{"pageNumber":"6937","pageRowStart":"173400","pageSize":"25","recordCount":184769,"records":[{"id":70010475,"text":"70010475 - 1956 - Half-life of Th232 and the branching ratio of Bi212","interactions":[],"lastModifiedDate":"2020-11-27T22:17:05.297294","indexId":"70010475","displayToPublicDate":"1956-01-01T00:00:00","publicationYear":"1956","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":3060,"text":"Physical Review","active":true,"publicationSubtype":{"id":10}},"displayTitle":"Half-life of Th232 and the branching ratio of Bi212","title":"Half-life of Th232 and the branching ratio of Bi212","docAbstract":"

The half-life of Th232 has been calculated by determining an absolute gamma-disintegration rate for Tl208 in equilibrium with Th232 for three old thorium nitrate salts and one natural thorite sample. The branching ratio, α/(α+β), for Bi212, a necessary parameter in the calculation, was also measured. The half-life of Th232 was found to be 1.42×1010 years within an estimated error of 5%, which is essentially in agreement with the presently accepted value. The branching ratio, α/(α+β), of Bi212 was found to be 0.362±0.006, about 7.4% higher than the currently accepted value.

","language":"English","publisher":"American Physical Society","doi":"10.1103/PhysRev.104.1629","usgsCitation":"Senftle, F.E., Farley, T.A., and Lazar, N., 1956, Half-life of Th232 and the branching ratio of Bi212: Physical Review, v. 104, no. 6, p. 1629-1632, https://doi.org/10.1103/PhysRev.104.1629.","productDescription":"4 p.","startPage":"1629","endPage":"1632","numberOfPages":"4","costCenters":[],"links":[{"id":219144,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"104","issue":"6","noUsgsAuthors":false,"publicationDate":"1956-12-15","publicationStatus":"PW","scienceBaseUri":"505a2f5be4b0c8380cd5cd07","contributors":{"authors":[{"text":"Senftle, F. E.","contributorId":47788,"corporation":false,"usgs":true,"family":"Senftle","given":"F.","email":"","middleInitial":"E.","affiliations":[],"preferred":false,"id":359005,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Farley, T. A.","contributorId":102576,"corporation":false,"usgs":true,"family":"Farley","given":"T.","email":"","middleInitial":"A.","affiliations":[],"preferred":false,"id":359006,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Lazar, N.","contributorId":15756,"corporation":false,"usgs":true,"family":"Lazar","given":"N.","email":"","affiliations":[],"preferred":false,"id":359004,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}} ,{"id":70175983,"text":"70175983 - 1955 - Report of the Arkansas-White-Red Basins Inter-Agency Committee","interactions":[],"lastModifiedDate":"2016-08-23T10:53:51","indexId":"70175983","displayToPublicDate":"2016-08-23T00:00:00","publicationYear":"1955","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":6,"text":"USGS Unnumbered Series"},"title":"Report of the Arkansas-White-Red Basins Inter-Agency Committee","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/70175983","usgsCitation":"U.S. Geological Survey, 1955, Report of the Arkansas-White-Red Basins Inter-Agency Committee, v. 2, no. 17, 122 p. , https://doi.org/10.3133/70175983.","productDescription":"122 p. ","costCenters":[{"id":353,"text":"Kansas Water Science Center","active":false,"usgs":true}],"links":[{"id":327625,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"}],"volume":"2","issue":"17","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"57bd659ae4b03fd6b7de7270","contributors":{"authors":[{"text":"U.S. Geological Survey","contributorId":152492,"corporation":true,"usgs":false,"organization":"U.S. Geological Survey","id":646754,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":70175985,"text":"70175985 - 1955 - Ground-water resources of Osage County [Kansas]","interactions":[],"lastModifiedDate":"2016-08-23T11:07:56","indexId":"70175985","displayToPublicDate":"2016-01-11T00:00:00","publicationYear":"1955","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":2579,"text":"Kansas Geological Survey Bulletin","active":true,"publicationSubtype":{"id":10}},"title":"Ground-water resources of Osage County [Kansas]","language":"English","publisher":"University of Kansas","publisherLocation":"Lawrence, KS","usgsCitation":"O’Connor, H., 1955, Ground-water resources of Osage County [Kansas]: Kansas Geological Survey Bulletin, v. 13, no. 3, p. 28-49.","productDescription":"21 p. ","startPage":"28","endPage":"49","costCenters":[{"id":353,"text":"Kansas Water Science Center","active":false,"usgs":true}],"links":[{"id":327629,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"},{"id":327628,"rank":1,"type":{"id":15,"text":"Index Page"},"url":"https://www.kgs.ku.edu/General/geologyBulls.html","linkHelpText":"http://www.kgs.ku.edu/General/geologyBulls.html"}],"volume":"13","issue":"3","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"57bd73dde4b03fd6b7df2d12","contributors":{"authors":[{"text":"O’Connor, H.G.","contributorId":173877,"corporation":false,"usgs":false,"family":"O’Connor","given":"H.G.","email":"","affiliations":[],"preferred":false,"id":646756,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":70160577,"text":"70160577 - 1955 - A mycosis-like granuloma of fish","interactions":[],"lastModifiedDate":"2021-04-02T15:06:25.722348","indexId":"70160577","displayToPublicDate":"2015-12-23T00:00:00","publicationYear":"1955","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":2353,"text":"Journal of Infectious Diseases","active":true,"publicationSubtype":{"id":10}},"title":"A mycosis-like granuloma of fish","docAbstract":"

