Water resources data for the 1981 water year for Connecticut consist of records of stage, discharge, and water quality of streams; contents and water quality of lakes and reservoirs; and water levels and water quality of ground-water wells. This volume contains records for water discharge at 55 gaging stations; storm discharge at 7 gaging stations; stage only at 1 gaging station; tidal volume at 1 gaging station; storm rainfall at 6 gaging stations; stage only records at 3 tidal-gaging stations; contents at 35 lakes and reservoirs; water quality at 40 gaging stations, 4 lakes and reservoirs, 2 harbors, and 16 wells; and water levels at 58 observation wells. Also included are data for 43 crest-stage partial-record stations. Locations of these sites are shown on figures 2, 3, and 4. Additional water data were collected at various sites, not involved in the systematic data-collection program, and are published as miscellaneous measurements and analyses. A few pertinent stations (not included above) in bordering States are also enclosed in this volume. These data represent that part of the National Water Data System operated by the U.S. Geological Survey and cooperating State, local, and Federal agencies in Connecticut.
","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/wdrCT811","collaboration":"Prepared in cooperation with State of Connecticut and with other agencies","usgsCitation":"Water Resources Division, U.S. Geological Survey, 1982, Water resources data for Connecticut, water year 1981: U.S. Geological Survey Water Data Report CT-81-1, ix, 325 p., https://doi.org/10.3133/wdrCT811.","productDescription":"ix, 325 p.","costCenters":[],"links":[{"id":410078,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wdr/1981/ct-81-1/report.pdf"},{"id":174017,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wdr/1981/ct-81-1/report-thumb.jpg"}],"country":"United 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\"}}]}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e49fee4b07f02db5f73ef","contributors":{"authors":[{"text":"Water Resources Division, U.S. Geological Survey","contributorId":128075,"corporation":true,"usgs":false,"organization":"Water Resources Division, U.S. Geological Survey","id":532296,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":27999,"text":"wri824074 - 1982 - Physical and hydrologic environments of the Mulberry coal reserves in eastern Kansas","interactions":[],"lastModifiedDate":"2012-02-02T00:08:40","indexId":"wri824074","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1982","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":342,"text":"Water-Resources Investigations Report","code":"WRI","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"82-4074","title":"Physical and hydrologic environments of the Mulberry coal reserves in eastern Kansas","docAbstract":"Strippable reserves of Mulberry coal underlie an area of approximately 300 square miles of Miami, Linn, and Bourbon Counties of eastern Kansas. Although subject to State reclamation law, current and projected strip mining of this relatively thin coal seam could alter and hydrologic environment of the study area. Drained by the Marais des Cygnes and Little Osage Rivers and their tributaries, this area is characterized by low relief and moderately impermeable soils. Streamflows are poorly sustained by ground-water discharge and fluctuate widely due to climatic extremes and usage of surface-water supplies. Because ground-water supplies are generally unreliable in quantity and quality, surface water is used to meet most water requirements in the study area. Primary used of surface waters are for domestic supplies, maintenance of wildlife and recreational areas, and cooling needs at LaCygne Power Plant. The prevailing chemical type of the natural streamflow is calcium bicarbonate, with concentrations of dissolved solids generally less than 500 milligrams per liter and pH near neutral. Additional streamflow and water-quality data are needed to evaluate the premining characteristics of and the anticipated changes in the hydrologic environment as strip mining proceeds within the study area. A network of data-collection stations and a sampling scheme have been established to acquire this additional information. (USGS)","language":"ENGLISH","publisher":"U.S. Geological Survey, WRD,","doi":"10.3133/wri824074","usgsCitation":"Kenny, J.F., Bevans, H., and Diaz, A., 1982, Physical and hydrologic environments of the Mulberry coal reserves in eastern Kansas: U.S. Geological Survey Water-Resources Investigations Report 82-4074, 50 p. :ill., maps ;28 cm., https://doi.org/10.3133/wri824074.","productDescription":"50 p. :ill., maps ;28 cm.","costCenters":[],"links":[{"id":122828,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wri/1982/4074/report-thumb.jpg"},{"id":56826,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wri/1982/4074/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4adbe4b07f02db685c0f","contributors":{"authors":[{"text":"Kenny, J. F.","contributorId":100378,"corporation":false,"usgs":true,"family":"Kenny","given":"J.","email":"","middleInitial":"F.","affiliations":[],"preferred":false,"id":199042,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Bevans, H.E.","contributorId":102892,"corporation":false,"usgs":true,"family":"Bevans","given":"H.E.","email":"","affiliations":[],"preferred":false,"id":199043,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Diaz, A.M.","contributorId":27084,"corporation":false,"usgs":true,"family":"Diaz","given":"A.M.","email":"","affiliations":[],"preferred":false,"id":199041,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}} ,{"id":9624,"text":"ofr82554 - 1982 - Water resources program of the U.S. Geological Survey related to agriculture in Louisiana","interactions":[],"lastModifiedDate":"2012-02-02T00:06:15","indexId":"ofr82554","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":"82-554","title":"Water resources program of the U.S. Geological Survey related to agriculture in Louisiana","docAbstract":"Surveillance activities of the U.S. Geological Survey Louisiana District include long-term, hydrologic-data-collection sites that serve a current-purpose, management function and (or) that furnish a data base for interpretative studies. The proposed program for 1982 includes a network of 69 surface-water data sites (continuous gaging stations), 250 flood-data sites (crest-stage stations), 679 ground-water wells (water-level observation and water-quality monitor wells), and 138 water-quality sites. The geographic distribution of the data sites is shown in the report. Interpretive studies have objectives that are oriented toward a particular geographic area , to a