{"pageNumber":"5857","pageRowStart":"146400","pageSize":"25","recordCount":184595,"records":[{"id":70047447,"text":"70047447 - 1977 - Floods in Pennsylvania: a manual for estimation of their magnitude and frequency","interactions":[{"subject":{"id":18929,"text":"ofr76391 - 1976 - Floods in Pennsylvania: A manual for estimation of their magnitude and frequency","indexId":"ofr76391","publicationYear":"1976","noYear":false,"title":"Floods in Pennsylvania: A manual for estimation of their magnitude and frequency"},"predicate":"SUPERSEDED_BY","object":{"id":70047447,"text":"70047447 - 1977 - Floods in Pennsylvania: a manual for estimation of their magnitude and frequency","indexId":"70047447","publicationYear":"1977","noYear":false,"title":"Floods in Pennsylvania: a manual for estimation of their magnitude and frequency"},"id":1}],"lastModifiedDate":"2013-08-06T11:54:36","indexId":"70047447","displayToPublicDate":"2013-01-01T11:53:20","publicationYear":"1977","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":2,"text":"State or Local Government Series"},"seriesTitle":{"id":105,"text":"Bulletin","active":false,"publicationSubtype":{"id":2}},"seriesNumber":"13","title":"Floods in Pennsylvania: a manual for estimation of their magnitude and frequency","language":"English","publisher":"Pennsylvania Department of Environmental Resources","usgsCitation":"Flippo, H., 1977, Floods in Pennsylvania: a manual for estimation of their magnitude and frequency: Bulletin 13, 59 p.","productDescription":"59 p.","costCenters":[],"links":[{"id":276117,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"52021ae3e4b0e21cafa49c40","contributors":{"authors":[{"text":"Flippo, H.N. Jr.","contributorId":96301,"corporation":false,"usgs":true,"family":"Flippo","given":"H.N.","suffix":"Jr.","affiliations":[],"preferred":false,"id":482057,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":70047792,"text":"70047792 - 1977 - Uranium and phosphate resources in Cooper Formation in the Charleston region, South Carolina","interactions":[{"subject":{"id":7591,"text":"ofr78586 - 1978 - Uranium and phosphate resources in the Cooper Formation of the Charleston region, South Carolina","indexId":"ofr78586","publicationYear":"1978","noYear":false,"title":"Uranium and phosphate resources in the Cooper Formation of the Charleston region, South Carolina"},"predicate":"SUPERSEDED_BY","object":{"id":70047792,"text":"70047792 - 1977 - Uranium and phosphate resources in Cooper Formation in the Charleston region, South Carolina","indexId":"70047792","publicationYear":"1977","noYear":false,"title":"Uranium and phosphate resources in Cooper Formation in the Charleston region, South Carolina"},"id":1}],"lastModifiedDate":"2014-05-30T14:24:10","indexId":"70047792","displayToPublicDate":"2013-01-01T11:17:00","publicationYear":"1977","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1777,"text":"Geologic Notes","active":true,"publicationSubtype":{"id":10}},"title":"Uranium and phosphate resources in Cooper Formation in the Charleston region, South Carolina","largerWorkType":{"id":2,"text":"Article"},"largerWorkTitle":"Geologic Notes","largerWorkSubtype":{"id":10,"text":"Journal Article"},"language":"English","publisher":"South Carolina Geological Survey","publisherLocation":"Columbia, SC","usgsCitation":"Force, E.R., Gohn, G.S., Force, L., and Higgins, B., 1977, Uranium and phosphate resources in Cooper Formation in the Charleston region, South Carolina: Geologic Notes, v. 22, no. 1, p. 17-31.","productDescription":"15 p.","startPage":"17","endPage":"31","numberOfPages":"15","costCenters":[],"links":[{"id":276952,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United States","state":"South Carolina","city":"Charleston","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -80.31,32.5922 ], [ -80.31,33.0254 ], [ -79.6283,33.0254 ], [ -79.6283,32.5922 ], [ -80.31,32.5922 ] ] ] } } ] }","volume":"22","issue":"1","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"5218846de4b0e27b926cc6fa","contributors":{"authors":[{"text":"Force, E. R.","contributorId":28235,"corporation":false,"usgs":true,"family":"Force","given":"E.","email":"","middleInitial":"R.","affiliations":[],"preferred":false,"id":482974,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Gohn, G. S.","contributorId":25937,"corporation":false,"usgs":true,"family":"Gohn","given":"G.","email":"","middleInitial":"S.","affiliations":[],"preferred":false,"id":482973,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Force, L.M.","contributorId":7266,"corporation":false,"usgs":true,"family":"Force","given":"L.M.","email":"","affiliations":[],"preferred":false,"id":482971,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Higgins, B.B.","contributorId":8091,"corporation":false,"usgs":true,"family":"Higgins","given":"B.B.","email":"","affiliations":[],"preferred":false,"id":482972,"contributorType":{"id":1,"text":"Authors"},"rank":4}]}}
,{"id":70047715,"text":"70047715 - 1977 - Water resources of the Weiser River basin, west-central Idaho","interactions":[{"subject":{"id":11791,"text":"ofr77418 - 1977 - Water resources of the Weiser River basin, west-central Idaho","indexId":"ofr77418","publicationYear":"1977","noYear":false,"title":"Water resources of the Weiser River basin, west-central Idaho"},"predicate":"SUPERSEDED_BY","object":{"id":70047715,"text":"70047715 - 1977 - Water resources of the Weiser River basin, west-central Idaho","indexId":"70047715","publicationYear":"1977","noYear":false,"title":"Water resources of the Weiser River basin, west-central Idaho"},"id":1}],"lastModifiedDate":"2013-08-20T10:44:59","indexId":"70047715","displayToPublicDate":"2013-01-01T10:38:38","publicationYear":"1977","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":2,"text":"State or Local Government Series"},"seriesTitle":{"id":141,"text":"Water Information Bulletin","active":false,"publicationSubtype":{"id":2}},"seriesNumber":"44","title":"Water resources of the Weiser River basin, west-central Idaho","docAbstract":"The study area comprises about 1,600 square miles (4,100 square kilometers) in west-central Idaho and includes the entire Weiser River basin and small areas both west and south of Weiser outside the basin. The basin is sparsely populated and the economy is chiefly agricultural.","language":"English","publisher":"Idaho Department of Water Resources","publisherLocation":"Boise, ID","collaboration":"Prepared by the United States Geological Survey in cooperation with the Idaho Department of Water Resources","usgsCitation":"Young, H., Harenberg, W., and Seitz, H.R., 1977, Water resources of the Weiser River basin, west-central Idaho: Water Information Bulletin 44, vii, 104 p.; Maps: 9 Sheets.","productDescription":"vii, 104 p.; Maps: 9 Sheets","numberOfPages":"122","costCenters":[],"links":[{"id":276799,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/70047715.JPG"},{"id":276798,"type":{"id":11,"text":"Document"},"url":"https://www.idwr.idaho.gov/WaterInformation/Publications/wib/wib44-weiser_river_basin.pdf"}],"country":"United States","state":"Idaho","otherGeospatial":"Weiser River Basin","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -117.24,41.99 ], [ -117.24,49.0 ], [ -111.04,49.0 ], [ -111.04,41.99 ], [ -117.24,41.99 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"52148fe7e4b06d85e08fb52f","contributors":{"authors":[{"text":"Young, H.W.","contributorId":68278,"corporation":false,"usgs":true,"family":"Young","given":"H.W.","email":"","affiliations":[],"preferred":false,"id":482793,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Harenberg, W. A.","contributorId":78743,"corporation":false,"usgs":true,"family":"Harenberg","given":"W. A.","affiliations":[],"preferred":false,"id":482794,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Seitz, Harold R.","contributorId":61814,"corporation":false,"usgs":true,"family":"Seitz","given":"Harold","email":"","middleInitial":"R.","affiliations":[],"preferred":false,"id":482792,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":70047785,"text":"70047785 - 1977 - Planimetric Martian triangulations","interactions":[{"subject":{"id":7756,"text":"ofr76767 - 1976 - Planimetric Martian triangulations","indexId":"ofr76767","publicationYear":"1976","noYear":false,"title":"Planimetric Martian triangulations"},"predicate":"SUPERSEDED_BY","object":{"id":70047785,"text":"70047785 - 1977 - Planimetric Martian triangulations","indexId":"70047785","publicationYear":"1977","noYear":false,"title":"Planimetric Martian triangulations"},"id":1}],"lastModifiedDate":"2013-08-23T10:26:26","indexId":"70047785","displayToPublicDate":"2013-01-01T10:23:00","publicationYear":"1977","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":3052,"text":"Photogrammetric Engineering and Remote Sensing","active":true,"publicationSubtype":{"id":10}},"title":"Planimetric Martian triangulations","docAbstract":"Narrow-angle photographs, which