exceeding channel capacity increased dramatically from an average of two to more than ten per year. Simultaneously, the channel area began to increase. Despite the trend toward increasing cross-sectional area, the net result after 20 yrs was a channel smaller by 20 percent than it had been originally. Urbanization did not alter the rate of channel migration.</span></p>","language":"English","publisher":"Geological Society of America","doi":"10.1130/0016-7606(1973)84<1845:RCCWTA>2.0.CO;2 ","usgsCitation":"Leopold, L.B., 1973, River channel change with time : An example: Geological Society of America Bulletin, v. 84, no. 6, p. 1845-1860, https://doi.org/10.1130/0016-7606(1973)84<1845:RCCWTA>2.0.CO;2 .","productDescription":"16 p.","startPage":"1845","endPage":"1860","costCenters":[],"links":[{"id":338512,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United States","state":" Maryland","city":"Rockville","otherGeospatial":"Watts Branch","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -77.1902847290039,\n              39.07890809706475\n            ],\n            [\n              -77.15629577636717,\n              39.07890809706475\n            ],\n            [\n              -77.15629577636717,\n              39.11034974912018\n            ],\n            [\n              -77.1902847290039,\n              39.11034974912018\n            ],\n            [\n              -77.1902847290039,\n              39.07890809706475\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","volume":"84","issue":"6","publicComments":"Address as retiring president of The Geological Society of America, Minneapolis, Minnesota, November 1972","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"58dcc822e4b02ff32c685760","contributors":{"authors":[{"text":"Leopold, Luna Bergere","contributorId":93884,"corporation":false,"usgs":true,"family":"Leopold","given":"Luna","email":"","middleInitial":"Bergere","affiliations":[],"preferred":false,"id":686710,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":70159795,"text":"70159795 - 1973 - Rapid determination of sulfur in rocks","interactions":[],"lastModifiedDate":"2015-11-23T12:03:26","indexId":"70159795","displayToPublicDate":"1973-01-01T00:00:00","publicationYear":"1973","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":2446,"text":"Journal of Research of the U.S. Geological Survey","active":true,"publicationSubtype":{"id":10}},"title":"Rapid determination of sulfur in rocks","docAbstract":"<p>Sulfur is determined turbidimetrically as barium sulfate&nbsp;after an aqua regia attack. The turbidity is formed in an ammoniacal&nbsp;solution from which R2O3 has been centrifuged. Reproducibility of&nbsp;turbidity is obtained by adding barium chloride as a solid rather than as&nbsp;a solution. Sulfur is determined in the range 0.01-4 percent within&nbsp;&plusmn;0.02 absolute, or approximately 5 percent of the amount present,&nbsp;whichever is larger. A 100-mg sample is used for sulfur concentrations&nbsp;of up to 0.50 percent S, a 20-mg sample for higher levels. A&nbsp;determination requires about 5 minutes.</p>","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Reston, VA","usgsCitation":"Shapiro, L., 1973, Rapid determination of sulfur in rocks: Journal of Research of the U.S. Geological Survey, v. 1, no. 1, p. 81-84.","productDescription":"4 p.","startPage":"81","endPage":"84","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[],"links":[{"id":311656,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"},{"id":311655,"rank":1,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/journal/1973/vol1issue1/report.pdf","text":"Report","size":"22.2 MB","linkFileType":{"id":1,"text":"pdf"}}],"volume":"1","issue":"1","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"565446c5e4b071e7ea53d4d6","contributors":{"authors":[{"text":"Shapiro, Leonard","contributorId":61406,"corporation":false,"usgs":true,"family":"Shapiro","given":"Leonard","email":"","affiliations":[],"preferred":false,"id":580485,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":70159811,"text":"70159811 - 1973 - New data on cuprobismutite","interactions":[],"lastModifiedDate":"2015-11-25T12:59:59","indexId":"70159811","displayToPublicDate":"1973-01-01T00:00:00","publicationYear":"1973","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":2446,"text":"Journal of Research of the