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,{"id":70098179,"text":"tei400 - 1954 - U.S. Geological Survey Trace Elements and related reports through 1953","interactions":[],"lastModifiedDate":"2014-06-11T13:25:03","indexId":"tei400","displayToPublicDate":"1954-01-01T15:52:00","publicationYear":"1954","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":"400","title":"U.S. Geological Survey Trace Elements and related reports through 1953","docAbstract":"<p>This report combines and brings up-to-date the information previously given in Trace Elements Investigations Report 325, \"Numerical list of U.S. Geological Survey Trace Elements Reports to April 30, 1953,\" and Trace Elements Investigations Report 301, \"Topical index and bibliography of U.S. Geological Survey Trace Elements and related reports.\"<p>\n<br/>\n<p>Part I is a numerical list of U.S. Geological Survey Trace Elements Investigations and Memorandum reports. It supersedes TEI-325. This part lists not only reports (followed by a date) that have been transmitted to the U.S. Atomic Energy Commission, but also reports in preparation (followed by an asterisk) for which tentative titles were available on December 31, 1953. Reports that have been published are indicated by the abbreviation of the medium of publication. (See also part II.)</p>\n <br/>\n<p>Part II is a reference guide to Trace Elements and related reports that are available to the public; this part supersedes Part 2 of the TEI-301 (published as Geological survey Circular 281). These reports are grouped according to the type of publication or release. Abstracts published in Nuclear Science Abstracts are not included in Part II, although certain TEI and TEM reports, the abstracts of which have been published in NSA, are so indicated in Part I. Publications in process on December 31, 1953, are designated by an asterisk.</p>\n<br/>\n<p>Part III is a finding list of states, areas, and subjects. It is based on information derived mostly from the titles of reports and, where titles are of a general nature, from a cursory review of the reports. This list is not a complete index of the information given in Trace Elements and related reports, but is designed to find subjects of major interest. Because of the numerous entries for Colorado and Utah, information has been listed by counties and, where possible, by subject under these states. Other states have county listings only if a county is included in the title of a report; otherwise, areas may be listed separately under the state. Major subjects are listed separately in the index and also where appropriate under states. Analytical methods and subjects related to analytical research are listed under Analytical Methods and Research, but not separately throughout the index. Most mineralogic studies are included under the heading Mineralogy, but are not necessarily listed according to location.</p>\n<br/>\n<p>Part IV is a finding list of authors. The words “with” and “and” are used to indicate seniority of authorship. For example, a listing of Jones and Brown indicates that Jones is the senior author. A listing of Jones with Brown indicates that Brown is the senior author.</p>\n<br/>\n<p>In both parts III and IV all Trace Elements reports are listed, as well as other related reports that have not been issued as Trace Elements reports.</p>\n<br/>\n<p>The following standard abbreviations have been used: TEI, Trace Elements Investigations report; TEM, Trace Elements Memorandum report; P, Professional Paper; B, Bulletin; C, Circular; J, Journal; OF, open file; TIS, Technical Information Service release; NSA, Nuclear Science Abstracts; QM, Quadrangle Map Series; and OM, Oil and Gas map or Mineral Investigations map or report.</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/tei400","collaboration":"This report concerns work done on behalf of the Divisions of Raw Materials and Research of the U.S. Atomic Energy Commission","usgsCitation":"Wallace, J.H., Blatcher, V.K., and Smith, H., 1954, U.S. Geological Survey Trace Elements and related reports through 1953: U.S. Geological Survey Trace Elements Investigations 400, 267 p., https://doi.org/10.3133/tei400.","productDescription":"267 p.","numberOfPages":"269","costCenters":[],"links":[{"id":284103,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/tei400.jpg"},{"id":285824,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/tei/0400/report.pdf"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"535595d4e4b0120853e8c2ba","contributors":{"authors":[{"text":"Wallace, Jane H.","contributorId":95119,"corporation":false,"usgs":true,"family":"Wallace","given":"Jane","email":"","middleInitial":"H.","affiliations":[],"preferred":false,"id":491675,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Blatcher, Virginia K.","contributorId":55332,"corporation":false,"usgs":true,"family":"Blatcher","given":"Virginia","email":"","middleInitial":"K.","affiliations":[],"preferred":false,"id":491673,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Smith, Harriet B.","contributorId":59097,"corporation":false,"usgs":true,"family":"Smith","given":"Harriet B.","affiliations":[],"preferred":false,"id":491674,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":70210898,"text":"70210898 - 1954 - Geologic map of Oklahoma","interactions":[],"lastModifiedDate":"2020-08-04T21:24:50.838406","indexId":"70210898","displayToPublicDate":"1954-01-01T15:47:40","publicationYear":"1954","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":6,"text":"USGS Unnumbered Series"},"title":"Geologic map of Oklahoma","docAbstract":"<p>No abstract available.</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/70210898","collaboration":"Prepared cooperatively by the United States Geological Survey and the Oklahoma Geological Survey","usgsCitation":"Miser, H.D., 1954, Geologic map of Oklahoma, HTML Document, https://doi.org/10.3133/70210898.","productDescription":"HTML Document","costCenters":[],"links":[{"id":376075,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":376074,"rank":1,"type":{"id":15,"text":"Index 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,{"id":70095693,"text":"tei464 - 1954 - Reconnaissance for uranium in black shale, Northern Rocky Mountains and Great Plains, 1953","interactions":[],"lastModifiedDate":"2014-06-03T12:45:16","indexId":"tei464","displayToPublicDate":"1954-01-01T15:44:00","publicationYear":"1954","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":"464","title":"Reconnaissance for uranium in black shale, Northern Rocky Mountains and Great Plains, 1953","docAbstract":"<p>Reconnaissance examinations for uranium in 22 formations containing black shale were conducted in parts of Montana, North Dakota, Utah, Idaho, and Oregon during 1953. About 150 samples from 80 outcrop localities and 5 oil and gas wells were submitted for uranium determinations. Most of the black shale deposits examined contain less than 0.003 percent uranium; however, thin beds of black shale at the base of the Mississippian system contain 0.005 percent uranium at 2 outcrop localities in southwestern Montana and as much as 0.007 percent uranium in a well in northeastern Montana. An eight-foot bed of phosphatic black shale at the base of the Brazer limestone of Late Mississippian age in Rich County, Utah, contains as much as 0.009 percent uranium.</p>\n<br/>\n<p>Commercial gamma ray logs of oil and gas wells drilled in Montana and adjacent parts of the Dakotas indicate that locally the Heath shale of Late Mississippian age contains as much as 0.01 percent equivalent uranium, and black shales of Late Cretaceous age contain as much as 0.008 percent equivalent uranium.