{"pageNumber":"6638","pageRowStart":"165925","pageSize":"25","recordCount":184904,"records":[{"id":6319,"text":"pp488 - 1965 - Geomorphology and Quaternary geology of the Owensboro quadrangle, Indiana and Kentucky","interactions":[],"lastModifiedDate":"2022-03-22T22:25:02.834032","indexId":"pp488","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1965","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":"488","title":"Geomorphology and Quaternary geology of the Owensboro quadrangle, Indiana and Kentucky","docAbstract":"<p>No abstract available.</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/pp488","usgsCitation":"Ray, L.L., 1965, Geomorphology and Quaternary geology of the Owensboro quadrangle, Indiana and Kentucky: U.S. Geological Survey Professional Paper 488, Report: iv, 72 p.; 1 Plate: 33.00 × 38.50 inches, https://doi.org/10.3133/pp488.","productDescription":"Report: iv, 72 p.; 1 Plate: 33.00 × 38.50 inches","costCenters":[],"links":[{"id":397438,"rank":4,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_4498.htm"},{"id":33615,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/pp/0488/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":33614,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/pp/0488/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":121695,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/pp/0488/report-thumb.jpg"}],"country":"United States","state":"Indiana, Kentucky","otherGeospatial":"Owensboro quadrangle","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -87.25,\n              37.75\n            ],\n            [\n              -87,\n              37.75\n            ],\n            [\n              -87,\n              38\n            ],\n            [\n              -87.25,\n              38\n            ],\n            [\n              -87.25,\n              37.75\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ac9e4b07f02db67c4e4","contributors":{"authors":[{"text":"Ray, Louis L.","contributorId":48527,"corporation":false,"usgs":true,"family":"Ray","given":"Louis","email":"","middleInitial":"L.","affiliations":[],"preferred":false,"id":152501,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":5669,"text":"pp479 - 1965 - Geology of the Sierra Blanca area, Hudspeth County, Texas","interactions":[],"lastModifiedDate":"2023-01-09T21:26:37.875238","indexId":"pp479","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1965","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":"479","title":"Geology of the Sierra Blanca area, Hudspeth County, Texas","docAbstract":"<p>No abstract available.</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/pp479","usgsCitation":"Albritton, C.C., and Smith, J.F., 1965, Geology of the Sierra Blanca area, Hudspeth County, Texas: U.S. Geological Survey Professional Paper 479, Report: vi, 131 p.; 10 Plates: 45.85 x 25.60 inches or smaller, https://doi.org/10.3133/pp479.","productDescription":"Report: vi, 131 p.; 10 Plates: 45.85 x 25.60 inches or smaller","costCenters":[],"links":[{"id":264475,"rank":5,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/pp/0479/plate-2.pdf","text":"Plate 2","linkFileType":{"id":1,"text":"pdf"}},{"id":264474,"rank":4,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/pp/0479/plate-1_south.pdf","text":"Plate 1 South","linkFileType":{"id":1,"text":"pdf"}},{"id":264476,"rank":6,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/pp/0479/plate-3.pdf","text":"Plate 3","linkFileType":{"id":1,"text":"pdf"}},{"id":264473,"rank":3,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/pp/0479/plate-1_north.pdf","text":"Plate 1 North","linkFileType":{"id":1,"text":"pdf"}},{"id":104469,"rank":13,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_4484.htm","linkFileType":{"id":5,"text":"html"},"description":"4484"},{"id":32187,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/pp/0479/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":264477,"rank":7,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/pp/0479/plate-4.pdf","text":"Plate 4","linkFileType":{"id":1,"text":"pdf"}},{"id":264478,"rank":8,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/pp/0479/plate-5.pdf","text":"Plate 5","linkFileType":{"id":1,"text":"pdf"}},{"id":264479,"rank":9,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/pp/0479/plate-6.pdf","text":"Plate 6","linkFileType":{"id":1,"text":"pdf"}},{"id":264480,"rank":10,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/pp/0479/plate-7.pdf","text":"Plate 7","linkFileType":{"id":1,"text":"pdf"}},{"id":117864,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/pp/0479/report-thumb.jpg"},{"id":264482,"rank":12,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/pp/0479/plate-9.pdf","text":"Plate 