{"pageNumber":"5607","pageRowStart":"140150","pageSize":"25","recordCount":184774,"records":[{"id":5221619,"text":"5221619 - 1980 - Dieldrin and heptachlor residues in dead gray bats, Franklin County, Missouri--1976 versus 1977","interactions":[],"lastModifiedDate":"2020-05-11T14:56:04.048522","indexId":"5221619","displayToPublicDate":"1980-06-16T12:19:25","publicationYear":"1980","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":3038,"text":"Pesticides Monitoring Journal","onlineIssn":" 0031-615","printIssn":" 0031-615","active":true,"publicationSubtype":{"id":10}},"title":"Dieldrin and heptachlor residues in dead gray bats, Franklin County, Missouri--1976 versus 1977","docAbstract":"<p>Lethal dieldrin concentrations were found in the brains of dead gray bats (<i>Myotis grisescens</i>) collected during 1976 and 1977 beneath a maternity roost in a Missouri cave. In addition, residues of heptachlor epoxide, oxychlordane, cis-chlordane, and trans-nonachlor increased significantly in both brains and carcasses of bats collected during 1977. These increases appear to reflect a switch by local farmers from aldrin, dieldrin's parent compound, to heptachlor for the control of cutworms. They also constitute an additional threat to this colony of this endangered bat species.</p>","largerWorkTitle":"","language":"English","publisher":"Federal Committee on Pest Control","usgsCitation":"Clark, D.R., LaVal, R.K., and Krynitsky, A.J., 1980, Dieldrin and heptachlor residues in dead gray bats, Franklin County, Missouri--1976 versus 1977: Pesticides Monitoring Journal, v. 13, no. 4, p. 137-140.","productDescription":"4 p.","startPage":"137","endPage":"140","numberOfPages":"4","costCenters":[{"id":531,"text":"Patuxent Wildlife Research Center","active":true,"usgs":true}],"links":[{"id":196747,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"13","issue":"4","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a9ae4b07f02db65d92d","contributors":{"authors":[{"text":"Clark, D. R. Jr.","contributorId":40928,"corporation":false,"usgs":true,"family":"Clark","given":"D.","suffix":"Jr.","middleInitial":"R.","affiliations":[],"preferred":false,"id":334286,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"LaVal, R. K.","contributorId":8945,"corporation":false,"usgs":true,"family":"LaVal","given":"R.","email":"","middleInitial":"K.","affiliations":[],"preferred":false,"id":334285,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Krynitsky, A. J.","contributorId":73954,"corporation":false,"usgs":true,"family":"Krynitsky","given":"A.","middleInitial":"J.","affiliations":[],"preferred":false,"id":334287,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":5221628,"text":"5221628 - 1980 - Pollution ecology of breeding great blue herons in the Columbia Basin, Oregon and Washington","interactions":[],"lastModifiedDate":"2020-05-12T15:53:40.599745","indexId":"5221628","displayToPublicDate":"1980-06-16T12:19:23","publicationYear":"1980","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":2793,"text":"Murrelet","active":true,"publicationSubtype":{"id":10}},"title":"Pollution ecology of breeding great blue herons in the Columbia Basin, Oregon and Washington","docAbstract":"<p>Approximately 40 pairs of Great Blue Herons (<i>Ardea herodias</i>) formerly nested in trees on or near Blalock Island about 95 km downstream from Richland, Washington, in the Columbia River (Nehls 1972 ). In conjunction with construction of the John Day Lock and Dam and before creating Lake Umatilla in 1968, large trees along the shoreline, including those in the heronry on Blalock Island, were removed except for about six cottonwood trees (<i>Populus</i> sp.) that were left standing near the south bank of the river (David Lenhart, pers. comm.). As a mitigation procedure, the Umatilla National Wildlife Refuge (Umatilla) was established in 1967. The herons subsequently established a secondary heronry in the six cottonwoods; 20 pairs were present in 1971 (Nehls 1972). The inundated trees died and deteriorated; only two trees with eight nests remained in 1976 (Henny and Kurtz 1978), and we found just two nests in one tree in 1978. With a decrease in traditional nesting sites, the birds nested on islands in big sagebrush (<i>Artemisia tridentata</i>), on