{"pageNumber":"5334","pageRowStart":"133325","pageSize":"25","recordCount":184769,"records":[{"id":10860,"text":"ofr82980 - 1982 - Integrated model of the shallow and deep hydrothermal systems in the East Mesa area, Imperial Valley, California","interactions":[],"lastModifiedDate":"2012-02-02T00:06:34","indexId":"ofr82980","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":"82-980","title":"Integrated model of the shallow and deep hydrothermal systems in the East Mesa area, Imperial Valley, California","docAbstract":"Geological, geophysical, thermal, petrophysical and hydrological data available for the East Mesa hydrothermal system that are pertinent to the construction of a computer model of the natural flow of heat and fluid mass within the system are assembled and correlated. A conceptual model of the full system is developed and a subregion selected for quantitative modeling. By invoking the .Boussinesq approximation, valid for describing the natural flow of heat and mass in a liquid hydrothermal system, it is found practical to carry computer simulations far enough in time to ensure that steady-state conditions are obtained. Initial calculations for an axisymmetric model approximating the system demonstrate that the vertical formation permeability of the deep East Mesa system must be very low (kv ~ 0.25 to 0.5 md). Since subsurface temperature and surface heat flow data exhibit major deviations from the axisymmetric approximation, exploratory three-dimensional calculations are performed to assess the effects of various mechanisms which might operate to produce such observed asymmetries. A three-dimensional model evolves from this iterative data synthesis and computer analysis which includes a hot fluid convective source distributed along a leaky fault radiating northward from the center of the hot spot and realistic variations in the reservoir formation properties.","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/ofr82980","usgsCitation":"Riney, T.D., Pritchett, J., and Rice, L., 1982, Integrated model of the shallow and deep hydrothermal systems in the East Mesa area, Imperial Valley, California: U.S. Geological Survey Open-File Report 82-980, 118 p., ill., maps ;28 cm., https://doi.org/10.3133/ofr82980.","productDescription":"118 p., ill., maps ;28 cm.","costCenters":[],"links":[{"id":144916,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1982/0980/report-thumb.jpg"},{"id":38644,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1982/0980/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e499ee4b07f02db5bcb4b","contributors":{"authors":[{"text":"Riney, T. David","contributorId":92674,"corporation":false,"usgs":true,"family":"Riney","given":"T.","email":"","middleInitial":"David","affiliations":[],"preferred":false,"id":162090,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Pritchett, J.W.","contributorId":29433,"corporation":false,"usgs":true,"family":"Pritchett","given":"J.W.","email":"","affiliations":[],"preferred":false,"id":162088,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Rice, L.F.","contributorId":59799,"corporation":false,"usgs":true,"family":"Rice","given":"L.F.","email":"","affiliations":[],"preferred":false,"id":162089,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":11476,"text":"ofr82473 - 1982 - Borehole-gravity surveys in basin-fill deposits of central and southern Arizona","interactions":[],"lastModifiedDate":"2012-02-02T00:06:34","indexId":"ofr82473","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":"82-473","title":"Borehole-gravity surveys in basin-fill deposits of central and southern Arizona","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/ofr82473","usgsCitation":"Tucci, P., Schmoker, J., and Robbins, S.L., 1982, Borehole-gravity surveys in basin-fill deposits of central and southern Arizona: U.S. Geological Survey Open-File Report 82-473, 24 p., ill., map ;28 cm., https://doi.org/10.3133/ofr82473.","productDescription":"24 p., ill., map ;28 cm.","costCenters":[],"links":[{"id":144906,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1982/0473/report-thumb.jpg"},{"id":39347,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1982/0473/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a14e4b07f02db602991","contributors":{"authors":[{"text":"Tucci, Patrick ptucci@usgs.gov","contributorId":926,"corporation":false,"usgs":true,"family":"Tucci","given":"Patrick","email":"ptucci@usgs.gov","affiliations":[],"preferred":true,"id":163201,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Schmoker, J. W.","contributorId":69964,"corporation":false,"usgs":true,"family":"Schmoker","given":"J. W.","affiliations":[],"preferred":false,"id":163203,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Robbins, S. L.","contributorId":49766,"corporation":false,"usgs":true,"family":"Robbins","given":"S.","email":"","middleInitial":"L.","affiliations":[],"preferred":false,"id":163202,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":10533,"text":"ofr82170 - 1982 - Water resources of the Black Hand Sandstone Member of the Cuyahoga Formation aquifers of Mississippian age in southeastern Ohio","interactions":[],"lastModifiedDate":"2012-02-02T00:06:25","indexId":"ofr82170","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":"82-170","title":"Water resources of the Black Hand Sandstone Member of the Cuyahoga Formation aquifers of Mississippian age in southeastern Ohio","docAbstract":"The Black Hand Sandstone Member of the Cuyahoga Formation and associated acquifers of Mississippian age, including the Allensville Conglomerate Member of the Logan Formation, (both members of the local usage) were investigated in a 1 ,500-square-mile area in southeastern Ohio. These aquifers are the chief sources of water beneath the coal-bearing rocks of the Pennsylvanian System and are widely use for farm and home requirements. The aquifers crop out in the western part of the area and dip southeastward 35 feet per mile. At Lake Hope, in northeastern Vinton County, the aquifers are the deepest sources of ground water in Ohio, occurring at depths locally exceeding 700 feet. At McArthur, in Vinton County, the aquifers yield about 300,000 gallons per day for municipal and industrial use, but withdrawal has been accompanied by declining ground-water levels during the past 10 years in a 10-square-mile area. (USGS)","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/ofr82170","usgsCitation":"Norris, S., and Mayer, G., 1982, Water resources of the Black Hand Sandstone Member of the Cuyahoga Formation aquifers of Mississippian age in southeastern Ohio: U.S. Geological Survey Open-File Report 82-170, 77 p. :ill., maps ;28 cm., https://doi.org/10.3133/ofr82170.","productDescription":"77 p. :ill., maps ;28 cm.","costCenters":[],"links":[{"id":142980,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1982/0170/report-thumb.jpg"},{"id":38376,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1982/0170/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e49f4e4b07f02db5f0661","contributors":{"authors":[{"text":"Norris, S.E.","contributorId":43771,"corporation":false,"usgs":true,"family":"Norris","given":"S.E.","email":"","affiliations":[],"preferred":false,"id":161557,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Mayer, G.C.","contributorId":73206,"corporation":false,"usgs":true,"family":"Mayer","given":"G.C.","email":"","affiliations":[],"preferred":false,"id":161558,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":10865,"text":"ofr82911 - 1982 - Effects of urbanization on the magnitude and frequency of floods on small streams in Tennessee; basic data report no. 