{"pageNumber":"5375","pageRowStart":"134350","pageSize":"25","recordCount":184769,"records":[{"id":70011440,"text":"70011440 - 1982 - Introduction: seismology and earthquake engineering in Mexico and Central and South America.","interactions":[],"lastModifiedDate":"2012-03-12T17:18:30","indexId":"70011440","displayToPublicDate":"1982-01-01T00:00:00","publicationYear":"1982","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1435,"text":"Earthquake Information Bulletin (USGS)","active":true,"publicationSubtype":{"id":10}},"title":"Introduction: seismology and earthquake engineering in Mexico and Central and South America.","docAbstract":"The results from seismological studies that are used by the engineering community are just one of the benefits obtained from research aimed at mitigating the earthquake hazard. In this issue of Earthquake Information Bulletin current programs in seismology and earthquake engineering, seismic networks, future plans and some of the cooperative programs with different internation organizations are described by Latin-American seismologists. The article describes the development of seismology in Latin America and the seismological interest of the OAS. -P.N.Chroston","largerWorkType":{"id":2,"text":"Article"},"largerWorkTitle":"Earthquake Information Bulletin (USGS)","largerWorkSubtype":{"id":10,"text":"Journal Article"},"language":"English","usgsCitation":"Espinosa, A.F., 1982, Introduction: seismology and earthquake engineering in Mexico and Central and South America.: Earthquake Information Bulletin (USGS), v. 14, no. 1, p. 4-6.","startPage":"4","endPage":"6","numberOfPages":"3","costCenters":[],"links":[{"id":221289,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"14","issue":"1","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"505a3e0ee4b0c8380cd63a7f","contributors":{"authors":[{"text":"Espinosa, A. F.","contributorId":63782,"corporation":false,"usgs":true,"family":"Espinosa","given":"A.","email":"","middleInitial":"F.","affiliations":[],"preferred":false,"id":361101,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":70011438,"text":"70011438 - 1982 - Sedimentation of lithogenic particles in the deep ocean","interactions":[],"lastModifiedDate":"2018-04-09T13:07:32","indexId":"70011438","displayToPublicDate":"1982-01-01T00:00:00","publicationYear":"1982","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":2667,"text":"Marine Geology","active":true,"publicationSubtype":{"id":10}},"title":"Sedimentation of lithogenic particles in the deep ocean","docAbstract":"<p>Investigation of lithogenic particles collected by sediment traps in open-ocean stations revealed that the sediment flux increased linearly with depth in the water column. This rate of increase decreased with distance of the station from the continent; it was largest at the Panama Basin station and almost negligible at the E. Hawaii Abyssal Plain station. At the Panama Basin station, smectite flux increased with depth. We suggest that smectite resuspended from bottom sediments of the continental slope west of the sediment-trap station is advected by easterly deep currents, and the suspended particles are then possibly entrapped by large settling particles. On the other hand, the flux of hemipelagic clay particles, kaolinite and chlorite, was nearly constant at all depths; this can be explained by incorporation of these particles in fecal pellets which then settle from the surface water. At the Demerara Abyssal Basin Station, flux of illite and chlorite particles increased with depth and the flux of smectite was constant. A sudden increase of the flux of illite and chlorite was observed near the bottom traps at the So??hm Abyssal Plain station. The flux of quartz and feldspar was 10 to 15% of the clay flux.&nbsp;</p>","largerWorkType":{"id":2,"text":"Article"},"largerWorkTitle":"Marine Geology","largerWorkSubtype":{"id":10,"text":"Journal Article"},"language":"English","doi":"10.1016/0025-3227(82)90139-6","issn":"00253227","usgsCitation":"Honjo, S., Manganini, S., and Poppe, L., 1982, Sedimentation of lithogenic particles in the deep ocean: Marine Geology, v. 50, no. 3, p. 199-220, https://doi.org/10.1016/0025-3227(82)90139-6.","productDescription":"22 p.","startPage":"199","endPage":"220","costCenters":[{"id":678,"text":"Woods Hole Coastal and Marine Science Center","active":true,"usgs":true}],"links":[{"id":221238,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"50","issue":"3","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"505b8a71e4b08c986b3171c5","contributors":{"authors":[{"text":"Honjo, S.","contributorId":97227,"corporation":false,"usgs":true,"family":"Honjo","given":"S.","email":"","affiliations":[],"preferred":false,"id":361099,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Manganini, S.J.","contributorId":80417,"corporation":false,"usgs":true,"family":"Manganini","given":"S.J.","email":"","affiliations":[],"preferred":false,"id":361098,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Poppe, L.J.","contributorId":72782,"corporation":false,"usgs":true,"family":"Poppe","given":"L.J.","affiliations":[],"preferred":false,"id":361097,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":70010391,"text":"70010391 - 1982 - Stability studies of surficial sediments in the Wilmington-Lindenkohl Canyons area, eastern U.S. margin","interactions":[],"lastModifiedDate":"2012-03-12T17:18:25","indexId":"70010391","displayToPublicDate":"1982-01-01T00:00:00","publicationYear":"1982","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1742,"text":"Geo-Marine Letters","active":true,"publicationSubtype":{"id":10}},"title":"Stability studies of surficial sediments in the Wilmington-Lindenkohl Canyons area, eastern U.S. margin","docAbstract":"Stability analysis, based on infinite slope analysis and geotechnical data from a suite of 34 cores collected from the continental slope between Wilmington and Lindenkohl Canyons, indicates that the Quaternary surficial silty clay sediments on gentle slopes are stable; that sediment stability on steeper slopes (14??-19??) is marginal; and that on precipitous slopes (>50??) only a thin veneer of unconsolidated sediments can exist. Small earthquake-induced accelerations or the effects of internal waves can result in slope sediment instabilities. ?? 1982 A. M. Dowden, Inc.","largerWorkType":{"id":2,"text":"Article"},"largerWorkTitle":"Geo-Marine Letters","largerWorkSubtype":{"id":10,"text":"Journal Article"},"language":"English","publisherLocation":"Springer-Verlag","doi":"10.1007/BF02462753","issn":"02760460","usgsCitation":"Almagor, G., Bennett, R., Mc Gregor, B., and Shephard, L., 1982, Stability studies of surficial sediments in the Wilmington-Lindenkohl Canyons area, eastern U.S. margin: Geo-Marine Letters, v. 2, no. 3-4, p. 129-134, https://doi.org/10.1007/BF02462753.","startPage":"129","endPage":"134","numberOfPages":"6","costCenters":[],"links":[{"id":204898,"rank":9999,"type":{"id":10,"text":"Digital Object Identifier"},"url":"https://dx.doi.org/10.1007/BF02462753"},{"id":218947,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"2","issue":"3-4","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"505b965ee4b08c986b31b478","contributors":{"authors":[{"text":"Almagor, G.","contributorId":16973,"corporation":false,"usgs":true,"family":"Almagor","given":"G.","email":"","affiliations":[],"preferred":false,"id":358812,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Bennett, R.H.","contributorId":34649,"corporation":false,"usgs":true,"family":"Bennett","given":"R.H.","email":"","affiliations":[],"preferred":false,"id":358813,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Mc Gregor, B.A.","contributorId":82054,"corporation":false,"usgs":true,"family":"Mc Gregor","given":"B.A.","email":"","affiliations":[],"preferred":false,"id":358815,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Shephard, L.E.","contributorId":53940,"corporation":false,"usgs":true,"family":"Shephard","given":"L.E.","email":"","affiliations":[],"preferred":false,"id":358814,"contributorType":{"id":1,"text":"Authors"},"rank":4}]}}
