{"pageNumber":"5904","pageRowStart":"147575","pageSize":"25","recordCount":165658,"records":[{"id":70009780,"text":"70009780 - 1967 - The occurrence and origin of lamellar troilite in iron meteorites","interactions":[],"lastModifiedDate":"2024-03-07T16:19:02.936871","indexId":"70009780","displayToPublicDate":"1967-01-01T00:00:00","publicationYear":"1967","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":"The occurrence and origin of lamellar troilite in iron meteorites","docAbstract":"<p>A number of iron meteorites contain elongated inclusions consisting predominantly of troilite, which have been termed Reichenbach lamellae. Two types of inclusions exist, the first up to 6 cm long and 0·2 mm wide, the second up to 2 cm long and 3 mm wide. The first type contains troilite with subordinate daubreelite and is commonly rimmed by schreibersite and swathing kamacite; the second consists largely of troilite with daubreelite and rare graphite and silicate grains.</p><p>Both types formed from a residual sulfide melt after the solidification of Ni<img src=\"https://sdfestaticassets-us-east-1.sciencedirectassets.com/shared-assets/55/entities/sbnd.gif\" alt=\"single bond\" data-mce-src=\"https://sdfestaticassets-us-east-1.sciencedirectassets.com/shared-assets/55/entities/sbnd.gif\">Fe metal. Swatching kamacite surrounding troilite in iron meteorites formed by nucleation at the troilite-metal interface during the formation of the Widmanstätten texture.</p><p>Meteorites containing troilite inclusions of the second type appear to have cooled more rapidly than most iron meteorites.</p><p>In view of the confusion surrounding the use of the term Reichenbach lamella, it is suggested that the term be dropped from the literature.</p>","language":"English","publisher":"Elsevier","doi":"10.1016/S0016-7037(67)80027-9","issn":"00167037","usgsCitation":"Brett, R., and Henderson, E., 1967, The occurrence and origin of lamellar troilite in iron meteorites: Geochimica et Cosmochimica Acta, v. 31, no. 5, p. 721-730, https://doi.org/10.1016/S0016-7037(67)80027-9.","productDescription":"10 p.","startPage":"721","endPage":"730","costCenters":[],"links":[{"id":219644,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"31","issue":"5","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"505bae37e4b08c986b323f5c","contributors":{"authors":[{"text":"Brett, R.","contributorId":106632,"corporation":false,"usgs":true,"family":"Brett","given":"R.","email":"","affiliations":[],"preferred":false,"id":357120,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Henderson, E.P.","contributorId":100040,"corporation":false,"usgs":true,"family":"Henderson","given":"E.P.","email":"","affiliations":[],"preferred":false,"id":357119,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":70009964,"text":"70009964 - 1967 - Potassium-argon ages of recent rhyolites of the Mono and Inyo craters, California","interactions":[],"lastModifiedDate":"2023-12-13T13:24:56.6749","indexId":"70009964","displayToPublicDate":"1967-01-01T00:00:00","publicationYear":"1967","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":"Potassium-argon ages of recent rhyolites of the Mono and Inyo craters, California","docAbstract":"<div id=\"abstracts\" class=\"Abstracts u-font-serif text-s\"><div id=\"aep-abstract-id4\" class=\"abstract author\"><div id=\"aep-abstract-sec-id5\"><p id=\"SP0005\">Twenty-two KAr ages were determined for sanidine samples from 10 rhyolite domes of the Mono and Inyo Craters to test the applicability of KAr dating to volcanic rocks of Recent age. Comparison of the results with ‘blank’ and dosed analyses shows that radiogenic<span>&nbsp;</span><sup>40</sup>Ar was detected and was measured to within a factor of two or better. The estimated standard deviation of precision is 12% for analyses containing 5% or more radiogenic<span>&nbsp;</span><sup>40</sup>Ar. A statistical analysis suggests that real differences in apparent age were detected between three of the analyzed domes. The ages, which range from 6400 to 10,200 years for experiments with 5% or more radiogenic<span>&nbsp;</span><sup>40</sup>Ar, are, in general, consistent with ionium ages on 5 of the same samples and with glacial and<span>&nbsp;</span><sup>14</sup>C evidence of age. They suggest that most of the Mono Craters volcanos are on the order of 10,000 years old or less. The results also suggest that the problem of excess<span>&nbsp;</span><sup>40</sup>Ar may not be severe for KAr dating of volcanic rocks.</p></div></div></div>","language":"English","publisher":"Elsevier","doi":"10.1016/0012-821X(67)90050-7","issn":"0012821X","usgsCitation":"Dalrymple, G.B., 1967, Potassium-argon ages of recent rhyolites of the Mono and Inyo craters, California: Earth and Planetary Science Letters, v. 3, no. C, p. 289-298, https://doi.org/10.1016/0012-821X(67)90050-7.","productDescription":"10 p.","startPage":"289","endPage":"298","numberOfPages":"10","costCenters":[],"links":[{"id":219340,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"3","issue":"C","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"505a7eaee4b0c8380cd7a6a6","contributors":{"authors":[{"text":"Dalrymple, G. Brent","contributorId":55146,"corporation":false,"usgs":true,"family":"Dalrymple","given":"G.","email":"","middleInitial":"Brent","affiliations":[],"preferred":false,"id":357545,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":2198,"text":"wsp1832 - 1967 - Hydrology of the Valley-fill and carbonate-rock reservoirs, Pahrump Valley, Nevada-California","interactions":[],"lastModifiedDate":"2023-03-14T20:27:11.946442","indexId":"wsp1832","displayToPublicDate":"1967-01-01T00:00:00","publicationYear":"1967","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":"1832","title":"Hydrology of the Valley-fill and carbonate-rock reservoirs, Pahrump Valley, Nevada-California","docAbstract":"This is the second appraisal of the water supply of Pahrump Valley, made 15 years after the first cooperative study. In the first report the average recharge was estimated to be 23,000 acre-feet per year, only 1,000 acre-feet more than the estimate made in this report. All this recharge was considered to be available for development. Because of the difficulty in salvaging the subsurface outflow from the deep carbonate-rock reservoir, this report concludes that the perennial yield may be only 25,000 acre-feet. \r\n\r\nIn 1875, Bennetts and Manse Springs reportedly discharged a total of nearly 10,000 acre-feet of water from the valley-fill reservoir. After the construction of several flowing wells in 1910, the spring discharge began to decline. In the mid-1940's many irrigation wells were drilled, and large-capacity pumps were installed. During the 4-year period of this study (1959-62), the net pumping draft averaged about 25,000 acre-feet per year, or about twice the estimated yield. In 1962 Bennetts Spring was dry, and the discharge from Marse Spring was only 1,400 acre-feet. \r\n\r\nDuring the period February 1959-February 1962, pumping caused an estimated storage depletion of 45,000 acre-feet, or 15,000 acre-feet per year. If the overdraft is maintained, depletion of stored water will continue and pumping costs will increase. Water levels in the vicinity of the Pahrump, Manse, and Fowler Ranches declined more than ]0 feet in response to the pumping during this period, and they can be expected to continue to decline at ,the projected rate of more than 3 feet per year. \r\n\r\nThe chemical quality of the pumped water has been satisfactory for irrigation and domestic use. Recycling of water pumped or irrigation, however, could result in deterioration of the water quality with time.","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/wsp1832","usgsCitation":"Malmberg, G.T., 1967, Hydrology of the Valley-fill and carbonate-rock reservoirs, Pahrump Valley, Nevada-California: U.S. Geological Survey Water Supply Paper 1832, iv, 47 p., https://doi.org/10.3133/wsp1832.","productDescription":"iv, 47 