{"pageNumber":"5260","pageRowStart":"131475","pageSize":"25","recordCount":184617,"records":[{"id":1013811,"text":"1013811 - 1983 - What's New : Parker new scientific director","interactions":[],"lastModifiedDate":"2012-02-02T00:04:29","indexId":"1013811","displayToPublicDate":"1983-01-01T00:00:00","publicationYear":"1983","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1624,"text":"Farm Pond Harvest","active":true,"publicationSubtype":{"id":10}},"title":"What's New : Parker new scientific director","largerWorkType":{"id":2,"text":"Article"},"largerWorkTitle":"Farm Pond Harvest","largerWorkSubtype":{"id":10,"text":"Journal Article"},"language":"English","collaboration":"None/TIS","usgsCitation":"Gutsell, G., 1983, What's New : Parker new scientific director: Farm Pond Harvest, v. 17, no. 1, p. 2-3.","productDescription":"p. 2-3","startPage":"2","endPage":"3","numberOfPages":"2","costCenters":[{"id":365,"text":"Leetown Science Center","active":true,"usgs":true}],"links":[{"id":131905,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"17","issue":"1","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e49cce4b07f02db5d8ce0","contributors":{"authors":[{"text":"Gutsell, G.S.","contributorId":88694,"corporation":false,"usgs":true,"family":"Gutsell","given":"G.S.","email":"","affiliations":[],"preferred":false,"id":319278,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":1013809,"text":"1013809 - 1983 - What's New : Keep fish culture sites free of rats","interactions":[],"lastModifiedDate":"2012-02-02T00:04:29","indexId":"1013809","displayToPublicDate":"1983-01-01T00:00:00","publicationYear":"1983","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1624,"text":"Farm Pond Harvest","active":true,"publicationSubtype":{"id":10}},"title":"What's New : Keep fish culture sites free of rats","largerWorkType":{"id":2,"text":"Article"},"largerWorkTitle":"Farm Pond Harvest","largerWorkSubtype":{"id":10,"text":"Journal Article"},"language":"English","collaboration":"None/TIS","usgsCitation":"Gutsell, G., 1983, What's New : Keep fish culture sites free of rats: Farm Pond Harvest, v. 17, no. 1.","productDescription":"3 p.","startPage":"3","numberOfPages":"3","costCenters":[{"id":365,"text":"Leetown Science Center","active":true,"usgs":true}],"links":[{"id":131879,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"17","issue":"1","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e49dee4b07f02db5e2870","contributors":{"authors":[{"text":"Gutsell, G.S.","contributorId":88694,"corporation":false,"usgs":true,"family":"Gutsell","given":"G.S.","email":"","affiliations":[],"preferred":false,"id":319276,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":70011332,"text":"70011332 - 1983 - Snow and ice in a changing hydrological world","interactions":[],"lastModifiedDate":"2024-01-22T16:20:10.42955","indexId":"70011332","displayToPublicDate":"1983-01-01T00:00:00","publicationYear":"1983","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1927,"text":"Hydrological Sciences Journal","active":true,"publicationSubtype":{"id":10}},"title":"Snow and ice in a changing hydrological world","docAbstract":"<p><span>On the occasion of the 60th anniversary of the International Association of Hydrological Sciences, the 100th and 50th anniversaries of the First and Second International Polar Years, and the 25th anniversary of the International Geophysical Year, it seems appropriate to re-examine the world's water balance and the role of snow and ice in the global hydrological climatic system. Snow cover on land (especially in the Northern Hemisphere) and sea ice (especially in the Southern Hemisphere) vary seasonally, and this seasonal change has an important effect on the world climate because snow and sea ice reflect solar radiation efficiently and affect other heat flow processes between atmosphere and land or ocean. Glaciers, including ice sheets, store most of the fresh water on Earth, but change dimensions relatively slowly. There is no clear evidence that the glacier ice volume currently is declining, but more needs to be known about mountain glacier and ice sheet mass balances. The current rise in sea level poses an enigma: thermal expansion of the oceans may account for half of the present rise, but the other half is unexplained. Although major changes in the large ice sheets take place over time scales of 10</span><sup>4</sup><span>&nbsp;to 10</span><sup>5</sup><span>&nbsp;years, marine ice sheets may be subject to rapid disintegration due to grounding line instability, perhaps accompanied by surging. Ice cores may produce remarkably complete histories of air temperature, precipitation, fallout, and atmospheric composition. A recent core through the Greenland Ice Sheet shows an abrupt transition from glacial to modern climate just over 10000 years ago, suggesting that climate is an “almost intransitive” system. Because of the possibility of abrupt climate transitions and the uncertain stability of the West Antarctic Ice Sheet, future climatic variations are difficult to predict. The calculated heating of the atmosphere in the polar regions due to CO</span><sub>2</sub><span>&nbsp;increase is, therefore, of special interest.</span></p>","language":"English","publisher":"Taylor & Francis","doi":"10.1080/02626668309491140","usgsCitation":"Meier, M.F., 1983, Snow and ice in a changing hydrological world: Hydrological Sciences Journal, v. 28, no. 1, p. 3-22, https://doi.org/10.1080/02626668309491140.","productDescription":"20 p.","startPage":"3","endPage":"22","numberOfPages":"20","costCenters":[],"links":[{"id":480236,"rank":2,"type":{"id":40,"text":"Open Access Publisher Index Page"},"url":"https://doi.org/10.1080/02626668309491140","text":"Publisher Index Page"},{"id":220700,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"28","issue":"1","noUsgsAuthors":false,"publicationDate":"2009-12-24","publicationStatus":"PW","scienceBaseUri":"505b91b1e4b08c986b319a33","contributors":{"authors":[{"text":"Meier, M. F.","contributorId":98713,"corporation":false,"usgs":true,"family":"Meier","given":"M.","email":"","middleInitial":"F.","affiliations":[],"preferred":false,"id":360856,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":70011996,"text":"70011996 - 1983 - Groundwater contamination by organic bases derived from coal-tar wastes","interactions":[],"lastModifiedDate":"2024-02-12T15:48:03.766099","indexId":"70011996","displayToPublicDate":"1983-01-01T00:00:00","publicationYear":"1983","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1571,"text":"Environmental