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An appraisal of asphalt-bearing rocks as potential sources of uranium was made during 1953 and 1954 by examining deposits in 45 areas in California, Utah, Wyoming, Montana, New Mexico, Texas, Oklahoma, and Missouri.  A total of 202 samples from these areas was analyzed for uranium. The oldest rocks sampled are Ordovician in age, and the youngest are Recent. Although none of the deposits are of value at this time as a source of uranium, some of the deposits may constitute a low grade uranium resource whose recovery will depend upon the primary use to which the asphalt is placed.

\n

Significant amounts of uranium in the ash of the extracted oil were found in samples from 7 of the 45 areas examined. These areas are Chalone Creek, McKittrick, Edna, and Los Alamos areas, California: Vernal area, Utah; Sulphur area, Oklahoma; and the Ellis area, Missouri. The average uranium content of samples from these seven areas ranges: from 0.028 to 0.376 percent in the ash of the extracted oil.  All except the Chalone Creek area contain large estimated reserves of asphalt-bearing rock, ranging from 15,000,000 to almost 2,000,000,000 tons.  The average uranium content of samples from 13 additional areas ranges from 0.020 to 0.068 percent in the ash of the extracted oil.  Many of these areas contain very large reserves of asphalt-bearing rocks.

\n

Evaluation of field data indicates that naturally occurring asphalts with a relatively high uranium content probably originated in, or migrated through, rocks that contain more than average amounts of uranium. It is believed that some of the uranium was present as an original constituent of the oil but that some uranium may have been introduced during migration of the oil.

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In southwestern Colorado and southeastern Utah strata of conglomeratic sandstone are localized at the base of the Brush Basin shale member of the Morrison formation of Jurassic age. These strata are discrete lithologic units that contain sedimentary structures oriented in a prevailing easterly direction, they locally rest upon sandstone in the Salt Wash that is ore bearing, and they are believed to cover about one-third of the underlying Salt Wash sandstone member in southwestern Colorado and southeastern Utah. Easterly trending planar cross-stratification and trough cross-stratification-type bedding and a general westward coarsening of sediments in the strata suggest they are the products of stream aggradation from westerly source areas.

\n

Uranium-vanadium deposits in the uppermost, almost continuous, layer of sandstone of the Salt Wash member have been classified according to their association with the conglomerate strata. Of the 364 deposits that have been studied in the uppermost sandstone layer of the Salt Wash, 29 percent of the total are directly below a conglomeratic sandstone stratum, 61 percent are below their projected trend, 6 percent are beyond the safe limits of projection, and 4 percent are lateral to their margins. Locally, a conglomeratic sandstone stratum may be mineralized.  Where this happens, it is usually near clusters of deposits in the uppermost sandstone of the underlying Salt Wash member. 

\n

Late Jurassic Morrison ground-water conditions can be postulated to localize uranium-vanadium rich ground water below the conglomerate strata.

\n

 

