{"pageNumber":"5038","pageRowStart":"125925","pageSize":"25","recordCount":184617,"records":[{"id":70006849,"text":"70006849 - 1984 - An optimist's view of the future","interactions":[],"lastModifiedDate":"2012-07-10T01:01:45","indexId":"70006849","displayToPublicDate":"2012-01-01T13:52:00","publicationYear":"1984","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":4,"text":"Other Government Series"},"seriesTitle":{"id":300,"text":"University of Maryland Sea Grant Publication","active":false,"publicationSubtype":{"id":4}},"seriesNumber":"UM-SG-MAP-84-01","title":"An optimist's view of the future","docAbstract":"No abstract available at this time","largerWorkType":{"id":18,"text":"Report"},"largerWorkTitle":"The Aquaculture of Striped Bass: A Proceedings","largerWorkSubtype":{"id":9,"text":"Other Report"},"language":"English","publisher":"University of Maryland Sea Grant Publication","publisherLocation":"College Park, MD","collaboration":"None","usgsCitation":"McCraren, J.P., 1984, An optimist's view of the future: University of Maryland Sea Grant Publication UM-SG-MAP-84-01, 5 p.","productDescription":"5 p.","startPage":"255","endPage":"259","numberOfPages":"5","costCenters":[{"id":365,"text":"Leetown Science Center","active":true,"usgs":true}],"links":[{"id":258323,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"},{"id":258303,"rank":100,"type":{"id":15,"text":"Index Page"},"url":"https://www.worldcat.org/title/aquaculture-of-striped-bass-a-proceedings/oclc/12557857","linkFileType":{"id":5,"text":"html"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"5059eaa5e4b0c8380cd489be","contributors":{"authors":[{"text":"McCraren, J. P.","contributorId":55370,"corporation":false,"usgs":true,"family":"McCraren","given":"J.","email":"","middleInitial":"P.","affiliations":[],"preferred":false,"id":355353,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":70039035,"text":"70039035 - 1984 - United States Geological Survey Yearbook, fiscal year 1983","interactions":[{"subject":{"id":70179651,"text":"70179651 - 1984 - Flooding: A unique year","indexId":"70179651","publicationYear":"1984","noYear":false,"title":"Flooding: A unique year"},"predicate":"IS_PART_OF","object":{"id":70039035,"text":"70039035 - 1984 - United States Geological Survey Yearbook, fiscal year 1983","indexId":"70039035","publicationYear":"1984","noYear":false,"title":"United States Geological Survey Yearbook, fiscal year 1983"},"id":1}],"lastModifiedDate":"2018-06-08T16:18:53","indexId":"70039035","displayToPublicDate":"2012-01-01T11:58:51","publicationYear":"1984","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":6,"text":"USGS Unnumbered Series"},"seriesTitle":{"id":392,"text":"Yearbook","active":false,"publicationSubtype":{"id":6}},"title":"United States Geological Survey Yearbook, fiscal year 1983","docAbstract":"The fiscal year 1983 Yearbook summarizes the activities of the U.S. Geological Survey in response to its scientific and regulatory missions.","language":"English","publisher":"U.S. Government Printing Office","publisherLocation":"Washington, D.C.","doi":"10.3133/70039035","usgsCitation":"Water Resources Division, U.S. Geological Survey, 1984, United States Geological Survey Yearbook, fiscal year 1983: Yearbook, vi, 113 p., https://doi.org/10.3133/70039035.","productDescription":"vi, 113 p.","costCenters":[{"id":312,"text":"Geology, Minerals, Energy, and Geophysics Science Center","active":true,"usgs":true}],"links":[{"id":261276,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/unnumbered/70039035/report-thumb.jpg"},{"id":261275,"rank":800,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/unnumbered/70039035/report.pdf","text":"Report","size":"41.50 mb","linkFileType":{"id":1,"text":"pdf"},"description":"Report"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"505bbc93e4b08c986b328cfb","contributors":{"authors":[{"text":"Water Resources Division, U.S. Geological Survey","contributorId":128075,"corporation":true,"usgs":false,"organization":"Water Resources Division, U.S. Geological Survey","id":535204,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":70006947,"text":"70006947 - 1984 - Salmonid whirling disease : new findings provide evidence that the infectious form is a Triactinomyxon produced in a tubificid worm","interactions":[],"lastModifiedDate":"2012-07-10T01:01:45","indexId":"70006947","displayToPublicDate":"2012-01-01T11:58:17","publicationYear":"1984","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":4,"text":"Other Government Series"},"seriesTitle":{"id":284,"text":"Research Information Bulletin","active":false,"publicationSubtype":{"id":4}},"seriesNumber":"59","title":"Salmonid whirling disease : new findings provide evidence that the infectious form is a Triactinomyxon produced in a tubificid worm","docAbstract":"No abstract available at this time","language":"English","publisher":"U.S. Fish and Wildlife Service","publisherLocation":"Arlington, VA","collaboration":"None","usgsCitation":"Wolf, K., and Markiw, M., 1984, Salmonid whirling disease : new findings provide evidence that the infectious form is a Triactinomyxon produced in a tubificid worm: Research Information Bulletin 59, 2 p.","productDescription":"2 p.","startPage":"1","endPage":"2","costCenters":[{"id":365,"text":"Leetown Science Center","active":true,"usgs":true}],"links":[{"id":258290,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"505ab00de4b0c8380cd878eb","contributors":{"authors":[{"text":"Wolf, K.","contributorId":16344,"corporation":false,"usgs":true,"family":"Wolf","given":"K.","email":"","affiliations":[],"preferred":false,"id":355523,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Markiw, M.E.","contributorId":44865,"corporation":false,"usgs":true,"family":"Markiw","given":"M.E.","affiliations":[],"preferred":false,"id":355524,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":70006928,"text":"70006928 - 1984 - Monoclonal antibody against IHN virus","interactions":[],"lastModifiedDate":"2012-07-07T01:01:38","indexId":"70006928","displayToPublicDate":"2012-01-01T11:56:54","publicationYear":"1984","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1649,"text":"Fish Health Section Newsletter","active":true,"publicationSubtype":{"id":10}},"title":"Monoclonal antibody against IHN virus","largerWorkType":{"id":2,"text":"Article"},"largerWorkTitle":"Fish Health Section Newsletter","largerWorkSubtype":{"id":10,"text":"Journal Article"},"language":"English","publisher":"American Fisheries Society","publisherLocation":"Bethesda, MD","collaboration":"None","usgsCitation":"Schultz, C.L., Lidgerding, B.C., McAllister, P.E., and Hetrick, F.M., 1984, Monoclonal antibody against IHN virus: Fish Health Section Newsletter, v. 12, no. 4, p. 5-5.","productDescription":"1 p.","startPage":"5","endPage":"5","numberOfPages":"1","costCenters":[{"id":365,"text":"Leetown Science Center","active":true,"usgs":true}],"links":[{"id":258241,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"12","issue":"4","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"505a5e02e4b0c8380cd70750","contributors":{"authors":[{"text":"Schultz, C. L.","contributorId":24308,"corporation":false,"usgs":false,"family":"Schultz","given":"C.","email":"","middleInitial":"L.","affiliations":[],"preferred":false,"id":355482,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Lidgerding, B. C.","contributorId":8028,"corporation":false,"usgs":true,"family":"Lidgerding","given":"B.","email":"","middleInitial":"C.","affiliations":[],"preferred":false,"id":355481,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"McAllister, P. E.","contributorId":71913,"corporation":false,"usgs":true,"family":"McAllister","given":"P.","email":"","middleInitial":"E.","affiliations":[],"preferred":false,"id":355483,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Hetrick, F. M.","contributorId":74337,"corporation":false,"usgs":false,"family":"Hetrick","given":"F.","email":"","middleInitial":"M.","affiliations":[],"preferred":false,"id":355484,"contributorType":{"id":1,"text":"Authors"},"rank":4}]}}
