{"pageNumber":"6997","pageRowStart":"174900","pageSize":"25","recordCount":184733,"records":[{"id":70048214,"text":"tei353 - 1954 - Thorium and rare earth minerals in the Powderhorn district, Gunnison County, Colorado","interactions":[],"lastModifiedDate":"2014-06-19T06:31:20","indexId":"tei353","displayToPublicDate":"1990-01-09T10:20:00","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":"353","title":"Thorium and rare earth minerals in the Powderhorn district, Gunnison County, Colorado","docAbstract":"<p>Thorium has been found since 1949 in at least 33 deposits in an area 6 miles wide and 20 miles long in the Powderhorn district, Gunnison County, Colo. The district is composed largely of pre-Jurassic metamorphic and igneous rocks, which are chiefly if not entirely pre-Cambrian in age. The metamorphic and igneous rocks are overlain by sandstone of the Morrison formation of Jurassic age, and by volcanic rocks of the Alboroto group and Hinsdale formation of Miocene and Pliocene (?) age, respectively.</p>\n<br>\n<p>The thorium deposits occur in or near alkalic igneous rocks in which such elements as titanium, rare earths, barium, strontium, and niobium occur in greater-than-average amounts. The greatest mass of the alkalic igneous rocks the Iron Hill composite stoc,- occupies an area of 12 square miles in the southeastern part of the district. The age of the thorium deposits, like that of the alkalic igneous rocks, is not known other than pre-Jurassic.</p> \n<br>\n<p>The thorium veins and mineralized shear zones range from a few inches to 18 feet in thickness and from a few feet to 3,500 feet in length. The veins are composed of calcite,.dolomite, siderite, ankerite, quartz, barite, pyrite, sphalerite, galena, goethite,. apatite, alkali feldspar, and many other minerals. The thorium occurs at least partly in thorite or hydrothorite. Sparse xenotime has been tentatively identified in one deposit. Several minerals containing rare earths of the cerium group as major constituents are found in carbonate veins near Iron Hill. Bastnaesite has been identified by X-ray methods, and cerite and synchisite are probably present also.The fluorapatite in some veins and in parts of the carbonate rock mass that occupies 2 square miles in the central part of the Iron Hill complex contains rare earths of the cerium group, generally in amounts of a fraction of a percent of the rock.</p> \n<br>\n<p>The radioactivity of the deposits appears to be due almost entirely to thorium and its daughter products The ThO<sub>2</sub> content of selected highgrade samples from the Little Johnnie vein is as much as 4 percent. The ThO<sub>2</sub> content of the veins is generally less than 1 percent, however, and is only 0.05 to 0.1 percent in many of the veins studied.</p> \n<br>\n<p>The little Johnnie vein, which was mapped in detail, can be traced discontinuously for a distance of more than 3,500 feet. The thoriumbearing material occurs as irregular veinlets and thin films introduced into the fault zone. The mineralized shear zone ranges from less than 6 inches to 5 feet in thickness. Near its west end the vein is broken by many faults in a zone that marks the edge of a roughly circular fault block, 1<sub>1/2.</sub>miles in diameter, that has dropped 1,000 feet or more since the deposition of Miocene volcanic-rocks that now floor the Milkranch basin.</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/tei353","collaboration":"This report concerns work done on behalf of the Division of Raw Materials of the U.S. Atomic Energy Commission","usgsCitation":"Olson, J.C., and Wallace, S., 1954, Thorium and rare earth minerals in the Powderhorn district, Gunnison County, Colorado: U.S. Geological Survey Trace Elements Investigations 353, Report: 58 p.; 2 Plates: 20.93 x 11.91 inches and 9.29 x 11.96 inches, https://doi.org/10.3133/tei353.","productDescription":"Report: 58 p.; 2 Plates: 20.93 x 11.91 inches and 9.29 x 11.96 inches","numberOfPages":"58","additionalOnlineFiles":"Y","costCenters":[],"links":[{"id":288854,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":288851,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/tei/0353/figure-2.pdf"},{"id":288852,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/tei/0353/figure-3.pdf"},{"id":288853,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/tei/0353/report.pdf"}],"country":"United States","state":"Colorado","county":"Gunnison County","otherGeospatial":"Powderhorn District","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -109.0603,36.9924 ], [ -109.0603,41.0024 ], [ -102.0416,41.0024 ], [ -102.0416,36.9924 ], [ -109.0603,36.9924 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"523979fde4b04b9308ae4fbc","contributors":{"authors":[{"text":"Olson, Jerry C.","contributorId":89202,"corporation":false,"usgs":true,"family":"Olson","given":"Jerry","email":"","middleInitial":"C.","affiliations":[],"preferred":false,"id":484022,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Wallace, Stewart R.","contributorId":53371,"corporation":false,"usgs":true,"family":"Wallace","given":"Stewart R.","affiliations":[],"preferred":false,"id":484021,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":70173589,"text":"70173589 - 1954 - The quality and character of Pacific Northwest waters","interactions":[],"lastModifiedDate":"2016-06-21T14:05:03","indexId":"70173589","displayToPublicDate":"1959-12-31T00:00:00","publicationYear":"1954","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":6,"text":"USGS Unnumbered Series"},"seriesTitle":{"id":375,"text":"Open-File Report","active":false,"publicationSubtype":{"id":6}},"title":"The quality and character of Pacific Northwest waters","docAbstract":"<p>This paper is a general discussion of the quality and chemical character of surface and ground waters in the Pacific Northwest as shown by the available data. Previous quality of water studies reported in the literature are reviewed. The composition of natural waters is considered as to the source and significance of the different mineral constituents. Analytical data are presented showing mineral constituents and physical properties of selected surface and ground waters in the region.</p>","conferenceTitle":"Pacific Northwest Metals and Minerals Conference, American Mining and Metallurgical Engineers","conferenceDate":"April 30, 1954","conferenceLocation":"Portland, OR","language":"English","publisher":"U.S. Government Printing Office","publisherLocation":"Washington, D.C.","doi":"10.3133/70173589","usgsCitation":"Swenson, H.A., 1954, The quality and character of Pacific Northwest waters: Open-File Report, 9 p., https://doi.org/10.3133/70173589.","productDescription":"9 p.","numberOfPages":"18","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[{"id":518,"text":"Oregon Water Science Center","active":true,"usgs":true}],"links":[{"id":323087,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/70173589.jpg"},{"id":324137,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/unnumbered/70173589/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"5757f064e4b04f417c24dd28","contributors":{"authors":[{"text":"Swenson, Herbert A.","contributorId":93461,"corporation":false,"usgs":true,"family":"Swenson","given":"Herbert","email":"","middleInitial":"A.","affiliations":[],"preferred":false,"id":637377,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":71522,"text":"tei496 - 1954 - Germanium and uranium in coalified wood from Upper Devonian black shale","interactions":[],"lastModifiedDate":"2014-05-27T14:34:26","indexId":"tei496","displayToPublicDate":"1955-01-01T14:39:00","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":"496","title":"Germanium and uranium in coalified wood from Upper Devonian black shale","docAbstract":"<p>Microscopic study of black, vitreous, carbonaceous material occurring in the Chattanooga shale in Tennessee and in the Cleveland member of the Ohio shale in Ohio has revealed coalified woody plant tissue. Some samples have shown sufficient detail to be identified with the genus Callixylon. Similar material has been reported in the literature as \"bituminous\" or \"asphaltic\" stringers.