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Water resources data for the 1980 water year for Arizona consist of records of stage, discharge, and water quality of streams; stage, contents, and water quality of lakes and reservoirs; water levels of observation wells; and quality of ground water. This report contains discharge records for 240 gaging stations, annual peaks for 61 crest-stage partial-record stations, and discharge measurements at 14 miscellaneous sites; contents only records for 9 lakes and reservoirs; stage and contents for 1 lake; elevation and discharge for 1 streamflow station; elevation only for 1 stream-flow station; gage height only for I head over a dam; 16 supplementary records, included with gaging-station records, consisting of month end or monthly stage, contents, and evaporation of lakes and reservoirs, diversions, and return flows; water-quality records for 62 continuous-record stations and 9 miscellaneous sites; water levels for 93 observation wells; and water-quality data for water from 741 wells. The data represent that part of the National Water Data System operated by the U.S. Geological Survey and cooperating Federal and State Agencies in Arizona.

","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/wdrAZ801","collaboration":"Prepared in cooperation with the State of Arizona and with other agencies","usgsCitation":"Water Resources Division, U.S. Geological Survey, 1982, Water resources data for Arizona, water year 1980: U.S. Geological Survey Water Data Report AZ-80-1, xiv, 568 p., https://doi.org/10.3133/wdrAZ801.","productDescription":"xiv, 568 p.","costCenters":[],"links":[{"id":497329,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wdr/1980/az-80-1/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":184413,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wdr/1980/az-80-1/report-thumb.jpg"}],"country":"United States","state":"Arizona","geographicExtents":"{\"type\":\"FeatureCollection\",\"features\":[{\"type\":\"Feature\",\"id\":\"4\",\"properties\":{\"name\":\"Arizona\",\"nation\":\"USA 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S.","contributorId":102884,"corporation":false,"usgs":true,"family":"Grim","given":"M.","email":"","middleInitial":"S.","affiliations":[],"preferred":false,"id":159344,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Behrendt, John C. jbehrendt@usgs.gov","contributorId":25945,"corporation":false,"usgs":true,"family":"Behrendt","given":"John","email":"jbehrendt@usgs.gov","middleInitial":"C.","affiliations":[{"id":218,"text":"Denver Federal Center","active":false,"usgs":true},{"id":213,"text":"Crustal Imaging and Characterization Team","active":false,"usgs":true}],"preferred":false,"id":159342,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Klitgord, Kim D.","contributorId":82307,"corporation":false,"usgs":true,"family":"Klitgord","given":"Kim","email":"","middleInitial":"D.","affiliations":[{"id":678,"text":"Woods Hole Coastal and Marine Science Center","active":true,"usgs":true}],"preferred":false,"id":159343,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}} ,{"id":9420,"text":"ofr82857 - 1982 - Supplement to the New Mexico three-dimensional model","interactions":[],"lastModifiedDate":"2012-02-02T00:06:15","indexId":"ofr82857","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1982","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":"82-857","title":"Supplement to the New Mexico three-dimensional model","docAbstract":"The computer program documented in Open-File Report 80-421 has continued to evolve in response to needs. By January 1981, changes included the following: (1) treatment of head-dependent boundaries and specified-flow boundaries and (2) code which executes on the CRAY-1 computer. This report provides instructions for compiling and executing the computer program on the CRAY-1 at Kirtland Air Force Base. (USGS)","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/ofr82857","usgsCitation":"Hearne, G.A., 1982, Supplement to the New Mexico three-dimensional model: U.S. Geological Survey Open-File Report 82-857, v, 95 p. :ill. ;28 cm., https://doi.org/10.3133/ofr82857.","productDescription":"v, 95 p. :ill. ;28 cm.","costCenters":[],"links":[{"id":141822,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1982/0857/report-thumb.jpg"},{"id":37131,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1982/0857/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4afde4b07f02db6970d6","contributors":{"authors":[{"text":"Hearne, Glenn A.","contributorId":50882,"corporation":false,"usgs":true,"family":"Hearne","given":"Glenn","email":"","middleInitial":"A.","affiliations":[],"preferred":false,"id":159656,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":9518,"text":"ofr821096 - 1982 - Progress report on the potash deposits of the Khorat Plateau, Thailand","interactions":[],"lastModifiedDate":"2012-02-02T00:06:11","indexId":"ofr821096","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1982","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":"82-1096","title":"Progress report on the potash deposits of the Khorat Plateau, Thailand","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/ofr821096","usgsCitation":"Hite, R.J., 1982, Progress report on the potash deposits of the Khorat Plateau, Thailand: U.S. Geological Survey Open-File Report 82-1096, 75 p. ill., map ;28 cm., https://doi.org/10.3133/ofr821096.","productDescription":"75 p. ill., map ;28 cm.","costCenters":[],"links":[{"id":141035,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1982/1096/report-thumb.jpg"},{"id":37236,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1982/1096/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a9be4b07f02db65dd92","contributors":{"authors":[{"text":"Hite, R. J.","contributorId":82701,"corporation":false,"usgs":true,"family":"Hite","given":"R.","email":"","middleInitial":"J.","affiliations":[],"preferred":false,"id":159823,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":60186,"text":"mf1450 - 1982 - Geologic map of the Broke Off Mountain Quadrangle, Rio Arriba County, New Mexico","interactions":[],"lastModifiedDate":"2012-02-10T00:10:34","indexId":"mf1450","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1982","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":"1450","title":"Geologic map of the Broke Off Mountain Quadrangle, Rio Arriba County, New Mexico","language":"ENGLISH","doi":"10.3133/mf1450","usgsCitation":"Manley, K., 1982, Geologic map of the Broke Off Mountain Quadrangle, Rio Arriba County, New Mexico: U.S. Geological Survey Miscellaneous Field Studies Map 1450, 1 map ; 58 x 47 cm., https://doi.org/10.3133/mf1450.","productDescription":"1 map ; 58 x 47 cm.","costCenters":[],"links":[{"id":105876,"rank":700,"type":{"id":15,"text":"Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_7201.htm","linkFileType":{"id":5,"text":"html"},"description":"7201"},{"id":180298,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"}],"scale":"0","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -106.25,36.75 ], [ -106.25,36.8675 ], [ -106.11749999999999,36.8675 ], [ -106.11749999999999,36.75 ], [ -106.25,36.75 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b0be4b07f02db69d7bf","contributors":{"authors":[{"text":"Manley, Kim","contributorId":27844,"corporation":false,"usgs":true,"family":"Manley","given":"Kim","email":"","affiliations":[],"preferred":false,"id":263283,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":9406,"text":"ofr82316 - 1982 - 1981 annual index of current earthquake literature","interactions":[],"lastModifiedDate":"2012-02-02T00:06:14","indexId":"ofr82316","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1982","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":"82-316","title":"1981 annual index of current earthquake literature","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/ofr82316","usgsCitation":"Hayashida, B., Kauffmann, M.L., and Lee, W., 1982, 1981 annual index of current earthquake literature: U.S. Geological Survey Open-File Report 82-316, 649 p. ;28 cm., https://doi.org/10.3133/ofr82316.","productDescription":"649 p. ;28 cm.","costCenters":[],"links":[{"id":121937,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1982/0316/report-thumb.jpg"},{"id":37118,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1982/0316/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"53cd4913e4b0b290850eedc9","contributors":{"authors":[{"text":"Hayashida, B.S.","contributorId":42212,"corporation":false,"usgs":true,"family":"Hayashida","given":"B.S.","email":"","affiliations":[],"preferred":false,"id":159631,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Kauffmann, Mari L.","contributorId":42594,"corporation":false,"usgs":true,"family":"Kauffmann","given":"Mari","email":"","middleInitial":"L.","affiliations":[],"preferred":false,"id":159632,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Lee, William Hung Kan","contributorId":83502,"corporation":false,"usgs":true,"family":"Lee","given":"William Hung Kan","affiliations":[],"preferred":false,"id":159633,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}} ,{"id":9511,"text":"ofr82263 - 1982 - Investigation of trends in flooding in the Tug Fork basin of Kentucky, Virginia, and West Virginia","interactions":[{"subject":{"id":9511,"text":"ofr82263 - 1982 - Investigation of trends in flooding in the Tug Fork basin of Kentucky, Virginia, and West Virginia","indexId":"ofr82263","publicationYear":"1982","noYear":false,"title":"Investigation of trends in flooding in the Tug Fork basin of Kentucky, Virginia, and West Virginia"},"predicate":"SUPERSEDED_BY","object":{"id":1890,"text":"wsp2203 - 1982 - Investigation of trends in flooding in the Tug Fork basin of Kentucky, Virginia, and West Virginia","indexId":"wsp2203","publicationYear":"1982","noYear":false,"title":"Investigation of trends in flooding in the Tug Fork basin of Kentucky, Virginia, and West Virginia"},"id":1}],"supersededBy":{"id":1890,"text":"wsp2203 - 1982 - Investigation of trends in flooding in the Tug Fork basin of Kentucky, Virginia, and West Virginia","indexId":"wsp2203","publicationYear":"1982","noYear":false,"title":"Investigation of trends in flooding in the Tug Fork basin of Kentucky, Virginia, and West Virginia"},"lastModifiedDate":"2022-11-16T19:31:16.442225","indexId":"ofr82263","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1982","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":"82-263","title":"Investigation of trends in flooding in the Tug Fork basin of Kentucky, Virginia, and West Virginia","docAbstract":"

Statistical analysis indicates that the average size of annual flood peaks of the Tug Fork (West Virginia and Kentucky) has been increasing. However, additional statistical analysis does not indicate that flood levels exceeded typically once or twice a year in the period 1947-1979 are any more likely to be exceeded now than in 1947. Possible trends in stream-channel size are also investigated at three locations. No discernable trends in channel size are noted. Further statistical analysis of the trend in the size of annual flood peaks shows that much of the annual variation is related to nearby rainfall and to the \"natural\" hydrologic response in a relatively undisturbed sub-basin. However, some statistical indication of trend persists after accounting for these natural factors, though the indication is of borderline statistical significance. This suggests the need for further study in the basin that may relate flood magnitudes to both rainfall and to land use.

