{"pageNumber":"4496","pageRowStart":"112375","pageSize":"25","recordCount":184769,"records":[{"id":70044331,"text":"70044331 - 1989 - Anadarko Basin conodont studies","interactions":[],"lastModifiedDate":"2013-03-03T10:08:34","indexId":"70044331","displayToPublicDate":"2013-01-01T00:00:00","publicationYear":"1989","noYear":false,"publicationType":{"id":5,"text":"Book chapter"},"publicationSubtype":{"id":24,"text":"Book Chapter"},"seriesNumber":"90","title":"Anadarko Basin conodont studies","docAbstract":"Preliminary analysis of early Paleozoic conodonts from the subsurface within and adjacent to the Anadarko basin demonstrates their utility in stratigraphic and thermal evolution studies in the basin. More than 100 samples from 30 drill holes produced conodonts that can be correlated with faunas known from rock sequences exposed along the southern flanks of the basin. For the Middle Ordovician to Devonian, extant biozonations and/or recent published literature based on Oklahoma surface sections allow good biostratigraphic correlation into the subsurface and often allow testing of physical correlations. In contrast, conodonts from the Arbuckle Group (Lower to Middle Ordovician) are less well known. Faunas from the upper half of the group are documented only in unpublished theses, and published faunas are in need of restudy and revision. However, this limited information, along with work in progress in Oklahoma and data from carbonate platform facies elsewhere in North America, still permit correlations into the subsurface with the promise of increasingly improved resolution.","largerWorkType":{"id":18,"text":"Report"},"largerWorkTitle":"Anadarko Basin symposium, 1988 (Circular 90)","largerWorkSubtype":{"id":4,"text":"Other Government Series"},"language":"English","publisher":"Oklahoma Geological Survey","publisherLocation":"Norman, OK","collaboration":"Proceedings of a symposium held April 5-6, 1988, at Norman, Oklahoma; cosponsored by the Oklahoma Geological Survey and the U.S. Geological Survey","usgsCitation":"Repetski, J.E., 1989, Anadarko Basin conodont studies, chap. <i>of</i> Anadarko Basin symposium, 1988 (Circular 90), p. 133-133.","productDescription":"1 p.","startPage":"133","endPage":"133","costCenters":[],"links":[{"id":268675,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"},{"id":268674,"type":{"id":11,"text":"Document"},"url":"https://www.ogs.ou.edu/pubsscanned/Circulars/Circular90.pdf"}],"country":"United States","state":"Oklahoma","otherGeospatial":"Anadarko Basin","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -103.0,33.62 ], [ -103.0,37.0 ], [ -94.43,37.0 ], [ -94.43,33.62 ], [ -103.0,33.62 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"51347ef4e4b0e1603e4fec34","contributors":{"authors":[{"text":"Repetski, John E. 0000-0002-2298-7120 jrepetski@usgs.gov","orcid":"https://orcid.org/0000-0002-2298-7120","contributorId":2596,"corporation":false,"usgs":true,"family":"Repetski","given":"John","email":"jrepetski@usgs.gov","middleInitial":"E.","affiliations":[{"id":243,"text":"Eastern Geology and Paleoclimate Science Center","active":true,"usgs":true},{"id":40020,"text":"Florence Bascom Geoscience Center","active":true,"usgs":true}],"preferred":true,"id":475301,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":70044340,"text":"70044340 - 1989 - Analysis of sedimentary facies and petrofacies of lower Morrowan-upper Chesterian sandstones, Anadarko Basin, Oklahoma","interactions":[],"lastModifiedDate":"2013-03-03T18:47:28","indexId":"70044340","displayToPublicDate":"2013-01-01T00:00:00","publicationYear":"1989","noYear":false,"publicationType":{"id":5,"text":"Book chapter"},"publicationSubtype":{"id":24,"text":"Book Chapter"},"seriesNumber":"90","title":"Analysis of sedimentary facies and petrofacies of lower Morrowan-upper Chesterian sandstones, Anadarko Basin, Oklahoma","docAbstract":"Three major lithofacies have been identified within the Morrow (Pennsylvanian) and Springer (Pennsylvanian-Mississippian) units, in core from 30 drill holes ranging from the Oklahoma Panhandle to the southwestern portion of the Anadarko basin. The study included inspection of ~6,500 ft of core, examination of ~100 thin sections, and a scanning-electron-microscope study of butts of the material used for thin-section preparation. The lithofacies identified are (1) fluvial-influenced coastal, which includes the deltaic facies described by Swanson (1979), (2) tidal-influenced nearshore, and (3) mixed, which shows mixed tidal and nontidal marine influence. Our interpretation is supported by the investigations of Moore (1979), Haiduk (1987), and Swanson (1979). The fluvial-influenced coastal facies is restricted to the northwestern (Panhandle) portion of the Anadarko basin.","largerWorkType":{"id":18,"text":"Report"},"largerWorkTitle":"Anadarko Basin symposium, 1988 (Circular 90)","largerWorkSubtype":{"id":4,"text":"Other Government Series"},"language":"English","publisher":"Oklahoma Geological Survey","publisherLocation":"Norman, OK","collaboration":"Proceedings of a symposium held April 5-6, 1988, at Norman, Oklahoma; cosponsored by the Oklahoma Geological Survey and the U.S. Geological Survey","usgsCitation":"Keighin, C.W., and Flores, R.M., 1989, Analysis of sedimentary facies and petrofacies of lower Morrowan-upper Chesterian sandstones, Anadarko Basin, Oklahoma, chap. <i>of</i> Anadarko Basin symposium, 1988 (Circular 90), p. 236-238.","productDescription":"3 p.","startPage":"236","endPage":"238","costCenters":[],"links":[{"id":268692,"type":{"id":11,"text":"Document"},"url":"https://www.ogs.ou.edu/pubsscanned/Circulars/Circular90.pdf"},{"id":268693,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United States","state":"Oklahoma","otherGeospatial":"Anadarko Basin","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -103.0,33.62 ], [ -103.0,37.0 ], [ -94.43,37.0 ], [ -94.43,33.62 ], [ -103.0,33.62 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"51347f02e4b0e1603e4fec38","contributors":{"authors":[{"text":"Keighin, C. William","contributorId":36804,"corporation":false,"usgs":true,"family":"Keighin","given":"C.","email":"","middleInitial":"William","affiliations":[],"preferred":false,"id":475319,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Flores, Romeo M. rflores@usgs.gov","contributorId":71984,"corporation":false,"usgs":true,"family":"Flores","given":"Romeo","email":"rflores@usgs.gov","middleInitial":"M.","affiliations":[{"id":165,"text":"Central Energy Resources Team","active":false,"usgs":true}],"preferred":false,"id":475320,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":70044335,"text":"70044335 - 1989 - Paleohydrology of the Anadarko Basin, central United States","interactions":[],"lastModifiedDate":"2013-03-03T10:52:25","indexId":"70044335","displayToPublicDate":"2013-01-01T00:00:00","publicationYear":"1989","noYear":false,"publicationType":{"id":5,"text":"Book chapter"},"publicationSubtype":{"id":24,"text":"Book Chapter"},"seriesNumber":"90","title":"Paleohydrology of the Anadarko Basin, central United States","docAbstract":"Geohydrologic systems in the Anadarko basin in the central United States are controlled by topography, climate, geologic structures, and aquifer hydraulic properties, all of which are the result of past geologic and hydrologic processes, including tectonics and diagenesis. From Late Cambrian through Middle Ordovician time, a generally transgressive but cyclic sea covered the area. The first deposits were permPable sand, followed by calcareous mud. During periods of sea transgression, burial diagenesis decreased porosity and permeability. During periods of sea recession, uplift diagenesis increased porosity and permeability, especially in exposed rocks. During most of Silurian and Devonian time, the sea receded; increased porosity and permeability resulted from uplift diagenesis. However, at the end of the Devonian and during the Early Mississippian, very slightly permeable clay, which now is a regional confining unit, was deposited in a mostly euxinic sea. Later during Mississippian time, calcareous muds, which became limestone, were deposited in and adjacent to the Anadarko basin and underwent burial diagenesis. During Pennsylvanian time, rapid sedimentation accompanied rapid subsidence in the Anadarko basin. A geopressure zone probably resulted when sediments with little permeability trapped depositional water in Lower Pennsylvanian sands. Burial diagenesis included compaction and thermal alteration of deeply buried organic material, which released carbon dioxide, water, and hydrocarbons. By Middle Pennsylvanian time, the sea had submerged most of the central United States, including the Ozarks, as tectonic activity reached its maximum. During Late Pennsylvanian and Early Permian time, the Ouachita uplift had been formed and was higher than the Ozarks. Uplift was accompanied by a regional upward tilt toward the Ouachita-Ozarks area; the sea receded westward, depositing large quantities of calcareous mud and clay, and precipitating evaporitic material in the restricted-circulation environment. By the end of Permian time, > 20,000 ft of Pennsylvanian and Permian sediments had been deposited in the Anadarko basin. These thick sediments caused rapid and extreme burial diagenesis, including alteration of organic material. During Permian time in the Ozarks area, development of the Ozark Plateaus aquifer system commenced in the permeable Cambrian-Mississippian rocks near the St. Francois Mountains as the Pennsylvanian confining material was removed. Since Permian time, uplift diagenesis has been more active than burial diagenesis in the Anadarko basin. Synopsis of paleohydrologic interpretation indicates that Cambrian-Mississippian rocks in the Anadarko basin should be relatively impermeable, except for local secondary permeability, because rocks in the basin have undergone little uplift diagenesis.","largerWorkType":{"id":18,"text":"Report"},"largerWorkTitle":"Anadarko Basin symposium (Circular 