{"pageNumber":"5371","pageRowStart":"134250","pageSize":"25","recordCount":184769,"records":[{"id":70011667,"text":"70011667 - 1982 - Three FORTRAN programs for finite-difference solutions to binary diffusion in one and two phases with composition-and time-dependent diffusion coefficients","interactions":[],"lastModifiedDate":"2013-01-21T15:53:05","indexId":"70011667","displayToPublicDate":"1982-01-01T00:00:00","publicationYear":"1982","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1315,"text":"Computers & Geosciences","printIssn":"0098-3004","active":true,"publicationSubtype":{"id":10}},"title":"Three FORTRAN programs for finite-difference solutions to binary diffusion in one and two phases with composition-and time-dependent diffusion coefficients","docAbstract":"Geological examples of binary diffusion are numerous. They are potential indicators of the duration and rates of geological processes. Analytical solutions to the diffusion equations generally do not allow for variable diffusion coefficients, changing boundary conditions, and impingement of diffusion fields. The three programs presented here are based on Crank-Nicholson finite-difference approximations, which can take into account these complicating factors. Program 1 describes the diffusion of a component into an initially homogeneous phase that has a constant surface composition. Specifically it is written for Fe-Mg exchange in olivine at oxygen fugacities appropriate for the lunar crust, but other components, phases, or fugacities may be substituted by changing the values of the diffusion coefficient. Program 2 simulates the growth of exsolution lamellae. Program 3 describes the growth of reaction rims. These two programs are written for pseudobinary Ca-(Mg, Fe) exchange in pyroxenes. In all three programs, the diffusion coefficients and boundary conditions can be varied systematically with time. To enable users to employ widely different numerical values for diffusion coefficients and diffusion distance, the grid spacing in the space dimension and the increment by which the grid spacing in the time dimension is increased at each time step are input constants that can be varied each time the programs are run to yield a solution of the desired accuracy. ?? 1982.","largerWorkType":{"id":2,"text":"Article"},"largerWorkTitle":"Computers and Geosciences","largerWorkSubtype":{"id":10,"text":"Journal Article"},"language":"English","publisher":"Elsevier","publisherLocation":"Amsterdam, Netherlands","doi":"10.1016/0098-3004(82)90001-2","issn":"00983004","usgsCitation":"Sanford, R., 1982, Three FORTRAN programs for finite-difference solutions to binary diffusion in one and two phases with composition-and time-dependent diffusion coefficients: Computers & Geosciences, v. 8, no. 3-4, p. 235-263, https://doi.org/10.1016/0098-3004(82)90001-2.","startPage":"235","endPage":"263","numberOfPages":"29","costCenters":[],"links":[{"id":266195,"type":{"id":10,"text":"Digital Object Identifier"},"url":"https://dx.doi.org/10.1016/0098-3004(82)90001-2"},{"id":221685,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"8","issue":"3-4","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"505bb2ffe4b08c986b325b0c","contributors":{"authors":[{"text":"Sanford, R.F.","contributorId":38562,"corporation":false,"usgs":true,"family":"Sanford","given":"R.F.","email":"","affiliations":[],"preferred":false,"id":361660,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":70011671,"text":"70011671 - 1982 - Pyridine radical cation and its fluorine substituted derivatives","interactions":[],"lastModifiedDate":"2013-03-11T18:31:38","indexId":"70011671","displayToPublicDate":"1982-01-01T00:00:00","publicationYear":"1982","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":2207,"text":"Journal of Chemical Physics","active":true,"publicationSubtype":{"id":10}},"title":"Pyridine radical cation and its fluorine substituted derivatives","docAbstract":"The spectra and relaxation of the pyridine cation and of several of its fluorinated derivatives are studied in low temperature Ne matrices. The ions are generated by direct photoionization of the parent compounds. Of the compounds studied, laser induced → and → fluorescence is observed only for the 2, 6‐difluoropyridine cation. The analysis of the spectrum indicates that the ion is planar both in the  and  states. The large variety in the spectroscopic and relaxation behavior of fluoropyridine radical cations is explained in terms of their electronic structure and of the differential shifts of the individual electronic states caused by the fluorine substitution.","largerWorkType":{"id":2,"text":"Article"},"largerWorkTitle":"Journal of Chemical Physics","largerWorkSubtype":{"id":10,"text":"Journal Article"},"language":"English","publisher":"American Institute of Physics","doi":"10.1063/1.443723","issn":"00219606","usgsCitation":"Bondybey, V., English, J., and Shiley, R., 1982, Pyridine radical cation and its fluorine substituted derivatives: Journal of Chemical Physics, v. 77, no. 10, p. 4826-4831, https://doi.org/10.1063/1.443723.","startPage":"4826","endPage":"4831","numberOfPages":"6","costCenters":[],"links":[{"id":480265,"rank":1,"type":{"id":40,"text":"Open Access Publisher Index Page"},"url":"https://doi.org/10.1063/1.443723","text":"Publisher Index Page"},{"id":220715,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"},{"id":269081,"type":{"id":10,"text":"Digital Object Identifier"},"url":"https://dx.doi.org/10.1063/1.443723"}],"volume":"77","issue":"10","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"505a9051e4b0c8380cd7fc77","contributors":{"authors":[{"text":"Bondybey, V.E.","contributorId":74879,"corporation":false,"usgs":true,"family":"Bondybey","given":"V.E.","email":"","affiliations":[],"preferred":false,"id":361676,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"English, J.H.","contributorId":28746,"corporation":false,"usgs":true,"family":"English","given":"J.H.","email":"","affiliations":[],"preferred":false,"id":361674,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Shiley, R.H.","contributorId":44282,"corporation":false,"usgs":true,"family":"Shiley","given":"R.H.","email":"","affiliations":[],"preferred":false,"id":361675,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":1013612,"text":"1013612 - 1982 - Immunosuppression induced by a corticosteroid of an alkylating agent in rainbow trout (Salmo gairdneri) administered in a Yersinia ruckeri bacterin","interactions":[],"lastModifiedDate":"2012-02-02T00:04:30","indexId":"1013612","displayToPublicDate":"1982-01-01T00:00:00","publicationYear":"1982","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1383,"text":"Developmental and Comparative Immunology","active":true,"publicationSubtype":{"id":10}},"title":"Immunosuppression induced by a corticosteroid of an alkylating agent in rainbow trout (Salmo gairdneri) administered in a Yersinia ruckeri bacterin","largerWorkType":{"id":2,"text":"Article"},"largerWorkTitle":"Developmental and Comparative Immunology","largerWorkSubtype":{"id":10,"text":"Journal Article"},"language":"English","collaboration":"457/FH","usgsCitation":"Anderson, D.P., Roberson, B., and Dixon, O.W., 1982, Immunosuppression induced by a corticosteroid of an alkylating agent in rainbow trout (Salmo gairdneri) administered in a Yersinia ruckeri bacterin: Developmental and Comparative Immunology, p. 197-204.","productDescription":"p. 197-204","startPage":"197","endPage":"204","numberOfPages":"8","costCenters":[{"id":365,"text":"Leetown Science Center","active":true,"usgs":true}],"links":[{"id":132100,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a09e4b07f02db5fa9d5","contributors":{"authors":[{"text":"Anderson, D. P.","contributorId":32469,"corporation":false,"usgs":true,"family":"Anderson","given":"D.","email":"","middleInitial":"P.","affiliations":[],"preferred":false,"id":318857,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Roberson, B.S.","contributorId":103986,"corporation":false,"usgs":true,"family":"Roberson","given":"B.S.","email":"","affiliations":[],"preferred":false,"id":318859,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Dixon, O. W.","contributorId":101588,"corporation":false,"usgs":true,"family":"Dixon","given":"O.","email":"","middleInitial":"W.","affiliations":[],"preferred":false,"id":318858,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":1013762,"text":"1013762 - 1982 - Gross and histological signs of dietary deficiencies of biotin and pantothenic acid in lake trout, Salvelinus namaycush","interactions":[],"lastModifiedDate":"2012-02-02T00:04:10","indexId":"1013762","displayToPublicDate":"1982-01-01T00:00:00","publicationYear":"1982","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1340,"text":"Cornell Veterinarian","active":true,"publicationSubtype":{"id":10}},"title":"Gross and histological signs of dietary deficiencies of biotin and pantothenic acid in lake trout, Salvelinus namaycush","largerWorkType":{"id":2,"text":"Article"},"largerWorkTitle":"Cornell Veterinarian","largerWorkSubtype":{"id":10,"text":"Journal