2","interactions":[{"subject":{"id":23687,"text":"ofr80572 - 1980 - Effects of Urbanization on the Magnitude and Frequency of Floods on Small Streams in Tennessee - Basic Data Report No. 1","indexId":"ofr80572","publicationYear":"1980","noYear":false,"title":"Effects of Urbanization on the Magnitude and Frequency of Floods on Small Streams in Tennessee - Basic Data Report No. 1"},"predicate":"SUPERSEDED_BY","object":{"id":10865,"text":"ofr82911 - 1982 - Effects of urbanization on the magnitude and frequency of floods on small streams in Tennessee; basic data report no. 2","indexId":"ofr82911","publicationYear":"1982","noYear":false,"title":"Effects of urbanization on the magnitude and frequency of floods on small streams in Tennessee; basic data report no. 2"},"id":1}],"lastModifiedDate":"2013-08-12T10:51:53","indexId":"ofr82911","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":"82-911","title":"Effects of urbanization on the magnitude and frequency of floods on small streams in Tennessee; basic data report no. 2","docAbstract":"Peak stages, discharges, and rainfall recorded at 22 gaging stations on streams draining small (less than 25 mi super 2) urbanized basins across Tennessee are presented. The gaged basins are in 17 different municipalities with populations ranging between 5,000 and 100,000. The report gives a description of each gaged site along with a data sheet on which peak stages, discharges, and corresponding rainfall are listed. The description gives the station location, type of gage, basin characteristics, and general remarks. (USGS)","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/ofr82911","usgsCitation":"Robbins, C.H., 1982, Effects of urbanization on the magnitude and frequency of floods on small streams in Tennessee; basic data report no. 2: U.S. Geological Survey Open-File Report 82-911, iii, 28 p. :map ;28 cm., https://doi.org/10.3133/ofr82911.","productDescription":"iii, 28 p. :map ;28 cm.","costCenters":[],"links":[{"id":971,"rank":100,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.water.usgs.gov/ofr_82-911","linkFileType":{"id":5,"text":"html"}},{"id":145078,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":276364,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1982/ofr_82-911/pdf/ofr_82-911_a.pdf"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a26e4b07f02db60fce8","contributors":{"authors":[{"text":"Robbins, Clarence H.","contributorId":44159,"corporation":false,"usgs":true,"family":"Robbins","given":"Clarence","email":"","middleInitial":"H.","affiliations":[],"preferred":false,"id":162097,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":10868,"text":"ofr82277 - 1982 - Principal facts and density estimates for borehole gravity stations in exploratory wells Ue4ah, Ue7j, Ue1h, Ue1q, Ue2co, and USW-H1 at the Nevada Test Site, Nye County, Nevada","interactions":[],"lastModifiedDate":"2012-02-02T00:06:32","indexId":"ofr82277","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":"82-277","title":"Principal facts and density estimates for borehole gravity stations in exploratory wells Ue4ah, Ue7j, Ue1h, Ue1q, Ue2co, and USW-H1 at the Nevada Test Site, Nye County, Nevada","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/ofr82277","usgsCitation":"Robbins, S.L., Schmoker, J., and Hester, T., 1982, Principal facts and density estimates for borehole gravity stations in exploratory wells Ue4ah, Ue7j, Ue1h, Ue1q, Ue2co, and USW-H1 at the Nevada Test Site, Nye County, Nevada: U.S. Geological Survey Open-File Report 82-277, 36 p. :ill., map ;28 cm., https://doi.org/10.3133/ofr82277.","productDescription":"36 p. :ill., map ;28 cm.","costCenters":[],"links":[{"id":143918,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1982/0277/report-thumb.jpg"},{"id":38648,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1982/0277/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ae5e4b07f02db68a7d7","contributors":{"authors":[{"text":"Robbins, S. L.","contributorId":49766,"corporation":false,"usgs":true,"family":"Robbins","given":"S.","email":"","middleInitial":"L.","affiliations":[],"preferred":false,"id":162101,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Schmoker, J. W.","contributorId":69964,"corporation":false,"usgs":true,"family":"Schmoker","given":"J. W.","affiliations":[],"preferred":false,"id":162102,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Hester, T.C.","contributorId":93054,"corporation":false,"usgs":true,"family":"Hester","given":"T.C.","email":"","affiliations":[],"preferred":false,"id":162103,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":77055,"text":"fwsobs82_12 - 1982 - COASTAL*FISH user's guide--a finfish/shellfish information base for Mississippi Sound and Mobile Bay","interactions":[],"lastModifiedDate":"2012-02-02T00:13:56","indexId":"fwsobs82_12","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1982","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":1,"text":"Federal Government Series"},"seriesTitle":{"id":20,"text":"FWS/OBS","active":false,"publicationSubtype":{"id":1}},"seriesNumber":"82/12","title":"COASTAL*FISH user's guide--a finfish/shellfish information base for Mississippi Sound and Mobile Bay","docAbstract":"COASTAL *FISH is a computerized database that includes current information on spawning, nursery areas, migrations, distribution, and environmental requirements of finfish and shellfish. This User's Guide was prepared to access and query the finfish and shell fish database. It provides basic information required to query the database.","language":"ENGLISH","publisher":"U.S. Fish and Wildlife Service","usgsCitation":"Jones, B., and Benson, N., 1982, COASTAL*FISH user's guide--a finfish/shellfish information base for Mississippi Sound and Mobile Bay: FWS/OBS 82/12, 133 p.","productDescription":"133 p.","numberOfPages":"133","costCenters":[{"id":455,"text":"National Wetlands Research Center","active":true,"usgs":true}],"links":[{"id":191074,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e49dbe4b07f02db5e079c","contributors":{"authors":[{"text":"Jones, B.","contributorId":44241,"corporation":false,"usgs":false,"family":"Jones","given":"B.","affiliations":[],"preferred":false,"id":288417,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Benson, N.","contributorId":38238,"corporation":false,"usgs":true,"family":"Benson","given":"N.","affiliations":[],"preferred":false,"id":288416,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":10532,"text":"ofr82721 - 1982 - Juan de Fuca Ridge massive sulfide samples; sample distribution policy","interactions":[],"lastModifiedDate":"2012-02-02T00:06:25","indexId":"ofr82721","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":"82-721","title":"Juan de Fuca Ridge massive sulfide samples; sample distribution policy","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/ofr82721","usgsCitation":"Normark, W.R., and Koski, R., 1982, Juan de Fuca Ridge massive sulfide samples; sample distribution policy: U.S. Geological Survey Open-File Report 82-721, 2 p., 28 cm., https://doi.org/10.3133/ofr82721.","productDescription":"2 p., 28 cm.","costCenters":[],"links":[{"id":142979,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1982/0721/report-thumb.jpg"},{"id":38375,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1982/0721/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b32e4b07f02db6b48e9","contributors":{"authors":[{"text":"Normark, W. R.","contributorId":87137,"corporation":false,"usgs":true,"family":"Normark","given":"W.","email":"","middleInitial":"R.","affiliations":[],"preferred":false,"id":161556,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Koski, R.A.","contributorId":16006,"corporation":false,"usgs":true,"family":"Koski","given":"R.A.","email":"","affiliations":[],"preferred":false,"id":161555,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":10587,"text":"ofr82649 - 1982 - January 1982 water levels, and data related to water-level changes, western and south-central Kansas","interactions":[],"lastModifiedDate":"2012-02-02T00:06:25","indexId":"ofr82649","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":"82-649","title":"January 1982 water levels, and data related to water-level changes, western and south-central Kansas","docAbstract":"Water-level measurements were made, mostly in January 1982, in about 1,530 wells in western and south-central Kansas. The measurements were made in mid-winter when pumping was minimal and water levels had recovered, for the most part, from the effects of pumping during the previous irrigation season. Annual hydrologic data are provided for relating water-level changes from a ' base-reference year ' (predevelopment year), a year of abnormally high rainfall and minimum pumpage (1966 or 1974), and each of seven consecutive years of measurement (1976-82), the ' base-reference year ' is designated as 1940 for the southwestern area, 1944 for the south-central area, and 1950 for the northwestern and west-central areas. Water levels for the ' base-reference year ' are established by measurements made during that year and by interpretation of maps showing water-level altitudes. Data also are provided for relating the average annual water-level changes, saturated thicknesses of the deposits, and percentage changes in saturated thicknesses. (USGS)","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/ofr82649","usgsCitation":"Pabst, M., 1982, January 1982 water levels, and data related to water-level changes, western and south-central Kansas: U.S. Geological Survey Open-File Report 82-649, 167 p. :map ;28 cm., https://doi.org/10.3133/ofr82649.","productDescription":"167 p. :map ;28 cm.","costCenters":[],"links":[{"id":143111,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1982/0649/report-thumb.jpg"},{"id":38413,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1982/0649/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4aa7e4b07f02db666fde","contributors":{"authors":[{"text":"Pabst, M.E.","contributorId":17608,"corporation":false,"usgs":true,"family":"Pabst","given":"M.E.","email":"","affiliations":[],"preferred":false,"id":161637,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":10706,"text":"ofr82405 - 1982 - Gravity observations in the Walker Lake 1 degree x 2 degrees Quadrangle, California-Nevada","interactions":[],"lastModifiedDate":"2012-02-02T00:06:25","indexId":"ofr82405","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":"82-405","title":"Gravity observations in the Walker Lake 1 degree x 2 degrees Quadrangle, California-Nevada","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/ofr82405","usgsCitation":"Plouff, D., 1982, Gravity observations in the Walker Lake 1 degree x 2 degrees Quadrangle, California-Nevada: U.S. Geological Survey Open-File Report 82-405, i, 107 p. :ill., map ;28 cm., https://doi.org/10.3133/ofr82405.","productDescription":"i, 107 p. :ill., map ;28 cm.","costCenters":[],"links":[{"id":143280,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1982/0405/report-thumb.jpg"},{"id":38522,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1982/0405/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4abae4b07f02db672057","contributors":{"authors":[{"text":"Plouff, Donald","contributorId":94657,"corporation":false,"usgs":true,"family":"Plouff","given":"Donald","email":"","affiliations":[],"preferred":false,"id":161831,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":10568,"text":"ofr81128 - 1982 - Sediment and channel-geometry investigations for the Kansas River bank stabilization study, Kansas, Nebraska, and Colorado","interactions":[],"lastModifiedDate":"2012-02-02T00:06:28","indexId":"ofr81128","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":"81-128","title":"Sediment and channel-geometry investigations for the Kansas River bank stabilization study, Kansas, Nebraska, and Colorado","docAbstract":"Analysis of hydrologic data from the Kansas River basin suggests that the channels of the lower Solomon, Saline, and Smoky Hill Rivers have narrowed and stabilized as a result of construction of upstream reservoirs. The Kansas River channel, however, remains relatively unstable and locally active. Streamflow regulation and sediment trapping by reservoirs are possible causes of changes occurring at various Kansas River sites. An inferred deficiency of the suspended-sediment load, however, is likely to cause continuing instability. Suspended sediment in the Kansas River apparently is too sparse to form and maintain stable alluvial banks. The deficiency probably results in an increase of bed material movement, general channel widening, and local braiding. Significant channel degradation is lacking at most sites, but may occur in response to long-term (decades-to-centuries) regulation. Recent degradation near Bonner Springs, Kans., may be the result of sand and gravel removal. Any imposed changes that shorten the channel or reduce the suspended-sediment discharge of the Kansas River are expected to cause additional channel instability. (USGS)","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/ofr81128","usgsCitation":"Osterkamp, W.R., Curtis, R., and Crowther, H., 1982, Sediment and channel-geometry investigations for the Kansas River bank stabilization study, Kansas, Nebraska, and Colorado: U.S. Geological Survey Open-File Report 81-128, 71 p.  :ill., maps ;28 cm., https://doi.org/10.3133/ofr81128.","productDescription":"71 p.  :ill., maps ;28 cm.","costCenters":[],"links":[{"id":144152,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1981/0128/report-thumb.jpg"},{"id":38401,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1981/0128/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b23e4b07f02db6ae003","contributors":{"authors":[{"text":"Osterkamp, W. R.","contributorId":46044,"corporation":false,"usgs":true,"family":"Osterkamp","given":"W.","email":"","middleInitial":"R.","affiliations":[],"preferred":false,"id":161607,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Curtis, R.E.","contributorId":80741,"corporation":false,"usgs":true,"family":"Curtis","given":"R.E.","email":"","affiliations":[],"preferred":false,"id":161608,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Crowther, H.G.","contributorId":86629,"corporation":false,"usgs":true,"family":"Crowther","given":"H.G.","email":"","affiliations":[],"preferred":false,"id":161609,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":10774,"text":"ofr82859 - 1982 - Ground-water levels in Wyoming, 1971 through part of 1980","interactions":[],"lastModifiedDate":"2012-02-02T00:06:20","indexId":"ofr82859","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":"82-859","title":"Ground-water levels in Wyoming, 1971 through part of 1980","docAbstract":"Ground-water levels are measured periodically in a network of about 280 observation wells in Wyoming, mostly in areas where ground water is used in large quantities for irrigation or municipal purposes. The program is conducted by the U.S. Geological Survey in cooperation with the Wyoming State Engineer and the city of Cheyenne. This report contains maps showing the locations of selected wells, tables listing well histories and highest and lowest water levels for the period of record, and hydrographs for most of the wells. (USGS)","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/ofr82859","usgsCitation":"Ragsdale, J.O., 