{"pageNumber":"3076","pageRowStart":"76875","pageSize":"25","recordCount":184800,"records":[{"id":31337,"text":"ofr01326 - 2001 - Archive of boomer seismic reflection data collected during USGS cruise 99SCE01, Little River Inlet to the entrance of Winyah Bay, South Carolina, 8 June-16 June, 1999","interactions":[],"lastModifiedDate":"2022-12-09T22:50:04.433962","indexId":"ofr01326","displayToPublicDate":"2001-11-01T00:00:00","publicationYear":"2001","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":"2001-326","title":"Archive of boomer seismic reflection data collected during USGS cruise 99SCE01, Little River Inlet to the entrance of Winyah Bay, South Carolina, 8 June-16 June, 1999","docAbstract":"<p>No abstract available.</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr01326","usgsCitation":"Brewer, G.M., Morton, R., and Wiese, D.S., 2001, Archive of boomer seismic reflection data collected during USGS cruise 99SCE01, Little River Inlet to the entrance of Winyah Bay, South Carolina, 8 June-16 June, 1999: U.S. Geological Survey Open-File Report 2001-326, HTML Document, https://doi.org/10.3133/ofr01326.","productDescription":"HTML Document","costCenters":[],"links":[{"id":159936,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":410252,"rank":3,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_43718.htm","linkFileType":{"id":5,"text":"html"}},{"id":2993,"rank":1,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.usgs.gov/of/2001/of01-326/","linkFileType":{"id":5,"text":"html"}}],"country":"United States","state":"South Carolina","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"coordinates\": [\n          [\n            [\n              -79.01084381056796,\n              33.7381328011203\n            ],\n            [\n              -79.01084381056796,\n              33.441906202991504\n            ],\n            [\n              -78.78744942774979,\n              33.441906202991504\n            ],\n            [\n              -78.78744942774979,\n              33.7381328011203\n            ],\n            [\n              -79.01084381056796,\n              33.7381328011203\n            ]\n          ]\n        ],\n        \"type\": \"Polygon\"\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ac5e4b07f02db679c78","contributors":{"authors":[{"text":"Brewer, Gina M.","contributorId":56269,"corporation":false,"usgs":true,"family":"Brewer","given":"Gina","email":"","middleInitial":"M.","affiliations":[],"preferred":false,"id":205722,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Morton, Robert A.","contributorId":88333,"corporation":false,"usgs":true,"family":"Morton","given":"Robert A.","affiliations":[],"preferred":false,"id":205723,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Wiese, Dana S. dwiese@usgs.gov","contributorId":2476,"corporation":false,"usgs":true,"family":"Wiese","given":"Dana","email":"dwiese@usgs.gov","middleInitial":"S.","affiliations":[{"id":574,"text":"St. Petersburg Coastal and Marine Science Center","active":true,"usgs":true}],"preferred":true,"id":205721,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":30938,"text":"wri014143 - 2001 - Susceptibility index to surface contamination for the Little Cross Creek watershed, Cumberland County, North Carolina","interactions":[],"lastModifiedDate":"2017-01-18T16:52:06","indexId":"wri014143","displayToPublicDate":"2001-11-01T00:00:00","publicationYear":"2001","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":"2001-4143","title":"Susceptibility index to surface contamination for the Little Cross Creek watershed, Cumberland County, North Carolina","docAbstract":"An index of surface-water contamination potential was constructed for the Little Cross Creek Basin, a 9.7-square-mile, water-supply watershed in Cumberland County, North Carolina. The index was developed because previous water-quality investigations raised concerns regarding inputs of bacteria, suspended sediment, and phosphorus from nonpoint sources in the watershed. A geographic information system was used to build map overlays and to categorize and rate three factors that affect the transport of water and contaminants-land-surface slope, distance to water, and land use/land cover. Each factor was weighted to reflect its potential contribution to surface-water contamination; the factors then were combined to estimate susceptibility values for the entire watershed. The numerical susceptibility values were categorized to indicate lowest to highest potential for surface-water contamination, and a map was produced showing the spatial distribution of these categories within the watershed.\n\nThe susceptibility index for about 17 percent of the Little Cross Creek watershed is rated in the high or highest category. These areas have high slopes, short distances to the nearest surface water, impervious land cover, and land uses that generate contaminants. About 38 percent of the watershed area is rated as having low or lowest susceptibility to contamination. These areas contain flat terrain, greater distances to water, land cover that promotes infiltration, and land uses that pose little risk for generating contaminants. Approximately 43 percent of the watershed is in the moderate category of susceptibility. Open water, which is not rated, accounts for the remaining area.\n\nThe susceptibility index provides water-resource managers with a tool that can aid in prioritizing areas within the Little Cross Creek Basin for monitoring, protection, and remediation. Previous suspended sediment, total phosphorus, and fecal coliform data collected in the Little Cross Creek watershed support the results of the susceptibility analysis. Although this susceptibility index is specific to the Little Cross Creek Basin, the methods used to develop the index are transferable to other watersheds.","language":"ENGLISH","doi":"10.3133/wri014143","usgsCitation":"Giorgino, M., and Terziotti, S., 2001, Susceptibility index to surface contamination for the Little Cross Creek watershed, Cumberland County, North Carolina: U.S. Geological Survey Water-Resources Investigations Report 2001-4143, 1 over-size sheet., https://doi.org/10.3133/wri014143.","productDescription":"1 over-size sheet.","costCenters":[{"id":13634,"text":"South Atlantic Water Science Center","active":true,"usgs":true}],"links":[{"id":161260,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":274640,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wri/2001/4143/plate-1.pdf"}],"country":"United States","state":"North Carolina","county":"Cumberland County","otherGeospatial":"Little Cross Creek","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a09e4b07f02db5facf7","contributors":{"authors":[{"text":"Giorgino, M. J.","contributorId":97149,"corporation":false,"usgs":true,"family":"Giorgino","given":"M. J.","affiliations":[],"preferred":false,"id":204400,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Terziotti, Silvia 0000-0003-3559-5844 seterzio@usgs.gov","orcid":"https://orcid.org/0000-0003-3559-5844","contributorId":1613,"corporation":false,"usgs":true,"family":"Terziotti","given":"Silvia","email":"seterzio@usgs.gov","affiliations":[{"id":13634,"text":"South Atlantic Water Science Center","active":true,"usgs":true},{"id":476,"text":"North Carolina Water Science Center","active":true,"usgs":true}],"preferred":true,"id":204399,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":31334,"text":"ofr01310 - 2001 - Potentiometric surface of the upper Floridan Aquifer, west-central Florida, May 2001","interactions":[],"lastModifiedDate":"2012-02-02T00:09:01","indexId":"ofr01310","displayToPublicDate":"2001-11-01T00:00:00","publicationYear":"2001","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":"2001-310","title":"Potentiometric surface of the upper Floridan Aquifer, west-central Florida, May 2001","language":"ENGLISH","doi":"10.3133/ofr01310","usgsCitation":"Duerr, A.D., 2001, Potentiometric surface of the upper Floridan Aquifer, west-central Florida, May 2001: U.S. Geological Survey Open-File Report 2001-310, 1 map ;72 x 69 cm., folded to 22 x 26 cm., https://doi.org/10.3133/ofr01310.","productDescription":"1 map ;72 x 69 cm., folded to 22 x 26 cm.","costCenters":[],"links":[{"id":159928,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":59748,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/2001/0310/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}}],"scale":"500000","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ad4e4b07f02db682c42","contributors":{"authors":[{"text":"Duerr, A. D.","contributorId":29821,"corporation":false,"usgs":true,"family":"Duerr","given":"A.","email":"","middleInitial":"D.","affiliations":[],"preferred":false,"id":205717,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":30943,"text":"wri014181 - 2001 - Water quality in the upper Shoal Creek basin, southwestern Missouri, 1999-2000","interactions":[],"lastModifiedDate":"2012-02-02T00:09:12","indexId":"wri014181","displayToPublicDate":"2001-11-01T00:00:00","publicationYear":"2001","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":"2001-4181","title":"Water quality in the upper Shoal Creek basin, southwestern Missouri, 1999-2000","docAbstract":"Results of a water-quality investigation of the upper Shoal Creek Basin in southwestern Missouri\r\nindicate that concentrations of total nitrite plus nitrate as nitrogen (NO2t+NO3t) in water samples\r\nfrom Shoal Creek were unusually large [mean of 2.90 mg/L (milligrams per liter), n (sample size)=60] compared to other Missouri streams (mean of 1.02 mg/L, n=1,340). A comparison of instantaneous base-flow loads of NO2t+NO3t indicates\r\nthat at base-flow conditions, most NO2t+NO3t discharged by Shoal Creek is from nonpoint sources. Nearly all the base-flow instantaneous\r\nload of total phosphorus as P (Pt) discharged\r\nby Shoal Creek can be attributed to effluent from a municipal wastewater treatment plant. Samples collected from a single runoff event indicate that substantial quantities of Pt can be transported during runoff events compared to base-flow transport. Only minor quantities of NO2t+NO3t are transported during runoff events compared to base-flow transport. Fecal coliform bacteria densities at several locations exceed the Missouri Department of Natural\r\nResources (MDNR) standard of 200 col/100 mL (colonies per 100 milliliters) for whole-body contact recreation. During 13 months of monitoring\r\nat 13 stream sites, fecal coliform densities (median of 277 and 400 col/100 mL) at two sites (sites 2 and 3) on Shoal Creek exceeded the MDNR standard at base-flow conditions. The maximum fecal coliform density of 120,000 col/100 mL was detected at site 3 (MDNR monitoring\r\nsite) during a runoff event in April 1999 at a peak discharge of 1,150 ft3/s (cubic feet per second).