90)","largerWorkSubtype":{"id":4,"text":"Other Government Series"},"language":"English","publisher":"Oklahoma Geological Survey","publisherLocation":"Norman, OK","collaboration":"Proceedings of a symposium held April 5-6, 1988, at Norman, Oklahoma; cosponsored by the Oklahoma Geological Survey and the U.S. Geological Survey","usgsCitation":"Jorgensen, D.G., 1989, Paleohydrology of the Anadarko Basin, central United States, chap. <i>of</i> Anadarko Basin symposium (Circular 90), p. 176-193.","productDescription":"18 p.","startPage":"176","endPage":"193","costCenters":[],"links":[{"id":268683,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"},{"id":268682,"type":{"id":11,"text":"Document"},"url":"https://www.ogs.ou.edu/pubsscanned/Circulars/Circular90.pdf"}],"country":"United States","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -126.0,23.5 ], [ -126.0,50.0 ], [ -66.9,50.0 ], [ -66.9,23.5 ], [ -126.0,23.5 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"51347f09e4b0e1603e4fec62","contributors":{"authors":[{"text":"Jorgensen, Donald G.","contributorId":19537,"corporation":false,"usgs":true,"family":"Jorgensen","given":"Donald","email":"","middleInitial":"G.","affiliations":[],"preferred":false,"id":475307,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":70044336,"text":"70044336 - 1989 - Mineralogic and textural relations in deeply buried rocks of the Simpson Group (Middle Ordovician)--implications in diagenesis and petroleum geology","interactions":[],"lastModifiedDate":"2013-03-03T11:09:31","indexId":"70044336","displayToPublicDate":"2013-01-01T00:00:00","publicationYear":"1989","noYear":false,"publicationType":{"id":5,"text":"Book chapter"},"publicationSubtype":{"id":24,"text":"Book Chapter"},"seriesNumber":"90","title":"Mineralogic and textural relations in deeply buried rocks of the Simpson Group (Middle Ordovician)--implications in diagenesis and petroleum geology","docAbstract":"The mineral composition and petrography of sandstones, shales, carbonates, and intermediate lithologies were determined on 112 core samples of the Middle Ordovician Simpson Group in the Sunray DX Parker No. 1 Mazur well, Grady County, Oklahoma. Core was recovered from present depths of about 15,900-17,200 ft and included all or parts of the Bromide, Tulip Creek, McLish, Oil Creek, and Joins Formations. The bulk-rock mineral composition of Simpson Group rocks is diverse. The mean weighted composition of 50 sandstone samples is 66% quartz, 14% clay, and 18% carbonate, as determined by X-ray powder diffraction (XRD). Some sandstones from the Oil Creek and Tulip Creek Formations contain as much as 96% quartz. These quartz-rich sandstones were cemented early by silica. Feldspar averages 2%; some sandstones from the McLish Formation contain as much as 15% feldspar. Potassium feldspar is commonly more abundant than plagioclase; potassium feldspar overgrowths are found in some of the sandstones. Most of the shales are clay-rich and quartz-poor, averaging about 85% clay minerals, 7% quartz, and 3% feldspar, by weight, as determined by XRD. Carbonate, fluorapatite, and pyrite are present in variable amounts. Such high clay/quartz ratios are not characteristic of shales and suggest that silica has been expelled by diagenetic processes during burial. The main clay mineral in the Simpson Group at these depths is illite, although iron-rich chlorite is locally concentrated in sandstones. Illite typically makes up >90 wt. % of the clay minerals in sandstones and >95 wt. % of those in shale and carbonate. Total clay content, determined from XRD, correlates closely with total gamma-ray intensity from geophysical logs, because illite is the primary potassium-bearing phase in these deeply buried rocks. Therefore, the gamma-ray log is a good indicator of \"shaliness\" in potential Simpson reservoirs at similar depths. Much of the carbonate was introduced into the sandstones during burial as calcite, dolomite, or ankerite cement. Early iron-free calcite is commonly replaced by iron-bearing calcite, dolomite, or ankerite. Sandstones and carbonate rocks also contain rhombic dolomite. Many of the dolomite rhombs contain overgrowths of ferroan dolomite or ankerite, as evidenced by staining. Ankerite cementation is later and less selective than earlier dolomite and commonly replaces earlier carbonate or silica cements. Dolomite commonly replaces detrital clay and calcite. Spatial and textural relations suggest that the conversion of smectite to illite contributed, in part, to the formation of dolomite and ankerite cements. Scanning electron miscroscopy reveals that much of the diagenetic illite occurs as tabular fibers in pores or as pseudomorphic intergrowths after smectite. Most chlorite in sandstones is authigenic and occurs as a pore-lining cement or as a pseudomorphic replacement after kaolinite. Secondary porosity, formed mainly from the dissolution of intergranular carbonate cements, is best developed in sandstones from the Oil Creek and Tulip Creek Formations.","largerWorkType":{"id":18,"text":"Report"},"largerWorkTitle":"Anadarko Basin symposium, 1998 (Circular 90)","largerWorkSubtype":{"id":4,"text":"Other Government Series"},"language":"English","publisher":"Oklahoma Geological Survey","publisherLocation":"Norman, OK","collaboration":"Proceedings of a symposium held April 5-6, 1988, at Norman, Oklahoma; cosponsored by the Oklahoma Geological Survey and the U.S. Geological Survey","usgsCitation":"Pollastro, R.M., 1989, Mineralogic and textural relations in deeply buried rocks of the Simpson Group (Middle Ordovician)--implications in diagenesis and petroleum geology, chap. <i>of</i> Anadarko Basin symposium, 1998 (Circular 90), p. 194-208.","productDescription":"15 p.","startPage":"194","endPage":"208","costCenters":[],"links":[{"id":268685,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"},{"id":268684,"type":{"id":11,"text":"Document"},"url":"https://www.ogs.ou.edu/pubsscanned/Circulars/Circular90.pdf"}],"country":"United States","state":"Oklahoma","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -103.0,33.62 ], [ -103.0,37.0 ], [ -94.43,37.0 ], [ -94.43,33.62 ], [ -103.0,33.62 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"51347f09e4b0e1603e4fec5e","contributors":{"authors":[{"text":"Pollastro, Richard M.","contributorId":25100,"corporation":false,"usgs":true,"family":"Pollastro","given":"Richard","email":"","middleInitial":"M.","affiliations":[],"preferred":false,"id":475308,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":70044337,"text":"70044337 - 1989 - Sulfide mineralization and magnetization, Cement oil field, Oklahoma","interactions":[],"lastModifiedDate":"2013-03-03T18:12:37","indexId":"70044337","displayToPublicDate":"2013-01-01T00:00:00","publicationYear":"1989","noYear":false,"publicationType":{"id":5,"text":"Book chapter"},"publicationSubtype":{"id":24,"text":"Book Chapter"},"seriesNumber":"90","title":"Sulfide mineralization and magnetization, Cement oil field, Oklahoma","docAbstract":"Geochemical, petrographic, and rock-magnetic studies were undertaken to investigate possible sources for reported positive aeromagnetic anomalies over the Cement oil field, Oklahoma. Ferrimagnetic pyrrhotite (monoclinic, Fe<sup>7</sup>S<sup>8</sup> ), intergrown with more-abundant, nonmagnetic pyrite (FeS<sup>2</sup>), is present in well-cutting, core, and quarry samples at Cement, and it is the only identified source of possible enhanced magnetization in rocks over the field. Magnetite, found only in well cuttings from Cement, is contamination from drilling. Magnetite was considered previously by others to be the source of magnetic anomalies at Cement.","largerWorkType":{"id":18,"text":"Report"},"largerWorkTitle":"Anadarko Basin symposium, 1988 (Circular 90)","largerWorkSubtype":{"id":4,"text":"Other Government Series"},"language":"English","publisher":"Oklahoma Geological Survey","publisherLocation":"Norman, OK","collaboration":"Proceedings of a symposium held April 5-6, 1988, at Norman, Oklahoma; cosponsored by the Oklahoma Geological Survey and the U.S. Geological Survey","usgsCitation":"Reynolds, R.L., Fishman, N.S., Webring, M.W., Wanty, R.B., and Goldhaber, M.B., 1989, Sulfide mineralization and magnetization, Cement oil field, Oklahoma, chap. <i>of</i> Anadarko Basin symposium, 1988 (Circular 90), p. 209-209.","productDescription":"1 p.","startPage":"209","endPage":"209","costCenters":[],"links":[{"id":268687,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"},{"id":268686,"type":{"id":11,"text":"Document"},"url":"https://www.ogs.ou.edu/pubsscanned/Circulars/Circular90.pdf"}],"country":"United States","state":"Oklahoma","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -103.0,33.62 ], [ -103.0,37.0 ], [ -94.43,37.0 ], [ -94.43,33.62 ], [ -103.0,33.62 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"51347f0de4b0e1603e4fec76","contributors":{"authors":[{"text":"Reynolds, Richard L. 0000-0002-4572-2942 rreynolds@usgs.gov","orcid":"https://orcid.org/0000-0002-4572-2942","contributorId":441,"corporation":false,"usgs":true,"family":"Reynolds","given":"Richard","email":"rreynolds@usgs.gov","middleInitial":"L.","affiliations":[{"id":271,"text":"Federal Center","active":false,"usgs":true}],"preferred":true,"id":475309,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Fishman, Neil S.","contributorId":106464,"corporation":false,"usgs":true,"family":"Fishman","given":"Neil","email":"","middleInitial":"S.","affiliations":[],"preferred":false,"id":475313,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Webring, Michael W. mwebring@usgs.gov","contributorId":1221,"corporation":false,"usgs":true,"family":"Webring","given":"Michael","email":"mwebring@usgs.gov","middleInitial":"W.","affiliations":[],"preferred":true,"id":475311,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Wanty, Richard B. 0000-0002-2063-6423 rwanty@usgs.gov","orcid":"https://orcid.org/0000-0002-2063-6423","contributorId":443,"corporation":false,"usgs":true,"family":"Wanty","given":"Richard","email":"rwanty@usgs.gov","middleInitial":"B.","affiliations":[{"id":211,"text":"Crustal Geophysics and Geochemistry Science Center","active":true,"usgs":true}],"preferred":true,"id":475310,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"Goldhaber, Martin B. 0000-0002-1785-4243 mgold@usgs.gov","orcid":"https://orcid.org/0000-0002-1785-4243","contributorId":1339,"corporation":false,"usgs":true,"family":"Goldhaber","given":"Martin","email":"mgold@usgs.gov","middleInitial":"B.","affiliations":[{"id":211,"text":"Crustal Geophysics and Geochemistry Science Center","active":true,"usgs":true},{"id":171,"text":"Central Mineral and Environmental Resources Science Center","active":true,"usgs":true}],"preferred":true,"id":475312,"contributorType":{"id":1,"text":"Authors"},"rank":5}]}}