have severe drawbacks for stereophotogrammetry, have advantages for simple plane triangulations. Rectified narrow-angle pictures corrected for map projection effects can be combined in the map plane in relatively accurate planimetric triangulations. Provided the strict precepts of least squares are not followed, these triangulations can incorporate considerable overdetermination without increase in the labor of solving the equations. These plane triangulations have been used successfully in the cartography of Mars and are illustrated here by a triangulation of the environs of the prime Martian landing site.","largerWorkType":{"id":2,"text":"Article"},"largerWorkTitle":"Photogrammetric Engineering and Remote Sensing","largerWorkSubtype":{"id":10,"text":"Journal Article"},"language":"English","publisher":"ASPRS","usgsCitation":"Arthur, D., and McMacken, D., 1977, Planimetric Martian triangulations: Photogrammetric Engineering and Remote Sensing, v. 43, no. 6, p. 701-707.","productDescription":"7 p.","startPage":"701","endPage":"707","costCenters":[],"links":[{"id":276942,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"},{"id":276941,"type":{"id":11,"text":"Document"},"url":"https://eserv.asprs.org/PERS/1977journal/jun/1977_jun_701-707.pdf"}],"otherGeospatial":"Mars","volume":"43","issue":"6","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"52188469e4b0e27b926cc6c3","contributors":{"authors":[{"text":"Arthur, D.W.G.","contributorId":20463,"corporation":false,"usgs":true,"family":"Arthur","given":"D.W.G.","email":"","affiliations":[],"preferred":false,"id":482962,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"McMacken, D.K.","contributorId":102481,"corporation":false,"usgs":true,"family":"McMacken","given":"D.K.","affiliations":[],"preferred":false,"id":482963,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":70047784,"text":"70047784 - 1977 - Preliminary bedrock geologic map of part of the northern disturbed belt, Lewis and Clark, Teton, Pondera, Glacier, Flathead, and Powell Counties, Montana","interactions":[{"subject":{"id":10433,"text":"ofr7725 - 1976 - Preliminary bedrock geologic map of part of the northern disturbed belt, Lewis and Clark, Teton, Pondera, Glacier, Flathead, and Powell Counties, Montana","indexId":"ofr7725","publicationYear":"1976","noYear":false,"title":"Preliminary bedrock geologic map of part of the northern disturbed belt, Lewis and Clark, Teton, Pondera, Glacier, Flathead, and Powell Counties, Montana"},"predicate":"SUPERSEDED_BY","object":{"id":70047784,"text":"70047784 - 1977 - Preliminary bedrock geologic map of part of the northern disturbed belt, Lewis and Clark, Teton, Pondera, Glacier, Flathead, and Powell Counties, Montana","indexId":"70047784","publicationYear":"1977","noYear":false,"title":"Preliminary bedrock geologic map of part of the northern disturbed belt, Lewis and Clark, Teton, Pondera, Glacier, Flathead, and Powell Counties, Montana"},"id":1}],"lastModifiedDate":"2013-08-23T10:17:04","indexId":"70047784","displayToPublicDate":"2013-01-01T10:10:00","publicationYear":"1977","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":3312,"text":"Rocky Mountain thrust belt geology and resources (29th Annual Field Conference Guidebook)","active":true,"publicationSubtype":{"id":10}},"title":"Preliminary bedrock geologic map of part of the northern disturbed belt, Lewis and Clark, Teton, Pondera, Glacier, Flathead, and Powell Counties, Montana","docAbstract":"The geologic map covers the Sawtooth and Lewis and Clark Ranges and part of the Flathead Range. It includes most of the disturbed belt in northwestern Moutana except the area east of the northern Rocky Mountains and the norhtern and southern parts of the belt. Most data are from an unpublished map of the Bob Marshall Wilderness and of the many proposed additions to the Wilderness. Strike and dip symbols are omitted from the map, and all contacts are shown in solid lines, alhough locally they are inferred beneath a Quaternary cover. Future studies will complete mapping of the northern disturbed belt in Montana.","largerWorkType":{"id":18,"text":"Report"},"largerWorkTitle":"Rocky Mountain thrust belt geology and resources (29th Annual Field Conference Guidebook)","largerWorkSubtype":{"id":2,"text":"State or Local Government Series"},"language":"English","publisher":"Wyoming Geological Association","publisherLocation":"Casper, WY","usgsCitation":"Mudge, M., Earhart, R.L., and Rice, D.D., 1977, Preliminary bedrock geologic map of part of the northern disturbed belt, Lewis and Clark, Teton, Pondera, Glacier, Flathead, and Powell Counties, Montana: Rocky Mountain thrust belt geology and resources (29th Annual Field Conference Guidebook), p. 471-478.","productDescription":"8 p.","startPage":"471","endPage":"478","costCenters":[],"links":[{"id":276940,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"},{"id":276939,"type":{"id":15,"text":"Index Page"},"url":"https://archives.datapages.com/data/wga/data/033/033001/471_wga0330471.htm"}],"country":"United States","state":"Montana","county":"Lewis And Clark County;Teton County;Pondera County;Glacier County;Flathead County;Powell County","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -116.05,44.36 ], [ -116.05,49.0 ], [ -104.04,49.0 ], [ -104.04,44.36 ], [ -116.05,44.36 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"52188469e4b0e27b926cc6ca","contributors":{"editors":[{"text":"Heisey, E.L.","contributorId":112874,"corporation":false,"usgs":true,"family":"Heisey","given":"E.L.","email":"","affiliations":[],"preferred":false,"id":509581,"contributorType":{"id":2,"text":"Editors"},"rank":1}],"authors":[{"text":"Mudge, Melville R.","contributorId":72370,"corporation":false,"usgs":true,"family":"Mudge","given":"Melville R.","affiliations":[],"preferred":false,"id":482960,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Earhart, Robert L.","contributorId":74729,"corporation":false,"usgs":true,"family":"Earhart","given":"Robert","email":"","middleInitial":"L.","affiliations":[],"preferred":false,"id":482961,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Rice, Dudley D.","contributorId":11601,"corporation":false,"usgs":true,"family":"Rice","given":"Dudley","email":"","middleInitial":"D.","affiliations":[],"preferred":false,"id":482959,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":70047906,"text":"70047906 - 1977 - Analysis of borehole geophysical data in an evaporite sequence at Salt Valley, Utah","interactions":[],"lastModifiedDate":"2013-08-30T09:47:29","indexId":"70047906","displayToPublicDate":"2013-01-01T09:44:00","publicationYear":"1977","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":3413,"text":"Society of Professional Well Log Analysts, Transactions","active":true,"publicationSubtype":{"id":10}},"title":"Analysis of borehole geophysical data in an evaporite sequence at Salt Valley, Utah","largerWorkType":{"id":2,"text":"Article"},"largerWorkTitle":"Society of Professional Well Log Analysts, Transactions","largerWorkSubtype":{"id":10,"text":"Journal Article"},"language":"English","publisher":"Society of Professional Well Log Analysts","usgsCitation":"Daniels, J., Scott, J.H., and Hite, R.J., 1977, Analysis of borehole geophysical data in an evaporite sequence at Salt Valley, Utah: Society of Professional Well Log Analysts, Transactions, v. 20, p. M1-M19.","productDescription":"19 p.","startPage":"M1","endPage":"M19","costCenters":[],"links":[{"id":277173,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United States","state":"Utah","otherGeospatial":"Salt Valley","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -109.713199,38.603166 ], [ -109.713199,38.846933 ], [ -109.477713,38.846933 ], [ -109.477713,38.603166 ], [ -109.713199,38.603166 ] ] ] } } ] }","volume":"20","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"5221bee0e4b001cbb8a34ec7","contributors":{"authors":[{"text":"Daniels, J.J.","contributorId":75929,"corporation":false,"usgs":true,"family":"Daniels","given":"J.J.","email":"","affiliations":[],"preferred":false,"id":483260,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Scott, J. H.","contributorId":15204,"corporation":false,"usgs":true,"family":"Scott","given":"J.","email":"","middleInitial":"H.","affiliations":[],"preferred":false,"id":483259,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Hite, R. J.","contributorId":82701,"corporation":false,"usgs":true,"family":"Hite","given":"R.","email":"","middleInitial":"J.","affiliations":[],"preferred":false,"id":483261,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":70043932,"text":"70043932 - 1977 - Hydrologic evaluation of the upper Duchesne River Valley, northern Uinta Basin area, Utah","interactions":[{"subject":{"id":9559,"text":"ofr76771 - 1976 - Hydrologic evaluation of the Upper Duchesne River Valley, Northern Uinta Basin area, Utah","indexId":"ofr76771","publicationYear":"1976","noYear":false,"title":"Hydrologic