{"pageNumber":"6303","pageRowStart":"157550","pageSize":"25","recordCount":184937,"records":[{"id":1144,"text":"wsp1757M - 1972 - Significance of ground-water chemistry in performance of North Sahara Tube wells in Algeria and Tunisia","interactions":[],"lastModifiedDate":"2012-02-02T00:05:18","indexId":"wsp1757M","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1972","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":"1757","chapter":"M","title":"Significance of ground-water chemistry in performance of North Sahara Tube wells in Algeria and Tunisia","docAbstract":"Nine ground-water samples from the principal shallow and deep North Sahara aquifers of Algeria and Tunisia were examined to determine the relation of their chemical composition to corrosion and mineral encrustation thought to be contributing to observed decline in well capacities within a UNESCO/UNDP Special Fund Project area. Although the shallow and deep waters differ significantly in certain quality factors, all are sulfochloride types with corrosion potentials ranging from moderate to extreme. None appear to be sufficiently supersaturated with troublesome mineral species to cause rapid or severe encrustation of filter pipes or other well parts. However, calcium carbonate encrustation of deep-well cooling towers and related irrigation pipes can be expected because of loss of carbon dioxide and water during evaporative cooling. \r\n\r\nCorrosion products, particularly iron sulfide, can be expected to deposit in wells producing waters from the deep aquifers. This could reduce filterpipe openings and increase casing roughness sufficiently to cause significant reduction in well capacity. It seems likely, however, that normal pressure reduction due to exploitation of the artesian systems is a more important control of well performance. If troublesome corrosion and related encrustation are confirmed by downhole inspection, use of corrosion-resisting materials, such as fiber-glass casing and saw-slotted filter pipe (shallow wells only), or stainless-steel screen, will minimize the effects of the waters represented by these samples. A combination of corrosion-resisting stainless steel filter pipe electrically insulated from the casing with a nonconductive spacer and cathodic protection will minimize external corrosion of steel casing, if this is found to be a problem. However, such installations are difficult to make in very deep wells and difficult to control in remote areas. Both the shallow waters and the deep waters examined in this study will tend to cause soil salinization because their salt contents are relatively high, and both have sodium absorption ratios which are unfavorable to sodium-sensitive soils and vegetation. Proper drainage and soil treatment are the only means of overcoming these problems during irrigation.","language":"ENGLISH","publisher":"U.S. Govt. Print. Off.,","doi":"10.3133/wsp1757M","usgsCitation":"Clarke, F., and Jones, B.F., 1972, Significance of ground-water chemistry in performance of North Sahara Tube wells in Algeria and Tunisia: U.S. Geological Survey Water Supply Paper 1757, vi, M1-M39 p. :illus. ;24 cm., https://doi.org/10.3133/wsp1757M.","productDescription":"vi, M1-M39 p. :illus. ;24 cm.","costCenters":[],"links":[{"id":137623,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wsp/1757m/report-thumb.jpg"},{"id":25925,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wsp/1757m/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e49f9e4b07f02db5f3ccc","contributors":{"authors":[{"text":"Clarke, Frank Eldridge","contributorId":107255,"corporation":false,"usgs":true,"family":"Clarke","given":"Frank Eldridge","affiliations":[],"preferred":false,"id":143252,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Jones, Blair F. bfjones@usgs.gov","contributorId":2784,"corporation":false,"usgs":true,"family":"Jones","given":"Blair","email":"bfjones@usgs.gov","middleInitial":"F.","affiliations":[{"id":436,"text":"National Research Program - Eastern Branch","active":true,"usgs":true}],"preferred":true,"id":143251,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":1217,"text":"wsp1999H - 1972 - Subsurface geology of the late Tertiary and Quaternary water-bearing deposits of the southern part of the San Joaquin Valley, California","interactions":[],"lastModifiedDate":"2012-02-02T00:05:17","indexId":"wsp1999H","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1972","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":"1999","chapter":"H","title":"Subsurface geology of the late Tertiary and Quaternary water-bearing deposits of the southern part of the San Joaquin Valley, California","docAbstract":"The study area, which includes about 5,000 square miles of the southern part of the San Joaquin Valley, is a broad structural trough of mostly interior drainage. The Sierra Nevada on the east is composed of consolidated igneous and metamorphic rocks of pre-Tertiary age. The surface of these rocks slopes 4?