p.","costCenters":[],"links":[{"id":414133,"rank":3,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_25037.htm","linkFileType":{"id":5,"text":"html"}},{"id":27854,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wsp/1832/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":138285,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wsp/1832/report-thumb.jpg"}],"country":"United States","state":"California, Nevada","otherGeospatial":"Pahrump Valley","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"coordinates\": [\n          [\n            [\n              -116.25,\n              36.467\n            ],\n            [\n              -116.25,\n              35.617\n            ],\n            [\n              -115.517,\n              35.617\n            ],\n            [\n              -115.517,\n              36.467\n            ],\n            [\n              -116.25,\n              36.467\n            ]\n          ]\n        ],\n        \"type\": \"Polygon\"\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ac9e4b07f02db67ca1e","contributors":{"authors":[{"text":"Malmberg, Glenn T.","contributorId":11196,"corporation":false,"usgs":true,"family":"Malmberg","given":"Glenn","email":"","middleInitial":"T.","affiliations":[],"preferred":false,"id":144812,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":1000252,"text":"1000252 - 1967 - Diatoms as food of larval sea lampreys in a small tributary of northern Lake Michigan","interactions":[],"lastModifiedDate":"2016-02-22T09:22:41","indexId":"1000252","displayToPublicDate":"1967-01-01T00:00:00","publicationYear":"1967","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":3624,"text":"Transactions of the American Fisheries Society","active":true,"publicationSubtype":{"id":10}},"title":"Diatoms as food of larval sea lampreys in a small tributary of northern Lake Michigan","docAbstract":"<p>The food and food preferences of sea lamprey ammocoetes have not been investigated. The food of the larval American brook lamprey, Lampetra lamottei, in the Great Lakes region consisted mainly of diatoms and desmids according to Creaser and Hann. Schroll discussed the biology of feeding of ammocoetes of Lampetra planeri and Eudontomyzon danfordi in Europe. This report presents data on the availability and use of diatoms by sea lamprey, Petromyzon marinus Linnaeus, ammocoetes in a small tributary of northern Lake Michigan.</p>","language":"English","publisher":"Taylor & Francis","doi":"10.1577/1548-8659(1967)96[224:DAFOLS]2.0.CO;2","usgsCitation":"Manion, P.J., 1967, Diatoms as food of larval sea lampreys in a small tributary of northern Lake Michigan: Transactions of the American Fisheries Society, v. 96, no. 2, p. 224-226, https://doi.org/10.1577/1548-8659(1967)96[224:DAFOLS]2.0.CO;2.","productDescription":"3 p.","startPage":"224","endPage":"226","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[{"id":324,"text":"Great Lakes Science Center","active":true,"usgs":true}],"links":[{"id":132768,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"96","issue":"2","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a9ae4b07f02db65da87","contributors":{"authors":[{"text":"Manion, Patrick J.","contributorId":99080,"corporation":false,"usgs":true,"family":"Manion","given":"Patrick","email":"","middleInitial":"J.","affiliations":[],"preferred":false,"id":308295,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":1000253,"text":"1000253 - 1967 - Morphological abnormalities among lampreys","interactions":[],"lastModifiedDate":"2023-12-06T22:24:33.709457","indexId":"1000253","displayToPublicDate":"1967-01-01T00:00:00","publicationYear":"1967","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1337,"text":"Copeia","active":true,"publicationSubtype":{"id":10}},"title":"Morphological abnormalities among lampreys","docAbstract":"The experimental control of the sea lamprey (Petromyzon marinus) in the Great Lakes has required the collection of thousands of lampreys.  Representatives of each life stage of the four species of the Lake Superior basin were examined for structural abnormalities.  The most common aberration was the presence of additional tails.  The accessory tails were always postanal and smaller than the normal tail.  The point of origin varied; the extra tails occurred on dorsal, ventral, or lateral surfaces.  Some of the extra tails were misshaped and curled, but others were normal in shape and pigment pattern.  Other abnormalities in larval sea lampreys were malformed or twisted tails and bodies.  The cause of the structural abnormalities is unknown.  The presence of extra caudal fins could be genetically controlled, or be due to partial amputation or injury followed by abnormal regeneration.  Few if any lampreys with structural abnormalities live to sexual maturity.","language":"English","publisher":"American Society of Ichthyologists and Herpetologists (ASIH)","doi":"10.2307/1442255","usgsCitation":"Manion, P.J., 1967, Morphological abnormalities among lampreys: Copeia, v. 1967, no. 3, p. 680-681, https://doi.org/10.2307/1442255.","productDescription":"2 p.","startPage":"680","endPage":"681","numberOfPages":"2","costCenters":[{"id":324,"text":"Great Lakes Science Center","active":true,"usgs":true}],"links":[{"id":132838,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"1967","issue":"3","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b02e4b07f02db698cb9","contributors":{"authors":[{"text":"Manion, Patrick J.","contributorId":99080,"corporation":false,"usgs":true,"family":"Manion","given":"Patrick","email":"","middleInitial":"J.","affiliations":[],"preferred":false,"id":308296,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":2001036,"text":"2001036 - 1967 - Labor-saving devices for bioassay laboratories","interactions":[],"lastModifiedDate":"2012-02-02T00:15:02","indexId":"2001036","displayToPublicDate":"1967-01-01T00:00:00","publicationYear":"1967","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":1,"text":"Federal Government Series"},"seriesTitle":{"id":39,"text":"Investigations in Fish Control","active":false,"publicationSubtype":{"id":1}},"seriesNumber":"21","title":"Labor-saving devices for bioassay laboratories","docAbstract":"Abstract not submitted to date","language":"English","publisher":"U.S. Bureau of Sport Fisheries and Wildlife","publisherLocation":"La Crosse, WI","usgsCitation":"Hesselberg, R., and Burress, R., 1967, Labor-saving devices for bioassay laboratories: Investigations in Fish Control 21, 8.","productDescription":"8","startPage":"0","endPage":"8","numberOfPages":"8","costCenters":[{"id":606,"text":"Upper Midwest Environmental Sciences Center","active":true,"usgs":true}],"links":[{"id":197972,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b32e4b07f02db6b453e","contributors":{"authors":[{"text":"Hesselberg, R.J.","contributorId":72339,"corporation":false,"usgs":true,"family":"Hesselberg","given":"R.J.","affiliations":[],"preferred":false,"id":325326,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Burress, R.M.","contributorId":21107,"corporation":false,"usgs":true,"family":"Burress","given":"R.M.","affiliations":[],"preferred":false,"id":325325,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":70009974,"text":"70009974 - 1967 - Ground-water research in the U.S.A.","interactions":[],"lastModifiedDate":"2023-09-29T15:15:47.424462","indexId":"70009974","displayToPublicDate":"1967-01-01T00:00:00","publicationYear":"1967","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1431,"text":"Earth-Science Reviews","active":true,"publicationSubtype":{"id":10}},"title":"Ground-water research in the U.S.A.","docAbstract":"Ground-water reservoirs and the overlying unsaturated zone-collectively, the \"subsurface\"-have an enormous capacity to supply water to wells and useful plants, to store water to meet future needs for the same purposes, and, under suitable precautions, to accept wastes. This capacity can be exploited on a maximum scale, however, only on the basis of information one or more orders of magnitude greater than that available at present on the distribution, recoverability, and replenishability of subsurface water. Because usable water must be made available, and waste water must be disposed of, at costs of only a cent or a few cents per cubic meter, there is a critical need for research to devise methods of accomplishing these water-management tasks at reasonable cost. Among the chief target areas for research in subsurface hydrology are permeability distribution, including vertical permeability; prediction of the departure of the storage coefficient from the theoretically \"instantaneous\" property assumed in flow equations; theory of unsaturated flow based on fundamental soil characteristics that can be measured practicably; geochemical relations including the effects of injecting water of one composition into zones occupied by waters of different composition, generation of acid mine water, occurrence of saline water, and salt-fresh-water relations in coastal and other areas; prediction of the fate of wastes injected underground; geophysical techniques both surface and subsurface to extend, at low cost, information obtained by other means; and practical techniques of artificial recharge, especially through wells. ?? 