evaluation of the Upper Duchesne River Valley, Northern Uinta Basin area, Utah"},"predicate":"SUPERSEDED_BY","object":{"id":70043932,"text":"70043932 - 1977 - Hydrologic evaluation of the upper Duchesne River Valley, northern Uinta Basin area, Utah","indexId":"70043932","publicationYear":"1977","noYear":false,"title":"Hydrologic evaluation of the upper Duchesne River Valley, northern Uinta Basin area, Utah"},"id":1}],"lastModifiedDate":"2016-12-12T14:04:30","indexId":"70043932","displayToPublicDate":"2013-01-01T00:00:00","publicationYear":"1977","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":4,"text":"Other Government Series"},"seriesTitle":{"id":294,"text":"Technical Publication","active":false,"publicationSubtype":{"id":4}},"seriesNumber":"57","title":"Hydrologic evaluation of the upper Duchesne River Valley, northern Uinta Basin area, Utah","docAbstract":"The upper Duchesne River valley was studied during 1971-74 as part of an investigation of the northern Uinta Basin area, Utah and Colorado. The purpose of the study was to determine the relation of ground water to surface water, to estimate the quantity of ground water that moves to the Duchesne River, and to assess the probable effect of increased ground-water withdrawal on streamflow.","language":"English","publisher":"Utah Department of Natural Resources, Division of Water Rights","publisherLocation":"Salt Lake City, UT","collaboration":"Prepared by the United State Geological Survey in cooperation with the Utah Department of Natural Resources Division of Water Rights","usgsCitation":"Hood, J.W., 1977, Hydrologic evaluation of the upper Duchesne River Valley, northern Uinta Basin area, Utah: Technical Publication 57, iv, 34 p.","productDescription":"iv, 34 p.","numberOfPages":"42","costCenters":[{"id":610,"text":"Utah Water Science Center","active":true,"usgs":true}],"links":[{"id":268026,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"},{"id":268025,"type":{"id":11,"text":"Document"},"url":"https://waterrights.utah.gov/docSys/v920/w920/w920009j.pdf"},{"id":331952,"rank":3,"type":{"id":15,"text":"Index Page"},"url":"https://www.waterrights.utah.gov/cgi-bin/libview.exe?Modinfo=Viewpub&LIBNUM=20-5-410"}],"country":"United States","state":"Utah","otherGeospatial":"Duchesne River, Uinta Basin","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -111.86279296875,\n              39.232253141714885\n            ],\n            [\n              -111.86279296875,\n              40.94671366508002\n            ],\n            [\n              -108.56689453125,\n              40.94671366508002\n            ],\n            [\n              -108.56689453125,\n              39.232253141714885\n            ],\n            [\n              -111.86279296875,\n              39.232253141714885\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"5129f32ae4b04edf7e93f8de","contributors":{"authors":[{"text":"Hood, James W.","contributorId":66115,"corporation":false,"usgs":true,"family":"Hood","given":"James","email":"","middleInitial":"W.","affiliations":[],"preferred":false,"id":474509,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":70042821,"text":"70042821 - 1977 - Black monazite from Taiwan","interactions":[{"subject":{"id":15285,"text":"ofr71221 - 1971 - Monazite in Taiwan","indexId":"ofr71221","publicationYear":"1971","noYear":false,"title":"Monazite in Taiwan"},"predicate":"SUPERSEDED_BY","object":{"id":70042821,"text":"70042821 - 1977 - Black monazite from Taiwan","indexId":"70042821","publicationYear":"1977","noYear":false,"title":"Black monazite from Taiwan"},"id":1}],"lastModifiedDate":"2013-02-13T14:35:38","indexId":"70042821","displayToPublicDate":"2013-01-01T00:00:00","publicationYear":"1977","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":3153,"text":"Proceedings of the Geological Society of China","active":true,"publicationSubtype":{"id":10}},"title":"Black monazite from Taiwan","docAbstract":"Two forms of detrital monazite are known in offshore bars in southwestern Taiwan: a yellow-green to colorless form and an unusual but abundant pelletlike form, generally black but also colored gray or brown. These black pellets, which are about 160 by 200 microns in size, are composed of fine-grained monazite crystals from 2 to 20 microns in size. The pellets are associated with highly variable amounts of discrete grains of detrital quartz, rutile, amphibole, tourmaline, and other minerals. Intergrown with the monazite are quartz, a cerium oxide mineral, chlorite, sulfides, and other minerals. Opaqueness of the pelletlike monazite is due principally to the cryptocrystalline nature of part of the monazite; only a small part of the opaqueness can be attributed to opaque inclusions. The black pelletlike monazite lacks thorium and has a high content of europium. In this respect, as in color, shape, size, and inclusions, the pelletlike monazite differs from the yellow-green detrital monazite. Despite the fact that they occur together in the littoral placers, they appear to have had different origins. The yellow-green monazite originated as an accessory mineral in plutonic rocks and has accumulated at the coast through erosion and transport. The origin of the pelletlike monazite is as yet unknown, but it is here inferred that it originated in unconsolidated coastal plain sediments through migration of cerium from the detrital monazite during weathering, and of the intermediate weight mobile rare earths from clay minerals during diagenesis. Possibly these pelletlike grains are detrital particles formed through erosion and transport from originally larger aggregates cemented by diagenetic monazite.","largerWorkType":{"id":2,"text":"Article"},"largerWorkTitle":"Proceedings of the Geological Society of China","largerWorkSubtype":{"id":10,"text":"Journal Article"},"language":"English","publisher":"Geological Society of China","publisherLocation":"Beijing, China","usgsCitation":"Matzko, J., and Overstreet, W., 1977, Black monazite from Taiwan: Proceedings of the Geological Society of China, v. 20, p. 16-35.","productDescription":"10 p.","startPage":"16","endPage":"35","costCenters":[{"id":387,"text":"Mineral Resources Program","active":true,"usgs":true}],"links":[{"id":266425,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"Taiwan","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ 119.103,21.5576 ], [ 119.103,25.8299 ], [ 122.297,25.8299 ], [ 122.297,21.5576 ], [ 119.103,21.5576 ] ] ] } } ] }","volume":"20","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"51026607e4b0d4f5ea817bae","contributors":{"authors":[{"text":"Matzko, J.J.","contributorId":87927,"corporation":false,"usgs":true,"family":"Matzko","given":"J.J.","email":"","affiliations":[],"preferred":false,"id":472327,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Overstreet, W.C.","contributorId":105294,"corporation":false,"usgs":true,"family":"Overstreet","given":"W.C.","email":"","affiliations":[],"preferred":false,"id":472328,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":70042638,"text":"70042638 - 1977 - Model for evaluating the effects of dikes on the water and salt balance of Great Salt Lake, Utah","interactions":[{"subject":{"id":16395,"text":"ofr76256 - 1976 - Model for evaluating the effects of dikes on the water and salt balance of Great Salt Lake, Utah","indexId":"ofr76256","publicationYear":"1976","noYear":false,"title":"Model for evaluating the effects of dikes on the water and salt balance of Great Salt Lake, Utah"},"predicate":"SUPERSEDED_BY","object":{"id":70042638,"text":"70042638 - 1977 - Model for evaluating the effects of dikes on the water and salt balance of Great Salt Lake, Utah","indexId":"70042638","publicationYear":"1977","noYear":false,"title":"Model for evaluating the effects of dikes on the water and salt balance of Great Salt Lake, Utah"},"id":1}],"lastModifiedDate":"2017-09-06T17:31:51","indexId":"70042638","displayToPublicDate":"2013-01-01T00:00:00","publicationYear":"1977","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":2,"text":"State or Local Government Series"},"seriesTitle":{"id":5485,"text":"Utah Geological and Mineralogical Survey Water-Resources Bulletin","active":false,"publicationSubtype":{"id":2}},"seriesNumber":"21","title":"Model for evaluating the effects of dikes on the water and salt balance of Great Salt Lake, Utah","docAbstract":"A model was developed for predicting the water and salt budget for various diking options in Great Salt Lake.","language":"English","publisher":"Utah Geological and Mineral Survey","publisherLocation":"Salt Lake City, UT","collaboration":"Prepared by the United States Geological Survey in cooperation with the Utah Geological and Mineral Survey","usgsCitation":"Waddell, K., and Fields, F., 1977, Model for evaluating the effects of dikes on the water and salt balance of Great Salt Lake, Utah: Utah Geological and Mineralogical Survey Water-Resources