{"pageNumber":"5259","pageRowStart":"131450","pageSize":"25","recordCount":184617,"records":[{"id":70012039,"text":"70012039 - 1983 - Landsat analysis of the Yangjiatan tungsten district, Hunan Province, People's Republic of China","interactions":[],"lastModifiedDate":"2013-01-20T09:21:02","indexId":"70012039","displayToPublicDate":"1983-01-01T00:00:00","publicationYear":"1983","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":661,"text":"Advances in Space Research","active":true,"publicationSubtype":{"id":10}},"title":"Landsat analysis of the Yangjiatan tungsten district, Hunan Province, People's Republic of China","docAbstract":"The Yangjiatan tungsten district at latitude 27??28??? N. and longitude 111??54???E. is located about 140 km southwest of the city of Changsha and 35 km northeast of the town of Shaoyang, southeast Hunan Province, People's Republic of China. The deposits, consisting largely of scheelite in veins (Wang, 1975), are contained in highly folded and faulted sedimentary rocks of Paleozoic, Mesozoic, and Cenozoic age intruded by granitic plutons that are circular in plan view. The major faults and folds trend in a northeasterly direction; whereas, the plutons are clustered in a more easterly trending band across the Landsat image. Landsat image E-2338-02202, acquired December 26, 1975, is number 470 in the \"Landsat Image Atlas of the People's Republic of China\" printed by the Publishing House of Geology in 1979. A computer-compatible tape of the image was analyzed and used as a demonstration project under a United Nations technical assistance program. Supervised classification of soils, rocks, and vegetation; band ratioing to detect limonite alteration; and edge enhancement were all conducted to demonstrate the flexibility and capability of interactive computer systems. Field evaluation of the results of this work will be conducted by colleagues of the Remote Sensing Center for Geology, Ministry of Geology, in China. ?? 1983.","largerWorkType":{"id":2,"text":"Article"},"largerWorkTitle":"Advances in Space Research","largerWorkSubtype":{"id":10,"text":"Journal Article"},"language":"English","publisher":"Elsevier","doi":"10.1016/0273-1177(83)90110-2","issn":"02731177","usgsCitation":"Carter, W.D., and Kiilsgaard, T.H., 1983, Landsat analysis of the Yangjiatan tungsten district, Hunan Province, People's Republic of China: Advances in Space Research, v. 3, no. 2, p. 113-123, https://doi.org/10.1016/0273-1177(83)90110-2.","startPage":"113","endPage":"123","numberOfPages":"11","costCenters":[],"links":[{"id":222572,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"},{"id":266026,"type":{"id":10,"text":"Digital Object Identifier"},"url":"https://dx.doi.org/10.1016/0273-1177(83)90110-2"}],"volume":"3","issue":"2","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"505a43d4e4b0c8380cd6664a","contributors":{"authors":[{"text":"Carter, W. D.","contributorId":75633,"corporation":false,"usgs":true,"family":"Carter","given":"W.","email":"","middleInitial":"D.","affiliations":[],"preferred":false,"id":362585,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Kiilsgaard, T. H.","contributorId":102043,"corporation":false,"usgs":true,"family":"Kiilsgaard","given":"T.","email":"","middleInitial":"H.","affiliations":[],"preferred":false,"id":362586,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":70011246,"text":"70011246 - 1983 - Clay mineral formation and transformation in rocks and soils","interactions":[],"lastModifiedDate":"2020-01-19T11:27:27","indexId":"70011246","displayToPublicDate":"1983-01-01T00:00:00","publicationYear":"1983","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":3047,"text":"Philosophical Transactions of the Royal Society A: Mathematical, Physical and Engineering Sciences","active":true,"publicationSubtype":{"id":10}},"title":"Clay mineral formation and transformation in rocks and soils","docAbstract":"Three mechanisms for clay mineral formation (inheritance, neoformation, and transformation) operating in three geological environments (weathering, sedimentary, and diagenetic-hydrothermal) yield nine possibilities for the origin of clay minerals in nature. Several of these possibilities are discussed in terms of the rock cycle. The mineralogy of clays neoformed in the weathering environment is a function of solution chemistry, with the most dilute solutions favoring formation of the least soluble clays. After erosion and transportation, these clays may be deposited on the ocean floor in a lateral sequence that depends on floccule size. Clays undergo little reaction in the ocean, except for ion exchange and the neoformation of smectite; therefore, most clays found on the ocean floor are inherited from adjacent continents. Upon burial and heating, however, dioctahedral smectite reacts in the diagenetic environment to yield mixed-layer illite-smectite, and finally illite. With uplift and weathering, the cycle begins again. Refs.","language":"English","publisher":"Royal Society of London","doi":"10.1098/rsta.1984.0026","usgsCitation":"Eberl, D.D., 1983, Clay mineral formation and transformation in rocks and soils: Philosophical Transactions of the Royal Society A: Mathematical, Physical and Engineering Sciences, v. 311, no. 1517, p. 241-257, https://doi.org/10.1098/rsta.1984.0026.","productDescription":"17 p.","startPage":"241","endPage":"257","numberOfPages":"17","costCenters":[{"id":589,"text":"Toxic Substances Hydrology Program","active":true,"usgs":true}],"links":[{"id":221512,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"311","issue":"1517","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"5059f2d0e4b0c8380cd4b3c5","contributors":{"authors":[{"text":"Eberl, D. D.","contributorId":66282,"corporation":false,"usgs":true,"family":"Eberl","given":"D.","email":"","middleInitial":"D.","affiliations":[],"preferred":false,"id":360653,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":70011247,"text":"70011247 - 1983 - SELECTED CHEMICAL ANALYSES AND GEOTHERMOMETRY OF HOT SPRING WATERS FROM THE CALABOZOS CALDERA, CENTRAL CHILE.","interactions":[],"lastModifiedDate":"2012-03-12T17:18:27","indexId":"70011247","displayToPublicDate":"1983-01-01T00:00:00","publicationYear":"1983","noYear":false,"publicationType":{"id":24,"text":"Conference Paper"},"publicationSubtype":{"id":19,"text":"Conference Paper"},"title":"SELECTED CHEMICAL ANALYSES AND GEOTHERMOMETRY OF HOT SPRING WATERS FROM THE CALABOZOS CALDERA, CENTRAL CHILE.","docAbstract":"Hot springs discharging from the active hydrothermal system associated with the Calabozos caldera, Chile, have measured orifice temperatures as high as 98. 5 degree C and calculated geothermometer temperatures as high as 250 degree C. Three types of spring waters can be identified from the chemical analyses: a Na-Cl type, a Na-HCO//3 type and a Na-mixed anion type. Chloride-enthalpy relations indicate that the hydrothermal reservoir water may attain temperatures near 342 degree C and that most spring waters are mixed with cold meteoric water. Despite the proximity of Mesozoic marine gypsum deposits, the Cl/Br weight ratio of the Calabozos spring waters does not appear to indicate that these waters have a significant 'marine' signature. Refs.","largerWorkTitle":"Transactions - Geothermal Resources Council","conferenceTitle":"Geothermal Resources: Energy on Tap! Geothermal Resources Council 1983 Annual Meeting.","conferenceLocation":"Portland, OR, USA","language":"English","publisher":"Geothermal Resources Council","publisherLocation":"Davis, CA, USA","issn":"01935933","isbn":"093441257X","usgsCitation":"Thompson, J., Grunder, A., and Hildreth, W., 1983, SELECTED CHEMICAL ANALYSES AND GEOTHERMOMETRY OF HOT SPRING WATERS FROM THE CALABOZOS CALDERA, CENTRAL CHILE., <i>in</i> Transactions - Geothermal Resources Council, v. 7, Portland, OR, USA, p. 331-335.","startPage":"331","endPage":"335","numberOfPages":"5","costCenters":[],"links":[{"id":221513,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"7","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"505aaf31e4b0c8380cd87435","contributors":{"authors":[{"text":"Thompson, J. M.","contributorId":77142,"corporation":false,"usgs":true,"family":"Thompson","given":"J. M.","affiliations":[],"preferred":false,"id":360656,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Grunder, A.L.","contributorId":71314,"corporation":false,"usgs":true,"family":"Grunder","given":"A.L.","affiliations":[],"preferred":false,"id":360655,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Hildreth, Wes","contributorId":15996,"corporation":false,"usgs":true,"family":"Hildreth","given":"Wes","email":"","affiliations":[],"preferred":false,"id":360654,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":70012051,"text":"70012051 - 1983 - Sm-Nd age and isotopic systematics of the bimodal suite, ancient gneiss complex, Swaziland","interactions":[],"lastModifiedDate":"2012-03-12T17:18:44","indexId":"70012051","displayToPublicDate":"1983-01-01T00:00:00","publicationYear":"1983","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":2840,"text":"Nature","active":true,"publicationSubtype":{"id":10}},"title":"Sm-Nd age and isotopic systematics of the bimodal suite, ancient gneiss complex, Swaziland","docAbstract":"Studies of the development and stabilization of the Archaean crust often focus on the relative temporal relationships between the metamorphosed basaltic to ultramafic volcanic units (greenstone belts) and the sialic gneiss terrains that make up the oldest sections of the terrestrial crust. At the heart of this interest are the questions of the processes responsible for crust formation in the Archaean and whether or not the various units of an Archaean crustal section represent new additions to the crust from the mantle or are products of the reprocessing of even older crustal materials. One area where this controversy has been particularly pronounced is the Archaean crustal section of south-west Africa1-6. The oldest rocks in the Kaapvaal craton consist of the Onverwacht Group of mafic to ultramafic metavolcanics of the Barberton greenstone belt and a grey-gneiss complex termed the ancient gneiss complex (AGC) of Swaziland. We report here the results of a whole-rock Sm-Nd isotopic study of the AGC and the implications these data may have for crustal evolution in the Kaapvaal craton. ?? 1983 Nature Publishing Group.","largerWorkType":{"id":2,"text":"Article"},"largerWorkTitle":"Nature","largerWorkSubtype":{"id":10,"text":"Journal Article"},"language":"English","doi":"10.1038/305701a0","issn":"00280836","usgsCitation":"Carlson, R.W., Hunter, D., and Barker, F., 1983, Sm-Nd age and isotopic systematics of the bimodal suite, ancient gneiss complex, Swaziland: Nature, v. 305, no. 5936, p. 701-704, https://doi.org/10.1038/305701a0.","startPage":"701","endPage":"704","numberOfPages":"4","costCenters":[],"links":[{"id":222758,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"},{"id":205295,"rank":9999,"type":{"id":10,"text":"Digital Object Identifier"},"url":"https://dx.doi.org/10.1038/305701a0"}],"volume":"305","issue":"5936","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"505b9178e4b08c986b319913","contributors":{"authors":[{"text":"Carlson, R. W.","contributorId":85331,"corporation":false,"usgs":false,"family":"Carlson","given":"R.","email":"","middleInitial":"W.","affiliations":[],"preferred":false,"id":362618,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Hunter, D.R.","contributorId":79909,"corporation":false,"usgs":true,"family":"Hunter","given":"D.R.","email":"","affiliations":[],"preferred":false,"id":362617,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Barker, F.","contributorId":101368,"corporation":false,"usgs":true,"family":"Barker","given":"F.","affiliations":[],"preferred":false,"id":362619,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":70012052,"text":"70012052 - 1983 - Bedform distribution and inferred sand transport on Georges Bank, United States Atlantic continental shelf.","interactions":[],"lastModifiedDate":"2017-08-17T10:22:20","indexId":"70012052","displayToPublicDate":"1983-01-01T00:00:00","publicationYear":"1983","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":3369,"text":"Sedimentology","active":true,"publicationSubtype":{"id":10}},"title":"Bedform distribution and inferred sand transport on Georges Bank, United States Atlantic continental shelf.","docAbstract":"Four bedform provinces have been identified using sidescan-sonar and echo-sounding techniques: large sand waves superimposed on sand ridges, small sand waves, megaripples, and featureless seafloor. Sand-wave asymmetry and surface-sediment texture have been used to infer bedload transport paths and although the asymmetry of megaripples could not be determined, the occurrence of megaripples between the small sand-wave province and areas of featureless seafloor suggests a decreasing effectiveness of sand transport away from the bank crest. This sand dispersal pattern is further supported by the surface sediments which become progressively finer to the N and SW away from the crest of Georges Bank.-from Author","largerWorkType":{"id":2,"text":"Article"},"largerWorkTitle":"Sedimentology","largerWorkSubtype":{"id":10,"text":"Journal Article"},"language":"English","doi":"10.1111/j.1365-3091.1983.tb00703.x","issn":"00370746","usgsCitation":"Twichell, D., 1983, Bedform distribution and inferred sand transport on Georges Bank, United States Atlantic continental shelf.: Sedimentology, v. 30, no. 5, p. 695-710, https://doi.org/10.1111/j.1365-3091.1983.tb00703.x.","productDescription":"16 p.","startPage":"695","endPage":"710","costCenters":[{"id":678,"text":"Woods Hole Coastal and Marine Science Center","active":true,"usgs":true}],"links":[{"id":222759,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United States","state":"Massachusetts","otherGeospatial":"Georges Bank","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -70,\n              40\n            ],\n            [\n              -66,\n              40\n            ],\n            [\n              -66,\n             43\n            ],\n            [\n              -70,\n              43\n            ],\n            [\n              -70,\n              40\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","volume":"30","issue":"5","noUsgsAuthors":false,"publicationDate":"2006-06-14","publicationStatus":"PW","scienceBaseUri":"5059f040e4b0c8380cd4a699","contributors":{"authors":[{"text":"Twichell, D.C.","contributorId":84304,"corporation":false,"usgs":true,"family":"Twichell","given":"D.C.","affiliations":[],"preferred":false,"id":362620,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":70011582,"text":"70011582 - 1983 - The Eastern Gas Shales Project (EGSP) Data System: A case study in data base design, development, and application","interactions":[],"lastModifiedDate":"2012-03-12T17:18:30","indexId":"70011582","displayToPublicDate":"1983-01-01T00:00:00","publicationYear":"1983","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":2554,"text":"Journal of the International Association for Mathematical Geology","active":true,"publicationSubtype":{"id":10}},"title":"The Eastern Gas Shales Project (EGSP) Data System: A case study in data base design, development, and application","docAbstract":"The U.S. Geological Survey and Petroleum Information Corporation in Denver, Colorado, developed the Eastern Gas Shale Project (EGSP)Data System for the U.S. Department of Energy, Morgantown, West Virginia. Geological, geochemical, geophysical, and engineering data from Devonian shale samples from more than 5800 wells and outcrops in the Appalachian basin were edited and converted to a Petroleum Information Corporation data base. Well and sample data may be retrieved from this data system to produce (1)production-test summaries by formation and well location; (2)contoured isopach, structure, and trendsurface maps of Devonian shale units; (3)sample summary reports for samples by location, well, contractor, and sample number; (4)cross sections displaying digitized log traces, geochemical, and lithologic data by depth for wells; and (5)frequency distributions and bivariate plots. Although part of the EGSP Data System is proprietary, and distribution of complete well histories is prohibited by contract, maps and aggregated well-data listings are being made available to the public through published reports. ?? 