{"pageNumber":"4670","pageRowStart":"116725","pageSize":"25","recordCount":165549,"records":[{"id":11443,"text":"ofr83408 - 1983 - Mineral resource potential of the Thousand Lakes Wilderness, Shasta County, California","interactions":[],"lastModifiedDate":"2012-02-02T00:06:33","indexId":"ofr83408","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1983","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":"83-408","title":"Mineral resource potential of the Thousand Lakes Wilderness, Shasta County, California","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/ofr83408","usgsCitation":"Till, A.B., McHugh, E.L., and Ramsey, C.M., 1983, Mineral resource potential of the Thousand Lakes Wilderness, Shasta County, California: U.S. Geological Survey Open-File Report 83-408, 14 p. ill., maps ;28 cm., https://doi.org/10.3133/ofr83408.","productDescription":"14 p. ill., maps ;28 cm.","costCenters":[],"links":[{"id":145041,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1983/0408/report-thumb.jpg"},{"id":39299,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1983/0408/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b09e4b07f02db69bd7e","contributors":{"authors":[{"text":"Till, Alison B. atill@usgs.gov","contributorId":2482,"corporation":false,"usgs":true,"family":"Till","given":"Alison","email":"atill@usgs.gov","middleInitial":"B.","affiliations":[{"id":119,"text":"Alaska Science Center Geology Minerals","active":true,"usgs":true}],"preferred":true,"id":163147,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"McHugh, Edward L.","contributorId":77157,"corporation":false,"usgs":true,"family":"McHugh","given":"Edward","email":"","middleInitial":"L.","affiliations":[],"preferred":false,"id":163149,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Ramsey, Clayton M.","contributorId":65471,"corporation":false,"usgs":true,"family":"Ramsey","given":"Clayton","email":"","middleInitial":"M.","affiliations":[],"preferred":false,"id":163148,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":29555,"text":"wri834061 - 1983 - Distribution of chloride concentrations in the principal aquifers of the New Jersey coastal plain, 1977-81","interactions":[],"lastModifiedDate":"2012-02-02T00:09:01","indexId":"wri834061","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1983","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":342,"text":"Water-Resources Investigations Report","code":"WRI","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"83-4061","title":"Distribution of chloride concentrations in the principal aquifers of the New Jersey coastal plain, 1977-81","docAbstract":"The U.S. Geological Survey maintains a saltwater monitoring network in New Jersey to document and evaluate the movement of saline water into freshwater aquifers that serve as sources of water supply. Areas in the Coastal Plain with existing or potential saltwater intrusion are delineated. Data collected through 1981 indicate that freshwater aquifers in parts of seven Coastal-Plain counties are contaminated by saline water. Encroachment of saltwater into freshwater aquifers in the Sayreville area of Middlesex County and in the lower peninsula of Cape May County has been reported for about 40 years and is now more extensive. Several other areas are experiencing limited saltwater intrusion. These include the Keyport-Union Beach area in Monmouth County, areas along the Delaware estuary in Gloucester and Salem Counties, and at Point Pleasant Beach and Seaside Heights in Ocean County. The continuing updip movement of saline water in the Potomac-Raritan-Magothy aquifer system is also threatening existing freshwater supplies in the interior areas of Gloucester and Salem Counties. Saltwater intrusion has resulted from extensive ground-water withdrawals. The resultant freshwater head declines have caused reversals in the natural hydraulic gradients that permit inland movement of saline water from adjacent saltwater bodies. (USGS)","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/wri834061","usgsCitation":"Schaefer, F., 1983, Distribution of chloride concentrations in the principal aquifers of the New Jersey coastal plain, 1977-81: U.S. Geological Survey Water-Resources Investigations Report 83-4061, iv, 56 p. :ill., maps ;28 cm., https://doi.org/10.3133/wri834061.","productDescription":"iv, 56 p. :ill., maps ;28 cm.","costCenters":[],"links":[{"id":121865,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wri/1983/4061/report-thumb.jpg"},{"id":58385,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wri/1983/4061/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a7fe4b07f02db6486ca","contributors":{"authors":[{"text":"Schaefer, F. L.","contributorId":91085,"corporation":false,"usgs":true,"family":"Schaefer","given":"F. L.","affiliations":[],"preferred":false,"id":201710,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":11425,"text":"ofr83311 - 1983 - Chemical analyses of thermal and nonthermal springs in Lassen Volcanic National Park and vicinity, California","interactions":[],"lastModifiedDate":"2012-02-02T00:06:29","indexId":"ofr83311","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1983","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":"83-311","title":"Chemical analyses of thermal and nonthermal springs in Lassen Volcanic National Park and vicinity, California","docAbstract":"Most thermal waters issuing in Lassen Volcanic National Park (LVNP) are acidic (pH =3.5), low-Cl (concentrations =30 mg/L) hot springs which are characteristic of vapor-dominated hydrothermal systems and, as such, are not useful for liquid chemical geothermometry. Thermal waters at Drakesbad and in Little Hot Springs Valley, hot spring localities characterized by neutral pH and low Cl containing water, may have equilibrated in shallow aquifers so that temperatures estimated by both the Na-K-Ca and Na-Li geothermometers approach the measured spring temperatures of 65? to 95?C. Waters rich in chloride (>2000 mg/L), such as those at Growler Hot Spring and Morgan Hot Springs, situated south of LVNP, are the most appropriate springs for liquid chemical geothermometry and indicate subsurface temperatures between 220? and 230?C. The chemical and thermal characteristics of these springs may result either from boiling at depth and subsequent mixing with meteoric water or from conductive cooling during lateral flow. In either case ~220? to 230?C thermal water probably originates inside LVNP and flows south to Morgan Hot Springs.","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/ofr83311","usgsCitation":"Thompson, J., 1983, Chemical analyses of thermal and nonthermal springs in Lassen Volcanic National Park and vicinity, California: U.S. Geological Survey Open-File Report 83-311, 27 p. ill., maps ;28 cm., https://doi.org/10.3133/ofr83311.","productDescription":"27 p. ill., maps ;28 cm.","costCenters":[],"links":[{"id":144142,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1983/0311/report-thumb.jpg"},{"id":39277,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1983/0311/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e49e1e4b07f02db5e496d","contributors":{"authors":[{"text":"Thompson, J. M.","contributorId":77142,"corporation":false,"usgs":true,"family":"Thompson","given":"J. M.","affiliations":[],"preferred":false,"id":163118,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":69589,"text":"i1542 - 1983 - Petroleum potential of wilderness lands, Nevada","interactions":[],"lastModifiedDate":"2012-02-10T00:11:34","indexId":"i1542","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1983","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":"1542","title":"Petroleum potential of wilderness lands, Nevada","language":"ENGLISH","doi":"10.3133/i1542","usgsCitation":"Sandberg, C.A., 1983, Petroleum potential of wilderness lands, Nevada: U.S. Geological Survey IMAP 1542, 1 map : col. ; 94 x 59 cm., folded in envelope 30 x 24 cm. + 1 pamphlet (11 p. : maps ; 26 