,{"id":70044342,"text":"70044342 - 1989 - Formation resistivity as an indicator of the onset of oil generation in the Woodford Shale, Anadarko Basin, Oklahoma","interactions":[],"lastModifiedDate":"2013-03-03T19:24:48","indexId":"70044342","displayToPublicDate":"2013-01-01T00:00:00","publicationYear":"1989","noYear":false,"publicationType":{"id":5,"text":"Book chapter"},"publicationSubtype":{"id":24,"text":"Book Chapter"},"seriesNumber":"90","title":"Formation resistivity as an indicator of the onset of oil generation in the Woodford Shale, Anadarko Basin, Oklahoma","docAbstract":"The Upper Devonian and Lower Mississippian Woodford Shale is a black, organic-rich shale that is a major hydrocarbon source rock in the Anadarko basin. With the onset of oil generation, nonconductive hydrocarbons begin to replace conductive pore water in the Woodford, and formation resistivity increases. Crossplots of formation resistivity versus either vitrinite reflectance (R<sub>O</sub>) or Lopatin's time-temperature index of thermal maturity (TTI) define two data populations that represent immature shales and shales that have generated oil. The midpoint of the resistivity zone marking the transition between immature and mature shales is -35 ohm-m. The onset of appreciable oil generation in the Woodford Shale of the study area occurs at maturity levels of R<sub>O</sub> near 0.57% and of TTI between 33 and 48.","largerWorkType":{"id":18,"text":"Report"},"largerWorkTitle":"Anadarko Basin symposium, 1988 (Circular 90)","largerWorkSubtype":{"id":4,"text":"Other Government Series"},"language":"English","publisher":"Oklahoma Geological Survey","publisherLocation":"Norman, OK","collaboration":"Proceedings of a symposium held April 5-6, 1988, at Norman, Oklahoma; cosponsored by the Oklahoma Geological Survey and the U.S. Geological Survey","usgsCitation":"Schmoker, J.W., and Hester, T.C., 1989, Formation resistivity as an indicator of the onset of oil generation in the Woodford Shale, Anadarko Basin, Oklahoma, chap. <i>of</i> Anadarko Basin symposium, 1988 (Circular 90), p. 262-266.","productDescription":"5 p.","startPage":"262","endPage":"266","costCenters":[],"links":[{"id":268697,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"},{"id":268696,"type":{"id":11,"text":"Document"},"url":"https://www.ogs.ou.edu/pubsscanned/Circulars/Circular90.pdf"}],"country":"United States","state":"Oklahoma","otherGeospatial":"Anadarko Basin","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -103.0,33.62 ], [ -103.0,37.0 ], [ -94.43,37.0 ], [ -94.43,33.62 ], [ -103.0,33.62 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"51347f05e4b0e1603e4fec4c","contributors":{"authors":[{"text":"Schmoker, James W.","contributorId":52171,"corporation":false,"usgs":true,"family":"Schmoker","given":"James","email":"","middleInitial":"W.","affiliations":[],"preferred":false,"id":475324,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Hester, Timothy C.","contributorId":21995,"corporation":false,"usgs":true,"family":"Hester","given":"Timothy","email":"","middleInitial":"C.","affiliations":[],"preferred":false,"id":475323,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":70044338,"text":"70044338 - 1989 - Regional gravity of the Anadarko Basin area and a more detailed look at the Wichita frontal fault zone","interactions":[],"lastModifiedDate":"2013-03-03T18:22:19","indexId":"70044338","displayToPublicDate":"2013-01-01T00:00:00","publicationYear":"1989","noYear":false,"publicationType":{"id":5,"text":"Book chapter"},"publicationSubtype":{"id":24,"text":"Book Chapter"},"seriesNumber":"90","title":"Regional gravity of the Anadarko Basin area and a more detailed look at the Wichita frontal fault zone","docAbstract":"We presented poster displays on gravity surveys in and around the Anadarko basin at the Anadarko Basin Workshop in Norman, Oklahoma, on April 5-6, 1988.","largerWorkType":{"id":18,"text":"Report"},"largerWorkTitle":"Anadarko Basin symposium, 1988 (Circular 90)","largerWorkSubtype":{"id":4,"text":"Other Government Series"},"language":"English","publisher":"Oklahoma Geological Survey","publisherLocation":"Norman, OK","collaboration":"Proceedings of a symposium held April 5-6, 1988, at Norman, Oklahoma; cosponsored by the Oklahoma Geological Survey and the U.S. Geological Survey","usgsCitation":"Robbins, S.L., Jones-Cecil, M., and Keller, G.R., 1989, Regional gravity of the Anadarko Basin area and a more detailed look at the Wichita frontal fault zone, chap. <i>of</i> Anadarko Basin symposium, 1988 (Circular 90), p. 225-227.","productDescription":"3 p.","startPage":"225","endPage":"227","costCenters":[],"links":[{"id":268688,"type":{"id":11,"text":"Document"},"url":"https://www.ogs.ou.edu/pubsscanned/Circulars/Circular90.pdf"},{"id":268689,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United States","state":"Oklahoma","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -103.0,33.62 ], [ -103.0,37.0 ], [ -94.43,37.0 ], [ -94.43,33.62 ], [ -103.0,33.62 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"51347f0be4b0e1603e4fec6a","contributors":{"authors":[{"text":"Robbins, S. L.","contributorId":49766,"corporation":false,"usgs":true,"family":"Robbins","given":"S.","email":"","middleInitial":"L.","affiliations":[],"preferred":false,"id":475314,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Jones-Cecil, Meridee","contributorId":68313,"corporation":false,"usgs":true,"family":"Jones-Cecil","given":"Meridee","email":"","affiliations":[],"preferred":false,"id":475315,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Keller, G. R. Jr.","contributorId":85031,"corporation":false,"usgs":true,"family":"Keller","given":"G.","suffix":"Jr.","email":"","middleInitial":"R.","affiliations":[],"preferred":false,"id":475316,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":70044341,"text":"70044341 - 1989 - Relationship of clay-mineral diagenesis to temperature, age, and hydrocarbon generation&ndash;an example from the Anadarko Basin, Oklahoma","interactions":[],"lastModifiedDate":"2013-03-03T19:16:11","indexId":"70044341","displayToPublicDate":"2013-01-01T00:00:00","publicationYear":"1989","noYear":false,"publicationType":{"id":5,"text":"Book chapter"},"publicationSubtype":{"id":24,"text":"Book Chapter"},"seriesNumber":"90","title":"Relationship of clay-mineral diagenesis to temperature, age, and hydrocarbon generation&ndash;an example from the Anadarko Basin, Oklahoma","docAbstract":"Randomly interstratified illite/smectite (I/S) is present in Springeran and Morrowan rocks (Late Mississippian and Early Pennsylvanian) of the Anadarko basin, Oklahoma, at present-day depths <2,750 m, but disappears at depths of 2,750-3,050 m. Only ordered I/S is found in samples below 3,050 m. The work reported here relates the diagenesis of I/S to burial history and oil generation in the Anadarko basin and tests the dependence of the smectite-to-illite reaction on temperature and time. Published temperature models of clay diagenesis suggest that, for Tertiary and Cretaceous rocks, the transition from randomly interstratified I/S to ordered I/S occurs at 100-110°C. Burial reconstructions for the Anadarko basin indicate that maximum temperatures of 100-110°C correspond to present-day burial depths between 2,700 and 3,100 m. These independently calculated depths for the 100-110°C isotherm match the depths at which randomly interstratified I/S is observed to disappear in Morrowan-Springeran rocks. Thus, random I/S disappears at the same temperature in rocks that differ in age by some 300 m.y. Although the extent of the smectite-to-illite reaction is controlled by kinetics, and effects of time are apparent in laboratory experiments and short-lived geologic systems, the results of this study suggest that time plays a secondary role in long-term diagenetic settings.","largerWorkType":{"id":18,"text":"Report"},"largerWorkTitle":"Anadarko Basin symposium, 1988 (Circular 90)","largerWorkSubtype":{"id":4,"text":"Other Government Series"},"language":"English","publisher":"Oklahoma Geological Survey","publisherLocation":"Norman, OK","collaboration":"Proceedings of a symposium held April 5-6, 1988, at Norman, Oklahoma; cosponsored by the Oklahoma Geological Survey and the U.S. Geological Survey","usgsCitation":"Pollastro, R.M., and Schmoker, J.W., 1989, Relationship of clay-mineral diagenesis to temperature, age, and hydrocarbon generation&ndash;an example from the Anadarko Basin, Oklahoma, chap. <i>of</i> Anadarko Basin symposium, 1988 (Circular 90), p. 257-261.","productDescription":"4 p.","startPage":"257","endPage":"261","costCenters":[],"links":[{"id":268695,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"},{"id":268694,"type":{"id":11,"text":"Document"},"url":"https://www.ogs.ou.edu/pubsscanned/Circulars/Circular90.pdf"}],"country":"United States","state":"Oklahoma","otherGeospatial":"Anadarko Basin","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -103.0,33.62 ], [ -103.0,37.0 ], [ -94.43,37.0 ], [ -94.43,33.62 ], [ -103.0,33.62 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"51347f0be4b0e1603e4fec6e","contributors":{"authors":[{"text":"Pollastro, Richard