1983 Plenum Publishing Corporation.","largerWorkType":{"id":2,"text":"Article"},"largerWorkTitle":"Journal of the International Association for Mathematical Geology","largerWorkSubtype":{"id":10,"text":"Journal Article"},"language":"English","publisherLocation":"Kluwer Academic Publishers-Plenum Publishers","doi":"10.1007/BF01036076","issn":"00205958","usgsCitation":"Dyman, T.S., and Wilcox, L., 1983, The Eastern Gas Shales Project (EGSP) Data System: A case study in data base design, development, and application: Journal of the International Association for Mathematical Geology, v. 15, no. 2, p. 363-369, https://doi.org/10.1007/BF01036076.","startPage":"363","endPage":"369","numberOfPages":"7","costCenters":[],"links":[{"id":221453,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"},{"id":205124,"rank":9999,"type":{"id":10,"text":"Digital Object Identifier"},"url":"https://dx.doi.org/10.1007/BF01036076"}],"volume":"15","issue":"2","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"505ba713e4b08c986b321352","contributors":{"authors":[{"text":"Dyman, T. S.","contributorId":21161,"corporation":false,"usgs":false,"family":"Dyman","given":"T.","middleInitial":"S.","affiliations":[],"preferred":false,"id":361458,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Wilcox, L.A.","contributorId":8098,"corporation":false,"usgs":true,"family":"Wilcox","given":"L.A.","email":"","affiliations":[],"preferred":false,"id":361457,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":70012053,"text":"70012053 - 1983 - DETERMINATION OF MODE OF OCCURRENCE OF TRACE ELEMENTS IN THE UPPER FREEPORT COAL BED USING SIZE AND DENSITY SEPARATION PROCEDURES.","interactions":[],"lastModifiedDate":"2012-03-12T17:18:44","indexId":"70012053","displayToPublicDate":"1983-01-01T00:00:00","publicationYear":"1983","noYear":false,"publicationType":{"id":24,"text":"Conference Paper"},"publicationSubtype":{"id":19,"text":"Conference Paper"},"title":"DETERMINATION OF MODE OF OCCURRENCE OF TRACE ELEMENTS IN THE UPPER FREEPORT COAL BED USING SIZE AND DENSITY SEPARATION PROCEDURES.","docAbstract":"A procedure has been developed using low temperature ashing, followed by size and sink-float separation of the ash, X-ray diffraction analysis, and instrumental neutron activation analysis to give both qualitative and quantitative information for major, minor and trace minerals and their associated trace elements in coal.","conferenceTitle":"Proceedings - 1983 International Conference on Coal Science.","conferenceLocation":"Pittsburgh, PA, USA","language":"English","usgsCitation":"Palmer, C., and Filby, R., 1983, DETERMINATION OF MODE OF OCCURRENCE OF TRACE ELEMENTS IN THE UPPER FREEPORT COAL BED USING SIZE AND DENSITY SEPARATION PROCEDURES., Proceedings - 1983 International Conference on Coal Science., Pittsburgh, PA, USA, p. 365-368.","startPage":"365","endPage":"368","numberOfPages":"4","costCenters":[],"links":[{"id":222760,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"5059fd43e4b0c8380cd4e71d","contributors":{"authors":[{"text":"Palmer, C.A.","contributorId":81894,"corporation":false,"usgs":true,"family":"Palmer","given":"C.A.","email":"","affiliations":[],"preferred":false,"id":362622,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Filby, R.H.","contributorId":26071,"corporation":false,"usgs":true,"family":"Filby","given":"R.H.","email":"","affiliations":[],"preferred":false,"id":362621,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":70011566,"text":"70011566 - 1983 - Preparing a Detailed Landslide-Inventory Map for Hazard Evaluation and Reduction","interactions":[],"lastModifiedDate":"2023-11-03T00:52:54.226482","indexId":"70011566","displayToPublicDate":"1983-01-01T00:00:00","publicationYear":"1983","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1115,"text":"Bulletin of the Association of Engineering Geologists","active":true,"publicationSubtype":{"id":10}},"title":"Preparing a Detailed Landslide-Inventory Map for Hazard Evaluation and Reduction","docAbstract":"A method of preparing a detailed landslide-inventory map has been developed which provides the engineering geologist with the basic information for evaluating and reducing landslide hazards or risk on a regional or community level. For each landslide, the map depicts state of activity, certainty of identification, dominant type of slope movement, primary direction of movement, estimated thickness of material involved in landsliding, and date(s) of known activity. This information is developed from interpreting aerial photographs and examining landslide features in the field. Although preparing detailed landslide-inventory maps involves considerably more time and effort than landslide reconnaissance mapping, these maps are directly useable by planners and decisionmakers as a basis for requiring site-specific investigations prior to development or adopting land-use regulations. Refs.","language":"English","publisher":"Association of Engineering Geologists","doi":"10.2113/gseegeosci.xxi.3.337","issn":"00045691","usgsCitation":"Wieczorek, G.F., 1983, Preparing a Detailed Landslide-Inventory Map for Hazard Evaluation and Reduction: Bulletin of the Association of Engineering Geologists, v. 21, no. 3, p. 337-342, https://doi.org/10.2113/gseegeosci.xxi.3.337.","productDescription":"6 p.","startPage":"337","endPage":"342","numberOfPages":"6","costCenters":[],"links":[{"id":221242,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"21","issue":"3","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"505a7373e4b0c8380cd7703b","contributors":{"authors":[{"text":"Wieczorek, Gerald F.","contributorId":81889,"corporation":false,"usgs":true,"family":"Wieczorek","given":"Gerald","email":"","middleInitial":"F.","affiliations":[],"preferred":false,"id":361417,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":70011251,"text":"70011251 - 1983 - Distribution of differentiated tholeiitic basalts on the lower east rift zone of Kilauea Volcano, Hawaii: A possible guide to geothermal exploration","interactions":[],"lastModifiedDate":"2024-01-31T01:38:15.121082","indexId":"70011251","displayToPublicDate":"1983-01-01T00:00:00","publicationYear":"1983","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1796,"text":"Geology","active":true,"publicationSubtype":{"id":10}},"title":"Distribution of differentiated tholeiitic basalts on the lower east rift zone of Kilauea Volcano, Hawaii: A possible guide to geothermal exploration","docAbstract":"<div id=\"15567678\" class=\"article-section-wrapper js-article-section js-content-section  \" data-section-parent-id=\"0\"><p>Geologic mapping of the lower east rift zone of Kilauea Volcano, Hawaii, indicates that more than 100 eruptions have extruded an estimated 10 km<sup>3</sup><span>&nbsp;</span>of basalt during the past 2,000 yr. Six eruptions in the past 200 yr have extruded about 1 km<sup>3</sup>. The eruptive recurrence interval has ranged from 1 to 115 yr since the middle 18th century and has averaged 20 yr or less over the past 2,000 yr.</p><p>One hundred new chemical analyses indicate that the erupted tholeiites commonly are differentiated beyond olivine control or are hybrid mixtures of differentiates with more mafic (olivine-controlled) summit magmas. The distribution of vents for differentiated lavas indicates that several large magma chambers underlie the lower east rift zone. Several workers have recognized that a chamber underlies the area near a producing well, HGP-A; petrologic and<span>&nbsp;</span><sup>14</sup>C data indicate that it has existed for at least 1,300 yr. Stratigraphy, petrology, and surface deformation patterns suggest that two other areas, Heiheiahulu and Kaliu, also overlie large magma chambers and appear to be favorable geothermal prospects.</p></div>","language":"English","publisher":"Geological Society of America","doi":"10.1130/0091-7613(1983)11<136:DODTBO>2.0.CO;2","issn":"00917613","usgsCitation":"Moore, R.B., 1983, Distribution of differentiated tholeiitic basalts on the lower east rift zone of Kilauea Volcano, Hawaii: A possible guide to geothermal exploration: Geology, v. 11, no. 3, p. 136-140, https://doi.org/10.1130/0091-7613(1983)11<136:DODTBO>2.0.CO;2.","productDescription":"5 p.","startPage":"136","endPage":"140","numberOfPages":"5","costCenters":[],"links":[{"id":221653,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"11","issue":"3","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"505a02c8e4b0c8380cd501d9","contributors":{"authors":[{"text":"Moore, R. B.","contributorId":98720,"corporation":false,"usgs":true,"family":"Moore","given":"R.","email":"","middleInitial":"B.","affiliations":[],"preferred":false,"id":360663,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":70011268,"text":"70011268 - 1983 - Hashemite, Ba(Cr,S)O4, a new mineral from Jordan.","interactions":[],"lastModifiedDate":"2013-02-14T10:10:15","indexId":"70011268","displayToPublicDate":"1983-01-01T00:00:00","publicationYear":"1983","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":"Hashemite, Ba(Cr,S)O4, a new mineral from Jordan.","docAbstract":"Hashemite, Ba(Cr,S)O4, the isostructural chromate analogue of baryte, has been found in west-central Jordan. It is associated with chromian ettringite, apatite and calcite in a phosphatic carbonate rock analogous to the Hatrurim formation in Israel. The mineral is orthorhombic, Pnma, with a 9.112(2), b 5.541(1), c 7.343(1) A, Z = 4. Strongest XRD lines are 3.516(100), 3.171(80), 3.669(60), 2.175(60), 2.150(45) A. Hashemite occurs as small, euhedral, dark brown, commonly zoned crystals with an average D 4.59 g/cm3 and H. 31/2. It is biaxial positive; dark varieties have alpha 1.952(2), beta 1.960(2), gamma 1.977(2); light varieties have alpha 1.810(2), beta 1.813(2), gamma 1.824(2), 2Vgamma  35o-57o.