</p>\n<br/>\n<p>Spectrographic analyses of the ash from the coalified wood have shown unusually high percentages of germanium, uranium, vanadium, and nickel. The inverse relationship between uranium and germanium in the ash and the ash content of various samples shows an association of these elements with the organic constituents of the coal.</p>\n<br/>\n<p>On the basis of geochemical considerations, it seems most probable that the wood or coalified wood was germanium-bearing at the time logs or woody fragments were floated into the basins of deposition of the Chattanooga shale and the Cleveland member of the Ohio shale. Once within the marine environment, the material probably absorbed uranium with the formation of organo-uranium compounds such as have been found to exist in coals.</p>\n<br/>\n<p>It is suggested that a more systematic search for germaniferous coals in the vicinity of the Chattanooga shale and the Cleveland member of the Ohio shale might be rewarding.</p>","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Reston, VA","doi":"10.3133/tei496","collaboration":"This report concerns work done on behalf of the Division of Raw Materials of the U.S. Atomic Energy Commission","usgsCitation":"Breger, I., and Schopf, J., 1954, Germanium and uranium in coalified wood from Upper Devonian black shale: U.S. Geological Survey Trace Elements Investigations 496, 13 p., https://doi.org/10.3133/tei496.","productDescription":"13 p.","costCenters":[],"links":[{"id":284572,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/tei/0496/report.pdf"},{"id":284573,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/tei/0496/report-thumb.jpg"}],"scale":"100000","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"5355946fe4b0120853e8bfdc","contributors":{"authors":[{"text":"Breger, Irving A.","contributorId":41901,"corporation":false,"usgs":true,"family":"Breger","given":"Irving A.","affiliations":[],"preferred":false,"id":284318,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Schopf, James M.","contributorId":94297,"corporation":false,"usgs":true,"family":"Schopf","given":"James M.","affiliations":[],"preferred":false,"id":284319,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":70111703,"text":"tei229 - 1954 - Radioactive deposits in California","interactions":[],"lastModifiedDate":"2014-06-19T06:25:32","indexId":"tei229","displayToPublicDate":"1955-01-01T12:50:00","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":"229","title":"Radioactive deposits in California","docAbstract":"<p>Reconnaissance examination by Government geologists of many areas, mine properties, and prospects in California during the period between 1948 and 1953 has confirmed the presence of radioactive materials in place at more than 40 localities. Abnormal radioactivity at these localities is due to concentrations of primary and secondary uranium minerals, to radon gas, radium (?), and to thorium minerals. Of the known occurrences only three were thought to contain uranium oxide (uranitite or pitchblende), 4 contained uranium-bearing columbate, tantalate, or titanate minerals, 12 contained secondary uranium minerals, such as autunite, carnotite, and torbernite, one contained radon gas, 7 contained thorium minerals, and, at the remaining 16 localities, the source of the anomalous radiation was not positively determined.</p>\n<br/>\n<p>The occurrences in which uranium oxide has been tentatively identified include the Rathgeb mine (Calaveras County), the Yerih group of claims (San Bernardino County), and the Rainbow claim (Madera County). Occurrences of secondary uranium minerals are largely confined to the arid desert regions of south-eastern California including deposits in San Bernardino, Kern, Inyo, and Imperial Counties. Uranium-bearing columbate, tantalate, or titanate minerals have been reported from pegmatite and granitic rock in southeastern and eastern California.</p>\n<br/>\n<p>Thorium minerals have been found in vein deposits in eastern San Bernardino County and from pegmatites and granitic rocks in various parts of southeastern California; placer concentrations of thorium minerals are known from nearly all areas in the State that are underlain, in part, by plutonic crystalline rocks.</p>\n<br/>\n<p>The primary uranium minerals occur principally as minute accessory crystals in pegmatite or granitic rock, or with base-metal sulfide minerals in veins. Thorium minerals also occur as accessory crystals in pegmatite or granitic rock, in placer deposits derived from such rock, and, at Mountain Pass, in veins containing rare earths. Secondary uranium minerals have been found as fracture coatings and as disseminations in various types of wall rock, although they are largely confined to areas of Tertiary volcanic rocks. Probably the uranium in the uraniferous deposits in California is related genetically to felsic crystalline rocks and felsic volcanic rocks; the present distribution of the secondary uranium minerals has been controlled, in part, by circulating ground waters and probably, in part, by magmatic waters related to the Tertiary volcanic activity. The thorium minerals are genetically related to the intrusion of pegmatite and plutonic crystalline rocks.</p>\n<br/>\n<p>None of the known deposits of radioactive minerals in California contain marketable reserves of uranium or thorium ore under economic conditions existing in 1952. With a favorable local market small lots of uranium ore may be available in the following places: the Rosamund prospect, the Rafferty and Chilson properties, the Lucky Star claim, and the Yerih group. The commercial production of thorium minerals will be possible, in the near future, only if these minerals can be recovered cheaply as a byproduct either from the mining of rare earths minerals at Mountain Pass or as a byproduct of placer mining for gold.</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/tei229","collaboration":"This report concerns work done on behalf of the Division of Raw Materials of the U.S. Atomic Energy Commission.","usgsCitation":"Walker, G.W., and Lovering, T., 1954, Radioactive deposits in California: U.S. Geological Survey Trace Elements Investigations 229, Report: 69 p.; Plate: 15.74 x 19.77 inches, https://doi.org/10.3133/tei229.","productDescription":"Report: 69 p.; Plate: 15.74 x 19.77 inches","numberOfPages":"78","additionalOnlineFiles":"Y","costCenters":[],"links":[{"id":288850,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":288848,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/tei/0229/plate-1.pdf"},{"id":288849,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/tei/0229/report.pdf"}],"country":"United States","state":"California","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -124.41,32.53 ], [ -124.41,42.01 ], [ -114.13,42.01 ], [ -114.13,32.53 ], [ -124.41,32.53 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"53ae77fde4b0abf75cf2c688","contributors":{"authors":[{"text":"Walker, George W.","contributorId":101308,"corporation":false,"usgs":true,"family":"Walker","given":"George","email":"","middleInitial":"W.","affiliations":[],"preferred":false,"id":494447,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Lovering, Tom G.","contributorId":31679,"corporation":false,"usgs":true,"family":"Lovering","given":"Tom G.","affiliations":[],"preferred":false,"id":494446,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":70207417,"text":"70207417 - 1954 - Geology of the iron deposits of the Congonhas District, Minas Gerais, Brazil","interactions":[],"lastModifiedDate":"2019-12-19T08:57:08","indexId":"70207417","displayToPublicDate":"1954-12-31T08:53:29","publicationYear":"1954","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":3338,"text":"Science","active":true,"publicationSubtype":{"id":10}},"title":"Geology of the iron deposits of the Congonhas District, Minas Gerais, Brazil","docAbstract":"<p>No abstract available.