{"pageNumber":"5319","pageRowStart":"132950","pageSize":"25","recordCount":184757,"records":[{"id":10555,"text":"ofr8278 - 1982 - Low-level radioactive-waste burial at the Palos Forest Preserve, Illinois; Part II, geology and hydrology of the glacial drift as related to the migration of tritium","interactions":[{"subject":{"id":10555,"text":"ofr8278 - 1982 - Low-level radioactive-waste burial at the Palos Forest Preserve, Illinois; Part II, geology and hydrology of the glacial drift as related to the migration of tritium","indexId":"ofr8278","publicationYear":"1982","noYear":false,"title":"Low-level radioactive-waste burial at the Palos Forest Preserve, Illinois; Part II, geology and hydrology of the glacial drift as related to the migration of tritium"},"predicate":"SUPERSEDED_BY","object":{"id":2414,"text":"wsp2226 - 1984 - Low-level radioactive-waste burial at the Palos Forest Preserve, Illinois: Geology and hydrology of the glacial drift, as related to the migration of tritium","indexId":"wsp2226","publicationYear":"1984","noYear":false,"title":"Low-level radioactive-waste burial at the Palos Forest Preserve, Illinois: Geology and hydrology of the glacial drift, as related to the migration of tritium"},"id":1}],"supersededBy":{"id":2414,"text":"wsp2226 - 1984 - Low-level radioactive-waste burial at the Palos Forest Preserve, Illinois: Geology and hydrology of the glacial drift, as related to the migration of tritium","indexId":"wsp2226","publicationYear":"1984","noYear":false,"title":"Low-level radioactive-waste burial at the Palos Forest Preserve, Illinois: Geology and hydrology of the glacial drift, as related to the migration of tritium"},"lastModifiedDate":"2019-11-07T11:35:12","indexId":"ofr8278","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":"82-78","title":"Low-level radioactive-waste burial at the Palos Forest Preserve, Illinois; Part II, geology and hydrology of the glacial drift as related to the migration of tritium","docAbstract":"<p>No abstract available.&nbsp;</p>","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Reston, VA","doi":"10.3133/ofr8278","usgsCitation":"Olimpio, J., 1982, Low-level radioactive-waste burial at the Palos Forest Preserve, Illinois; Part II, geology and hydrology of the glacial drift as related to the migration of tritium: U.S. Geological Survey Open-File Report 82-78, v, 57 p., https://doi.org/10.3133/ofr8278.","productDescription":"v, 57 p.","costCenters":[],"links":[{"id":142501,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1982/0078/report-thumb.jpg"},{"id":369038,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1982/0078/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"country":"United States","state":"Illinois","otherGeospatial":"Palos Forest Preserve","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -87.9290771484375,\n              41.66162721430806\n            ],\n            [\n              -87.83294677734375,\n              41.66162721430806\n            ],\n            [\n              -87.83294677734375,\n              41.72213058512578\n            ],\n            [\n              -87.9290771484375,\n              41.72213058512578\n            ],\n            [\n              -87.9290771484375,\n              41.66162721430806\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a7fe4b07f02db64880f","contributors":{"authors":[{"text":"Olimpio, J.C.","contributorId":36137,"corporation":false,"usgs":true,"family":"Olimpio","given":"J.C.","email":"","affiliations":[],"preferred":false,"id":161585,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":10554,"text":"ofr82692 - 1982 - Data for wells at the low-level radioactive-waste burial site in the Palos Forest Preserve, Illinois","interactions":[],"lastModifiedDate":"2012-02-02T00:06:20","indexId":"ofr82692","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":"82-692","title":"Data for wells at the low-level radioactive-waste burial site in the Palos Forest Preserve, Illinois","docAbstract":"The U.S. Geological Survey is studying the geologic, hydrologic, and geochemical properties of the glacial drift and underlying bedrock at a low-level radioactive-waste burial site in the Palos Forest Preserve, 22 kilometers southwest of Chicago. Data collected from the 33 test wells drilled into the drift plus data from 4 wells drilled into the underlying dolomite bedrock are presented. Data include maps showing the location of the test wells, a general description of the drift, well-construction information, and lithologic descriptions of cores from the wells finished in the drift.","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/ofr82692","usgsCitation":"Olimpio, J., 1982, Data for wells at the low-level radioactive-waste burial site in the Palos Forest Preserve, Illinois: U.S. Geological Survey Open-File Report 82-692, iii, 101 p., ill., map ;28 cm., https://doi.org/10.3133/ofr82692.","productDescription":"iii, 101 p., ill., map ;28 cm.","costCenters":[],"links":[{"id":142500,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1982/0692/report-thumb.jpg"},{"id":38392,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1982/0692/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ac9e4b07f02db67c902","contributors":{"authors":[{"text":"Olimpio, J.C.","contributorId":36137,"corporation":false,"usgs":true,"family":"Olimpio","given":"J.C.","email":"","affiliations":[],"preferred":false,"id":161584,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":28409,"text":"wri824087 - 1982 - Suspended sediment in selected streams of southeastern Montana","interactions":[],"lastModifiedDate":"2012-02-02T00:08:50","indexId":"wri824087","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":"82-4087","title":"Suspended sediment in selected streams of southeastern Montana","docAbstract":"The relatively flat Badger Road area near Fairbanks occupies part of the alluvial plain of the Chena and Tanana Rivers and is underlain by scattered areas of permafrost. The water table of the high-transmissivity aquifer that underlies the area is generally shallower than 15 feet, fluctuates seasonally about 2 feet, and slopes northwesterly, the direction of ground-water flow. Private domestic-supply wells obtain water from the upper part of the aquifer. Septic systems used to dispose of waste water are installed at or only slightly above the water table in the same aquifer. Analyses of samples from 16 observation wells in undeveloped parts of the study area and from 33 domestic wells indicated that water quality has not been significantly degraded by on-site waste disposal. Three samples had detectable but minor contamination by fecal coliform bacteria. Anomalous values of chloride and ammonia in one third of the domestic wells may indicate incipient degradation of ground-water quality by septic-tank effluent. (USGS)","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/wri824087","usgsCitation":"Litke, D.W., 1982, Suspended sediment in selected streams of southeastern Montana: U.S. Geological Survey Water-Resources Investigations Report 82-4087, v, 52 p. :ill., maps ;28 cm., https://doi.org/10.3133/wri824087.","productDescription":"v, 52 p. :ill., maps ;28 cm.","costCenters":[],"links":[{"id":159275,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wri/1982/4087/report-thumb.jpg"},{"id":57213,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wri/1982/4087/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ae0e4b07f02db687fe0","contributors":{"authors":[{"text":"Litke, D. W.","contributorId":94346,"corporation":false,"usgs":true,"family":"Litke","given":"D.","email":"","middleInitial":"W.","affiliations":[],"preferred":false,"id":199748,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":10419,"text":"ofr82587 - 1982 - The determination of total volatiles in rocks by loss-on-fusion","interactions":[],"lastModifiedDate":"2012-02-02T00:06:40","indexId":"ofr82587","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":"82-587","title":"The determination of total volatiles in rocks by loss-on-fusion","docAbstract":"A fast and accurate technique has been developed for the determination of the total volatile content of rocks. The loss on fusion (LOF) results are comparable to the conventional time-consuming wet-chemical procedure but require no additional effort or cost when