9","linkFileType":{"id":1,"text":"pdf"}},{"id":264481,"rank":11,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/pp/0479/plate-8.pdf","text":"Plate 8","linkFileType":{"id":1,"text":"pdf"}}],"country":"United States","state":"Texas","county":"Hudspeth County","otherGeospatial":"Sierra Blanca area","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"coordinates\": [\n          [\n            [\n              -105.8417,\n              30.9661\n            ],\n            [\n              -105.25,\n              30.9661\n            ],\n            [\n              -105.25,\n              31.5\n            ],\n            [\n              -105.8417,\n              31.5\n            ],\n            [\n              -105.8417,\n              30.9661\n            ]\n          ]\n        ],\n        \"type\": \"Polygon\"\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4acce4b07f02db67e524","contributors":{"authors":[{"text":"Albritton, Claude C. Jr.","contributorId":87129,"corporation":false,"usgs":true,"family":"Albritton","given":"Claude","suffix":"Jr.","email":"","middleInitial":"C.","affiliations":[],"preferred":false,"id":151401,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Smith, J. Fred Jr.","contributorId":106482,"corporation":false,"usgs":true,"family":"Smith","given":"J.","suffix":"Jr.","email":"","middleInitial":"Fred","affiliations":[],"preferred":false,"id":151402,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":6120,"text":"pp451 - 1965 - Geology and artesian water supply of the Grand Junction area, Colorado","interactions":[],"lastModifiedDate":"2023-03-23T21:01:06.54278","indexId":"pp451","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1965","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":"451","title":"Geology and artesian water supply of the Grand Junction area, Colorado","docAbstract":"<p>No abstract available.</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/pp451","usgsCitation":"Lohman, S.W., 1965, Geology and artesian water supply of the Grand Junction area, Colorado: U.S. Geological Survey Professional Paper 451, Report: v, 149 p.; 2 Plates: 41.00 x 55.00 inches and 14.00 x 20.00 inches, https://doi.org/10.3133/pp451.","productDescription":"Report: v, 149 p.; 2 Plates: 41.00 x 55.00 inches and 14.00 x 20.00 inches","costCenters":[],"links":[{"id":33177,"rank":3,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/pp/0451/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":414662,"rank":5,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_4454.htm","linkFileType":{"id":5,"text":"html"}},{"id":33179,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/pp/0451/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":117744,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/pp/0451/report-thumb.jpg"},{"id":33178,"rank":4,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/pp/0451/plate-2.pdf","linkFileType":{"id":1,"text":"pdf"}}],"country":"United States","state":"Colorado","city":"Grand Junction","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"coordinates\": [\n          [\n            [\n              -108.68133892061891,\n              39.21589336033844\n            ],\n            [\n              -108.68133892061891,\n              38.92375994348936\n            ],\n            [\n              -108.43048689657363,\n              38.92375994348936\n            ],\n            [\n              -108.43048689657363,\n              39.21589336033844\n            ],\n            [\n              -108.68133892061891,\n              39.21589336033844\n            ]\n          ]\n        ],\n        \"type\": \"Polygon\"\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4adde4b07f02db686d37","contributors":{"authors":[{"text":"Lohman, Stanley William","contributorId":53361,"corporation":false,"usgs":true,"family":"Lohman","given":"Stanley","email":"","middleInitial":"William","affiliations":[],"preferred":false,"id":152152,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":15753,"text":"ofr65141 - 1965 - Geology of the Romanzof Mountains, Brooks Range, northeastern Alaska","interactions":[{"subject":{"id":15753,"text":"ofr65141 - 1965 - Geology of the Romanzof Mountains, Brooks Range, northeastern Alaska","indexId":"ofr65141","publicationYear":"1965","noYear":false,"title":"Geology of the Romanzof Mountains, Brooks Range, northeastern Alaska"},"predicate":"SUPERSEDED_BY","object":{"id":6313,"text":"pp897 - 1977 - Geology of the western Romanzof Mountains, Brooks Range, northeastern Alaska","indexId":"pp897","publicationYear":"1977","noYear":false,"title":"Geology of the western Romanzof Mountains, Brooks