cm.) , https://doi.org/10.3133/i1542.","productDescription":"1 map : col. ; 94 x 59 cm., folded in envelope 30 x 24 cm. + 1 pamphlet (11 p. : maps ; 26 cm.) ","costCenters":[],"links":[{"id":106799,"rank":700,"type":{"id":15,"text":"Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_9306.htm","linkFileType":{"id":5,"text":"html"},"description":"9306"},{"id":101477,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/imap/1542/report.pdf","size":"1339","linkFileType":{"id":1,"text":"pdf"}},{"id":191114,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/imap/1542/report-thumb.jpg"},{"id":91716,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/imap/1542/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}}],"scale":"1000000","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -120,35 ], [ -120,42 ], [ -114.05,42 ], [ -114.05,35 ], [ -120,35 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4adee4b07f02db6875c5","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":280680,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":56651,"text":"fwsobs82_10_58 - 1983 - Habitat Suitability Index Models: Alewife and blueback herring","interactions":[],"lastModifiedDate":"2022-02-09T15:25:41.078632","indexId":"fwsobs82_10_58","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1983","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":1,"text":"Federal Government Series"},"seriesTitle":{"id":20,"text":"FWS/OBS","active":false,"publicationSubtype":{"id":1}},"seriesNumber":"82/10.58","subseriesTitle":"Habitat Suitability Index","title":"Habitat Suitability Index Models: Alewife and blueback herring","docAbstract":"Alewives and blueback herring are anadromous clupeids found along the Atlantic coast in marine, estuarine, and riverine habitats, depending upon life stage. Both are important commercial species, used fresh or salted for human consumption, and used as crab bait, fish meal (particularly in animal food manufacturing), and fish oil. Alewife and blueback herring are marketed collectively as 'river herring,' a term that will be used for both species in this report. River herring play important ecological roles. In marine, estuarine, and riverine food webs, they occupy a level between zooplankton, their principal food, and piscivores.","language":"English","publisher":"U.S. Fish and Wildlife Service","usgsCitation":"Pardue, G.B., 1983, Habitat Suitability Index Models: Alewife and blueback herring: FWS/OBS 82/10.58, vi, 22 p.","productDescription":"vi, 22 p.","costCenters":[{"id":595,"text":"U.S. Geological Survey","active":false,"usgs":true}],"links":[{"id":181766,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a81e4b07f02db649e1f","contributors":{"authors":[{"text":"Pardue, Garland B.","contributorId":53014,"corporation":false,"usgs":true,"family":"Pardue","given":"Garland","email":"","middleInitial":"B.","affiliations":[],"preferred":false,"id":255600,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":56650,"text":"fwsobs82_10_50 - 1983 - Habitat Suitability Index Models: Roseate spoonbill","interactions":[],"lastModifiedDate":"2022-02-09T15:26:11.161465","indexId":"fwsobs82_10_50","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1983","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":1,"text":"Federal Government Series"},"seriesTitle":{"id":20,"text":"FWS/OBS","active":false,"publicationSubtype":{"id":1}},"seriesNumber":"82/10.50","subseriesTitle":"Habitat Suitability Index","title":"Habitat Suitability Index Models: Roseate spoonbill","docAbstract":"<p>The roseate spoonbill is a long-legged wading bird with a height of approximately 80 cm (31.5 inches), a wingspan of 1.3 m (4.3 ft), and a weight of 1.6 kg (3.5 Ib }. The bill is narrower near the base (2-3 em, 0.8-1.2 inches) than at the flattened tip (5 cm, 2 inches) and is 15-18 cm (5.9-7.1 inches) in length.</p><p>Roseate spoonbills occur and nest in peninsular Florida, coastal Louisiana, and Texas, south through the West Indies, Mexico, Central and South America to Argentina and Chile. Marine, brackish, and freshwater habitats are utilized, but brackish areas are favored (Blacklock et al. 1978). In the late 1970·s there were 2,500 pairs nesting along the Texas coast (Texas Colonial Waterbird Society 1982), 1,300 pairs in southwestern Louisiana (Portnoy 1977), and 1,400 pairs in Florida (Robertson et al. 1983). These birds are resident year round in Florida, Louisiana, and Texas, but fewer bi rds are present duri ng the nonbreedi ng season than in the breeding season. Some individuals move northward after nesting and have been reported in Georgia, Nebraska, Pennsylvania, Utah, and Wisconsin, but most spoonbills move south when they leave the breeding area.</p>","language":"English","publisher":"U.S. Fish and Wildlife Service","usgsCitation":"Lewis, J., 1983, Habitat Suitability Index Models: Roseate spoonbill: FWS/OBS 82/10.50, vi, 16 p.","productDescription":"vi, 16 p.","costCenters":[{"id":595,"text":"U.S. Geological Survey","active":false,"usgs":true}],"links":[{"id":181765,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a80e4b07f02db64977c","contributors":{"authors":[{"text":"Lewis, James C.","contributorId":88799,"corporation":false,"usgs":true,"family":"Lewis","given":"James C.","affiliations":[],"preferred":false,"id":255599,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":56648,"text":"fwsobs82_10_36 - 1983 - Habitat Suitability Index Models: Smallmouth bass","interactions":[],"lastModifiedDate":"2022-02-09T15:27:17.4465","indexId":"fwsobs82_10_36","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1983","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":1,"text":"Federal Government Series"},"seriesTitle":{"id":20,"text":"FWS/OBS","active":false,"publicationSubtype":{"id":1}},"seriesNumber":"82/10.36","subseriesTitle":"Habitat Suitability Index","title":"Habitat Suitability Index Models: Smallmouth bass","docAbstract":"A review and synthesis of existing information were used to develop riverine and lacustrine habitat models for Smallmouth bass (Micropterus dolomieui), a freshwater species. The models are scaled to produce an index of habitat suitability between 0 (unsuitable habitat) and 1 (optimally suitable habitat) for freshwater areas of the continental United States. Habitat suitability indexes (HSI's) are designed for use with the habitat evaluation procedures developed by the U.S. Fish and Wildlife Service. The instream flow suitability curves are intended for use with the Instream Flow Incremental Methodology.\r\n\r\nAlso included are discussions of Suitability Index (SI) curves as used by the Instream Flow Incremental Methodology (IFIM) and SI curves available for an IFIM analysis of Smallmouth bass habitat.","language":"English","publisher":"U.S. Fish and Wildlife Service","usgsCitation":"Edwards, E.A., Gebhart, G., and Maughan, O.E., 1983, Habitat Suitability Index Models: Smallmouth bass: FWS/OBS 82/10.36, viii, 47 p.","productDescription":"viii, 47 p.","costCenters":[{"id":595,"text":"U.S. Geological Survey","active":false,"usgs":true}],"links":[{"id":181661,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a80e4b07f02db64975f","contributors":{"authors":[{"text":"Edwards, Elizabeth A.","contributorId":39421,"corporation":false,"usgs":true,"family":"Edwards","given":"Elizabeth","email":"","middleInitial":"A.","affiliations":[],"preferred":false,"id":255594,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Gebhart, Glen","contributorId":52237,"corporation":false,"usgs":true,"family":"Gebhart","given":"Glen","email":"","affiliations":[],"preferred":false,"id":255596,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Maughan, O. Eugene","contributorId":43006,"corporation":false,"usgs":true,"family":"Maughan","given":"O.","email":"","middleInitial":"Eugene","affiliations":[],"preferred":false,"id":255595,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":60887,"text":"mf1435 - 1983 - Maps showing distribution, thickness, and mass of late Pleistocene and Holocene tephra from major volcanoes in the Pacific Northwest of the United States: A preliminary assessment of hazards from volcanic ejecta to nuclear reactors in the Pacific Northwest","interactions":[],"lastModifiedDate":"2022-08-31T11:14:56.638137","indexId":"mf1435","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1983","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":325,"text":"Miscellaneous Field Studies Map","code":"MF","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"1435","title":"Maps showing distribution, thickness, and mass of late Pleistocene and Holocene tephra from major volcanoes in the Pacific Northwest of the United States: A preliminary assessment of hazards from volcanic ejecta to nuclear reactors in the Pacific Northwest","docAbstract":"<p>No abstract available.