\r\nFecal coliform densities also exceeded the MDNR standard in three tributaries with the largest\r\ndensities (median of 580 col/100 mL) detected in Pogue Creek. Results of ribopattern analyses indicate that most Escherichia coli (E. coli) bacteria in water samples from the study area probably are from nonhuman sources. The study area contains about 25,000 cattle, and has an estimated annual production\r\nof 33 million broilers and 300,000 turkeys. Probable nonhuman sources included turkeys, horses, chickens, and cattle; however, wildlife sources such as deer, raccoon, muskrat, and opossum\r\nwere not evaluated. Human waste was an important source of E. coli in water samples collected\r\nat the MDNR monitoring site (site 3) on Shoal Creek and at two tributary sites (Joyce Creek and Woodward Creek). In general, the detection of human ribopatterns was consistent with the detection of organic compounds commonly\r\nassociated with human wastewater such as caffeine, triclosan, or phenol, and the fecal indicators\r\ncholesterol and 3B-coprostanol. Ribopattern analysis indicate that horses were an important source of E. coli in Woodward Creek, which was consistent with horses being pastured immediately upstream from the sampling site on this creek. Pogue Creek contains a large density of turkey barns and five of eight E. coli isolates from one sample from Pogue Creek were matched to turkeys.\r\nWater samples from Pogue Creek generally did not contain detectable concentrations of human wastewater compounds, but one sample did contain detectable quantities of the antibiotics tylosin and lincomycin (widely used in the animal industry), and sulfamethoxazole (human use only). Although promising, the ability of ribopattern\r\nanalyses to positively identify the source of a particular isolate is uncertain because of the small sample size, possible differences between animal source patterns in the study area and database used, lack of native wildlife source patterns, and variation in results depending on the number of possible animal host considered. Results of this study indicate that a trend of increasing fecal coliform densities with increasing time detected by the MDNR is, in part, caused by trends in annual precipitation and stream discharge,\r\nand not necessarily changes in land use or densities of animal operations. A multiple linear regression (MLR) model using specific conductance\r\nand wate","language":"ENGLISH","doi":"10.3133/wri014181","usgsCitation":"Schumacher, J., 2001, Water quality in the upper Shoal Creek basin, southwestern Missouri, 1999-2000: U.S. Geological Survey Water-Resources Investigations Report 2001-4181, 60 p. , https://doi.org/10.3133/wri014181.","productDescription":"60 p. ","costCenters":[],"links":[{"id":2912,"rank":100,"type":{"id":15,"text":"Index Page"},"url":"https://mo.water.usgs.gov/Reports/wrir01-4181-schu/index.htm","linkFileType":{"id":5,"text":"html"}},{"id":95886,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wri/2001/4181/report.pdf","size":"9307","linkFileType":{"id":1,"text":"pdf"}},{"id":119502,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wri/2001/4181/report-thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a07e4b07f02db5f9772","contributors":{"authors":[{"text":"Schumacher, John G. jschu@usgs.gov","contributorId":2055,"corporation":false,"usgs":true,"family":"Schumacher","given":"John G.","email":"jschu@usgs.gov","affiliations":[{"id":396,"text":"Missouri Water Science Center","active":true,"usgs":true}],"preferred":true,"id":204411,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":33066,"text":"b2201E - 2001 - Petroleum geology and resources of the Dnieper-Donets Basin, Ukraine and Russia","interactions":[],"lastModifiedDate":"2024-10-11T10:55:22.655334","indexId":"b2201E","displayToPublicDate":"2001-11-01T00:00:00","publicationYear":"2001","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":"2201","chapter":"E","title":"Petroleum geology and resources of the Dnieper-Donets Basin, Ukraine and Russia","docAbstract":"The Dnieper-Donets basin is almost entirely in Ukraine, and it is the principal producer of hydrocarbons in that country. A small southeastern part of the basin is in Russia. The basin is bounded by the Voronezh high of the Russian craton to the northeast and by the Ukrainian shield to the southwest. The basin is principally a Late Devonian rift that is overlain by a Carboniferous to Early Permian postrift sag. The Devonian rift structure extends northwestward into the Pripyat basin of Belarus; the two basins are separated by the Bragin-Loev uplift, which is a Devonian volcanic center. Southeastward, the Dnieper-Donets basin has a gradational boundary with the Donbas foldbelt, which is a structurally inverted and deformed part of the basin.\r\nThe sedimentary succession of the basin consists of four tectono-stratigraphic sequences. The prerift platform sequence includes Middle Devonian to lower Frasnian, mainly clastic, rocks that were deposited in an extensive intracratonic basin.\r\n1\r\nThe Upper Devonian synrift sequence probably is as thick as 4?5 kilometers. It is composed of marine carbonate, clastic, and volcanic rocks and two salt formations, of Frasnian and Famennian age, that are deformed into salt domes and plugs. The postrift sag sequence consists of Carboniferous and Lower Permian clastic marine and alluvial deltaic rocks that are as thick as 11 kilometers in the southeastern part of the basin. The Lower Permian interval includes a salt formation that is an important regional seal for oil and gas fields. The basin was affected by strong compression in Artinskian (Early Permian) time, when southeastern basin areas were uplifted and deeply eroded and the Donbas foldbelt was formed. The postrift platform sequence includes Triassic through Tertiary rocks that were deposited in a shallow platform depression that extended far beyond the Dnieper-Donets basin boundaries.\r\nA single total petroleum system encompassing the entire sedimentary succession is identified in the Dnieper-Donets basin. Discovered reserves of the system are 1.6 billion barrels of oil and 59 trillion cubic feet of gas. More than one-half of the reserves are in Lower Permian rocks below the salt seal. Most of remaining reserves are in upper Visean-Serpukhovian (Lower Carboniferous) strata. The majority of discovered fields are in salt-cored anticlines or in drapes over Devonian horst blocks; little exploration has been conducted for stratigraphic traps. Synrift Upper Devonian carbonate reservoirs are almost unexplored.\r\nTwo identified source-rock intervals are the black anoxic shales and carbonates in the lower Visean and Devonian sections.\r\nHowever, additional source rocks possibly are present in the deep central area of the basin. The role of Carboniferous coals as a source rock for gas is uncertain; no coal-related gas has been identified by the limited geochemical studies. The source rocks are in the gas-generation window over most of the basin area; consequently gas dominates over oil in the reserves.\r\nThree assessment units were identified in the Dnieper-Donets Paleozoic total petroleum system. The assessment unit that contains all discovered reserves embraces postrift Carboniferous\r\nand younger rocks. This unit also contains the largest portion of undiscovered resources, especially gas. Stratigraphic and combination structural and stratigraphic traps probably will be the prime targets for future exploration. The second assessment\r\nunit includes poorly known synrift Devonian rocks. Carbonate reef reservoirs along the basin margins probably will contain most of the undiscovered resources. The third assessment\r\nunit is an unconventional, continuous, basin-centered gas accumulation in Carboniferous low-permeability clastic rocks. The entire extent of this accumulation is unknown, but it occupies much of the basin area. Resources of this assessment unit were not estimated quantitatively.","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/b2201E","usgsCitation":"Ulmishek, G.F., 2001, Petroleum geology and resources of the Dnieper-Donets Basin, Ukraine and Russia (Version 1.0): U.S. Geological Survey Bulletin 2201, 14 p., https://doi.org/10.3133/b2201E.","productDescription":"14 p.","costCenters":[],"links":[{"id":462805,"rank":3,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/bul/2201/E/b2201-e.pdf","text":"Report","size":"1.39 MB","linkFileType":{"id":1,"text":"pdf"}},{"id":161285,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":3239,"rank":2,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.usgs.gov/bul/2201/E/index.html","linkFileType":{"id":5,"text":"html"}}],"edition":"Version 1.0","contact":"<p><a href=\"https://pubs.usgs.gov/contact\" data-mce-href=\"../contact\">Contact Pubs Warehouse</a></p>","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ae0e4b07f02db687ead","contributors":{"authors":[{"text":"Ulmishek, Gregory F.","contributorId":48971,"corporation":false,"usgs":true,"family":"Ulmishek","given":"Gregory","email":"","middleInitial":"F.","affiliations":[],"preferred":false,"id":209809,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":33064,"text":"b2201C - 2001 - Petroleum geology and resources of the Nepa-Botuoba High, Angara-Lena Terrace, and Cis-Patom Foredeep, southeastern Siberian Craton, Russia","interactions":[],"lastModifiedDate":"2024-10-11T10:55:52.037904","indexId":"b2201C","displayToPublicDate":"2001-11-01T00:00:00","publicationYear":"2001","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":"2201","chapter":"C","title":"Petroleum geology and resources of the Nepa-Botuoba High, Angara-Lena Terrace, and Cis-Patom Foredeep, southeastern Siberian Craton, Russia","docAbstract":"Three structural provinces of this report, the Nepa-Botuoba High, the Angara-Lena Terrace, and the Cis-Patom Foredeep, occupy the southeastern part of the Siberian craton northwest of the Baikal-Patom folded region (fig. 1). The provinces are similar in many aspects of their history of development, stratigraphic composition, and petroleum geology characteristics. The sedimentary\r\ncover of the provinces overlies the Archean?Lower Proterozoic\r\nbasement of the Siberian craton. Over most of the area of the provinces, the basement is covered by Vendian (uppermost Proterozoic, 650?570 Ma) clastic and carbonate rocks. Unlike the case in the more northwestern areas of the craton, older Riphean sedimentary rocks here are largely absent and they appear in the stratigraphic sequence only in parts of the Cis-Patom Foredeep province. Most of the overlying sedimentary section consists of Cambrian and Ordovician carbonate and clastic rocks, and it includes a thick Lower Cambrian salt-bearing formation. Younger rocks are thin and are present only in marginal areas.\r\n1\r\nA single total petroleum system (TPS) embraces all three provinces. The TPS is unique in two aspects: (1) its rich hydro-carbon reserves are derived from Precambrian source rocks and (2) preservation of oil and gas fields is extremely long owing to the presence of the Lower Cambrian undeformed salt seal. Discovered\r\nreserves of the TPS are about 2 billion barrels of oil and more than 30 trillion cubic feet of gas. The stratigraphic distribution\r\nof oil and gas reserves is narrow; all fields are in Vendian to lowermost Cambrian clastic and carbonate reservoirs that occur below Lower Cambrian salt. Both structural and stratigraphic traps are known. Source rocks are absent in the sedimentary cover of the provinces, with the possible exception of a narrow zone on the margin of the Cis-Patom Foredeep province. Source rocks are interpreted here to be Riphean and Vendian organic-rich shales of the Baikal-Patom folded region. These rocks presently\r\nare deformed and metamorphosed, but they generated oil and gas before the deformation occurred in Late Silurian and Devonian time. Generated hydrocarbons migrated updip onto the craton margin. The time of migration and formation of fields is constrained by the deposition of Lower Cambrian salt and by the Late Silurian or Devonian metamorphism of source rocks. This time frame indicates that the TPS is one of the oldest petroleum systems in the world.