-6? southwestward from the foothills and underlies the valley. The Coast Ranges on the west consist mostly of complexly folded and faulted consolidated marine and nonmarine sedimentary rocks of Jurassic, Cretaceous, and Tertiary age, which dip eastward and overlie the basement complex. Unconsolidated deposits, of late Pliocene to Holocene age, blanket the underlying consolidated rocks in the valley and are the source of most of the fresh ground water. The unconsolidated deposits, the subject of this report, are divided into informal stratigraphic units on the basis of source of sediment, environment of deposition, and texture. \r\n\r\nFlood-basin, lacustrine, and marsh deposits are fine grained and underlie the valley trough. They range in age from late Pliocene to Holocene. These deposits, consisting of nearly impermeable gypsiferous fine sand, silt, and clay, are more than 3,000 feet thick beneath parts of Tulare Lake bed. In other parts of the trough, flood-basin, lacustrine, and marsh deposits branch into clayey or silty clay tongues designated by the letter symbols A to F. Three of these tongues, the E, C, and A clays, lie beneath large areas of the southern part of the valley. \r\n\r\nThe E clay includes the Corcoran Clay Member of the Tulare Formation, the most extensive hydrologic confining layer in the valley. The E clay underlies about 3,500 square miles of bottom land and western slopes. The beds generally are dark-greenish-gray mostly diatomaceous silty clay of Pleistocene age. Marginally, the unit bifurcates into an upper and a lower stratum that contains thin beds of moderately yellowish-brown silt and sand. The E clay is warped into broad, gentle northwesterly trending anticlines and synclines. \r\n\r\nThe C clay, of Pleistocene age, is a fine-grained lacustrine or paludal deposit occurring 220-300 feet beneath Tulare Lake bed and parts of Fresno Slough. The beds consist of bluish-gray silty clay. Structural contours indicate that the C clay has been extensively warped and folded. \r\n\r\nThe A clay of Pleistocene and Holocene (?) age is a fine-grained lacustrine or paludal deposit occurring 10-60 feet beneath Buena Vista, Kern, and Tulare Lake beds, and parts of Fresno Slough. The clay is mainly blue or dark greenish gray, plastic, and highly organic. In some areas the unit is separated into an upper and a lower stratum by several feet of sand. A radiocarbon date of 26,780 ? 600 years was obtained from wood cored 3 feet beneath the clay. \r\n\r\nContinental deposits are arkosic beds of late Pliocene and Pleistocene (?) age and were derived from the Sierra Nevada, Tehachapi, and San Emigdio Mountains. In places, a reduced-oxidized contact transgresses the deposits derived from the Sierra Nevada. The reduced deposits consist of moderately permeable bluish-green or bluish-gray fine to medium sand, silt, and clay. The oxidized deposits consist mainly of poorly permeable yellowish-brown silt and fine sand. Deposits derived from the Tehachapi and the San Emigdio Mountains consist of poorly to moderately permeable yellowish-brown sand and silt. Continental and alluvial deposits of Tertiary and Quaternary age that were derived from the Coast Ranges consist mainly of poorly to moderately permeable yellowish-brown gravel, sand, silt, and clay. They include the Tulare Formation and overlying alluvial deposits. \r\n\r\nAlluvium is composed of coarse arkosic deposits derived from the Sierra Nevada, Tehachapi, and San Emigdio Mountains. A reduced-oxidized contact also transgresses the alluvial deposits derived from the Sierra Nevada. The oxidized deposits consist of poorly to highly permeable yellowish-brown gravel, sand, silt, and clay. The reduc","language":"ENGLISH","publisher":"U.S. Govt. Print. Off.,","doi":"10.3133/wsp1999H","usgsCitation":"Croft, M., 1972, Subsurface geology of the late Tertiary and Quaternary water-bearing deposits of the southern part of the San Joaquin Valley, California: U.S. Geological Survey Water Supply Paper 1999, iv, 29 p. :illus. and portfolio (6 plates) ;24 cm., https://doi.org/10.3133/wsp1999H.","productDescription":"iv, 29 p. :illus. and portfolio (6 plates) ;24 cm.","costCenters":[],"links":[{"id":137986,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wsp/1999h/report-thumb.jpg"},{"id":26116,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wsp/1999h/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":26117,"rank":401,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wsp/1999h/plate-2.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":26118,"rank":402,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wsp/1999h/plate-3.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":26119,"rank":403,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wsp/1999h/plate-4.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":26120,"rank":404,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wsp/1999h/plate-5.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":26121,"rank":405,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wsp/1999h/plate-6.