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Jr.","contributorId":51370,"corporation":false,"usgs":true,"family":"Wilson","given":"H.D.","suffix":"Jr.","email":"","affiliations":[],"preferred":false,"id":257625,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":16284,"text":"ofr55182 - 1955 - Surficial geology of an area adjoining the edge of the Matanuska Valley, Alaska","interactions":[{"subject":{"id":16284,"text":"ofr55182 - 1955 - Surficial geology of an area adjoining the edge of the Matanuska Valley, Alaska","indexId":"ofr55182","publicationYear":"1955","noYear":false,"title":"Surficial geology of an area adjoining the edge of the Matanuska Valley, Alaska"},"predicate":"SUPERSEDED_BY","object":{"id":2832,"text":"wsp1494 - 1960 - Geology and ground-water resources of the Matanuska Valley agricultural area, Alaska","indexId":"wsp1494","publicationYear":"1960","noYear":false,"title":"Geology and ground-water resources of the Matanuska Valley agricultural area, Alaska"},"id":1}],"supersededBy":{"id":2832,"text":"wsp1494 - 1960 - Geology and ground-water resources of the Matanuska Valley agricultural area, Alaska","indexId":"wsp1494","publicationYear":"1960","noYear":false,"title":"Geology and ground-water resources of the Matanuska Valley agricultural area, Alaska"},"lastModifiedDate":"2012-02-02T00:07:17","indexId":"ofr55182","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1955","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":330,"text":"Open-File Report","code":"OFR","onlineIssn":"2331-1258","printIssn":"0196-1497","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"55-182","title":"Surficial geology of an area adjoining the edge of the Matanuska Valley, Alaska","language":"ENGLISH","publisher":"U.S. Geological Survey],","doi":"10.3133/ofr55182","usgsCitation":"Trainer, F.W., 1955, Surficial geology of an area adjoining the edge of the Matanuska Valley, Alaska: U.S. Geological Survey Open-File Report 55-182, 6 p, https://doi.org/10.3133/ofr55182.","productDescription":"6 p","costCenters":[],"links":[{"id":111234,"rank":100,"type":{"id":15,"text":"Index Page"},"url":"https://www.dggs.dnr.state.ak.us/pubs/id/10582","linkFileType":{"id":5,"text":"html"}},{"id":150504,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ae2e4b07f02db688baa","contributors":{"authors":[{"text":"Trainer, Frank W.","contributorId":103655,"corporation":false,"usgs":true,"family":"Trainer","given":"Frank","email":"","middleInitial":"W.","affiliations":[],"preferred":false,"id":172549,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":71595,"text":"tei571 - 1955 - The thoron-tartaric acid systems for the spectrophotometric determination of thorium","interactions":[],"lastModifiedDate":"2015-10-20T13:14:20","indexId":"tei571","displayToPublicDate":"1994-01-01T00:00:00","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":"571","title":"The thoron-tartaric acid systems for the spectrophotometric determination of thorium","docAbstract":"

Thoron is popularly used for the spectrophotometric determination of thorium.  An undesirable feature of its use is the high sensitivity of the reagent toward zirconium. This study describes the use of tartaric acid as a masking reagent for zirconium. Three tartaric acid-thoron systems, developed for the determination of thorium, differ with respect to the concentrations of thoron and tartaric acid. Mesotataric acid, used in one of the systems, is found to be most effective in masking zirconium. The behavior of various rarer elements, usually found associated with thorium ores, is determined in two of the systems, and a dilution method is described for the direct determination of thorium in monazite concentrates.

","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Washington D.C.","doi":"10.3133/tei571","usgsCitation":"Grimaldi, F.S., and Fletcher, M., 1955, The thoron-tartaric acid systems for the spectrophotometric determination of thorium: U.S. Geological Survey Trace Elements Investigations 571, 25 p., https://doi.org/10.3133/tei571.","productDescription":"25 p.","numberOfPages":"26","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[],"links":[{"id":193054,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/tei/571/report-thumb.jpg"},{"id":90865,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/tei/571/report.pdf","text":"Report","size":"7.00 MB","linkFileType":{"id":1,"text":"pdf"},"description":"Report"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a60e4b07f02db634ce9","contributors":{"authors":[{"text":"Grimaldi, F. S.","contributorId":94286,"corporation":false,"usgs":true,"family":"Grimaldi","given":"F.","email":"","middleInitial":"S.","affiliations":[],"preferred":false,"id":284445,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Fletcher, Mary H.","contributorId":52954,"corporation":false,"usgs":true,"family":"Fletcher","given":"Mary H.","affiliations":[],"preferred":false,"id":284444,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":71593,"text":"tei569 - 1955 - Some physical properties of naturally irradiated fluorite","interactions":[],"lastModifiedDate":"2015-10-07T14:28:53","indexId":"tei569","displayToPublicDate":"1994-01-01T00:00:00","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":"569","title":"Some physical properties of naturally irradiated fluorite","docAbstract":"