</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/mf1435","usgsCitation":"Shipley, S., and Sarna-Wojcicki, A., 1983, Maps showing distribution, thickness, and mass of late Pleistocene and Holocene tephra from major volcanoes in the Pacific Northwest of the United States: A preliminary assessment of hazards from volcanic ejecta to nuclear reactors in the Pacific Northwest: U.S. Geological Survey Miscellaneous Field Studies Map 1435, Report: 27 p.; 1 Plate: 33.50 × 26.00 inches, https://doi.org/10.3133/mf1435.","productDescription":"Report: 27 p.; 1 Plate: 33.50 × 26.00 inches","costCenters":[],"links":[{"id":105862,"rank":700,"type":{"id":15,"text":"Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_7183.htm","linkFileType":{"id":5,"text":"html"},"description":"7183"},{"id":183496,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/mf/1983/1435/report-thumb.jpg"},{"id":88879,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/mf/1983/1435/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":88880,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/mf/1983/1435/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"country":"United States","otherGeospatial":"Pacific Northwest","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -125,\n              39\n            ],\n            [\n              -106,\n              39\n            ],\n            [\n              -106,\n              50\n            ],\n            [\n              -125,\n              50\n            ],\n            [\n              -125,\n              39\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a19e4b07f02db6057db","contributors":{"authors":[{"text":"Shipley, Susan","contributorId":94650,"corporation":false,"usgs":true,"family":"Shipley","given":"Susan","email":"","affiliations":[],"preferred":false,"id":264556,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Sarna-Wojcicki, A.M. 0000-0002-0244-9149","orcid":"https://orcid.org/0000-0002-0244-9149","contributorId":104022,"corporation":false,"usgs":true,"family":"Sarna-Wojcicki","given":"A.M.","affiliations":[],"preferred":false,"id":264557,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":29288,"text":"wri834022 - 1983 - Simulations of non-steady flow in a glacial outwash aquifer, southern Franklin County, Ohio","interactions":[],"lastModifiedDate":"2012-02-02T00:08:45","indexId":"wri834022","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1983","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":342,"text":"Water-Resources Investigations Report","code":"WRI","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"83-4022","title":"Simulations of non-steady flow in a glacial outwash aquifer, southern Franklin County, Ohio","docAbstract":"A two-dimensional, finite-difference model is used to simulate transient flow conditions in a glacial outwash aquifer in southern Franklin County, Ohio. The model was calibrated by matching observed and simulated water-level changes for December 1977 through March 1980. Drawdowns for three different hypothetical pumping rates are simulated with the calibrated flow model. An increase in the pumping rate from the steady-state rate of 10 cubic feet per second to 48 cubic feet per second results in water-level declines of 10 to 20 feet near the area of the pumping wells. Declines of 20 to 40 feet result when the pumping rate is increased to 70 cubic feet per second, and a simulated pumping well goes dry when the combined pumping is increased to 94 cubic feet per second. For the first two cases, steady-flow conditions are reached after 12 years of pumping; infiltration through riverbeds accounts for 28 to 33% of the pumpage.","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/wri834022","usgsCitation":"Razem, A., 1983, Simulations of non-steady flow in a glacial outwash aquifer, southern Franklin County, Ohio: U.S. Geological Survey Water-Resources Investigations Report 83-4022, iv, 21 p. :ill., maps ;28 cm., https://doi.org/10.3133/wri834022.","productDescription":"iv, 21 p. :ill., maps ;28 cm.","costCenters":[],"links":[{"id":158906,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wri/1983/4022/report-thumb.jpg"},{"id":58133,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wri/1983/4022/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e49f6e4b07f02db5f1a6d","contributors":{"authors":[{"text":"Razem, A. C.","contributorId":34924,"corporation":false,"usgs":true,"family":"Razem","given":"A. C.","affiliations":[],"preferred":false,"id":201285,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":60703,"text":"mf1496A - 1983 - Isopach and structure contour maps of the Burro Canyon(?) Formation in the Mesa Golondrina and Mesa de los Viejos areas, Chama Basin, New Mexico","interactions":[],"lastModifiedDate":"2016-08-23T09:10:47","indexId":"mf1496A","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1983","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":325,"text":"Miscellaneous Field Studies Map","code":"MF","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"1496","chapter":"A","title":"Isopach and structure contour maps of the Burro Canyon(?) Formation in the Mesa Golondrina and Mesa de los Viejos areas, Chama Basin, New Mexico","docAbstract":"<p>In the Chama Basin a wequence of conglomerate, sandstone, and red, gray-green, and pale-purple mudstone occurs stratigraphically between the Upper Jurassic Morrison Formation and Upper Cretaceous Dakota Sandstone. This stratigraphic interval has been called the Burro Canyon Formation by several workers (Craig and others, 1959; Smith and others, 1961; Saucier, 1974). Although similarities in lithology and stratigraphic position exist between this unit and the Burro Canyon Formation in Colorado, no direct correlation has been made between the two. For this reason the unit in the Chama Basin is called the Burro Canyon(?) Formation.&nbsp;</p>","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Reston, VA","doi":"10.3133/mf1496A","usgsCitation":"Ridgley, J.L., 1983, Isopach and structure contour maps of the Burro Canyon(?) Formation in the Mesa Golondrina and Mesa de los Viejos areas, Chama Basin, New Mexico: U.S. Geological Survey Miscellaneous Field Studies Map 1496, 44.56 x 36.03 inches and 40.71 x 36.25 inches, https://doi.org/10.3133/mf1496A.","productDescription":"44.56 x 36.03 inches and 40.71 x 36.25 inches","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[],"links":[{"id":180227,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/mf1496A.PNG"},{"id":327453,"rank":1,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/mf/1496-A/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":327454,"rank":2,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/mf/1496-A/plate-2.pdf","linkFileType":{"id":1,"text":"pdf"}}],"scale":"24000","country":"United States","state":"New Mexico","otherGeospatial":"Mesa De Los Viejos, Mesa Golondria","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -106.75,36.333333333333336 ], [ -106.75,36.5 ], [ -106.5,36.5 ], [ -106.5,36.333333333333336 ], [ -106.75,36.333333333333336 