Toxicology and Chemistry","active":true,"publicationSubtype":{"id":10}},"title":"Groundwater contamination by organic bases derived from coal-tar wastes","docAbstract":"<p><span>A fluid sample from a shallow aquifer contaminated by coal-tar wastes was analyzed for organic bases. The sample consisted of a mixture of aqueous and oily-tar phases. The phases were separated by centrifugation and filtration. Organic bases were isolated from each phase by pH adjustment and solvent extraction. Organic bases in the oily-tar phase were further purified by neutral-alumina, micro-column adsorption chromatography. Separation and identification of the organic bases in each phase were achieved by using capillary gas chromatography-mass spectrometry-computer (GC-MS-COM) and probe distillation-high resolution mass spectrometry (PD-HRMS) techniques. Organic bases present in the aqueous phase included primary aromatic amines (such as aniline, alkylated anilines, and naphthylamines) as well as azaarenes (such as alkylated pyridines, quinolines, acridine, and benzoquinolines). The oily-tar phase contained acridine, benzacridines, dibenzacridines, and numerous other azaarenes, the elemental compositions of which were determined by PD-HRMS. Azaarenes in the oily-tar phase, varying in size from 6 to 12 rings, are reported for the first time. The origin and environmental significance of these compounds are discussed.</span></p>","language":"English","publisher":"Society of Environmental Toxicology and Chemistry","doi":"10.1002/etc.5620020304","issn":"07307268","usgsCitation":"Pereira, W.E., Rostad, C., Garbarino, J., and Hult, M.F., 1983, Groundwater contamination by organic bases derived from coal-tar wastes: Environmental Toxicology and Chemistry, v. 2, no. 3, p. 283-294, https://doi.org/10.1002/etc.5620020304.","productDescription":"12 p.","startPage":"283","endPage":"294","numberOfPages":"12","costCenters":[],"links":[{"id":220805,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"2","issue":"3","noUsgsAuthors":false,"publicationDate":"1983-07-01","publicationStatus":"PW","scienceBaseUri":"505a2d99e4b0c8380cd5bf48","contributors":{"authors":[{"text":"Pereira, W. E.","contributorId":46981,"corporation":false,"usgs":true,"family":"Pereira","given":"W.","email":"","middleInitial":"E.","affiliations":[],"preferred":false,"id":362470,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Rostad, C.E.","contributorId":50939,"corporation":false,"usgs":true,"family":"Rostad","given":"C.E.","email":"","affiliations":[],"preferred":false,"id":362471,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Garbarino, J.R.","contributorId":76326,"corporation":false,"usgs":true,"family":"Garbarino","given":"J.R.","email":"","affiliations":[],"preferred":false,"id":362472,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Hult, M. F.","contributorId":29817,"corporation":false,"usgs":true,"family":"Hult","given":"M.","email":"","middleInitial":"F.","affiliations":[],"preferred":false,"id":362469,"contributorType":{"id":1,"text":"Authors"},"rank":4}]}}
,{"id":1013808,"text":"1013808 - 1983 - What's New : Gould new director","interactions":[],"lastModifiedDate":"2012-02-02T00:04:29","indexId":"1013808","displayToPublicDate":"1983-01-01T00:00:00","publicationYear":"1983","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1624,"text":"Farm Pond Harvest","active":true,"publicationSubtype":{"id":10}},"title":"What's New : Gould new director","largerWorkType":{"id":2,"text":"Article"},"largerWorkTitle":"Farm Pond Harvest","largerWorkSubtype":{"id":10,"text":"Journal Article"},"language":"English","collaboration":"None/TIS","usgsCitation":"Gutsell, G., 1983, What's New : Gould new director: Farm Pond Harvest, v. 17, no. 2.","productDescription":"p. 2, 28","startPage":"2, 28","costCenters":[{"id":365,"text":"Leetown Science Center","active":true,"usgs":true}],"links":[{"id":131878,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"17","issue":"2","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e49f4e4b07f02db5f0897","contributors":{"authors":[{"text":"Gutsell, G.S.","contributorId":88694,"corporation":false,"usgs":true,"family":"Gutsell","given":"G.S.","email":"","affiliations":[],"preferred":false,"id":319275,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":1013807,"text":"1013807 - 1983 - What's New : Fisheries information available","interactions":[],"lastModifiedDate":"2012-02-02T00:04:29","indexId":"1013807","displayToPublicDate":"1983-01-01T00:00:00","publicationYear":"1983","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1624,"text":"Farm Pond Harvest","active":true,"publicationSubtype":{"id":10}},"title":"What's New : Fisheries information available","largerWorkType":{"id":2,"text":"Article"},"largerWorkTitle":"Farm Pond Harvest","largerWorkSubtype":{"id":10,"text":"Journal Article"},"language":"English","collaboration":"None/TIS","usgsCitation":"Gutsell, G., 1983, What's New : Fisheries information available: Farm Pond Harvest, v. 17, no. 1.","productDescription":"22 p.","startPage":"22","numberOfPages":"22","costCenters":[{"id":365,"text":"Leetown Science Center","active":true,"usgs":true}],"links":[{"id":131877,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"17","issue":"1","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e49d9e4b07f02db5dfab5","contributors":{"authors":[{"text":"Gutsell, G.S.","contributorId":88694,"corporation":false,"usgs":true,"family":"Gutsell","given":"G.S.","email":"","affiliations":[],"preferred":false,"id":319274,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":70011995,"text":"70011995 - 1983 - The relationship of acquisition systems to automated stereo correlation.","interactions":[],"lastModifiedDate":"2012-03-12T17:18:34","indexId":"70011995","displayToPublicDate":"1983-01-01T00:00:00","publicationYear":"1983","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":3052,"text":"Photogrammetric Engineering and Remote Sensing","active":true,"publicationSubtype":{"id":10}},"title":"The relationship of acquisition systems to automated stereo correlation.","docAbstract":"Today a concerted effort is being made to expedite the mapping process through automated correlation of stereo data. Stereo correlation involves the comparison of radiance (brightness) signals or patterns recorded by sensors. Conventionally, two-dimensional area correlation is utilized but this is a rather slow and cumbersome procedure. Digital correlation can be performed in only one dimension where suitable signal patterns exist, and the one-dimensional mode is much faster. Electro-optical (EO) systems, suitable for space use, also have much greater flexibility than film systems. Thus, an EO space system can be designed which will optimize one-dimensional stereo correlation and lead toward the automation of topographic mapping.