\r\nAll three provinces are exploration frontiers, and available geologic data are limited; therefore, only one assessment unit has been identified. The largest undiscovered hydrocarbon resources are expected to be in Vendian clastic reservoirs in both structural and stratigraphic traps of the Nepa-Botuoba High province. The petroleum potential of Vendian?lowermost Cambrian carbonate reservoirs is smaller. Nevertheless, these reservoirs may contain significant resources. Gas is expected to dominate over oil in the resource base.","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/b2201C","usgsCitation":"Ulmishek, G.F., 2001, Petroleum geology and resources of the Nepa-Botuoba High, Angara-Lena Terrace, and Cis-Patom Foredeep, southeastern Siberian Craton, Russia (Version 1.0): U.S. Geological Survey Bulletin 2201, 16 p., https://doi.org/10.3133/b2201C.","productDescription":"16 p.","costCenters":[],"links":[{"id":161250,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":462804,"rank":3,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/bul/2201/C/b2201-c.pdf","text":"Report","size":"3.65 MB","linkFileType":{"id":1,"text":"pdf"}},{"id":3237,"rank":2,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.usgs.gov/bul/2201/C/index.html","linkFileType":{"id":5,"text":"html"}}],"edition":"Version 1.0","contact":"<p><a href=\"https://pubs.usgs.gov/contact\" data-mce-href=\"../contact\">Contact Pubs Warehouse</a></p>","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4adce4b07f02db686345","contributors":{"authors":[{"text":"Ulmishek, Gregory F.","contributorId":48971,"corporation":false,"usgs":true,"family":"Ulmishek","given":"Gregory","email":"","middleInitial":"F.","affiliations":[],"preferred":false,"id":209807,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":33067,"text":"b2201F - 2001 - Petroleum geology and resources of the Baykit High province, East Siberia, Russia","interactions":[],"lastModifiedDate":"2024-10-11T10:56:22.299966","indexId":"b2201F","displayToPublicDate":"2001-11-01T00:00:00","publicationYear":"2001","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":"2201","chapter":"F","title":"Petroleum geology and resources of the Baykit High province, East Siberia, Russia","docAbstract":"The Baykit High province consists of two principal structural\r\nunits?the Baykit regional high in the west, which occupies most of the province, and the Katanga structural saddle in the east. The province is on the western margin of the Siberian craton east of theYenisey Ridge foldbelt. The province is an exploration frontier\r\nand only a few prospects have been drilled. The oldest sedimentary\r\nrocks of the province, Riphean carbonate and clastic strata of Late Proterozoic age (1,650?650 million years old) that were deposited on the passive margin, cover the Archean?Lower Proterozoic basement. Basal Vendian (uppermost Proterozoic, 650?570 million years old) clastic rocks unconformably overlie various units of the Riphean and locally lie directly on the basement.\r\nYounger Vendian and lowermost Cambrian rocks are primarily dolomites. The Vendian/Cambrian boundary is con-formable, and its exact stratigraphic position has not been identified\r\nwith certainty. The Lower Cambrian section is thick, and it consists of alternating beds of dolomite and evaporites (mostly salt). Middle and Upper Cambrian strata are composed of shale and dolomite. Ordovician-Silurian and upper Paleozoic rocks are thin, and they are present only in the northern areas of the province.\r\nStructural pattern of Riphean rocks differs substantially from that of Vendian-Cambrian rocks.\r\nA single total petroleum system (TPS) was identified in the Baykit High province. Discovered oil of the system is chiefly concentrated in Riphean carbonate reservoirs of the Yurubchen-Tokhom zone that is currently being explored and that has the\r\nAbstract 1\r\npotential to become a giant field (or group of fields). The TPS also contains about 5 trillion cubic feet of discovered recover-able gas in clastic reservoir rocks at the base of the Vendian section.\r\nPetroleum source rocks are absent in the stratigraphic succession over most of the TPS area. Riphean organic-rich shales and carbonates that crop out in the Yenisey Ridge foldbelt west of the Baykit high are probable source rocks. Their areal distribution extends from the foldbelt into the foredeep along the province?s western margin. Potential source rocks also are present in platform depressions in eastern areas of the province. Hydrocarbon generation and migration west of the province started as early as Riphean time, before the beginning of the deformation in the Yenisey Ridge foldbelt that occurred about 820?850 million years ago. However, the presently known oil and gas accumulations were formed after deposition of the Lower Cambrian salt seal.\r\nAvailable data allow identification of only one assessment unit, and it covers the entire TPS area. Undiscovered oil and gas resources are moderate, primarily due to the poor quality of reservoir\r\nrocks. However, the reserve growth in the Yurubchen-Tokhom zone may be large and may exceed the volume of undiscovered\r\nresources in the rest of the province. Most oil and gas resourcesareexpectedtobeinstructuralandstratigraphictrapsin Riphean carbonate reservoirs. Vendian clastic reservoirs are probably\r\ngas-prone.","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/b2201F","usgsCitation":"Ulmishek, G.F., 2001, Petroleum geology and resources of the Baykit High province, East Siberia, Russia (Version 1.0): U.S. Geological Survey Bulletin 2201, 18 p., https://doi.org/10.3133/b2201F.","productDescription":"18 p.","costCenters":[],"links":[{"id":161314,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":3240,"rank":2,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.usgs.gov/bul/2201/F/index.html","linkFileType":{"id":5,"text":"html"}},{"id":462806,"rank":3,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/bul/2201/F/b2201-f.pdf","text":"Report","size":"5.05 MB","linkFileType":{"id":1,"text":"pdf"}}],"edition":"Version 1.0","contact":"<p><a href=\"https://pubs.usgs.gov/contact\" data-mce-href=\"../contact\">Contact Pubs Warehouse</a></p>","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ae0e4b07f02db687ea3","contributors":{"authors":[{"text":"Ulmishek, Gregory F.","contributorId":48971,"corporation":false,"usgs":true,"family":"Ulmishek","given":"Gregory","email":"","middleInitial":"F.","affiliations":[],"preferred":false,"id":209810,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":61485,"text":"mf2370 - 2001 - Interpretive geologic cross sections for the Death Valley regional flow system and surrounding areas, Nevada and California","interactions":[],"lastModifiedDate":"2018-02-21T17:45:47","indexId":"mf2370","displayToPublicDate":"2001-11-01T00:00:00","publicationYear":"2001","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":"2370","title":"Interpretive geologic cross sections for the Death Valley regional flow system and surrounding areas, Nevada and California","docAbstract":"This report presents a network of 28 geologic cross sections that portray subsurface geologic relations within the Death Valley regional ground-water system, a ground-water basin that encompasses a 3? x 3? area (approximately 70,000 km2) in southern Nevada and eastern California. The cross sections transect that part of the southern Great Basin that includes Death Valley, the Nevada Test Site, and the potential high-level nuclear waste underground repository at Yucca Mountain. The specific geometric relationships portrayed on the cross sections are discussed in the context of four general sub-regions that have stratigraphic similarities and general consistency of structural style: (1) the Nevada Test Site vicinity; (2) the Spring Mountains, Pahrump Valley and Amargosa Desert region; (3) the Death Valley region; and (4) the area east of the Nevada Test Site. \r\nThe subsurface geologic interpretations portrayed on the cross sections are based on an integration of existing geologic maps, measured stratigraphic sections, published cross sections, well data, and geophysical data and interpretations. The estimated top of pre-Cenozoic rocks in the cross sections is based on inversion of gravity data, but the deeper parts of the sections are based on geologic conceptual models and are more speculative. \r\nThe region transected by the cross sections includes part of the southern Basin and Range Province, the northwest-trending Walker Lane belt, the Death Valley region, and the northern Mojave Desert. The region is structurally complex, where a locally thick Tertiary volcanic and sedimentary section unconformably overlies previously deformed Proterozoic through Paleozoic rocks. All of these rocks have been deformed by complex Neogene ex-tensional normal and strike-slip faults. These cross sections form a three-dimensional network that portrays the interpreted stratigraphic and structural relations in the region; the sections form part of the geologic framework that will be incorporated in a complex numerical model of ground-water flow in the Death Valley region.","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/mf2370","usgsCitation":"Sweetkind, D.S., Dickerson, R., Blakely, R., and Denning, P., 2001, Interpretive geologic cross sections for the Death Valley regional flow system and surrounding areas, Nevada and California: U.S. Geological Survey Miscellaneous Field Studies Map 2370, Three sheets: Sheet 1, 60 by 36 inches; sheet 2, 84 by 36 inches; sheet 3, 71 by 36 inches (all in color).  Sheet 1, scale 1:750,000 and 1:1,500,000; sheet 2 and 3, scale 1:100,000 and 1:250,000 and 1:1,500,000; Accompanied by 35 p. text., https://doi.org/10.3133/mf2370.","productDescription":"Three sheets: Sheet 1, 60 by 36 inches; sheet 2, 84 by 36 inches; sheet 3, 71 by 36 inches (all in color).  Sheet 1, scale 1:750,000 and 1:1,500,000; sheet 2 and 3, scale 1:100,000 and 1:250,000 and 1:1,500,000; Accompanied by 35 p. text.","costCenters":[],"links":[{"id":186978,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":110217,"rank":700,"type":{"id":15,"text":"Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_44623.htm","linkFileType":{"id":5,"text":"html"},"description":"44623"},{"id":6050,"rank":100,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.usgs.gov/mf/2001/mf-2370/","linkFileType":{"id":5,"text":"html"}}],"scale":"0","country":"United States","state":"California, Nevada","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -118,35 ], [ -118,38 ], [ -115,38 ], [ -115,35 ], [ -118,35 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e48b2e4b07f02db530ce7","contributors":{"authors":[{"text":"Sweetkind, D. S.","contributorId":61507,"corporation":false,"usgs":true,"family":"Sweetkind","given":"D.","email":"","middleInitial":"S.","affiliations":[],"preferred":false,"id":265789,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Dickerson, R. P.","contributorId":23968,"corporation":false,"usgs":true,"family":"Dickerson","given":"R. P.","affiliations":[],"preferred":false,"id":265787,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Blakely, R.J. 0000-0003-1701-5236","orcid":"https://orcid.org/0000-0003-1701-5236","contributorId":70755,"corporation":false,"usgs":true,"family":"Blakely","given":"R.J.","affiliations":[],"preferred":false,"id":265790,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Denning, Paul pdenning@usgs.gov","contributorId":168842,"corporation":false,"usgs":true,"family":"Denning","given":"Paul","email":"pdenning@usgs.gov","affiliations":[{"id":171,"text":"Central Mineral and Environmental Resources Science Center","active":true,"usgs":true}],"preferred":true,"id":265788,"contributorType":{"id":1,"text":"Authors"},"rank":4}]}}