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":26122,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wsp/1999h/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b05e4b07f02db699a52","contributors":{"authors":[{"text":"Croft, M.G.","contributorId":55413,"corporation":false,"usgs":true,"family":"Croft","given":"M.G.","email":"","affiliations":[],"preferred":false,"id":143384,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":63307,"text":"gq952 - 1972 - Geologic map of the Mount Harvard quadrangle, Chaffee and Gunnison Counties, Colorado","interactions":[{"subject":{"id":47078,"text":"ofr669 - 1966 - Geologic map of the Mt. Harvard quadrangle, Gunnison and Chaffee Counties, Colorado","indexId":"ofr669","publicationYear":"1966","noYear":false,"title":"Geologic map of the Mt. Harvard quadrangle, Gunnison and Chaffee Counties, Colorado"},"predicate":"SUPERSEDED_BY","object":{"id":63307,"text":"gq952 - 1972 - Geologic map of the Mount Harvard quadrangle, Chaffee and Gunnison Counties, Colorado","indexId":"gq952","publicationYear":"1972","noYear":false,"title":"Geologic map of the Mount Harvard quadrangle, Chaffee and Gunnison Counties, Colorado"},"id":1}],"lastModifiedDate":"2012-02-10T00:10:45","indexId":"gq952","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1972","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":316,"text":"Geologic Quadrangle","code":"GQ","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"952","title":"Geologic map of the Mount Harvard quadrangle, Chaffee and Gunnison Counties, Colorado","language":"ENGLISH","doi":"10.3133/gq952","usgsCitation":"Brock, M.R., and Barker, F., 1972, Geologic map of the Mount Harvard quadrangle, Chaffee and Gunnison Counties, Colorado: U.S. Geological Survey Geologic Quadrangle 952, 1 map :col. ;45 x 35 cm. on sheet 63 x 84 cm. folded to 26 x 21 cm. in envelope 30 x 24 cm., https://doi.org/10.3133/gq952.","productDescription":"1 map :col. ;45 x 35 cm. on sheet 63 x 84 cm. folded to 26 x 21 cm. in envelope 30 x 24 cm.","costCenters":[],"links":[{"id":103666,"rank":700,"type":{"id":15,"text":"Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_2252.htm","linkFileType":{"id":5,"text":"html"},"description":"2252"},{"id":249411,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/gq/0952/report.pdf","size":"38","linkFileType":{"id":1,"text":"pdf"}},{"id":252810,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/gq/0952/report-thumb.jpg"}],"scale":"62500","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -106.5,38.75 ], [ -106.5,39 ], [ -106.25,39 ], [ -106.25,38.75 ], [ -106.5,38.75 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4afce4b07f02db69659a","contributors":{"authors":[{"text":"Brock, M. R.","contributorId":96230,"corporation":false,"usgs":true,"family":"Brock","given":"M.","email":"","middleInitial":"R.","affiliations":[],"preferred":false,"id":268649,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Barker, Fred","contributorId":78332,"corporation":false,"usgs":true,"family":"Barker","given":"Fred","email":"","affiliations":[],"preferred":false,"id":268648,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":64285,"text":"gp839 - 1972 - Bouguer gravity and generalized geologic map of New England and adjoining areas","interactions":[],"lastModifiedDate":"2025-07-10T13:19:45.572237","indexId":"gp839","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1972","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":317,"text":"Geophysical Investigations Map","code":"GP","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"839","title":"Bouguer gravity and generalized geologic map of New England and adjoining areas","docAbstract":"<p>No abstract available.</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/gp839","usgsCitation":"Kane, M.F., Simmons, G., Diment, W., Fitzpatrick, M., Joyner, W.B., and Bromery, R.W., 1972, Bouguer gravity and generalized geologic map of New England and adjoining areas: U.S. Geological Survey Geophysical Investigations Map 839, Report: 6 p.; 1 Plate: 37.96 x 33.77 inches, https://doi.org/10.3133/gp839.","productDescription":"Report: 6 p.; 1 Plate: 37.96 x 33.77 inches","costCenters":[],"links":[{"id":491909,"rank":4,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_6192.htm","linkFileType":{"id":5,"text":"html"}},{"id":250899,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/gp/0839/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":250900,"rank":3,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/gp/0839/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":254317,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/gp/0839/report-thumb.jpg"}],"scale":"1000000","country":"United States","otherGeospatial":"New England","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"coordinates\": [\n          [\n            [\n              -66.8624533212809,\n              44.824136898815055\n            ],\n            [\n              -67.52495998966934,\n              45.59691566824631\n            ],\n            [\n              -67.8073398811139,\n              45.74869578591097\n            ],\n            [\n              -67.81820064616875,\n              47.13316009909525\n            ],\n            [\n              -68.32865660378042,\n              47.36906803336473\n            ],\n            [\n              -68.94180818680786,\n              47.171192878641335\n            ],\n            [\n              -69.07804939261327,\n              47.31755295835566\n            ],\n            [\n              -69.01512983773468,\n              47.42406324342426\n            ],\n            [\n              -69.2161454304456,\n              47.481029181715684\n            ],\n            [\n              -70.01220364951189,\n              46.665517774541826\n            ],\n            [\n              -70.9322742234754,\n              45.37370786389937\n            ],\n            [\n              -71.46468964077665,\n              45.11844402311891\n            ],\n            [\n              -74.75093571659585,\n              45.03573422019801\n            ],\n            [\n              -75.27824151112951,\n              42.15027816778536\n            ],\n            [\n              -72.83218722601997,\n              41.2249529600561\n            ],\n            [\n              -69.94938119322659,\n              41.175742545104725\n            ],\n            [\n              -69.55483706132496,\n              41.55760438046897\n            ],\n            [\n              -66.73399698655857,\n              44.826583253887975\n            ],\n            [\n              -66.8624533212809,\n              44.824136898815055\n            ]\n          ]\n        ],\n        \"type\": \"Polygon\"\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a13e4b07f02db601ef2","contributors":{"authors":[{"text":"Kane, M. F.","contributorId":45708,"corporation":false,"usgs":true,"family":"Kane","given":"M.","email":"","middleInitial":"F.","affiliations":[],"preferred":false,"id":270437,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Simmons, Gene","contributorId":50975,"corporation":false,"usgs":true,"family":"Simmons","given":"Gene","email":"","affiliations":[],"preferred":false,"id":270438,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Diment, W.H.","contributorId":54992,"corporation":false,"usgs":true,"family":"Diment","given":"W.H.","affiliations":[],"preferred":false,"id":270439,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Fitzpatrick, M.M.","contributorId":20413,"corporation":false,"usgs":true,"family":"Fitzpatrick","given":"M.M.","email":"","affiliations":[],"preferred":false,"id":270436,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"Joyner, W. B.","contributorId":70746,"corporation":false,"usgs":true,"family":"Joyner","given":"W.","email":"","middleInitial":"B.","affiliations":[],"preferred":false,"id":270440,"contributorType":{"id":1,"text":"Authors"},"rank":5},{"text":"Bromery, R. W.","contributorId":11676,"corporation":false,"usgs":true,"family":"Bromery","given":"R.","email":"","middleInitial":"W.","affiliations":[],"preferred":false,"id":270435,"contributorType":{"id":1,"text":"Authors"},"rank":6}]}}
,{"id":63300,"text":"gq932 - 1972 - Geologic map of the Highland Peak quadrangle, Pitkin County, Colorado","interactions":[{"subject":{"id":46613,"text":"ofr7045 - 1972 - Geologic map of the Highland Peak quadrangle, Pitkin County, Colorado","indexId":"ofr7045","publicationYear":"1972","noYear":false,"title":"Geologic map of the Highland Peak quadrangle, Pitkin County, Colorado"},"predicate":"SUPERSEDED_BY","object":{"id":63300,"text":"gq932 - 1972 - Geologic map of the Highland Peak quadrangle, Pitkin County, Colorado","indexId":"gq932","publicationYear":"1972","noYear":false,"title":"Geologic map of the Highland Peak quadrangle, Pitkin County, Colorado"},"id":1}],"lastModifiedDate":"2012-02-10T00:10:45","indexId":"gq932","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1972","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":316,"text":"Geologic Quadrangle","code":"GQ","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"932","title":"Geologic map of the Highland Peak quadrangle, Pitkin County, Colorado","language":"ENGLISH","doi":"10.3133/gq932","usgsCitation":"Bryant, B., 1972, Geologic map of the Highland Peak quadrangle, Pitkin County, Colorado: U.S. Geological Survey Geologic Quadrangle 932, 1 map :col. ;58 x 45 cm., on sheet 82 x 127 cm., folded to 26 x 20 cm., in envelope 30 x 24 cm., https://doi.org/10.3133/gq932.","productDescription":"1 map :col. ;58 x 45 cm., on sheet 82 x 127 cm., folded to 26 x 20 cm., in envelope 30 x 24 cm.","costCenters":[],"links":[{"id":103646,"rank":700,"type":{"id":15,"text":"Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_2232.htm","linkFileType":{"id":5,"text":"html"},"description":"2232"},{"id":249404,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/gq/0932/report.pdf","size":"33","linkFileType":{"id":1,"text":"pdf"}},{"id":252803,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/gq/0932/report-thumb.jpg"}],"scale":"24000","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -107,39.1175 ], [ -107,39.25 ], [ -106.86749999999999,39.25 ], [ -106.86749999999999,39.1175 ], [ -107,39.1175 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b00e4b07f02db698157","contributors":{"authors":[{"text":"Bryant, Bruce bbryant@usgs.gov","contributorId":1355,"corporation":false,"usgs":true,"family":"Bryant","given":"Bruce","email":"bbryant@usgs.gov","affiliations":[],"preferred":false,"id":268632,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