&nbsp;</p>","language":"English","doi":"10.1126/science.119.3096.616","issn":"00368075","usgsCitation":"Guild, P.W., 1954, Geology of the iron deposits of the Congonhas District, Minas Gerais, Brazil: Science, v. 119, no. 3096, p. 616-616, https://doi.org/10.1126/science.119.3096.616.","productDescription":"1 p. ","startPage":"616","endPage":"616","costCenters":[],"links":[{"id":370458,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"Brazil","geographicExtents":"{\"type\":\"FeatureCollection\",\"features\":[{\"type\":\"Feature\",\"geometry\":{\"type\":\"Polygon\",\"coordinates\":[[[-57.62513,-30.21629],[-56.2909,-28.85276],[-55.16229,-27.88192],[-54.49073,-27.47476],[-53.64874,-26.92347],[-53.62835,-26.12487],[-54.13005,-25.54764],[-54.62529,-25.73926],[-54.42895,-25.16218],[-54.29348,-24.5708],[-54.29296,-24.02101],[-54.65283,-23.83958],[-55.0279,-24.00127],[-55.40075,-23.95694],[-55.51764,-23.572],[-55.61068,-22.65562],[-55.79796,-22.35693],[-56.47332,-22.0863],[-56.88151,-22.28215],[-57.93716,-22.09018],[-57.87067,-20.73269],[-58.16639,-20.1767],[-57.8538,-19.97],[-57.95,-19.4],[-57.67601,-18.96184],[-57.49837,-18.17419],[-57.73456,-17.55247],[-58.2808,-17.27171],[-58.38806,-16.87711],[-58.24122,-16.29957],[-60.15839,-16.25828],[-60.54297,-15.09391],[-60.25115,-15.07722],[-60.26433,-14.64598],[-60.4592,-14.35401],[-60.5033,-13.77595],[-61.08412,-13.47938],[-61.7132,-13.4892],[-62.12708,-13.19878],[-62.80306,-13.00065],[-63.1965,-12.62703],[-64.31635,-12.46198],[-65.40228,-11.56627],[-65.3219,-10.89587],[-65.44484,-10.51145],[-65.33844,-9.76199],[-66.64691,-9.93133],[-67.1738,-10.30681],[-68.04819,-10.71206],[-68.27125,-11.01452],[-68.78616,-11.03638],[-69.52968,-10.95173],[-70.09375,-11.12397],[-70.54869,-11.00915],[-70.48189,-9.49012],[-71.30241,-10.07944],[-72.18489,-10.0536],[-72.56303,-9.52019],[-73.22671,-9.46221],[-73.01538,-9.03283],[-73.57106,-8.42445],[-73.98724,-7.52383],[-73.7234,-7.341],[-73.72449,-6.9186],[-73.12003,-6.62993],[-73.21971,-6.08919],[-72.96451,-5.74125],[-72.89193,-5.27456],[-71.74841,-4.59398],[-70.92884,-4.40159],[-70.79477,-4.25126],[-69.89364,-4.29819],[-69.4441,-1.55629],[-69.42049,-1.12262],[-69.57707,-0.54999],[-70.02066,-0.18516],[-70.01557,0.54141],[-69.4524,0.70616],[-69.25243,0.60265],[-69.21864,0.98568],[-69.8046,1.08908],[-69.81697,1.71481],[-67.86857,1.69246],[-67.53781,2.03716],[-67.26,1.72],[-67.06505,1.13011],[-66.87633,1.25336],[-66.32577,0.72445],[-65.54827,0.78925],[-65.35471,1.09528],[-64.61101,1.32873],[-64.19931,1.49285],[-64.08309,1.91637],[-63.36879,2.2009],[-63.42287,2.41107],[-64.27,2.49701],[-64.40883,3.12679],[-64.36849,3.79721],[-64.81606,4.05645],[-64.62866,4.14848],[-63.88834,4.02053],[-63.0932,3.77057],[-62.80453,4.00697],[-62.08543,4.16212],[-60.96689,4.53647],[-60.60118,4.9181],[-60.73357,5.20028],[-60.21368,5.24449],[-59.98096,5.01406],[-60.111,4.57497],[-59.76741,4.4235],[-59.53804,3.9588],[-59.81541,3.6065],[-59.97452,2.75523],[-59.71855,2.24963],[-59.64604,1.78689],[-59.03086,1.3177],[-58.54001,1.26809],[-58.42948,1.46394],[-58.11345,1.5072],[-57.66097,1.68258],[-57.33582,1.94854],[-56.7827,1.86371],[-56.53939,1.89952],[-55.9957,1.81767],[-55.9056,2.022],[-56.07334,2.22079],[-55.97332,2.51036],[-55.56976,2.42151],[-55.09759,2.52375],[-54.52475,2.31185],[-54.08806,2.10556],[-53.77852,2.3767],[-53.55484,2.3349],[-53.41847,2.05339],[-52.93966,2.12486],[-52.55642,2.50471],[-52.24934,3.24109],[-51.6578,4.15623],[-51.31715,4.20349],[-51.06977,3.6504],[-50.50888,1.90156],[-49.97408,1.73648],[-49.9471,1.04619],[-50.69925,0.22298],[-50.38821,-0.07844],[-48.62057,-0.23549],[-48.5845,-1.23781],[-47.82496,-0.58162],[-46.56658,-0.94103],[-44.9057,-1.55174],[-44.41762,-2.13775],[-44.58159,-2.69131],[-43.41879,-2.38311],[-41.47266,-2.91202],[-39.97867,-2.87305],[-38.50038,-3.70065],[-37.22325,-4.82095],[-36.45294,-5.1094],[-35.5978,-5.1495],[-35.23539,-5.46494],[-34.89603,-6.73819],[-34.72999,-7.34322],[-35.12821,-8.9964],[-35.63697,-9.64928],[-37.04652,-11.04072],[-37.68361,-12.17119],[-38.42388,-13.03812],[-38.67389,-13.05765],[-38.95328,-13.79337],[-38.8823,-15.66705],[-39.16109,-17.20841],[-39.26734,-17.86775],[-39.58352,-18.2623],[-39.76082,-19.59911],[-40.77474,-20.90451],[-40.94476,-21.93732],[-41.75416,-22.37068],[-41.98828,-22.97007],[-43.0747,-22.96769],[-44.64781,-23.35196],[-45.35214,-23.79684],[-46.47209,-24.08897],[-47.64897,-24.8852],[-48.49546,-25.87702],[-48.641,-26.6237],[-48.47474,-27.17591],[-48.66152,-28.18613],[-48.88846,-28.67412],[-49.58733,-29.22447],[-50.69687,-30.98447],[-51.57623,-31.7777],[-52.25608,-32.24537],[-52.7121,-33.19658],[-53.37366,-33.76838],[-53.65054,-33.202],[-53.20959,-32.72767],[-53.78795,-32.04724],[-54.57245,-31.49451],[-55.60151,-30.85388],[-55.97324,-30.88308],[-56.97603,-30.10969],[-57.62513,-30.21629]]]},\"properties\":{\"name\":\"Brazil\"}}]}","volume":"119","issue":"3096","noUsgsAuthors":false,"publicationStatus":"PW","contributors":{"authors":[{"text":"Guild, P. W.","contributorId":39039,"corporation":false,"usgs":true,"family":"Guild","given":"P.","email":"","middleInitial":"W.","affiliations":[],"preferred":false,"id":777934,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":70197719,"text":"70197719 - 1954 - Tungsten in southeastern California: Chapter 8","interactions":[],"lastModifiedDate":"2023-06-07T18:27:54.517069","indexId":"70197719","displayToPublicDate":"1954-12-31T00:00:00","publicationYear":"1954","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":2,"text":"State or Local Government Series"},"seriesTitle":{"id":5710,"text":"California Division of Mines and Geology Bulletin","active":true,"publicationSubtype":{"id":2}},"seriesNumber":"170","title":"Tungsten in southeastern California: Chapter 8","docAbstract":"<p>No abstract available.</p>","largerWorkType":{"id":18,"text":"Report"},"largerWorkTitle":"Geology of southern California","language":"English","publisher":"California Division of Mines","usgsCitation":"Bateman, P.C., and Irwin, W., 1954, Tungsten in southeastern California: Chapter 8: California Division of Mines and Geology Bulletin 170, 10 p.","productDescription":"10 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,{"id":70010823,"text":"70010823 - 1954 - Avelinoite, a new hydrous sodium ferric phosphate mineral from Minas Gerais, Brazil","interactions":[],"lastModifiedDate":"2026-03-03T15:51:52.003258","indexId":"70010823","displayToPublicDate":"1954-12-24T00:00:00","publicationYear":"1954","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":3338,"text":"Science","active":true,"publicationSubtype":{"id":10}},"title":"Avelinoite, a new hydrous sodium ferric phosphate mineral from Minas Gerais, Brazil","docAbstract":"<p>No abstract available.</p>","language":"English","publisher":"American Association for the Advancement of Science","doi":"10.1126/science.120.3130.1074","issn":"00368075","usgsCitation":"Lindberg, M., and Pecora, W.T., 1954, Avelinoite, a new hydrous sodium ferric phosphate mineral from Minas Gerais, Brazil: Science, v. 120, no. 3130, p. 1074-1075, https://doi.org/10.1126/science.120.3130.1074.","productDescription":"2 p.","startPage":"1074","endPage":"1075","costCenters":[],"links":[{"id":218750,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"Brazil","otherGeospatial":"Minas Gerais","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"coordinates\": [\n          [\n            [\n              -46.86192993649934,\n              -17.032175049995274\n            ],\n            [\n              -46.86192993649934,\n              -20.174696829591767\n            ],\n            [\n              -42.667407376985835,\n              -20.174696829591767\n            ],\n            [\n              -42.667407376985835,\n              -17.032175049995274\n            ],\n            [\n              -46.86192993649934,\n              -17.032175049995274\n            ]\n          ]\n        ],\n        \"type\": \"Polygon\"\n      }\n    }\n  ]\n}","volume":"120","issue":"3130","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"5059ef53e4b0c8380cd4a1ca","contributors":{"authors":[{"text":"Lindberg, M.L.","contributorId":104033,"corporation":false,"usgs":true,"family":"Lindberg","given":"M.L.","email":"","affiliations":[],"preferred":false,"id":359729,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Pecora, W. T.","contributorId":96315,"corporation":false,"usgs":true,"family":"Pecora","given":"W.","email":"","middleInitial":"T.","affiliations":[],"preferred":false,"id":359728,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":70221435,"text":"70221435 - 1954 - Change of the isotopic abundance ratio within a sphere due to diffusion","interactions":[],"lastModifiedDate":"2021-06-15T18:39:26.488512","indexId":"70221435","displayToPublicDate":"1954-12-01T13:35:27","publicationYear":"1954","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":2171,"text":"Journal of Applied Physics","active":true,"publicationSubtype":{"id":10}},"title":"Change of the isotopic abundance ratio within a sphere due to diffusion","docAbstract":"<p>No abstract available.