conducted as part of the usual sample preparation procedure for quantitative X-ray fluorescence spectrometric analysis (XRF). The technique utilizes the weight loss of the rock when fused with a suitable blend of lithium tetraborate and lithium nitrate. A simple mass balance model is used to represent the thermogravimetric results and to identify the nature of the high temperature mass alteration reactions taking place in the fusion melt. Under the sample preparation conditions used in this study, sulfide appears to be retained quantitatively in the fusion disc sulfate, a phenomenon permitting the determination of sulfide in prepared by a conventional fusion procedure in the form of \r\nrock samples.","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/ofr82587","usgsCitation":"Mossotti, V., and King, B., 1982, The determination of total volatiles in rocks by loss-on-fusion: U.S. Geological Survey Open-File Report 82-587, 23 p., ill. ;28 cm., https://doi.org/10.3133/ofr82587.","productDescription":"23 p., ill. ;28 cm.","costCenters":[],"links":[{"id":145652,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1982/0587/report-thumb.jpg"},{"id":38278,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1982/0587/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4aa9e4b07f02db6687ee","contributors":{"authors":[{"text":"Mossotti, V.G.","contributorId":43785,"corporation":false,"usgs":true,"family":"Mossotti","given":"V.G.","affiliations":[],"preferred":false,"id":161358,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"King, B.","contributorId":78750,"corporation":false,"usgs":true,"family":"King","given":"B.","affiliations":[],"preferred":false,"id":161359,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":10610,"text":"ofr82266 - 1982 - Installation and sampling of observation wells and analyses of water from the shallow aquifer at selected waste-disposal sites in the Memphis area, Tennessee","interactions":[],"lastModifiedDate":"2012-02-02T00:06:21","indexId":"ofr82266","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":"82-266","title":"Installation and sampling of observation wells and analyses of water from the shallow aquifer at selected waste-disposal sites in the Memphis area, Tennessee","docAbstract":"Observation wells were installed and sampled at six abandoned waste-disposal sites in the Memphis area that have been identified as having received unknown quantities and types of industrial waste. Ten wells were installed adjacent to and downgradient from these sites in the shallow water-table aquifer. Water samples were collected from these 10 wells and from two other wells in the shallow water-table aquifer. Most wells were sampled twice -- initially in the early summer when water levels were high and again in the fall when water levels were low. Other wells were sampled only once in either the summer or fall. The water was analyzed for common constituents, selected trace constituents, and selected organic compounds. (USGS)","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/ofr82266","usgsCitation":"Parks, W.S., Graham, D., and Lowery, J., 1982, Installation and sampling of observation wells and analyses of water from the shallow aquifer at selected waste-disposal sites in the Memphis area, Tennessee: U.S. Geological Survey Open-File Report 82-266, iv, 36 p. :ill., maps ;28 cm., https://doi.org/10.3133/ofr82266.","productDescription":"iv, 36 p. :ill., maps ;28 cm.","costCenters":[],"links":[{"id":965,"rank":100,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.water.usgs.gov/ofr82-266","linkFileType":{"id":5,"text":"html"}},{"id":142545,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e49f1e4b07f02db5ee32a","contributors":{"authors":[{"text":"Parks, W. S.","contributorId":99555,"corporation":false,"usgs":true,"family":"Parks","given":"W.","email":"","middleInitial":"S.","affiliations":[],"preferred":false,"id":161677,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Graham, D. D.","contributorId":68314,"corporation":false,"usgs":true,"family":"Graham","given":"D. D.","affiliations":[],"preferred":false,"id":161676,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Lowery, J.F.","contributorId":18367,"corporation":false,"usgs":true,"family":"Lowery","given":"J.F.","email":"","affiliations":[],"preferred":false,"id":161675,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":46025,"text":"ofr82653 - 1982 - Landslides and related features, Kentucky and Tennessee, Corbin 1° x 2° sheet","interactions":[],"lastModifiedDate":"2021-10-14T22:12:10.489351","indexId":"ofr82653","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":"82-653","title":"Landslides and related features, Kentucky and Tennessee, Corbin 1° x 2° sheet","docAbstract":"<p>No abstract available.</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr82653","usgsCitation":"Taylor, A.R., and Thomas, R.E., 1982, Landslides and related features, Kentucky and Tennessee, Corbin 1° x 2° sheet: U.S. Geological Survey Open-File Report 82-653, 128 Plates: 21.00 × 42.00 inches or smaller, https://doi.org/10.3133/ofr82653.","productDescription":"128 Plates: 21.00 × 42.00 inches or 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,{"id":10619,"text":"ofr811121 - 1982 - Water resources of the Ochlockonee River area, northwest Florida","interactions":[],"lastModifiedDate":"2022-08-31T19:15:04.672539","indexId":"ofr811121","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":"81-1121","title":"Water resources of the Ochlockonee River area, northwest Florida","docAbstract":"<p>The Ochlockonee River area comprises about 1,420 square miles in the panhandle of northwest Florida. In 1975, the population of the area was about 48,000. Water use averaged 11.4 million gallons per day; about half was pumped from wells and half from streams.</p><p>The area receives 57 inches of precipitation per year on the average. Much of this water enters the surficial sand aquifer, seeps to streams, or enters the underlying water-bearing zone of the upper confining unit and the Floridan aquifer.</p><p>The water-bearing zone of the upper confining unit is used for rural domestic supplies and is also important because the water it stores is a source of recharge to the underlying Floridan aquifer.</p><p>The Floridan aquifer underlies all of the Ochlockonee River area and, except for the city of Quincy, is the principal source of municipal water supply. Well yields range from as little as 20 gallons per minute in Gadsden County to as much as 4,500 gallons per minute in Leon County. The transmissivity of the Floridan aquifer ranges from about 170 feet squared per day in the southern part of the area to 5,100 feet squared per day in the northern part. Storage coefficients calculated from two aquifer tests are 2 x 10-4 and 2.6 x 10-4. At Tallahassee, directly east of the Ochlockonee River, transmissivity is as high as 130,000 feet squared per day. The Floridan aquifer is recharged by downward leakage of water from the surficial sand aquifer and from the water-bearing zone of the upper confining unit. The Floridan aquifer is also recharged directly by rainfall in northern Leon County and in southern Georgia where it is near or at land surface. Ground water moves toward the southeast from the potentiometric high in southwestern Gadsden County and south from Leon County toward Wakulla Springs, located about 10 miles south of Tallahassee. The potentiometric surface of the upper part of the Floridan aquifer ranges from about 50 feet higher than that of the middle and lower part of the Floridan aquifer in southwestern Gadsden County to about 10 feet higher near Midway in eastern Gadsden County. The aquifer discharge in the basin area is by wells and by natural discharge through seeps and springs along the Ochlockonee River and at Ochlockonee Bay.</p><p>Water levels in the Floridan aquifer fluctuate in response to seasonal and long-term variations in rainfall. Hydrographs do not show evidence of any long-term water-level declining trend.</p><p>Saline water (more than 1,000 milligrams per liter of dissolved solids) occurs naturally within the Floridan aquifer throughout the Ochlockonee River area at depths ranging from 200 to 600 feet below sea level. The depth below which dissolved solids in water exceed 500 milligrams per liter in the Havana area ranges from 200 to 250 feet below sea level; in the Quincy area, from 400 to 450 feet below; and in the Greensboro area, from 200 to 250 feet below.