1982, Ground-water levels in Wyoming, 1971 through part of 1980: U.S. Geological Survey Open-File Report 82-859, iv, 203 p. :chiefly ill., maps ;28 cm., https://doi.org/10.3133/ofr82859.","productDescription":"iv, 203 p. :chiefly ill., maps ;28 cm.","costCenters":[],"links":[{"id":142364,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1982/0859/report-thumb.jpg"},{"id":38576,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1982/0859/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4aa9e4b07f02db667f31","contributors":{"authors":[{"text":"Ragsdale, Jess O.","contributorId":61038,"corporation":false,"usgs":true,"family":"Ragsdale","given":"Jess","email":"","middleInitial":"O.","affiliations":[],"preferred":false,"id":161942,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":10715,"text":"ofr82967 - 1982 - Disturbed zones: Indicators of deep-seated subsurface faults in the Valley and Ridge and Appalachian structural front of Pennsylvania","interactions":[],"lastModifiedDate":"2021-12-17T20:26:15.820299","indexId":"ofr82967","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":"82-967","title":"Disturbed zones: Indicators of deep-seated subsurface faults in the Valley and Ridge and Appalachian structural front of Pennsylvania","docAbstract":"Field studies of geologic structures in the Valley and Ridge and adjacent parts of the Appalachian Plateau provinces in Pennsylvania have shown a new type of structure, formerly poorly understood and frequently unmapped, is a significant indicator of deep-seated subsurface faulting. These structures, herein called disturbed zones, are formed by movement between closely spaced pairs of thrust faults. Disturbed zones are characterized at the surface by long, narrow, intensely folded and faulted zones of rocks in a relatively undisturbed stratigraphic sequence. These zones are frequently kilometers to tens of kilometers long and tens to hundreds of meters wide. Although disturbed zones generally occur in sequences of alternating siltstone and shale beds, they can also occur in other lithologies including massively-bedded sandstones and carbonates. \r\n\r\nDisturbed zones are not only easily recognized in outcrop but their presence can also be inferred on geologic maps by disharmonic fold patterns, which necessitates a detachment between adjacent units that show the disharmony. \r\n\r\nA number of geologic problems can be clarified by understanding the principles of the sequence of formation and the method of location of disturbed zones, including the interpretation of some published geologic cross sections and maps. \r\n\r\nThe intense folding and faulting which accompanies the formation of a typical disturbed zone produces a region of fracture porosity which, if sealed off from the surface, might well serve as a commercially-exploitable hydrocarbon trap. We believe that the careful mapping of concentrations of disturbed zones can serve as an important exploration method which is much less expensive than speculation seismic lines.","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr82967","usgsCitation":"Pohn, H.A., and Purdy, T.L., 1982, Disturbed zones: Indicators of deep-seated subsurface faults in the Valley and Ridge and Appalachian structural front of Pennsylvania: U.S. Geological Survey Open-File Report 82-967, Report: 87 p.; 1 Plate: 29.75 × 30.57 inches, https://doi.org/10.3133/ofr82967.","productDescription":"Report: 87 p.; 1 Plate: 29.75 × 30.57 inches","costCenters":[],"links":[{"id":393053,"rank":4,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_13879.htm"},{"id":38526,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1982/0967/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":38525,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1982/0967/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":143310,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1982/0967/report-thumb.jpg"}],"country":"United States","state":"Pennsylvania","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -78.875,\n              39.75\n            ],\n            [\n              -76.75,\n              39.75\n            ],\n            [\n              -76.75,\n              41.3750\n            ],\n            [\n              -78.875,\n              41.3750\n            ],\n            [\n              -78.875,\n              39.75\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a6be4b07f02db63d8d3","contributors":{"authors":[{"text":"Pohn, Howard A.","contributorId":66681,"corporation":false,"usgs":true,"family":"Pohn","given":"Howard","email":"","middleInitial":"A.","affiliations":[],"preferred":false,"id":161845,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Purdy, Terri L.","contributorId":87950,"corporation":false,"usgs":true,"family":"Purdy","given":"Terri","email":"","middleInitial":"L.","affiliations":[],"preferred":false,"id":161846,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":10816,"text":"ofr8262 - 1982 - Earthquake hazard and prediction in NW Mexico and the California/Mexico border","interactions":[],"lastModifiedDate":"2012-02-02T00:06:33","indexId":"ofr8262","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":"82-62","title":"Earthquake hazard and prediction in NW Mexico and the California/Mexico border","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/ofr8262","usgsCitation":"Reichle, M., and Brune, J., 1982, Earthquake hazard and prediction in NW Mexico and the California/Mexico border: U.S. Geological Survey Open-File Report 82-62, 30 p., ill. ;28 cm., https://doi.org/10.3133/ofr8262.","productDescription":"30 p., ill. ;28 cm.","costCenters":[],"links":[{"id":144002,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1982/0062/report-thumb.jpg"},{"id":38624,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1982/0062/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a51e4b07f02db62982c","contributors":{"authors":[{"text":"Reichle, Michael","contributorId":23954,"corporation":false,"usgs":true,"family":"Reichle","given":"Michael","affiliations":[],"preferred":false,"id":162016,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Brune, J.N.","contributorId":49362,"corporation":false,"usgs":true,"family":"Brune","given":"J.N.","email":"","affiliations":[],"preferred":false,"id":162017,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":10787,"text":"ofr82829 - 1982 - Organic geochemistry of sediments on the flanks of Tanner and Cortes banks offshore from southern California","interactions":[],"lastModifiedDate":"2012-02-02T00:06:34","indexId":"ofr82829","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":"82-829","title":"Organic geochemistry of sediments on the flanks of Tanner and Cortes banks offshore from southern California","docAbstract":"Holocene sediment, composed mainly of foram tests, occurs on the flanks of the Tanner and Cortes Banks, offshore southern California. The organic matter in this sediment differs in content and composition from the organic matter in nearby basins. Two sources of hydrocarbons are indicated: terrestrial plants and biodegraded or immature petroleum.","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/ofr82829","usgsCitation":"Rapp, J.B., and Kvenvolden, K., 1982, Organic geochemistry of sediments on the flanks of Tanner and Cortes banks offshore from southern California: U.S. Geological Survey Open-File Report 82-829, 18 p., ill., map ;28 cm., https://doi.org/10.3133/ofr82829.","productDescription":"18 p., ill., map ;28 