&nbsp;</p>","language":"English","publisher":"AIP","doi":"10.1063/1.1721618","usgsCitation":"Bracken, J., and Senftle, F.E., 1954, Change of the isotopic abundance ratio within a sphere due to diffusion: Journal of Applied Physics, v. 25, no. 2, p. 267-268, https://doi.org/10.1063/1.1721618.","productDescription":"2 p.","startPage":"267","endPage":"268","costCenters":[],"links":[{"id":480430,"rank":0,"type":{"id":41,"text":"Open Access External Repository Page"},"url":"https://digital.library.unt.edu/ark:/67531/metadc1050604/","text":"External Repository"},{"id":386507,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"25","issue":"2","noUsgsAuthors":false,"publicationStatus":"PW","contributors":{"authors":[{"text":"Bracken, J.T.","contributorId":260295,"corporation":false,"usgs":false,"family":"Bracken","given":"J.T.","email":"","affiliations":[],"preferred":false,"id":817697,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Senftle, F. E.","contributorId":47788,"corporation":false,"usgs":true,"family":"Senftle","given":"F.","email":"","middleInitial":"E.","affiliations":[],"preferred":false,"id":817698,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":70221434,"text":"70221434 - 1954 - 75th anniversary of the United States Geological Survey, March 3, 1954","interactions":[],"lastModifiedDate":"2021-06-15T18:25:30.571635","indexId":"70221434","displayToPublicDate":"1954-12-01T13:21:57","publicationYear":"1954","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":3338,"text":"Science","active":true,"publicationSubtype":{"id":10}},"title":"75th anniversary of the United States Geological Survey, March 3, 1954","docAbstract":"<p>No abstract available.&nbsp;</p>","language":"English","publisher":"AAAS","doi":"10.1126/science.119.3088.3a","usgsCitation":"Wrather, W., 1954, 75th anniversary of the United States Geological Survey, March 3, 1954: Science, v. 119, no. 3088, p. 3A-3A, https://doi.org/10.1126/science.119.3088.3a.","productDescription":"1 p.","startPage":"3A","endPage":"3A","costCenters":[],"links":[{"id":386506,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"119","issue":"3088","noUsgsAuthors":false,"publicationStatus":"PW","contributors":{"authors":[{"text":"Wrather, W.E.","contributorId":260294,"corporation":false,"usgs":false,"family":"Wrather","given":"W.E.","email":"","affiliations":[],"preferred":false,"id":817696,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":70221466,"text":"70221466 - 1954 - Criteria for the mode of emplacement of the alkaline stock at Mount Monadnock, Vermont","interactions":[],"lastModifiedDate":"2021-06-16T16:23:34.929682","indexId":"70221466","displayToPublicDate":"1954-12-01T11:18:48","publicationYear":"1954","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1786,"text":"Geological Society of America Bulletin","active":true,"publicationSubtype":{"id":10}},"title":"Criteria for the mode of emplacement of the alkaline stock at Mount Monadnock, Vermont","docAbstract":"<p><span>The&nbsp;</span>alkaline<span>&nbsp;</span>stock<span>&nbsp;</span>at<span>&nbsp;</span>Mount<span>&nbsp;</span>Monadnock<span>,&nbsp;</span>Vermont<span>, described briefly by Wolff (1929), has been restudied in detail. Its petrography and structure are discussed here and conclusions are drawn as to its&nbsp;</span>mode<span>&nbsp;of&nbsp;</span>emplacement<span>. The&nbsp;</span>stock<span>&nbsp;consists of plutonic and hypabyssal rocks which intrude folded Ordovician (?) schist and quartzite. The longer axis, trending north-northwest across the strike of the country rock, is 3 miles long, and the shorter one about 2 1/2 miles. Essentially the&nbsp;</span>stock<span>&nbsp;consists of quartz syenite, but it encloses a long arcuate mass of older essexite and transition rock, and along its eastern edge are later intrusions of granite. Late dikes of various compositions cut the plutonics and surrounding metamorphic rocks. The following facts have been established: (1) The igneous rocks are typical representatives of the White Mountain magma series (Mississippian?), quite lacking in foliation and lineation. (2) The&nbsp;</span>stock<span>&nbsp;is discordant and has an elliptical ground plan. (3) In detail the boundary is irregular and characterized by abundant dikes and xenoliths. (4) The igneous rocks make sharp contacts with the metamorphosed country rock. (5) The arcuate mass of older essexite is undoubtedly a screen. (6) The small bodies of late granite resemble ring dikes. (7) The&nbsp;</span>stock<span>&nbsp;is cut by prominent sets of steeply dipping radial and tangential joints. (8) The late dikes show radial and tangential patterns. (9) Along the northern and southern margins of the&nbsp;</span>stock<span>&nbsp;the country rock shows strikes and dips which differ from the regional ones. From these&nbsp;</span>criteria<span>&nbsp;it is concluded that the plutonic rocks have invaded the crust by cauldron subsidence accompanied by the stoping of large arcuate slabs and smaller blocks from the walls of the magma reservoir.</span></p>","language":"English","publisher":"Geological Society of America","doi":"10.1130/0016-7606(1954)65[97:CFTMOE]2.0.CO;2","usgsCitation":"Chapman, R.W., 1954, Criteria for the mode of emplacement of the alkaline stock at Mount Monadnock, Vermont: Geological Society of America Bulletin, v. 65, no. 2, p. 97-114, https://doi.org/10.1130/0016-7606(1954)65[97:CFTMOE]2.0.CO;2.","productDescription":"18 p.","startPage":"97","endPage":"114","costCenters":[],"links":[{"id":386546,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United  States","state":"Vermont","otherGeospatial":"Monadnock Mountain","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -71.806640625,\n              44.84223815129917\n            ],\n            [\n              -71.4825439453125,\n              44.84223815129917\n            ],\n            [\n              -71.4825439453125,\n              44.999767019181284\n            ],\n            [\n              -71.806640625,\n              44.999767019181284\n            ],\n            [\n              -71.806640625,\n              44.84223815129917\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","volume":"65","issue":"2","noUsgsAuthors":false,"publicationStatus":"PW","contributors":{"authors":[{"text":"Chapman, Randolph W.","contributorId":86057,"corporation":false,"usgs":true,"family":"Chapman","given":"Randolph","email":"","middleInitial":"W.","affiliations":[],"preferred":false,"id":817772,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":70221465,"text":"70221465 - 1954 - Age determinations of the San Gabriel Anorthosite Massif, California","interactions":[],"lastModifiedDate":"2021-06-16T16:17:55.851369","indexId":"70221465","displayToPublicDate":"1954-12-01T11:14:58","publicationYear":"1954","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1786,"text":"Geological Society of America Bulletin","active":true,"publicationSubtype":{"id":10}},"title":"Age determinations of the San Gabriel Anorthosite Massif, California","docAbstract":"<p>No abstract available.</p>","language":"English","publisher":"Geological Society of America","doi":"10.1130/0016-7606(1954)65[465:ADOTSG]2.0.CO;2","usgsCitation":"Neuerburg, G.J., and Gottfried, D., 1954, Age determinations of the San Gabriel Anorthosite Massif, California: Geological Society of America Bulletin, v. 65, no. 5, p. 465-466, https://doi.org/10.1130/0016-7606(1954)65[465:ADOTSG]2.0.CO;2.","productDescription":"2 p.","startPage":"465","endPage":"466","costCenters":[],"links":[{"id":386545,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"65","issue":"5","noUsgsAuthors":false,"publicationStatus":"PW","contributors":{"authors":[{"text":"Neuerburg, G. J.","contributorId":29395,"corporation":false,"usgs":true,"family":"Neuerburg","given":"G.","middleInitial":"J.","affiliations":[],"preferred":false,"id":817769,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Gottfried, David","contributorId":82295,"corporation":false,"usgs":true,"family":"Gottfried","given":"David","email":"","affiliations":[],"preferred":false,"id":817770,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":70221462,"text":"70221462 - 1954 - Correlation of reverse remanent magnetism and negative anomalies with certain minerals","interactions":[],"lastModifiedDate":"2021-06-17T10:34:47.913452","indexId":"70221462","displayToPublicDate":"1954-12-01T11:01:13","publicationYear":"1954","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":2310,"text":"Journal of Geomagnetism & Geoelectricity","active":true,"publicationSubtype":{"id":10}},"title":"Correlation of reverse remanent magnetism and negative anomalies with certain minerals","docAbstract":"<p>No abstract available.