M.","contributorId":25100,"corporation":false,"usgs":true,"family":"Pollastro","given":"Richard","email":"","middleInitial":"M.","affiliations":[],"preferred":false,"id":475321,"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":475322,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":70044325,"text":"70044325 - 1989 - Thermal maturity of the Anadarko Basin","interactions":[],"lastModifiedDate":"2013-03-03T09:35:17","indexId":"70044325","displayToPublicDate":"2013-01-01T00:00:00","publicationYear":"1989","noYear":false,"publicationType":{"id":5,"text":"Book chapter"},"publicationSubtype":{"id":24,"text":"Book Chapter"},"seriesNumber":"90","title":"Thermal maturity of the Anadarko Basin","docAbstract":"Levels of thermal maturity are estimated for Paleozoic strata in five areas of the central Anadarko basin for times between the Paleozoic and the present, and depths of the oil window are plotted as a function of geologic time. Mean surface temperature assumed here for calculating Lopatin's time-temperature index of thermal maturity (TTl) in the central Anadarko basin declines from 80°F (27°C) to 60°F (16°C) from early Paleozoic time to the present. Shallow-water carbonates and lower paleolatitudes suggest warmer climates in the Paleozoic for this area. The geothermal gradient is assumed to equal 4.0°F/100 ft (7.3°C/100 m) in the Late Cambrian and to decay over a 100-m.y. period to the present regional gradient of 1.3°F/100 ft (2.4°C/100 m). Initial\nbasin formation was caused by crustal thinning. Accumulation of thick Pennsylvanian sediments in a foreland-style basin dominated by vertical lithospheric flexure represents a second major period of subsidence. An elevated geothermal gradient during this time is not assumed for TTl calculations, because mathematical models suggest time-invariant heat flows in such basins. TTl computations based on these assumptions indicate that oil could have been generated in the ancestral Anadarko basin >350 m.y. ago. By the end of the Pennsylvanian, significant volumes of kerogen were in the oil window (and perhaps beyond), and significant volumes have remained in the oil window up to the present day. These circumstances may partially explain the unusual richness of the Anadarko basin as a Paleozoic hydrocarbon province.","largerWorkType":{"id":18,"text":"Report"},"largerWorkTitle":"Anadarko Basin symposium, 1988 (Circular 90)","largerWorkSubtype":{"id":4,"text":"Other Government Series"},"language":"English","publisher":"Oklahoma Geological Survey","publisherLocation":"Norman, OK","collaboration":"Proceedings of a symposium held April 5-6, 1988, at Norman, Oklahoma; cosponsored by the Oklahoma Geological Survey and the U.S. Geological Survey","usgsCitation":"Schmoker, J.W., 1989, Thermal maturity of the Anadarko Basin, chap. <i>of</i> Anadarko Basin symposium, 1988 (Circular 90), p. 25-31.","productDescription":"7 p.","startPage":"25","endPage":"31","costCenters":[],"links":[{"id":268665,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"},{"id":268664,"type":{"id":11,"text":"Document"},"url":"https://www.ogs.ou.edu/pubsscanned/Circulars/Circular90.pdf"}],"country":"United States","state":"Oklahoma","otherGeospatial":"Anadarko Basin","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -103.0,33.62 ], [ -103.0,37.0 ], [ -94.43,37.0 ], [ -94.43,33.62 ], [ -103.0,33.62 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"51347f0ee4b0e1603e4fec7a","contributors":{"authors":[{"text":"Schmoker, James W.","contributorId":52171,"corporation":false,"usgs":true,"family":"Schmoker","given":"James","email":"","middleInitial":"W.","affiliations":[],"preferred":false,"id":475293,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":70044327,"text":"70044327 - 1989 - Geochemistry of oils and hydrocarbon source rocks, greater Anadarko Basin: evidence for multiple sources of oils and long-distance oil migration","interactions":[],"lastModifiedDate":"2013-03-03T09:30:32","indexId":"70044327","displayToPublicDate":"2013-01-01T00:00:00","publicationYear":"1989","noYear":false,"publicationType":{"id":5,"text":"Book chapter"},"publicationSubtype":{"id":24,"text":"Book Chapter"},"seriesNumber":"90","title":"Geochemistry of oils and hydrocarbon source rocks, greater Anadarko Basin: evidence for multiple sources of oils and long-distance oil migration","docAbstract":"Organic geochemical analyses of 104 crude oils and 190 core samples of dark-colored shales from the greater Anadarko basin show three major oil types which generally correlate with reservoir age and source-rock age. Analyses include C<sub>3</sub>-C<sub>30</sub> whole-oil gas chromatography, C<sub>10+</sub> saturated-hydrocarbon-fraction gas chromatography, and carbon stable isotopes (ppt relative to PDB) of saturated (sat) and aromatic (arom) hydrocarbon fractions. Three samples from Middle Ordovician Simpson Group reservoirs are \"typical\" Ordovician oils (type 1), having strong odd-carbon predominance in the C<sub>13</sub> to C<sub>19</sub> n-alkanes, containing little or no acyclic isoprenoids, an &delta;<sup>13</sup>C values of -33.9 ppt (sat) and -33.7 ppt (arom). Oils from Silurian to Devonian and Mississippian reservoirs (type 2) show little or no odd-carbon predominance in the n-alkanes, a regular decrease in abundance of n-alkanes with increasing carbon number, pristane/phytane ratios (pr/ph) of 1.1 to 1.5, and &delta;<sup>13</sup>C values of -30.6 ppt (sat) and -30.1 ppt (arom). Oils in Pennsylvanian reservoirs (type 3) have the greatest amounts of C<sub>15+</sub> hydrocarbons, are isotopically heavy (-27.5 ppt [sat] and -26.4 ppt [arom]), have methyl-cyclohexane as the most abundant hydrocarbon, and have pr/ph values from 2.0 to 0.9. Oils from the Kansas shelf area of the Anadarko basin are similar to the Anadarko oil types except that they have only traces of toluene and no detectable benzene. The relative abundance of toluene in the C<sub>7</sub> hydrocarbons systematically decreases with distance from the depocenter of the basin. The aromatic compounds are removed by water-washing, and hence could have been lost by contact with progressively greater amounts of formation water during long-distance migration. The lack of thermally mature source rocks in southern and central Kansas supports this hypothesis.","largerWorkType":{"id":18,"text":"Report"},"largerWorkTitle":"Anadarko Basin symposium, 1988 (Circular 90)","largerWorkSubtype":{"id":4,"text":"Other Government Series"},"language":"English","publisher":"Oklahoma Geological Survey","publisherLocation":"Norman, OK","collaboration":"Proceedings of a symposium held April 5-6, 1988, at Norman, Oklahoma; cosponsored by the Oklahoma Geological Survey and the U.S. Geological Survey","usgsCitation":"Burruss, R., and Hatch, J.R., 1989, Geochemistry of oils and hydrocarbon source rocks, greater Anadarko Basin: evidence for multiple sources of oils and long-distance oil migration, chap. <i>of</i> Anadarko Basin symposium, 1988 (Circular 90), p. 53-64.","productDescription":"12 p.","startPage":"53","endPage":"64","costCenters":[],"links":[{"id":268669,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"},{"id":268668,"type":{"id":11,"text":"Document"},"url":"https://www.ogs.ou.edu/pubsscanned/Circulars/Circular90.pdf"}],"country":"United States","state":"Oklahoma","otherGeospatial":"Anadarko Basin","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -103.0,33.62 ], [ -103.0,37.0 ], [ -94.43,37.0 ], [ -94.43,33.62 ], [ -103.0,33.62 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"51347f06e4b0e1603e4fec50","contributors":{"authors":[{"text":"Burruss, R.C. 0000-0001-6827-804X","orcid":"https://orcid.org/0000-0001-6827-804X","contributorId":99574,"corporation":false,"usgs":true,"family":"Burruss","given":"R.C.","affiliations":[],"preferred":false,"id":475298,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Hatch, J. R.","contributorId":14775,"corporation":false,"usgs":true,"family":"Hatch","given":"J.","email":"","middleInitial":"R.","affiliations":[],"preferred":false,"id":475297,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":70046669,"text":"70046669 - 1989 - United States Geological Survey yearbook, fiscal year 1988","interactions":[],"lastModifiedDate":"2017-03-08T16:09:36","indexId":"70046669","displayToPublicDate":"2013-01-01T00:00:00","publicationYear":"1989","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":6,"text":"USGS Unnumbered Series"},"seriesTitle":{"id":392,"text":"Yearbook","active":false,"publicationSubtype":{"id":6}},"title":"United States Geological Survey yearbook, fiscal year 1988","docAbstract":"<p><span>The fiscal year 1988 Yearbook summarizes the activities of the U.S. Geological Survey in response to its scientific and regulatory missions.