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,{"id":70010589,"text":"70010589 - 1956 - Pollen from Leda clay of Maine","interactions":[],"lastModifiedDate":"2026-03-02T16:08:29.394326","indexId":"70010589","displayToPublicDate":"1956-06-22T00:00:00","publicationYear":"1956","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":3338,"text":"Science","active":true,"publicationSubtype":{"id":10}},"title":"Pollen from Leda clay of Maine","docAbstract":"<p>No abstract available.</p>","language":"English","publisher":"American Association for the Advancement of Science","doi":"10.1126/science.123.3208.1118.b","issn":"00368075","usgsCitation":"Knox, A., 1956, Pollen from Leda clay of Maine: Science, v. 123, no. 3208, p. 1118-1119, https://doi.org/10.1126/science.123.3208.1118.b.","productDescription":"2 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,{"id":5220249,"text":"5220249 - 1956 - An appraisal of bicolor lespedeza in quail management","interactions":[],"lastModifiedDate":"2025-01-31T16:45:20.22532","indexId":"5220249","displayToPublicDate":"1956-04-02T00:00:00","publicationYear":"1956","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":2508,"text":"Journal of Wildlife Management","active":true,"publicationSubtype":{"id":10}},"title":"An appraisal of bicolor lespedeza in quail management","docAbstract":"<p>No abstract available.&nbsp;</p>","language":"English","publisher":"Wiley","doi":"10.2307/3797413","usgsCitation":"Rosene, W., 1956, An appraisal of bicolor lespedeza in quail management: Journal of Wildlife Management, v. 20, no. 2, p. 104-110, https://doi.org/10.2307/3797413.","productDescription":"7 p.","startPage":"104","endPage":"110","costCenters":[{"id":531,"text":"Patuxent Wildlife Research 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,{"id":70213489,"text":"70213489 - 1956 - Application of the modified Einstein procedure for computation of total sediment load","interactions":[],"lastModifiedDate":"2020-09-17T20:47:30.58128","indexId":"70213489","displayToPublicDate":"1956-04-01T15:44:31","publicationYear":"1956","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1578,"text":"Eos, Transactions, American Geophysical Union","onlineIssn":"2324-9250","printIssn":"0096-394","active":true,"publicationSubtype":{"id":10}},"title":"Application of the modified Einstein procedure for computation of total sediment load","docAbstract":"<p><span>A method that enables good estimates to be made of total sediment load has been tested with data from several western streams. The method, which uses both theoretical and empirical formulas, combines a modification of Einstein's procedure for computing bed‐material load and the usually available data from suspended‐sediment measurements. Basic data, including data from large natural and artificial turbulent flumes, and the results of computations are given.</span></p>","language":"English","publisher":"American Geophysical Union","doi":"10.1029/TR037i002p00197","usgsCitation":"Schroeder, K.B., and Hembree, C., 1956, Application of the modified Einstein procedure for computation of total sediment load: Eos, Transactions, American Geophysical Union, v. 37, no. 2, p. 197-212, https://doi.org/10.1029/TR037i002p00197.","productDescription":"15 p.","startPage":"197","endPage":"212","costCenters":[],"links":[{"id":378546,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"37","issue":"2","noUsgsAuthors":false,"publicationDate":"2014-08-18","publicationStatus":"PW","contributors":{"authors":[{"text":"Schroeder, K. B.","contributorId":240920,"corporation":false,"usgs":false,"family":"Schroeder","given":"K.","email":"","middleInitial":"B.","affiliations":[],"preferred":false,"id":799132,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Hembree, C. H.","contributorId":106866,"corporation":false,"usgs":true,"family":"Hembree","given":"C. H.","affiliations":[],"preferred":false,"id":799133,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":37790,"text":"37790 - 1956 - Public use of National Wildlife Refuges, 1955","interactions":[],"lastModifiedDate":"2014-07-24T08:47:57","indexId":"37790","displayToPublicDate":"1956-04-01T08:47:18","publicationYear":"1956","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":1,"text":"Federal Government Series"},"seriesTitle":{"id":98,"text":"Wildlife Leaflet","active":false,"publicationSubtype":{"id":1}},"seriesNumber":"375","title":"Public use of National Wildlife Refuges, 1955","docAbstract":"No abstract available.","language":"English","publisher":"U.S. Fish and Wildlife Service, Branch of Wildlife Refuges","publisherLocation":"Washington, D.C.","usgsCitation":"U.S. Fish and Wildlife Service, 1956, Public use of National Wildlife Refuges, 1955 (Reissued from Wildlife Leaflet 366 (1955).): Wildlife Leaflet 375, 4 p.","productDescription":"4 p.","numberOfPages":"4","costCenters":[],"links":[{"id":290847,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"edition":"Reissued from Wildlife Leaflet 366 (1955).","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"57ffd4a2e4b0824b2d177353","contributors":{"authors":[{"text":"U.S. Fish and Wildlife Service","contributorId":128143,"corporation":true,"usgs":false,"organization":"U.S. Fish and Wildlife Service","id":529724,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":70010480,"text":"70010480 - 1956 - U. S. Geological Survey radiocarbon dates III","interactions":[],"lastModifiedDate":"2026-03-02T16:45:28.032379","indexId":"70010480","displayToPublicDate":"1956-03-16T00:00:00","publicationYear":"1956","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":3338,"text":"Science","active":true,"publicationSubtype":{"id":10}},"title":"U. S. Geological Survey radiocarbon dates III","docAbstract":"<p>No abstract available.