particular set of hydrologic phenomena, or to obtain information for use in solving specific problems. Current studies of interest to agriculture include the following: (1) Flood hydraulics and hydrology, (2) Low-flow or base-flow of streams in Louisiana, (3) Hydrologic studies in southwestern Louisiana, (4) Hydrologic impacts of surface mining in northern Louisiana, (5) Sparta aquifer study, and (6) Limnology of freshwater lakes. A network of partial record sites is also maintained to monitor specific flows. Peak stages (crest stage) are only recorded at sites where flood information is of interest. At other sites, only the low-flow or base-flow recession is obtained for use in determining relations between ground water and surface water, to assess water supply, and for effluent studies. (USGS)","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/ofr82554","usgsCitation":"Huntzinger, T., 1982, Water resources program of the U.S. Geological Survey related to agriculture in Louisiana: U.S. Geological Survey Open-File Report 82-554, iii, 22 p., ill., maps ;28 cm., https://doi.org/10.3133/ofr82554.","productDescription":"iii, 22 p., ill., maps ;28 cm.","costCenters":[],"links":[{"id":141762,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1982/0554/report-thumb.jpg"},{"id":37355,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1982/0554/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e49f3e4b07f02db5ef463","contributors":{"authors":[{"text":"Huntzinger, T.L.","contributorId":67503,"corporation":false,"usgs":true,"family":"Huntzinger","given":"T.L.","email":"","affiliations":[],"preferred":false,"id":160012,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":9630,"text":"ofr821003 - 1982 - Plankton studies in San Francisco Bay; VI, Zooplankton species composition and abundance in the North Bay, 1979-1980","interactions":[],"lastModifiedDate":"2016-07-27T11:36:04","indexId":"ofr821003","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":"82-1003","title":"Plankton studies in San Francisco Bay; VI, Zooplankton species composition and abundance in the North Bay, 1979-1980","docAbstract":"Data are presented that summarize zooplankton species composition and abundance in North San Francisco Bay during 1979 and 1980. Sampling was conducted once monthly at six stations during 1979 and twice monthly at sixteen stations during 1980. Samples were collected by pump at three depths in the shipping channel and at one depth over the shoals. Subsamples were enumerated while alive. Total zooplankton biomass, as carbon, was calculated from estimated carbon quotas and abundances of each organism enumerated.
","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr821003","usgsCitation":"Hutchinson, A., 1982, Plankton studies in San Francisco Bay; VI, Zooplankton species composition and abundance in the North Bay, 1979-1980: U.S. Geological Survey Open-File Report 82-1003, 202 p., https://doi.org/10.3133/ofr821003.","productDescription":"202 p.","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[{"id":552,"text":"San Francisco Bay-Delta","active":false,"usgs":true},{"id":5079,"text":"Pacific Regional Director's Office","active":true,"usgs":true}],"links":[{"id":37361,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1982/1003/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":142938,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1982/1003/report-thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4adae4b07f02db68555a","contributors":{"authors":[{"text":"Hutchinson, Anne","contributorId":45316,"corporation":false,"usgs":true,"family":"Hutchinson","given":"Anne","email":"","affiliations":[],"preferred":false,"id":160018,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":9725,"text":"ofr82977 - 1982 - Prediction of earthquake response spectra","interactions":[],"lastModifiedDate":"2012-02-02T00:06:30","indexId":"ofr82977","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":"82-977","title":"Prediction of earthquake response spectra","docAbstract":"We have developed empirical equations for predicting earthquake response spectra in terms of magnitude, distance, and site conditions, using a two-stage regression method similar to the one we used previously for peak horizontal acceleration and velocity. We analyzed horizontal pseudo-velocity response at 5 percent damping for 64 records of 12 shallow earthquakes in Western North America, including the recent Coyote Lake and Imperial Valley, California, earthquakes. We developed predictive equations for 12 different periods between 0.1 and 4.0 s, both for the larger of two horizontal components and for the random horizontal component. The resulting spectra show amplification at soil sites compared to rock sites for periods greater than or equal to 0.3 s, with maximum amplification exceeding a factor of 2 at 2.0 s. For periods less than 0.3 s there is slight deamplification at the soil sites. These results are generally consistent with those of several earlier studies. A particularly significant aspect of the predicted spectra is the change of shape with magnitude (confirming earlier results by McGuire and by Irifunac and Anderson). This result indicates that the conventional practice of scaling a constant spectral shape by peak acceleration will not give accurate answers. The Newmark and Hall method of spectral scaling, using both peak acceleration and peak velocity, largely avoids this error. Comparison of our spectra with the Nuclear Regulatory Commission's Regulatory Guide 1.60 spectrum anchored at the same value at 0.1 s shows that the Regulatory Guide 1.60 spectrum is exceeded at soil sites for a magnitude of 7.5 at all distances for periods greater than about 0.5 s. Comparison of our spectra for soil sites with the corresponding ATC-3 curve of lateral design force coefficient for the highest seismic zone indicates that the ATC-3 curve is exceeded within about 7 km of a magnitude 6.5 earthquake and within about 15 km of a magnitude 7.5 event. The amount by which it is exceeded for the 7.5 event is largest in the period range from 0.5 to 2.0 s.","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/ofr82977","usgsCitation":"Joyner, W.B., and Boore, D.M., 1982, Prediction of earthquake response spectra: U.S. Geological Survey Open-File Report 82-977, 17 p., ill. ;28 cm., https://doi.org/10.3133/ofr82977.","productDescription":"17 p., ill. ;28 cm.","costCenters":[],"links":[{"id":144207,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1982/0977/report-thumb.jpg"},{"id":37467,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1982/0977/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ac9e4b07f02db67c9f7","contributors":{"authors":[{"text":"Joyner, W. B.","contributorId":70746,"corporation":false,"usgs":true,"family":"Joyner","given":"W.","email":"","middleInitial":"B.","affiliations":[],"preferred":false,"id":160192,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Boore, David