</p>","language":"English","publisher":"J Stage","doi":"10.5636/jgg.6.176","usgsCitation":"Balsley, J.R., and Buddington, A.F., 1954, Correlation of reverse remanent magnetism and negative anomalies with certain minerals: Journal of Geomagnetism & Geoelectricity, v. 6, no. 4, p. 176-181, https://doi.org/10.5636/jgg.6.176.","productDescription":"6 p.","startPage":"176","endPage":"181","costCenters":[],"links":[{"id":494117,"rank":0,"type":{"id":40,"text":"Open Access Publisher Index Page"},"url":"https://doi.org/10.5636/jgg.6.176","text":"Publisher Index Page"},{"id":386542,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"6","issue":"4","noUsgsAuthors":false,"publicationStatus":"PW","contributors":{"authors":[{"text":"Balsley, James R.","contributorId":10010,"corporation":false,"usgs":true,"family":"Balsley","given":"James","email":"","middleInitial":"R.","affiliations":[],"preferred":false,"id":817765,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Buddington, A. F.","contributorId":40211,"corporation":false,"usgs":true,"family":"Buddington","given":"A.","email":"","middleInitial":"F.","affiliations":[],"preferred":false,"id":817766,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":76951,"text":"tem867 - 1954 - Economic geology of the aluminum phosphate zone on property owned by the Royster Guano Company, land-pebble phosphate district, Florida","interactions":[],"lastModifiedDate":"2014-07-16T10:40:48","indexId":"tem867","displayToPublicDate":"1954-12-01T10:39:13","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":"867","title":"Economic geology of the aluminum phosphate zone on property owned by the Royster Guano Company, 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/tem867","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 Royster Guano Company, land-pebble phosphate district, Florida: U.S. Geological Survey Trace Elements Memorandum 867, 33 p., https://doi.org/10.3133/tem867.","productDescription":"33 p.","numberOfPages":"33","costCenters":[],"links":[{"id":290263,"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":"53c79eece4b019484164242f","contributors":{"authors":[{"text":"Cathcart, James Bachelder","contributorId":19540,"corporation":false,"usgs":true,"family":"Cathcart","given":"James","email":"","middleInitial":"Bachelder","affiliations":[],"preferred":false,"id":288202,"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":288203,"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":288201,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":76950,"text":"tem868 - 1954 - Economic geology of the aluminum phosphate zone on properties owned by the Virginia-Carolina Chemical Corporation, land-pebble phosphate district, Florida","interactions":[],"lastModifiedDate":"2014-07-16T10:37:30","indexId":"tem868","displayToPublicDate":"1954-12-01T10:36:10","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":"868","title":"Economic geology of the aluminum phosphate zone on properties owned by the Virginia-Carolina Chemical Corporation, 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/tem868","collaboration":"Performed for the Division of Raw Materials, U.S. Atomic Energy Commission.","usgsCitation":"Cathcart, J.B., Coleman, A., and McGreevy, L.J., 1954, Economic geology of the aluminum phosphate zone on properties owned by the Virginia-Carolina Chemical Corporation, land-pebble phosphate district, Florida: U.S. Geological Survey Trace Elements Memorandum 868, 58 p., https://doi.org/10.3133/tem868.","productDescription":"58 p.","numberOfPages":"58","costCenters":[],"links":[{"id":290261,"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":"53c79ee9e4b0194841642427","contributors":{"authors":[{"text":"Cathcart, James Bachelder","contributorId":19540,"corporation":false,"usgs":true,"family":"Cathcart","given":"James","email":"","middleInitial":"Bachelder","affiliations":[],"preferred":false,"id":288199,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Coleman, A.M.","contributorId":15531,"corporation":false,"usgs":true,"family":"Coleman","given":"A.M.","email":"","affiliations":[],"preferred":false,"id":288198,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"McGreevy, Laurence James","contributorId":33797,"corporation":false,"usgs":true,"family":"McGreevy","given":"Laurence","email":"","middleInitial":"James","affiliations":[],"preferred":false,"id":288200,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":76947,"text":"tem871 - 1954 - Economic geology of the aluminum phosphate zone on property owned by Wayne Thomas, land-pebble phosphate district, Florida","interactions":[],"lastModifiedDate":"2014-07-16T10:29:44","indexId":"tem871","displayToPublicDate":"1954-12-01T10:27:37","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":"871","title":"Economic geology of the aluminum phosphate zone on property owned by Wayne Thomas, 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/tem871","usgsCitation":"Cathcart, J.B., Coleman, A., and McGreevy, L.J., 1954, Economic geology of the aluminum phosphate zone on property owned by Wayne Thomas, land-pebble phosphate district, Florida: U.S. Geological Survey Trace Elements Memorandum 871, 29 p., https://doi.org/10.3133/tem871.","productDescription":"29 p.","numberOfPages":"29","costCenters":[],"links":[{"id":290258,"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":"53c79eeae4b0194841642429","contributors":{"authors":[{"text":"Cathcart, James Bachelder","contributorId":19540,"corporation":false,"usgs":true,"family":"Cathcart","given":"James","email":"","middleInitial":"Bachelder","affiliations":[],"preferred":false,"id":288193,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Coleman, A.M.","contributorId":15531,"corporation":false,"usgs":true,"family":"Coleman","given":"A.M.","email":"","affiliations":[],"preferred":false,"id":288192,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"McGreevy, Laurence James","contributorId":33797,"corporation":false,"usgs":true,"family":"McGreevy","given":"Laurence","email":"","middleInitial":"James","affiliations":[],"preferred":false,"id":288194,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":78606,"text":"tem729 - 1954 - Interim report on exploration in the La Sal Creek area, Paradox district, Montrose County, Colorado, and San Juan County, Utah","interactions":[],"lastModifiedDate":"2014-07-17T09:26:10","indexId":"tem729","displayToPublicDate":"1954-12-01T09:22:13","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":"729","title":"Interim report on exploration in the La Sal Creek area, Paradox district, Montrose County, Colorado, and San Juan County, Utah","docAbstract":"No abstract available.","language":"English","publisher":"U.S. Department of the Interior, Geological Survey","publisherLocation":"Washington, D.C.","doi":"10.3133/tem729","collaboration":"Performed for the Division of Raw Materials of the U.S. Atomic Energy Commission.","usgsCitation":"Carter, W.D., Warman, J.C., and Gualtieri, J.L., 1954, Interim report on exploration in the La Sal Creek area, Paradox district, Montrose County, Colorado, and San Juan County, Utah: U.S. Geological Survey Trace Elements Memorandum 729, 11 p., https://doi.org/10.3133/tem729.","productDescription":"11 p.","numberOfPages":"11","costCenters":[],"links":[{"id":290346,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"}],"country":"United States","state":"Colorado;Utah","county":"Montrose County;San Juan County","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -111.41,37.0 ], [ -111.41,38.5 ], [ -105.86,38.5 ], [ -105.86,37.0 ], [ -111.41,37.0 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"53cd62d0e4b0b290850fe6d3","contributors":{"authors":[{"text":"Carter, William