,{"id":70006820,"text":"70006820 - 1984 - You asked for it! New edition of the report to the fish farmers","interactions":[],"lastModifiedDate":"2012-11-27T00:19:58","indexId":"70006820","displayToPublicDate":"2012-01-01T00:00:00","publicationYear":"1984","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":"You asked for it! New edition of the report to the fish farmers","largerWorkType":{"id":2,"text":"Article"},"largerWorkTitle":"Aquaculture Magazine","largerWorkSubtype":{"id":10,"text":"Journal Article"},"language":"English","publisher":"Achill River Corporation","publisherLocation":"Asheville, NC","collaboration":"None","usgsCitation":"Martin, M., 1984, You asked for it! New edition of the report to the fish farmers: Aquaculture Magazine, v. 11, no. 2, p. 37-37.","productDescription":"1 p.","startPage":"37","endPage":"37","numberOfPages":"1","costCenters":[{"id":365,"text":"Leetown Science Center","active":true,"usgs":true}],"links":[{"id":263388,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"11","issue":"2","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"50b49ddee4b0b3fb1a229190","contributors":{"authors":[{"text":"Martin, M.","contributorId":103217,"corporation":false,"usgs":true,"family":"Martin","given":"M.","affiliations":[],"preferred":false,"id":355291,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":70000656,"text":"70000656 - 1984 - Submarine-fan facies associations of the Upper Cretaceous and Paleocene Gottero Sandstone, Ligurian Apennines, Italy","interactions":[],"lastModifiedDate":"2012-03-08T17:16:36","indexId":"70000656","displayToPublicDate":"2010-09-28T23:09:27","publicationYear":"1984","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1742,"text":"Geo-Marine Letters","active":true,"publicationSubtype":{"id":10}},"title":"Submarine-fan facies associations of the Upper Cretaceous and Paleocene Gottero Sandstone, Ligurian Apennines, Italy","docAbstract":"The Upper Cretaceous and Paleocene Gottero Sandstone was deposited as a small deep-sea fan on ophiolitic crust in a trench-slope basin. It was thrust northeastward as an allochthonous sheet in Early and Middle Cenozoic time. The Gottero, as thick as 1500 m, was probably derived from erosion of Hercynian granites and associated metamorphic rocks in northern Corsica. Outcrops of inner-fan channel, middle-fan channel and interchannel, outer-fan lobe, fan-fringe, and basin-plain facies associations indicate that the depositional model of Mutti and Ricci Lucchi for mixed-sediment deep-sea fans can be used. The original fan had a radius of 30 to 50 km. ?? 1984 Springer-Verlag New York Inc.","largerWorkType":{"id":2,"text":"Article"},"largerWorkTitle":"Geo-Marine Letters","largerWorkSubtype":{"id":10,"text":"Journal Article"},"language":"English","publisher":"Springer-Verlag","doi":"10.1007/BF02462467","issn":"02760460","usgsCitation":"Nilsen, T.H., and Abbate, E., 1984, Submarine-fan facies associations of the Upper Cretaceous and Paleocene Gottero Sandstone, Ligurian Apennines, Italy: Geo-Marine Letters, v. 3, no. 2-4, p. 193-197, https://doi.org/10.1007/BF02462467.","startPage":"193","endPage":"197","costCenters":[],"links":[{"id":203766,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"},{"id":18993,"rank":9999,"type":{"id":10,"text":"Digital Object Identifier"},"url":"https://dx.doi.org/10.1007/BF02462467"}],"volume":"3","issue":"2-4","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b05e4b07f02db699b70","contributors":{"authors":[{"text":"Nilsen, T. H.","contributorId":93057,"corporation":false,"usgs":true,"family":"Nilsen","given":"T.","email":"","middleInitial":"H.","affiliations":[],"preferred":false,"id":346451,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Abbate, E.","contributorId":50274,"corporation":false,"usgs":true,"family":"Abbate","given":"E.","email":"","affiliations":[],"preferred":false,"id":346450,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":70000655,"text":"70000655 - 1984 - Submarine-fan facies associations of the Eocene Butano Sandstone, Santa Cruz mountains, California","interactions":[],"lastModifiedDate":"2012-03-08T17:16:36","indexId":"70000655","displayToPublicDate":"2010-09-28T23:09:27","publicationYear":"1984","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1742,"text":"Geo-Marine Letters","active":true,"publicationSubtype":{"id":10}},"title":"Submarine-fan facies associations of the Eocene Butano Sandstone, Santa Cruz mountains, California","docAbstract":"The Eocene Butano Sandstone was deposited as a submarine fan in a relatively small, partly restricted basin in a borderland setting. It is possibly as thick as 3000 m and was derived from erosion of nearly Mesozoic granitic and older metamorphic rocks located to the south. Deposition was at lower bathyal to abyssal water depths. The original fan may have been 120-to 160-km long and 80-km wide. Outcrops of submarine-canyon, innerfan, middle-fan, and outer-fan facies associations indicate that the depositional model of Mutti and Ricci Lucchi can be used to describe the Butano Sandstone. ?? 1984 Springer-Verlag New York Inc.","largerWorkType":{"id":2,"text":"Article"},"largerWorkTitle":"Geo-Marine Letters","largerWorkSubtype":{"id":10,"text":"Journal Article"},"language":"English","publisher":"Springer-Verlag","doi":"10.1007/BF02462463","issn":"02760460","usgsCitation":"Nilsen, T.H., 1984, Submarine-fan facies associations of the Eocene Butano Sandstone, Santa Cruz mountains, California: Geo-Marine Letters, v. 3, no. 2-4, p. 167-171, https://doi.org/10.1007/BF02462463.","startPage":"167","endPage":"171","costCenters":[],"links":[{"id":203321,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"},{"id":18992,"rank":9999,"type":{"id":10,"text":"Digital Object Identifier"},"url":"https://dx.doi.org/10.1007/BF02462463"}],"volume":"3","issue":"2-4","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b05e4b07f02db699b86","contributors":{"authors":[{"text":"Nilsen, T. H.","contributorId":93057,"corporation":false,"usgs":true,"family":"Nilsen","given":"T.","email":"","middleInitial":"H.","affiliations":[],"preferred":false,"id":346449,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":70000657,"text":"70000657 - 1984 - Monterey Fan: Growth pattern control by basin morphology and changing sea levels","interactions":[],"lastModifiedDate":"2012-03-08T17:16:36","indexId":"70000657","displayToPublicDate":"2010-09-28T23:09:27","publicationYear":"1984","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1742,"text":"Geo-Marine Letters","active":true,"publicationSubtype":{"id":10}},"title":"Monterey Fan: Growth pattern control by basin morphology and changing sea levels","docAbstract":"Monterey Fan is the largest modern fan off the California shore. Two main submarine canyon systems feed it via a complex pattern of fan valleys and channels. The northern Ascension Canyon system is relatively inactive during high sea-level periods. In contrast, Monterey Canyon and its tributaries to the south cut across the shelf and remain active during high sea level. Deposition on the upper fan is controlled primarily by the relative activity within these two canyon systems. Deposition over the rest of the fan is controlled by the oceanic crust topography, resulting in an irregular fan shape and periodic major shifts in the locus of deposition. ?? 