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4aa7e4b07f02db66713f","contributors":{"authors":[{"text":"Ridgley, Jennie L. ridgley@usgs.gov","contributorId":1248,"corporation":false,"usgs":true,"family":"Ridgley","given":"Jennie","email":"ridgley@usgs.gov","middleInitial":"L.","affiliations":[],"preferred":true,"id":264254,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":11719,"text":"ofr83721 - 1983 - Preliminary map of the resource areas in the Basin and Range Province of Nevada","interactions":[],"lastModifiedDate":"2012-02-02T00:06:30","indexId":"ofr83721","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1983","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":"83-721","title":"Preliminary map of the resource areas in the Basin and Range Province of Nevada","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/ofr83721","usgsCitation":"Wong, G., 1983, Preliminary map of the resource areas in the Basin and Range Province of Nevada: U.S. Geological Survey Open-File Report 83-721, i, 37 leaves :map ;28 cm.; 1 over-size sheet; scale 1:500000 (1 inch = about 8 miles), https://doi.org/10.3133/ofr83721.","productDescription":"i, 37 leaves :map ;28 cm.; 1 over-size sheet; scale 1:500000 (1 inch = about 8 miles)","costCenters":[],"links":[{"id":108469,"rank":700,"type":{"id":15,"text":"Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_14192.htm","linkFileType":{"id":5,"text":"html"},"description":"14192"},{"id":143919,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1983/0721/report-thumb.jpg"},{"id":39604,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1983/0721/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":39605,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1983/0721/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"scale":"500000","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4afce4b07f02db696942","contributors":{"authors":[{"text":"Wong, George","contributorId":25543,"corporation":false,"usgs":true,"family":"Wong","given":"George","email":"","affiliations":[],"preferred":false,"id":163616,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":40679,"text":"ofr83420N - 1983 - Distribution and abundance of molybdenum, determined by spectrographic analysis, in the minus-80-mesh fraction of stream sediments, Petersburg area, southeast Alaska","interactions":[],"lastModifiedDate":"2022-01-31T20:21:02.136738","indexId":"ofr83420N","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1983","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":"83-420","chapter":"N","title":"Distribution and abundance of molybdenum, determined by spectrographic analysis, in the minus-80-mesh fraction of stream sediments, Petersburg area, southeast Alaska","docAbstract":"<p>No abstract available.</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr83420N","usgsCitation":"Cathrall, J.B., Day, G., Hoffman, J.D., and McDanal, S., 1983, Distribution and abundance of molybdenum, determined by spectrographic analysis, in the minus-80-mesh fraction of stream sediments, Petersburg area, southeast Alaska: U.S. Geological Survey Open-File Report 83-420, 1 Plate: 39.11 × 26.00 inches, https://doi.org/10.3133/ofr83420N.","productDescription":"1 Plate: 39.11 × 26.00 inches","costCenters":[],"links":[{"id":136511,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":395176,"rank":3,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_14031.htm"},{"id":77955,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1983/0420n/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}}],"country":"United States","state":"Alaska","otherGeospatial":"Petersburg area","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -134.560546875,\n              55.96150096848812\n            ],\n            [\n              -132.0062255859375,\n              55.96150096848812\n            ],\n            [\n              -132.0062255859375,\n              57.07060297861011\n            ],\n            [\n              -134.560546875,\n              57.07060297861011\n            ],\n            [\n              -134.560546875,\n              55.96150096848812\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a81e4b07f02db64a03b","contributors":{"authors":[{"text":"Cathrall, John B.","contributorId":26668,"corporation":false,"usgs":true,"family":"Cathrall","given":"John","email":"","middleInitial":"B.","affiliations":[],"preferred":false,"id":223712,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Day, G.W.","contributorId":63363,"corporation":false,"usgs":true,"family":"Day","given":"G.W.","email":"","affiliations":[],"preferred":false,"id":223713,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Hoffman, J. D.","contributorId":8419,"corporation":false,"usgs":true,"family":"Hoffman","given":"J.","email":"","middleInitial":"D.","affiliations":[],"preferred":false,"id":223711,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"McDanal, S.K.","contributorId":108078,"corporation":false,"usgs":true,"family":"McDanal","given":"S.K.","email":"","affiliations":[],"preferred":false,"id":223714,"contributorType":{"id":1,"text":"Authors"},"rank":4}]}}
,{"id":41343,"text":"ofr82162 - 1983 - Potentiometric surface of the Lloyd Aquifer, Long Island, New York, in January 1979","interactions":[],"lastModifiedDate":"2012-02-02T00:10:33","indexId":"ofr82162","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1983","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":"82-162","title":"Potentiometric surface of the Lloyd Aquifer, Long Island, New York, in January 1979","language":"ENGLISH","doi":"10.3133/ofr82162","usgsCitation":"Donaldson, C.D., and Koszalka, E.J., 1983, Potentiometric surface of the Lloyd Aquifer, Long Island, New York, in January 1979: U.S. Geological Survey Open-File Report 82-162, 1 map on 2 sheets ;59 x 152 cm., on sheets 66 x 75 cm. and 66 x 83 cm., folded in envelope 30 x 23 cm., https://doi.org/10.3133/ofr82162.","productDescription":"1 map on 2 sheets ;59 x 152 cm., on sheets 66 x 75 cm. and 66 x 83 cm., folded in envelope 30 x 23 cm.","costCenters":[],"links":[{"id":172755,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":79105,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1982/0162/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":79106,"rank":401,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1982/0162/plate-2.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ad4e4b07f02db682f76","contributors":{"authors":[{"text":"Donaldson, Cynthia D.","contributorId":24837,"corporation":false,"usgs":true,"family":"Donaldson","given":"Cynthia","email":"","middleInitial":"D.","affiliations":[],"preferred":false,"id":224860,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Koszalka, Edward J.","contributorId":47850,"corporation":false,"usgs":true,"family":"Koszalka","given":"Edward","email":"","middleInitial":"J.","affiliations":[],"preferred":false,"id":224861,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":40678,"text":"ofr83420O - 1983 - Distribution and abundance of molybdenum, determined by spectrographic analysis, in nonmagnetic fraction of heavy-mineral concentrates from stream sediments, Petersburg area, southeast Alaska","interactions":[],"lastModifiedDate":"2012-02-02T00:05:03","indexId":"ofr83420O","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1983","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":"83-420","chapter":"O","title":"Distribution and abundance of molybdenum, determined by spectrographic analysis, in nonmagnetic fraction of heavy-mineral concentrates from stream sediments, Petersburg area, southeast Alaska","language":"ENGLISH","doi":"10.3133/ofr83420O","usgsCitation":"Cathrall, J.B., Day, G., Hoffman, J.D., and McDanal, S., 1983, Distribution and abundance of molybdenum, determined by spectrographic analysis, in nonmagnetic fraction of heavy-mineral concentrates from stream sediments, Petersburg area, southeast Alaska: U.S. Geological Survey Open-File Report 83-420, 1 map :photocopy ;53 