,{"id":23674,"text":"ofr94260C - 2001 - Duration of sedimentation of the Creede Formation","interactions":[{"subject":{"id":23674,"text":"ofr94260C - 2001 - Duration of sedimentation of the Creede Formation","indexId":"ofr94260C","publicationYear":"2001","noYear":false,"chapter":"C","title":"Duration of sedimentation of the Creede Formation"},"predicate":"IS_PART_OF","object":{"id":70226622,"text":"ofr94260AP - 2001 - Preliminary scientific results of the Creede Caldera Continental Scientific Drilling Program, Chapters A-P","indexId":"ofr94260AP","publicationYear":"2001","noYear":false,"chapter":"A-P","title":"Preliminary scientific results of the Creede Caldera Continental Scientific Drilling Program, Chapters A-P"},"id":1}],"isPartOf":{"id":70226622,"text":"ofr94260AP - 2001 - Preliminary scientific results of the Creede Caldera Continental Scientific Drilling Program, Chapters A-P","indexId":"ofr94260AP","publicationYear":"2001","noYear":false,"title":"Preliminary scientific results of the Creede Caldera Continental Scientific Drilling Program, Chapters A-P"},"lastModifiedDate":"2021-11-30T17:51:05.24239","indexId":"ofr94260C","displayToPublicDate":"2001-11-01T00:00:00","publicationYear":"2001","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":"94-260","chapter":"C","title":"Duration of sedimentation of the Creede Formation","docAbstract":"<p>No abstract available.</p>","largerWorkType":{"id":18,"text":"Report"},"largerWorkTitle":"Preliminary scientific results of the Creede Caldera Continental Scientific Drilling Program, Chapters A-P","largerWorkSubtype":{"id":5,"text":"USGS Numbered Series"},"language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr94260C","issn":"0094-9140","usgsCitation":"Lanphere, M.A., 2001, Duration of sedimentation of the Creede Formation: U.S. Geological Survey Open-File Report 94-260, 4 p., https://doi.org/10.3133/ofr94260C.","productDescription":"4 p.","costCenters":[],"links":[{"id":52931,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1994/0260c/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":157471,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1994/0260c/report-thumb.jpg"}],"country":"United States","state":"Colorado","city":"Creede","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -106.97319030761719,\n              37.791337175930686\n            ],\n            [\n              -106.66351318359375,\n              37.791337175930686\n            ],\n            [\n              -106.66351318359375,\n              37.99183365313853\n            ],\n            [\n              -106.97319030761719,\n              37.99183365313853\n            ],\n            [\n              -106.97319030761719,\n              37.791337175930686\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a59e4b07f02db62fd46","contributors":{"authors":[{"text":"Lanphere, Marvin A. alder@usgs.gov","contributorId":2696,"corporation":false,"usgs":true,"family":"Lanphere","given":"Marvin","email":"alder@usgs.gov","middleInitial":"A.","affiliations":[],"preferred":true,"id":190525,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":23327,"text":"ofr94260D - 2001 - Structural resurgence and intracaldera volcanism - Creede Caldera, Colorado","interactions":[{"subject":{"id":23327,"text":"ofr94260D - 2001 - Structural resurgence and intracaldera volcanism - Creede Caldera, Colorado","indexId":"ofr94260D","publicationYear":"2001","noYear":false,"chapter":"D","title":"Structural resurgence and intracaldera volcanism - Creede Caldera, Colorado"},"predicate":"IS_PART_OF","object":{"id":70226622,"text":"ofr94260AP - 2001 - Preliminary scientific results of the Creede Caldera Continental Scientific Drilling Program, Chapters A-P","indexId":"ofr94260AP","publicationYear":"2001","noYear":false,"chapter":"A-P","title":"Preliminary scientific results of the Creede Caldera Continental Scientific Drilling Program, Chapters A-P"},"id":1}],"isPartOf":{"id":70226622,"text":"ofr94260AP - 2001 - Preliminary scientific results of the Creede Caldera Continental Scientific Drilling Program, Chapters A-P","indexId":"ofr94260AP","publicationYear":"2001","noYear":false,"title":"Preliminary scientific results of the Creede Caldera Continental Scientific Drilling Program, Chapters A-P"},"lastModifiedDate":"2021-11-30T17:52:40.807726","indexId":"ofr94260D","displayToPublicDate":"2001-11-01T00:00:00","publicationYear":"2001","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":"94-260","chapter":"D","title":"Structural resurgence and intracaldera volcanism - Creede Caldera, Colorado","docAbstract":"<p>No abstract available.</p>","largerWorkType":{"id":18,"text":"Report"},"largerWorkTitle":"Preliminary scientific results of the Creede Caldera Continental Scientific Drilling Program, Chapters A-P","largerWorkSubtype":{"id":5,"text":"USGS Numbered Series"},"language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr94260D","issn":"0094-9140","usgsCitation":"Heiken, G., Krier, D.J., and McCormick, T., 2001, Structural resurgence and intracaldera volcanism - Creede Caldera, Colorado: U.S. Geological Survey Open-File Report 94-260, 8 p., https://doi.org/10.3133/ofr94260D.","productDescription":"8 p.","costCenters":[],"links":[{"id":156199,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1994/0260d/report-thumb.jpg"},{"id":52629,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1994/0260d/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"country":"United States","state":"Colorado","city":"Creede","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -106.97319030761719,\n              37.791337175930686\n            ],\n            [\n              -106.66351318359375,\n              37.791337175930686\n            ],\n            [\n              -106.66351318359375,\n              37.99183365313853\n            ],\n            [\n              -106.97319030761719,\n              37.99183365313853\n            ],\n            [\n              -106.97319030761719,\n              37.791337175930686\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b15e4b07f02db6a49bd","contributors":{"authors":[{"text":"Heiken, Grant","contributorId":88773,"corporation":false,"usgs":true,"family":"Heiken","given":"Grant","email":"","affiliations":[],"preferred":false,"id":189910,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Krier, Donathon J.","contributorId":98353,"corporation":false,"usgs":true,"family":"Krier","given":"Donathon","email":"","middleInitial":"J.","affiliations":[],"preferred":false,"id":189912,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"McCormick, Tamsin","contributorId":91141,"corporation":false,"usgs":true,"family":"McCormick","given":"Tamsin","email":"","affiliations":[],"preferred":false,"id":189911,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":23676,"text":"ofr94260E - 2001 - Depositional environments and authigenic mineral distributions in the Oligocene Creede Formation, Colorado, USA","interactions":[{"subject":{"id":23676,"text":"ofr94260E - 2001 - Depositional environments and authigenic mineral distributions in the Oligocene Creede Formation, Colorado, USA","indexId":"ofr94260E","publicationYear":"2001","noYear":false,"chapter":"E","title":"Depositional environments and authigenic mineral distributions in the Oligocene Creede Formation, Colorado, USA"},"predicate":"IS_PART_OF","object":{"id":70226622,"text":"ofr94260AP - 2001 - Preliminary scientific results of the Creede Caldera Continental Scientific Drilling Program, Chapters A-P","indexId":"ofr94260AP","publicationYear":"2001","noYear":false,"chapter":"A-P","title":"Preliminary scientific results of the Creede Caldera Continental Scientific Drilling Program, Chapters A-P"},"id":1}],"isPartOf":{"id":70226622,"text":"ofr94260AP - 2001 - Preliminary scientific results of the Creede Caldera Continental Scientific Drilling Program, Chapters A-P","indexId":"ofr94260AP","publicationYear":"2001","noYear":false,"title":"Preliminary scientific results of the Creede Caldera Continental Scientific Drilling Program, Chapters A-P"},"lastModifiedDate":"2022-09-06T20:12:56.587156","indexId":"ofr94260E","displayToPublicDate":"2001-11-01T00:00:00","publicationYear":"2001","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":"94-260","chapter":"E","title":"Depositional environments and authigenic mineral distributions in the Oligocene Creede Formation, Colorado, USA","docAbstract":"<p>No abstract available.</p>","largerWorkType":{"id":18,"text":"Report"},"largerWorkTitle":"Preliminary scientific results of the Creede caldera Continental Scientific Drilling Program, Chapters A-P (Open-File Report 94-260)","largerWorkSubtype":{"id":5,"text":"USGS Numbered Series"},"language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr94260E","usgsCitation":"Larsen, D., and Crossey, L.J., 2001, Depositional environments and authigenic mineral distributions in the Oligocene Creede Formation, Colorado, USA: U.S. Geological Survey Open-File Report 94-260, 76 p., https://doi.org/10.3133/ofr94260E.","productDescription":"76 p.","costCenters":[],"links":[{"id":406265,"rank":3,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_36780.htm","linkFileType":{"id":5,"text":"html"}},{"id":52932,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1994/0260e/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":157473,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1994/0260e/report-thumb.jpg"}],"country":"United States","state":"Colorado","city":"Creede","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -107.067,\n              37.679\n            ],\n            [\n              -106.638,\n              37.679\n            ],\n            [\n              -106.638,\n              37.862\n            ],\n            [\n              -107.067,\n              37.862\n            ],\n            [\n              -107.067,\n              37.679\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ab1e4b07f02db66e95f","contributors":{"authors":[{"text":"Larsen, Daniel","contributorId":27495,"corporation":false,"usgs":true,"family":"Larsen","given":"Daniel","affiliations":[],"preferred":false,"id":190529,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Crossey, Laura J.","contributorId":56265,"corporation":false,"usgs":true,"family":"Crossey","given":"Laura","email":"","middleInitial":"J.","affiliations":[],"preferred":false,"id":190530,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":38265,"text":"pp1416F - 2001 - Ground-water flow in the Gulf Coast aquifer systems, south-central United States","interactions":[],"lastModifiedDate":"2017-01-06T12:09:33","indexId":"pp1416F","displayToPublicDate":"2001-11-01T00:00:00","publicationYear":"2001","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":"1416","chapter":"F","title":"Ground-water flow in the Gulf Coast aquifer systems, south-central United States","docAbstract":"The Gulf Coast regional aquifer systems constitute one of the largest, most complicated, and most interdependent aquifer systems in the United States. Ground-water flow in a 230,000-square-mile area of the south-central United States was modeled for the effect of withdrawing freshwater at the rate of nearly 10 billion gallons per day in 1985 from regional aquifers in the Mississippi Embayment, the Texas coastal uplands, and the coastal lowlands aquifer systems. The 1985 rate of pumping was three times the average rate of recharge to the aquifers before development. The report also estimates the effects of even greater withdrawal rates in the aquifer systems. About two-thirds of the water in the aquifers is saline to brine, which complicates the modeling. Land subsidence due to water withdrawal also was modeled.","largerWorkType":{"id":18,"text":"Report"},"largerWorkTitle":"Regional aquifer-system analysis--Gulf Coastal Plain","largerWorkSubtype":{"id":5,"text":"USGS Numbered Series"},"language":"ENGLISH","doi":"10.3133/pp1416F","usgsCitation":"Williamson, A.K., and Grubb, H.F., 2001, Ground-water flow in the Gulf Coast aquifer systems, south-central United States: U.S. Geological Survey Professional Paper 1416, p. F1-F173, https://doi.org/10.3133/pp1416F.","productDescription":"p. F1-F173","costCenters":[],"links":[{"id":122515,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/pp/1416f/report-thumb.jpg"},{"id":64642,"rank":401,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/pp/1416f/plate-01.