Article"},"language":"English","collaboration":"None/TL","usgsCitation":"Poston, H.A., and Page, J.W., 1982, Gross and histological signs of dietary deficiencies of biotin and pantothenic acid in lake trout, Salvelinus namaycush: Cornell Veterinarian, v. 72, no. 3, p. 242-261.","productDescription":"p. 242-261","startPage":"242","endPage":"261","numberOfPages":"20","costCenters":[{"id":365,"text":"Leetown Science Center","active":true,"usgs":true}],"links":[{"id":129292,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"72","issue":"3","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ab1e4b07f02db66de94","contributors":{"authors":[{"text":"Poston, H. A.","contributorId":21893,"corporation":false,"usgs":true,"family":"Poston","given":"H.","email":"","middleInitial":"A.","affiliations":[],"preferred":false,"id":319209,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Page, J. W.","contributorId":28559,"corporation":false,"usgs":true,"family":"Page","given":"J.","middleInitial":"W.","affiliations":[],"preferred":false,"id":319210,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":1013733,"text":"1013733 - 1982 - Plasma corticosteroids and chlorides in striped bass exposed to tricaine methanesulfonate, quinaldine, etomidate, and salt","interactions":[],"lastModifiedDate":"2025-08-08T15:55:38.457028","indexId":"1013733","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":"Plasma corticosteroids and chlorides in striped bass exposed to tricaine methanesulfonate, quinaldine, etomidate, and salt","docAbstract":"<p><span>Plasma chloride and corticosteroid concentrations were measured in yearling striped bass (Morone saxatilis) exposed to 25 mg/L tricaine methanesulfonate, 2.5 mg/L quinaldine, or 0.1 mg/L etomidate (an experimental drug), alone and in combination with 10 g/L salt (NaCl). Plasma chloride levels were unaffected in all treatments during a 15‐min exposure and during a 10‐min period of close confinement in a dipnet. Plasma corticosteroids increased in fish exposed to salt alone and in fish exposed to tricaine methanesulfonate or quinaldine, either alone or in combination with salt. Etomidate alone or combined with salt limited the increase in plasma corticosteroids during exposure and confinement. Etomidate appears to be a useful drug for suppressing physiological changes during the handling and transportation of striped bass.</span></p>","language":"English","publisher":"Oxford Academic","doi":"10.1577/1548-8659(1982)44[205:PCACIS]2.0.CO;2","usgsCitation":"Davis, K.B., Parker, N., and Suttle, M.A., 1982, Plasma corticosteroids and chlorides in striped bass exposed to tricaine methanesulfonate, quinaldine, etomidate, and salt: Progressive Fish-Culturist, v. 44, no. 4, p. 205-207, https://doi.org/10.1577/1548-8659(1982)44[205:PCACIS]2.0.CO;2.","productDescription":"3 p.","startPage":"205","endPage":"207","numberOfPages":"3","costCenters":[{"id":365,"text":"Leetown Science Center","active":true,"usgs":true}],"links":[{"id":130012,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"44","issue":"4","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ad9e4b07f02db684ff0","contributors":{"authors":[{"text":"Davis, K. B.","contributorId":83869,"corporation":false,"usgs":true,"family":"Davis","given":"K.","email":"","middleInitial":"B.","affiliations":[],"preferred":false,"id":319159,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Parker, N. C.","contributorId":101209,"corporation":false,"usgs":true,"family":"Parker","given":"N. C.","affiliations":[],"preferred":false,"id":319160,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Suttle, M. A.","contributorId":54926,"corporation":false,"usgs":true,"family":"Suttle","given":"M.","email":"","middleInitial":"A.","affiliations":[],"preferred":false,"id":319158,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":1013712,"text":"1013712 - 1982 - Influence of the eyes and pineal gland on gonadal development and Spawning in channel catfish, Ictalurus punctatus","interactions":[],"lastModifiedDate":"2012-02-02T00:04:10","indexId":"1013712","displayToPublicDate":"1982-01-01T00:00:00","publicationYear":"1982","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":749,"text":"American Zoologist","active":true,"publicationSubtype":{"id":10}},"title":"Influence of the eyes and pineal gland on gonadal development and Spawning in channel catfish, Ictalurus punctatus","largerWorkType":{"id":2,"text":"Article"},"largerWorkTitle":"American Zoologist","largerWorkSubtype":{"id":10,"text":"Journal Article"},"language":"English","collaboration":"None/SE","usgsCitation":"Davis, K.B., Simco, B., Goudie, C.A., and Parker, N., 1982, Influence of the eyes and pineal gland on gonadal development and Spawning in channel catfish, Ictalurus punctatus: American Zoologist, v. 22, no. 4.","productDescription":"864 p.","startPage":"864","numberOfPages":"864","costCenters":[{"id":365,"text":"Leetown Science Center","active":true,"usgs":true}],"links":[{"id":129675,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"22","issue":"4","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e49f1e4b07f02db5ee7d0","contributors":{"authors":[{"text":"Davis, K. B.","contributorId":83869,"corporation":false,"usgs":true,"family":"Davis","given":"K.","email":"","middleInitial":"B.","affiliations":[],"preferred":false,"id":319101,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Simco, B.A.","contributorId":101216,"corporation":false,"usgs":true,"family":"Simco","given":"B.A.","email":"","affiliations":[],"preferred":false,"id":319104,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Goudie, C. A.","contributorId":97851,"corporation":false,"usgs":false,"family":"Goudie","given":"C.","email":"","middleInitial":"A.","affiliations":[],"preferred":false,"id":319102,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Parker, N. C.","contributorId":101209,"corporation":false,"usgs":true,"family":"Parker","given":"N. C.","affiliations":[],"preferred":false,"id":319103,"contributorType":{"id":1,"text":"Authors"},"rank":4}]}}
,{"id":70011749,"text":"70011749 - 1982 - Accumulation rates of Th-230, Pa-231, and some transition metals on the Bermuda Rise","interactions":[],"lastModifiedDate":"2024-03-18T14:15:55.23402","indexId":"70011749","displayToPublicDate":"1982-01-01T00:00:00","publicationYear":"1982","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1759,"text":"Geochimica et Cosmochimica Acta","active":true,"publicationSubtype":{"id":10}},"title":"Accumulation rates of Th-230, Pa-231, and some transition metals on the Bermuda Rise","docAbstract":"<p><span>Measurements of&nbsp;</span><sup>238</sup><span>U,&nbsp;</span><sup>234</sup><span>U,&nbsp;</span><sup>230</sup><span>Th,&nbsp;</span><sup>232</sup><span>Th,&nbsp;</span><sup>231</sup><span>Pa, Mn, Fe, Co, Ni, Cu, and Zn were made on 23 samples from core GPC-5, a 29-m giant piston core from a water depth of 4583 m on the northeastern Bermuda Rise (33°41.2′N, 57°36.9′W). This area is characterized by rapid deposition of sediment transported by abyssal currents. Unsupported&nbsp;</span><sup>230</sup><span>Th and&nbsp;</span><sup>231</sup><span>Pa are present throughout the core but, because of large variations in the sedimentation rate, show marked departures from exponential decay with depth. The trend with depth of the&nbsp;</span><span class=\"math\"><span id=\"MathJax-Element-1-Frame\" class=\"MathJax_SVG\" data-mathml=\"<math xmlns=&quot;http://www.w3.org/1998/Math/MathML&quot;><msup><mi></mi><mn>231</mn></msup><mtext>Pa</mtext><msub><mi></mi><mn>ex</mn></msub><msup><mi></mi><mn>230</mn></msup><mtext>Th</mtext><msub><mi></mi><mn>ex</mn></msub></math>\"><span class=\"MJX_Assistive_MathML\"><sup>231</sup>Pa<sub>ex</sub><sup>230</sup>Th<sub>ex</sub></span></span></span><span>&nbsp;ratio is consistent with the average accumulation rate of 36 cm/1000 y reported earlier on the basis of radiocarbon dating and CaCO</span><sub>3</sub><span>&nbsp;stratigraphy. When expressed on a carbonate-free basis, concentrations of Mn, Co, Ni, Cu, Zn,&nbsp;</span><sup>230</sup><span>Th</span><sub>ex</sub><span>, and&nbsp;</span><sup>231</sup><span>Pa</span><sub>ex</sub><span>&nbsp;all show cyclic variations positively correlated with those of CaCO</span><sub>3</sub><span>. The correlations can be explained by a model in which all of these constituents, including CaCO</span><sub>3</sub><span>, are supplied to the sediments from the water column at a constant rate. Concentration variations are controlled mainly by varying inputs of terrigenous detritus, with low inputs occurring during interglacials and high inputs during glacials. Relationships between the metal and&nbsp;</span><sup>230</sup><span>Th</span><sub>ex</sub><span>&nbsp;concentrations permit estimates of the rates at which the metals are removed to the sediment by scavenging from the water column. The results, in μg/cm</span><sup>2</sup><span>-1000 y, are: 4300 ± 1100 for Mn, 46 ± 16 for Ni and 76 ± 26 for Cu. These rates are somewhat larger than ocean-wide averages estimated by other methods, and the absolute rate of&nbsp;</span><sup>230</sup><span>Th accumulation in GPC-5 averages about nine times higher than production in the overlying water column. This part of the Bermuda Rise and similar bottom-current deposits may act as important accumulators of elements scavenged from seawater.