{"pageNumber":"1602","pageRowStart":"40025","pageSize":"25","recordCount":46651,"records":[{"id":10953,"text":"ofr83298 - 1983 - Geophysical investigations of the Umm ar Rummf copper prospect, Al Qunfudhah Quadrangle, Kingdom of Saudi Arabia","interactions":[],"lastModifiedDate":"2012-02-02T00:06:28","indexId":"ofr83298","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1983","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":"83-298","title":"Geophysical investigations of the Umm ar Rummf copper prospect, Al Qunfudhah Quadrangle, Kingdom of Saudi Arabia","docAbstract":"The Umm ar Rummf copper prospect, located about 30 km east of Al Qunfudhah, Kingdom of Saudi Arabia, consists of zones of malachite disseminations and fracture fillings in outcrops of north-trending impure quartzite of the Bahah group. Systematic Crone electromagnetic and self-potential surveys indicate that weakly conductive tabular bodies having a weak to moderate self-potential effect extend downdip from two discontinuously exposed, parallel ridges of mineralized quartzite. Crone electromagnetic data were quantitatively interpreted using characteristic parameter lines adapted for use at 1830 and 5010 Hz, the frequencies employed at Umm ar Rummf. Depths to the top of the conductors were computed to be from 20 to 40 m or about the thickness of the oxidized zone, which behaves as a variably conductive overburden. Both tabular conductors can also be traced geophysically to the north and south of the copper-bearing outcrops. The association of the geophysical anomalies with copper-mineralized rocks has been proved by drilling. \r\n\r\nReconnaissance MAXMIN electromagnetic profiles across the target using a wide coil separation show broad, low-amplitude anomalies that may indicate mineralized rocks at depth, and reconnaissance ground-magnetic profiles show strong total-field intensity anomalies associated with basaltic dikes of probable Tertiary age. In the central part of the area of investigation, these dikes produce large disturbances of the electrical fields.","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/ofr83298","usgsCitation":"Sadek, H.S., and Blank, H.R., 1983, Geophysical investigations of the Umm ar Rummf copper prospect, Al Qunfudhah Quadrangle, Kingdom of Saudi Arabia: U.S. Geological Survey Open-File Report 83-298, iii, 37 p. ill., maps ;28 cm., https://doi.org/10.3133/ofr83298.","productDescription":"iii, 37 p. ill., maps ;28 cm.","costCenters":[],"links":[{"id":144187,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1983/0298/report-thumb.jpg"},{"id":38723,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1983/0298/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":38724,"rank":401,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1983/0298/plate-2.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":38725,"rank":402,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1983/0298/plate-3.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":38726,"rank":403,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1983/0298/plate-4.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":38727,"rank":404,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1983/0298/plate-5.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":38728,"rank":405,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1983/0298/plate-6.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":38729,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1983/0298/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ac8e4b07f02db67c0c3","contributors":{"authors":[{"text":"Sadek, Hamdy S.","contributorId":19158,"corporation":false,"usgs":true,"family":"Sadek","given":"Hamdy","email":"","middleInitial":"S.","affiliations":[],"preferred":false,"id":162262,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Blank, H. Richard","contributorId":69541,"corporation":false,"usgs":true,"family":"Blank","given":"H.","email":"","middleInitial":"Richard","affiliations":[],"preferred":false,"id":162263,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":8216,"text":"ofr83399 - 1983 - Sourcebook of locations of geophysical surveys in tunnels and horizontal holes including results of seismic-refraction surveys, Rainier Mesa, Aqueduct Mesa, and Area 16, Nevada Test Site","interactions":[],"lastModifiedDate":"2021-11-23T20:25:52.204531","indexId":"ofr83399","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1983","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":"83-399","title":"Sourcebook of locations of geophysical surveys in tunnels and horizontal holes including results of seismic-refraction surveys, Rainier Mesa, Aqueduct Mesa, and Area 16, Nevada Test Site","docAbstract":"<p>Seismic refraction surveys have been obtained sporadically in tunnels in zeolitized tuff at the Nevada Test Site since the late 1950's. Commencing in 1967 and continuing to date (1982), extensive measurements of shear- and compressional-wave velocities have been made in five tunnel complexes in Rainier and Aqueduct Mesas and in one tunnel complex in Shoshone Mountain. The results of these surveys to 1980 are compiled in this report. In addition, extensive horizontal drilling was initiated in 1967 in connection with geologic exploration in these tunnel complexes for sites for nuclear weapons tests. Seismic and electrical surveys were conducted in the majority of these holes. The type and location of these tunnel and borehole surveys are indexed in this report. Synthesis of the seismic refraction data indicates a mean compressional-wave velocity near the nuclear device point (WP) of 23 tunnel events of 2,430 m/s (7,970 f/s) with a range of 1,846-2,753 m/s (6,060-9,030 f/s). The mean shear-wave velocity of 17 tunnel events is 1,276 m/s (4,190 f/s) with a range of 1,140-1,392 m/s (3,740-4,570 f/s). Experience indicates that these velocity variations are due chiefly to the extent of fracturing and (or) the presence of partially saturated rock in the region of the survey.</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr83399","usgsCitation":"Carroll, R.D., and Kibler, J.E., 1983, Sourcebook of locations of geophysical surveys in tunnels and horizontal holes including results of seismic-refraction surveys, Rainier Mesa, Aqueduct Mesa, and Area 16, Nevada Test Site: U.S. Geological Survey Open-File Report 83-399, Report: iv, 85 p.; 12 Plates: 24.94 × 9.99 inches or smaller, https://doi.org/10.3133/ofr83399.","productDescription":"Report: iv, 85 p.; 12 Plates: 24.94 × 9.99 inches or smaller","costCenters":[],"links":[{"id":141557,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1983/0399/report-thumb.jpg"},{"id":35830,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1983/0399/plate-01.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":35831,"rank":401,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1983/0399/plate-02.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":35832,"rank":402,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1983/0399/plate-03.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":35833,"rank":403,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1983/0399/plate-04.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":35834,"rank":404,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1983/0399/plate-05.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":35835,"rank":405,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1983/0399/plate-06.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":35836,"rank":406,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1983/0399/plate-07.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":35837,"rank":407,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1983/0399/plate-08.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":35838,"rank":408,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1983/0399/plate-09.