No abstract available.
","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/gp226","usgsCitation":"Bromery, R.W., and Zandle, G.L., 1960, Aeromagnetic map of part of the Unionville quadrangle, Chester County, Pennsylvania: U.S. Geological Survey Geophysical Investigations Map 226, 1 Plate: 22.68 x 27.04 inches, https://doi.org/10.3133/gp226.","productDescription":"1 Plate: 22.68 x 27.04 inches","costCenters":[],"links":[{"id":251985,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/gp/0226/report-thumb.jpg"},{"id":251180,"rank":3,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/gp/0226/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":251179,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/gp/0226/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":484259,"rank":4,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_3147.htm","linkFileType":{"id":5,"text":"html"}}],"scale":"24000","country":"United States","state":"Pennsylvania","county":"Chester County","otherGeospatial":"Unionville quadrangle","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -75.75,39.8675 ], [ -75.75,40 ], [ -75.61749999999999,40 ], [ -75.61749999999999,39.8675 ], [ -75.75,39.8675 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4afee4b07f02db6975d3","contributors":{"authors":[{"text":"Bromery, Randolph Wilson","contributorId":22746,"corporation":false,"usgs":true,"family":"Bromery","given":"Randolph","email":"","middleInitial":"Wilson","affiliations":[],"preferred":false,"id":270923,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Zandle, G. L.","contributorId":39863,"corporation":false,"usgs":true,"family":"Zandle","given":"G.","email":"","middleInitial":"L.","affiliations":[],"preferred":false,"id":270924,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":2930,"text":"wsp1569 - 1960 - Surface water supply of Hawaii, 1956-58","interactions":[],"lastModifiedDate":"2012-02-02T00:05:34","indexId":"wsp1569","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1960","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":341,"text":"Water Supply Paper","code":"WSP","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"1569","title":"Surface water supply of Hawaii, 1956-58","language":"ENGLISH","publisher":"U.S. G.P.O.,","doi":"10.3133/wsp1569","usgsCitation":"Wells, J.V., 1960, Surface water supply of Hawaii, 1956-58: U.S. Geological Survey Water Supply Paper 1569, vii, 295 p. ;24 cm., https://doi.org/10.3133/wsp1569.","productDescription":"vii, 295 p. ;24 cm.","costCenters":[],"links":[{"id":139017,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wsp/1569/report-thumb.jpg"},{"id":29639,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wsp/1569/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4afee4b07f02db69769a","contributors":{"authors":[{"text":"Wells, J. V. B.","contributorId":57037,"corporation":false,"usgs":true,"family":"Wells","given":"J.","email":"","middleInitial":"V. B.","affiliations":[],"preferred":false,"id":146016,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":2959,"text":"wsp1629 - 1960 - Surface water supply of the United States, 1959, Part 6-A, Missouri River Basin above Sioux City, Iowa","interactions":[],"lastModifiedDate":"2012-02-02T00:05:39","indexId":"wsp1629","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1960","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":341,"text":"Water Supply Paper","code":"WSP","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"1629","title":"Surface water supply of the United States, 1959, Part 6-A, Missouri River Basin above Sioux City, Iowa","language":"ENGLISH","publisher":"U.S. Govt. Print. Off.,","doi":"10.3133/wsp1629","usgsCitation":"Wells, J.V., 1960, Surface water supply of the United States, 1959, Part 6-A, Missouri River Basin above Sioux City, Iowa: U.S. Geological Survey Water Supply Paper 1629, x, 415 p. :ill., tables ;25 cm., https://doi.org/10.3133/wsp1629.","productDescription":"x, 415 p. :ill., tables ;25 cm.","costCenters":[],"links":[{"id":139282,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wsp/1629/report-thumb.jpg"},{"id":29668,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wsp/1629/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4af8e4b07f02db69437f","contributors":{"authors":[{"text":"Wells, J. V. B.","contributorId":57037,"corporation":false,"usgs":true,"family":"Wells","given":"J.","email":"","middleInitial":"V. B.","affiliations":[],"preferred":false,"id":146045,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":2188,"text":"wsp1484 - 1960 - Geology and ground-water features of Shasta Valley, Siskiyou County, California","interactions":[],"lastModifiedDate":"2012-02-02T00:05:23","indexId":"wsp1484","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1960","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":341,"text":"Water Supply Paper","code":"WSP","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"1484","title":"Geology and ground-water features of Shasta Valley, Siskiyou County, California","language":"ENGLISH","publisher":"U.S. Govt. Print. Off.,","doi":"10.3133/wsp1484","usgsCitation":"Mack, S., 1960, Geology and ground-water features of Shasta Valley, Siskiyou County, California: U.S. Geological Survey Water Supply Paper 1484, v, 115 p. :illus., maps (2 fold., 1 col., in pocket) ;24 cm., https://doi.org/10.3133/wsp1484.","productDescription":"v, 115 p. :illus., maps (2 fold., 1 col., in pocket) ;24 cm.","costCenters":[],"links":[{"id":138565,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wsp/1484/report-thumb.jpg"},{"id":27826,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wsp/1484/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":27827,"rank":401,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wsp/1484/plate-2.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":27828,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wsp/1484/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4adbe4b07f02db685fb8","contributors":{"authors":[{"text":"Mack, Seymour","contributorId":101247,"corporation":false,"usgs":true,"family":"Mack","given":"Seymour","email":"","affiliations":[],"preferred":false,"id":144796,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":3324,"text":"cir427 - 1960 - A field instrument for quantitative determination of beryllium by activation analysis","interactions":[],"lastModifiedDate":"2018-01-02T20:38:35","indexId":"cir427","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1960","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":307,"text":"Circular","code":"CIR","onlineIssn":"2330-5703","printIssn":"1067-084X","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"427","title":"A field instrument for quantitative determination of beryllium by activation analysis","docAbstract":"A low-cost instrument has been developed for quantitative determinations of beryllium in the field by activation analysis. The instrument makes use of the gamma-neutron reaction between gammas emitted by an artificially radioactive source (Sb124) and beryllium as it occurs in nature. The instrument and power source are mounted in a panel-type vehicle. Samples are prepared by hand-crushing the rock to approximately ?-inch mesh size and smaller. Sample volumes are kept constant by means of a standard measuring cup. Instrument calibration, made by using standards of known BeO content, indicates the analyses are reproducible and accurate to within ? 