</p><p>Concentrations of dissolved solids in water pumped from wells tapping the Floridan aquifer in the Ochlockonee River area range from 60 to 1,370 milligrams per liter; chloride from 0 to 630 milligrams per liter; sulfate from 0.0 to 280 milligrams per liter; and fluoride from 0.0 to 1.3 milligrams per liter.</p><p>Streamflow originating in the Ochlockonee River area in Florida averages about 1,000 million gallons per day; minimum discharge during dry periods is about 285 million gallons per day. Stream yields range from 0.90 to 2.62 cubic feet per second per square mile. Quincy Creek, at State Highway 267 at Quincy, the primary source of water for the city of Quincy, yields an average flow of 19 million gallons per day, has a 7-day 10-year low flow of 2.8 million gallons per day, and contains water of acceptable quality. The chemical quality of most streams in the basin is acceptable for most uses. Dissolved-solids concentration is generally less than 135 milligrams per liter; pH ranges from 5.3 to 7.3 units; color from 20 to 90 platinum-cobalt units; and turbidity from 3 to 85 Jackson turbidity units. Variations in chloride concentration in water from the Ochlockonee River (5.2 to 140 milligrams per liter) are influenced by discharge of food processing waste and municipal sewage plant effluent to the river.</p><p>The three large lakes in the basin range from 4,000 to 7,000 acres in surface area. All are now used primarily for recreation. Dissolved-solids concentrations of water from the lakes range from less than 20 to 50 milligrams per liter. A major flood occurred in 1975 when the Ochlockonee River near Havana reached the third highest stage of record and the peak flood at the Sopchoppy River exceeded that for the period of record (11 years in 1975); no significant damage occurred.</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr811121","collaboration":"Prepared in cooperation with the Northwest Florida Water Management District, Gadsden County and the City of Quincy","usgsCitation":"Pascale, C.A., and Wagner, J.R., 1982, Water resources of the Ochlockonee River area, northwest Florida: U.S. Geological Survey Open-File Report 81-1121, vii, 114 p., https://doi.org/10.3133/ofr811121.","productDescription":"vii, 114 p.","costCenters":[],"links":[{"id":406025,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1981/1121/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":142486,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1981/1121/report-thumb.jpg"}],"country":"United States","state":"Florida","otherGeospatial":"Ochlockonee River area","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -84.75814819335936,\n              29.846599772557077\n            ],\n            [\n              -84.38735961914062,\n              29.846599772557077\n            ],\n            [\n              -84.38735961914062,\n              30.198552988693212\n            ],\n            [\n              -84.75814819335936,\n              30.198552988693212\n            ],\n            [\n              -84.75814819335936,\n              29.846599772557077\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e49f4e4b07f02db5f0499","contributors":{"authors":[{"text":"Pascale, Charles A.","contributorId":99978,"corporation":false,"usgs":true,"family":"Pascale","given":"Charles","email":"","middleInitial":"A.","affiliations":[],"preferred":false,"id":161693,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Wagner, Jeffry R.","contributorId":48179,"corporation":false,"usgs":true,"family":"Wagner","given":"Jeffry","email":"","middleInitial":"R.","affiliations":[],"preferred":false,"id":161692,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":28474,"text":"wri824072 - 1982 - A data-management system for areal interpretive data for the High Plains in parts of Colorado, Kansas, Nebraska, New Mexico, Oklahoma, South Dakota, Texas, and Wyoming","interactions":[],"lastModifiedDate":"2012-02-02T00:08:47","indexId":"wri824072","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":"82-4072","title":"A data-management system for areal interpretive data for the High Plains in parts of Colorado, Kansas, Nebraska, New Mexico, Oklahoma, South Dakota, Texas, and Wyoming","docAbstract":"The High Plains Regional Aquifer System Analysis has developed a regional water-resources (and related) data storage and retrieval system to organize and preserve areal interpretative data. The system is general and can easily be adapted for other studies. This report documents the High Plains data base as well as the general system that is independent of the High Plains area. The system is built around a hierarchically structured data base consisting of related latitude-longitude blocks. Various parameters in the data base are stored at different degrees of detail, with the finest detail being a block of 1 minute of latitude by 1 minute longitude (approximately 1 square mile). (USGS)","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/wri824072","usgsCitation":"Luckey, R.R., and Ferrigno, C., 1982, A data-management system for areal interpretive data for the High Plains in parts of Colorado, Kansas, Nebraska, New Mexico, Oklahoma, South Dakota, Texas, and Wyoming: U.S. Geological Survey Water-Resources Investigations Report 82-4072, vii, 112 p. :ill. ;28 cm., https://doi.org/10.3133/wri824072.","productDescription":"vii, 112 p. :ill. ;28 cm.","costCenters":[],"links":[{"id":118797,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wri/1982/4072/report-thumb.jpg"},{"id":57274,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wri/1982/4072/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b25e4b07f02db6af2a1","contributors":{"authors":[{"text":"Luckey, R. R.","contributorId":93055,"corporation":false,"usgs":true,"family":"Luckey","given":"R.","email":"","middleInitial":"R.","affiliations":[],"preferred":false,"id":199867,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Ferrigno, C.F.","contributorId":27092,"corporation":false,"usgs":true,"family":"Ferrigno","given":"C.F.","email":"","affiliations":[],"preferred":false,"id":199866,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"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":10418,"text":"ofr82142 - 1982 - Spectrographic analyses of subsurface Cambrian whole-rock samples from southern Missouri","interactions":[],"lastModifiedDate":"2012-02-02T00:06:40","indexId":"ofr82142","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":"82-142","title":"Spectrographic analyses of subsurface Cambrian whole-rock samples from southern Missouri","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/ofr82142","usgsCitation":"Mosier, E.L., Erickson, M.S., and McDanal, S., 1982, Spectrographic analyses of subsurface Cambrian whole-rock samples from southern Missouri: U.S. Geological Survey Open-File Report 82-142, 94 p., map ;28 cm., https://doi.org/10.3133/ofr82142.","productDescription":"94 p., map ;28 cm.","costCenters":[],"links":[{"id":145635,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1982/0142/report-thumb.jpg"},{"id":38277,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1982/0142/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e49e2e4b07f02db5e4ddf","contributors":{"authors":[{"text":"Mosier, E. L.","contributorId":71537,"corporation":false,"usgs":true,"family":"Mosier","given":"E.","email":"","middleInitial":"L.","affiliations":[],"preferred":false,"id":161356,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Erickson, M. S.","contributorId":35302,"corporation":false,"usgs":true,"family":"Erickson","given":"M.","email":"","middleInitial":"S.","affiliations":[],"preferred":false,"id":161355,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"McDanal, S.K.","contributorId":108078,"corporation":false,"usgs":true,"family":"McDanal","given":"S.K.","email":"","affiliations":[],"preferred":false,"id":161357,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":10336,"text":"ofr8231 - 1982 - Water for western oil shale development: Potential local supplies","interactions":[],"lastModifiedDate":"2022-09-23T20:26:58.565482","indexId":"ofr8231","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":"82-31","title":"Water for western oil shale development: Potential local supplies","docAbstract":"<p>Commercial-scale development of western oil shale resources will require a supply of water for both extraction and reclamation purposes. This paper summarizes some of the information on the occurrence of potential local supplies of water in the Piceance Creek Basin-Uinta Basin areas of northwest Colorado and northeast Utah. The discussion is somewhat hypothetical in that it is restricted to the physical occurrence of water with emphasis on water resources in each basin. Of course, the many potential constraints on water use (including economics, water quality, legal and other institutional factors) are necessarily secondary to the ultimate constraint, its physical occurrence. Perhaps the most obvious constraint is that of water rights and water laws. For example, \"mining\" of some of the ground water is herein assumed to be necessary for technically sound management and utilization of the water resource, but the hydrologic effects of such \"mining\" would require accommodation under water laws and agreements.