Mycoses of systemic distribution are rarely observed in fresh-water fish in this country. In a recent review of atypical cell growths in fishes, Nigrelli cited the only known instance of a mycetoma in a North American fresh-water fish which occurred in the head of fingerling landlocked salmon from an Idaho hatchery. The fungus associated with this granuloma was characterized by a branching septate mycelium. Rucker reported a streptomycete which was pathogenic to blueblack salmon. This organism produced internal nodules containing masses of hyphae but no inflammatory response. A pathogenic fungus has been observed frequently in marine fish, however, and in both marine and fresh-water fish in Europe. This organism was tentatively classified as a Phycomycete in or near the order Chytridiales and was assigned to the genus and species Ichthyophonus hoferi, later reclassified as Ichthyosporidium hoferi. The graduloma described in this report occurs in fresh-water trout and is apparently caused by a budding, yeast-like form with no hyphae which evokes a tremendous inflammatory reaction. Morphologically, the organism does not resemble the previously described Ichthyosporidium. The lesions were first seen accidentally in sections prepared from a diplobacillus infection of brook trout termed “kidney disease.” Subsequently, the granuloma was observed in three widely separated infections involving the diplobacillus in each instance.
The histological material was received in a fixed condition; thus, no cultural data was available and the nomenclature and classification of the mycotic organism were not attempted. The present distribution of the disease, however, with its potential threat to domestic fish populations, seemed to warrant a description and discussion of the disease. Efforts are in progress to culture the organism.