</p>","language":"English","publisher":"American Association for the Advancement of Science","doi":"10.1126/science.123.3194.442","issn":"00368075","usgsCitation":"Rubin, M., and Suess, H.E., 1956, U. S. Geological Survey radiocarbon dates III: Science, v. 123, no. 3194, p. 442-448, https://doi.org/10.1126/science.123.3194.442.","productDescription":"7 p.","startPage":"442","endPage":"448","costCenters":[],"links":[{"id":219149,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"123","issue":"3194","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"505bba3be4b08c986b328055","contributors":{"authors":[{"text":"Rubin, M.","contributorId":88079,"corporation":false,"usgs":true,"family":"Rubin","given":"M.","email":"","affiliations":[],"preferred":false,"id":359020,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Suess, H. E.","contributorId":69292,"corporation":false,"usgs":false,"family":"Suess","given":"H.","email":"","middleInitial":"E.","affiliations":[],"preferred":false,"id":359019,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":71235,"text":"tei137 - 1956 - Non-pegmatitic resources of beryllium in United States","interactions":[],"lastModifiedDate":"2014-03-25T08:36:59","indexId":"tei137","displayToPublicDate":"1956-03-06T10:02:00","publicationYear":"1956","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":337,"text":"Trace Elements Investigations","code":"TEI","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"137","title":"Non-pegmatitic resources of beryllium in United States","docAbstract":"During the period from 1948 to 1950 the U.S. Geological Survey conducted a program of field\nand laboratory research w determine the mode of occurrence of beryllium in non-pegmatitic rocks and\nmineral deposits as part of the Beryllium Program of the Division of Raw Materials of the U.S. Atomic\nEnergy Commission. Approximately 23 man months were spent in the field collecting samples from 146\nlocalities in 15 states; a total of 680 samples were collected and analyzed for beryllium. Additional\nsamples collected by the Geological Survey. U.S. Bureau of Mines, various state Geological Surveys\nand other institutions. and private companies were analyzed for beryllium. In total, the beryllium\ncontent of 1,238 samples from about 600 localities in the United States is compiled in the final report\nwhich is being prepared for publication by the U.S. Geological Survey. The main topics discussed are:\nuses and properties of beryllium; methods of analysis and mineralogy of beryllium; occurrence of\nberyllium in igneous, sedimentary and metamorphic rocks, pyrometasomatic and related deposits, vein\ndeposits, and hot spring deposits; the genesis of beryllium deposits; and a description of the deposits\nexamined. This abstract and table 1 summarize the more pertinent economic data.\nBeryllium is more abundant than arsenic, gold, silver, and molybdenum in the lithosphere, but\nits chemical and physical properties prohibit its concentration in minerals which are common w large\ncommercial vein and replacement deposits. There are 29 minerals in which beryllium is an essential\nconstituent but of these only beryl, mined from granite pegmatites, is an ore of beryllium., Beryl also\noccurs disseminated in granites and high-temperature veins. The other 28 minerals occur as rare\nconstituents in syenite and granite pegmatites, granites, and pyrometasomatic deposits. Beryllium, as\na trace constituent, has been detected in 49 minerals but recovery of the beryllium requires metallurgical\nmethods as yet unknown.","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Reston, VA","doi":"10.3133/tei137","collaboration":"This report concerns work done on behalf of the Division of Raw Materials of the U.S. Atomic Energy Commissione","usgsCitation":"Warner, L.A., Holser, W., Wilmarth, V., and Cameron, E., 1956, Non-pegmatitic resources of beryllium in United States: U.S. Geological Survey Trace Elements Investigations 137, 10 p., https://doi.org/10.3133/tei137.","productDescription":"10 p.","costCenters":[],"links":[{"id":284516,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/tei/0137/report.pdf"},{"id":283405,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/tei137.png"}],"country":"United States","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -124.8,24.5 ], [ -124.8,49.383333 ], [ -66.95,49.383333 ], [ -66.95,24.5 ], [ -124.8,24.5 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"53cd6928e4b0b2908510286c","contributors":{"authors":[{"text":"Warner, Lawrence Allen","contributorId":25144,"corporation":false,"usgs":true,"family":"Warner","given":"Lawrence","email":"","middleInitial":"Allen","affiliations":[],"preferred":false,"id":283843,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Holser, W.T.","contributorId":81964,"corporation":false,"usgs":true,"family":"Holser","given":"W.T.","email":"","affiliations":[],"preferred":false,"id":283845,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Wilmarth, V.R.","contributorId":20803,"corporation":false,"usgs":true,"family":"Wilmarth","given":"V.R.","email":"","affiliations":[],"preferred":false,"id":283842,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Cameron, E.N.","contributorId":63860,"corporation":false,"usgs":true,"family":"Cameron","given":"E.N.","email":"","affiliations":[],"preferred":false,"id":283844,"contributorType":{"id":1,"text":"Authors"},"rank":4}]}}