Range, northeastern Alaska"},"id":1},{"subject":{"id":15754,"text":"ofr59106 - 1959 - Preliminary report on sedimentary and metamorphic rocks in part of the Romanzof Mountains, Brooks Range, northeastern Alaska","indexId":"ofr59106","publicationYear":"1959","noYear":false,"title":"Preliminary report on sedimentary and metamorphic rocks in part of the Romanzof Mountains, Brooks Range, northeastern Alaska"},"predicate":"SUPERSEDED_BY","object":{"id":15753,"text":"ofr65141 - 1965 - Geology of the Romanzof Mountains, Brooks Range, northeastern Alaska","indexId":"ofr65141","publicationYear":"1965","noYear":false,"title":"Geology of the Romanzof Mountains, Brooks Range, northeastern Alaska"},"id":2}],"supersededBy":{"id":6313,"text":"pp897 - 1977 - Geology of the western Romanzof Mountains, Brooks Range, northeastern Alaska","indexId":"pp897","publicationYear":"1977","noYear":false,"title":"Geology of the western Romanzof Mountains, Brooks Range, northeastern Alaska"},"lastModifiedDate":"2024-03-25T18:59:14.568941","indexId":"ofr65141","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1965","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":"65-141","title":"Geology of the Romanzof Mountains, Brooks Range, northeastern Alaska","docAbstract":"<p>This remote 700 square mile area in the Brooks Range is topographically rugged and geologically diverse; it contains a granitic pluton, low-grade metamorphic rocks, sedimentary rocks, and mafic igneous rocks, as well as glacial features.</p><p>Rocks of sedimentary origin include from oldest to youngest:</p><p>1.Neruokpuk Formation Middle and Upper Devonian(?), more than 4000 feet thick, a variety of units which represent the greenschist facies, including quartzitic- and schistose-feldspathic graywacke; phyllite, argillite, and slate, as well as dark limestone, sandy limestone, and silicified carbonate rocks. The succession of units in parts of the area is uncertain. Correlations between these units and with others in the eastern Brooks Range are provisional.</p><p>2.Kekiktuk Conglomerate and Kayak(?) Shale (Upper Devonian(?) to Upper Mississippian), a single map unit, from absent(?) to 400+ feet thick, containing dark shale Kayak(?) in its uppermost part and quartzite, interbedded dark shale, and some pebble- to boulder-conglomerate in the locally absent lower part (Kekiktuk). The unit overlies the Neruokpuk with angular unconformity, which may reflect either a pre-Kayak(?) or pre-Kekiktuk hiatus or both.</p><p>3.Lisburne Group, almost entirely carbonate rocks, and relatively thin in this area, 600 to 800 feet thick. Alapah Limestone (Upper Mississippian), to 560 feet thick, includes gray sandy, crystalline, and cherty limestone; minor dark shale; and dark cherty carbonate rocks in the upper part. The lower contact is gradational with the Kayak(?). Wahoo(?) Limestone (Pennsylvanian(?) to Permian) conformably overlies the Alapah, is absent to 200+ feet thick, and is characterized by light-gray crinoidal limestones in its upper part.</p><p>4. Sadlerochit Formation, consisting of three intraconformable units: ferruginous sandstone member (Permian) of ironstained orthoquartzite and dark slate, 175 to 240 feet thick which unconformably overlies the Wahoo(?) and Alapah Limestones; shale member of dark shale, slate, and minor quartzite averaging 400 feet in thickness; and quartzite member (Lower(?) Triassic), 700 feet thick, mostly orthoquartzite with minor shale and conglomerate. The basal clastics were probably shed from the north.</p><p>5.Shublik Formation (Middle(?) and Upper Triassic), 600 to 700 feet thick, with the thin phosphatic sandstone member overlain by dark phosphatic limestones and limy shales of the limestone member.</p><p>6.Kingak Formation (Jurassic), more than 1000 feet thick. The siltstone member, resistant sandstone and siltstone 75 to 150 feet thick, is overlain by an undetermined thickness of black shale. The basal part contrasts sharply with the underlying Shublik, indicating possible disconformity.</p><p>7.Ignek(?) Formation (Cretaceous), represented in the foothills where lithic graywacke, shale, and coaly shale constitute the few exposures examined.</p><p>8.Glacial and glaciofluvial materials of five advances recognized on the basis of morphology and position, which are tentatively correlated with five glaciations 15 miles west of the area.</p><p>9. Recent alluvial and colluvial deposits including fans which appear to represent at least three stages of encroachment.