","language":"English","publisher":"University of Chicago Press","publisherLocation":"Chicago","doi":"10.1093/infdis/97.3.262","usgsCitation":"Wood, E.M., Yasutake, W.T., and Lehman, W.L., 1955, A mycosis-like granuloma of fish: Journal of Infectious Diseases, v. 97, no. 3, p. 262-267, https://doi.org/10.1093/infdis/97.3.262.","productDescription":"6 p.","startPage":"262","endPage":"267","numberOfPages":"6","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[{"id":654,"text":"Western Fisheries Research Center","active":true,"usgs":true}],"links":[{"id":312788,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United States","geographicExtents":"{\"type\":\"FeatureCollection\",\"features\":[{\"type\":\"Feature\",\"geometry\":{\"type\":\"MultiPolygon\",\"coordinates\":[[[[-66.28243,18.51476],[-65.7713,18.42668],[-65.591,18.22803],[-65.84716,17.97591],[-66.59993,17.98182],[-67.18416,17.94655],[-67.24243,18.37446],[-67.10068,18.5206],[-66.28243,18.51476]]],[[[-155.54211,19.08348],[-155.68817,18.91619],[-155.93665,19.05939],[-155.90806,19.33888],[-156.07347,19.70294],[-156.02368,19.81422],[-155.85008,19.97729],[-155.91907,20.17395],[-155.86108,20.26721],[-155.78505,20.2487],[-155.40214,20.07975],[-155.22452,19.99302],[-155.06226,19.8591],[-154.80741,19.50871],[-154.83147,19.45328],[-155.22217,19.23972],[-155.54211,19.08348]]],[[[-156.07926,20.64397],[-156.41445,20.57241],[-156.58673,20.783],[-156.70167,20.8643],[-156.71055,20.92676],[-156.61258,21.01249],[-156.25711,20.91745],[-155.99566,20.76404],[-156.07926,20.64397]]],[[[-156.75824,21.17684],[-156.78933,21.06873],[-157.32521,21.09777],[-157.25027,21.21958],[-156.75824,21.17684]]],[[[-157.65283,21.32217],[-157.70703,21.26442],[-157.7786,21.27729],[-158.12667,21.31244],[-158.2538,21.53919],[-158.29265,21.57912],[-158.0252,21.71696],[-157.94161,21.65272],[-157.65283,21.32217]]],[[[-159.34512,21.982],[-159.46372,21.88299],[-159.80051,22.06533],[-159.74877,22.1382],[-159.5962,22.23618],[-159.36569,22.21494],[-159.34512,21.982]]],[[[-94.81758,49.38905],[-94.64,48.84],[-94.32914,48.67074],[-93.63087,48.60926],[-92.61,48.45],[-91.64,48.14],[-90.83,48.27],[-89.6,48.01],[-89.27292,48.01981],[-88.37811,48.30292],[-87.43979,47.94],[-86.46199,47.55334],[-85.65236,47.22022],[-84.87608,46.90008],[-84.77924,46.6371],[-84.54375,46.53868],[-84.6049,46.4396],[-84.3367,46.40877],[-84.14212,46.51223],[-84.09185,46.27542],[-83.89077,46.11693],[-83.61613,46.11693],[-83.46955,45.99469],[-83.59285,45.81689],[-82.55092,45.34752],[-82.33776,44.44],[-82.13764,43.57109],[-82.43,42.98],[-82.9,42.43],[-83.12,42.08],[-83.142,41.97568],[-83.02981,41.8328],[-82.69009,41.67511],[-82.43928,41.67511],[-81.27775,42.20903],[-80.24745,42.3662],[-78.93936,42.86361],[-78.92,42.965],[-79.01,43.27],[-79.17167,43.46634],[-78.72028,43.62509],[-77.73789,43.62906],[-76.82003,43.62878],[-76.5,44.01846],[-76.375,44.09631],[-75.31821,44.81645],[-74.867,45.00048],[-73.34783,45.00738],[-71.50506,45.0082],[-71.405,45.255],[-71.08482,45.30524],[-70.66,45.46],[-70.305,45.915],[-69.99997,46.69307],[-69.23722,47.44778],[-68.905,47.185],[-68.23444,47.35486],[-67.79046,47.06636],[-67.79134,45.70281],[-67.13741,45.13753],[-66.96466,44.8097],[-68.03252,44.3252],[-69.06,43.98],[-70.11617,43.68405],[-70.64548,43.09024],[-70.81489,42.8653],[-70.825,42.335],[-70.495,41.805],[-70.08,41.78],[-70.185,42.145],[-69.88497,41.92283],[-69.96503,41.63717],[-70.64,41.475],[-71.12039,41.49445],[-71.86,41.32],[-72.295,41.27],[-72.87643,41.22065],[-73.71,40.9311],[-72.24