</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr8231","usgsCitation":"Miller, G., 1982, Water for western oil shale development: Potential local supplies: U.S. Geological Survey Open-File Report 82-31, 6 p., https://doi.org/10.3133/ofr8231.","productDescription":"6 p.","costCenters":[],"links":[{"id":143503,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1982/0031/report-thumb.jpg"},{"id":407297,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1982/0031/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"country":"United States","state":"Colorado, Utah","otherGeospatial":"Piceance Creek Basin, Uinta Basin","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -110.9893798828125,\n              40.17047886718109\n            ],\n            [\n              -108.2537841796875,\n              40.17047886718109\n            ],\n            [\n              -108.2537841796875,\n              40.925964939514294\n            ],\n            [\n              -110.9893798828125,\n              40.925964939514294\n            ],\n            [\n              -110.9893798828125,\n              40.17047886718109\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a08e4b07f02db5fa1f2","contributors":{"authors":[{"text":"Miller, G.A.","contributorId":107671,"corporation":false,"usgs":true,"family":"Miller","given":"G.A.","email":"","affiliations":[],"preferred":false,"id":161215,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"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":10417,"text":"ofr82143 - 1982 - Spectrographic analyses of subsurface Cambrian insoluble-residue samples from southern Missouri","interactions":[],"lastModifiedDate":"2012-02-02T00:06:40","indexId":"ofr82143","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":"82-143","title":"Spectrographic analyses of subsurface Cambrian insoluble-residue samples from southern Missouri","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/ofr82143","usgsCitation":"Mosier, E.L., Erickson, M.S., and McDanal, S., 1982, Spectrographic analyses of subsurface Cambrian insoluble-residue samples from southern Missouri: U.S. Geological Survey Open-File Report 82-143, 90 p., map ;28 cm., https://doi.org/10.3133/ofr82143.","productDescription":"90 p., map ;28 cm.","costCenters":[],"links":[{"id":145634,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1982/0143/report-thumb.jpg"},{"id":38276,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1982/0143/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e49e2e4b07f02db5e4e4b","contributors":{"authors":[{"text":"Mosier, E. L.","contributorId":71537,"corporation":false,"usgs":true,"family":"Mosier","given":"E.","email":"","middleInitial":"L.","affiliations":[],"preferred":false,"id":161353,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Erickson, M. S.","contributorId":35302,"corporation":false,"usgs":true,"family":"Erickson","given":"M.","email":"","middleInitial":"S.","affiliations":[],"preferred":false,"id":161352,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"McDanal, S.K.","contributorId":108078,"corporation":false,"usgs":true,"family":"McDanal","given":"S.K.","email":"","affiliations":[],"preferred":false,"id":161354,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":33427,"text":"b1516AD - 1982 - Mineral resources of the Minarets Wilderness and adjacent areas, Madera and Mono counties, California","interactions":[{"subject":{"id":9046,"text":"ofr791472 - 1979 - Mineral resources of the Minarets Wilderness and adjacent areas, Madera and Mono counties, California","indexId":"ofr791472","publicationYear":"1979","noYear":false,"title":"Mineral resources of the Minarets Wilderness and adjacent areas, Madera and Mono counties, California"},"predicate":"SUPERSEDED_BY","object":{"id":33427,"text":"b1516AD - 1982 - Mineral resources of the Minarets Wilderness and adjacent areas, Madera and Mono counties, California","indexId":"b1516AD","publicationYear":"1982","noYear":false,"chapter":"A-D","title":"Mineral resources of the Minarets Wilderness and adjacent areas, Madera and Mono counties, California"},"id":1}],"lastModifiedDate":"2012-02-02T00:09:37","indexId":"b1516AD","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1982","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":306,"text":"Bulletin","code":"B","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"1516","chapter":"A-D","title":"Mineral resources of the Minarets Wilderness and adjacent areas, Madera and Mono counties, California","language":"ENGLISH","publisher":"U.S. G.P.O.,","doi":"10.3133/b1516AD","usgsCitation":"Huber, N., Oliver, H.W., Bailey, R., Thurber, H.K., Miller, M.S., Hillman, C., Lindsey, D., and Morris, R., 1982, Mineral resources of the Minarets Wilderness and adjacent areas, Madera and Mono counties, California: U.S. Geological Survey Bulletin 1516, 159 p., 3 folded leaves of plates :ill. (some col.) ;23 cm., https://doi.org/10.3133/b1516AD.","productDescription":"159 p., 3 folded leaves of plates :ill. (some col.) ;23 cm.","costCenters":[],"links":[{"id":247397,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/bul/1516a-d/report.pdf","size":"11266","linkFileType":{"id":1,"text":"pdf"}},{"id":247398,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/bul/1516a-d/plate-1.pdf","size":"11401","linkFileType":{"id":1,"text":"pdf"}},{"id":247399,"rank":401,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/bul/1516a-d/plate-2.pdf","size":"11597","linkFileType":{"id":1,"text":"pdf"}},{"id":247400,"rank":402,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/bul/1516a-d/plate-3.pdf","size":"12533","linkFileType":{"id":1,"text":"pdf"}},{"id":251835,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/bul/1516a-d/report-thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b06e4b07f02db69a200","contributors":{"authors":[{"text":"Huber, N.K.","contributorId":73610,"corporation":false,"usgs":true,"family":"Huber","given":"N.K.","affiliations":[],"preferred":false,"id":211026,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Oliver, H. W.","contributorId":85570,"corporation":false,"usgs":true,"family":"Oliver","given":"H.","email":"","middleInitial":"W.","affiliations":[],"preferred":false,"id":211028,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Bailey, R. A.","contributorId":87531,"corporation":false,"usgs":true,"family":"Bailey","given":"R. A.","affiliations":[],"preferred":false,"id":211029,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Thurber, H. K.","contributorId":59457,"corporation":false,"usgs":true,"family":"Thurber","given":"H.","email":"","middleInitial":"K.","affiliations":[],"preferred":false,"id":211024,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"Miller, M. S.","contributorId":69107,"corporation":false,"usgs":true,"family":"Miller","given":"M.","email":"","middleInitial":"S.","affiliations":[],"preferred":false,"id":211025,"contributorType":{"id":1,"text":"Authors"},"rank":5},{"text":"Hillman, C.T.","contributorId":6112,"corporation":false,"usgs":true,"family":"Hillman","given":"C.T.","email":"","affiliations":[],"preferred":false,"id":211022,"contributorType":{"id":1,"text":"Authors"},"rank":6},{"text":"Lindsey, D.S.","contributorId":79096,"corporation":false,"usgs":true,"family":"Lindsey","given":"D.S.","email":"","affiliations":[],"preferred":false,"id":211027,"contributorType":{"id":1,"text":"Authors"},"rank":7},{"text":"Morris, R.W.","contributorId":34577,"corporation":false,"usgs":true,"family":"Morris","given":"R.W.","email":"","affiliations":[],"preferred":false,"id":211023,"contributorType":{"id":1,"text":"Authors"},"rank":8}]}}