-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":"Hauff, P.L., Foord, E., and Rosenblum, S., 1983, Hashemite, Ba(Cr,S)O4, a new mineral from Jordan.: American Mineralogist, v. 68, no. 11-12, p. 1223-1225.","startPage":"1223","endPage":"1225","numberOfPages":"3","costCenters":[],"links":[{"id":220828,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"},{"id":267375,"type":{"id":11,"text":"Document"},"url":"https://www.minsocam.org/ammin/AM68/AM68_1223.pdf"}],"volume":"68","issue":"11-12","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"505a2f84e4b0c8380cd5ce5d","contributors":{"authors":[{"text":"Hauff, P. L.","contributorId":95470,"corporation":false,"usgs":true,"family":"Hauff","given":"P.","email":"","middleInitial":"L.","affiliations":[],"preferred":false,"id":360711,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Foord, E.E.","contributorId":86835,"corporation":false,"usgs":true,"family":"Foord","given":"E.E.","email":"","affiliations":[],"preferred":false,"id":360710,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Rosenblum, S.","contributorId":85326,"corporation":false,"usgs":true,"family":"Rosenblum","given":"S.","email":"","affiliations":[],"preferred":false,"id":360709,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":70011267,"text":"70011267 - 1983 - Major and trace elements in Mahogany zone oil shale in two cores from the Green River Formation, piceance basin, Colorado","interactions":[],"lastModifiedDate":"2012-03-12T17:18:27","indexId":"70011267","displayToPublicDate":"1983-01-01T00:00:00","publicationYear":"1983","noYear":false,"publicationType":{"id":24,"text":"Conference Paper"},"publicationSubtype":{"id":19,"text":"Conference Paper"},"title":"Major and trace elements in Mahogany zone oil shale in two cores from the Green River Formation, piceance basin, Colorado","docAbstract":"The Parachute Creek Member of the lacustrine Green River Formation contains thick sequences of rich oil-shale. The richest sequence and the richest oil-shale bed occurring in the member are called the Mahogany zone and the Mahogany bed, respectively, and were deposited in ancient Lake Uinta. The name \"Mahogany\" is derived from the red-brown color imparted to the rock by its rich-kerogen content. Geochemical abundance and distribution of eight major and 18 trace elements were determined in the Mahogany zone sampled from two cores, U. S. Geological Survey core hole CR-2 and U. S. Bureau of Mines core hole O1-A (Figure 1). The oil shale from core hole CR-2 was deposited nearer the margin of Lake Uinta than oil shale from core hole O1-A. The major- and trace-element chemistry of the Mahogany zone from each of these two cores is compared using elemental abundances and Q-mode factor modeling. The results of chemical analyses of 44 CR-2 Mahogany samples and 76 O1-A Mahogany samples are summarized in Figure 2. The average geochemical abundances for shale (1) and black shale (2) are also plotted on Figure 2 for comparison. The elemental abundances in the samples from the two cores are similar for the majority of elements. Differences at the 95% probability level are higher concentrations of Ca, Cu, La, Ni, Sc and Zr in the samples from core hole CR-2 compared to samples from core hole O1-A and higher concentrations of As and Sr in samples from core hole O1-A compared to samples from core hole CR-2. These differences presumably reflect slight differences in depositional conditions or source material at the two sites. The Mahogany oil shale from the two cores has lower concentrations of most trace metals and higher concentrations of carbonate-related elements (Ca, Mg, Sr and Na) compared to the average shale and black shale. During deposition of the Mahogany oil shale, large quantities of carbonates were precipitated resulting in the enrichment of carbonate-related elements and dilution of most trace elements as pointed out in several previous studies. Q-mode factor modeling is a statistical method used to group samples on the basis of compositional similarities. Factor end-member samples are chosen by the model. All other sample compositions are represented by varying proportions of the factor end-members and grouped as to their highest proportion. The compositional similarities defined by the Q-mode model are helpful in understanding processes controlling multi-element distributions. The models for each core are essentially identical. A four-factor model explains 70% of the variance in the CR-2 data and 64% of the O1-A data (the average correlation coefficients are 0. 84 and 0. 80, respectively). Increasing the number of factors above 4 results in the addition of unique instead of common factors. Table I groups the elements based on high factor-loading scores (the amount of influence each element has in defining the model factors). Similar elemental associations are found in both cores. Elemental abundances are plotted as a function of core depth using a five-point weighted moving average of the original data to smooth the curve (Figure 3 and 4). The plots are grouped according to the four factors defined by the Q-mode models and show similar distributions for elements within the same factor. Factor 1 samples are rich in most trace metals. High oil yield and the presence of illite characterize the end-member samples for this factor (3, 4) suggesting that adsorption of metals onto clay particles or organic matter is controlling the distribution of the metals. Precipitation of some metals as sulfides is possible (5). Factor 2 samples are high in elements commonly associated with minerals of detrital or volcanogenic origin. Altered tuff beds and lenses are prevalent within the Mahogany zone. The CR-2 end-member samples for this factor contain analcime (3) which is an alteration product within the tuff beds of the Green River Formation. Th","largerWorkTitle":"Preprints Symposia","language":"English","issn":"05693799","usgsCitation":"Tuttle, M.L., Dean, W., and Parduhn, N.L., 1983, Major and trace elements in Mahogany zone oil shale in two cores from the Green River Formation, piceance basin, Colorado, <i>in</i> Preprints Symposia, v. 28, no. 1, p. 85-90.","startPage":"85","endPage":"90","numberOfPages":"6","costCenters":[],"links":[{"id":220827,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"28","issue":"1","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"505a4c0ae4b0c8380cd69972","contributors":{"authors":[{"text":"Tuttle, M. L.","contributorId":71992,"corporation":false,"usgs":true,"family":"Tuttle","given":"M.","email":"","middleInitial":"L.","affiliations":[],"preferred":false,"id":360707,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Dean, W.E.","contributorId":97099,"corporation":false,"usgs":true,"family":"Dean","given":"W.E.","email":"","affiliations":[],"preferred":false,"id":360708,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Parduhn, N. L.","contributorId":69136,"corporation":false,"usgs":true,"family":"Parduhn","given":"N.","email":"","middleInitial":"L.","affiliations":[],"preferred":false,"id":360706,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":1014529,"text":"1014529 - 1983 - Inbreeding in fish populations used for aquaculture","interactions":[],"lastModifiedDate":"2023-08-09T14:49:26.080773","indexId":"1014529","displayToPublicDate":"1983-01-01T00:00:00","publicationYear":"1983","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":853,"text":"Aquaculture","active":true,"publicationSubtype":{"id":10}},"title":"Inbreeding in fish populations used for aquaculture","docAbstract":"<p>The theoretical causes of inbreeding depression are reviewed. Studies to measure depression at a series of inbreeding levels in rainbow trout populations using the method of inbred-outbred half-sib families are discussed. While the actual depression estimates varied widely between populations and inbreeding levels, significant levels of depression were found in many hatchery, field, and brood stock performance traits after only one generation of brother-sister mating. Especially susceptible to inbreeding depression, were measures of growth based upon attained fish weight at a given age in each test situation examined: 147 day weight (0.0 to 19.1%), 364 day weight (6.2 to 62.8%), weight after 6 months in fishing pond (−4.6 to 25.4%), weight after 12 months in fishing pond (13.0 to 29.1%), 2-year male weight (11.3 to 55.3%), and 2-year female weight (10.2 to 57.0%). Other hatchery performance traits that showed inbreeding depression were: egg hatch-ability (−0.2 to 53.1%), fry survival (0.4 to 8.2%), feed conversion efficiency (5.0 to 9.0%), fish length at 2-years of age (4.7 to 36.9%), and egg mass produced at 2-years (12.1 to 57.0%). Field performance traits that yielded inbreeding depression were percent recovery of fish stocked (−2.5 to 41.1%) and biomass index (16.2 to 47.7%).