x 70 cm., https://doi.org/10.3133/ofr83420O.","productDescription":"1 map :photocopy ;53 x 70 cm.","costCenters":[],"links":[{"id":136510,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":77954,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1983/0420o/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a81e4b07f02db64a03d","contributors":{"authors":[{"text":"Cathrall, John B.","contributorId":26668,"corporation":false,"usgs":true,"family":"Cathrall","given":"John","email":"","middleInitial":"B.","affiliations":[],"preferred":false,"id":223708,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Day, G.W.","contributorId":63363,"corporation":false,"usgs":true,"family":"Day","given":"G.W.","email":"","affiliations":[],"preferred":false,"id":223709,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Hoffman, J. D.","contributorId":8419,"corporation":false,"usgs":true,"family":"Hoffman","given":"J.","email":"","middleInitial":"D.","affiliations":[],"preferred":false,"id":223707,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"McDanal, S.K.","contributorId":108078,"corporation":false,"usgs":true,"family":"McDanal","given":"S.K.","email":"","affiliations":[],"preferred":false,"id":223710,"contributorType":{"id":1,"text":"Authors"},"rank":4}]}}
,{"id":11457,"text":"ofr83473 - 1983 - Mineral resource potential of the Greenhorn Mountain Wilderness Study Area, Huerfano and Pueblo counties, Colorado","interactions":[],"lastModifiedDate":"2012-02-02T00:06:34","indexId":"ofr83473","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1983","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":"83-473","title":"Mineral resource potential of the Greenhorn Mountain Wilderness Study Area, Huerfano and Pueblo counties, Colorado","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/ofr83473","usgsCitation":"Toth, M.I., Birch, D.R., and Baskin, G.D., 1983, Mineral resource potential of the Greenhorn Mountain Wilderness Study Area, Huerfano and Pueblo counties, Colorado: U.S. Geological Survey Open-File Report 83-473, 12 p. maps ;28 cm., https://doi.org/10.3133/ofr83473.","productDescription":"12 p. maps ;28 cm.","costCenters":[],"links":[{"id":144861,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1983/0473/report-thumb.jpg"},{"id":39317,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1983/0473/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b09e4b07f02db69c128","contributors":{"authors":[{"text":"Toth, Margo I.","contributorId":18365,"corporation":false,"usgs":true,"family":"Toth","given":"Margo","email":"","middleInitial":"I.","affiliations":[],"preferred":false,"id":163168,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Birch, Daniel R.","contributorId":77537,"corporation":false,"usgs":true,"family":"Birch","given":"Daniel","email":"","middleInitial":"R.","affiliations":[],"preferred":false,"id":163170,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Baskin, G. David","contributorId":37334,"corporation":false,"usgs":true,"family":"Baskin","given":"G.","email":"","middleInitial":"David","affiliations":[],"preferred":false,"id":163169,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":11542,"text":"ofr83219 - 1983 - Ground-water data for selected coal areas in western North Dakota","interactions":[],"lastModifiedDate":"2018-03-15T16:47:54","indexId":"ofr83219","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1983","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":"83-219","title":"Ground-water data for selected coal areas in western North Dakota","docAbstract":"<p>Ground-water data are provided in this report for the Sand Creek-Hanks, New England-Mott, Dickinson, and Bowman-Gascoyne coal areas, western North Dakota. The report contains the following: (1) Maps showing the location of wells, springs, and test holes; the location of wells and test holes where drillers' logs are available; and the location of wells with chemical analyses; and (2) tables showing well, spring, and testhole records; logs; and chemical analyses of water. Descriptions of the location of data-collection sites and methods used to collect data are included.</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr83219","usgsCitation":"Wald, J.D., and Norbeck, S.W., 1983, Ground-water data for selected coal areas in western North Dakota: U.S. Geological Survey Open-File Report 83-219, Report: 244 p.; 9 Plates, https://doi.org/10.3133/ofr83219.","productDescription":"Report: 244 p.; 9 Plates","costCenters":[{"id":478,"text":"North Dakota Water Science Center","active":true,"usgs":true},{"id":34685,"text":"Dakota Water Science Center","active":true,"usgs":true}],"links":[{"id":39411,"rank":406,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1983/0219/plate-7.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":39412,"rank":407,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1983/0219/plate-8.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":39413,"rank":408,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1983/0219/plate-9.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":145332,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1983/0219/report-thumb.jpg"},{"id":39405,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1983/0219/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":39406,"rank":401,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1983/0219/plate-2.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":39407,"rank":402,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1983/0219/plate-3.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":39408,"rank":403,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1983/0219/plate-4.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":39409,"rank":404,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1983/0219/plate-5.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":39410,"rank":405,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1983/0219/plate-6.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":39414,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1983/0219/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4aafe4b07f02db66ce32","contributors":{"authors":[{"text":"Wald, James D.","contributorId":64263,"corporation":false,"usgs":true,"family":"Wald","given":"James","email":"","middleInitial":"D.","affiliations":[],"preferred":false,"id":163329,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Norbeck, Steven W.","contributorId":29824,"corporation":false,"usgs":true,"family":"Norbeck","given":"Steven","email":"","middleInitial":"W.","affiliations":[],"preferred":false,"id":163328,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":29492,"text":"wri834132 - 1983 - Regional geohydrology of the northern Louisiana salt-dome basin, part IV, hydraulic characteristics of the Wilcox-Carrizo aquifer","interactions":[],"lastModifiedDate":"2021-12-21T20:34:05.033918","indexId":"wri834132","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1983","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":342,"text":"Water-Resources Investigations Report","code":"WRI","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"83-4132","title":"Regional geohydrology of the northern Louisiana salt-dome basin, part IV, hydraulic characteristics of the Wilcox-Carrizo aquifer","docAbstract":"The Wilcox Group of Paleocene-Eocence age and the Carrizo Sand of Eocene age compose the Wilcox-Carrizo aquifer. Results of 25 aquifer tests and permeability determinations from 43 sidewall cores show that the hydraulic characteristics of the aquifer are variable. Studies of the Carrizo showed that hydraulic conductivity increased as sand-bed thickness increased. Hydraulic conductivity averaged 29 feet per day for sand beds 25 to 100 feet in thickness and 40 feet per day for sand beds 100 to 200 feet in thickness. Based on the aquifer tests and sidewall core analyses, hydraulic conductivity does not increase with increased thickness for the Wilcox part of the aquifer. Permeabilities determined from sidewall cores ranged from less than 1 to more than 3,000 millidarcies (less than 0.002 to more than 7.3 feet per day). Values of hydraulic conductivity determined from aquifer tests ranged from less than 1 to 35 feet per day. (USGS)","language":"English","publisher":"U.S. Geological Survey,","doi":"10.3133/wri834132","usgsCitation":"Ryals, G., 1983, Regional geohydrology of the northern Louisiana salt-dome basin, part IV, hydraulic characteristics of the Wilcox-Carrizo aquifer: U.S. Geological Survey Water-Resources Investigations Report 83-4132, Report: iv, 9 p.; 2 Plates: 17.51 × 20.17 inches and 14.06 × 12.11 inches, https://doi.org/10.3133/wri834132.","productDescription":"Report: iv, 9 p.; 2 Plates: 17.51 × 20.17 inches and 14.06 × 12.11 inches","costCenters":[],"links":[{"id":393243,"rank":5,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_49170.htm"},{"id":264599,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wri/1983/4132/plate-2.