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Jersey\",\"nation\":\"USA \"}}]}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e49f8e4b07f02db5f26b5","contributors":{"authors":[{"text":"Bauersfeld, W.R.","contributorId":72451,"corporation":false,"usgs":true,"family":"Bauersfeld","given":"W.R.","email":"","affiliations":[],"preferred":false,"id":254129,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Moshinsky, E.W.","contributorId":104972,"corporation":false,"usgs":true,"family":"Moshinsky","given":"E.W.","email":"","affiliations":[],"preferred":false,"id":254130,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Pustay, E.A.","contributorId":62604,"corporation":false,"usgs":true,"family":"Pustay","given":"E.A.","affiliations":[],"preferred":false,"id":254127,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Jones, W.D.","contributorId":68384,"corporation":false,"usgs":true,"family":"Jones","given":"W.D.","email":"","affiliations":[],"preferred":false,"id":254128,"contributorType":{"id":1,"text":"Authors"},"rank":4}]}} ,{"id":19275,"text":"ofr88114 - 1988 - National water-information clearinghouse activities; ground-water perspective","interactions":[],"lastModifiedDate":"2012-02-02T00:07:32","indexId":"ofr88114","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1988","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":"88-114","title":"National water-information clearinghouse activities; ground-water perspective","docAbstract":"The US Geological Survey (USGS) has functioned for many years as an informal clearinghouse for water resources information, enabling users to access groundwater information effectively. Water resources clearinghouse activities of the USGS are conducted through several separate computerized water information programs that are involved in the collection, storage, retrieval, and distribution of different types of water information. The following USGS programs perform water information clearinghouse functions and provide the framework for a formalized National Water-Information Clearinghouse: (1) The National Water Data Exchange--a nationwide confederation of more than 300 Federal, State, local, government, academic, and private water-oriented organizations that work together to improve access to water data; (2) the Water Resources Scientific Information Center--acquires, abstracts, and indexes the major water-resources-related literature of the world, and provides this information to the water resources community; (3) the Information Transfer Program--develops innovative approaches to transfer information and technology developed within the USGS to audiences in the public and private sectors; (4) the Hydrologic Information Unit--provides responses to a variety of requests, both technical and lay-oriented, for water resources information , and helps efforts to conduct water resources research; (5) the Water Data Storage and Retrieval System--maintains accessible computerized files of hydrologic data collected nationwide, by the USGS and other governmental agencies, from stream gaging stations, groundwater observation wells, and surface- and groundwater quality sampling sites; (6) the Office of Water Data Coordination--coordinate the water data acquisition activities of all agencies of the Federal Government, and is responsible for the planning, design, and inter-agency coordination of a national water data and information network; and (7) the Water Resources Research Institute Program--coordinates and evaluates activities performed by a variety of groundwater contamination studies ranging from field investigations to analysis of socioeconomic issues. (Lantz-PTT)","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/ofr88114","usgsCitation":"Haupt, C., and Jensen, R., 1988, National water-information clearinghouse activities; ground-water perspective: U.S. Geological Survey Open-File Report 88-114, 2 p. :ill. ;28 cm., https://doi.org/10.3133/ofr88114.","productDescription":"2 p. :ill. ;28 cm.","costCenters":[],"links":[{"id":151295,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1988/0114/report-thumb.jpg"},{"id":48737,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1988/0114/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b00e4b07f02db69802c","contributors":{"authors":[{"text":"Haupt, C.A.","contributorId":87570,"corporation":false,"usgs":true,"family":"Haupt","given":"C.A.","email":"","affiliations":[],"preferred":false,"id":180603,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Jensen, R.A.","contributorId":71570,"corporation":false,"usgs":true,"family":"Jensen","given":"R.A.","email":"","affiliations":[],"preferred":false,"id":180602,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":66623,"text":"i1775 - 1988 - Geologic and aeromagnetic map of a part of the Mescalero Apache Indian Reservation, Otero County, New Mexico","interactions":[],"lastModifiedDate":"2012-02-10T00:11:04","indexId":"i1775","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1988","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":320,"text":"IMAP","code":"I","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"1775","subseriesTitle":"NONE","title":"Geologic and aeromagnetic map of a part of the Mescalero Apache Indian Reservation, Otero County, New Mexico","language":"ENGLISH","doi":"10.3133/i1775","usgsCitation":"Moore, S.L., Foord, E., and Meyer, G., 1988, Geologic and aeromagnetic map of a part of the Mescalero Apache Indian Reservation, Otero County, New Mexico: U.S. Geological Survey IMAP 1775, 1 map :col. ;67 x 96 cm., on sheet 142 x 101 cm., https://doi.org/10.3133/i1775.","productDescription":"1 map :col. ;67 x 96 cm., on sheet 142 x 101 cm.","costCenters":[],"links":[{"id":107121,"rank":700,"type":{"id":15,"text":"Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_9908.htm","linkFileType":{"id":5,"text":"html"},"description":"9908"},{"id":189508,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"}],"scale":"50000","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -105.81777777777778,33 ], [ -105.81777777777778,33.300555555555555 ], [ -105.30138888888888,33.300555555555555 ], [ -105.30138888888888,33 ], [ -105.81777777777778,33 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b1ae4b07f02db6a8342","contributors":{"authors":[{"text":"Moore, S. L.","contributorId":82385,"corporation":false,"usgs":true,"family":"Moore","given":"S.","email":"","middleInitial":"L.","affiliations":[],"preferred":false,"id":274810,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Foord, E.E.","contributorId":86835,"corporation":false,"usgs":true,"family":"Foord","given":"E.E.","email":"","affiliations":[],"preferred":false,"id":274812,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Meyer, G.A.","contributorId":82798,"corporation":false,"usgs":true,"family":"Meyer","given":"G.A.","email":"","affiliations":[],"preferred":false,"id":274811,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}} ,{"id":19277,"text":"ofr88140 - 1988 - U.S. Geological Survey ground-water studies in Oklahoma","interactions":[],"lastModifiedDate":"2012-02-02T00:07:32","indexId":"ofr88140","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1988","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":"88-140","title":"U.S. Geological Survey ground-water studies in Oklahoma","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/ofr88140","usgsCitation":"Havens, J., 1988, U.S. Geological Survey ground-water studies in Oklahoma: U.S. Geological Survey Open-File Report 88-140, 2 p . :ill. ;28 cm., https://doi.org/10.3133/ofr88140.","productDescription":"2 p . :ill. ;28 cm.","costCenters":[],"links":[{"id":151297,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1988/0140/report-thumb.jpg"},{"id":48739,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1988/0140/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a2ae4b07f02db612764","contributors":{"authors":[{"text":"Havens, J.S.","contributorId":12043,"corporation":false,"usgs":true,"family":"Havens","given":"J.S.","email":"","affiliations":[],"preferred":false,"id":180605,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":12069,"text":"ofr86541 - 1988 - Geologic logs for selected deep wells in parts of Oklahoma, Texas, and New Mexico","interactions":[],"lastModifiedDate":"2012-02-02T00:06:36","indexId":"ofr86541","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1988","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":"86-541","title":"Geologic logs for selected deep wells in parts of Oklahoma, Texas, and New Mexico","docAbstract":"A computerized data base of geologic logs for selected deep wells in parts of Oklahoma, Texas, and New Mexico was prepared by the U.S. Geological Survey as part of the Central Midwest Regional Aquifer-System Analysis. At least one well per county in the study area was selected, and the geologic logs for the wells were entered into the data base. Summaries of the geologic logs are presented in this report. Geophysical logs were used for interpretation of the geologic logs, and a list of these geophysical logs also is presented. These geophysical logs are available for inspection at the U.S. Geological Survey office in Oklahoma City, Oklahoma.","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/ofr86541","usgsCitation":"Christenson, S.C., Morton, R.B., Havens, J., and Fairchild, R., 1988, Geologic logs for selected deep wells in parts of Oklahoma, Texas, and New Mexico: U.S. Geological Survey Open-File Report 86-541, iv, 161 p. :ill., map ;28 cm., https://doi.org/10.3133/ofr86541.","productDescription":"iv, 161 p. :ill., map ;28 cm.","costCenters":[],"links":[{"id":144401,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1986/0541/report-thumb.jpg"},{"id":40100,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1986/0541/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b15e4b07f02db6a4ed0","contributors":{"authors":[{"text":"Christenson, Scott C. schris@usgs.gov","contributorId":980,"corporation":false,"usgs":true,"family":"Christenson","given":"Scott","email":"schris@usgs.gov","middleInitial":"C.","affiliations":[{"id":516,"text":"Oklahoma Water Science Center","active":true,"usgs":true}],"preferred":true,"id":164924,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Morton, R. B.","contributorId":36521,"corporation":false,"usgs":true,"family":"Morton","given":"R.","email":"","middleInitial":"B.","affiliations":[],"preferred":false,"id":164926,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Havens, J.S.","contributorId":12043,"corporation":false,"usgs":true,"family":"Havens","given":"J.S.","email":"","affiliations":[],"preferred":false,"id":164925,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Fairchild, R.W.","contributorId":85189,"corporation":false,"usgs":true,"family":"Fairchild","given":"R.W.","email":"","affiliations":[],"preferred":false,"id":164927,"contributorType":{"id":1,"text":"Authors"},"rank":4}]}} ,{"id":12552,"text":"ofr88546 - 1988 - Results of a gravity survey of McCarthy's Marsh, Seward Peninsula, Alaska","interactions":[],"lastModifiedDate":"2022-08-09T19:40:43.314449","indexId":"ofr88546","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1988","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":"88-546","title":"Results of a gravity survey of McCarthy's Marsh, Seward Peninsula, Alaska","docAbstract":"No abstract available.
","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr88546","usgsCitation":"Barnes, D., and Morin, R.L., 1988, Results of a gravity survey of McCarthy's Marsh, Seward Peninsula, Alaska: U.S. Geological Survey Open-File Report 88-546, Report: 12 p.; 2 Plates: 31.90 × 39.60 inches and 31.60 × 39.29 inches, https://doi.org/10.3133/ofr88546.","productDescription":"Report: 12 p.; 2 Plates: 31.90 × 39.60 inches and 31.60 × 39.29 inches","costCenters":[],"links":[{"id":109013,"rank":700,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_19073.htm","linkFileType":{"id":5,"text":"html"},"description":"19073"},{"id":40934,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1988/0546/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":40933,"rank":401,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1988/0546/plate-2.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":40932,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1988/0546/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":145247,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1988/0546/report-thumb.jpg"}],"country":"United States","state":"Alaska","otherGeospatial":"McCarthy's Marsh, Seward Peninsula","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"type\": \"Polygon\",\n \"coordinates\": [\n [\n [\n -163.5,\n 64.75\n ],\n [\n -162.5,\n 64.75\n ],\n [\n -162.5,\n 65.25\n ],\n [\n -163.5,\n 65.25\n ],\n [\n -163.5,\n 64.75\n ]\n ]\n ]\n }\n }\n ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b1ae4b07f02db6a8112","contributors":{"authors":[{"text":"Barnes, David F.","contributorId":72787,"corporation":false,"usgs":true,"family":"Barnes","given":"David F.","affiliations":[],"preferred":false,"id":166319,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Morin, Robert L.","contributorId":82671,"corporation":false,"usgs":true,"family":"Morin","given":"Robert","email":"","middleInitial":"L.","affiliations":[],"preferred":false,"id":166320,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":12138,"text":"ofr88344 - 1988 - Location maps and list of U.S. Geological Survey reports on water resources in