1967.","language":"English","publisher":"Elsevier","doi":"10.1016/0012-8252(67)90376-5","usgsCitation":"McGuinness, C.L., 1967, Ground-water research in the U.S.A.: Earth-Science Reviews, v. 3, no. C, p. 181-202, https://doi.org/10.1016/0012-8252(67)90376-5.","productDescription":"22 p.","startPage":"181","endPage":"202","numberOfPages":"22","costCenters":[{"id":493,"text":"Office of Ground Water","active":true,"usgs":true}],"links":[{"id":219579,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United States","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -130.67138671875,\n              54.686534234529695\n            ],\n            [\n              -129.9462890625,\n              55.36662484928637\n            ],\n            [\n              -130.1220703125,\n              56.145549500679074\n            ],\n            [\n              -131.9677734375,\n              56.9449741808516\n       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,{"id":70011548,"text":"70011548 - 1967 - Geological exploration in an East Coast submarine canyon from a research submersible","interactions":[],"lastModifiedDate":"2020-11-24T21:40:27.331881","indexId":"70011548","displayToPublicDate":"1967-01-01T00:00:00","publicationYear":"1967","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":3338,"text":"Science","active":true,"publicationSubtype":{"id":10}},"title":"Geological exploration in an East Coast submarine canyon from a research submersible","docAbstract":"<div class=\"panel-pane pane-highwire-panel-tabs-container article__body\"><div class=\"pane-content\"><div id=\"panels-ajax-tab-container-highwire_article_tabs\" class=\"panels-ajax-tab-container\" data-panels-ajax-tab-preloaded=\"jnl_sci_tab_art\"><div class=\"panels-ajax-tab-wrap-jnl_sci_tab_art\"><div class=\"panel-display panel-1col clearfix\"><div class=\"panel-panel panel-col\"><div><div class=\"panel-pane pane-highwire-markup\"><div class=\"pane-content\"><div class=\"highwire-markup\"><div id=\"content-block-markup\" data-highwire-cite-ref-tooltip-instance=\"highwire_reflinks_tooltip\" data-highwire-glossary-tooltip-instance=\"highwire_reflinks_tooltip\"><div class=\"article abstract-view \"><div id=\"abstract-1\" class=\"section abstract\"><p id=\"p-1\">Large talus blocks litter the flat floor of Oceanographer Canyon at a depth of 1460 meters; they indicate down-axis mass transport of floor sediment at an unknown time and rate. From 1460 to 1310 meters the sidewall is covered by unconsolidated sediment lying at 35° to 40° from the horizontal. An outcrop of Pleistocene or younger sediment at 1460 meters is probably a remnant of a former fill.</p></div></div><span id=\"related-urls\"></span></div></div></div></div></div></div></div></div></div></div></div>","language":"English","publisher":"AAAS","doi":"10.1126/science.158.3799.370","issn":"00368075","usgsCitation":"Trumbull, J.V., and McCamis, M., 1967, Geological exploration in an East Coast submarine canyon from a research submersible: Science, v. 158, no. 3799, p. 370-372, https://doi.org/10.1126/science.158.3799.370.","productDescription":"3 p.","startPage":"370","endPage":"372","numberOfPages":"3","costCenters":[],"links":[{"id":220980,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"158","issue":"3799","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"505a2260e4b0c8380cd56fb9","contributors":{"authors":[{"text":"Trumbull, J. V. A.","contributorId":17309,"corporation":false,"usgs":true,"family":"Trumbull","given":"J.","email":"","middleInitial":"V. A.","affiliations":[],"preferred":false,"id":361371,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"McCamis, M.J.","contributorId":29130,"corporation":false,"usgs":true,"family":"McCamis","given":"M.J.","email":"","affiliations":[],"preferred":false,"id":361372,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":70009975,"text":"70009975 - 1967 - On the chemistry of Jupiter's upper atmosphere","interactions":[],"lastModifiedDate":"2025-02-28T17:09:58.131404","indexId":"70009975","displayToPublicDate":"1967-01-01T00:00:00","publicationYear":"1967","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1963,"text":"Icarus","active":true,"publicationSubtype":{"id":10}},"title":"On the chemistry of Jupiter's upper atmosphere","docAbstract":"<p><span>We conduct a first investigation into the ion-molecule chemistry of the upper Jovian atmosphere. Experimental results show that intense ultraviolet radiation reacts with the constituents of the Jovian atmosphere to produce C</span><sub>2</sub><span>H</span><sub>4</sub><span>, C</span><sub>2</sub><span>H</span><sub>6</sub><span>, C</span><sub>3</sub><span>H</span><sub>8</sub><span>, and higher polymers. The general procedure for calculating both equilibrium and nonequilibrium abundances of these products is formulated and applied to the case of the surface passage of a satellite shadow. A specific example is made of ethylene, for which an analytical approximation gives 10</span><sup>10</sup><span>&nbsp;molecules in an atmospheric column of 1 cm</span><sup>2</sup><span>&nbsp;cross section after a very rapid rise to equilibrium. Such a concentration of ethylene does not substantially affect the infrared radiation in the shadow.</span></p>","language":"English","publisher":"Elsevier","doi":"10.1016/0019-1035(67)90050-4","issn":"00191035","usgsCitation":"Saslaw, W., and Wildey, R., 1967, On the chemistry of Jupiter's upper atmosphere: Icarus, v. 7, no. 1-3, p. 85-93, https://doi.org/10.1016/0019-1035(67)90050-4.","productDescription":"9 p.","startPage":"85","endPage":"93","numberOfPages":"9","costCenters":[],"links":[{"id":219580,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"7","issue":"1-3","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"505a6dbae4b0c8380cd752c2","contributors":{"authors":[{"text":"Saslaw, W.C.","contributorId":42350,"corporation":false,"usgs":true,"family":"Saslaw","given":"W.C.","email":"","affiliations":[],"preferred":false,"id":357569,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Wildey, R.L.","contributorId":9700,"corporation":false,"usgs":true,"family":"Wildey","given":"R.L.","email":"","affiliations":[],"preferred":false,"id":357568,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":1000362,"text":"1000362 - 1967 - The effect of the lamprey larvicide, 3-trifluormethyl-4-nitrophenol, on selected aquatic invertebrates","interactions":[],"lastModifiedDate":"2016-02-22T09:16:56","indexId":"1000362","displayToPublicDate":"1967-01-01T00:00:00","publicationYear":"1967","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":3624,"text":"Transactions of the American Fisheries Society","active":true,"publicationSubtype":{"id":10}},"title":"The effect of the lamprey larvicide, 3-trifluormethyl-4-nitrophenol, on selected aquatic invertebrates","docAbstract":"<p>The chemical compound 3-trifluoromethyl-4-nitrophenol (TFM) is used to control the sea lamprey (Petromyzon marinus) in the upper Great Lakes. It is introduced into streams in which sea lampreys