U.S. Geological Survey","active":true,"publicationSubtype":{"id":10}},"title":"New data on cuprobismutite","docAbstract":"<p>Cuprobismutite from Tunnel Extension Number Two&nbsp;mine, Ohio mining district, Utah, was chemically analyzed using the<br />electron microprobe. &nbsp;Its empirical formula was determined to be&nbsp;Cu<sub>20.8</sub> Ag<sub>0.97</sub> Pb<sub>0.35</sub> Mn<sub>0.22</sub> Bi<sub>26.7</sub>Sb<sub>0.06</sub> Te<sub>0.05</sub> Se<sub>0.55</sub> S<sub>50.4. &nbsp;</sub>The tentative conclusion is that unsubstituted cuprobismutite has the&nbsp;chemical formula 6Cu<sub>2</sub>S*6Bi<sub>2</sub>S<sub>3</sub> rather than the previously ascribed&nbsp;formula 6Cu<sub>2</sub>S*6Bi<sub>2</sub>S<sub>3</sub>&nbsp;and that cuprobismutite is therefore not&nbsp;dimorphous with emplectite.</p>","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Reston, VA","usgsCitation":"Taylor, C.M., Radtke, A.S., and Christ, C., 1973, New data on cuprobismutite: Journal of Research of the U.S. Geological Survey, v. 1, no. 1, p. 99-103.","productDescription":"5 pg","startPage":"99","endPage":"103","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[],"links":[{"id":311711,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"},{"id":311710,"rank":1,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/journal/1973/vol1issue1/report.pdf","text":"Report","size":"22.2 MB","linkFileType":{"id":1,"text":"pdf"}}],"country":"United States of America","state":"Utah","otherGeospatial":"Tunnel Extension Number Two Mine","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -112.27787017822266,\n              38.37288556789897\n            ],\n            [\n              -112.36061096191406,\n              38.38553501423449\n            ],\n            [\n              -112.39185333251953,\n              38.4291182807668\n            ],\n            [\n              -112.35923767089844,\n              38.480738480909324\n            ],\n            [\n              -112.32181549072266,\n              38.49095060018781\n            ],\n            [\n              -112.26585388183594,\n              38.49444388772503\n            ],\n            [\n              -112.20817565917967,\n              38.48046972138692\n            ],\n            [\n              -112.1982192993164,\n              38.42965618153018\n            ],\n            [\n              -112.20920562744139,\n              38.396029684120315\n            ],\n            [\n              -112.27787017822266,\n              38.37288556789897\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","volume":"1","issue":"1","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"5656e9bbe4b071e7ea53eeca","contributors":{"authors":[{"text":"Taylor, Charles M.","contributorId":150037,"corporation":false,"usgs":false,"family":"Taylor","given":"Charles","email":"","middleInitial":"M.","affiliations":[],"preferred":false,"id":580563,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Radtke, Arthur S.","contributorId":63795,"corporation":false,"usgs":true,"family":"Radtke","given":"Arthur","email":"","middleInitial":"S.","affiliations":[],"preferred":false,"id":580564,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Christ, C. L.","contributorId":53906,"corporation":false,"usgs":true,"family":"Christ","given":"C. L.","affiliations":[],"preferred":false,"id":580565,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":70010934,"text":"70010934 - 1973 - Determination of lead, uranium, thorium, and thallium in silicate glass standard materials by isotope dilution mass spectrometry","interactions":[],"lastModifiedDate":"2023-03-17T16:48:17.539084","indexId":"70010934","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":"Determination of lead, uranium, thorium, and thallium in silicate glass standard materials by isotope dilution mass spectrometry","docAbstract":"A set of four standard glasses has been prepared which have been doped with 61 different elements at the 500-, 50-, 1-, and 0.02-ppm level. The concentrations of lead, uranium, thorium, and thallium have been determined by isotope dilution mass spectrometry at a number of points in each of the glasses. The results obtained from independent determinations in two laboratories demonstrate the homogeneity of the samples and that precision of the order of 0.5% (95% L.E.) may be obtained by the method even