Alaska, 1950 to 1988","interactions":[{"subject":{"id":12138,"text":"ofr88344 - 1988 - Location maps and list of U.S. Geological Survey reports on water resources in Alaska, 1950 to 1988","indexId":"ofr88344","publicationYear":"1988","noYear":false,"title":"Location maps and list of U.S. Geological Survey reports on water resources in Alaska, 1950 to 1988"},"predicate":"SUPERSEDED_BY","object":{"id":17308,"text":"ofr9160 - 1991 - Location maps and list of U.S. Geological Survey reports on water resources in Alaska 1950 to 1990","indexId":"ofr9160","publicationYear":"1991","noYear":false,"title":"Location maps and list of U.S. Geological Survey reports on water resources in Alaska 1950 to 1990"},"id":1}],"supersededBy":{"id":17308,"text":"ofr9160 - 1991 - Location maps and list of U.S. Geological Survey reports on water resources in Alaska 1950 to 1990","indexId":"ofr9160","publicationYear":"1991","noYear":false,"title":"Location maps and list of U.S. Geological Survey reports on water resources in Alaska 1950 to 1990"},"lastModifiedDate":"2023-08-08T22:12:55.946273","indexId":"ofr88344","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1988","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":"88-344","title":"Location maps and list of U.S. Geological Survey reports on water resources in Alaska, 1950 to 1988","docAbstract":"The objective of this compilation is to provide a listing of water-resources reports in Alaska by location. For the purposes of this report, Alaska has been divided into six geographic sections: Arctic Slope, West, Southwest, East-Central, Southcentral, and Southeast. In addition, reports are cited in the following categories: Statewide and Topical, Trans-Alaska Pipeline System, and Glaciers. The Statewide and Topical reports are not located on maps. The index to the location maps is on the facing page. The numbers on the location maps refer to the bibliographic citations. (Gaps have been left in the numbering system for additional reports in future editions of this compilation.)
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\"}}]}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a0ce4b07f02db5fcba6","contributors":{"authors":[{"text":"Water Resources Division, U.S. Geological Survey","contributorId":128075,"corporation":true,"usgs":false,"organization":"Water Resources Division, U.S. Geological Survey","id":533108,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":1663,"text":"wsp2284 - 1988 - Evaluation of the ground-water resources of the lower Susquehanna River basin, Pennsylvania and Maryland","interactions":[{"subject":{"id":9106,"text":"ofr84748 - 1985 - Evaluation of the ground-water resources of the lower Susquehanna River basin, Pennsylvania and Maryland","indexId":"ofr84748","publicationYear":"1985","noYear":false,"title":"Evaluation of the ground-water resources of the lower Susquehanna River basin, Pennsylvania and Maryland"},"predicate":"SUPERSEDED_BY","object":{"id":1663,"text":"wsp2284 - 1988 - Evaluation of the ground-water resources of the lower Susquehanna River basin, Pennsylvania and Maryland","indexId":"wsp2284","publicationYear":"1988","noYear":false,"title":"Evaluation of the ground-water resources of the lower Susquehanna River basin, Pennsylvania and Maryland"},"id":1}],"lastModifiedDate":"2017-07-06T09:23:06","indexId":"wsp2284","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1988","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":341,"text":"Water Supply Paper","code":"WSP","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"2284","title":"Evaluation of the ground-water resources of the lower Susquehanna River basin, Pennsylvania and Maryland","docAbstract":"Ground water in the 3,458-square-mile lower Susquehanna River basin occupies secondary openings in bedrock. The distribution of openings is a function of lithology, depth, and topography. Local flow systems account for most of the total ground-water flow. Average annual recharge for the lower basin is 1,857 million gallons per day, most of which discharges to streams. The water table is a subdued replica of land surface; its depth varies with topography but is generally 20 to 70 feet below land surface. Ground water circulates to depths of 500 to 600 feet below the water table. \r\n\r\nA digital model of regional, unconfined groundwater flow was developed and used to evaluate the ground-water resources of the lower basin. On the basis of lithologic and hydrologic differences, the area was subdivided into 21 hydrogeologic units, each with different hydrologic characteristics. Each unit was divided into two layers to take into account decreasing secondary permeability with depth. A finite-difference grid with square blocks approximately 1 mile on a side was used. The model was calibrated under steady-state and transient conditions. In the steady-state calibration, the model-generated results were compared with estimated water-table altitudes and estimated base flows. In the transient calibration, the model-generated results were compared with observed changes in water-table altitude from November 1, 1980, through April 22, 1981. \r\n\r\nHydraulic conductivity increases from hilltops to Valley bottoms. The average hydraulic conductivity for carbonate units is about 21 feet per day, which is an order of magnitude greater than the corresponding averages for Paleozoic sedimentary, Triassic sedimentary, and crystalline units. The Cumberland Valley carbonate rocks have the greatest average hydraulic conductivity-about 174 feet per day in valley bottoms. The average gaining-stream leakage coefficient for all carbonate units is about 16 feet per day, which is two orders of magnitude greater than the corresponding averages for the other lithologies. The Cumberland Valley carbonate rocks have the greatest gaining-stream leakage coefficient--about 43 feet per day. The specific yields are 0.035, 0.020, 0.020, and 0.007 for the carbonate, Paleozoic sedimentary, crystalline, and Triassic sedimentary units, respectively. \r\n\r\nThe calibrated model was used to simulate the effects of a ground-water withdrawal of 1 inch per year on water-table altitudes and average annual base flows in the modeled area. The overall effect is least for the carbonate units and greatest for the Triassic sedimentary units. The model also was used to simulate a standardized potential yield for each unit by assuming that the maximum acceptable consequence of a hypothetical withdrawal scheme is an ultimate 50-percent reduction in average annual base flow. Based on this, the potential yield for the modeled area is 891 million gallons per day. The Cumberland Valley carbonate rocks have the greatest potential yield--0.47 million gallons per day per square