have spawned, to kill the larvae. These 'treatments' are carried out at intervals shorter than the larval phase of the sea lamprey's life cycle (about 4 to 7 years) to prevent movement of the metamorphosed parasitic lampreys into the lakes. Most of the streams which contain sea lamprey larvae also have valuable resident fish or serve as spawning and nursery areas for fish of the Great Lakes. These species must be protected from both the direct toxic effects of the control method and from indirect effects such as destruction of food supplies. Studies have shown that TFM is nontoxic to most species of fish when used at the concentrations that kill larval lampreys. Information on the effect of TFM on aquatic invertebrates is meager. Applegate et al. reported that TFM was not harmful to selected invertebrates which they included in simulated stream tests. They also stated that no harmful effects to invertebrates were observed during actual stream application. The variety of invertebrate species used in simulated stream tests was limited, and close observation of invertebrates under stream conditions is difficult. Therefore, the present laboratory bioassays were conducted to determine the toxicity of TFM to representatives of a number of groups of invertebrates.</p>","language":"English","publisher":"Taylor & Francis","doi":"10.1577/1548-8659(1967)96[410:TEOTLL]2.0.CO;2","usgsCitation":"Smith, A.J., 1967, The effect of the lamprey larvicide, 3-trifluormethyl-4-nitrophenol, on selected aquatic invertebrates: Transactions of the American Fisheries Society, v. 96, no. 4, p. 410-413, https://doi.org/10.1577/1548-8659(1967)96[410:TEOTLL]2.0.CO;2.","productDescription":"4 p.","startPage":"410","endPage":"413","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[{"id":324,"text":"Great Lakes Science Center","active":true,"usgs":true}],"links":[{"id":132919,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"96","issue":"4","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a51e4b07f02db629e90","contributors":{"authors":[{"text":"Smith, Allen J.","contributorId":69937,"corporation":false,"usgs":true,"family":"Smith","given":"Allen","email":"","middleInitial":"J.","affiliations":[],"preferred":false,"id":308455,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":34623,"text":"b1163D - 1967 - Geology of the Taunton quadrangle, Bristol and Plymouth Counties, Massachusetts","interactions":[],"lastModifiedDate":"2023-03-23T22:08:57.607713","indexId":"b1163D","displayToPublicDate":"1967-01-01T00:00:00","publicationYear":"1967","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":"1163","chapter":"D","title":"Geology of the Taunton quadrangle, Bristol and Plymouth Counties, Massachusetts","docAbstract":"<p>No abstract available.</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/b1163D","usgsCitation":"Hartshorn, J.H., 1967, Geology of the Taunton quadrangle, Bristol and Plymouth Counties, Massachusetts: U.S. Geological Survey Bulletin 1163, Report: 67 p.; 1 Plate: 25.95 x 26.85 inches, https://doi.org/10.3133/b1163D.","productDescription":"Report: 67 p.; 1 Plate: 25.95 x 26.85 inches","costCenters":[],"links":[{"id":167559,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/bul/1163d/report-thumb.jpg"},{"id":96531,"rank":3,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/bul/1163d/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":96530,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/bul/1163d/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":109448,"rank":4,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_20926.htm","linkFileType":{"id":5,"text":"html"},"description":"20926"}],"country":"United States","state":"Massachusetts","county":"Bristol County, Plymouth County","otherGeospatial":"Taunton quadrangle","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"coordinates\": [\n          [\n            [\n              -71.125,\n              42\n            ],\n            [\n              -71.125,\n              41.875\n            ],\n            [\n              -71,\n              41.875\n            ],\n            [\n              -71,\n              42\n            ],\n            [\n              -71.125,\n              42\n            ]\n          ]\n        ],\n        \"type\": \"Polygon\"\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4acbe4b07f02db67e3a8","contributors":{"authors":[{"text":"Hartshorn, Joseph H.","contributorId":89862,"corporation":false,"usgs":true,"family":"Hartshorn","given":"Joseph","email":"","middleInitial":"H.","affiliations":[],"preferred":false,"id":213283,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":70010595,"text":"70010595 - 1967 - U.S. Geological Survey silicate rock standards","interactions":[],"lastModifiedDate":"2020-11-24T22:23:28.228634","indexId":"70010595","displayToPublicDate":"1967-01-01T00:00:00","publicationYear":"1967","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":"U.S. Geological Survey silicate rock standards","docAbstract":"<div id=\"abstracts\" class=\"Abstracts u-font-serif\"><div id=\"aep-abstract-id4\" class=\"abstract author\"><div id=\"aep-abstract-sec-id5\"><p>The U.S. Geological Survey has processed six silicate rocks to provide new reference samples to supplement G-1 and W-1. Complete conventional, rapid rock, and spectrochemical analyses by the U.S. Geological Survey are reported for a granite (replacement for G-1), a granodiorite, an andesite, a peridotite, a dunite, and a basalt. Analyses of variance for nickel, chromium, copper, and zirconium in each rock sample showed that for these elements, the rocks can be considered homogeneous. Spectrochemical estimates are given for the nickel, chromium, copper, and zirconium contents of the samples. The petrography of five of the six rocks is described and CIPW norms are presented.</p></div></div></div><ul id=\"issue-navigation\" class=\"issue-navigation u-margin-s-bottom u-bg-grey1\"></ul>","language":"English","publisher":"Elsevier","doi":"10.1016/0016-7037(67)90043-9","issn":"00167037","usgsCitation":"Flanagan, F., 1967, U.S. Geological Survey silicate rock standards: Geochimica et Cosmochimica Acta, v. 31, no. 3, p. 289-308, https://doi.org/10.1016/0016-7037(67)90043-9.","productDescription":"20 p.","startPage":"289","endPage":"308","numberOfPages":"20","costCenters":[],"links":[{"id":219094,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"31","issue":"3","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"505bbb14e4b08c986b3284b7","contributors":{"authors":[{"text":"Flanagan, F.J.","contributorId":50139,"corporation":false,"usgs":true,"family":"Flanagan","given":"F.J.","email":"","affiliations":[],"preferred":false,"id":359238,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":70169229,"text":"70169229 - 1967 - Government and industry cooperate in nuclear detonation","interactions":[],"lastModifiedDate":"2016-03-23T16:15:10","indexId":"70169229","displayToPublicDate":"1967-01-01T00:00:00","publicationYear":"1967","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1435,"text":"Earthquake Information Bulletin (USGS)","active":true,"publicationSubtype":{"id":10}},"title":"Government and industry cooperate in nuclear detonation","language":"English","publisher":"U.S Geological Survey","usgsCitation":"Mickey, M.V., 1967, Government and industry cooperate in nuclear detonation: Earthquake Information Bulletin (USGS), v. 1, no. 6, p. 2-3.","productDescription":"2 p.","startPage":"2","endPage":"3","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[],"links":[{"id":319268,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"1","issue":"6","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"56f3be42e4b0f59b85e02e8d","contributors":{"authors":[{"text":"Mickey, M. V.","contributorId":167743,"corporation":false,"usgs":false,"family":"Mickey","given":"M.","email":"","middleInitial":"V.","affiliations":[],"preferred":false,"id":623367,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":70010564,"text":"70010564 - 1967 - Precision measurement of lead isotopes ratios: preliminary analyses from the U.S. mine, Bingham Canyon, Utah","interactions":[],"lastModifiedDate":"2023-12-13T13:18:38.53336","indexId":"70010564","displayToPublicDate":"1967-01-01T00:00:00","publicationYear":"1967","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":"Precision measurement of lead isotopes ratios: preliminary analyses from the U.S. mine, Bingham Canyon, Utah","docAbstract":"<div id=\"abstracts\" class=\"Abstracts u-font-serif text-s\"><div id=\"ab1\" class=\"abstract author\" lang=\"en\"><div id=\"aep-abstract-sec-id8\"><p>A gas-source mass spectrometer has been constructed for the precise measurement of lead isotope ratios. Sixteen analyses on 4 different preparations of the same galena made over a period of 2 months gave 95% confidence limits (per analysis) of<span>&nbsp;</span><i><sup>206</sup>Pb/<sup>204</sup>Pb= 0.080%,<span>&nbsp;</span><sup>207</sup>Pb/<sup>206</sup>Pb= 0.042%and<sup>208</sup>Pb/<sup>206</sup>Pb= 0.046%</i>.