Douglas","contributorId":93892,"corporation":false,"usgs":true,"family":"Carter","given":"William","email":"","middleInitial":"Douglas","affiliations":[],"preferred":false,"id":288978,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Warman, James C.","contributorId":74052,"corporation":false,"usgs":true,"family":"Warman","given":"James","email":"","middleInitial":"C.","affiliations":[],"preferred":false,"id":288977,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Gualtieri, James Louis","contributorId":46491,"corporation":false,"usgs":true,"family":"Gualtieri","given":"James","email":"","middleInitial":"Louis","affiliations":[],"preferred":false,"id":288976,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":70220058,"text":"70220058 - 1954 - The occurrence of cobalt and nickel in the Silver Summit Mine, Coeur d'Alene district, Idaho","interactions":[],"lastModifiedDate":"2021-04-16T20:42:38.621345","indexId":"70220058","displayToPublicDate":"1954-11-01T15:38:03","publicationYear":"1954","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1472,"text":"Economic Geology","active":true,"publicationSubtype":{"id":10}},"title":"The occurrence of cobalt and nickel in the Silver Summit Mine, Coeur d'Alene district, Idaho","docAbstract":"<p><span>Cobalt and nickel of possible commercial interest have been discovered in the Silver Summit mine, Coeur d'Alene district, Idaho. Assay data indicate that an ore shoot contained about 0.40 percent cobalt and about 1.0 percent nickel in addition to the copper and rich silver ores. The cobalt-nickel mineral gersdorffite occurs in tetrahedrite-siderite veins. Gersdorffite is widespread in small amounts and appears to have been the first of the \"ore shoot\" minerals. The known occurrence of either cobalt bloom or gersdorffite in other properties of the Coeur d'Alene district Silver Belt suggests that other ore shoots may exist that contain commercial quantities of cobalt and nickel.</span></p>","language":"English","publisher":"American Geological Institute","doi":"10.2113/gsecongeo.49.7.753","usgsCitation":"Fryklund, V.C., and Hutchinson, M.W., 1954, The occurrence of cobalt and nickel in the Silver Summit Mine, Coeur d'Alene district, Idaho: Economic Geology, v. 49, no. 7, p. 753-758, https://doi.org/10.2113/gsecongeo.49.7.753.","productDescription":"6 p.","startPage":"753","endPage":"758","costCenters":[],"links":[{"id":385185,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United  States","state":"Idaho","otherGeospatial":"Silver Summit Mine","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -116.89453125,\n              46.9502622421856\n            ],\n            [\n              -115.48828125000001,\n              46.9502622421856\n            ],\n            [\n              -115.48828125000001,\n              48.951366470947725\n            ],\n            [\n              -116.89453125,\n              48.951366470947725\n            ],\n            [\n              -116.89453125,\n              46.9502622421856\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","volume":"49","issue":"7","noUsgsAuthors":false,"publicationDate":"1954-11-01","publicationStatus":"PW","contributors":{"authors":[{"text":"Fryklund, Verne Charles Jr.","contributorId":104886,"corporation":false,"usgs":true,"family":"Fryklund","given":"Verne","suffix":"Jr.","email":"","middleInitial":"Charles","affiliations":[],"preferred":false,"id":814469,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Hutchinson, Murl W.","contributorId":257519,"corporation":false,"usgs":false,"family":"Hutchinson","given":"Murl","email":"","middleInitial":"W.","affiliations":[],"preferred":false,"id":814470,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":70217846,"text":"70217846 - 1954 - The White Pine copper deposit, Ontonagon County, Michigan","interactions":[],"lastModifiedDate":"2021-02-05T19:13:05.034899","indexId":"70217846","displayToPublicDate":"1954-11-01T13:09:12","publicationYear":"1954","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1472,"text":"Economic Geology","active":true,"publicationSubtype":{"id":10}},"title":"The White Pine copper deposit, Ontonagon County, Michigan","docAbstract":"<p><span>Copper, largely in the mineral chalcocite, is found in the lowermost beds of the Nonesuch shale over many square miles near White Pine, Ontonagon County, Mich. The Nonesuch shale, of late Keweenawan age, is about 600 feet thick and is composed largely of gray siltstone. It overlies 2,300 to 5,500 feet of red sandstones and conglomerates, the Copper Harbor conglomerate. This formation, in turn, overlies the middle Keweenawan Portage Lake lava series, in which occur the famous native-copper deposits of the south shore of Lake Superior. The White Pine mine is 45 to 70 miles west-southwest of the principal native copper mines.The copper-bearing beds at White Pine are primarily in the lower 20to 25 feet of the Nonesuch shale. This cupriferous zone is divided in local usage into four stratigraphic units, which are, in ascending order, the lower sandstone (the uppermost bed of the Copper Harbor conglomerate), the parting shale, the upper sandstone, and the upper shale. The sequence of beds is almost identical in the upper and parting shales, suggesting cyclic sedimentation. This sequence and the distribution of sedimentary facies are attributed to two submergences, separated by an emergence, of a deltaic area.Practically all the copper occurs in the upper and parting shales, except in a small area near the White Pine fault where it is abundant in the upper and lower sandstones. It is present in five different layers in amounts that average from 1 to 3 percent. The total amount of copper in each bed is generally higher where the bed is thick, and thickness, in turn, seems to be greatest in areas that were hollows away from the main channel or channels of the ancient delta. Copper content of the shale beds typically decreases as their sand content increases. The extent of individual copper-bearing beds 1 to 3 feet thick is measurable in square miles.The local occurrence of copper in the upper and lower sandstone beds can be reasonably explained as the result of hydrothermal transportation from the White Pine fault up the dip of the relatively permeable sandstone to the crest of an adjacent anticline. Distribution of copper in the parting and upper shales, on the other hand, seems to be completely independent of local structure, faults, and rock permeability. For the area as a whole the control is lithologic and stratigraphic. Probably the copper was dropped into or precipitated within the original mud; it may conceivably have replaced with exquisite detail something else that was so deposited.</span></p>","language":"English","publisher":"American Geological Institute","doi":"10.2113/gsecongeo.49.7.675","usgsCitation":"White, W.S., and Wright, J.C., 1954, The White Pine copper deposit, Ontonagon County, Michigan: Economic Geology, v. 49, no. 7, p. 675-716, https://doi.org/10.2113/gsecongeo.49.7.675.","productDescription":"42 p.","startPage":"675","endPage":"716","costCenters":[],"links":[{"id":383064,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United States","state":"Michigan","county":"Ontonagon