126,41.11948],[-71.945,40.93],[-73.345,40.63],[-73.982,40.628],[-73.95232,40.75075],[-74.25671,40.47351],[-73.96244,40.42763],[-74.17838,39.70926],[-74.90604,38.93954],[-74.98041,39.1964],[-75.20002,39.24845],[-75.52805,39.4985],[-75.32,38.96],[-75.07183,38.78203],[-75.05673,38.40412],[-75.37747,38.01551],[-75.94023,37.21689],[-76.03127,37.2566],[-75.72205,37.93705],[-76.23287,38.31921],[-76.35,39.15],[-76.54272,38.71762],[-76.32933,38.08326],[-76.99,38.23999],[-76.30162,37.91794],[-76.25874,36.9664],[-75.9718,36.89726],[-75.86804,36.55125],[-75.72749,35.55074],[-76.36318,34.80854],[-77.39763,34.51201],[-78.05496,33.92547],[-78.55435,33.86133],[-79.06067,33.49395],[-79.20357,33.15839],[-80.30132,32.50935],[-80.86498,32.0333],[-81.33629,31.44049],[-81.49042,30.72999],[-81.31371,30.03552],[-80.98,29.18],[-80.53558,28.47213],[-80.53,28.04],[-80.05654,26.88],[-80.08801,26.20576],[-80.13156,25.81677],[-80.38103,25.20616],[-80.68,25.08],[-81.17213,25.20126],[-81.33,25.64],[-81.71,25.87],[-82.24,26.73],[-82.70515,27.49504],[-82.85526,27.88624],[-82.65,28.55],[-82.93,29.1],[-83.70959,29.93656],[-84.1,30.09],[-85.10882,29.63615],[-85.28784,29.68612],[-85.7731,30.15261],[-86.4,30.4],[-87.53036,30.27433],[-88.41782,30.3849],[-89.18049,30.31598],[-89.59383,30.15999],[-89.41373,29.89419],[-89.43,29.48864],[-89.21767,29.29108],[-89.40823,29.15961],[-89.77928,29.30714],[-90.15463,29.11743],[-90.88022,29.14854],[-91.62678,29.677],[-92.49906,29.5523],[-93.22637,29.78375],[-93.84842,29.71363],[-94.69,29.48],[-95.60026,28.73863],[-96.59404,28.30748],[-97.14,27.83],[-97.37,27.38],[-97.38,26.69],[-97.33,26.21],[-97.14,25.87],[-97.53,25.84],[-98.24,26.06],[-99.02,26.37],[-99.3,26.84],[-99.52,27.54],[-100.11,28.11],[-100.45584,28.69612],[-100.9576,29.38071],[-101.6624,29.7793],[-102.48,29.76],[-103.11,28.97],[-103.94,29.27],[-104.45697,29.57196],[-104.70575,30.12173],[-105.03737,30.64402],[-105.63159,31.08383],[-106.1429,31.39995],[-106.50759,31.75452],[-108.24,31.75485],[-108.24194,31.34222],[-109.035,31.34194],[-111.02361,31.33472],[-113.30498,32.03914],[-114.815,32.52528],[-114.72139,32.72083],[-115.99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States\"}}]}","volume":"97","issue":"3","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"567bc5a7e4b0a04ef491a1c8","contributors":{"authors":[{"text":"Wood, E. M.","contributorId":68685,"corporation":false,"usgs":true,"family":"Wood","given":"E.","email":"","middleInitial":"M.","affiliations":[],"preferred":false,"id":583178,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Yasutake, W. T.","contributorId":103222,"corporation":false,"usgs":true,"family":"Yasutake","given":"W.","email":"","middleInitial":"T.","affiliations":[],"preferred":false,"id":583179,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Lehman, W. L.","contributorId":150829,"corporation":false,"usgs":false,"family":"Lehman","given":"W.","email":"","middleInitial":"L.","affiliations":[],"preferred":false,"id":583180,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}} ,{"id":70160580,"text":"70160580 - 1955 - Histopathology of fish: I. Techniques and principles","interactions":[],"lastModifiedDate":"2021-03-25T21:26:19.06826","indexId":"70160580","displayToPublicDate":"2015-12-23T00:00:00","publicationYear":"1955","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":3196,"text":"Progressive Fish-Culturist","active":true,"publicationSubtype":{"id":10}},"title":"Histopathology of fish: I. Techniques and principles","docAbstract":"