0.25 percent BeO in the range from 1 to 20 percent BeO with a sample counting time of 5 minutes. Sensitivity of the instrument maybe increased somewhat by increasing the source size, the sample size, or by enlarging the cross-sectional area of the neutron-sensitive phosphor normal to the neutron flux.","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/cir427","usgsCitation":"Vaughn, W., Wilson, E., and Ohm, J., 1960, A field instrument for quantitative determination of beryllium by activation analysis: U.S. Geological Survey Circular 427, 9 p. :illus. ;27cm., https://doi.org/10.3133/cir427.","productDescription":"9 p. :illus. ;27cm.","costCenters":[],"links":[{"id":30333,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/circ/1960/0427/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":124688,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/circ/1960/0427/report-thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b24e4b07f02db6aec8d","contributors":{"authors":[{"text":"Vaughn, William W.","contributorId":107267,"corporation":false,"usgs":true,"family":"Vaughn","given":"William W.","affiliations":[],"preferred":false,"id":146669,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Wilson, E.E.","contributorId":68299,"corporation":false,"usgs":true,"family":"Wilson","given":"E.E.","email":"","affiliations":[],"preferred":false,"id":146667,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Ohm, J.M.","contributorId":83508,"corporation":false,"usgs":true,"family":"Ohm","given":"J.M.","email":"","affiliations":[],"preferred":false,"id":146668,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}} ,{"id":2334,"text":"wsp1490 - 1960 - Geology and ground-water resources of Platte County, Wyoming, with a section on Chemical quality of the water","interactions":[],"lastModifiedDate":"2012-02-02T00:05:22","indexId":"wsp1490","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1960","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":341,"text":"Water Supply Paper","code":"WSP","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"1490","title":"Geology and ground-water resources of Platte County, Wyoming, with a section on Chemical quality of the water","docAbstract":"Platte County, Wyo., has an area of 2,114 square miles and, in 1950, had a population of 7,925; it lies within parts of two major physiographic provinces, the northern extension of the Southern Rocky Mountains and the northwestern part of the Great Plains. The Laramie Range and related structures lie along the western margin of the county and constitute the eastern limit of the Rocky Mountain Front Range. The High Plains section of the Great Plains province extends eastward from the Laramie Range over the remainder of the county. The original surface of the High Plains has been deeply eroded, and in the northeastern part of the county it is broken by the broad uplifted structural platform of the Hartville Hills. The North Platte River and its tributaries have entrenched their channels as much as 1,000 feet into the plains, leaving wide, very flat intervalley areas that are interrupted by a few isolated buttes and outlying ridges. Well-defined terraces, locally called the Wheatland Flats, have been formed in central Platte County. The climate is semiarid, the average annual precipitation being about 15 inches. Farming and stockraising are the principal occupations in the county. \r\n\r\nMost of the rocks exposed in the county are of Tertiary and Quaternary age, although rocks as old as Precambrian crop out locally. The Arikaree and Brule formations and younger deposits, including Tertiary ( ?) deposits (undifferentiated) and terrace, flood-plain, and other alluvial deposits, underlie more than two-thirds of the county. Mesozoic, Paleozoic, and Precambrian rocks crop out in the other third and underlie the younger rocks at great depths elsewhere. Small supplies of ground water adequate for domestic and stock use can be obtained from shallow wells in the Casper, Hartville, Cloverly, Brule, and Arikaree formations and in the terrace and flood-plain deposits. Small to moderate amounts of ground water can be obtained from the 'Converse sand' of the Hartville formation. Several flowing wells obtain water from this sand near Glendo. Moderate to large supplies of ground water adequate for small-scale irrigation or industrial uses or for public supply can be obtained from properly constructed wells penetrating thick saturated sections of the Arikaree formation and from the terrace and flood-plain deposits. Large supplies of ground water can be obtained from the flood-plain deposits of the North Platte River near Guernsey, where wells commonly yield more than 1,000 gpm (gallons per minute). The aquifers with greatest potential for additional groundwater development in Platte County, in decreasing order of importance, are the flood-plain deposits along the North Platte River and its tributaries, the Arikaree formation and terrace deposits in parts of the Wheatland Flats, and the 'Converse sand' in the general vicinity of Glendo.","language":"ENGLISH","publisher":"U.S. G.P.O.,","doi":"10.3133/wsp1490","usgsCitation":"Morris, D.A., Babcock, H.M., and Langford, R., 1960, Geology and ground-water resources of Platte County, Wyoming, with a section on Chemical quality of the water: U.S. Geological Survey Water Supply Paper 1490, vi, 195 p. :ill., maps, charts ;24 cm., https://doi.org/10.3133/wsp1490.","productDescription":"vi, 195 p. :ill., maps, charts ;24 cm.","costCenters":[],"links":[{"id":109950,"rank":700,"type":{"id":15,"text":"Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_24431.htm","linkFileType":{"id":5,"text":"html"},"description":"24431"},{"id":138465,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wsp/1490/report-thumb.jpg"},{"id":28195,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wsp/1490/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":28196,"rank":401,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wsp/1490/plate-2.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":28197,"rank":402,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wsp/1490/plate-3.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":28198,"rank":403,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wsp/1490/plate-4.