</span></p>","language":"English","publisher":"Elsevier","doi":"10.1016/0016-7037(82)90166-1","issn":"00167037","usgsCitation":"Bacon, M., and Rosholt, J., 1982, Accumulation rates of Th-230, Pa-231, and some transition metals on the Bermuda Rise: Geochimica et Cosmochimica Acta, v. 46, no. 4, p. 651-666, https://doi.org/10.1016/0016-7037(82)90166-1.","productDescription":"16 p.","startPage":"651","endPage":"666","numberOfPages":"16","costCenters":[],"links":[{"id":221194,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"46","issue":"4","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"5059e685e4b0c8380cd4747d","contributors":{"authors":[{"text":"Bacon, M.P.","contributorId":76069,"corporation":false,"usgs":false,"family":"Bacon","given":"M.P.","email":"","affiliations":[{"id":6706,"text":"Woods Hole Oceanographic Institution,","active":true,"usgs":false}],"preferred":false,"id":361869,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Rosholt, J.N.","contributorId":37749,"corporation":false,"usgs":true,"family":"Rosholt","given":"J.N.","email":"","affiliations":[],"preferred":false,"id":361868,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":70011750,"text":"70011750 - 1982 - Laboratory measurements of reservoir rock from the Geysers geothermal field, California","interactions":[],"lastModifiedDate":"2013-01-18T13:20:42","indexId":"70011750","displayToPublicDate":"1982-01-01T00:00:00","publicationYear":"1982","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":2071,"text":"International Journal of Rock Mechanics and Mining Sciences & Geomechanics Abstracts","active":true,"publicationSubtype":{"id":10}},"title":"Laboratory measurements of reservoir rock from the Geysers geothermal field, California","docAbstract":"Rock samples taken from two outcrops, as well as rare cores from three well bores at the Geysers geothermal field, California, were tested at temperatures and pressures similar to those found in the geothermal field. Both intact and 30?? sawcut cylinders were deformed at confining pressures of 200-1000 bars, pore pressure of 30 bars and temperatures of 150?? and 240??C. Thin-section and X-ray analysis revealed that some borehole samples had undergone extensive alteration and recrystallization. Constant strain rate tests of 10-4 and 10-6 per sec gave a coefficient of friction of 0.68. Due to the highly fractured nature of the rocks taken from the production zone, intact samples were rarely 50% stronger than the frictional strength. This result suggests that the Geysers reservoir can support shear stresses only as large as its frictional shear strength. Velocity of p-waves (6.2 km/sec) was measured on one sample. Acoustic emission and sliding on a sawcut were related to changes in pore pressure. b-values computed from the acoustic emissions generated during fluid injection were typically about 0.55. An unusually high b-value (approximately 1.3) observed during sudden injection of water into the sample may have been related to thermal cracking. ?? 1982.","largerWorkType":{"id":2,"text":"Article"},"largerWorkTitle":"International Journal of Rock Mechanics and Mining Sciences & Geomechanics Abstracts","largerWorkSubtype":{"id":10,"text":"Journal Article"},"language":"English","publisher":"Elsevier","doi":"10.1016/0148-9062(82)91632-1","issn":"01489062","usgsCitation":"Lockner, D., Summers, R., Moore, D., and Byerlee, J., 1982, Laboratory measurements of reservoir rock from the Geysers geothermal field, California: International Journal of Rock Mechanics and Mining Sciences & Geomechanics Abstracts, v. 19, no. 2, p. 65-80, https://doi.org/10.1016/0148-9062(82)91632-1.","productDescription":"p.65-80","startPage":"65","endPage":"80","numberOfPages":"16","costCenters":[],"links":[{"id":265944,"type":{"id":10,"text":"Digital Object Identifier"},"url":"https://dx.doi.org/10.1016/0148-9062(82)91632-1"},{"id":221195,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"19","issue":"2","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"505a4112e4b0c8380cd65289","contributors":{"authors":[{"text":"Lockner, D.A. 0000-0001-8630-6833","orcid":"https://orcid.org/0000-0001-8630-6833","contributorId":85603,"corporation":false,"usgs":true,"family":"Lockner","given":"D.A.","affiliations":[],"preferred":false,"id":361872,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Summers, R.","contributorId":65483,"corporation":false,"usgs":true,"family":"Summers","given":"R.","email":"","affiliations":[],"preferred":false,"id":361870,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Moore, D.","contributorId":105307,"corporation":false,"usgs":true,"family":"Moore","given":"D.","affiliations":[],"preferred":false,"id":361873,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Byerlee, J.D.","contributorId":69982,"corporation":false,"usgs":true,"family":"Byerlee","given":"J.D.","affiliations":[],"preferred":false,"id":361871,"contributorType":{"id":1,"text":"Authors"},"rank":4}]}}
,{"id":70011751,"text":"70011751 - 1982 - Variation in sand body types on the eastern Bering Sea epicontinental shelf.","interactions":[],"lastModifiedDate":"2012-03-12T17:18:27","indexId":"70011751","displayToPublicDate":"1982-01-01T00:00:00","publicationYear":"1982","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1794,"text":"Geologie en Mijnbouw","active":true,"publicationSubtype":{"id":10}},"title":"Variation in sand body types on the eastern Bering Sea epicontinental shelf.","docAbstract":"The eastern epicontinental shelf of the Bering Sea is characterized by variations in river and glacial sediment supply, wave energy, tidal range (microtidal to mesotidal), and tidal, geostrophic, and storm-induced currents. These factors, combined with the effect of the Holocene rise in sea level, have resulted in the formation of a complex assemblage of generally linear sand bodies of similar morphology anad lithology, but different origins. The sand bodies are large features found from the present shoreline to tens of kilometers offshore, in water depths up to 50m. -from Authors","largerWorkType":{"id":2,"text":"Article"},"largerWorkTitle":"Geologie en Mijnbouw","largerWorkSubtype":{"id":10,"text":"Journal Article"},"language":"English","usgsCitation":"Nelson, C., Dupre, W., Field, M., and Howard, J., 1982, Variation in sand body types on the eastern Bering Sea epicontinental shelf.: Geologie en Mijnbouw, v. 61, no. 1, p. 37-48.","startPage":"37","endPage":"48","numberOfPages":"12","costCenters":[],"links":[{"id":221196,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"61","issue":"1","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"505bc164e4b08c986b32a555","contributors":{"authors":[{"text":"Nelson, C.H.","contributorId":88346,"corporation":false,"usgs":true,"family":"Nelson","given":"C.H.","email":"","affiliations":[],"preferred":false,"id":361876,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Dupre, W.R.","contributorId":57540,"corporation":false,"usgs":true,"family":"Dupre","given":"W.R.","email":"","affiliations":[],"preferred":false,"id":361875,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Field, M.E.","contributorId":27052,"corporation":false,"usgs":true,"family":"Field","given":"M.E.","affiliations":[],"preferred":false,"id":361874,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Howard, J.D.","contributorId":103413,"corporation":false,"usgs":true,"family":"Howard","given":"J.D.","email":"","affiliations":[],"preferred":false,"id":361877,"contributorType":{"id":1,"text":"Authors"},"rank":4}]}}