at the 20-ppb level for these elements. The chemical and mass spectrometric procedures necessary are presented.","language":"English","publisher":"ACS Publications","doi":"10.1021/ac60328a005","usgsCitation":"Barnes, I.L., Garner, E.L., Gramlich, J.W., Moore, L.J., Murphy, T.J., Machlan, L.A., Shields, W.R., Tatsumoto, M., and Knight, R.J., 1973, Determination of lead, uranium, thorium, and thallium in silicate glass standard materials by isotope dilution mass spectrometry: Analytical Chemistry, v. 45, no. 6, p. 880-885, https://doi.org/10.1021/ac60328a005.","productDescription":"6 p.","startPage":"880","endPage":"885","numberOfPages":"6","costCenters":[],"links":[{"id":220736,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"45","issue":"6","noUsgsAuthors":false,"publicationDate":"2002-05-01","publicationStatus":"PW","scienceBaseUri":"5059ffb1e4b0c8380cd4f332","contributors":{"authors":[{"text":"Barnes, I. L.","contributorId":8342,"corporation":false,"usgs":false,"family":"Barnes","given":"I.","email":"","middleInitial":"L.","affiliations":[],"preferred":false,"id":359921,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Garner, E. L.","contributorId":52322,"corporation":false,"usgs":false,"family":"Garner","given":"E.","email":"","middleInitial":"L.","affiliations":[],"preferred":false,"id":359922,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Gramlich, J. W.","contributorId":69967,"corporation":false,"usgs":false,"family":"Gramlich","given":"J.","email":"","middleInitial":"W.","affiliations":[],"preferred":false,"id":359924,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Moore, L. J.","contributorId":53132,"corporation":false,"usgs":false,"family":"Moore","given":"L.","email":"","middleInitial":"J.","affiliations":[],"preferred":false,"id":359923,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"Murphy, T. J.","contributorId":90982,"corporation":false,"usgs":false,"family":"Murphy","given":"T.","email":"","middleInitial":"J.","affiliations":[],"preferred":false,"id":359926,"contributorType":{"id":1,"text":"Authors"},"rank":5},{"text":"Machlan, L. A.","contributorId":90983,"corporation":false,"usgs":false,"family":"Machlan","given":"L.","email":"","middleInitial":"A.","affiliations":[],"preferred":false,"id":359927,"contributorType":{"id":1,"text":"Authors"},"rank":6},{"text":"Shields, W. R.","contributorId":7412,"corporation":false,"usgs":false,"family":"Shields","given":"W.","email":"","middleInitial":"R.","affiliations":[],"preferred":false,"id":359920,"contributorType":{"id":1,"text":"Authors"},"rank":7},{"text":"Tatsumoto, Mitsunobu","contributorId":10444,"corporation":false,"usgs":true,"family":"Tatsumoto","given":"Mitsunobu","email":"","affiliations":[],"preferred":false,"id":359925,"contributorType":{"id":1,"text":"Authors"},"rank":8},{"text":"Knight, R. J.","contributorId":96255,"corporation":false,"usgs":true,"family":"Knight","given":"R.","email":"","middleInitial":"J.","affiliations":[],"preferred":false,"id":359928,"contributorType":{"id":1,"text":"Authors"},"rank":9}]}}
,{"id":1001284,"text":"1001284 - 1973 - Selective predation by mink, Mustela vison, on waterfowl","interactions":[],"lastModifiedDate":"2023-02-15T17:47:19.430685","indexId":"1001284","displayToPublicDate":"1973-01-01T00:00:00","publicationYear":"1973","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":737,"text":"American Midland Naturalist","active":true,"publicationSubtype":{"id":10}},"title":"Selective predation by mink, Mustela vison, on waterfowl","docAbstract":"<p>Predation by mink (<i>Mustela vison</i>) on three types of ducks (captive, pen-reared-released and wild) was documented in two studies at the Northern Prairie Wildlife Research Center, Jamestown, North Dakota. In the first study, 36 of 60 flightless adult and juvenile ducks held on eight 0.1-acre experimental ponds disappeared between 10 July and 4 August 1969. Available evidence indicated that all were killed by a large adult mink. The mink selected recently released incubator-hatched ducklings, females in the process of incubating, and adults and juveniles on a marginal food supply.In the second study, 152 wood duck ducklings (<i>Aix sponsa</i>) were released on a 76-acre marsh during 1971. Half of the ducklings, when 24 to 27 days old, were placed at weekly intervals in four floating pens and allowed to escape after 4 days. Each time birds were placed in the floating pens, a comparable group was placed in a predator-proof shoreline pen. Birds in the shoreline pen escaped as they learned to fly when approximately 60 days old. The shoreline of the marsh was periodically searched, and the remains of 21 (28%) of the floating-pen birds were identified in food remains found at 16 mink dens. No remains of birds from the shoreline pen were found at the dens. Coots (<i>Fulica americana</i>) were also taken commonly. Wild ducklings appeared to have been almost totally consumed, but the legs and feet of the wood ducks were often left uneaten because of bands and tags.