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":28199,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wsp/1490/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4adbe4b07f02db6859f9","contributors":{"authors":[{"text":"Morris, D. A.","contributorId":56204,"corporation":false,"usgs":true,"family":"Morris","given":"D.","email":"","middleInitial":"A.","affiliations":[],"preferred":false,"id":145028,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Babcock, H. M.","contributorId":90698,"corporation":false,"usgs":true,"family":"Babcock","given":"H.","email":"","middleInitial":"M.","affiliations":[],"preferred":false,"id":145030,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Langford, R.H.","contributorId":59426,"corporation":false,"usgs":true,"family":"Langford","given":"R.H.","email":"","affiliations":[],"preferred":false,"id":145029,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}} ,{"id":2584,"text":"wsp1536B - 1960 - Water levels near a well discharging from an unconfined aquifer","interactions":[],"lastModifiedDate":"2012-02-02T00:05:20","indexId":"wsp1536B","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1960","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":341,"text":"Water Supply Paper","code":"WSP","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"1536","chapter":"B","title":"Water levels near a well discharging from an unconfined aquifer","language":"ENGLISH","publisher":"U.S. Department of the Interior, Geological Survey ;","doi":"10.3133/wsp1536B","isbn":"pbk","usgsCitation":"Remson, I., McNeary, S., and Randolph, J., 1960, Water levels near a well discharging from an unconfined aquifer: U.S. Geological Survey Water Supply Paper 1536, iii, [13] p. ;23 cm., https://doi.org/10.3133/wsp1536B.","productDescription":"iii, [13] p. ;23 cm.","costCenters":[],"links":[{"id":137841,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wsp/1536b/report-thumb.jpg"},{"id":28858,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wsp/1536b/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a08e4b07f02db5f9cec","contributors":{"authors":[{"text":"Remson, Irwin","contributorId":89115,"corporation":false,"usgs":true,"family":"Remson","given":"Irwin","email":"","affiliations":[],"preferred":false,"id":145442,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"McNeary, S.S.","contributorId":14797,"corporation":false,"usgs":true,"family":"McNeary","given":"S.S.","email":"","affiliations":[],"preferred":false,"id":145440,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Randolph, J.R.","contributorId":19532,"corporation":false,"usgs":true,"family":"Randolph","given":"J.R.","email":"","affiliations":[],"preferred":false,"id":145441,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}} ,{"id":2929,"text":"wsp1449 - 1960 - Surface water supply of Hawaii, 1955-56","interactions":[],"lastModifiedDate":"2012-02-02T00:05:34","indexId":"wsp1449","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1960","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":341,"text":"Water Supply Paper","code":"WSP","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"1449","title":"Surface water supply of Hawaii, 1955-56","language":"ENGLISH","publisher":"U.S. G.P.O.,","doi":"10.3133/wsp1449","usgsCitation":"Wells, J.V., 1960, Surface water supply of Hawaii, 1955-56: U.S. Geological Survey Water Supply Paper 1449, vi, 150 p. :ill. ;24 cm., https://doi.org/10.3133/wsp1449.","productDescription":"vi, 150 p. :ill. ;24 cm.","costCenters":[],"links":[{"id":139016,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wsp/1449/report-thumb.jpg"},{"id":29638,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wsp/1449/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4afee4b07f02db69766d","contributors":{"authors":[{"text":"Wells, J. V. B.","contributorId":57037,"corporation":false,"usgs":true,"family":"Wells","given":"J.","email":"","middleInitial":"V. B.","affiliations":[],"preferred":false,"id":146015,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":68392,"text":"ha39 - 1960 - Floods near Chicago Heights, Illinois","interactions":[],"lastModifiedDate":"2021-08-24T19:41:32.039873","indexId":"ha39","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1960","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":318,"text":"Hydrologic Atlas","code":"HA","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"39","title":"Floods near Chicago Heights, Illinois","docAbstract":"No abstract available.
","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ha39","usgsCitation":"Water Resources Division, U.S. Geological Survey, 1960, Floods near Chicago Heights, Illinois: U.S. Geological Survey Hydrologic Atlas 39, 1 Plate: 30.50 × 30.00 inches, https://doi.org/10.3133/ha39.","productDescription":"1 Plate: 30.50 × 30.00 inches","costCenters":[],"links":[{"id":185621,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":388450,"rank":2,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_15770.htm"},{"id":89892,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/ha/039/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}}],"scale":"24000","country":"United States","state":"Illinois","city":"Chicago Heights","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -87.61749999999999,41.5 ], [ -87.61749999999999,41.6175 ], [ -87.5,41.6175 ], [ -87.5,41.5 ], [ -87.61749999999999,41.5 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e49dbe4b07f02db5e07ed","contributors":{"authors":[{"text":"Water Resources Division, U.S. Geological Survey","contributorId":128075,"corporation":true,"usgs":false,"organization":"Water Resources Division, U.S. Geological Survey","id":534509,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":61982,"text":"mr11 - 1960 - Antimony, bismuth, and mercury occurrences in Alaska","interactions":[{"subject":{"id":13038,"text":"ofr5920 - 1959 - Antimony, bismuth, and mercury in Alaska","indexId":"ofr5920","publicationYear":"1959","noYear":false,"title":"Antimony, bismuth, and mercury in Alaska"},"predicate":"SUPERSEDED_BY","object":{"id":61982,"text":"mr11 - 1960 - Antimony, bismuth, and mercury occurrences in Alaska","indexId":"mr11","publicationYear":"1960","noYear":false,"title":"Antimony, bismuth, and mercury occurrences in Alaska"},"id":1}],"lastModifiedDate":"2012-02-10T00:10:35","indexId":"mr11","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1960","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":324,"text":"Mineral Investigations Resource Map","code":"MR","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"11","title":"Antimony, bismuth, and mercury occurrences in Alaska","language":"ENGLISH","doi":"10.3133/mr11","usgsCitation":"Cobb, E.H., 1960, Antimony, bismuth, and mercury occurrences in Alaska: U.S. Geological Survey Mineral Investigations Resource Map 11, 1 map :col. ;79 x 116 cm. folded in envelope 30 x 24 cm., https://doi.org/10.3133/mr11.","productDescription":"1 map :col. ;79 x 116 cm. folded in envelope 30 x 24 cm.","costCenters":[],"links":[{"id":103225,"rank":700,"type":{"id":15,"text":"Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_1745.htm","linkFileType":{"id":5,"text":"html"},"description":"1745"},{"id":180056,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"}],"scale":"2500000","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -172.25,52 ], [ -172.25,70 ], [ -129.1175,70 ], [ -129.1175,52 ], [ -172.25,52 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ac7e4b07f02db67b02d","contributors":{"authors":[{"text":"Cobb, Edward Huntington","contributorId":25916,"corporation":false,"usgs":true,"family":"Cobb","given":"Edward","email":"","middleInitial":"Huntington","affiliations":[],"preferred":false,"id":266650,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":64333,"text":"gp232 - 1960 - Aeromagnetic map of the Boyertown quadrangle, Berks and Montgomery Counties, Pennsylvania","interactions":[],"lastModifiedDate":"2021-12-06T21:45:44.031628","indexId":"gp232","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1960","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":317,"text":"Geophysical Investigations Map","code":"GP","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"232","title":"Aeromagnetic map of the Boyertown quadrangle, Berks and Montgomery Counties, Pennsylvania","docAbstract":"No abstract available.