","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr82263","collaboration":"Prepared in cooperation with the Office of Surface Mining Reclamation and Enforcement and the U.S. Bureau of Mines","usgsCitation":"Hirsch, R., Scott, A.G., and Wyant, T., 1982, Investigation of trends in flooding in the Tug Fork basin of Kentucky, Virginia, and West Virginia: U.S. Geological Survey Open-File Report 82-263, vii, 83 p., https://doi.org/10.3133/ofr82263.","productDescription":"vii, 83 p.","costCenters":[],"links":[{"id":409391,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1982/0263/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":140999,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1982/0263/report-thumb.jpg"}],"country":"United States","state":"Kentucky, Virginia, West Virginia","otherGeospatial":"Tug Fork basin","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"type\": \"Polygon\",\n \"coordinates\": [\n [\n [\n -83.69384765625,\n 36.60670888641815\n ],\n [\n -83.69384765625,\n 38.96795115401593\n ],\n [\n -80.70556640625,\n 38.96795115401593\n ],\n [\n -80.70556640625,\n 36.60670888641815\n ],\n [\n -83.69384765625,\n 36.60670888641815\n ]\n ]\n ]\n }\n }\n ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e47a5e4b07f02db4979f9","contributors":{"authors":[{"text":"Hirsch, Robert 0000-0002-4534-075X","orcid":"https://orcid.org/0000-0002-4534-075X","contributorId":257741,"corporation":false,"usgs":false,"family":"Hirsch","given":"Robert","affiliations":[{"id":7065,"text":"USGS emeritus","active":true,"usgs":false}],"preferred":false,"id":159814,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Scott, Arthur G.","contributorId":81885,"corporation":false,"usgs":true,"family":"Scott","given":"Arthur","email":"","middleInitial":"G.","affiliations":[],"preferred":false,"id":159813,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Wyant, Timothy","contributorId":26672,"corporation":false,"usgs":true,"family":"Wyant","given":"Timothy","email":"","affiliations":[],"preferred":false,"id":159812,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}} ,{"id":9432,"text":"ofr82358 - 1982 - Hydrologic investigations and data-collection network in strippable coal-resource areas in northwestern New Mexico","interactions":[],"lastModifiedDate":"2012-02-02T00:06:22","indexId":"ofr82358","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1982","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":"82-358","title":"Hydrologic investigations and data-collection network in strippable coal-resource areas in northwestern New Mexico","docAbstract":"This report presents hydrologic investigations and data collections conducted by the U.S. Geological Survey in the strippable coal areas of northwestern New Mexico. Streamflow, ground-water, and quality-of-water data were collected to provide information about baseline or prevailing hydrologic conditions. A network of hydrologic data-collection sites in the strippable coal areas of the Fruitland Formation was designed to meet the need of detailed investigations, including site-specific studies, and to provide hydrologic data in support of the expanding mining activity. The network consists of 34 continuous-record streamflow-gaging stations (32 included water-quality sampling), 20 miscellaneous water quality of streamflow stations, 12 annual maximum discharge stations, 27 observation wells completed in strata associated with the strippable coal seams, and 24 observation wells completed in channel alluvium downstream from strippable coal areas. (USGS)","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/ofr82358","usgsCitation":"Hejl, H., 1982, Hydrologic investigations and data-collection network in strippable coal-resource areas in northwestern New Mexico: U.S. Geological Survey Open-File Report 82-358, 36 p. :maps ;28 cm., https://doi.org/10.3133/ofr82358.","productDescription":"36 p. :maps ;28 cm.","costCenters":[],"links":[{"id":143431,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1982/0358/report-thumb.jpg"},{"id":37137,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1982/0358/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a1ae4b07f02db606948","contributors":{"authors":[{"text":"Hejl, H.R.","contributorId":92259,"corporation":false,"usgs":true,"family":"Hejl","given":"H.R.","email":"","affiliations":[],"preferred":false,"id":159674,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":8850,"text":"ofr82597 - 1982 - Phase 3 geophysical studies in the Wadi Bidah District, Kingdom of Saudi Arabia","interactions":[],"lastModifiedDate":"2012-02-02T00:06:13","indexId":"ofr82597","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1982","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":"82-597","title":"Phase 3 geophysical studies in the Wadi Bidah District, Kingdom of Saudi Arabia","docAbstract":"Detailed geophysical measurements have been made in the Rabathan area, Wadi Bidah district, Kingdom of Saudi Arabia, at the site of diamond drill holes RAB-1, -2, and -3; these measurements suggest that the causative source for the anomalous EM (electromagnetic) and SP (self-potential) responses is probably highly conductive zones of Precambrian siliceous-carbonaceous rocks. Although many of the zones are no more than a few meters wide, they commonly contain 50 to 80 percent carbonaceous material and locally abundant pyrite. In places, several thin layers of highly concentrated carbonaceous material interlayered with chert form a multiple conductive zone that is seen in the geophysical data as complex anomaly patterns. In the geologic environment of Wadi Bidah, massive sulfide-bearing zones cannot be distinguished from siliceous-carbonaceous zones on the basis of the EM-SP responses. In