,{"id":70142169,"text":"70142169 - 1982 - Evaluating depth to shallow groundwater using Heat Capacity Mapping Mission (HCMM) data","interactions":[],"lastModifiedDate":"2017-01-18T14:51:34","indexId":"70142169","displayToPublicDate":"1982-01-01T00:00:00","publicationYear":"1982","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":3052,"text":"Photogrammetric Engineering and Remote Sensing","active":true,"publicationSubtype":{"id":10}},"title":"Evaluating depth to shallow groundwater using Heat Capacity Mapping Mission (HCMM) data","docAbstract":"<p>Four dates of Heat Capacity Mapping Mission (HCMM) data were analyzed to evaluate the utility of HCMM thermal data for evaluating depth to shallow groundwater. During the summer, shallow water tables can create lower soil temperatures throughout the diurnal temperature cycle. Because of large spatial and temporal ground cover variations, HCMM daytime radiometric temperatures alone did not correlate with water table depth. The radiometric temperatures consisted of radiance contributions from different crop canopies and their respective soil backgrounds. However, when surface soil temperatures were empirically estimated from HCMM temperatures and percent cover of each pixel, significant correlations were obtained between estimated soil temperatures and water table depth. Correlations increased as the season progressed and temperature gradients within the soil profile increased. However, estimated soil temperatures were also correlated with near-surface soil moisture since during the daytime, increasing soil moisture reduced surface soil temperature. Complementary effects of shallow water tables and soil moisture on daytime temperatures cannot be separated.</p>","language":"English","publisher":"American Society for Photogrammetry and Remote Sensing","usgsCitation":"Heilman, J.L., and Moore, D.G., 1982, Evaluating depth to shallow groundwater using Heat Capacity Mapping Mission (HCMM) data: Photogrammetric Engineering and Remote Sensing, v. 48, no. 12, p. 1903-1906.","productDescription":"4 p.","startPage":"1903","endPage":"1906","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[{"id":222,"text":"Earth Resources Observation and Science (EROS) Center","active":true,"usgs":true}],"links":[{"id":298206,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"48","issue":"12","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"54f597c7e4b02419550d2f42","contributors":{"authors":[{"text":"Heilman, J. L.","contributorId":85723,"corporation":false,"usgs":true,"family":"Heilman","given":"J.","email":"","middleInitial":"L.","affiliations":[],"preferred":false,"id":541655,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Moore, Donald G.","contributorId":41146,"corporation":false,"usgs":true,"family":"Moore","given":"Donald","email":"","middleInitial":"G.","affiliations":[],"preferred":false,"id":541656,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":1000116,"text":"1000116 - 1982 - Comparative hatching success of lake trout eggs in Lake Michigan water and well water","interactions":[],"lastModifiedDate":"2016-04-01T08:54:15","indexId":"1000116","displayToPublicDate":"1982-01-01T00:00:00","publicationYear":"1982","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":3196,"text":"Progressive Fish-Culturist","active":true,"publicationSubtype":{"id":10}},"title":"Comparative hatching success of lake trout eggs in Lake Michigan water and well water","docAbstract":"<p>A study was undertaken to examine the influence of water from southern Lake Michigan on the survival of lake trout (Salvelinus namaycush) eggs by comparing the hatching success of eggs from the same source incubated in water from Lake Michigan, or from the laboratory well. It is concluded that the observed differences in hatching are probably attributable to chemical constituents of water from the lake (eg, chlorinated hydrocarbons, metals and other industrial and agricultural chemicals).</p>","language":"English","publisher":"Taylor & Francis","doi":"10.1577/1548-8659(1982)44[47:CHSOLT]2.0.CO;2","usgsCitation":"Edsall, C., and Mac, M.J., 1982, Comparative hatching success of lake trout eggs in Lake Michigan water and well water: Progressive Fish-Culturist, v. 44, no. 1, p. 47-48, https://doi.org/10.1577/1548-8659(1982)44[47:CHSOLT]2.0.CO;2.","productDescription":"2 p.","startPage":"47","endPage":"48","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[{"id":324,"text":"Great Lakes Science Center","active":true,"usgs":true}],"links":[{"id":133361,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"44","issue":"1","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b24e4b07f02db6ae551","contributors":{"authors":[{"text":"Edsall, Carol C.","contributorId":39726,"corporation":false,"usgs":true,"family":"Edsall","given":"Carol C.","affiliations":[],"preferred":false,"id":308103,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Mac, Michael J.","contributorId":16772,"corporation":false,"usgs":true,"family":"Mac","given":"Michael","email":"","middleInitial":"J.","affiliations":[],"preferred":false,"id":308102,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":1013900,"text":"1013900 - 1982 - Hydrocarbons depress growth and reproduction of the Daphnia pulex (Cladocera)","interactions":[],"lastModifiedDate":"2012-02-02T00:04:27","indexId":"1013900","displayToPublicDate":"1982-01-01T00:00:00","publicationYear":"1982","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1169,"text":"Canadian Journal of Fisheries and Aquatic Sciences","active":true,"publicationSubtype":{"id":10}},"title":"Hydrocarbons depress growth and reproduction of the Daphnia pulex (Cladocera)","largerWorkType":{"id":2,"text":"Article"},"largerWorkTitle":"Canadian Journal of Fisheries and Aquatic Sciences","largerWorkSubtype":{"id":10,"text":"Journal Article"},"language":"English","collaboration":"None/SE","usgsCitation":"Geiger, J.G., and Buikema, A., 1982, Hydrocarbons depress growth and reproduction of the Daphnia pulex (Cladocera): Canadian Journal of Fisheries and Aquatic Sciences, v. 39, no. 6, p. 830-836.","productDescription":"p. 830-836","startPage":"830","endPage":"836","numberOfPages":"7","costCenters":[{"id":365,"text":"Leetown Science Center","active":true,"usgs":true}],"links":[{"id":132144,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"39","issue":"6","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a50e4b07f02db628f24","contributors":{"authors":[{"text":"Geiger, J. G.","contributorId":29340,"corporation":false,"usgs":true,"family":"Geiger","given":"J.","email":"","middleInitial":"G.","affiliations":[],"preferred":false,"id":319415,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Buikema, A.L. Jr.","contributorId":43717,"corporation":false,"usgs":true,"family":"Buikema","given":"A.L.","suffix":"Jr.","email":"","affiliations":[],"preferred":false,"id":319416,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":70011632,"text":"70011632 - 1982 - Evaluation of 0.46- to 2.36-mu m multispectral scanner images of the east Tintic mining district, Utah, for mapping hydrothermally altered rocks","interactions":[],"lastModifiedDate":"2024-01-12T16:47:28.042972","indexId":"70011632","displayToPublicDate":"1982-01-01T00:00:00","publicationYear":"1982","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1472,"text":"Economic Geology","active":true,"publicationSubtype":{"id":10}},"title":"Evaluation of 0.46- to 2.36-mu m multispectral scanner images of the east Tintic mining district, Utah, for mapping hydrothermally altered rocks","docAbstract":"<p><span>Airborne multispectral scanner images recorded in the 0.46- to 2.36-mu m region for the East Tintic mining district, Utah, were evaluated to determine their usefulness for distinguishing six types of hydrothermally altered rocks from a wide range of sedimentary and igneous rock types. Limestone, dolomite, and argillaceous rocks were of particular interest because these have spectral reflectance features