","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/gp232","usgsCitation":"Bromery, R.W., and Zandle, G.L., 1960, Aeromagnetic map of the Boyertown quadrangle, Berks and Montgomery Counties, Pennsylvania: U.S. Geological Survey Geophysical Investigations Map 232, 1 Plate: 22.99 × 27.33 inches, https://doi.org/10.3133/gp232.","productDescription":"1 Plate: 22.99 × 27.33 inches","costCenters":[],"links":[{"id":251722,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/gp/0232/report-thumb.jpg"},{"id":250982,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/gp/0232/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":250981,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/gp/0232/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":392525,"rank":4,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_3154.htm"}],"scale":"24000","country":"United States","state":"Pennsylvania","county":"Berks County, Montgomery County","otherGeospatial":"Boyertown quadrangle","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -75.75,40.25 ], [ -75.75,40.375 ], [ -75.625,40.375 ], [ -75.625,40.25 ], [ -75.75,40.25 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ae6e4b07f02db68b516","contributors":{"authors":[{"text":"Bromery, Randolph Wilson","contributorId":22746,"corporation":false,"usgs":true,"family":"Bromery","given":"Randolph","email":"","middleInitial":"Wilson","affiliations":[],"preferred":false,"id":270613,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Zandle, G. L.","contributorId":39863,"corporation":false,"usgs":true,"family":"Zandle","given":"G.","email":"","middleInitial":"L.","affiliations":[],"preferred":false,"id":270614,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":14369,"text":"ofr6084 - 1960 - Experimental drill hole logging in potash deposits of the Carlsbad district, New Mexico","interactions":[],"lastModifiedDate":"2017-12-01T11:10:56","indexId":"ofr6084","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1960","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":330,"text":"Open-File Report","code":"OFR","onlineIssn":"2331-1258","printIssn":"0196-1497","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"60-84","title":"Experimental drill hole logging in potash deposits of the Carlsbad district, New Mexico","docAbstract":"Experimental logging of holes drilled through potash deposits in the Carlsbad district, southeastern New Mexico, demonstrate the considerable utility of gamma-ray, neutron, and electrical resistivity logging in the search for and identification of mineable deposits of sylvite and langbeinite. Such deposits are strongly radioactive with both gamma-ray and neutron well logging. Their radlioactivity serves to distinguish them from claystone, sandstone, and polyhalite beds and from potash deposits containing carnallite, leonite, and kainite. These latter strata and deposits are radioactive with gamma-ray logging but yield no radiation with neutron logging. Porous beds, such as sandstone strata, and solution cavities, such as those commonly formed in potash deposits by rotary drilling of evaporites, are less resistive than other materials. Low resistivity provides a means for differentiating between potash deposits and polyhalite beds on electrical resistivity logs of holes drilled with fresh-water and salt-base muds.","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr6084","usgsCitation":"Jones, C., Bowles, C.G., and Bell, K.G., 1960, Experimental drill hole logging in potash deposits of the Carlsbad district, New Mexico: U.S. Geological Survey Open-File Report 60-84, Report: 22 p.; 5 Plates: 39.51 x 47.99 inches or smaller, https://doi.org/10.3133/ofr6084.","productDescription":"Report: 22 p.; 5 Plates: 39.51 x 47.99 inches or smaller","costCenters":[],"links":[{"id":349618,"rank":3,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1960/0084/figure-1.pdf","text":"Figure 1","linkFileType":{"id":1,"text":"pdf"}},{"id":349619,"rank":4,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1960/0084/figure-2.pdf","text":"Figure 2","linkFileType":{"id":1,"text":"pdf"}},{"id":349620,"rank":5,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1960/0084/figure-3.pdf","text":"Figure 3","linkFileType":{"id":1,"text":"pdf"}},{"id":349621,"rank":6,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1960/0084/figure-4.pdf","text":"Figure 4","linkFileType":{"id":1,"text":"pdf"}},{"id":349622,"rank":7,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1960/0084/figure-5.pdf","text":"Figure 5","linkFileType":{"id":1,"text":"pdf"}},{"id":43047,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1960/0084/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":147591,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1960/0084/report-thumb.jpg"}],"country":"United States","state":"New Mexico","otherGeospatial":"Carlsbad District","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"type\": \"Polygon\",\n \"coordinates\": [\n [\n [\n -104.43878173828125,\n 32.31383067137085\n ],\n [\n -103.75076293945312,\n 32.31383067137085\n ],\n [\n -103.75076293945312,\n 32.76302656020649\n ],\n [\n -104.43878173828125,\n 32.76302656020649\n ],\n [\n -104.43878173828125,\n 32.31383067137085\n ]\n ]\n ]\n }\n }\n ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a07e4b07f02db5f9295","contributors":{"authors":[{"text":"Jones, C.L.","contributorId":60218,"corporation":false,"usgs":true,"family":"Jones","given":"C.L.","email":"","affiliations":[],"preferred":false,"id":169339,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Bowles, C. Gilbert","contributorId":60607,"corporation":false,"usgs":true,"family":"Bowles","given":"C.","email":"","middleInitial":"Gilbert","affiliations":[],"preferred":false,"id":169340,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Bell, Kenneth Granville","contributorId":61431,"corporation":false,"usgs":true,"family":"Bell","given":"Kenneth","email":"","middleInitial":"Granville","affiliations":[],"preferred":false,"id":169341,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}} ,{"id":64356,"text":"gp222 - 1960 - Aeromagnetic map of the Pottstown quadrangle, Berks, Chester, and Montgomery Counties, Pennsylvania","interactions":[],"lastModifiedDate":"2025-04-04T20:40:35.184591","indexId":"gp222","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1960","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":317,"text":"Geophysical Investigations Map","code":"GP","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"222","title":"Aeromagnetic map of the Pottstown quadrangle, Berks, Chester, and Montgomery Counties, Pennsylvania","docAbstract":"No abstract available.