North America in similar environments, complex resistivity methods used in experimental research have successfully discriminated between sulfide and carbonaceous conductors. Tests of such methods in the Wadi Bidah district are recommended. \r\n\r\nGeologic, geochemical, and geophysical data at the Jabal Mohr prospect suggest the possibility of mineralized rocks at depth over a possible strike length of 400 m.","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/ofr82597","usgsCitation":"Flanigan, V.J., Sadek, H., and Smith, C.W., 1982, Phase 3 geophysical studies in the Wadi Bidah District, Kingdom of Saudi Arabia: U.S. Geological Survey Open-File Report 82-597, ii, 47 p., ill., maps ;28 cm., https://doi.org/10.3133/ofr82597.","productDescription":"ii, 47 p., ill., maps ;28 cm.","costCenters":[],"links":[{"id":142175,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1982/0597/report-thumb.jpg"},{"id":36429,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1982/0597/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4adce4b07f02db686875","contributors":{"authors":[{"text":"Flanigan, V. J.","contributorId":81097,"corporation":false,"usgs":true,"family":"Flanigan","given":"V.","email":"","middleInitial":"J.","affiliations":[],"preferred":false,"id":158434,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Sadek, Hamdy","contributorId":97491,"corporation":false,"usgs":true,"family":"Sadek","given":"Hamdy","affiliations":[],"preferred":false,"id":158435,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Smith, C. W.","contributorId":57457,"corporation":false,"usgs":true,"family":"Smith","given":"C.","email":"","middleInitial":"W.","affiliations":[],"preferred":false,"id":158433,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}} ,{"id":9508,"text":"ofr82733 - 1982 - A field study of large-scale oscillation ripples in a very coarse-grained, high-energy marine environment","interactions":[],"lastModifiedDate":"2012-02-02T00:06:11","indexId":"ofr82733","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1982","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":"82-733","title":"A field study of large-scale oscillation ripples in a very coarse-grained, high-energy marine environment","docAbstract":"Monastery Beach, Carmel, California is a pocket beach that sits within 200 m of the head of Carmel Submarine Canyon. Coarse to very coarse sand covers both the beach and adjacent shelf; in the latter area incoming waves have shaped the sand into large oscillation ripples. The accessibility of this area and a variable wave climate produce a unique opportunity to study large-scale coarse-grained ripples in a high-energy environment. These ripples, which only occur in very coarse sand, form under the intense, wave-generated currents that exist during storm conditions. Once formed, these ripples do not significantly change under lower energy waves. On three separate occasions scuba divers measured ripples and collected sand samples from ripple crests near fixed reference stakes along three transects. Ripple wavelength and grain size decreased with an increase in water depth. Sediment sorting was best closest to the surf zone and poorest at the rim of Carmel Canyon. Cobbles and gravel observed in ripple troughs represent lag deposits. \r\n\r\nCarmel Canyon refracts waves approaching Monastery Beach such that wave energy is focused towards the northern and southern portions of the beach, leaving the central part of the beach lower in energy. This energy distribution causes spatial variations in the ripples and grain sizes with the shortest wavelengths and smallest grain sizes being in the central part of the shelf.","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/ofr82733","usgsCitation":"Hirschaut, D., and Dingler, J., 1982, A field study of large-scale oscillation ripples in a very coarse-grained, high-energy marine environment: U.S. Geological Survey Open-File Report 82-733, 35 p., ill., maps ;28 cm., https://doi.org/10.3133/ofr82733.","productDescription":"35 p., ill., maps ;28 cm.","costCenters":[],"links":[{"id":140996,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1982/0733/report-thumb.jpg"},{"id":37225,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1982/0733/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b24e4b07f02db6aebb3","contributors":{"authors":[{"text":"Hirschaut, D.W.","contributorId":43761,"corporation":false,"usgs":true,"family":"Hirschaut","given":"D.W.","email":"","affiliations":[],"preferred":false,"id":159806,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Dingler, J.R.","contributorId":64247,"corporation":false,"usgs":true,"family":"Dingler","given":"J.R.","email":"","affiliations":[],"preferred":false,"id":159807,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":9327,"text":"ofr82511 - 1982 - Water quality of coal deposits and abandoned mines, Saginaw County, Michigan","interactions":[],"lastModifiedDate":"2017-07-12T11:21:42","indexId":"ofr82511","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1982","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":"82-511","title":"Water quality of coal deposits and abandoned mines, Saginaw County, Michigan","docAbstract":"

Surface water arid;ground water from an area underlain by coal- bearing rocks in the vicinity of St. Charles Michigan, were analyzed to determine the quality characteristics of these water resources and to assess the relation between the two. Data for 15 constituents, including boron, phenol, lithium, strontium and manganese, were in such high concentrations that they could be used to differentiate between water from wells drilled into coal-bearing beds and water from streams not directly associated with coal deposits.

