{"pageNumber":"5633","pageRowStart":"140800","pageSize":"25","recordCount":165626,"records":[{"id":70010095,"text":"70010095 - 1973 - Radial particle-size segregation during packing of particulates into cylindrical containers","interactions":[],"lastModifiedDate":"2020-12-30T15:10:51.612357","indexId":"70010095","displayToPublicDate":"1973-01-01T00:00:00","publicationYear":"1973","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":3107,"text":"Powder Technology","active":true,"publicationSubtype":{"id":10}},"title":"Radial particle-size segregation during packing of particulates into cylindrical containers","docAbstract":"<p>In a series of experiments, soil materials were placed in long cylindrical containers, using various packing procedures. Soil columns produced by deposition and simultaneous vibratory compaction were dense and axially uniform, but showed significant radial segregation of particle sizes. Similar results were obtained with deposition and simultaneous impact-type compaction when the impacts resulted in significant container “bouncing”. The latter procedure, modified to minimize “bouncing” produced dense, uniform soil columns, showing little radial particle-size segregation. Other procedures tested (deposition alone and deposition followed by compaction) did not result in radial segregation, but produced columns showing either relatively low or axially nonuniform densities.</p><p>Current data suggest that radial particle-size segregation is mainly due to vibration-induced particle circulation in which particles of various sizes have different circulation rates and paths.</p>","language":"English","publisher":"Elsevier","doi":"10.1016/0032-5910(73)80079-8","issn":"00325910","usgsCitation":"Ripple, C., James, R., and Rubin, J., 1973, Radial particle-size segregation during packing of particulates into cylindrical containers: Powder Technology, v. 8, no. 3-4, p. 165-175, https://doi.org/10.1016/0032-5910(73)80079-8.","productDescription":"11 p.","startPage":"165","endPage":"175","numberOfPages":"11","costCenters":[],"links":[{"id":219666,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"8","issue":"3-4","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"505a9390e4b0c8380cd80ed4","contributors":{"authors":[{"text":"Ripple, C.D.","contributorId":11586,"corporation":false,"usgs":true,"family":"Ripple","given":"C.D.","email":"","affiliations":[],"preferred":false,"id":357883,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"James, R.V.","contributorId":106634,"corporation":false,"usgs":true,"family":"James","given":"R.V.","email":"","affiliations":[],"preferred":false,"id":357885,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Rubin, J.","contributorId":26433,"corporation":false,"usgs":true,"family":"Rubin","given":"J.","email":"","affiliations":[],"preferred":false,"id":357884,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":70010292,"text":"70010292 - 1973 - 18O 16O ratios in cherts associated with the saline lake deposits of East Africa","interactions":[],"lastModifiedDate":"2023-12-14T00:52:52.624675","indexId":"70010292","displayToPublicDate":"1973-01-01T00:00:00","publicationYear":"1973","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1427,"text":"Earth and Planetary Science Letters","active":true,"publicationSubtype":{"id":10}},"title":"18O 16O ratios in cherts associated with the saline lake deposits of East Africa","docAbstract":"<div id=\"abstracts\" class=\"Abstracts u-font-serif text-s\"><div id=\"ab1\" class=\"abstract author\" lang=\"en\"><div id=\"aep-abstract-sec-id6\"><p>The cherts formed from sodium silicate precursors in East African saline, alkaline lakes have δ<sup>18</sup>O values ranging from 31.1 to 44.1. The δ<sup>18</sup>O values correlate in general with lake salinities as inferred from geologic evidence, indicating that most chert was formed from its precursor in contact with lake water trapped at the time of deposition. A few of the analyzed cherts probably formed in contact with dilute meteoric water. From the widely varying δ<sup>18</sup>O values we conclude that precursors were transformed to chert in fluids of widely varying salinity and a<sub>Na<sup>+</sup></sub>/a<sub>H<sup>+</sup></sub><span>&nbsp;</span>ratio.</p></div></div></div><ul id=\"issue-navigation\" class=\"issue-navigation u-margin-s-bottom u-bg-grey1\"></ul>","language":"English","publisher":"Elsevier","doi":"10.1016/0012-821X(73)90126-X","issn":"0012821X","usgsCitation":"O’Neil, J.R., and Hay, R.L., 1973, 18O 16O ratios in cherts associated with the saline lake deposits of East Africa: Earth and Planetary Science Letters, v. 19, no. 2, p. 257-266, https://doi.org/10.1016/0012-821X(73)90126-X.","productDescription":"10 p.","startPage":"257","endPage":"266","numberOfPages":"10","costCenters":[],"links":[{"id":219223,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"19","issue":"2","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"5059e22ae4b0c8380cd459eb","contributors":{"authors":[{"text":"O’Neil, J. R.","contributorId":69633,"corporation":false,"usgs":true,"family":"O’Neil","given":"J.","email":"","middleInitial":"R.","affiliations":[],"preferred":false,"id":358536,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Hay, R. L.","contributorId":34170,"corporation":false,"usgs":true,"family":"Hay","given":"R.","email":"","middleInitial":"L.","affiliations":[],"preferred":false,"id":358535,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":70010113,"text":"70010113 - 1973 - Isotopic composition of oil-field brines from Kettleman North Dome, California, and their geologic implications","interactions":[],"lastModifiedDate":"2020-12-30T15:25:29.654987","indexId":"70010113","displayToPublicDate":"1973-01-01T00:00:00","publicationYear":"1973","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":"Isotopic composition of oil-field brines from Kettleman North Dome, California, and their geologic implications","docAbstract":"<p>Deuterium and O<sup>18</sup><span>&nbsp;</span>analyses were made on 25 formation-water samples from Miocene (Temblor Formation) and Eocene (McAdams Formation) reservoir rocks at Kettleman North Dome oil field, California, and on three surface water samples from Reef Ridge located about three miles to the west of the field. The<span>&nbsp;</span><i>δO</i><sup>18</sup><span>&nbsp;</span>values obtained generally increase with depth and most probably are due to temperature controlled exchange reactions with carbonate cement and dissolved carbonate species. The δD values obtained seem to be controlled primarily by the membrane behavior of shales modifying the assumed original values. The contribution of isotopic exchange between water and clays cannot be evaluated at present.</p><p>The isotopic data support the conclusions based on a detailed study of geology, hydrodynamics, and formation water geochemistry (<span class=\"small-caps\">Kharaka</span>, 1971) which indicate that:</p><p>1. The Temblor Formation waters are probably meteoric in origin concentrated chemically and isotopically by shale membranes, and 2. The McAdams Formation waters were most probably obtained by squeezing the original interstitial marine connate waters of deposition from the underlying Mesozoic sediments.</p>","language":"English","publisher":"Elsevier","doi":"10.1016/0016-7037(73)90148-8","issn":"00167037","usgsCitation":"Kharaka, Y., Berry, F., and Friedman, I., 1973, Isotopic composition of oil-field brines from Kettleman North Dome, California, and their geologic implications: Geochimica et Cosmochimica Acta, v. 37, no. 8, p. 1899-1908, https://doi.org/10.1016/0016-7037(73)90148-8.","productDescription":"10 p.","startPage":"1899","endPage":"1908","numberOfPages":"10","costCenters":[],"links":[{"id":381758,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United States","state":"California","otherGeospatial":"Kettleman North Dome","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -119.58892822265626,\n              35.980228800645676\n            ],\n            [\n              -119.41177368164061,\n              35.980228800645676\n            ],\n            [\n              -119.41177368164061,\n              36.094609063015085\n            ],\n            [\n              -119.58892822265626,\n              36.094609063015085\n            ],\n            [\n              -119.58892822265626,\n              35.980228800645676\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","volume":"37","issue":"8","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"505a3fa3e4b0c8380cd646aa","contributors":{"authors":[{"text":"Kharaka, Y.K.","contributorId":23568,"corporation":false,"usgs":true,"family":"Kharaka","given":"Y.K.","email":"","affiliations":[],"preferred":false,"id":357954,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Berry, F.A.F.","contributorId":15755,"corporation":false,"usgs":true,"family":"Berry","given":"F.A.F.","email":"","affiliations":[],"preferred":false,"id":357953,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Friedman, I.","contributorId":95596,"corporation":false,"usgs":true,"family":"Friedman","given":"I.","email":"","affiliations":[],"preferred":false,"id":357955,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":70010055,"text":"70010055 - 1973 - Lead concentration and isotopic composition in five peridotite inclusions of probable mantle origin","interactions":[],"lastModifiedDate":"2020-12-29T20:58:05.380091","indexId":"70010055","displayToPublicDate":"1973-01-01T00:00:00","publicationYear":"1973","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1427,"text":"Earth and Planetary Science Letters","active":true,"publicationSubtype":{"id":10}},"title":"Lead concentration and isotopic composition in five peridotite inclusions of probable mantle origin","docAbstract":"<div id=\"abstracts\" class=\"Abstracts u-font-serif\"><div id=\"ab1\" class=\"abstract author\" lang=\"en\"><div id=\"aep-abstract-sec-id6\"><p>The lead content of five whole-rock peridotite inclusions (four lherzolites and one harzburgite) in alkali basalt ranges from 82 to 570 ppb (parts per billion). Approximately 30–60 ppb of this amount can be accounted for by analyzed major silicate minerals (olivine ≤ 10 ppb; enstatite 5–28 ppb; chrome diopside ∼400 ppb). Through a series of acid leaching experiments, the remainder of the lead is shown to be quite labile and to reside in either glassy or microcrystalline veinlets or accessory mineral phases, such as apatite and mica. The lead isotopic composition of the peridotites (<sup>206</sup>Pb/<sup>204</sup>Pb= 18.01–18.90;<sup>207</sup>Pb/<sup>204</sup>Pb= 15.52–15.61;<sup>208</sup>Pb/<sup>204</sup>Pb= 37.80–38.86) lies within the range of values defined by many modern volcanic rocks and, in particular, is essentially coextensive with the abyssal tholeiite field. In all but one instance, isotopic differences were found between the peridotite and its host alkali basalt. Two of the peridotites clearly demonstrated internal isotopic heterogeneity between<span>&nbsp;</span><i>leachable</i><span>&nbsp;</span>and<span>&nbsp;</span><i>residual</i><span>&nbsp;</span>fractions that could not simply be due to contamination by the host basalt. However, there is no evidence that these ultramafic rocks form some layer in the mantle with isotopic characteristics fundamentally different from those of the magma sources of volcanic rocks.</p></div></div></div><ul id=\"issue-navigation\" class=\"issue-navigation u-margin-s-bottom u-bg-grey1\"></ul>","language":"English","publisher":"Elsevier","doi":"10.1016/0012-821X(73)90139-8","issn":"0012821X","usgsCitation":"Zartman, R., and Tera, F., 1973, Lead concentration and isotopic composition in five peridotite inclusions of probable mantle origin: Earth and Planetary Science Letters, v. 20, no. 1, p. 54-66, https://doi.org/10.1016/0012-821X(73)90139-8.","productDescription":"13 p.","startPage":"54","endPage":"66","numberOfPages":"13","costCenters":[],"links":[{"id":218840,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"20","issue":"1","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"505a45b2e4b0c8380cd67481","contributors":{"authors":[{"text":"Zartman, R. E.","contributorId":15632,"corporation":false,"usgs":true,"family":"Zartman","given":"R. E.","affiliations":[],"preferred":false,"id":357785,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Tera, F.","contributorId":18102,"corporation":false,"usgs":true,"family":"Tera","given":"F.","email":"","affiliations":[],"preferred":false,"id":357786,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":70010123,"text":"70010123 - 1973 - Tertiary plate tectonics and high-pressure metamorphism in New Caledonia","interactions":[],"lastModifiedDate":"2020-12-30T20:31:49.041071","indexId":"70010123","displayToPublicDate":"1973-01-01T00:00:00","publicationYear":"1973","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":3525,"text":"Tectonophysics","active":true,"publicationSubtype":{"id":10}},"title":"Tertiary plate tectonics and high-pressure metamorphism in New Caledonia","docAbstract":"<p>The sialic basement of New Caledonia is a Permian-Jurassic greywacke sequence which was folded and metamorphosed to prehnite-pumpellyite or low-grade greenschist facies by the Late Jurassic. Succeeding Cretaceous-Eocene sediments unconformably overlie this basement and extend outwards onto oceanic crust. Tertiary tectonism occurred in three distinct phases.</p><dl class=\"list\"><dt class=\"list-label\">1. During the Late Eocene a nappe of peridotite was obducted onto southern New Caledonia from northeast to southwest, but without causing significant metamorphism in the underlying sialic rocks.</dt><dt class=\"list-label\">2. Oligocene compressive thrust tectonics in the northern part of the island accompanied a major east-west subduction zone, at least 30 km wide, which is identified by an imbricate system of tectonically intruded melanges and by development of lawsonite-bearing assemblages in adjacent country rocks; this high-pressure mineralogy constituted a primary metamorphism for the Cretaceous-Eocene sedimentary pile, but was overprinted on the Mesozoic prehnite-pumpellyite metagreywackes.</dt><dt class=\"list-label\">3. Post-Oligocene transcurrent faulting along a northwest-southeast line (the&nbsp;<i>sillon</i>) parallel to the west coast caused at least 150 km of dextral offset of the southwest frontal margin of the Eocene ultramafic nappe.</dt></dl><p>At the present time, the tectonics of the southwest Pacific are related to a series of opposite facing subduction (Benioff) zones connected by transform faults extending from New Britain-Solomon Islands south through the New Hebrides to New Zealand and marking the boundary between the Australian and Pacific plates. Available geologic data from this region suggest that a similar geometry existed during the Tertiary and that the microcontinents of New Guinea, New Caledonia and New Zealand all lay along the former plate boundary which has since migrated north and east by a complex process of sea-floor spreading behind the active island arcs.</p>","language":"English","publisher":"Elsevier","doi":"10.1016/0040-1951(73)90046-2","issn":"00401951","usgsCitation":"Brothers, R., and Blake, M., 1973, Tertiary plate tectonics and high-pressure metamorphism in New Caledonia: Tectonophysics, v. 17, no. 4, p. 337-358, https://doi.org/10.1016/0040-1951(73)90046-2.","productDescription":"22 p.","startPage":"337","endPage":"358","costCenters":[{"id":312,"text":"Geology, Minerals, Energy, and Geophysics Science Center","active":true,"usgs":true}],"links":[{"id":218927,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"17","issue":"4","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"505ba57fe4b08c986b320ab3","contributors":{"authors":[{"text":"Brothers, R.N.","contributorId":90866,"corporation":false,"usgs":true,"family":"Brothers","given":"R.N.","email":"","affiliations":[],"preferred":false,"id":358020,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Blake, M.C. Jr.","contributorId":27094,"corporation":false,"usgs":true,"family":"Blake","given":"M.C.","suffix":"Jr.","affiliations":[],"preferred":false,"id":358019,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":93791,"text":"93791 - 1973 - Duck plague (duck virus enteritis) in wild waterfowl","interactions":[],"lastModifiedDate":"2017-10-20T11:55:26","indexId":"93791","displayToPublicDate":"1973-01-01T00:00:00","publicationYear":"1973","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":6,"text":"USGS Unnumbered Series"},"title":"Duck plague (duck virus enteritis) in wild waterfowl","docAbstract":"<p>No abstract availablie.<br data-mce-bogus=\"1\"></p>","language":"English","publisher":"U.S. Government Printing Office","publisherLocation":"Washington, D.C.","doi":"10.3133/93791","usgsCitation":"Friend, M., and Pearson, G.L., 1973, Duck plague (duck virus enteritis) in wild waterfowl, 16 p., https://doi.org/10.3133/93791.","productDescription":"16 p.","costCenters":[{"id":456,"text":"National Wildlife Health Center","active":true,"usgs":true},{"id":480,"text":"Northern Prairie Wildlife Research Center","active":true,"usgs":true}],"links":[{"id":292377,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a5ee4b07f02db633b3e","contributors":{"authors":[{"text":"Friend, Milton 0000-0002-2882-3629","orcid":"https://orcid.org/0000-0002-2882-3629","contributorId":31332,"corporation":false,"usgs":true,"family":"Friend","given":"Milton","email":"","affiliations":[{"id":456,"text":"National Wildlife Health Center","active":true,"usgs":true}],"preferred":true,"id":297927,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Pearson, Gary L.","contributorId":76676,"corporation":false,"usgs":true,"family":"Pearson","given":"Gary","email":"","middleInitial":"L.","affiliations":[],"preferred":false,"id":297928,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":5778,"text":"pp765 - 1973 - Geology of the oxidized uranium ore deposits of the Tordilla Hill-Deweesville area, Karnes County, Texas; a study of a district before mining","interactions":[],"lastModifiedDate":"2023-03-23T21:52:46.450541","indexId":"pp765","displayToPublicDate":"1973-01-01T00:00:00","publicationYear":"1973","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":331,"text":"Professional Paper","code":"PP","onlineIssn":"2330-7102","printIssn":"1044-9612","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"765","title":"Geology of the oxidized uranium ore deposits of the Tordilla Hill-Deweesville area, Karnes County, Texas; a study of a district before mining","docAbstract":"<p>No abstract available.