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":35839,"rank":409,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1983/0399/plate-10.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":35842,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1983/0399/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":392065,"rank":16,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_14011.htm"},{"id":35840,"rank":410,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1983/0399/plate-11.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":35841,"rank":411,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1983/0399/plate-12.pdf","linkFileType":{"id":1,"text":"pdf"}}],"country":"United States","state":"Nevada","otherGeospatial":"Aqueduct Mesa, Area 16, Nevada Test Site, Rainier Mesa","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,\n              37\n            ],\n            [\n              -116,\n              37.25\n            ],\n            [\n              -116.25,\n              37.25\n            ],\n            [\n              -116.25,\n              37\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e49e6e4b07f02db5e76e6","contributors":{"authors":[{"text":"Carroll, R. D.","contributorId":53373,"corporation":false,"usgs":true,"family":"Carroll","given":"R.","email":"","middleInitial":"D.","affiliations":[],"preferred":false,"id":157358,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Kibler, J. E.","contributorId":49358,"corporation":false,"usgs":true,"family":"Kibler","given":"J.","email":"","middleInitial":"E.","affiliations":[],"preferred":false,"id":157357,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":29860,"text":"wri834066 - 1983 - Exploratory drilling and aquifer testing at the Kipahulu District, Haleakala National Park, Maui, Hawaii","interactions":[],"lastModifiedDate":"2023-01-09T20:45:17.860682","indexId":"wri834066","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1983","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":"83-4066","title":"Exploratory drilling and aquifer testing at the Kipahulu District, Haleakala National Park, Maui, Hawaii","docAbstract":"<p>An exploratory well, located at 388 feet above sea level in Kipahulu Valley on Maui, Hawaii, was completed and tested in October 1980. The 410-foot well penetrates a series of very dense basaltic lava flows of the Hana Formation. At an elevation of 10 feet above mean sea level, the well penetrated a water-bearing zone of permeable basaltic rock. Water from this zone had a head of about 76 feet above sea level. In October of 1980, the well was pump tested for 9 hours at various discharge rates up to 350 gallons per minute with a maximum drawdown of about 12 feet. Based on the test data, the well should produce water at a rate of 200 gallons per minute with a drawdown of less than 3 feet. The water level in the well was continuously monitored from October 1980 to mid-November 1981, during which period a maximum decline of 20 feet was recorded. Water level fluctuations in the well can be correlated to the flow in nearby Palikea Stream. The long-term water level in the well should stabilize at about 75 feet above sea level. Water quality was excellent. The total dissolved-solids content was 49 milligrams per liter and the chloride content was 4.2 milligrams per liter.&nbsp;</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/wri834066","usgsCitation":"Souza, W.R., 1983, Exploratory drilling and aquifer testing at the Kipahulu District, Haleakala National Park, Maui, Hawaii: U.S. Geological Survey Water-Resources Investigations Report 83-4066, v, 26 p., https://doi.org/10.3133/wri834066.","productDescription":"v, 26 p.","costCenters":[],"links":[{"id":58671,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wri/1983/4066/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":123551,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wri/1983/4066/report-thumb.jpg"},{"id":411586,"rank":3,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_35701.htm","linkFileType":{"id":5,"text":"html"}}],"country":"United States","state":"Hawaii","otherGeospatial":"Haleakala National Park","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -156.25717163085938,\n              20.580081709180345\n            ],\n            [\n              -156.01547241210938,\n              20.580081709180345\n            ],\n            [\n              -156.01547241210938,\n              20.78693059257028\n            ],\n            [\n              -156.25717163085938,\n              20.78693059257028\n            ],\n            [\n              -156.25717163085938,\n              20.580081709180345\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e49ffe4b07f02db5f78f4","contributors":{"authors":[{"text":"Souza, W. R.","contributorId":102114,"corporation":false,"usgs":true,"family":"Souza","given":"W.","email":"","middleInitial":"R.","affiliations":[],"preferred":false,"id":202254,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":61507,"text":"mf1381C - 1983 - Map and interpretation of aeromagnetic data for the Wild Rogue Wilderness, Coos and Curry Counties, Oregon","interactions":[],"lastModifiedDate":"2016-08-23T10:35:31","indexId":"mf1381C","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1983","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":"1381","chapter":"C","title":"Map and interpretation of aeromagnetic data for the Wild Rogue Wilderness, Coos and Curry Counties, Oregon","docAbstract":"<p>The Wild Rogue Wilderness is located in Coos and Curry Counties, southwestern Oregon and covers part of the Bone Mountain, Marial, and Agness 15-minute quadrangles (fig. 1). It is an elongate area 19 mi by 1 to 3 mi (31 km by 1.3 to 5 km) and covers approximately 35,818 acres extending from the town of Agness to Mount Bolivar.</p>\n<p>The mapped geology of the Wild Rogue Wilderness (Gray and others, 1982) consists of a tectonic wedge of volcanic and intrusive rocks of Jurassic age surrounded on all sides by thick sequences of Jurassic, Creacetous, and Tertiary sedimentary rocks. Normally, volcanic and intrusive rocks are more magnetic than sedimentary rocks, a property which should be reflected by the areomagnetic data. We conclude, however, that most of the magnetic anomalies of the Wild Rogue Wilderness are caused by magnetic rocks that are not exposed but which occur at relatively shallow depth below the topographic surface.&nbsp;</p>","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Reston, VA","doi":"10.3133/mf1381C","usgsCitation":"Blakely, R.J., and Senior, L., 1983, Map and interpretation of aeromagnetic data for the Wild Rogue Wilderness, Coos and Curry Counties, Oregon: U.S. Geological Survey Miscellaneous Field Studies Map 1381, 36.37 x 34.88 inches, https://doi.org/10.3133/mf1381C.","productDescription":"36.37 x 34.88 inches","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[],"links":[{"id":180497,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/mf1381C.PNG"},{"id":327598,"rank":1,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/mf/1381-C/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}}],"scale":"48000","country":"United States","state":"Oregon","county":"Coos, Curry","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -124.08333333333333,42.583333333333336 ], [ -124.08333333333333,42.833333333333336 ], [ -123.83333333333333,42.833333333333336 ], [ -123.83333333333333,42.583333333333336 ], [ -124.08333333333333,42.583333333333336 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a8fe4b07f02db655409","contributors":{"authors":[{"text":"Blakely, Richard J. 0000-0003-1701-5236 