M. boore@usgs.gov","contributorId":2509,"corporation":false,"usgs":true,"family":"Boore","given":"David","email":"boore@usgs.gov","middleInitial":"M.","affiliations":[{"id":237,"text":"Earthquake Science Center","active":true,"usgs":true}],"preferred":false,"id":160191,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":9734,"text":"ofr82353 - 1982 - Specific conductance and dissolved chloride concentrations of freshwater aquifers and streams in petroleum producing areas in Mississippi","interactions":[],"lastModifiedDate":"2012-02-02T00:06:25","indexId":"ofr82353","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":"82-353","title":"Specific conductance and dissolved chloride concentrations of freshwater aquifers and streams in petroleum producing areas in Mississippi","docAbstract":"Specific conductance and dissolved chloride reconnasissance sampling was conducted in six oil-producing areas of Mississippi during periods of low streamflow in 1980 and 1981. Water samples were collected at 224 ground-water and 190 suface-water sites. Samples from 55 surface-water and 17 ground-water sites contained dissolved chloride concentrations in excess of 100 milligrams per liter. All data collected are presented in tables without interpretation. (USGS)","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/ofr82353","usgsCitation":"Kalkhoff, S., 1982, Specific conductance and dissolved chloride concentrations of freshwater aquifers and streams in petroleum producing areas in Mississippi: U.S. Geological Survey Open-File Report 82-353, iv, 37 p. :maps ;28 cm., https://doi.org/10.3133/ofr82353.","productDescription":"iv, 37 p. :maps ;28 cm.","costCenters":[],"links":[{"id":143077,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1982/0353/report-thumb.jpg"},{"id":37476,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1982/0353/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a60e4b07f02db634dd0","contributors":{"authors":[{"text":"Kalkhoff, S. J.","contributorId":28967,"corporation":false,"usgs":true,"family":"Kalkhoff","given":"S. J.","affiliations":[],"preferred":false,"id":160204,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":9721,"text":"ofr82881 - 1982 - Estimation of response-spectral values as functions of magnitude, distance, and site conditions","interactions":[],"lastModifiedDate":"2012-02-02T00:06:28","indexId":"ofr82881","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":"82-881","title":"Estimation of response-spectral values as functions of magnitude, distance, and site conditions","docAbstract":"We have developed empirical predictive equations for the horizontal pseudo-velocity response at 5-percent damping for 12 different periods from 0.1 to 4.0 s. Using a multiple linear-regression method similar to the one we used previously for peak horizontal acceleration and velocity, we analyzed response spectra period by period for 64 records of 12 shallow earthquakes in western North America, including the recent Coyote Lake and Imperial Valley, California, earthquakes. The resulting predictive equations show amplification of the response values at soil sites for periods greater than or equal to 0.5 s, with maximum amplification exceeding a factor of 2 at 1.5 s. For periods less than 0.5 s there is no statistically significant difference between rock sites and the soil sites represented in the data set. These results are consistent with those of several earlier studies. A particularly significant aspect of the predictive equations is that the response values at different periods are different functions of magnitude (confirming earlier results by McGuire and by Trifunac and Anderson). The slope of the least-squares straight line relating log response to moment magnitude ranges from 0.21 at a period of 0.1 s to greater than 0.5 at periods of 1 s and longer. This result indicates that the conventional practice of scaling a constant spectral shape by peak acceleration will not give accurate answers. The Newmark and Hall method of spectral scaling, using both peak acceleration and peak velocity, largely avoids this error. Comparison of our spectra with the Regulatory Guide 1.60 spectrum anchored at the same value at 0.1 s shows that the Regulatory Guide 1.60 spectrum is exceeded at soil sites for a magnitude of 7.5 at all distances for periods greater than about 0.5 s. Comparison of our spectra for soil sites with the corresponding ATC-3 curve of lateral design force coefficients for the highest seismic zone indicates that the ATC-3 curve is exceeded within about 5 km of a magnitude 6.5 earthquake and within about 20 km of a magnitude 7.5 event. The amount by which it is exceeded is largest in the period range from 0.5 to 2.0 s.","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/ofr82881","usgsCitation":"Joyner, W.B., and Boore, D.M., 1982, Estimation of response-spectral values as functions of magnitude, distance, and site conditions: U.S. Geological Survey Open-File Report 82-881, 29 p., ill. ;28 cm., https://doi.org/10.3133/ofr82881.","productDescription":"29 p., ill. ;28 cm.","costCenters":[],"links":[{"id":144170,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1982/0881/report-thumb.jpg"},{"id":37466,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1982/0881/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a54e4b07f02db62c212","contributors":{"authors":[{"text":"Joyner, W. B.","contributorId":70746,"corporation":false,"usgs":true,"family":"Joyner","given":"W.","email":"","middleInitial":"B.","affiliations":[],"preferred":false,"id":160185,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Boore, David M. boore@usgs.gov","contributorId":2509,"corporation":false,"usgs":true,"family":"Boore","given":"David","email":"boore@usgs.gov","middleInitial":"M.","affiliations":[{"id":237,"text":"Earthquake Science Center","active":true,"usgs":true}],"preferred":false,"id":160184,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":9762,"text":"ofr82604 - 1982 - Slides showing preliminary mosaic aeromagnetic and complete Bouguer gravity anomaly maps of the Dillon 1 by 2 degrees Quadrangle, Montana and Idaho","interactions":[],"lastModifiedDate":"2012-02-02T00:06:10","indexId":"ofr82604","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":"82-604","title":"Slides showing preliminary mosaic aeromagnetic and complete Bouguer gravity anomaly maps of the Dillon 1 by 2 degrees Quadrangle, Montana and