,{"id":37791,"text":"37791 - 1956 - Inventory of big-game animals of the United States, 1954","interactions":[],"lastModifiedDate":"2014-07-24T08:50:03","indexId":"37791","displayToPublicDate":"1956-03-01T08:49:29","publicationYear":"1956","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":1,"text":"Federal Government Series"},"seriesTitle":{"id":98,"text":"Wildlife Leaflet","active":false,"publicationSubtype":{"id":1}},"seriesNumber":"376","title":"Inventory of big-game animals of the United States, 1954","docAbstract":"No abstract available.","language":"English","publisher":"U.S. Department of the Interior","publisherLocation":"Washington, D.C.","collaboration":"Compiled by Denver Wildlife Research Laboratory, Branch of Wildlife Research.","usgsCitation":"Wildlife Research Laboratory, 1956, Inventory of big-game animals of the United States, 1954 (Reissued from Wildlife Leaflet 342 (1952).): Wildlife Leaflet 376, 3 p.","productDescription":"3 p.","numberOfPages":"3","costCenters":[],"links":[{"id":290848,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"edition":"Reissued from Wildlife Leaflet 342 (1952).","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"57ffd4a2e4b0824b2d177355","contributors":{"authors":[{"text":"Wildlife Research Laboratory","contributorId":128030,"corporation":true,"usgs":false,"organization":"Wildlife Research Laboratory","id":529725,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":37789,"text":"37789 - 1956 - Text of some Federal laws on wildlife protection","interactions":[],"lastModifiedDate":"2014-07-24T08:45:56","indexId":"37789","displayToPublicDate":"1956-03-01T08:45:23","publicationYear":"1956","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":1,"text":"Federal Government Series"},"seriesTitle":{"id":98,"text":"Wildlife Leaflet","active":false,"publicationSubtype":{"id":1}},"seriesNumber":"374","title":"Text of some Federal laws on wildlife protection","docAbstract":"No abstract available.","language":"English","publisher":"U.S. Department of the Interior","publisherLocation":"Washington, D.C.","collaboration":"Compiled in the Branch of Game Management.","usgsCitation":"U.S. Fish and Wildlife Service, 1956, Text of some Federal laws on wildlife protection: Wildlife Leaflet 374, 47 p.","productDescription":"47 p.","numberOfPages":"47","costCenters":[],"links":[{"id":290846,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"57ffd4a2e4b0824b2d177357","contributors":{"authors":[{"text":"U.S. Fish and Wildlife Service","contributorId":128143,"corporation":true,"usgs":false,"organization":"U.S. Fish and Wildlife Service","id":529723,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":70048375,"text":"tei624 - 1956 - Uranium content of ground and surface waters in western Kansas, eastern Colorado, and the Oklahoma Panhande","interactions":[],"lastModifiedDate":"2013-11-22T09:25:50","indexId":"tei624","displayToPublicDate":"1956-01-10T11:43:00","publicationYear":"1956","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":337,"text":"Trace Elements Investigations","code":"TEI","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"624","title":"Uranium content of ground and surface waters in western Kansas, eastern Colorado, and the Oklahoma Panhande","docAbstract":"During 1954, 1955, and 1956, 324 water samples were collected in western Kansas, eastern Colorado, the Oklahoma Panhandle, and northeastern New Mexico, to determine the uranium content of water from the various rock units and geologic terranes in the region, and to locate areas in which, large amounts of uranium in the water might reflect the presence of nearby uranium accumulations. Three geologic terranes are present in the report area: the Tertiary-Quaternary tuff ace o us terrane, the Upper Cretaceous shale terrane, and the upper Permian through Lower Cretaceous sandstone terrane. The average uranium content of 179 water samples from the tuffaceous terrane, which is composed primarily of tuffaceous, fluviatile rocks ranging in age from Pliocene to Pleistocene, is 6.7 parts per billion. A total of 48 samples from the Upper Cretaceous shale terrane, which is composed almost entirely\nof shale and limestone of marine origin, contain an average of 20.4 parts per billion uranium , Sandstone, silt stone, and clay stone of terrestrial and near-shore marine origin are the predominant constituents of the upper Permian through Lower Cretaceous sandstone terrane, and the 83 water samples collected from, or related to, rock units of this terrane contain an average of 10.2 parts per billion uranium. The average uranium content figure derived for the tipper Cretaceous shale terrane may not be representative of the uranium content of waters from