mile. The carbonate units have the greatest average potential yield, followed by the Paleozoic sedimentary, crystalline, and Triassic sedimentary units. About 90 percent of the eventual decline in water-table altitudes and the eventual reduction in average annual base flows occurs within 5 years of the implementation of the hypothetical withdrawal scheme. Nearly all of the ground water withdrawn is derived from reduced discharge to streams. \r\n\r\nThe calibrated model can be used to estimate the impacts of ground-water development schemes on regional ground-water levels and base flows of streams, it cannot be used to simulate local cones of depression or local base-flow changes. The reliability of the model is a function of its approximation of the physical characteristics of the ground-water flow system, the two calibrations, various simplifying assumptions, and the lack of calibration under ground-water withdrawal conditions, it ca","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/wsp2284","usgsCitation":"Gerhart, J.M., and Lazorchick, G.J., 1988, Evaluation of the ground-water resources of the lower Susquehanna River basin, Pennsylvania and Maryland: U.S. Geological Survey Water Supply Paper 2284, vi, 128 p. :ill., maps ;28 cm.; 2 plates in pocket, https://doi.org/10.3133/wsp2284.","productDescription":"vi, 128 p. :ill., maps ;28 cm.; 2 plates in pocket","costCenters":[{"id":532,"text":"Pennsylvania Water Science Center","active":true,"usgs":true}],"links":[{"id":138535,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wsp/2284/report-thumb.jpg"},{"id":26735,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wsp/2284/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":26736,"rank":401,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wsp/2284/plate-2.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":26737,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wsp/2284/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b32e4b07f02db6b4340","contributors":{"authors":[{"text":"Gerhart, James M.","contributorId":35717,"corporation":false,"usgs":true,"family":"Gerhart","given":"James","email":"","middleInitial":"M.","affiliations":[],"preferred":false,"id":143937,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Lazorchick, George J.","contributorId":18743,"corporation":false,"usgs":true,"family":"Lazorchick","given":"George","email":"","middleInitial":"J.","affiliations":[],"preferred":false,"id":143936,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":2569,"text":"wsp2342 - 1988 - Volatilization of benzene and eight alkyl-substituted benzene compounds from water","interactions":[],"lastModifiedDate":"2012-02-02T00:05:29","indexId":"wsp2342","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1988","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":341,"text":"Water Supply Paper","code":"WSP","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"2342","title":"Volatilization of benzene and eight alkyl-substituted benzene compounds from water","docAbstract":"Predicting the fate of organic compounds in streams and rivers often requires knowledge of the volatilization characteristics of the compounds. The reference-substance concept, involving laboratory-determined ratios of the liquid-film coefficients for volatilization of the organic compounds to the liquid-film coefficient for oxygen absorption, is used to predict liquid-film coefficients for streams and rivers. In the absence of experimental data, two procedures have been used for estimating these liquid-film coefficient ratios. These procedures, based on the molecular-diffusion coefficient and on the molecular weight, have been widely used but never extensively evaluated. \r\n\r\nLiquid-film coefficients for the volatilization of benzene and eight alkyl-substituted benzene compounds (toluene through n-octylbenzene) from water were measured in a constant-temperature, stirred water bath. Liquid-film coefficients for oxygen absorption were measured simultaneously. A range of water mixing conditions was used with a water temperature of 298.2 K. \r\n\r\nThe ratios of the liquid-film coefficients for volatilization to the liquid-film coefficient for oxygen absorption for all of the organic compounds were independent of mixing conditions in the water. Experimental ratios ranged from 0.606 for benzene to 0.357 for n-octylbenzene. \r\n\r\nThe molecular-diffusion-coefficient procedure accurately predicted the ratios for ethylbenzene through n-pentylbenzene with a power dependence of 0.566 on the molecular-diffusion coefficient, in agreement with published values. Predicted ratios for benzene and toluene were slightly larger than the experimental ratios. These differences were attributed to possible interactions between the molecules of these compounds and the water molecules and to benzene-benzene interactions that form dimers. Because these interactions also are likely to occur in natural waters, it was concluded that the experimental ratios are more correct than the predicted ratios for application purposes in the reference-substance concept. Predicted ratios for n-hexylbenzene, n-heptylbenzene, and n-octylbenzene were larger than the experimental ratios. These differences were attributed to a sorption-desorption process between these compounds and the surfaces of the constant-temperature water bath. Other experimental problems associated with preparing water solutions of these slightly soluble compounds also may have contributed to the differences. Because these processes are not part of the true volatilization process, it was concluded that the predicted ratios for these three compounds are probably more correct than the experimental ratios for application purposes in the reference-substance concept. Any model of the fate of these compounds in streams and rivers would have to include terms accounting for sorption processes, however.