that might make them difficult to separate from some of the altered rocks when these images are used.The laboratory and field evaluation of a color ratio composite image, supported by in situ spectral reflectance measurements and an alteration map compiled from a published map, shows that silicified, argillized, and pyritized rocks can be mapped in detail utilizing an intense OH absorption band centered near 2.2 mu m. This absorption band is absent or weak in most of the unaltered rocks. However, the 2.2-mu m band is also weak in the reflectance spectra representing the other three types of altered rocks--hydrothermal dolomite, calcitic volcanic rocks, and chloritized rocks. Consequently, these altered rocks are not consistently distinguished from unaltered rocks in these images. Furthermore, very pure dolomite spectra have an intense 2.33- mu m CO (super -3) absorption band that is not distinguishable from the 2.2-mu m band in these images; therefore, the pure dolomite exposures were distinguished from the silicified, argillized, and pyritized rocks through field checking. The 2.33-mu m absorption feature is weak in spectra for less pure carbonate rocks. Separation of these altered rocks and local exposures of argillaceous rocks also posed problems because of their mineralogic and hence spectral reflectance similarities.These results are especially important for estimating the potential of the 1.6- and 2.2-mu m bands in the Landsat D thematic mapper for mapping altered rocks. Here, as we found in an earlier study in south-central Nevada, limonite-poor hydrothermally altered rocks that were not consistently distinguished in Landsat multispectral scanner images should be detectable using these two thematic mapper bands in combination with other bands at shorter wave-lengths. However, distinguishing among some hydrothermally altered and unaltered rocks will require other approaches, including analysis of high-spectral resolution measurements in the 2.0- and 2.5-mu m region and multispectral thermal infrared data.</span></p>","language":"English","publisher":"Society of Economic Geologists","doi":"10.2113/gsecongeo.77.2.441","issn":"03610128","usgsCitation":"Rowan, L.C., and Kahle, A., 1982, Evaluation of 0.46- to 2.36-mu m multispectral scanner images of the east Tintic mining district, Utah, for mapping hydrothermally altered rocks: Economic Geology, v. 77, no. 2, p. 441-452, https://doi.org/10.2113/gsecongeo.77.2.441.","productDescription":"12 p.","startPage":"441","endPage":"452","numberOfPages":"12","costCenters":[],"links":[{"id":221187,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"77","issue":"2","noUsgsAuthors":false,"publicationDate":"1982-04-01","publicationStatus":"PW","scienceBaseUri":"505a0c0ae4b0c8380cd529ec","contributors":{"authors":[{"text":"Rowan, L. C.","contributorId":40584,"corporation":false,"usgs":true,"family":"Rowan","given":"L.","email":"","middleInitial":"C.","affiliations":[],"preferred":false,"id":361581,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Kahle, A.B.","contributorId":36928,"corporation":false,"usgs":true,"family":"Kahle","given":"A.B.","email":"","affiliations":[],"preferred":false,"id":361580,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":1014066,"text":"1014066 - 1982 - Pathogenicity and histopathology of an unusually intense infection of white grubs (Posthodiplostomum m minimum) in the fathead minnow (Pimephales promelas)","interactions":[],"lastModifiedDate":"2024-07-22T23:59:08.210057","indexId":"1014066","displayToPublicDate":"1982-01-01T00:00:00","publicationYear":"1982","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":2507,"text":"Journal of Wildlife Diseases","active":true,"publicationSubtype":{"id":10}},"title":"Pathogenicity and histopathology of an unusually intense infection of white grubs (Posthodiplostomum m minimum) in the fathead minnow (Pimephales promelas)","docAbstract":"<p>No abstract available.</p>","language":"English","publisher":"Wildlife Disease Association","doi":"10.7589/0090-3558-18.1.51","usgsCitation":"Mitchell, A., Smith, C.E., and Hoffman, G.L., 1982, Pathogenicity and histopathology of an unusually intense infection of white grubs (Posthodiplostomum m minimum) in the fathead minnow (Pimephales promelas): Journal of Wildlife Diseases, v. 18, no. 13, p. 51-57, https://doi.org/10.7589/0090-3558-18.1.51.","productDescription":"7 p.","startPage":"51","endPage":"57","numberOfPages":"7","costCenters":[{"id":365,"text":"Leetown Science Center","active":true,"usgs":true}],"links":[{"id":480258,"rank":2,"type":{"id":40,"text":"Open Access Publisher Index Page"},"url":"https://doi.org/10.7589/0090-3558-18.1.51","text":"Publisher Index Page"},{"id":131170,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"18","issue":"13","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ae2e4b07f02db688c6a","contributors":{"authors":[{"text":"Mitchell, A.J.","contributorId":16345,"corporation":false,"usgs":true,"family":"Mitchell","given":"A.J.","email":"","affiliations":[],"preferred":false,"id":319704,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Smith, C. E.","contributorId":29344,"corporation":false,"usgs":true,"family":"Smith","given":"C.","email":"","middleInitial":"E.","affiliations":[],"preferred":false,"id":319705,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Hoffman, G. L.","contributorId":70713,"corporation":false,"usgs":true,"family":"Hoffman","given":"G.","email":"","middleInitial":"L.","affiliations":[],"preferred":false,"id":319706,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":1013782,"text":"1013782 - 1982 - Aquaculture training available at nearby National Fisheries Center","interactions":[],"lastModifiedDate":"2012-02-02T00:04:30","indexId":"1013782","displayToPublicDate":"1982-01-01T00:00:00","publicationYear":"1982","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":3598,"text":"Tidewater Fisheries News","active":true,"publicationSubtype":{"id":10}},"title":"Aquaculture training available at nearby National Fisheries Center","largerWorkType":{"id":2,"text":"Article"},"largerWorkTitle":"Tidewater Fisheries News","largerWorkSubtype":{"id":10,"text":"Journal Article"},"language":"English","collaboration":"None/TIS","usgsCitation":"Gutsell, G., 1982, Aquaculture training available at nearby National Fisheries Center: Tidewater Fisheries News, v. 15, no. 5.","productDescription":"4 p.","startPage":"4","numberOfPages":"4","costCenters":[{"id":365,"text":"Leetown Science Center","active":true,"usgs":true}],"links":[{"id":132205,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"15","issue":"5","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ac5e4b07f02db67a113","contributors":{"authors":[{"text":"Gutsell, G.S.","contributorId":88694,"corporation":false,"usgs":true,"family":"Gutsell","given":"G.S.","email":"","affiliations":[],"preferred":false,"id":319251,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":1014489,"text":"1014489 - 1982 - Zinc supplements prevents cataracts","interactions":[],"lastModifiedDate":"2012-02-02T00:04:32","indexId":"1014489","displayToPublicDate":"1982-01-01T00:00:00","publicationYear":"1982","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":855,"text":"Aquaculture Magazine","active":true,"publicationSubtype":{"id":10}},"title":"Zinc supplements prevents cataracts","largerWorkType":{"id":2,"text":"Article"},"largerWorkTitle":"Aquaculture Magazine","largerWorkSubtype":{"id":10,"text":"Journal Article"},"language":"English","collaboration":"None/TL","usgsCitation":"Ketola, H.G., 1982, Zinc supplements prevents cataracts: Aquaculture Magazine, v. 8, no. 2, p. 47-48.","productDescription":"p. 47-48","startPage":"47","endPage":"48","numberOfPages":"2","costCenters":[{"id":365,"text":"Leetown Science Center","active":true,"usgs":true}],"links":[{"id":131733,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"8","issue":"2","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a9ae4b07f02db65d97c","contributors":{"authors":[{"text":"Ketola, H. G.","contributorId":60976,"corporation":false,"usgs":true,"family":"Ketola","given":"H.","middleInitial":"G.","affiliations":[],"preferred":false,"id":320456,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":1014488,"text":"1014488 - 1982 - Effect of phosphorus in trout diets on water pollution","interactions":[],"lastModifiedDate":"2012-02-02T00:04:32","indexId":"1014488","displayToPublicDate":"1982-01-01T00:00:00","publicationYear":"1982","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":3330,"text":"Salmonid","active":true,"publicationSubtype":{"id":10}},"title":"Effect of phosphorus in trout diets on water pollution","largerWorkType":{"id":2,"text":"Article"},"largerWorkTitle":"Salmonid","largerWorkSubtype":{"id":10,"text":"Journal Article"},"language":"English","collaboration":"None/TL","usgsCitation":"Ketola, H.G., 1982, Effect of phosphorus in trout diets on water pollution: Salmonid, v. 6, no. 2, p. 12-15.","productDescription":"p. 12-15","startPage":"12","endPage":"15","numberOfPages":"4","costCenters":[{"id":365,"text":"Leetown Science Center","active":true,"usgs":true}],"links":[{"id":131732,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"6","issue":"2","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a4be4b07f02db6255b7","contributors":{"authors":[{"text":"Ketola, H. G.","contributorId":60976,"corporation":false,"usgs":true,"family":"Ketola","given":"H.","middleInitial":"G.","affiliations":[],"preferred":false,"id":320455,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":70182482,"text":"70182482 - 1982 - Breeding ecology of the black turnstones: a study in behavior and energetics","interactions":[],"lastModifiedDate":"2018-05-20T17:42:34","indexId":"70182482","displayToPublicDate":"1982-01-01T00:00:00","publicationYear":"1982","noYear":false,"publicationType":{"id":21,"text":"Thesis"},"publicationSubtype":{"id":28,"text":"Thesis"},"title":"Breeding ecology of the black turnstones: a study in behavior and energetics","docAbstract":"<p>No abstract available&nbsp;</p>","language":"English","publisher":"University of California","publisherLocation":"Davis, CA","usgsCitation":"Handel, C.M., 1982, Breeding ecology of the black turnstones: a study in behavior and energetics, 96 p. .","productDescription":"96 p. ","costCenters":[{"id":654,"text":"Western Fisheries Research Center","active":true,"usgs":true}],"links":[{"id":336091,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"publicComments":"Master's Thesis","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"58b002dce4b01ccd54fb2821","contributors":{"authors":[{"text":"Handel, Colleen M. 0000-0002-0267-7408 cmhandel@usgs.gov","orcid":"https://orcid.org/0000-0002-0267-7408","contributorId":3067,"corporation":false,"usgs":true,"family":"Handel","given":"Colleen","email":"cmhandel@usgs.gov","middleInitial":"M.","affiliations":[{"id":117,"text":"Alaska Science Center Biology WTEB","active":true,"usgs":true}],"preferred":true,"id":671242,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":1000093,"text":"1000093 - 1982 - Food of freshwater drum in western Lake Erie","interactions":[],"lastModifiedDate":"2016-03-31T15:29:19","indexId":"1000093","displayToPublicDate":"1982-01-01T00:00:00","publicationYear":"1982","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":2330,"text":"Journal of Great Lakes Research","active":true,"publicationSubtype":{"id":10}},"title":"Food of freshwater drum in western Lake Erie","docAbstract":"<p>The abundance of freshwater drum (Aplodinotus grunniens) suggests they play an important role in the Lake Erie ecosystem. Our analysis of freshwater drum digestive tracts and macrobenthic samples collected from western Lake Erie indicates that drum were selective feeders. Planktonic cladocerans and larval midges (Chironomidae) were the primary prey organisms eaten by drum. Young-of-the-year fed mostly on cladocerans, while yearling and older drum ate both cladocerans and midge larvae. Decapods, pelecypods, and fish were found only in the digestive tracts of drum longer than 250 mm. While the most abundant organisms in benthic samples were cladocerans (ephippial) and oligochaetes (89.5% by number), they constituted less than 1% of the diet. An evaluation of food selectivity, using Ivlev's index of electivity for benthic organisms, indicated that adult drum preferred midges to any other benthic food.</p>","language":"English","publisher":"Elsevier","doi":"10.1016/S0380-1330(82)72007-6","usgsCitation":"Bur, M.T., 1982, Food of freshwater drum in western Lake Erie: Journal of Great Lakes Research, v. 8, no. 4, p. 672-675, https://doi.org/10.1016/S0380-1330(82)72007-6.","productDescription":"4 p.","startPage":"672","endPage":"675","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[{"id":324,"text":"Great Lakes Science Center","active":true,"usgs":true}],"links":[{"id":132935,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"8","issue":"4","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b24e4b07f02db6ae6c0","contributors":{"authors":[{"text":"Bur, Michael T.","contributorId":102015,"corporation":false,"usgs":true,"family":"Bur","given":"Michael","email":"","middleInitial":"T.","affiliations":[],"preferred":false,"id":308068,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":70182312,"text":"70182312 - 1982 - Relation between size of Chinook salmon, Oncorhynchus tshawytscha, released at hatcheries and returns to hatcheries and ocean fisheries","interactions":[],"lastModifiedDate":"2017-02-22T14:42:52","indexId":"70182312","displayToPublicDate":"1982-01-01T00:00:00","publicationYear":"1982","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1153,"text":"California Fish and Game","active":true,"publicationSubtype":{"id":10}},"title":"Relation between size of Chinook salmon, Oncorhynchus tshawytscha, released at hatcheries and returns to hatcheries and ocean fisheries","docAbstract":"<p>No abstract available&nbsp;</p>","language":"English","publisher":"State of California","usgsCitation":"Reisenbichler, R., McIntyre, J., and Hallock, R., 1982, Relation between size of Chinook salmon, Oncorhynchus tshawytscha, released at hatcheries and returns to hatcheries and ocean fisheries: California Fish and Game, v. 68, no. 1, p. 57-59.","productDescription":"3 p. ","startPage":"57","endPage":"59","costCenters":[{"id":654,"text":"Western Fisheries Research Center","active":true,"usgs":true}],"links":[{"id":335985,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"},{"id":335984,"rank":1,"type":{"id":15,"text":"Index Page"},"url":"https://www.wildlife.ca.gov/Publications/Journal/Contents#1982"}],"volume":"68","issue":"1","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"58aeb153e4b01ccd54f9ee86","contributors":{"authors":[{"text":"Reisenbichler, R.R.","contributorId":77356,"corporation":false,"usgs":true,"family":"Reisenbichler","given":"R.R.","email":"","affiliations":[],"preferred":false,"id":670473,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"McIntyre, J.D.","contributorId":27006,"corporation":false,"usgs":true,"family":"McIntyre","given":"J.D.","email":"","affiliations":[],"preferred":false,"id":670474,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Hallock, R.J.","contributorId":100413,"corporation":false,"usgs":true,"family":"Hallock","given":"R.J.","email":"","affiliations":[],"preferred":false,"id":670475,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":1015636,"text":"1015636 - 1982 - [Book review] The Desert Bighorn, by Gale Monson","interactions":[],"lastModifiedDate":"2012-09-25T17:16:32","indexId":"1015636","displayToPublicDate":"1982-01-01T00:00:00","publicationYear":"1982","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":2508,"text":"Journal of Wildlife Management","active":true,"publicationSubtype":{"id":10}},"title":"[Book review] The Desert Bighorn, by Gale Monson","docAbstract":"Review of: The Desert Bighorn: Its Life History, Ecology, and Management. By Gale Monson. 