The techniques of histopathology have been used for many years in the study of human and animal diseases. Until very recent times, however, histology has been applied to fish studies only very infrequently. This brief discussion is intended to acquaint the reader with the techniques and principles involved and to explain how histological studies may help to overcome fish diseases and nutritional problems.

","language":"English","publisher":"Department of Commerce, Bureau of Fisheries","publisherLocation":"Washington D.C.","doi":"10.1577/1548-8659(1955)17[166:HOF]2.0.CO;2","usgsCitation":"Wood, E.M., and Yasutake, W.T., 1955, Histopathology of fish: I. Techniques and principles: Progressive Fish-Culturist, v. 17, no. 4, p. 166-171, https://doi.org/10.1577/1548-8659(1955)17[166:HOF]2.0.CO;2.","productDescription":"6 p.","startPage":"166","endPage":"171","numberOfPages":"6","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[{"id":654,"text":"Western Fisheries Research Center","active":true,"usgs":true}],"links":[{"id":312792,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"17","issue":"4","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"567bc5abe4b0a04ef491a1d2","contributors":{"authors":[{"text":"Wood, E. M.","contributorId":68685,"corporation":false,"usgs":true,"family":"Wood","given":"E.","email":"","middleInitial":"M.","affiliations":[],"preferred":false,"id":583258,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Yasutake, W. T.","contributorId":103222,"corporation":false,"usgs":true,"family":"Yasutake","given":"W.","email":"","middleInitial":"T.","affiliations":[],"preferred":false,"id":583259,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":70175986,"text":"70175986 - 1955 - Geology and ground-water resources of Jewell County, Kansas","interactions":[],"lastModifiedDate":"2016-08-23T11:11:48","indexId":"70175986","displayToPublicDate":"2015-11-24T00:00:00","publicationYear":"1955","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":2579,"text":"Kansas Geological Survey Bulletin","active":true,"publicationSubtype":{"id":10}},"title":"Geology and ground-water resources of Jewell County, Kansas","language":"English","publisher":"University of Kansas","publisherLocation":"Lawrence, KS","usgsCitation":"Fishel, V., and Leonard, A., 1955, Geology and ground-water resources of Jewell County, Kansas: Kansas Geological Survey Bulletin, v. 115, 152 p.","productDescription":"152 p.","costCenters":[{"id":353,"text":"Kansas Water Science Center","active":false,"usgs":true}],"links":[{"id":327633,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"},{"id":327632,"rank":1,"type":{"id":15,"text":"Index Page"},"url":"https://www.kgs.ku.edu/General/geologyBulls.html"}],"volume":"115","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"57bd73dae4b03fd6b7df2cd5","contributors":{"authors":[{"text":"Fishel, V.C.","contributorId":6126,"corporation":false,"usgs":true,"family":"Fishel","given":"V.C.","email":"","affiliations":[],"preferred":false,"id":646757,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Leonard, A.R.","contributorId":101669,"corporation":false,"usgs":true,"family":"Leonard","given":"A.R.","email":"","affiliations":[],"preferred":false,"id":646758,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":70175984,"text":"70175984 - 1955 - Geology and ground-water resources of Graham County, Kansas","interactions":[],"lastModifiedDate":"2016-08-23T11:09:17","indexId":"70175984","displayToPublicDate":"2015-11-16T00:00:00","publicationYear":"1955","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":2579,"text":"Kansas Geological Survey Bulletin","active":true,"publicationSubtype":{"id":10}},"title":"Geology and ground-water resources of Graham County, Kansas","language":"English","publisher":"University of Kansas","publisherLocation":"Lawrence, KS","usgsCitation":"Prescott, G., 1955, Geology and ground-water resources of Graham County, Kansas: Kansas Geological Survey Bulletin, v. 110, 98 p.","productDescription":"98 p.","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[{"id":353,"text":"Kansas Water Science Center","active":false,"usgs":true}],"links":[{"id":327627,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"},{"id":327631,"type":{"id":15,"text":"Index Page"},"url":"https://www.kgs.ku.edu/General/geologyBulls.html"}],"volume":"110","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"57bd73dae4b03fd6b7df2ccf","contributors":{"authors":[{"text":"Prescott, G.C. Jr.","contributorId":103352,"corporation":false,"usgs":true,"family":"Prescott","given":"G.C.","suffix":"Jr.","email":"","affiliations":[],"preferred":false,"id":646755,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":70159020,"text":"tei570 - 1955 - Stratigraphic sections of the Phosphoria formation 1953 and 1954","interactions":[],"lastModifiedDate":"2015-10-22T11:31:26","indexId":"tei570","displayToPublicDate":"2015-06-08T05:15:00","publicationYear":"1955","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":"570","title":"Stratigraphic sections of the Phosphoria formation 1953 and 1954","docAbstract":"