blakely@usgs.gov","orcid":"https://orcid.org/0000-0003-1701-5236","contributorId":1540,"corporation":false,"usgs":true,"family":"Blakely","given":"Richard","email":"blakely@usgs.gov","middleInitial":"J.","affiliations":[{"id":312,"text":"Geology, Minerals, Energy, and Geophysics Science Center","active":true,"usgs":true},{"id":662,"text":"Western Mineral and Environmental Resources Science Center","active":true,"usgs":true}],"preferred":true,"id":265841,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Senior, Lisa","contributorId":81989,"corporation":false,"usgs":true,"family":"Senior","given":"Lisa","affiliations":[],"preferred":false,"id":265842,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":18571,"text":"ofr83856 - 1983 - Geohydrologic data for test well USW H-6 Yucca Mountain area, Nye County, Nevada","interactions":[],"lastModifiedDate":"2012-02-02T00:07:29","indexId":"ofr83856","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1983","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":"83-856","title":"Geohydrologic data for test well USW H-6 Yucca Mountain area, Nye County, Nevada","docAbstract":"The following data are presented for test well USW H-6: drilling operations, lithology, availability of borehole geophysical logs , water levels, future availability of core analyses, water chemistry, pumping tests, and packer-injection tests. The well is one of a series of test wells drilled in and near Yucca Mountain adjacent to the Nevada Test Site, Nye County, Nevada, in cooperation with the U.S. Department of Energy. These investigations are part of the Nevada Nuclear Waste Storage Investigations to identify suitable sites for underground storage of high-level radioactive wastes. Test well USW H-6 was drilled to a total depth of 1,220 m. Rocks penetrated are predominantly ash-flow tuffs. Lava was encountered from 877 to 1 ,126 m. The composite static water level is approximately 526 m below land surface. The well was pumped during two periods. Maximum drawdown was about 18 m after pumping for 4,822 min at 28 L/sec, and 12 m after pumping for 2,226 min at 27 L/sec. A borehole flow survey showed that 91% of the water withdrawn from the well came from the depth intervals from 616 to 631 m, and from 777 to 788 m. (Author 's abstract)","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/ofr83856","usgsCitation":"Craig, R.W., Reed, R., and Spengler, R., 1983, Geohydrologic data for test well USW H-6 Yucca Mountain area, Nye County, Nevada: U.S. Geological Survey Open-File Report 83-856, v, 52 p. :ill., maps ;28 cm., https://doi.org/10.3133/ofr83856.","productDescription":"v, 52 p. :ill., maps ;28 cm.","costCenters":[],"links":[{"id":151993,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1983/0856/report-thumb.jpg"},{"id":47925,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1983/0856/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b1be4b07f02db6a8f29","contributors":{"authors":[{"text":"Craig, R. W.","contributorId":40984,"corporation":false,"usgs":true,"family":"Craig","given":"R.","email":"","middleInitial":"W.","affiliations":[],"preferred":false,"id":179357,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Reed, R.L.","contributorId":20332,"corporation":false,"usgs":true,"family":"Reed","given":"R.L.","email":"","affiliations":[],"preferred":false,"id":179356,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Spengler, R.W.","contributorId":7281,"corporation":false,"usgs":true,"family":"Spengler","given":"R.W.","email":"","affiliations":[],"preferred":false,"id":179355,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":7764,"text":"ofr8329 - 1983 - Pumpage data from irrigation wells in eastern Laramie County, Wyoming, and Kimball County, Nebraska","interactions":[],"lastModifiedDate":"2017-09-20T15:56:09","indexId":"ofr8329","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1983","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":"83-29","title":"Pumpage data from irrigation wells in eastern Laramie County, Wyoming, and Kimball County, Nebraska","docAbstract":"Quantitative information concerning pumpage by irrigation wells is an integral component of the U.S. Geological Survey High Plains Regional Aquifer System Analysis. Thus, operation time, discharge rate, and irrigated acreage were measured at approximately 450 randomly selected irrigation wells within 10 areas of the High Plains during the 1980 irrigation season. The data were used to estimate the seasonal mean application of water to crops and to project total pumpage by irrigation wells in 1980 throughout the High Plains area. As part of the sampling effort, 50 irrigation wells were randomly chosen from the area of eastern Laramie County, Wyoming, and Kimball County, Nebraska. Required information was collected on only 40 of the wells. For these wells, the seasonal mean application of water on the irrigated land was 15.2 inches. For the major crop types, the seasonal mean application, in inches, were as follows: alfalfa, 19.8; corn, 15.4; potatoes, 13.8; beans, 12.8; and small grains 10.2. (USGS)","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/ofr8329","usgsCitation":"Avery, C., 1983, Pumpage data from irrigation wells in eastern Laramie County, Wyoming, and Kimball County, Nebraska: U.S. Geological Survey Open-File Report 83-29, 25 p. maps ;28 cm., https://doi.org/10.3133/ofr8329.","productDescription":"25 p. maps ;28 cm.","costCenters":[{"id":5050,"text":"WY-MT Water Science Center","active":true,"usgs":true}],"links":[{"id":142268,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1983/0029/report-thumb.jpg"},{"id":35242,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1983/0029/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a90e4b07f02db65586e","contributors":{"authors":[{"text":"Avery, Charles","contributorId":70739,"corporation":false,"usgs":true,"family":"Avery","given":"Charles","affiliations":[],"preferred":false,"id":156560,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":56202,"text":"wdrNY821 - 1983 - Water resources data, New York, water year 1982, volume 1, eastern New York, excluding Long Island","interactions":[],"lastModifiedDate":"2020-05-12T23:04:07.044521","indexId":"wdrNY821","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1983","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":340,"text":"Water Data Report","code":"WDR","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"NY-82-1","title":"Water resources data, New York, water year 1982, volume 1, eastern New York, excluding Long Island","docAbstract":"<p>No abstract available.&nbsp;</p>","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Reston, VA","doi":"10.3133/wdrNY821","usgsCitation":"Zembrzuski, T., Burke, P.M., Archer, R., and Robideau, J., 1983, Water resources data, New York, water year 1982, volume 1, eastern New York, excluding Long Island: U.S. Geological Survey Water Data Report NY-82-1, viii, 267 p. , https://doi.org/10.3133/wdrNY821.","productDescription":"viii, 267 p. 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Jr.","contributorId":75594,"corporation":false,"usgs":true,"family":"Zembrzuski","given":"T.J.","suffix":"Jr.","email":"","affiliations":[],"preferred":false,"id":254914,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Burke, P. M.","contributorId":8478,"corporation":false,"usgs":true,"family":"Burke","given":"P.","email":"","middleInitial":"M.","affiliations":[],"preferred":false,"id":254911,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Archer, R.J.","contributorId":55069,"corporation":false,"usgs":true,"family":"Archer","given":"R.J.","email":"","affiliations":[],"preferred":false,"id":254913,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Robideau, J.A.","contributorId":17617,"corporation":false,"usgs":true,"family":"Robideau","given":"J.A.","email":"","affiliations":[],"preferred":false,"id":254912,"contributorType":{"id":1,"text":"Authors"},"rank":4}]}}