370 pp. / 6.00 in x 9.00 in / 1980 Paper (978-0-8165-0713-9).","largerWorkType":{"id":2,"text":"Article"},"largerWorkTitle":"Journal of Wildlife Management","largerWorkSubtype":{"id":10,"text":"Journal Article"},"language":"English","usgsCitation":"Schonewald-Cox, C., 1982, [Book review] The Desert Bighorn, by Gale Monson: Journal of Wildlife Management, v. 46, no. 2, p. 565-566.","productDescription":"2 p.","startPage":"565","endPage":"566","numberOfPages":"2","costCenters":[{"id":651,"text":"Western Ecological Research Center","active":true,"usgs":true}],"links":[{"id":132819,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"},{"id":262036,"rank":100,"type":{"id":15,"text":"Index Page"},"url":"https://www.jstor.org/stable/3808685","linkFileType":{"id":5,"text":"html"}}],"volume":"46","issue":"2","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a14e4b07f02db602eca","contributors":{"authors":[{"text":"Schonewald-Cox, C.","contributorId":91433,"corporation":false,"usgs":true,"family":"Schonewald-Cox","given":"C.","affiliations":[],"preferred":false,"id":323021,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":1017151,"text":"1017151 - 1982 - Fish cell lines: characterization of six cell lines by enzyme profiles","interactions":[],"lastModifiedDate":"2012-02-02T00:04:35","indexId":"1017151","displayToPublicDate":"1982-01-01T00:00:00","publicationYear":"1982","noYear":false,"publicationType":{"id":24,"text":"Conference Paper"},"publicationSubtype":{"id":18,"text":"Abstract or summary"},"seriesTitle":{"id":476,"text":"In Vitro","active":false,"publicationSubtype":{"id":18}},"title":"Fish cell lines: characterization of six cell lines by enzyme profiles","docAbstract":"No abstract available at this time","largerWorkType":{"id":2,"text":"Article"},"largerWorkTitle":"In Vitro","largerWorkSubtype":{"id":10,"text":"Journal Article"},"language":"English","collaboration":"640/FH","usgsCitation":"Lidgerding, B.C., and Schill, W.B., 1982, Fish cell lines: characterization of six cell lines by enzyme profiles, <i>in</i> In Vitro, v. 18, no. 3, Part II.","productDescription":"295 p.","startPage":"295","numberOfPages":"295","costCenters":[{"id":365,"text":"Leetown Science Center","active":true,"usgs":true}],"links":[{"id":133056,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"18","issue":"3, Part II","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e49f8e4b07f02db5f2e0e","contributors":{"authors":[{"text":"Lidgerding, B. C.","contributorId":8028,"corporation":false,"usgs":true,"family":"Lidgerding","given":"B.","email":"","middleInitial":"C.","affiliations":[],"preferred":false,"id":324635,"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":324636,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":70011459,"text":"70011459 - 1982 - Origin of biotite-hornblende-garnet coronas between oxides and plagioclase in olivine metagabbros, Adirondack region, New York","interactions":[],"lastModifiedDate":"2012-03-12T17:19:02","indexId":"70011459","displayToPublicDate":"1982-01-01T00:00:00","publicationYear":"1982","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1336,"text":"Contributions to Mineralogy and Petrology","active":true,"publicationSubtype":{"id":10}},"title":"Origin of biotite-hornblende-garnet coronas between oxides and plagioclase in olivine metagabbros, Adirondack region, New York","docAbstract":"Complex multivariant reactions involving Fe-Ti oxide minerals, plagioclase and olivine have produced coronas of biotite, hornblende and garnet between ilmenite and plagioclase in Adirondack olivine metagabbros. Both the biotite (6-10% TiO2) and the hornblende (3-6% TiO2) are exceptionally Titanium-rich. The garnet is nearly identical in composition to the garnet in coronas around olivine in the same rocks. The coronas form in two stages: (a) Plagioclase+Fe-Ti Oxides+Olivine+water =Hornblende+Spinel+Orthopyroxene??Biotite +more-sodic Plagioclase (b) Hornblende+Orthopyroxene??Spinel+Plagioclase =Garnet+Clinopyroxene+more-sodic Plagioclase The Orthopyroxene and part of the clinopyroxene form adjacent to olivine. Both reactions are linked by exchange of Mg2+ and Fe2+ with the reactions forming pyroxene and garnet coronas around olivine in the same rocks. The reactions occur under granulite fades metamorphic conditions, either during isobaric cooling or with increasing pressure at high temperature. ?? 1983 Springer-Verlag.","largerWorkType":{"id":2,"text":"Article"},"largerWorkTitle":"Contributions to Mineralogy and Petrology","largerWorkSubtype":{"id":10,"text":"Journal Article"},"language":"English","publisherLocation":"Springer-Verlag","doi":"10.1007/BF00371173","issn":"00107999","usgsCitation":"Whitney, P., and McLelland, J.M., 1982, Origin of biotite-hornblende-garnet coronas between oxides and plagioclase in olivine metagabbros, Adirondack region, New York: Contributions to Mineralogy and Petrology, v. 82, no. 1, p. 34-41, https://doi.org/10.1007/BF00371173.","startPage":"34","endPage":"41","numberOfPages":"8","costCenters":[],"links":[{"id":205130,"rank":9999,"type":{"id":10,"text":"Digital Object Identifier"},"url":"https://dx.doi.org/10.1007/BF00371173"},{"id":221591,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"82","issue":"1","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"505a70c6e4b0c8380cd76231","contributors":{"authors":[{"text":"Whitney, P.R.","contributorId":46671,"corporation":false,"usgs":true,"family":"Whitney","given":"P.R.","email":"","affiliations":[],"preferred":false,"id":361167,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"McLelland, J. M.","contributorId":85604,"corporation":false,"usgs":true,"family":"McLelland","given":"J.","email":"","middleInitial":"M.","affiliations":[],"preferred":false,"id":361168,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":70011914,"text":"70011914 - 1982 - The UThPb age of equilibrated L chondrites and a solution to the excess radiogenic Pb problem in chondrites","interactions":[],"lastModifiedDate":"2023-12-12T12:24:40.6249","indexId":"70011914","displayToPublicDate":"1982-01-01T00:00:00","publicationYear":"1982","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1427,"text":"Earth and Planetary Science Letters","active":true,"publicationSubtype":{"id":10}},"title":"The UThPb age of equilibrated L chondrites and a solution to the excess radiogenic Pb problem in chondrites","docAbstract":"<p>U, Th, and Pb analyses of whole-rock and troilite separates from seven L chondrites suggest that the excess radiogenic Pb relative to U and the large variations in Pb<img src=\"https://sdfestaticassets-us-east-1.sciencedirectassets.com/shared-assets/55/entities/sbnd.gif\" alt=\"single bond\" data-mce-src=\"https://sdfestaticassets-us-east-1.sciencedirectassets.com/shared-assets/55/entities/sbnd.gif\">Pb model ages commonly observed in chondritic meteorites are largely due to terrestrial Pb contamination induced prior to analyses. Using the Pb isotopic composition of troilite separates to calculate the isotopic composition of the Pb contaminants, the whole-rock data have been corrected for pre-analysis terrestrial Pb contamination. Two approaches have been used: (1) the chondrite-troilite apparent initial Pb isotopic compositions were used to approximate the mixture of indigenous intial Pb and terrestrial Pb in the whole-rock sample, and (2) a single-stage (concordant) model was applied using the assumption that the excess radiogenic Pb in these samples was terrestrial. Data for L5 and L6 chondrites yield a<i>4551 ± 7My</i><span>&nbsp;</span>age using the former correction and a<i>4550 ± 5My</i><span>&nbsp;</span>age using the latter one.