</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/pp765","usgsCitation":"Bunker, C.M., and MacKallor, J., 1973, Geology of the oxidized uranium ore deposits of the Tordilla Hill-Deweesville area, Karnes County, Texas; a study of a district before mining: U.S. Geological Survey Professional Paper 765, Report: iii, 37 p.; 1 Plate: 41.00 x 28.00 inches, https://doi.org/10.3133/pp765.","productDescription":"Report: iii, 37 p.; 1 Plate: 41.00 x 28.00 inches","costCenters":[],"links":[{"id":32455,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/pp/0765/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":32454,"rank":3,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/pp/0765/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":118015,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/pp/0765/report-thumb.jpg"},{"id":414668,"rank":4,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_5037.htm","linkFileType":{"id":5,"text":"html"}}],"country":"United States","state":"Texas","county":"Karnes County","otherGeospatial":"Tordilla Hill-Deweesville area","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"coordinates\": [\n          [\n            [\n              -98.3214,\n              29\n            ],\n            [\n              -98.3214,\n              28.6017\n            ],\n            [\n              -97.9761,\n              28.6017\n            ],\n            [\n              -97.9761,\n              29\n            ],\n            [\n              -98.3214,\n              29\n            ]\n          ]\n        ],\n        \"type\": \"Polygon\"\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b1be4b07f02db6a9040","contributors":{"authors":[{"text":"Bunker, C. M.","contributorId":75138,"corporation":false,"usgs":true,"family":"Bunker","given":"C.","email":"","middleInitial":"M.","affiliations":[],"preferred":false,"id":151570,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"MacKallor, J. A.","contributorId":75528,"corporation":false,"usgs":true,"family":"MacKallor","given":"J. A.","affiliations":[],"preferred":false,"id":151571,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":5892,"text":"pp675 - 1973 - Landslides in the vicinity of the Fort Randall Reservoir, South Dakota","interactions":[{"subject":{"id":13546,"text":"ofr6556 - 1965 - Landslides in the vicinity of the Fort Randall Reservoir, South Dakota","indexId":"ofr6556","publicationYear":"1965","noYear":false,"title":"Landslides in the vicinity of the Fort Randall Reservoir, South Dakota"},"predicate":"SUPERSEDED_BY","object":{"id":5892,"text":"pp675 - 1973 - Landslides in the vicinity of the Fort Randall Reservoir, South Dakota","indexId":"pp675","publicationYear":"1973","noYear":false,"title":"Landslides in the vicinity of the Fort Randall Reservoir, South Dakota"},"id":1}],"lastModifiedDate":"2023-04-13T21:53:36.56182","indexId":"pp675","displayToPublicDate":"1973-01-01T00:00:00","publicationYear":"1973","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":331,"text":"Professional Paper","code":"PP","onlineIssn":"2330-7102","printIssn":"1044-9612","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"675","title":"Landslides in the vicinity of the Fort Randall Reservoir, South Dakota","docAbstract":"<p>No abstract available.</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/pp675","usgsCitation":"Erskine, C., 1973, Landslides in the vicinity of the Fort Randall Reservoir, South Dakota: U.S. Geological Survey Professional Paper 675, Report: iv, 65 p.; 5 Plates: 40.00x 35.00 inches or smaller, https://doi.org/10.3133/pp675.","productDescription":"Report: iv, 65 p.; 5 Plates: 40.00x 35.00 inches or smaller","costCenters":[],"links":[{"id":32741,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/pp/0675/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":32740,"rank":7,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/pp/0675/plate-5.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":32739,"rank":6,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/pp/0675/plate-4.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":32738,"rank":5,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/pp/0675/plate-3.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":32737,"rank":4,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/pp/0675/plate-2.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":104721,"rank":8,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_4991.htm","linkFileType":{"id":5,"text":"html"},"description":"4991"},{"id":32736,"rank":3,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/pp/0675/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":121477,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/pp/0675/report-thumb.jpg"}],"country":"United States","state":"South Dakota","otherGeospatial":"Fort Randall Reservoir","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"coordinates\": [\n          [\n            [\n              -98.45,\n              42.9833\n            ],\n            [\n              -98.45,\n              43.7667\n            ],\n            [\n              -99.4833,\n              43.7667\n            ],\n            [\n              -99.4833,\n              42.9833\n            ],\n            [\n              -98.45,\n              42.9833\n            ]\n          ]\n        ],\n        \"type\": \"Polygon\"\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b24e4b07f02db6ae5d7","contributors":{"authors":[{"text":"Erskine, Christopher F.","contributorId":92241,"corporation":false,"usgs":true,"family":"Erskine","given":"Christopher F.","affiliations":[],"preferred":false,"id":151756,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":36282,"text":"b1331C - 1973 - Petrography and stratigraphy of glacial drift, Mesabi-Vermilion Iron Range area, northeastern Minnesota","interactions":[],"lastModifiedDate":"2023-03-15T21:17:09.956941","indexId":"b1331C","displayToPublicDate":"1973-01-01T00:00:00","publicationYear":"1973","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":306,"text":"Bulletin","code":"B","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"1331","chapter":"C","title":"Petrography and stratigraphy of glacial drift, Mesabi-Vermilion Iron Range area, northeastern Minnesota","docAbstract":"<p>Glacial deposits in the Mesabi-Vermilion Iron Range area consist of four major till units and associated glaciofluvial sediments. Particle-size data and pebble, heavy-mineral, clay-mineral, and percentage-soluble content were used in addition to field description of color and texture to describe and correlate the drift units.</p>\n<p>The lowermost till unit, basal till, occurs in only a small number of mines, but the mines are scattered across the entire Iron Range. The till is dark gray to dark greenish gray and brownish gray, sandy, silty, and calcareous. Pebbles are largely granitic and metamorphic rocks of local origin, but include limestone, dolomite, shale, basalt, felsite, agate, and gabbro. Clay-mineral content is largely illite. The age of the till is probably middle or early Wisconsin but could be pre-Wisconsin.</p>\n<p>The middle till unit, bouldery till, is the thickest and most widespread of the four tills. It is gray, yellow, red, orange, or brown, sandy, silty, noncalcareous and contains abundant cobbles and boulders. Pebbles are largely granitic and metamorphic rocks of local origin, but also include gabbro, basalt, and felsite in minor amounts. Montmorillonite is the most common clay mineral. Colored bouldery till below gray bouldery till may be a separate subunit distinguished largely on particle-size differences, but the overall characteristics are similar to the other bouldery till. The till was deposited by the Rainy lobe, which has a minimum age of 14,000 to 16,000 years before present.</p>\n<p>The uppermost, or surficial, tills were deposited contemporaneously by two minor sublobes of the Des Moines lobe about 12,000 years ago. Brown silty till occurs in the western and north-central part of the study area. It is light to medium brown, sandy, silty, and calcareous. Pebbles are largely granitic and metamorphic rocks of local origin, but include limestone, dolomite, shale, basalt, felsite, and gabbro. Clay-mineral content is largely mixed-layered montmorillonite and illite.