Idaho","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/ofr82604","usgsCitation":"Kaufmann, H.E., and Hanna, W.F., 1982, Slides showing preliminary mosaic aeromagnetic and complete Bouguer gravity anomaly maps of the Dillon 1 by 2 degrees Quadrangle, Montana and Idaho: U.S. Geological Survey Open-File Report 82-604, 4 p., maps (1 col.) ;28 cm., https://doi.org/10.3133/ofr82604.","productDescription":"4 p., maps (1 col.) ;28 cm.","costCenters":[],"links":[{"id":141188,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1982/0604/report-thumb.jpg"},{"id":37511,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1982/0604/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e49f1e4b07f02db5ee338","contributors":{"authors":[{"text":"Kaufmann, H. E.","contributorId":40215,"corporation":false,"usgs":true,"family":"Kaufmann","given":"H.","email":"","middleInitial":"E.","affiliations":[],"preferred":false,"id":160252,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Hanna, W. F.","contributorId":6835,"corporation":false,"usgs":true,"family":"Hanna","given":"W.","email":"","middleInitial":"F.","affiliations":[],"preferred":false,"id":160251,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":8884,"text":"ofr82848 - 1982 - Remanent magnetization and magnetic susceptibility of two-oriented cores, Cement oil field, Oklahoma; a reference data set","interactions":[],"lastModifiedDate":"2012-02-02T00:06:18","indexId":"ofr82848","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":"82-848","title":"Remanent magnetization and magnetic susceptibility of two-oriented cores, Cement oil field, Oklahoma; a reference data set","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/ofr82848","usgsCitation":"Forgey, R., and Donovan, T., 1982, Remanent magnetization and magnetic susceptibility of two-oriented cores, Cement oil field, Oklahoma; a reference data set: U.S. Geological Survey Open-File Report 82-848, 39 p., maps ;28 cm., https://doi.org/10.3133/ofr82848.","productDescription":"39 p., maps ;28 cm.","costCenters":[],"links":[{"id":142673,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1982/0848/report-thumb.jpg"},{"id":36448,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1982/0848/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ac8e4b07f02db67bfb4","contributors":{"authors":[{"text":"Forgey, R.L.","contributorId":91858,"corporation":false,"usgs":true,"family":"Forgey","given":"R.L.","email":"","affiliations":[],"preferred":false,"id":158485,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Donovan, T.J.","contributorId":43762,"corporation":false,"usgs":true,"family":"Donovan","given":"T.J.","email":"","affiliations":[],"preferred":false,"id":158484,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":1890,"text":"wsp2203 - 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}],"lastModifiedDate":"2012-02-02T00:05:23","indexId":"wsp2203","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1982","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":341,"text":"Water Supply Paper","code":"WSP","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"2203","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 (Ky., Va., and W. Va.) has been increasing. However, additional statistical analysis does not indicate that the flood levels that were exceeded typically once or twice a year in the period 1947-79 are any more likely to be exceeded now than in 1947. Possible trends in streamchannel size also are investigated at three locations. No discernible 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 local rainfall and to the 'natural' hydrologic response in a relatively undisturbed subbasin. However, some statistical indication of trend persists after accounting for these natural factors, though it is of borderline statistical significance. Further study in the basin may relate flood magnitudes to both rainfall and to land use.","language":"ENGLISH","publisher":"U.S. G.P.O.,","doi":"10.3133/wsp2203","usgsCitation":"Hirsch, R.M., 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 Water Supply Paper 2203, iv, 37 p. : ill., maps ; 29 cm., https://doi.org/10.3133/wsp2203.","productDescription":"iv, 37 p. : ill., maps ; 29 cm.","costCenters":[],"links":[{"id":138390,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wsp/2203/report-thumb.jpg"},{"id":27179,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wsp/2203/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e47b3e4b07f02db49ed01","contributors":{"authors":[{"text":"Hirsch, Robert M. 0000-0002-4534-075X rhirsch@usgs.gov","orcid":"https://orcid.org/0000-0002-4534-075X","contributorId":2005,"corporation":false,"usgs":true,"family":"Hirsch","given":"Robert","email":"rhirsch@usgs.gov","middleInitial":"M.","affiliations":[{"id":502,"text":"Office of Surface Water","active":true,"usgs":true},{"id":436,"text":"National Research Program - Eastern Branch","active":true,"usgs":true},{"id":37316,"text":"WMA - Integrated Information Dissemination Division","active":true,"usgs":true},{"id":37778,"text":"WMA - Integrated Modeling and Prediction Division","active":true,"usgs":true}],"preferred":true,"id":144317,"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":144319,"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":144318,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}} ,{"id":9768,"text":"ofr82528 - 1982 - Characteristics and description of cores from the USGS core hole CRU-1, Parachute Creek Member, Green River Formation, east-central Uinta Basin, Utah","interactions":[],"lastModifiedDate":"2012-02-02T00:06:14","indexId":"ofr82528","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":"82-528","title":"Characteristics and description of cores from the USGS core hole CRU-1, Parachute Creek Member, Green River Formation, east-central Uinta Basin, Utah","docAbstract":"Oil-yield, lithologic, and mineral distribution data were determined for cores taken from a 497.7-foot drill hole in the upper part of the Parachute Creek Member of the Eocene Green River Formation. The drill hole, 1050 feet FEL, 700 feet FNL, sec. 3, T. 12 S., R. 24 E., Uintah County, Utah, started slightly below the contact between the Uinta Formation, also of Eocene age, and the underlying Green River Formation. It ended 32 feet below the base of the Mahogany bed (the richest oil-shale bed between A groove and B groove--which define the upper and lower boundaries, respectively, of the Mahogany zone). Most of the interval studied is kerogen- or carbonate-rich, commonly tuffaceous, and is very fine grained. \r\n\r\nSeveral thin (<3 feet) oil-shale beds which yield as much as 25 gallons of oil per ton occur above the Mahogany zone, but are probably not of economic interest. The cored sequence contains several tuff beds. The