Bulletin 21, v, 54 p.","productDescription":"v, 54 p.","numberOfPages":"63","costCenters":[{"id":610,"text":"Utah Water Science Center","active":true,"usgs":true}],"links":[{"id":265725,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"},{"id":265724,"type":{"id":11,"text":"Document"},"url":"https://ugspub.nr.utah.gov/publications/water_resources_bulletins/WRB-21.pdf"}],"country":"United States","state":"Utah","otherGeospatial":"Great Salt Lake","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -113.1012,40.669 ], [ -113.1012,41.705 ], [ -111.9302,41.705 ], [ -111.9302,40.669 ], [ -113.1012,40.669 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"50f6888de4b0f5392eb7e7b0","contributors":{"authors":[{"text":"Waddell, K.M.","contributorId":59009,"corporation":false,"usgs":true,"family":"Waddell","given":"K.M.","email":"","affiliations":[],"preferred":false,"id":471948,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Fields, F.K.","contributorId":90826,"corporation":false,"usgs":true,"family":"Fields","given":"F.K.","email":"","affiliations":[],"preferred":false,"id":471949,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":70046305,"text":"70046305 - 1977 - Ground-water resources of Griggs and Steele Counties, North Dakota","interactions":[{"subject":{"id":42456,"text":"ofr741023 - 1974 - Preliminary map showing availability of ground water from major glacial-drift aquifers in Griggs and Steele Counties, North Dakota","indexId":"ofr741023","publicationYear":"1974","noYear":false,"title":"Preliminary map showing availability of ground water from major glacial-drift aquifers in Griggs and Steele Counties, North Dakota"},"predicate":"SUPERSEDED_BY","object":{"id":70046305,"text":"70046305 - 1977 - Ground-water resources of Griggs and Steele Counties, North Dakota","indexId":"70046305","publicationYear":"1977","noYear":false,"title":"Ground-water resources of Griggs and Steele Counties, North Dakota"},"id":1}],"lastModifiedDate":"2018-05-23T12:55:59","indexId":"70046305","displayToPublicDate":"2013-01-01T00:00:00","publicationYear":"1977","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":4,"text":"Other Government Series"},"seriesTitle":{"id":242,"text":"Bulletin","active":false,"publicationSubtype":{"id":4}},"seriesNumber":"64-3","title":"Ground-water resources of Griggs and Steele Counties, North Dakota","docAbstract":"Griggs and Steele Counties, in east-central North Dakota, are underlain by bedrock of Ordovician, Jurassic, and Cretaceous ages. The Fall River and Lakota Formations of Cretaceous age form the Dakota aquifer. The fractured upper part of the Pierre Formation (shale), also of Cretaceous age, forms another bedrock aquifer. The Dakota aquifer, which consists mainly of interbedded shale and sandstone units, may yield as much as 500 gallons per minute (32 liters per second) of sodium sulfate water to wells at selected locations. The Pierre aquifer yields from 1 to 10 gallons per minute (0.06 to 0.63 liters per second) of sodium bicarbonate or sodium sulfate water to wells. Four major glacial-drift aquifers are present in the study area. The Spiritwood aquifer system may supply as much as 1,500 gallons per minute (95 liters per second) of water to wells. Water samples contained dissolved-solids concentrations ranging from 244 to 9,800 milligrams per liter. The Galesburg aquifer will yield as much as 1,000 gallons per minute (63 liters per second) of water to wells. Water samples contained dissolved-solids concentrations ranging from 317 to 2,170 milligrams per liter. The McVille aquifer will yield as much as 500 gallons per minute (32 liters per second) to wells. Water samples contained dissolved-solids concentrations ranging from 449 to 2,200 milligrams per liter. The Elk Valley aquifer could yield 30 gallons per minute (2 liters per second) to wells. Water samples contained dissolved-solids concentrations ranging from 397 to 2,890 milligrams per liter. Six communities in the project area use ground-water supplies. Rural water districts are being developed in the two-county area that will provide dependable ground-water supplies for many farms and small municipalities. The Spiritwood aquifer system and the McVille and Galesburg aquifers are capable of supplying the water needs of these districts and could also provide water for irrigation.","language":"English","publisher":"North Dakota Geological Survey","publisherLocation":"Grand Forks, ND","collaboration":"Prepared by the U.S. Geological Survey in cooperation with the North Dakota Geological Survey, North Dakota State Water Commission, Griggs County Water Management District and the Steele County Water Management District; This report was also published as North Dakota County Ground-Water Studies 21-3","usgsCitation":"Downey, J.S., and Armstrong, C.A., 1977, Ground-water resources of Griggs and Steele Counties, North Dakota: Bulletin 64-3, iii, 33 p.; Maps: 2 Sheets: 31 x 20 inches.","productDescription":"iii, 33 p.; Maps: 2 Sheets: 31 x 20 inches","numberOfPages":"37","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":273365,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/70046305.png"},{"id":273363,"type":{"id":11,"text":"Document"},"url":"https://www.swc.nd.gov/4dlink9/4dcgi/GetSubContentPDF/PB-255/GriggsSteel_Part_3.pdf"},{"id":273364,"type":{"id":17,"text":"Plate"},"url":"https://www.swc.nd.gov/4dlink9/4dcgi/GetSubContentPDF/PB-256/GriggsSteele_Part_3_Plates.pdf"}],"country":"United States","state":"North Dakota","county":"Griggs County, Steele County","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -98.5019,47.2394 ], [ -98.5019,47.6742 ], [ -97.4504,47.6742 ], [ -97.4504,47.2394 ], [ -98.5019,47.2394 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"51b1bbd2e4b022a6a540f9d3","contributors":{"authors":[{"text":"Downey, Joe S.","contributorId":102454,"corporation":false,"usgs":true,"family":"Downey","given":"Joe","email":"","middleInitial":"S.","affiliations":[],"preferred":false,"id":479432,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Armstrong, C. A.","contributorId":66231,"corporation":false,"usgs":true,"family":"Armstrong","given":"C.","email":"","middleInitial":"A.","affiliations":[],"preferred":false,"id":479431,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":70043961,"text":"70043961 - 1977 - Seepage study of the Sevier Valley-Piute Canal, Sevier County, Utah","interactions":[{"subject":{"id":8474,"text":"ofr77326 - 1977 - Seepage study of the Sevier Valley-Piute Canal, Sevier County, Utah","indexId":"ofr77326","publicationYear":"1977","noYear":false,"title":"Seepage study of the Sevier Valley-Piute Canal, Sevier County, Utah"},"predicate":"SUPERSEDED_BY","object":{"id":70043961,"text":"70043961 - 1977 - Seepage study of the Sevier Valley-Piute Canal, Sevier County, Utah","indexId":"70043961","publicationYear":"1977","noYear":false,"title":"Seepage study of the Sevier Valley-Piute Canal, Sevier County, Utah"},"id":1}],"lastModifiedDate":"2016-12-12T14:16:26","indexId":"70043961","displayToPublicDate":"2013-01-01T00:00:00","publicationYear":"1977","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":4,"text":"Other Government Series"},"seriesTitle":{"id":294,"text":"Technical Publication","active":false,"publicationSubtype":{"id":4}},"seriesNumber":"58","title":"Seepage study of the Sevier Valley-Piute Canal, Sevier County, Utah","docAbstract":"A study of the gains or losses of the Sevier Valley-Piute Canal from near Joseph to near Aurora, Sevier County, Utah, was made to aid in water allocation for the canal system. Four sets of seepage measurements were made in 1976, with the three most representative being used in the analysis. Adjustments for fluctuations in flow in the canals were made from information obtained from water-stage recorders operated at selected locations along the canal during the time of each seepage run.","language":"English","publisher":"Utah Department of Natural Resources,Division of Water Rights","publisherLocation":"Salt Lake City, UT","collaboration":"Prepared by the United States Geological Survey in cooperation with the Utah Department of Natural Resources Division of Water Rights","usgsCitation":"Cruff, R., 1977, Seepage study of the Sevier Valley-Piute Canal, Sevier County, Utah: Technical Publication 58, iv, 31 p.","productDescription":"iv, 31 p.","numberOfPages":"36","costCenters":[{"id":610,"text":"Utah Water Science Center","active":true,"usgs":true}],"links":[{"id":268162,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"},{"id":331957,"rank":3,"type":{"id":15,"text":"Index Page"},"url":"https://www.waterrights.utah.gov/cgi-bin/libview.exe?Modinfo=Viewpub&LIBNUM=20-5-430"},{"id":268161,"type":{"id":11,"text":"Document"},"url":"https://waterrights.utah.gov/docSys/v920/w920/w920009k.pdf"}],"country":"United States","state":"Utah","county":"Sevier County","otherGeospatial":"Piute Canal, Sevier Valley, Sevier Valley