</p><p>Literature on the effects of inbreeding in fish populations is reviewed and the breeding approaches for controlling the rate of inbreeding accumulation in brood stock populations are outlined and discussed.</p>","language":"English","publisher":"Elsevier","doi":"10.1016/0044-8486(83)90402-7","usgsCitation":"Kincaid, H.L., 1983, Inbreeding in fish populations used for aquaculture: Aquaculture, v. 33, no. 1-4, p. 215-227, https://doi.org/10.1016/0044-8486(83)90402-7.","productDescription":"13 p.","startPage":"215","endPage":"227","numberOfPages":"13","costCenters":[{"id":365,"text":"Leetown Science Center","active":true,"usgs":true}],"links":[{"id":130726,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"33","issue":"1-4","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e49fce4b07f02db5f58f7","contributors":{"authors":[{"text":"Kincaid, Harold L.","contributorId":15978,"corporation":false,"usgs":true,"family":"Kincaid","given":"Harold","email":"","middleInitial":"L.","affiliations":[],"preferred":false,"id":320535,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":70012009,"text":"70012009 - 1983 - Geotherm: the U.S. geological survey geothermal information system","interactions":[],"lastModifiedDate":"2013-01-21T15:50:49","indexId":"70012009","displayToPublicDate":"1983-01-01T00:00:00","publicationYear":"1983","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":"Geotherm: the U.S. geological survey geothermal information system","docAbstract":"GEOTHERM is a comprehensive system of public databases and software used to store, locate, and evaluate information on the geology, geochemistry, and hydrology of geothermal systems. Three main databases address the general characteristics of geothermal wells and fields, and the chemical properties of geothermal fluids; the last database is currently the most active. System tasks are divided into four areas: (1) data acquisition and entry, involving data entry via word processors and magnetic tape; (2) quality assurance, including the criteria and standards handbook and front-end data-screening programs; (3) operation, involving database backups and information extraction; and (4) user assistance, preparation of such items as application programs, and a quarterly newsletter. The principal task of GEOTHERM is to provide information and research support for the conduct of national geothermal-resource assessments. The principal users of GEOTHERM are those involved with the Geothermal Research Program of the U.S. Geological Survey. Information in the system is available to the public on request. ?? 1983.","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(83)90034-1","issn":"00983004","usgsCitation":"Bliss, J.D., and Rapport, A., 1983, Geotherm: the U.S. geological survey geothermal information system: Computers & Geosciences, v. 9, no. 1, p. 35-39, https://doi.org/10.1016/0098-3004(83)90034-1.","startPage":"35","endPage":"39","numberOfPages":"5","costCenters":[],"links":[{"id":266193,"type":{"id":10,"text":"Digital Object Identifier"},"url":"https://dx.doi.org/10.1016/0098-3004(83)90034-1"},{"id":222179,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"9","issue":"1","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"505a28c8e4b0c8380cd5a3e0","contributors":{"authors":[{"text":"Bliss, J. D.","contributorId":25564,"corporation":false,"usgs":true,"family":"Bliss","given":"J.","email":"","middleInitial":"D.","affiliations":[],"preferred":false,"id":362509,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Rapport, A.","contributorId":97109,"corporation":false,"usgs":true,"family":"Rapport","given":"A.","email":"","affiliations":[],"preferred":false,"id":362510,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":70012010,"text":"70012010 - 1983 - Geo-botanical evidence of Late Quaternary mass wasting in block field areas of Virginia","interactions":[],"lastModifiedDate":"2019-08-14T10:52:24","indexId":"70012010","displayToPublicDate":"1983-01-01T00:00:00","publicationYear":"1983","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1425,"text":"Earth Surface Processes and Landforms","active":true,"publicationSubtype":{"id":10}},"title":"Geo-botanical evidence of Late Quaternary mass wasting in block field areas of Virginia","docAbstract":"<p>Studies of block fields at Massanutten Mountain, Virginia, document and provide information on the magnitude and frequency of mass movement on these coarse-grained slopes. Although Pleistocene periglacial climate may have facilitated original formation of block fields, some block fields now continue to spread downslope during intense runoff events. Present block-field mass wasting may be the principal erosional process in these areas of resistant rock.</p>","largerWorkType":{"id":2,"text":"Article"},"largerWorkTitle":"Earth Surface Processes and Landforms","largerWorkSubtype":{"id":10,"text":"Journal Article"},"language":"English","publisher":"Wiley","doi":"10.1002/esp.3290080505","usgsCitation":"Hupp, C.R., 1983, Geo-botanical evidence of Late Quaternary mass wasting in block field areas of Virginia: Earth Surface Processes and Landforms, v. 8, no. 5, p. 439-450, https://doi.org/10.1002/esp.3290080505.","startPage":"439","endPage":"450","numberOfPages":"12","costCenters":[{"id":37277,"text":"WMA - Earth System Processes Division","active":true,"usgs":true}],"links":[{"id":222180,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"},{"id":269259,"type":{"id":10,"text":"Digital Object Identifier"},"url":"https://dx.doi.org/10.1002/esp.3290080505"}],"country":"United States","state":"Virginia","otherGeospatial":"Massanutten Mountain","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -78.25286865234375,\n              38.958340924837714\n            ],\n            [\n              -78.35861206054687,\n              38.99570671505043\n            ],\n            [\n              -78.65249633789062,\n              38.753012320665185\n            ],\n            [\n              -78.84063720703123,\n              38.39118617958438\n            ],\n            [\n              -78.75,\n              38.35350340353833\n            ],\n            [\n              -78.46023559570312,\n              38.687653678261704\n            ],\n            [\n              -78.25286865234375,\n              38.958340924837714\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","volume":"8","issue":"5","noUsgsAuthors":false,"publicationDate":"2006-07-18","publicationStatus":"PW","scienceBaseUri":"505a1597e4b0c8380cd54eae","contributors":{"authors":[{"text":"Hupp, Cliff R. 0000-0003-1853-9197 crhupp@usgs.gov","orcid":"https://orcid.org/0000-0003-1853-9197","contributorId":2344,"corporation":false,"usgs":true,"family":"Hupp","given":"Cliff","email":"crhupp@usgs.gov","middleInitial":"R.","affiliations":[{"id":436,"text":"National Research Program - Eastern Branch","active":true,"usgs":true},{"id":37277,"text":"WMA - Earth System Processes Division","active":true,"usgs":true}],"preferred":true,"id":362511,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":70012011,"text":"70012011 - 1983 - Mammoth Lakes earthquakes and ground uplift: precursors to possible volcanic activity ( USA)?","interactions":[],"lastModifiedDate":"2012-03-12T17:19:09","indexId":"70012011","displayToPublicDate":"1983-01-01T00:00:00","publicationYear":"1983","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":"Mammoth