","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/gp222","usgsCitation":"Bromery, R.W., and Zandle, G.L., 1960, Aeromagnetic map of the Pottstown quadrangle, Berks, Chester, and Montgomery Counties, Pennsylvania: U.S. Geological Survey Geophysical Investigations Map 222, 1 Plate: 22.99 x 27.10 inches, https://doi.org/10.3133/gp222.","productDescription":"1 Plate: 22.99 x 27.10 inches","costCenters":[],"links":[{"id":484221,"rank":4,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_3143.htm","linkFileType":{"id":5,"text":"html"}},{"id":251744,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/gp/0222/report-thumb.jpg"},{"id":251025,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/gp/0222/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":251026,"rank":3,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/gp/0222/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}}],"scale":"24000","country":"United States","state":"Pennsylvania","county":"Berks County, Chester County, Montgomery County","otherGeospatial":"Pottstown quadrangle","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -75.75,40.125 ], [ -75.75,40.25 ], [ -75.625,40.25 ], [ -75.625,40.125 ], [ -75.75,40.125 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4af3e4b07f02db691b81","contributors":{"authors":[{"text":"Bromery, Randolph Wilson","contributorId":22746,"corporation":false,"usgs":true,"family":"Bromery","given":"Randolph","email":"","middleInitial":"Wilson","affiliations":[],"preferred":false,"id":270680,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Zandle, G. L.","contributorId":39863,"corporation":false,"usgs":true,"family":"Zandle","given":"G.","email":"","middleInitial":"L.","affiliations":[],"preferred":false,"id":270681,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":64341,"text":"gp262 - 1960 - Aeromagnetic map of the Telford quadrangle, Montgomery and Bucks Counties, Pennsylvania","interactions":[],"lastModifiedDate":"2025-04-07T18:08:03.617672","indexId":"gp262","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1960","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":317,"text":"Geophysical Investigations Map","code":"GP","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"262","title":"Aeromagnetic map of the Telford quadrangle, Montgomery and Bucks Counties, Pennsylvania","docAbstract":"No abstract available.
","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/gp262","usgsCitation":"Bromery, R.W., and Zandle, G.L., 1960, Aeromagnetic map of the Telford quadrangle, Montgomery and Bucks Counties, Pennsylvania: U.S. Geological Survey Geophysical Investigations Map 262, 1 Plate: 22.53 x 27.25 inches, https://doi.org/10.3133/gp262.","productDescription":"1 Plate: 22.53 x 27.25 inches","costCenters":[],"links":[{"id":484270,"rank":4,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_3187.htm","linkFileType":{"id":5,"text":"html"}},{"id":250996,"rank":3,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/gp/0262/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":251729,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/gp/0262/report-thumb.jpg"},{"id":250995,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/gp/0262/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"scale":"24000","country":"United States","state":"Pennsylvania","county":"Bucks County, Montgomery County","otherGeospatial":"Telford quadrangle","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -75.375,40.25 ], [ -75.375,40.375 ], [ -75.25,40.375 ], [ -75.25,40.25 ], [ -75.375,40.25 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4af3e4b07f02db691aae","contributors":{"authors":[{"text":"Bromery, Randolph Wilson","contributorId":22746,"corporation":false,"usgs":true,"family":"Bromery","given":"Randolph","email":"","middleInitial":"Wilson","affiliations":[],"preferred":false,"id":270641,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Zandle, G. L.","contributorId":39863,"corporation":false,"usgs":true,"family":"Zandle","given":"G.","email":"","middleInitial":"L.","affiliations":[],"preferred":false,"id":270642,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":70220593,"text":"70220593 - 1960 - Minor element abundance in a part of the Brazilian shield","interactions":[],"lastModifiedDate":"2021-05-20T19:31:47.103483","indexId":"70220593","displayToPublicDate":"1960-12-31T14:24:56","publicationYear":"1960","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1759,"text":"Geochimica et Cosmochimica Acta","active":true,"publicationSubtype":{"id":10}},"title":"Minor element abundance in a part of the Brazilian shield","docAbstract":"Thirty-nine samples of granitic rocks from the Quadrilátero Ferrifero, Minas Gerais, Brazil, representing \"mixed\" ages and at least three distinct Pre-Cambrian ages were analysed for seventeen minor elements. The rocks are placed in five groups:, (1) 2400 million year old group;, (2) Bacao complex younger, a group of mixed rocks derived from, (1) and, (3);, (3) 1350 million year old group;, (4) a 500 million year old gneissic group;, (5) a 500 million year old silicic group, a later differentiate of a 500 million year old magma.