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":110221,"rank":700,"type":{"id":15,"text":"Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_44679.htm","linkFileType":{"id":5,"text":"html"},"description":"44679"},{"id":64643,"rank":402,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/pp/1416f/plate-02.pdf","text":"Plate 7A","linkFileType":{"id":1,"text":"pdf"}},{"id":64644,"rank":5,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/pp/1416f/plate-03.pdf","text":"Plate 7B","linkFileType":{"id":1,"text":"pdf"}},{"id":64645,"rank":403,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/pp/1416f/plate-04.pdf","text":"Plate 7C","linkFileType":{"id":1,"text":"pdf"}},{"id":64646,"rank":404,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/pp/1416f/plate-05.pdf","text":"Plate 7D","linkFileType":{"id":1,"text":"pdf"}},{"id":64647,"rank":405,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/pp/1416f/plate-06.pdf","text":"Plate 7E","linkFileType":{"id":1,"text":"pdf"}},{"id":64648,"rank":406,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/pp/1416f/plate-07.pdf","text":"Plate 7F","linkFileType":{"id":1,"text":"pdf"}},{"id":64649,"rank":407,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/pp/1416f/plate-08.pdf","text":"Plate 7G","linkFileType":{"id":1,"text":"pdf"}},{"id":64650,"rank":408,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/pp/1416f/plate-09.pdf","text":"Plate 7H","linkFileType":{"id":1,"text":"pdf"}},{"id":64651,"rank":409,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/pp/1416f/plate-10.pdf","text":"Plate 7I","linkFileType":{"id":1,"text":"pdf"}},{"id":64652,"rank":410,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/pp/1416f/plate-11.pdf","text":"Plate 7J","linkFileType":{"id":1,"text":"pdf"}},{"id":64653,"rank":301,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/pp/1416f/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4aade4b07f02db66b8db","contributors":{"authors":[{"text":"Williamson, A. K.","contributorId":57872,"corporation":false,"usgs":true,"family":"Williamson","given":"A.","email":"","middleInitial":"K.","affiliations":[],"preferred":false,"id":219454,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Grubb, H. F.","contributorId":16863,"corporation":false,"usgs":true,"family":"Grubb","given":"H.","email":"","middleInitial":"F.","affiliations":[],"preferred":false,"id":219453,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":52899,"text":"ofr01312 - 2001 - The containment of Soviet underground nuclear explosions","interactions":[],"lastModifiedDate":"2012-02-02T00:11:40","indexId":"ofr01312","displayToPublicDate":"2001-11-01T00:00:00","publicationYear":"2001","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":"2001-312","title":"The containment of Soviet underground nuclear explosions","language":"ENGLISH","doi":"10.3133/ofr01312","usgsCitation":"Adushkin, V.V., and Leith, W., 2001, The containment of Soviet underground nuclear explosions: U.S. Geological Survey Open-File Report 2001-312, 52 p., https://doi.org/10.3133/ofr01312.","productDescription":"52 p.","costCenters":[],"links":[{"id":4963,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://geology.er.usgs.gov/eespteam/pdf/USGSOFR01312.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":177056,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/2001/0312/report-thumb.jpg"},{"id":87039,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/2001/0312/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4aaae4b07f02db6689db","contributors":{"authors":[{"text":"Adushkin, Vitaly V.","contributorId":41512,"corporation":false,"usgs":true,"family":"Adushkin","given":"Vitaly","email":"","middleInitial":"V.","affiliations":[],"preferred":false,"id":246174,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Leith, William","contributorId":81502,"corporation":false,"usgs":true,"family":"Leith","given":"William","affiliations":[],"preferred":false,"id":246175,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":38263,"text":"pp729G - 2001 - The Quaternary and Pliocene Yellowstone Plateau volcanic field of Wyoming, Idaho, and Montana","interactions":[],"lastModifiedDate":"2025-04-16T19:22:11.609","indexId":"pp729G","displayToPublicDate":"2001-11-01T00:00:00","publicationYear":"2001","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":"729","chapter":"G","title":"The Quaternary and Pliocene Yellowstone Plateau volcanic field of Wyoming, Idaho, and Montana","docAbstract":"This region of Yellowstone National Park has been the active focus of one of the Earth's largest magmatic systems for more than 2 million years. The resulting volcanism has been characterized by the eruption of voluminous rhyolites and subordinate basalts but virtually no lavas of intermediate composition. The magmatic system at depth remains active and drives the massive hydrothermal circulation for which the park is widely known. Studies of the volcanic field using geologic mapping and petrology have defined three major cycles of rhyolitic volcanism, each climaxed by the eruption of a rhyolitic ash-flow sheet having a volume of hundreds of thousands of cubic kilometers. The field also has been analyzed in terms of its magmatic and tectonic evolution, including its regional relation to the Snake River plain and to basin-range tectonic extension.","largerWorkType":{"id":18,"text":"Report"},"largerWorkTitle":"Geology of Yellowstone National Park","largerWorkSubtype":{"id":5,"text":"USGS Numbered Series"},"language":"ENGLISH","doi":"10.3133/pp729G","usgsCitation":"Christiansen, R.L., 2001, The Quaternary and Pliocene Yellowstone Plateau volcanic field of Wyoming, Idaho, and Montana: U.S. Geological Survey Professional Paper 729, Report: 145 p.; 3 Plates: 50.90 x 41.80 inches or smaller, https://doi.org/10.3133/pp729G.","productDescription":"Report: 145 p.; 3 Plates: 50.90 x 41.80 inches or smaller","costCenters":[{"id":673,"text":"Western Volcano Hazards Program","active":false,"usgs":true}],"links":[{"id":484648,"rank":3,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_42941.htm","linkFileType":{"id":5,"text":"html"}},{"id":9262,"rank":2,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.usgs.gov/pp/pp729g/","linkFileType":{"id":5,"text":"html"}},{"id":123819,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/pp_729_g.jpg"}],"country":"United States","state":"Idaho, Montana, Wyoming","otherGeospatial":"Yellowstone Plateau volcanic field","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"coordinates\": [\n          [\n            [\n              -111.2483,\n              45.1075\n            ],\n            [\n              -111.2483,\n              44\n            ],\n            [\n              -109.6875,\n              44\n            ],\n            [\n              -109.6875,\n              45.1075\n            ],\n            [\n              -111.2483,\n              45.1075\n            ]\n          ]\n        ],\n        \"type\": \"Polygon\"\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ac7e4b07f02db67ad39","contributors":{"authors":[{"text":"Christiansen, Robert L. 0000-0002-8017-3918 rchris@usgs.gov","orcid":"https://orcid.org/0000-0002-8017-3918","contributorId":4412,"corporation":false,"usgs":true,"family":"Christiansen","given":"Robert","email":"rchris@usgs.gov","middleInitial":"L.","affiliations":[{"id":617,"text":"Volcano Science Center","active":true,"usgs":true}],"preferred":true,"id":219451,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":38275,"text":"pp1648 - 2001 - Geochemical landscapes of the conterminous United States — New map presentations for 22 elements","interactions":[],"lastModifiedDate":"2022-01-19T19:34:28.676161","indexId":"pp1648","displayToPublicDate":"2001-11-01T00:00:00","publicationYear":"2001","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":"1648","title":"Geochemical landscapes of the conterminous United States — New map presentations for 22 elements","docAbstract":"Geochemical maps of the conterminous United States have been prepared for seven major elements (Al, Ca, Fe, K, Mg, Na, and Ti) and 15 trace elements (As, Ba, Cr, Cu, Hg, Li, Mn, Ni, Pb, Se, Sr, V, Y, Zn, and Zr). The maps are based on an ultra low-density geochemical survey consisting of 1,323 samples of soils and other surficial materials collected from approximately 1960-1975. The data were published by Boerngen and Shacklette (1981) and black-and-white point-symbol geochemical maps were published by Shacklette and Boerngen (1984). 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]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b23e4b07f02db6ae243","contributors":{"authors":[{"text":"Gustavsson, N.","contributorId":100439,"corporation":false,"usgs":true,"family":"Gustavsson","given":"N.","email":"","affiliations":[],"preferred":false,"id":219488,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Bolviken, B.","contributorId":102120,"corporation":false,"usgs":true,"family":"Bolviken","given":"B.","email":"","affiliations":[],"preferred":false,"id":219489,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"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":219486,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Severson, R. C.","contributorId":46498,"corporation":false,"usgs":true,"family":"Severson","given":"R.","email":"","middleInitial":"C.","affiliations":[],"preferred":false,"id":219487,"contributorType":{"id":1,"text":"Authors"},"rank":4}]}}