</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/tei464","collaboration":"This report concerns work done on behalf of the Division of Raw Materials of the U.S. Atomic Energy Commission","usgsCitation":"Mapel, W.J., 1954, Reconnaissance for uranium in black shale, Northern Rocky Mountains and Great Plains, 1953: U.S. Geological Survey Trace Elements Investigations 464, 49 p., https://doi.org/10.3133/tei464.","productDescription":"49 p.","numberOfPages":"49","costCenters":[],"links":[{"id":283501,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/tei464.jpg"},{"id":284582,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/tei/0464/report.pdf"}],"country":"United States","state":"Idaho;Montana;North Dakota;Oregon;Utah","otherGeospatial":"Rocky Mountains","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -118.45,40.98 ], [ -118.45,49.0 ], [ -103.2,49.0 ], [ -103.2,40.98 ], [ -118.45,40.98 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"53559532e4b0120853e8c197","contributors":{"authors":[{"text":"Mapel, W. J.","contributorId":92225,"corporation":false,"usgs":true,"family":"Mapel","given":"W.","email":"","middleInitial":"J.","affiliations":[],"preferred":false,"id":491376,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":70048743,"text":"tem706 - 1954 - Geology of the Roc Creek quadrangle, Montrose county, Colorado","interactions":[{"subject":{"id":70048743,"text":"tem706 - 1954 - Geology of the Roc Creek quadrangle, Montrose county, Colorado","indexId":"tem706","publicationYear":"1954","noYear":false,"title":"Geology of the Roc Creek quadrangle, Montrose county, Colorado"},"predicate":"SUPERSEDED_BY","object":{"id":60889,"text":"mf23 - 1955 - Preliminary geologic map of the Roc Creek quadrangle, Colorado","indexId":"mf23","publicationYear":"1955","noYear":false,"title":"Preliminary geologic map of the Roc Creek quadrangle, Colorado"},"id":1}],"supersededBy":{"id":60889,"text":"mf23 - 1955 - Preliminary geologic map of the Roc Creek quadrangle, Colorado","indexId":"mf23","publicationYear":"1955","noYear":false,"title":"Preliminary geologic map of the Roc Creek quadrangle, Colorado"},"lastModifiedDate":"2014-03-04T14:29:02","indexId":"tem706","displayToPublicDate":"1954-01-01T15:37:00","publicationYear":"1954","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":"706","title":"Geology of the Roc Creek quadrangle, Montrose county, Colorado","docAbstract":"The Roc Creek quadrangle is one of eighteen 7 1/2-minute quadrangles covering the principal carnotite-producing area of southwestern Colorado.  The geology of these quadrangles was mapped by the U.S. Geological Survey for the U.S. Atomic Energy Commission as part of a comprehensive study of carnotite deposits.  The rocks exposed in the eighteen quadrangles consist of crystalline rocks of pre-Cambrian age and sedimentary rocks that range in age from late Paleozoic to Quaternary.  Over much of the area the sedimentary rocks are flat lying, but in places the rocks are disrupted by high-angle faults and northwest-trending folds.  Conspicuous among the folds are large anticlines having cores of intrusive salt and gypsum. Most of the carnotite deposits are confined to the Salt Wash sandstone member of the Jurassic Morrison formation. Within this sandstone, most of the deposits are spottily distributed through an arcuate zone known as the \"Uravan mineral belt\". Individual deposits range in size from irregular masses containing only a few tons of ore to large, tabular masses containing many thousands of tons.  The ore consists largely of sandstone selectively impregnated and in part replaced by uranium and vanadium minerals. Most of the deposits appear to be related to certain sedimentary in sandstones of favorable composition.","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/tem706","collaboration":"This report concerns work done on behalf of the Division of Raw Materials of the U.S. Atomic Energy Commission","usgsCitation":"Shoemaker, E., 1954, Geology of the Roc Creek quadrangle, Montrose county, Colorado: U.S. Geological Survey Trace Elements Memorandum 706, Report: 29 p.; 1 Plate: 33.82 x 28.06 inches, https://doi.org/10.3133/tem706.","productDescription":"Report: 29 p.; 1 Plate: 33.82 x 28.06 inches","numberOfPages":"31","additionalOnlineFiles":"Y","costCenters":[],"links":[{"id":278619,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/tem/0706/report-thumb.jpg"},{"id":283342,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/tem/0706/report.pdf"},{"id":283341,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/tem/0706/plate-1.pdf"}],"country":"United States","state":"Colorado","county":"Montrose County","otherGeospatial":"Roc Creek Quadrangle","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -109.0,38.375 ], [ -109.0,38.5 ], [ -108.875,38.5 ], [ -108.875,38.375 ], [ -109.0,38.375 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"52737befe4b097f32ac3db4c","contributors":{"authors":[{"text":"Shoemaker, E.M.","contributorId":81499,"corporation":false,"usgs":true,"family":"Shoemaker","given":"E.M.","email":"","affiliations":[],"preferred":false,"id":485527,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":70048299,"text":"tem377A - 1954 - Photogeologic map, Elk Ridge-16 Quadrangle, San Juan County, Utah","interactions":[{"subject":{"id":70048299,"text":"tem377A - 1954 - Photogeologic map, Elk Ridge-16 Quadrangle, San Juan County, Utah","indexId":"tem377A","publicationYear":"1954","noYear":false,"chapter":"A","title":"Photogeologic map, Elk Ridge-16 Quadrangle, San Juan County, Utah"},"predicate":"SUPERSEDED_BY","object":{"id":66569,"text":"i63 - 1955 - Photogeologic map of the Elk Ridge-16 quadrangle, San Juan County, Utah","indexId":"i63","publicationYear":"1955","noYear":false,"title":"Photogeologic map of the Elk Ridge-16 quadrangle, San Juan County, Utah"},"id":1}],"supersededBy":{"id":66569,"text":"i63 - 1955 - Photogeologic map of the Elk Ridge-16 quadrangle, San Juan County, Utah","indexId":"i63","publicationYear":"1955","noYear":false,"title":"Photogeologic map of the Elk Ridge-16 quadrangle, San Juan County, Utah"},"lastModifiedDate":"2014-02-28T14:44:14","indexId":"tem377A","displayToPublicDate":"1954-01-01T15:35:00","publicationYear":"1954","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":"377","chapter":"A","title":"Photogeologic map, Elk Ridge-16 Quadrangle, San Juan County, Utah","docAbstract":"No abstract available.","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/tem377A","collaboration":"Prepared in cooperation with the Atomic Energy Commission","usgsCitation":"Miller, C.F., 1954, Photogeologic map, Elk Ridge-16 Quadrangle, San Juan County, Utah: U.S. Geological Survey Trace Elements Memorandum 377, Report: 3 p.; 1 Plate: 23.67 x 29.05 inches, https://doi.org/10.3133/tem377A.","productDescription":"Report: 3 p.; 1 Plate: 23.67 x 29.05 inches","numberOfPages":"3","additionalOnlineFiles":"Y","costCenters":[],"links":[{"id":277943,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/tem/0377-A/report-thumb.jpg"},{"id":283111,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/tem/0377-A/plate-1.pdf"},{"id":283110,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/tem/0377-A/report.pdf"}],"scale":"24000","country":"United States","state":"Utah","county":"San Juan County","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -109.625,37.5 ], [ -109.625,37.625 ], [ -109.5,37.625 ], [ -109.5,37.5 ], [ -109.625,37.5 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"523c1cf2e4b024b60d407333","contributors":{"authors":[{"text":"Miller, C. F.","contributorId":89971,"corporation":false,"usgs":true,"family":"Miller","given":"C.","email":"","middleInitial":"F.","affiliations":[],"preferred":false,"id":484264,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":70095692,"text":"tei452 - 1954 - Reconnaissance for uranium-bearing lignite in the Ekalaka Lignite Field, Carter County, Montana","interactions":[],"lastModifiedDate":"2014-05-27T15:01:17","indexId":"tei452","displayToPublicDate":"1954-01-01T15:35:00","publicationYear":"1954","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":"452","title":"Reconnaissance for uranium-bearing lignite in the Ekalaka Lignite Field, Carter County, Montana","docAbstract":"<p>Uranium-bearing lignite beds 1.5 to 8 feet thick occur in the Fort Union formation of the southern part of the Ekalaka Hills, Carter County, Mont. Data from surface outcrops indicate that an area of about 1,400 acres is underlain by 16,500,000 tons of uranium-bearing lignite containing 700 tons of uranium. The uranium content of the lignite beds ranges from 0.001 to 0.034 percent.</p> \n<br/>\n<p>Ironstone concretions in the massive coarse-grained sandstones in the upper part of the Fort Union formation contain 0.005 percent uranium in the northern and eastern parts of the area. These sandstones are good potential host rocks for uranium mineralization and are lithologically similar to the massive coarse-grained uranium-bearing sandstones of the Wasatch formation in the Pumpkin Buttes area of the Powder River Basin.