,{"id":29011,"text":"wri834084 - 1983 - Simulated effects of anticipated coal mining on dissolved solids in selected tributaries of the Yampa River, northwestern Colorado","interactions":[],"lastModifiedDate":"2012-02-02T00:08:53","indexId":"wri834084","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1983","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":"83-4084","title":"Simulated effects of anticipated coal mining on dissolved solids in selected tributaries of the Yampa River, northwestern Colorado","docAbstract":"Identifying cumulative effects of coal mining on dissolved solids downstream from multipe coal-mining operations is particularly important in western basins. The problem of identifying cumulative effects is evident in the Trout Creek drainage, a tributary to the Yampa River in northwestern Colorado, where a number of mines are active and mine expansions are planned. As an evaluation tool, a model was developed and calibrated for the Trout Creek drainage and a reach of the Yampa River main stem. This model uses a series of nodes on the stream network to sum water quantity and quality through the network. The model operates on a monthly basis and uses data from water years 1976 to 1981. Output is mean monthly discharge, dissolved-solids concentration, and dissolved-solids load. Observed data are needed to initiate the model and for model calibration. Some data were extrapolated from records of nearby streamflow-gaging stations. Some nodes within the stream network were for inputs from anticipated mining and were inactive during calibrations. After calibration, these nodes were used to input water discharge at a given dissolved-solids concentration to reflect various future mine configurations. (USGS)","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/wri834084","usgsCitation":"Parker, R.S., and Norris, J.M., 1983, Simulated effects of anticipated coal mining on dissolved solids in selected tributaries of the Yampa River, northwestern Colorado: U.S. Geological Survey Water-Resources Investigations Report 83-4084, vi, 72 p. :ill., map ;28 cm., https://doi.org/10.3133/wri834084.","productDescription":"vi, 72 p. :ill., map ;28 cm.","costCenters":[],"links":[{"id":159492,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wri/1983/4084/report-thumb.jpg"},{"id":57877,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wri/1983/4084/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a80e4b07f02db64953e","contributors":{"authors":[{"text":"Parker, R. S.","contributorId":104510,"corporation":false,"usgs":true,"family":"Parker","given":"R.","email":"","middleInitial":"S.","affiliations":[],"preferred":false,"id":200784,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Norris, J. M.","contributorId":87953,"corporation":false,"usgs":true,"family":"Norris","given":"J.","email":"","middleInitial":"M.","affiliations":[],"preferred":false,"id":200783,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":41747,"text":"ofr83150 - 1983 - Approximate water-level changes in wells in the Chicot and Evangeline aquifers, 1977-83 and 1982-83 and measured compaction, 1973-83 in Harris and Galvestan counties, Texas","interactions":[],"lastModifiedDate":"2016-08-11T15:37:32","indexId":"ofr83150","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1983","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":"83-150","title":"Approximate water-level changes in wells in the Chicot and Evangeline aquifers, 1977-83 and 1982-83 and measured compaction, 1973-83 in Harris and Galvestan counties, Texas","docAbstract":"<p>This report, which was prepared in cooperation with the City of Hoston, the Harris-Galveston Coastal Subsidence District, and the Texas Department of Water Resources, presents data on water-level changes in the Chicot and Evangeline aquifers.</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr83150","usgsCitation":"Strause, J.L., and Ranzau, C., 1983, Approximate water-level changes in wells in the Chicot and Evangeline aquifers, 1977-83 and 1982-83 and measured compaction, 1973-83 in Harris and Galvestan counties, Texas: U.S. Geological Survey Open-File Report 83-150, 7 p., https://doi.org/10.3133/ofr83150.","productDescription":"7 p.","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[{"id":583,"text":"Texas Water Science Center","active":true,"usgs":true}],"links":[{"id":176676,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1983/0150/report-thumb.jpg"},{"id":79465,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1983/0150/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ac5e4b07f02db67a152","contributors":{"authors":[{"text":"Strause, Jeffrey L.","contributorId":61420,"corporation":false,"usgs":true,"family":"Strause","given":"Jeffrey","email":"","middleInitial":"L.","affiliations":[],"preferred":false,"id":225470,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Ranzau, C.E. Jr.","contributorId":41831,"corporation":false,"usgs":true,"family":"Ranzau","given":"C.E.","suffix":"Jr.","email":"","affiliations":[],"preferred":false,"id":225469,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":26699,"text":"wri834194 - 1983 - Estimating generalized flood skew coefficients for Michigan","interactions":[],"lastModifiedDate":"2016-09-16T10:19:33","indexId":"wri834194","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1983","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":"83-4194","title":"Estimating generalized flood skew coefficients for Michigan","docAbstract":"<p>Current estimates of station skew indicate that estimates of generalized skew obtained from the skew map of the United States prepared by the U.S. Water Resources Council have a -0.27 bias for Michigan. Station skew was recomputed using currently recommended statistical procedures of the Water Resources Council, and available data through 1982. Generalized skew is combined with station skew in order to improve estimates of flood-flow frequencies. As a result of this study, the mean station skew for each of three designated regions can be used to estimate generalized skew in Michigan. The Upper Peninsula has a skew of 0.12; the southwest part of the Lower Peninsula has a skew of 0.081; the remainder of the Lower Peninsula has a skew of -0.17. The mean-square error associated with generalized skew determined on the basis of designated regions is 0.2. </p>","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Lansing, MI","doi":"10.3133/wri834194","collaboration":"Prepared jointly with Michigan Department of Natural Resources, Water Management Division","usgsCitation":"Croskey, H., and Holtschlag, D., 1983, Estimating generalized flood skew coefficients for Michigan: U.S. Geological Survey Water-Resources Investigations Report 83-4194, iv, 27 p., https://doi.org/10.3133/wri834194.","productDescription":"iv, 27 p.","costCenters":[{"id":382,"text":"Michigan Water Science Center","active":true,"usgs":true}],"links":[{"id":121931,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wri/1983/4194/report-thumb.jpg"},{"id":55570,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wri/1983/4194/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"country":"United 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J. 0000-0001-5185-4928","orcid":"https://orcid.org/0000-0001-5185-4928","contributorId":102493,"corporation":false,"usgs":true,"family":"Holtschlag","given":"D. J.","affiliations":[],"preferred":false,"id":196849,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":8116,"text":"ofr83139 - 1983 - Hydrologic data from the Tamarack Wildlife Area and vicinity, Logan County, Colorado","interactions":[],"lastModifiedDate":"2012-02-02T00:06:05","indexId":"ofr83139","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1983","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":"83-139","title":"Hydrologic