channel markers in the Columbia River, and on nesting platforms constructed for Canada Geese (<i>Branta canadensis</i>). The purpose of this paper is to describe the breeding biology of Great Blue Herons at Umatilla and the McNary Recreation Area (McNary) in 1978 and the relationship of organochlorine residues in eggs to eggshell thickness and reproductive success. The primary reason for conducting this study was to determine if the heptachlor seed treatment that was severely affecting Canada Geese at Umatilla (Blus et al. 1979) was also a hazard to Great Blue Herons. At the same time we also investigated possible effects of other organochlorines on the herons.</p>","largerWorkTitle":"","language":"English","publisher":"Society for Northwestern Vertebrate Biology","doi":"10.2307/3535035","usgsCitation":"Blus, L.J., Henny, C.J., and Kaiser, T., 1980, Pollution ecology of breeding great blue herons in the Columbia Basin, Oregon and Washington: Murrelet, v. 61, no. 2, p. 63-71, https://doi.org/10.2307/3535035.","productDescription":"9 p.","startPage":"63","endPage":"71","numberOfPages":"9","costCenters":[{"id":531,"text":"Patuxent Wildlife Research Center","active":true,"usgs":true}],"links":[{"id":194218,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United States","state":"Oregon, Washington","otherGeospatial":"Columbia Basin, McNary Recreation Area, Umatilla National Wildlife Refuge","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -120.12451171875,\n              45.76943886620391\n            ],\n            [\n              -118.7841796875,\n              45.76943886620391\n            ],\n            [\n              -118.7841796875,\n              46.09609080214316\n            ],\n            [\n              -120.12451171875,\n              46.09609080214316\n            ],\n            [\n              -120.12451171875,\n              45.76943886620391\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","volume":"61","issue":"2","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ad7e4b07f02db684501","contributors":{"authors":[{"text":"Blus, L. J.","contributorId":38116,"corporation":false,"usgs":true,"family":"Blus","given":"L.","middleInitial":"J.","affiliations":[],"preferred":false,"id":334311,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Henny, Charles J.","contributorId":12578,"corporation":false,"usgs":true,"family":"Henny","given":"Charles","email":"","middleInitial":"J.","affiliations":[],"preferred":false,"id":334310,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Kaiser, T. E.","contributorId":75486,"corporation":false,"usgs":true,"family":"Kaiser","given":"T. E.","affiliations":[],"preferred":false,"id":334312,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":5221633,"text":"5221633 - 1980 - Transfer of crude oil from contaminated water to bird eggs","interactions":[],"lastModifiedDate":"2020-02-26T11:23:12","indexId":"5221633","displayToPublicDate":"1980-06-16T12:19:23","publicationYear":"1980","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1561,"text":"Environmental Research","active":true,"publicationSubtype":{"id":10}},"title":"Transfer of crude oil from contaminated water to bird eggs","docAbstract":"Paris of breeding mallard ducks were exposed to oiled water for 2 days during the first week of incubation. Hatching success of ducks exposed to 100 ml of Prudhoe Bay crude oil per square meter of water surface was significantly less than that of controls. Hatching success of ducks exposed to 5 ml of crude oil per square meter of water surface was less than that of controls but the difference was not significant. The presence of oil on the eggs of ducks exposed to oiled water was confirmed by chemical analysis. Thermocouple probes were used to monitor the egg and nest temperatures of some of the ducks in each of the three groups. Incubation temperatures of oiled females were not significantly different from those of the controls. The incubation behavior of females exposed to oiled water and the first-week survival of their ducklings was not affected by the oil.","language":"English","publisher":"ScienceDirect","doi":"10.1016/0013-9351(80)90143-7","usgsCitation":"Albers, P., 1980, Transfer of crude oil from contaminated water to bird eggs: Environmental Research, v. 22, no. 2, p. 307-314, https://doi.org/10.1016/0013-9351(80)90143-7.","productDescription":"8 p.","startPage":"307","endPage":"314","numberOfPages":"8","costCenters":[{"id":531,"text":"Patuxent Wildlife Research Center","active":true,"usgs":true}],"links":[{"id":193433,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"},{"id":18276,"rank":200,"type":{"id":11,"text":"Document"},"url":"https://www.sciencedirect.com/science?