thickest of these beds is approximately 2 feet thick; the average thickness is rarely greater than 0.5 feet. Two oil-saturated tuff beds occur approximately 65 feet above the Mahogany oil-shale bed. Although these two tuffs are exposed on nearby surface outcrops, no evidence of oil is seen on outcrop. The Mahogany zone is approximately 69 feet thick at the drill site; the lowermost few feet were not penetrated. At the site cored, the Mahogany zone is overlain by 435 feet of overburden. Fischer assays indicate that 42.3 feet of oil shale within the Mahogany zone could yield at least 25 gallons of oil per ton from beds at least 10 feet thick.","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/ofr82528","usgsCitation":"Keighin, C.W., 1982, Characteristics and description of cores from the USGS core hole CRU-1, Parachute Creek Member, Green River Formation, east-central Uinta Basin, Utah: U.S. Geological Survey Open-File Report 82-528, i, 46 p., ill., map ;28 cm., https://doi.org/10.3133/ofr82528.","productDescription":"i, 46 p., ill., map ;28 cm.","costCenters":[],"links":[{"id":142199,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1982/0528/report-thumb.jpg"},{"id":37527,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1982/0528/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e49e3e4b07f02db5e5592","contributors":{"authors":[{"text":"Keighin, C. W.","contributorId":79887,"corporation":false,"usgs":true,"family":"Keighin","given":"C.","email":"","middleInitial":"W.","affiliations":[],"preferred":false,"id":160263,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":9774,"text":"ofr821028 - 1982 - Mineral resource potential of the Winchester Roadless Area, Cochise County, Arizona","interactions":[],"lastModifiedDate":"2022-09-28T20:32:58.97565","indexId":"ofr821028","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":"82-1028","title":"Mineral resource potential of the Winchester Roadless Area, Cochise County, Arizona","docAbstract":"No abstract available.
","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr821028","usgsCitation":"Keith, W.J., Martin, R., and Kreidler, T.J., 1982, Mineral resource potential of the Winchester Roadless Area, Cochise County, Arizona: U.S. Geological Survey Open-File Report 82-1028, i, 7 p., https://doi.org/10.3133/ofr821028.","productDescription":"i, 7 p.","costCenters":[],"links":[{"id":407551,"rank":3,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_13623.htm","linkFileType":{"id":5,"text":"html"}},{"id":37535,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1982/1028/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":142782,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1982/1028/report-thumb.jpg"}],"country":"United States","state":"Arizona","county":"Cochise County","otherGeospatial":"Winchester Roadless Area","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"type\": \"Polygon\",\n \"coordinates\": [\n [\n [\n -110.1530,\n 32.426\n ],\n [\n -110.042,\n 32.426\n ],\n [\n -110.042,\n 32.312\n ],\n [\n -110.1530,\n 32.312\n ],\n [\n -110.1530,\n 32.426\n ]\n ]\n ]\n }\n }\n ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b09e4b07f02db69c067","contributors":{"authors":[{"text":"Keith, W. J.","contributorId":41827,"corporation":false,"usgs":true,"family":"Keith","given":"W.","middleInitial":"J.","affiliations":[],"preferred":false,"id":160274,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Martin, R.A.","contributorId":53379,"corporation":false,"usgs":true,"family":"Martin","given":"R.A.","email":"","affiliations":[],"preferred":false,"id":160275,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Kreidler, T. J.","contributorId":57460,"corporation":false,"usgs":true,"family":"Kreidler","given":"T.","email":"","middleInitial":"J.","affiliations":[],"preferred":false,"id":160276,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}} ,{"id":27476,"text":"wri8128 - 1982 - Characterization of urban runoff from Grange Hall Creek at Northglenn, Adams County, Colorado","interactions":[],"lastModifiedDate":"2012-02-02T00:08:27","indexId":"wri8128","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1982","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":342,"text":"Water-Resources Investigations Report","code":"WRI","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"81-28","title":"Characterization of urban runoff from Grange Hall Creek at Northglenn, Adams County, Colorado","language":"ENGLISH","publisher":"U.S. Geological Survey, Water Resources Division,","doi":"10.3133/wri8128","usgsCitation":"Hall, D.C., and Duncan, A., 1982, Characterization of urban runoff from Grange Hall Creek at Northglenn, Adams County, Colorado: U.S. Geological Survey Water-Resources Investigations Report 81-28, vii, 50 p. :ill., maps ;28 cm., https://doi.org/10.3133/wri8128.","productDescription":"vii, 50 p. :ill., maps ;28 cm.","costCenters":[],"links":[{"id":118746,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wri/1981/0028/report-thumb.jpg"},{"id":56327,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wri/1981/0028/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e49e2e4b07f02db5e4d09","contributors":{"authors":[{"text":"Hall, Dennis C.","contributorId":95473,"corporation":false,"usgs":true,"family":"Hall","given":"Dennis","email":"","middleInitial":"C.","affiliations":[],"preferred":false,"id":198187,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Duncan, A.C.","contributorId":70397,"corporation":false,"usgs":true,"family":"Duncan","given":"A.C.","email":"","affiliations":[],"preferred":false,"id":198186,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":9787,"text":"ofr82219 - 1982 - Lithologic and stratigraphic description of cores of organic-rich shale of Late Devonian and Early Mississippian age in northeastern Kentucky","interactions":[],"lastModifiedDate":"2012-02-02T00:06:19","indexId":"ofr82219","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":"82-219","title":"Lithologic and stratigraphic description of cores of organic-rich shale of Late Devonian and Early Mississippian age in northeastern Kentucky","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/ofr82219","usgsCitation":"Kepferle, R., Beard, J., and Pollock, J., 1982, Lithologic and stratigraphic description of cores of organic-rich shale of Late Devonian and Early Mississippian age in northeastern Kentucky: U.S. Geological Survey Open-File Report 82-219, 75 p., 1 over-size sheets, ill., maps ;28 cm., https://doi.org/10.3133/ofr82219.","productDescription":"75 p., 1 over-size sheets, ill., maps ;28 