,{"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":33484,"text":"b1506AE - 1982 - Mineral resources of the Sheep Mountain Wilderness study area and the Cucamonga Wilderness and additions, Los Angeles and San Bernardino Counties, California","interactions":[],"lastModifiedDate":"2012-02-02T00:09:35","indexId":"b1506AE","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1982","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":306,"text":"Bulletin","code":"B","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"1506","chapter":"A-E","title":"Mineral resources of the Sheep Mountain Wilderness study area and the Cucamonga Wilderness and additions, Los Angeles and San Bernardino Counties, California","language":"ENGLISH","publisher":"U.S. G.P.O.,","doi":"10.3133/b1506AE","usgsCitation":"Evans, J.G., Ridenour, J., Pankratz, L., Schmauch, S., and and Zilka, N.T., 1982, Mineral resources of the Sheep Mountain Wilderness study area and the Cucamonga Wilderness and additions, Los Angeles and San Bernardino Counties, California: U.S. Geological Survey Bulletin 1506, v, 92 p. : ill., maps ; 24 cm., https://doi.org/10.3133/b1506AE.","productDescription":"v, 92 p. : ill., maps ; 24 cm.","costCenters":[],"links":[{"id":167668,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/bul/1506a-e/report-thumb.jpg"},{"id":61392,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/bul/1506a-e/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":61390,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/bul/1506a-e/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":61391,"rank":401,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/bul/1506a-e/plate-2.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b06e4b07f02db69a0c9","contributors":{"authors":[{"text":"Evans, James G. jevans@usgs.gov","contributorId":2396,"corporation":false,"usgs":true,"family":"Evans","given":"James","email":"jevans@usgs.gov","middleInitial":"G.","affiliations":[],"preferred":true,"id":211337,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Ridenour, James","contributorId":87540,"corporation":false,"usgs":true,"family":"Ridenour","given":"James","email":"","affiliations":[],"preferred":false,"id":211341,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Pankratz, LeRoy","contributorId":32220,"corporation":false,"usgs":true,"family":"Pankratz","given":"LeRoy","affiliations":[],"preferred":false,"id":211339,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Schmauch, S. W.","contributorId":53790,"corporation":false,"usgs":true,"family":"Schmauch","given":"S. W.","affiliations":[],"preferred":false,"id":211340,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"and Zilka, N. T.","contributorId":12096,"corporation":false,"usgs":true,"family":"and Zilka","given":"N.","email":"","middleInitial":"T.","affiliations":[],"preferred":false,"id":211338,"contributorType":{"id":1,"text":"Authors"},"rank":5}]}}
,{"id":10727,"text":"ofr82136 - 1982 - A regional assessment of potential environmental hazards to and limitations on petroleum development of the Southeastern United States Atlantic continental shelf, slope, and rise, offshore North Carolina","interactions":[],"lastModifiedDate":"2012-02-02T00:06:23","indexId":"ofr82136","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":"82-136","title":"A regional assessment of potential environmental hazards to and limitations on petroleum development of the Southeastern United States Atlantic continental shelf, slope, and rise, offshore North Carolina","docAbstract":"More than 11,000 km of high-resolution seismic-reflection data, 325 km of mid-range sidescan-sonar data, and 500 km of long-range sidescan-sonar data were examined and used to construct an environmental geology map of the Continental Shelf, Slope, and Rise for the area of the U.S. Atlantic margin between lats. 32?N. and 37?N. Hardgrounds and two faults described in previous literature also are shown on the map. \r\n\r\nOn the Continental Shelf, at least two faults, the Helena Banks fault and the White Oak lineament, appear to be tectonic in origin. However, a lack of historical seismicity associated with these faults indicates that they are probably not active at the present time. Hardgrounds are widely scattered but are most abundant in Onslow Bay. Although paleostream channels are common nearshore, they do not appear to be common on the central and outer shelf except off Albemarle Sound where extensive Pleistocene, Pliocene, and late Miocene channels extend across the shelf. Mobile bottom sediments are confined mainly to the shoals off Cape Romain, Cape Fear, Cape Lookout, and Cape Hatteras. Elsewhere the sand cover is thin, and older more indurated rocks are present in subcrop. \r\n\r\nNo slope-instability features were noted on the Florida-Hatteras slope off North Carolina. The lack of features indicates that this slope is relatively stable. \r\n\r\nEvidence for scour by strong currents is ubiquitous on the northern Blake Plateau although deep-water reefs are sparse. The outer edge of the plateau is dominated by a major growth fault and numerous splay and antithetic faults. These faults are the product of salt tectonism in the Carolina trough and thus are not associated with seismicity. Displacements observed near the sea floor and breached diapirs offshore indicate that the main fault is still moving. Associated with the faults are collapse features that are interpreted to be caused by karst solution and cavernous porosity in Eocene and Oligocene limestones at depth. \r\n\r\nMajor slumps have taken place in two large areas of the Continental Slope. Seismic-reflection profiles of the southern area, centered on the lower slope at 1at. 33?N., long. 76?W., show a 80-m-hlgh scarp in which bedding has been truncated. Rotational slump faults are present in this area on the middle and upper slope. Sidescan images show that large blocks have slid downslope from the scarp face, furrowing the bottom. High-resolution (3.5-kHz) records show that the rotational slump faults upslope are active. The association of these slumps and the scarps with salt diapirs suggests subsidence accompanying salt tectonism as the cause. Seismic-reflection records over the northern area, at about fat. 36?20'N., long. 74?40'W., show two steep scarps, each about 225 m high on the upper and middle-slope. These slump scars and an absence of Pleistocene sediments indicate that large blocks of the slope have been removed by slumping. \r\n\r\nThe slope north of fat. 35?N. is highly dissected by canyons. Mid-range sidescan-sonar records suggest that the canyons are the product of mass wasting and have probably formed largely by slumping. \r\n\r\nSediments in a wide zone on the upper rise are highly disturbed and faulted owing to salt tectonism. Twenty-six salt diapirs are mapped, as is a zone of disturbed bottom related to salt tectonism. \r\n\r\nAn area of frozen bottom (clathrate) under which shallow free gas is trapped underlies the outer Blake Plateau, the slope, and the upper rise. Although the hazards of drilling into or through clathrates have not been tested, the release of gas from beneath this frozen layer may prove to be a primary hazard to exploration.","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/ofr82136","usgsCitation":"Popenoe, P., Coward, E., and Cashman, K.V., 1982, A regional assessment of potential environmental hazards to and limitations on petroleum development of the Southeastern United States Atlantic continental shelf, slope, and rise, offshore North Carolina: U.S. Geological Survey Open-File Report 82-136, 71 p., 1 over-size sheet, maps ;28 cm., https://doi.org/10.3133/ofr82136.","productDescription":"71 p., 1 over-size sheet, maps ;28 