_ob=ArticleURL&_udi=B6WDS-4F1YBYG-4W&_user=696292&_handle=V-WA-A-W-WC-MsSAYVW-UUW-U-AACAUEZWUU-AAVYZDDUUU-YEWVBAUZY-WC-U&_fmt=summary&_coverDate=08%2F31%2F1980&_rdoc=5&_orig=browse&_srch=%23toc%236774%231980%23999779997%23544458!&_cdi=6774&view=c&_acct=C000038819&_version=1&_urlVersion=0&_userid=696292&md5=b116a475681e116ec29ed67111623646","linkFileType":{"id":5,"text":"html"}}],"volume":"22","issue":"2","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a4de4b07f02db626d9e","contributors":{"authors":[{"text":"Albers, P.H.","contributorId":26646,"corporation":false,"usgs":true,"family":"Albers","given":"P.H.","email":"","affiliations":[],"preferred":false,"id":334322,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":70120137,"text":"70120137 - 1980 - Behavioral responses of wintering bald eagles to human activity on the Skagit River, Washington","interactions":[],"lastModifiedDate":"2014-08-12T14:02:08","indexId":"70120137","displayToPublicDate":"1980-06-15T14:01:00","publicationYear":"1980","noYear":false,"publicationType":{"id":4,"text":"Book"},"publicationSubtype":{"id":12,"text":"Conference publication"},"title":"Behavioral responses of wintering bald eagles to human activity on the Skagit River, Washington","docAbstract":"No abstract available.","largerWorkTitle":"Proceedings of the Washington Bald Eagle Symposium","conferenceTitle":"Washington Bald Eagle Symposium","conferenceDate":"1980-06-14T00:00:00","conferenceLocation":"Seattle, WA","language":"English","publisher":"The Nature Conservancy","publisherLocation":"Seattle, WA","usgsCitation":"Skagen, S.K., 1980, Behavioral responses of wintering bald eagles to human activity on the Skagit River, Washington, 11 p.","productDescription":"11 p.","numberOfPages":"11","costCenters":[],"links":[{"id":292040,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"53eb2a54e4b0461e447649b5","contributors":{"authors":[{"text":"Skagen, Susan K. 0000-0002-6744-1244 skagens@usgs.gov","orcid":"https://orcid.org/0000-0002-6744-1244","contributorId":2009,"corporation":false,"usgs":true,"family":"Skagen","given":"Susan","email":"skagens@usgs.gov","middleInitial":"K.","affiliations":[{"id":291,"text":"Fort Collins Science Center","active":true,"usgs":true}],"preferred":false,"id":497956,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":70210569,"text":"70210569 - 1980 - Comments and replies on ‘Collision-deformed Paleozoic continental margin, western Brooks Range, Alaska’: Reply","interactions":[],"lastModifiedDate":"2020-06-11T15:31:38.999484","indexId":"70210569","displayToPublicDate":"1980-06-09T13:57:56","publicationYear":"1980","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1796,"text":"Geology","active":true,"publicationSubtype":{"id":10}},"title":"Comments and replies on ‘Collision-deformed Paleozoic continental margin, western Brooks Range, Alaska’: Reply","docAbstract":"<p>No abstract available.</p>","language":"English","publisher":"GSA","doi":"10.1130/0091-7613(1980)8<356:CAROCP>2.0.CO;2","usgsCitation":"Churkin, M., and Nokleberg, W.J., 1980, Comments and replies on ‘Collision-deformed Paleozoic continental margin, western Brooks Range, Alaska’: Reply: Geology, v. 8, no. 8, p. 356-357, https://doi.org/10.1130/0091-7613(1980)8<356:CAROCP>2.0.CO;2.","productDescription":"2 p.","startPage":"356","endPage":"357","costCenters":[{"id":312,"text":"Geology, Minerals, Energy, and Geophysics Science Center","active":true,"usgs":true}],"links":[{"id":375476,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United States","state":"Alaska","otherGeospatial":"Brooks Range","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -159.4775390625,\n              66.53076810915225\n            ],\n            [\n              -149.326171875,\n              66.53076810915225\n            ],\n            [\n              -149.326171875,\n              68.6245436634471\n            ],\n            [\n              -159.4775390625,\n              68.6245436634471\n            ],\n            [\n              -159.4775390625,\n              66.53076810915225\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","volume":"8","issue":"8","noUsgsAuthors":false,"publicationStatus":"PW","contributors":{"authors":[{"text":"Churkin, Michael","contributorId":66677,"corporation":false,"usgs":true,"family":"Churkin","given":"Michael","affiliations":[],"preferred":false,"id":790794,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Nokleberg, Warren J. 0000-0002-1574-8869 wnokleberg@usgs.gov","orcid":"https://orcid.org/0000-0002-1574-8869","contributorId":2077,"corporation":false,"usgs":true,"family":"Nokleberg","given":"Warren","email":"wnokleberg@usgs.gov","middleInitial":"J.","affiliations":[{"id":312,"text":"Geology, Minerals, Energy, and Geophysics Science Center","active":true,"usgs":true}],"preferred":true,"id":790795,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":70157201,"text":"70157201 - 1980 - Main image file tape description","interactions":[],"lastModifiedDate":"2015-10-05T13:28:24","indexId":"70157201","displayToPublicDate":"1980-05-31T19:45:00","publicationYear":"1980","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":6,"text":"USGS Unnumbered Series"},"title":"Main image file tape description","docAbstract":"<p>This Main Image File Tape document defines the data content and file structure of the Main Image File Tape (MIFT) produced by the EROS Data Center (EDC). This document also defines an INQUIRY tape, which is just a subset of the MIFT. The format of the INQUIRY tape is identical to the MIFT except for two records; therefore, with the exception of these two records (described elsewhere in this document), every remark made about the MIFT is true for the INQUIRY tape.</p>","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Reston, VA","doi":"10.3133/70157201","usgsCitation":"Warriner, H.W., 1980, Main image file tape description, iii, 84 p., https://doi.org/10.3133/70157201.","productDescription":"iii, 84 p.","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[{"id":222,"text":"Earth Resources Observation and Science (EROS) Center","active":true,"usgs":true}],"links":[{"id":309508,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/70157201.JPG"},{"id":309507,"rank":1,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/unnumbered/70157201/report.pdf","text":"Report","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"55f7efbae4b05d6c4e4fa97e","contributors":{"authors":[{"text":"Warriner, Howard W.","contributorId":46422,"corporation":false,"usgs":true,"family":"Warriner","given":"Howard","email":"","middleInitial":"W.","affiliations":[],"preferred":false,"id":572244,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":70200638,"text":"70200638 - 1980 - Late Cenozoic volcanism, geochronology, and structure of the Coso Range, Inyo County, California","interactions":[],"lastModifiedDate":"2018-10-25T13:28:00","indexId":"70200638","displayToPublicDate":"1980-05-10T13:27:17","publicationYear":"1980","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":"Late Cenozoic volcanism, geochronology, and structure of the Coso Range, Inyo County, California","docAbstract":"<p><span>The Coso Range lies at the west edge of the Great Basin, adjacent to the southern part of the Sierra Nevada. A basement complex of pre‐Cenozoic plutonic and metamorphic rocks is partly buried by ∼35 km</span><sup>3</sup><span>&nbsp;of late Cenozoic volcanic rocks that were erupted during two periods, as defined by K‐Ar dating: (1) 4.0–2.5 m.y., ∼31 km</span><sup>3</sup><span>&nbsp;of basalt, rhyodacite, dacite, andesite, and rhyolite, in descending order of abundance, and (2) ≤1.1 m.y., nearly equal amounts of basalt and rhyolite, most of the rhyolite being ≤0.3 m.y. old. Vents for the volcanic rocks of the younger period are localized on and near a horst of basement rocks within a concavity defined by the distribution of vents of the older period. The alignment of many vents and the presence of a considerable number of roughly north‐trending normal faults of late Cenozoic age reflect basin and range tectonics dominated by roughly east‐west lithospheric extension. Fumaroles, intermittently active thermal springs, and associated altered rocks occur within and immediately east of the central part of the field of Quaternary rhyolite, in an area characterized by various geophysical anomalies that are evidently related to an active hot‐water geothermal system. This system apparently is heated by a reservoir of silicic magma at ≥8‐km depth, itself produced and sustained through partial melting of crustal rocks by thermal energy contained in mantle‐derived basaltic magma that intrudes the crust in response to lithospheric extension.