1984 Springer-Verlag New York Inc.","largerWorkType":{"id":2,"text":"Article"},"largerWorkTitle":"Geo-Marine Letters","largerWorkSubtype":{"id":10,"text":"Journal Article"},"language":"English","publisher":"Springer-Verlag","doi":"10.1007/BF02462453","issn":"02760460","usgsCitation":"Normark, W.R., Gutmacher, C., Chase, T.E., and Wilde, P., 1984, Monterey Fan: Growth pattern control by basin morphology and changing sea levels: Geo-Marine Letters, v. 3, no. 2-4, p. 93-99, https://doi.org/10.1007/BF02462453.","startPage":"93","endPage":"99","costCenters":[],"links":[{"id":203798,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"},{"id":18994,"rank":9999,"type":{"id":10,"text":"Digital Object Identifier"},"url":"https://dx.doi.org/10.1007/BF02462453"}],"volume":"3","issue":"2-4","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b03e4b07f02db698fc6","contributors":{"authors":[{"text":"Normark, W. R.","contributorId":87137,"corporation":false,"usgs":true,"family":"Normark","given":"W.","email":"","middleInitial":"R.","affiliations":[],"preferred":false,"id":346455,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Gutmacher, C. E.","contributorId":45284,"corporation":false,"usgs":true,"family":"Gutmacher","given":"C. E.","affiliations":[],"preferred":false,"id":346453,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Chase, T. E.","contributorId":14784,"corporation":false,"usgs":true,"family":"Chase","given":"T.","email":"","middleInitial":"E.","affiliations":[],"preferred":false,"id":346452,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Wilde, P.","contributorId":61885,"corporation":false,"usgs":true,"family":"Wilde","given":"P.","email":"","affiliations":[],"preferred":false,"id":346454,"contributorType":{"id":1,"text":"Authors"},"rank":4}]}}
,{"id":70000654,"text":"70000654 - 1984 - Ferrelo fan, California: Depositional system influenced by Eustatic sea level changes","interactions":[],"lastModifiedDate":"2012-03-08T17:16:36","indexId":"70000654","displayToPublicDate":"2010-09-28T23:09:27","publicationYear":"1984","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1742,"text":"Geo-Marine Letters","active":true,"publicationSubtype":{"id":10}},"title":"Ferrelo fan, California: Depositional system influenced by Eustatic sea level changes","docAbstract":"Remnants of an Eocene fan system are preserved onshore at San Diego and in the central part of the southern California borderland. Even though faults and erosion have truncated its margins, geophysical data and exploratory wells indicate that remaining parts of the fan extend beneath an offshore area nearly 400-km long and 40- to 100-km wide. Environments representing fluvial, fan-delta, shelf-channel, overlapping inner- to outer-fan, and basin-plain facies are recognized or inferred. Three progradational cycles onshore and two distinct pulses of sand accumulation offshore are attributable to eustatic low sea-level stands rather than to tectonic uplift or shifts in depositional patterns. ?? 1984 Springer-Verlag New York Inc.","largerWorkType":{"id":2,"text":"Article"},"largerWorkTitle":"Geo-Marine Letters","largerWorkSubtype":{"id":10,"text":"Journal Article"},"language":"English","publisher":"Springer-Verlag","doi":"10.1007/BF02462466","issn":"02760460","usgsCitation":"Howell, D.G., and Vedder, J.G., 1984, Ferrelo fan, California: Depositional system influenced by Eustatic sea level changes: Geo-Marine Letters, v. 3, no. 2-4, p. 187-192, https://doi.org/10.1007/BF02462466.","startPage":"187","endPage":"192","costCenters":[],"links":[{"id":203320,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"},{"id":18991,"rank":9999,"type":{"id":10,"text":"Digital Object Identifier"},"url":"https://dx.doi.org/10.1007/BF02462466"}],"volume":"3","issue":"2-4","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e49fce4b07f02db5f5c0c","contributors":{"authors":[{"text":"Howell, D. G.","contributorId":52546,"corporation":false,"usgs":true,"family":"Howell","given":"D.","email":"","middleInitial":"G.","affiliations":[],"preferred":false,"id":346447,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Vedder, J. G.","contributorId":97873,"corporation":false,"usgs":true,"family":"Vedder","given":"J.","middleInitial":"G.","affiliations":[],"preferred":false,"id":346448,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":70000648,"text":"70000648 - 1984 - Sedimentary, tectonic, and sea-level controls on submarine fan and slope-apron turbidite systems","interactions":[],"lastModifiedDate":"2012-03-08T17:16:38","indexId":"70000648","displayToPublicDate":"2010-09-28T23:09:26","publicationYear":"1984","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1742,"text":"Geo-Marine Letters","active":true,"publicationSubtype":{"id":10}},"title":"Sedimentary, tectonic, and sea-level controls on submarine fan and slope-apron turbidite systems","docAbstract":"To help understand factors that influence submarine fan deposition, we outline some of the principal sedimentary, tectonic, and sea-level controls involved in deep-water sedimentation, give some data on the rates at which they operate, and evaluate their probable effects. Three depositional end-member systems, two submarine fan types (elongate and radial), and a third nonfan, slope-apron system result primarily from variations in sediment type and supply. Tectonic setting and local and global sea-level changes further modify the nature of fan growth, the distribution of facies, and the resulting vertical stratigraphic sequences. ?? 1984 Springer-Verlag New York Inc.","largerWorkType":{"id":2,"text":"Article"},"largerWorkTitle":"Geo-Marine Letters","largerWorkSubtype":{"id":10,"text":"Journal Article"},"language":"English","publisher":"Springer-Verlag","doi":"10.1007/BF02462448","issn":"02760460","usgsCitation":"Stow, D., Howell, D.G., and Nelson, C., 1984, Sedimentary, tectonic, and sea-level controls on submarine fan and slope-apron turbidite systems: Geo-Marine Letters, v. 3, no. 2-4, p. 57-64, https://doi.org/10.1007/BF02462448.","startPage":"57","endPage":"64","costCenters":[],"links":[{"id":203415,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"},{"id":18986,"rank":9999,"type":{"id":10,"text":"Digital Object Identifier"},"url":"https://dx.doi.org/10.1007/BF02462448"}],"volume":"3","issue":"2-4","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a0be4b07f02db5fbd3c","contributors":{"authors":[{"text":"Stow, D.A.V.","contributorId":35441,"corporation":false,"usgs":true,"family":"Stow","given":"D.A.V.","email":"","affiliations":[],"preferred":false,"id":346425,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Howell, D. G.","contributorId":52546,"corporation":false,"usgs":true,"family":"Howell","given":"D.","email":"","middleInitial":"G.","affiliations":[],"preferred":false,"id":346426,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Nelson, C.H.","contributorId":88346,"corporation":false,"usgs":true,"family":"Nelson","given":"C.H.","email":"","affiliations":[],"preferred":false,"id":346427,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":70000641,"text":"70000641 - 1984 - Navy Fan, California Borderland: Growth pattern and depositional processes","interactions":[],"lastModifiedDate":"2012-03-08T17:16:34","indexId":"70000641","displayToPublicDate":"2010-09-28T23:09:26","publicationYear":"1984","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1742,"text":"Geo-Marine Letters","active":true,"publicationSubtype":{"id":10}},"title":"Navy Fan, California Borderland: Growth pattern and depositional processes","docAbstract":"Navy Fan is a Late Pleistocene sand-rich fan prograding into an irregularly shaped basin in the southern California Borderland. The middle fan, characterized by one active and two abandoned 'distributary' channels and associated lobe deposits, at present onlaps part of the basin slope directly opposite from the upper-fan valley, thus dividing the lower-fan/basin-plain regions into two separate parts of different depths. Fine-scale mesotopographic relief on the fan surface and correlation of individual turbidite beds through nearly 40 cores on the middle and lower fan provide data for evaluating the Late Pleistocene and Holocene depositional processes. ?? 