Five samples of purple fluorite found in association with radioactive, materials, and a synthetic colorless control sample were studied and compared.  Before and after heating, observations were made on specific gravity, index of refraction, unit-cell size, breadth of X-ray diffraction lines, and fluorescence.  The purple samples became colorless on heating above 175° C.  During the process, observations were made on color, thermoluminescence, and differential thermal analysis curves.  There were strong correlations between the various physical properties, and it was found possible to arrange the samples in order of increasing difference in their physical properties from the control sample. This order apparently represents increasing structural damage by radiation; if so, it correlates with decreasing specific gravity, increasing index of refraction, broadening of X-ray lines, and increasingly strong exothermic reactions on annealing. The differences between the samples in index of refraction and X-ray pattern are largely eliminated on annealing.  Annealing begins at 1750 C; thermoluminescence at lower temperatures is due to electrons escaping from the metastable potential traps, not the destruction of those traps which takes place on annealing.

","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/tei569","usgsCitation":"Berman, R., 1955, Some physical properties of naturally irradiated fluorite: U.S. Geological Survey Trace Elements Investigations 569, 24 p., https://doi.org/10.3133/tei569.","productDescription":"24 p.","numberOfPages":"25","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[],"links":[{"id":90864,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/tei/569/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":186568,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/tei/569/report-thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e49e8e4b07f02db5e8763","contributors":{"authors":[{"text":"Berman, Robert","contributorId":13315,"corporation":false,"usgs":true,"family":"Berman","given":"Robert","affiliations":[],"preferred":false,"id":284443,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":71557,"text":"tei531 - 1955 - Selected annotated bibliography and index map of thorium and rare-earth deposits in the United States and Alaska","interactions":[],"lastModifiedDate":"2012-02-02T00:13:44","indexId":"tei531","displayToPublicDate":"1994-01-01T00:00:00","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":"531","title":"Selected annotated bibliography and index map of thorium and rare-earth deposits in the United States and Alaska","language":"ENGLISH","doi":"10.3133/tei531","usgsCitation":"Buck, K.L., 1955, Selected annotated bibliography and index map of thorium and rare-earth deposits in the United States and Alaska: U.S. Geological Survey Trace Elements Investigations 531, 42 p., 2 fig., https://doi.org/10.3133/tei531.","productDescription":"42 p., 2 fig.","costCenters":[],"links":[{"id":185986,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/tei/531/report-thumb.jpg"},{"id":90832,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/tei/531/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"scale":"100000","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a09e4b07f02db5fa77b","contributors":{"authors":[{"text":"Buck, Katharine L.","contributorId":55059,"corporation":false,"usgs":true,"family":"Buck","given":"Katharine","email":"","middleInitial":"L.","affiliations":[],"preferred":false,"id":284388,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":35637,"text":"b1024A - 1955 - Radioactivity investigations in the Cache Creek area, Yentna district, Alaska, 1945","interactions":[],"lastModifiedDate":"2012-02-02T00:09:42","indexId":"b1024A","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1955","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":"1024","chapter":"A","title":"Radioactivity investigations in the Cache Creek area, Yentna district, Alaska, 1945","language":"ENGLISH","publisher":"U.S. Govt. Print. Off.,","doi":"10.3133/b1024A","usgsCitation":"Robinson, G.D., Wedow, H., and