,{"id":70011752,"text":"70011752 - 1982 - Solidification of basaltic magma during flow in a dike","interactions":[],"lastModifiedDate":"2023-02-08T17:49:26.619179","indexId":"70011752","displayToPublicDate":"1982-01-01T00:00:00","publicationYear":"1982","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":732,"text":"American Journal of Science","active":true,"publicationSubtype":{"id":10}},"title":"Solidification of basaltic magma during flow in a dike","docAbstract":"<p>No abstract available.</p>","language":"English","publisher":"American Journal of Science","doi":"10.2475/ajs.282.6.856","usgsCitation":"Delaney, P.T., and Pollard, D.D., 1982, Solidification of basaltic magma during flow in a dike: American Journal of Science, v. 282, no. 6, p. 856-885, https://doi.org/10.2475/ajs.282.6.856.","productDescription":"30 p.","startPage":"856","endPage":"885","numberOfPages":"30","costCenters":[],"links":[{"id":221197,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"282","issue":"6","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"505b923fe4b08c986b319db0","contributors":{"authors":[{"text":"Delaney, Paul T.","contributorId":15195,"corporation":false,"usgs":true,"family":"Delaney","given":"Paul","email":"","middleInitial":"T.","affiliations":[],"preferred":false,"id":361878,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Pollard, David D.","contributorId":38549,"corporation":false,"usgs":true,"family":"Pollard","given":"David","email":"","middleInitial":"D.","affiliations":[],"preferred":false,"id":361879,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":70011763,"text":"70011763 - 1982 - Unroofing history of a suture zone in the Himalaya of Pakistan by means of fission-track annealing ages","interactions":[],"lastModifiedDate":"2023-12-12T23:16:46.276496","indexId":"70011763","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":"Unroofing history of a suture zone in the Himalaya of Pakistan by means of fission-track annealing ages","docAbstract":"<div id=\"abstracts\" class=\"Abstracts u-font-serif text-s\"><div id=\"ab1\" class=\"abstract author\" lang=\"en\"><div id=\"aep-abstract-sec-id5\"><p>The uplift history of the Swat Valley and Hazara region of northwestern Pakistan has been established using 22 fission-track dates on apatite, zircon and sphene. A major fault, the Main Mantle Thrust (MMT) strikes east-west across the Swat Valley, separates regions of markedly differing fission-track age regimesm, and may be a suture zone separating an extinct island arc terrane on the north from the Indian plate to the south. Fission-track ages ranging from about 55 to 58 m.y. for sphene, 18 to 53 m.y. for zircon, and 9 to 17 m.y. for apatite were obtained from the region north of the MMT. To the south the fission-track age ranges are 20 to 25 m.y. for sphene, 17 to 26 m.y. for zircon, and 16 to 23 m.y. for apatite. Disparate zircon and sphene ages on each side of the MMT imply different cooling histories for each side of the fault prior to 15 m.y. Similar apatite ages on both sides of the fault imply similar cooling histories during the past 15 m.y. This may indicate that faulting ceased by 15 m.y. Mean uplift rates have been derived from the fission-track data using mainly the mineral-pair method. Uplift rates in the region north of the MMT increased from 0.07 to 0.20 mm/yr during the period 55 to 15 m.y. South of the fault, uplift rates averaged in excess of 0.70 mm/yr for the period 25 to 15 m.y. During the past 15 m.y. uplift across the MMT in the Swat Valley showsno discontinuities, ranging from 0.16 mm/yr in the south to 0.39 mm/yr in the north. A plausible interpretation for the fission-track uplift data has the MMT verging to the south with overthrusting taking place at a depth between 3.5 and 6.0 km, juxtaposing two terranes that were originally separated by a substantial, but unknown distance. In this model, regional uplift followed cessation of faulting just prior to 15 m.y.</p></div></div></div>","language":"English","publisher":"Elsevier","doi":"10.1016/0012-821X(82)90187-X","issn":"0012821X","usgsCitation":"Zeitler, P., Tahirkheli, R., Naeser, C.W., and Johnson, N., 1982, Unroofing history of a suture zone in the Himalaya of Pakistan by means of fission-track annealing ages: Earth and Planetary Science Letters, v. 57, no. 1, p. 227-240, https://doi.org/10.1016/0012-821X(82)90187-X.","productDescription":"14 p.","startPage":"227","endPage":"240","numberOfPages":"14","costCenters":[],"links":[{"id":221389,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"Pakistan","geographicExtents":"{\"type\":\"FeatureCollection\",\"features\":[{\"type\":\"Feature\",\"geometry\":{\"type\":\"Polygon\",\"coordinates\":[[[75.15803,37.13303],[75.8969,36.66681],[76.19285,35.8984],[77.83745,35.49401],[76.87172,34.65354],[75.75706,34.50492],[74.2402,34.74889],[73.74995,34.3177],[74.10429,33.44147],[74.45156,32.7649],[75.25864,32.27111],[74.40593,31.69264],[74.42138,30.97981],[73.45064,29.97641],[72.82375,28.96159],[71.77767,27.91318],[70.6165,27.9892],[69.51439,26.94097],[70.16893,26.49187],[70.28287,25.72223],[70.8447,25.2151],[71.04324,24.35652],[68.8426,24.35913],[68.17665,23.69197],[67.44367,23.94484],[67.14544,24.66361],[66.37283,25.42514],[64.53041,25.23704],[62.9057,25.21841],[61.49736,25.07824],[61.87419,26.23997],[63.31663,26.75653],[63.2339,27.21705],[62.75543,27.37892],[62.72783,28.25964],[61.77187,28.69933],[61.36931,29.30328],[60.87425,29.82924],[62.54986,29.31857],[63.55026,29.46833],[64.148,29.34082],[64.35042,29.56003],[65.04686,29.47218],[66.34647,29.88794],[66.38146,30.7389],[66.93889,31.30491],[67.68339,31.30315],[67.79269,31.58293],[68.55693,31.71331],[68.92668,31.62019],[69.31776,31.90141],[69.26252,32.50194],[69.68715,33.1055],[70.32359,33.35853],[69.93054,34.02012],[70.8818,33.98886],[71.15677,34.34891],[71.11502,34.73313],[71.61308,35.1532],[71.49877,35.65056],[71.26235,36.07439],[71.84629,36.50994],[72.92002,36.72001],[74.06755,36.83618],[74.57589,37.02084],[75.15803,37.13303]]]},\"properties\":{\"name\":\"Pakistan\"}}]}","volume":"57","issue":"1","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"505bbcefe4b08c986b328e5a","contributors":{"authors":[{"text":"Zeitler, P.K.","contributorId":49513,"corporation":false,"usgs":true,"family":"Zeitler","given":"P.K.","email":"","affiliations":[],"preferred":false,"id":361906,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Tahirkheli, R.A.K.","contributorId":37889,"corporation":false,"usgs":true,"family":"Tahirkheli","given":"R.A.K.","email":"","affiliations":[],"preferred":false,"id":361905,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Naeser, C. W.","contributorId":17582,"corporation":false,"usgs":true,"family":"Naeser","given":"C.","middleInitial":"W.","affiliations":[],"preferred":false,"id":361904,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Johnson, N.M.","contributorId":105429,"corporation":false,"usgs":true,"family":"Johnson","given":"N.M.","email":"","affiliations":[],"preferred":false,"id":361907,"contributorType":{"id":1,"text":"Authors"},"rank":4}]}}
,{"id":70011764,"text":"70011764 - 1982 - Geochemical indices of fine sediment transport, northwest Gulf of Mexico","interactions":[],"lastModifiedDate":"2024-05-21T23:46:01.539707","indexId":"70011764","displayToPublicDate":"1982-01-01T00:00:00","publicationYear":"1982","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":2450,"text":"Journal of Sedimentary Petrology","active":true,"publicationSubtype":{"id":10}},"title":"Geochemical indices of fine sediment transport, northwest Gulf of Mexico","docAbstract":"<div><div id=\"12458437\" class=\"article-section-wrapper js-article-section js-content-section  \" data-section-parent-id=\"0\"><p>The<span>&nbsp;</span><sup>210</sup><span>&nbsp;</span>Pb distribution, the clay mineralogy distribution, and the distribution of three trace metals, barium, lead, and manganese, in the sediments of the south Texas shelf are related to the dynamics of the sedimentary transport process.<span>&nbsp;</span><sup>210</sup><span>&nbsp;</span>Pb, whose concentration is time dependent, defines three loci of recent sediment accumulations. In addition, the variation of<span>&nbsp;</span><sup>210</sup><span>&nbsp;</span>Pb activity at the sediment-water interface delineates areas of terrestrial sedimentation from hemipelagic sedimentation. The clay mineralogy composition of the bottom and suspended sediments assists in defining the origin of the persistent nepheloid layer and bottom sediment. Barium, a major element used in drilling mud, tags sediment movement from areas of hydrocarbon exploration. Lead concentrations, anthropogenically introduced from urban areas, tag the sediment derived from the metropolitan complexes of coastal Texas. Manganese, because of diagenic mobilization, is concentrated in areas of very slow sediment accumulation. The distribution of these geochemical properties of the sediment are in direct response to the sediment regime of the shelf. Based on this data, a model of sediment transport and deposition which relates currents, wind, tides, sediment flux, and precipitation has been formulated. This model differs from the \"advective\" transport or convergent current schemes previously proposed for this shelf.</p></div></div>","language":"English","publisher":"SEPM","doi":"10.1306/212F7F3B-2B24-11D7-8648000102C1865D","issn":"00224472","usgsCitation":"Holmes, C.W., 1982, Geochemical indices of fine sediment transport, northwest Gulf of Mexico: Journal of Sedimentary Petrology, v. 52, no. 1, p. 307-321, https://doi.org/10.1306/212F7F3B-2B24-11D7-8648000102C1865D.","productDescription":"15 p.","startPage":"307","endPage":"321","numberOfPages":"15","costCenters":[],"links":[{"id":221390,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"52","issue":"1","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"505a1644e4b0c8380cd550f5","contributors":{"authors":[{"text":"Holmes, C. W.","contributorId":36076,"corporation":false,"usgs":true,"family":"Holmes","given":"C.","email":"","middleInitial":"W.","affiliations":[],"preferred":false,"id":361908,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":70011765,"text":"70011765 - 1982 - Late Pleistocene- Holocene transgressive sedimentation in deltaic and non-deltaic areas of the northeastern Bering epicontinental shelf.","interactions":[],"lastModifiedDate":"2012-03-12T17:18:32","indexId":"70011765","displayToPublicDate":"1982-01-01T00:00:00","publicationYear":"1982","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1794,"text":"Geologie en Mijnbouw","active":true,"publicationSubtype":{"id":10}},"title":"Late Pleistocene- Holocene transgressive sedimentation in deltaic and non-deltaic areas of the northeastern Bering epicontinental shelf.","docAbstract":"The distribution of late Pleistocene and Holocene surface sediments on the northern Bering Seafloor is patchy and dependent upon locations of seafloor bedrock and pre-late Pleistocene glacial debris, late Holocene river sediment influx, and modern strong bottom currents. Seafloor vibracores and high-resolution profiles record two different sedimentary environments in the northern Bering shelf: late Pleistocene-Holocene shoreline transgression in Chirikov Basin, and Holocene deposition from the Yukon River in Norton Sound.