<br></p><p>The Ramanzof granite, exposed in the Okpilak batholith and Jago stock, is mostly light-gray quartz monzonite to granite, and contains essential quartz, perthitic microcline, albite-oligoclase, and partly chloritized biotite. Limited modal and chemical data are presented. Three textural facies are: 1) porphyritic (marginal), with abundant large microcline megacrysts; 2) variable (middle to marginal), which exhibits textural and mineralogical banding; and 3) coarse (inner to marginal), which is gneissoid to equigranular. Facies relationships appear to be mostly gradational but may be locally intrusive. Some schistose metasedimentary(?) rock occurs in the granite. Aplite dikes, inclusions, tourmaline veins and replacements, and chlorite and quartz veins are locally common, as well as quartz monzonite and mafic igneous dikes. Contacts with Neruokpuk Formation rocks are mostly abrupt, concordant to cross-cutting, and locally adjoin tactite and hornfels of the albite-epidote-hornfels and hornblende-hornfels facies. Contacts with Kekiktuk Conglomerate are apparently gradational through a schistoze zone. Both primary and secondary structural elements are present in the Romanzof in granite. Textural and mineralogical banding and, in general, feldspar foliation are considered to be primary in origin; biotite foliation, gneissic and schistose foliation, and schistose zones are considered secondary. Lead-alpha age of zircons appears to be Late Devonian, K-Ar age of biotite is Cretaceous, possibly indicating updating by later reheating. Field age relationships are inconclusive but suggest pre-Kayak(?) (Upper Devonian) granite emplacement. The pluton is interpreted to be essentially the product of melt crystallization, synorogenically emplaced by forceful injection with minor stoping, and may include marginally granitized rock.<br></p><p>Mafic igneous rocks of altered basaltic composition (greenstones) include dikes in granitic and Neruokpuk Formation rocks, and volcanics(?). A late Paleozoic age is suggested for them.</p><p>Structural grain strikes east-northeast; south-dipping elements are common. Structures include the major positive nature of the area (first order), relatively broad folds (second order) which contain small tight folds (third order). Related south-dipping cleavage, schistosity, and biotite foliation in granite in the northern part of the area are cut by prominent sets of transverse joints and faults. Other features are longitudinal normal and reverse faults, at least one large-scale overthrust fault, and sheared zones in granite with possible attendant retrograde metamorphism.</p><p>Although Mesozoic and Tertiary deformational features are dominant in northern Alaska, the Romanzof area may have been part of a Late Devonian orogenic belt continuous with one in northern Canada. Three alternate trends of such a belt in northern Alaska are discussed, but evidence is inconclusive.</p><p>The mineral potential of the area is largely unknown. Minor amounts of metallic sulfides and oxides are present in granite and Neruokpuk Formation rocks. Analyses of stream silt samples suggest the possibility of tin and beryllium potential. The Shublik Formation contains rock phosphate.</p><p><br data-mce-bogus=\"1\"></p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr65141","usgsCitation":"Sable, E.G., 1965, Geology of the Romanzof Mountains, Brooks Range, northeastern Alaska: U.S. Geological Survey Open-File Report 65-141, Report: x, 218 p.; 7 Plates: 35.95 x 37.74 inches or smaller, https://doi.org/10.3133/ofr65141.","productDescription":"Report: x, 218 p.; 7 Plates: 35.95 x 37.74 inches or smaller","costCenters":[],"links":[{"id":427049,"rank":9,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1965/0141/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":427048,"rank":8,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1965/0141/plate-2.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":427047,"rank":7,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1965/0141/plate-3.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":427046,"rank":6,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1965/0141/plate-4.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":427045,"rank":5,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1965/0141/plate-5.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":427044,"rank":4,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1965/0141/plate-6.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":427043,"rank":3,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1965/0141/plate-7.