-from Author","largerWorkType":{"id":2,"text":"Article"},"largerWorkTitle":"Photogrammetric Engineering and Remote Sensing","largerWorkSubtype":{"id":10,"text":"Journal Article"},"language":"English","usgsCitation":"Colvocoresses, A., 1983, The relationship of acquisition systems to automated stereo correlation.: Photogrammetric Engineering and Remote Sensing, v. 49, no. 4, p. 539-544.","startPage":"539","endPage":"544","numberOfPages":"6","costCenters":[],"links":[{"id":220804,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"49","issue":"4","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"505baf21e4b08c986b324582","contributors":{"authors":[{"text":"Colvocoresses, A. P.","contributorId":82703,"corporation":false,"usgs":true,"family":"Colvocoresses","given":"A. P.","affiliations":[],"preferred":false,"id":362468,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":70011329,"text":"70011329 - 1983 - T-XCO2 stability relations and phase equilibria of a calcic carbonate scapolite","interactions":[],"lastModifiedDate":"2024-03-19T15:44:44.210458","indexId":"70011329","displayToPublicDate":"1983-01-01T00:00:00","publicationYear":"1983","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}},"displayTitle":"T-X<sub>CO<sub>2</sub></sub> stability relations and phase equilibria of a calcic carbonate scapolite","title":"T-XCO2 stability relations and phase equilibria of a calcic carbonate scapolite","docAbstract":"<p>At a total pressure of 5 kb, calcic, Cl-free scapolite (Me<sub>83</sub>) is stable relative to plagioclase-bearing assemblages at<span>&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;><mtext>T &amp;#x2267; 625&amp;#xB0;C</mtext></math>\"><span class=\"MJX_Assistive_MathML\">T ≧ 625°C</span></span></span>,<span>&nbsp;</span><span class=\"math\"><span id=\"MathJax-Element-2-Frame\" class=\"MathJax_SVG\" data-mathml=\"<math xmlns=&quot;http://www.w3.org/1998/Math/MathML&quot;><mtext>X</mtext><msub><mi></mi><mn><mtext>CO</mtext><msub><mi></mi><mn>2</mn></msub></mn></msub><mtext>&amp;#x2267; 0.12</mtext></math>\"><span class=\"MJX_Assistive_MathML\">X<sub>CO2</sub>≧ 0.12</span></span></span>. With decreasing temperature, scapolite breaks down to plagioclase + calcite. Scapolite is replaced by plagioclase + grossular + cancrinite + CO<sub>2</sub><span>&nbsp;</span>in the presence of H<sub>2</sub>O-rich fluids. The stable coexistence of scapolite and calcite, an assemblage typical of most natural occurrences of calcic scapolite, is limited by the reaction: scapolite + calcite → grossular + cancrinite + CO<sub>2</sub>, which occurs at 750°C,<span>&nbsp;</span><i>X</i><sub><i>CO</i>2</sub><span>&nbsp;</span>= 0.46; 700°C,<span>&nbsp;</span><i>X</i><sub><i>CO</i>2</sub><span>&nbsp;</span>= 0.33; 650°C,<span>&nbsp;</span><i>X</i><sub><i>CO</i>2</sub><span>&nbsp;</span>= 0.18, for the chosen bulk composition.</p><p>Generalization of the experimental results to encompass the complete range of fully carbonated scapolite compositions indicates that mizzonite (Me<sub>75</sub>) has the largest<span>&nbsp;</span><i>T</i>-<i>X</i><sub><i>CO</i>2</sub><span>&nbsp;</span>stability field. For scapolite more calcic than mizzonite, stable growth is restricted to conditions of increasingly higher temperature and<span>&nbsp;</span><i>X</i><sub><i>CO</i>2</sub>.</p><p>The experimental results are consistent with various petrologic features of scapolite-bearing rocks, particularly scapolite-clinopyroxene granulites, and indicate that such rocks were formed in the presence of CO<sub>2</sub>-rich fluids.</p>","language":"English","publisher":"Elsevier","doi":"10.1016/0016-7037(83)90258-2","issn":"00167037","usgsCitation":"Aitken, B., 1983, T-XCO2 stability relations and phase equilibria of a calcic carbonate scapolite: Geochimica et Cosmochimica Acta, v. 47, no. 3, p. 351-362, https://doi.org/10.1016/0016-7037(83)90258-2.","productDescription":"12 p.","startPage":"351","endPage":"362","numberOfPages":"12","costCenters":[],"links":[{"id":221748,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"47","issue":"3","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"505ba379e4b08c986b31fcfb","contributors":{"authors":[{"text":"Aitken, B.G.","contributorId":33058,"corporation":false,"usgs":true,"family":"Aitken","given":"B.G.","email":"","affiliations":[],"preferred":false,"id":360850,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":70011600,"text":"70011600 - 1983 - The saltwater-freshwater interface in the Tertiary limestone aquifer, southeast Atlantic outer-continental shelf of the U.S.A.","interactions":[],"lastModifiedDate":"2025-04-11T16:49:26.1536","indexId":"70011600","displayToPublicDate":"1983-01-01T00:00:00","publicationYear":"1983","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":2342,"text":"Journal of Hydrology","active":true,"publicationSubtype":{"id":10}},"title":"The saltwater-freshwater interface in the Tertiary limestone aquifer, southeast Atlantic outer-continental shelf of the U.S.A.","docAbstract":"<p><span>Hydrologic testing in an offshore oil well abandoned by Tenneco, Inc., determined the position of the saltwater-freshwater interface in Tertiary limestones underlying the Florida-Georgia continental shelf of the U.S.A. Previous drilling (JOIDES and U.S.G.S. AMCOR projects) established the existence of freshwater far offshore in this area. At the Tenneco well 55 mi. (∼88 km) east of Fernandina Beach, Florida, drill-stem tests made in the interval 1050–1070 ft. (320–326 m) below sea level in the Ocala Limestone recovered a sample with a chloride concentration of 7000 mg l</span><sup>−1</sup><span>. Formation water probably is slightly fresher. Pressure-head measurements indicated equivalent freshwater heads of 24–29 ft. (7.3–8.8 m) above sea level.