,{"id":33077,"text":"b2172C - 2001 - Probabilistic method for estimating future growth of oil and gas reserves","interactions":[],"lastModifiedDate":"2012-02-02T00:09:16","indexId":"b2172C","displayToPublicDate":"2001-11-01T00:00:00","publicationYear":"2001","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":"2172","chapter":"C","title":"Probabilistic method for estimating future growth of oil and gas reserves","language":"ENGLISH","doi":"10.3133/b2172C","usgsCitation":"Crovelli, R.A., and Schmoker, J.W., 2001, Probabilistic method for estimating future growth of oil and gas reserves (Version 1.0): U.S. Geological Survey Bulletin 2172, 12 p., https://doi.org/10.3133/b2172C.","productDescription":"12 p.","costCenters":[],"links":[{"id":164280,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":3280,"rank":100,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.usgs.gov/bul/b2172-c/","linkFileType":{"id":5,"text":"html"}}],"edition":"Version 1.0","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ae4e4b07f02db689f8e","contributors":{"authors":[{"text":"Crovelli, Robert A.","contributorId":92242,"corporation":false,"usgs":true,"family":"Crovelli","given":"Robert","email":"","middleInitial":"A.","affiliations":[],"preferred":false,"id":209839,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Schmoker, James W.","contributorId":52171,"corporation":false,"usgs":true,"family":"Schmoker","given":"James","email":"","middleInitial":"W.","affiliations":[],"preferred":false,"id":209838,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":31319,"text":"ofr01272 - 2001 - GIS Surface effects archive of underground nuclear detonations conducted at Yucca Flat and Pahute Mesa, Nevada Test Site, Nevada","interactions":[],"lastModifiedDate":"2012-02-02T00:09:00","indexId":"ofr01272","displayToPublicDate":"2001-11-01T00:00:00","publicationYear":"2001","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":"2001-272","title":"GIS Surface effects archive of underground nuclear detonations conducted at Yucca Flat and Pahute Mesa, Nevada Test Site, Nevada","language":"ENGLISH","doi":"10.3133/ofr01272","usgsCitation":"Grasso, D.N., 2001, GIS Surface effects archive of underground nuclear detonations conducted at Yucca Flat and Pahute Mesa, Nevada Test Site, Nevada (Version 1.0): U.S. Geological Survey Open-File Report 2001-272, map + pamphlet (34 p.), https://doi.org/10.3133/ofr01272.","productDescription":"map + pamphlet (34 p.)","costCenters":[],"links":[{"id":159862,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":2963,"rank":100,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.usgs.gov/of/2001/ofr-01-0272/","linkFileType":{"id":5,"text":"html"}}],"edition":"Version 1.0","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b28e4b07f02db6b1689","contributors":{"authors":[{"text":"Grasso, Dennis N.","contributorId":39402,"corporation":false,"usgs":true,"family":"Grasso","given":"Dennis","email":"","middleInitial":"N.","affiliations":[],"preferred":false,"id":205691,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":30944,"text":"wri014202 - 2001 - Evaluation of ground-water/surface-water relations, Chapman Creek,West-Central Ohio, by means of multiple methods","interactions":[],"lastModifiedDate":"2019-05-21T15:18:09","indexId":"wri014202","displayToPublicDate":"2001-11-01T00:00:00","publicationYear":"2001","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":"2001–4202","displayTitle":"Evaluation of Ground-Water/Surface-Water Relations, Chapman Creek,West-Central Ohio, by Means of Multiple Methods","title":"Evaluation of ground-water/surface-water relations, Chapman Creek,West-Central Ohio, by means of multiple methods","docAbstract":"<p>Chapman Creek, a tributary to the Mad River, passes within about 500 feet of a landfill near Tremont City, in Clark County, west-central Ohio. In autumn 2000, the ground-water/surface-water relation was investigated by use of piezometers, seepage meters, temperature monitors, and a gain-loss study. Four piezometers were installed in the streambed along about a 1-mile reach, inclusive of the landfill. Four seepage-meter tests were done at locations near two of the piezometers. Four temperature-monitoring stations were established along a reach of about 700 feet near the landfill. A fifth temperature station was located near a piezometer about 3,000 feet downstream from the landfill. A streamflow gain-loss study was done over a 3-mile reach that included the reaches studied with the other methods. The data from the piezometers, seepage meters, and temperature monitors indicated an apparent change from losing to gaining and back again several times over fairly short distances. The gain-loss data indicated that the creek was consistently a gaining stream over the 3-mile reach. Investigation of streambed conditions and local geology revealed that the streambed consists of sand and gravel overlying a finegrained till layer. The stream water readily moves in and out of the coarse streambed such that the piezometers, seepage meters, and temperature monitors measured the local flow in the streambed; therefore, these data did not reflect the true relation between the creek and ground water. On the other hand, the gain-loss study, less affected by the movement of water in the streambed, showed that Chapman Creek probably is a gaining stream throughout the 3-mile reach.</p>","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Reston, VA","doi":"10.3133/wri014202","collaboration":"Prepared in cooperation with the U.S. Environmental Protection Agency","usgsCitation":"Dumouchelle, D.H., 2001, Evaluation of ground-water/surface-water relations, Chapman Creek,West-Central Ohio, by means of multiple methods: U.S. Geological Survey Water-Resources Investigations Report 2001–4202, iv, 13 p., https://doi.org/10.3133/wri014202.","productDescription":"iv, 13 p.","numberOfPages":"20","onlineOnly":"Y","additionalOnlineFiles":"N","costCenters":[{"id":513,"text":"Ohio Water Science 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 \"}}]}","contact":"<p><a href=\"https://www.usgs.gov/centers/oki-water/\" data-mce-href=\"https://www.usgs.gov/centers/oki-water/\">Director, Ohio Water Science Center</a><br>U.S. Geological Survey<br>6460 Busch Blvd.<br>Columbus, OH 43229-1737</p>","tableOfContents":"<ul><li>Abstract</li><li>Introduction</li><li>Methods</li><li>Ground-water/surface-water relations</li><li>Summary and conclusions</li><li>References cited</li></ul>","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e49e4e4b07f02db5e64b8","contributors":{"authors":[{"text":"Dumouchelle, Denise H. ddumouch@usgs.gov","contributorId":1847,"corporation":false,"usgs":true,"family":"Dumouchelle","given":"Denise","email":"ddumouch@usgs.gov","middleInitial":"H.","affiliations":[{"id":513,"text":"Ohio Water Science Center","active":true,"usgs":true}],"preferred":true,"id":204412,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":31245,"text":"ofr0194 - 2001 - Water-level altitudes 2001, water-level changes 1977-2001 and 2000-2001, and compaction 1973-2000 in the Chicot and Evangeline aquifers, Houston-Galveston region, Texas","interactions":[],"lastModifiedDate":"2017-01-12T15:07:56","indexId":"ofr0194","displayToPublicDate":"2001-11-01T00:00:00","publicationYear":"2001","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":"2001-94","title":"Water-level altitudes 2001, water-level changes 1977-2001 and 2000-2001, and compaction 1973-2000 in the Chicot and Evangeline aquifers, Houston-Galveston region, Texas","docAbstract":"<p><span>This report is one in an annual series of reports that depicts water-level altitudes and water-level changes since 1977 and compaction since 1973 in the Chicot and Evangeline aquifers in the Houston-Galveston region, Texas. The report, prepared in cooperation with the City of Houston and the Harris-Galveston Coastal Subsidence District, presents maps for the Chicot and Evangeline aquifers showing the approximate water-level altitudes in wells in 2001 (figs 1,4) and approximate water-level changes in wells from 1977 to 2001 and from 2000 to 2001 (figs 2,3,5,6), a map showing extensometer site locations (fig. 7), and graphs showing measured compaction of subserface material at selected sites from 1973 to 2000 (fig. 8). The most recent previously published water-level-altitude maps and water-level-change maps for the two aquifers in the region are by Coplin and Santos.&nbsp;(2000). The&nbsp;Houston-Galveston region comprises Harris and Galveston Counties and adjacent parts of Brazoria, Fort Bend, Waller, Montgomery, Liberty, and Chambers Counties.</span></p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr0194","collaboration":"In cooperation with the City of Houston and the Harris-Galveston Coastal Subsidence District","usgsCitation":"Coplin, L., Houston, N.A., and Brown, D.W., 2001, Water-level altitudes 2001, water-level changes 1977-2001 and 2000-2001, and compaction 1973-2000 in the Chicot and Evangeline aquifers, Houston-Galveston region, Texas: U.S. Geological Survey Open-File Report 2001-94, 7 Sheets: 17 x 22 inches, https://doi.org/10.3133/ofr0194.","productDescription":"7 Sheets: 17 x 22 inches","costCenters":[{"id":583,"text":"Texas Water Science Center","active":true,"usgs":true}],"links":[{"id":160882,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/ofr0194.JPG"},{"id":19302,"rank":400,"type":{"id":26,"text":"Sheet"},"url":"https://pubs.usgs.gov/of/2001/0094/plate-1.pdf","text":"Sheet 1","size":"1.68 MB","linkFileType":{"id":1,"text":"pdf"},"description":"Sheet 1"},{"id":19303,"rank":400,"type":{"id":26,"text":"Sheet"},"url":"https://pubs.usgs.gov/of/2001/0094/plate-2.pdf","text":"Sheet 2","size":"1.33 MB","linkFileType":{"id":1,"text":"pdf"},"description":"Sheet 2"},{"id":19304,"rank":402,"type":{"id":26,"text":"Sheet"},"url":"https://pubs.usgs.gov/of/2001/0094/plate-3.pdf","text":"Sheet 3","size":"1.29 MB","linkFileType":{"id":1,"text":"pdf"},"description":"Sheet 3"},{"id":19305,"rank":403,"type":{"id":26,"text":"Sheet"},"url":"https://pubs.usgs.gov/of/2001/0094/plate-4.pdf","text":"Sheet 4","size":"1.34 MB","linkFileType":{"id":1,"text":"pdf"},"description":"Sheet 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County, Waller County","city":"Houston","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -95.23773193359375,\n              28.98171470422955\n            ],\n            [\n              -95.59478759765624,\n              29\n            ],\n            [\n              -95.8721923828125,\n              29.305561325527698\n            ],\n            [\n              -96.05621337890625,\n              29.604506272365295\n            ],\n            [\n              -96.21551513671875,\n              30.171250084367482\n            ],\n            [\n              -96.009521484375,\n              30.55043513509528\n            ],\n            [\n              -95.3778076171875,\n              30.5\n            ],\n            [\n              -94.82299804687499,\n        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Center","active":true,"usgs":true}],"preferred":true,"id":205458,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Brown, Dexter W. dwbrown@usgs.gov","contributorId":3062,"corporation":false,"usgs":true,"family":"Brown","given":"Dexter","email":"dwbrown@usgs.gov","middleInitial":"W.","affiliations":[],"preferred":true,"id":205460,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":58058,"text":"wri20014194 - 2001 - Water-quality characteristics in the Black Hills area, South Dakota","interactions":[],"lastModifiedDate":"2012-02-02T00:12:13","indexId":"wri20014194","displayToPublicDate":"2001-11-01T00:00:00","publicationYear":"2001","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":"2001-4194","title":"Water-quality characteristics in the Black Hills area, South Dakota","docAbstract":"This report summarizes the water-quality characteristics of ground-water and surface-water in the Black Hills area. Differences in groundwater quality by aquifer and differences in surfacewater quality by water source are presented. Ground-water characteristics are discussed individually for each of the major aquifers in the Black Hills area, referred to herein as the Precambrian, Deadwood, Madison, Minnelusa, Minnekahta, and Inyan Kara aquifers. Characteristics for minor aquifers also are discussed briefly. Surface-water characteristics are discussed for hydrogeologic settings including headwater springs, crystalline core sites, artesian springs, and exterior sites.