1984 Springer-Verlag New York Inc.","largerWorkType":{"id":2,"text":"Article"},"largerWorkTitle":"Geo-Marine Letters","largerWorkSubtype":{"id":10,"text":"Journal Article"},"language":"English","publisher":"Springer-Verlag","doi":"10.1007/BF02462454","issn":"02760460","usgsCitation":"Normark, W.R., and Piper, D., 1984, Navy Fan, California Borderland: Growth pattern and depositional processes: Geo-Marine Letters, v. 3, no. 2-4, p. 101-108, https://doi.org/10.1007/BF02462454.","startPage":"101","endPage":"108","costCenters":[],"links":[{"id":203431,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"},{"id":18980,"rank":9999,"type":{"id":10,"text":"Digital Object Identifier"},"url":"https://dx.doi.org/10.1007/BF02462454"}],"volume":"3","issue":"2-4","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b00e4b07f02db697fe3","contributors":{"authors":[{"text":"Normark, W. R.","contributorId":87137,"corporation":false,"usgs":true,"family":"Normark","given":"W.","email":"","middleInitial":"R.","affiliations":[],"preferred":false,"id":346415,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Piper, D.J.W.","contributorId":17351,"corporation":false,"usgs":false,"family":"Piper","given":"D.J.W.","email":"","affiliations":[{"id":7219,"text":"Natural Resources Canada","active":true,"usgs":false}],"preferred":false,"id":346414,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":70000639,"text":"70000639 - 1984 - Problems in turbidite research: A need for COMFAN","interactions":[],"lastModifiedDate":"2012-03-08T17:16:34","indexId":"70000639","displayToPublicDate":"2010-09-28T23:09:26","publicationYear":"1984","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1742,"text":"Geo-Marine Letters","active":true,"publicationSubtype":{"id":10}},"title":"Problems in turbidite research: A need for COMFAN","docAbstract":"Comparison of modern submarine fans and ancient turbidite sequences is still in its infancy, mainly because of the incompatibility of study approaches. Research on modern fan systems mainly deals with morphologic aspects and surficial sediments, while observations on ancient turbidite formations are mostly directed to vertical sequences. The lack of a common data set also results from different scales of observation. To review the current status of modern and ancient turbidite research, an international group of specialists formed COMFAN (Committee on Fans) and met in September 1982 at the Gulf Research and Development Company research facilities in Pennsylvania. ?? 1984 Springer-Verlag New York Inc.","largerWorkType":{"id":2,"text":"Article"},"largerWorkTitle":"Geo-Marine Letters","largerWorkSubtype":{"id":10,"text":"Journal Article"},"language":"English","publisher":"Springer-Verlag","doi":"10.1007/BF02462447","issn":"02760460","usgsCitation":"Normark, W.R., Mutti, E., and Bouma, A., 1984, Problems in turbidite research: A need for COMFAN: Geo-Marine Letters, v. 3, no. 2-4, p. 53-56, https://doi.org/10.1007/BF02462447.","startPage":"53","endPage":"56","costCenters":[],"links":[{"id":18978,"rank":9999,"type":{"id":10,"text":"Digital Object Identifier"},"url":"https://dx.doi.org/10.1007/BF02462447"},{"id":203723,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"3","issue":"2-4","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a9ee4b07f02db660a5b","contributors":{"authors":[{"text":"Normark, W. R.","contributorId":87137,"corporation":false,"usgs":true,"family":"Normark","given":"W.","email":"","middleInitial":"R.","affiliations":[],"preferred":false,"id":346411,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Mutti, E.","contributorId":86088,"corporation":false,"usgs":true,"family":"Mutti","given":"E.","email":"","affiliations":[],"preferred":false,"id":346410,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Bouma, A.H.","contributorId":107281,"corporation":false,"usgs":true,"family":"Bouma","given":"A.H.","email":"","affiliations":[],"preferred":false,"id":346412,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":70000647,"text":"70000647 - 1984 - Turbidite facies in an ancient subduction complex: Torlesse terrane, New Zealand","interactions":[],"lastModifiedDate":"2012-03-08T17:16:35","indexId":"70000647","displayToPublicDate":"2010-09-28T23:09:26","publicationYear":"1984","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1742,"text":"Geo-Marine Letters","active":true,"publicationSubtype":{"id":10}},"title":"Turbidite facies in an ancient subduction complex: Torlesse terrane, New Zealand","docAbstract":"The Torlesse terrane of New Zealand is an ancient subduction complex consisting of deformed turbidite-facies rocks. These are mainly thick-bedded sandstone (facies B and C) with subordinate mudstone (facies D and E), comparable to inner- and middle-fan deposits of a submarine fan. Strata were deposited in trench-floor and trench-slope settings that received sandy sediment from slope-cutting submarine canyons. The dominance of sandstone suggests that some mudstone may have been selectively subducted. Construction of a detailed sediment dispersal model is not possible because tectonic deformation has largely destroyed original facies relationships and paleocurrent patterns. ?? 1984 Springer-Verlag New York Inc.","largerWorkType":{"id":2,"text":"Article"},"largerWorkTitle":"Geo-Marine Letters","largerWorkSubtype":{"id":10,"text":"Journal Article"},"language":"English","publisher":"Springer-Verlag","doi":"10.1007/BF02462470","issn":"02760460","usgsCitation":"MacKinnon, T., and Howell, D.G., 1984, Turbidite facies in an ancient subduction complex: Torlesse terrane, New Zealand: Geo-Marine Letters, v. 3, no. 2-4, p. 211-216, https://doi.org/10.1007/BF02462470.","startPage":"211","endPage":"216","costCenters":[],"links":[{"id":203599,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"},{"id":18985,"rank":9999,"type":{"id":10,"text":"Digital Object Identifier"},"url":"https://dx.doi.org/10.1007/BF02462470"}],"volume":"3","issue":"2-4","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a49e4b07f02db623f0c","contributors":{"authors":[{"text":"MacKinnon, T.C.","contributorId":37871,"corporation":false,"usgs":true,"family":"MacKinnon","given":"T.C.","email":"","affiliations":[],"preferred":false,"id":346423,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Howell, D. G.","contributorId":52546,"corporation":false,"usgs":true,"family":"Howell","given":"D.","email":"","middleInitial":"G.","affiliations":[],"preferred":false,"id":346424,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":70000640,"text":"70000640 - 1984 - Trench-fill submarine-fan facies associations of the Upper Cretaceous Chugach terrane, southern Alaska","interactions":[],"lastModifiedDate":"2012-03-08T17:16:34","indexId":"70000640","displayToPublicDate":"2010-09-28T23:09:26","publicationYear":"1984","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1742,"text":"Geo-Marine Letters","active":true,"publicationSubtype":{"id":10}},"title":"Trench-fill submarine-fan facies associations of the Upper Cretaceous Chugach terrane, southern Alaska","docAbstract":"Turbidites of the Upper Cretaceous Chugach terrane of southern Alaska were deposited in a trench during northward-directed subduction. The fault-bounded outcrop belt of the Chugach terrane is about 2000-km long and 100-km wide and was accreted to Alaska during the Cenozoic. Turbidites are at least 5000 m thick, are extensively deformed, have been regionally metamorphosed, and have been intruded by anatectic granites. Facies associations indicate an east-to-west progression from inner-fan to middle-fan, outer-fan, fan-fringe, and basin-plain deposits. To the north is a marginal trench-slope facies association and a basin. ?? 