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":58334,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wri/1983/4132/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":58333,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wri/1983/4132/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":159715,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wri/1983/4132/report-thumb.jpg"}],"country":"United States","state":"Louisiana","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -93.55,\n              31.8889\n            ],\n            [\n              -92.8333,\n              31.8889\n            ],\n            [\n              -92.8333,\n              32.575\n            ],\n            [\n              -93.55,\n              32.575\n            ],\n            [\n              -93.55,\n              31.8889\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a60e4b07f02db63508f","contributors":{"authors":[{"text":"Ryals, G.N.","contributorId":47374,"corporation":false,"usgs":true,"family":"Ryals","given":"G.N.","email":"","affiliations":[],"preferred":false,"id":201604,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":60705,"text":"mf1496C - 1983 - Isopach and structure contour maps of the Burro Canyon(?) Formation in the Chama-El Vado Area, Chama Basin, New Mexico","interactions":[],"lastModifiedDate":"2016-08-23T09:09:31","indexId":"mf1496C","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1983","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":325,"text":"Miscellaneous Field Studies Map","code":"MF","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"1496","chapter":"C","title":"Isopach and structure contour maps of the Burro Canyon(?) Formation in the Chama-El Vado Area, Chama Basin, New Mexico","docAbstract":"<p><span>In the Chama Basin a wequence of conglomerate, sandstone, and red, gray-green, and pale-purple mudstone occurs stratigraphically between the Upper Jurassic Morrison Formation and Upper Cretaceous Dakota Sandstone. This stratigraphic interval has been called the Burro Canyon Formation by several workers (Craig and others, 1959; Smith and others, 1961; Saucier, 1974). Although similarities in lithology and stratigraphic position exist between this unit and the Burro Canyon Formation in Colorado, no direct correlation has been made between the two. For this reason the unit in the Chama Basin is called the Burro Canyon(?) Formation.&nbsp;</span></p>","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Reston, VA","doi":"10.3133/mf1496C","usgsCitation":"Ridgley, J.L., 1983, Isopach and structure contour maps of the Burro Canyon(?) Formation in the Chama-El Vado Area, Chama Basin, New Mexico: U.S. Geological Survey Miscellaneous Field Studies Map 1496, 35.33 x 20.38 inches, https://doi.org/10.3133/mf1496C.","productDescription":"35.33 x 20.38 inches","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[],"links":[{"id":180526,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/mf1496C.PNG"},{"id":327451,"rank":1,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/mf/1496-C/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}}],"scale":"62500","country":"United States","state":"New Mexico","otherGeospatial":"Chama Basin","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -106.75,36.666666666666664 ], [ -106.75,36.833333333333336 ], [ -106.5,36.833333333333336 ], [ -106.5,36.666666666666664 ], [ -106.75,36.666666666666664 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a93e4b07f02db65875f","contributors":{"authors":[{"text":"Ridgley, Jennie L. ridgley@usgs.gov","contributorId":1248,"corporation":false,"usgs":true,"family":"Ridgley","given":"Jennie","email":"ridgley@usgs.gov","middleInitial":"L.","affiliations":[],"preferred":true,"id":264256,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":40655,"text":"ofr83420L - 1983 - Distribution and abundance of tin determined by spectrographic analysis in nonmagnetic fraction of heavy-mineral concentrates from stream sediments, Petersburg area, southeast Alaska","interactions":[],"lastModifiedDate":"2012-02-02T00:05:06","indexId":"ofr83420L","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1983","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":"83-420","chapter":"L","title":"Distribution and abundance of tin determined by spectrographic analysis in nonmagnetic fraction of heavy-mineral concentrates from stream sediments, Petersburg area, southeast Alaska","language":"ENGLISH","doi":"10.3133/ofr83420L","usgsCitation":"Cathrall, J.B., Day, G., Hoffman, J.D., and McDanal, S., 1983, Distribution and abundance of tin determined by spectrographic analysis in nonmagnetic fraction of heavy-mineral concentrates from stream sediments, Petersburg area, southeast Alaska: U.S. Geological Survey Open-File Report 83-420, 1 map :photocopy ;53 x 70 cm., https://doi.org/10.3133/ofr83420L.","productDescription":"1 map :photocopy ;53 x 70 cm.","costCenters":[],"links":[{"id":136828,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":77740,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1983/0420l/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a81e4b07f02db64a001","contributors":{"authors":[{"text":"Cathrall, John B.","contributorId":26668,"corporation":false,"usgs":true,"family":"Cathrall","given":"John","email":"","middleInitial":"B.","affiliations":[],"preferred":false,"id":223657,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Day, G.W.","contributorId":63363,"corporation":false,"usgs":true,"family":"Day","given":"G.W.","email":"","affiliations":[],"preferred":false,"id":223658,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Hoffman, J. D.","contributorId":8419,"corporation":false,"usgs":true,"family":"Hoffman","given":"J.","email":"","middleInitial":"D.","affiliations":[],"preferred":false,"id":223656,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"McDanal, S.K.","contributorId":108078,"corporation":false,"usgs":true,"family":"McDanal","given":"S.K.","email":"","affiliations":[],"preferred":false,"id":223659,"contributorType":{"id":1,"text":"Authors"},"rank":4}]}}