Lakes earthquakes and ground uplift: precursors to possible volcanic activity ( USA)?","docAbstract":"Recent seismicity and ground uplift in the area are described. A comparison with other areas in the Cascades is made and the possibility of the Long Valley Magma Chamber as a source for eruptions is discussed. -P.N.Chroston","largerWorkType":{"id":2,"text":"Article"},"largerWorkTitle":"Earthquake Information Bulletin (USGS)","largerWorkSubtype":{"id":10,"text":"Journal Article"},"language":"English","usgsCitation":"Bailey, R., 1983, Mammoth Lakes earthquakes and ground uplift: precursors to possible volcanic activity ( USA)?: Earthquake Information Bulletin (USGS), v. 15, no. 3, p. 88-101.","startPage":"88","endPage":"101","numberOfPages":"14","costCenters":[],"links":[{"id":222233,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"15","issue":"3","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"505a4c59e4b0c8380cd69bbc","contributors":{"authors":[{"text":"Bailey, R. A.","contributorId":87531,"corporation":false,"usgs":true,"family":"Bailey","given":"R. A.","affiliations":[],"preferred":false,"id":362512,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":70012024,"text":"70012024 - 1983 - Hydrothermal reactivity of saponite","interactions":[],"lastModifiedDate":"2018-01-26T17:54:05","indexId":"70012024","displayToPublicDate":"1983-01-01T00:00:00","publicationYear":"1983","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1245,"text":"Clays and Clay Minerals","onlineIssn":"1552-8367","printIssn":"0009-8604","active":true,"publicationSubtype":{"id":10}},"title":"Hydrothermal reactivity of saponite","docAbstract":"<p>Saponite crystallizes from amorphous gel having an ideal saponite composition within 7 days at all experimental temperatures between 300° and 550°C at 1 kbar pressure. Reactions subsequent to this initial crystallization vary in type and degree, depending on the temperature of reaction and the type of interlayer cation. Above 450°C the intitially crystallized K-saponite dissolves, and talc and phlogopite nucleate and grow as discrete phases. At 450°C the initial K-saponite reacts to form talc and phlogopite layers, but the reaction proceeds via intracrystalline layer transformations rather than via dissolution and precipitation, producing a mixture of fully ordered, interstratified talc/saponite and fully ordered saponite/ phlogopite. The K-saponite shows subtle signs of reaction at 400°C after 200 days: this temperature is at least 150°C lower than experimental reaction temperatures previously reported for saponites. No reactions beyond the initial crystallization of saponite were observed below 400°C. K-saponite reacts more rapidly than either Na-saponite or Ca-saponite above 400°C and the Na-saponite and Ca-saponite produce no mica iayers during their transformation to mixed-layer clays. Interstratified talc/saponite formed in the Na-saponite system, and the Ca-saponite system produced both talc/saponite and chlorite/saponite.</p>","language":"English","publisher":"The Clay Minerals Society","doi":"10.1346/CCMN.1983.0310101","usgsCitation":"Whitney, G., 1983, Hydrothermal reactivity of saponite: Clays and Clay Minerals, v. 31, no. 1, p. 1-8, https://doi.org/10.1346/CCMN.1983.0310101.","productDescription":"8 p.","startPage":"1","endPage":"8","costCenters":[],"links":[{"id":222389,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"31","issue":"1","noUsgsAuthors":false,"publicationDate":"2024-04-02","publicationStatus":"PW","scienceBaseUri":"505a37a7e4b0c8380cd61058","contributors":{"authors":[{"text":"Whitney, Gene","contributorId":27049,"corporation":false,"usgs":true,"family":"Whitney","given":"Gene","email":"","affiliations":[],"preferred":false,"id":362544,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":70012025,"text":"70012025 - 1983 - SUBMICROSCOPIC ( less than 1 mu m) MINERAL CONTENTS OF VITRINITES IN SELECTED BITUMINOUS COAL BEDS.","interactions":[],"lastModifiedDate":"2012-03-12T17:19:03","indexId":"70012025","displayToPublicDate":"1983-01-01T00:00:00","publicationYear":"1983","noYear":false,"publicationType":{"id":24,"text":"Conference Paper"},"publicationSubtype":{"id":19,"text":"Conference Paper"},"title":"SUBMICROSCOPIC ( less than 1 mu m) MINERAL CONTENTS OF VITRINITES IN SELECTED BITUMINOUS COAL BEDS.","docAbstract":"An important aspect of the petrographic description of coal is the characterization of coal quality, including chemical attributes. For geologic investigations, data on the concentrations, distribution, and modes of occurrence of minor and trace elements provide a basis for reconstructing the probable geochemical environment of the swamp material that was converted into peat, and the geochemical conditions that prevailed during and subsequent to coalification. We have been using electron (EPMA) and proton (PIXE) microprobe analytical methods to obtain data on the chemical characteristics of specific coal constituents in their original associations within coal samples. The present study is aimed at evaluation of the nature of mineral occurrences and heterogeneous elemental concentrations within vitrinites. Vitrinites are usually the most abundant, and therefore most important, maceral group in bituminous coal. 8 refs.","largerWorkTitle":"Proceedings, Annual Conference - Microbeam Analysis Society","conferenceTitle":"Microbeam Analysis 1983, Proceedings of the 18th Annual Conference of the Microbeam Analysis Society.","conferenceLocation":"Phoenix, AZ, USA","language":"English","issn":"01466275","usgsCitation":"Minkin, J., Chao, E.C., Thompson, C., Wandless, M., Dulong, F., Larson, R., and Neuzil, S., 1983, SUBMICROSCOPIC ( less than 1 mu m) MINERAL CONTENTS OF VITRINITES IN SELECTED BITUMINOUS COAL BEDS., <i>in</i> Proceedings, Annual Conference - Microbeam Analysis Society, Phoenix, AZ, USA, p. 27-30.","startPage":"27","endPage":"30","numberOfPages":"4","costCenters":[],"links":[{"id":222390,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"505aafa0e4b0c8380cd876cb","contributors":{"editors":[{"text":"Gooley Ron","contributorId":128415,"corporation":true,"usgs":false,"organization":"Gooley Ron","id":536243,"contributorType":{"id":2,"text":"Editors"},"rank":1}],"authors":[{"text":"Minkin, J.A.","contributorId":38588,"corporation":false,"usgs":true,"family":"Minkin","given":"J.A.","affiliations":[],"preferred":false,"id":362547,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Chao, E. C. T.","contributorId":96713,"corporation":false,"usgs":true,"family":"Chao","given":"E.","email":"","middleInitial":"C. T.","affiliations":[],"preferred":false,"id":362551,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Thompson, C.L.","contributorId":12189,"corporation":false,"usgs":true,"family":"Thompson","given":"C.L.","email":"","affiliations":[],"preferred":false,"id":362545,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Wandless, M.-V.","contributorId":54611,"corporation":false,"usgs":true,"family":"Wandless","given":"M.-V.","email":"","affiliations":[],"preferred":false,"id":362548,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"Dulong, F.T.","contributorId":81490,"corporation":false,"usgs":true,"family":"Dulong","given":"F.T.","affiliations":[],"preferred":false,"id":362550,"contributorType":{"id":1,"text":"Authors"},"rank":5},{"text":"Larson, R.R.","contributorId":29803,"corporation":false,"usgs":true,"family":"Larson","given":"R.R.","email":"","affiliations":[],"preferred":false,"id":362546,"contributorType":{"id":1,"text":"Authors"},"rank":6},{"text":"Neuzil, S.G.","contributorId":73339,"corporation":false,"usgs":true,"family":"Neuzil","given":"S.G.","email":"","affiliations":[],"preferred":false,"id":362549,"contributorType":{"id":1,"text":"Authors"},"rank":7}]}}