1984 Springer-Verlag New York Inc.","largerWorkType":{"id":2,"text":"Article"},"largerWorkTitle":"Geo-Marine Letters","largerWorkSubtype":{"id":10,"text":"Journal Article"},"language":"English","publisher":"Springer-Verlag","doi":"10.1007/BF02462465","issn":"02760460","usgsCitation":"Nilsen, T.H., 1984, Trench-fill submarine-fan facies associations of the Upper Cretaceous Chugach terrane, southern Alaska: Geo-Marine Letters, v. 3, no. 2-4, p. 179-185, https://doi.org/10.1007/BF02462465.","startPage":"179","endPage":"185","costCenters":[],"links":[{"id":18979,"rank":9999,"type":{"id":10,"text":"Digital Object Identifier"},"url":"https://dx.doi.org/10.1007/BF02462465"},{"id":203625,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"3","issue":"2-4","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a4ce4b07f02db626834","contributors":{"authors":[{"text":"Nilsen, T. H.","contributorId":93057,"corporation":false,"usgs":true,"family":"Nilsen","given":"T.","email":"","middleInitial":"H.","affiliations":[],"preferred":false,"id":346413,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":70000646,"text":"70000646 - 1984 - Delgada Fan: Preliminary interpretation of channel development","interactions":[],"lastModifiedDate":"2012-03-08T17:16:35","indexId":"70000646","displayToPublicDate":"2010-09-28T23:09:26","publicationYear":"1984","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1742,"text":"Geo-Marine Letters","active":true,"publicationSubtype":{"id":10}},"title":"Delgada Fan: Preliminary interpretation of channel development","docAbstract":"The Delgada Fan, an irregularly shaped turbidite deposit extending more than 350 km offshore from northern California, consists of two large leveed-valley units each fed by a separate complex of coalescing submarine canyons and slope gullies. Although the leveed-valley units head within 25 km of each other, both appear to have developed independently during fan growth. The larger southern leveed-valley system has not developed middle-fan distributary channels and appears to illustrate a period of progressive valley abandonment. Although the lower-fan area is underlain by sandy sediments, little sand has been recovered in piston cores from the leveed-valley unit. ?? 1984 Springer-Verlag New York Inc.","largerWorkType":{"id":2,"text":"Article"},"largerWorkTitle":"Geo-Marine Letters","largerWorkSubtype":{"id":10,"text":"Journal Article"},"language":"English","publisher":"Springer-Verlag","doi":"10.1007/BF02462451","issn":"02760460","usgsCitation":"Normark, W.R., and Gutmacher, C., 1984, Delgada Fan: Preliminary interpretation of channel development: Geo-Marine Letters, v. 3, no. 2-4, p. 79-83, https://doi.org/10.1007/BF02462451.","startPage":"79","endPage":"83","costCenters":[],"links":[{"id":203568,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"},{"id":18984,"rank":9999,"type":{"id":10,"text":"Digital Object Identifier"},"url":"https://dx.doi.org/10.1007/BF02462451"}],"volume":"3","issue":"2-4","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4abae4b07f02db671d89","contributors":{"authors":[{"text":"Normark, W. R.","contributorId":87137,"corporation":false,"usgs":true,"family":"Normark","given":"W.","email":"","middleInitial":"R.","affiliations":[],"preferred":false,"id":346422,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Gutmacher, C. E.","contributorId":45284,"corporation":false,"usgs":true,"family":"Gutmacher","given":"C. E.","affiliations":[],"preferred":false,"id":346421,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":70000649,"text":"70000649 - 1984 - Fouling community of the Loxahatchee River estuary, Florida, 1980-81","interactions":[],"lastModifiedDate":"2023-10-16T15:59:41.492127","indexId":"70000649","displayToPublicDate":"2010-09-28T23:09:26","publicationYear":"1984","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1583,"text":"Estuaries","active":true,"publicationSubtype":{"id":10}},"title":"Fouling community of the Loxahatchee River estuary, Florida, 1980-81","docAbstract":"<p><span>Monthly growth of the fouling community at eight test panel sites in the Loxahatchee River Estuary was related to salinity and temperature. Growth was lowest in January 1981 (averaging 23 g per m</span><sup>2</sup><span>, dry weight), and increased during spring and early summer with increasing water temperature. Maximum growth occurred during early or midsummer at upstream locations, before river or canal discharge substantially reduced salinity, and in late summer at downstream locations. Growth was greatest at salinities slightly less than that of seawater and decreased at salinities less than about 10‰. Growth was suppressed throughout the estuary in August 1981, probably because of the sudden decrease in temperature and salinity, and perhaps the increase in physical scouring, caused by runoff from Tropical Storm Dennis. Large loads of nutrients transported to the estuary from storm runoff, however, may have subsequently stimulated growth, which increased in September 1981 to the maximum for the year (averaging 683 g per m</span><sup>2</sup><span>, dry weight).</span></p>","language":"English","publisher":"Springer-Verlag","doi":"10.2307/1351769","issn":"15592723","usgsCitation":"McPherson, B.F., Sonntag, W.H., and Sabanskas, M., 1984, Fouling community of the Loxahatchee River estuary, Florida, 1980-81: Estuaries, v. 7, no. 2, p. 149-157, https://doi.org/10.2307/1351769.","productDescription":"9 p.","startPage":"149","endPage":"157","costCenters":[],"links":[{"id":203416,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United States","state":"Florida","otherGeospatial":"Loxahatchee River Estuary","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": 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F.","contributorId":62983,"corporation":false,"usgs":true,"family":"McPherson","given":"B.","email":"","middleInitial":"F.","affiliations":[],"preferred":false,"id":346428,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Sonntag, W. H.","contributorId":106127,"corporation":false,"usgs":true,"family":"Sonntag","given":"W.","email":"","middleInitial":"H.","affiliations":[],"preferred":false,"id":346429,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Sabanskas, M.","contributorId":107405,"corporation":false,"usgs":true,"family":"Sabanskas","given":"M.","affiliations":[],"preferred":false,"id":346430,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":70000644,"text":"70000644 - 1984 - Aftermath of comfan-Comments, not solutions","interactions":[],"lastModifiedDate":"2012-03-08T17:16:34","indexId":"70000644","displayToPublicDate":"2010-09-28T23:09:26","publicationYear":"1984","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1742,"text":"Geo-Marine Letters","active":true,"publicationSubtype":{"id":10}},"title":"Aftermath of comfan-Comments, not solutions","docAbstract":"Comparison of descriptions of fans in this volume demonstrates the major problems in developing general models that incorporate modern fans and ancient turbidite sequences. Attempts to develop a unifying fan model are presently premature. The most pressing need is refined definition of the primary common characteristics of submarine turbidite systems such as fans. ?? 