Ground water from abandoned mines and undisturbed coal-bearing beds is highly mineralized, and contains higher concentrations of trace metals than surface water. Water from the undistrubed coal- bearing beds and abandoned mines is not suitable for domestic, public supply, or agricultural uses. Large amounts of this highly mineralized ground water reaching local streams would have a deleterious effect on surface-water quality.

","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Lansing, MI","doi":"10.3133/ofr82511","usgsCitation":"Handy, A., 1982, Water quality of coal deposits and abandoned mines, Saginaw County, Michigan: U.S. Geological Survey Open-File Report 82-511, v, 35 p, https://doi.org/10.3133/ofr82511.","productDescription":"v, 35 p","numberOfPages":"45","costCenters":[{"id":382,"text":"Michigan Water Science Center","active":true,"usgs":true}],"links":[{"id":343704,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1982/0511/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":142369,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1982/0511/report-thumb.jpg"}],"country":"United States","state":"Michigan","county":"Saginaw County","geographicExtents":"{\"type\":\"FeatureCollection\",\"features\":[{\"type\":\"Feature\",\"geometry\":{\"type\":\"Polygon\",\"coordinates\":[[[-84.1702,43.5689],[-84.0521,43.5668],[-84.0524,43.5235],[-83.8188,43.5217],[-83.8186,43.478],[-83.7,43.4787],[-83.7009,43.3941],[-83.6996,43.3317],[-83.6943,43.3252],[-83.694,43.2223],[-83.8154,43.2212],[-83.9318,43.2204],[-83.9294,43.1334],[-84.0519,43.1317],[-84.1687,43.1306],[-84.2874,43.1286],[-84.3684,43.1281],[-84.3698,43.2059],[-84.3701,43.2146],[-84.3717,43.3884],[-84.3718,43.4654],[-84.3713,43.4817],[-84.1719,43.4825],[-84.1702,43.5689]]]},\"properties\":{\"name\":\"Saginaw\",\"state\":\"MI\"}}]}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a07e4b07f02db5f99be","contributors":{"authors":[{"text":"Handy, A.H.","contributorId":104493,"corporation":false,"usgs":true,"family":"Handy","given":"A.H.","email":"","affiliations":[],"preferred":false,"id":159486,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":9366,"text":"ofr821060 - 1982 - Heavy-metal contamination of Crassostrea virginica and associated sediments of the Corpus Christi Bay system, Texas","interactions":[],"lastModifiedDate":"2012-02-02T00:06:00","indexId":"ofr821060","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1982","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":"82-1060","title":"Heavy-metal contamination of Crassostrea virginica and associated sediments of the Corpus Christi Bay system, Texas","docAbstract":"In a preliminary survey, Crassostrea virginica from areas of the Corpus Christi Bay system of Texas show significant concentrations of Cd, Cu, Pb, and Zn in their tissues and shells; concentrations of these same metals in associated sediments are also high in certain areas of the bay system. Zn and Cd concentrations in tissue show a high negative correlation to each other, whereas Zn and Pb in tissue and shell show a high positive correlation to one another. Sediment contents of Pb and Zn best reflect tissue values of the heavy metals; sediment concentrations of Cd and Cu show a poor inverse correlation to tissue concentrations. Some possible factors influencing these correlations are suspended-sediment type, physiological changes, water quality, and Ca intake.","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/ofr821060","usgsCitation":"Harrison, G., and Martin, E., 1982, Heavy-metal contamination of Crassostrea virginica and associated sediments of the Corpus Christi Bay system, Texas: U.S. Geological Survey Open-File Report 82-1060, 18 p., ill. ;28 cm., https://doi.org/10.3133/ofr821060.","productDescription":"18 p., ill. ;28 