cm.","costCenters":[],"links":[{"id":144867,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1982/0829/report-thumb.jpg"},{"id":38585,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1982/0829/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ae5e4b07f02db68a890","contributors":{"authors":[{"text":"Rapp, J. B.","contributorId":28987,"corporation":false,"usgs":true,"family":"Rapp","given":"J.","email":"","middleInitial":"B.","affiliations":[],"preferred":false,"id":161961,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Kvenvolden, K.A.","contributorId":80674,"corporation":false,"usgs":true,"family":"Kvenvolden","given":"K.A.","email":"","affiliations":[],"preferred":false,"id":161962,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":59918,"text":"mf1443 - 1982 - Detailed bathymetric map of the United States continental slope between Lindenkohl Canyon and Toms Canyon, offshore New Jersey","interactions":[],"lastModifiedDate":"2019-05-29T14:32:30","indexId":"mf1443","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":"1443","title":"Detailed bathymetric map of the United States continental slope between Lindenkohl Canyon and Toms Canyon, offshore New Jersey","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Reston, VA","doi":"10.3133/mf1443","usgsCitation":"Kirby, J., Robb, J.M., and Hampson, J., 1982, Detailed bathymetric map of the United States continental slope between Lindenkohl Canyon and Toms Canyon, offshore New Jersey: U.S. Geological Survey Miscellaneous Field Studies Map 1443, 1 map ;102 x 98 cm. folded in envleope 25 x 32 cm., https://doi.org/10.3133/mf1443.","productDescription":"1 map ;102 x 98 cm. folded in envleope 25 x 32 cm.","costCenters":[],"links":[{"id":364233,"rank":2,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/mf/1443/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":180010,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/mf/1443/report-thumb.jpg"}],"scale":"0","country":"United States","state":"New Jersey","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -73,38.833333333333336 ], [ -73,39.083333333333336 ], [ -72.33333333333333,39.083333333333336 ], [ -72.33333333333333,38.833333333333336 ], [ -73,38.833333333333336 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4aa8e4b07f02db667c7a","contributors":{"authors":[{"text":"Kirby, J.R.","contributorId":6428,"corporation":false,"usgs":true,"family":"Kirby","given":"J.R.","email":"","affiliations":[],"preferred":false,"id":262830,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Robb, James M.","contributorId":73272,"corporation":false,"usgs":true,"family":"Robb","given":"James","email":"","middleInitial":"M.","affiliations":[{"id":678,"text":"Woods Hole Coastal and Marine Science Center","active":true,"usgs":true}],"preferred":false,"id":262831,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Hampson, J.C. Jr.","contributorId":87945,"corporation":false,"usgs":true,"family":"Hampson","given":"J.C.","suffix":"Jr.","affiliations":[],"preferred":false,"id":262832,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":11670,"text":"ofr82225 - 1982 - Design review, Trans-Alaska Oil Pipeline, 1974-1976","interactions":[],"lastModifiedDate":"2012-02-02T00:06:33","indexId":"ofr82225","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":"82-225","title":"Design review, Trans-Alaska Oil Pipeline, 1974-1976","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/ofr82225","usgsCitation":"Williams, J., 1982, Design review, Trans-Alaska Oil Pipeline, 1974-1976: U.S. Geological Survey Open-File Report 82-225, 140 p. in various pagings :ill. ;28 cm., https://doi.org/10.3133/ofr82225.","productDescription":"140 p. in various pagings :ill. ;28 cm.","costCenters":[],"links":[{"id":144784,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1982/0225/report-thumb.jpg"},{"id":39530,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1982/0225/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4aa8e4b07f02db667a2c","contributors":{"authors":[{"text":"Williams, John R.","contributorId":41832,"corporation":false,"usgs":true,"family":"Williams","given":"John R.","affiliations":[],"preferred":false,"id":163548,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":10531,"text":"ofr82200A - 1982 - Geologic setting of massive sulfide deposits and hydrothermal vents along the southern Juan de Fuca Ridge","interactions":[],"lastModifiedDate":"2012-02-02T00:06:25","indexId":"ofr82200A","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":"82-200","chapter":"A","title":"Geologic setting of massive sulfide deposits and hydrothermal vents along the southern Juan de Fuca Ridge","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/ofr82200A","usgsCitation":"Normark, W.R., Morton, J.L., and Delaney, J., 1982, Geologic setting of massive sulfide deposits and hydrothermal vents along the southern Juan de Fuca Ridge: U.S. Geological Survey Open-File Report 82-200, 22 p., ill., maps ;28 cm., https://doi.org/10.3133/ofr82200A.","productDescription":"22 p., ill., maps ;28 cm.","costCenters":[],"links":[{"id":142978,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1982/0200a/report-thumb.jpg"},{"id":38374,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1982/0200a/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ae0e4b07f02db6882a1","contributors":{"authors":[{"text":"Normark, W. R.","contributorId":87137,"corporation":false,"usgs":true,"family":"Normark","given":"W.","email":"","middleInitial":"R.","affiliations":[],"preferred":false,"id":161554,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Morton, J. L.","contributorId":56196,"corporation":false,"usgs":true,"family":"Morton","given":"J.","email":"","middleInitial":"L.","affiliations":[],"preferred":false,"id":161553,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Delaney, J.R.","contributorId":10427,"corporation":false,"usgs":true,"family":"Delaney","given":"J.R.","email":"","affiliations":[],"preferred":false,"id":161552,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":10110,"text":"ofr821091 - 1982 - Heavy-mineral variability in beach and dune sands in the vicinity of the mouth of the Columbia River","interactions":[],"lastModifiedDate":"2012-02-02T00:06:38","indexId":"ofr821091","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":"82-1091","title":"Heavy-mineral variability in beach and dune sands in the vicinity of the mouth of the Columbia River","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/ofr821091","usgsCitation":"Luepke, G., 1982, Heavy-mineral variability in beach and dune sands in the vicinity of the mouth of the Columbia River: U.S. Geological Survey Open-File Report 82-1091, 18 p. :map ;28 cm., https://doi.org/10.3133/ofr821091.","productDescription":"18 p. :map ;28 cm.","costCenters":[],"links":[{"id":144588,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1982/1091/report-thumb.jpg"},{"id":37959,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1982/1091/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a6ae4b07f02db63c87c","contributors":{"authors":[{"text":"Luepke, Gretchen","contributorId":91827,"corporation":false,"usgs":true,"family":"Luepke","given":"Gretchen","email":"","affiliations":[],"preferred":false,"id":160832,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":10385,"text":"ofr82409 - 1982 - Three-dimensional modeling of the Nevada Test Site and vicinity from teleseismic P-wave residuals","interactions":[],"lastModifiedDate":"2012-02-02T00:06:20","indexId":"ofr82409","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":"82-409","title":"Three-dimensional modeling of the Nevada Test Site and vicinity from teleseismic P-wave residuals","docAbstract":"A teleseismic P-wave travel-time residual study is described which reveals the regional compressional-velocity structure of