Compared to granitic rocks elsewhere, these Brazilian rocks are about average in Ba, So, Zr, Pb, Nb, Co, Ni, Be and Mo; above average in La and Y; and below average in Cu, Sr, Ga, Sn, V and Cr. Compared to metasedimentary rocks elsewhere in the world., metasedimentary rocks of this region are about average in all seventeen minor elements.
Sr has its greatest abundance in the 2400 million year old rocks; Ba, V, Co, Sc, Cr, Ni and Cu in the 1350 million year; and La, Nb, Sn, Zr, Y and Ga in the 500 million year silicic. These abundances are in accord with the petrology and chemistry of the rocks. The 1350 million year rocks are the most mafic of the group and should logically concentrate Ba, V, Co, So, Or, Ni and Cu which are most abundant in earlier crystallates. The 500 million year old silicic rocks are the most felsic and should concentrate La, Nb, Sn, Zr, Y and Ga, which are all most abundant in the latest fractions of granitic magna crystallization.
The trace elements also lend support to the idea that the Bacao complex rocks developed by anatexis of 2400 million year rocks during the 1350 -pillion year orogeny. Cu, Sc, Ga, Zr, Sn and Nb have about the same magnitude in the Bagao and the 2400 million year rocks and Sr, V, Co, Or and Ni are lower in the BagAo than either the 2400 or the 1350 million yoar old rocks. This lower abundance is a probable effect of \"debasif-cation\" which is also brought out by the analysis of major constituents.
The effects of a geochemical migration of the elements in this part of the earth's crust may be indicated by the increased abundance of Y in successivol y younger rock types. The increase of La, Nb, Pb, Sn, Y and Zr in the 1350 million year rocks compared to the 2,100 million year rocks might also be an effect of a secular migration.
","language":"English","publisher":"Elsevier","doi":"10.1016/S0016-7037(60)80004-X","usgsCitation":"Herz, N., and Dutra, C.V., 1960, Minor element abundance in a part of the Brazilian shield: Geochimica et Cosmochimica Acta, v. 21, no. 1-2, p. 81-98, https://doi.org/10.1016/S0016-7037(60)80004-X.","productDescription":"18 p.","startPage":"81","endPage":"98","costCenters":[],"links":[{"id":385807,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"Brazil","otherGeospatial":"southeast Brazil","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"type\": \"Polygon\",\n \"coordinates\": [\n [\n [\n -48.1640625,\n -22.75592068148639\n ],\n [\n -40.60546875,\n -22.75592068148639\n ],\n [\n -40.60546875,\n -14.264383087562637\n ],\n [\n -48.1640625,\n -14.264383087562637\n ],\n [\n -48.1640625,\n -22.75592068148639\n ]\n ]\n ]\n }\n }\n ]\n}","volume":"21","issue":"1-2","noUsgsAuthors":false,"publicationStatus":"PW","contributors":{"authors":[{"text":"Herz, N.","contributorId":97626,"corporation":false,"usgs":true,"family":"Herz","given":"N.","affiliations":[],"preferred":false,"id":816108,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Dutra, C. V.","contributorId":37884,"corporation":false,"usgs":false,"family":"Dutra","given":"C.","email":"","middleInitial":"V.","affiliations":[],"preferred":false,"id":816109,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":70220592,"text":"70220592 - 1960 - A comprehensive system of automatic computation in magnetic and gravity interpretation","interactions":[],"lastModifiedDate":"2021-05-20T19:20:02.92688","indexId":"70220592","displayToPublicDate":"1960-12-31T14:15:30","publicationYear":"1960","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1808,"text":"Geophysics","active":true,"publicationSubtype":{"id":10}},"title":"A comprehensive system of automatic computation in magnetic and gravity interpretation","docAbstract":"In the interpretation of magnetic and gravity anomalies, downward continuation of fields and calculation of first and second vertical derivatives of fields have been recognized as effective means for bringing into focus the latent diagnostic features of the data. A comprehensive system has been devised for the calculation of any or all of these derived fields on modern electronic digital computing equipment. The integral for analytic continuation above the plane is used with a Lagrange extrapolation polynomial to derive a general determinantal expression from which the field at depth and the various derivatives on the surface and at depth can be obtained. It is shown that the general formula includes as special cases some of the formulas appearing in the literature. The process involves a \"once for all depths\" summing of grid values on a system of concentric circles about each point followed by application of the appropriate one or more of the 19 sets of coefficients derived for the purpose. Theoretical and observed multilevel data are used to illustrate the processes and to discuss the errors. The coefficients can be used for less extensive computations on a desk calculator.