cm.","costCenters":[],"links":[{"id":142838,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1982/0219/report-thumb.jpg"},{"id":37554,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1982/0219/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":37555,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1982/0219/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a0ce4b07f02db5fc292","contributors":{"authors":[{"text":"Kepferle, R.C.","contributorId":17588,"corporation":false,"usgs":true,"family":"Kepferle","given":"R.C.","affiliations":[],"preferred":false,"id":160299,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Beard, J.G.","contributorId":38837,"corporation":false,"usgs":true,"family":"Beard","given":"J.G.","email":"","affiliations":[],"preferred":false,"id":160300,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Pollock, J.D.","contributorId":7134,"corporation":false,"usgs":true,"family":"Pollock","given":"J.D.","email":"","affiliations":[],"preferred":false,"id":160298,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}} ,{"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":8955,"text":"ofr821074A - 1982 - Index of slides of geologic map, mineral occurrence maps, geochemical maps, heavy mineral maps, and mineral resource potential maps, Charlotte 1 degree x 2 degrees quadrangle, North Carolina and South Carolina (CUSMAP Program)","interactions":[],"lastModifiedDate":"2012-02-02T00:06:10","indexId":"ofr821074A","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":"82-1074","chapter":"A","title":"Index of slides of geologic map, mineral occurrence maps, geochemical maps, heavy mineral maps, and mineral resource potential maps, Charlotte 1 degree x 2 degrees quadrangle, North Carolina and South Carolina (CUSMAP Program)","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/ofr821074A","usgsCitation":"Gair, J.E., 1982, Index of slides of geologic map, mineral occurrence maps, geochemical maps, heavy mineral maps, and mineral resource potential maps, Charlotte 1 degree x 2 degrees quadrangle, North Carolina and South Carolina (CUSMAP Program): U.S. Geological Survey Open-File Report 82-1074, 17 p. ;28 cm., https://doi.org/10.3133/ofr821074A.","productDescription":"17 p. ;28 cm.","costCenters":[],"links":[{"id":141182,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1982/1074a/report-thumb.jpg"},{"id":36579,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1982/1074a/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e49fae4b07f02db5f4266","contributors":{"authors":[{"text":"Gair, Jacob Eugene","contributorId":14387,"corporation":false,"usgs":true,"family":"Gair","given":"Jacob","email":"","middleInitial":"Eugene","affiliations":[],"preferred":false,"id":158618,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":9797,"text":"ofr821099 - 1982 - Analytical determinations from samples taken in the Ten Mile West Roadless Area, Boise and Elmore counties, Idaho","interactions":[],"lastModifiedDate":"2012-02-02T00:06:15","indexId":"ofr821099","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":"82-1099","title":"Analytical determinations from samples taken in the Ten Mile West Roadless Area, Boise and Elmore counties, Idaho","docAbstract":"A total of 584 stream-sediment and rock samples were collected from within or near the Ten Mile West Roadless Area, Boise and Elmore Counties, Idaho, as part of a geologic study aimed at appraising the mineral resource potential of the area. Emphasis was placed on stream-sediment samples because stream sediments represent the erosional products of a drainage system and offer a rapid means of locating anomalous concentrations of ore-forming elements. An unusually high proportion of the stream-sediment samples contained concentrations of silver and molybdenum. Unaltered rocks of the area contain normal quantities of the common rock-forming elements. Some exposures of altered or mineralized rocks and some quartz veins contain significant quantities of gold and silver.","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/ofr821099","usgsCitation":"Kiilsgaard, T.H., 1982, Analytical determinations from samples taken in the Ten Mile West Roadless Area, Boise and Elmore counties, Idaho: U.S. Geological Survey Open-File Report 82-1099, 36 p. maps ;28 cm., https://doi.org/10.3133/ofr821099.","productDescription":"36 p. maps ;28 cm.","costCenters":[],"links":[{"id":141767,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1982/1099/report-thumb.jpg"},{"id":37560,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1982/1099/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":37561,"rank":401,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1982/1099/plate-2.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":37562,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1982/1099/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4acce4b07f02db67e475","contributors":{"authors":[{"text":"Kiilsgaard, Thor H.","contributorId":68738,"corporation":false,"usgs":true,"family":"Kiilsgaard","given":"Thor","email":"","middleInitial":"H.","affiliations":[],"preferred":false,"id":160317,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":9798,"text":"ofr82668 - 1982 - Geology of areas marked by geophysical anomalies (B-35 and B-34), Wadi Bidah District, Kingdom of Saudi Arabia","interactions":[],"lastModifiedDate":"2015-09-22T18:36:39","indexId":"ofr82668","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":"82-668","title":"Geology of areas marked by geophysical anomalies (B-35 and B-34), Wadi Bidah District, Kingdom of Saudi Arabia","docAbstract":"Geophysical surveys in the Wadi Bidah district, in the southwestern part of the Kingdom of Saudi Arabia, have revealed anomalies of the type that may be caused by deposits of massive sulfides. Accordingly, a study was undertaken to investigate the geologic environment associated with the geophysical anomalies and to determine whether mineral exploration of the anomalous areas might be warranted. An extensive geochemical sampling program did not disclose any evidence of ore mineral concentrations in the rocks. Detailed geologic mapping shows the anomalous areas to be underlain by Precambrian carbonaceous graywacke, the outcrop patterns of which closely fit the anomaly patterns. Field evidence and petrologic studies indicate that carbonaceous material in the rocks is the cause of the geophysical anomalies.
\nNothing was found in the anomalous areas that suggests the presence of mineral deposits of commercial grade, and further mineral investigations or exploration in the areas is not recommended.