</p>","language":"English","publisher":"Elsevier","doi":"10.1016/0012-821X(82)90104-2","issn":"0012821X","usgsCitation":"Unruh, D., 1982, The UThPb age of equilibrated L chondrites and a solution to the excess radiogenic Pb problem in chondrites: Earth and Planetary Science Letters, v. 58, no. 1, p. 75-94, https://doi.org/10.1016/0012-821X(82)90104-2.","productDescription":"20 p.","startPage":"75","endPage":"94","numberOfPages":"20","costCenters":[],"links":[{"id":221781,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"58","issue":"1","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"505ba955e4b08c986b3221ce","contributors":{"authors":[{"text":"Unruh, D.M.","contributorId":8498,"corporation":false,"usgs":true,"family":"Unruh","given":"D.M.","email":"","affiliations":[],"preferred":false,"id":362275,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":70011911,"text":"70011911 - 1982 - Air pollution: Household soiling and consumer welfare losses","interactions":[],"lastModifiedDate":"2024-04-22T14:52:15.92587","indexId":"70011911","displayToPublicDate":"1982-01-01T00:00:00","publicationYear":"1982","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":2254,"text":"Journal of Environmental Economics and Management","active":true,"publicationSubtype":{"id":10}},"title":"Air pollution: Household soiling and consumer welfare losses","docAbstract":"<p><span>This paper uses demand and supply functions for cleanliness to estimate household benefits from reduced particulate matter soiling. A demand curve for household cleanliness is estimated, based upon the assumption that households prefer more cleanliness to less. Empirical coefficients, related to particulate pollution levels, for shifting the cleanliness supply curve, are taken from available studies. Consumer welfare gains, aggregated across 123 SMSAs, from achieving the Federal primary particulate standard, are estimated to range from $0.9 to $3.2 million per year (1971 dollars).</span></p>","language":"English","publisher":"Elsevier","doi":"10.1016/0095-0696(82)90033-X","issn":"00950696","usgsCitation":"Watson, W., and Jaksch, J., 1982, Air pollution: Household soiling and consumer welfare losses: Journal of Environmental Economics and Management, v. 9, no. 3, p. 248-262, https://doi.org/10.1016/0095-0696(82)90033-X.","productDescription":"15 p.","startPage":"248","endPage":"262","numberOfPages":"15","costCenters":[],"links":[{"id":221622,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"9","issue":"3","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"5059e918e4b0c8380cd480c7","contributors":{"authors":[{"text":"Watson, W.D.","contributorId":96730,"corporation":false,"usgs":true,"family":"Watson","given":"W.D.","email":"","affiliations":[],"preferred":false,"id":362268,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Jaksch, J.A.","contributorId":29956,"corporation":false,"usgs":true,"family":"Jaksch","given":"J.A.","email":"","affiliations":[],"preferred":false,"id":362267,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":70011908,"text":"70011908 - 1982 - Clay mineralogy of weathering rinds and possible implications concerning the sources of clay minerals in soils","interactions":[],"lastModifiedDate":"2024-01-31T01:41:01.34446","indexId":"70011908","displayToPublicDate":"1982-01-01T00:00:00","publicationYear":"1982","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1796,"text":"Geology","active":true,"publicationSubtype":{"id":10}},"title":"Clay mineralogy of weathering rinds and possible implications concerning the sources of clay minerals in soils","docAbstract":"<div id=\"15567102\" class=\"article-section-wrapper js-article-section js-content-section  \" data-section-parent-id=\"0\"><p>Weathering rinds on volcanic clasts in Quaternary deposits in the western United States contain only very fine grained and poorly crystalline clay minerals. Rinds were sampled from soils containing well-developed argillic B horizons in deposits about 10<sup>5</sup><span>&nbsp;</span>yr old or more. The clay-size fraction of the rinds is dominated by allophane and iron hydroxy-oxides, whereas the B horizons contain abundant, well-crystallized clay minerals. The contrast between the clay mineralogy of the weathering rinds, in which weathering is isolated from other soil processes, and that of the associated soil matrices suggests a need to reassess assumptions concerning the rates at which clay minerals form and the sources of clay minerals in argillic B horizons. This study suggests that crystalline clay minerals form more slowly in weathering rinds than is generally assumed for soil environments and that the weathering of primary minerals may not be the dominant source of crystalline clay minerals in middle to late Pleistocene soils.</p></div>","language":"English","publisher":"Geological Society of America","doi":"10.1130/0091-7613(1982)10<370:CMOWRA>2.0.CO;2","issn":"00917613","usgsCitation":"Colman, S.M., 1982, Clay mineralogy of weathering rinds and possible implications concerning the sources of clay minerals in soils: Geology, v. 10, no. 7, p. 370-375, https://doi.org/10.1130/0091-7613(1982)10<370:CMOWRA>2.0.CO;2.","productDescription":"6 p.","startPage":"370","endPage":"375","numberOfPages":"6","costCenters":[],"links":[{"id":221555,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"10","issue":"7","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"5059f63ae4b0c8380cd4c61d","contributors":{"authors":[{"text":"Colman, Steven M. 0000-0002-0564-9576","orcid":"https://orcid.org/0000-0002-0564-9576","contributorId":77482,"corporation":false,"usgs":true,"family":"Colman","given":"Steven","email":"","middleInitial":"M.","affiliations":[{"id":678,"text":"Woods Hole Coastal and Marine Science Center","active":true,"usgs":true}],"preferred":false,"id":362262,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":70011898,"text":"70011898 - 1982 - Age and origin of the Cortlandt Complex, New York: Implications from Sm-Nd data","interactions":[],"lastModifiedDate":"2012-03-12T17:18:34","indexId":"70011898","displayToPublicDate":"1982-01-01T00:00:00","publicationYear":"1982","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1336,"text":"Contributions to Mineralogy and Petrology","active":true,"publicationSubtype":{"id":10}},"title":"Age and origin of the Cortlandt Complex, New York: Implications from Sm-Nd data","docAbstract":"Sm-Nd systematics for nine whole-rock samples of hornblende norites, pyroxenites and a lamprophyre from various parts of the Cortlandt Complex were analyzed. Six of these samples from the central and eastern parts of the complex give an isochron age of 430??34 (2 ??) Ma with an e{open}Nd value of -2.9??0.5, and the other three samples from the western part, including the lamprophyre, define a similar age of 394??33 (2 ??) Ma but with a distinctly different e{open}Nd value of -1.4??0.4. The two different initial 143Nd/144Nd ratios corresponding to these e{open}-values are interpreted to reflect continental crustal contamination of the lamprophyric parental liquid prior to final emplacement and crystal fractionation to produce the different rock types of the complex. The intrusion age of 430 Ma for the complex clearly post-dates the major metamorphic event of the Taconic orogeny. The Nd-isotopic data also suggest a relationship between the Cortlandt Complex and a belt of lamprophyric dike rocks to the west, known as the Beemerville trend, which cuts across the metamorphic trends of the Taconic (Ratcliffe 1981). ?? 