","language":"English","publisher":"Society of Exploration Geophysicists","doi":"10.1190/1.1438736","usgsCitation":"Henderson, R., 1960, A comprehensive system of automatic computation in magnetic and gravity interpretation: Geophysics, v. 25, no. 3, p. 569-585, https://doi.org/10.1190/1.1438736.","productDescription":"17 p.","startPage":"569","endPage":"585","costCenters":[],"links":[{"id":385806,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"25","issue":"3","noUsgsAuthors":false,"publicationStatus":"PW","contributors":{"authors":[{"text":"Henderson, R.G.","contributorId":72521,"corporation":false,"usgs":true,"family":"Henderson","given":"R.G.","email":"","affiliations":[],"preferred":false,"id":816107,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":70209156,"text":"70209156 - 1960 - A possible relationship between aquatic invertebrates and avian botulism","interactions":[],"lastModifiedDate":"2020-03-19T14:04:35","indexId":"70209156","displayToPublicDate":"1960-12-31T13:57:07","publicationYear":"1960","noYear":false,"publicationType":{"id":24,"text":"Conference Paper"},"publicationSubtype":{"id":19,"text":"Conference Paper"},"title":"A possible relationship between aquatic invertebrates and avian botulism","docAbstract":"No abstract available.
","largerWorkType":{"id":4,"text":"Book"},"largerWorkTitle":"Natural resources and american citizenship: Transactions of the twenty-fifth North American wildlife and natural resources conference","largerWorkSubtype":{"id":12,"text":"Conference publication"},"conferenceTitle":"North American Wildlife and Natural Resources Conference: 25th","conferenceDate":"Mar 7-9, 1960","conferenceLocation":"Dallas, TX","language":"English","publisher":"Wildlife Management Institute","usgsCitation":"Jensen, W.I., and Allen, J.P., 1960, A possible relationship between aquatic invertebrates and avian botulism, in Natural resources and american citizenship: Transactions of the twenty-fifth North American wildlife and natural resources conference, Dallas, TX, Mar 7-9, 1960, p. 171-180.","productDescription":"10 p.","startPage":"171","endPage":"180","costCenters":[],"links":[{"id":373379,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United States","state":"Utah","otherGeospatial":"Bear River Migratory Bird Refuge","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"type\": \"Polygon\",\n \"coordinates\": [\n [\n [\n -112.46292114257812,\n 41.39844522006508\n ],\n [\n -112.04132080078125,\n 41.39844522006508\n ],\n [\n -112.04132080078125,\n 41.5579215778042\n ],\n [\n -112.46292114257812,\n 41.5579215778042\n ],\n [\n -112.46292114257812,\n 41.39844522006508\n ]\n ]\n ]\n }\n }\n ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","contributors":{"authors":[{"text":"Jensen, W. I.","contributorId":74705,"corporation":false,"usgs":true,"family":"Jensen","given":"W.","email":"","middleInitial":"I.","affiliations":[],"preferred":false,"id":785157,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Allen, Jack P.","contributorId":223482,"corporation":false,"usgs":false,"family":"Allen","given":"Jack","email":"","middleInitial":"P.","affiliations":[],"preferred":false,"id":785158,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":70220539,"text":"70220539 - 1960 - Thickness and consolidation of deep-sea sediments: A discussion","interactions":[],"lastModifiedDate":"2021-05-18T18:19:13.269155","indexId":"70220539","displayToPublicDate":"1960-12-31T13:15:14","publicationYear":"1960","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":5935,"text":"Bulletin of the Geological Society of America","active":true,"publicationSubtype":{"id":10}},"title":"Thickness and consolidation of deep-sea sediments: A discussion","docAbstract":"Hamilton (1959) concluded that in most sediments excess pore-water pressure is equal to zero - that is, the hydrostatic pressure is at atmospheric pressure. This note points out that in terrestrial environments the occurrence of artesian water (excess pore-water pressure) is commonplace and widespread and that such excess pressure is the source of energy for flowing water wells and for many flowing oil wells, \"gushers,\" or \"blowouts\".
","language":"English","publisher":"Geological Society of America","doi":"10.1130/0016-7606(1960)71[1727:TACODS]2.0.CO;2","usgsCitation":"Davis, G., 1960, Thickness and consolidation of deep-sea sediments: A discussion: Bulletin of the Geological Society of America, v. 71, no. 11, p. 1727-1728, https://doi.org/10.1130/0016-7606(1960)71[1727:TACODS]2.0.CO;2.","productDescription":"2 p.","startPage":"1727","endPage":"1728","costCenters":[],"links":[{"id":385726,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"71","issue":"11","noUsgsAuthors":false,"publicationStatus":"PW","contributors":{"authors":[{"text":"Davis, G.H.","contributorId":258184,"corporation":false,"usgs":false,"family":"Davis","given":"G.H.","email":"","affiliations":[],"preferred":false,"id":815918,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":70220538,"text":"70220538 - 1960 - Grid method of determining mean flow-distance in a drainage basin","interactions":[],"lastModifiedDate":"2021-05-18T18:10:19.763809","indexId":"70220538","displayToPublicDate":"1960-12-31T13:07:06","publicationYear":"1960","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":5334,"text":"International Association of Scientific Hydrology - Bulletin ","onlineIssn":"2150-3435","printIssn":"0262-6667","active":false,"publicationSubtype":{"id":10}},"title":"Grid method of determining mean flow-distance in a drainage basin","docAbstract":"The basin characteristics Σal or L ca are useful in hydrologic studies, but existing methods of determining them are either tedious or somewhat inaccurate. The grid method presented herein lessens the amount of tedious labor and provides an accurate measure of either Σal or L ca . An adaptation of the method could be used to compute the lag time for the basin.