</p>","language":"English","publisher":"University of Notre Dame","doi":"10.2307/2424149","usgsCitation":"Sargeant, A.B., Swanson, G.A., and Doty, H.A., 1973, Selective predation by mink, Mustela vison, on waterfowl: American Midland Naturalist, v. 89, no. 1, p. 208-214, https://doi.org/10.2307/2424149.","productDescription":"7 p.","startPage":"208","endPage":"214","costCenters":[{"id":480,"text":"Northern Prairie Wildlife Research Center","active":true,"usgs":true}],"links":[{"id":133311,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"89","issue":"1","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e49e2e4b07f02db5e4c1e","contributors":{"authors":[{"text":"Sargeant, Alan B.","contributorId":89185,"corporation":false,"usgs":true,"family":"Sargeant","given":"Alan","email":"","middleInitial":"B.","affiliations":[],"preferred":false,"id":310802,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Swanson, George A.","contributorId":49654,"corporation":false,"usgs":true,"family":"Swanson","given":"George","email":"","middleInitial":"A.","affiliations":[],"preferred":false,"id":310804,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Doty, Harold A.","contributorId":17565,"corporation":false,"usgs":true,"family":"Doty","given":"Harold","email":"","middleInitial":"A.","affiliations":[],"preferred":false,"id":310803,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":1001295,"text":"1001295 - 1973 - Mortality among birds, mammals and certain snakes on 17 miles of Minnesota roads","interactions":[],"lastModifiedDate":"2018-01-05T10:39:54","indexId":"1001295","displayToPublicDate":"1973-01-01T00:00:00","publicationYear":"1973","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":2632,"text":"Loon","active":true,"publicationSubtype":{"id":10}},"title":"Mortality among birds, mammals and certain snakes on 17 miles of Minnesota roads","docAbstract":"Abstract has not been submitted","largerWorkType":{"id":2,"text":"Article"},"largerWorkTitle":"Loon","largerWorkSubtype":{"id":10,"text":"Journal Article"},"language":"English","usgsCitation":"Sargeant, A., and Forbes, J., 1973, Mortality among birds, mammals and certain snakes on 17 miles of Minnesota roads: Loon, v. 45, no. 1, p. 4-7.","productDescription":"4 p.","startPage":"4","endPage":"7","costCenters":[{"id":480,"text":"Northern Prairie Wildlife Research Center","active":true,"usgs":true}],"links":[{"id":130588,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"45","issue":"1","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b03e4b07f02db698e64","contributors":{"authors":[{"text":"Sargeant, A.B.","contributorId":13171,"corporation":false,"usgs":true,"family":"Sargeant","given":"A.B.","email":"","affiliations":[],"preferred":false,"id":310828,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Forbes, J.E.","contributorId":25106,"corporation":false,"usgs":true,"family":"Forbes","given":"J.E.","email":"","affiliations":[],"preferred":false,"id":310829,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":1001415,"text":"1001415 - 1973 - Computerized system for organizing and maintaining files of banding data","interactions":[],"lastModifiedDate":"2023-11-03T11:54:10.540333","indexId":"1001415","displayToPublicDate":"1973-01-01T00:00:00","publicationYear":"1973","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1054,"text":"Bird-Banding","active":true,"publicationSubtype":{"id":10}},"title":"Computerized system for organizing and maintaining files of banding data","docAbstract":"<p>No abstract available.