</span></p>","language":"English","publisher":"American Geophysical Union","doi":"10.1029/JB085iB05p02381","usgsCitation":"Duffield, W.A., Bacon, C.R., and Dalrymple, G.B., 1980, Late Cenozoic volcanism, geochronology, and structure of the Coso Range, Inyo County, California: Journal of Geophysical Research B: Solid Earth, v. 85, no. B5, p. 2381-2404, https://doi.org/10.1029/JB085iB05p02381.","productDescription":"24 p.","startPage":"2381","endPage":"2404","costCenters":[{"id":617,"text":"Volcano Science Center","active":true,"usgs":true}],"links":[{"id":358822,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United States","state":"California","county":"Inyo","otherGeospatial":"Coso Range","volume":"85","issue":"B5","noUsgsAuthors":false,"publicationDate":"2012-09-20","publicationStatus":"PW","contributors":{"authors":[{"text":"Duffield, Wendell A.","contributorId":14363,"corporation":false,"usgs":true,"family":"Duffield","given":"Wendell","email":"","middleInitial":"A.","affiliations":[],"preferred":false,"id":749798,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Bacon, Charles R. 0000-0002-2165-5618 cbacon@usgs.gov","orcid":"https://orcid.org/0000-0002-2165-5618","contributorId":2909,"corporation":false,"usgs":true,"family":"Bacon","given":"Charles","email":"cbacon@usgs.gov","middleInitial":"R.","affiliations":[{"id":617,"text":"Volcano Science Center","active":true,"usgs":true}],"preferred":true,"id":749799,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Dalrymple, G. Brent","contributorId":54564,"corporation":false,"usgs":true,"family":"Dalrymple","given":"G.","email":"","middleInitial":"Brent","affiliations":[],"preferred":false,"id":749800,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":70209873,"text":"70209873 - 1980 - Stability of sulfur slopes on Io","interactions":[],"lastModifiedDate":"2020-05-01T19:50:46.725727","indexId":"70209873","displayToPublicDate":"1980-05-01T14:48:26","publicationYear":"1980","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1963,"text":"Icarus","active":true,"publicationSubtype":{"id":10}},"title":"Stability of sulfur slopes on Io","docAbstract":"<p><span>The mechanical properties of elemental sulfur are such that the upper crust of Io cannot be primarily sulfur. For heat flows in the range 100–1000 ergs cm</span><sup>−2</sup><span>, sec</span><sup>−1</sup><span>, sulfur becomes ductile within several hundred meters of the surface and would prevent the formation of calderas with depths greater than this. However, the one caldera for which precise depth data are available is 2 km deep, and this value may be typical. A study of the mechanical equilibrium of simple slopes shows that the depth to the zone of rapid ductile flow strongly controls the maximum heights for sulfur slopes. Sulfur scarps with heights greater than 1 km will fail for all heat flows greater than 180 ergs cm</span><sup>−2</sup><span>&nbsp;sec</span><sup>−1</sup><span>&nbsp;and slope angles greater than 22.5°. The observed relief on Io is inconsistent with that anticipated for a predominantly sulfur crust. However, a silicate crust with several percent sulfur included satisfies both the mechanical constraints and the observed presence of sulfur on Io.