\r\n\r\nThe molecular-weight procedure accurately predicted the ratios for ethylbenzene through n-pentylbenzene, but only if the power dependence on the molecular weight was decreased from the commonly used -0.500 to -0.427. Deviations for the low- and high-molecular-weight compounds were similar to those observed for the molecular-diffusion-coefficient procedure.","language":"ENGLISH","publisher":"U.S. G.P.O.,","doi":"10.3133/wsp2342","usgsCitation":"Rathbun, R.E., and Tai, D.Y., 1988, Volatilization of benzene and eight alkyl-substituted benzene compounds from water: U.S. Geological Survey Water Supply Paper 2342, vi, 24 p. : ill. ;28 cm., https://doi.org/10.3133/wsp2342.","productDescription":"vi, 24 p. : ill. ;28 cm.","costCenters":[],"links":[{"id":138589,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wsp/2342/report-thumb.jpg"},{"id":28838,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wsp/2342/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e478fe4b07f02db48a0bd","contributors":{"authors":[{"text":"Rathbun, R. E.","contributorId":61796,"corporation":false,"usgs":true,"family":"Rathbun","given":"R.","email":"","middleInitial":"E.","affiliations":[],"preferred":false,"id":145417,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Tai, D. Y.","contributorId":59778,"corporation":false,"usgs":true,"family":"Tai","given":"D.","email":"","middleInitial":"Y.","affiliations":[],"preferred":false,"id":145416,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":1160,"text":"wsp2234C - 1988 - Phytoplankton dynamics of the fresh, tidal Potomac River, Maryland, for the summers of 1979 to 1981","interactions":[],"lastModifiedDate":"2022-02-07T19:58:22.718738","indexId":"wsp2234C","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1988","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":341,"text":"Water Supply Paper","code":"WSP","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"2234","chapter":"C","title":"Phytoplankton dynamics of the fresh, tidal Potomac River, Maryland, for the summers of 1979 to 1981","docAbstract":"The distribution and abundance of phytoplankton in the fresh, tidal Potomac River, Md., was different during 1979-81 from that observed in the 1960's and 1970's. Concentrations \r\nof phytoplankton in the 1960's and 1970's reached maximum attainable levels that were limited only by self-shading. A sag in phytoplankton abundance, apparent during the summers of 1980 and 1981 between Rosier Bluff and Marshall Hall, appears to have been caused by the Asiatic clam, Corbicula fluminea. Reduced abundance of phytoplankton throughout the entire fresh, tidal river during the summers of 1980 and 1981 may have been due to grazing by Corbicula, high discharge, and perhaps phosphorus limitation in late August at and downstream of Hallowing Point. Phytoplankton growth rates and chlorophyll-to-cell ratios were highest at Hatton Point and Marshall Hall (the sag reach). A model was constructed that predicted phytoplankton growth rates by varying only chlorophyll a concentration and light penetration. Nutrient concentrations were not required to make the model fit the data. \r\n\r\nPrimary productivity was highest for the year during August 1980 and August 1981. Productivity-per-unit chlorophyll was highest at Hatton Point, where reduced concentrations of phytoplankton permitted the deepest light penetration in the fresh, tidal river.","largerWorkType":{"id":18,"text":"Report"},"largerWorkTitle":"A water quality study of the tidal Potomac River and Estuary","largerWorkSubtype":{"id":5,"text":"USGS Numbered Series"},"language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/wsp2234C","usgsCitation":"Cohen, R.R., 1988, Phytoplankton dynamics of the fresh, tidal Potomac River, Maryland, for the summers of 1979 to 1981: U.S. Geological Survey Water Supply Paper 2234, vii, 34 p., https://doi.org/10.3133/wsp2234C.","productDescription":"vii, 34 p.","numberOfPages":"41","costCenters":[],"links":[{"id":395562,"rank":3,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_25405.htm"},{"id":25975,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wsp/2234c/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":137348,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wsp/2234c/report-thumb.jpg"}],"country":"United States","state":"Maryland","otherGeospatial":"Potomac River","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"type\": \"Polygon\",\n \"coordinates\": [\n [\n [\n -77.3712158203125,\n 38.212288054388175\n ],\n [\n -76.9097900390625,\n 38.212288054388175\n ],\n [\n -76.9097900390625,\n 38.89958342598271\n ],\n [\n -77.3712158203125,\n 38.89958342598271\n ],\n [\n -77.3712158203125,\n 38.212288054388175\n ]\n ]\n ]\n }\n }\n ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ad9e4b07f02db684ec2","contributors":{"authors":[{"text":"Cohen, Ronald R.H.","contributorId":87523,"corporation":false,"usgs":true,"family":"Cohen","given":"Ronald","email":"","middleInitial":"R.H.","affiliations":[],"preferred":false,"id":143278,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":2191,"text":"wsp2336A - 1988 - Simulation of flow in the Edwards Aquifer, San Antonio region, Texas, and refinement of storage and flow concepts","interactions":[{"subject":{"id":14775,"text":"ofr86532 - 1987 - Simulation of flow in the Edwards Aquifer, San Antonio region, Texas, and refinement of storage and flow concepts","indexId":"ofr86532","publicationYear":"1987","noYear":false,"title":"Simulation of flow in the Edwards Aquifer, San Antonio region, Texas, and refinement of storage and flow concepts"},"predicate":"SUPERSEDED_BY","object":{"id":2191,"text":"wsp2336A - 1988 - Simulation of flow in the Edwards Aquifer, San Antonio region, Texas, and refinement of storage and flow concepts","indexId":"wsp2336A","publicationYear":"1988","noYear":false,"chapter":"A","title":"Simulation of flow in the Edwards Aquifer, San Antonio region, Texas, and refinement of storage and flow concepts"},"id":1}],"lastModifiedDate":"2016-08-05T11:55:09","indexId":"wsp2336A","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1988","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":341,"text":"Water Supply Paper","code":"WSP","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"2336","chapter":"A","title":"Simulation of flow in the Edwards Aquifer, San Antonio region, Texas, and refinement of storage and flow concepts","docAbstract":"The Edwards aquifer is a complexly faulted, carbonate aquifer lying within the Balcones fault zone of south-central Texas. The aquifer consists of thin- to massive-bedded limestone and dolomite, most of which is in the form of mudstones and wackestones. Well-developed secondary porosity has formed in association with former erosional surfaces within the carbonate rocks, within dolomitized-burrowed tidal and evaporitic deposits, and along inclined fractures to produce an aquifer with transmissivities greater than 100 ft2/s. The aquifer is recharged mainly by streamflow losses in the outcrop area of the Edwards aquifer and is discharged by major springs located at considerable distances, as much as 150 mi, from the areas of recharge and by wells. Ground-water flow within the Edwards aquifer of the San Antonio region was simulated to investigate concepts relating to the storage and flow characteristics. The concepts of major interest were the effects of barrier faults on flow direction, water levels, springflow, and storage within the aquifer. A general-purpose, finite-difference model, modified to provide the capability of representing barrier faults, was used to