</p>\n<p>Red clayey till occurs in the south-central part of the area. It is red to reddish brown, clayey, silty, and calcareous. Pebbles are similar to those in the brown silty till, but contain less limestone than the brown till.</p>\n<p>Glaciofluvial sediments are common between the various till units throughout the area, but are thickest near the east and near the west ends of the Iron Range.</p>","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Washington, D.C.","doi":"10.3133/b1331C","collaboration":"Prepared in cooperation with the Minnesota Department of Iron Range Resources and Rehabilitation","usgsCitation":"Winter, T.C., Cotter, R.D., and Young, H.L., 1973, Petrography and stratigraphy of glacial drift, Mesabi-Vermilion Iron Range area, northeastern Minnesota: U.S. Geological Survey Bulletin 1331, Document: iv, 41 p.; 2 Plates: 26.0 x 43.1 inches and 21.5 x 27.0 inches, https://doi.org/10.3133/b1331C.","productDescription":"Document: iv, 41 p.; 2 Plates: 26.0 x 43.1 inches and 21.5 x 27.0 inches","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[{"id":392,"text":"Minnesota Water Science Center","active":true,"usgs":true}],"links":[{"id":64217,"rank":3,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/bul/1331c/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":164873,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/bul/1331c/report-thumb.jpg"},{"id":64218,"rank":4,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/bul/1331c/plate-2.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":64219,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/bul/1331c/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":414263,"rank":5,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_21438.htm","linkFileType":{"id":5,"text":"html"}}],"country":"United States","state":"Minnesota","otherGeospatial":"Mesabi-Vermilion Iron Range Area","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"coordinates\": [\n          [\n            [\n              -91.793,\n              47.032\n            ],\n            [\n              -91.793,\n              47.975\n            ],\n            [\n              -93.775,\n              47.975\n            ],\n            [\n              -93.775,\n              47.032\n            ],\n            [\n              -91.793,\n              47.032\n            ]\n          ]\n        ],\n        \"type\": \"Polygon\"\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ae0e4b07f02db688026","contributors":{"authors":[{"text":"Winter, Thomas C.","contributorId":84736,"corporation":false,"usgs":true,"family":"Winter","given":"Thomas","email":"","middleInitial":"C.","affiliations":[],"preferred":false,"id":216065,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Cotter, R. D.","contributorId":89874,"corporation":false,"usgs":true,"family":"Cotter","given":"R.","email":"","middleInitial":"D.","affiliations":[{"id":595,"text":"U.S. Geological Survey","active":false,"usgs":true}],"preferred":false,"id":216066,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Young, H. L.","contributorId":23922,"corporation":false,"usgs":true,"family":"Young","given":"H.","email":"","middleInitial":"L.","affiliations":[],"preferred":false,"id":216064,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":37635,"text":"37635 - 1973 - History of salmon in the Great Lakes, 1850-1970","interactions":[],"lastModifiedDate":"2012-02-02T00:04:33","indexId":"37635","displayToPublicDate":"1973-01-01T00:00:00","publicationYear":"1973","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":1,"text":"Federal Government Series"},"seriesTitle":{"id":89,"text":"Technical Paper","active":false,"publicationSubtype":{"id":1}},"seriesNumber":"68","title":"History of salmon in the Great Lakes, 1850-1970","docAbstract":"This history of the salmon in the Great Lakes describes the decline and extinction of the Atlantic salmon (Salmo salar) in Lake Ontario in the 1800's; the failure to establish, by salmon culture, permanent or sizable populations of Atlantic or Pacific salmon in any of the Great Lakes in 1867-1965; and the success of the plantings of coho (Oncorhynchus kisutch) and chinook salmon (O. tshawytsha) in the Great Lakes, in 1966-70 -- particularly in Lake Michigan.\r\nDespite plantings of 5 million fry and fingerlings from Lake Ontario stocks in 1866-84, the native Atlantic salmon in Lake Ontario became extinct in the late 1800's primarily because tributaries in which they spawned were blocked by mill dams. Plantings of 13 million chinook salmon and landlocked and anadromous forms of Atlantic salmon in Lake Ontario and the other Great Lakes in 1873-1947 failed completely. The first species to develop a self-sustaining population was the pink salmon (O. gorbuscha), which was planted in Lake Superior in 1956; however, it has not become abundant.\r\nA salmon fishery finally was established when 15 million coho salmon and 6 million chinook salmon were planted as smolt in the Great Lakes in 1966-70. In 1970, for example, 576,000 coho salmon (12% of those planted in 1969) were caught by anglers in Lake Michigan. Most weighed 5 to 10 pounds (2.3-4.5 kg). Sport fishing for salmon was fair in Lakes Superior and Huron, and poor in Lakes Erie and Ontario.\r\nBy 1970, natural reproduction of coho, chinook, pink, and kokanee (O. nerka) salmon had occurred in some tributaries of one or more of the upper three Great Lakes. It is expected, however, that the sport fishery will continue to be supported almost entirely by planted fish.","language":"English","publisher":"U.S. Bureau of Sport Fisheries and Wildlife","usgsCitation":"Parsons, J.W., 1973, History of salmon in the Great Lakes, 1850-1970: Technical Paper 68, 80 p. illus. 26 cm.","productDescription":"80 p. illus. 26 cm.","startPage":"0","endPage":"80","numberOfPages":"80","costCenters":[{"id":324,"text":"Great Lakes Science Center","active":true,"usgs":true}],"links":[{"id":131720,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e491ae4b07f02db5730a8","contributors":{"authors":[{"text":"Parsons, John W.","contributorId":21899,"corporation":false,"usgs":true,"family":"Parsons","given":"John","email":"","middleInitial":"W.","affiliations":[],"preferred":false,"id":218376,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":17363,"text":"ofr7393 - 1973 - Mineral resources of the Alpine Lakes study area, Chelan, King, and Kittitas Counties, Washington, with a section on aeromagnetic interpretation","interactions":[],"lastModifiedDate":"2023-11-20T22:52:53.226768","indexId":"ofr7393","displayToPublicDate":"1973-01-01T00:00:00","publicationYear":"1973","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":"73-93","title":"Mineral resources of the Alpine Lakes study area, Chelan, King, and Kittitas Counties, Washington, with a section on aeromagnetic interpretation","docAbstract":"<p>No abstract available.</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr7393","usgsCitation":"Gualtieri, J.L., Simmons, G.C., Thurber, H.K., Miller, M.S., and Davis, W., 1973, Mineral resources of the Alpine Lakes study area, Chelan, King, and Kittitas Counties, Washington, with a section on aeromagnetic interpretation: U.S. Geological Survey Open-File Report 73-93, Report: v, 132 p.; 2 Plates: 43.04 x 31.93 inches and 43.32 x 31.55 inches, https://doi.org/10.3133/ofr7393.","productDescription":"Report: v, 132 p.; 2 Plates: 43.04 x 31.93 inches and 43.32 x 31.55 inches","costCenters":[],"links":[{"id":422751,"rank":5,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_8840.htm","linkFileType":{"id":5,"text":"html"}},{"id":46499,"rank":4,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1973/0093/plate-2.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":46498,"rank":3,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1973/0093/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":46500,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1973/0093/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":150844,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1973/0093/report-thumb.jpg"}],"country":"United States","state":"Washington","county":"Chelan County, King County, Kittitas County","otherGeospatial":"Alpine Lakes study area","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"coordinates\": [\n          [\n            [\n              -121.4,\n              47.767\n            ],\n            [\n              -121.4,\n              47.4\n            ],\n            [\n              -120.683,\n              47.4\n            ],\n            [\n              -120.683,\n              47.767\n            ],\n            [\n              -121.4,\n              47.767\n            ]\n          ]\n        ],\n        \"type\": \"Polygon\"\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a17e4b07f02db6046ad","contributors":{"authors":[{"text":"Gualtieri, James Louis","contributorId":46491,"corporation":false,"usgs":true,"family":"Gualtieri","given":"James","email":"","middleInitial":"Louis","affiliations":[],"preferred":false,"id":176088,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Simmons, G. C.","contributorId":82737,"corporation":false,"usgs":true,"family":"Simmons","given":"G.","email":"","middleInitial":"C.","affiliations":[],"preferred":false,"id":176092,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Thurber, H. K.","contributorId":59457,"corporation":false,"usgs":true,"family":"Thurber","given":"H.","email":"","middleInitial":"K.","affiliations":[],"preferred":false,"id":176090,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Miller, M. S.","contributorId":69107,"corporation":false,"usgs":true,"family":"Miller","given":"M.","email":"","middleInitial":"S.","affiliations":[],"preferred":false,"id":176091,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"Davis, W. E.","contributorId":49228,"corporation":false,"usgs":true,"family":"Davis","given":"W. E.","affiliations":[],"preferred":false,"id":176089,"contributorType":{"id":1,"text":"Authors"},"rank":5}]}}