,{"id":70011237,"text":"70011237 - 1983 - FINDINGS ON THE USE OF LANDSAT-3 RETURN BEAM VIDICON IMAGERY FOR DETECTING LAND USE AND LAND COVER CHANGES.","interactions":[],"lastModifiedDate":"2012-03-12T17:18:32","indexId":"70011237","displayToPublicDate":"1983-01-01T00:00:00","publicationYear":"1983","noYear":false,"publicationType":{"id":24,"text":"Conference Paper"},"publicationSubtype":{"id":19,"text":"Conference Paper"},"title":"FINDINGS ON THE USE OF LANDSAT-3 RETURN BEAM VIDICON IMAGERY FOR DETECTING LAND USE AND LAND COVER CHANGES.","docAbstract":"The spatial resolution of imagery from the return beam vidicon (RBV) camera aboard the Landsat-3 satellite suggested that such data might prove useful in inspecting land use and land cover maps. In this study, a 1972 land use and land cover map derived from aerial photographs is compared with a 1978 Landsat RBV image to delineate areas of change. Findings indicate RBV imagery useful in establishing the fact of change and in identifying gross category changes.","largerWorkTitle":"Technical Papers of the American Congress of Surveying and Mapping","conferenceTitle":"Technical Papers of the 43rd Annual Meeting of the American Congress on Surveying and Mapping.","conferenceLocation":"Washington, DC, USA","language":"English","publisher":"American Congress on Surveying & Mapping","publisherLocation":"Falls Church, VA, USA","usgsCitation":"Milazzo, V.A., 1983, FINDINGS ON THE USE OF LANDSAT-3 RETURN BEAM VIDICON IMAGERY FOR DETECTING LAND USE AND LAND COVER CHANGES., <i>in</i> Technical Papers of the American Congress of Surveying and Mapping, Washington, DC, USA, p. 366-375.","startPage":"366","endPage":"375","numberOfPages":"10","costCenters":[],"links":[{"id":221100,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"505a0e76e4b0c8380cd53477","contributors":{"authors":[{"text":"Milazzo, Valerie A.","contributorId":88717,"corporation":false,"usgs":true,"family":"Milazzo","given":"Valerie","email":"","middleInitial":"A.","affiliations":[],"preferred":false,"id":360635,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":70011238,"text":"70011238 - 1983 - CHEMICAL STRUCTURES IN COAL: GEOCHEMICAL EVIDENCE FOR THE PRESENCE OF MIXED STRUCTURAL COMPONENTS.","interactions":[],"lastModifiedDate":"2012-03-12T17:18:31","indexId":"70011238","displayToPublicDate":"1983-01-01T00:00:00","publicationYear":"1983","noYear":false,"publicationType":{"id":24,"text":"Conference Paper"},"publicationSubtype":{"id":19,"text":"Conference Paper"},"title":"CHEMICAL STRUCTURES IN COAL: GEOCHEMICAL EVIDENCE FOR THE PRESENCE OF MIXED STRUCTURAL COMPONENTS.","docAbstract":"The purpose of this paper is to summarize work on the chemical structural components of coal, comparing them with their possible plant precursors in modern peat. Solid-state **1**3C nuclear magnetic resonance (NMR), infrared spectroscopy (IR), elemental analysis and, in some cases, individual compound analyses formed the bases for these comparisons.","conferenceTitle":"Proceedings - 1983 International Conference on Coal Science.","conferenceLocation":"Pittsburgh, PA, USA","language":"English","usgsCitation":"Hatcher, P.G., Breger, I.A., Maciel, G., and Szeverenyi, N., 1983, CHEMICAL STRUCTURES IN COAL: GEOCHEMICAL EVIDENCE FOR THE PRESENCE OF MIXED STRUCTURAL COMPONENTS., Proceedings - 1983 International Conference on Coal Science., Pittsburgh, PA, USA, p. 310-313.","startPage":"310","endPage":"313","numberOfPages":"4","costCenters":[],"links":[{"id":221159,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"5059f2cde4b0c8380cd4b3ad","contributors":{"authors":[{"text":"Hatcher, Patrick G.","contributorId":93625,"corporation":false,"usgs":true,"family":"Hatcher","given":"Patrick","email":"","middleInitial":"G.","affiliations":[],"preferred":false,"id":360639,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Breger, Irving A.","contributorId":65205,"corporation":false,"usgs":true,"family":"Breger","given":"Irving","email":"","middleInitial":"A.","affiliations":[],"preferred":false,"id":360637,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Maciel, G.E.","contributorId":43910,"corporation":false,"usgs":true,"family":"Maciel","given":"G.E.","email":"","affiliations":[],"preferred":false,"id":360636,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Szeverenyi, N.M.","contributorId":83663,"corporation":false,"usgs":true,"family":"Szeverenyi","given":"N.M.","email":"","affiliations":[],"preferred":false,"id":360638,"contributorType":{"id":1,"text":"Authors"},"rank":4}]}}
,{"id":70012036,"text":"70012036 - 1983 - NEW HORIZONS FOR THE NATIONAL HIGH-ALTITUDE PHOTOGRAPHY PROGRAM.","interactions":[],"lastModifiedDate":"2012-03-12T17:19:08","indexId":"70012036","displayToPublicDate":"1983-01-01T00:00:00","publicationYear":"1983","noYear":false,"publicationType":{"id":24,"text":"Conference Paper"},"publicationSubtype":{"id":19,"text":"Conference Paper"},"title":"NEW HORIZONS FOR THE NATIONAL HIGH-ALTITUDE PHOTOGRAPHY PROGRAM.","docAbstract":"The National High-Altitude Photography Program (NHAP) is a multi-Federal agency activity to acquire uniform imagery for the establishment of a national high-altitude photographic data base. Since the inception of NHAP in 1980, black-and-white and color infrared stereoscopic imagery has been acquired for about 50% of the 3,000,000 square miles in the conterminous United States. An additional 40% of the 48-State area is under contract to private aerial survey firms, and the sixth and final contract to achieve complete once-over coverage will be awarded early in 1985. Extensive use has been made of the newly established data base. The participating agencies have begun studies to define the requirements for a maintenance program which would provide cyclic coverage of the conterminous United States and imagery for specific agency needs.","conferenceTitle":"Proceedings - Pecora VIII Symposium: Satellite Land Remote Sensing Advancements for the Eighties.","conferenceLocation":"Sioux Falls, ND, USA","language":"English","publisher":"Augustana Coll","publisherLocation":"Sioux Falls, SD, USA","usgsCitation":"Bermel, P.F., 1983, NEW HORIZONS FOR THE NATIONAL HIGH-ALTITUDE PHOTOGRAPHY PROGRAM., Proceedings - Pecora VIII Symposium: Satellite Land Remote Sensing Advancements for the Eighties., Sioux Falls, ND, USA.","startPage":"172","costCenters":[],"links":[{"id":222569,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"505a6144e4b0c8380cd718a7","contributors":{"authors":[{"text":"Bermel, Peter F.","contributorId":43915,"corporation":false,"usgs":true,"family":"Bermel","given":"Peter","email":"","middleInitial":"F.","affiliations":[],"preferred":false,"id":362581,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":70012038,"text":"70012038 - 1983 - Sea ice melting in the marginal ice zone","interactions":[],"lastModifiedDate":"2024-06-28T16:13:08.959399","indexId":"70012038","displayToPublicDate":"1983-01-01T00:00:00","publicationYear":"1983","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":9107,"text":"Journal of Geophysical Research - Oceans","active":true,"publicationSubtype":{"id":10}},"title":"Sea ice melting in the marginal ice zone","docAbstract":"<p><span>The heat and salt flux boundary conditions together with the freezing curve relationship are a necessary component of any ice-sea water thermodynamic model. A neutral two-layer oceanic planetary boundary layer model that incorporates these boundary conditions gives the following results: The interfacial salinity is within 10% of the far-field salinity for conditions commonly encountered in the MIZ and depends only on the turbulent Lewis number and the far-field temperature and salinity. The predicted melt rates agree with the limited field observations, of the order of 1 m day</span><sup>−1</sup><span>. The Obukov lengths, determined from the predicted interface conditions and melt rates, are generally much greater than the Ekman layer thicknesses; hence, the surface buoyancy flux has little effect on the turbulence in the planetary boundary layer.</span></p>","language":"English","publisher":"American Geophysical Union","doi":"10.1029/JC088iC05p02841","issn":"01480227","usgsCitation":"Josberger, E., 1983, Sea ice melting in the marginal ice zone: Journal of Geophysical Research - Oceans, v. 88, no. C5, p. 2841-2844, https://doi.org/10.1029/JC088iC05p02841.","productDescription":"4 p.","startPage":"2841","endPage":"2844","numberOfPages":"4","costCenters":[],"links":[{"id":222571,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"88","issue":"C5","noUsgsAuthors":false,"publicationDate":"2012-09-20","publicationStatus":"PW","scienceBaseUri":"505b87dae4b08c986b3166b5","contributors":{"authors":[{"text":"Josberger, E.G.","contributorId":61161,"corporation":false,"usgs":true,"family":"Josberger","given":"E.G.","email":"","affiliations":[],"preferred":false,"id":362584,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":70135762,"text":"70135762 - 1983 - Bank margin environment","interactions":[],"lastModifiedDate":"2022-12-30T16:37:13.581906","indexId":"70135762","displayToPublicDate":"1983-01-01T00:00:00","publicationYear":"1983","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":606,"text":"AAPG Memoir","active":true,"publicationSubtype":{"id":10}},"chapter":"9","title":"Bank margin environment","docAbstract":"<p>No abstract available.