cm.","costCenters":[],"links":[{"id":140877,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1982/1060/report-thumb.jpg"},{"id":37077,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1982/1060/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4aa7e4b07f02db6671d7","contributors":{"authors":[{"text":"Harrison, G.","contributorId":94302,"corporation":false,"usgs":true,"family":"Harrison","given":"G.","email":"","affiliations":[],"preferred":false,"id":159552,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Martin, E.A.","contributorId":44148,"corporation":false,"usgs":true,"family":"Martin","given":"E.A.","email":"","affiliations":[],"preferred":false,"id":159551,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":9363,"text":"ofr81635 - 1982 - Ground-water storage depletion in Pahrump Valley, Nevada-California, 1962-75","interactions":[{"subject":{"id":9363,"text":"ofr81635 - 1982 - Ground-water storage depletion in Pahrump Valley, Nevada-California, 1962-75","indexId":"ofr81635","publicationYear":"1982","noYear":false,"title":"Ground-water storage depletion in Pahrump Valley, Nevada-California, 1962-75"},"predicate":"SUPERSEDED_BY","object":{"id":1806,"text":"wsp2279 - 1986 - Ground-water storage depletion in Pahrump Valley, Nevada-California, 1962-75","indexId":"wsp2279","publicationYear":"1986","noYear":false,"title":"Ground-water storage depletion in Pahrump Valley, Nevada-California, 1962-75"},"id":1}],"supersededBy":{"id":1806,"text":"wsp2279 - 1986 - Ground-water storage depletion in Pahrump Valley, Nevada-California, 1962-75","indexId":"wsp2279","publicationYear":"1986","noYear":false,"title":"Ground-water storage depletion in Pahrump Valley, Nevada-California, 1962-75"},"lastModifiedDate":"2018-02-05T14:59:16","indexId":"ofr81635","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1982","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":"81-635","title":"Ground-water storage depletion in Pahrump Valley, Nevada-California, 1962-75","docAbstract":"

During the 13-year period, February 1962 to February 1975, about 540,000 acre-feet of ground water was pumped from Pahrump Valley. This resulted in significant water-level declines along the base of the Pahrump and Manse fans where pumping was concentrated. Maximum observed net decline was slightly more than 60 feet. Much smaller declines occurred in the central valley, and locally, water levels in some shallow wells rose due to recharge derived from the deep percolation of irrigation water. The pumping resulted in about 219,000 acre-feet of storage depletion. Of this, 155,000 acre-feet was from the draining of unconsolidated material, 46,000 was from compaction of fine-grained sediments, and 18,000 acre-feet was from the elastic response of the aquifer and water. The total storage depletion was equal to about 40 percent of the total pumpage. The remaining pumped water was derived from the capture of natural ground-water discharge and reuse of pumped water that had recirculated back to ground water.

Natural recharge to and discharge from the ground-water system is estimated to be 37,000 acre-feet per year. Of this, 18,000 acre-feet per year leaves the area as subsurface outflow through carbonate-rock aquifers which form a multivalley flow system. The extent of this system was not precisely determined by this study. The most probable discharge area for this outflow is along the flood plain of the Amargosa River between the towns of Shoshone and Tecopa. This outflow probably cannot be economically captured by pumping from Pahrump Valley. Consequently, the maximum amount of natural discharge available for capture is 19,000 acre-feet per year. This is larger than the 12,000 acre-feet per year estimated in a previous study; the difference is due to different techniques used in the analysis.

As of 1975, pumping was causing an overdraft of 11,000 acre-feet per year on the ground-water system. No new equilibrium is probable in the foreseeable future. Water levels will probably continue to slowly decline until the pumping is reduced. The moderate rates of decline and very large amounts of ground water stored in the valley-fill reservoir suggest that a long time will be required before the valley-wide depletion of ground-water storage becomes critical. Problems involving water quality, land subsidence, and well interference will probably occur first.