Canal","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -112.25109100341797,\n              38.620894111290774\n            ],\n            [\n              -112.20611572265625,\n              38.601846852838094\n            ],\n            [\n              -112.0550537109375,\n              38.76532733447257\n            ],\n            [\n              -111.88888549804686,\n              38.91133881927712\n            ],\n            [\n              -111.93832397460938,\n              38.94819537985111\n            ],\n            [\n              -112.09007263183594,\n              38.82419583577267\n            ],\n            [\n              -112.15118408203125,\n              38.74444410121548\n            ],\n            [\n              -112.23426818847656,\n              38.65763297744505\n            ],\n            [\n              -112.25109100341797,\n              38.620894111290774\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"512b44bbe4b0523e997a81b4","contributors":{"authors":[{"text":"Cruff, R.W.","contributorId":77510,"corporation":false,"usgs":true,"family":"Cruff","given":"R.W.","email":"","affiliations":[],"preferred":false,"id":474553,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":70043723,"text":"70043723 - 1977 - Hydrologic evaluation of Ashley Valley, northern Uinta basin area, Utah","interactions":[{"subject":{"id":19438,"text":"ofr76496 - 1976 - Hydrologic evaluation of Ashley Valley, northern Uinta Basin area, Utah","indexId":"ofr76496","publicationYear":"1976","noYear":false,"title":"Hydrologic evaluation of Ashley Valley, northern Uinta Basin area, Utah"},"predicate":"SUPERSEDED_BY","object":{"id":70043723,"text":"70043723 - 1977 - Hydrologic evaluation of Ashley Valley, northern Uinta basin area, Utah","indexId":"70043723","publicationYear":"1977","noYear":false,"title":"Hydrologic evaluation of Ashley Valley, northern Uinta basin area, Utah"},"id":1},{"subject":{"id":52966,"text":"ofr5086 - 1950 - Progress report on ground-water investigation in Ashley Valley, Uintah County, Utah","indexId":"ofr5086","publicationYear":"1950","noYear":false,"title":"Progress report on ground-water investigation in Ashley Valley, Uintah County, Utah"},"predicate":"SUPERSEDED_BY","object":{"id":70043723,"text":"70043723 - 1977 - Hydrologic evaluation of Ashley Valley, northern Uinta basin area, Utah","indexId":"70043723","publicationYear":"1977","noYear":false,"title":"Hydrologic evaluation of Ashley Valley, northern Uinta basin area, Utah"},"id":2}],"lastModifiedDate":"2017-01-05T17:07:01","indexId":"70043723","displayToPublicDate":"2013-01-01T00:00:00","publicationYear":"1977","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":4,"text":"Other Government Series"},"seriesTitle":{"id":294,"text":"Technical Publication","active":false,"publicationSubtype":{"id":4}},"seriesNumber":"54","title":"Hydrologic evaluation of Ashley Valley, northern Uinta basin area, Utah","docAbstract":"<p>The water resources of the northern Uinta Basin, Utah and Colorado, were studied during 1971-74. Ashley Valley was evaluated in slightly greater detail than the general area, in order to assess the general relation of ground- and surface-water supplies.</p>\n<br>\n<p>In Ashley Valley , the principal source of both irrigation supply\nand ground-water recharge is the flow from Ashley Creek canyon .\nGround-water recharge to the valley fill, however, is mainly from canal\nand field losses along the west side of the valley. The permeability of\nthe fill in most places is high, and water-level records indicate rapid\nchanges in storage in response to the annual applications of irrigation\nwater.</p>\n<br>\n<p>Prior to the distribution of water from Steinaker Reservoir, the\nshort runoff season led to a brief, intense irrigation period that was\nfollowed by a long period of post-irrigation drainage. After the\nreservoir began operation, smaller applications of water were made\nduring a longer season, and ground-water levels rose in parts of the\nvalley , mainly the lower areas. Despite local water-level rises, no\nperennially gaining reaches of the canals were observed.</p>\n<br>\n<p>The amount of ground water available from storage in Ashley\nValley is estimated to be 50,000-75,000 acre-feet (62-92 cubic\nhectometres), or enough water to supply irrigation in the valley for a\nmaximum of 2 years. The ground-water storage varies annually about 10\npercent and has not changed significantly. Ground water is discharged\nfrom Ashley Valley both by seepage back to Ashley Creek and by\nevapotranspiration .</p>\n<br>\n<p>Evapotranspiration of surface and ground water has increased by an estimate 20 percent above the 48,000 acre-feet (59 cubic hectometers) determined for pre-reservoir conditions. As a result, the water that flows from Ashley Valley has been degraded in chemical quality.</p>\n<br>\n<p>The water from Ashley Creek canyon is fresh . Mixing of snowmelt\nand base flow in Steinaker Reservoir yields a water of more uniform\nquality; but despite some concentration by evaporation from the\nreservoir, the outflow from the reservoir is fresh. Ground water in\nmost of the valley is fresh , but the water increases in dissolved-solids\nconcentration toward the south and east as a result of both\nevapotranspiration and solution of minerals from the valley fill and\nsoils .</p>","language":"English","publisher":"Utah Department of Natural Resources, Division of Water Rights","publisherLocation":"Salt Lake City, UT","collaboration":"Prepared by the United States Geological Survey in cooperation with the Utah Department of Natural Resources Division of Water Rights","usgsCitation":"Hood, J.W., 1977, Hydrologic evaluation of Ashley Valley, northern Uinta basin area, Utah: Technical Publication 54, Report: iv, 25 p.; 1 Plate: 25.51 x 26.76 inches.","productDescription":"Report: iv, 25 p.; 1 Plate: 25.51 x 26.76 inches","numberOfPages":"31","costCenters":[{"id":610,"text":"Utah Water Science Center","active":true,"usgs":true}],"links":[{"id":267700,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/70043723.jpg"},{"id":286044,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/unnumbered/70043723/plate-1.pdf","text":"Plate 1"},{"id":331880,"rank":4,"type":{"id":15,"text":"Index Page"},"url":"https://www.waterrights.utah.gov/cgi-bin/libview.exe?Modinfo=Viewpub&LIBNUM=20-5-350"},{"id":286045,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/unnumbered/70043723/report.pdf"}],"country":"United States","state":"Utah","otherGeospatial":"Ashley Valley","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -114.0,37.0 ], [ -114.0,42.0 ], [ -109.0,42.0 ], [ -109.0,37.0 ], [ -114.0,37.0 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"5124ad43e4b0b6328103b447","contributors":{"authors":[{"text":"Hood, James W.","contributorId":66115,"corporation":false,"usgs":true,"family":"Hood","given":"James","email":"","middleInitial":"W.","affiliations":[],"preferred":false,"id":474171,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":70043713,"text":"70043713 - 1977 - Reconnaissance of water quality in the Duchesne River basin and some adjacent drainage areas, Utah","interactions":[{"subject":{"id":20221,"text":"ofr76506 - 1976 - Reconnaissance of water quality in the Duchesne River Basin and some adjacent drainage areas, Utah","indexId":"ofr76506","publicationYear":"1976","noYear":false,"title":"Reconnaissance of water quality in the Duchesne River Basin and some adjacent drainage areas, Utah"},"predicate":"SUPERSEDED_BY","object":{"id":70043713,"text":"70043713 - 1977 - Reconnaissance of water quality in the Duchesne River basin and some adjacent drainage areas, Utah","indexId":"70043713","publicationYear":"1977","noYear":false,"title":"Reconnaissance of water quality in the Duchesne River basin and some adjacent drainage areas, Utah"},"id":1}],"lastModifiedDate":"2016-12-12T13:55:03","indexId":"70043713","displayToPublicDate":"2013-01-01T00:00:00","publicationYear":"1977","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":4,"text":"Other Government Series"},"seriesTitle":{"id":294,"text":"Technical Publication","active":false,"publicationSubtype":{"id":4}},"seriesNumber":"55","title":"Reconnaissance of water quality in the Duchesne River basin and some adjacent drainage areas, Utah","docAbstract":"A water-quality reconnaissance in the Duchesne River basin and some adjacent drainage areas, Utah, covered an area of about 4,400 square miles (11,400 square kilometres)--about 4,000 square miles (10,360 square kilometres) in the Duchesne River basin and the remainder in the drainage areas of Pariette Draw and Pelican Lake. Data were obtained by the U.S. Geological Survey one or more times at 108 sites during the period March 1973 to September 1974 and by the Geological Surveyor other Federal agencies at 49 other sites during earlier years.","language":"English","publisher":"Utah Department of