</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/tei452","collaboration":"This report concerns work done on behalf of the Division of Raw Materials of the U.S. Atomic Energy Commission","usgsCitation":"Gill, J.R., 1954, Reconnaissance for uranium-bearing lignite in the Ekalaka Lignite Field, Carter County, Montana: U.S. Geological Survey Trace Elements Investigations 452, 27 p., https://doi.org/10.3133/tei452.","productDescription":"27 p.","numberOfPages":"28","costCenters":[],"links":[{"id":283500,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/tei452.jpg"},{"id":284569,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/tei/0452/report.pdf"}],"country":"United States","state":"Montana","county":"Carter County","otherGeospatial":"Ekalaka Hills","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -105.0394,44.9974 ], [ -105.0394,46.1369 ], [ -104.0396,46.1369 ], [ -104.0396,44.9974 ], [ -105.0394,44.9974 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"53559532e4b0120853e8c19d","contributors":{"authors":[{"text":"Gill, James R.","contributorId":44904,"corporation":false,"usgs":true,"family":"Gill","given":"James","email":"","middleInitial":"R.","affiliations":[],"preferred":false,"id":491375,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":70048298,"text":"tem370A - 1954 - Photogeologic map, Bluff-8 Quadrangle, San Juan County, Utah","interactions":[{"subject":{"id":70048298,"text":"tem370A - 1954 - Photogeologic map, Bluff-8 Quadrangle, San Juan County, Utah","indexId":"tem370A","publicationYear":"1954","noYear":false,"chapter":"A","title":"Photogeologic map, Bluff-8 Quadrangle, San Juan County, Utah"},"predicate":"SUPERSEDED_BY","object":{"id":66563,"text":"i61 - 1955 - Photogeologic map of the Bluff-8 quadrangle, San Juan County, Utah","indexId":"i61","publicationYear":"1955","noYear":false,"title":"Photogeologic map of the Bluff-8 quadrangle, San Juan County, Utah"},"id":1}],"supersededBy":{"id":66563,"text":"i61 - 1955 - Photogeologic map of the Bluff-8 quadrangle, San Juan County, Utah","indexId":"i61","publicationYear":"1955","noYear":false,"title":"Photogeologic map of the Bluff-8 quadrangle, San Juan County, Utah"},"lastModifiedDate":"2014-02-28T14:43:41","indexId":"tem370A","displayToPublicDate":"1954-01-01T15:05:00","publicationYear":"1954","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":"370","chapter":"A","title":"Photogeologic map, Bluff-8 Quadrangle, San Juan County, Utah","docAbstract":"No abstract available.","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/tem370A","collaboration":"Prepared in cooperation with the Atomic Energy Commission","usgsCitation":"Miller, C.F., 1954, Photogeologic map, Bluff-8 Quadrangle, San Juan County, Utah: U.S. Geological Survey Trace Elements Memorandum 370, Report: 3 p.; 1 Plate: 23.85 x 29.91 inches, https://doi.org/10.3133/tem370A.","productDescription":"Report: 3 p.; 1 Plate: 23.85 x 29.91 inches","numberOfPages":"3","additionalOnlineFiles":"Y","costCenters":[],"links":[{"id":277942,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/tem/0370-A/report-thumb.jpg"},{"id":283108,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/tem/0370-A/report.pdf"},{"id":283109,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/tem/0370-A/plate-1.pdf"}],"country":"United States","state":"Utah","city":"San Juan County","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -109.625,37.25 ], [ -109.625,37.366667 ], [ -109.5,37.366667 ], [ -109.5,37.25 ], [ -109.625,37.25 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"523c1cf1e4b024b60d40732f","contributors":{"authors":[{"text":"Miller, C. F.","contributorId":89971,"corporation":false,"usgs":true,"family":"Miller","given":"C.","email":"","middleInitial":"F.","affiliations":[],"preferred":false,"id":484263,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":70113791,"text":"tei463 - 1954 - Uranium-bearing lignite in southwestern North Dakota","interactions":[],"lastModifiedDate":"2014-07-14T14:21:30","indexId":"tei463","displayToPublicDate":"1954-01-01T14:54:00","publicationYear":"1954","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":"463","title":"Uranium-bearing lignite in southwestern North Dakota","docAbstract":"<p>Uranium-bearing lignite was mapped and sampled in the Bullion Butte, Sentinel Butte, HT Butte, and Chalky Buttes areas in southwestern North Dakota. The uraniferous lignite occurs at several stratigraphic positions in the Sentinel Butte member of the Fort Union formation of Paleocene age. A total of 261 samples were collected for uranium analysis from 85 localities, Lignite contained as much as 0.045 percent uranium, 10.0 percent ash, and 0.45 percent uranium in the ash was found although the average is lower. Inferred reserves for the four areas examined are estimated to be about 27 million tons of lignite in beds about 2 feet thick and containing more than 3000 tons of uranium. The lignite in beds about 2 feet thick and containing more than 3000 tons of uranium. The lignite averages more than 30 percent ash in the surface samples. The principal factor that seems to influence the uranium content of lignite beds is their stratigraphic position below the overlying rocks of the White River group of Oligocene age. All of the uranium-bearing beds closely underlie the base of the White River group. Although this relationship seems to be the controlling factor, the relative concentration of uranium may be modified by other conditions. Beds enclosed in permeable rocks are more uraniferous than beds in impermeable rocks, and thin beds have higher content of uranium than thick beds. In addition, thick lignite beds commonly have a top=preferential distribution of uranium. These and other factors suggest that the uranium is secondary and this it was introduced by ground water which had leached uranium from volcanic ash in the overlying rocks of the White River group. It is thought that the uranium is held in the lignite as part of a metallo-organic compound.</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/tei463","collaboration":"This report concerns work done on behalf of the Division of Raw Materials of the U.S. Atomic Energy Commission","usgsCitation":"Moore, G.W., Melin, R.E., and Kepferle, R.C., 1954, Uranium-bearing lignite in southwestern North Dakota: U.S. Geological Survey Trace Elements Investigations 463, Report: 35 p.; 1 Plate: 22.82 x 17.92 inches, https://doi.org/10.3133/tei463.","productDescription":"Report: 35 p.; 1 Plate: 22.82 x 17.92 inches","numberOfPages":"36","costCenters":[],"links":[{"id":289974,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":289973,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/tei/0463/report.pdf"},{"id":289970,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/tei/0463/plate-1.pdf"}],"country":"United States","state":"Montana;North Dakota;South Dakota","otherGeospatial":"Bullion Butte;Chalky Buttes;Ht Butte;Sentinel Butte","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -105.0299,44.9987 ], [ -105.0299,47.1933 ], [ -102.3265,47.1933 ], [ -102.3265,44.9987 ], [ -105.0299,44.9987 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"53ae7890e4b0abf75cf2d8ff","contributors":{"authors":[{"text":"Moore, George W.","contributorId":21625,"corporation":false,"usgs":true,"family":"Moore","given":"George","email":"","middleInitial":"W.","affiliations":[],"preferred":false,"id":495193,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Melin, Robert E.","contributorId":23198,"corporation":false,"usgs":true,"family":"Melin","given":"Robert","email":"","middleInitial":"E.","affiliations":[],"preferred":false,"id":495194,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Kepferle, Roy C.","contributorId":103586,"corporation":false,"usgs":true,"family":"Kepferle","given":"Roy","email":"","middleInitial":"C.","affiliations":[],"preferred":false,"id":495195,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":78584,"text":"tem786 - 1954 - Preliminary study of the clay minerals in some red and green mudstones from the Colorado Plateau","interactions":[],"lastModifiedDate":"2014-07-16T14:54:44","indexId":"tem786","displayToPublicDate":"1954-01-01T14:53:19","publicationYear":"1954","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":"786","title":"Preliminary study of the clay minerals in some red and green mudstones from the Colorado Plateau","docAbstract":"No abstract available.","language":"English","publisher":"U.S Department of the Interior, Geological Survey","publisherLocation":"Washington, D.C.","doi":"10.3133/tem786","usgsCitation":"Keller, W.D., 1954, Preliminary study of the clay minerals in some red and green mudstones from the Colorado Plateau: U.S. Geological Survey Trace Elements Memorandum 786, 16 p., https://doi.org/10.3133/tem786.","productDescription":"16 p.","numberOfPages":"16","costCenters":[],"links":[{"id":290315,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"}],"country":"United States","state":"Arizona;Utah","otherGeospatial":"Colorado Plateau","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -110.064986,36.964627 ], [ -110.064986,37.035916 ], [ -109.936926,37.035916 ], [ -109.936926,36.964627 ], [ -110.064986,36.964627 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"53c79f11e4b0194841642497","contributors":{"authors":[{"text":"Keller, Walter David","contributorId":27791,"corporation":false,"usgs":true,"family":"Keller","given":"Walter","email":"","middleInitial":"David","affiliations":[],"preferred":false,"id":288968,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":70048295,"text":"tem369A - 1954 - Photogeologic map, Bluff-1 Quadrangle, San Juan County, Utah","interactions":[{"subject":{"id":70048295,"text":"tem369A - 1954 - Photogeologic map, Bluff-1 Quadrangle, San Juan County, Utah","indexId":"tem369A","publicationYear":"1954","noYear":false,"chapter":"A","title":"Photogeologic map, Bluff-1 Quadrangle, San Juan County, Utah"},"predicate":"SUPERSEDED_BY","object":{"id":66560,"text":"i64 - 1955 - Photogeologic map of the Bluff-1 quadrangle, San