</p>","largerWorkType":{"id":4,"text":"Book"},"largerWorkTitle":"Carbonate depositional environments","largerWorkSubtype":{"id":15,"text":"Monograph"},"language":"English","publisher":"American Association of Petroleum Geologists","usgsCitation":"Halley, R., Harris, P., and Hine, A.C., 1983, Bank margin environment: AAPG Memoir, v. 33, p. 463-483.","productDescription":"21 p.","startPage":"463","endPage":"483","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[{"id":186,"text":"Coastal and Marine Geology Program","active":true,"usgs":true}],"links":[{"id":296729,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"},{"id":296728,"rank":2,"type":{"id":15,"text":"Index Page"},"url":"https://archives.datapages.com/data/specpubs/carbona3/data/a043/a043/0001/0450/0463.htm"}],"volume":"33","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"549165bee4b0d0759afaad7e","contributors":{"authors":[{"text":"Halley, Robert B.","contributorId":45692,"corporation":false,"usgs":true,"family":"Halley","given":"Robert B.","affiliations":[{"id":678,"text":"Woods Hole Coastal and Marine Science Center","active":true,"usgs":true}],"preferred":false,"id":536837,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Harris, Paul M.","contributorId":11530,"corporation":false,"usgs":true,"family":"Harris","given":"Paul M.","affiliations":[],"preferred":false,"id":536838,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Hine, Albert C.","contributorId":87580,"corporation":false,"usgs":true,"family":"Hine","given":"Albert","email":"","middleInitial":"C.","affiliations":[],"preferred":false,"id":536839,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":70010884,"text":"70010884 - 1983 - ESTIMATION OF RESPONSE-SPECTRAL VALUES AS FUNCTIONS OF MAGNITUDE, DISTANCE, AND SITE CONDITIONS.","interactions":[],"lastModifiedDate":"2012-03-12T17:18:30","indexId":"70010884","displayToPublicDate":"1983-01-01T00:00:00","publicationYear":"1983","noYear":false,"publicationType":{"id":24,"text":"Conference Paper"},"publicationSubtype":{"id":19,"text":"Conference Paper"},"title":"ESTIMATION OF RESPONSE-SPECTRAL VALUES AS FUNCTIONS OF MAGNITUDE, DISTANCE, AND SITE CONDITIONS.","docAbstract":"Horizontal pseudo-velocity response was analyzed for twelve shallow earthquakes in western North America. Estimation of response-spectral values was related to magnitude, distance and site conditions. Errors in the methods are analyzed.","largerWorkTitle":"National Bureau of Standards, Special Publication","conferenceTitle":"Wind and Seismic Effects, Proceedings of the 14th Joint Panel Conference of the US-Japan Cooperative Program in Natural Resources.","conferenceLocation":"Washington, DC, USA","language":"English","publisher":"NBS","publisherLocation":"Washington, DC, USA","issn":"00831883","usgsCitation":"Joyner, W.B., and Boore, D., 1983, ESTIMATION OF RESPONSE-SPECTRAL VALUES AS FUNCTIONS OF MAGNITUDE, DISTANCE, AND SITE CONDITIONS., <i>in</i> National Bureau of Standards, Special Publication, Washington, DC, USA, p. 53-74.","startPage":"53","endPage":"74","numberOfPages":"22","costCenters":[],"links":[{"id":221077,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"505a0469e4b0c8380cd5097a","contributors":{"editors":[{"text":"Chung Riley M.Lew H.S.Kovacs William D.","contributorId":128431,"corporation":true,"usgs":false,"organization":"Chung Riley M.Lew H.S.Kovacs William D.","id":536241,"contributorType":{"id":2,"text":"Editors"},"rank":1}],"authors":[{"text":"Joyner, W. B.","contributorId":70746,"corporation":false,"usgs":true,"family":"Joyner","given":"W.","email":"","middleInitial":"B.","affiliations":[],"preferred":false,"id":359838,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Boore, D.M. 0000-0002-8605-9673","orcid":"https://orcid.org/0000-0002-8605-9673","contributorId":64226,"corporation":false,"usgs":true,"family":"Boore","given":"D.M.","affiliations":[],"preferred":false,"id":359837,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":70011189,"text":"70011189 - 1983 - EFFICIENT TRANSFER OF DATA BETWEEN MAPS OF DIFFERENT PROJECTIONS.","interactions":[],"lastModifiedDate":"2012-03-12T17:18:27","indexId":"70011189","displayToPublicDate":"1983-01-01T00:00:00","publicationYear":"1983","noYear":false,"publicationType":{"id":24,"text":"Conference Paper"},"publicationSubtype":{"id":19,"text":"Conference Paper"},"title":"EFFICIENT TRANSFER OF DATA BETWEEN MAPS OF DIFFERENT PROJECTIONS.","docAbstract":"There are several ways to transfer data from an existing map to another map by computer. If the projection and parameters of both maps are known, analytic formulas may be used to convert rectangular coordinates of the first map to latitude and longitude and then to rectangular coordinates of the second map. This general solution, contained in a USGS computer program, involves inverse formulas for the first projection and forward formulas for the second projection.","largerWorkTitle":"Technical Papers of the American Congress of Surveying and Mapping","conferenceTitle":"Technical Papers of the 43rd Annual Meeting of the American Congress on Surveying and Mapping.","conferenceLocation":"Washington, DC, USA","language":"English","publisher":"American Congress on Surveying & Mapping","publisherLocation":"Falls Church, VA, USA","usgsCitation":"Snyder, J., 1983, EFFICIENT TRANSFER OF DATA BETWEEN MAPS OF DIFFERENT PROJECTIONS., <i>in</i> Technical Papers of the American Congress of Surveying and Mapping, Washington, DC, USA, p. 332-340.","startPage":"332","endPage":"340","numberOfPages":"9","costCenters":[],"links":[{"id":221431,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"505a045ce4b0c8380cd5092e","contributors":{"authors":[{"text":"Snyder, John P.","contributorId":16878,"corporation":false,"usgs":true,"family":"Snyder","given":"John P.","affiliations":[],"preferred":false,"id":360491,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":1013603,"text":"1013603 - 1983 - Flush exposure and injection immunization of rainbow trout to selected DNP conjugates","interactions":[],"lastModifiedDate":"2013-01-18T11:40:51","indexId":"1013603","displayToPublicDate":"1983-01-01T00:00:00","publicationYear":"1983","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":"Flush exposure and injection immunization of rainbow trout to selected DNP conjugates","largerWorkType":{"id":2,"text":"Article"},"largerWorkTitle":"Developmental and Comparative Immunology","largerWorkSubtype":{"id":10,"text":"Journal Article"},"language":"English","publisher":"Elsevier","doi":"10.1016/0145-305X(83)90007-1","collaboration":"491/FH","usgsCitation":"Anderson, D.P., Merchant, B., Dixon, O.W., and Schott C, L.E., 1983, Flush exposure and injection immunization of rainbow trout to selected DNP conjugates: Developmental and Comparative Immunology, v. 7, no. 2, p. 261-268, https://doi.org/10.1016/0145-305X(83)90007-1.","productDescription":"p. 261-268","startPage":"261","endPage":"268","numberOfPages":"8","costCenters":[{"id":365,"text":"Leetown Science Center","active":true,"usgs":true}],"links":[{"id":132156,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"},{"id":265927,"type":{"id":10,"text":"Digital Object Identifier"},"url":"https://dx.doi.org/10.1016/0145-305X(83)90007-1"}],"volume":"7","issue":"2","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e49d6e4b07f02db5de614","contributors":{"authors":[{"text":"Anderson, D. P.","contributorId":32469,"corporation":false,"usgs":true,"family":"Anderson","given":"D.","email":"","middleInitial":"P.","affiliations":[],"preferred":false,"id":318830,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Merchant, B.","contributorId":79432,"corporation":false,"usgs":true,"family":"Merchant","given":"B.","email":"","affiliations":[],"preferred":false,"id":318831,"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":318833,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Schott C, Lizzio E. F. E. F.","contributorId":99941,"corporation":false,"usgs":true,"family":"Schott C","given":"Lizzio","suffix":"E. F.","email":"","middleInitial":"E. F.","affiliations":[],"preferred":false,"id":318832,"contributorType":{"id":1,"text":"Authors"},"rank":4}]}}
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