</p><p>Eight samples from the U.S. mine in the Bingham district have a linear relationship over the 1% range of their<sup>206</sup>Pb/<sup>204</sup>Pb ratios. The simplest model fitting these data suggests that the lead was separated from a primary system<span>&nbsp;</span><i>(μ=8.98) 1630±150m.y.</i><span>&nbsp;</span>ago and subsequently mixed with a radiogenic lead of similar age; biotite K-Ar dates for altered intrusive rocks associated with the ores provide an apparent age of mineralization and suggest that isotopic evolution of the lead was terminated about 36 m.y. ago.</p></div></div></div>","language":"English","publisher":"Elsevier","doi":"10.1016/0012-821X(67)90195-1","issn":"0012821X","usgsCitation":"Stacey, J.S., Moore, W.J., and Rubright, R., 1967, Precision measurement of lead isotopes ratios: preliminary analyses from the U.S. mine, Bingham Canyon, Utah: Earth and Planetary Science Letters, v. 2, no. 5, p. 489-499, https://doi.org/10.1016/0012-821X(67)90195-1.","productDescription":"11 p.","startPage":"489","endPage":"499","numberOfPages":"11","costCenters":[],"links":[{"id":218966,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United States","state":"Utah","otherGeospatial":"Bingham Canyon","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"coordinates\": [\n          [\n            [\n              -112.3599157983052,\n              40.61550688525992\n            ],\n            [\n              -112.3599157983052,\n              40.21250278039901\n            ],\n            [\n              -111.85271775878975,\n              40.21250278039901\n            ],\n            [\n              -111.85271775878975,\n              40.61550688525992\n            ],\n            [\n              -112.3599157983052,\n              40.61550688525992\n            ]\n          ]\n        ],\n        \"type\": \"Polygon\"\n      }\n    }\n  ]\n}","volume":"2","issue":"5","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"505a8141e4b0c8380cd7b424","contributors":{"authors":[{"text":"Stacey, J. S.","contributorId":72785,"corporation":false,"usgs":true,"family":"Stacey","given":"J.","email":"","middleInitial":"S.","affiliations":[],"preferred":false,"id":359178,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Moore, W. J.","contributorId":84334,"corporation":false,"usgs":true,"family":"Moore","given":"W.","email":"","middleInitial":"J.","affiliations":[],"preferred":false,"id":359179,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Rubright, R.D.","contributorId":88871,"corporation":false,"usgs":true,"family":"Rubright","given":"R.D.","email":"","affiliations":[],"preferred":false,"id":359180,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":70171220,"text":"70171220 - 1967 - Dechlorination of 1,1,1-trichloro-2,2-bis(p-chlorophenyl)ethane by Aerobacter aerogenes: I. Metabolic products","interactions":[],"lastModifiedDate":"2023-09-14T13:22:34.991482","indexId":"70171220","displayToPublicDate":"1967-01-01T00:00:00","publicationYear":"1967","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":843,"text":"Applied Microbiology","active":true,"publicationSubtype":{"id":10}},"displayTitle":"Dechlorination of 1,1,1-trichloro-2,2-bis(<i>p</i>-chlorophenyl)ethane by <i>Aerobacter aerogenes</i>: I. Metabolic products","title":"Dechlorination of 1,1,1-trichloro-2,2-bis(p-chlorophenyl)ethane by Aerobacter aerogenes: I. Metabolic products","docAbstract":"<p><span>Whole cells or cell-free extracts of&nbsp;</span><i>Aerobacter aerogenes</i><span>&nbsp;catalyze the degradation of 1,1,1-trichloro-2,2-bis(</span><i>p</i><span>-chlorophenyl)ethane (DDT) in vitro to at least seven metabolites: 1,1-dichloro-2,2-bis(</span><i>p</i><span>-chlorophenyl)ethylene (DDE); 1,1-dichloro-2,2-bis(</span><i>p</i><span>-chlorophenyl)ethane (DDD); 1-chloro-2,2-bis(</span><i>p</i><span>-chlorophenyl)ethylene (DDMU); 1-chloro-2,2-bis(</span><i>p</i><span>-chlorophenyl)ethane (DDMS); unsym-bis(</span><i>p</i><span>-chlorophenyl)ethylene (DDNU); 2,2-bis(</span><i>p</i><span>-chlorophenyl)acetate (DDA); and 4,4&prime;-dichlorobenzophenone (DBP). The use of metabolic inhibitors together with&nbsp;</span><i>p</i><span>H and temperature studies indicated that discrete enzymes are involved. By use of the technique of sequential analysis, the metabolic pathway was shown to be: DDT &rarr; DDD &rarr;DDMU &rarr;DDMS &rarr; DDNU &rarr; DDA &rarr; DBP, or DDT &rarr; DDE. Dechlorination was marginally enhanced by light-activated flavin mononucleotide.</span></p>","language":"English","publisher":"American Society for Microbiology","doi":"10.1128/am.15.3.569-574.1967","usgsCitation":"Wedemeyer, G., 1967, Dechlorination of 1,1,1-trichloro-2,2-bis(p-chlorophenyl)ethane by Aerobacter aerogenes: I. Metabolic products: Applied Microbiology, v. 15, no. 3, p. 569-574, https://doi.org/10.1128/am.15.3.569-574.1967.","productDescription":"6 p.","startPage":"569","endPage":"574","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[{"id":192,"text":"Columbia Environmental Research Center","active":true,"usgs":true}],"links":[{"id":480346,"rank":2,"type":{"id":40,"text":"Open Access Publisher Index Page"},"url":"https://doi.org/10.1128/am.15.3.569-574.1967","text":"Publisher Index Page"},{"id":321683,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"15","issue":"3","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"5746ccb4e4b07e28b662dc63","contributors":{"authors":[{"text":"Wedemeyer, Gary","contributorId":169618,"corporation":false,"usgs":false,"family":"Wedemeyer","given":"Gary","affiliations":[],"preferred":false,"id":630300,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":33719,"text":"b1242E - 1967 - Coal resources of the Cape Lisburne-Colville River region, Alaska","interactions":[],"lastModifiedDate":"2023-03-03T22:56:57.772461","indexId":"b1242E","displayToPublicDate":"1967-01-01T00:00:00","publicationYear":"1967","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":"1242","chapter":"E","title":"Coal resources of the Cape Lisburne-Colville River region, Alaska","docAbstract":"<p>No abstract available.