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,{"id":5821,"text":"pp748 - 1972 - Structural geology of the Santa Rita Mountains, southeast of Tucson, Arizona","interactions":[],"lastModifiedDate":"2012-02-02T00:05:54","indexId":"pp748","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1972","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":"748","title":"Structural geology of the Santa Rita Mountains, southeast of Tucson, Arizona","language":"ENGLISH","publisher":"U.S. Govt. Print. Off.,","doi":"10.3133/pp748","usgsCitation":"Drewes, H., 1972, Structural geology of the Santa Rita Mountains, southeast of Tucson, Arizona: U.S. Geological Survey Professional Paper 748, 35 p., https://doi.org/10.3133/pp748.","productDescription":"35 p.","costCenters":[],"links":[{"id":104733,"rank":700,"type":{"id":15,"text":"Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_5029.htm","linkFileType":{"id":5,"text":"html"},"description":"5029"},{"id":122790,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/pp/0748/report-thumb.jpg"},{"id":32517,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/pp/0748/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":32518,"rank":401,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/pp/0748/plate-2.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":32519,"rank":402,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/pp/0748/plate-3.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":32520,"rank":403,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/pp/0748/plate-4.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":32521,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/pp/0748/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b13e4b07f02db6a319a","contributors":{"authors":[{"text":"Drewes, Harald","contributorId":52567,"corporation":false,"usgs":true,"family":"Drewes","given":"Harald","affiliations":[],"preferred":false,"id":151627,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":63021,"text":"gq978 - 1972 - Geologic map of the Tungsten quadrangle, Boulder, Gilpin, and Jefferson Counties, Colorado","interactions":[],"lastModifiedDate":"2012-02-10T00:10:46","indexId":"gq978","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1972","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":316,"text":"Geologic Quadrangle","code":"GQ","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"978","title":"Geologic map of the Tungsten quadrangle, Boulder, Gilpin, and Jefferson Counties, Colorado","language":"ENGLISH","doi":"10.3133/gq978","usgsCitation":"Gable, D.J., 1972, Geologic map of the Tungsten quadrangle, Boulder, Gilpin, and Jefferson Counties, Colorado: U.S. Geological Survey Geologic Quadrangle 978, 1 map :col. ;58 x 45 cm. folded to 27 x 19 cm. in envelope 30 x 24 cm., https://doi.org/10.3133/gq978.","productDescription":"1 map :col. ;58 x 45 cm. folded to 27 x 19 cm. in envelope 30 x 24 cm.","costCenters":[],"links":[{"id":103691,"rank":700,"type":{"id":15,"text":"Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_2277.htm","linkFileType":{"id":5,"text":"html"},"description":"2277"},{"id":249154,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/gq/0978/report.pdf","size":"34","linkFileType":{"id":1,"text":"pdf"}},{"id":252155,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/gq/0978/report-thumb.jpg"}],"scale":"24000","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -105.5,39.8675 ], [ -105.5,40 ], [ -105.36749999999999,40 ], [ -105.36749999999999,39.8675 ], [ -105.5,39.8675 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ae4e4b07f02db68a24f","contributors":{"authors":[{"text":"Gable, Dolores J.","contributorId":52957,"corporation":false,"usgs":true,"family":"Gable","given":"Dolores","email":"","middleInitial":"J.","affiliations":[],"preferred":false,"id":268208,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":63023,"text":"gq988 - 1972 - Geologic map of the Wise River quadrangle, Silver Bow and Beaverhead Counties, Montana","interactions":[],"lastModifiedDate":"2012-02-10T00:10:46","indexId":"gq988","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1972","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":316,"text":"Geologic Quadrangle","code":"GQ","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"988","title":"Geologic map of the Wise River quadrangle, Silver Bow and Beaverhead Counties, Montana","language":"ENGLISH","doi":"10.3133/gq988","usgsCitation":"Fraser, G.D., and Waldrop, H.A., 1972, Geologic map of the Wise River quadrangle, Silver Bow and Beaverhead Counties, Montana: U.S. Geological Survey Geologic Quadrangle 988, 1 map., https://doi.org/10.3133/gq988.","productDescription":"1 map.","costCenters":[],"links":[{"id":103700,"rank":700,"type":{"id":15,"text":"Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_2286.htm","linkFileType":{"id":5,"text":"html"},"description":"2286"},{"id":249156,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/gq/0988/report.pdf","size":"35","linkFileType":{"id":1,"text":"pdf"}},{"id":252157,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/gq/0988/report-thumb.jpg"}],"scale":"24000","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -113,45.75 ], [ -113,45.8675 ], [ -112.86749999999999,45.8675 ], [ -112.86749999999999,45.75 ], [ -113,45.75 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a0ce4b07f02db5fc72e","contributors":{"authors":[{"text":"Fraser, George D.","contributorId":103647,"corporation":false,"usgs":true,"family":"Fraser","given":"George","email":"","middleInitial":"D.","affiliations":[],"preferred":false,"id":268212,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Waldrop, Henry A.","contributorId":38955,"corporation":false,"usgs":true,"family":"Waldrop","given":"Henry","email":"","middleInitial":"A.","affiliations":[],"preferred":false,"id":268211,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":64861,"text":"i785E - 1972 - Slope map of the Aspen Quadrangle, Pitkin County, Colorado","interactions":[],"lastModifiedDate":"2012-02-10T00:10:59","indexId":"i785E","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1972","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":320,"text":"IMAP","code":"I","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"785","subseriesTitle":"NONE","chapter":"E","title":"Slope map of the Aspen Quadrangle, Pitkin County, Colorado","language":"ENGLISH","doi":"10.3133/i785E","usgsCitation":"Bryant, B., 1972, Slope map of the Aspen Quadrangle, Pitkin County, Colorado: U.S. Geological Survey IMAP 785, 1 map :col. ;58 x 45 cm., folded to 27 x 22 cm., in envelope 30 x 24 cm., https://doi.org/10.3133/i785E.","productDescription":"1 map :col. ;58 x 45 cm., folded to 27 x 22 cm., in envelope 30 x 24 cm.","costCenters":[],"links":[{"id":187050,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":260721,"rank":900,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/imap/0785e/plate-1.pdf"}],"scale":"24000","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -106.86749999999999,39.1175 ], [ -106.86749999999999,39.25 ], [ -106.75,39.25 ], [ -106.75,39.1175 ], [ -106.86749999999999,39.1175 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e49f0e4b07f02db5ee25a","contributors":{"authors":[{"text":"Bryant, Bruce bbryant@usgs.gov","contributorId":1355,"corporation":false,"usgs":true,"family":"Bryant","given":"Bruce","email":"bbryant@usgs.gov","affiliations":[],"preferred":false,"id":272274,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":6221,"text":"pp725A - 1972 - Physical environment of the National Reactor Testing Station, Idaho; a summary","interactions":[],"lastModifiedDate":"2018-10-22T18:54:48","indexId":"pp725A","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1972","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":"725","chapter":"A","title":"Physical environment of the National Reactor Testing Station, Idaho; a summary","language":"ENGLISH","publisher":"U.S. Govt. Print. Off.,","doi":"10.3133/pp725A","usgsCitation":"Nace, R.L., Deutsch, M., and Voegeli, P., 1972, Physical environment of the National Reactor Testing Station, Idaho; a summary: U.S. Geological Survey Professional Paper 725, 37 p.; 1 plate in pocket, https://doi.org/10.3133/pp725A.","productDescription":"37 p.; 1 plate in pocket","costCenters":[],"links":[{"id":33422,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/pp/0725a/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":33423,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/pp/0725a/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":121392,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/pp/0725a/report-thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4adbe4b07f02db685bcc","contributors":{"editors":[{"text":"Subitzky, Seymour","contributorId":99111,"corporation":false,"usgs":true,"family":"Subitzky","given":"Seymour","email":"","affiliations":[],"preferred":false,"id":749285,"contributorType":{"id":2,"text":"Editors"},"rank":1}],"authors":[{"text":"Nace, Raymond L.","contributorId":93460,"corporation":false,"usgs":true,"family":"Nace","given":"Raymond","email":"","middleInitial":"L.","affiliations":[],"preferred":false,"id":152330,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Deutsch, Morris","contributorId":69119,"corporation":false,"usgs":true,"family":"Deutsch","given":"Morris","email":"","affiliations":[],"preferred":false,"id":152329,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Voegeli, Paul T.","contributorId":19937,"corporation":false,"usgs":true,"family":"Voegeli","given":"Paul T.","affiliations":[],"preferred":false,"id":152327,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":41816,"text":"ofr72392 - 1972 - Aeromagnetic map of the Klamath Falls and part of the Crescent 1° by 2° quadrangles, Oregon","interactions":[],"lastModifiedDate":"2021-11-23T21:32:42.939069","indexId":"ofr72392","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1972","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":"72-392","title":"Aeromagnetic map of the Klamath Falls and part of the Crescent 1° by 2° quadrangles, Oregon","docAbstract":"<p>No abstract available.