</span></p>","language":"English","publisher":"U.S. Government Printing Office","doi":"10.3133/70046669","usgsCitation":"Water Resources Division, U.S. Geological Survey, 1989, United States Geological Survey yearbook, fiscal year 1988: Yearbook, iii, 134 p., https://doi.org/10.3133/70046669.","productDescription":"iii, 134 p.","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[],"links":[{"id":309899,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/yb/1988/report.pdf","text":"Report","size":"59.95 MB","linkFileType":{"id":1,"text":"pdf"},"description":"Report"},{"id":274018,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/yb/1988/report-thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"51c42462e4b03c77dce65a69","contributors":{"authors":[{"text":"Water Resources Division, U.S. Geological Survey","contributorId":128075,"corporation":true,"usgs":false,"organization":"Water Resources Division, U.S. Geological Survey","id":535555,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":70044330,"text":"70044330 - 1989 - Horizontal stresses from well-bore breakouts and lithologies associated with their formation, Oklahoma and Texas Panhandle","interactions":[],"lastModifiedDate":"2013-03-03T10:00:00","indexId":"70044330","displayToPublicDate":"2013-01-01T00:00:00","publicationYear":"1989","noYear":false,"publicationType":{"id":5,"text":"Book chapter"},"publicationSubtype":{"id":24,"text":"Book Chapter"},"seriesNumber":"90","title":"Horizontal stresses from well-bore breakouts and lithologies associated with their formation, Oklahoma and Texas Panhandle","docAbstract":"Orientations of crustal stresses are inferred from stress-induced well-bore breakouts in three areas in the south-central United States: the eastern part of the Anadarko basin in central Oklahoma, the Marietta basin in south-central Oklahoma, and the Bravo dome area of the central Texas Panhandle. Inferred directions of maximum horizontal principal stress (SH<sub>max</sub>) are ENE for the eastern Anadarko basin, and NE for the Marietta basin and the Bravo dome area. For the Bravo dome area, the magnitudes of the three principal stresses (S<sub>1</sub>, S<sub>2</sub>, S<sub>3</sub>) are known from existing hydraulic-fracturing (hydrofrac) measurements, and a normal-faulting stress regime (S<sub>V</sub> > SH<sub>max</sub> > SH<sub>min</sub>) is implied. For the eastern Anadarko basin and the Marietta basin, the magnitudes of the principal stresses are not known. Because Quaternary left-lateral oblique slip on the Meers fault in south-central Oklahoma suggests strike-slip (SHmax > Sv > SHmin) and reverse faulting (SH<sub>max</sub> > SH<sub>min</sub> > S<sub>V</sub>), the study region is inferred to be a possible transition zone between areas of extensional and compressional stresses. Breakout data from the eastern Anadarko basin yield a single consistent SH<sub>max</sub> orientation. Data from the Marietta basin and the Bravo dome area have bimodal-orthogonal distributions consisting of breakouts and orthogonal sets of well-bore enlargement orientations. Orthogonal trends in the data are probably related to drilling-induced hydraulic fracturing of the well bore, or to preexisting natural fractures or joint sets intersecting the well bore. On the dipmeter log, breakouts and fracture enlargements have elliptical cross sections of similar size and shape. Orthogonally oriented well-bore enlargements are differentiated by comparing their long-axis orientations with directions of known or inferred horizontal stress. Dispersion, or data scatter, among enlargement orientations (bimodal data sets) increases the standard deviations for many well data sets from the Marietta basin and the Bravo dome area. In these two areas, some dispersion may reflect variation in stress conditions across fault-bounded blocks and the orientations of fractures or joints within these blocks. Although breakouts and fracture enlargements formed in all parts of the thick sequences of sedimentary rocks logged, they occurred primarily in limestone, shale, and dolomitic rocks, reflecting the abundance of these rock types in the study areas.","largerWorkType":{"id":18,"text":"Report"},"largerWorkTitle":"Anadarko Basin symposium, 1988 (Circular 90)","largerWorkSubtype":{"id":4,"text":"Other Government Series"},"language":"English","publisher":"Oklahoma Geological Survey","publisherLocation":"Norman, OK","collaboration":"Proceedings of a symposium held April 5-6, 1988, at Norman, Oklahoma; cosponsored by the Oklahoma Geological Survey and the U.S. Geological Survey","usgsCitation":"Dart, R.L., 1989, Horizontal stresses from well-bore breakouts and lithologies associated with their formation, Oklahoma and Texas Panhandle, chap. <i>of</i> Anadarko Basin symposium, 1988 (Circular 90), p. 97-120.","productDescription":"24 p.","startPage":"97","endPage":"120","costCenters":[],"links":[{"id":268673,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"},{"id":268672,"type":{"id":11,"text":"Document"},"url":"https://www.ogs.ou.edu/pubsscanned/Circulars/Circular90.pdf"}],"country":"United States","state":"Oklahoma;Texas","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -104.0,33.0 ], [ -104.0,38.0 ], [ -94.0,38.0 ], [ -94.0,33.0 ], [ -104.0,33.0 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"51347f07e4b0e1603e4fec54","contributors":{"authors":[{"text":"Dart, Richard L. dart@usgs.gov","contributorId":1209,"corporation":false,"usgs":true,"family":"Dart","given":"Richard","email":"dart@usgs.gov","middleInitial":"L.","affiliations":[],"preferred":true,"id":475300,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":70006517,"text":"70006517 - 1989 - Behavior of fish predators and their prey: Habitat choice between open water and dense vegetation","interactions":[],"lastModifiedDate":"2020-09-01T22:56:17.578049","indexId":"70006517","displayToPublicDate":"2012-07-06T00:00:00","publicationYear":"1989","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1528,"text":"Environmental Biology of Fishes","active":true,"publicationSubtype":{"id":10}},"title":"Behavior of fish predators and their prey: Habitat choice between open water and dense vegetation","docAbstract":"<p><span>Behavior of largemouth bass,&nbsp;</span><i class=\"EmphasisTypeItalic \">Micropterus salmoides</i><span>, and northern pike,&nbsp;</span><i class=\"EmphasisTypeItalic \">Esox lucius</i><span>, foraging on fathead minnows,&nbsp;</span><i class=\"EmphasisTypeItalic \">Pimephales promelas</i><span>, or bluegills,&nbsp;</span><i class=\"EmphasisTypeItalic \">Lepomis macrochirus</i><span>, was quantified in pools with 50% cover (half the pool had artificial stems at a density of 1000 stems m</span><sup><span>&minus;2</span></sup><span>). Both predators spent most of their time in the vegetation. Largemouth bass searched for bluegills and ambushed minnows, whereas the relatively immobile northern pike ambushed all prey. Minnows were closer to predators and were captured more frequently than bluegills. Even when minnows dispersed, they moved continually and eventually wandered within striking distance of a predator. Bluegills dispersed in the cover with predators. Bass captured the few bluegills that strayed into the open and pike captured those that approached too closely in the cover. The ability of predators to capture prey while residing in habitats containing patches of dense cover may explain their residence in areas often considered to be poor ones for foraging.</span></p>","language":"English","publisher":"Springer","doi":"10.1007/BF00001402","usgsCitation":"Savino, J.F., and Stein, R., 1989, Behavior of fish predators and their prey: Habitat choice between open water and dense vegetation: Environmental Biology of Fishes, v. 24, no. 4, p. 287-293, https://doi.org/10.1007/BF00001402.","productDescription":"7 p.","startPage":"287","endPage":"293","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[{"id":324,"text":"Great Lakes Science Center","active":true,"usgs":true}],"links":[{"id":479862,"rank":2,"type":{"id":41,"text":"Open Access External Repository Page"},"url":"http://hdl.handle.net/1811/37301","text":"External Repository"},{"id":259084,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United States","volume":"24","issue":"4","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"5059f09fe4b0c8380cd4a802","contributors":{"authors":[{"text":"Savino, Jacqueline F. jsavino@usgs.gov","contributorId":2213,"corporation":false,"usgs":true,"family":"Savino","given":"Jacqueline","email":"jsavino@usgs.gov","middleInitial":"F.","affiliations":[{"id":324,"text":"Great Lakes Science Center","active":true,"usgs":true}],"preferred":true,"id":354660,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Stein, Roy A.","contributorId":21494,"corporation":false,"usgs":true,"family":"Stein","given":"Roy A.","affiliations":[],"preferred":false,"id":354661,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":70006740,"text":"70006740 - 1989 - Avian botulism: geographic expansion of a historic disease","interactions":[],"lastModifiedDate":"2018-03-23T16:24:33","indexId":"70006740","displayToPublicDate":"2012-02-17T00:00:00","publicationYear":"1989","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":1,"text":"Federal Government Series"},"seriesTitle":{"id":24,"text":"Fish and Wildlife Leaflet","active":false,"publicationSubtype":{"id":1}},"seriesNumber":"13.2.4","title":"Avian botulism: geographic expansion of a historic disease","docAbstract":"<p>Avian botulism is a paralytic, often fatal disease of birds resulting from ingestion of toxin produced by the bacterium Clostridium botulinum. Waterfowl die-offs from the botulism are usually caused by type C toxin; sporadic die-offs among fish-eating birds, such as common loons (Gavia immer) and gulls, have been caused by type E toxin.</p>","largerWorkType":{"id":18,"text":"Report"},"largerWorkTitle":"Waterfowl Management Handbook","largerWorkSubtype":{"id":1,"text":"Federal Government Series"},"language":"English","publisher":"U.S. Fish and Wildlife Service","publisherLocation":"Washington, DC","usgsCitation":"Locke, L.N., and Friend, M., 1989, Avian botulism: geographic expansion of a historic disease: Fish and Wildlife Leaflet 13.2.4, 6 p.","productDescription":"6 p.","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[{"id":456,"text":"National Wildlife Health Center","active":true,"usgs":true}],"links":[{"id":204598,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"},{"id":115812,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://archive.usgs.gov/archive/sites/www.nwrc.usgs.gov/wdb/pub/wmh/13_2_4.