this terrane throughout the report area because more than half of the samples assigned to the terrane were collected in an area in which most water samples contain relatively large amounts of uranium. Compared to the shale terrane, the tuffaceous terrane and the sandstone terrane are both represented by a greater number of samples collected over a much larger area and the average uranium content figures derived for them are believed to be representative of the uranium content of waters from, or related to, rock units of the two terranes in the report area. The average uranium content figures derived for different rock units, or groups of rock units, subdivided by the source type from which the samples were collected (well, spring, stream, municipal water system, reservoir, or lake), and in some cases by geographic parts of the report area, are believed to be of more potential use in any future hydrogeochemical exploration in the area than are the average uranium content figures derived for the three geologic terranes. The average uranium content of ground-water samples from 12 individual rock units or groups of rock units ranges from less than 1. 0 to 38 parts per billion. Several rock units were sampled over large enough areas to indicate that waters from the same rock unit in different parts of the report area may range widely in average uranium content. Water samples from some of the rock units in the area, particularly those of Triassic and Permian age, contain large amounts of uranium,\nand in some parts of the report area, such as the Cimarron River area of westernmost Oklahoma and northeastern New Mexico, and the Rule Creek area in Bent and Las Animas Counties, Colo. , most, or all, of the water samples collected contain relatively large amounts of uranium. Further exploration to determine the source of the uranium in the water from these rock units and areas may be worthwhile.","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/tei624","collaboration":"Prepared in cooperation with the U.S. Atomic Energy Commission","usgsCitation":"Landis, E., 1956, Uranium content of ground and surface waters in western Kansas, eastern Colorado, and the Oklahoma Panhande: U.S. Geological Survey Trace Elements Investigations 624, Report: 73 p.; Plate 1: 33.36 inches x 23.81 inches, https://doi.org/10.3133/tei624.","productDescription":"Report: 73 p.; Plate 1: 33.36 inches x 23.81 inches","additionalOnlineFiles":"Y","costCenters":[],"links":[{"id":278037,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/tei/624/report-thumb.jpg"},{"id":279537,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/tei/624/plate-1.pdf"},{"id":279536,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/tei/624/report.pdf"}],"country":"United States","state":"Colorado;Kansas;New Mexico;Oklahoma","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -104.62,36.13 ], [ -104.62,40.11 ], [ -99.47,40.11 ], [ -99.47,36.13 ], [ -104.62,36.13 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"5242b466e4b096ee62464206","contributors":{"authors":[{"text":"Landis, E.R.","contributorId":40605,"corporation":false,"usgs":true,"family":"Landis","given":"E.R.","email":"","affiliations":[],"preferred":false,"id":484476,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":5220815,"text":"5220815 - 1956 - Validity of mail survey data on bagged waterfowl","interactions":[],"lastModifiedDate":"2025-01-31T17:00:50.840908","indexId":"5220815","displayToPublicDate":"1956-01-02T00:00:00","publicationYear":"1956","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":2508,"text":"Journal of Wildlife Management","active":true,"publicationSubtype":{"id":10}},"title":"Validity of mail survey data on bagged waterfowl","docAbstract":"<p>No abstract available.&nbsp;</p>","language":"English","publisher":"Wiley","doi":"10.2307/3797241","usgsCitation":"Atwood, E.L., 1956, Validity of mail survey data on bagged waterfowl: Journal of Wildlife Management, v. 20, no. 1, p. 1-16, https://doi.org/10.2307/3797241.","productDescription":"16 p.","startPage":"1","endPage":"16","costCenters":[{"id":531,"text":"Patuxent Wildlife Research 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,{"id":5220592,"text":"5220592 - 1956 - Incidence of Shope's rabbit fibroma in cottontails at the Patuxent Research Refuge","interactions":[],"lastModifiedDate":"2025-01-31T16:49:48.235815","indexId":"5220592","displayToPublicDate":"1956-01-02T00:00:00","publicationYear":"1956","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":2508,"text":"Journal of Wildlife Management","active":true,"publicationSubtype":{"id":10}},"title":"Incidence of Shope's rabbit fibroma in cottontails at the Patuxent Research Refuge","docAbstract":"<p>No abstract available.