cm.","costCenters":[],"links":[{"id":143343,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1982/0136/report-thumb.jpg"},{"id":38538,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1982/0136/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":38539,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1982/0136/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b1ae4b07f02db6a849d","contributors":{"authors":[{"text":"Popenoe, Peter","contributorId":62206,"corporation":false,"usgs":true,"family":"Popenoe","given":"Peter","email":"","affiliations":[{"id":678,"text":"Woods Hole Coastal and Marine Science Center","active":true,"usgs":true}],"preferred":false,"id":161864,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Coward, E. L.","contributorId":84375,"corporation":false,"usgs":true,"family":"Coward","given":"E. L.","affiliations":[],"preferred":false,"id":161865,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Cashman, K. V.","contributorId":16831,"corporation":false,"usgs":true,"family":"Cashman","given":"K.","email":"","middleInitial":"V.","affiliations":[],"preferred":false,"id":161863,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":10612,"text":"ofr8339 - 1982 - Compilation of ground-water quality data for selected wells in Elmore, Owyhee, Ada, and Canyon counties, Idaho, 1945 through 1982","interactions":[],"lastModifiedDate":"2013-11-12T13:18:24","indexId":"ofr8339","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":"83-39","title":"Compilation of ground-water quality data for selected wells in Elmore, Owyhee, Ada, and Canyon counties, Idaho, 1945 through 1982","docAbstract":"Well-inventory and groundwater-quality data for 665 sites with a total of 1,318 chemical analyses were compiled from Elmore, Owyhee, Ada, and Canyon Counties. Data are sorted by water temperature (less than 20 degrees Celsius is considered nonthermal; 20 degrees Celcius or greater is considered thermal) to facilitate their use.","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Boise, ID","doi":"10.3133/ofr8339","collaboration":"Prepared in cooperation with the Idaho Department of Water Resources","usgsCitation":"Parliman, D., 1982, Compilation of ground-water quality data for selected wells in Elmore, Owyhee, Ada, and Canyon counties, Idaho, 1945 through 1982: U.S. Geological Survey Open-File Report 83-39, 156 p. ill., maps ;28 cm., https://doi.org/10.3133/ofr8339.","productDescription":"156 p. ill., maps ;28 cm.","costCenters":[{"id":343,"text":"Idaho Water Science Center","active":true,"usgs":true}],"links":[{"id":142547,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1983/0039/report-thumb.jpg"},{"id":38445,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1983/0039/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"country":"United States","state":"Idaho","county":"Ada County;Canyon County;Elmore County;Owyhee County","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -117.0,42.0 ], [ -117.0,44.125 ], [ -115.0,44.125 ], [ -115.0,42.0 ], [ -117.0,42.0 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b24e4b07f02db6ae507","contributors":{"authors":[{"text":"Parliman, D. J.","contributorId":64220,"corporation":false,"usgs":true,"family":"Parliman","given":"D. J.","affiliations":[],"preferred":false,"id":161681,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":10230,"text":"ofr82685 - 1982 - Knik Glacier, Alaska; summary of 1979, 1980, and 1981 data and introduction of new surveying techniques","interactions":[],"lastModifiedDate":"2012-02-02T00:06:29","indexId":"ofr82685","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":"82-685","title":"Knik Glacier, Alaska; summary of 1979, 1980, and 1981 data and introduction of new surveying techniques","docAbstract":"Knik Glacier in south-central Alaska has the potential to reform Lake George, Alaska 's largest glacier-dammed lake. Measurements of surface altitude, snow depth, terminus position, glacier speed, and ice depth are being made in an attempt to determine the mechanisms that could cause a significant re-advance of the glacier. New surveying and data reduction techniques were developed by the authors and employed successfully at Knik Glacier. These include precise geodetic surveying by the ' trisection ' technique, calculation of surface altitude at a specially-fixed ' index point ' from three point measurements on a rough, moving glacier surface, and calculation of ice thickness from low frequency radar measurements. In addition, this report summarizes the data collected from 1979 to 1981 in support of this goal. (USGS)","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/ofr82685","usgsCitation":"Mayo, L., and Trabant, D., 1982, Knik Glacier, Alaska; summary of 1979, 1980, and 1981 data and introduction of new surveying techniques: U.S. Geological Survey Open-File Report 82-685, vi, 32 p., ill., maps ;28 cm., https://doi.org/10.3133/ofr82685.","productDescription":"vi, 32 p., ill., maps ;28 cm.","costCenters":[],"links":[{"id":144323,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1982/0685/report-thumb.jpg"},{"id":38099,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1982/0685/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b32e4b07f02db6b48fe","contributors":{"authors":[{"text":"Mayo, L.R.","contributorId":21541,"corporation":false,"usgs":true,"family":"Mayo","given":"L.R.","email":"","affiliations":[],"preferred":false,"id":161046,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Trabant, D.C.","contributorId":42209,"corporation":false,"usgs":true,"family":"Trabant","given":"D.C.","email":"","affiliations":[],"preferred":false,"id":161047,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":10633,"text":"ofr821054 - 1982 - Use of microcomputer in mapping depth of stratigraphic horizons in National Petroleum Reserve in Alaska","interactions":[],"lastModifiedDate":"2012-02-02T00:06:29","indexId":"ofr821054","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":"82-1054","title":"Use of microcomputer in mapping depth of stratigraphic horizons in National Petroleum Reserve in Alaska","docAbstract":"REGIONAL MAPPER is a menu-driven system in the BASIC language for computing and plotting (1) time, depth, and average velocity to geologic horizons, (2) interval time, thickness, and interval velocity of stratigraphic intervals, and (3) subcropping and onlapping intervals at unconformities. The system consists of three programs: FILER, TRAVERSER, and PLOTTER. A control point is a shot point with velocity analysis or a shot point at or near a well with velocity check-shot survey. Reflection time to and code number of seismic horizons are filed by digitizing tablet from record sections. TRAVERSER starts at a point of geologic control and, in traversing to another, parallels seismic events, records loss of horizons by onlap and truncation, and stores reflection time for geologic horizons at traversed shot points. TRAVERSER is basically a phantoming procedure. \r\n\r\nPermafrost thickness and velocity variations, buried canyons with low-velocity fill, and error in seismically derived velocity cause velocity anomalies that complicate depth mapping. Two depths to the top of the pebble is based shale are computed for each control point. One depth, designated Zs on seismically derived velocity. The other (Zw) is based on interval velocity interpolated linearly between wells and multiplied by interval time (isochron) to give interval thickness. Z w is computed for all geologic horizons by downward summation of interval thickness. \r\n\r\nUnknown true depth (Z) to the pebble shale may be expressed as\r\n\r\nZ = Zs + es and Z = Zw + ew\r\n\r\nwhere the e terms represent error. Equating the two expressions gives the depth difference \r\n\r\nD = Zs + Zw = ew + es\r\n\r\nA plot of D for the top of the pebble shale is readily contourable but smoothing is required to produce a reasonably simple surface. \r\n\r\nSeismically derived velocity used in computing Zs includes the effect of velocity anomalies but is subject to some large randomly distributed errors resulting in depth errors (es). Well-derived velocity used in computing Zw does not include the effect of velocity anomalies, but the error (ew) should reflect these anomalies and should be contourable (non-random). The D surface as contoured with smoothing is assumed to represent ew, that is, the depth effect of variations in permafrost thickness and velocity and buried canyon depth. \r\n\r\nEstimated depth (Zest) to