Juan County, Utah","indexId":"i64","publicationYear":"1955","noYear":false,"title":"Photogeologic map of the Bluff-1 quadrangle, San Juan County, Utah"},"id":1}],"supersededBy":{"id":66560,"text":"i64 - 1955 - Photogeologic map of the Bluff-1 quadrangle, San Juan County, Utah","indexId":"i64","publicationYear":"1955","noYear":false,"title":"Photogeologic map of the Bluff-1 quadrangle, San Juan County, Utah"},"lastModifiedDate":"2014-02-28T14:42:37","indexId":"tem369A","displayToPublicDate":"1954-01-01T14:48:00","publicationYear":"1954","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":"369","chapter":"A","title":"Photogeologic map, Bluff-1 Quadrangle, San Juan County, Utah","docAbstract":"No abstract available.","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/tem369A","collaboration":"Prepared in cooperation with the Atomic Energy Commission","usgsCitation":"Miller, C.F., 1954, Photogeologic map, Bluff-1 Quadrangle, San Juan County, Utah: U.S. Geological Survey Trace Elements Memorandum 369, Report: 3 p.; 1 Plate: 23.67 x 28.39 inches, https://doi.org/10.3133/tem369A.","productDescription":"Report: 3 p.; 1 Plate: 23.67 x 28.39 inches","numberOfPages":"3","additionalOnlineFiles":"Y","costCenters":[],"links":[{"id":277936,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/tem/0369-A/report-thumb.jpg"},{"id":283106,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/tem/0369-A/report.pdf"},{"id":283107,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/tem/0369-A/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\": [ [ [ -109.616667,37.375 ], [ -109.616667,37.5 ], [ -109.5,37.5 ], [ -109.5,37.375 ], [ -109.616667,37.375 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"523c1cf1e4b024b60d40732b","contributors":{"authors":[{"text":"Miller, C. F.","contributorId":89971,"corporation":false,"usgs":true,"family":"Miller","given":"C.","email":"","middleInitial":"F.","affiliations":[],"preferred":false,"id":484259,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":70048740,"text":"tem703 - 1954 - Geology of the Paradox quadrangle, Montrose county, Colorado","interactions":[{"subject":{"id":70048740,"text":"tem703 - 1954 - Geology of the Paradox quadrangle, Montrose county, Colorado","indexId":"tem703","publicationYear":"1954","noYear":false,"title":"Geology of the Paradox quadrangle, Montrose county, Colorado"},"predicate":"SUPERSEDED_BY","object":{"id":61237,"text":"mf22 - 1955 - Preliminary geologic map of the Paradox quadrangle, Colorado","indexId":"mf22","publicationYear":"1955","noYear":false,"title":"Preliminary geologic map of the Paradox quadrangle, Colorado"},"id":1}],"supersededBy":{"id":61237,"text":"mf22 - 1955 - Preliminary geologic map of the Paradox quadrangle, Colorado","indexId":"mf22","publicationYear":"1955","noYear":false,"title":"Preliminary geologic map of the Paradox quadrangle, Colorado"},"lastModifiedDate":"2014-03-04T14:26:53","indexId":"tem703","displayToPublicDate":"1954-01-01T14:46:00","publicationYear":"1954","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":"703","title":"Geology of the Paradox quadrangle, Montrose county, Colorado","docAbstract":"The Paradox quadrangle is one of eighteen 7 1/2-minute quadrangles covering the principal carnotite-producing area of southwestern Colorado.  The geology of these quadrangles was mapped by the U.S. Geological Survey for the Atomic Energy Commission as part of a comprehensive study of carnotite deposits.  The rocks exposed in the eighteen quadrangles consist of crystalline rocks of pre-Cambrian age and sedimentary rocks that range in age from late Paleozoic to Quaternary. Over much of the area the sedimentary rocks are flat lying, but in places the rocks are disrupted by high-angle faults, and northwest-trending folds. Conspicuous among the folds are large anticlines having cores of intrusive salt and gypsum.  Most of the carnotite deposits are confined to the Salt Wash sandstone member of the Jurassic Morrison formation, Within this sandstone, most of the deposits are spottily distributed through an arcuate zone known as the \"Uravan Mineral Belt\". Individual deposits range in size from irregular masses containing only a few tons of ore to large, tabular masses containing thousands of tons. The ore consists largely of sandstone selectively impregnated and in part replaced by uranium and vanadium minerals. Most of the deposits appear to be related to certain sedimentary structures in sandstones of favorable composition.","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/tem703","collaboration":"This report concerns work done on behalf of the Division of Raw Materials of the U.S. Atomic Energy Commission","usgsCitation":"Withington, C.F., 1954, Geology of the Paradox quadrangle, Montrose county, Colorado: U.S. Geological Survey Trace Elements Memorandum 703, Report: 28 p.; 1 Plate: 33.88 x 27.86 inches, https://doi.org/10.3133/tem703.","productDescription":"Report: 28 p.; 1 Plate: 33.88 x 27.86 inches","numberOfPages":"30","additionalOnlineFiles":"Y","costCenters":[],"links":[{"id":278614,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/tem/0703/report-thumb.jpg"},{"id":283335,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/tem/0703/plate-1.pdf"},{"id":283336,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/tem/0703/report.pdf"}],"country":"United States","state":"Colorado","county":"Montrose County","otherGeospatial":"Paradox Quadrangle","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -109.0,38.25 ], [ -109.0,38.375 ], [ -108.875,38.375 ], [ -108.875,38.25 ], [ -109.0,38.25 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"52737beee4b097f32ac3db43","contributors":{"authors":[{"text":"Withington, C. F.","contributorId":98394,"corporation":false,"usgs":true,"family":"Withington","given":"C.","email":"","middleInitial":"F.","affiliations":[],"preferred":false,"id":485523,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":71419,"text":"tei382 - 1954 - Occurrences of uranium at Clinton, Hunterdon County, New Jersey","interactions":[],"lastModifiedDate":"2014-06-11T12:47:57","indexId":"tei382","displayToPublicDate":"1954-01-01T14:34:00","publicationYear":"1954","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":"382","title":"Occurrences of uranium at Clinton, Hunterdon County, New Jersey","docAbstract":"<p>An occurrence of uranium at Clinton, Hunterdon County, N. J. was first brought to the attention of the U.S. Geological Survey when Mr. Thomas L. Eak of Avenel, N. J. submitted to the Survey a sample containing 0.068 percent uranium. Subsequent examinations of the area around Clinton indicated that detailed mapping and study were warranted.</p>\n<br/>\n<p>The uranium occurrences at Clinton are in or associated with fault zones in the Kittatinny limestone of Cambro-Ordovician age. The limestone generally light gray, thick bedded, and dolomitic; chert is common but not abundant. Regionally and locally, faults are the most significant structural features. The local faults at Clinton are the loci for most of the uranium. The largest fault can be traced for about 700 feet and is radioactive everywhere it crops out. Samples from this fault contain as much as 0.038 percent uranium; the average content is about 0.010 percent uranium. Uranium also occurs disseminated in two 4-inch layers of black feldspathic dolomite and in several zones of residual soil derived from the Kittatinny limestone. The black layers contain as much as 0.046 percent uranium and can be traced only about 20 feet along strike. They are cut by a small fault that is also radioactive. The radioactive soil zones are roughly elongated parallel to bedding. Soil from them contains up to 0.008 percent uranium. The uranium occurrences are best explained by a supergene origin.</p>\n<br/>\n<p>The sampling, mapping, and radioactivity testing of uranium occurrences at Clinton indicate they are too low grade to be of current economic interest.