1982 Springer-Verlag.","largerWorkType":{"id":2,"text":"Article"},"largerWorkTitle":"Contributions to Mineralogy and Petrology","largerWorkSubtype":{"id":10,"text":"Journal Article"},"language":"English","publisherLocation":"Springer-Verlag","doi":"10.1007/BF00371520","issn":"00107999","usgsCitation":"Domenick, M., and Basu, A.R., 1982, Age and origin of the Cortlandt Complex, New York: Implications from Sm-Nd data: Contributions to Mineralogy and Petrology, v. 79, no. 3, p. 290-294, https://doi.org/10.1007/BF00371520.","startPage":"290","endPage":"294","numberOfPages":"5","costCenters":[],"links":[{"id":221398,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"},{"id":205117,"rank":9999,"type":{"id":10,"text":"Digital Object Identifier"},"url":"https://dx.doi.org/10.1007/BF00371520"}],"volume":"79","issue":"3","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"5059e8dfe4b0c8380cd47f29","contributors":{"authors":[{"text":"Domenick, M.A.","contributorId":69710,"corporation":false,"usgs":true,"family":"Domenick","given":"M.A.","email":"","affiliations":[],"preferred":false,"id":362242,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Basu, A. R.","contributorId":99697,"corporation":false,"usgs":true,"family":"Basu","given":"A.","email":"","middleInitial":"R.","affiliations":[],"preferred":false,"id":362243,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":70011894,"text":"70011894 - 1982 - Geomagnetic local and regional harmonic analyses","interactions":[],"lastModifiedDate":"2024-07-16T14:50:22.95464","indexId":"70011894","displayToPublicDate":"1982-01-01T00:00:00","publicationYear":"1982","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":6453,"text":"Journal of Geophysical Research Solid Earth","active":true,"publicationSubtype":{"id":10}},"title":"Geomagnetic local and regional harmonic analyses","docAbstract":"<p><span>Procedures are developed for using rectangular and cylindrical harmonic analyses in local and regional areas. Both the linear least squares analysis, applicable when component data are available, and the nonlinear least squares analysis, applicable when only total field data are available, are treated. When component data are available, it is advantageous to work with residual fields obtained by subtracting components derived from a harmonic potential from the observed components. When only total field intensity data are available, they must be used directly. Residual values cannot be used. Cylindrical harmonic analyses are indicated when fields tend toward cylindrical symmetry; otherwise, rectangular harmonic analyses will be more advantageous. Examples illustrating each type of analysis are given.</span></p>","language":"English","publisher":"American Geophysical Union","doi":"10.1029/JB087iB03p01921","issn":"01480227","usgsCitation":"Alldredge, L., 1982, Geomagnetic local and regional harmonic analyses: Journal of Geophysical Research Solid Earth, v. 87, no. B3, p. 1921-1926, https://doi.org/10.1029/JB087iB03p01921.","productDescription":"6 p.","startPage":"1921","endPage":"1926","numberOfPages":"6","costCenters":[],"links":[{"id":221325,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"87","issue":"B3","noUsgsAuthors":false,"publicationDate":"2012-09-20","publicationStatus":"PW","scienceBaseUri":"505a275ae4b0c8380cd597d9","contributors":{"authors":[{"text":"Alldredge, L.R.","contributorId":53457,"corporation":false,"usgs":true,"family":"Alldredge","given":"L.R.","email":"","affiliations":[],"preferred":false,"id":362233,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":70011893,"text":"70011893 - 1982 - Margaritasite: a new mineral of hydrothermal origin from the Pena Blanca uranium district, Mexico.","interactions":[],"lastModifiedDate":"2013-02-14T09:52:09","indexId":"70011893","displayToPublicDate":"1982-01-01T00:00:00","publicationYear":"1982","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":738,"text":"American Mineralogist","active":true,"publicationSubtype":{"id":10}},"title":"Margaritasite: a new mineral of hydrothermal origin from the Pena Blanca uranium district, Mexico.","docAbstract":"Margaritasite, (Cs,K,H3O)2(UO2)2V2O8.nH2O (where Cs > K, H3O and n approx 1), a 10.514, b 8.425, c 7.25 A, beta 106.01o, P21/a, Z = 2, is a newly recognized uranium ore mineral named for the Margaritas deposit, Pena Blanca uranium district, Chihuahua, Mexico, at which it was discovered. A Cs-rich analogue of carnotite, margaritasite is the natural equivalent of synthetic Cs-uranyl vanadate (A.M. 43- 799, 50-825). A fine-grained yellow mineral, it is most easily distinguished from carnotite by XRD; X-ray powder patterns (CuKalpha radiation) show that the (001) reflection of margaritasite lies at 12.7o (2theta ), while that of carnotite is found at 13.8o (2theta ). The shift of the (001) reflection in margaritasite reflects the structural changes caused when Cs occupies the sites filled by K in carnotite. Synthesis experiments indicate that margaritasite also differs from carnotite in a higher-T hydrothermal origin. Chemical analyses and XRD data for margaritasite and synthetic Cs- carnotite, and chemical analyses for rocks from Sierra Pena Blanca and vicinity, are tabulated.-J.A.Z.","largerWorkType":{"id":2,"text":"Article"},"largerWorkTitle":"American Mineralogist","largerWorkSubtype":{"id":10,"text":"Journal Article"},"language":"English","publisher":"Mineralogical Society of America","issn":"0003004X","usgsCitation":"Wenrich, K., Modreski, P., Zielinski, R.A., and Seeley, J.L., 1982, Margaritasite: a new mineral of hydrothermal origin from the Pena Blanca uranium district, Mexico.: American Mineralogist, v. 67, no. 11-12, p. 1273-1289.","startPage":"1273","endPage":"1289","numberOfPages":"17","costCenters":[],"links":[{"id":221324,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"},{"id":267367,"type":{"id":11,"text":"Document"},"url":"https://www.minsocam.org/ammin/AM67/AM67_1273.pdf"}],"volume":"67","issue":"11-12","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"505a51c3e4b0c8380cd6bf0e","contributors":{"authors":[{"text":"Wenrich, K. J.","contributorId":40203,"corporation":false,"usgs":true,"family":"Wenrich","given":"K. J.","affiliations":[],"preferred":false,"id":362229,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Modreski, P.J.","contributorId":98335,"corporation":false,"usgs":true,"family":"Modreski","given":"P.J.","affiliations":[],"preferred":false,"id":362231,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Zielinski, R. A. 0000-0002-4047-5129","orcid":"https://orcid.org/0000-0002-4047-5129","contributorId":106930,"corporation":false,"usgs":true,"family":"Zielinski","given":"R.","email":"","middleInitial":"A.","affiliations":[{"id":164,"text":"Central Energy Resources Science Center","active":true,"usgs":true}],"preferred":false,"id":362232,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Seeley, J. L.","contributorId":57864,"corporation":false,"usgs":true,"family":"Seeley","given":"J.","email":"","middleInitial":"L.","affiliations":[],"preferred":false,"id":362230,"contributorType":{"id":1,"text":"Authors"},"rank":4}]}}
,{"id":70011892,"text":"70011892 - 1982 - Lead and strontium isotopes and related trace elements as genetic tracers in the Upper Cenozoic rhyolite-basalt association of the Yellowstone Plateau volcanic field","interactions":[],"lastModifiedDate":"2024-07-16T14:46:02.2975","indexId":"70011892","displayToPublicDate":"1982-01-01T00:00:00","publicationYear":"1982","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":6453,"text":"Journal of Geophysical Research Solid Earth","active":true,"publicationSubtype":{"id":10}},"title":"Lead and strontium isotopes and related trace elements as genetic tracers in the Upper Cenozoic rhyolite-basalt association of the Yellowstone Plateau volcanic field","docAbstract":"<p><span>Supported by various field geologic and petrologic data, the contents of Pb, U, Th, Rb, and Sr and the isotopic compositions of Pb and Sr for upper Cenozoic volcanic rocks of the Yellowstone Plateau volcanic field are consistent with the hypothesis of derivation of the basaltic and rhyolitic magmas by partial melting of distinct source regions in the upper mantle and lower crust, respectively. All the basalt samples analyzed but one have systematically lower values of&nbsp;</span><sup>207</sup><span>Pb/</span><sup>204</sup><span>Pb and&nbsp;</span><sup>87</sup><span>Sr/</span><sup>86</sup><span>Sr than the rhyolites. The values of&nbsp;</span><sup>206</sup><span>Pb/</span><sup>204</sup><span>Pb are smaller, and&nbsp;</span><sup>87</sup><span>Sr/</span><sup>86</sup><span>Sr are mostly larger than known values in oceanic basalts. In all but one case, the values of&nbsp;</span><sup>207</sup><span>Pb/</span><sup>204</sup><span>Pb are higher than expected from an extrapolation of known values in oceanic basalts to less radiogenic values of&nbsp;</span><sup>206</sup><span>Pb/</span><sup>204</sup><span>Pb. Because there are no xenoliths, phenocrysts are only moderate to sparse in abundance, REE patterns are low