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"5059ef5ce4b0c8380cd4a1f0","contributors":{"authors":[{"text":"Locke, Louis N.","contributorId":71233,"corporation":false,"usgs":true,"family":"Locke","given":"Louis","email":"","middleInitial":"N.","affiliations":[],"preferred":false,"id":355114,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Friend, Milton 0000-0002-2882-3629","orcid":"https://orcid.org/0000-0002-2882-3629","contributorId":31332,"corporation":false,"usgs":true,"family":"Friend","given":"Milton","email":"","affiliations":[{"id":456,"text":"National Wildlife Health Center","active":true,"usgs":true}],"preferred":true,"id":355115,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":70039577,"text":"70039577 - 1989 - Resident research associateships, postdoctoral research awards 1989: opportunities for research at the U.S. Geological Survey, U.S. Department of the Interior","interactions":[],"lastModifiedDate":"2012-08-14T01:01:44","indexId":"70039577","displayToPublicDate":"2012-01-01T21:10:00","publicationYear":"1989","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":6,"text":"USGS Unnumbered Series"},"seriesTitle":{"id":371,"text":"Monograph","active":false,"publicationSubtype":{"id":6}},"title":"Resident research associateships, postdoctoral research awards 1989: opportunities for research at the U.S. Geological Survey, U.S. Department of the Interior","docAbstract":"The scientists of the U.S. Geological Survey are engaged in a wide range of geologic, geophysical, geochemical, hydrologic, and cartographic programs, including the application of computer science to them. These programs offer exciting possibilities for scientific achievement and professional growth to young scientists through participation as Research Associates.","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Reston, VA","doi":"10.3133/70039577","usgsCitation":"Water Resources Division, U.S. Geological Survey, and U.S. National Research Council, 1989, Resident research associateships, postdoctoral research awards 1989: opportunities for research at the U.S. Geological Survey, U.S. Department of the Interior: Monograph, v, 122 p., https://doi.org/10.3133/70039577.","productDescription":"v, 122 p.","numberOfPages":"130","costCenters":[],"links":[{"id":259585,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"505aa97be4b0c8380cd85e0e","contributors":{"authors":[{"text":"Water Resources Division, U.S. Geological Survey","contributorId":128075,"corporation":true,"usgs":false,"organization":"Water Resources Division, U.S. Geological Survey","id":535373,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"U.S. National Research Council","contributorId":128227,"corporation":true,"usgs":false,"organization":"U.S. National Research Council","id":535374,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":70006866,"text":"70006866 - 1989 - Comparison of fish catches with buoyant pop nets and seines in vegetated and nonvegetated habitats","interactions":[],"lastModifiedDate":"2012-08-24T01:02:05","indexId":"70006866","displayToPublicDate":"2012-01-01T16:15:00","publicationYear":"1989","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":2886,"text":"North American Journal of Fisheries Management","active":true,"publicationSubtype":{"id":10}},"title":"Comparison of fish catches with buoyant pop nets and seines in vegetated and nonvegetated habitats","docAbstract":"Two models of pop nets were developed to sample fish in shallow riverine waters, one for use in vegetated areas and the other for nonvegetated areas. Both nets have a mechanical release mechanism that can be tripped from the water surface. Replicated field tests were conducted to compare pop-net catches with bag-seine collections every 2 weeks from May through mid-October. Overall, total catch per effort did not vary significantly (<i>P</i> < 0.05) between the two gears at either the vegetated or nonvegetated site. However, collections with the pop net were not as diverse as with the seine at either sampling site, perhaps because the area sampled by pop nets (5.6 m<sup>2</sup>) was smaller than the area swept by the average seine haul (70-140 m<sup>2</sup>). The pop net effectively sampled fish in shallow nonvegetated habitats and was useful in heavily vegetated areas where seining or electroshocking was difficult.","largerWorkType":{"id":2,"text":"Article"},"largerWorkTitle":"North American Journal of Fisheries Management","largerWorkSubtype":{"id":10,"text":"Journal Article"},"language":"English","publisher":"Taylor & Francis","publisherLocation":"Philadelphia, PA","doi":"10.1577/1548-8675(1989)009<0249:COFCWB>2.3.CO;2","collaboration":"Abstract has subscript/superscript to be fixed","usgsCitation":"Dewey, M.R., Holland-Bartels, L., and Zigler, S.J., 1989, Comparison of fish catches with buoyant pop nets and seines in vegetated and nonvegetated habitats: North American Journal of Fisheries Management, v. 9, no. 2, p. 249-253, https://doi.org/10.1577/1548-8675(1989)009<0249:COFCWB>2.3.CO;2.","productDescription":"5 p.","startPage":"249","endPage":"253","numberOfPages":"5","costCenters":[{"id":606,"text":"Upper Midwest Environmental Sciences Center","active":true,"usgs":true}],"links":[{"id":259816,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"},{"id":259804,"rank":9999,"type":{"id":10,"text":"Digital Object Identifier"},"url":"https://dx.doi.org/10.1577/1548-8675(1989)009<0249:COFCWB>2.3.CO;2","linkFileType":{"id":5,"text":"html"}}],"volume":"9","issue":"2","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"5059f863e4b0c8380cd4d081","contributors":{"authors":[{"text":"Dewey, M. R.","contributorId":48908,"corporation":false,"usgs":true,"family":"Dewey","given":"M.","email":"","middleInitial":"R.","affiliations":[],"preferred":false,"id":355379,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Holland-Bartels, L. E.","contributorId":53221,"corporation":false,"usgs":true,"family":"Holland-Bartels","given":"L. E.","affiliations":[],"preferred":false,"id":355380,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Zigler, S. J.","contributorId":21513,"corporation":false,"usgs":true,"family":"Zigler","given":"S.","email":"","middleInitial":"J.","affiliations":[],"preferred":false,"id":355378,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":70007005,"text":"70007005 - 1989 - Commercial diets for lake trout fry","interactions":[],"lastModifiedDate":"2012-07-17T01:01:41","indexId":"70007005","displayToPublicDate":"2012-01-01T15:48:00","publicationYear":"1989","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":3330,"text":"Salmonid","active":true,"publicationSubtype":{"id":10}},"title":"Commercial diets for lake trout fry","docAbstract":"No abstract available at this time.","largerWorkType":{"id":2,"text":"Article"},"largerWorkTitle":"Salmonid","largerWorkSubtype":{"id":10,"text":"Journal Article"},"language":"English","publisher":"United States Trout Farmers Association","publisherLocation":"Pine Bluff, AR","collaboration":"None","usgsCitation":"Ketola, H.G., Zitzow, R., and Edsall, D., 1989, Commercial diets for lake trout fry: Salmonid, v. 13, no. 1, p. 12-14.","productDescription":"3 p.","startPage":"12","endPage":"14","numberOfPages":"1","costCenters":[{"id":365,"text":"Leetown Science Center","active":true,"usgs":true}],"links":[{"id":258939,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"},{"id":258928,"rank":100,"type":{"id":15,"text":"Index Page"},"url":"https://www.ustfa.org/salmonid/salmonidindex.html#1989","linkFileType":{"id":5,"text":"html"}}],"volume":"13","issue":"1","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"5059f7f8e4b0c8380cd4cde8","contributors":{"authors":[{"text":"Ketola, H. G.","contributorId":60976,"corporation":false,"usgs":true,"family":"Ketola","given":"H.","middleInitial":"G.","affiliations":[],"preferred":false,"id":355639,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Zitzow, R.","contributorId":103133,"corporation":false,"usgs":true,"family":"Zitzow","given":"R.","email":"","affiliations":[],"preferred":false,"id":355641,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Edsall, D.","contributorId":96137,"corporation":false,"usgs":true,"family":"Edsall","given":"D.","email":"","affiliations":[],"preferred":false,"id":355640,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":70038761,"text":"70038761 - 1989 - Borax in the supraglacial moraine of the Lewis Cliff, Buckley Island quadrangle--first Antarctic occurrence","interactions":[],"lastModifiedDate":"2012-06-20T01:01:36","indexId":"70038761","displayToPublicDate":"2012-01-01T15:23:00","publicationYear":"1989","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":812,"text":"Antarctic Journal of the United States","active":true,"publicationSubtype":{"id":10}},"title":"Borax in the supraglacial moraine of the Lewis Cliff, Buckley Island quadrangle--first Antarctic occurrence","docAbstract":"During the 1987-1988 austral summer field season, membersof the south party of the antarctic search for meteorites south-ern team* working in the Lewis Cliff/Colbert Hills region dis-covered several areas of unusual mineralization within theLewis Cliff ice tongue and its associated moraine field (figure1). The Lewis Cliff ice tongue (84&deg;15'S 161&deg;25'E) is a meteorite-stranding surface of ablating blue ice, about 2.3 by 7.0 kilo-meters, bounded on the west by the Lewis Cliff, on the northand northeast by a large supraglacial moraine, and on the eastby the Colbert Hills. To the south it opens to the Walcott N&eacute;v&eacute;.Because it is a meteorite-stranding surface, the major component of ice motion in the area is believed to be vertical(Whillans and Cassidy 1983). The presence of Thule-Baffinmoraines at the northern terminus of the blue ice tends tosupport the hypothesis that the area underlying the moraineis essentially stagnant and that ice arriving from the south ispiling up against it. Areas containing mineral deposits werefound within the moraine field to the north and east of theblue ice margin and also along the east margins of the blue iceitself. Subsequent X-ray diffraction analyses of these depositshave shown that they are composed predominantly of nah-colite (NaHCO<sub>3</sub>), trona [Na<sub>3</sub>(CO<sub>3</sub>)(HCO<sub>3</sub>) &middot; 2H<sub>2</sub>0], borax[Na<sub>2</sub>B<sub>4</sub>0<sub>5</sub>(OH)<sub>4</sub> &middot; 8H<sub>2</sub>0], and a new hexagonal hydrous sulfatespecies. This paper reports the details of the borax occurrence,because it is the first known on the continent.","largerWorkType":{"id":2,"text":"Article"},"largerWorkTitle":"Antarctic Journal of the United States","largerWorkSubtype":{"id":10,"text":"Journal Article"},"language":"English","publisher":"National Science