</span></p><p><span>At the coast (Fernandina Beach), a relatively thin transition zone separating freshwater and saltwater occurs at a depth of 2100 ft. (640 m) below sea level. Fifty-five miles (∼88 km) offshore, at the Tenneco well, the base of freshwater is ∼1100 ft. (∼335 m) below sea level. The difference in approximate depth to the freshwater-saltwater transition at these two locations suggests an interface with a very slight landward slope. Assuming the Hubbert interface equation applies here (because the interface and therefore freshwater flow lines are nearly horizontal) the equilibrium depth to the interface should be 40 times the freshwater head above sea level. Using present-day freshwater heads along the coast in the Hubbert equation results in depths to the interface of less than the observed 2100 ft. (640 m). Substituting predevelopment heads in the equation yields depths greater than 2100 ft. (640 m). Thus the interface appears to be in a transient position between the position that would be compatible with present-day heads and the position that would be compatible with predevelopment heads. This implies that some movement of the interface from the predevelopment position has occurred during the past hundred years. The implied movement is incompatible with the hypothesis that the freshwater occurring far offshore in this area is trapped water remaining since the Pleistocene Epoch.</span></p>","language":"English","publisher":"Elsevier","doi":"10.1016/0022-1694(83)90251-2","issn":"00221694","usgsCitation":"Johnston, R., 1983, The saltwater-freshwater interface in the Tertiary limestone aquifer, southeast Atlantic outer-continental shelf of the U.S.A.: Journal of Hydrology, v. 61, no. 1-3, p. 239-249, https://doi.org/10.1016/0022-1694(83)90251-2.","productDescription":"11 p.","startPage":"239","endPage":"249","costCenters":[],"links":[{"id":220712,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United States","state":"Florida, Georgia","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"coordinates\": [\n          [\n            [\n              -82.49895094186574,\n              30.906206797439737\n            ],\n            [\n              -82.49895094186574,\n              29.80296540535703\n            ],\n            [\n              -81.27672743461723,\n              29.80296540535703\n            ],\n            [\n              -81.27672743461723,\n              30.906206797439737\n            ],\n            [\n              -82.49895094186574,\n              30.906206797439737\n            ]\n          ]\n        ],\n        \"type\": \"Polygon\"\n      }\n    }\n  ]\n}","volume":"61","issue":"1-3","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"505bafb0e4b08c986b324998","contributors":{"authors":[{"text":"Johnston, R.H.","contributorId":19536,"corporation":false,"usgs":true,"family":"Johnston","given":"R.H.","email":"","affiliations":[],"preferred":false,"id":361516,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":1013795,"text":"1013795 - 1983 - Leptospirosis","interactions":[],"lastModifiedDate":"2012-02-02T00:04:23","indexId":"1013795","displayToPublicDate":"1983-01-01T00:00:00","publicationYear":"1983","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":3658,"text":"Trout Growers Creel","active":true,"publicationSubtype":{"id":10}},"title":"Leptospirosis","largerWorkType":{"id":2,"text":"Article"},"largerWorkTitle":"Trout Growers Creel","largerWorkSubtype":{"id":10,"text":"Journal Article"},"language":"English","collaboration":"None/TIS","usgsCitation":"Gutsell, G., 1983, Leptospirosis: Trout Growers Creel, v. 16, no. 2.","productDescription":"12 p.","startPage":"12","numberOfPages":"12","costCenters":[{"id":365,"text":"Leetown Science Center","active":true,"usgs":true}],"links":[{"id":130762,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"16","issue":"2","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b16e4b07f02db6a5670","contributors":{"authors":[{"text":"Gutsell, G.S.","contributorId":88694,"corporation":false,"usgs":true,"family":"Gutsell","given":"G.S.","email":"","affiliations":[],"preferred":false,"id":319263,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":1013790,"text":"1013790 - 1983 - Fisheries news: NFC hosts Fish Health Workshop","interactions":[],"lastModifiedDate":"2023-12-13T11:14:42.935785","indexId":"1013790","displayToPublicDate":"1983-01-01T00:00:00","publicationYear":"1983","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1657,"text":"Fisheries","onlineIssn":"1548-8446","printIssn":"0363-2415","active":true,"publicationSubtype":{"id":10}},"title":"Fisheries news: NFC hosts Fish Health Workshop","docAbstract":"<p>No abstract available.</p>","language":"English","publisher":"Wiley","usgsCitation":"Gutsell, G., 1983, Fisheries news: NFC hosts Fish Health Workshop: Fisheries, v. 8, no. 5, p. 39-39.","productDescription":"1 p.","startPage":"39","endPage":"39","costCenters":[{"id":365,"text":"Leetown Science Center","active":true,"usgs":true}],"links":[{"id":423478,"rank":2,"type":{"id":15,"text":"Index Page"},"url":"https://doi.org/10.1577/1548-8446-8-5"},{"id":132312,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United States","state":"West Virginia","city":"Leetown","otherGeospatial":"National Fisheries Center","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"coordinates\": [\n          [\n            [\n              -77.94176291222891,\n              39.35314400869396\n            ],\n            [\n              -77.94332127643847,\n              39.35266582894124\n            ],\n            [\n              -77.94322233267935,\n              39.35224502805204\n            ],\n            [\n              -77.9413671371917,\n              39.351728587133465\n            ],\n            [\n              -77.94013034019942,\n              39.35117388708008\n            ],\n            [\n              -77.9388935432079,\n              39.351460801450344\n            ],\n            [\n              -77.93693940396041,\n              39.349528888615794\n            ],\n            [\n              -77.93565313508893,\n              39.349069812365286\n            ],\n            [\n              -77.93416897869851,\n              39.34786472285808\n            ],\n            [\n              -77.93263535042891,\n              39.3490124276216\n            ],\n            [\n              -77.92974124546794,\n              39.35352655014\n            ],\n            [\n              -77.92852918441565,\n              39.35436813394793\n            ],\n            [\n              -77.92890022351365,\n              39.35469328861336\n            ],\n            [\n              -77.92894969539282,\n              39.355037568374485\n            ],\n            [\n              -77.93033490802414,\n              39.35580262843618\n            ],\n            [\n              -77.9313243456175,\n              39.35607039747876\n            ],\n            [\n              -77.93147276125653,\n              39.35645292290201\n            ],\n            [\n              -77.93288270982706,\n              39.35752398294329\n            ],\n            [\n              -77.9339710911803,\n              39.35779174538811\n            ],\n            [\n              -77.93454001779651,\n              39.357638738402386\n            ],\n            [\n              -77.93543051163076,\n              39.35708408527057\n            ],\n            [\n              -77.93632100546425,\n              39.35509494817006\n            ],\n            [\n              -77.94176291222891,\n              39.35314400869396\n            ]\n          ]\n        ],\n        \"type\": \"Polygon\"\n      }\n    }\n  ]\n}","volume":"8","issue":"5","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e49f2e4b07f02db5ef292","contributors":{"authors":[{"text":"Gutsell, G.S.","contributorId":88694,"corporation":false,"usgs":true,"family":"Gutsell","given":"G.S.","email":"","affiliations":[],"preferred":false,"id":319258,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":1013789,"text":"1013789 - 1983 - Elimination of rats provides protection from leptospirosis","interactions":[],"lastModifiedDate":"2012-02-02T00:04:30","indexId":"1013789","displayToPublicDate":"1983-01-01T00:00:00","publicationYear":"1983","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":855,"text":"Aquaculture Magazine","active":true,"publicationSubtype":{"id":10}},"title":"Elimination of rats provides protection from leptospirosis","largerWorkType":{"id":2,"text":"Article"},"largerWorkTitle":"Aquaculture Magazine","largerWorkSubtype":{"id":10,"text":"Journal Article"},"language":"English","collaboration":"None/TIS","usgsCitation":"Gutsell, G., 1983, Elimination of rats provides protection from leptospirosis: Aquaculture Magazine, v. 9, no. 2.","productDescription":"13 p.","startPage":"13","numberOfPages":"13","costCenters":[{"id":365,"text":"Leetown Science Center","active":true,"usgs":true}],"links":[{"id":132311,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"9","issue":"2","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a19e4b07f02db605a74","contributors":{"authors":[{"text":"Gutsell, G.S.","contributorId":88694,"corporation":false,"usgs":true,"family":"Gutsell","given":"G.S.","email":"","affiliations":[],"preferred":false,"id":319257,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":70011227,"text":"70011227 - 1983 - Calorimetric investigation of the excess entropy of mixing in analbite-sanidine solid solutions: lack of evidence for Na,K short- range order and implications for two-feldspar thermometry.","interactions":[],"lastModifiedDate":"2013-02-14T10:12:23","indexId":"70011227","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":"Calorimetric investigation of the excess entropy of mixing in analbite-sanidine solid solutions: lack of evidence for Na,K short- range order and implications for two-feldspar thermometry.","docAbstract":"Heat capacities (5-380 K) have been measured by adiabatic calorimetry for five highly disordered alkali feldspars (Ab99Or1, Ab85Or15, Ab55Or45, Ab25Or75 and Ab1Or99). The thermodynamic and mineralogical implications of the results are discussed. The new data are also combined with recent data for plagioclases in order to derive a revised expression for the two-feldspar thermometer. T calculated from the revised expression tend to be higher than previous calculations.-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":"Haselton, H., Hovis, G., Hemingway, B.S., and Robie, R.A., 1983, Calorimetric investigation of the excess entropy of mixing in analbite-sanidine solid solutions: lack of evidence for Na,K short- range order and implications for two-feldspar thermometry.: American Mineralogist, v. 68, no. 3-4, p. 398-413.","startPage":"398","endPage":"413","numberOfPages":"16","costCenters":[],"links":[{"id":220967,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"},{"id":267377,"type":{"id":11,"text":"Document"},"url":"https://www.minsocam.org/ammin/AM68/AM68_398.pdf"}],"volume":"68","issue":"3-4","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"5059f328e4b0c8380cd4b621","contributors":{"authors":[{"text":"Haselton, H.T. Jr.","contributorId":83520,"corporation":false,"usgs":true,"family":"Haselton","given":"H.T.","suffix":"Jr.","email":"","affiliations":[],"preferred":false,"id":360616,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Hovis, G.L.","contributorId":63532,"corporation":false,"usgs":true,"family":"Hovis","given":"G.L.","affiliations":[],"preferred":false,"id":360614,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Hemingway, B. S.","contributorId":7268,"corporation":false,"usgs":true,"family":"Hemingway","given":"B.","email":"","middleInitial":"S.","affiliations":[],"preferred":false,"id":360613,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Robie, R. A.","contributorId":71237,"corporation":false,"usgs":true,"family":"Robie","given":"R.","email":"","middleInitial":"A.","affiliations":[],"preferred":false,"id":360615,"contributorType":{"id":1,"text":"Authors"},"rank":4}]}}
,{"id":70011228,"text":"70011228 - 1983 - In situ studies of velocity in fractured crystalline rocks","interactions":[],"lastModifiedDate":"2024-07-16T14:50:02.269257","indexId":"70011228","displayToPublicDate":"1983-01-01T00:00:00","publicationYear":"1983","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":6453,"text":"Journal of Geophysical Research Solid Earth","active":true,"publicationSubtype":{"id":10}},"title":"In situ studies of velocity in fractured crystalline rocks","docAbstract":"<p><span>A study of the effects of macroscopic fractures on&nbsp;</span><i>P</i><span>&nbsp;and&nbsp;</span><i>S</i><span>&nbsp;wave velocities has been conducted in four wells drilled in granitic rock to depths between 0.6 and 1.2 km. The effect of macroscopic fractures is to decrease both&nbsp;</span><i>V<sub>p</sub></i><span>&nbsp;and&nbsp;</span><i>V<sub>s</sub></i><span>&nbsp;and increase&nbsp;</span><i>V<sub>p</sub></i><span>/</span><i>V<sub>s</sub></i><span>. In wells with a relatively low density of macroscopic fractures, the in situ velocity is similar to that of saturated core samples under confining pressure in the laboratory, and there is a clear correlation between zones with macroscopic fractures and anomalously low velocities. In wells with numerous macroscopic fractures, the in situ velocity is lower than that of intact samples under pressure, and there is a correlation between the rate at which in situ velocity increases with depth and the rate at which the velocity of laboratory samples increases with pressure. Differences in in situ&nbsp;</span><i>P</i><span>&nbsp;wave velocity between wells cannot be explained solely by differences in the degree of macroscopic fracturing, thus emphasizing the importance of composition and microcracks on velocity. In one highly fractured well the in situ&nbsp;</span><i>P</i><span>&nbsp;wave velocity is essentially the same for frequencies ranging from 10 Hz to 20 kHz; this suggests that the macrofractures affect velocity similarly over a broad frequency range. Chemical alteration of rock adjacent to macroscopic fractures appears to play an important role in reducing in situ velocities. Synthetic reflection seismograms generated from the velocity logs suggest that fracture zones are one possible source of deep-crustal reflectors observed on seismic reflection profiles.