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":427042,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1965/0141/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":148683,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1965/0141/report-thumb.jpg"}],"scale":"63360","country":"United States","state":"Alaska","otherGeospatial":"Brooks Range, Romanzof Mountains","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"coordinates\": [\n          [\n            [\n              -144.61982095290645,\n              69.45543761208387\n            ],\n            [\n              -144.61982095290645,\n              68.6489771949642\n            ],\n            [\n              -142.45135071338586,\n              68.6489771949642\n            ],\n            [\n              -142.45135071338586,\n              69.45543761208387\n            ],\n            [\n              -144.61982095290645,\n              69.45543761208387\n            ]\n          ]\n        ],\n        \"type\": \"Polygon\"\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4acce4b07f02db67e733","contributors":{"authors":[{"text":"Sable, Edward G.","contributorId":51273,"corporation":false,"usgs":true,"family":"Sable","given":"Edward","email":"","middleInitial":"G.","affiliations":[],"preferred":false,"id":171648,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
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,{"id":15761,"text":"ofr65142 - 1965 - Geology and ore deposits of the central York Mountains, western Seward Peninsula, Alaska","interactions":[{"subject":{"id":15761,"text":"ofr65142 - 1965 - Geology and ore deposits of the central York Mountains, western Seward Peninsula, Alaska","indexId":"ofr65142","publicationYear":"1965","noYear":false,"title":"Geology and ore deposits of the central York Mountains, western Seward Peninsula, Alaska"},"predicate":"SUPERSEDED_BY","object":{"id":35708,"text":"b1287 - 1969 - Geology and ore deposits of the Central York Mountains, western Seward Peninsula, Alaska","indexId":"b1287","publicationYear":"1969","noYear":false,"title":"Geology and ore deposits of the Central York Mountains, western Seward Peninsula, Alaska"},"id":1}],"supersededBy":{"id":35708,"text":"b1287 - 1969 - Geology and ore deposits of the Central York Mountains, western Seward Peninsula, Alaska","indexId":"b1287","publicationYear":"1969","noYear":false,"title":"Geology and ore deposits of the Central York Mountains, western Seward Peninsula, Alaska"},"lastModifiedDate":"2024-05-20T19:22:29.519521","indexId":"ofr65142","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1965","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":"65-142","title":"Geology and ore deposits of the central York Mountains, western Seward Peninsula, Alaska","docAbstract":"<p>In the central York Mountains, carbonate rocks of Lower and Middle Ordovician age and aggregating at least 8,000 feet thick are thrust northward over slate and argillaceous limestone of pre-Ordovician age which were intruded by gabbro in pre-Ordovician time. Normal faults of four distinct systems cut the thrust plates, and in Late Cretaceous time, stocks of biotite granite, abnormally rich in beryllium, tin, boron and certain other trace elements, pierced the thrust plates. In part following the intrusion of the granites, a strong set of normal faults developed striking N. 60°-85° E. through the central York Mountains and locally these faults cut the granites. Dikes of granite, rhyolite porphyry, and lamprophyre were injected into some of these faults, the lamprophyres being younger. Trace elements in the lamprophyres prove they are mafic rocks probably derived from the lama, and that they cannot be related genetically to granite. Shortly after the intrusion of lamprophyre dikes, ore deposits of tin, beryllium, and fluorite were formed from solutions probably derived from deeply-buried hot granite where the granite was ruptured by normal faults. Ore shoots were localized beneath thrust faults where the faults are intruded by dikes, and a major ore-bearing structure, the Rapid River fault, is mineralized for half its length for a distance of eight miles. The tin deposits contain cassiterite and stannite in topaz greisen with abundant sulfides of copper, lead, zinc, and iron, as well as wolframite. The beryllium deposits contain fluorite, chrysoberyl, diaspore, muscovite, and tourmaline, with trace to small amounts of euclase, bertrandite, helvite, phenikite(?), todorokite and hematite. Beryl occurs sparingly in late veins of quartz and fluorite. Chrysoberyl is the earliest and commonest beryllium mineral, followed by euclase and bertrandite, and then phenakite(?) and beryl. Helvite is restricted to banded skarns near granite, and which consist of magnetite and fluorite. Throughout the district, a strong zonation is displayed from tin deposits in greisen through transitional veins of sulfide minerals with fluorite and chrysoberyl to fluorite-beryllium