","language":"English","publisher":"Taylor & Francis","doi":"10.1080/02626666009493188","usgsCitation":"Busby, M., and Benson, M.A., 1960, Grid method of determining mean flow-distance in a drainage basin: International Association of Scientific Hydrology - Bulletin , v. 5, no. 4, p. 32-36, https://doi.org/10.1080/02626666009493188.","productDescription":"5 p.","startPage":"32","endPage":"36","costCenters":[],"links":[{"id":480387,"rank":0,"type":{"id":40,"text":"Open Access Publisher Index Page"},"url":"https://doi.org/10.1080/02626666009493188","text":"Publisher Index Page"},{"id":385725,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"5","issue":"4","noUsgsAuthors":false,"publicationStatus":"PW","contributors":{"authors":[{"text":"Busby, M.W.","contributorId":16040,"corporation":false,"usgs":true,"family":"Busby","given":"M.W.","email":"","affiliations":[],"preferred":false,"id":815916,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Benson, M. A.","contributorId":32510,"corporation":false,"usgs":true,"family":"Benson","given":"M.","email":"","middleInitial":"A.","affiliations":[],"preferred":false,"id":815917,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":70220534,"text":"70220534 - 1960 - Transcurrent faulting and volcanism in Owens Valley, California","interactions":[],"lastModifiedDate":"2021-05-18T17:37:57.667428","indexId":"70220534","displayToPublicDate":"1960-12-31T12:33:49","publicationYear":"1960","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":5935,"text":"Bulletin of the Geological Society of America","active":true,"publicationSubtype":{"id":10}},"title":"Transcurrent faulting and volcanism in Owens Valley, California","docAbstract":"In the Owens Valley region of California, volcanic activity of Cenozoic age was confined mainly to three areas near the ends of important faults. The volcanic eruptions seemingly took place in regions of relative tension, if the horizontal movement along these faults was left lateral. The deep depression of Owens Valley may have resulted from compression associated with left-lateral horizontal fault movement. The transfer of molten rock from beneath this deep depression laterally into the regions of tension and thence to the surface seems to account for the relief of abnormal stresses and the volume of the volcanic rocks.
","language":"English","publisher":"Geological Society of America","doi":"10.1130/0016-7606(1960)71[153:TFAVIO]2.0.CO;2","usgsCitation":"Pakiser, L.C., 1960, Transcurrent faulting and volcanism in Owens Valley, California: Bulletin of the Geological Society of America, v. 71, no. 2, p. 153-160, https://doi.org/10.1130/0016-7606(1960)71[153:TFAVIO]2.0.CO;2.","productDescription":"8 p.","startPage":"153","endPage":"160","costCenters":[],"links":[{"id":385721,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United States","state":"California","otherGeospatial":"Owens Valley","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"type\": \"Polygon\",\n \"coordinates\": [\n [\n [\n -120.16845703125,\n 37.125286284966805\n ],\n [\n -118.47656249999999,\n 37.125286284966805\n ],\n [\n -118.47656249999999,\n 38.839707613545144\n ],\n [\n -120.16845703125,\n 38.839707613545144\n ],\n [\n -120.16845703125,\n 37.125286284966805\n ]\n ]\n ]\n }\n }\n ]\n}","volume":"71","issue":"2","noUsgsAuthors":false,"publicationStatus":"PW","contributors":{"authors":[{"text":"Pakiser, L. C.","contributorId":83512,"corporation":false,"usgs":true,"family":"Pakiser","given":"L.","email":"","middleInitial":"C.","affiliations":[],"preferred":false,"id":815911,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":70220533,"text":"70220533 - 1960 - Foothills fault system, western Sierra Nevada, California","interactions":[],"lastModifiedDate":"2021-05-18T17:31:01.879116","indexId":"70220533","displayToPublicDate":"1960-12-31T12:27:00","publicationYear":"1960","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":5935,"text":"Bulletin of the Geological Society of America","active":true,"publicationSubtype":{"id":10}},"title":"Foothills fault system, western Sierra Nevada, California","docAbstract":"A large fault system, here named the Foothills fault system, is the dominant structural feature of the western Sierra Nevada. The steeply dipping to vertical component faults trend northwestward through an area about 200 miles long and 30 miles wide north of 37°30' north latitude. The faulted Paleozoic and Mesozoic rocks are overlapped by unfaulted younger rocks, and the total extent of the fault system is not known. It is probably not limited to the western Sierra Nevada. Faults are marked by belts as much as 4 miles wide of cataclastically deformed and recrystallized rocks and by truncated folds. Along one fault, Upper Jurassic rocks are juxtaposed against Paleozoic rocks for at least 100 miles. The direction of fault movement has not been determined. Net displacement on some of the component faults exceeds 3000 feet and may be measurable in miles. Major faults cut beds of Late Jurassic age and are in turn cut by plutonic rocks of probable Late Jurassic and Middle Cretaceous age. Faults that controlled deposition of quartz veins and gold ore bodies of the Mother Lode belt are apparently younger and structurally less important features superimposed on one of the fault zones of the large system.
","language":"English","publisher":"Geological Society of America","doi":"10.1130/0016-7606(1960)71[483:FFSWSN]2.0.CO;2","usgsCitation":"Clark, L.D., 1960, Foothills fault system, western Sierra Nevada, California: Bulletin of the Geological Society of America, v. 71, no. 4, p. 483-496, https://doi.org/10.1130/0016-7606(1960)71[483:FFSWSN]2.0.CO;2.","productDescription":"14 p.","startPage":"483","endPage":"496","costCenters":[],"links":[{"id":385720,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United States","state":"California, Nevada","otherGeospatial":"Sierra Nevada Mountains","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"type\": \"Polygon\",\n \"coordinates\": [\n [\n [\n -121.025390625,\n 36.70365959719456\n ],\n [\n -117.75146484375,\n 36.70365959719456\n ],\n [\n -117.75146484375,\n 39.232253141714885\n ],\n [\n -121.025390625,\n 39.232253141714885\n ],\n [\n -121.025390625,\n 36.70365959719456\n ]\n ]\n ]\n }\n }\n ]\n}","volume":"71","issue":"4","noUsgsAuthors":false,"publicationStatus":"PW","contributors":{"authors":[{"text":"Clark, L. D.","contributorId":11189,"corporation":false,"usgs":true,"family":"Clark","given":"L.","email":"","middleInitial":"D.","affiliations":[],"preferred":false,"id":815910,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ]}