</span></p>","language":"English","publisher":"American Geophysical Union","doi":"10.1029/JB088iB03p02345","issn":"01480227","usgsCitation":"Moos, D., and Zoback, M.D., 1983, In situ studies of velocity in fractured crystalline rocks: Journal of Geophysical Research Solid Earth, v. 88, no. B3, p. 2345-2358, https://doi.org/10.1029/JB088iB03p02345.","productDescription":"14 p.","startPage":"2345","endPage":"2358","numberOfPages":"14","costCenters":[],"links":[{"id":480237,"rank":2,"type":{"id":40,"text":"Open Access Publisher Index Page"},"url":"https://doi.org/10.1029/jb088ib03p02345","text":"Publisher Index Page"},{"id":221031,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"88","issue":"B3","noUsgsAuthors":false,"publicationDate":"2012-09-20","publicationStatus":"PW","scienceBaseUri":"505a39ade4b0c8380cd619e2","contributors":{"authors":[{"text":"Moos, Daniel","contributorId":105048,"corporation":false,"usgs":true,"family":"Moos","given":"Daniel","affiliations":[],"preferred":false,"id":360618,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Zoback, Mark D.","contributorId":80275,"corporation":false,"usgs":true,"family":"Zoback","given":"Mark","middleInitial":"D.","affiliations":[],"preferred":false,"id":360617,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":1007649,"text":"1007649 - 1983 - Light/dark control of diurnal acid metabolism in the submerged aquatic Isoetes howellii","interactions":[],"lastModifiedDate":"2012-02-02T00:04:17","indexId":"1007649","displayToPublicDate":"1983-01-01T00:00:00","publicationYear":"1983","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1136,"text":"Bulletin of the Southern California Academy of Sciences","active":true,"publicationSubtype":{"id":10}},"title":"Light/dark control of diurnal acid metabolism in the submerged aquatic Isoetes howellii","largerWorkType":{"id":2,"text":"Article"},"largerWorkTitle":"Bulletin of the Southern California Academy of Sciences","largerWorkSubtype":{"id":10,"text":"Journal Article"},"language":"English","usgsCitation":"Keeley, J., 1983, Light/dark control of diurnal acid metabolism in the submerged aquatic Isoetes howellii: Bulletin of the Southern California Academy of Sciences, v. 82, p. 39-42.","productDescription":"p. 39-42","startPage":"39","endPage":"42","numberOfPages":"4","costCenters":[{"id":651,"text":"Western Ecological Research Center","active":true,"usgs":true}],"links":[{"id":129782,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"82","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b16e4b07f02db6a534c","contributors":{"authors":[{"text":"Keeley, Jon E. 0000-0002-4564-6521","orcid":"https://orcid.org/0000-0002-4564-6521","contributorId":69082,"corporation":false,"usgs":true,"family":"Keeley","given":"Jon E.","affiliations":[],"preferred":false,"id":315789,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":70011318,"text":"70011318 - 1983 - A short-pulse electromagnetic transponder for hole-to-hole use","interactions":[],"lastModifiedDate":"2024-01-25T17:33:37.607312","indexId":"70011318","displayToPublicDate":"1983-01-01T00:00:00","publicationYear":"1983","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1944,"text":"IEEE Transactions on Geoscience and Remote Sensing","active":true,"publicationSubtype":{"id":10}},"title":"A short-pulse electromagnetic transponder for hole-to-hole use","docAbstract":"<p><span>We have made hole-to-hole observations through nearly 20 m of granite using an electromagnetic transponder (an active reflector) in one borehole and a single-hole short-pulse radar in another. We found that the transponder is inexpensive, operationally simple, and effective in extending the capability of a short-pulse borehole radar system to allow hole-to-hole operation without requiring timing cables. A detector in the transponder senses the arrival of each pulse from the radar (which may be millivolts in amplitude); each pulse detection triggers a kilovolt-amplitude pulse for retransmission. The transponder “echo” may be stronger than that of a passive reflector by a factor of as much as 120 dB. The result is an increase in range capability by a factor which depends on attenuation in the medium and hole-to-hole wavepath geometry. Single-hole reflection-mode echoes are still available at times prior to the transponder pulse arrival. The transponder is helpful in yielding velocity information, because the radar-transponder distance is known and the echo time is observed. Field tests have demonstrated that the transponder is a useful alternative to employing timing cables in some short-pulse hole-to-hole measurement situations.