1984 Springer-Verlag New York Inc.","largerWorkType":{"id":2,"text":"Article"},"largerWorkTitle":"Geo-Marine Letters","largerWorkSubtype":{"id":10,"text":"Journal Article"},"language":"English","publisher":"Springer-Verlag","doi":"10.1007/BF02462472","issn":"02760460","usgsCitation":"Normark, W.R., and Barnes, N., 1984, Aftermath of comfan-Comments, not solutions: Geo-Marine Letters, v. 3, no. 2-4, p. 223-224, https://doi.org/10.1007/BF02462472.","startPage":"223","endPage":"224","costCenters":[],"links":[{"id":203468,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"},{"id":18982,"rank":9999,"type":{"id":10,"text":"Digital Object Identifier"},"url":"https://dx.doi.org/10.1007/BF02462472"}],"volume":"3","issue":"2-4","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ae4e4b07f02db6898ef","contributors":{"authors":[{"text":"Normark, W. R.","contributorId":87137,"corporation":false,"usgs":true,"family":"Normark","given":"W.","email":"","middleInitial":"R.","affiliations":[],"preferred":false,"id":346419,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Barnes, N.E.","contributorId":15322,"corporation":false,"usgs":true,"family":"Barnes","given":"N.E.","email":"","affiliations":[],"preferred":false,"id":346418,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":70000645,"text":"70000645 - 1984 - The Astoria Fan: An elongate type fan","interactions":[],"lastModifiedDate":"2012-03-08T17:16:35","indexId":"70000645","displayToPublicDate":"2010-09-28T23:09:26","publicationYear":"1984","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1742,"text":"Geo-Marine Letters","active":true,"publicationSubtype":{"id":10}},"title":"The Astoria Fan: An elongate type fan","docAbstract":"The Astoria Fan, a modern system, is located on a subducting oceanic crust and fills a north-south-trending trench along the Oregon continental margin. Well-developed channels cross the entire fan length; they display classic inner-fan leveed profiles but evolve into distributaries in the midfan area where the gradient decreases sharply. During periods of low sea level, inner- and middle-fan channels funnel sand to distal depositional sites in the outer-fan area where the sand/shale ratios are highest. This pattern of sand displacement and efficiency of transport appears to be characteristic of elongate fans fed by a major river and submarine canyon. ?? 1984 Springer-Verlag New York Inc.","largerWorkType":{"id":2,"text":"Article"},"largerWorkTitle":"Geo-Marine Letters","largerWorkSubtype":{"id":10,"text":"Journal Article"},"language":"English","publisher":"Springer-Verlag","doi":"10.1007/BF02462449","issn":"02760460","usgsCitation":"Nelson, C., 1984, The Astoria Fan: An elongate type fan: Geo-Marine Letters, v. 3, no. 2-4, p. 65-70, https://doi.org/10.1007/BF02462449.","startPage":"65","endPage":"70","costCenters":[],"links":[{"id":203567,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"},{"id":18983,"rank":9999,"type":{"id":10,"text":"Digital Object Identifier"},"url":"https://dx.doi.org/10.1007/BF02462449"}],"volume":"3","issue":"2-4","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ad4e4b07f02db682c99","contributors":{"authors":[{"text":"Nelson, C.H.","contributorId":88346,"corporation":false,"usgs":true,"family":"Nelson","given":"C.H.","email":"","affiliations":[],"preferred":false,"id":346420,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":70000635,"text":"70000635 - 1984 - Defining geologic Hazards for natural resources management using tree-ring analysis","interactions":[],"lastModifiedDate":"2012-03-08T17:16:33","indexId":"70000635","displayToPublicDate":"2010-09-28T23:09:26","publicationYear":"1984","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1540,"text":"Environmental Geology and Water Sciences","active":true,"publicationSubtype":{"id":10}},"title":"Defining geologic Hazards for natural resources management using tree-ring analysis","docAbstract":"Landslides, avalanches, floods, and other geologic hazards impair natural resources management by jeopardizing public safety, damaging or restricting resource utilization, and necessitating expenditures for corrective measures The negative impact of geologic hazard events can be reduced by tailoring resources management to hazard potential of an area This requires assessment of where and how frequently the events occur National forests and other managed wildlands often lack monitoring or historical records to compute frequency of hazard occurrence Tree-ring analysis, based on internal growth response to external events such as tilting and abrasion, can provide frequency data Two examples of the use of tree-ring analysis to date landslide activity illustrate advantages and limitations of the technique An example from the Fishlake National Forest in central Utah illustrates assessment for planning purposes An example from the Sierra National Forest in east-central California shows assessment applied to project design Many geologic hazards in addition to landslides are suited to tree-ring analysis to establish frequency of occurrence Hazard reduction efforts in natural resources management could be enhanced by careful application of tree-ring analysis ?? 1984 Springer-Verlag New York Inc.","largerWorkType":{"id":2,"text":"Article"},"largerWorkTitle":"Environmental Geology and Water Sciences","largerWorkSubtype":{"id":10,"text":"Journal Article"},"language":"English","publisher":"Springer-Verlag","doi":"10.1007/BF02509908","issn":"00990094","usgsCitation":"DeGraff, J., and Agard, S., 1984, Defining geologic Hazards for natural resources management using tree-ring analysis: Environmental Geology and Water Sciences, v. 6, no. 3, p. 147-155, https://doi.org/10.1007/BF02509908.","startPage":"147","endPage":"155","costCenters":[],"links":[{"id":18977,"rank":9999,"type":{"id":10,"text":"Digital Object Identifier"},"url":"https://dx.doi.org/10.1007/BF02509908"},{"id":203306,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"6","issue":"3","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4abbe4b07f02db67253f","contributors":{"authors":[{"text":"DeGraff, J.V.","contributorId":57999,"corporation":false,"usgs":true,"family":"DeGraff","given":"J.V.","email":"","affiliations":[],"preferred":false,"id":346409,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Agard, S.S.","contributorId":28668,"corporation":false,"usgs":true,"family":"Agard","given":"S.S.","email":"","affiliations":[],"preferred":false,"id":346408,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":70000651,"text":"70000651 - 1984 - Specific-lon electrode determinations of sulfide preconcentrated from San Francisco Bay waters","interactions":[],"lastModifiedDate":"2012-03-08T17:16:35","indexId":"70000651","displayToPublicDate":"2010-09-28T23:09:26","publicationYear":"1984","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1540,"text":"Environmental Geology and Water Sciences","active":true,"publicationSubtype":{"id":10}},"title":"Specific-lon electrode determinations of sulfide preconcentrated from San Francisco Bay waters","docAbstract":"Measurements of low-level dissolved-sulfide concentrations in estuarine water from San Francisco Bay have been made using the sulfide-specific electrode after preservation, separation, and preconcentration of the sulfide species. The separation and preconcentration were acheived by coprecipitation of ZnS with Zn(OH)2 followed by collection and dissolution of the precipitate, giving concentration factors up to 160-fold Preconcentration provided sulfide solutions that were adequately measurable within the practical working range of the specific-ion electrode The sulfide detection limit with the preconcentration step is 0 02 ??g/l Spike recoveries in the range of 81 to 10 1% have been achieved for laboratory-prepared samples having S2- concentrations as low as 0 6 ??g/l and 84 to 100% for an estuarine sample spiked in the field with 2 ??g/l (S(-II) Positive correlations have been found between dissolved S(-II) concentrations and concentrations of dissolved Cd, Cu, and Ni, negative correlations have been found between bisulfide (HS-) activity and activities of Cd2+, Cu2+, and Ag+ species ?? 