data from the Tamarack Wildlife Area and vicinity, Logan County, Colorado","docAbstract":"Hydrologic data were collected from the Tamarack Ranch Wildlife area and vicinity near Crook, Colo., during the period September 1979 to August 1981. These data will aid in the analysis of the effects of proposed water-development projects on the hydrologic system of the wildlife area. The data collected included a reconnaissance evaluation of specific conductance, a 24-hour sampling of air and water temperature at 6 sites, and periodic measurements of water levels, temperature, and specific conductance at 57 sites.","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/ofr83139","usgsCitation":"Burns, A.W., 1983, Hydrologic data from the Tamarack Wildlife Area and vicinity, Logan County, Colorado: U.S. Geological Survey Open-File Report 83-139, 126 p. ill., maps ;28 cm., https://doi.org/10.3133/ofr83139.","productDescription":"126 p. ill., maps ;28 cm.","costCenters":[],"links":[{"id":140649,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1983/0139/report-thumb.jpg"},{"id":35719,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1983/0139/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":35720,"rank":401,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1983/0139/plate-2.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":35721,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1983/0139/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a1be4b07f02db6076dc","contributors":{"authors":[{"text":"Burns, Alan W.","contributorId":41419,"corporation":false,"usgs":true,"family":"Burns","given":"Alan","email":"","middleInitial":"W.","affiliations":[],"preferred":false,"id":157177,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":29005,"text":"wri834020 - 1983 - Initial assessment of time of travel and mixing through Gulf Island Pond and the lower Androscoggin River, Maine","interactions":[],"lastModifiedDate":"2012-02-02T00:08:52","indexId":"wri834020","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1983","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":"83-4020","title":"Initial assessment of time of travel and mixing through Gulf Island Pond and the lower Androscoggin River, Maine","docAbstract":"Flow-stratification patterns were observed in Gulf Island Pond during time-of-travel studies in May and August 1980. The stratification patterns in this 70 million cubic-meter impoundment were due to a temperature differences between inflowing water and reservoir water. Separation was observed at temperature differences of 0.5 degrees C in May 1980 and 1.0 degrees C in August 1980. The pathway taken by inflowing water through the reservoir was governed by the temperature-related density forces acting between the two water masses. Data collected during August 1980 to define differences in dye concentrations with depth at two fixed profile points in Gulf Island Pond showed average water velocity to be seven times faster near the bottom than near the surface. A concept of mass flow was used to analyze data collected at sites downstream from Gulf Island Dam where flow varied rapidly with time. This report presents the mathematical derivation of controid traveltime, skewness, and percentage recovery of dye mass as determined from mass versus time curves. (USGS)","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/wri834020","usgsCitation":"Parker, G., and Hunt, G., 1983, Initial assessment of time of travel and mixing through Gulf Island Pond and the lower Androscoggin River, Maine: U.S. Geological Survey Water-Resources Investigations Report 83-4020, vii, 60 p. :ill., maps ;28 cm., https://doi.org/10.3133/wri834020.","productDescription":"vii, 60 p. :ill., maps ;28 cm.","costCenters":[],"links":[{"id":123299,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wri/1983/4020/report-thumb.jpg"},{"id":57872,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wri/1983/4020/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e49c1e4b07f02db5d33cb","contributors":{"authors":[{"text":"Parker, G.W.","contributorId":100374,"corporation":false,"usgs":true,"family":"Parker","given":"G.W.","email":"","affiliations":[],"preferred":false,"id":200775,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Hunt, G.S.","contributorId":20360,"corporation":false,"usgs":true,"family":"Hunt","given":"G.S.","email":"","affiliations":[],"preferred":false,"id":200774,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":18599,"text":"ofr83695 - 1983 - Annual water-resources review, White Sands Missile Range, New Mexico, 1982","interactions":[],"lastModifiedDate":"2022-01-07T21:35:47.318265","indexId":"ofr83695","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1983","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":"83-695","title":"Annual water-resources review, White Sands Missile Range, New Mexico, 1982","docAbstract":"<p>Ground-water data were collected in 1982 at White Sands Missile Range in south-central New Mexico. Depth-to-water measurements in the Post Headquarters supply wells continued to show seasonal declines. Test wells east of the Headquarters well field continue to show long-term declines as well as seasonal fluctuations. The total amount of water pumped from White Sands Missile Range supply wells was 66,226,600 gallons more in 1982 than in 1981. The difference in the specific-conductance values of the water samples collected from the Post Headquarters supply wells in the winter and summer increased in 1982.</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr83695","usgsCitation":"Cruz, R.R., 1983, Annual water-resources review, White Sands Missile Range, New Mexico, 1982: U.S. Geological Survey Open-File Report 83-695, iv, 20 p., https://doi.org/10.3133/ofr83695.","productDescription":"iv, 20 p.","costCenters":[],"links":[{"id":47944,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1983/0695/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":394070,"rank":3,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_14176.htm"},{"id":150690,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1983/0695/report-thumb.jpg"}],"country":"United States","state":"New Mexico","otherGeospatial":"White Sands Missile Range","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -106.816,\n              32.316\n            ],\n            [\n              -106.041,\n              32.316\n            ],\n            [\n              -106.041,\n              34.325\n            ],\n            [\n              -106.816,\n              34.325\n            ],\n            [\n              -106.816,\n              32.316\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ac8e4b07f02db67b77e","contributors":{"authors":[{"text":"Cruz, R. R.","contributorId":97496,"corporation":false,"usgs":true,"family":"Cruz","given":"R.","email":"","middleInitial":"R.","affiliations":[],"preferred":false,"id":179407,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":7946,"text":"ofr83435 - 1983 - Oregon; basic data for thermal springs and wells as recorded in Geotherm","interactions":[],"lastModifiedDate":"2012-02-02T00:06:02","indexId":"ofr83435","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1983","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":"83-435","title":"Oregon; basic data for thermal springs and wells as recorded in Geotherm","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/ofr83435","usgsCitation":"Bliss, J.D., 1983, Oregon; basic data for thermal springs and wells as recorded in Geotherm: U.S. Geological Survey Open-File Report 83-435, iv, 342 leaves ;28 cm., https://doi.org/10.3133/ofr83435.","productDescription":"iv, 342 leaves ;28 