Foundation, Office of Polar Programs","publisherLocation":"Washington, D.C.","usgsCitation":"Fitzpatrick, J.J., and Muhs, D., 1989, Borax in the supraglacial moraine of the Lewis Cliff, Buckley Island quadrangle--first Antarctic occurrence: Antarctic Journal of the United States, v. 24, no. 5, p. 63-65.","productDescription":"3 p.","startPage":"63","endPage":"65","costCenters":[{"id":308,"text":"Geology and Environmental Change Science Center","active":false,"usgs":true}],"links":[{"id":257720,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"},{"id":257696,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://s3.amazonaws.com/Antarctica/AJUS/AJUSvXXIVn5/AJUSvXXIVn5p63.pdf","linkFileType":{"id":1,"text":"pdf"}}],"otherGeospatial":"Lewis Cliff;Buckley Island;Antarctica","volume":"24","issue":"5","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"5059f211e4b0c8380cd4afbc","contributors":{"authors":[{"text":"Fitzpatrick, J. J.","contributorId":95078,"corporation":false,"usgs":true,"family":"Fitzpatrick","given":"J.","email":"","middleInitial":"J.","affiliations":[],"preferred":false,"id":464883,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Muhs, D.R. 0000-0001-7449-251X","orcid":"https://orcid.org/0000-0001-7449-251X","contributorId":61460,"corporation":false,"usgs":true,"family":"Muhs","given":"D.R.","affiliations":[],"preferred":false,"id":464882,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":70038760,"text":"70038760 - 1989 - Uranium-series ages, faunal correlations and tectonic deformation of marine terraces within the Agua Blanca fault zone at Punta Banda, northern Baja California, Mexico","interactions":[],"lastModifiedDate":"2012-06-20T01:01:36","indexId":"70038760","displayToPublicDate":"2012-01-01T15:12:42","publicationYear":"1989","noYear":false,"publicationType":{"id":5,"text":"Book chapter"},"publicationSubtype":{"id":24,"text":"Book Chapter"},"title":"Uranium-series ages, faunal correlations and tectonic deformation of marine terraces within the Agua Blanca fault zone at Punta Banda, northern Baja California, Mexico","largerWorkType":{"id":4,"text":"Book"},"largerWorkTitle":"Geologic Studies in Baja California: Book 63","largerWorkSubtype":{"id":4,"text":"Other Government Series"},"language":"English","usgsCitation":"Rockwell, T.K., Muhs, D., Kennedy, G.L., Hatch, M., Wilson, S., and Klinger, R., 1989, Uranium-series ages, faunal correlations and tectonic deformation of marine terraces within the Agua Blanca fault zone at Punta Banda, northern Baja California, Mexico, chap. <i>of</i> Geologic Studies in Baja California: Book 63, p. 1-16.","productDescription":"16 p.","startPage":"1","endPage":"16","costCenters":[{"id":308,"text":"Geology and Environmental Change Science Center","active":false,"usgs":true}],"links":[{"id":257716,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"Mexico","state":"Baja California","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"505bbdf1e4b08c986b32930d","contributors":{"editors":[{"text":"Abbott, P. L.","contributorId":14115,"corporation":false,"usgs":true,"family":"Abbott","given":"P.","email":"","middleInitial":"L.","affiliations":[],"preferred":false,"id":508991,"contributorType":{"id":2,"text":"Editors"},"rank":1}],"authors":[{"text":"Rockwell, T. K.","contributorId":34688,"corporation":false,"usgs":false,"family":"Rockwell","given":"T.","email":"","middleInitial":"K.","affiliations":[],"preferred":false,"id":464878,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Muhs, D.R. 0000-0001-7449-251X","orcid":"https://orcid.org/0000-0001-7449-251X","contributorId":61460,"corporation":false,"usgs":true,"family":"Muhs","given":"D.R.","affiliations":[],"preferred":false,"id":464880,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Kennedy, G. L.","contributorId":23944,"corporation":false,"usgs":true,"family":"Kennedy","given":"G.","email":"","middleInitial":"L.","affiliations":[],"preferred":false,"id":464877,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Hatch, M.E.","contributorId":64495,"corporation":false,"usgs":true,"family":"Hatch","given":"M.E.","email":"","affiliations":[],"preferred":false,"id":464881,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"Wilson, S.M.","contributorId":52731,"corporation":false,"usgs":true,"family":"Wilson","given":"S.M.","email":"","affiliations":[],"preferred":false,"id":464879,"contributorType":{"id":1,"text":"Authors"},"rank":5},{"text":"Klinger, R.E.","contributorId":13807,"corporation":false,"usgs":true,"family":"Klinger","given":"R.E.","email":"","affiliations":[],"preferred":false,"id":464876,"contributorType":{"id":1,"text":"Authors"},"rank":6}]}}
,{"id":70006752,"text":"70006752 - 1989 - Stress in lake trout reared in gas supersaturation can be measured by immune response","interactions":[],"lastModifiedDate":"2012-08-25T01:02:00","indexId":"70006752","displayToPublicDate":"2012-01-01T15:00:00","publicationYear":"1989","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1649,"text":"Fish Health Section Newsletter","active":true,"publicationSubtype":{"id":10}},"title":"Stress in lake trout reared in gas supersaturation can be measured by immune response","largerWorkType":{"id":2,"text":"Article"},"largerWorkTitle":"Fish Health Section Newsletter","largerWorkSubtype":{"id":10,"text":"Journal Article"},"language":"English","publisher":"American Fisheries Society","publisherLocation":"Bethesda, MD","collaboration":"None","usgsCitation":"Krise, W.F., 1989, Stress in lake trout reared in gas supersaturation can be measured by immune response: Fish Health Section Newsletter, v. 17, no. 1, p. 6-6.","productDescription":"1 p.","startPage":"6","endPage":"6","numberOfPages":"1","costCenters":[{"id":365,"text":"Leetown Science Center","active":true,"usgs":true}],"links":[{"id":259913,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"17","issue":"1","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"505b9b5be4b08c986b31ce10","contributors":{"authors":[{"text":"Krise, W. F.","contributorId":50842,"corporation":false,"usgs":true,"family":"Krise","given":"W.","middleInitial":"F.","affiliations":[],"preferred":false,"id":355144,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":70006501,"text":"70006501 - 1989 - Reversed-phase high-performance liquid chromatography of unsubstituted aminobenzoic acids","interactions":[],"lastModifiedDate":"2012-08-25T01:02:00","indexId":"70006501","displayToPublicDate":"2012-01-01T14:55:00","publicationYear":"1989","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":2370,"text":"Journal of Liquid Chromatography","active":true,"publicationSubtype":{"id":10}},"title":"Reversed-phase high-performance liquid chromatography of unsubstituted aminobenzoic acids","docAbstract":"High-performance liquid chromatographic (HPLC) characteristics of three position isomers of aminobenzoic acids (potential metabolites of important anesthetic drugs), were delineated with respect to their interactions with various mobile phases and stationary phases. HPLC with five hydrocarbonaceous phase, I?-cyclodextrin silica (CDS), macrophase MP-1 polymer (MP), macroporous polystyrene/divinylbenzene (MPD), octadecylsilica (ODS), and propylphenylsilica (PPS), yielded results explicable in terms of substituent effects derived from the bifunctional amino- and carboxy groups. For cases where mobile phases contained sulfonates or quaternary ammonium salts both having longer chain alkyls, retention of analytes on all but CDS appeared to proceed predominantly via an ion-pairing mechanism. The extent of the corresponding counter-ion effects decreased in the order: MPD > ODS > PPS > MP, while the analyte retention order paralleled thier pH<sub>2</sub> values. On the other hand, an inverse relationship between the magnitude of capacity factors (k') and pK<sub>1</sub> values of the title compounds was observed in experiments that produced retention data incompatible with ion-pair interaction rationales. The unique HPLC results obtained with the CDS phase are compared with those obtained with other phases.","largerWorkType":{"id":2,"text":"Article"},"largerWorkTitle":"Journal of Liquid Chromatography","largerWorkSubtype":{"id":10,"text":"Journal Article"},"language":"English","publisher":"Taylor & Francis","publisherLocation":"Philadelphia, PA","doi":"10.1080/01483918908051761","collaboration":"Abstract has subscript/superscript to be fixed","usgsCitation":"Abidi, S.L., 1989, Reversed-phase high-performance liquid chromatography of unsubstituted aminobenzoic acids: Journal of Liquid Chromatography, v. 12, no. 4, p. 595-611, https://doi.org/10.1080/01483918908051761.","productDescription":"17 p.","startPage":"595","endPage":"611","numberOfPages":"17","costCenters":[{"id":606,"text":"Upper Midwest Environmental Sciences Center","active":true,"usgs":true}],"links":[{"id":259909,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"},{"id":259894,"rank":9999,"type":{"id":10,"text":"Digital Object Identifier"},"url":"https://dx.doi.org/10.1080/01483918908051761","linkFileType":{"id":5,"text":"html"}}],"volume":"12","issue":"4","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"505aac39e4b0c8380cd86c0d","contributors":{"authors":[{"text":"Abidi, S. L.","contributorId":19898,"corporation":false,"usgs":true,"family":"Abidi","given":"S.","email":"","middleInitial":"L.","affiliations":[],"preferred":false,"id":354634,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":70039068,"text":"70039068 - 1989 - Earthquakes & Volcanoes, Volume 21, Number 1, 1989: Featuring the U.S. Geological Survey's National Earthquake Information Center in Golden, Colorado, USA","interactions":[],"lastModifiedDate":"2017-05-22T11:26:50","indexId":"70039068","displayToPublicDate":"2012-01-01T14:27:00","publicationYear":"1989","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":6,"text":"USGS Unnumbered Series"},"title":"Earthquakes & Volcanoes, Volume 21, Number 1, 1989: Featuring the U.S. Geological Survey's National Earthquake Information Center in