Natural Resources","publisherLocation":"Salt Lake City, Utah","collaboration":"Prepared by the United States Geological Survey in cooperation with the Utah Department of Natural Resources Division of Water Rights","usgsCitation":"Mundorff, J.C., 1977, Reconnaissance of water quality in the Duchesne River basin and some adjacent drainage areas, Utah: Technical Publication 55, vi, 47 p.","productDescription":"vi, 47 p.","numberOfPages":"58","costCenters":[{"id":610,"text":"Utah Water Science Center","active":true,"usgs":true}],"links":[{"id":267694,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"},{"id":331946,"rank":3,"type":{"id":15,"text":"Index 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C.","contributorId":63374,"corporation":false,"usgs":true,"family":"Mundorff","given":"J.","email":"","middleInitial":"C.","affiliations":[],"preferred":false,"id":474152,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":70043185,"text":"70043185 - 1977 - Application of linear statistical models of earthquake magnitude versus fault length in estimating maximum expectable earthquakes","interactions":[{"subject":{"id":10170,"text":"ofr77549 - 1977 - Application of linear statistical models of earthquake magnitude versus fault length in estimating maximum expectable earthquakes","indexId":"ofr77549","publicationYear":"1977","noYear":false,"title":"Application of linear statistical models of earthquake magnitude versus fault length in estimating maximum expectable earthquakes"},"predicate":"SUPERSEDED_BY","object":{"id":70043185,"text":"70043185 - 1977 - Application of linear statistical models of earthquake magnitude versus fault length in estimating maximum expectable earthquakes","indexId":"70043185","publicationYear":"1977","noYear":false,"title":"Application of linear statistical models of earthquake magnitude versus fault length in estimating maximum expectable earthquakes"},"id":1}],"lastModifiedDate":"2020-09-11T18:11:48.744298","indexId":"70043185","displayToPublicDate":"2013-01-01T00:00:00","publicationYear":"1977","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1796,"text":"Geology","active":true,"publicationSubtype":{"id":10}},"title":"Application of linear statistical models of earthquake magnitude versus fault length in estimating maximum expectable earthquakes","docAbstract":"<p><span>Correlation or linear regression estimates of earthquake magnitude from data on historical magnitude and length of surface rupture should be based upon the correct regression. For example, the regression of magnitude on the logarithm of the length of surface rupture&nbsp;</span><i>L</i><span>&nbsp;can be used to estimate magnitude, but the regression of log&nbsp;</span><i>L</i><span>&nbsp;on magnitude cannot. Regression estimates are most probable values, and estimates of maximum values require consideration of one-sided confidence limits.</span></p>","language":"English","publisher":"Geological Society of America","publisherLocation":"Boulder,CO","doi":"10.1130/0091-7613(1977)5%3C464:AOLSMO%3E2.0.CO;2","usgsCitation":"Mark, R., 1977, Application of linear statistical models of earthquake magnitude versus fault length in estimating maximum expectable earthquakes: Geology, v. 5, no. 8, p. 464-466, https://doi.org/10.1130/0091-7613(1977)5%3C464:AOLSMO%3E2.0.CO;2.","productDescription":"3 p.","startPage":"464","endPage":"466","costCenters":[{"id":237,"text":"Earthquake Science Center","active":true,"usgs":true}],"links":[{"id":267101,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"5","issue":"8","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"5114daf7e4b0ca7af0743afc","contributors":{"authors":[{"text":"Mark, Robert K.","contributorId":30648,"corporation":false,"usgs":true,"family":"Mark","given":"Robert K.","affiliations":[],"preferred":false,"id":473123,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":70043278,"text":"70043278 - 1977 - Submarine faults and slides on the continental shelf, northern Gulf of Alaska","interactions":[{"subject":{"id":12910,"text":"ofr76294 - 1976 - Submarine faults and slides that disrupt surficial sedimentary units, northern Gulf of Alaska","indexId":"ofr76294","publicationYear":"1976","noYear":false,"title":"Submarine faults and slides that disrupt surficial sedimentary units, northern Gulf of Alaska"},"predicate":"SUPERSEDED_BY","object":{"id":70043278,"text":"70043278 - 1977 - Submarine faults and slides on the continental shelf, northern Gulf of Alaska","indexId":"70043278","publicationYear":"1977","noYear":false,"title":"Submarine faults and slides on the continental shelf, northern Gulf of Alaska"},"id":1}],"lastModifiedDate":"2013-02-09T18:53:59","indexId":"70043278","displayToPublicDate":"2013-01-01T00:00:00","publicationYear":"1977","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":2670,"text":"Marine Geotechnology","active":true,"publicationSubtype":{"id":10}},"title":"Submarine faults and slides on the continental shelf, northern Gulf of Alaska","docAbstract":"Submarine faults and slides or slumps of Quaternary age are potential environmental hazards on the outer continental shelf (OCS) of the northern Gulf of Alaska. Most faults that approach or reach the seafloor cut strata that may be equivalent in age to the upper Yakataga Formation (Pliocene‐Pleistocene). Along several faults, the seafloor is vertically offset from 5 to 20 m. A few faults appear to cut Holocene sediments, but none of these shows displacement at the seafloor. Submarine slides or slumps have been found in two places in the OCS region: (1) seaward of the Malaspina Glacier and Icy Bay, an area of 1200 km<sup>2</sup> with a slope of less than 0.5°, and (2) across the entire span of the Copper river prodelta, an area of 1730 km<sup>2</sup>, having a slope of about 0.5°. Seismic profiles across these areas show disrupted reflectors and irregular topography commonly associated with submarine slides or slumps. Potential slide or slump areas have been delineated in areas of thick sediment accumulation and relatively steep slopes. These areas include (1) Kayak Trough, (2) parts of Hinchinbrook Entrance and Sea Valley, (3) parts of the outer shelf and upper slope between Kayak Island and Yakutat Bay, and (4) Bering Trough.","largerWorkType":{"id":2,"text":"Article"},"largerWorkTitle":"Marine Geotechnology","largerWorkSubtype":{"id":10,"text":"Journal Article"},"language":"English","publisher":"Taylor & Francis","publisherLocation":"Philadelphia, PA","doi":"10.1080/10641197709379784","usgsCitation":"Carlson, P.R., and Molnia, B.F., 1977, Submarine faults and slides on the continental shelf, northern Gulf of Alaska: Marine Geotechnology, v. 2, no. 1-4, p. 275-290, https://doi.org/10.1080/10641197709379784.","productDescription":"16 p.","startPage":"275","endPage":"290","costCenters":[],"links":[{"id":267162,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"},{"id":267161,"type":{"id":10,"text":"Digital Object Identifier"},"url":"https://dx.doi.org/10.1080/10641197709379784"}],"country":"United States","state":"Alaska","otherGeospatial":"Gulf Of Alaska","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ 172.5,51.2 ], [ 172.5,71.4 ], [ -130.0,71.4 ], [ -130.0,51.2 ], [ 172.5,51.2 ] ] ] } } ] }","volume":"2","issue":"1-4","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"51177e06e4b0893acf3fffd4","contributors":{"authors":[{"text":"Carlson, Paul R.","contributorId":81469,"corporation":false,"usgs":true,"family":"Carlson","given":"Paul","email":"","middleInitial":"R.","affiliations":[],"preferred":false,"id":473274,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Molnia, Bruce F. bmolnia@usgs.gov","contributorId":4002,"corporation":false,"usgs":true,"family":"Molnia","given":"Bruce","email":"bmolnia@usgs.gov","middleInitial":"F.","affiliations":[{"id":410,"text":"National Center","active":false,"usgs":true}],"preferred":false,"id":473273,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":70043281,"text":"70043281 - 1977 - Hydrologic reconnaissance of the Tule Valley drainage basin, Juab and Millard Counties, Utah","interactions":[{"subject":{"id":11326,"text":"ofr76709 - 1976 - Hydrologic reconnaissance of the Tule Valley drainage basin, Juab and Millard counties, Utah","indexId":"ofr76709","publicationYear":"1976","noYear":false,"title":"Hydrologic reconnaissance of the Tule Valley drainage basin, Juab and Millard counties, Utah"},"predicate":"SUPERSEDED_BY","object":{"id":70043281,"text":"70043281 - 1977 - Hydrologic reconnaissance of the Tule Valley drainage basin, Juab and Millard Counties, Utah","indexId":"70043281","publicationYear":"1977","noYear":false,"title":"Hydrologic reconnaissance of the Tule Valley drainage basin, Juab and Millard Counties, Utah"},"id":1}],"lastModifiedDate":"2016-12-12T14:00:31","indexId":"70043281","displayToPublicDate":"2013-01-01T00:00:00","publicationYear":"1977","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":4,"text":"Other