southern Nevada and neighboring parts of California to a depth of 280 km. During 1980, 98 teleseismic events were recorded at as many as 53 sites in this area. P-wave residuals were calculated relative to a network-wide average residual for each event and are displayed on maps of the stations for each of four event-azimuth quadrants. Fluctuations in these map-patterns of residuals with approach azimuth combined with results of linear, three-dimensional inversions of some 2887 residuals indicate the following characteristics of the velocity structure of the southern Nevada region: 1) a low-velocity body exists in the upper crust 50 km northeast of Beatty, Nevada, near the Miocene Timber Mountain-Silent Canyon caldera complex. Another highly-localized low-velocity anomaly occurs near the southwest corner of the Nevada Test Site (NTS). These two anomalies seem to be part of a low-velocity trough extending from Death Valley, California, to about 50 km north of NTS. 2) There is a high-velocity body in the mantle between 81 and 131 km deep centered about i0 km north of the edge of the Timber Mountain caldera, 3) a broad low-velocity body is delineated between 81 and 131 km deep centered about 30 km north of Las Vegas, 4) there is a monotonic increase in travel-time delays from west to east across the region, probably indicating an eastward decrease in velocity, and lower than average velocities in southeastern Nevada below 31 km, and 5) considerable complexity in three-dimensional velocity structure exists in this part of the southern Great Basin. \r\n\r\nInversions of teleseismic P-wave travel-time residuals were also performed on data from 12 seismometers in the immediate vicinity of the Nevada Test Site to make good use of the closer station spacing i in that area. Results of these inversions show more details of the velocity structure but generally the same features as those found in the regional study.","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/ofr82409","usgsCitation":"Monfort, M.E., and Evans, J.R., 1982, Three-dimensional modeling of the Nevada Test Site and vicinity from teleseismic P-wave residuals: U.S. Geological Survey Open-File Report 82-409, 70 p. :ill. ;28 cm., https://doi.org/10.3133/ofr82409.","productDescription":"70 p. :ill. ;28 cm.","costCenters":[],"links":[{"id":142336,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1982/0409/report-thumb.jpg"},{"id":38215,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1982/0409/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a53e4b07f02db62b857","contributors":{"authors":[{"text":"Monfort, Mary E.","contributorId":93491,"corporation":false,"usgs":true,"family":"Monfort","given":"Mary","email":"","middleInitial":"E.","affiliations":[],"preferred":false,"id":161296,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Evans, John R. jrevans@usgs.gov","contributorId":529,"corporation":false,"usgs":true,"family":"Evans","given":"John","email":"jrevans@usgs.gov","middleInitial":"R.","affiliations":[{"id":237,"text":"Earthquake Science Center","active":true,"usgs":true}],"preferred":true,"id":161295,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":10924,"text":"ofr82745 - 1982 - A survey of asbestos-related disease in trades and mining occupations and in factory and mining communities as a means of predicting health risks of nonoccupational exposure to fibrous minerals","interactions":[],"lastModifiedDate":"2012-02-02T00:06:21","indexId":"ofr82745","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":"82-745","title":"A survey of asbestos-related disease in trades and mining occupations and in factory and mining communities as a means of predicting health risks of nonoccupational exposure to fibrous minerals","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/ofr82745","usgsCitation":"Ross, M., 1982, A survey of asbestos-related disease in trades and mining occupations and in factory and mining communities as a means of predicting health risks of nonoccupational exposure to fibrous minerals: U.S. Geological Survey Open-File Report 82-745, 51 p., ill. ;28 cm., https://doi.org/10.3133/ofr82745.","productDescription":"51 p., ill. ;28 cm.","costCenters":[],"links":[{"id":142480,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1982/0745/report-thumb.jpg"},{"id":38690,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1982/0745/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b17e4b07f02db6a5e62","contributors":{"authors":[{"text":"Ross, Malcolm","contributorId":100372,"corporation":false,"usgs":true,"family":"Ross","given":"Malcolm","email":"","affiliations":[],"preferred":false,"id":162213,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":11361,"text":"ofr82297 - 1982 - An alternative hypothesis for sink development above salt cavities in the Detroit area","interactions":[],"lastModifiedDate":"2012-02-02T00:06:20","indexId":"ofr82297","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":"82-297","title":"An alternative hypothesis for sink development above salt cavities in the Detroit area","docAbstract":"Subsidence and sink formation resulting from brining operations in the Windsor-Detroit area include the 1954 sink at the Canadian Salt Company brine field near Windsor, Ontario, and the 1971 sinks at the BASF Wyandotte Corporation brine field at Grosse Ile, Mich. Earlier investigations into both occurrences concluded that the mechanism of sink development consisted of the gradual stoping of poorly supported brine-gallery roof rock to the near surface with subsequent surface collapse. A more recent study attempted to describe the mechanism of sink development in terms of the geometry of a cylindrical chimney formed by stoping of roof rock, the height of a cavity at depth, the depth of overlying rock, and the bulking ratio of the rubble formed during stoping. \r\n\r\nPersons with extensive experience in solution mining in the Windsor-Detroit area have expressed doubt that the stoping mechanism could fully explain the development of these sinks. Further, they have proposed that the relatively shallow (300-ft-deep) Sylvania Sandstone, in this case, may be responsible for the sinks by a secondary undermining mechanism to be examined in this paper. The mechanism involves downwarping of the beds overlying the salt cavity and development of a shallower cavity in the Sylvania Sandstone by downward migration of cohesionless sand grains from the Sylvania through openings in the disturbed rock to the lower cavity. This study indicates that under natural conditions the Sylvania will not migrate, even in the presence of large underground water flows because the sandstone possesses some cohesion throughout its depth. However, further investigation has formulated a mechanism that could allow the Sylvania Sandstone to loose its cohesion in response to high horizontal stresses. These stresses could be the result of deformation that accompanies general subsidence and (or) of past geologic processes.