simulate ground-water flow and storage in the aquifer. The approach in model development was to conduct a series of simulations beginning with a simple representation of the aquifer framework and then proceeding to subsequent representations of increasing complexity. The simulations investigated the effects of complex geologic structures and of significant changes in transmissivity, anisotropy, and storage coefficient. Initial values of transmissivity, anisotropy, and storage coefficient were estimated based on concepts developed in previous studies. Results of the simulations confirmed the original estimates of transmissivity values (greater than 100 square feet/s) in the confined zone of the aquifer between San Antonio and Comal Springs. A storage coefficient of 0.05 in the unconfined zone of the aquifer produced the best simulation of water levels and springflow. A major interpretation resulting from the simulations is that two essentially independent areas of regional flow were identified in the west and central part of the study area. Flows from the two areas converge at Comal Springs. The directions of computed flux vectors reflected the presence of major barrier faults, which locally deflect patterns of ground-water movement. The most noticeable deflection is the convergence of flow through a geologic structural opening, the Knippa gap, in eastern Uvalde County. A second significant interpretation is that ground-water flow in northeastern Bexar, Comal, and Hays Counties is diverted by barrier faults toward San Marcos Springs, a regional discharge point. Simulations showed that several barrier faults in the northwestern part of the San Antonio area had a significant effect on storage, water levels, and springflow within the Edwards aquifer.
","language":"English","publisher":"U.S. Government Printing Office","publisherLocation":"Washington, D.C.","doi":"10.3133/wsp2336A","usgsCitation":"Maclay, R.W., and Land, L.F., 1988, Simulation of flow in the Edwards Aquifer, San Antonio region, Texas, and refinement of storage and flow concepts: U.S. Geological Survey Water Supply Paper 2336, iv, 48 p., https://doi.org/10.3133/wsp2336A.","productDescription":"iv, 48 p.","endPage":"54","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[{"id":583,"text":"Texas Water Science Center","active":true,"usgs":true}],"links":[{"id":27832,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wsp/2336a/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":138266,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wsp/2336a/report-thumb.jpg"}],"country":"United States","state":"Texas","otherGeospatial":"Edwards Aquifer","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e49f8e4b07f02db5f2e45","contributors":{"authors":[{"text":"Maclay, Robert W.","contributorId":13210,"corporation":false,"usgs":true,"family":"Maclay","given":"Robert","email":"","middleInitial":"W.","affiliations":[],"preferred":false,"id":144799,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Land, Larry F.","contributorId":60612,"corporation":false,"usgs":true,"family":"Land","given":"Larry","email":"","middleInitial":"F.","affiliations":[],"preferred":false,"id":144800,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":33493,"text":"b1702A - 1988 - Mineral resources of the Table Top mountain Wilderness Study Area, Maricopa and Pinal counties, Arizona","interactions":[],"lastModifiedDate":"2012-02-02T00:09:34","indexId":"b1702A","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1988","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":"1702","chapter":"A","title":"Mineral resources of the Table Top mountain Wilderness Study Area, Maricopa and Pinal counties, Arizona","language":"ENGLISH","publisher":"U.S. G.P.O.,","doi":"10.3133/b1702A","usgsCitation":"Peterson, J.A., Nowlan, G., Hanna, W.F., Pitkin, J.A., and McDonell, J., 1988, Mineral resources of the Table Top mountain Wilderness Study Area, Maricopa and Pinal counties, Arizona: U.S. Geological Survey Bulletin 1702, v, A18 p. :ill., maps (1 col.) ;28 cm., https://doi.org/10.3133/b1702A.","productDescription":"v, A18 p. :ill., maps (1 col.) ;28 cm.","costCenters":[],"links":[{"id":247408,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/bul/1702a/report.pdf","size":"4537","linkFileType":{"id":1,"text":"pdf"}},{"id":251842,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/bul/1702a/report-thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b06e4b07f02db69a02d","contributors":{"authors":[{"text":"Peterson, Jocelyn A.","contributorId":13954,"corporation":false,"usgs":true,"family":"Peterson","given":"Jocelyn","email":"","middleInitial":"A.","affiliations":[],"preferred":false,"id":211368,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Nowlan, G.A.","contributorId":99131,"corporation":false,"usgs":true,"family":"Nowlan","given":"G.A.","affiliations":[],"preferred":false,"id":211371,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Hanna, W. F.","contributorId":6835,"corporation":false,"usgs":true,"family":"Hanna","given":"W.","email":"","middleInitial":"F.","affiliations":[],"preferred":false,"id":211367,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Pitkin, J. A.","contributorId":85194,"corporation":false,"usgs":true,"family":"Pitkin","given":"J.","middleInitial":"A.","affiliations":[],"preferred":false,"id":211370,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"McDonell, J.R. Jr.","contributorId":52247,"corporation":false,"usgs":true,"family":"McDonell","given":"J.R.","suffix":"Jr.","email":"","affiliations":[],"preferred":false,"id":211369,"contributorType":{"id":1,"text":"Authors"},"rank":5}]}} ,{"id":33801,"text":"b1795 - 1988 - Development of a velocity model for locating aftershocks in the Sierra Pie de Palo region of western Argentina","interactions":[],"lastModifiedDate":"2012-02-02T00:09:37","indexId":"b1795","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1988","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":"1795","title":"Development of a velocity model for locating aftershocks in the Sierra Pie de Palo region of western Argentina","language":"ENGLISH","publisher":"U.S. G.P.O.,","doi":"10.3133/b1795","usgsCitation":"Bollinger, G.A., and Langer, C., 1988, Development of a velocity model for locating aftershocks in the Sierra Pie de Palo region of western Argentina: U.S. Geological Survey Bulletin 1795, iii, 16 p. :ill., maps ;28 cm., https://doi.org/10.3133/b1795.","productDescription":"iii, 16 p. :ill., maps ;28 