","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Reston, VA","doi":"10.3133/ofr82668","usgsCitation":"Kiilsgaard, T.H., 1982, Geology of areas marked by geophysical anomalies (B-35 and B-34), Wadi Bidah District, Kingdom of Saudi Arabia: U.S. Geological Survey Open-File Report 82-668, 37 p., https://doi.org/10.3133/ofr82668.","productDescription":"37 p.","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[],"links":[{"id":37563,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1982/0668/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":141783,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1982/0668/report-thumb.jpg"}],"country":"Saudi Arabia","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"type\": \"Polygon\",\n \"coordinates\": [\n [\n [\n 41,\n 20\n ],\n [\n 41,\n 21\n ],\n [\n 41.5,\n 21\n ],\n [\n 41.5,\n 20\n ],\n [\n 41,\n 20\n ]\n ]\n ]\n }\n }\n ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ad5e4b07f02db683699","contributors":{"authors":[{"text":"Kiilsgaard, Thor H.","contributorId":68738,"corporation":false,"usgs":true,"family":"Kiilsgaard","given":"Thor","email":"","middleInitial":"H.","affiliations":[],"preferred":false,"id":160318,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":9825,"text":"ofr82748 - 1982 - Coal exploratory drilling during 1979 in western Powder River County, Montana","interactions":[],"lastModifiedDate":"2012-02-02T00:06:14","indexId":"ofr82748","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":"82-748","title":"Coal exploratory drilling during 1979 in western Powder River County, Montana","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/ofr82748","usgsCitation":"Kirschbaum, M., Correia, G., and McPhillips, M., 1982, Coal exploratory drilling during 1979 in western Powder River County, Montana: U.S. Geological Survey Open-File Report 82-748, i, 143 p., ill., map ;28 cm., https://doi.org/10.3133/ofr82748.","productDescription":"i, 143 p., ill., map ;28 cm.","costCenters":[],"links":[{"id":142247,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1982/0748/report-thumb.jpg"},{"id":37608,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1982/0748/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e49d6e4b07f02db5ddfc4","contributors":{"authors":[{"text":"Kirschbaum, M.A.","contributorId":79471,"corporation":false,"usgs":true,"family":"Kirschbaum","given":"M.A.","email":"","affiliations":[],"preferred":false,"id":160367,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Correia, G.A.","contributorId":99551,"corporation":false,"usgs":true,"family":"Correia","given":"G.A.","email":"","affiliations":[],"preferred":false,"id":160368,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"McPhillips, M.","contributorId":55824,"corporation":false,"usgs":true,"family":"McPhillips","given":"M.","email":"","affiliations":[],"preferred":false,"id":160366,"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":9808,"text":"ofr82860 - 1982 - Geohydrologic reconnaissance of drainage wells in Florida; an interim report","interactions":[],"lastModifiedDate":"2012-02-02T00:06:15","indexId":"ofr82860","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":"82-860","title":"Geohydrologic reconnaissance of drainage wells in Florida; an interim report","docAbstract":"Drainage wells are used to inject surface waters directly into an aquifer, or shallow ground waters directly into a deeper aquifer, primarily by gravity. Such wells in Florida may be grouped into two broad types: (1) Surface-water injection wells, and (2) interaquifer connector wells. Surface-water injection wells are commonly used to supplement drainage for urban areas in karst terranes of central and north Florida. Data are available for 25 wells in the Ocala, Live Oak, and Orlando areas that allow comparison of the quality of water samples from these Floridan aquifer drainage wells with allowable contaminant levels. Comparison indicates that maximum contaminant levels for turbidity, color, and iron, manganese, and lead concentrations are equaled or exceeded in some drainage-well samples, and relatively high counts for coliform bacteria are present in most wells. Interaquifer connector wells are used in the phosphate mining areas of Polk and Hillsborough Counties, to drain mining operations and recharge the Floridan aquifer. Water-quality data available from 13 connector wells indicate that samples from most of these wells exceed standards values for iron concentration and turbidity. One well yielded a highly mineralized water, and samples from 6 of the other 12 wells exceed standards values for gross alpha concentrations. (USGS)","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/ofr82860","usgsCitation":"Kimrey, J.O., and Fayard, L.D., 1982, Geohydrologic reconnaissance of drainage wells in Florida; an interim report: U.S. Geological Survey Open-File Report 82-860, iv, 63 p. :ill., maps ;28 cm., https://doi.org/10.3133/ofr82860.","productDescription":"iv, 63 p. :ill., maps ;28 cm.","costCenters":[],"links":[{"id":141825,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1982/0860/report-thumb.jpg"},{"id":37594,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1982/0860/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b1be4b07f02db6a8e28","contributors":{"authors":[{"text":"Kimrey, Joel O.","contributorId":96262,"corporation":false,"usgs":true,"family":"Kimrey","given":"Joel","email":"","middleInitial":"O.","affiliations":[],"preferred":false,"id":160335,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Fayard, Larry D.","contributorId":78326,"corporation":false,"usgs":true,"family":"Fayard","given":"Larry","email":"","middleInitial":"D.","affiliations":[],"preferred":false,"id":160334,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":9454,"text":"ofr82699 - 1982 - A heat-pulse flowmeter for measuring minimal discharge rates in boreholes","interactions":[],"lastModifiedDate":"2012-02-02T00:06:17","indexId":"ofr82699","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":"82-699","title":"A heat-pulse flowmeter for measuring minimal discharge rates in boreholes","docAbstract":"The U.S. Geological Survey has tested a borehole-configured heat-pulse flowmeter which has good low-velocity flow-measuring sensitivity. The flowmeter was tested in the laboratory in 51-, 102-, and 152-millimeter-diameter columns using water velocities ranging from 0.35 to 250 millimeters per second. The heat-pulse flowmeter also was tested in a 15-meter-deep granite test pit with controlled water flow, and in a 58-meter-deep borehole in sedimentary materials. The flowmeter's capability to detect and measure naturally occurring, low-velocity, thermally induced convection currents in boreholes was demonstrated. Further improvements to the heat-pulse-flowmeter system are needed to increase its reliability and improve its response through four-conductor logging cable.","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/ofr82699","usgsCitation":"Hess, A., 