</p>","language":"English","publisher":"Association of Field Ornithologists","doi":"10.2307/4511959","usgsCitation":"Cowardin, L., and Davenport, D., 1973, Computerized system for organizing and maintaining files of banding data: Bird-Banding, v. 44, no. 3, p. 187-195, https://doi.org/10.2307/4511959.","productDescription":"9 p.","startPage":"187","endPage":"195","costCenters":[{"id":480,"text":"Northern Prairie Wildlife Research Center","active":true,"usgs":true}],"links":[{"id":502561,"rank":2,"type":{"id":41,"text":"Open Access External Repository Page"},"url":"https://digitalcommons.usf.edu/bird_banding/vol44/iss3/5","text":"External Repository"},{"id":129158,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"44","issue":"3","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a82e4b07f02db64ae1a","contributors":{"authors":[{"text":"Cowardin, L.M.","contributorId":106435,"corporation":false,"usgs":true,"family":"Cowardin","given":"L.M.","email":"","affiliations":[],"preferred":false,"id":311001,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Davenport, D.A.","contributorId":71126,"corporation":false,"usgs":true,"family":"Davenport","given":"D.A.","email":"","affiliations":[],"preferred":false,"id":311000,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":1001298,"text":"1001298 - 1973 - Canada goose restoration in North Dakota","interactions":[],"lastModifiedDate":"2018-01-02T12:41:53","indexId":"1001298","displayToPublicDate":"1973-01-01T00:00:00","publicationYear":"1973","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":2891,"text":"North Dakota Outdoors","active":true,"publicationSubtype":{"id":10}},"title":"Canada goose restoration in North Dakota","docAbstract":"Abstract has not been submitted","largerWorkType":{"id":2,"text":"Article"},"largerWorkTitle":"North Dakota Outdoors","largerWorkSubtype":{"id":10,"text":"Journal Article"},"language":"English","usgsCitation":"Lee, F., Kruse, A., and Schroeder, C., 1973, Canada goose restoration in North Dakota: North Dakota Outdoors, v. 35, no. 8, p. 18-21.","productDescription":"4 p.","startPage":"18","endPage":"21","costCenters":[{"id":480,"text":"Northern Prairie Wildlife Research Center","active":true,"usgs":true}],"links":[{"id":130590,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"35","issue":"8","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e49ffe4b07f02db5f7c12","contributors":{"authors":[{"text":"Lee, F.B.","contributorId":30174,"corporation":false,"usgs":true,"family":"Lee","given":"F.B.","email":"","affiliations":[],"preferred":false,"id":310836,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Kruse, A.D.","contributorId":19900,"corporation":false,"usgs":true,"family":"Kruse","given":"A.D.","email":"","affiliations":[],"preferred":false,"id":310835,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Schroeder, C.H.","contributorId":104846,"corporation":false,"usgs":true,"family":"Schroeder","given":"C.H.","email":"","affiliations":[],"preferred":false,"id":310837,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":70011040,"text":"70011040 - 1973 - Yukon River: Evidence for extensive migration during the Holocene transgression","interactions":[],"lastModifiedDate":"2026-01-23T21:41:23.653766","indexId":"70011040","displayToPublicDate":"1973-01-01T00:00:00","publicationYear":"1973","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":3338,"text":"Science","active":true,"publicationSubtype":{"id":10}},"title":"Yukon River: Evidence for extensive migration during the Holocene transgression","docAbstract":"The shift of the Yukon River, during the Holocene sea-level transgression, from south of Nunivak Island during the Wisconsin maximum to its present location (a distance greater than 300 kilometers) is indicated by remanent channels, distinct subbottom structures, deltaic sediments, and anomalous rates of sediment accumulation on the continental shelf of the east-central Bering Sea. These features were produced as the ancestral river migrated northward across the easternmost part of this area before 11,000 years ago.","language":"English","publisher":"American Association for the Advancement of Science","doi":"10.1126/science.179.4079.1230","issn":"00368075","usgsCitation":"Knebel, H., and Creager, J., 1973, Yukon River: Evidence for extensive migration during the Holocene transgression: Science, v. 179, no. 4079, p. 1230-1232, https://doi.org/10.1126/science.179.4079.1230.","productDescription":"3 p.","startPage":"1230","endPage":"1232","costCenters":[],"links":[{"id":220683,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United