\r\n\r\nTo characterize the water quality of aquifers and streams in the Black Hills area, data from the U.S. Geological Survey National Water Information System water-quality database were examined. This included samples collected as part of the Black Hills Hydrology Study as well as for other studies within the time frame of October 1, 1930, to September 30, 1998. Tables of individual results are not presented in this report, only summaries. Constituents summarized and discussed include physical properties, common ions, nutrients, trace elements, and radionuclides. Comparisons of concentration levels are made to drinking-water standards as well as beneficial-use and aquatic-life criteria.\r\n\r\nGround water within the Black Hills and surrounding area generally is fresh and hard to very hard. Concentrations exceeding various Secondary and Maximum Contaminant Levels may affect the use of the water in some areas for many aquifers within the study area. Concentrations that exceed Secondary Maximum Contaminant Levels (SMCL's) generally affect the water only aesthetically. Radionuclide concentrations may be especially high in some of the major aquifers used within the study area and preclude the use of water in some areas. The sodiumadsorption ratio and specific conductance may affect irrigation use for some wells.\r\n\r\nHigh concentrations of iron and manganese are the only concentrations that may hamper the use of water from Precambrian aquifers. The principal deterrents to use of water from the Deadwood aquifer are the high concentrations of radionuclides as well as iron and manganese. Iron, manganese, and hardness may deter use of water from the Madison aquifer as well as dissolved solids and sulfate in downgradient wells (generally deeper than 2,000 feet). Iron, manganese, and hardness may also deter use of the Minnelusa aquifer. Water from the Minnekahta aquifer generally is suitable for all water uses although it is hard to very hard. High concentrations of dissolved solids, iron, sulfate, and manganese may hamper the use of water from the Inyan Kara aquifer. In the southern Black Hills, radium-226 and uranium concentrations also may preclude use of water from the Inyan Kara aquifer. Suitability for irrigation may be affected by high specific conductance and sodium-adsorption ratio for the Inyan Kara.\r\n\r\nSurface-water quality within the Black Hills and surrounding area generally is very good but the water is hard to very hard. Concentrations of some constituents in the study area tend to be higher exterior to the Black Hills, primarily due to influences from the Cretaceous-age marine shales, including dissolved solids, sodium, sulfate, selenium, and uranium. Headwater springs have relatively constant discharge, specific conductance, dissolved solids, and concentrations of most other constituents.\r\n\r\nConcentrations at crystalline core sites are very similar to those found in samples from Precambrian aquifers. Some high nitrate concentrations greater than the Maximum Contaminant Level (MCL) of 10 mg/L (milligrams per liter) have occurred at Annie Creek near Lead, which have been attributed to mining impacts. Trace elements generally are low with the exception of arsenic, for which 60 percent of samples exceed the proposed MCL of 10 ug/L (micrograms per liter) and one sample","language":"ENGLISH","publisher":"U.S. Geological Survey","doi":"10.3133/wri20014194","collaboration":"Prepared in cooperation with the \r\nSouth Dakota Department of Environment and Natural Resources and the West Dakota Water Development District ","usgsCitation":"Williamson, J., and Carter, J.M., 2001, Water-quality characteristics in the Black Hills area, South Dakota: U.S. Geological Survey Water-Resources Investigations Report 2001-4194, 196 p. , https://doi.org/10.3133/wri20014194.","productDescription":"196 p. ","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[],"links":[{"id":184067,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":5987,"rank":100,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.usgs.gov/wri/wri014194/","linkFileType":{"id":5,"text":"html"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a09e4b07f02db5fafad","contributors":{"authors":[{"text":"Williamson, Joyce E. jewillia@usgs.gov","contributorId":1964,"corporation":false,"usgs":true,"family":"Williamson","given":"Joyce E.","email":"jewillia@usgs.gov","affiliations":[{"id":562,"text":"South Dakota Water Science Center","active":true,"usgs":true}],"preferred":false,"id":258240,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Carter, Janet M. 0000-0002-6376-3473 jmcarter@usgs.gov","orcid":"https://orcid.org/0000-0002-6376-3473","contributorId":339,"corporation":false,"usgs":true,"family":"Carter","given":"Janet","email":"jmcarter@usgs.gov","middleInitial":"M.","affiliations":[{"id":34685,"text":"Dakota Water Science Center","active":true,"usgs":true},{"id":562,"text":"South Dakota Water Science Center","active":true,"usgs":true}],"preferred":false,"id":258239,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":23429,"text":"ofr94260I - 2001 - Sulfur, carbon and oxygen systematics during diagenesis and fluid infiltration in the Creede caldera, Colorado","interactions":[{"subject":{"id":23429,"text":"ofr94260I - 2001 - Sulfur, carbon and oxygen systematics during diagenesis and fluid infiltration in the Creede caldera, Colorado","indexId":"ofr94260I","publicationYear":"2001","noYear":false,"chapter":"I","title":"Sulfur, carbon and oxygen systematics during diagenesis and fluid infiltration in the Creede caldera, Colorado"},"predicate":"IS_PART_OF","object":{"id":70226622,"text":"ofr94260AP - 2001 - Preliminary scientific results of the Creede Caldera Continental Scientific Drilling Program, Chapters A-P","indexId":"ofr94260AP","publicationYear":"2001","noYear":false,"chapter":"A-P","title":"Preliminary scientific results of the Creede Caldera Continental Scientific Drilling Program, Chapters A-P"},"id":1}],"isPartOf":{"id":70226622,"text":"ofr94260AP - 2001 - Preliminary scientific results of the Creede Caldera Continental Scientific Drilling Program, Chapters A-P","indexId":"ofr94260AP","publicationYear":"2001","noYear":false,"title":"Preliminary scientific results of the Creede Caldera Continental Scientific Drilling Program, Chapters A-P"},"lastModifiedDate":"2021-12-01T16:16:24.055691","indexId":"ofr94260I","displayToPublicDate":"2001-11-01T00:00:00","publicationYear":"2001","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":"94-260","chapter":"I","title":"Sulfur, carbon and oxygen systematics during diagenesis and fluid infiltration in the Creede caldera, Colorado","docAbstract":"<p>No abstract available.</p>","largerWorkType":{"id":18,"text":"Report"},"largerWorkTitle":"Preliminary scientific results of the Creede Caldera Continental Scientific Drilling Program, Chapters A-P","largerWorkSubtype":{"id":5,"text":"USGS Numbered Series"},"language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr94260I","issn":"0094-9140","usgsCitation":"Ilchik, R.P., and Rumble, D., 2001, Sulfur, carbon and oxygen systematics during diagenesis and fluid infiltration in the Creede caldera, Colorado: U.S. Geological Survey Open-File Report 94-260, 24 p., https://doi.org/10.3133/ofr94260I.","productDescription":"24 p.","costCenters":[],"links":[{"id":52754,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1994/0260i/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":156968,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1994/0260i/report-thumb.jpg"}],"country":"United States","state":"Colorado","city":"Creede","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -106.97319030761719,\n              37.791337175930686\n            ],\n            [\n              -106.66351318359375,\n              37.791337175930686\n            ],\n            [\n              -106.66351318359375,\n              37.99183365313853\n            ],\n            [\n              -106.97319030761719,\n              37.99183365313853\n            ],\n            [\n              -106.97319030761719,\n              37.791337175930686\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b05e4b07f02db699868","contributors":{"authors":[{"text":"Ilchik, Robert P.","contributorId":46125,"corporation":false,"usgs":true,"family":"Ilchik","given":"Robert","email":"","middleInitial":"P.","affiliations":[],"preferred":false,"id":190088,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Rumble, Douglas III","contributorId":18408,"corporation":false,"usgs":true,"family":"Rumble","given":"Douglas","suffix":"III","email":"","affiliations":[],"preferred":false,"id":190087,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":22852,"text":"ofr94260O - 2001 - Thermal data for Creede Caldera Moat project coreholes","interactions":[{"subject":{"id":22852,"text":"ofr94260O - 2001 - Thermal data for Creede Caldera Moat project coreholes","indexId":"ofr94260O","publicationYear":"2001","noYear":false,"chapter":"O","title":"Thermal data for Creede Caldera Moat project coreholes"},"predicate":"IS_PART_OF","object":{"id":70226622,"text":"ofr94260AP - 2001 - Preliminary scientific results of the Creede Caldera Continental Scientific Drilling Program, Chapters A-P","indexId":"ofr94260AP","publicationYear":"2001","noYear":false,"chapter":"A-P","title":"Preliminary scientific results of the Creede Caldera Continental Scientific Drilling Program, Chapters A-P"},"id":1}],"isPartOf":{"id":70226622,"text":"ofr94260AP - 2001 - Preliminary scientific results of the Creede Caldera Continental Scientific Drilling Program, Chapters A-P","indexId":"ofr94260AP","publicationYear":"2001","noYear":false,"title":"Preliminary scientific results of the Creede Caldera Continental Scientific Drilling Program, Chapters A-P"},"lastModifiedDate":"2021-12-01T16:27:17.515344","indexId":"ofr94260O","displayToPublicDate":"2001-11-01T00:00:00","publicationYear":"2001","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":"94-260","chapter":"O","title":"Thermal data for Creede Caldera Moat project coreholes","docAbstract":"<p>No abstract available.