and flat at the radiogenic end of lead isotopic compositions, several values of Rb/Sr are low, and 80% of the basalt samples form a well-developed secondary isochron separate from the rhyolites, we favor an interpretation for basalt genesis wherein isotopic signatures of most mafic magmas were attained in a continental ‘keel’ of mantlelike character about 2.6 b.y. old or somewhat older attached to the crust, and these signatures were unaltered by magma passage through the crust. At the very least, the current data continue to cast serious doubt as to the inevitability of crustal contamination for basaltic magma intruding the continental environment and postulate that much can be learned about the mantle under continents through the study of continental basalts. One basalt unit with an unusually low value of&nbsp;</span><sup>207</sup><span>Pb/</span><sup>204</sup><span>Pb and an&nbsp;</span><sup>87</sup><span>Ar/</span><sup>86</sup><span>Ar less than 0.704 may represent subcontinental ‘keel’-derived magma that rose unaltered to the surface. Our data also are not consistent with formation of this rhyolite-basalt association primarily by such processes as crystal fractionation, separation of immiscible silicate liquids from a common parental magma, or fractional melting of a homogeneous source. Rather as a conceptual model, we envision large mafic intrusions to have been injected into the lower crust resulting in rhyolite generation through partial anatexis of the adjacent wall rocks which probably had a&nbsp;</span><sup>206</sup><span>Pb/</span><sup>204</sup><span>Pb &lt; 17 and&nbsp;</span><sup>87</sup><span>Sr/</span><sup>86</sup><span>Sr &gt; 0.709; a model that has much in common with that proposed by Holmes (1931). All the other hypotheses listed have the necessary added complication that either the basalt or the rhyolite or both become contaminated after the two magma types separated, have problems accounting for the lack of igneous rocks of intermediate compositions or production of such large volumes of rhyolitic material (∼5000 km</span><sup>3</sup><span>), and fail to explain why rhyolitic magma is not a more common occurrence in the ocean basin. We appeal to bouyancy of rhyolites to generate a barrier for basalt magma migration and account for the great preponderance of rhyolite relative to basalt at the surface. Furthermore, the complex isotopic picture in the rhyolites indicates that many of these magmas interacted with the upper crustal geologic units that they traversed. The interactions involved diverse processes, probably including reacton with hydrothermal fluids or hydrothermally altered rocks at high levels as well as by contamination with Phanerozoic sedimentary and Precambrian crystalline rocks at deeper levels. At the very least, we feel our study adds a cautionary note to the currently increasingly popular hypothesis that differentiation of basalt or gabbro magmas to rhyolite or granite (as distinct from tonalite or dacite) is a common occurrence and is therefore an important continential building process. Models for formation of rhyolite and granite predominantly by reworking of crust (anatexis) must still be considered. The primitive Archean mantle of the region was characterized by higher Rb/Sr, U/Pb, and Th/U values than are typical of modern suboceanic mantle. The mantle residuum within the continental subcrustal lithosperic ‘keel’ that resulted from the Archean crustal differentiation event probably was depleted in Rb/Sr and U/Pb, and the crust was correspondingly enriched in these ratios. The crust probably was further differentiated by an Archean high-grade metamorphism, during or after the primary event, into a granulitic lower crust depleted in U/Pb and Rb/Sr and a lower-grade upper crust enriched in these ratios.</span></p>","language":"English","publisher":"American Geophysical Union","doi":"10.1029/JB087iB06p04785","issn":"01480227","usgsCitation":"Doe, B.R., Leeman, W., Christiansen, R., and Hedge, C., 1982, Lead and strontium isotopes and related trace elements as genetic tracers in the Upper Cenozoic rhyolite-basalt association of the Yellowstone Plateau volcanic field: Journal of Geophysical Research Solid Earth, v. 87, no. B6, p. 4785-4806, https://doi.org/10.1029/JB087iB06p04785.","productDescription":"22 p.","startPage":"4785","endPage":"4806","numberOfPages":"22","costCenters":[],"links":[{"id":221323,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"87","issue":"B6","noUsgsAuthors":false,"publicationDate":"2012-09-20","publicationStatus":"PW","scienceBaseUri":"505a45ade4b0c8380cd67474","contributors":{"authors":[{"text":"Doe, B. R.","contributorId":52173,"corporation":false,"usgs":true,"family":"Doe","given":"B.","email":"","middleInitial":"R.","affiliations":[],"preferred":false,"id":362227,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Leeman, W.P.","contributorId":7841,"corporation":false,"usgs":true,"family":"Leeman","given":"W.P.","affiliations":[],"preferred":false,"id":362225,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Christiansen, R.L. 0000-0002-8017-3918","orcid":"https://orcid.org/0000-0002-8017-3918","contributorId":25565,"corporation":false,"usgs":true,"family":"Christiansen","given":"R.L.","affiliations":[],"preferred":false,"id":362226,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Hedge, C. E.","contributorId":73611,"corporation":false,"usgs":true,"family":"Hedge","given":"C. E.","affiliations":[],"preferred":false,"id":362228,"contributorType":{"id":1,"text":"Authors"},"rank":4}]}}
,{"id":70011891,"text":"70011891 - 1982 - Heat capacity and entropy of fayalite (Fe2SiO4) between 5.1 and 383 K: comparison of calorimetric and equilibrium valus for the QFM buffer reaction.","interactions":[],"lastModifiedDate":"2013-02-14T09:55:53","indexId":"70011891","displayToPublicDate":"1982-01-01T00:00:00","publicationYear":"1982","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":738,"text":"American Mineralogist","active":true,"publicationSubtype":{"id":10}},"title":"Heat capacity and entropy of fayalite (Fe2SiO4) between 5.1 and 383 K: comparison of calorimetric and equilibrium valus for the QFM buffer reaction.","docAbstract":"At 298.15 K, 017Cop and So are 131.9 and 151.0 J/(mole.K). Also 045DELTA Hof,298 = -1478.17 and 045DELTA Gof,298 = -1378.98 kJ/mole. The temperature dependence of the equilibrium constant for the quartz - fayalite - magnetite buffer reaction is thus calculated.-K.A.R.","largerWorkType":{"id":2,"text":"Article"},"largerWorkTitle":"American Mineralogist","largerWorkSubtype":{"id":10,"text":"Journal Article"},"language":"English","publisher":"Mineralogical Society of America","issn":"0003004X","usgsCitation":"Robie, R.A., Finch, C., and Hemingway, B.S., 1982, Heat capacity and entropy of fayalite (Fe2SiO4) between 5.1 and 383 K: comparison of calorimetric and equilibrium valus for the QFM buffer reaction.: American Mineralogist, v. 67, no. 5-6, p. 463-469.","startPage":"463","endPage":"469","numberOfPages":"7","costCenters":[],"links":[{"id":221322,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"},{"id":267370,"type":{"id":11,"text":"Document"},"url":"https://www.minsocam.org/ammin/AM67/AM67_463.pdf"}],"volume":"67","issue":"5-6","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"505a2fefe4b0c8380cd5d210","contributors":{"authors":[{"text":"Robie, R. A.","contributorId":71237,"corporation":false,"usgs":true,"family":"Robie","given":"R.","email":"","middleInitial":"A.","affiliations":[],"preferred":false,"id":362224,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Finch, C.B.","contributorId":30361,"corporation":false,"usgs":true,"family":"Finch","given":"C.B.","email":"","affiliations":[],"preferred":false,"id":362223,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Hemingway, B. S.","contributorId":7268,"corporation":false,"usgs":true,"family":"Hemingway","given":"B.","email":"","middleInitial":"S.","affiliations":[],"preferred":false,"id":362222,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
]}