1984 Springer-Verlag New York Inc.","largerWorkType":{"id":2,"text":"Article"},"largerWorkTitle":"Environmental Geology and Water Sciences","largerWorkSubtype":{"id":10,"text":"Journal Article"},"language":"English","publisher":"Springer-Verlag","doi":"10.1007/BF02509914","issn":"00990094","usgsCitation":"Vivit, D., Ball, J., and Jenne, E., 1984, Specific-lon electrode determinations of sulfide preconcentrated from San Francisco Bay waters: Environmental Geology and Water Sciences, v. 6, no. 2, p. 79-90, https://doi.org/10.1007/BF02509914.","startPage":"79","endPage":"90","costCenters":[],"links":[{"id":203790,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"},{"id":18988,"rank":9999,"type":{"id":10,"text":"Digital Object Identifier"},"url":"https://dx.doi.org/10.1007/BF02509914"}],"volume":"6","issue":"2","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e49e4e4b07f02db5e5e64","contributors":{"authors":[{"text":"Vivit, D.V.","contributorId":28609,"corporation":false,"usgs":true,"family":"Vivit","given":"D.V.","email":"","affiliations":[],"preferred":false,"id":346436,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Ball, J.W.","contributorId":67507,"corporation":false,"usgs":true,"family":"Ball","given":"J.W.","affiliations":[],"preferred":false,"id":346438,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Jenne, E. A.","contributorId":45716,"corporation":false,"usgs":true,"family":"Jenne","given":"E. A.","affiliations":[],"preferred":false,"id":346437,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":70000650,"text":"70000650 - 1984 - The Crati Submarine Fan, Ionian Sea","interactions":[],"lastModifiedDate":"2012-03-08T17:16:36","indexId":"70000650","displayToPublicDate":"2010-09-28T23:09:26","publicationYear":"1984","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1742,"text":"Geo-Marine Letters","active":true,"publicationSubtype":{"id":10}},"title":"The Crati Submarine Fan, Ionian Sea","docAbstract":"The Crati Fan is located in the tectonically active submerged extension of the Apennines chain and foretrough. The small fan system is growing in a relatively shallow (200 to 450 m), elongate nearshore basin receiving abundant input from the Crati River. The fan is characterized by a short, steep, channelized section (inner or upper fan) and a smooth, slightly bulging distal section (outer or lower fan). The numerous subparallel channels head in the shelf or littoral zone and do not form branching distributary patterns. Sand and mud depositional lobes of the outer fan stretch over more than 60% of fan length. ?? 1984 Springer-Verlag New York Inc.","largerWorkType":{"id":2,"text":"Article"},"largerWorkTitle":"Geo-Marine Letters","largerWorkSubtype":{"id":10,"text":"Journal Article"},"language":"English","publisher":"Springer-Verlag","doi":"10.1007/BF02462450","issn":"02760460","usgsCitation":"Lucchi, F., Colella, A., Gabbianelli, G., Rossi, S., and Normark, W.R., 1984, The Crati Submarine Fan, Ionian Sea: Geo-Marine Letters, v. 3, no. 2-4, p. 71-77, https://doi.org/10.1007/BF02462450.","startPage":"71","endPage":"77","costCenters":[],"links":[{"id":203576,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"},{"id":18987,"rank":9999,"type":{"id":10,"text":"Digital Object Identifier"},"url":"https://dx.doi.org/10.1007/BF02462450"}],"volume":"3","issue":"2-4","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4acce4b07f02db67ec69","contributors":{"authors":[{"text":"Lucchi, F.R.","contributorId":102988,"corporation":false,"usgs":true,"family":"Lucchi","given":"F.R.","email":"","affiliations":[],"preferred":false,"id":346435,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Colella, A.","contributorId":24074,"corporation":false,"usgs":true,"family":"Colella","given":"A.","email":"","affiliations":[],"preferred":false,"id":346431,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Gabbianelli, G.","contributorId":53925,"corporation":false,"usgs":true,"family":"Gabbianelli","given":"G.","email":"","affiliations":[],"preferred":false,"id":346432,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Rossi, S.","contributorId":96812,"corporation":false,"usgs":true,"family":"Rossi","given":"S.","email":"","affiliations":[],"preferred":false,"id":346434,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"Normark, W. R.","contributorId":87137,"corporation":false,"usgs":true,"family":"Normark","given":"W.","email":"","middleInitial":"R.","affiliations":[],"preferred":false,"id":346433,"contributorType":{"id":1,"text":"Authors"},"rank":5}]}}
,{"id":70000643,"text":"70000643 - 1984 - Miocene Blanca Fan, Northern Channel Islands, California: Small fans reflecting tectonism and volcanism","interactions":[],"lastModifiedDate":"2012-03-08T17:16:34","indexId":"70000643","displayToPublicDate":"2010-09-28T23:09:26","publicationYear":"1984","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1742,"text":"Geo-Marine Letters","active":true,"publicationSubtype":{"id":10}},"title":"Miocene Blanca Fan, Northern Channel Islands, California: Small fans reflecting tectonism and volcanism","docAbstract":"Blanca fan is a submarine fan composed of Miocene volcaniclastic strata. Parts of the fan system are exposed on Santa Cruz and Santa Rosa Islands, and possibly correlative strata crop out on San Miguel and Santa Catalina Islands. The Blanca fan and underlying breccia reflect regional transcurrent faulting in the California Continental Borderland and development of a system of rapidly subsiding basins and uplifted linear ridges during early and middle Miocene time. Erosion of uplifted crystalline basement rocks followed by the onset of silicic volcanism created linear sediment sources for the alluvial and submarine fans, respectively. ?? 1984 Springer-Verlag New York Inc.","largerWorkType":{"id":2,"text":"Article"},"largerWorkTitle":"Geo-Marine Letters","largerWorkSubtype":{"id":10,"text":"Journal Article"},"language":"English","publisher":"Springer-Verlag","doi":"10.1007/BF02462462","issn":"02760460","usgsCitation":"McLean, H., and Howell, D.G., 1984, Miocene Blanca Fan, Northern Channel Islands, California: Small fans reflecting tectonism and volcanism: Geo-Marine Letters, v. 3, no. 2-4, p. 161-166, https://doi.org/10.1007/BF02462462.","startPage":"161","endPage":"166","costCenters":[],"links":[{"id":203467,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"},{"id":18981,"rank":9999,"type":{"id":10,"text":"Digital Object Identifier"},"url":"https://dx.doi.org/10.1007/BF02462462"}],"volume":"3","issue":"2-4","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b05e4b07f02db699c6d","contributors":{"authors":[{"text":"McLean, H.","contributorId":11212,"corporation":false,"usgs":true,"family":"McLean","given":"H.","email":"","affiliations":[],"preferred":false,"id":346416,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Howell, D. G.","contributorId":52546,"corporation":false,"usgs":true,"family":"Howell","given":"D.","email":"","middleInitial":"G.","affiliations":[],"preferred":false,"id":346417,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":70000653,"text":"70000653 - 1984 - The Ebro Deep-Sea Fan system","interactions":[],"lastModifiedDate":"2012-03-08T17:16:35","indexId":"70000653","displayToPublicDate":"2010-09-28T23:09:26","publicationYear":"1984","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1742,"text":"Geo-Marine Letters","active":true,"publicationSubtype":{"id":10}},"title":"The Ebro Deep-Sea Fan system","docAbstract":"The Ebro Fan System consists of en echelon channel-levee complexes, 50??20 km in area and 200-m thick. A few strong reflectors in a generally transparent seismic facies identify the sand-rich channel floors and levee crests. Numerous continuous acoustic reflectors characterize overbank turbidites and hemipelagites that blanket abandoned channel-levee complexes. The interlobe areas between channel complexes fill with homogeneous mud and sand from mass flow and overbank deposition; these exhibit a transparent seismic character. The steep continental rise and sediment 'drainage' of Valencia Trough at the end of the channel-levee complexes prevent the development of distributary channels and midfan lobe deposits. ?? 