deposits and thence to barren veins of silica and fluorite with trace amounts of beryllium. This zonal arrangement of deposits probably will be found elsewhere in the world where greisen tin deposits occur in carbonate rocks. The geochemical cycle of the trace elements Be, Sn, W, B, Li, Cu, Pb, Zn and Nb shows that these elements were enriched in the biotite granites and were strongly fractionated among the minerals of granites. Fran the granites, these rare elements moved outward into contact rocks and ore deposits. During the supergene cycle, clear geochemical anomalies were formed in stream sediments, soils and plants near ore deposits, and geochemical prospecting led to the discovery of the beryllium lodes. With the possible exception of zinc and niobium, the rare elements that are associated in the rocks and ores remain associated in the supergene processes. Fixation of zinc in clay soil and tundra plants may account for the relatively small amount of zinc in strew sediments.</p><p>Datable Pleistocene events in the York Mountains begin with the Yarmouth Interglaciation when the York Terrace, a wide marine platform, was cut. In Illinoian time, the York Terrace was uplifted almost 400 feet, and during the Sangamon Interglaciation a second marine platform (Lost River Terrace) was cut and is not deformed. During Wisconsin time the widespread York Glaciation was followed by the more restricted Mint River Glaciation. Because uplift of the York Terrace extended into the Bering Strait, it is probable that prior to the uplift in Illinoian time the Bering Strait was a seaway and a barrier to land migration rather than a land bridge.</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr65142","usgsCitation":"Sainsbury, C., 1965, Geology and ore deposits of the central York Mountains, western Seward Peninsula, Alaska: U.S. Geological Survey Open-File Report 65-142, Report: 149 p.; 15 Plates: 20.55 x 27.89 inches or smaller; 8 Tables: 20.88 x 30.29 inches or smaller, https://doi.org/10.3133/ofr65142.","productDescription":"Report: 149 p.; 15 Plates: 20.55 x 27.89 inches or smaller; 8 Tables: 20.88 x 30.29 inches or 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,{"id":62020,"text":"mr43 - 1965 - Barite in the United States, exclusive of Alaska and Hawaii","interactions":[],"lastModifiedDate":"2025-05-13T16:00:20.885004","indexId":"mr43","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1965","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":324,"text":"Mineral Investigations Resource Map","code":"MR","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"43","title":"Barite in the United States, exclusive of Alaska and Hawaii","docAbstract":"<p>The mineral barite, barium sulfate, is the chief source of barium and its compounds needed for many industrial processes and products. Barite is found the world over and is abundant and widely distributed throughout the United States. The barite deposits of the United States (exclusive of Alaska and Hawaii) are shown on the accompanying map. The principal geologic type of deposit is indicated by the shape of symbol and the relative importance of the deposit is indicated by the size of symbol.</p><p>This text lists localities by State, and index numbers are keyed to the map. Localities are distinguished by name of mine, prospect, or geographic area; their coordinates are given to the nearest minute of latitude and longitude. Geologic relations of each occurrence, if known, are summarized briefly. The text and map were compiled from published and unpublished information, and at least one reference is given for each locality, if reports have been published. The listings in some States are preceded by a principal reference which is a major source of information about deposits in those States.</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/mr43","usgsCitation":"Brobst, D.A., 1965, Barite in the United States, exclusive of Alaska and Hawaii: U.S. Geological Survey Mineral Investigations Resource Map 43, Report: 10 p.; 1 Plate: 63.99 x 41.00 inches, https://doi.org/10.3133/mr43.","productDescription":"Report: 10 p.; 1 Plate: 63.99 x 41.00 inches","costCenters":[],"links":[{"id":180065,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/mr/43/report-thumb.jpg"},{"id":260469,"rank":2,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/mr/43/plate-1.pdf"},{"id":485827,"rank":3,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/mr/43/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"scale":"3168000","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -127.25,24.25 ], [ -127.25,49.25 ], [ -66.5,49.25 ], [ -66.5,24.25 ], [ -127.25,24.25 