County","geographicExtents":"{\"type\":\"FeatureCollection\",\"features\":[{\"type\":\"Feature\",\"geometry\":{\"type\":\"Polygon\",\"coordinates\":[[[-89.8875,46.7677],[-89.8767,46.7758],[-89.8441,46.8],[-89.822,46.8093],[-89.8188,46.8103],[-89.7952,46.8168],[-89.7769,46.8223],[-89.7624,46.8236],[-89.7433,46.8282],[-89.7156,46.8311],[-89.6904,46.8317],[-89.6891,46.8317],[-89.6686,46.8336],[-89.6533,46.8312],[-89.6282,46.8212],[-89.6163,46.8205],[-89.6065,46.8235],[-89.5953,46.827],[-89.5855,46.8295],[-89.5658,46.8336],[-89.5605,46.8347],[-89.5579,46.8347],[-89.5534,46.8376],[-89.5488,46.839],[-89.5434,46.8364],[-89.5282,46.8395],[-89.5191,46.8424],[-89.5112,46.8435],[-89.4944,46.8402],[-89.4837,46.8386],[-89.4705,46.8389],[-89.442,46.84],[-89.438,46.8405],[-89.4295,46.8421],[-89.4078,46.8462],[-89.4045,46.8472],[-89.3868,46.8531],[-89.3658,46.8581],[-89.3541,46.863],[-89.3449,46.8659],[-89.3319,46.8726],[-89.3097,46.8813],[-89.2987,46.8871],[-89.2855,46.8901],[-89.2653,46.8983],[-89.2359,46.9099],[-89.2203,46.918],[-89.2011,46.9349],[-89.1985,46.9368],[-89.196,46.9401],[-89.1877,46.9485],[-89.1851,46.9513],[-89.1768,46.9602],[-89.1717,46.9649],[-89.1567,46.9711],[-89.1491,46.9818],[-89.1433,46.9861],[-89.1355,46.9895],[-89.129,46.9937],[-89.1244,46.9947],[-89.1237,46.9947],[-89.119,46.9939],[-89.1134,46.9876],[-89.0847,46.9849],[-89.0828,46.9849],[-89.0768,46.986],[-89.0709,46.9875],[-89.0578,46.9923],[-89.0545,46.9937],[-89.0427,46.9981],[-89.0249,47.0016],[-89.0209,47.0022],[-89.022,46.9966],[-89.0173,46.9949],[-88.9948,46.9967],[-88.9783,47.0011],[-88.9678,47.0045],[-88.9567,47.0098],[-88.947,47.0173],[-88.9438,47.021],[-88.9405,47.0229],[-88.9399,47.0238],[-88.9355,47.0294],[-88.934,46.9358],[-88.9328,46.8499],[-88.9317,46.7655],[-88.8641,46.7658],[-88.8645,46.7415],[-88.8643,46.6795],[-88.9537,46.6803],[-88.9821,46.6802],[-88.9921,46.68],[-88.9927,46.591],[-88.9927,46.5759],[-88.9927,46.4182],[-88.9921,46.3311],[-89.0513,46.3314],[-89.1159,46.3315],[-89.2404,46.3328],[-89.3661,46.3329],[-89.3655,46.3948],[-89.3652,46.4182],[-89.365,46.5044],[-89.4924,46.5053],[-89.6113,46.5054],[-89.7388,46.5071],[-89.7377,46.5919],[-89.8363,46.5933],[-89.866,46.5934],[-89.8648,46.6348],[-89.8638,46.6788],[-89.864,46.71],[-89.864,46.7224],[-89.863,46.7674],[-89.8875,46.7677]]]},\"properties\":{\"name\":\"Ontonagon\",\"state\":\"MI\"}}]}","volume":"49","issue":"7","noUsgsAuthors":false,"publicationDate":"1954-11-01","publicationStatus":"PW","contributors":{"authors":[{"text":"White, Walter Stanley","contributorId":96701,"corporation":false,"usgs":true,"family":"White","given":"Walter","email":"","middleInitial":"Stanley","affiliations":[],"preferred":false,"id":809894,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Wright, James C.","contributorId":83936,"corporation":false,"usgs":true,"family":"Wright","given":"James","email":"","middleInitial":"C.","affiliations":[],"preferred":false,"id":809895,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":70221467,"text":"70221467 - 1954 - Stratigraphy and history of the Moenkopi formation of Triassic age","interactions":[],"lastModifiedDate":"2021-06-16T17:25:34.154802","indexId":"70221467","displayToPublicDate":"1954-11-01T12:21:44","publicationYear":"1954","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":2711,"text":"Memoir of the Geological Society of America","active":true,"publicationSubtype":{"id":10}},"title":"Stratigraphy and history of the Moenkopi formation of Triassic age","docAbstract":"<p><span>The&nbsp;</span>Moenkopi<span>&nbsp;</span>formation<span>&nbsp;of&nbsp;</span>Triassic<span>&nbsp;</span>age<span>&nbsp;is composed of a series of deposits that form a wedge thinning eastward from a maximum of about 2000 feet in western Utah and southern Nevada to the vanishing point along an irregular margin in western Colorado, northeastern Arizona, and western New Mexico. Partly marine and partly continental in the thick western sections, it is entirely continental in the east. Invertebrate faunas indicate that deposition began either during or preceding the middle of the Early&nbsp;</span>Triassic<span>&nbsp;(Meekoceras zone) and continued into late Early&nbsp;</span>Triassic<span>&nbsp;(Tirolites zone) and probably into Medial&nbsp;</span>Triassic<span>&nbsp;time. Vertebrate faunas also indicate an Early&nbsp;</span>Triassic<span>&nbsp;and probably, in part, a Medial&nbsp;</span>Triassic<span>&nbsp;</span>age<span>. Studies of the deposits indicate three major transgressions and three regressions across southern Utah and northern Arizona. Analysis of sedimentary rock types and original structures in them suggests a complex mixture of environments involved in the development of the&nbsp;</span>formation<span>: stream beds, lagoons, playas, flood plains or tidal flats, shallow sea floors, and others. Some types are clear cut and readily demonstrated; others are open to question. Evidence from flora, fauna, and sediments indicates a semiarid to arid climate. Except for uplift in the Uncompahgre region of Colorado indicated by conglomeratic beds in the&nbsp;</span>Moenkopi<span>&nbsp;near by, the entire region probably remained very low and flat during&nbsp;</span>Moenkopi<span>&nbsp;deposition.</span></p>","language":"English","publisher":"Geological Society of America","doi":"10.1130/MEM61-p1","usgsCitation":"McKee, E.D., 1954, Stratigraphy and history of the Moenkopi formation of Triassic age: Memoir of the Geological Society of America, v. 61, no. 1, 26 p., https://doi.org/10.1130/MEM61-p1.","productDescription":"26 p.","costCenters":[],"links":[{"id":386547,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United  States","state":"Colorado, Arizona, New Mexico","otherGeospatial":"western Colorado, northeastern Arizona, and western New Mexico","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -109.09423828125,\n              41.09591205639546\n            ],\n            [\n              -109.072265625,\n              36.96744946416934\n            ],\n            [\n              -111.07177734375,\n              37.055177106660814\n            ],\n            [\n              -111.20361328125,\n              31.372399104880525\n            ],\n            [\n              -109.18212890625,\n              31.372399104880525\n            ],\n            [\n              -108.17138671875,\n              31.297327991404266\n            ],\n            [\n              -108.1494140625,\n              31.784216884487385\n            ],\n            [\n              -106.787109375,\n              31.80289258670676\n            ],\n            [\n              -106.63330078125,\n              41.07935114946899\n            ],\n            [\n              -109.09423828125,\n              41.09591205639546\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","volume":"61","issue":"1","noUsgsAuthors":false,"publicationDate":"1954-01-01","publicationStatus":"PW","contributors":{"authors":[{"text":"McKee, Edwin D.","contributorId":60207,"corporation":false,"usgs":true,"family":"McKee","given":"Edwin","email":"","middleInitial":"D.","affiliations":[],"preferred":false,"id":817773,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":70221453,"text":"70221453 - 1954 - Nature of the ore-forming fluids at various stages-a suggested approach","interactions":[],"lastModifiedDate":"2021-06-16T13:32:20.054133","indexId":"70221453","displayToPublicDate":"1954-11-01T08:27:21","publicationYear":"1954","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1472,"text":"Economic Geology","active":true,"publicationSubtype":{"id":10}},"title":"Nature of the ore-forming fluids at various stages-a suggested approach","docAbstract":"<p>No abstract available.&nbsp;</p>","language":"English","publisher":"Society of Economic Geologists","doi":"10.2113/gsecongeo.49.7.727","usgsCitation":"Ingerson, E., 1954, Nature of the ore-forming fluids at various stages-a suggested approach: Economic Geology, v. 49, no. 7, p. 727-733, https://doi.org/10.2113/gsecongeo.49.7.727.","productDescription":"7 p.","startPage":"727","endPage":"733","costCenters":[],"links":[{"id":386530,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"49","issue":"7","noUsgsAuthors":false,"publicationDate":"1954-11-01","publicationStatus":"PW","contributors":{"authors":[{"text":"Ingerson, E.","contributorId":48305,"corporation":false,"usgs":true,"family":"Ingerson","given":"E.","email":"","affiliations":[],"preferred":false,"id":817753,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":70221452,"text":"70221452 - 1954 - Some considerations regarding liquid inclusions as geologic thermometers","interactions":[],"lastModifiedDate":"2021-06-16T13:23:27.626797","indexId":"70221452","displayToPublicDate":"1954-11-01T08:20:47","publicationYear":"1954","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1472,"text":"Economic Geology","active":true,"publicationSubtype":{"id":10}},"title":"Some considerations regarding liquid inclusions as geologic thermometers","docAbstract":"<p>No abstract available.