,{"id":70171173,"text":"70171173 - 1973 - Federal Great Lakes fishery research objectives, priorities, and projects","interactions":[],"lastModifiedDate":"2016-05-25T11:41:02","indexId":"70171173","displayToPublicDate":"1973-01-01T00:00:00","publicationYear":"1973","noYear":false,"publicationType":{"id":24,"text":"Conference Paper"},"publicationSubtype":{"id":19,"text":"Conference Paper"},"title":"Federal Great Lakes fishery research objectives, priorities, and projects","docAbstract":"<p><span>Fishery productivity of the Great Lakes has declined drastically since settlement of the area. Premium quality fishes of the Great Lakes such as whitefish, lake trout, and walleyes have been replaced by less desired species. This change is attributed to selective overfishing, pollution, and the extreme instability of fish populations. Sea lamprey predation is still a vexing problem but progress is being made in controlling this parasite. The federal fishery research program with headquarters in Ann Arbor, Michigan, has the objective of providing baseline information, needed in resource use decisions, about the fishes of the Great Lakes. Studies of the habitat requirements of fish are high priority. The program includes fish population assessments, studies of the effects of mercury and other contaminants on fish, thermal effects studies, and general investigation of the impact of engineering projects on Great Lakes fisheries. The work is closely coordinated with state and Canadian agencies&nbsp;</span><span>through the Great Lakes Fishery Commission. Four small research vessels and four field stations are utilized with a staff of 90 and an annual budget of about $1.5 million.</span></p>","largerWorkType":{"id":24,"text":"Conference Paper"},"largerWorkTitle":"Proceedings of the First Federal Conference on the Great Lakes","largerWorkSubtype":{"id":19,"text":"Conference Paper"},"conferenceTitle":"First Federal Conference on the Great Lakes","conferenceDate":"December 13-15, 1972","conferenceLocation":"Ann Arbor, MI","language":"English","publisher":"National Technical Information Service","usgsCitation":"Tait, H.D., 1973, Federal Great Lakes fishery research objectives, priorities, and projects, <i>in</i> Proceedings of the First Federal Conference on the Great Lakes, Ann Arbor, MI, December 13-15, 1972, p. 44-47.","productDescription":"4 p.","startPage":"44","endPage":"47","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[{"id":324,"text":"Great Lakes Science Center","active":true,"usgs":true}],"links":[{"id":321615,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"5746ccb8e4b07e28b662dca7","contributors":{"authors":[{"text":"Tait, Howard D.","contributorId":33805,"corporation":false,"usgs":true,"family":"Tait","given":"Howard","email":"","middleInitial":"D.","affiliations":[],"preferred":false,"id":630162,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":70176022,"text":"70176022 - 1973 - Ground-water discharge from the Edwards and associated limestones, San Antonio area, Texas, 1972","interactions":[],"lastModifiedDate":"2016-08-23T15:26:55","indexId":"70176022","displayToPublicDate":"1973-01-01T00:00:00","publicationYear":"1973","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":2,"text":"State or Local Government Series"},"seriesTitle":{"id":5177,"text":"Edwards Underground Water District Bulletin","active":true,"publicationSubtype":{"id":2}},"seriesNumber":"31","title":"Ground-water discharge from the Edwards and associated limestones, San Antonio area, Texas, 1972","docAbstract":"<p>No abstract available.</p>","language":"English","publisher":"Edwards Underground Water District","usgsCitation":"Puente, C., 1973, Ground-water discharge from the Edwards and associated limestones, San Antonio area, Texas, 1972: Edwards Underground Water District Bulletin 31, 8 p.","productDescription":"8 p.","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[{"id":583,"text":"Texas Water Science Center","active":true,"usgs":true}],"links":[{"id":327747,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"57bd73dde4b03fd6b7df2cfd","contributors":{"authors":[{"text":"Puente, Celso","contributorId":36140,"corporation":false,"usgs":true,"family":"Puente","given":"Celso","email":"","affiliations":[],"preferred":false,"id":646810,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":70175502,"text":"70175502 - 1973 - Time of travel of solutes, field observations of water quality, and suspended-sediment data for stream reaches in the Trinity River Basin, Texas, July 31 to August 14, 1972","interactions":[],"lastModifiedDate":"2016-08-15T14:53:47","indexId":"70175502","displayToPublicDate":"1973-01-01T00:00:00","publicationYear":"1973","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":"Time of travel of solutes, field observations of water quality, and suspended-sediment data for stream reaches in the Trinity River Basin, Texas, July 31 to August 14, 1972","docAbstract":"<p>No abstract available.</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/70175502","usgsCitation":"Ollman, R., 1973, Time of travel of solutes, field observations of water quality, and suspended-sediment data for stream reaches in the Trinity River Basin, Texas, July 31 to August 14, 1972: Open-File Report, 2 Sheets, https://doi.org/10.3133/70175502.","productDescription":"2 Sheets","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[{"id":583,"text":"Texas Water Science Center","active":true,"usgs":true}],"links":[{"id":326499,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"57b2e7cde4b03bcb0102e993","contributors":{"authors":[{"text":"Ollman, R.H.","contributorId":88806,"corporation":false,"usgs":true,"family":"Ollman","given":"R.H.","email":"","affiliations":[],"preferred":false,"id":645511,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":70175496,"text":"70175496 - 1973 - Annual compilation and analysis of hydrologic data for urban studies in the San Antonio, Texas, metropolitan area, 1971","interactions":[],"lastModifiedDate":"2017-06-14T11:10:34","indexId":"70175496","displayToPublicDate":"1973-01-01T00:00:00","publicationYear":"1973","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":"Annual compilation and analysis of hydrologic data for urban studies in the San Antonio, Texas, metropolitan area, 1971","docAbstract":"<p>No abstract available.</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/70175496","usgsCitation":"Steger, R., 1973, Annual compilation and analysis of hydrologic data for urban studies in the San Antonio, Texas, metropolitan area, 1971: Open-File Report, 109 p., https://doi.org/10.3133/70175496.","productDescription":"109 p.","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[{"id":583,"text":"Texas Water Science Center","active":true,"usgs":true}],"links":[{"id":326492,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"}],"country":"United States","state":"Texas","city":"San Antonio","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -98.8165283203125,\n              29.123373210819224\n            ],\n            [\n              -98.19580078125,\n              29.123373210819224\n            ],\n            [\n              -98.19580078125,\n              29.699982298744377\n            ],\n            [\n              -98.8165283203125,\n              29.699982298744377\n            ],\n            [\n              -98.8165283203125,\n              29.123373210819224\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"57b2e7b2e4b03bcb0102e83d","contributors":{"authors":[{"text":"Steger, R.D.","contributorId":78008,"corporation":false,"usgs":true,"family":"Steger","given":"R.D.","email":"","affiliations":[],"preferred":false,"id":645500,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":70175495,"text":"70175495 - 1973 - Annual compilation and analysis of hydrologic data for urban studies in the Dallas, Texas, metropolitan area, 1971","interactions":[],"lastModifiedDate":"2016-08-15T14:33:51","indexId":"70175495","displayToPublicDate":"1973-01-01T00:00:00","publicationYear":"1973","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":"Annual compilation and analysis of hydrologic data for urban studies in the Dallas, Texas, metropolitan area, 1971","docAbstract":"<p>No abstract available.