</p>","largerWorkType":{"id":18,"text":"Report"},"largerWorkTitle":"Preliminary scientific results of the Creede Caldera Continental Scientific Drilling Program, Chapters A-P","largerWorkSubtype":{"id":5,"text":"USGS Numbered Series"},"language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr94260O","issn":"0094-9140","usgsCitation":"Decker, E.R., 2001, Thermal data for Creede Caldera Moat project coreholes: U.S. Geological Survey Open-File Report 94-260, 12 p., https://doi.org/10.3133/ofr94260O.","productDescription":"12 p.","costCenters":[],"links":[{"id":52272,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1994/0260o/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":155881,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1994/0260o/report-thumb.jpg"}],"country":"United States","state":"Colorado","city":"Creede","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -106.97319030761719,\n              37.791337175930686\n            ],\n            [\n              -106.66351318359375,\n              37.791337175930686\n            ],\n            [\n              -106.66351318359375,\n              37.99183365313853\n            ],\n            [\n              -106.97319030761719,\n              37.99183365313853\n            ],\n            [\n              -106.97319030761719,\n              37.791337175930686\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b15e4b07f02db6a4be1","contributors":{"authors":[{"text":"Decker, Edward R.","contributorId":23975,"corporation":false,"usgs":true,"family":"Decker","given":"Edward","email":"","middleInitial":"R.","affiliations":[],"preferred":false,"id":188998,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":30676,"text":"ds62B - 2001 - Global GIS database. Digital atlas of Africa","interactions":[],"lastModifiedDate":"2026-04-10T15:12:53.746385","indexId":"ds62B","displayToPublicDate":"2001-11-01T00:00:00","publicationYear":"2001","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":310,"text":"Data Series","code":"DS","onlineIssn":"2327-638X","printIssn":"2327-0271","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"62","chapter":"B","title":"Global GIS database. Digital atlas of Africa","docAbstract":"This CD-ROM contains a digital atlas of the countries of Africa. This atlas is part of a global database compiled from USGS and other data sources at a nominal scale of 1:1 million and is intended to be used as a regional-scale reference and analytical tool by government officials, researchers, the private sector, and the general public. The atlas includes free GIS software or may be used with ESRI's ArcView software. Customized ArcView tools, specifically designed to make this atlas easier to use, are also included.","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ds62B","usgsCitation":"Hearn, P., Hare, T., Schruben, P., Sherrill, D., LaMar, C., and Tsushima, P., 2001, Global GIS database. 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,{"id":30778,"text":"cir1196A - 2001 - Gold recycling in the United States in 1998","interactions":[{"subject":{"id":22325,"text":"ofr00195 - 2000 - Gold recycling; a materials flow study","indexId":"ofr00195","publicationYear":"2000","noYear":false,"title":"Gold recycling; a materials flow study"},"predicate":"SUPERSEDED_BY","object":{"id":30778,"text":"cir1196A - 2001 - Gold recycling in the United States in 1998","indexId":"cir1196A","publicationYear":"2001","noYear":false,"chapter":"A","title":"Gold recycling in the United States in 1998"},"id":1}],"lastModifiedDate":"2012-02-02T00:09:08","indexId":"cir1196A","displayToPublicDate":"2001-11-01T00:00:00","publicationYear":"2001","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":307,"text":"Circular","code":"CIR","onlineIssn":"2330-5703","printIssn":"1067-084X","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"1196","chapter":"A","title":"Gold recycling in the United States in 1998","docAbstract":"In 1998, 175 metric tons (t) of refined gold was recovered by U.S. refiners from old and new scrap. The overall recycling rate was 29 percent when scrap consumption was compared with apparent domestic supply. Sources of old scrap includes discarded jewelry, dental materials, plating solutions, and electronic equipment. A very high old scrap recycling efficiency of 96 percent was reached in 1998, the supply of old scrap peaked, gold prices were at an 18-year low, and substantial amounts of old scrap were exported. U.S. net exports of old scrap had a gold content of 28 t.","largerWorkType":{"id":18,"text":"Report"},"largerWorkTitle":"Flow studies for recycling metal commodities in the United States","largerWorkSubtype":{"id":5,"text":"USGS Numbered Series"},"language":"ENGLISH","doi":"10.3133/cir1196A","collaboration":"Supersedes OFR 00-195-A","usgsCitation":"Amey, E., 2001, Gold recycling in the United States in 1998: U.S. Geological Survey Circular 1196, p. A1-A8, https://doi.org/10.3133/cir1196A.","productDescription":"p. A1-A8","costCenters":[],"links":[{"id":160644,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":2601,"rank":100,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.usgs.gov/circular/c1196a/","linkFileType":{"id":5,"text":"html"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4abde4b07f02db674020","contributors":{"authors":[{"text":"Amey, Earle B.","contributorId":67864,"corporation":false,"usgs":true,"family":"Amey","given":"Earle B.","affiliations":[],"preferred":false,"id":203886,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":31232,"text":"ofr0171 - 2001 - Quality-assurance data for routine water quality analyses by the U. S. Geological Survey laboratory in Troy, New York; July 1993 through June 1995","interactions":[],"lastModifiedDate":"2012-02-02T00:09:09","indexId":"ofr0171","displayToPublicDate":"2001-11-01T00:00:00","publicationYear":"2001","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":"2001-71","title":"Quality-assurance data for routine water quality analyses by the U. S. Geological Survey laboratory in Troy, New York; July 1993 through June 1995","docAbstract":"A laboratory for analysis of low-ionic strength water has been developed at the U.S. Geological Survey (USGS) office in Troy, N.Y., to analyze samples collected by USGS projects in the Northeast. The laboratory's quality-assurance program is based on internal and interlaboratory quality-assurance samples and quality-control procedures developed to ensure proper sample collection, processing, and analysis. The quality-assurance/quality-control data are stored in the laboratory's SAS data-management system, which provides efficient review, compilation, and plotting of quality-assurance/quality-control data. This report presents and discusses samples analyzed from July 1993 through June 1995.  \r\n\r\nQuality-control results for 18 analytical procedures were evaluated for bias and precision. Control charts show that data from seven of the analytical procedures were biased throughout the analysis period for either high-concentration or low-concentration samples but were within control limits; these procedures were: acid-neutralizing capacity, dissolved inorganic carbon, dissolved organic carbon (soil expulsions), chloride, magnesium, nitrate (colorimetric method), and pH. Three of the analytical procedures were occasionally biased but were within control limits; they were: calcium (high for high-concentration samples for May 1995), dissolved organic carbon (high for highconcentration samples from January through September 1994), and fluoride (high in samples for April and June 1994). No quality-control sample has been developed for the organic monomeric aluminum procedure.  \r\n\r\nResults from the filter-blank and analytical-blank analyses indicate that all analytical procedures in which blanks were run were within control limits, although values for a few blanks were outside the control limits. Blanks were not analyzed for acid-neutralizing capacity, dissolved inorganic carbon, fluoride, nitrate (colorimetric method), or pH.  \r\n\r\nSampling and analysis precision are evaluated herein in terms of the coefficient of variation obtained for triplicate samples in 14 of the 18 procedures. Data-quality objectives were met by more than 90 percent of the samples analyzed in all procedures except total monomeric aluminum (85 percent of samples met objectives), total aluminum (70 percent of samples met objectives), and dissolved organic carbon (85 percent of samples met objectives). Triplicate samples were not analyzed for ammonium, fluoride, dissolved inorganic carbon, or nitrate (colorimetric method).  \r\n\r\nResults of the USGS interlaboratory Standard Reference Sample Program indicated high data quality with a median result of 3.6 of a possible 4.0. Environment Canada's LRTAP interlaboratory study results indicated that more than 85 percent of the samples met data-quality objectives in 6 of the 12 analyses; exceptions were calcium, dissolved organic carbon, chloride, pH, potassium, and sodium. Data-quality objectives were not met for calcium samples in one LRTAP study, but 94 percent of samples analyzed were within control limits for the remaining studies. Data-quality objectives were not met by 35 percent of samples analyzed for dissolved organic carbon, but 94 percent of sample values were within 20 percent of the most probable value. Data-quality objectives were not met for 30 percent of samples analyzed for chloride, but 90 percent of sample values were within 20 percent of the most probable value. Measurements of samples with a pH above 6.0 were biased high in 54 percent of the samples, although 85 percent of the samples met data-quality objectives for pH measurements below 6.0. Data-quality objectives for potassium and sodium were not met in one study (only 33 percent of the samples analyzed met the objectives), although 85 percent of the sample values were within control limits for the other studies. Measured sodium values were above the upper control limit in all studies.  \r\n\r\nResults from blind reference-sample analyses indicated that data","language":"ENGLISH","doi":"10.3133/ofr0171","usgsCitation":"Lincoln, T.A., Horan-Ross, D.A., McHale, M.R., and Lawrence, G.B., 2001, Quality-assurance data for routine water quality analyses by the U. S. Geological Survey laboratory in Troy, New York; July 1993 through June 1995: U.S. Geological Survey Open-File Report 2001-71, v, 25 p. : ill. ; 28 cm. , https://doi.org/10.3133/ofr0171.","productDescription":"v, 25 p. : ill. ; 28 cm. ","costCenters":[],"links":[{"id":2801,"rank":100,"type":{"id":15,"text":"Index Page"},"url":"https://ny.water.usgs.gov/pubs/of/of01071/","linkFileType":{"id":5,"text":"html"}},{"id":95912,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/2001/0071/report.pdf","size":"2649","linkFileType":{"id":1,"text":"pdf"}},{"id":160558,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/2001/0071/report-thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a62e4b07f02db63685d","contributors":{"authors":[{"text":"Lincoln, Tricia A. tarenga@usgs.gov","contributorId":3803,"corporation":false,"usgs":true,"family":"Lincoln","given":"Tricia","email":"tarenga@usgs.gov","middleInitial":"A.","affiliations":[],"preferred":true,"id":205401,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Horan-Ross, Debra A. dhross@usgs.gov","contributorId":3809,"corporation":false,"usgs":true,"family":"Horan-Ross","given":"Debra","email":"dhross@usgs.gov","middleInitial":"A.","affiliations":[],"preferred":true,"id":205402,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"McHale, Michael R. 0000-0003-3780-1816 mmchale@usgs.gov","orcid":"https://orcid.org/0000-0003-3780-1816","contributorId":1735,"corporation":false,"usgs":true,"family":"McHale","given":"Michael","email":"mmchale@usgs.gov","middleInitial":"R.","affiliations":[{"id":474,"text":"New York Water Science Center","active":true,"usgs":true}],"preferred":true,"id":205400,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Lawrence, Gregory B. 0000-0002-8035-2350 glawrenc@usgs.gov","orcid":"https://orcid.org/0000-0002-8035-2350","contributorId":867,"corporation":false,"usgs":true,"family":"Lawrence","given":"Gregory","email":"glawrenc@usgs.gov","middleInitial":"B.","affiliations":[{"id":474,"text":"New York Water Science Center","active":true,"usgs":true}],"preferred":true,"id":205399,"contributorType":{"id":1,"text":"Authors"},"rank":4}]}}
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