,{"id":42466,"text":"ofr83295 - 1983 - Reconnaissance geology of the Al Ufayriyah quadrangle, sheet 20/42 A, Kingdom of Saudi Arabia","interactions":[],"lastModifiedDate":"2012-02-02T00:05:03","indexId":"ofr83295","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1983","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":"83-295","title":"Reconnaissance geology of the Al Ufayriyah quadrangle, sheet 20/42 A, Kingdom of Saudi Arabia","docAbstract":"The Al Ufayriyah quadrangle is located in the Najd Plateau of southwestern Saudi Arabia between lat 20?30' and 21?00' N.,. long 42?00' and 42?30' E. Two-thirds of the quadrangle is underlain by Precambrian metasedimentary, metavolcanic, plutonic, and hypabyssal intrusive rocks; this area is in part mountainous and in part uneven plains. One-third is underlain by Cenozoic basalt and is part of Harrat Buqum. Flows, which surround volcanic cones, form an east-dipping surface of low relief. \r\n\r\nPrecambrian metavolcanic and metasedimentary rocks are mostly metamorphosed andesite and basalt flow rocks and turfs and are divided into two principal belts in the eastern and central to western parts of the quadrangle. Plutonic rocks, which are part of the An Nimas batholith, consist of tonalite, diorite, and some quartz diorite. These rocks are postdated by younger plutonic and hypabyssal rocks that include extensive graphic granite and rhyolite, several small bodies of granite, and meta-andesite dikes. \r\n\r\nVolcanoes on Harrat Buqum are cinder cones, composite cones, shield volcanoes, and lava cones; basalt flows originating in some of the volcanoes can be traced down the slope of the harrat, and some have blocked Wadi Ranyah causing deposition of silt, sand, and gravel. \r\n\r\nRadiometric age dating of Precambrian rocks from adjacent quadrangles suggests that the layered rocks of the Al Ufayriyah quadrangle may have formed about 900 Ma ago, plutonic rocks of the An Nimas batholith 835 to 800 Ma ago, and younger plutonic rocks from 640 to 570 Ma ago. Basalts of Harrat Buqum range in age from 3.5 to 1.72 \r\n\r\nA zone in the eastern part of the quadrangle contains small gold-quartz veins, a quartz breccia reef, and a contact metasomatic iron deposit.","language":"ENGLISH","doi":"10.3133/ofr83295","usgsCitation":"Greene, R.C., 1983, Reconnaissance geology of the Al Ufayriyah quadrangle, sheet 20/42 A, Kingdom of Saudi Arabia: U.S. Geological Survey Open-File Report 83-295, 1 map ;48 x 45 cm. +1 booklet (21 p. : map ; 28 cm.), https://doi.org/10.3133/ofr83295.","productDescription":"1 map ;48 x 45 cm. +1 booklet (21 p. : map ; 28 cm.)","costCenters":[],"links":[{"id":135383,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1983/0295/report-thumb.jpg"},{"id":80230,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1983/0295/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":80231,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1983/0295/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a6fe4b07f02db640cef","contributors":{"authors":[{"text":"Greene, Robert C.","contributorId":36108,"corporation":false,"usgs":true,"family":"Greene","given":"Robert","email":"","middleInitial":"C.","affiliations":[],"preferred":false,"id":226550,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":42841,"text":"ofr83802 - 1983 - Preliminary geologic map of Wyoming","interactions":[{"subject":{"id":42841,"text":"ofr83802 - 1983 - Preliminary geologic map of Wyoming","indexId":"ofr83802","publicationYear":"1983","noYear":false,"title":"Preliminary geologic map of Wyoming"},"predicate":"SUPERSEDED_BY","object":{"id":70046739,"text":"70046739 - 1985 - Geologic map of Wyoming","indexId":"70046739","publicationYear":"1985","noYear":false,"title":"Geologic map of Wyoming"},"id":1}],"supersededBy":{"id":70046739,"text":"70046739 - 1985 - Geologic map of Wyoming","indexId":"70046739","publicationYear":"1985","noYear":false,"title":"Geologic map of Wyoming"},"lastModifiedDate":"2022-04-08T22:36:06.044594","indexId":"ofr83802","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1983","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":330,"text":"Open-File 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,{"id":60706,"text":"mf1523B - 1983 - Mineral resource potential map of the Chama River Canyon Wilderness and contiguous roadless area, Rio Arriba County, New Mexico","interactions":[],"lastModifiedDate":"2015-10-22T14:07:49","indexId":"mf1523B","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1983","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":325,"text":"Miscellaneous Field Studies Map","code":"MF","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"1523","chapter":"B","title":"Mineral resource potential map of the Chama River Canyon Wilderness and contiguous roadless area, Rio Arriba County, New Mexico","docAbstract":"<p>The Chama River Canyon Wilderness and Roadless Area have a moderate to high potential for the presence&nbsp;of small deposits of copper with associated uranium and silver. These deposits, as yet undetected, would occur in&nbsp;the Permian Cutler Formation and in the lower part of the Triassic Chinle Formation, rock units that are, for the&nbsp;most part, present only in the subsurface. The presence of these deposits is inferred because such deposits occur&nbsp;in rocks of equivalent age in adjacent areas. Gypsum, of probable minable quality and quantity, occurs throughout&nbsp;the area. Oil and gas are possibly present in Pennsylvanian strata in the subsurface, although no drilling in the&nbsp;study area has tested this hypothesis. Other commodities, including noncopper-related uranium, kaolinite,&nbsp;chromium, vanadium, manganese, and bitumen, although present locally in anomalous concentrations, do not&nbsp;appear to constitute potential resources for these commodities.</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/mf1523B","usgsCitation":"Ridgley, J.L., and Light, T., 1983, Mineral resource potential map of the Chama River Canyon Wilderness and contiguous roadless area, Rio Arriba County, New Mexico: U.S. Geological Survey Miscellaneous Field Studies Map 1523, Report: 8 p.; Plate: 37.57 x 43.89 inches, https://doi.org/10.3133/mf1523B.","productDescription":"Report: 8 p.; Plate: 37.57 x 43.89 inches","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[],"links":[{"id":310533,"rank":1,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/mf/1523-B/report.pdf","text":"Report","linkFileType":{"id":1,"text":"pdf"}},{"id":310534,"rank":2,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/mf/1523-B/plate-1.pdf","text":"Plate","linkFileType":{"id":1,"text":"pdf"}},{"id":180585,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/mf1523B.jpg"}],"country":"United States","state":"New Mexico","county":"Rio Arriba County","otherGeospatial":"Chama River Canyon Wilderness and Contiguous Roadless Area","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -106.75,36.166666666666664 ], [ -106.75,36.583333333333336 ], [ -106.5,36.583333333333336 ], [ -106.5,36.166666666666664 ], [ -106.75,36.166666666666664 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4afee4b07f02db69754d","contributors":{"authors":[{"text":"Ridgley, Jennie L. ridgley@usgs.gov","contributorId":1248,"corporation":false,"usgs":true,"family":"Ridgley","given":"Jennie","email":"ridgley@usgs.gov","middleInitial":"L.","affiliations":[],"preferred":true,"id":264257,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Light, Thomas D.","contributorId":46098,"corporation":false,"usgs":true,"family":"Light","given":"Thomas D.","affiliations":[],"preferred":false,"id":264258,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":40691,"text":"ofr83420S - 1983 - Distribution and abundance of cobalt, determined by spectrographic analysis, in the nonmagnetic fraction of heavy-mineral concentrates from stream sediments, Petersburg area, southeast Alaska","interactions":[],"lastModifiedDate":"2012-02-02T00:05:03","indexId":"ofr83420S","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1983","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":"83-420","chapter":"S","title":"Distribution and abundance of cobalt, determined by spectrographic analysis, in the nonmagnetic fraction of heavy-mineral concentrates from stream sediments, Petersburg area, southeast Alaska","language":"ENGLISH","doi":"10.3133/ofr83420S","usgsCitation":"Cathrall, J.B., Day, G., Hoffman, J.D., and McDanal, S., 1983, Distribution and abundance of cobalt, determined by spectrographic analysis, in the nonmagnetic fraction of heavy-mineral concentrates from stream sediments, Petersburg area, southeast Alaska: U.S. Geological Survey Open-File Report 83-420, 1 map :photocopy ;53 x 70 cm., https://doi.org/10.3133/ofr83420S.","productDescription":"1 map :photocopy ;53 x 70 cm.","costCenters":[],"links":[{"id":135663,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":77970,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1983/0420s/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a81e4b07f02db64a117","contributors":{"authors":[{"text":"Cathrall, John B.","contributorId":26668,"corporation":false,"usgs":true,"family":"Cathrall","given":"John","email":"","middleInitial":"B.","affiliations":[],"preferred":false,"id":223756,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Day, G.W.","contributorId":63363,"corporation":false,"usgs":true,"family":"Day","given":"G.W.","email":"","affiliations":[],"preferred":false,"id":223757,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Hoffman, J. D.","contributorId":8419,"corporation":false,"usgs":true,"family":"Hoffman","given":"J.","email":"","middleInitial":"D.","affiliations":[],"preferred":false,"id":223755,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"McDanal, S.K.","contributorId":108078,"corporation":false,"usgs":true,"family":"McDanal","given":"S.K.","email":"","affiliations":[],"preferred":false,"id":223758,"contributorType":{"id":1,"text":"Authors"},"rank":4}]}}