</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/70175495","usgsCitation":"Massey, B., 1973, Annual compilation and analysis of hydrologic data for urban studies in the Dallas, Texas, metropolitan area, 1971: Open-File Report, 84 p., https://doi.org/10.3133/70175495.","productDescription":"84 p.","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[{"id":583,"text":"Texas Water Science Center","active":true,"usgs":true}],"links":[{"id":326491,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"57b2e7b2e4b03bcb0102e839","contributors":{"authors":[{"text":"Massey, B.C.","contributorId":102483,"corporation":false,"usgs":true,"family":"Massey","given":"B.C.","email":"","affiliations":[],"preferred":false,"id":645499,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":70175636,"text":"70175636 - 1973 - Ground water in selected areas in the Klamath Basin, Oregon","interactions":[],"lastModifiedDate":"2016-08-17T14:06:46","indexId":"70175636","displayToPublicDate":"1973-01-01T00:00:00","publicationYear":"1973","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":2,"text":"State or Local Government Series"},"seriesTitle":{"id":115,"text":"Ground Water Report","active":false,"publicationSubtype":{"id":2}},"title":"Ground water in selected areas in the Klamath Basin, Oregon","docAbstract":"<p><span class=\"EXLDetailsDisplayVal\">GROUNDWATER FEATURES OF SIX LOWLAND <span class=\"searchword\">AREAS</span> IN THE <span class=\"searchword\">KLAMATH</span> <span class=\"searchword\">BASIN</span> OF <span class=\"searchword\">OREGON</span>--<span class=\"searchword\">KLAMATH</span> MARSH AREA, AND SPRAGUE RIVER, SWAN LAKE, YONNA, POE, AND LANGELL VALLEYS--ARE DESCRIBED. RUGGED MOUNTAINS AND RIDGES SURROUND AND SEPARATE THESE LOWLANDS WHERE FLOORS RANGE IN ALTITUDE FROM 4,100 FEET IN POE VALLEY TO 4,600 FEET NORTH OF <span class=\"searchword\">KLAMATH</span> MARSH. THE SIX <span class=\"searchword\">AREAS</span> EXTEND OVER A NORTH-SOUTH DISTANCE OF 70 MILES, AN EAST-WEST DISTANCE OF 40 MILES, AND INCLUDE AN AREA OF APPROXIMATELY 600 SQUARE MILES. THE AREA IS SEMIARID AND RECEIVED ABOUT 14 TO 18 INCHES OF PRECIPITATION A YEAR. EXTINCT VOLCANOES AND THEIR EXTRUSIONS CHARACTERIZE THE AREA. MOST WELLS TAP PERMEABLE BASALT OR CINDERY RUBBLE BENEATH THE LACUSTRINE BEDS. THE DEPTHS OF WELLS RANGE FROM LESS THAN 50 TO NEARLY 2,000 FEET--MOST ARE BETWEEN 100 AND 1,000 FEET DEEP. FLOWING WELLS OCCUR IN ALL <span class=\"searchword\">AREAS</span> EXCEPT SWAN LAKE VALLEY. THE MOST EXTENSIVE AREA OF FLOWING WELLS IS IN THE SPRAGUE RIVER VALLEY, WHERE ABOUT 25 WELLS, SOME FLOWING MORE THAN 2,000 GPM, SUPPLY WATER FOR IRRIGATION. WATER LEVELS IN WELLS FLUCTUATE SEASONALLY FROM 1 TO 4 FEET. GROUNDWATER IN THE BASIN IS OF EXCELLENT QUALITY FOR DRINKING, IRRIGATION, AND MOST INDUSTRIAL USES. </span></p>","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Reston, VA","usgsCitation":"Leonard, A., and Harris, A., 1973, Ground water in selected areas in the Klamath Basin, Oregon: Ground Water Report.","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[{"id":518,"text":"Oregon Water Science Center","active":true,"usgs":true}],"links":[{"id":326724,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United States","state":"Oregon","otherGeospatial":"Klamath Basin","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"57b58acfe4b03bcb0104bba9","contributors":{"authors":[{"text":"Leonard, A.R.","contributorId":101669,"corporation":false,"usgs":true,"family":"Leonard","given":"A.R.","email":"","affiliations":[],"preferred":false,"id":645901,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Harris, A.B.","contributorId":92290,"corporation":false,"usgs":true,"family":"Harris","given":"A.B.","email":"","affiliations":[],"preferred":false,"id":645902,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":70171174,"text":"70171174 - 1973 - The role of the Bureau of Sport Fisheries and Wildlife in the Great Lakes","interactions":[],"lastModifiedDate":"2016-05-25T11:40:28","indexId":"70171174","displayToPublicDate":"1973-01-01T00:00:00","publicationYear":"1973","noYear":false,"publicationType":{"id":24,"text":"Conference Paper"},"publicationSubtype":{"id":19,"text":"Conference Paper"},"title":"The role of the Bureau of Sport Fisheries and Wildlife in the Great Lakes","docAbstract":"<p><span>Ecological blunders of man, such as timber exploitation, draining of wetlands, construction of canals and dams, and pollution have been mainly responsible for serious environmental degradation and catastrophic losses of fish and wildlife values in the Great Lakes Basin. Consequently, the major emphasis of the Bureau of Sport Fisheries and Wildlife must be on the protection and enhancement of the Great Lakes habitat -- primarily as a single large ecosystem, rather than as a number of political units separated by ecologically meaningless boundaries. By authority of Congress, the Bureau has long been concerned in the Great Lakes region with such diverse activities as establishing refuges for migratory waterfowl, conducting fishery research, evaluating the effects of federally sponsored water resource development projects on fish and wildlife, rearing and stocking of game fish, and assisting the states in fish and wildlife management by giving technical advice and financial assistance. Thus, the Bureau shares a strong common interest with other federal administrative units, as well as with state, interstate, and international agencies, in protecting, enhancing, and ensuring the wise use of fish and wildlife in the Great Lakes Basin.</span></p>","largerWorkType":{"id":24,"text":"Conference Paper"},"largerWorkTitle":"Proceedings of the First Federal Conference on the Great Lakes","largerWorkSubtype":{"id":19,"text":"Conference Paper"},"conferenceTitle":"First Federal Conference on the Great Lakes","conferenceDate":"December 13-15, 1972","conferenceLocation":"Ann Arbor, MI","language":"English","publisher":"National Technical Information Service","usgsCitation":"Hester, F.E., 1973, The role of the Bureau of Sport Fisheries and Wildlife in the Great Lakes, <i>in</i> Proceedings of the First Federal Conference on the Great Lakes, Ann Arbor, MI, December 13-15, 1972, p. 39-43.","productDescription":"5 p.","startPage":"39","endPage":"43","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[{"id":324,"text":"Great Lakes Science Center","active":true,"usgs":true}],"links":[{"id":321616,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"5746ccc5e4b07e28b662dd50","contributors":{"authors":[{"text":"Hester, F. Eugene","contributorId":169588,"corporation":false,"usgs":false,"family":"Hester","given":"F.","email":"","middleInitial":"Eugene","affiliations":[],"preferred":false,"id":630161,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":70190912,"text":"70190912 - 1973 - Selected hydrologic data, lower Bear River drainage basin, Box Elder County, Utah","interactions":[],"lastModifiedDate":"2017-09-17T11:55:57","indexId":"70190912","displayToPublicDate":"1973-01-01T00:00:00","publicationYear":"1973","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":2,"text":"State or Local Government Series"},"seriesTitle":{"id":5498,"text":"Utah Basic-Data Release","active":true,"publicationSubtype":{"id":2}},"seriesNumber":"23","title":"Selected hydrologic data, lower Bear River drainage basin, Box Elder County, Utah","docAbstract":"<p>This report presents selected basic data from a study of the ground- water resources of the lower Bear River drainage basin, Box Elder County, Utah. The study was made during 1970-72 by the U.S. Geological Survey in cooperation with the Utah Department of Natural Resources, Division of Water Rights. Incorporated in this report are data collected by the Geological Survey and by other organizations since 1935. This report is intended to make the data conveniently available and to supplement an interpretive report which will be published separately.