-from Author","largerWorkType":{"id":2,"text":"Article"},"largerWorkTitle":"Geologie en Mijnbouw","largerWorkSubtype":{"id":10,"text":"Journal Article"},"language":"English","usgsCitation":"Nelson, C., 1982, Late Pleistocene- Holocene transgressive sedimentation in deltaic and non-deltaic areas of the northeastern Bering epicontinental shelf.: Geologie en Mijnbouw, v. 61, no. 1, p. 5-18.","startPage":"5","endPage":"18","numberOfPages":"14","costCenters":[],"links":[{"id":221467,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"61","issue":"1","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"505a451ae4b0c8380cd67037","contributors":{"authors":[{"text":"Nelson, C.H.","contributorId":88346,"corporation":false,"usgs":true,"family":"Nelson","given":"C.H.","email":"","affiliations":[],"preferred":false,"id":361909,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":70011766,"text":"70011766 - 1982 - Interfingering of the Frontier Formation and Aspen Shale, Cumberland Gap, Wyoming.","interactions":[],"lastModifiedDate":"2012-03-12T17:18:32","indexId":"70011766","displayToPublicDate":"1982-01-01T00:00:00","publicationYear":"1982","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":2789,"text":"Mountain Geologist","active":true,"publicationSubtype":{"id":10}},"title":"Interfingering of the Frontier Formation and Aspen Shale, Cumberland Gap, Wyoming.","docAbstract":"The basal part, or the Chalk Creek Member, of the non-marine lower Frontier Formation (Upper Cretaceous) includes a thin coal bed that grades S into a carbonaceous shale. The latter plus associated sandstones and shales pinch out S of Cumberland Gap and lie stratigraphically below the top of the Aspen Shale. The beds in the upper part of the Aspen, in turn, pinch out within the Frontier Formation. The coal bed and equivalent carbonaceous shale represent in-place accumulation of peat. The interfingering suggests that in SW Wyoming the Lower/Upper Cretaceous boundary is within the Chalk Creek Member. -from Author","largerWorkType":{"id":2,"text":"Article"},"largerWorkTitle":"Mountain Geologist","largerWorkSubtype":{"id":10,"text":"Journal Article"},"language":"English","issn":"0027254X","usgsCitation":"M'gonigle, J., 1982, Interfingering of the Frontier Formation and Aspen Shale, Cumberland Gap, Wyoming.: Mountain Geologist, v. 19, no. 2, p. 59-61.","startPage":"59","endPage":"61","numberOfPages":"3","costCenters":[],"links":[{"id":221468,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"19","issue":"2","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"505a3d01e4b0c8380cd6320c","contributors":{"authors":[{"text":"M'gonigle, J.","contributorId":63165,"corporation":false,"usgs":true,"family":"M'gonigle","given":"J.","affiliations":[],"preferred":false,"id":361910,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":70011781,"text":"70011781 - 1982 - Geology of continental shelf, Onslow Bay, North Carolina, as revealed by submarine outcrops","interactions":[],"lastModifiedDate":"2023-01-11T16:49:27.167622","indexId":"70011781","displayToPublicDate":"1982-01-01T00:00:00","publicationYear":"1982","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":701,"text":"American Association of Petroleum Geologists Bulletin","active":true,"publicationSubtype":{"id":10}},"title":"Geology of continental shelf, Onslow Bay, North Carolina, as revealed by submarine outcrops","docAbstract":"Lithologic and stratigraphic data from rocks dredged from the continental shelf off Onslow Bay, North Carolina, provide surface control for seismic studies of the southeastern United States continental margin and help to explain the distribution of potentially economic phosphate-rich sediments on this shelf. Outcropping Miocene rocks in this area indicate that the region has long been a positive geologic feature and has received relatively little Pliocene and Pleistocene sedimentation. -from Authors","language":"English","publisher":"American Association of Petroleum Geologists","doi":"10.1306/03B59A1C-16D1-11D7-8645000102C1865D","usgsCitation":"Blackwelder, B.W., Macintyre, I.G., and Pilkey, O.H., 1982, Geology of continental shelf, Onslow Bay, North Carolina, as revealed by submarine outcrops: American Association of Petroleum Geologists Bulletin, v. 66, no. 1, p. 44-56, https://doi.org/10.1306/03B59A1C-16D1-11D7-8645000102C1865D.","productDescription":"13 p.","startPage":"44","endPage":"56","numberOfPages":"13","costCenters":[],"links":[{"id":221695,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United States","state":"North Carolina","otherGeospatial":"Onslow Bay","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"coordinates\": [\n          [\n            [\n              -76.44373147728382,\n              34.79157094249153\n            ],\n            [\n              -78.03355465391473,\n              34.79157094249153\n            ],\n            [\n              -78.03355465391473,\n              33.75214968374051\n            ],\n            [\n              -76.44373147728382,\n              33.75214968374051\n            ],\n            [\n              -76.44373147728382,\n              34.79157094249153\n            ]\n          ]\n        ],\n        \"type\": \"Polygon\"\n      }\n    }\n  ]\n}","volume":"66","issue":"1","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"505a24bee4b0c8380cd58352","contributors":{"authors":[{"text":"Blackwelder, Blake W.","contributorId":56640,"corporation":false,"usgs":true,"family":"Blackwelder","given":"Blake","email":"","middleInitial":"W.","affiliations":[],"preferred":false,"id":361947,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Macintyre, Ian G.","contributorId":94037,"corporation":false,"usgs":true,"family":"Macintyre","given":"Ian","email":"","middleInitial":"G.","affiliations":[],"preferred":false,"id":361946,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Pilkey, Orrin H.","contributorId":11606,"corporation":false,"usgs":true,"family":"Pilkey","given":"Orrin","email":"","middleInitial":"H.","affiliations":[],"preferred":false,"id":361948,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":70011784,"text":"70011784 - 1982 - Geotechnical characteristics of bottom sediments in the northeastern Bering Sea.","interactions":[],"lastModifiedDate":"2012-03-12T17:19:03","indexId":"70011784","displayToPublicDate":"1982-01-01T00:00:00","publicationYear":"1982","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1794,"text":"Geologie en Mijnbouw","active":true,"publicationSubtype":{"id":10}},"title":"Geotechnical characteristics of bottom sediments in the northeastern Bering Sea.","docAbstract":"Sediment of Holocene age derived from the Yukon River, consisting dominantly of silty fine sand and sandy silt, covers the bottom of central and western Norton Sound, which is a high energy environment involving extensive ice loading, high waves, and strong bottom currents. The sediment characteristics indicate that it is susceptible to liquefaction during major storms. Substantially finer grained, weak and highly compressible sediment of Holocene age covers eastern Norton Sound and the Port Clarence embayment, which are low energy environments. Pleistocene peaty deposits underlie the Holocene and late Pleistocene deposits in both Norton Sound and Chirikov Basin and are somewhat overconsolidated. The presence of gas indicates high in situ pore pressure and hence low material strength.