Government Series"},"seriesTitle":{"id":294,"text":"Technical Publication","active":false,"publicationSubtype":{"id":4}},"seriesNumber":"56","title":"Hydrologic reconnaissance of the Tule Valley drainage basin, Juab and Millard Counties, Utah","docAbstract":"The Tule Valley drainage basin is an area of about 940 square miles in Juab and Millard Counties in west-central Utah. Precipitation in the basin averages about 8 inches annually. There is no surface outflow and all streams are ephemeral. Annual runoff averages about 0.09 inch. Because there is no sustained runoff, and flow is local and infrequent, reservoirs do not provide dependable water supplies. Ground-water recharge from precipitation in the basin is estimated to average 7,600 acre-feet annually. Discharge, principally by evapotranspiration, averages about 40,000 acre-feet annually. Subsurface inflow from adjacent areas is estimated to average about 32,000 acre-feet annually.","language":"English","publisher":"Utah Department of Natural Resources, Division of Water Rights","publisherLocation":"Salt Lake City, UT","collaboration":"Prepared by the U.S. Geological Survey in cooperation with the Utah Department of Natural Resources, Division of Water Rights","usgsCitation":"Stephens, J., 1977, Hydrologic reconnaissance of the Tule Valley drainage basin, Juab and Millard Counties, Utah: Technical Publication 56, iv., 37 p.","productDescription":"iv., 37 p.","numberOfPages":"43","costCenters":[{"id":610,"text":"Utah Water Science Center","active":true,"usgs":true}],"links":[{"id":267167,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"},{"id":331950,"rank":3,"type":{"id":11,"text":"Document"},"url":"https://waterrights.utah.gov/docSys/v920/w920/w920009i.pdf"},{"id":331949,"rank":2,"type":{"id":15,"text":"Index Page"},"url":"https://www.waterrights.utah.gov/cgi-bin/libview.exe?Modinfo=Viewpub&LIBNUM=20-5-390"}],"country":"United States","state":"Utah","county":"Juab County, Millard County","otherGeospatial":"Tule Valley Basin","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -113.78265380859374,\n              38.805470223177466\n            ],\n            [\n              -113.78265380859374,\n              39.69239407904182\n            ],\n            [\n              -113.32122802734375,\n              39.69239407904182\n            ],\n            [\n              -113.32122802734375,\n              38.805470223177466\n            ],\n            [\n              -113.78265380859374,\n              38.805470223177466\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"51177e02e4b0893acf3fffbf","contributors":{"authors":[{"text":"Stephens, J.C.","contributorId":74010,"corporation":false,"usgs":true,"family":"Stephens","given":"J.C.","email":"","affiliations":[],"preferred":false,"id":473279,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":70046155,"text":"70046155 - 1977 - High-resolution gamma-ray spectrometry in uranium exploration","interactions":[{"subject":{"id":20212,"text":"ofr76399 - 1976 - High-resolution gamma-ray spectrometry in uranium exploration","indexId":"ofr76399","publicationYear":"1976","noYear":false,"title":"High-resolution gamma-ray spectrometry in uranium exploration"},"predicate":"SUPERSEDED_BY","object":{"id":70046155,"text":"70046155 - 1977 - High-resolution gamma-ray spectrometry in uranium exploration","indexId":"70046155","publicationYear":"1977","noYear":false,"title":"High-resolution gamma-ray spectrometry in uranium exploration"},"id":1}],"lastModifiedDate":"2019-11-18T13:49:00","indexId":"70046155","displayToPublicDate":"2013-01-01T00:00:00","publicationYear":"1977","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":2446,"text":"Journal of Research of the U.S. Geological Survey","active":true,"publicationSubtype":{"id":10}},"title":"High-resolution gamma-ray spectrometry in uranium exploration","docAbstract":"Sedimentary-type uranium deposits accumulate at favorable sites along a migration path which may be kilometers in length. Their source is a large volume of rock from which the uranium has been leached. The geochemical mobilities and half lives of uranium and its daughter products vary widely so that they are transported from the source rocks, at different rates, along the migration path to their ultimate site. The radioactive disequilibrium resulting from this process has been well documented in the immediate vicinity of ore deposits, and disequilibrium is commonly recorded on gamma-ray logs up the hydraulic gradient from uranium ore. Little is known about the state of secular equilibrium in the leached host rocks, which often represent the only part of the migration path that is at or near the surface and is thus most accessible to the exploration geophysicist. High-resolution gamma-ray spectrometry provides a means of investigating the disequilibrium associated with uranium leaching and migration. Direct measurement of uranium can be made by this method, and the equivalent weight percents can be determined for six of the seven daughter-product decay groups that characterize the state of radioactive equilibrium. The technique has been used quantitatively in laboratory studies, where the results compare favorably with radiochemical analyses; field experiments suggest that semi-quantitative data may be obtained at the outcrop.","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Reston, VA","usgsCitation":"Moxham, R.M., and Tanner, A.B., 1977, High-resolution gamma-ray spectrometry in uranium exploration: Journal of Research of the U.S. Geological Survey, v. 5, no. 6, p. 783-785.","productDescription":"13 p.","startPage":"783","endPage":"785","costCenters":[],"links":[{"id":272955,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"},{"id":272954,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/journal/1977/vol5issue6/report.pdf","text":"Report","size":"26.7 MB","linkFileType":{"id":1,"text":"pdf"},"description":"Report"}],"volume":"5","issue":"6","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"51a72369e4b09db86f875cf9","contributors":{"authors":[{"text":"Moxham, Robert M.","contributorId":56210,"corporation":false,"usgs":true,"family":"Moxham","given":"Robert","email":"","middleInitial":"M.","affiliations":[],"preferred":false,"id":479064,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Tanner, Allan B.","contributorId":11611,"corporation":false,"usgs":true,"family":"Tanner","given":"Allan","email":"","middleInitial":"B.","affiliations":[],"preferred":false,"id":479063,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":70046170,"text":"70046170 - 1977 - Combined use of digital aquifer models and field base-flow data to identify recharge-leakage areas of artesian aquifers","interactions":[{"subject":{"id":49297,"text":"ofr76795 - 1976 - Combined use of digital aquifer models and field base-flow data to identify recharge leakage areas of artesian aquifers","indexId":"ofr76795","publicationYear":"1976","noYear":false,"title":"Combined use of digital aquifer models and field base-flow data to identify recharge leakage areas of artesian aquifers"},"predicate":"SUPERSEDED_BY","object":{"id":70046170,"text":"70046170 - 1977 - Combined use of digital aquifer models and field base-flow data to identify recharge-leakage areas of artesian aquifers","indexId":"70046170","publicationYear":"1977","noYear":false,"title":"Combined use of digital aquifer models and field base-flow data to identify recharge-leakage areas of artesian aquifers"},"id":1}],"lastModifiedDate":"2015-08-21T16:41:27","indexId":"70046170","displayToPublicDate":"2013-01-01T00:00:00","publicationYear":"1977","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":2446,"text":"Journal of Research of the U.S. Geological Survey","active":true,"publicationSubtype":{"id":10}},"title":"Combined use of digital aquifer models and field base-flow data to identify recharge-leakage areas of artesian aquifers","docAbstract":"<p>As a result of continuous pumping since the 1890's, a regional cone of depression encompassing 363 km<sup>2</sup> has developed within the artesian Miocene Cheswold aquifer at Dover, Del. The aquifer is not being recharged significantly by leakage near the center of the cone, nor is major recharge induced in the updip subcrop area. The source of pumped water is apparently an area of about 65 km<sup>2</sup> northwest of Dover, where vertical leakage is substantial. This area was delineated by use of a digital aquifer model and streamflow data. A model of the unconfined aquifer was used to compute the unconfined aquifer's natural discharge to streams, assuming no leakage to underlying artesian aquifers. The area of substantial leakage to the underlying Cheswold was delineated as being coincident with that area where model-computed values of stream discharge were substantially larger than actual values of stream discharge determined in the field.