&nbsp;</p>","language":"English","publisher":"Society of Economic Geologists","doi":"10.2113/gsecongeo.49.7.786","usgsCitation":"Richter, D., and Ingerson, E., 1954, Some considerations regarding liquid inclusions as geologic thermometers: Economic Geology, v. 49, no. 7, p. 786-789, https://doi.org/10.2113/gsecongeo.49.7.786.","productDescription":"4 p.","startPage":"786","endPage":"789","costCenters":[],"links":[{"id":386529,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"49","issue":"7","noUsgsAuthors":false,"publicationDate":"1954-11-01","publicationStatus":"PW","contributors":{"authors":[{"text":"Richter, D.H.","contributorId":43325,"corporation":false,"usgs":true,"family":"Richter","given":"D.H.","email":"","affiliations":[{"id":595,"text":"U.S. Geological Survey","active":false,"usgs":true}],"preferred":false,"id":817751,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Ingerson, E.","contributorId":48305,"corporation":false,"usgs":true,"family":"Ingerson","given":"E.","email":"","affiliations":[],"preferred":false,"id":817752,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":70210088,"text":"70210088 - 1954 - Eelgrass status and environmental relations","interactions":[],"lastModifiedDate":"2020-05-13T18:54:29.072571","indexId":"70210088","displayToPublicDate":"1954-10-31T13:51:43","publicationYear":"1954","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":2508,"text":"Journal of Wildlife Management","active":true,"publicationSubtype":{"id":10}},"title":"Eelgrass status and environmental relations","docAbstract":"<p>No abstract available.</p>","language":"English","publisher":"Wiley","doi":"10.2307/3797080","usgsCitation":"Cottam, C., and Munro, D.A., 1954, Eelgrass status and environmental relations: Journal of Wildlife Management, v. 18, no. 4, p. 449-460, https://doi.org/10.2307/3797080.","productDescription":"12 p.","startPage":"449","endPage":"460","costCenters":[],"links":[{"id":374793,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"18","issue":"4","noUsgsAuthors":false,"publicationStatus":"PW","contributors":{"authors":[{"text":"Cottam, Clarence","contributorId":41490,"corporation":false,"usgs":true,"family":"Cottam","given":"Clarence","email":"","affiliations":[],"preferred":false,"id":789062,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Munro, D. A.","contributorId":36657,"corporation":false,"usgs":true,"family":"Munro","given":"D.","email":"","middleInitial":"A.","affiliations":[],"preferred":false,"id":789063,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":70206101,"text":"70206101 - 1954 - Caribbean land and sea through the ages ","interactions":[],"lastModifiedDate":"2020-03-19T14:32:06","indexId":"70206101","displayToPublicDate":"1954-10-22T10:21:45","publicationYear":"1954","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1786,"text":"Geological Society of America Bulletin","active":true,"publicationSubtype":{"id":10}},"title":"Caribbean land and sea through the ages ","docAbstract":"<p>The oldest part of the Caribbean region proper is in northern Central America, where Permian (?) and Lower Permian marine deposits rest on metamorphic rocks of unknown, possibly middle Paleozoic, age. According to present dating, geosynclinal deposition spread eastward in Late Jurassic time to include Cuba, farther eastward and southward in Early Cretaceous time to include Hispaniola and probably Jamaica, and still farther eastward in Late Cretaceous time to include Puerto Rico, the Virgin Islands, and St. Croix. Throughout the Caribbean region, the Cretaceous is characterized by volcanics of great thickness, pyroclastics being more widespread and thicker than flows. These volcanics evidently were derived from lands of unknown size that are now under the waters of the Caribbean Sea. Land still persisted south of eastern Cuba during Eocene time. Thereafter no geological evidence is now available pointing to land in the Caribbean Sea. © 1954, The Geological Society of America, Inc.</p>","language":"English ","publisher":"Geological Society of America ","doi":"10.1130/0016-7606(1954)65[719:CLASTT]2.0.CO;2","issn":"00167606","usgsCitation":"Woodring, W.P., 1954, Caribbean land and sea through the ages : Geological Society of America Bulletin, v. 65, no. 8, p. 719-732, https://doi.org/10.1130/0016-7606(1954)65[719:CLASTT]2.0.CO;2.","productDescription":"14 p. ","startPage":"719","endPage":"732","costCenters":[],"links":[{"id":368489,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"Cuba, Jamaica ","state":" Puerto Rico, the U.S. Virgin Islands, British Virgin Islands ","otherGeospatial":"Caribbean, Central America, 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,{"id":70011005,"text":"70011005 - 1954 - A geothermal measuring circuit","interactions":[],"lastModifiedDate":"2026-03-03T15:56:04.399647","indexId":"70011005","displayToPublicDate":"1954-10-08T00:00:00","publicationYear":"1954","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":3338,"text":"Science","active":true,"publicationSubtype":{"id":10}},"title":"A geothermal measuring circuit","docAbstract":"<p>No abstract available.</p>","language":"English","publisher":"American Association for the Advancement of Science","doi":"10.1126/science.120.3119.573","issn":"00368075","usgsCitation":"Swartz, J., 1954, A geothermal measuring circuit: Science, v. 120, no. 3119, p. 573-574, https://doi.org/10.1126/science.120.3119.573.","productDescription":"2 p.","startPage":"573","endPage":"574","costCenters":[],"links":[{"id":221633,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"120","issue":"3119","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"5059e408e4b0c8380cd46371","contributors":{"authors":[{"text":"Swartz, J.H.","contributorId":101721,"corporation":false,"usgs":true,"family":"Swartz","given":"J.H.","email":"","affiliations":[],"preferred":false,"id":360076,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":70095688,"text":"tei471 - 1954 - Botanical prospecting for uranium on La Ventana Mesa, Sandoval County, New Mexico","interactions":[],"lastModifiedDate":"2014-05-27T13:56:26","indexId":"tei471","displayToPublicDate":"1954-10-01T13:54:00","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":"471","title":"Botanical prospecting for uranium on La Ventana Mesa, Sandoval County, New Mexico","docAbstract":"A botanical sampling program has been completed by the U.S. Geological Survey on La Ventana Mesa, Sandoval County, N. Mex. A uranium-bearing coal in the Allison-Gibson members of the Cretaceous Mesaverde formation crops out in erosional remnants of the mesa.The coal is capped by a well-fractured 65-foot sandstone bed through which roots of a pinyon-juniper forest penetrate. Samples of several hundred branches of trees growing on top of the mesa were collected and analyzed for uranium. The assays ranged from 0.1 part per million to 2.3 ppm uranium in the wood ash. Dead branches, which were found to contain more uranium in the ash than live branches, were sampled where possible. The results have been contoured to indicated probable areas of mineralized coal. Parts of the north butte are recommended as favorable for physical exploration.","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Reston, VA","doi":"10.3133/tei471","collaboration":"Report concerns work done on behalf of the Division of Raw Materials of the U.S. Atomic Energy Commission.","usgsCitation":"Starrett, H., and Cannon, H., 1954, Botanical prospecting for uranium on La Ventana Mesa, Sandoval County, New Mexico: U.S. Geological Survey Trace Elements Investigations 471, 16  p., https://doi.org/10.3133/tei471.","productDescription":"16  p.","costCenters":[],"links":[{"id":283493,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/tei471.png"},{"id":284570,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/tei/0471/report.pdf"}],"country":"United States","state":"New Mexico","county":"Sandoval County","otherGeospatial":"La Ventana Mesa","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -107.6265,35.1977 ], [ -107.6265,36.2198 ], [ -106.2452,36.2198 ], [ -106.2452,35.1977 ], [ -107.6265,35.1977 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"53558fcde4b0120853e8be5e","contributors":{"authors":[{"text":"Starrett, H.","contributorId":65766,"corporation":false,"usgs":true,"family":"Starrett","given":"H.","email":"","affiliations":[],"preferred":false,"id":491359,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Cannon, Helen L.","contributorId":96249,"corporation":false,"usgs":true,"family":"Cannon","given":"Helen L.","affiliations":[],"preferred":false,"id":491360,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
]}