<br></p>","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Salt Lake City, UT","collaboration":"Prepared in cooperation with The Utah Department of Natural Resources, Division of Water Rights","usgsCitation":"Bjorklund, L., and McGreevy, L.J., 1973, Selected hydrologic data, lower Bear River drainage basin, Box Elder County, Utah: Utah Basic-Data Release 23, iii, 22 p.","productDescription":"iii, 22 p.","numberOfPages":"29","costCenters":[{"id":610,"text":"Utah Water Science Center","active":true,"usgs":true}],"links":[{"id":345839,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"},{"id":345838,"rank":1,"type":{"id":15,"text":"Index Page"},"url":"https://www.waterrights.utah.gov/cgi-bin/docview.exe?Folder=TP21-1-460&Title=Basic+Data+Report+23"}],"country":"United States","state":"Utah","county":"Box Elder County","otherGeospatial":"Bear River drainage basin","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"59bf899ce4b091459a5e0887","contributors":{"authors":[{"text":"Bjorklund, L.J.","contributorId":14035,"corporation":false,"usgs":true,"family":"Bjorklund","given":"L.J.","email":"","affiliations":[],"preferred":false,"id":710680,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"McGreevy, L. J.","contributorId":108124,"corporation":false,"usgs":true,"family":"McGreevy","given":"L.","email":"","middleInitial":"J.","affiliations":[],"preferred":false,"id":710681,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":70046404,"text":"70046404 - 1973 - Floods in New York, 1971","interactions":[],"lastModifiedDate":"2019-06-11T15:18:47","indexId":"70046404","displayToPublicDate":"1973-01-01T00:00:00","publicationYear":"1973","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":"Floods in New York, 1971","docAbstract":"<p>This report, for the calendar year 1971, was prepared at the request of the New York State Department of Transportation under provisions of an agreement between the New York State Department of Environmental Conservation and the U.S. Geological Survey fore a cooperative statewide program investigate the water resources of the State. The report was complied in the New York, Water Resources Division, U.S. Geological Survey, under the direction of Robert J. Dingman, District Chief. The information was obtained from newspaper clippings, publications of the National Weather Service, and the Environmental Data Service, and the Environmental Data Service of the National Oceanic and Atmospheric Administration (\"Climatological Data\" and \"Storm Data\"), and records of the U.S. Geological Survey.</p>","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Albany, NY","doi":"10.3133/70046404","collaboration":"Prepared in cooperation with the New York State Department of Transportation and New York State Department of Environmental Conservation","usgsCitation":"Robison, F.L., 1973, Floods in New York, 1971: Open-File Report, iii, 33 p., https://doi.org/10.3133/70046404.","productDescription":"iii, 33 p.","numberOfPages":"40","additionalOnlineFiles":"N","costCenters":[],"links":[{"id":273607,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":274607,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/unnumbered/70046404/report.pdf"}],"country":"United States","state":"New York","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -79.765000,40.494444 ], [ -79.765000,45.011667 ], [ -71.790278,45.011667 ], [ -71.790278,40.494444 ], [ -79.765000,40.494444 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"51b846e6e4b03203c522b1cf","contributors":{"authors":[{"text":"Robison, F. Luman","contributorId":103264,"corporation":false,"usgs":true,"family":"Robison","given":"F.","email":"","middleInitial":"Luman","affiliations":[],"preferred":false,"id":479621,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":70045438,"text":"70045438 - 1973 - Summary of ground-water data, Post Headquarters and adjacent areas, White Sands Missile Range","interactions":[],"lastModifiedDate":"2018-10-30T13:01:07","indexId":"70045438","displayToPublicDate":"1973-01-01T00:00:00","publicationYear":"1973","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":"Summary of ground-water data, Post Headquarters and adjacent areas, White Sands Missile Range","docAbstract":"<p>Geohydrologic data have been obtained from more than 100 wells and test holes that have been drilled in the Post Headquarters and adjacent areas of White Sands Missile Range. Observation-well data show that, in general, a continuous decline of the water table has occurred in the vicinity of the well field since production began in 1949. Approximately 40,000 acre-feet of water has been produced from the aquifer to date (1972). </p><p>A series of maps are presented which show the changes that have occurred in the well field as the result of development.</p>","language":"English","publisher":"U.S Geological Survey","publisherLocation":"Albuquerque, NM","doi":"10.3133/70045438","collaboration":"Prepared in cooperation with White Sands Missile Range","usgsCitation":"Kelly, T.E., 1973, Summary of ground-water data, Post Headquarters and adjacent areas, White Sands Missile Range: Open-File Report, Report: 66 p.; 4 Plates: 28.47 x 46.17 inches or smaller, https://doi.org/10.3133/70045438.","productDescription":"Report: 66 p.; 4 Plates: 28.47 x 46.17 inches or smaller","numberOfPages":"68","additionalOnlineFiles":"N","costCenters":[],"links":[{"id":272733,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/unnumbered/70045438/report.pdf"},{"id":270992,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/unnumbered/70045438/report-thumb.jpg"},{"id":358953,"rank":3,"type":{"id":29,"text":"Figure"},"url":"https://pubs.usgs.gov/unnumbered/70045438/figure-30.pdf","text":"Figure 30","linkFileType":{"id":1,"text":"pdf"}},{"id":358954,"rank":4,"type":{"id":29,"text":"Figure"},"url":"https://pubs.usgs.gov/unnumbered/70045438/figure-31.pdf","text":"Figure 31","linkFileType":{"id":1,"text":"pdf"}},{"id":358955,"rank":5,"type":{"id":29,"text":"Figure"},"url":"https://pubs.usgs.gov/unnumbered/70045438/figure-32.pdf","text":"Figure 32","linkFileType":{"id":1,"text":"pdf"}},{"id":358956,"rank":6,"type":{"id":29,"text":"Figure"},"url":"https://pubs.usgs.gov/unnumbered/70045438/figure-33.pdf","text":"Figure 33","linkFileType":{"id":1,"text":"pdf"}}],"country":"United States","state":"New Mexico","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -106.61666667,\n              32.13333333\n            ],\n            [\n              -106.28333333,\n              32.13333333\n            ],\n            [\n              -106.28333333,\n              32.58333333\n            ],\n            [\n              -106.61666667,\n              32.58333333\n            ],\n            [\n              -106.61666667,\n              32.13333333\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"516e72efe4b00154e4368c48","contributors":{"authors":[{"text":"Kelly, T. E.","contributorId":63824,"corporation":false,"usgs":true,"family":"Kelly","given":"T.","email":"","middleInitial":"E.","affiliations":[],"preferred":false,"id":477500,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":70045441,"text":"70045441 - 1973 - Annual compilation and analysis of hydrologic data for urban studies  in the Austin, Texas Metropolitan Area, 1971","interactions":[],"lastModifiedDate":"2016-08-23T14:00:15","indexId":"70045441","displayToPublicDate":"1973-01-01T00:00:00","publicationYear":"1973","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":2,"text":"State or Local Government Series"},"seriesTitle":{"id":128,"text":"Open-File Report","active":false,"publicationSubtype":{"id":2}},"title":"Annual compilation and analysis of hydrologic data for urban studies  in the Austin, Texas Metropolitan Area, 1971","docAbstract":"<p>The U.S. Geological Survey, in cooperation with the Texas Water Development Board, began hydrologic studies in the Austin urban area in 1954. The objectives of this project are as follows: </p><p style=\"padding-left: 30px;\" data-mce-style=\"padding-left: 30px;\">1. To determine the effects of progressive urbanization on infiltration, rates of peak discharge, and rainfall-runoff relations in the Waller Creek watershed. </p><p style=\"padding-left: 30px;\" data-mce-style=\"padding-left: 30px;\">2. To provide rainfall-and-runoff data from the rural Wilbarger Creek watershed to be used for comparative purposes in determining the effects of existing and progressive urbanization in the Waller Creek watershed. </p><p style=\"padding-left: 30px;\" data-mce-style=\"padding-left: 30px;\">3. To provide applied research facilities for studies at the University of Texas at Austin. </p><p style=\"padding-left: 30px;\" data-mce-style=\"padding-left: 30px;\">The purpose of this report is to present rainfall-and-runoff data for the Waller Creek and Wilbarger Creek study areas for the 1971 water year (October 1, 1970, to September 30, 1971). </p><p style=\"padding-left: 30px;\" data-mce-style=\"padding-left: 30px;\">To facilitate the publication and distribution of this report at the earliest feasible time, certain material has been included that does not conform to the formal publication standards of the U.S. Geological