\r\n\r\nIncluded in this study were experimental and analytical investigations. As determined by uniaxial and triaxial testing, the Sylvania Sandstone in the Detroit area has been shown to have low compressive strength. In addition, it exhibits an explosive type failure whereby over 50 percent of the sample is reduced to loose granular sand. As a result of these characteristics, the Sylvania Sandstone can loose its cohesion when subjected to high horizontal stresses. \r\n\r\nEfforts at mechanically modeling the Sylvania were made to account for the measurements and observations. Linear arch theory was used for an elastic analysis. Linear arch theory predicts two modes of failure: (1) arch crushing, a compressive failure of the upper portion of the arch due to compressive stresses exceeding the compressive strength of the material, and (2) arch collapse, a sagging of the beds due to compressive strains which reduce the arch line to a length less than the original arch length. The arch crushing mode of failure would then yield the loose granular sand as observed in laboratory testing. Arch collapse would simply result in bed sagging without granulation of the sandstone. Arch collapse is favored by thin-bedded material while arch crushing is favored by thick-bedded material. Arch crushing seems to be a likely mode of failure for the Windsor-Detroit sinks. \r\n\r\nIt is believed that after a crushing failure the sand-water slurry (specific gravity 1.2) which exceeds the density of the cavity brine will migrate downward through cracks and open joints eventually reaching the practically limitless open spaces of the rubble column and salt cavity. As the extent of the cavity within the Sylvania increases in depth and width because of sand migration, a critical span will be reached where the immediately overlying upper Sylvania and the overlying Detroit River Dolomite will fail. The collapse will allow a path for the approximately 100 ft of clay to collapse, resulting in a sink as the surface manifestation.","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/ofr82297","usgsCitation":"Stump, D., Nieto, A., and Ege, J., 1982, An alternative hypothesis for sink development above salt cavities in the Detroit area: U.S. Geological Survey Open-File Report 82-297, 65 p., ill., map ;28 cm., https://doi.org/10.3133/ofr82297.","productDescription":"65 p., ill., map ;28 cm.","costCenters":[],"links":[{"id":142525,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1982/0297/report-thumb.jpg"},{"id":39188,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1982/0297/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4adbe4b07f02db685bad","contributors":{"authors":[{"text":"Stump, Daniel","contributorId":35318,"corporation":false,"usgs":true,"family":"Stump","given":"Daniel","email":"","affiliations":[],"preferred":false,"id":163001,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Nieto, A.S.","contributorId":30629,"corporation":false,"usgs":true,"family":"Nieto","given":"A.S.","email":"","affiliations":[],"preferred":false,"id":163000,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Ege, J. R.","contributorId":106117,"corporation":false,"usgs":false,"family":"Ege","given":"J. R.","affiliations":[],"preferred":false,"id":163002,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":9397,"text":"ofr82725 - 1982 - Literature powder data reflections and abbreviated bibliography for selected zeolites; computer formatted data file","interactions":[],"lastModifiedDate":"2012-02-02T00:06:17","indexId":"ofr82725","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":"82-725","title":"Literature powder data reflections and abbreviated bibliography for selected zeolites; computer formatted data file","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/ofr82725","usgsCitation":"Hauff, P.L., and Phillips, R., 1982, Literature powder data reflections and abbreviated bibliography for selected zeolites; computer formatted data file: U.S. Geological Survey Open-File Report 82-725, 90 p., ill. ;28 cm., https://doi.org/10.3133/ofr82725.","productDescription":"90 p., ill. ;28 cm.","costCenters":[],"links":[{"id":142924,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1982/0725/report-thumb.jpg"},{"id":37113,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1982/0725/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b15e4b07f02db6a4eb2","contributors":{"authors":[{"text":"Hauff, P. L.","contributorId":95470,"corporation":false,"usgs":true,"family":"Hauff","given":"P.","email":"","middleInitial":"L.","affiliations":[],"preferred":false,"id":159615,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Phillips, R.H.","contributorId":79475,"corporation":false,"usgs":true,"family":"Phillips","given":"R.H.","email":"","affiliations":[],"preferred":false,"id":159614,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":10302,"text":"ofr82650 - 1982 - Water quality of Belton Lake, central Texas","interactions":[],"lastModifiedDate":"2016-08-11T15:16:38","indexId":"ofr82650","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":"82-650","title":"Water quality of Belton Lake, central Texas","docAbstract":"<p>The concentrations of dissolved solids, chloride, and sulfate in Belton Lake on the Leon River in central Texas average about 240 milligrams per liter, 40 milligrams per liter, and 30 milligrams per liter, respectively. The water is hard or very hard, averaging 170 milligrams per liter as calcium carbonate. The average concentrations of these constituents and hardness are least during late summer and early fall after periods of sustained high inflow.</p>\n<p>Thermal stratification begins to develop in Belton Lake in late February or early March. The water usually is stratified into three fairly distinct layers by early June, and stratification usually persists until September or October. Thermal stratification and seasonal variations in the concentrations of dissolved constituents in inflow result in stratification of the principal dissolved constituents. Dissolved solids in water at the surface of deep sites during summer differ from those at the bottom by about 40 milligrams per liter. Thermal stratification also results in significant seasonal and areal variations in dissolved oxygen, dissolved iron, dissolved manganese, total inorganic nitrogen, and total phosphorus.</p>\n<p>Oxygen used in the oxidation of dead organisms and other organic material near the bottom of the lake is not replaced during periods of summer stagnation. Consequently, water below depths of 35 to 40 feet (10.7 to 12.2 meters) usually contains less than 1.0 milligram per liter of dissolved oxygen during these periods.</p>\n<p>Water near the surface at most sites in the lake throughout the year usually contains less than 30 micrograms per liter of dissolved iron and 20 micrograms per liter of dissolved manganese. Reducing conditions during periods of summer stagnation result in tile dissolution of iron and manganese from the sediments in deep areas of the lake. The concentrations of both constituents are greatest near the bottom at site Ac, a deep site near Belton Dam. Iron concentrations at this site during the summer have ranged from 0 to 600 micrograms per liter and have averaged about 290 micrograms per liter; manganese concentrations have ranged from 0 to 540 micrograms per liter and have averaged about 320 micrograms per liter.</p>\n<p>Concentrations of total inorganic nitrogen and total phosphorus are greatest at deep sites during periods of summer stagnation when decay of aquatic organisms and chemical reduction of bottom sediments release the constituents to the water. The concentrations of total inorganic nitrogen and total phosphorus in the bottom stratum of water at site A c during the summer average about 0.75 milligram per liter of nitrogen and 0.10 milligram per liter of phosphorus. The concentrations of these constituents in the surface stratum at site A C during the summer average about 0.02 milligram per liter of nitrogen and 0.01 milligram per liter of phosphorus.</p>\n<p>The maximum concentrations of chlorinated hydrocarbon insecticides or their degradation products detected in bottom sediments collected from the lake during four lake surveys included 1.1 micrograms per kilogram of DDT, 3.0 micrograms per kilogram of DDD, 11 micrograms per kilogram of DDE, and 2 micrograms per kilogram of chlordane.