-from Authors","largerWorkType":{"id":2,"text":"Article"},"largerWorkTitle":"Geologie en Mijnbouw","largerWorkSubtype":{"id":10,"text":"Journal Article"},"language":"English","usgsCitation":"Olsen, H.W., Clukey, E., and Nelson, C., 1982, Geotechnical characteristics of bottom sediments in the northeastern Bering Sea.: Geologie en Mijnbouw, v. 61, no. 1, p. 91-103.","startPage":"91","endPage":"103","numberOfPages":"13","costCenters":[],"links":[{"id":221775,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"61","issue":"1","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"505a28b7e4b0c8380cd5a34b","contributors":{"authors":[{"text":"Olsen, H. W.","contributorId":10060,"corporation":false,"usgs":true,"family":"Olsen","given":"H.","email":"","middleInitial":"W.","affiliations":[],"preferred":false,"id":361952,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Clukey, E.C.","contributorId":52720,"corporation":false,"usgs":true,"family":"Clukey","given":"E.C.","email":"","affiliations":[],"preferred":false,"id":361953,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Nelson, C.H.","contributorId":88346,"corporation":false,"usgs":true,"family":"Nelson","given":"C.H.","email":"","affiliations":[],"preferred":false,"id":361954,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":70011788,"text":"70011788 - 1982 - The oxygen isotope composition of granitoid and sedimentary rocks of the southern Snake Range, Nevada","interactions":[],"lastModifiedDate":"2012-03-12T17:18:32","indexId":"70011788","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":"The oxygen isotope composition of granitoid and sedimentary rocks of the southern Snake Range, Nevada","docAbstract":"Six diverse intrusive igneous types are exposed as discrete outcrops within an area of 900 km2 in the southern Snake Range, White Pine County, Nevada. The previously recognized variety among these igneous types is reflected in the wide range of ??18O values (-1.1 to 13.4 permil) found in these rocks. This range of ??18O values probably results from differences in source material and post-crystallization history of the different intrusive types. The Jurassic intrusive of the Snake Creek-Williams Canyon area represents the chemical equivalent of a large part of a differentiation sequence, with the entire range of composition (63-76 percent SiO2) exposed over a horizontal distance of about five km. The rather regular increase of ??18O values from the most mafic to the most felsic parts of this pluton, together with ??18O values determined for constituent minerals recovered from five of the samples, supports a fractional crystallization model. The high ??18O values found (10.2-12.2 permil) indicate that the magma likely was derived from or assimilated sedimentary materials. Nine samples of the Cretaceous two-mica granite of the Pole Canyon-Can Young Canyon area have ??18O values in the range 10.6-12.1 permil. These high ??18O values, an initial87Sr/86Sr ratio of 0.7165, and the presence of muscovite along with an accessory mineral suite limited to monazite, apatite, zircon, and an allanite-like mineral, characterize this intrusive mass as an S-type granite. It probably formed through anatexis of late Precambrian pelitic rocks. The granitoid rock exposed in the Young Canyon-Kious Basin area is Tertiary (32 m.y.). Most of this intrusive has been cataclastically deformed as a result of late (18 m.y.) movement on the overlying Snake Range decollement. The undeformed portion of this intrusive has ??18O values of 8.7-10.0 permil. However, the deformed portion of this intrusive has ??18O values as low as -1.1 permil, apparently resulting from isotopic exchange between this rock and ground water at the time of cataclasis. Although the igneous types exposed in the southern Snake Range differ petrologically and range in age from Jurassic to Tertiary, most have relatively high ??18O values compared with other granitoid rocks of the Basin-Range Province. ?? 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/BF01132884","issn":"00107999","usgsCitation":"Lee, D.E., Friedman, I., and Gleason, J., 1982, The oxygen isotope composition of granitoid and sedimentary rocks of the southern Snake Range, Nevada: Contributions to Mineralogy and Petrology, v. 79, no. 2, p. 150-158, https://doi.org/10.1007/BF01132884.","startPage":"150","endPage":"158","numberOfPages":"9","costCenters":[],"links":[{"id":205059,"rank":9999,"type":{"id":10,"text":"Digital Object Identifier"},"url":"https://dx.doi.org/10.1007/BF01132884"},{"id":220721,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"79","issue":"2","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"505bae78e4b08c986b324104","contributors":{"authors":[{"text":"Lee, D. E.","contributorId":96705,"corporation":false,"usgs":true,"family":"Lee","given":"D.","email":"","middleInitial":"E.","affiliations":[],"preferred":false,"id":361962,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Friedman, I.","contributorId":95596,"corporation":false,"usgs":true,"family":"Friedman","given":"I.","email":"","affiliations":[],"preferred":false,"id":361961,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Gleason, J.D.","contributorId":27072,"corporation":false,"usgs":true,"family":"Gleason","given":"J.D.","email":"","affiliations":[],"preferred":false,"id":361960,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":70011244,"text":"70011244 - 1982 - Stratigraphy, structure, absolute age, and paleontology of the upper Pleistocene deposits at Sankaty Head, Nantucket Island, Massachusetts","interactions":[],"lastModifiedDate":"2017-09-27T15:19:12","indexId":"70011244","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":"Stratigraphy, structure, absolute age, and paleontology of the upper Pleistocene deposits at Sankaty Head, Nantucket Island, Massachusetts","docAbstract":"<p>The Sankaty Head cliff exposes drift of at least two glaciations and interglacial marine deposits. Radiocarbon, amino-acid- racemization, and uranium-thorium analyses were used to determine the absolute ages of the beds. The results indicate that 1) the Sankaty Sand correlates with oxygen-isotope stage 5 (Sangamonian), 2) the underlying drift is older than stage 5 (Illinoian or older) , and 3) the overlying drift is Wisconsinan in age. -from Authors</p>","language":"English","publisher":"Geological Society of America","doi":"10.1130/0091-7613(1982)10<246:SSAAAP>2.0.CO;2","issn":"00917613","usgsCitation":"Oldale, R.N., Valentine, P.C., Cronin, T.M., Spiker, E., Blackwelder, B.W., Belknap, D.F., Wehmiller, J., and Szabo, B.J., 1982, Stratigraphy, structure, absolute age, and paleontology of the upper Pleistocene deposits at Sankaty Head, Nantucket Island, Massachusetts: Geology, v. 10, no. 5, p. 246-252, https://doi.org/10.1130/0091-7613(1982)10<246:SSAAAP>2.0.CO;2.","productDescription":"7 p.","startPage":"246","endPage":"252","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[{"id":186,"text":"Coastal and Marine Geology Program","active":true,"usgs":true},{"id":678,"text":"Woods Hole Coastal and Marine Science Center","active":true,"usgs":true}],"links":[{"id":221435,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United States","state":"Massachusetts","otherGeospatial":"Nantucket Island, Sankaty Head","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -70.04470825195312,\n              41.24554677159086\n            ],\n            [\n              -70.04470825195312,\n              41.281418560948055\n            ],\n            [\n              -69.95784759521484,\n              41.281418560948055\n            ],\n            [\n              -69.95784759521484,\n              41.24554677159086\n            ],\n            [\n              -70.04470825195312,\n              41.24554677159086\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","volume":"10","issue":"5","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"505b9a50e4b08c986b31c889","contributors":{"authors":[{"text":"Oldale, Robert N.","contributorId":38953,"corporation":false,"usgs":true,"family":"Oldale","given":"Robert","email":"","middleInitial":"N.","affiliations":[{"id":678,"text":"Woods Hole Coastal and Marine Science Center","active":true,"usgs":true}],"preferred":false,"id":360649,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Valentine, Page C. 0000-0002-0485-6266 pvalentine@usgs.gov","orcid":"https://orcid.org/0000-0002-0485-6266","contributorId":1947,"corporation":false,"usgs":true,"family":"Valentine","given":"Page","email":"pvalentine@usgs.gov","middleInitial":"C.","affiliations":[{"id":678,"text":"Woods Hole Coastal and Marine Science Center","active":true,"usgs":true}],"preferred":true,"id":525248,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Cronin, T. M. 0000-0002-2643-0979","orcid":"https://orcid.org/0000-0002-2643-0979","contributorId":42613,"corporation":false,"usgs":true,"family":"Cronin","given":"T.","email":"","middleInitial":"M.","affiliations":[{"id":40020,"text":"Florence Bascom Geoscience Center","active":true,"usgs":true}],"preferred":false,"id":525249,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Spiker, E.C.","contributorId":103275,"corporation":false,"usgs":true,"family":"Spiker","given":"E.C.","affiliations":[],"preferred":false,"id":525250,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"Blackwelder, B. W.","contributorId":104136,"corporation":false,"usgs":true,"family":"Blackwelder","given":"B.","email":"","middleInitial":"W.","affiliations":[],"preferred":false,"id":525251,"contributorType":{"id":1,"text":"Authors"},"rank":5},{"text":"Belknap, D. F.","contributorId":96739,"corporation":false,"usgs":true,"family":"Belknap","given":"D.","email":"","middleInitial":"F.","affiliations":[],"preferred":false,"id":525252,"contributorType":{"id":1,"text":"Authors"},"rank":6},{"text":"Wehmiller, J.F.","contributorId":37891,"corporation":false,"usgs":false,"family":"Wehmiller","given":"J.F.","email":"","affiliations":[],"preferred":false,"id":525253,"contributorType":{"id":1,"text":"Authors"},"rank":7},{"text":"Szabo, Barney J.","contributorId":6848,"corporation":false,"usgs":true,"family":"Szabo","given":"Barney","email":"","middleInitial":"J.","affiliations":[],"preferred":false,"id":525254,"contributorType":{"id":1,"text":"Authors"},"rank":8}]}}