cm.","costCenters":[],"links":[{"id":140871,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1983/0435/report-thumb.jpg"},{"id":35517,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1983/0435/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4aeee4b07f02db691238","contributors":{"authors":[{"text":"Bliss, James D. jbliss@usgs.gov","contributorId":2790,"corporation":false,"usgs":true,"family":"Bliss","given":"James","email":"jbliss@usgs.gov","middleInitial":"D.","affiliations":[{"id":312,"text":"Geology, Minerals, Energy, and Geophysics Science Center","active":true,"usgs":true}],"preferred":true,"id":156874,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":55704,"text":"wdrMO821 - 1983 - Water resources data, Missouri, water year 1982","interactions":[],"lastModifiedDate":"2025-07-18T16:13:05.364494","indexId":"wdrMO821","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1983","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":340,"text":"Water Data Report","code":"WDR","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"MO-82-1","title":"Water resources data, Missouri, water year 1982","docAbstract":"<p>Water resources data for the 1982 water year for Missouri consist of records of stage, discharge, and water quality of lakes and reservoirs; contains records for water discharge at 112 gaging stations; stage and contents at 9 lakes and reservoirs; water quality at 30 gaging stations (including 1 lake) and data for 47 crest-stage, and 17 water-quality partial record stations.</p>","language":"English","publisher":"U.S. 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,{"id":7949,"text":"ofr83436 - 1983 - Texas; basic data for thermal springs and wells as recorded in Geotherm","interactions":[],"lastModifiedDate":"2012-02-02T00:06:02","indexId":"ofr83436","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1983","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":"83-436","title":"Texas; basic data for thermal springs and wells as recorded in Geotherm","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/ofr83436","usgsCitation":"Bliss, J.D., 1983, Texas; basic data for thermal springs and wells as recorded in Geotherm: U.S. Geological Survey Open-File Report 83-436, v, 437 p.  ;28 cm., https://doi.org/10.3133/ofr83436.","productDescription":"v, 437 p.  ;28 cm.","costCenters":[],"links":[{"id":140885,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1983/0436/report-thumb.jpg"},{"id":35520,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1983/0436/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ad5e4b07f02db683762","contributors":{"authors":[{"text":"Bliss, James D. jbliss@usgs.gov","contributorId":2790,"corporation":false,"usgs":true,"family":"Bliss","given":"James","email":"jbliss@usgs.gov","middleInitial":"D.","affiliations":[{"id":312,"text":"Geology, Minerals, Energy, and Geophysics Science Center","active":true,"usgs":true}],"preferred":true,"id":156877,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":7156,"text":"ofr83403 - 1983 - Geochemical data for samples of rock, stream sediment, and nonmagnetic dense-mineral concentrate in the Andrews Mountain, Mazourka, and Paiute Roadless Areas, Inyo County, California","interactions":[],"lastModifiedDate":"2012-02-02T00:06:04","indexId":"ofr83403","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1983","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":"83-403","title":"Geochemical data for samples of rock, stream sediment, and nonmagnetic dense-mineral concentrate in the Andrews Mountain, Mazourka, and Paiute Roadless Areas, Inyo County, California","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/ofr83403","usgsCitation":"Donahoe, J.L., Chaffee, M., Fey, D., Hill, R.H., and Sutley, S.J., 1983, Geochemical data for samples of rock, stream sediment, and nonmagnetic dense-mineral concentrate in the Andrews Mountain, Mazourka, and Paiute Roadless Areas, Inyo County, California: U.S. Geological Survey Open-File Report 83-403, 152 p. maps ;28 cm., https://doi.org/10.3133/ofr83403.","productDescription":"152 p. maps ;28 cm.","costCenters":[],"links":[{"id":140517,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1983/0403/report-thumb.jpg"},{"id":34500,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1983/0403/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":34501,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1983/0403/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b24e4b07f02db6ae44f","contributors":{"authors":[{"text":"Donahoe, James L.","contributorId":48554,"corporation":false,"usgs":true,"family":"Donahoe","given":"James","email":"","middleInitial":"L.","affiliations":[],"preferred":false,"id":154532,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Chaffee, M.A.","contributorId":108049,"corporation":false,"usgs":true,"family":"Chaffee","given":"M.A.","affiliations":[],"preferred":false,"id":154535,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Fey, D.L.","contributorId":44537,"corporation":false,"usgs":true,"family":"Fey","given":"D.L.","email":"","affiliations":[],"preferred":false,"id":154531,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Hill, R. H.","contributorId":57059,"corporation":false,"usgs":true,"family":"Hill","given":"R.","email":"","middleInitial":"H.","affiliations":[],"preferred":false,"id":154533,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"Sutley, S. J.","contributorId":91484,"corporation":false,"usgs":true,"family":"Sutley","given":"S.","email":"","middleInitial":"J.","affiliations":[],"preferred":false,"id":154534,"contributorType":{"id":1,"text":"Authors"},"rank":5}]}}
,{"id":57293,"text":"wdrWV821 - 1983 - Water resources data West Virginia, water year 1982","interactions":[],"lastModifiedDate":"2025-02-26T20:00:54.138059","indexId":"wdrWV821","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1983","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":340,"text":"Water Data Report","code":"WDR","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"WV-82-1","title":"Water resources data West Virginia, water year 1982","docAbstract":"<p>Water resources data for the 1982 water year for West Virginia consist of records of stage, discharge, and water quality of streams and springs; stage and contents of lakes and reservoirs; and water levels in wells. This report contains discharge records for 116 gaging stations; stage only records for 9 gaging stations; stage and contents for 8 lakes and reservoirs; contents for 1 reservoir; change in contents for 1 reservoir; water quality for 55 gaging stations; and water levels for 29 observation wells. Also included are 2 crest-stage partial-record stations, and 1 low-flow partial record station. Additional water data were collected at various sites, not part of the systematic data collections program, and are published as miscellaneous measurements and analyses. These data represent that part of the National Water Data System operated by the U.S. Geological Survey and cooperating State and Federal Agencies in West Virginia. <br></p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/wdrWV821","collaboration":"Prepared in cooperation with the State of West Virginia and with other agencies","usgsCitation":"Embree, W., Friel, E., Ehlke, T.A., and Ward, S., 1983, Water resources data West Virginia, water year 1982: U.S. Geological Survey Water Data Report WV-82-1, ix, 342 p., https://doi.org/10.3133/wdrWV821.","productDescription":"ix, 342 p.","costCenters":[],"links":[{"id":482456,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wdr/1982/wv-82-1/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":181887,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wdr/1982/wv-82-1/report-thumb.jpg"}],"country":"United States","state":"West 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,{"id":7552,"text":"ofr83493 - 1983 - A summary of U.S. Geological Survey marine geological data collected in the Beaufort Sea, Alaska, 