&nbsp;</p>","language":"English","publisher":"Wiley","doi":"10.2307/3797254","usgsCitation":"Herman, C.M., Kilham, L., and Warbach, O., 1956, Incidence of Shope's rabbit fibroma in cottontails at the Patuxent Research Refuge: Journal of Wildlife Management, v. 20, no. 1, p. 85-89, https://doi.org/10.2307/3797254.","productDescription":"5 p.","startPage":"85","endPage":"89","costCenters":[{"id":531,"text":"Patuxent Wildlife Research Center","active":true,"usgs":true}],"links":[{"id":196003,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United States","state":"Maryland","otherGeospatial":"Patuxent Research Refuge","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"coordinates\": [\n          [\n            [\n              -76.8267394802776,\n              39.061664792964535\n            ],\n            [\n              -76.8267394802776,\n              39.00844081179906\n            ],\n            [\n              -76.74208265301516,\n              39.00844081179906\n            ],\n            [\n              -76.74208265301516,\n              39.061664792964535\n            ],\n            [\n              -76.8267394802776,\n              39.061664792964535\n            ]\n          ]\n        ],\n        \"type\": \"Polygon\"\n      }\n    }\n  ]\n}","volume":"20","issue":"1","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e49e3e4b07f02db5e539a","contributors":{"authors":[{"text":"Herman, C. M.","contributorId":101335,"corporation":false,"usgs":true,"family":"Herman","given":"C.","email":"","middleInitial":"M.","affiliations":[],"preferred":false,"id":332078,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Kilham, L.","contributorId":26394,"corporation":false,"usgs":true,"family":"Kilham","given":"L.","email":"","affiliations":[],"preferred":false,"id":332076,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Warbach, O.","contributorId":92767,"corporation":false,"usgs":true,"family":"Warbach","given":"O.","email":"","affiliations":[],"preferred":false,"id":332077,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":70048300,"text":"tem379B - 1956 - Photogeologic map, Mt. Peale-6 Quadrangle, San Juan County, Utah","interactions":[],"lastModifiedDate":"2014-02-28T14:44:50","indexId":"tem379B","displayToPublicDate":"1956-01-01T15:58:00","publicationYear":"1956","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":338,"text":"Trace Elements Memorandum","code":"TEM","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"379","chapter":"B","title":"Photogeologic map, Mt. Peale-6 Quadrangle, San Juan County, Utah","docAbstract":"No abstract available.","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/tem379B","collaboration":"Prepared in cooperation with the U.S. Atomic Energy Commission","usgsCitation":"Hackman, R., 1956, Photogeologic map, Mt. Peale-6 Quadrangle, San Juan County, Utah: U.S. Geological Survey Trace Elements Memorandum 379, Report: 4 p.; 1 Plate: 23.62 x 28.50 inches, https://doi.org/10.3133/tem379B.","productDescription":"Report: 4 p.; 1 Plate: 23.62 x 28.50 inches","numberOfPages":"4","additionalOnlineFiles":"Y","costCenters":[],"links":[{"id":277944,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/tem/0379-B/report-thumb.jpg"},{"id":283113,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/tem/0379-B/report.pdf"},{"id":283112,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/tem/0379-B/plate-1.pdf"}],"scale":"24000","country":"United States","state":"Utah","county":"San Juan County","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -109.375,38.258333 ], [ -109.375,38.375 ], [ -109.25,38.375 ], [ -109.25,38.258333 ], [ -109.375,38.258333 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"523c1cf3e4b024b60d40733f","contributors":{"authors":[{"text":"Hackman, R.H.","contributorId":78985,"corporation":false,"usgs":true,"family":"Hackman","given":"R.H.","email":"","affiliations":[],"preferred":false,"id":484265,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":71651,"text":"tei633 - 1956 - Some limitations on the possible composition of the ore-forming fluid","interactions":[],"lastModifiedDate":"2014-07-15T07:50:28","indexId":"tei633","displayToPublicDate":"1956-01-01T15:43:00","publicationYear":"1956","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":337,"text":"Trace Elements Investigations","code":"TEI","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"633","title":"Some limitations on the possible composition of the ore-forming fluid","docAbstract":"<p>The activity rations of various important anions (S, CO<sub>3</sub>, SO<sub>4</sub>, OH, F, and Cl) in hydrothermal solutions at the time of deposition are evaluated using a simple thermodynamic technique. The rations are interpreted in the light of the mineralogy of ore deposits and limites are placed on the variability of each ratio in hydrothermal solutions. All of the calculations are made for 25&deg;C and cautious extrapolation to higher temperatures seems justified; however, additional data for elevated temperatures and pressures are needed before more than approximate values may be assigned to these ratios in the ore-forming fluid.</p>\n<br>\n<p>The calculated partial pressure of CO<sub>2</sub> in the ore fluid is generally less than one atmosphere, which suggests that a dense CO<sub>2</sub> phase cannot be considered an importatn ore fluid for most deposits. The partial pressure of H<sub>2</sub>S is usually less than 10<sup>-4</sup> atmospheres which makes it extremely difficult to defend the heory that metals (other than the easily complexible mercury, arsenic, antimony, and perhaps fols and silver) are transported in quantity as complex sulfide and hydrosulfides. The sulfate to sulfide ration is such that the oxidation potential at the time of deposition is defined by the following equation: Eh (in volts) = 0.22 &plusmn; 0.04 - 0.059 pH.