cm.","costCenters":[],"links":[{"id":167170,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/bul/1795/report-thumb.jpg"},{"id":61706,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/bul/1795/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a9be4b07f02db65e19e","contributors":{"authors":[{"text":"Bollinger, G. A.","contributorId":55809,"corporation":false,"usgs":true,"family":"Bollinger","given":"G.","email":"","middleInitial":"A.","affiliations":[],"preferred":false,"id":211958,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Langer, C.J.","contributorId":31395,"corporation":false,"usgs":true,"family":"Langer","given":"C.J.","email":"","affiliations":[],"preferred":false,"id":211957,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":35427,"text":"b1729C - 1988 - Mineral resources of the Meadow Valley Range Wilderness Study Area, Lincoln and Clark Counties, Nevada","interactions":[],"lastModifiedDate":"2012-02-02T00:09:48","indexId":"b1729C","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1988","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":"1729","chapter":"C","title":"Mineral resources of the Meadow Valley Range Wilderness Study Area, Lincoln and Clark Counties, Nevada","language":"ENGLISH","publisher":"U.S. G.P.O.,","doi":"10.3133/b1729C","usgsCitation":"Pampeyan, E.H., Blank, H.R., and Campbell, H.W., 1988, Mineral resources of the Meadow Valley Range Wilderness Study Area, Lincoln and Clark Counties, Nevada: U.S. Geological Survey Bulletin 1729, v, C24 p. :ill., maps ; 28 cm., https://doi.org/10.3133/b1729C.","productDescription":"v, C24 p. :ill., maps ; 28 cm.","costCenters":[],"links":[{"id":165064,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/bul/1729c/report-thumb.jpg"},{"id":63311,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/bul/1729c/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b06e4b07f02db69a220","contributors":{"authors":[{"text":"Pampeyan, Earl Haig","contributorId":52974,"corporation":false,"usgs":true,"family":"Pampeyan","given":"Earl","email":"","middleInitial":"Haig","affiliations":[],"preferred":false,"id":214616,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Blank, H. Richard Jr.","contributorId":17968,"corporation":false,"usgs":true,"family":"Blank","given":"H.","suffix":"Jr.","email":"","middleInitial":"Richard","affiliations":[],"preferred":false,"id":214615,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Campbell, Harry W.","contributorId":67509,"corporation":false,"usgs":true,"family":"Campbell","given":"Harry","email":"","middleInitial":"W.","affiliations":[],"preferred":false,"id":214617,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}} ,{"id":12130,"text":"ofr88510 - 1988 - The isotopic composition of ore lead of the Creede mining district and vicinity, San Juan Mountains, Colorado: Text of a talk presented at the San Juan Mountains symposium to honor Thomas A. Steven; Rocky Mountain Section meeting of the Geological Society of America, May 2, 1987, Boulder, Colorado","interactions":[],"lastModifiedDate":"2016-03-08T14:15:00","indexId":"ofr88510","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1988","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":"88-510","title":"The isotopic composition of ore lead of the Creede mining district and vicinity, San Juan Mountains, Colorado: Text of a talk presented at the San Juan Mountains symposium to honor Thomas A. Steven; Rocky Mountain Section meeting of the Geological Society of America, May 2, 1987, Boulder, Colorado","docAbstract":"Galenas from the major Creede veins and their northern extensions are remarkably homogeneous in Pb-isotopic composition and are too radiogenic to have been derived from any magma comparable in composition to the principal volcanic rocks. This pattern was identified by Doe et al. in 1979 who proposed that the lead was derived from the Precambrian basement. The homogeneity of the ore leads, however, requires a uniform reservoir; an unlikely prospect for lead from the Precambrian basement. We report on 16 new analyses of geographically and paragenetically dispersed galenas from the Creede district and other areas as far as 11 km to the north. The lead values range from 18.972 to 19.060 for 206Pb/204Pb, from 15.591 to 15.671 for 207Pb/204Pb, and from 37.781 to 37.921 for 208Pb/204Pb. These ranges overlap those previously reported for the main ore zone.
\nRecent work allows us to extend the results of Doe et al. and to consider alternative processes to explain the widespread homogeneity and radiogenic nature of the ore lead: 1) David Matty (pers. commun., 1986) has shown that some minor volcanic units in the area have unusually radiogneic lead values; magmas comparable in composition to the units are a possible, though improbable, source of the ore lead. 2) The uniformity of the isotopic values of galenas may have resulted from homogenization during an extensive potassium-metasomatic event that predated the ores; this possibility is being tested in an on-going study of feldspars from metasomatized and unmetasomatized rocks. 3) Recent regional studies suggest the possibility of a prevolcanic, NNW-trending graben system filled by clastic sediments derived from the Precambrian basement, a process that would have an homogenizing effect on the lead isotopes. This interpretation implies importation, deep within the Creede hydrologic system, of fluids from remote sources. These alternatives show that the Pbisotope systematics may have a profound impact on the interpretation of the Creede hydrothermal system, and that further study is warranted.
","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr88510","usgsCitation":"Foley, N., Barton, P., Bethke, P.M., and Doe, B.R., 1988, The isotopic composition of ore lead of the Creede mining district and vicinity, San Juan Mountains, Colorado: Text of a talk presented at the San Juan Mountains symposium to honor Thomas A. Steven; Rocky Mountain Section meeting of the Geological Society of America, May 2, 1987, Boulder, Colorado: U.S. Geological Survey Open-File Report 88-510, 24 p., https://doi.org/10.3133/ofr88510.","productDescription":"24 p.","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[],"links":[{"id":40159,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1988/0510/report.pdf","text":"Report","size":"5.91 MB","linkFileType":{"id":1,"text":"pdf"},"description":"Report"},{"id":145805,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1988/0510/report-thumb.jpg"}],"country":"United States","state":"Colorado","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"type\": \"Polygon\",\n \"coordinates\": [\n [\n [\n -108.5943603515625,\n 37.00693943418586\n ],\n [\n -108.5943603515625,\n 38.805470223177466\n ],\n [\n -106.116943359375,\n 38.805470223177466\n ],\n [\n -106.116943359375,\n 37.00693943418586\n ],\n [\n -108.5943603515625,\n 37.00693943418586\n ]\n ]\n ]\n }\n }\n ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4822e4b07f02db4e1f1f","contributors":{"authors":[{"text":"Foley, N.K.","contributorId":10801,"corporation":false,"usgs":true,"family":"Foley","given":"N.K.","email":"","affiliations":[],"preferred":false,"id":165185,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Barton, P.B.","contributorId":78751,"corporation":false,"usgs":true,"family":"Barton","given":"P.B.","email":"","affiliations":[],"preferred":false,"id":165188,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Bethke, P. M.","contributorId":32921,"corporation":false,"usgs":true,"family":"Bethke","given":"P.","email":"","middleInitial":"M.","affiliations":[],"preferred":false,"id":165186,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Doe, B. R.","contributorId":52173,"corporation":false,"usgs":true,"family":"Doe","given":"B.","email":"","middleInitial":"R.","affiliations":[],"preferred":false,"id":165187,"contributorType":{"id":1,"text":"Authors"},"rank":4}]}} ,{"id":33560,"text":"b1870 - 1988 - Petroleum systems of the United States","interactions":[],"lastModifiedDate":"2012-02-02T00:09:29","indexId":"b1870","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1988","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":"1870","title":"Petroleum systems of the United States","language":"ENGLISH","publisher":"U.S. G.P.O.,","doi":"10.3133/b1870","usgsCitation":"Magoon, L.B., 1988, Petroleum systems of the United States: U.S. Geological Survey Bulletin 1870, iv, 68 p. :ill. ;28 cm., https://doi.org/10.3133/b1870.","productDescription":"iv, 68 p. :ill. ;28 cm.","costCenters":[],"links":[{"id":167119,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/bul/1870/report-thumb.jpg"},{"id":61450,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/bul/1870/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4adfe4b07f02db687ce1","contributors":{"authors":[{"text":"Magoon, Leslie B. lmagoon@usgs.gov","contributorId":2383,"corporation":false,"usgs":true,"family":"Magoon","given":"Leslie","email":"lmagoon@usgs.gov","middleInitial":"B.","affiliations":[],"preferred":true,"id":211552,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":38418,"text":"pp1486 - 1988 - Palynological analyses of Upper Pennsylvanian coal beds and adjacent strata from the proposed Pennsylvanian System stratotype in West Virginia","interactions":[],"lastModifiedDate":"2012-02-02T00:09:53","indexId":"pp1486","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1988","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":331,"text":"Professional Paper","code":"PP","onlineIssn":"2330-7102","printIssn":"1044-9612","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"1486","title":"Palynological analyses of Upper Pennsylvanian coal beds and adjacent strata from the proposed Pennsylvanian System stratotype in West Virginia","language":"ENGLISH","doi":"10.3133/pp1486","usgsCitation":"Kosanke, R., 1988, Palynological analyses of Upper Pennsylvanian coal beds and adjacent strata from the proposed Pennsylvanian System stratotype in West Virginia: U.S. Geological Survey Professional Paper 1486, 24 p., https://doi.org/10.3133/pp1486.","productDescription":"24 p.","costCenters":[],"links":[{"id":119189,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/pp/1486/report-thumb.jpg"},{"id":64803,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/pp/1486/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ae3e4b07f02db6897f2","contributors":{"authors":[{"text":"Kosanke, R.M.","contributorId":97517,"corporation":false,"usgs":true,"family":"Kosanke","given":"R.M.","email":"","affiliations":[],"preferred":false,"id":219787,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":33462,"text":"b1710E - 1988 - Mineral resources of the Orocopia Mountains Wilderness Study Area, Riverside County, California","interactions":[],"lastModifiedDate":"2012-02-02T00:09:44","indexId":"b1710E","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1988","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":"1710","chapter":"E","title":"Mineral resources of the Orocopia Mountains Wilderness Study Area, Riverside County, California","language":"ENGLISH","publisher":"U.S. G.P.O.,","doi":"10.3133/b1710E","usgsCitation":"Haxel, G.B., Smith, D.B., Whittington, C.L., Griscom, A., Diveley-White, D.V., Powell, R.E., and Kreidler, T.J., 1988, Mineral resources of the Orocopia Mountains Wilderness Study Area, Riverside County, California: U.S. Geological Survey Bulletin 1710, v, p. E1-E22, ill., maps (some col.) ;28 cm., https://doi.org/10.3133/b1710E.","productDescription":"v, p. E1-E22, ill., maps (some col.) ;28 cm.","costCenters":[],"links":[{"id":247404,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/bul/1710e/report.pdf","size":"5368","linkFileType":{"id":1,"text":"pdf"}},{"id":251838,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/bul/1710e/report-thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b06e4b07f02db69a173","contributors":{"authors":[{"text":"Haxel, Gordon B. gbhaxel@usgs.gov","contributorId":5666,"corporation":false,"usgs":true,"family":"Haxel","given":"Gordon","email":"gbhaxel@usgs.gov","middleInitial":"B.","affiliations":[{"id":312,"text":"Geology, Minerals, Energy, and Geophysics Science Center","active":true,"usgs":true}],"preferred":true,"id":211207,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Smith, D. B. davidsmith@usgs.gov","contributorId":12840,"corporation":false,"usgs":true,"family":"Smith","given":"D.","email":"davidsmith@usgs.gov","middleInitial":"B.","affiliations":[],"preferred":false,"id":211208,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Whittington, C. L.","contributorId":33310,"corporation":false,"usgs":true,"family":"Whittington","given":"C.","email":"","middleInitial":"L.","affiliations":[],"preferred":false,"id":211210,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Griscom, Andrew","contributorId":23520,"corporation":false,"usgs":true,"family":"Griscom","given":"Andrew","email":"","affiliations":[],"preferred":false,"id":211209,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"Diveley-White, D. V.","contributorId":86403,"corporation":false,"usgs":true,"family":"Diveley-White","given":"D.","email":"","middleInitial":"V.","affiliations":[],"preferred":false,"id":211212,"contributorType":{"id":1,"text":"Authors"},"rank":5},{"text":"Powell, R. E.","contributorId":93046,"corporation":false,"usgs":true,"family":"Powell","given":"R.","email":"","middleInitial":"E.","affiliations":[],"preferred":false,"id":211213,"contributorType":{"id":1,"text":"Authors"},"rank":6},{"text":"Kreidler, T. J.","contributorId":57460,"corporation":false,"usgs":true,"family":"Kreidler","given":"T.","email":"","middleInitial":"J.","affiliations":[],"preferred":false,"id":211211,"contributorType":{"id":1,"text":"Authors"},"rank":7}]}} ]}