</p>","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Austin, TX","doi":"10.3133/ofr82650","usgsCitation":"Mendieta, H., and Pate, D.L., 1982, Water quality of Belton Lake, central Texas: U.S. Geological Survey Open-File Report 82-650, Report: vi, 70 p.; Plate: 10.52 x 16.63 inches, https://doi.org/10.3133/ofr82650.","productDescription":"Report: vi, 70 p.; Plate: 10.52 x 16.63 inches","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[{"id":583,"text":"Texas Water Science Center","active":true,"usgs":true}],"links":[{"id":38160,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1982/0650/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":38161,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1982/0650/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":144093,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1982/0650/report-thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e478fe4b07f02db48a09f","contributors":{"authors":[{"text":"Mendieta, H.B.","contributorId":38965,"corporation":false,"usgs":true,"family":"Mendieta","given":"H.B.","email":"","affiliations":[],"preferred":false,"id":161164,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Pate, Dale L.","contributorId":55007,"corporation":false,"usgs":true,"family":"Pate","given":"Dale","email":"","middleInitial":"L.","affiliations":[],"preferred":false,"id":161165,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":10641,"text":"ofr82158 - 1982 - Hydrologic data for urban studies in the San Antonio, Texas, metropolitan area, 1979-80","interactions":[],"lastModifiedDate":"2017-03-29T14:28:14","indexId":"ofr82158","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":"82-158","title":"Hydrologic data for urban studies in the San Antonio, Texas, metropolitan area, 1979-80","docAbstract":"<p>Hydrologic investigations of urban drainage basins in Texas were begun by the U.S. Geological Survey in 1954. These studies are now in progress in Austin, Houston, and San Antonio. Studies were completed in the Fort Worth metropolitan area at the end of the 1977 water year, and in the Dallas metropolitan area at the end of the 1979 water year.</p>\n<p>The Geological Survey, in cooperation with the Texas Department of Water Resources, expanded the existing streamflow network in the San Antonio metropolitan area in May 1968 to begin urban hydrology studies in this area. In September 1968, the program was further expanded to include the collection of water-quality data.</p>\n<p>The operation and maintenance of stations 08178000, San Antonio River at San Antonio; 08178700, Salado Creek (upper station) at San Antonio; and 08178800, Sal ado Creek (lower station) at San Antonio are funded by the San Antonio River Authority in conjunction with the Texas Department of Water Resources and the U.S. Geological Survey.</p>\n<p>The operation and maintenance and collection of water-quality data at station 08178720, Lorence Creek at Thousand Oaks Blvd., San Antonio, station 08178640, West Elm Creek at San Antonio, and station 08178645, East Eln Creek at San Antonio, are funded by the Edwards Underground Water District in cooperation with the Texas Department of Water Resources and the U.S. Geological Survey. Station 08178640, West Elm Creek at San Antonio, and station 08178645, East Elm Creek at San Antonio will provide hydrologic data on similar and adjacent watersheds. The West Elm watershed is still predominately rural but is undergoing extensive urbanization in some areas. The East Elm watershed is relatively stable and undeveloped.</p>\n<p>The objectives of the San Antonio urban hydrology study are:</p>\n<ol>\n<li>To provide data showing the effects of various stages of urbanization on flood discharge and runoff.</li>\n<li>To provide water-quality data on surface-water runoff from floods of various magnitudes, during all seasons of the year from areas with different types of urban development.</li>\n</ol>\n<p>Annual publication of the San Antonio urban studies was initiated in 1969.</p>\n<p>A defination of terms related to streamflow, water quality, and other hydrologic data, as used in this report, are defined in the U.S. Geological Survey's 1979 and 1980 \"Water resources data for Texas\" reports.</p>","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Austin, TX","doi":"10.3133/ofr82158","collaboration":"Prepared in cooperation with the Texas Department of Water Resources","usgsCitation":"Perez, R., 1982, Hydrologic data for urban studies in the San Antonio, Texas, metropolitan area, 1979-80: U.S. Geological Survey Open-File Report 82-158, 125 p., https://doi.org/10.3133/ofr82158.","productDescription":"125 p.","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[{"id":583,"text":"Texas Water Science Center","active":true,"usgs":true}],"links":[{"id":38475,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1982/0158/report.pdf","text":"Report","size":"2.41 MB","linkFileType":{"id":1,"text":"pdf"},"description":"Report"},{"id":144072,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1982/0158/report-thumb.jpg"}],"country":"United States","state":"Texas","city":"San Antonio","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -98.8165283203125,\n              29.123373210819224\n            ],\n            [\n              -98.19580078125,\n              29.123373210819224\n            ],\n            [\n              -98.19580078125,\n              29.699982298744377\n            ],\n            [\n              -98.8165283203125,\n              29.699982298744377\n            ],\n            [\n              -98.8165283203125,\n              29.123373210819224\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a1ce4b07f02db607eb9","contributors":{"authors":[{"text":"Perez, Roberto","contributorId":97114,"corporation":false,"usgs":true,"family":"Perez","given":"Roberto","email":"","affiliations":[],"preferred":false,"id":161727,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":8885,"text":"ofr82467 - 1982 - Semiquantitative spectrographic analyses of rocks from the Mount Jordan vicinity, Custer County, Idaho","interactions":[],"lastModifiedDate":"2017-06-28T11:55:26","indexId":"ofr82467","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":"82-467","title":"Semiquantitative spectrographic analyses of rocks from the Mount Jordan vicinity, Custer County, Idaho","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr82467","usgsCitation":"Foster, F., and Cooley, E., 1982, Semiquantitative spectrographic analyses of rocks from the Mount Jordan vicinity, Custer County, Idaho: U.S. Geological Survey Open-File Report 82-467, 13 p., maps ;28 cm., https://doi.org/10.3133/ofr82467.","productDescription":"13 p., maps ;28 cm.","costCenters":[{"id":532,"text":"Pennsylvania Water Science Center","active":true,"usgs":true}],"links":[{"id":36449,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1982/0467/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":142674,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1982/0467/report-thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e49ffe4b07f02db5f7a1a","contributors":{"authors":[{"text":"Foster, Fess","contributorId":94308,"corporation":false,"usgs":true,"family":"Foster","given":"Fess","email":"","affiliations":[],"preferred":false,"id":158487,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Cooley, E.F.","contributorId":83072,"corporation":false,"usgs":true,"family":"Cooley","given":"E.F.","email":"","affiliations":[],"preferred":false,"id":158486,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
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