Survey. </p>","language":"English","publisher":"U.S. Gelogical Survey, Water Resources Division","publisherLocation":"Reston, VA","collaboration":"Prepared in cooperation with the Texas Water Development Board","usgsCitation":"Tovar, F., 1973, Annual compilation and analysis of hydrologic data for urban studies  in the Austin, Texas Metropolitan Area, 1971: Open-File Report, iv, 73 p.","productDescription":"iv, 73 p.","numberOfPages":"77","additionalOnlineFiles":"N","temporalStart":"1970-10-01","temporalEnd":"1971-09-30","costCenters":[{"id":583,"text":"Texas Water Science Center","active":true,"usgs":true}],"links":[{"id":271000,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/unnumbered/70045441/report-thumb.jpg"},{"id":272734,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/unnumbered/70045441/report.pdf"}],"country":"United States","state":"Texas","city":"Austin","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"516e72dee4b00154e4368b7f","contributors":{"authors":[{"text":"Tovar, F.H.","contributorId":42116,"corporation":false,"usgs":true,"family":"Tovar","given":"F.H.","email":"","affiliations":[],"preferred":false,"id":477505,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":85560,"text":"85560 - 1973 - The use of fish bioassays to determine the rate of deactivation of pesticides","interactions":[],"lastModifiedDate":"2012-02-02T00:15:15","indexId":"85560","displayToPublicDate":"1973-01-01T00:00:00","publicationYear":"1973","noYear":false,"publicationType":{"id":5,"text":"Book chapter"},"publicationSubtype":{"id":24,"text":"Book Chapter"},"title":"The use of fish bioassays to determine the rate of deactivation of pesticides","docAbstract":"Abstract not submitted to date","largerWorkType":{"id":4,"text":"Book"},"largerWorkTitle":"Bioassay techniques and environmental chemistry","largerWorkSubtype":{"id":4,"text":"Other Government Series"},"language":"English","publisher":"Ann Arbor Science Publishers Inc.","publisherLocation":"Ann Arbor, MI","usgsCitation":"Marking, L.L., and Walker, C., 1973, The use of fish bioassays to determine the rate of deactivation of pesticides, chap. <i>of</i> Bioassay techniques and environmental chemistry, 357-366.","productDescription":"357-366","costCenters":[{"id":606,"text":"Upper Midwest Environmental Sciences Center","active":true,"usgs":true}],"links":[{"id":201423,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a5fe4b07f02db634977","contributors":{"editors":[{"text":"Glass, G.E.","contributorId":37853,"corporation":false,"usgs":true,"family":"Glass","given":"G.E.","email":"","affiliations":[],"preferred":false,"id":504524,"contributorType":{"id":2,"text":"Editors"},"rank":1}],"authors":[{"text":"Marking, L. L.","contributorId":90661,"corporation":false,"usgs":true,"family":"Marking","given":"L.","middleInitial":"L.","affiliations":[],"preferred":false,"id":296078,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Walker, C.R.","contributorId":69097,"corporation":false,"usgs":true,"family":"Walker","given":"C.R.","email":"","affiliations":[],"preferred":false,"id":296077,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":40880,"text":"ofr7358 - 1973 - Preliminary geologic map of the Calaveras Reservoir Quadrangle, Alameda and Santa Clara counties, California","interactions":[],"lastModifiedDate":"2022-09-16T12:36:46.257296","indexId":"ofr7358","displayToPublicDate":"1973-01-01T00:00:00","publicationYear":"1973","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":"73-58","title":"Preliminary geologic map of the Calaveras Reservoir Quadrangle, Alameda and Santa Clara counties, California","docAbstract":"<p>No abstract available.</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr7358","usgsCitation":"Dibblee, T.W., 1973, Preliminary geologic map of the Calaveras Reservoir Quadrangle, Alameda and Santa Clara counties, California: U.S. Geological Survey Open-File Report 73-58, 1 map, https://doi.org/10.3133/ofr7358.","productDescription":"1 map","costCenters":[],"links":[{"id":173588,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":106563,"rank":700,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_8835.htm","linkFileType":{"id":5,"text":"html"}},{"id":78757,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1973/0058/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}}],"scale":"24000","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ac8e4b07f02db67bc41","contributors":{"authors":[{"text":"Dibblee, T. W. Jr.","contributorId":95445,"corporation":false,"usgs":true,"family":"Dibblee","given":"T.","suffix":"Jr.","middleInitial":"W.","affiliations":[],"preferred":false,"id":224107,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":70010228,"text":"70010228 - 1973 - Inorganic chemical investigation by x-ray fluorescence analysis: The Viking Mars Lander","interactions":[],"lastModifiedDate":"2025-02-28T16:52:00.529379","indexId":"70010228","displayToPublicDate":"1973-01-01T00:00:00","publicationYear":"1973","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1963,"text":"Icarus","active":true,"publicationSubtype":{"id":10}},"title":"Inorganic chemical investigation by x-ray fluorescence analysis: The Viking Mars Lander","docAbstract":"<div class=\"u-margin-s-bottom\">The inorganic chemical investigation added in August 1972 to the Viking Lander scientific package will utilize an energy-dispersive X-ray fluorescence spectrometer in which four sealed, gas-filled proportional counters will detect X-rays emitted from samples of the Martian surface materials irradiated by X-rays from radioisotope sources (<sup>55</sup>Fe and<span>&nbsp;</span><sup>109</sup>Cd). The output of the proportional counters will be subjected to pulse-height analysis by an on-board step-scanning single-channel analyzer with adjustable counting periods. The data will be returned to Earth, via the Viking Orbiter relay system, and the spectra constructed, calibrated, and interpreted here. The instrument is inside the Lander body, and samples are to be delivered to it by the Viking Lander Surface Sampler. Calibration standards are an integral part of the instrument.</div><div class=\"u-margin-s-bottom\">The results of the investigation will characterize the surface materials of Mars as to elemental composition with accuracies ranging from a few tens of parts per million (at the trace-element level) to a few percent (for major elements) depending on the element in question. Elements of atomic number 11 or less are determined only as a group, though useful estimates of their individual abundances maybe achieved by indirect means. The expected radiation environment will not seriously hamper the measurements. Based on the results, inferences can be drawn regarding (1) the surface mineralogy and lithology; (2) the nature of weathering processes, past and present, and the question of equilibrium between the atmosphere and the surface; and (3) the extent and type of differentiation that the planet has undergone.</div><div class=\"u-margin-s-bottom\">The Inorganic Chemical Investigation supports and is supported by most other Viking Science investigations.</div>","language":"English","publisher":"Elsevier","doi":"10.1016/0019-1035(73)90048-1","issn":"00191035","usgsCitation":"Toulmin, P., Baird, A.K., Clark, B.C., Keil, K., and Rose, H.J., 1973, Inorganic chemical investigation by x-ray fluorescence analysis: The Viking Mars Lander: Icarus, v. 20, no. 2, p. 153-178, https://doi.org/10.1016/0019-1035(73)90048-1.","productDescription":"26 p.","startPage":"153","endPage":"178","numberOfPages":"26","costCenters":[],"links":[{"id":219294,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"20","issue":"2","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"505a3c08e4b0c8380cd629f4","contributors":{"authors":[{"text":"Toulmin, P. III","contributorId":81244,"corporation":false,"usgs":true,"family":"Toulmin","given":"P.","suffix":"III","email":"","affiliations":[],"preferred":false,"id":358368,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Baird, A. K.","contributorId":65148,"corporation":false,"usgs":true,"family":"Baird","given":"A.","email":"","middleInitial":"K.","affiliations":[],"preferred":false,"id":358366,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Clark, B. C.","contributorId":39918,"corporation":false,"usgs":true,"family":"Clark","given":"B.","middleInitial":"C.","affiliations":[],"preferred":false,"id":358364,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Keil, Klaus","contributorId":55955,"corporation":false,"usgs":true,"family":"Keil","given":"Klaus","email":"","affiliations":[],"preferred":false,"id":358365,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"Rose, H. J. Jr.","contributorId":79465,"corporation":false,"usgs":true,"family":"Rose","given":"H.","suffix":"Jr.","email":"","middleInitial":"J.","affiliations":[],"preferred":false,"id":358367,"contributorType":{"id":1,"text":"Authors"},"rank":5}]}}
]}