,{"id":70011243,"text":"70011243 - 1982 - An analysis of input errors in precipitation-runoff models using regression with errors in the independent variables","interactions":[],"lastModifiedDate":"2018-02-05T12:39:08","indexId":"70011243","displayToPublicDate":"1982-01-01T00:00:00","publicationYear":"1982","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":3722,"text":"Water Resources Research","onlineIssn":"1944-7973","printIssn":"0043-1397","active":true,"publicationSubtype":{"id":10}},"title":"An analysis of input errors in precipitation-runoff models using regression with errors in the independent variables","docAbstract":"<p><span>Errors in runoff prediction caused by input data errors are analyzed by treating precipitation-runoff models as regression (conditional expectation) models. Independent variables of the regression consist of precipitation and other input measurements; the dependent variable is runoff. In models using erroneous input data, prediction errors are inflated and estimates of expected storm runoff for given observed input variables are biased. This bias in expected runoff estimation results in biased parameter estimates if these parameter estimates are obtained by a least squares fit of predicted to observed runoff values. The problems of error inflation and bias are examined in detail for a simple linear regression of runoff on rainfall and for a nonlinear U.S. Geological Survey precipitation-runoff model. Some implications for flood frequency analysis are considered. A case study using a set of data from Turtle Creek near Dallas, Texas illustrates the problems of model input errors.</span></p>","language":"English","publisher":"American Geophysical Union","doi":"10.1029/WR018i004p00947","usgsCitation":"Troutman, B.M., 1982, An analysis of input errors in precipitation-runoff models using regression with errors in the independent variables: Water Resources Research, v. 18, no. 4, p. 947-964, https://doi.org/10.1029/WR018i004p00947.","productDescription":"18 p.","startPage":"947","endPage":"964","costCenters":[],"links":[{"id":221434,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United States","state":"Texas","city":"Dallas","otherGeospatial":"Turtle Creek","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -96.81529998779297,\n              32.79275826977453\n            ],\n            [\n              -96.78749084472655,\n              32.79275826977453\n            ],\n            [\n              -96.78749084472655,\n              32.85132662142229\n            ],\n            [\n              -96.81529998779297,\n              32.85132662142229\n            ],\n            [\n              -96.81529998779297,\n              32.79275826977453\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","volume":"18","issue":"4","noUsgsAuthors":false,"publicationDate":"2010-07-09","publicationStatus":"PW","scienceBaseUri":"5059e9f0e4b0c8380cd4853d","contributors":{"authors":[{"text":"Troutman, Brent M.","contributorId":195329,"corporation":false,"usgs":false,"family":"Troutman","given":"Brent","email":"","middleInitial":"M.","affiliations":[],"preferred":false,"id":360648,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":1013685,"text":"1013685 - 1982 - Immersion and injection vaccination of salmonids against furunculosis with an avirulent strain of Aeromonas salmonicida","interactions":[],"lastModifiedDate":"2025-08-08T15:53:37.612482","indexId":"1013685","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":"Immersion and injection vaccination of salmonids against furunculosis with an avirulent strain of Aeromonas salmonicida","docAbstract":"<p><span>Replicate groups of brook trout (Salvelinus fontinalis) immunized by intraperitoneal injection of graded dilutions of an avirulent strain of Aeromonas salmonicida were protected from a virulent challenge. Mean mortality after challenge was 88% in control trout, 66% in trout immunized with 3 × 10</span><sup>6</sup><span>&nbsp;or 3 × 10</span><sup>5</sup><span>&nbsp;cells, and 39% in trout immunized with 3 × 10</span><sup>4</sup><span>&nbsp;to 3 × 10¹ cells. In brook trout challenged after immersion for 60 s in a culture containing 2.3 × 10</span><sup>9</sup><span>&nbsp;avirulent cells of A. salmonicida per milliliter, mortality was 44%, compared with 94% in controls. In Atlantic salmon (Salmo salar), similarly vaccinated by immersion, mortality was 12.5% after challenge compared with 87.5% in controls. In additional studies, mean mortality of Atlantic salmon vaccinated by immersion was 14%, whereas that of control salmon was 92%.</span></p>","language":"English","publisher":"Oxford Academic","doi":"10.1577/1548-8659(1982)44[167:IAIVOS]2.0.CO;2","usgsCitation":"Cipriano, R.C., and Starliper, C.E., 1982, Immersion and injection vaccination of salmonids against furunculosis with an avirulent strain of Aeromonas salmonicida: Progressive Fish-Culturist, v. 44, no. 4, p. 167-169, https://doi.org/10.1577/1548-8659(1982)44[167:IAIVOS]2.0.CO;2.","productDescription":"3 p.","startPage":"167","endPage":"169","numberOfPages":"3","costCenters":[{"id":365,"text":"Leetown Science Center","active":true,"usgs":true}],"links":[{"id":129697,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"44","issue":"4","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a09e4b07f02db5fa9fc","contributors":{"authors":[{"text":"Cipriano, R. C.","contributorId":12400,"corporation":false,"usgs":true,"family":"Cipriano","given":"R.","middleInitial":"C.","affiliations":[],"preferred":false,"id":319042,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Starliper, C. E.","contributorId":59739,"corporation":false,"usgs":true,"family":"Starliper","given":"C.","middleInitial":"E.","affiliations":[],"preferred":false,"id":319043,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":70011230,"text":"70011230 - 1982 - Infiltration formulas by curve number procedure.","interactions":[],"lastModifiedDate":"2013-03-18T08:02:10","indexId":"70011230","displayToPublicDate":"1982-01-01T00:00:00","publicationYear":"1982","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":2550,"text":"Journal of the Hydraulics Division","active":true,"publicationSubtype":{"id":10}},"title":"Infiltration formulas by curve number procedure.","docAbstract":"The Soil Conservation Service (SCS) curve number procedure for estimating runoff volume is examined in terms of the validity and applicability of the derived infiltration equations. -from ASCE Publications Abstracts","largerWorkType":{"id":2,"text":"Article"},"largerWorkTitle":"Journal of the Hydraulics Division","largerWorkSubtype":{"id":10,"text":"Journal Article"},"language":"English","publisher":"ASCE","doi":"10.1061/(ASCE)0733-9429(1984)110:3(347)","usgsCitation":"Chen, C., 1982, Infiltration formulas by curve number procedure.: Journal of the Hydraulics Division, v. 108, no. HY7, p. 823-829, https://doi.org/10.1061/(ASCE)0733-9429(1984)110:3(347).","startPage":"823","endPage":"829","numberOfPages":"7","costCenters":[],"links":[{"id":221033,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"},{"id":269587,"type":{"id":10,"text":"Digital Object Identifier"},"url":"https://dx.doi.org/10.1061/(ASCE)0733-9429(1984)110:3(347)"}],"volume":"108","issue":"HY7","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"505a3af3e4b0c8380cd620df","contributors":{"authors":[{"text":"Chen, Chiu-Lan","contributorId":100979,"corporation":false,"usgs":true,"family":"Chen","given":"Chiu-Lan","email":"","affiliations":[],"preferred":false,"id":360620,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":70011229,"text":"70011229 - 1982 - Obtaining maps and data from the U.S. Geological Survey","interactions":[],"lastModifiedDate":"2023-09-21T16:24:00.08603","indexId":"70011229","displayToPublicDate":"1982-01-01T00:00:00","publicationYear":"1982","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1317,"text":"Computers, Environment and Urban Systems","active":true,"publicationSubtype":{"id":10}},"title":"Obtaining maps and data from the U.S. Geological Survey","docAbstract":"<p><span>The U.S. Geological Survey produces a variety of resource information for the United States. This includes many data bases of particular interest to planners such as land use and terrain information prepared by the National Mapping Division, water quantity and quality data collected by Water Resources Division, and coal resource information gathered by the Geologic Division. These data are stored in various forms, and information on their availability can be obtained from appropriate offices in the U.S. Geological Survey as well as from USGS Circular 777. These data have been used for the management, development, and monitoring of our Nation's resources by Federal, State, and local agencies.