</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/tei382","collaboration":"This report concerns work done on behalf of the Division of Raw Materials of the U.S. Atomic Energy Commission","usgsCitation":"McKeown, F.A., Klemic, H., and Choquette, P., 1954, Occurrences of uranium at Clinton, Hunterdon County, New Jersey: U.S. Geological Survey Trace Elements Investigations 382, Report: 19 p.; 2 Plates: 12.09 x 11.20 inches and 12.76 x 16.20 inches, https://doi.org/10.3133/tei382.","productDescription":"Report: 19 p.; 2 Plates: 12.09 x 11.20 inches and 12.76 x 16.20 inches","numberOfPages":"20","costCenters":[],"links":[{"id":284088,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/tei382.jpg"},{"id":285798,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/tei/0382/figure-1.pdf"},{"id":285799,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/tei/0382/figure-2.pdf"},{"id":285800,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/tei/0382/report.pdf"}],"country":"United States","state":"New Jersey","county":"Hunterdon County","city":"Clinton","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -75.166667,40.5 ], [ -75.166667,40.833333 ], [ -74.5,40.833333 ], [ -74.5,40.5 ], [ -75.166667,40.5 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"535594e4e4b0120853e8c0b8","contributors":{"authors":[{"text":"McKeown, F. A.","contributorId":106100,"corporation":false,"usgs":true,"family":"McKeown","given":"F.","email":"","middleInitial":"A.","affiliations":[],"preferred":false,"id":284148,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Klemic, H.","contributorId":23066,"corporation":false,"usgs":true,"family":"Klemic","given":"H.","email":"","affiliations":[],"preferred":false,"id":284147,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Choquette, P.W.","contributorId":13144,"corporation":false,"usgs":true,"family":"Choquette","given":"P.W.","email":"","affiliations":[],"preferred":false,"id":284146,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":70048738,"text":"tem701 - 1954 - Geology of the Juanita Arch quadrangle, Mesa county, Colorado","interactions":[],"lastModifiedDate":"2014-03-04T14:25:15","indexId":"tem701","displayToPublicDate":"1954-01-01T14:11:00","publicationYear":"1954","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":"701","title":"Geology of the Juanita Arch quadrangle, Mesa county, Colorado","docAbstract":"The Juanita Arch quadrangle is one of eighteen 7 1/2-minute quadrangles covering the principal carnotite-producing area of southwestern Colorado.  The geology of these quadrangles was mapped by the U.S. Geological Survey for the Atomic Energy Commission as part of a comprehensive study of carnotite deposits.  The rocks exposed in the eighteen quadrangles consist of crystalline rocks of pre-Cambrian age and sedimentary rocks that range in age from late Paleozoic to Quaternary.  Over much of the area the sedimentary rocks are flat lying, but in places the rocks are disrupted by high-angle faults and northwest-trending folds.  Conspicuous among the folds are large anticlines having cores of intrusive salt and gypsum. Most of the carnotite deposits are confined to the Salt Wash sandstone member of the Jurassic Morrison formation. Within this sandstone, most of the deposits are spottily distributed through an arcuate zone known as the \"Uravan Mineral Belt\".  Individual deposits range in size from irregular masses containing only a few tons of ore ro large, tabular masses containing many thousands of tons. The ore consists largely of sandstone selectively impregnated and in part replaced by uranium and vanadium minerals. Most of the deposits appear to be related to certain sedimentary structures in sandstone of favorable construction.","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/tem701","collaboration":"This report concerns work done on behalf of the Division of Raw Materials of the U.S. Atomic Energy Commission","usgsCitation":"Shoemaker, E., 1954, Geology of the Juanita Arch quadrangle, Mesa county, Colorado: U.S. Geological Survey Trace Elements Memorandum 701, Report: 35 p.; 1 Plate: 33.76 x 28.14 inches, https://doi.org/10.3133/tem701.","productDescription":"Report: 35 p.; 1 Plate: 33.76 x 28.14 inches","numberOfPages":"37","additionalOnlineFiles":"Y","costCenters":[],"links":[{"id":278611,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/tem/0701/report-thumb.jpg"},{"id":283331,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/tem/0701/plate-1.pdf"},{"id":283332,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/tem/0701/report.pdf"}],"country":"United States","state":"Colorado","county":"Mesa County","otherGeospatial":"Juanita Arch Quadrangle","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -109.0,38.5 ], [ -109.0,38.625 ], [ -108.875,38.625 ], [ -108.875,38.5 ], [ -109.0,38.5 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"52737bede4b097f32ac3db3d","contributors":{"authors":[{"text":"Shoemaker, Eugene M.","contributorId":59335,"corporation":false,"usgs":true,"family":"Shoemaker","given":"Eugene M.","affiliations":[],"preferred":false,"id":485520,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":33215,"text":"b1012 - 1954 - Fluorspar deposits in western Kentucky","interactions":[{"subject":{"id":44261,"text":"b1012A - 1955 - Fluorspar deposits in western Kentucky, part 1: Introduction","indexId":"b1012A","publicationYear":"1955","noYear":false,"chapter":"A","title":"Fluorspar deposits in western Kentucky, part 1: Introduction"},"predicate":"IS_PART_OF","object":{"id":33215,"text":"b1012 - 1954 - Fluorspar deposits in western Kentucky","indexId":"b1012","publicationYear":"1954","noYear":false,"title":"Fluorspar deposits in western Kentucky"},"id":1},{"subject":{"id":44262,"text":"b1012B - 1955 - Babb fault system, Crittenden and Livingston Counties","indexId":"b1012B","publicationYear":"1955","noYear":false,"chapter":"B","title":"Babb fault system, Crittenden and Livingston Counties"},"predicate":"IS_PART_OF","object":{"id":33215,"text":"b1012 - 1954 - Fluorspar deposits in western Kentucky","indexId":"b1012","publicationYear":"1954","noYear":false,"title":"Fluorspar deposits in western Kentucky"},"id":2},{"subject":{"id":44263,"text":"b1012C - 1954 - Central part of the Commodore fault system, Crittenden County","indexId":"b1012C","publicationYear":"1954","noYear":false,"chapter":"C","title":"Central part of the Commodore fault system, Crittenden County"},"predicate":"IS_PART_OF","object":{"id":33215,"text":"b1012 - 1954 - Fluorspar deposits in western Kentucky","indexId":"b1012","publicationYear":"1954","noYear":false,"title":"Fluorspar deposits in western Kentucky"},"id":3},{"subject":{"id":44264,"text":"b1012D - 1954 - Mineral Ridge area, Livingston and Crittenden Counties","indexId":"b1012D","publicationYear":"1954","noYear":false,"chapter":"D","title":"Mineral Ridge area, Livingston and Crittenden Counties"},"predicate":"IS_PART_OF","object":{"id":33215,"text":"b1012 - 1954 - Fluorspar deposits in western Kentucky","indexId":"b1012","publicationYear":"1954","noYear":false,"title":"Fluorspar deposits in western Kentucky"},"id":4},{"subject":{"id":44265,"text":"b1012E - 1954 - Moore Hill fault system, Crittenden and Livingston Counties","indexId":"b1012E","publicationYear":"1954","noYear":false,"chapter":"E","title":"Moore Hill fault system, Crittenden and Livingston Counties"},"predicate":"IS_PART_OF","object":{"id":33215,"text":"b1012 - 1954 - Fluorspar deposits in western Kentucky","indexId":"b1012","publicationYear":"1954","noYear":false,"title":"Fluorspar deposits in western Kentucky"},"id":5},{"subject":{"id":44266,"text":"b1012F - 1954 - Senator-Schwenck area, Tabb fault system, Caldwell county","indexId":"b1012F","publicationYear":"1954","noYear":false,"chapter":"F","title":"Senator-Schwenck area, Tabb fault system, Caldwell county"},"predicate":"IS_PART_OF","object":{"id":33215,"text":"b1012 - 1954 - Fluorspar deposits in western Kentucky","indexId":"b1012","publicationYear":"1954","noYear":false,"title":"Fluorspar deposits in western Kentucky"},"id":6}],"lastModifiedDate":"2017-08-08T15:45:42","indexId":"b1012","displayToPublicDate":"1954-01-01T14:07:00","publicationYear":"1954","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":"1012","title":"Fluorspar deposits in western Kentucky","docAbstract":"No abstract available.","language":"English","publisher":"U.S. Government Printing Office","doi":"10.3133/b1012","usgsCitation":"Williams, J.S., 1954, Fluorspar deposits in western Kentucky: U.S. Geological Survey Bulletin 1012, iii, 127 p., https://doi.org/10.3133/b1012.","productDescription":"iii, 127 p.","costCenters":[],"links":[{"id":344679,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/bul/1012/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":289238,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/bul/1012/report-thumb.jpg"}],"country":"United States","state":"Kentucky","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -89.5693,36.4972 ], [ -89.5693,39.1475 ], [ -85.162,39.1475 ], [ -85.162,36.4972 ], [ -89.5693,36.4972 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"53b286ebe4b07b8813a5549f","contributors":{"authors":[{"text":"Williams, James S.","contributorId":29315,"corporation":false,"usgs":true,"family":"Williams","given":"James","email":"","middleInitial":"S.","affiliations":[],"preferred":false,"id":210178,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":70260861,"text":"70260861 - 1954 - Geologic map index of Colorado","interactions":[],"lastModifiedDate":"2025-04-25T14:12:59.037415","indexId":"70260861","displayToPublicDate":"1954-01-01T14:02:27","publicationYear":"1954","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":6,"text":"USGS Unnumbered Series"},"title":"Geologic map index of Colorado","docAbstract":"<p>No abstract available.