Lyons, J.B., 1955, Radioactivity investigations in the Cache Creek area, Yentna district, Alaska, 1945: U.S. Geological Survey Bulletin 1024, p. 1-23, ill., maps (part fold. in pocket) ;24 cm., https://doi.org/10.3133/b1024A.","productDescription":"p. 1-23, ill., maps (part fold. in pocket) ;24 cm.","costCenters":[],"links":[{"id":109154,"rank":700,"type":{"id":15,"text":"Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_20567.htm","linkFileType":{"id":5,"text":"html"},"description":"20567"},{"id":166721,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/bul/1024a/report-thumb.jpg"},{"id":63524,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/bul/1024a/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":63525,"rank":401,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/bul/1024a/plate-2.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":63526,"rank":402,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/bul/1024a/plate-3.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":63527,"rank":403,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/bul/1024a/plate-4.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":63528,"rank":404,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/bul/1024a/plate-5.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":63529,"rank":405,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/bul/1024a/plate-6.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":63530,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/bul/1024a/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a80e4b07f02db649d07","contributors":{"authors":[{"text":"Robinson, G. D.","contributorId":96669,"corporation":false,"usgs":true,"family":"Robinson","given":"G.","email":"","middleInitial":"D.","affiliations":[],"preferred":false,"id":214988,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Wedow, Helmuth","contributorId":67495,"corporation":false,"usgs":true,"family":"Wedow","given":"Helmuth","affiliations":[],"preferred":false,"id":214986,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Lyons, John B.","contributorId":68801,"corporation":false,"usgs":true,"family":"Lyons","given":"John","email":"","middleInitial":"B.","affiliations":[],"preferred":false,"id":214987,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}} ,{"id":71552,"text":"tei526 - 1955 - Selected annotated bibliography of the geology of sandstone-type uranium deposits in the United States","interactions":[],"lastModifiedDate":"2012-02-02T00:13:44","indexId":"tei526","displayToPublicDate":"1994-01-01T00:00:00","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":"526","title":"Selected annotated bibliography of the geology of sandstone-type uranium deposits in the United States","language":"ENGLISH","doi":"10.3133/tei526","usgsCitation":"Melin, R.E., 1955, Selected annotated bibliography of the geology of sandstone-type uranium deposits in the United States: U.S. Geological Survey Trace Elements Investigations 526, 393 p. [no page 2]; 4 indices; 1 plate, https://doi.org/10.3133/tei526.","productDescription":"393 p. [no page 2]; 4 indices; 1 plate","costCenters":[],"links":[{"id":185982,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/tei/526/report-thumb.jpg"},{"id":90828,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/tei/526/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"scale":"100000","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a09e4b07f02db5fa756","contributors":{"authors":[{"text":"Melin, Robert E.","contributorId":23198,"corporation":false,"usgs":true,"family":"Melin","given":"Robert","email":"","middleInitial":"E.","affiliations":[],"preferred":false,"id":284374,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":71550,"text":"tei524 - 1955 - Stratigraphy of the area between Hernando and Hardee counties, Florida","interactions":[],"lastModifiedDate":"2014-05-23T16:03:41","indexId":"tei524","displayToPublicDate":"1994-01-01T00:00:00","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":"524","title":"Stratigraphy of the area between Hernando and Hardee counties, Florida","docAbstract":"