</span></p>","language":"English","publisher":"IEEE","doi":"10.1109/TGRS.1984.6499195","issn":"01962892","usgsCitation":"Wright, D.L., Watts, R.D., and Bramsoe, E., 1983, A short-pulse electromagnetic transponder for hole-to-hole use: IEEE Transactions on Geoscience and Remote Sensing, v. GE-22, no. 6, p. 720-725, https://doi.org/10.1109/TGRS.1984.6499195.","productDescription":"6 p.","startPage":"720","endPage":"725","numberOfPages":"6","costCenters":[],"links":[{"id":221579,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"GE-22","issue":"6","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"505aaf42e4b0c8380cd874a2","contributors":{"authors":[{"text":"Wright, David L. dwright@usgs.gov","contributorId":1132,"corporation":false,"usgs":true,"family":"Wright","given":"David","email":"dwright@usgs.gov","middleInitial":"L.","affiliations":[],"preferred":true,"id":360827,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Watts, Raymond D.","contributorId":105713,"corporation":false,"usgs":true,"family":"Watts","given":"Raymond","email":"","middleInitial":"D.","affiliations":[],"preferred":false,"id":360829,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Bramsoe, Erik","contributorId":72448,"corporation":false,"usgs":true,"family":"Bramsoe","given":"Erik","email":"","affiliations":[],"preferred":false,"id":360828,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":1007690,"text":"1007690 - 1983 - Status of the West Indian manatee in Honduras","interactions":[],"lastModifiedDate":"2023-09-14T17:49:58.584542","indexId":"1007690","displayToPublicDate":"1983-01-01T00:00:00","publicationYear":"1983","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1015,"text":"Biological Conservation","active":true,"publicationSubtype":{"id":10}},"title":"Status of the West Indian manatee in Honduras","docAbstract":"<p><span>Aerial surveys and interviews with fisherman in Honduras indicate that manatee numbers are low. There is an abundance of suitable habitat, and evidence on the proportion of calves indicates that manatees are reproducing. Although natural mortality occurs when the animals are trapped in small landlocked coastal lagoons, the greatest threat to manatees is from subsistence hunting for their meat. Harpooning from a small motorised canoe is the most common means of capture; however, entanglement in gill nets may also be employed. Enforcement of existing protective laws and enlistment of public support is required to preserve the remaining manatees in Honduras.</span></p>","language":"English","publisher":"Elsevier","doi":"10.1016/0006-3207(83)90094-0","usgsCitation":"Rathbun, G.B., Powell, J.A., and Cruz, G., 1983, Status of the West Indian manatee in Honduras: Biological Conservation, v. 26, no. 4, p. 301-308, https://doi.org/10.1016/0006-3207(83)90094-0.","productDescription":"8 p.","startPage":"301","endPage":"308","costCenters":[{"id":651,"text":"Western Ecological Research Center","active":true,"usgs":true}],"links":[{"id":130545,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"Honduras","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"coordinates\": [\n          [\n            [\n              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,{"id":70182501,"text":"70182501 - 1983 - Rangeland applications","interactions":[],"lastModifiedDate":"2017-03-22T15:34:37","indexId":"70182501","displayToPublicDate":"1983-01-01T00:00:00","publicationYear":"1983","noYear":false,"publicationType":{"id":5,"text":"Book chapter"},"publicationSubtype":{"id":24,"text":"Book Chapter"},"title":"Rangeland applications","docAbstract":"<p>No abstract available.</p>","largerWorkType":{"id":4,"text":"Book"},"largerWorkTitle":"Manual of remote sensing","language":"English","publisher":"American Society for Photogrammetry","publisherLocation":"Madison, WI","usgsCitation":"Carneggie, D., Schrumpf, B., and Mouat, D., 1983, Rangeland applications, chap. <i>of</i> Manual of remote sensing, p. 2325-2384.","productDescription":"60 p. ","startPage":"2325","endPage":"2384","costCenters":[{"id":222,"text":"Earth Resources Observation and Science (EROS) Center","active":true,"usgs":true}],"links":[{"id":336119,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"edition":"2nd ","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"58b002dbe4b01ccd54fb281b","contributors":{"authors":[{"text":"Carneggie, D. M.","contributorId":62795,"corporation":false,"usgs":true,"family":"Carneggie","given":"D. M.","affiliations":[],"preferred":false,"id":671283,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Schrumpf, B.J.","contributorId":182369,"corporation":false,"usgs":false,"family":"Schrumpf","given":"B.J.","email":"","affiliations":[],"preferred":false,"id":671284,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Mouat, D.A.","contributorId":8224,"corporation":false,"usgs":true,"family":"Mouat","given":"D.A.","affiliations":[],"preferred":false,"id":671285,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":70135750,"text":"70135750 - 1983 - Earthquakes in the Orozco transform zone: seismicity, source mechanisms, and tectonics","interactions":[],"lastModifiedDate":"2017-08-24T14:29:34","indexId":"70135750","displayToPublicDate":"1983-01-01T00:00:00","publicationYear":"1983","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":2314,"text":"Journal of Geophysical Research B: Solid Earth","active":true,"publicationSubtype":{"id":10}},"title":"Earthquakes in the Orozco transform zone: seismicity, source mechanisms, and tectonics","docAbstract":"<p><span>As part of the Rivera Ocean Seismic Experiment, a network of ocean bottom seismometers and hydrophones was deployed in order to determine the seismic characteristics of the Orozco transform fault in the central eastern Pacific. We present hypocentral locations and source mechanisms for 70 earthquakes recorded by this network. All epicenters are within the transform region of the Orozco Fracture Zone and clearly delineate the active plate boundary. About half of the epicenters define a narrow line of activity parallel to the spreading direction and situated along a deep topographic trough that forms the northern boundary of the transform zone (region 1). Most focal depths for these events are very shallow, within 4 km of the seafloor; several well-determined focal depths, however, are as great as 7 km. No shallowing of seismic activity is observed as the rise-transform intersection is approached; to the contrary, the deepest events are within 10 km of the intersection. First motion polarities for most of the earthquakes in region 1 are compatible with right-lateral strike slip faulting along a nearly vertical plane, striking parallel to the spreading direction. Another zone of activity is observed in the central part of the transform (region 2). The apparent horizontal and vertical distribution of activity in this region is more scattered than in the first, and the first motion radiation patterns of these events do not appear to be compatible with any known fault mechanism. Pronounced lateral variations in crustal velocity structure are indicated for the transform region from refraction data and measurements of wave propagation directions. The effect of this lateral heterogeneity on hypocenters and fault plane solutions is evaluated by tracing rays through a three-dimensional velocity grid. While findings for events in region 1 are not significantly affected, in region 2, epicentral mislocations of up to 10 km and azimuthal deflections of up to 45&deg; may result from assuming a laterally homogeneous velocity structure. When corrected for the effects of lateral heterogeneity, the epicenters and fault plane solutions for earthquakes in region 2 are compatible with predominantly normal faulting along a topographic trough trending NW&ndash;SE; the focal depths, however, are poorly constrained. These results suggest an en echelon spreading center or leaky transform regime in the central transform region.