Since 1947, the U.S. Geological Survey has measured and sampled phosphatic parts of the Permian Phosphoria formation and its partial stratigraphic correlatives at many localities in Montana, Idaho, Wyoming, and Utah.  Preliminary data on the thickness of the beds and their composition at localities sampled prior to 1952 have been issued already in TEI-183, 184, 185, 186, 187, 188, 360, 361, 362, 363, 364, 365, 375, 376, 377, and 378. This report presents similar data on the localitites sampled in 1953 and 1954 (figs. 1, 2, and 3).  The field and laboratory procedures adopted in these investigations are described in a previous report (McKelvey and others 1953a).

","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/tei570","usgsCitation":"Swanson, R.W., Carswell, L., Sheldon, R., and Cheney, T.M., 1955, Stratigraphic sections of the Phosphoria formation 1953 and 1954: U.S. Geological Survey Trace Elements Investigations 570, 39 p., https://doi.org/10.3133/tei570.","productDescription":"39 p.","numberOfPages":"40","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[],"links":[{"id":309851,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/tei570.jpg"},{"id":310437,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/tei/570/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"country":"United States","state":"Colorado, Idaho, Montana, Utah, 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\"}}]}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"561e2b39e4b0cdb063e59cf1","contributors":{"authors":[{"text":"Swanson, R. W.","contributorId":7711,"corporation":false,"usgs":true,"family":"Swanson","given":"R.","email":"","middleInitial":"W.","affiliations":[],"preferred":false,"id":577271,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Carswell, L.D.","contributorId":6435,"corporation":false,"usgs":true,"family":"Carswell","given":"L.D.","email":"","affiliations":[],"preferred":false,"id":577272,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Sheldon, R.P.","contributorId":71158,"corporation":false,"usgs":true,"family":"Sheldon","given":"R.P.","email":"","affiliations":[],"preferred":false,"id":577273,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Cheney, T. M.","contributorId":13606,"corporation":false,"usgs":true,"family":"Cheney","given":"T.","email":"","middleInitial":"M.","affiliations":[],"preferred":false,"id":577274,"contributorType":{"id":1,"text":"Authors"},"rank":4}]}} ,{"id":70158927,"text":"tei226 - 1955 - Geology and beryl deposits of the Peerless pegmatite, Pennington County, South Dakota","interactions":[],"lastModifiedDate":"2015-10-20T12:35:16","indexId":"tei226","displayToPublicDate":"2015-05-02T00:00:00","publicationYear":"1955","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":"226","title":"Geology and beryl deposits of the Peerless pegmatite, Pennington County, South Dakota","docAbstract":"

The Peerless pegmatite, half a mile south of Keystone, Pennington County, S. Dak., has been a large source of scrap mica and beryl. Feldspar, amblygonite, tantalite-columbite, and cassiterite also have been recovered.