</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/70260861","usgsCitation":"Boardman, L., 1954, Geologic map index of Colorado (Revised 1954), 1 Plate: 46.18 x 37.75 inches, https://doi.org/10.3133/70260861.","productDescription":"1 Plate: 46.18 x 37.75 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,{"id":33284,"text":"b1002 - 1954 - Geophysical abstracts, 152-155, January-December 1953","interactions":[{"subject":{"id":44285,"text":"b1002A - 1954 - Geophysical abstracts 152, January-March 1953","indexId":"b1002A","publicationYear":"1954","noYear":false,"chapter":"A","title":"Geophysical abstracts 152, January-March 1953"},"predicate":"IS_PART_OF","object":{"id":33284,"text":"b1002 - 1954 - Geophysical abstracts, 152-155, January-December 1953","indexId":"b1002","publicationYear":"1954","noYear":false,"title":"Geophysical abstracts, 152-155, January-December 1953"},"id":1},{"subject":{"id":44286,"text":"b1002B - 1954 - Geophysical abstracts 153, April-June 1953","indexId":"b1002B","publicationYear":"1954","noYear":false,"chapter":"B","title":"Geophysical abstracts 153, April-June 1953"},"predicate":"IS_PART_OF","object":{"id":33284,"text":"b1002 - 1954 - Geophysical abstracts, 152-155, January-December 1953","indexId":"b1002","publicationYear":"1954","noYear":false,"title":"Geophysical abstracts, 152-155, January-December 1953"},"id":2},{"subject":{"id":44287,"text":"b1002C - 1954 - Geophysical abstracts 154, July-September 1953","indexId":"b1002C","publicationYear":"1954","noYear":false,"chapter":"C","title":"Geophysical abstracts 154, July-September 1953"},"predicate":"IS_PART_OF","object":{"id":33284,"text":"b1002 - 1954 - Geophysical abstracts, 152-155, January-December 1953","indexId":"b1002","publicationYear":"1954","noYear":false,"title":"Geophysical abstracts, 152-155, January-December 1953"},"id":3},{"subject":{"id":44288,"text":"b1002D - 1954 - Geophysical abstracts 155, October-December 1953","indexId":"b1002D","publicationYear":"1954","noYear":false,"chapter":"D","title":"Geophysical abstracts 155, October-December 1953"},"predicate":"IS_PART_OF","object":{"id":33284,"text":"b1002 - 1954 - Geophysical abstracts, 152-155, January-December 1953","indexId":"b1002","publicationYear":"1954","noYear":false,"title":"Geophysical abstracts, 152-155, January-December 1953"},"id":4}],"lastModifiedDate":"2014-07-07T13:56:43","indexId":"b1002","displayToPublicDate":"1954-01-01T13:53:00","publicationYear":"1954","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":"1002","title":"Geophysical abstracts, 152-155, January-December 1953","docAbstract":"No abstract available.","language":"English","publisher":"U.S. Government Printing Office","doi":"10.3133/b1002","usgsCitation":"U.S. Government Printing Office, 1954, Geophysical abstracts, 152-155, January-December 1953: U.S. Geological Survey Bulletin 1002, 284 p., https://doi.org/10.3133/b1002.","productDescription":"284 p.","temporalStart":"1953-01-01","temporalEnd":"1953-12-31","costCenters":[],"links":[{"id":289482,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"53bbc16fe4b084059e8bfecc"}
,{"id":71389,"text":"tei343 - 1954 - Exploration for uranium deposits in the Spring Creek Mesa area, Montrose County, Colorado","interactions":[],"lastModifiedDate":"2014-06-06T15:07:45","indexId":"tei343","displayToPublicDate":"1954-01-01T13:29:00","publicationYear":"1954","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":"343","title":"Exploration for uranium deposits in the Spring Creek Mesa area, Montrose County, Colorado","docAbstract":"<p>The U.S. Geological Survey explored the Spring Creek Mesa area from July 11, 1951, to August 14, 1953. During that period, 280 diamond-drill holes were completed for a total of 180,287 feet. </p>\n<br/>\t\n<p>Sedimentary rocks of Mesozoic age are exposed in and adjacent to the Spring Creek Mesa area. These rocks consist of, from oldest to youngest: the Upper Jurassic Morrison formation, the Lower Cretaceous Burro Canyon formation, and the Upper Cretaceous Dakota formation.</p>\n<br/>\n<p>The Morrison formation consists of two members in the Spring Creek Mesa area: the lower is the Salt Wash member and the upper is the Brusby Basin member. All of the large uranium-bearing deposits discovered by the Geological Survey drilling in the Spring Creek Mesa area are in a series of coalescing sandstone lenses in the uppermost part of the Salt Wash member of the Morrison formation. Most of the ore deposits are believed to be irregular tabular or lens-shaped masses and probably lie parallel to the bedding, although in detail, they may crosscut the bedding. Also, ore deposits that take the form of narrow elongate concretionary-like structures, locally called “rolls”, may be present in the Spring Creek Mesa area. The mineralized material consists mostly of sandstone which has been selectively impregnated and in part replaced by uranium and vanadium minerals. Also, rich concentrations of uranium and vanadium are commonly associated with thin mudstone seams, beds of mudstone pebbles, and carbonaceous material of various types. Two suites of ore minerals are present in the ore deposits - - an oxidized suite of secondary uranium and vanadium minerals and a relatively unoxidized suite of “primary” uranium and vanadium minerals.</p>\n<br/>\n<p>The following geologic criteria are useful as guides to ore in the Spring Creek Mesa area:</p>\n<p>1. Large ore deposits generally occur where the “ore-bearing sandstone” is more than 40 feet thick.</p>\n<p>2. The color of the mudstone associated with the “ore-bearing sandstone” in the vicinity of large ore deposits is commonly gray instead of the usual red.</p>\n<p>3. The “ore-bearing sandstone” is normally a light red, but in the vicinity of oxidized ore deposits it is light brown and in the vicinity of relatively unoxidized ore deposits it is gray.</p>\n<p>4. The “ore-bearing sandstone” in the vicinity of relatively unoxidized ore deposits commonly contains sparse to abundant disseminated pyrite. In the vicinity of oxidized deposits it commonly contains abundant limonite spots and widespread limonite staining.</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/tei343","collaboration":"This report concerns work done on behalf of the Division of Raw Materials of the U.S. Atomic Energy Commission","usgsCitation":"Roach, C.H., 1954, Exploration for uranium deposits in the Spring Creek Mesa area, Montrose County, Colorado: U.S. Geological Survey Trace Elements Investigations 343, Report: 55 p.; 2 Plates: 24.57 x 36.66 inches and 42.16 x 28.38 inches, https://doi.org/10.3133/tei343.","productDescription":"Report: 55 p.; 2 Plates: 24.57 x 36.66 inches and 42.16 x 28.38 inches","numberOfPages":"56","costCenters":[],"links":[{"id":284081,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/tei343.jpg"},{"id":285793,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/tei/0343/figure-2.pdf"},{"id":285794,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/tei/0343/figure-3.pdf"},{"id":285795,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/tei/0343/report.pdf"}],"country":"United States","state":"Colorado","county":"Montrose County","otherGeospatial":"Spring Creek Mesa","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -109.060256,38.151752 ], [ -109.060256,38.667801 ], [ -107.498924,38.667801 ], [ -107.498924,38.151752 ], [ -109.060256,38.151752 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"53559434e4b0120853e8bf6e","contributors":{"authors":[{"text":"Roach, Carl Houston","contributorId":103295,"corporation":false,"usgs":true,"family":"Roach","given":"Carl","email":"","middleInitial":"Houston","affiliations":[],"preferred":false,"id":284094,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":70268054,"text":"70268054 - 1954 - The volcano letter: A weekly news leaflet of the Hawaiian Volcano Research Association - 1954","interactions":[{"subject":{"id":70268054,"text":"70268054 - 1954 - The volcano letter: A weekly news leaflet of the Hawaiian Volcano Research Association - 1954","indexId":"70268054","publicationYear":"1954","noYear":false,"title":"The volcano letter: A weekly news leaflet of the Hawaiian Volcano Research Association - 1954"},"predicate":"IS_PART_OF","object":{"id":70246900,"text":"70246900 - 1925 - The volcano letter: A weekly news leaflet of the Hawaiian Volcano Research Association","indexId":"70246900","publicationYear":"1925","noYear":false,"title":"The volcano letter: A weekly news leaflet of the Hawaiian Volcano Research Association"},"id":1}],"isPartOf":{"id":70246900,"text":"70246900 - 1925 - The volcano letter: A weekly news leaflet of the Hawaiian Volcano Research Association","indexId":"70246900","publicationYear":"1925","noYear":false,"title":"The volcano letter: A weekly news leaflet of the Hawaiian Volcano Research Association"},"lastModifiedDate":"2025-06-20T13:42:36.261404","indexId":"70268054","displayToPublicDate":"1954-01-01T13:25:06","publicationYear":"1954","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":3,"text":"Organization Series"},"title":"The volcano letter: A weekly news leaflet of the Hawaiian Volcano Research Association - 1954","docAbstract":"<p>The Volcano Letter was an informal publication issued at irregular intervals by the Hawaiian Volcano Observatory (HVO) during the years 1925 to 1955. Individual issues contain information on volcanic activity, volcano research, and volcano monitoring in Hawaii. Information on volcanic activity at other locations is also occasionally included.