1982, A heat-pulse flowmeter for measuring minimal discharge rates in boreholes: U.S. Geological Survey Open-File Report 82-699, iv, 44 p. ill. ;28 cm., https://doi.org/10.3133/ofr82699.","productDescription":"iv, 44 p. ill. ;28 cm.","costCenters":[],"links":[{"id":142763,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1982/0699/report-thumb.jpg"},{"id":37159,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1982/0699/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b24e4b07f02db6ae4ae","contributors":{"authors":[{"text":"Hess, A.E.","contributorId":71979,"corporation":false,"usgs":true,"family":"Hess","given":"A.E.","email":"","affiliations":[],"preferred":false,"id":159715,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":9813,"text":"ofr821072 - 1982 - Principal facts for six gravity profiles across the Midcontinent Gravity High in Iowa and Nebraska","interactions":[],"lastModifiedDate":"2012-02-02T00:06:16","indexId":"ofr821072","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":"82-1072","title":"Principal facts for six gravity profiles across the Midcontinent Gravity High in Iowa and Nebraska","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/ofr821072","usgsCitation":"King, E.R., and Mattick, R., 1982, Principal facts for six gravity profiles across the Midcontinent Gravity High in Iowa and Nebraska: U.S. Geological Survey Open-File Report 82-1072, 18 p., map ;28 cm., https://doi.org/10.3133/ofr821072.","productDescription":"18 p., map ;28 cm.","costCenters":[],"links":[{"id":141769,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1982/1072/report-thumb.jpg"},{"id":37596,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1982/1072/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4aa8e4b07f02db6676a9","contributors":{"authors":[{"text":"King, E. R.","contributorId":93482,"corporation":false,"usgs":true,"family":"King","given":"E.","email":"","middleInitial":"R.","affiliations":[],"preferred":false,"id":160344,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Mattick, R.E.","contributorId":85162,"corporation":false,"usgs":true,"family":"Mattick","given":"R.E.","affiliations":[],"preferred":false,"id":160343,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":9814,"text":"ofr82964 - 1982 - Analytical data for minus-80-mesh stream-sediment samples collected during 1981 from the Solomon and Bendeleben quadrangles, Alaska","interactions":[],"lastModifiedDate":"2012-02-02T00:06:16","indexId":"ofr82964","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":"82-964","title":"Analytical data for minus-80-mesh stream-sediment samples collected during 1981 from the Solomon and Bendeleben quadrangles, Alaska","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/ofr82964","usgsCitation":"King, H.D., Sutley, S.J., O’Leary, R.M., McDougal, C.M., and Duttweiler, K., 1982, Analytical data for minus-80-mesh stream-sediment samples collected during 1981 from the Solomon and Bendeleben quadrangles, Alaska: U.S. Geological Survey Open-File Report 82-964, 46 p., 2 over-size sheets, maps ;28 cm., https://doi.org/10.3133/ofr82964.","productDescription":"46 p., 2 over-size sheets, maps ;28 cm.","costCenters":[],"links":[{"id":141770,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1982/0964/report-thumb.jpg"},{"id":37597,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1982/0964/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":37598,"rank":401,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1982/0964/plate-2.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":37599,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1982/0964/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4acfe4b07f02db67ff8b","contributors":{"authors":[{"text":"King, H. D.","contributorId":89113,"corporation":false,"usgs":true,"family":"King","given":"H.","email":"","middleInitial":"D.","affiliations":[],"preferred":false,"id":160348,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Sutley, S. J.","contributorId":91484,"corporation":false,"usgs":true,"family":"Sutley","given":"S.","email":"","middleInitial":"J.","affiliations":[],"preferred":false,"id":160349,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"O’Leary, R. M.","contributorId":44894,"corporation":false,"usgs":true,"family":"O’Leary","given":"R.","email":"","middleInitial":"M.","affiliations":[],"preferred":false,"id":160346,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"McDougal, C. M.","contributorId":21129,"corporation":false,"usgs":true,"family":"McDougal","given":"C.","email":"","middleInitial":"M.","affiliations":[],"preferred":false,"id":160345,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"Duttweiler, K.A.","contributorId":68310,"corporation":false,"usgs":true,"family":"Duttweiler","given":"K.A.","affiliations":[],"preferred":false,"id":160347,"contributorType":{"id":1,"text":"Authors"},"rank":5}]}} ,{"id":9816,"text":"ofr821044 - 1982 - A study of surface and subsurface ground motions at Calico Hills, Nevada Test Site","interactions":[],"lastModifiedDate":"2012-02-02T00:06:17","indexId":"ofr821044","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":"82-1044","title":"A study of surface and subsurface ground motions at Calico Hills, Nevada Test Site","docAbstract":"A study of earthquake ground motions recorded at depth in a drill hole and at the ground surface has derived the surface to subsurface transfer functions such as might be expected at a potential nuclear waste repository in a similar setting. The site under investigation has small seismic velocity contrasts in the layers of rock between the surface and the subsurface seismometer location. The subsurface seismic motions were similar in spectral characteristics to the surface motions and were lower in amplitude across the recorded band-width by a factor of 1.5.","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/ofr821044","usgsCitation":"King, K.W., 1982, A study of surface and subsurface ground motions at Calico Hills, Nevada Test Site: U.S. Geological Survey Open-File Report 82-1044, 20 p. ill. ;28 cm., https://doi.org/10.3133/ofr821044.","productDescription":"20 p. ill. ;28 cm.","costCenters":[],"links":[{"id":142769,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1982/1044/report-thumb.jpg"},{"id":37601,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1982/1044/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b17e4b07f02db6a618f","contributors":{"authors":[{"text":"King, Kenneth W.","contributorId":54213,"corporation":false,"usgs":true,"family":"King","given":"Kenneth","email":"","middleInitial":"W.","affiliations":[],"preferred":false,"id":160352,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ]}