</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/b1242E","usgsCitation":"Barnes, F.F., 1967, Coal resources of the Cape Lisburne-Colville River region, Alaska: U.S. Geological Survey Bulletin 1242, Report: iii, 37 p.; 1 Plate: 30.14 x 19.48 inches, https://doi.org/10.3133/b1242E.","productDescription":"Report: iii, 37 p.; 1 Plate: 30.14 x 19.48 inches","costCenters":[],"links":[{"id":163762,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/bul/1242e/report-thumb.jpg"},{"id":96075,"rank":3,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/bul/1242e/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":96074,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/bul/1242e/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":109668,"rank":4,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_21324.htm","linkFileType":{"id":5,"text":"html"},"description":"21324"}],"country":"United States","state":"Alaska","otherGeospatial":"Cape Lisburne-Colville River region","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"coordinates\": [\n          [\n            [\n              -150,\n              71\n            ],\n            [\n              -166.417,\n              71\n            ],\n            [\n              -166.417,\n              68\n            ],\n            [\n              -150,\n              68\n            ],\n            [\n              -150,\n              71\n            ]\n          ]\n        ],\n        \"type\": \"Polygon\"\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b25e4b07f02db6aee1d","contributors":{"authors":[{"text":"Barnes, Farrell F.","contributorId":58624,"corporation":false,"usgs":true,"family":"Barnes","given":"Farrell","email":"","middleInitial":"F.","affiliations":[],"preferred":false,"id":211828,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":42164,"text":"ofr67251 - 1967 - Aeromagnetic map of the San Antonio Ranch, Baxter Spring, Lone Mountain, and Tonopah quadrangles and part of the Antelope Spring quadrangle, Nevada","interactions":[],"lastModifiedDate":"2023-03-21T19:58:28.028531","indexId":"ofr67251","displayToPublicDate":"1967-01-01T00:00:00","publicationYear":"1967","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":"67-251","title":"Aeromagnetic map of the San Antonio Ranch, Baxter Spring, Lone Mountain, and Tonopah quadrangles and part of the Antelope Spring quadrangle, Nevada","docAbstract":"<p>No abstract available.</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr67251","usgsCitation":"Water Resources Division, U.S. Geological Survey, 1967, Aeromagnetic map of the San Antonio Ranch, Baxter Spring, Lone Mountain, and Tonopah quadrangles and part of the Antelope Spring quadrangle, Nevada: U.S. Geological Survey Open-File Report 67-251, 1 Plate: 45.00 x 42.00 inches, https://doi.org/10.3133/ofr67251.","productDescription":"1 Plate: 45.00 x 42.00 inches","costCenters":[],"links":[{"id":172631,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":414492,"rank":3,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_8206.htm","linkFileType":{"id":5,"text":"html"}},{"id":98809,"rank":2,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1967/0251/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}}],"country":"United States","state":"Nevada","otherGeospatial":"San Antonio Ranch, Baxter Spring, Lone Mountain, Tonopah, and Antelope Spring quadrangles","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"coordinates\": [\n          [\n            [\n              -117.5,\n              38.5\n            ],\n            [\n              -117.5,\n              38\n            ],\n            [\n              -116.911,\n              38\n            ],\n            [\n              -116.911,\n              38.5\n            ],\n            [\n              -117.5,\n              38.5\n            ]\n          ]\n        ],\n        \"type\": \"Polygon\"\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4aefe4b07f02db69145b","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":530881,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":70139641,"text":"70139641 - 1967 - Northern part, Ten Mile and Taunton River basins","interactions":[],"lastModifiedDate":"2015-02-09T10:21:18","indexId":"70139641","displayToPublicDate":"1967-01-01T00:00:00","publicationYear":"1967","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":367,"text":"Massachusetts Hydrologic - Data Report","active":false,"publicationSubtype":{"id":6}},"seriesNumber":"10","title":"Northern part, Ten Mile and Taunton River basins","docAbstract":"<p>The northern part of the Ten Mile and Taunton River basins is an area of about 195 square miles within Norfolk, Plymouth, and Bristol Counties in southeastern Massachusetts. The northern boundary of the area (plate 1) is the drainage divide separating these basins from that of the Charles, Neponset, and Weymouth River basins. The western boundary is, for the most part, the divide separating the basins from the Blackstone River basin. The eastern boundary is at the edge of the Brockton-Pembroke area (Petersen, 1962; Petersen and Shaw, 1961). The southern boundary in Seekonk is the northern limit of the East Providence quadrangle, for which a ground-water map was prepared by Allen and Gorman (1959); eastward, the southern boundaries of the city of Attleboro and the towns of Norton, Easton, and West Bridgewater form the southern boundary of the area.</p>\n<p>This report is one of two prepared by the Geological Survey for the Water Resources Commission. The principal purpose of this report is to make available the basic data on which the other, a map showing availability of ground water, is based. This basic-data report also can be used by engineers, planners, and others interested in or responsible for water-resources planning to determine the materials to be encountered (tables 3 and 4) and the yields which may be obtained from wells and test holes (tables 1 and 2) in the stratified sand and gravel that are the principal source of ground water and in bedrock. Partial and complete chemical analyses (tables 7 and 8) of these test holes and of some privately-owned wells provide information on the general quality of the water for domestic and other uses. A tabulation of existing municipal supplies, their capacity, production (table 5), and chemical quality of the water (table 6) may be used for regional planning purposes. Water-level measurements (figure 1) can be used to determine the annual fluctuations of the water table in certain types of materials. Seismic work (table 9) in the Canoe River valley, Norton, and test drilling with a power augur (tables 2 and 4) were done for the Geological Survey as&nbsp; part of the investigation.</p>","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Boston, MA","doi":"10.3133/70139641","collaboration":"Prepared in cooperation with the Commonwealth of Massachusetts, Water Resources Commission","usgsCitation":"Williams, J.R., and Willey, R.E., 1967, Northern part, Ten Mile and Taunton River basins: U.S. Geological Survey Massachusetts Hydrologic - Data Report 10, Report: 56 p.; 1 Map, https://doi.org/10.3133/70139641.","productDescription":"Report: 56 p.; 1 Map","numberOfPages":"62","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[],"links":[{"id":297609,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"}],"country":"United States","state":"Massachusetts","otherGeospatial":"Taunton River, Ten Mile River","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -71.378173828125,\n              41.87160608117939\n            ],\n            [\n              -71.378173828125,\n              42.187829010590825\n            ],\n            [\n              -70.9991455078125,\n              42.187829010590825\n            ],\n            [\n              -70.9991455078125,\n              41.87160608117939\n            ],\n            [\n              -71.378173828125,\n              41.87160608117939\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"54dd2c1ae4b08de9379b3627","contributors":{"authors":[{"text":"Williams, John R.","contributorId":107260,"corporation":false,"usgs":true,"family":"Williams","given":"John","email":"","middleInitial":"R.","affiliations":[{"id":595,"text":"U.S. Geological Survey","active":false,"usgs":true}],"preferred":false,"id":539477,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Willey, Richard E.","contributorId":30972,"corporation":false,"usgs":true,"family":"Willey","given":"Richard","email":"","middleInitial":"E.","affiliations":[],"preferred":false,"id":539478,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":70011659,"text":"70011659 - 1967 - Sulfide solubilities in alteration-controlled systems","interactions":[],"lastModifiedDate":"2020-11-24T20:54:01.352699","indexId":"70011659","displayToPublicDate":"1967-01-01T00:00:00","publicationYear":"1967","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":3338,"text":"Science","active":true,"publicationSubtype":{"id":10}},"title":"Sulfide solubilities in alteration-controlled systems","docAbstract":"<div class=\"panel-pane pane-highwire-panel-tabs-container article__body\"><div class=\"pane-content\"><div