</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr72392","usgsCitation":"Water Resources Division, U.S. Geological Survey, 1972, Aeromagnetic map of the Klamath Falls and part of the Crescent 1° by 2° quadrangles, Oregon: U.S. Geological Survey Open-File Report 72-392, 1 Plate: 28.32 × 35.65 inches, https://doi.org/10.3133/ofr72392.","productDescription":"1 Plate: 28.32 × 35.65 inches","costCenters":[],"links":[{"id":167937,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":79538,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1972/0392/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":392073,"rank":3,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_8724.htm"}],"scale":"250000","country":"United States","state":"Oregon","otherGeospatial":"Klamath Falls and part of the Crescent 1° by 2° quadrangles","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -122,\n              42\n            ],\n            [\n              -120,\n              42\n            ],\n            [\n              -120,\n              43.5\n            ],\n            [\n              -122,\n              43.5\n            ],\n            [\n              -122,\n              42\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4af4e4b07f02db691f90","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":530642,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":65000,"text":"i706 - 1972 - Geologic map of the Clavius Quadrangle of the Moon","interactions":[{"subject":{"id":13225,"text":"ofr6966 - 1969 - Preliminary geologic map of the Clavius quadrangle of the Moon","indexId":"ofr6966","publicationYear":"1969","noYear":false,"title":"Preliminary geologic map of the Clavius quadrangle of the Moon"},"predicate":"SUPERSEDED_BY","object":{"id":65000,"text":"i706 - 1972 - Geologic map of the Clavius Quadrangle of the Moon","indexId":"i706","publicationYear":"1972","noYear":false,"title":"Geologic map of the Clavius Quadrangle of the Moon"},"id":1}],"lastModifiedDate":"2023-05-09T11:19:41.465201","indexId":"i706","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1972","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":320,"text":"IMAP","code":"I","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"706","subseriesTitle":"MOON","title":"Geologic map of the Clavius Quadrangle of the Moon","docAbstract":"<p><span class=\"TextRun SCXW198490714 BCX8\" lang=\"EN-US\" xml:lang=\"EN-US\" data-contrast=\"auto\"><span class=\"NormalTextRun SCXW198490714 BCX8\">The Clavius quadrangle</span><span class=\"NormalTextRun SCXW198490714 BCX8\"> is in the southern lunar highlands about 500 km south of the Mare </span><span class=\"NormalTextRun SCXW198490714 BCX8\">Nubium</span><span class=\"NormalTextRun SCXW198490714 BCX8\"> and 150 km south of the large young crater Tycho.</span><span class=\"NormalTextRun SCXW198490714 BCX8\"> This part of the </span><span class=\"NormalTextRun SCXW198490714 BCX8\">M</span><span class=\"NormalTextRun SCXW198490714 BCX8\">oon is characterized by densely cratered </span><span class=\"NormalTextRun SCXW198490714 BCX8\">topography and the absence of mare materials. Geologic units in the quadrangle cannot be directly </span><span class=\"NormalTextRun SCXW198490714 BCX8\">correlated</span> <span class=\"NormalTextRun SCXW198490714 BCX8\">with those in the vicinity of Mare </span><span class=\"NormalTextRun SCXW198490714 BCX8\">Imbrium</span><span class=\"NormalTextRun SCXW198490714 BCX8\">, 2500 km to the north, which define</span><span class=\"NormalTextRun SCXW198490714 BCX8\"> most of the lunar </span><span class=\"NormalTextRun SCXW198490714 BCX8\">time-stratigraphic systems (Shoemaker and Hackman, 1962</span><span class=\"NormalTextRun SCXW198490714 BCX8\">; </span><span class=\"NormalTextRun SCXW198490714 BCX8\">Wilhelms</span><span class=\"NormalTextRun SCXW198490714 BCX8\">, 1970). However, the relative ages of rock units, including </span><span class=\"NormalTextRun SCXW198490714 BCX8\">crater materials, have been determined by established geologic methods, such as superposition and cross-cutting relations. In addition, crater materials have been positioned within the lunar time </span><span class=\"NormalTextRun SCXW198490714 BCX8\">stratigraphic framework (</span><span class=\"NormalTextRun SCXW198490714 BCX8\">Offield</span><span class=\"NormalTextRun SCXW198490714 BCX8\">, 1971) by estimates. Based on morphology, of their state of erosion (</span><span class=\"SpellingError SCXW198490714 BCX8\">Pohn</span><span class=\"NormalTextRun SCXW198490714 BCX8\"> and </span><span class=\"NormalTextRun SCXW198490714 BCX8\">Offi</span><span class=\"NormalTextRun SCXW198490714 BCX8\">e</span><span class=\"NormalTextRun SCXW198490714 BCX8\">ld</span><span class=\"NormalTextRun SCXW198490714 BCX8\">, 1970).