</span></p>","language":"English","publisher":"Elsevier","doi":"10.1016/0019-1035(80)90022-6","usgsCitation":"Clow, G.D., and Carr, M.H., 1980, Stability of sulfur slopes on Io: Icarus, v. 44, no. 2, p. 268-279, https://doi.org/10.1016/0019-1035(80)90022-6.","productDescription":"12 p.","startPage":"268","endPage":"279","costCenters":[{"id":131,"text":"Astrogeology Science Center","active":true,"usgs":true},{"id":318,"text":"Geosciences and Environmental Change Science Center","active":true,"usgs":true}],"links":[{"id":374438,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"44","issue":"2","noUsgsAuthors":false,"publicationStatus":"PW","contributors":{"authors":[{"text":"Clow, Gary D. 0000-0002-2262-3853 clow@usgs.gov","orcid":"https://orcid.org/0000-0002-2262-3853","contributorId":2066,"corporation":false,"usgs":true,"family":"Clow","given":"Gary","email":"clow@usgs.gov","middleInitial":"D.","affiliations":[{"id":318,"text":"Geosciences and Environmental Change Science Center","active":true,"usgs":true}],"preferred":true,"id":788355,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Carr, M. H.","contributorId":84727,"corporation":false,"usgs":true,"family":"Carr","given":"M.","email":"","middleInitial":"H.","affiliations":[{"id":131,"text":"Astrogeology Science Center","active":true,"usgs":true}],"preferred":false,"id":788356,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":70006696,"text":"70006696 - 1980 - Re-evaluation of dietary riboflavin requirement of rainbow trout (Salmo gairdneri)","interactions":[],"lastModifiedDate":"2012-09-06T01:02:24","indexId":"70006696","displayToPublicDate":"1980-05-01T11:25:00","publicationYear":"1980","noYear":false,"publicationType":{"id":21,"text":"Thesis"},"publicationSubtype":{"id":28,"text":"Thesis"},"title":"Re-evaluation of dietary riboflavin requirement of rainbow trout (Salmo gairdneri)","docAbstract":"No abstract available at this time","language":"English","publisher":"Cornell University","publisherLocation":"Ithaca, NY","collaboration":"Submitted for a Master's of Science","usgsCitation":"Hughes, S.G., 1980, Re-evaluation of dietary riboflavin requirement of rainbow trout (Salmo gairdneri), ix, 82 p.","productDescription":"ix, 82 p.","costCenters":[{"id":365,"text":"Leetown Science Center","active":true,"usgs":true}],"links":[{"id":260188,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"505a9572e4b0c8380cd81a09","contributors":{"authors":[{"text":"Hughes, Steven Gerard","contributorId":98990,"corporation":false,"usgs":true,"family":"Hughes","given":"Steven","email":"","middleInitial":"Gerard","affiliations":[],"preferred":false,"id":355039,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":70231349,"text":"70231349 - 1980 - Environmental stratification — A method to improve Landsat digital analysis accuracy and land cover map utility","interactions":[],"lastModifiedDate":"2022-05-06T14:46:46.733007","indexId":"70231349","displayToPublicDate":"1980-05-01T09:42:29","publicationYear":"1980","noYear":false,"publicationType":{"id":24,"text":"Conference Paper"},"publicationSubtype":{"id":19,"text":"Conference Paper"},"title":"Environmental stratification — A method to improve Landsat digital analysis accuracy and land cover map utility","docAbstract":"<p>No abstract available.</p>","largerWorkType":{"id":4,"text":"Book"},"largerWorkTitle":"Proceedings of the 14th International Symposium on Remote Sensing of the Environment","largerWorkSubtype":{"id":12,"text":"Conference publication"},"conferenceTitle":"14th International Symposium on Remote Sensing of the Environment","conferenceDate":"April 23-30, 1980","conferenceLocation":"San José, Costa Rica","language":"English","publisher":"University of Michigan","usgsCitation":"Pettinger, L.R., 1980, Environmental stratification — A method to improve Landsat digital analysis accuracy and land cover map utility, <i>in</i> Proceedings of the 14th International Symposium on Remote Sensing of the Environment, v. 3, San José, Costa Rica, April 23-30, 1980, p. 1587-1599.","productDescription":"13 p.","startPage":"1587","endPage":"1599","costCenters":[{"id":222,"text":"Earth Resources Observation and Science (EROS) Center","active":true,"usgs":true}],"links":[{"id":400288,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"},{"id":400287,"rank":1,"type":{"id":15,"text":"Index Page"},"url":"https://symposia.org/past_symposia.htm"}],"volume":"3","noUsgsAuthors":false,"publicationStatus":"PW","contributors":{"authors":[{"text":"Pettinger, L. R.","contributorId":85949,"corporation":false,"usgs":true,"family":"Pettinger","given":"L.","email":"","middleInitial":"R.","affiliations":[],"preferred":false,"id":842357,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":70231348,"text":"70231348 - 1980 - Opportunities in remote sensing training for the international scientific community","interactions":[],"lastModifiedDate":"2022-05-06T14:40:57.249965","indexId":"70231348","displayToPublicDate":"1980-05-01T09:34:40","publicationYear":"1980","noYear":false,"publicationType":{"id":24,"text":"Conference Paper"},"publicationSubtype":{"id":19,"text":"Conference Paper"},"title":"Opportunities in remote sensing training for the international scientific community","docAbstract":"<p>No abstract available.