</span></p>","language":"English","publisher":"American Geophysical Union","doi":"10.1029/JB088iB10p08203","usgsCitation":"Trehu, A.M., and Solomon, S.C., 1983, Earthquakes in the Orozco transform zone: seismicity, source mechanisms, and tectonics: Journal of Geophysical Research B: Solid Earth, v. 88, no. B10, p. 8203-8225, https://doi.org/10.1029/JB088iB10p08203.","productDescription":"23 p.","startPage":"8203","endPage":"8225","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":296714,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"88","issue":"B10","noUsgsAuthors":false,"publicationDate":"2012-09-20","publicationStatus":"PW","scienceBaseUri":"549165c2e4b0d0759afaad82","contributors":{"authors":[{"text":"Trehu, Anne M.","contributorId":49884,"corporation":false,"usgs":false,"family":"Trehu","given":"Anne","email":"","middleInitial":"M.","affiliations":[{"id":6680,"text":"Oregon State University","active":true,"usgs":false}],"preferred":false,"id":536810,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Solomon, Sean C.","contributorId":14698,"corporation":false,"usgs":false,"family":"Solomon","given":"Sean","email":"","middleInitial":"C.","affiliations":[{"id":7171,"text":"Columbia University","active":true,"usgs":false}],"preferred":false,"id":536811,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":70170301,"text":"70170301 - 1983 - Volcanoes of the Cascade Range in North America","interactions":[],"lastModifiedDate":"2016-12-13T13:31:25","indexId":"70170301","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":"Volcanoes of the Cascade Range in North America","language":"English","publisher":"U.S Geological Survey","publisherLocation":"Reston, VA","usgsCitation":"Foxworthy, B., and Hile, M., 1983, Volcanoes of the Cascade Range in North America: Earthquake Information Bulletin (USGS), v. 15, no. 2, p. 60-71.","productDescription":"12 p.","startPage":"60","endPage":"71","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[],"links":[{"id":320093,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"15","issue":"2","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"571210bae4b0ef3b7ca6445f","contributors":{"authors":[{"text":"Foxworthy, B. L.","contributorId":45686,"corporation":false,"usgs":true,"family":"Foxworthy","given":"B. L.","affiliations":[],"preferred":false,"id":626810,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Hile, M.","contributorId":168637,"corporation":false,"usgs":false,"family":"Hile","given":"M.","email":"","affiliations":[],"preferred":false,"id":626811,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":70175044,"text":"70175044 - 1983 - Anaerobic oxalate degradation: Widespread natural occurrence in aquatic sediments","interactions":[],"lastModifiedDate":"2023-01-26T18:33:35.793734","indexId":"70175044","displayToPublicDate":"1983-01-01T00:00:00","publicationYear":"1983","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":850,"text":"Applied and Environmental Microbiology","active":true,"publicationSubtype":{"id":10}},"title":"Anaerobic oxalate degradation: Widespread natural occurrence in aquatic sediments","docAbstract":"<div id=\"abstract-1\" class=\"section abstract\"><p id=\"p-1\">Significant concentrations of oxalate (dissolved plus particulate) were present in sediments taken from a diversity of aquatic environments, ranging from 0.1 to 0.7 mmol/liter of sediment. These included pelagic and littoral sediments from two freshwater lakes (Searsville Lake, Calif., and Lake Tahoe, Calif.), a hypersaline, meromictic, alkaline lake (Big Soda Lake, Nev.), and a South San Francisco Bay mud flat and salt marsh. The oxalate concentration of several plant species which are potential detrital inputs to these aquatic sediments ranged from 0.1 to 5.0% (wt/wt). In experiments with litter bags, the oxalate content of&nbsp;<i>Myriophyllum</i>&nbsp;sp. samples buried in freshwater littoral sediments decreased to 7% of the original value in 175 days. This suggests that plant detritus is a potential source of the oxalate within these sediments. [<sup>14</sup>C]oxalic acid was anaerobically degraded to<sup>14</sup>CO<sub>2</sub>&nbsp;in all sediment types tested, with higher rates evident in littoral sediments than in the pelagic sediments of the lakes studied. The turnover time of the added [<sup>14</sup>C]oxalate was less than 1 day in Searsville Lake littoral sediments. The total sediment oxalate concentration did not vary significantly between littoral and pelagic sediments and therefore did not appear to be controlling the rate of oxalate degradation. However, depth profiles of [<sup>14</sup>C]oxalate mineralization and dissolved oxalate concentration were closely correlated in freshwater littoral sediments; both were greatest in the surface sediments (0 to 5 cm) and decreased with depth. The dissolved oxalate concentration (9.1 μmol/liter of sediment) was only 3% of the total extractable oxalate (277 μmol/liter of sediment) at the sediment surface. These results suggest that anaerobic oxalate degradation is a widespread phenomenon in aquatic sediments and may be limited by the dissolved oxalate concentration within these sediments.</p></div>","language":"English","publisher":"American Society for Microbiology","doi":"10.1128/aem.46.1.106-113.1983","usgsCitation":"Smith, R.L., and Oremland, R.S., 1983, Anaerobic oxalate degradation: Widespread natural occurrence in aquatic sediments: Applied and Environmental Microbiology, v. 46, no. 1, p. 106-113, https://doi.org/10.1128/aem.46.1.106-113.1983.","productDescription":"8 p.","startPage":"106","endPage":"113","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[{"id":552,"text":"San Francisco Bay-Delta","active":false,"usgs":true},{"id":5079,"text":"Pacific Regional Director's Office","active":true,"usgs":true}],"links":[{"id":480232,"rank":2,"type":{"id":40,"text":"Open Access Publisher Index Page"},"url":"https://doi.org/10.1128/aem.46.1.106-113.1983","text":"Publisher Index 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