1982","interactions":[],"lastModifiedDate":"2012-02-02T00:06:01","indexId":"ofr83493","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1983","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":"83-493","title":"A summary of U.S. Geological Survey marine geological data collected in the Beaufort Sea, Alaska, 1982","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/ofr83493","usgsCitation":"Kempema, E.W., Barnes, P.W., Reimnitz, E., Asbury, J., and Rearic, D., 1983, A summary of U.S. Geological Survey marine geological data collected in the Beaufort Sea, Alaska, 1982: U.S. Geological Survey Open-File Report 83-493, 10 p. ill., maps ;28 cm., https://doi.org/10.3133/ofr83493.","productDescription":"10 p. ill., maps ;28 cm.","costCenters":[],"links":[{"id":140698,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1983/0493/report-thumb.jpg"},{"id":35015,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1983/0493/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b17e4b07f02db6a60c4","contributors":{"authors":[{"text":"Kempema, Edward W.","contributorId":39780,"corporation":false,"usgs":true,"family":"Kempema","given":"Edward","email":"","middleInitial":"W.","affiliations":[],"preferred":false,"id":156092,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Barnes, P. W.","contributorId":8819,"corporation":false,"usgs":true,"family":"Barnes","given":"P.","email":"","middleInitial":"W.","affiliations":[],"preferred":false,"id":156090,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Reimnitz, Erk","contributorId":17963,"corporation":false,"usgs":true,"family":"Reimnitz","given":"Erk","email":"","affiliations":[],"preferred":false,"id":156091,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Asbury, J.L.","contributorId":79098,"corporation":false,"usgs":true,"family":"Asbury","given":"J.L.","email":"","affiliations":[],"preferred":false,"id":156094,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"Rearic, D.M.","contributorId":65463,"corporation":false,"usgs":true,"family":"Rearic","given":"D.M.","affiliations":[],"preferred":false,"id":156093,"contributorType":{"id":1,"text":"Authors"},"rank":5}]}}
,{"id":7939,"text":"ofr83429 - 1983 - Colorado; basic data for thermal springs and wells as recorded in Geotherm","interactions":[],"lastModifiedDate":"2012-02-02T00:06:02","indexId":"ofr83429","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1983","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":"83-429","title":"Colorado; basic data for thermal springs and wells as recorded in Geotherm","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/ofr83429","usgsCitation":"Bliss, J.D., 1983, Colorado; basic data for thermal springs and wells as recorded in Geotherm: U.S. Geological Survey Open-File Report 83-429, 176 p.  ;28 cm., https://doi.org/10.3133/ofr83429.","productDescription":"176 p.  ;28 cm.","costCenters":[],"links":[{"id":140808,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1983/0429/report-thumb.jpg"},{"id":35510,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1983/0429/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b24e4b07f02db6ae7e8","contributors":{"authors":[{"text":"Bliss, James D. jbliss@usgs.gov","contributorId":2790,"corporation":false,"usgs":true,"family":"Bliss","given":"James","email":"jbliss@usgs.gov","middleInitial":"D.","affiliations":[{"id":312,"text":"Geology, Minerals, Energy, and Geophysics Science Center","active":true,"usgs":true}],"preferred":true,"id":156867,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":7942,"text":"ofr83431A - 1983 - Idaho; basic data for thermal springs and wells as recorded in Geotherm; Part A","interactions":[],"lastModifiedDate":"2012-02-02T00:06:02","indexId":"ofr83431A","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1983","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":"83-431","chapter":"A","title":"Idaho; basic data for thermal springs and wells as recorded in Geotherm; Part A","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/ofr83431A","usgsCitation":"Bliss, J.D., 1983, Idaho; basic data for thermal springs and wells as recorded in Geotherm; Part A: U.S. Geological Survey Open-File Report 83-431, 64 p.  ;28 cm., https://doi.org/10.3133/ofr83431A.","productDescription":"64 p.  ;28 cm.","costCenters":[],"links":[{"id":140867,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1983/0431a/report-thumb.jpg"},{"id":35513,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1983/0431a/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a09e4b07f02db5faae3","contributors":{"authors":[{"text":"Bliss, James D. jbliss@usgs.gov","contributorId":2790,"corporation":false,"usgs":true,"family":"Bliss","given":"James","email":"jbliss@usgs.gov","middleInitial":"D.","affiliations":[{"id":312,"text":"Geology, Minerals, Energy, and Geophysics Science Center","active":true,"usgs":true}],"preferred":true,"id":156870,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":7934,"text":"ofr83426 - 1983 - Alaska; basic data for thermal springs and wells as recorded in Geotherm","interactions":[],"lastModifiedDate":"2012-02-02T00:06:02","indexId":"ofr83426","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1983","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":"83-426","title":"Alaska; basic data for thermal springs and wells as recorded in Geotherm","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/ofr83426","usgsCitation":"Bliss, J.D., 1983, Alaska; basic data for thermal springs and wells as recorded in Geotherm: U.S. Geological Survey Open-File Report 83-426, 1 v. in various pagings ;28 cm., https://doi.org/10.3133/ofr83426.","productDescription":"1 v. in various pagings ;28 cm.","costCenters":[],"links":[{"id":140798,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1983/0426/report-thumb.jpg"},{"id":35505,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1983/0426/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ae0e4b07f02db6883aa","contributors":{"authors":[{"text":"Bliss, James D. jbliss@usgs.gov","contributorId":2790,"corporation":false,"usgs":true,"family":"Bliss","given":"James","email":"jbliss@usgs.gov","middleInitial":"D.","affiliations":[{"id":312,"text":"Geology, Minerals, Energy, and Geophysics Science Center","active":true,"usgs":true}],"preferred":true,"id":156862,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":7936,"text":"ofr83428A - 1983 - California; basic data for thermal springs and wells as recorded in Geotherm; Part A","interactions":[],"lastModifiedDate":"2012-02-02T00:06:02","indexId":"ofr83428A","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1983","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":"83-428","chapter":"A","title":"California; basic data for thermal springs and wells as recorded in Geotherm; Part A","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/ofr83428A","usgsCitation":"Bliss, J.D., 1983, California; basic data for thermal springs and wells as recorded in Geotherm; Part A: U.S. Geological Survey Open-File Report 83-428, 109 p.  ;28 cm., https://doi.org/10.3133/ofr83428A.","productDescription":"109 p.  ;28 cm.","costCenters":[],"links":[{"id":140800,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1983/0428a/report-thumb.jpg"},{"id":35507,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1983/0428a/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a06e4b07f02db5f8be1","contributors":{"authors":[{"text":"Bliss, James D. jbliss@usgs.gov","contributorId":2790,"corporation":false,"usgs":true,"family":"Bliss","given":"James","email":"jbliss@usgs.gov","middleInitial":"D.","affiliations":[{"id":312,"text":"Geology, Minerals, Energy, and Geophysics Science Center","active":true,"usgs":true}],"preferred":true,"id":156864,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":8965,"text":"ofr83517 - 1983 - Mineralogical and sedimentological data collected on the shelf and upper slope adjacent to the Russian River, Northern California","interactions":[],"lastModifiedDate":"2012-02-02T00:06:10","indexId":"ofr83517","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1983","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":"83-517","title":"Mineralogical and sedimentological data collected on the shelf and upper slope adjacent to the Russian River, Northern California","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/ofr83517","usgsCitation":"Gardner, J.V., and Klise, D.H., 1983, Mineralogical and sedimentological data collected on the shelf and upper slope adjacent to the Russian River, Northern California: U.S. Geological Survey Open-File Report 83-517, 35 p. ill., maps ;28 cm., https://doi.org/10.3133/ofr83517.","productDescription":"35 p. ill., maps ;28 cm.","costCenters":[],"links":[{"id":141144,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1983/0517/report-thumb.jpg"},{"id":36585,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1983/0517/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b05e4b07f02db699e88","contributors":{"authors":[{"text":"Gardner, James V.","contributorId":93035,"corporation":false,"usgs":true,"family":"Gardner","given":"James","email":"","middleInitial":"V.","affiliations":[],"preferred":false,"id":158636,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Klise, David H.","contributorId":13977,"corporation":false,"usgs":true,"family":"Klise","given":"David","email":"","middleInitial":"H.","affiliations":[],"preferred":false,"id":158635,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":7277,"text":"ofr83296 - 1983 - Late Proterozoic island-arc complexes and tectonic belts in the southern part of the Arabian Shield, Kingdom of Saudi Arabia","interactions":[],"lastModifiedDate":"2012-02-02T00:05:57","indexId":"ofr83296","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1983","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":"83-296","title":"Late Proterozoic island-arc complexes and tectonic belts in the southern part of the Arabian Shield, Kingdom of Saudi Arabia","docAbstract":"Two main subdivisions of layered rocks are recognized in the southern Arabian Shield south of lat 22? N. These are an older ensimatic-arc complex, which formed 1100-800 m.y. ago, and a younger marginal-arc complex, which formed 800-690 m.y. ago. The older ensimatic-arc complex, located in the southwestern part of the Shield, includes graywacke and mafic to intermediate volcanic rocks of the essentially contemporaneous Baish, Bahah, and Jiddah groups. Although the younger arc complex is also dominantly ensimatic in character, it is also partly superimposed over the older ensimaticarc complex. The superimposed portions of the younger arc complex are represented by the Ablah, Samran, and possibly the Ararat groups. The ensimatic portion of the younger arc group is represented by the Halaban group, which was deposited to the east and northeast of the older ensimatic-arc complex. The Halaban group includes andesitic and dacitic volcanic rocks and associated clastic sedimentary rocks. The layered rocks of both arc complexes are intruded by dioritic (quartz diorite, tonalite, trondhjemite) plutonic rocks. \r\n\r\nThe southern Shield is also subdivided into a number of structurally bounded, north-trending tectonic belts. Within the older ensimatic complex, three belts are recognized. From west to east, these are the Lith, Bidah, and Tayyah belts. Within these three belts, progressive facies changes indicate a gradation from deep-water facies in the south to shallow-water or-terrestrial facies in the north. The distribution of dioritic batholiths, as well as the distribution of layered-rock facies, suggests a northwest-trending axis for the older ensimatic-arc complex. The younger arc complex is present within six belts, the Makkah source papers. In Fleck and others (1980), the term 'quartz diorite' includes both tonalite and quartz diorite as defined in the International Union of Geological Sciences (IUGS) system of plutonic rock classification (Streckeisen, 1973). \r\n\r\nInitial 87Sr/86Sr ratios are not included in the appendix, but all rocks more than 660 m.y. old have initial ratios in the range 0.7021-0.7035, with only two greater than 0.7030. Thus, nothing in the Rb-Sr data suggests involvement of an older continental crust during the evolution of the southern Shield. A lead isotope study of ore minerals and potassium feldspars of the Arabian Shield by Stacey and others (1980) also suggests that no older (Archean to early Proterozoic) evolved continental-type crust underlies the southern Shield. An early summary of mapping (Schmidt and others, 1973) suggests that older sialic basement underlies the late Proterozoic layered rocks in the southern Shield. However, subsequent-mapping and the isotopic studies cited above have established that all of these rocks are of late Proterozoic age and that all rocks of the southern Shield that are more than 660 m.y. old have ensimatic or mantle isotopic characteristics. \r\n\r\nFigure 2 shows, with only two exceptions, that rocks more than 800 m.y. old are present west of the boundary separating the Tayyah and Khadra belts. The exceptions are two poorly controlled Rb-Sr ages obtained by Fleck (1980) on two quartz diorite plutons in the Malahah region (appendix 1, localities 26 and 27). Preliminary uranium-thorium zircon data of Stacey now suggest that one of these quartz diorite plutons (locality 26) has an age of approximately 640 m.y. Therefore, we prefer to discount the two dates of Fleck until further information is available. \r\n\r\nAs noted earlier and as described below, most of the rocks of the southern Arabian Shield have characteristics typical of those formed in the island-arc environment by subduction-related processes. We shall refer to the group of rocks in the western part of the southern Shield, which formed from 1100 to 800 m.y. ago, as the 'older ensimatic-arc complex' and those in the eastern and northwestern parts, which formed from 800 to 690 m.y. ago, as the 'younger marginal-arc compl","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/ofr83296","usgsCitation":"Greenwood, W., Stoeser, D.B., Fleck, R., and Stacey, J.S., 1983, Late Proterozoic island-arc complexes and tectonic belts in the southern part of the Arabian Shield, Kingdom of Saudi Arabia: U.S. Geological Survey Open-File Report 83-296, 49 p. maps ;28 cm., https://doi.org/10.3133/ofr83296.","productDescription":"49 p. maps ;28 cm.","costCenters":[],"links":[{"id":140032,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1983/0296/report-thumb.jpg"},{"id":34654,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1983/0296/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b1be4b07f02db6a8b9a","contributors":{"authors":[{"text":"Greenwood, William R.","contributorId":53789,"corporation":false,"usgs":true,"family":"Greenwood","given":"William R.","affiliations":[],"preferred":false,"id":155009,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Stoeser, D. B.","contributorId":18735,"corporation":false,"usgs":true,"family":"Stoeser","given":"D.","email":"","middleInitial":"B.","affiliations":[],"preferred":false,"id":155007,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Fleck, R.J.","contributorId":25147,"corporation":false,"usgs":true,"family":"Fleck","given":"R.J.","email":"","affiliations":[],"preferred":false,"id":155008,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Stacey, J. S.","contributorId":72785,"corporation":false,"usgs":true,"family":"Stacey","given":"J.","email":"","middleInitial":"S.","affiliations":[],"preferred":false,"id":155010,"contributorType":{"id":1,"text":"Authors"},"rank":4}]}}
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