","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr81635","collaboration":"Prepared in cooperation with the Nevada Division of Water Resources","usgsCitation":"Harrill, J.R., 1982, Ground-water storage depletion in Pahrump Valley, Nevada-California, 1962-75: U.S. Geological Survey Open-File Report 81-635, Report: viii, 76 p.; 3 Plates: 20.16 x 27.02 inches or smaller, https://doi.org/10.3133/ofr81635.","productDescription":"Report: viii, 76 p.; 3 Plates: 20.16 x 27.02 inches or smaller","costCenters":[],"links":[{"id":140860,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1981/0635/report-thumb.jpg"},{"id":351018,"rank":3,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1981/0635/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":351019,"rank":4,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1981/0635/plate-2.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":351020,"rank":5,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1981/0635/plate-3.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":351017,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1981/0635/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"country":"United States","state":"California, Nevada","otherGeospatial":"Pahrump Valley","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"type\": \"Polygon\",\n \"coordinates\": [\n [\n [\n -116.30,\n 35.5\n ],\n [\n -115.25,\n 35.5\n ],\n [\n -115.25,\n 36.5\n ],\n [\n -116.30,\n 36.5\n ],\n [\n -116.30,\n 35.5\n ]\n ]\n ]\n }\n }\n ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4afce4b07f02db6968fa","contributors":{"authors":[{"text":"Harrill, James R.","contributorId":99533,"corporation":false,"usgs":true,"family":"Harrill","given":"James","email":"","middleInitial":"R.","affiliations":[],"preferred":false,"id":159546,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":9641,"text":"ofr82370 - 1982 - Land subsidence in the San Joaquin Valley, California, as of 1980","interactions":[{"subject":{"id":9641,"text":"ofr82370 - 1982 - Land subsidence in the San Joaquin Valley, California, as of 1980","indexId":"ofr82370","publicationYear":"1982","noYear":false,"title":"Land subsidence in the San Joaquin Valley, California, as of 1980"},"predicate":"SUPERSEDED_BY","object":{"id":38899,"text":"pp437I - 1984 - Land subsidence in the San Joaquin Valley, California, as of 1980","indexId":"pp437I","publicationYear":"1984","noYear":false,"chapter":"I","title":"Land subsidence in the San Joaquin Valley, California, as of 1980"},"id":1}],"supersededBy":{"id":38899,"text":"pp437I - 1984 - Land subsidence in the San Joaquin Valley, California, as of 1980","indexId":"pp437I","publicationYear":"1984","noYear":false,"title":"Land subsidence in the San Joaquin Valley, California, as of 1980"},"lastModifiedDate":"2012-02-02T00:06:13","indexId":"ofr82370","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1982","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":"82-370","title":"Land subsidence in the San Joaquin Valley, California, as of 1980","docAbstract":"Land subsidence due to ground-water overdraft in the San Joaquin Valley began in the mid-1920 's and continued at alarming rates until surface was imported through major canals and aqueducts in the 1950 's and late 1960's. In areas where surface water replaced withdrawal of ground-water, water levels in the confined system rose sharply and subsidence slowed. In the late 1960 's and early 1970 's water levels in wells recovered to levels of the 1940 's and 1950 's throughout most of the western and southern parts of the Valley, in response to the importation of surface water through the California aqueduct. During the 1976-77 drought data collected at water-level and extensometer sites showed the effect of heavy demand on the ground-water resevoir. With the ' water of compaction ' gone, artesian head declined 10 to 20 times as fast as during the first cycle of long-term drawdown that ended in the late 1960's. In the 1978-79 water levels recovered to or above the 1976 pre-drought levels. The report suggests continued monitoring of land subsidence in the San Joaquin Valley. (USGS)","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/ofr82370","usgsCitation":"Ireland, R.L., Poland, J.F., and Riley, F.S., 1982, Land subsidence in the San Joaquin Valley, California, as of 1980: U.S. Geological Survey Open-File Report 82-370, viii, 134 p., 2 over-size sheets, ill., maps ;28 cm., https://doi.org/10.3133/ofr82370.","productDescription":"viii, 134 p., 2 over-size sheets, ill., maps ;28 cm.","costCenters":[],"links":[{"id":141970,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b30e4b07f02db6b40fe","contributors":{"authors":[{"text":"Ireland, R. L.","contributorId":89893,"corporation":false,"usgs":true,"family":"Ireland","given":"R.","email":"","middleInitial":"L.","affiliations":[],"preferred":false,"id":160036,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Poland, J. F.","contributorId":64223,"corporation":false,"usgs":true,"family":"Poland","given":"J.","email":"","middleInitial":"F.","affiliations":[],"preferred":false,"id":160035,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Riley, F. S.","contributorId":7701,"corporation":false,"usgs":true,"family":"Riley","given":"F.","middleInitial":"S.","affiliations":[],"preferred":false,"id":160034,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}} ,{"id":9225,"text":"ofr82233 - 1982 - Earthquake hazards information dissemination; a study of Charleston, South Carolina","interactions":[],"lastModifiedDate":"2012-02-02T00:06:18","indexId":"ofr82233","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1982","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":"82-233","title":"Earthquake hazards information dissemination; a study of Charleston, South Carolina","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/ofr82233","usgsCitation":"Greene, M.R., and Gori, P.L., 1982, Earthquake hazards information dissemination; a study of Charleston, South Carolina: U.S. Geological Survey Open-File Report 82-233, [iii], 61 p. :maps ;28 cm., https://doi.org/10.3133/ofr82233.","productDescription":"[iii], 61 p. :maps ;28 cm.","costCenters":[],"links":[{"id":142856,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1982/0233/report-thumb.jpg"},{"id":36860,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1982/0233/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a51e4b07f02db6297f3","contributors":{"authors":[{"text":"Greene, Marjorie