Golden, Colorado, USA","docAbstract":"Earthquakes and Volcanoes is published bimonthly by the U.S. Geological Survey to provide current information on earthquakes and seismology, volcanoes, and related natural hazards of interest to both generalized and specialized readers. The Secretary of the Interior has determined that the publication of this periodical is necessary in the transaction of the public business required by law of this Department. Use of funds for printing this periodical has been approved by the Office of Management and Budget through June 30, 1989. Any use of trade, product, or firm names is for descriptive purposes only and does not imply endorsement by the U.S. Government.","language":"English","publisher":"U.S. Government Printing Office","publisherLocation":"Washington, D.C.","doi":"10.3133/70039068","usgsCitation":"Water Resources Division, U.S. Geological Survey, Spall, H., and Schnabel, D.C., 1989, Earthquakes & Volcanoes, Volume 21, Number 1, 1989: Featuring the U.S. Geological Survey's National Earthquake Information Center in Golden, Colorado, USA, 63 p., https://doi.org/10.3133/70039068.","productDescription":"63 p.","numberOfPages":"64","costCenters":[{"id":415,"text":"National Earthquake Information Center","active":false,"usgs":true}],"links":[{"id":261289,"rank":800,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/unnumbered/70039068/report.pdf"},{"id":261290,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/unnumbered/70039068/report-thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"505a050de4b0c8380cd50c37","contributors":{"authors":[{"text":"Water Resources Division, U.S. Geological Survey","contributorId":128075,"corporation":true,"usgs":false,"organization":"Water Resources Division, U.S. Geological Survey","id":535212,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Spall, Henry","contributorId":77933,"corporation":false,"usgs":true,"family":"Spall","given":"Henry","email":"","affiliations":[],"preferred":false,"id":465561,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Schnabel, Diane C.","contributorId":94538,"corporation":false,"usgs":true,"family":"Schnabel","given":"Diane","email":"","middleInitial":"C.","affiliations":[],"preferred":false,"id":465562,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":70006784,"text":"70006784 - 1989 - Survival of Florida Bay fish tagged with internally anchored Spaghetti tags","interactions":[],"lastModifiedDate":"2012-08-16T01:02:05","indexId":"70006784","displayToPublicDate":"2012-01-01T11:54:42","publicationYear":"1989","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1106,"text":"Bulletin of Marine Science","active":true,"publicationSubtype":{"id":10}},"title":"Survival of Florida Bay fish tagged with internally anchored Spaghetti tags","largerWorkType":{"id":2,"text":"Article"},"largerWorkTitle":"Bulletin of Marine Science","largerWorkSubtype":{"id":10,"text":"Journal Article"},"language":"English","publisher":"University of Miami","publisherLocation":"Miami, FL","collaboration":"None","usgsCitation":"Ludwig, G., Skjeveland, J., Funicelli, N., Bryant, H., Meineke, D., Mengel, L., and Dewey, M.R., 1989, Survival of Florida Bay fish tagged with internally anchored Spaghetti tags: Bulletin of Marine Science, v. 44, no. 1, p. 518-518.","productDescription":"1 p.","startPage":"518","endPage":"518","numberOfPages":"1","costCenters":[{"id":365,"text":"Leetown Science Center","active":true,"usgs":true}],"links":[{"id":259630,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United States","state":"Florida","otherGeospatial":"Florida Bay","volume":"44","issue":"1","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"505ba2c2e4b08c986b31f93b","contributors":{"authors":[{"text":"Ludwig, G.M.","contributorId":70721,"corporation":false,"usgs":true,"family":"Ludwig","given":"G.M.","email":"","affiliations":[],"preferred":false,"id":355218,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Skjeveland, J.E.","contributorId":80224,"corporation":false,"usgs":true,"family":"Skjeveland","given":"J.E.","email":"","affiliations":[],"preferred":false,"id":355220,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Funicelli, N.A.","contributorId":13573,"corporation":false,"usgs":true,"family":"Funicelli","given":"N.A.","email":"","affiliations":[],"preferred":false,"id":355214,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Bryant, H.E.","contributorId":77092,"corporation":false,"usgs":true,"family":"Bryant","given":"H.E.","email":"","affiliations":[],"preferred":false,"id":355219,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"Meineke, D.A.","contributorId":30178,"corporation":false,"usgs":true,"family":"Meineke","given":"D.A.","email":"","affiliations":[],"preferred":false,"id":355215,"contributorType":{"id":1,"text":"Authors"},"rank":5},{"text":"Mengel, L.J.","contributorId":54141,"corporation":false,"usgs":true,"family":"Mengel","given":"L.J.","email":"","affiliations":[],"preferred":false,"id":355217,"contributorType":{"id":1,"text":"Authors"},"rank":6},{"text":"Dewey, M. R.","contributorId":48908,"corporation":false,"usgs":true,"family":"Dewey","given":"M.","email":"","middleInitial":"R.","affiliations":[],"preferred":false,"id":355216,"contributorType":{"id":1,"text":"Authors"},"rank":7}]}}
,{"id":70006774,"text":"70006774 - 1989 - Uniformity of Edwardsiella ictaluri isolates is corroborated by genetic analysis","interactions":[],"lastModifiedDate":"2012-08-18T01:01:45","indexId":"70006774","displayToPublicDate":"2012-01-01T11:39:45","publicationYear":"1989","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1649,"text":"Fish Health Section Newsletter","active":true,"publicationSubtype":{"id":10}},"title":"Uniformity of Edwardsiella ictaluri isolates is corroborated by genetic analysis","largerWorkType":{"id":2,"text":"Article"},"largerWorkTitle":"Fish Health Section Newsletter","largerWorkSubtype":{"id":10,"text":"Journal Article"},"language":"English","publisher":"American Fisheries Society","publisherLocation":"Bethesda, MD","collaboration":"None","usgsCitation":"Starliper, C.E., and Schill, W.B., 1989, Uniformity of Edwardsiella ictaluri isolates is corroborated by genetic analysis: Fish Health Section Newsletter, v. 17, no. 1, p. 4-4.","productDescription":"1 p.","startPage":"4","endPage":"4","numberOfPages":"1","costCenters":[{"id":365,"text":"Leetown Science Center","active":true,"usgs":true}],"links":[{"id":259711,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"17","issue":"1","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"505bbc82e4b08c986b328c84","contributors":{"authors":[{"text":"Starliper, C. E.","contributorId":59739,"corporation":false,"usgs":true,"family":"Starliper","given":"C.","middleInitial":"E.","affiliations":[],"preferred":false,"id":355191,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Schill, W. B.","contributorId":60146,"corporation":false,"usgs":true,"family":"Schill","given":"W.","email":"","middleInitial":"B.","affiliations":[],"preferred":false,"id":355192,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":1439,"text":"1439 - 1989 - Cartography at the U.S. Geological Survey: the National Mapping Division's cartographic programs, products, design, and technology","interactions":[],"lastModifiedDate":"2018-02-12T11:18:24","indexId":"1439","displayToPublicDate":"2012-01-01T11:04:00","publicationYear":"1989","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":6,"text":"USGS Unnumbered Series"},"seriesTitle":{"id":362,"text":"General Information Product","active":false,"publicationSubtype":{"id":6}},"title":"Cartography at the U.S. Geological Survey: the National Mapping Division's cartographic programs, products, design, and technology","docAbstract":"<p>The U.S. Geological Survey (USGS) is the prime source of many kinds of topographic and special-purpose maps of the United States and its outlying areas. It is also a prime source of digital map data.</p><p>One main goal of the USGS is to provide large-scale topographic map coverage of the entire United States. Most of the Nation is already covered. We expect that initial coverage will be completed by 1991.</p><p>For many purposes, many public agencies, private organizations, and individuals need reliable cartographic and geographic knowledge about our Nation. To serve such needs, all USGS maps are compiled to exacting standards of accuracy and content.</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/1439","usgsCitation":"Ogrosky, C.E., Gwynn, W., and Jannace, R., 1989, Cartography at the U.S. Geological Survey: the National Mapping Division's cartographic programs, products, design, and technology: General Information Product, 26 p., https://doi.org/10.3133/1439.","productDescription":"26 p.","numberOfPages":"30","costCenters":[{"id":429,"text":"National Mapping Division","active":false,"usgs":true}],"links":[{"id":260254,"rank":800,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/gip/1439/report.pdf"},{"id":260255,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/gip/1439/report-thumb.jpg"}],"publicComments":"Originally prepared for the 1987 U.S. National Report to the International Cartographic Association","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"5059f384e4b0c8380cd4b861","contributors":{"authors":[{"text":"Ogrosky, Charles E.","contributorId":28477,"corporation":false,"usgs":true,"family":"Ogrosky","given":"Charles","email":"","middleInitial":"E.","affiliations":[],"preferred":false,"id":143731,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Gwynn, William","contributorId":74625,"corporation":false,"usgs":true,"family":"Gwynn","given":"William","email":"","affiliations":[],"preferred":false,"id":143733,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Jannace, Richard","contributorId":28855,"corporation":false,"usgs":true,"family":"Jannace","given":"Richard","email":"","affiliations":[],"preferred":false,"id":143732,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
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