</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/tei633","collaboration":"This report concerns work done partly on behalf of the Division of Raw Materials of the U.S. Atomic Energy Commission","usgsCitation":"Barton, P.B., 1956, Some limitations on the possible composition of the ore-forming fluid: U.S. Geological Survey Trace Elements Investigations 633, 41 p., https://doi.org/10.3133/tei633.","productDescription":"41 p.","numberOfPages":"42","costCenters":[],"links":[{"id":290071,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":290070,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/tei/0633/report.pdf"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"53a94c80e4b0f1f8e2fa8677","contributors":{"authors":[{"text":"Barton, Paul B. Jr.","contributorId":68406,"corporation":false,"usgs":true,"family":"Barton","given":"Paul","suffix":"Jr.","email":"","middleInitial":"B.","affiliations":[],"preferred":false,"id":284543,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":71634,"text":"tei614 - 1956 - Volumetric determination of uranium using titanous sulfate as reductant before oxidimetric titration","interactions":[],"lastModifiedDate":"2014-07-15T07:02:13","indexId":"tei614","displayToPublicDate":"1956-01-01T15:16:00","publicationYear":"1956","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":337,"text":"Trace Elements Investigations","code":"TEI","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"614","title":"Volumetric determination of uranium using titanous sulfate as reductant before oxidimetric titration","docAbstract":"<p>A new method for determining uranium in samples containing 0.05 percent or more U<sub>3</sub>O<sub>8</sub>, using titanous sulfate as reducing agent, is much shorter, faster, and has fewer interferences than conventional methods using reductor columns.</p>\n<br>\n<p>The sample is dissolved with sulfuric, nitric, perchloric, and hydrofluoric acids. Elements that would otherwise form insoluble fluorides are kept in solution by complexing the fluoride ion with boric acid. A precipitation is made with cupferron to remove interfering elements. The solution is filtered to remove the precipitated cupferrates instead of extracting them with chloroform as is usually done. Filtration is preferred to extraction because any niobium that may be in solution forms an insoluble cupferrate that may be removed by filtering but is very difficult to extract with chloroform.</p>\n<br>\n<p>Excess cupferron is destroyed by oxidizing with nitric and perchloric acids, and evaporating to dense fumes of sulfuric acid. The uranium is reduced to U(IV) by the addition of titanous sulfate, with cupric sulfate used as an indicator of the completeness of the reduction. Metallic copper is formed when all the uranium is reduced. The reduced copper is then reoxidized by the addition of mercuric perchlorate, an excess of ferric sulfate added, and the solution titrated immediately with standard ceric sulfate with ferroin as an indicator.</p>\n<br>\n<p>Precision of the method compared favorable with methods in common use, both for uranium ores and for most types of uranium-rich materials.</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/tei614","collaboration":"This report concerns work done on behalf of the Division of Raw Materials of the U.S. Atomic Energy Commission","usgsCitation":"Wahlberg, J.S., Skinner, D.L., and Rader, L., 1956, Volumetric determination of uranium using titanous sulfate as reductant before oxidimetric titration: U.S. Geological Survey Trace Elements Investigations 614, 20 p., https://doi.org/10.3133/tei614.","productDescription":"20 p.","numberOfPages":"21","costCenters":[],"links":[{"id":290045,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":290044,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/tei/0614/report.pdf"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"53ae78a0e4b0abf75cf2db8c","contributors":{"authors":[{"text":"Wahlberg, James S.","contributorId":10481,"corporation":false,"usgs":true,"family":"Wahlberg","given":"James","email":"","middleInitial":"S.","affiliations":[],"preferred":false,"id":284514,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Skinner, Dwight L.","contributorId":56559,"corporation":false,"usgs":true,"family":"Skinner","given":"Dwight","email":"","middleInitial":"L.","affiliations":[],"preferred":false,"id":284515,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Rader, Lewis F.","contributorId":77238,"corporation":false,"usgs":true,"family":"Rader","given":"Lewis F.","affiliations":[],"preferred":false,"id":284516,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":70048448,"text":"tem568 - 1956 - Alteration of sandstone as a guide to uranium deposits and their origin, northern Black Hills, South Dakota","interactions":[],"lastModifiedDate":"2014-03-04T13:44:58","indexId":"tem568","displayToPublicDate":"1956-01-01T14:56:00","publicationYear":"1956","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":338,"text":"Trace Elements Memorandum","code":"TEM","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"568","title":"Alteration of sandstone as a guide to uranium deposits and their origin, northern Black Hills, South Dakota","docAbstract":"Several uranium deposits are present in the Fall River sandstone of Early Cretaceous age on the northeast flank of the Black Hills, Butte County, South Dakota.  