</p><p>The Volcano Letter was published by HVO through multiple changes in administration, including the Hawaiian Volcano Research Association (1925 to 1932), the U.S. Geological Survey (1932 to 1935), the Department of the Interior (1935 to 1938), and the University of Hawai‘i (1938 to 1955). Issues 1-262 were published weekly from January 1, 1925, to January 2, 1930, and consisted of a single page of text. Issues 263-384, also published weekly, from January 9, 1930, to May 5, 1932, were generally longer—four pages— and provided more detail on volcanic activity, including photographs, maps, and plots. Weekly issues 385-387, published May 12-26, 1932, were a single page of text due to budget reductions brought on by the Great Depression. Budget restrictions reduced the publishing frequency to monthly for issues 388-428, covering the period of June 1932 to October 1935; these issues were generally shorter, 1-2 pages, and sometimes featured figures. From November 1935 to July 1938, issues 429-461 remained monthly but increased in length (generally eight pages) and featured figures frequently. Issues 462-530, published over the period of August 1938 to December 1955, varied in length from 2-15 pages, but were published quarterly, rather than monthly.</p><p>Six of the Volcano Letters are misnumbered:<br>Jan. 21, 1926 number is 55 though it should 56<br>July 29, 1926 number is 82 though it should be 83<br>Feb. 16, 1928 number is 161 though it should be 164<br>May 31, 1928 number is 197 though it should be 179<br>Nov. 29, 1928 number is 204 though it should be 205</p>","language":"English","publisher":"Hawaiian Volcano Research Association","usgsCitation":"Hawaiian Volcano Research Association, 1954, The volcano letter: A weekly news leaflet of the Hawaiian Volcano Research Association - 1954, 37 p.","productDescription":"37 p.","costCenters":[{"id":336,"text":"Hawaiian Volcano 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,{"id":71342,"text":"tei292 - 1954 - Reconnaissance for radioactive deposits in eastern Alaska, 1952","interactions":[],"lastModifiedDate":"2014-05-27T12:40:11","indexId":"tei292","displayToPublicDate":"1954-01-01T13:16:00","publicationYear":"1954","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":"292","title":"Reconnaissance for radioactive deposits in eastern Alaska, 1952","docAbstract":"<p>Reconnaissance for radioactive deposits was conducted in selected areas of eastern Alaska during 1952. Examination of copper, silver, and molybdenum occurrences and of a reported nickel prospect in the Slana-Nabesna and Chisana districts in the eastern Alaska Range revealed a maximum radioactivity of about 0.003 percent equivalent uranium. No appreciable radioactivity anomolies were indicated by aerial and foot traverses in the area.</p>\n<br/>\n<p>Reconnaissance for possible lode concentrations of uranium minerals in the vicinity of reported fluoride occurrences in the Hope Creek and Miller House-Circle Hot Springs areas of the Circle quadrangle and in the Fortymile district found a maximum of 0.055 percent equivalent uranium in a float fragment of ferruginous breccia in the Hope Creek area; analysis of samples obtained in the vicinity of the other fluoride occurrences showed a maximum of only 0.005 percent equivalent uranium.</p>\n<br/>\n<p>No uraniferous loads were discovered in the Koyukuk-Chandalar region, nor was the source of the monazite, previously reported in the placer concentrates from the Chandalar mining district, located. The source of the uranotheorianite in the placers at Gold Bench on the South Fork of the Koyukuk River was not found during a brief reconaissance, but a placer concentrate was obtained that contains 0.18 percent equivalent uranium. This concentrate is about ten times more radioactive than concentrates previously available from the area.</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/tei292","collaboration":"This report concerns work done on behalf of the Division of Raw Materials of the U.S. Atomic Energy Commission","usgsCitation":"Nelson, A.E., West, W., and Matzko, J., 1954, Reconnaissance for radioactive deposits in eastern Alaska, 1952: U.S. Geological Survey Trace Elements Investigations 292, Report: 55 p.; 2 Plates: 14.70 x 13.76 inches and 13.37 x 11.30 inches, https://doi.org/10.3133/tei292.","productDescription":"Report: 55 p.; 2 Plates: 14.70 x 13.76 inches and 13.37 x 11.30 inches","numberOfPages":"56","temporalStart":"1952-01-01","temporalEnd":"1952-12-31","costCenters":[],"links":[{"id":283489,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/tei292.jpg"},{"id":284533,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/tei/0292/plate-1.pdf"},{"id":284534,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/tei/0292/plate-2.pdf"},{"id":284535,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/tei/0292/report.pdf"}],"country":"United States","state":"Alaska","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -149.84,61.34 ], [ -149.84,68.95 ], [ -139.66,68.95 ], [ -139.66,61.34 ], [ -149.84,61.34 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"53559531e4b0120853e8c18a","contributors":{"authors":[{"text":"Nelson, Arthur Edward","contributorId":39459,"corporation":false,"usgs":true,"family":"Nelson","given":"Arthur","email":"","middleInitial":"Edward","affiliations":[],"preferred":false,"id":284016,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"West, Walter S.","contributorId":32511,"corporation":false,"usgs":true,"family":"West","given":"Walter S.","affiliations":[],"preferred":false,"id":284015,"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":284017,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":70113714,"text":"tei125 - 1954 - Uranium deposits in the Eureka Gulch area, Central City district, Gilpin County, Colorado","interactions":[],"lastModifiedDate":"2014-07-14T11:16:16","indexId":"tei125","displayToPublicDate":"1954-01-01T11:52:00","publicationYear":"1954","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":"125","title":"Uranium deposits in the Eureka Gulch area, Central City district, Gilpin County, Colorado","docAbstract":"<p>The Eureka Gulch area of the Central City district, Gilpin County, Colo., was mined for ores of gold, silver, copper, lead, and zinc; but there has been little mining activity in the area since World War I. Between 1951 and 1953 nine radioactive mine dumps were discovered in the area by the U.S. Geological Survey and by prospectors. the importance of the discoveries has not been determined as all but one of the mines are inaccessible, but the distribution, quantity, and grade of the radioactive materials found on the mine dumps indicate that the area is worth of additional exploration as a possible source of uranium ore.</p>\n<br>\n<p>The uranium ans other metals are in and near steeply dipping mesothermal veins of Laramide age intrusive rocks. Pitchblende is present in at least four veins, and metatorbernite, associated at places with kosolite, is found along two veins for a linear distance of about 700 feet. The pitchblends and metatorbernite appear to be mutually exclusive and seem to occur in different veins. Colloform grains of pitchblende were deposited in the vein essentially contemporaneously with pyrite. The pitchblende is earlier in the sequence of deposition than galena and sphalerite. The metatorbernite replaces altered biotite-quartz-plagioclase gneiss and altered amphibolite, and to a lesser extent forms coatings on fractures in these rocks adjacent to the veins; the kasolite fills vugs in highly altered material and in altered wall rocks. Much of the pitchblende found on the dumps has been partly leached subsequent to mining and is out of equilibrium. Selected samples of metatorbernite-bearing rock from one mine dump contain as much as 6.11 percent uranium.</p>\n<br>\n<p>The pitchblende is a primary vein mineral deposited from uranium-bearing hydrothermal solutions. The metatorbernite probably formed by oxidation, solution, and transportation of uranium from primary pitchblende, but it may be a primary mineral deposited directly from fluids of different composition from these that deposited pitchblende.