R.","contributorId":100845,"corporation":false,"usgs":true,"family":"Greene","given":"Marjorie","email":"","middleInitial":"R.","affiliations":[],"preferred":false,"id":159316,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Gori, Paula L.","contributorId":10027,"corporation":false,"usgs":true,"family":"Gori","given":"Paula","email":"","middleInitial":"L.","affiliations":[],"preferred":false,"id":159315,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":9440,"text":"ofr82619 - 1982 - Thermodynamic properties of selected uranium compounds and aqueous species at 298.15 K and 1 bar and at higher temperatures; preliminary models for the origin of coffinite deposits","interactions":[],"lastModifiedDate":"2012-02-02T00:06:09","indexId":"ofr82619","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1982","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":"82-619","title":"Thermodynamic properties of selected uranium compounds and aqueous species at 298.15 K and 1 bar and at higher temperatures; preliminary models for the origin of coffinite deposits","docAbstract":"Thermodynamic values for 110 uranium-bearing phases and 28 aqueous uranium solution species (298.15 K and l bar) are tabulated based upon evaluated experimental data (largely from calorimetric experiments) and estimated values. Molar volume data are given for most of the solid phases. Thermodynamic values for 16 uranium-bearing phases are presented for higher temperatures in the form of and as a supplement to U.S. Geological Survey Bulletin 1452 (Robie et al., 1979). \r\n\r\nThe internal consistency of the thermodynamic values reported herein is dependent upon the reliability of the experimental results for several uranium phases that have been used as secondary calorimetric reference phases. The data for the reference phases and for those phases evaluated with respect to the secondary reference phases are discussed. \r\n\r\nA preliminary model for coffinite formation has been proposed together with an estimate of the free energy of formation of coffinite. Free energy values are estimated for several other uranium-bearing silicate phases that have been reported as secondary uranium phases associated with uranium ore deposits and that could be expected to develop wherever uranium is leached by groundwaters.","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/ofr82619","usgsCitation":"Hemingway, B.S., 1982, Thermodynamic properties of selected uranium compounds and aqueous species at 298.15 K and 1 bar and at higher temperatures; preliminary models for the origin of coffinite deposits: U.S. Geological Survey Open-File Report 82-619, iv, 95 p., ill. ;28 cm., https://doi.org/10.3133/ofr82619.","productDescription":"iv, 95 p., ill. ;28 cm.","costCenters":[],"links":[{"id":141003,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1982/0619/report-thumb.jpg"},{"id":37149,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1982/0619/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a08e4b07f02db5fa599","contributors":{"authors":[{"text":"Hemingway, B. S.","contributorId":7268,"corporation":false,"usgs":true,"family":"Hemingway","given":"B.","email":"","middleInitial":"S.","affiliations":[],"preferred":false,"id":159687,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":8856,"text":"ofr82783 - 1982 - The lanthanides and yttrium in minerals of the apatite group; a review","interactions":[],"lastModifiedDate":"2012-02-02T00:06:11","indexId":"ofr82783","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1982","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":"82-783","title":"The lanthanides and yttrium in minerals of the apatite group; a review","docAbstract":"More than 1000 analyses have been tabulated of the distribution of the lanthanides and yttrium in minerals of the apatite group, recalculated to atomic percentages. Average compositions have been calculated for apatites from 14 types of rocks. These show a progressive change of composition from apatites of granitic pegmatites, highest in the heavy lanthanides and yttrium, to those from alkalic pegmatites, highest in the light lanthanides and lowest in yttrium. This progression is clearly shown in plots of S (= at % La+Ce+Pr) vs the ratio La/Nd and of S vs the ratio 100Y/(Y+Ln), where Ln is the sum of the lanthanides. \r\n\r\nApatites of sedimentary phosphorites occupy a special position, being relatively depleted in Ce and relatively enriched in yttrium and the heavy lanthanides, consequences of deposition from sea water. \r\n\r\nApatites associated with iron ores are close in composition to apatites of carbonatites, alkalic ultramafic, and ultramafic rocks, being enriched in the light lanthanides and depleted in the heavy lanthanides. Their compositions do not support the hypothesis of Parak that the Kiruna-type ores are of sedimentary origin. \r\n\r\nTable 9 and Figures 1-3 show the dependence of lanthanide distribution on the nature of the host rock. Although a given analysis of the lanthanides does not unequivocally permit certain identification of the host rock, it can indicate a choice of highly probable host rocks.","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/ofr82783","usgsCitation":"Fleischer, M., and Altschuler, Z., 1982, The lanthanides and yttrium in minerals of the apatite group; a review: U.S. Geological Survey Open-File Report 82-783, i, 156 p., ill. ;28 cm., https://doi.org/10.3133/ofr82783.","productDescription":"i, 156 p., ill. ;28 cm.","costCenters":[],"links":[{"id":141107,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1982/0783/report-thumb.jpg"},{"id":36434,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1982/0783/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e48e8e4b07f02db55334c","contributors":{"authors":[{"text":"Fleischer, Michael","contributorId":65835,"corporation":false,"usgs":true,"family":"Fleischer","given":"Michael","email":"","affiliations":[],"preferred":false,"id":158444,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Altschuler, Z. S.","contributorId":42962,"corporation":false,"usgs":true,"family":"Altschuler","given":"Z. S.","affiliations":[],"preferred":false,"id":158443,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ]}