The deposits are within a fine-grained, well-sorted, persistent basal sandstone unit that ranges in thickness from 2 to 18 feet and dips about 4&deg; NE. Detailed mapping of about 2 square miles surrounding the deposits have shown that all the uranium occurrences and most of the areas of high radioactivity are where the color changes in the basal sandstone from reddish on the up-dip side of the the occurrences to yellowish-gray or buff down-dip. Radioactivity measurements show that uranium is distributed almost continuously along the sinuous red-buff contact for more than 5 miles. Laboratory work indicates that the red color is caused by the hematite resulting from the alteration of ferrous iron minerals and hydrous ferric oxides. The close association of the red-buff contact and the uranium deposits suggest that the two were formed by the same solutions. The uranium was probably deposited originally from ground water which moved down-dip and gradually changed from an oxidizing solution near the surface to a mildly reducing solution at depth. Concentrations of uranium have resulted from the localization of reducing conditions cause perhaps by structures superimposed on the regional dip, local thinning or decrease in permeability of the sandstone, or concentrations of pyritiferous carbonaceous material. The red alteration is probably the result of pre-Oligocene weathering that has extended downward in the more permeable beds about 200 feet below the ancient erosion surface. Oxidation of the primary uranium during the present weathering cycle has resulted in the formation of carnotite and possibly other secondary uranium minerals.","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/tem568","collaboration":"This report concerns work done on behalf of the Division of Raw Materials of the U.S. Atomic Energy Commission","usgsCitation":"Vickers, R., 1956, Alteration of sandstone as a guide to uranium deposits and their origin, northern Black Hills, South Dakota: U.S. Geological Survey Trace Elements Memorandum 568, Report: 24 p.; 1 Plate: 23.97 x 19.67 inches, https://doi.org/10.3133/tem568.","productDescription":"Report: 24 p.; 1 Plate: 23.97 x 19.67 inches","numberOfPages":"27","additionalOnlineFiles":"Y","costCenters":[],"links":[{"id":278154,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/tem/0568/report-thumb.jpg"},{"id":283256,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/tem/0568/report.pdf"},{"id":283255,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/tem/0568/plate-3.pdf"}],"country":"United States","state":"South Dakota","county":"Butte County","otherGeospatial":"Black Hills","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -104.0577,45.2143 ], [ -104.0577,44.5709 ], [ -102.9576,44.5709 ], [ -102.9576,45.2143 ], [ -104.0577,45.2143 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"52455762e4b0b3d37307e16b","contributors":{"authors":[{"text":"Vickers, R.C.","contributorId":50583,"corporation":false,"usgs":true,"family":"Vickers","given":"R.C.","email":"","affiliations":[],"preferred":false,"id":484679,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":33227,"text":"b965 - 1956 - Geologic investigations in the Parícutin area, Mexico","interactions":[{"subject":{"id":56977,"text":"b965A - 1950 - Erosion studies at Paricutin, State of Michoacan, Mexico","indexId":"b965A","publicationYear":"1950","noYear":false,"chapter":"A","title":"Erosion studies at Paricutin, State of Michoacan, Mexico"},"predicate":"IS_PART_OF","object":{"id":33227,"text":"b965 - 1956 - Geologic investigations in the Parícutin area, Mexico","indexId":"b965","publicationYear":"1956","noYear":false,"title":"Geologic investigations in the Parícutin area, Mexico"},"id":1},{"subject":{"id":56978,"text":"b965B - 1950 - Volcanoes of the Paricutin region, Mexico","indexId":"b965B","publicationYear":"1950","noYear":false,"chapter":"B","title":"Volcanoes of the Paricutin region, Mexico"},"predicate":"IS_PART_OF","object":{"id":33227,"text":"b965 - 1956 - Geologic investigations in the Parícutin area, Mexico","indexId":"b965","publicationYear":"1956","noYear":false,"title":"Geologic investigations in the Parícutin area, Mexico"},"id":2},{"subject":{"id":56979,"text":"b965C - 1954 - Petrology of Paricutin volcano, Mexico","indexId":"b965C","publicationYear":"1954","noYear":false,"chapter":"C","title":"Petrology of Paricutin volcano, Mexico"},"predicate":"IS_PART_OF","object":{"id":33227,"text":"b965 - 1956 - Geologic investigations in the Parícutin area, Mexico","indexId":"b965","publicationYear":"1956","noYear":false,"title":"Geologic investigations in the Parícutin area, Mexico"},"id":3},{"subject":{"id":56980,"text":"b965D - 1956 - Birth and development of Paricutin volcano, Mexico","indexId":"b965D","publicationYear":"1956","noYear":false,"chapter":"D","title":"Birth and development of Paricutin volcano, Mexico"},"predicate":"IS_PART_OF","object":{"id":33227,"text":"b965 - 1956 - Geologic investigations in the Parícutin area, Mexico","indexId":"b965","publicationYear":"1956","noYear":false,"title":"Geologic investigations in the Parícutin