</p>","largerWorkType":{"id":2,"text":"Article"},"largerWorkTitle":"Journal of Research of the U.S. Geological Survey","largerWorkSubtype":{"id":10,"text":"Journal Article"},"language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Reston, VA","usgsCitation":"Johnston, R.H., and Leahy, P.P., 1977, Combined use of digital aquifer models and field base-flow data to identify recharge-leakage areas of artesian aquifers: Journal of Research of the U.S. Geological Survey, v. 5, no. 4, p. 491-496.","productDescription":"6 p.","startPage":"491","endPage":"496","numberOfPages":"6","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[],"links":[{"id":272963,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"},{"id":272964,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/journal/1977/vol5issue4/report.pdf"}],"country":"United States","state":"Delaware","city":"Dover","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -75.85,\n              38.89\n            ],\n            [\n              -75.85,\n              39.1\n            ],\n            [\n              -75.645,\n              39.1\n            ],\n            [\n              -75.64,\n              38.89\n            ],\n            [\n              -75.85,\n              38.89\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","volume":"5","issue":"4","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"51a72363e4b09db86f875cba","contributors":{"authors":[{"text":"Johnston, Richard H.","contributorId":95860,"corporation":false,"usgs":true,"family":"Johnston","given":"Richard","email":"","middleInitial":"H.","affiliations":[],"preferred":false,"id":479084,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Leahy, P. Patrick","contributorId":80648,"corporation":false,"usgs":true,"family":"Leahy","given":"P.","email":"","middleInitial":"Patrick","affiliations":[],"preferred":false,"id":479083,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":70046178,"text":"70046178 - 1977 - Lisburne Group (Mississippian and Pennsylvanian), potential major hydrocarbon objective of Arctic Slope, Alaska","interactions":[{"subject":{"id":7895,"text":"ofr76786 - 1976 - The Lisburne Group: A potential major hydrocarbon objective of the Arctic Slope, Alaska","indexId":"ofr76786","publicationYear":"1976","noYear":false,"title":"The Lisburne Group: A potential major hydrocarbon objective of the Arctic Slope, Alaska"},"predicate":"SUPERSEDED_BY","object":{"id":70046178,"text":"70046178 - 1977 - Lisburne Group (Mississippian and Pennsylvanian), potential major hydrocarbon objective of Arctic Slope, Alaska","indexId":"70046178","publicationYear":"1977","noYear":false,"title":"Lisburne Group (Mississippian and Pennsylvanian), potential major hydrocarbon objective of Arctic Slope, Alaska"},"id":1}],"lastModifiedDate":"2023-01-25T16:20:48.469383","indexId":"70046178","displayToPublicDate":"2013-01-01T00:00:00","publicationYear":"1977","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":605,"text":"AAPG Bulletin","printIssn":"0149-1423","active":true,"publicationSubtype":{"id":10}},"title":"Lisburne Group (Mississippian and Pennsylvanian), potential major hydrocarbon objective of Arctic Slope, Alaska","docAbstract":"<p>The Lisburne Group, a thick carbonate-rock unit of Mississippian and Pennsylvanian age, is one of the most widespread potential reservoir-rock units in northern Alaska. A comprehensive review of the Lisburne in the subsurface of the eastern Arctic Slope indicates attractive reservoir characteristics in a favorable source and migration setting where numerous trapping mechanisms appear to be available. Evaluation of this group as a potential exploration objective is particularly timely because of impending offshore sales in the Beaufort Sea and current exploration programs under way in the Prudhoe Bay area and the Naval Petroleum Reserve.</p><p>Dolomite and sandstone have been identified as reservoir rocks. Oolitic grainstone is a common rock type, but observations indicate little reservoir potential owing to complete void filling by calcite cement. The most important reservoir rock as judged by thickness, areal extent, and predictability is microsucrosic (10 to 30μ) dolomite of intertidal to supratidal origin. It is present throughout the Lisburne and is most abundant near the middle of the sequence. Northward it decreases in thickness from 1,000 ft (300 m) to less than 100 ft (30 m). Porosity of the dolomite as determined in selected wells averages between 10 and 15% and attains a maximum of slightly more than 25%. Net thickness of reservoir rocks (i.e., rocks with greater than 5% porosity) ranges in these wells from 140 to 390 ft (40 to 120 m). Oil shows are common, and drill-stem tests have yielded as much as 1,600 bbl/day of oil and 22 MMcf/day of gas in the Lisburne pool of the Prudhoe Bay field and as much as 2,057 bbl/day of salt water outside the field area. The occurrence of dolomite over such a large area makes its presence in the offshore Beaufort Sea and adjacent Naval Petroleum Reserve 4 fairly certain. The presence of sandstone as thick as 140 ft (40 m) in the middle and upper part of the Lisburne in two coastal wells suggests that larger areas of sandstone may be found on the north in offshore areas. Shows of oil and gas and a saltwater flow of 1,470 bbl/day have been recorded from this sandstone facies.</p><p>Shales of Permian and Cretaceous ages unconformably overlie the Lisburne, providing adequate sealing beds above potential reservoirs. Impermeable limestone (completely cemented grainstone) and thin beds of shale may serve as seals within the Lisburne, but the possibility of fractures in these units may negate their sealing capability.</p><p>The most favorable source rock for Lisburne hydrocarbons appears to be Cretaceous shale that unconformably overlies the Lisburne east of Prudhoe Bay. This shale is reported to be a rich source rock and is the most likely source for the entire Prudhoe Bay field. A source within the Lisburne or within the underlying Kayak Shale is postulated for oil shows in the southernmost Lisburne wells. This postulated source may be in a more basinal facies of the Lisburne and may be similar to dark shale in the upper Lisburne in thrust slices to dark shale in the upper Lisburne in thrust slices in the Brooks Range. Coal in the underlying Endicott Group is a possible source for dry gas. At present, much of this coal probably is in a gas-generating regime downdip from the Prudhoe Bay field.</p><p>Stratigraphic traps involving the Lisburne Group may have resulted from widespread Permian and Cretaceous unconformities. Structural traps related to normal faulting may be present along the trend of the Barrow arch, and faulted anticlines are numerous in the foothills of the Brooks Range. Combination traps are possible along the trend of the Barrow arch.</p>","language":"English","publisher":"American Association of Petroleum Geologists","doi":"10.1306/C1EA45BD-16C9-11D7-8645000102C1865D","usgsCitation":"Bird, K.J., and Jordan, C.F., 1977, Lisburne Group (Mississippian and Pennsylvanian), potential major hydrocarbon objective of Arctic Slope, Alaska: AAPG Bulletin, v. 61, no. 9, p. 1493-1512, https://doi.org/10.1306/C1EA45BD-16C9-11D7-8645000102C1865D.","productDescription":"20 p.","startPage":"1493","endPage":"1512","costCenters":[{"id":255,"text":"Energy Resources Program","active":true,"usgs":true}],"links":[{"id":272982,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United States","state":"Alaska","otherGeospatial":"Arctic Slope","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"coordinates\": [\n          [\n            [\n              -141,\n              72.4734904387575\n            ],\n            [\n              -167.27168160592308,\n              72.4734904387575\n            ],\n            [\n              -167.27168160592308,\n              66.28413846905073\n            ],\n            [\n              -141,\n              66.28413846905073\n            ],\n            [\n              -141,\n              72.4734904387575\n            ]\n          ]\n        ],\n        \"type\": \"Polygon\"\n      }\n    }\n  ]\n}","volume":"61","issue":"9","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"51a7236ae4b09db86f875d06","contributors":{"authors":[{"text":"Bird, Kenneth J. kbird@usgs.gov","contributorId":1015,"corporation":false,"usgs":true,"family":"Bird","given":"Kenneth","email":"kbird@usgs.gov","middleInitial":"J.","affiliations":[{"id":255,"text":"Energy Resources Program","active":true,"usgs":true}],"preferred":true,"id":479097,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Jordan, Clifton F.","contributorId":95203,"corporation":false,"usgs":true,"family":"Jordan","given":"Clifton","email":"","middleInitial":"F.","affiliations":[],"preferred":false,"id":479098,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
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