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a80e4b07f02db649aab","contributors":{"authors":[{"text":"Brobst, Donald Albert","contributorId":36117,"corporation":false,"usgs":true,"family":"Brobst","given":"Donald","email":"","middleInitial":"Albert","affiliations":[],"preferred":false,"id":266728,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":61630,"text":"gq386 - 1965 - Geology of the Cub Run quadrangle, Kentucky","interactions":[],"lastModifiedDate":"2012-02-10T00:10:35","indexId":"gq386","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1965","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":"386","title":"Geology of the Cub Run quadrangle, Kentucky","language":"ENGLISH","doi":"10.3133/gq386","usgsCitation":"Sandberg, C.A., and Bowles, C.G., 1965, Geology of the Cub Run quadrangle, Kentucky: U.S. Geological Survey Geologic Quadrangle 386, 1 map :col. ;85 x 85 cm., https://doi.org/10.3133/gq386.","productDescription":"1 map :col. ;85 x 85 cm.","costCenters":[],"links":[{"id":102401,"rank":700,"type":{"id":15,"text":"Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_850.htm","linkFileType":{"id":5,"text":"html"},"description":"850"},{"id":247935,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/gq/0386/report.pdf","size":"35","linkFileType":{"id":1,"text":"pdf"}},{"id":252360,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/gq/0386/report-thumb.jpg"}],"scale":"24000","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -86.11749999999999,37.25 ], [ -86.11749999999999,37.3675 ], [ -86,37.3675 ], [ -86,37.25 ], [ -86.11749999999999,37.25 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b24e4b07f02db6ae6f4","contributors":{"authors":[{"text":"Sandberg, Charles A. sandberg@usgs.gov","contributorId":2362,"corporation":false,"usgs":true,"family":"Sandberg","given":"Charles","email":"sandberg@usgs.gov","middleInitial":"A.","affiliations":[{"id":595,"text":"U.S. Geological Survey","active":false,"usgs":true}],"preferred":false,"id":266163,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Bowles, C. Gilbert","contributorId":60607,"corporation":false,"usgs":true,"family":"Bowles","given":"C.","email":"","middleInitial":"Gilbert","affiliations":[],"preferred":false,"id":266164,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":38976,"text":"pp433C - 1965 - Transport and dispersion of labeled bed material, North Loup River, Nebraska","interactions":[{"subject":{"id":52364,"text":"ofr63118 - 1963 - Transport and dispersion of labeled bed material, North Loup River, Nebraska","indexId":"ofr63118","publicationYear":"1963","noYear":false,"title":"Transport and dispersion of labeled bed material, North Loup River, Nebraska"},"predicate":"SUPERSEDED_BY","object":{"id":38976,"text":"pp433C - 1965 - Transport and dispersion of labeled bed material, North Loup River, Nebraska","indexId":"pp433C","publicationYear":"1965","noYear":false,"chapter":"C","title":"Transport and dispersion of labeled bed material, North Loup River, Nebraska"},"id":1}],"lastModifiedDate":"2012-02-02T00:10:32","indexId":"pp433C","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1965","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":"433","chapter":"C","title":"Transport and dispersion of labeled bed material, North Loup River, Nebraska","language":"ENGLISH","doi":"10.3133/pp433C","usgsCitation":"Sayre, W., and Hubbell, D.W., 1965, Transport and dispersion of labeled bed material, North Loup River, Nebraska: U.S. Geological Survey Professional Paper 433, p. C1-C48, https://doi.org/10.3133/pp433C.","productDescription":"p. C1-C48","costCenters":[],"links":[{"id":120403,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/pp/0433c/report-thumb.jpg"},{"id":66080,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/pp/0433c/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a4de4b07f02db626c7f","contributors":{"authors":[{"text":"Sayre, W.W.","contributorId":12899,"corporation":false,"usgs":true,"family":"Sayre","given":"W.W.","email":"","affiliations":[],"preferred":false,"id":220750,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Hubbell, D. W.","contributorId":15997,"corporation":false,"usgs":true,"family":"Hubbell","given":"D.","email":"","middleInitial":"W.","affiliations":[],"preferred":false,"id":220751,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":61673,"text":"gq370 - 1965 - Bedrock geologic map of the Tariffville quadrangle, Hartford County, Connecticut and Hampden County, Massachusetts","interactions":[],"lastModifiedDate":"2021-12-29T20:39:47.691391","indexId":"gq370","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1965","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":"370","title":"Bedrock geologic map of the Tariffville quadrangle, Hartford County, Connecticut and Hampden County, Massachusetts","docAbstract":"<p>No abstract available.