States","state":"Alaska","otherGeospatial":"Nunivak Island","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"coordinates\": [\n          [\n            [\n              -167.64116793346082,\n              60.49914455348872\n            ],\n            [\n              -167.64116793346082,\n              59.684080613886096\n            ],\n            [\n              -165.2448127086173,\n              59.684080613886096\n            ],\n            [\n              -165.2448127086173,\n              60.49914455348872\n            ],\n            [\n              -167.64116793346082,\n              60.49914455348872\n            ]\n          ]\n        ],\n        \"type\": \"Polygon\"\n      }\n    }\n  ]\n}","volume":"179","issue":"4079","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"505bd257e4b08c986b32f76b","contributors":{"authors":[{"text":"Knebel, H.J.","contributorId":79092,"corporation":false,"usgs":true,"family":"Knebel","given":"H.J.","affiliations":[],"preferred":false,"id":360132,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Creager, J.S.","contributorId":80414,"corporation":false,"usgs":true,"family":"Creager","given":"J.S.","email":"","affiliations":[],"preferred":false,"id":360133,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":70161849,"text":"70161849 - 1973 - Open-jaw syndrome in chinook salmon (<i>Oncorhynchus tshawytscha</i>) at a hatchery","interactions":[],"lastModifiedDate":"2016-08-15T21:19:09","indexId":"70161849","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":"Open-jaw syndrome in chinook salmon (<i>Oncorhynchus tshawytscha</i>) at a hatchery","docAbstract":"<p><span>Nearly 0.5% of the yearling spring chinook salmon (</span><i>Oncorhynchus tshawytscha</i><span>) at a national fish hatchery were observed with mouth agape, the condition occurring in two of 16 ponds. X-radiographs and histological preparations indicated that the articular bone of the lower jaw was malformed and dislocated dorsal and posterior to its normal point of attachment. The bone appeared to be embedded in the mandibular muscle and surrounded by an extensive fibrous tissue network. Genetic aberration, environmental interaction, and teratogenic substances are discussed as possible causes of the anomaly.</span></p>","language":"English","publisher":"NRC Research Press","doi":"10.1139/f73-304","usgsCitation":"Crouch, D.E., Yasutake, W.T., and Rucker, R.R., 1973, Open-jaw syndrome in chinook salmon (<i>Oncorhynchus tshawytscha</i>) at a hatchery: Journal of the Fisheries Research Board of Canada, v. 30, no. 12, p. 1890-1892, https://doi.org/10.1139/f73-304.","productDescription":"3 p.","startPage":"1890","endPage":"1892","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[{"id":654,"text":"Western Fisheries Research Center","active":true,"usgs":true}],"links":[{"id":313988,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"30","issue":"12","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"568e4921e4b0e7a44bc41a1c","contributors":{"authors":[{"text":"Crouch, Dennis E.","contributorId":152101,"corporation":false,"usgs":false,"family":"Crouch","given":"Dennis","email":"","middleInitial":"E.","affiliations":[],"preferred":false,"id":587920,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Yasutake, William T.","contributorId":70444,"corporation":false,"usgs":true,"family":"Yasutake","given":"William","email":"","middleInitial":"T.","affiliations":[],"preferred":false,"id":587921,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Rucker, Robert R.","contributorId":69615,"corporation":false,"usgs":true,"family":"Rucker","given":"Robert","email":"","middleInitial":"R.","affiliations":[],"preferred":false,"id":587922,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":70161848,"text":"70161848 - 1973 - Computer program for sample sizes required to determine disease incidence in fish populations","interactions":[],"lastModifiedDate":"2016-01-06T16:19:15","indexId":"70161848","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":"Computer program for sample sizes required to determine disease incidence in fish populations","docAbstract":"<p><span>A computer program is described for generating the sample size tables required in fish hatchery disease inspection and certification. The program was designed to aid in detection of infectious pancreatic necrosis (IPN) in salmonids, but it is applicable to any fish disease inspection when the sampling plan follows the hypergeometric distribution.