id=\"panels-ajax-tab-container-highwire_article_tabs\" class=\"panels-ajax-tab-container\" data-panels-ajax-tab-preloaded=\"jnl_sci_tab_art\"><div class=\"panels-ajax-tab-wrap-jnl_sci_tab_art\"><div class=\"panel-display panel-1col clearfix\"><div class=\"panel-panel panel-col\"><div><div class=\"panel-pane pane-highwire-markup\"><div class=\"pane-content\"><div class=\"highwire-markup\"><div id=\"content-block-markup\" data-highwire-cite-ref-tooltip-instance=\"highwire_reflinks_tooltip\" data-highwire-glossary-tooltip-instance=\"highwire_reflinks_tooltip\"><div class=\"article abstract-view \"><div id=\"abstract-1\" class=\"section abstract\"><p id=\"p-1\">Solubilities of sphalerite (ZnS) and galena (PbS) were determined at 300° to 500°C and 1000 bars total pressure in a chemical environment buffered by silicate mineral equilibria. Chloride solutions and muscovite-bearing assemblages characteristic of hydrothermal wall-rock alteration were used; weak acidities at temperature were therefore involved. The metal concentrations encountered tended to be higher than those observed in high bisulfide-H<sub>2</sub>S systems at neutral to weakly basic<span>&nbsp;</span>pH used in most previous experimentation; the chemical conditions of the work, although not completely satisfactory, are geologically more realistic than previous experimentation done in the basic-pH region.</p></div></div><span id=\"related-urls\"></span></div></div></div></div></div></div></div></div></div></div></div>","language":"English","publisher":"AAAS","doi":"10.1126/science.158.3808.1580","issn":"00368075","usgsCitation":"Hemley, J., Meyer, C., Hodgson, C., and Thatcher, A., 1967, Sulfide solubilities in alteration-controlled systems: Science, v. 158, no. 3808, p. 1580-1582, https://doi.org/10.1126/science.158.3808.1580.","productDescription":"3 p.","startPage":"1580","endPage":"1582","numberOfPages":"3","costCenters":[],"links":[{"id":221539,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"158","issue":"3808","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"505b9dc8e4b08c986b31da9e","contributors":{"authors":[{"text":"Hemley, J.J.","contributorId":59556,"corporation":false,"usgs":true,"family":"Hemley","given":"J.J.","email":"","affiliations":[],"preferred":false,"id":361636,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Meyer, C.","contributorId":108055,"corporation":false,"usgs":true,"family":"Meyer","given":"C.","email":"","affiliations":[],"preferred":false,"id":361638,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Hodgson, C.J.","contributorId":101013,"corporation":false,"usgs":true,"family":"Hodgson","given":"C.J.","email":"","affiliations":[],"preferred":false,"id":361637,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Thatcher, A.B.","contributorId":13751,"corporation":false,"usgs":true,"family":"Thatcher","given":"A.B.","email":"","affiliations":[],"preferred":false,"id":361635,"contributorType":{"id":1,"text":"Authors"},"rank":4}]}}
,{"id":70011608,"text":"70011608 - 1967 - Carbon-13-rich diagenetic carbonates in miocene formations of California and Oregon","interactions":[],"lastModifiedDate":"2020-11-24T21:11:12.723002","indexId":"70011608","displayToPublicDate":"1967-01-01T00:00:00","publicationYear":"1967","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":3338,"text":"Science","active":true,"publicationSubtype":{"id":10}},"title":"Carbon-13-rich diagenetic carbonates in miocene formations of California and Oregon","docAbstract":"<div class=\"panel-pane pane-highwire-panel-tabs-container article__body\"><div class=\"pane-content\"><div id=\"panels-ajax-tab-container-highwire_article_tabs\" class=\"panels-ajax-tab-container\" data-panels-ajax-tab-preloaded=\"jnl_sci_tab_art\"><div class=\"panels-ajax-tab-wrap-jnl_sci_tab_art\"><div class=\"panel-display panel-1col clearfix\"><div class=\"panel-panel panel-col\"><div><div class=\"panel-pane pane-highwire-markup\"><div class=\"pane-content\"><div class=\"highwire-markup\"><div id=\"content-block-markup\" data-highwire-cite-ref-tooltip-instance=\"highwire_reflinks_tooltip\" data-highwire-glossary-tooltip-instance=\"highwire_reflinks_tooltip\"><div class=\"article abstract-view \"><div id=\"abstract-1\" class=\"section abstract\"><p id=\"p-1\">Carbon unusually rich in C<sup>13</sup>(δC<sup>13</sup><span>&nbsp;</span>= +5.4 to +19.0 per mil relative to the Peedee belemnite carbonate standard of the University of Chicago) is characteristic of certain diagenetic limestones and dolomites in the Miocene Monterey Shale of California and the Nye Mudstone of Oregon. This heavy carbon may have originated through low-temperature equilibration between CO<sub>3</sub>- - and CO<sub>2</sub><span>&nbsp;</span>in migrating carbonated waters or between CH<sub>4</sub><span>&nbsp;</span>and CO<sub>2</sub><span>&nbsp;</span>in natural gas. Light carbon (δC<sup>13</sup><span>&nbsp;</span>= -5.6 to -18.2 per mil) derived through nonequilibrium oxidation of organic matter also occurs in the carbonate of Monterey Shale in some localities, but at most places it is much less common than heavy carbon.</p></div></div><span id=\"related-urls\"></span></div></div></div></div></div></div></div></div></div></div></div>","language":"English","publisher":"Nature","doi":"10.1126/science.156.3781.1484","issn":"00368075","usgsCitation":"Murata, K.J., Friedman, I., and Madsen, B., 1967, Carbon-13-rich diagenetic carbonates in miocene formations of California and Oregon: Science, v. 156, no. 3781, p. 1484-1486, https://doi.org/10.1126/science.156.3781.1484.","productDescription":"3 p.","startPage":"1484","endPage":"1486","numberOfPages":"3","costCenters":[],"links":[{"id":220847,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United States","state":"California, 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,{"id":70200881,"text":"wdrID661 - 1967 - Water resources data for Idaho, water year 1966; Part 1, Surface water records; Part 2, Water quality records","interactions":[],"lastModifiedDate":"2021-01-26T20:48:31.768535","indexId":"wdrID661","displayToPublicDate":"1966-01-01T10:39:47","publicationYear":"1967","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":340,"text":"Water Data Report","code":"WDR","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"ID-66-1","title":"Water resources data for Idaho, water year 1966; Part 1, Surface water records; Part 2, Water quality records","docAbstract":"<p>No abstract available.</p>","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Reston, VA","doi":"10.3133/wdrID661","collaboration":"Prepared in cooperation with the State of Idaho and with other agencies","usgsCitation":"U.S. Geological Survey, 1967, Water resources 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,{"id":70231177,"text":"70231177 - 1967 - Guidebook for the Annual Field Conference of Pennsylvania Geologists: Geology in the region of the Delaware to Lehigh water gaps","interactions":[],"lastModifiedDate":"2022-05-02T16:23:37.241868","indexId":"70231177","displayToPublicDate":"1964-12-31T11:11:00","publicationYear":"1967","noYear":false,"publicationType":{"id":4,"text":"Book"},"publicationSubtype":{"id":12,"text":"Conference publication"},"title":"Guidebook for the Annual Field Conference of Pennsylvania Geologists: Geology in the region of the Delaware to Lehigh water gaps","docAbstract":"<p>No abstract available.