area, Mexico"},"id":4}],"lastModifiedDate":"2017-08-08T13:12:34","indexId":"b965","displayToPublicDate":"1956-01-01T14:27:00","publicationYear":"1956","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":306,"text":"Bulletin","code":"B","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"965","title":"Geologic investigations in the Parícutin area, Mexico","docAbstract":"No abstract available.","language":"English","publisher":"U.S. Government Printing Office","doi":"10.3133/b965","usgsCitation":"Segerstrom, K.K., Williams, H., Wilcox, R., Foshag, W., and Gonzales, J.R., 1956, Geologic investigations in the Parícutin area, Mexico: U.S. Geological Survey Bulletin 965, vii, 489 p., https://doi.org/10.3133/b965.","productDescription":"vii, 489 p.","costCenters":[],"links":[{"id":289245,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/bul/965/report-thumb.jpg"},{"id":344656,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/bul/965/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"country":"Mexico","otherGeospatial":"Par�cutin","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -102.379059,19.408831 ], [ -102.379059,19.577126 ], [ -102.122941,19.577126 ], [ -102.122941,19.408831 ], [ -102.379059,19.408831 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"53b286ece4b07b8813a554a9","contributors":{"authors":[{"text":"Segerstrom, Kenneth K.","contributorId":105276,"corporation":false,"usgs":true,"family":"Segerstrom","given":"Kenneth","email":"","middleInitial":"K.","affiliations":[],"preferred":false,"id":210218,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Williams, H.","contributorId":51486,"corporation":false,"usgs":true,"family":"Williams","given":"H.","affiliations":[],"preferred":false,"id":210215,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Wilcox, R.E.","contributorId":107348,"corporation":false,"usgs":true,"family":"Wilcox","given":"R.E.","email":"","affiliations":[],"preferred":false,"id":210219,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Foshag, W.P.","contributorId":79163,"corporation":false,"usgs":true,"family":"Foshag","given":"W.P.","affiliations":[],"preferred":false,"id":210217,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"Gonzales, Jenaro R.","contributorId":52086,"corporation":false,"usgs":true,"family":"Gonzales","given":"Jenaro","email":"","middleInitial":"R.","affiliations":[],"preferred":false,"id":210216,"contributorType":{"id":1,"text":"Authors"},"rank":5}]}}
,{"id":70048293,"text":"tem357 - 1956 - Radiometric traverse along the Yukon River from Fort Yukon to Ruby, Alaska, 1949","interactions":[],"lastModifiedDate":"2014-03-04T13:37:08","indexId":"tem357","displayToPublicDate":"1956-01-01T14:07:00","publicationYear":"1956","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":338,"text":"Trace Elements Memorandum","code":"TEM","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"357","title":"Radiometric traverse along the Yukon River from Fort Yukon to Ruby, Alaska, 1949","docAbstract":"In 1949, a radiometric traverse was made of rocks exposed along the banks of and near the Yukon River about Fort Yukon to Ruby, Alaska.  Granitic rocks of Tertiary age and of Devonian or Carboniferous age and sandstone beds of Cretaceous age gave the highest readings obtained in the field. Other rock types examined were greenstone of Devonian or Carboniferous age and metamorphic rocks of Devonian and pre-Devonian age, sedimentary rocks, and liginite of Tertiary age, and alluvial deposits of Quaternary age.  The most radioactive sample, from Melozitna River canyon, contained only 0.017 percent equivalent uranium.","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/tem357","collaboration":"The report concerns work done on behalf of the Division of Raw Materials of the U.S. Atomic Energy Commission","usgsCitation":"White, M., Stevens, J.M., and Matzko, J., 1956, Radiometric traverse along the Yukon River from Fort Yukon to Ruby, Alaska, 1949: U.S. Geological Survey Trace Elements Memorandum 357, 14 p., https://doi.org/10.3133/tem357.","productDescription":"14 p.","numberOfPages":"17","additionalOnlineFiles":"Y","costCenters":[],"links":[{"id":277930,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/tem/0357/report-thumb.jpg"},{"id":283236,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/tem/0357/report.pdf"}],"country":"United States","state":"Alaska","otherGeospatial":"Yukon River","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -155.7095,64.6876 ], [ -155.7095,66.0817 ], [ -148.8671,66.0817 ], [ -148.8671,64.6876 ], [ -155.7095,64.6876 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"523c1cf9e4b024b60d407385","contributors":{"authors":[{"text":"White, Max G.","contributorId":22426,"corporation":false,"usgs":true,"family":"White","given":"Max G.","affiliations":[],"preferred":false,"id":484256,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Stevens, John M.","contributorId":18746,"corporation":false,"usgs":true,"family":"Stevens","given":"John","email":"","middleInitial":"M.","affiliations":[],"preferred":false,"id":484255,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Matzko, John J.","contributorId":79459,"corporation":false,"usgs":true,"family":"Matzko","given":"John J.","affiliations":[],"preferred":false,"id":484257,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
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