</span></p>","language":"English","publisher":"NRC Research Press","doi":"10.1139/f73-223","usgsCitation":"Ossiander, F.J., and Wedemeyer, G., 1973, Computer program for sample sizes required to determine disease incidence in fish populations: Journal of the Fisheries Research Board of Canada, v. 30, no. 9, p. 1383-1384, https://doi.org/10.1139/f73-223.","productDescription":"2 p.","startPage":"1383","endPage":"1384","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[{"id":654,"text":"Western Fisheries Research Center","active":true,"usgs":true}],"links":[{"id":313987,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"30","issue":"9","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"568e48e9e4b0e7a44bc418be","contributors":{"authors":[{"text":"Ossiander, Frank J.","contributorId":152100,"corporation":false,"usgs":false,"family":"Ossiander","given":"Frank","email":"","middleInitial":"J.","affiliations":[],"preferred":false,"id":587918,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Wedemeyer, Gary gwedemeyer@usgs.gov","contributorId":5504,"corporation":false,"usgs":true,"family":"Wedemeyer","given":"Gary","email":"gwedemeyer@usgs.gov","affiliations":[],"preferred":true,"id":587919,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":5778,"text":"pp765 - 1973 - Geology of the oxidized uranium ore deposits of the Tordilla Hill-Deweesville area, Karnes County, Texas; a study of a district before mining","interactions":[],"lastModifiedDate":"2023-03-23T21:52:46.450541","indexId":"pp765","displayToPublicDate":"1973-01-01T00:00:00","publicationYear":"1973","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":331,"text":"Professional Paper","code":"PP","onlineIssn":"2330-7102","printIssn":"1044-9612","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"765","title":"Geology of the oxidized uranium ore deposits of the Tordilla Hill-Deweesville area, Karnes County, Texas; a study of a district before mining","docAbstract":"<p>No abstract available.</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/pp765","usgsCitation":"Bunker, C.M., and MacKallor, J., 1973, Geology of the oxidized uranium ore deposits of the Tordilla Hill-Deweesville area, Karnes County, Texas; a study of a district before mining: U.S. Geological Survey Professional Paper 765, Report: iii, 37 p.; 1 Plate: 41.00 x 28.00 inches, https://doi.org/10.3133/pp765.","productDescription":"Report: iii, 37 p.; 1 Plate: 41.00 x 28.00 inches","costCenters":[],"links":[{"id":32455,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/pp/0765/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":32454,"rank":3,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/pp/0765/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":118015,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/pp/0765/report-thumb.jpg"},{"id":414668,"rank":4,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_5037.htm","linkFileType":{"id":5,"text":"html"}}],"country":"United States","state":"Texas","county":"Karnes County","otherGeospatial":"Tordilla Hill-Deweesville area","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"coordinates\": [\n          [\n            [\n              -98.3214,\n              29\n            ],\n            [\n              -98.3214,\n              28.6017\n            ],\n            [\n              -97.9761,\n              28.6017\n            ],\n            [\n              -97.9761,\n              29\n            ],\n            [\n              -98.3214,\n              29\n            ]\n          ]\n        ],\n        \"type\": \"Polygon\"\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b1be4b07f02db6a9040","contributors":{"authors":[{"text":"Bunker, C. M.","contributorId":75138,"corporation":false,"usgs":true,"family":"Bunker","given":"C.","email":"","middleInitial":"M.","affiliations":[],"preferred":false,"id":151570,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"MacKallor, J. A.","contributorId":75528,"corporation":false,"usgs":true,"family":"MacKallor","given":"J. A.","affiliations":[],"preferred":false,"id":151571,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
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