each geologic horizon is the sum of Z w for that horizon and a constant e w as contoured for the pebble shale, which is the first highly continuous seismic horizon below the zone of anomalous velocity. Results of this 'depthing' procedure are compared with those of Tetra Tech, Inc., the subcontractor responsible for geologic and geophysical interpretation and mapping.","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/ofr821054","usgsCitation":"Payne, T.G., 1982, Use of microcomputer in mapping depth of stratigraphic horizons in National Petroleum Reserve in Alaska: U.S. Geological Survey Open-File Report 82-1054, ii, 42 p. ill. ;28 cm., https://doi.org/10.3133/ofr821054.","productDescription":"ii, 42 p. ill. ;28 cm.","costCenters":[],"links":[{"id":144042,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1982/1054/report-thumb.jpg"},{"id":38467,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1982/1054/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e49d5e4b07f02db5ddeb7","contributors":{"authors":[{"text":"Payne, Thomas G.","contributorId":60653,"corporation":false,"usgs":true,"family":"Payne","given":"Thomas","email":"","middleInitial":"G.","affiliations":[],"preferred":false,"id":161716,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":10720,"text":"ofr82931 - 1982 - Preliminary appraisal of gravity and magnetic data at Syncline Ridge, western Yucca Flat, Nevada Test Site, Nye County, Nevada","interactions":[],"lastModifiedDate":"2021-12-02T22:27:21.928652","indexId":"ofr82931","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":"82-931","title":"Preliminary appraisal of gravity and magnetic data at Syncline Ridge, western Yucca Flat, Nevada Test Site, Nye County, Nevada","docAbstract":"A gravity and magnetic study of the Syncline Ridge area was conducted as part of an investigation of argillite rocks of the Eleana Formation under consideration as a medium for the possible storage of high-level radioactive waste. \r\n\r\nBouguer gravity anomaly data, viewed in light of densities obtained by gamma-gamma logs and previous work of D. L. Healey (1968), delineate two regions of steep negative gradient where Cenozoic rocks and sediments are inferred to abruptly thicken: (1) the western third of the study area where Tertiary volcanic rocks are extensively exposed and (2) the northeast corner of the area where Quaternary alluvium is exposed and where volcanic rocks are inferred to occur at depth. In the remainder of the area, a region extending contiguously from Mine Mountain northwestward through Syncline Ridge to the Eleana Range, the gravity data indicate that the Eleana Formation, where not exposed, is buried at depths of less than about 200 m, except in a limited area of exposed older Paleozoic rocks on Mine Mountain. Quaternary alluvium and Tertiary volcanic rocks are inferred to occur in this region as veneers or shallow dishes of deposit on Tippipah Limestone or Eleana Formation. Low-level aeromagnetic anomaly data, covering the western two-thirds of the study area, delineate relatively magnetic tuff units within the Tertiary volcanic rocks and provide a very attractive means for distinguishing units of normal polarization from units of reversed polarization. If used in conjunction with results of previous magnetization studies of G. D. Bath (1968), the low-level survey may prove to be an effective tool for mapping specific tuff members in the volcanic terrane. \r\n\r\nThe important question of the feasibility of discriminating high-quartz argillite from low-quartz argillite of the Eleana Formation using surface gravity data remains unresolved. If the more highly competent, denser, high-quartz phase should occur as stratigraphic units many tens of meters thick, closely spaced gravity data may reliably detect these units. If the high-quartz phase occurs only as relatively thin units, interbedded with low-quartz phase, borehole gravity surveying can be used much more effectively than equivalent surface gravity surveying.","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr82931","usgsCitation":"Ponce, D.A., and Hanna, W.F., 1982, Preliminary appraisal of gravity and magnetic data at Syncline Ridge, western Yucca Flat, Nevada Test Site, Nye County, Nevada: U.S. Geological Survey Open-File Report 82-931, ii, 22 p., https://doi.org/10.3133/ofr82931.","productDescription":"ii, 22 p.","costCenters":[],"links":[{"id":392418,"rank":3,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_13861.htm"},{"id":38531,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1982/0931/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":143210,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1982/0931/report-thumb.jpg"}],"country":"United States","state":"Nevada","county":"Nye County","otherGeospatial":"Syncline Ridge, western Yucca Flat","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -116.25,\n              37\n            ],\n            [\n              -116.125,\n              37\n            ],\n            [\n              -116.125,\n              37.117\n            ],\n            [\n              -116.25,\n              37.117\n            ],\n            [\n              -116.25,\n              37\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ac9e4b07f02db67ca72","contributors":{"authors":[{"text":"Ponce, David A. 0000-0003-4785-7354 ponce@usgs.gov","orcid":"https://orcid.org/0000-0003-4785-7354","contributorId":1049,"corporation":false,"usgs":true,"family":"Ponce","given":"David","email":"ponce@usgs.gov","middleInitial":"A.","affiliations":[{"id":300,"text":"Geologic Hazards Science Center","active":true,"usgs":true},{"id":312,"text":"Geology, Minerals, Energy, and Geophysics Science Center","active":true,"usgs":true}],"preferred":true,"id":161853,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Hanna, William F.","contributorId":104045,"corporation":false,"usgs":true,"family":"Hanna","given":"William","email":"","middleInitial":"F.","affiliations":[],"preferred":false,"id":161854,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":10630,"text":"ofr82504 - 1982 - Quality of runoff from small watersheds in the Twin Cities metropolitan area, Minnesota: Hydrologic data for 1980","interactions":[],"lastModifiedDate":"2018-03-19T10:48:45","indexId":"ofr82504","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":"82-504","title":"Quality of runoff from small watersheds in the Twin Cities metropolitan area, Minnesota: Hydrologic data for 1980","docAbstract":"<p>An intensive study of nonpoint-source runoff was conducted in the Twin Cities metropolitan area in Minnesota during 1980. The purpose of the study was to determine the relationships between land use, watershed characteristics, and the quantity, quality, and timing of runoff.</p>\n<p>Discharge and water-quality data were collected at 19 sites located in 6 rural and 4 urban watersheds. Basin characteristics and land use were determined for each watershed. Recording instruments provided continuous discharge records at 17 sites and continuous rainfall records at 12 sites. Automatic samplers were used at 12 sites. Water-quality samples were collected at 15- to 60-minute intervals during periods of increased runoff. Samples were collected periodically during low flow. Primary emphasis was placed on analysis of samples for suspended solids, nutrients, and oxygen-demanding constituents. Secondary emphasis was placed on analysis for chloride, metals, bacteria, pesticides, and PCB's. Wetfall and dryfall precipitation-quality data were collected at six sites.</p>\n<p>Discharge and water-quality data were used to calculate storm and daily loads of chemical oxygen demand, total suspended solids, ammonia plus organic nitrogen, nitrite plus nitrate-nitrogen, total phosphorus, chloride, and lead.</p>\n<p>All data collected during the study are documented in tables that contain watershed characteristics and land use, daily and unit values for discharge and rainfall, rainfall characteristics, water-quality data for runoff and precipitation, results of laboratory settling tests, results of quality-assurance tests, dally loads, and storm loads.