</p>","largerWorkType":{"id":4,"text":"Book"},"largerWorkTitle":"Proceedings of the 14th International Symposium on Remote Sensing of Environment","largerWorkSubtype":{"id":12,"text":"Conference publication"},"conferenceTitle":"14th International Symposium on Remote Sensing of Environment","conferenceDate":"April 23-30, 1980","conferenceLocation":"San José, Costa Rica","language":"English","publisher":"University of Michigan","usgsCitation":"Draeger, W., 1980, Opportunities in remote sensing training for the international scientific community, <i>in</i> Proceedings of the 14th International Symposium on Remote Sensing of Environment, v. 1, San José, Costa Rica, April 23-30, 1980, p. 243-247.","productDescription":"5 p.","startPage":"243","endPage":"247","costCenters":[{"id":222,"text":"Earth Resources Observation and Science (EROS) Center","active":true,"usgs":true}],"links":[{"id":400286,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"},{"id":400285,"rank":1,"type":{"id":15,"text":"Index Page"},"url":"https://symposia.org/past_symposia.htm"}],"volume":"1","noUsgsAuthors":false,"publicationStatus":"PW","contributors":{"authors":[{"text":"Draeger, W. C.","contributorId":67231,"corporation":false,"usgs":true,"family":"Draeger","given":"W. C.","affiliations":[],"preferred":false,"id":842356,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":70012433,"text":"70012433 - 1980 - Sediment transport in Norton Sound, Alaska","interactions":[],"lastModifiedDate":"2024-10-11T15:35:55.48006","indexId":"70012433","displayToPublicDate":"1980-05-01T00:00:00","publicationYear":"1980","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":2667,"text":"Marine Geology","active":true,"publicationSubtype":{"id":10}},"title":"Sediment transport in Norton Sound, Alaska","docAbstract":"<p>The Yukon River, the largest single source of Bering Sea sediment, delivers &gt; 95% of its sediment load at the southwest comer of Norton Sound during the ice-free months of late May through October. During this period, surface winds in the northern Bering Sea area are generally light from the south and southwest, and surface waves are not significant. Although wind stress may cause some transport of low-density turbid surface water into the head of Norton Sound, the most significant transport of Yukon River suspended matter occurs within advective currents flowing north across the outer part of the sound. The thickest accumulations of modern Yukon silt and very fine sand occur beneath this persistent current.</p><p><span>We monitored temporal variations in bottom currents, pressure, and suspended-matter concentrations within this major transport pathway for 80 days in the summer of 1977 using a Geological Processes Bottom Environmental (GEOPROBE) tripod system. The record reveals two distinctive periods of bottom flow and sediment transport: an initial 59 days (July 8–September 5) of fair-weather conditions, characterized by tidally dominated currents and relatively low, stable suspended-matter concentrations; and a 21-day period (September 5–September 26) during which several storms traversed the northern Bering Sea, mean suspended-matter concentrations near the bottom increased by a factor of five, and the earlier tidal dominance was overshadowed by wind-driven and oscillatory wave-generated currents.