,{"id":11552,"text":"ofr83417 - 1983 - Alteration and vein mineralization, Schwartzwalder uranium deposit, Front Range, Colorado","interactions":[],"lastModifiedDate":"2012-02-02T00:06:44","indexId":"ofr83417","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1983","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":"83-417","title":"Alteration and vein mineralization, Schwartzwalder uranium deposit, Front Range, Colorado","docAbstract":"The Schwartzwalder uranium deposit, in the Front Range west of Denver, Colorado, is the largest vein-type uranium deposit in the United States. The deposit is situated in a steeply dipping fault system that cuts Proterozoic metamorphic rocks. The host rocks represent a submarine volcanic system with associated chert and iron- and sulfide-rich pelitic rocks. Where faulted, the more competent garnetiferous and quartzitic units behaved brittlely and created a deep, narrow conduit. \r\n\r\nThe ores formed 70-72 m.y. ago beneath 3 km of Phanerozoic sedimentary rocks. Mineralization included two episodes of alteration and three stages of vein-mineralization. Early carbonate-sericite alteration pseudomorphically replaced mafic minerals, whereas the ensuing hematite-adularia episode replaced only the earlier alteration assemblage. Early vein mineralization produced a minor sulfide-adularia-carbonate assemblage. Later vein mineralization generated the uranium ores in two successive stages. Carbonates, sulfides, and adularia filled the remaining voids. Clastic dikes composed of fault gouge and, locally, ore were injected into new and existing fractures. \r\n\r\nGeologic and chemical evidence suggest that virtually all components of the deposit were derived from major hornblende gneiss units and related rocks. The initial fluids were evolved connate/metamorphic water that infiltrated and resided along the extensive fault zones. Complex fault movements in the frontal zone of the eastern Front Range caused the fluids to migrate to the most permeable segments of the fault zones. Heat was supplied by increased crustal heat flow related to igneous activity in the nearby Colorado mineral belt. Temperatures decreased from 225?C to 125?C during later mineralization, and the pressure episodically dropped from 1000 bars. The CO2 fugacity was initially near 100 bars, and uranium was carried as a dicarbonate complex. Sudden decreases in confining pressure during fault movement caused evolution of CO2 and a consequent increase in pH. Uranium was released with destruction of the uranyl complexes; it was subsequently reduced by aqueous sulfur species, thereby leading to the precipitation of pitchblende.","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/ofr83417","usgsCitation":"Wallace, A.R., 1983, Alteration and vein mineralization, Schwartzwalder uranium deposit, Front Range, Colorado: U.S. Geological Survey Open-File Report 83-417, 186 p. ill. ;28 cm., https://doi.org/10.3133/ofr83417.","productDescription":"186 p. ill. ;28 cm.","costCenters":[],"links":[{"id":145473,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1983/0417/report-thumb.jpg"},{"id":39426,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1983/0417/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4adee4b07f02db68751b","contributors":{"authors":[{"text":"Wallace, Alan R.","contributorId":6024,"corporation":false,"usgs":true,"family":"Wallace","given":"Alan","email":"","middleInitial":"R.","affiliations":[],"preferred":false,"id":163345,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":24045,"text":"ofr83942 - 1983 - Preliminary stage-discharge relations for Tombigbee River at Gainesville Dam, near Gainesville, Alabama","interactions":[],"lastModifiedDate":"2012-02-02T00:08:10","indexId":"ofr83942","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1983","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":"83-942","title":"Preliminary stage-discharge relations for Tombigbee River at Gainesville Dam, near Gainesville, Alabama","docAbstract":"The construction of Gainesville Dam and other related channel alterations, completed in 1979, has resulted in changes to the stage-discharge relations in the vicinity. The lack of current-meter measurements, coupled with backwater conditions, makes definition of a single stage-discharge relation impossible. However, limit curves can be defined that would encompass such a relation. Backwater is defined as water backed up or retarded in its course as compared with water flowing under normal or natural conditions. This results in a rise in stage above normal water level while the discharge remains unaffected. Backwater is usually caused by temporary obstruction(s) to the flow downstream. Backwater at Gainesville Dam is due to large tributary inflow and return of flood plain flows to the main channel during recessions. The discharges obtained from 105 computations of flow through the dam for the tailwater and 59 for the pool were plotted versus stage. These plots illustrate, by the scatter of these data points, the variations in backwater. Curves were drawn to envelope the extreme plot patterns showing possible ranges of several feet in stage for any given discharge for both the pool and the tailwater.","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/ofr83942","issn":"0094-9140","usgsCitation":"Nelson, G.H., and Ming, C.O., 1983, Preliminary stage-discharge relations for Tombigbee River at Gainesville Dam, near Gainesville, Alabama: U.S. Geological Survey Open-File Report 83-942, 16 p. :ill., maps ;28 cm., https://doi.org/10.3133/ofr83942.","productDescription":"16 p. :ill., maps ;28 cm.","costCenters":[],"links":[{"id":156317,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1983/0942/report-thumb.jpg"},{"id":53211,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1983/0942/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":53212,"rank":401,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1983/0942/plate-2.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":53213,"rank":402,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1983/0942/plate-3.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":53214,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1983/0942/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b32e4b07f02db6b48f2","contributors":{"authors":[{"text":"Nelson, G. H.","contributorId":48186,"corporation":false,"usgs":true,"family":"Nelson","given":"G.","email":"","middleInitial":"H.","affiliations":[],"preferred":false,"id":191214,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Ming, C. O.","contributorId":9266,"corporation":false,"usgs":true,"family":"Ming","given":"C.","email":"","middleInitial":"O.","affiliations":[],"preferred":false,"id":191213,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
]}