</p>","conferenceTitle":"32nd Annual Field Conference of Pennsylvania Geologists","conferenceDate":"Sep 29-30, 1967","conferenceLocation":"East Stroudsburg, PA","language":"English","publisher":"Field Conference of Pennsylvania Geologists","usgsCitation":"Epstein, J.B., and Epstein, A.G., 1967, Guidebook for the Annual Field Conference of Pennsylvania Geologists: Geology in the region of the Delaware to Lehigh water gaps, v. 32, iv, 89 p.","productDescription":"iv, 89 p.","costCenters":[{"id":243,"text":"Eastern Geology and Paleoclimate Science Center","active":true,"usgs":true}],"links":[{"id":399975,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"},{"id":399974,"rank":1,"type":{"id":15,"text":"Index Page"},"url":"https://www.fcopg.org/download-guidebooks"}],"country":"United States","state":"New Jersey, Pennsylvania","otherGeospatial":"Delaware River","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -74.8663330078125,\n              41.33970040774419\n            ],\n            [\n              -75.22064208984375,\n              40.94048973170136\n            ],\n            [\n              -75.0860595703125,\n              40.91973905106219\n            ],\n            [\n              -74.73175048828124,\n              41.25509730187495\n            ],\n            [\n              -74.8663330078125,\n              41.33970040774419\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","volume":"32","noUsgsAuthors":false,"publicationStatus":"PW","contributors":{"authors":[{"text":"Epstein, Jack B. jepstein@usgs.gov","contributorId":1412,"corporation":false,"usgs":true,"family":"Epstein","given":"Jack","email":"jepstein@usgs.gov","middleInitial":"B.","affiliations":[{"id":40020,"text":"Florence Bascom Geoscience Center","active":true,"usgs":true},{"id":243,"text":"Eastern Geology and Paleoclimate Science Center","active":true,"usgs":true}],"preferred":true,"id":841864,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Epstein, Anita G.","contributorId":47360,"corporation":false,"usgs":true,"family":"Epstein","given":"Anita","email":"","middleInitial":"G.","affiliations":[],"preferred":false,"id":841865,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":70198514,"text":"70198514 - 1966 - Geology and mineral resources of Frederick County","interactions":[],"lastModifiedDate":"2018-08-06T14:31:24","indexId":"70198514","displayToPublicDate":"2018-01-01T14:31:16","publicationYear":"1966","noYear":false,"publicationType":{"id":4,"text":"Book"},"title":"Geology and mineral resources of Frederick County","largerWorkTitle":"Virginia Division of Mineral Resources Bulletin","publisher":"Virginia Division of Mineral Resources","publisherLocation":"Charlottesville, VA","usgsCitation":"Butts, C., and Edmundson, R., 1966, Geology and mineral resources of Frederick County, v. 80, 142 p.","productDescription":"142 p.","costCenters":[{"id":37280,"text":"Virginia and West Virginia Water Science Center ","active":true,"usgs":true}],"links":[{"id":356202,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United States","state":"Virginia","county":"Frederick County","volume":"80","noUsgsAuthors":false,"publicationStatus":"PW","contributors":{"authors":[{"text":"Butts, Charles","contributorId":75988,"corporation":false,"usgs":true,"family":"Butts","given":"Charles","email":"","affiliations":[],"preferred":false,"id":741741,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Edmundson, R.S.","contributorId":206778,"corporation":false,"usgs":false,"family":"Edmundson","given":"R.S.","email":"","affiliations":[],"preferred":false,"id":741742,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":70180003,"text":"70180003 - 1966 - Developing a state water plan: Ground-water conditions in Utah, spring of 1966","interactions":[],"lastModifiedDate":"2017-01-23T11:32:16","indexId":"70180003","displayToPublicDate":"2016-12-01T00:00:00","publicationYear":"1966","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":2,"text":"State or Local Government Series"},"seriesTitle":{"id":110,"text":"Cooperative Investigations Report","active":true,"publicationSubtype":{"id":2}},"seriesNumber":"4","title":"Developing a state water plan: Ground-water conditions in Utah, spring of 1966","docAbstract":"<p>This report is the third in a series of annual reports that describe ground-water conditions in Utah. Reports in this series are prepared cooperatively by the U.S. Geological Survey and the Utah Water and Power Board and are designed to provide data to enable interested parties such as legislators, administrators, and planners to keep abreast of changing ground-water conditions.</p><p>This report, like the first two (Arnow and others, 1964, 1965), contains information on well construction, ground-water withdrawals, water-level changes, and related changes in precipitation and streamflow. It also contains supplementary data that are related to ground-water use in some individual areas. In reports of this series, the inclusion of such supplementary data as graphs showing chemical quality of water and maps showing water-table slope is intended only for those years or areas for which applicable data are available and are important to a discussion of changing ground-water conditions.</p><p>The report includes individual discussions of the most important areas of ground-water withdrawal in the State for the calendar year 1965. Water-level fluctuations, however, are described for the period spring 1965 through spring 1966. Many of the data used in the report were collected by the Geological Survey in cooperation with the Utah State Engineer.</p>","language":"English","publisher":"Utah Water and Power Board","publisherLocation":"Salt Lake City, UT","collaboration":"Prepared in cooperation with the State of Utah","usgsCitation":"Hood, J.W., Herbert, L.R., Butler, R., Mower, R.W., Handy, A., Cordova, R., Feltis, R., Bjorklund, L., Robinson, G., and Sandberg, G.W., 1966, Developing a state water plan: Ground-water conditions in Utah, spring of 1966: Cooperative Investigations Report 4, 95 p.","productDescription":"95 p.","numberOfPages":"96","costCenters":[{"id":610,"text":"Utah Water Science Center","active":true,"usgs":true}],"links":[{"id":333670,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"},{"id":333669,"rank":1,"type":{"id":15,"text":"Index Page"},"url":"https://www.waterrights.utah.gov/cgi-bin/libview.exe?Modinfo=Viewpub&LIBNUM=50-1-199"}],"country":"United States","state":"Utah","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"58863a15e4b0cad700058b6d","contributors":{"authors":[{"text":"Hood, J. 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,{"id":70179892,"text":"70179892 - 1966 - Bibliography of U.S. Geological Survey water-resources reports for Utah","interactions":[],"lastModifiedDate":"2017-01-19T16:47:01","indexId":"70179892","displayToPublicDate":"2016-12-01T00:00:00","publicationYear":"1966","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":2,"text":"State or Local Government Series"},"seriesTitle":{"id":5270,"text":"Utah Division of Water Rights Information Bulletin","active":false,"publicationSubtype":{"id":2}},"seriesNumber":"17","title":"Bibliography of U.S. Geological Survey water-resources reports for Utah","docAbstract":"<p>This bibliography contains a complete listing to December 1966 of reports relating to the water resources of Utah prepared by personnel of the U.S. Geological Survey. Discussions of the related subjects of geology, hydrology, and chemical quality of the water are included in many of the reports. The reports were, for the most part, prepared by personnel assigned to the Water Resources Division, Utah District, in cooperation with State and local agencies.</p>","language":"English","publisher":"Utah State Engineer's Office","publisherLocation":"Salt Lake City, UT","usgsCitation":"1966, Bibliography of U.S. Geological Survey water-resources reports for Utah: Utah Division of Water Rights Information Bulletin 17, 37 p.","productDescription":"37 p.","numberOfPages":"40","costCenters":[{"id":610,"text":"Utah Water Science Center","active":true,"usgs":true}],"links":[{"id":333497,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"},{"id":333496,"rank":1,"type":{"id":15,"text":"Index Page"},"url":"https://www.waterrights.utah.gov/cgi-bin/libview.exe?Modinfo=Viewpub&LIBNUM=21-4-340"}],"country":"United States","state":"Utah","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"5881def9e4b01192927d9ff9","contributors":{"compilers":[{"text":"Keller, Olive A.","contributorId":178486,"corporation":false,"usgs":true,"family":"Keller","given":"Olive","email":"","middleInitial":"A.","affiliations":[],"preferred":false,"id":659133,"contributorType":{"id":3,"text":"Compilers"},"rank":1}]}}
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