Eocene, Oligocene, Miocene, and Recent rocks are exposed between Hernando and Hardee Counties. Eocene and Oligocene formations are fossiliferous limestones but Miocene rocks are largely unconsolidated\nsands and clays in which fossils are scarce. Correlation of Miocene strata therefore is necessarily based\nmainly on lithology and stratigraphic position. Where rocks are altered by weathering, correlation is based\non original rather than present gross Tithelogy. Quartz sand was found to be valuable in correlation because\nit is not affected by weathering.

\n
\n

Rocks in the report area previously mapped as the upper Miocene or lower Pliocene Alachua and Bone\nValley formations .were found to range from lower to middle Miocene and are assigned to the Tampa and\nHawthorn formations. The Citronelle formation of Pliocene or later age apparently does not extend into\npeninsular Florida, Clayey sand that has been considered as Citromelle equivalent in the report area is\nlate middle Miocene or early upper Miocene in age.

\n
\n

Hardrock phosphate deposits in the area are in lower Miocene beds which are assigned to the Tampa\nLimestone. Hardrock phosphate particles appear to consist of two types: cementation concretions and\nlimestone replacements.

\n
\n

Land-pebble phosphate deposits range in age from middle Miocene to Pleistocene. In the area of\nthis report they are mainly residual deposits of middle Miocene age.

\n
\n

In the report area uranium is confined mainly to lower and middle Miocene rocks with the greatest\nconcentrations in the Hawthorn formation.

","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/tei524","collaboration":"This report concerns work done on behalf of the Division of Raw Materials of the U.S. Atomic Energy Commission","usgsCitation":"Ketner, K.B., and McGreevy, L., 1955, Stratigraphy of the area between Hernando and Hardee counties, Florida: U.S. Geological Survey Trace Elements Investigations 524, Report: 114 p.; 3 Plates: 51.89 x 30.21 inches and smaller, https://doi.org/10.3133/tei524.","productDescription":"Report: 114 p.; 3 Plates: 51.89 x 30.21 inches and smaller","numberOfPages":"121","costCenters":[],"links":[{"id":185981,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/tei/524/report-thumb.jpg"},{"id":90827,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/tei/524/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":285957,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/tei/0524/plate-1.pdf"},{"id":285958,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/tei/0524/plate-2.pdf"},{"id":285959,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/tei/0524/plate-3.pdf"}],"country":"United States","state":"Florida","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -83.5997,26.9805 ], [ -83.5997,30.0639 ], [ -80.0768,30.0639 ], [ -80.0768,26.9805 ], [ -83.5997,26.9805 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b16e4b07f02db6a5576","contributors":{"authors":[{"text":"Ketner, Keith B.","contributorId":957,"corporation":false,"usgs":true,"family":"Ketner","given":"Keith","email":"","middleInitial":"B.","affiliations":[],"preferred":true,"id":284371,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"McGreevy, Laurence J.","contributorId":98706,"corporation":false,"usgs":true,"family":"McGreevy","given":"Laurence J.","affiliations":[],"preferred":false,"id":284372,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":71548,"text":"tei522 - 1955 - Scintillation spectrometer II: simultaneous measurement of uranium, thorium and potassium in common rocks","interactions":[],"lastModifiedDate":"2012-02-02T00:13:44","indexId":"tei522","displayToPublicDate":"1994-01-01T00:00:00","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":"522","title":"Scintillation spectrometer II: simultaneous measurement of uranium, thorium and potassium in common rocks","language":"ENGLISH","doi":"10.3133/tei522","usgsCitation":"Hurley, P.M., 1955, Scintillation spectrometer II: simultaneous measurement of uranium, thorium and potassium in common rocks: U.S. Geological Survey Trace Elements Investigations 522, 24 p. , https://doi.org/10.3133/tei522.","productDescription":"24 p. ","costCenters":[],"links":[{"id":185918,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/tei/522/report-thumb.jpg"},{"id":90825,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/tei/522/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"scale":"100000","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a0de4b07f02db5fd206","contributors":{"authors":[{"text":"Hurley, Patrick M.","contributorId":12121,"corporation":false,"usgs":true,"family":"Hurley","given":"Patrick","email":"","middleInitial":"M.","affiliations":[],"preferred":false,"id":284365,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":71544,"text":"tei518 - 1955 - Geology and mineralogy of the J. J. Mine, Jo Dandy area, Montrose County, Colorado","interactions":[],"lastModifiedDate":"2012-02-02T00:13:44","indexId":"tei518","displayToPublicDate":"1994-01-01T00:00:00","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":"518","title":"Geology and mineralogy of the J. J. Mine, Jo Dandy area, Montrose County, Colorado","language":"ENGLISH","doi":"10.3133/tei518","usgsCitation":"Elston, D.P., and Botinelly, T., 1955, Geology and mineralogy of the J. J. 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This report and accompanying maps summarize the status or ownership or many phosphate bearing lands in southwestern Montana and northeastern Idaho. Ownership categories discussed are (1) phosphate rights owned by Federal Government, (2) phosphate rights not owned by Federal Government, and (3) ownership status uncertain.

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No abstract available.

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