</span></p>","language":"English","publisher":"Elsevier","doi":"10.1016/0198-9715(82)90016-3","usgsCitation":"Hallam, C.A., 1982, Obtaining maps and data from the U.S. Geological Survey: Computers, Environment and Urban Systems, v. 7, no. 4, p. 283-294, https://doi.org/10.1016/0198-9715(82)90016-3.","productDescription":"12 p.","startPage":"283","endPage":"294","numberOfPages":"12","costCenters":[],"links":[{"id":221032,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"7","issue":"4","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"505a6b0ee4b0c8380cd744c6","contributors":{"authors":[{"text":"Hallam, Cheryl A.","contributorId":59012,"corporation":false,"usgs":true,"family":"Hallam","given":"Cheryl","email":"","middleInitial":"A.","affiliations":[],"preferred":false,"id":360619,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":1013628,"text":"1013628 - 1982 - Survival, growth, and catchability of rainbow trout of four strains","interactions":[],"lastModifiedDate":"2025-04-01T16:13:18.312541","indexId":"1013628","displayToPublicDate":"1982-01-01T00:00:00","publicationYear":"1982","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":"Survival, growth, and catchability of rainbow trout of four strains","docAbstract":"<p><span>Fingerling rainbow trout (<i>Salmo gairdneri</i>) of genetically different strains survived, grew, and were caught at different rates by anglers and in gill nets after release from a hatchery into a 1‐hectare pond. When two domestic strains were compared, more fish of the strain genetically selected for fast growth were caught per unit of angling effort than were fish of a strain not selected for this characteristic. When fish of a natural and domestic strain were released together, survival was higher in the natural strain, but growth was slower. Strain population estimates reflected differences in catchability and were erroneous for the strain selected for growth. These observations imply that rainbow trout of different strains vary in their suitability for different fishery management practices.</span></p>","language":"English","publisher":"Oxford Academic","doi":"10.1577/1548-8659(1982)2<1:SGACOR>2.0.CO;2","usgsCitation":"Brauhn, J., and Kincaid, H., 1982, Survival, growth, and catchability of rainbow trout of four strains: North American Journal of Fisheries Management, v. 2, no. 1, p. 1-10, https://doi.org/10.1577/1548-8659(1982)2<1:SGACOR>2.0.CO;2.","productDescription":"10 p.","startPage":"1","endPage":"10","costCenters":[{"id":365,"text":"Leetown Science Center","active":true,"usgs":true}],"links":[{"id":132189,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"2","issue":"1","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ae0e4b07f02db6880f1","contributors":{"authors":[{"text":"Brauhn, J.L.","contributorId":59767,"corporation":false,"usgs":true,"family":"Brauhn","given":"J.L.","affiliations":[],"preferred":false,"id":318908,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Kincaid, H.","contributorId":22273,"corporation":false,"usgs":true,"family":"Kincaid","given":"H.","affiliations":[],"preferred":false,"id":318907,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":1013624,"text":"1013624 - 1982 - Differentiation of soluble proteins in cataracts caused by deficiencies of methionine, riboflavin or zinc in diets fed to Atlantic salmon, Salmo salar, rainbow trout, Salmo gairdneri, and lake trout, Salvelinus namaycush","interactions":[],"lastModifiedDate":"2012-02-02T00:04:29","indexId":"1013624","displayToPublicDate":"1982-01-01T00:00:00","publicationYear":"1982","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1340,"text":"Cornell Veterinarian","active":true,"publicationSubtype":{"id":10}},"title":"Differentiation of soluble proteins in cataracts caused by deficiencies of methionine, riboflavin or zinc in diets fed to Atlantic salmon, Salmo salar, rainbow trout, Salmo gairdneri, and lake trout, Salvelinus namaycush","largerWorkType":{"id":2,"text":"Article"},"largerWorkTitle":"Cornell Veterinarian","largerWorkSubtype":{"id":10,"text":"Journal Article"},"language":"English","collaboration":"None/TL","usgsCitation":"Barash, H., Poston, H.A., and Rumsey, G.L., 1982, Differentiation of soluble proteins in cataracts caused by deficiencies of methionine, riboflavin or zinc in diets fed to Atlantic salmon, Salmo salar, rainbow trout, Salmo gairdneri, and lake trout, Salvelinus namaycush: Cornell Veterinarian, v. 72, no. 4, p. 361-371.","productDescription":"p. 361-371","startPage":"361","endPage":"371","numberOfPages":"11","costCenters":[{"id":365,"text":"Leetown Science Center","active":true,"usgs":true}],"links":[{"id":131875,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"72","issue":"4","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a9ae4b07f02db65d6b5","contributors":{"authors":[{"text":"Barash, H.","contributorId":21503,"corporation":false,"usgs":true,"family":"Barash","given":"H.","email":"","affiliations":[],"preferred":false,"id":318894,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Poston, H. A.","contributorId":21893,"corporation":false,"usgs":true,"family":"Poston","given":"H.","email":"","middleInitial":"A.","affiliations":[],"preferred":false,"id":318895,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Rumsey, G. L.","contributorId":80604,"corporation":false,"usgs":true,"family":"Rumsey","given":"G.","email":"","middleInitial":"L.","affiliations":[],"preferred":false,"id":318896,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":1014347,"text":"1014347 - 1982 - Biological effects of dietary T-2 toxin on rainbow trout, Salmo gairdneri","interactions":[],"lastModifiedDate":"2023-03-03T19:29:08.230568","indexId":"1014347","displayToPublicDate":"1982-01-01T00:00:00","publicationYear":"1982","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":874,"text":"Aquatic Toxicology","active":true,"publicationSubtype":{"id":10}},"title":"Biological effects of dietary T-2 toxin on rainbow trout, Salmo gairdneri","docAbstract":"<p>A 16-wk feeding study was conducted to evaluate the chronic toxicity of graded levels (0, 1.0, 2.5.5, 10 and 15 mg/kg of chemically pure dietary T-2 toxin (4,15-diacetoxy-8-(3-methylbutyryloxy)-12,13-epoxy-Δ<sup>9</sup>-tricothecen-3-ol) in 1-g rainbow trout,<span>&nbsp;</span><i>Salmo gairdneri</i>, held in 9°C single-passage well water. Levels of T-2 toxin &gt; 2.5 mg/kg depressed growth, efficiency of feed use, hematocrit, blood hemoglobin concentration and feed acceptance, and caused a transitory edema in a dose-dependent manner. Growth of trout fed a semipurified diet containing the toxin was described by the function:<span>&nbsp;</span><i>Y</i><span>&nbsp;</span>= 0.265 + 142.075 e<sup>(0.029<i>X</i><sub>1</sub></sup>− 1.554x<sub>2<sup>3.7</sup></sub>), where<span>&nbsp;</span><i>Y</i><span>&nbsp;</span>= gain as percentage starting weight per wk;<span>&nbsp;</span><i>X</i><sub>1</sub><span>&nbsp;</span>is time in wk and 0 ⩽<span>&nbsp;</span><i>X</i><sub>1</sub>⩽16; and<span>&nbsp;</span><i>X</i><sub>2</sub><span>&nbsp;</span>is T-2 content of diet in mg/kgand 0⩽<i>X</i><sub>2</sub>⩽15.</p><p>Exposure of fish to T-2 toxin did not affect activity of intestinal lumen chymoirypsin or trypsin, nitrogen digestibility or metabolizabte energy. Feeding of 15 mg/kg T-2 toxin to adult trout caused hemorrhaging in the intestines and regurgitation of subsequently intubated feed regardless of T-2 loxin content.</p>","language":"English","publisher":"Elsevier","doi":"10.1016/0166-445X(82)90007-8","usgsCitation":"Poston, H.A., Coffine, J.L., and Combs, G.F., 1982, Biological effects of dietary T-2 toxin on rainbow trout, Salmo gairdneri: Aquatic Toxicology, v. 2, no. 2, p. 79-88, https://doi.org/10.1016/0166-445X(82)90007-8.","productDescription":"10 p.","startPage":"79","endPage":"88","numberOfPages":"10","costCenters":[{"id":365,"text":"Leetown Science Center","active":true,"usgs":true}],"links":[{"id":131421,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"2","issue":"2","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a48e4b07f02db6234bd","contributors":{"authors":[{"text":"Poston, H. A.","contributorId":21893,"corporation":false,"usgs":true,"family":"Poston","given":"H.","email":"","middleInitial":"A.","affiliations":[],"preferred":false,"id":320222,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Coffine, J. L.","contributorId":55391,"corporation":false,"usgs":false,"family":"Coffine","given":"J.","email":"","middleInitial":"L.","affiliations":[],"preferred":false,"id":320224,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Combs, G. F. Jr.","contributorId":31352,"corporation":false,"usgs":false,"family":"Combs","given":"G.","suffix":"Jr.","email":"","middleInitial":"F.","affiliations":[],"preferred":false,"id":320223,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
]}