</span></span></p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/i706","usgsCitation":"Cummings, D., 1972, Geologic map of the Clavius Quadrangle of the Moon: U.S. Geological Survey IMAP 706, 1 Plate: 61.33 × 35.33 inches, https://doi.org/10.3133/i706.","productDescription":"1 Plate: 61.33 × 35.33 inches","costCenters":[],"links":[{"id":190293,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":100810,"rank":2,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/imap/0706/plate-1.pdf","size":"6684","linkFileType":{"id":1,"text":"pdf"}}],"scale":"1000000","otherGeospatial":"Moon","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b09e4b07f02db69c13a","contributors":{"authors":[{"text":"Cummings, David","contributorId":50911,"corporation":false,"usgs":true,"family":"Cummings","given":"David","email":"","affiliations":[],"preferred":false,"id":272488,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":63847,"text":"gp840 - 1972 - Aeromagnetic map of the Ridgway-Pagosa Springs area, southwestern Colorado","interactions":[],"lastModifiedDate":"2025-07-09T16:26:45.222921","indexId":"gp840","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1972","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":317,"text":"Geophysical Investigations Map","code":"GP","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"840","title":"Aeromagnetic map of the Ridgway-Pagosa Springs area, southwestern Colorado","docAbstract":"<p>No abstract available.</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/gp840","usgsCitation":"Water Resources Division, U.S. Geological Survey, 1972, Aeromagnetic map of the Ridgway-Pagosa Springs area, southwestern Colorado: U.S. Geological Survey Geophysical Investigations Map 840, 1 Plate: 30.02 x 20.99 inches, https://doi.org/10.3133/gp840.","productDescription":"1 Plate: 30.02 x 20.99 inches","costCenters":[],"links":[{"id":253620,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/gp/0840/report-thumb.jpg"},{"id":250109,"rank":3,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/gp/0840/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":250108,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/gp/0840/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":491910,"rank":4,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_6193.htm","linkFileType":{"id":5,"text":"html"}}],"scale":"250000","country":"United States","state":"Colorado","otherGeospatial":"Ridgway-Pagosa Springs area","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -108.25,\n              38.25\n            ],\n            [\n              -108.25,\n              37.25\n            ],\n            [\n              -106.5,\n              37.25\n            ],\n            [\n              -106.5,\n              38.25\n            ],\n            [\n              -108.25,\n              38.25\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4af3e4b07f02db691a09","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":533316,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":15622,"text":"ofr72312 - 1972 - Preliminary interpretation of seismic profiles in the Prudhoe Bay area, Beaufort Sea, Alaska","interactions":[],"lastModifiedDate":"2012-02-02T00:06:52","indexId":"ofr72312","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1972","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":"72-312","title":"Preliminary interpretation of seismic profiles in the Prudhoe Bay area, Beaufort Sea, Alaska","language":"ENGLISH","publisher":"U.S. Geological Survey],","doi":"10.3133/ofr72312","usgsCitation":"Reimnitz, E., Wolf, S.C., and Rodeick, C.A., 1972, Preliminary interpretation of seismic profiles in the Prudhoe Bay area, Beaufort Sea, Alaska: U.S. Geological Survey Open-File Report 72-312, 11 leaves (2 p. per leaf) :3 folded maps ;21 cm.; 4 sheets, scale 1:80,000, https://doi.org/10.3133/ofr72312.","productDescription":"11 leaves (2 p. per leaf) :3 folded maps ;21 cm.; 4 sheets, scale 1:80,000","costCenters":[],"links":[{"id":147058,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1972/0312/report-thumb.jpg"},{"id":44582,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1972/0312/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":44583,"rank":401,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1972/0312/plate-2.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":44584,"rank":402,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1972/0312/plate-3.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":44585,"rank":403,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1972/0312/plate-4.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":44586,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1972/0312/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"scale":"80000","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4abce4b07f02db672ca4","contributors":{"authors":[{"text":"Reimnitz, Erk","contributorId":17963,"corporation":false,"usgs":true,"family":"Reimnitz","given":"Erk","email":"","affiliations":[],"preferred":false,"id":171449,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Wolf, Stephen C.","contributorId":38148,"corporation":false,"usgs":true,"family":"Wolf","given":"Stephen","email":"","middleInitial":"C.","affiliations":[],"preferred":false,"id":171450,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Rodeick, Craig A.","contributorId":80290,"corporation":false,"usgs":true,"family":"Rodeick","given":"Craig","email":"","middleInitial":"A.","affiliations":[],"preferred":false,"id":171451,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
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