\n

The pegmatite is intrusive into Precambrian quartz-mica schist. Much of the schist contains staurolite and chlorite. Staurolite has been partly altered to mica, quartz, and chlorite, especially near pegmatite contacts. The pegmatite is generally discordant with the schist, but in many places secondary schistosity has been developed parallel to the contact. Tourmaline and muscovite, presumably introduced by pegmatitic solutions, are characteristic of the wall rock near discordant contacts.

\n

At the surface the pegmatite is tadpole-shaped and is 580 feet long and 360 feet wide. In cross-section the pegmatite has an anticlinal form that suggests control of the intrusion by fractures bearing N. 30°W. and dipping 45°NE. and SW. Dike-like apophyses extending from the main pegmatite have various attitudes.

\n

The Peerless pegmatite is a complex pegmatite consisting of seven zones, two replacement units, and two types of fracture-fillings. These are: Zone 1, quartz-muscovite-plagioclase pegmatite (border zone); Zone 2, albite-quartz-muscovite pegmatite (wall zone); Zone 3, cleavelandite-quartz-muscovite pegmatite (first intermediate zone); Zone 4, perthite-cleavelandite-quartz pegmatite (second intermediate zone); Zone 5, clevelandite-quartz pegmatite (third intermediate zone); Zones 6a and b, quartz-microcline pegmatite and quartz pegmatite (fourth intermediate zone); Zone 7, lithia mica-cleavelandite pegmatite (core); lithia mica-cleavelandite-quartz replacement unit; muscovite-cleavelandite replacement unit; quartz fracture-fillings; and tourmaline-quartz fracture-fillings.

\n

Zones 1 and 2 consist of alternating layers of different texture and mineralogy that are parallel to the contact.  The layers contain differing proportions of quartz, plagioclase, muscovite, perthite, and accessory minerals. Sugary albite-quartz aggregates are important constituents of some layers. Layers of similar composition may occur two, three, or perhaps more times. The overall mineralogic composition of Zones 1 and 2 is similar to the composition of wall zones in many other Black Hills pegmatite, Zones 3 to 7 are in the normal sequence of zones in Black Hills pegmatites.

\n

The structural, textural, and mineralogic data confirm previously published evidence from other Black Hills pegmatites that indicates crystallization of a magma-like fluid from the wall inward. Repetition of layers in Zones 1 and 2 indicates changes in composition of the fluid at the crystallizing face. These changes may have been caused by addition of new material from below, by loss of material to the wall rocks, or by failure of convection to maintain equilibrium throughout the fluid in the pegmatite chamber.  Zone 3 to 7 are in the normal sequence of zoned pegmatites that indicates crystallization from a restricted or nearly closed system. The lithia mica-cleavelandite replacement unit, which extends outward from the core, shows that in, the very late stages of crystallization a pneumatolytic or hydrothermal fluid escaped outward and replaced previously crystallized pegmatite.

\n

Accessory minerals of the pegmatite include tourmaline, beryl, apatite, amblygonite (variety, montebrasite), lithia mica, cassiterite, tantalite-columbite, garnet, spodumene, svanbergite, loellingite (?), vivianite (?), triploidite (?), dahllite, and vari-colored phosphate minerals of the lithiophilitetriphylite group and their alteration products.

\n

The chemical composition of the pegmatite has been determined by estimating the mineral, constitution of the various units and by calculating the tonnage of these units by use of successive geologic sections.  The principal constituents are: SiO2 (77.0 percent), Al2O3 (13.7 percent), Na2O (5.0 percent), and K2O (1.7 percent).