</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/tei125","collaboration":"This report concerns work done on behalf of the Division of Raw Materials of the U.S Atomic Energy Commission","usgsCitation":"Sims, P., Osterwald, F.W., and Tooker, E.W., 1954, Uranium deposits in the Eureka Gulch area, Central City district, Gilpin County, Colorado: U.S. Geological Survey Trace Elements Investigations 125, Report: 52 p.; 2 Plates: 21.75 x 11.51 inches and 20.29 x 12.76 inches, https://doi.org/10.3133/tei125.","productDescription":"Report: 52 p.; 2 Plates: 21.75 x 11.51 inches and 20.29 x 12.76 inches","numberOfPages":"53","costCenters":[],"links":[{"id":289895,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":289892,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/tei/0125/figure-2.pdf"},{"id":289893,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/tei/0125/figure-3.pdf"},{"id":289894,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/tei/0125/report.pdf"}],"country":"United States","state":"Colorado","county":"Gilpin County","otherGeospatial":"Eureka Gulch Area","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -105.55,39.75 ], [ -105.55,39.8 ], [ -105.5,39.8 ], [ -105.5,39.75 ], [ -105.55,39.75 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"53ae788ee4b0abf75cf2d899","contributors":{"authors":[{"text":"Sims, P.K.","contributorId":30191,"corporation":false,"usgs":true,"family":"Sims","given":"P.K.","email":"","affiliations":[],"preferred":false,"id":495172,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Osterwald, F. W.","contributorId":46950,"corporation":false,"usgs":true,"family":"Osterwald","given":"F.","email":"","middleInitial":"W.","affiliations":[],"preferred":false,"id":495173,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Tooker, E. W.","contributorId":102071,"corporation":false,"usgs":true,"family":"Tooker","given":"E.","email":"","middleInitial":"W.","affiliations":[],"preferred":false,"id":495174,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":71938,"text":"tem866 - 1954 - Economic geology of the aluminum phosphate zone on property owned by the Armour Fertilizer Works, land-pebble phosphate district, Florida","interactions":[],"lastModifiedDate":"2014-07-16T11:53:09","indexId":"tem866","displayToPublicDate":"1954-01-01T11:51:29","publicationYear":"1954","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":"866","title":"Economic geology of the aluminum phosphate zone on property owned by the Armour Fertilizer Works, land-pebble phosphate district, Florida","docAbstract":"No abstract available.","language":"English","publisher":"U.S. Department of the Interior, Geological Survey","publisherLocation":"Washington, D.C.","doi":"10.3133/tem866","collaboration":"Performed for the Division of Raw Materials, U.S. Atomic Energy Commission.","usgsCitation":"Cathcart, J.B., McGreevy, L.J., and Coleman, A., 1954, Economic geology of the aluminum phosphate zone on property owned by the Armour Fertilizer Works, land-pebble phosphate district, Florida: U.S. Geological Survey Trace Elements Memorandum 866, 14 p., https://doi.org/10.3133/tem866.","productDescription":"14 p.","numberOfPages":"14","costCenters":[],"links":[{"id":290277,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"}],"country":"United States","state":"Florida","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -87.6349,24.5211 ], [ -87.6349,31.001 ], [ -80.0311,31.001 ], [ -80.0311,24.5211 ], [ -87.6349,24.5211 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"53c79eebe4b019484164242d","contributors":{"authors":[{"text":"Cathcart, James Bachelder","contributorId":19540,"corporation":false,"usgs":true,"family":"Cathcart","given":"James","email":"","middleInitial":"Bachelder","affiliations":[],"preferred":false,"id":284909,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"McGreevy, Laurence James","contributorId":33797,"corporation":false,"usgs":true,"family":"McGreevy","given":"Laurence","email":"","middleInitial":"James","affiliations":[],"preferred":false,"id":284910,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Coleman, A.M.","contributorId":15531,"corporation":false,"usgs":true,"family":"Coleman","given":"A.M.","email":"","affiliations":[],"preferred":false,"id":284908,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":70048727,"text":"tem695 - 1954 - Geology of the Egnar quadrangle, Dolores and San Miguel counties, Colorado","interactions":[],"lastModifiedDate":"2014-03-04T14:21:07","indexId":"tem695","displayToPublicDate":"1954-01-01T11:46:00","publicationYear":"1954","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":"695","title":"Geology of the Egnar quadrangle, Dolores and San Miguel counties, Colorado","docAbstract":"The Egnar quadrangle is one of eighteen 7 1/2-minute quadrangles covering the principal carnotite-producing area of southwestern Colorado. The geology of these quadrangles was mapped by the U.S. Geological Survey for the Atomic Energy Commission as part of a comprehensive study of carnotite deposits. The rocks exposed in the eighteen quadrangles consist of crystalline rocks of pre-Cambrian age and sedimentary rocks that range in age from late Paleozoic to Quaternary. Over much of the area the sedimentary rocks are flat lying, but in places the rocks are disrupted by hih-angle faults, and northwest-trending folds. Conspicuous among the folds are large anticlines having cores of intrusive salt and gypsum. Most of the carnotite deposits are confined to the Salt Wash sandstone member of Jurassic Morrison formation. Within this sandstone, most of the deposits are spottily distributed through an arcuate zone known as \"Uruvan Mineral Belt\". Individual deposits range in size from irregular masses containing only a few tons of ore to large, tabular masses containing many thousands of tons. The ore consists largely of sandstone selectively impregnated and in part replaced by uranium and vanadium minerals. Most of the deposits appear to be related to certain sedimentary structures in sandstones of favorable composition.","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/tem695","collaboration":"This report concerns work done partly on behalf of the Division of Raw Materials of the U.S. Atomic Energy Commission","usgsCitation":"Cater, F.W., Bush, A., and Bell, H., 1954, Geology of the Egnar quadrangle, Dolores and San Miguel counties, Colorado: U.S. Geological Survey Trace Elements Memorandum 695, Report: 25 p.; 1 Plate: 34.63 x 28.48 inches, https://doi.org/10.3133/tem695.","productDescription":"Report: 25 p.; 1 Plate: 34.63 x 28.48 inches","numberOfPages":"28","additionalOnlineFiles":"Y","costCenters":[],"links":[{"id":278604,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/tem/0695/report-thumb.jpg"},{"id":283319,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/tem/0695/plate-1.pdf"},{"id":283320,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/tem/0695/report.pdf"}],"country":"United States","state":"Colorado","county":"Dolores County;San Miguel County","otherGeospatial":"Egnar Quadrangle","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -109.0,37.875 ], [ -109.0,38.0 ], [ -108.875,38.0 ], [ -108.875,37.875 ], [ -109.0,37.875 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"52737beae4b097f32ac3db27","contributors":{"authors":[{"text":"Cater, Fred W. Jr.","contributorId":36988,"corporation":false,"usgs":true,"family":"Cater","given":"Fred","suffix":"Jr.","email":"","middleInitial":"W.","affiliations":[],"preferred":false,"id":485494,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Bush, A.L.","contributorId":70404,"corporation":false,"usgs":true,"family":"Bush","given":"A.L.","email":"","affiliations":[],"preferred":false,"id":485496,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Bell, Henry III","contributorId":37710,"corporation":false,"usgs":true,"family":"Bell","given":"Henry","suffix":"III","email":"","affiliations":[],"preferred":false,"id":485495,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":76955,"text":"tem861 - 1954 - A bibliography of phosphate deposits in southeastern United States","interactions":[],"lastModifiedDate":"2014-07-16T11:40:00","indexId":"tem861","displayToPublicDate":"1954-01-01T11:38:00","publicationYear":"1954","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":"861","title":"A bibliography of phosphate deposits in southeastern United States","docAbstract":"No abstract available.","language":"English","publisher":"U.S. Department of the Interior, Geological Survey","publisherLocation":"Washington, D.C.","doi":"10.3133/tem861","usgsCitation":"Ketner, K., 1954, A bibliography of phosphate deposits in southeastern United States: U.S. Geological Survey Trace Elements Memorandum 861, 21 p., https://doi.org/10.3133/tem861.","productDescription":"21 p.","numberOfPages":"21","costCenters":[],"links":[{"id":290273,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"53c79ee0e4b0194841642412","contributors":{"authors":[{"text":"Ketner, Keith Brindley","contributorId":18332,"corporation":false,"usgs":true,"family":"Ketner","given":"Keith Brindley","affiliations":[],"preferred":false,"id":288211,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
]}