</p>","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"St. Paul, MN","doi":"10.3133/ofr82504","collaboration":"Prepared in cooperation with the Metropolitan Council of the Twin Cities","usgsCitation":"Payne, G.A., Ayers, M.A., and Brown, R.G., 1982, Quality of runoff from small watersheds in the Twin Cities metropolitan area, Minnesota: Hydrologic data for 1980: U.S. Geological Survey Open-File Report 82-504, iv, 289 p., https://doi.org/10.3133/ofr82504.","productDescription":"iv, 289 p.","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[{"id":392,"text":"Minnesota Water Science Center","active":true,"usgs":true}],"links":[{"id":142533,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1982/0504/report-thumb.jpg"},{"id":38464,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1982/0504/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"country":"United States","state":"Minnesota","otherGeospatial":"Twin Cities Metropolitan Area","geographicExtents":"{\"type\":\"FeatureCollection\",\"features\":[{\"type\":\"Feature\",\"geometry\":{\"type\":\"Polygon\",\"coordinates\":[[[-93.5093,45.4163],[-93.1289,45.4153],[-93.0186,45.4131],[-93.0188,45.2984],[-92.7894,45.297],[-92.7439,45.2963],[-92.7516,45.2935],[-92.7551,45.2927],[-92.7583,45.2904],[-92.7597,45.2872],[-92.7604,45.2845],[-92.7591,45.2794],[-92.7559,45.2739],[-92.7527,45.2694],[-92.7515,45.2657],[-92.7526,45.2626],[-92.7535,45.2584],[-92.7561,45.2541],[-92.7575,45.2502],[-92.7569,45.2443],[-92.7557,45.2397],[-92.7553,45.2356],[-92.7538,45.2305],[-92.7536,45.2276],[-92.7521,45.2236],[-92.752,45.2196],[-92.7527,45.2168],[-92.7546,45.2136],[-92.7573,45.2107],[-92.7603,45.2065],[-92.7619,45.2041],[-92.7632,45.2009],[-92.7637,45.1972],[-92.764,45.1895],[-92.7629,45.1853],[-92.7557,45.178],[-92.7522,45.1759],[-92.7493,45.173],[-92.748,45.1698],[-92.7472,45.1634],[-92.7483,45.1597],[-92.7475,45.1551],[-92.7473,45.1515],[-92.7484,45.1483],[-92.749,45.1419],[-92.7484,45.1373],[-92.7441,45.1264],[-92.7415,45.1172],[-92.7422,45.1135],[-92.7446,45.11],[-92.7467,45.1076],[-92.7513,45.1045],[-92.7591,45.0999],[-92.7624,45.0972],[-92.7803,45.0849],[-92.7847,45.083],[-92.7885,45.0806],[-92.7917,45.0791],[-92.795,45.0772],[-92.7982,45.0746],[-92.8001,45.0723],[-92.8019,45.0647],[-92.8016,45.0597],[-92.8005,45.0567],[-92.7984,45.0531],[-92.7952,45.0499],[-92.7926,45.0481],[-92.7881,45.0453],[-92.7837,45.0421],[-92.7745,45.0373],[-92.7707,45.0344],[-92.7683,45.0325],[-92.7645,45.0265],[-92.7639,45.0237],[-92.7639,45.0196],[-92.7682,45.0005],[-92.7694,44.9909],[-92.7686,44.9796],[-92.7646,44.9711],[-92.7547,44.9571],[-92.7527,44.9527],[-92.7523,44.9481],[-92.753,44.9369],[-92.7534,44.9237],[-92.7547,44.9159],[-92.7569,44.9105],[-92.7606,44.9068],[-92.7645,44.9046],[-92.767,44.9039],[-92.7707,44.9023],[-92.7729,44.901],[-92.775,44.8982],[-92.7738,44.8933],[-92.7689,44.8848],[-92.7632,44.8759],[-92.7628,44.8716],[-92.763,44.8671],[-92.7644,44.8622],[-92.7682,44.8554],[-92.7683,44.853],[-92.7671,44.8494],[-92.7652,44.8462],[-92.7646,44.8423],[-92.7644,44.8382],[-92.766,44.8308],[-92.7679,44.8265],[-92.7719,44.8211],[-92.7751,44.8161],[-92.7784,44.8125],[-92.7801,44.8095],[-92.781,44.8056],[-92.7823,44.8029],[-92.783,44.7966],[-92.7858,44.7893],[-92.7909,44.7842],[-92.7993,44.7765],[-92.802,44.7729],[-92.8046,44.7683],[-92.8059,44.7624],[-92.8073,44.7524],[-92.8061,44.7483],[-92.8054,44.7473],[-92.8022,44.7446],[-92.7901,44.7381],[-92.7805,44.7344],[-92.7722,44.7317],[-92.7658,44.7289],[-92.7569,44.7234],[-92.7536,44.7226],[-92.7471,44.7204],[-92.7415,44.7192],[-92.7339,44.7157],[-92.737,44.658],[-92.7386,44.6329],[-92.7957,44.6305],[-92.7915,44.5452],[-92.9165,44.5449],[-92.9179,44.5221],[-92.9218,44.518],[-92.9282,44.5158],[-92.9321,44.513],[-92.941,44.5149],[-92.9449,44.5131],[-92.9494,44.5104],[-92.9584,44.514],[-92.9634,44.5177],[-92.975,44.5159],[-92.9827,44.5173],[-92.991,44.5215],[-93.0057,44.5197],[-93.0121,44.5175],[-93.0166,44.5166],[-93.0275,44.5198],[-93.0301,44.5148],[-93.0346,44.5148],[-93.039,44.5171],[-93.0406,44.4729],[-93.2826,44.473],[-93.2798,44.546],[-93.5259,44.5466],[-93.9091,44.5446],[-93.9117,44.5492],[-93.9078,44.5528],[-93.9027,44.5524],[-93.9008,44.5492],[-93.8956,44.5483],[-93.8937,44.5515],[-93.8963,44.5561],[-93.9008,44.5606],[-93.8996,44.5647],[-93.8957,44.5675],[-93.8958,44.5711],[-93.8996,44.5743],[-93.8958,44.5775],[-93.8939,44.5807],[-93.8959,44.5871],[-93.8991,44.5903],[-93.8908,44.5962],[-93.8857,44.5967],[-93.8838,44.6012],[-93.878,44.6013],[-93.878,44.6077],[-93.8716,44.6063],[-93.8658,44.6063],[-93.8569,44.6168],[-93.8563,44.6218],[-93.8505,44.6219],[-93.8447,44.6201],[-93.8422,44.6233],[-93.8358,44.6242],[-93.8319,44.6251],[-93.8217,44.6297],[-93.8031,44.6366],[-93.7999,44.6361],[-93.7967,44.6343],[-93.7935,44.6311],[-93.7883,44.632],[-93.78,44.6362],[-93.7768,44.6385],[-93.7729,44.6366],[-93.7723,44.6325],[-93.7691,44.6312],[-93.7665,44.6362],[-93.7685,44.6417],[-93.7686,44.675],[-93.8887,44.6756],[-93.8902,44.7185],[-94.0104,44.719],[-94.0085,44.8947],[-94.0136,44.8951],[-94.0117,44.9796],[-93.7692,44.9789],[-93.7702,45.0734],[-93.7663,45.077],[-93.7631,45.0839],[-93.7534,45.0853],[-93.7399,45.0894],[-93.7341,45.0922],[-93.7322,45.0963],[-93.7257,45.1022],[-93.7225,45.11],[-93.72,45.1205],[-93.7155,45.1269],[-93.7019,45.1374],[-93.6852,45.1489],[-93.6793,45.1525],[-93.6716,45.1562],[-93.6574,45.1585],[-93.6554,45.1599],[-93.6529,45.1631],[-93.6503,45.169],[-93.6516,45.1841],[-93.6549,45.1905],[-93.6555,45.1969],[-93.6562,45.201],[-93.6471,45.2079],[-93.6387,45.2074],[-93.6361,45.206],[-93.6329,45.2056],[-93.6258,45.2092],[-93.6167,45.2115],[-93.6096,45.2111],[-93.6031,45.2111],[-93.5967,45.2134],[-93.5857,45.2189],[-93.5792,45.2189],[-93.5734,45.2202],[-93.5676,45.2225],[-93.5617,45.2289],[-93.554,45.2298],[-93.5462,45.2289],[-93.5371,45.2294],[-93.5332,45.2317],[-93.5197,45.2417],[-93.5158,45.2458],[-93.5138,45.2454],[-93.5093,45.4163]]]},\"properties\"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,{"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":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":10340,"text":"ofr82744 - 1982 - Documentation and user's guide for interactive spectral analysis and filter program package useful in the processing of seismic reflection data","interactions":[],"lastModifiedDate":"2012-02-02T00:06:23","indexId":"ofr82744","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":"82-744","title":"Documentation and user's guide for interactive spectral analysis and filter program package useful in the processing of seismic reflection data","docAbstract":"The spectral analysis and filter program package is written in the BASIC language for the HP-9845T desktop computer. The program's main purpose is to perform spectral analyses on digitized time-domain data. In addition, band-pass filtering of the data can be performed in the time domain. Various other processes such as autocorrelation can be performed to the time domain data in order to precondition them for spectral analyses. The frequency domain data can also be transformed back into the time domain if desired. Any data can be displayed on the CRT in graphic form using a variety of plot routines. A hard copy can be obtained immediately using the internal thermal printer. Data can also be displayed in tabular form on the CRT or internal thermal printer or it can be stored permanently on a mass storage device like a tape or disk. A list of the processes performed in the order in which they occurred can be displayed at any time.","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/ofr82744","usgsCitation":"Miller, J.J., 1982, Documentation and user's guide for interactive spectral analysis and filter program package useful in the processing of seismic reflection data: U.S. Geological Survey Open-File Report 82-744, 55 p., ill. ;28 cm., https://doi.org/10.3133/ofr82744.","productDescription":"55 p., ill. ;28 cm.","costCenters":[],"links":[{"id":143662,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1982/0744/report-thumb.jpg"},{"id":38191,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1982/0744/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a6be4b07f02db63d7a6","contributors":{"authors":[{"text":"Miller, J. J.","contributorId":54588,"corporation":false,"usgs":true,"family":"Miller","given":"J.","email":"","middleInitial":"J.","affiliations":[],"preferred":false,"id":161220,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
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