\n

Chemical composition has also been determined for four subdivisions of the pegmatite: (A) Zones 1 and 2, (B) Zones 3 and 4, (C) Zone 5, and (D) Zones 6 and 7 and the replacement units. The content of Si02 increases and the content of Al2O3 decreases from the outer pan of the pegmatite inward. Na2O forms only 0.4 percent of the inner subdivision (D), but 4 .7 to 6.5 percent of the other subdivisions.  K2O forms 4.0 percent of subdivision (B), but only 0.7 to 1.3 percent of the other subdivisions.

\n

Zone 3, the principal minable unit, contains 1. 7 percent beryl and 28 percent scrap mica. Beryl also constitutes more than 1 percent of parts of the wall zone, especially albite-rich layers of the inner part of the unit in the upper part of the pegmatite. Beryl is a less important constituent of other units of the pegmatite.

\n

Potash feldspar is mined chiefly from Zone 4.  Clevelandite that can be hand-cobbed and sold as soda-feldspar occurs in Zones 3, 4, and 5. Amblygomlte forms between 0.5 and 1.0 percent of Zone 5.

\n

Reserves of beryl, scrap mica, potash feldspar, and amblygonite are one to six times past production.

\n

 

","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Washington, D.C.","doi":"10.3133/tei226","collaboration":"This report concerns work done on behalf of the Division of Raw Materials of the U.S. Atomic Energy Commission.","usgsCitation":"Sheridan, D.M., Stephens, H.G., Staatz, M.H., and Norton, J., 1955, Geology and beryl deposits of the Peerless pegmatite, Pennington County, South Dakota: U.S. Geological Survey Trace Elements Investigations 226, Report: 145 p.; 5 Plates: 46.49 x 35.93 inches or smaller, https://doi.org/10.3133/tei226.","productDescription":"Report: 145 p.; 5 Plates: 46.49 x 35.93 inches or smaller","numberOfPages":"181","onlineOnly":"N","additionalOnlineFiles":"Y","costCenters":[],"links":[{"id":309729,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/tei226.jpg"},{"id":310143,"rank":3,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/tei/226/figure-2.pdf","text":"Figure 2","size":"10.17 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Douglas M.","contributorId":13966,"corporation":false,"usgs":true,"family":"Sheridan","given":"Douglas","email":"","middleInitial":"M.","affiliations":[],"preferred":false,"id":576890,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Stephens, Hal G.","contributorId":51785,"corporation":false,"usgs":true,"family":"Stephens","given":"Hal","email":"","middleInitial":"G.","affiliations":[],"preferred":false,"id":576891,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Staatz, Mortimer H.","contributorId":55494,"corporation":false,"usgs":true,"family":"Staatz","given":"Mortimer","email":"","middleInitial":"H.","affiliations":[],"preferred":false,"id":576892,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Norton, James J.","contributorId":6127,"corporation":false,"usgs":true,"family":"Norton","given":"James J.","affiliations":[],"preferred":false,"id":576893,"contributorType":{"id":1,"text":"Authors"},"rank":4}]}} ,{"id":70157478,"text":"70157478 - 1955 - Some effects of preciptiation on ground water in Wisconsin","interactions":[],"lastModifiedDate":"2018-01-08T19:52:04","indexId":"70157478","displayToPublicDate":"2015-04-06T08:00:00","publicationYear":"1955","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":2,"text":"State or Local Government Series"},"seriesTitle":{"id":5596,"text":"Wisconsin Geological & Natural History Survey Information Circular","active":true,"publicationSubtype":{"id":2}},"seriesNumber":"1","title":"Some effects of preciptiation on ground water in Wisconsin","docAbstract":"

The importance of our water supplies has become increasingly apparent to most of us in recent years. The importance of water was forcefully dramatized by the water shortage in New York City in 1950. In nearly every State in the Union, one or more communities now has or has had a water problem whose effect on the citizens has been no less to them as was the one in New York City to New Yorkers. The increasing numbers of these problems have led to widespread speculation as to the adequacy of the Nation' s water supplies.

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