1984 Springer-Verlag New York Inc.","largerWorkType":{"id":2,"text":"Article"},"largerWorkTitle":"Geo-Marine Letters","largerWorkSubtype":{"id":10,"text":"Journal Article"},"language":"English","publisher":"Springer-Verlag","doi":"10.1007/BF02462457","issn":"02760460","usgsCitation":"Nelson, C., Maldonado, A., Coumes, F., Got, H., and Manaco, A., 1984, The Ebro Deep-Sea Fan system: Geo-Marine Letters, v. 3, no. 2-4, p. 125-131, https://doi.org/10.1007/BF02462457.","startPage":"125","endPage":"131","costCenters":[],"links":[{"id":203273,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"},{"id":18990,"rank":9999,"type":{"id":10,"text":"Digital Object Identifier"},"url":"https://dx.doi.org/10.1007/BF02462457"}],"volume":"3","issue":"2-4","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4acce4b07f02db67e438","contributors":{"authors":[{"text":"Nelson, C.H.","contributorId":88346,"corporation":false,"usgs":true,"family":"Nelson","given":"C.H.","email":"","affiliations":[],"preferred":false,"id":346444,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Maldonado, A.","contributorId":90437,"corporation":false,"usgs":true,"family":"Maldonado","given":"A.","affiliations":[],"preferred":false,"id":346445,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Coumes, F.","contributorId":22476,"corporation":false,"usgs":true,"family":"Coumes","given":"F.","email":"","affiliations":[],"preferred":false,"id":346442,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Got, H.","contributorId":33821,"corporation":false,"usgs":true,"family":"Got","given":"H.","email":"","affiliations":[],"preferred":false,"id":346443,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"Manaco, A.","contributorId":96807,"corporation":false,"usgs":true,"family":"Manaco","given":"A.","email":"","affiliations":[],"preferred":false,"id":346446,"contributorType":{"id":1,"text":"Authors"},"rank":5}]}}
,{"id":70000652,"text":"70000652 - 1984 - The Laurentian Fan: Sohm Abyssal Plain","interactions":[],"lastModifiedDate":"2012-03-08T17:16:35","indexId":"70000652","displayToPublicDate":"2010-09-28T23:09:26","publicationYear":"1984","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1742,"text":"Geo-Marine Letters","active":true,"publicationSubtype":{"id":10}},"title":"The Laurentian Fan: Sohm Abyssal Plain","docAbstract":"The 0.5- to 2-km thick Quaternary Laurentian Fan is built over Tertiary and Mesozoic sediments that rest on oceanic crust. Two 400-km long fan valleys, with asymmetric levees up to 700-m high, lead to an equally long, sandy, lobate basin plain (northern Sohm Abyssal Plain). The muddy distal Sohm Abyssal Plain is a further 400-km long. The sediment supplied to the fan is glacial in origin, and in part results from seismically triggered slumping on the upper continental slope. Sandy turbidity currents, such as the 1929 Grand Banks earthquake event, probably erode the fan-valley floors; but thick muddy turbidity currents build up the high levees. ?? 1984 Springer-Verlag New York Inc.","largerWorkType":{"id":2,"text":"Article"},"largerWorkTitle":"Geo-Marine Letters","largerWorkSubtype":{"id":10,"text":"Journal Article"},"language":"English","publisher":"Springer-Verlag","doi":"10.1007/BF02462459","issn":"02760460","usgsCitation":"Piper, D., Stow, D., and Normark, W.R., 1984, The Laurentian Fan: Sohm Abyssal Plain: Geo-Marine Letters, v. 3, no. 2-4, p. 141-146, https://doi.org/10.1007/BF02462459.","startPage":"141","endPage":"146","costCenters":[],"links":[{"id":203791,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"},{"id":18989,"rank":9999,"type":{"id":10,"text":"Digital Object Identifier"},"url":"https://dx.doi.org/10.1007/BF02462459"}],"volume":"3","issue":"2-4","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ac8e4b07f02db67bef6","contributors":{"authors":[{"text":"Piper, D.J.W.","contributorId":17351,"corporation":false,"usgs":false,"family":"Piper","given":"D.J.W.","email":"","affiliations":[{"id":7219,"text":"Natural Resources Canada","active":true,"usgs":false}],"preferred":false,"id":346439,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Stow, D.A.V.","contributorId":35441,"corporation":false,"usgs":true,"family":"Stow","given":"D.A.V.","email":"","affiliations":[],"preferred":false,"id":346440,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Normark, W. R.","contributorId":87137,"corporation":false,"usgs":true,"family":"Normark","given":"W.","email":"","middleInitial":"R.","affiliations":[],"preferred":false,"id":346441,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":5221897,"text":"5221897 - 1984 - Formalin preservation of avian blood for metal and DDE analysis","interactions":[],"lastModifiedDate":"2012-02-02T00:14:43","indexId":"5221897","displayToPublicDate":"2010-06-16T12:19:29","publicationYear":"1984","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1103,"text":"Bulletin of Environmental Contamination and Toxicology","active":true,"publicationSubtype":{"id":10}},"title":"Formalin preservation of avian blood for metal and DDE analysis","largerWorkType":{"id":2,"text":"Article"},"largerWorkTitle":"Bulletin of Environmental Contamination and Toxicology","largerWorkSubtype":{"id":10,"text":"Journal Article"},"language":"English","usgsCitation":"Wiemeyer, S.N., Moore, J.F., and Mulhern, B., 1984, Formalin preservation of avian blood for metal and DDE analysis: Bulletin of Environmental Contamination and Toxicology, v. 33, no. 5, p. 525-532.","productDescription":"525-532","startPage":"525","endPage":"532","numberOfPages":"8","costCenters":[{"id":531,"text":"Patuxent Wildlife Research Center","active":true,"usgs":true}],"links":[{"id":197370,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"},{"id":18424,"rank":200,"type":{"id":11,"text":"Document"},"url":"https://www.springerlink.com/content/q2123nh5630u5020/?p=06c788a3c2ff48329eb9031021f814fb&pi=77","linkFileType":{"id":5,"text":"html"}}],"volume":"33","issue":"5","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e49d6e4b07f02db5de181","contributors":{"authors":[{"text":"Wiemeyer, Stanley N.","contributorId":78279,"corporation":false,"usgs":true,"family":"Wiemeyer","given":"Stanley","email":"","middleInitial":"N.","affiliations":[],"preferred":false,"id":334951,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Moore, John F.","contributorId":30185,"corporation":false,"usgs":true,"family":"Moore","given":"John","email":"","middleInitial":"F.","affiliations":[],"preferred":false,"id":334950,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Mulhern, B.M.","contributorId":98683,"corporation":false,"usgs":true,"family":"Mulhern","given":"B.M.","email":"","affiliations":[],"preferred":false,"id":334952,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
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