</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/gq370","usgsCitation":"Schnabel, R.W., and Eric, J.H., 1965, Bedrock geologic map of the Tariffville quadrangle, Hartford County, Connecticut and Hampden County, Massachusetts: U.S. Geological Survey Geologic Quadrangle 370, Report: 1 p.; Plate, https://doi.org/10.3133/gq370.","productDescription":"Report: 1 p.; Plate","costCenters":[],"links":[{"id":252552,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/gq/0370/report-thumb.jpg"},{"id":247975,"rank":299,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/gq/0370/report.pdf","size":"37","linkFileType":{"id":1,"text":"pdf"}},{"id":102384,"rank":699,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_833.htm","linkFileType":{"id":5,"text":"html"},"description":"833"}],"scale":"24000","country":"United States","state":"Connecticut,  Massachusetts","county":"Hampden County, Hartford County","otherGeospatial":"Tariffville quadrangle","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -72.875,41.875 ], [ -72.875,42 ], [ -72.75,42 ], [ -72.75,41.875 ], [ -72.875,41.875 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a61e4b07f02db636139","contributors":{"authors":[{"text":"Schnabel, Robert Wayne","contributorId":57859,"corporation":false,"usgs":true,"family":"Schnabel","given":"Robert","email":"","middleInitial":"Wayne","affiliations":[],"preferred":false,"id":266220,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Eric, John H.","contributorId":89530,"corporation":false,"usgs":true,"family":"Eric","given":"John","email":"","middleInitial":"H.","affiliations":[],"preferred":false,"id":266221,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":63270,"text":"gq419 - 1965 - Geology of the Whitesville quadrangle, Kentucky","interactions":[],"lastModifiedDate":"2012-02-10T00:10:41","indexId":"gq419","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1965","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":"419","title":"Geology of the Whitesville quadrangle, Kentucky","language":"ENGLISH","doi":"10.3133/gq419","usgsCitation":"Calvert, R.H., 1965, Geology of the Whitesville quadrangle, Kentucky: U.S. Geological Survey Geologic Quadrangle 419, 1 map :col. ;76 x 85 cm., https://doi.org/10.3133/gq419.","productDescription":"1 map :col. ;76 x 85 cm.","costCenters":[],"links":[{"id":102438,"rank":700,"type":{"id":15,"text":"Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_887.htm","linkFileType":{"id":5,"text":"html"},"description":"887"},{"id":249376,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/gq/0419/report.pdf","size":"35","linkFileType":{"id":1,"text":"pdf"}},{"id":252775,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/gq/0419/report-thumb.jpg"}],"scale":"24000","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -86.86749999999999,37.6175 ], [ -86.86749999999999,37.75 ], [ -86.75,37.75 ], [ -86.75,37.6175 ], [ -86.86749999999999,37.6175 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ac9e4b07f02db67c96d","contributors":{"authors":[{"text":"Calvert, Ronald H.","contributorId":71248,"corporation":false,"usgs":true,"family":"Calvert","given":"Ronald","email":"","middleInitial":"H.","affiliations":[],"preferred":false,"id":268584,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":38977,"text":"pp433D - 1965 - Mineralogy and cation-exchange capacity of sediments from selected streams","interactions":[],"lastModifiedDate":"2012-02-02T00:10:32","indexId":"pp433D","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1965","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":"433","chapter":"D","title":"Mineralogy and cation-exchange capacity of sediments from selected streams","language":"ENGLISH","doi":"10.3133/pp433D","usgsCitation":"Kennedy, V.C., 1965, Mineralogy and cation-exchange capacity of sediments from selected streams: U.S. Geological Survey Professional Paper 433, p. D1-D28, https://doi.org/10.3133/pp433D.","productDescription":"p. D1-D28","costCenters":[],"links":[{"id":120404,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/pp/0433d/report-thumb.jpg"},{"id":66081,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/pp/0433d/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4afbe4b07f02db696239","contributors":{"authors":[{"text":"Kennedy, V. C.","contributorId":46080,"corporation":false,"usgs":true,"family":"Kennedy","given":"V.","email":"","middleInitial":"C.","affiliations":[],"preferred":false,"id":220752,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
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