</span></p><p><span>Friction velocities (u<sub>*</sub>) at the GEOPROBE site were generally subcritical during the initial fair-weather period. In contrast, the 21-day stormy period was characterized by uFriction velocities (u<sub>*</sub>) at the GEOPROBE site were generally subcritical during the initial fair-weather period. In contrast, the 21-day stormy period was characterized by u<sub>*</sub>values that exceeded the critical level of 1.3 cm/s more than 60% of the time. The GEOPROBE data suggest that the very fine sand constituting about 50% of the sediment on the outer part of the Yukon prodelta is transported during a few late-summer and fall storms each year. A conservative estimate shows that suspended-matter transport during the storms in September 1977 was equal to four months of fair-weather transport.  values that exceeded the critical level of 1.3 cm/s more than 60% of the time. The GEOPROBE data suggest that the very fine sand constituting about 50% of the sediment on the outer part of the Yukon prodelta is transported during a few late-summer and fall storms each year. A conservative estimate shows that suspended-matter transport during the storms in September 1977 was equal to four months of fair-weather transport. </span></p>","language":"English","publisher":"Elsevier","doi":"10.1016/0025-3227(80)90043-2","usgsCitation":"Drake, D., Cacchione, D., Muench, R., and Nelson, C., 1980, Sediment transport in Norton Sound, Alaska: Marine Geology, v. 36, no. 1-2, p. 97-126, https://doi.org/10.1016/0025-3227(80)90043-2.","productDescription":"30 p.","startPage":"97","endPage":"126","costCenters":[],"links":[{"id":222201,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United States","state":"Alaska","otherGeospatial":"Norton Sound","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"coordinates\": [\n          [\n            [\n              -166.93816207810704,\n              65.1847517876121\n            ],\n            [\n              -166.93816207810704,\n              62.997485781439735\n            ],\n            [\n              -160.32671205235334,\n              62.997485781439735\n            ],\n            [\n              -160.32671205235334,\n              65.1847517876121\n            ],\n            [\n              -166.93816207810704,\n              65.1847517876121\n            ]\n          ]\n        ],\n        \"type\": \"Polygon\"\n      }\n    }\n  ]\n}","volume":"36","issue":"1-2","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"505b89d9e4b08c986b316ee5","contributors":{"authors":[{"text":"Drake, D.E.","contributorId":48150,"corporation":false,"usgs":true,"family":"Drake","given":"D.E.","email":"","affiliations":[],"preferred":false,"id":363567,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Cacchione, D.A.","contributorId":65448,"corporation":false,"usgs":true,"family":"Cacchione","given":"D.A.","affiliations":[{"id":520,"text":"Pacific Coastal and Marine Science Center","active":true,"usgs":true}],"preferred":false,"id":363568,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Muench, R.D.","contributorId":83270,"corporation":false,"usgs":true,"family":"Muench","given":"R.D.","email":"","affiliations":[],"preferred":false,"id":363569,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Nelson, C.H.","contributorId":88346,"corporation":false,"usgs":true,"family":"Nelson","given":"C.H.","email":"","affiliations":[],"preferred":false,"id":363570,"contributorType":{"id":1,"text":"Authors"},"rank":4}]}}
,{"id":70209771,"text":"70209771 - 1980 - Allochthonous Jurassic ophiolite in northwest Washington","interactions":[],"lastModifiedDate":"2020-04-24T19:36:33.816797","indexId":"70209771","displayToPublicDate":"1980-04-24T14:26:00","publicationYear":"1980","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1723,"text":"GSA Bulletin","active":true,"publicationSubtype":{"id":10}},"title":"Allochthonous Jurassic ophiolite in northwest Washington","docAbstract":"<p>Fragments of Jurassic ophiolite having U-Pb zircon ages narrowly grouped at 160 to 170 m.y. are widespread over parts of northwest Washington. The Haystack thrust fault is inferred to mark the base of the ophiolite in the San Juan Islands and adjacent Cascade foothills; other bodies of mafic and ultramafic rock in the western Cascades may be klippen of the Haystack thrust plate. The Haystack thrust fault is probably the structurally highest and possibly most extensive thrust yet recognized within a family of Late Cretaceous thrust faults in northwest Washington.</p><p>The ophiolite and its time of emplacement (bracketed between about 100 and 88 m.y.) suggest a similarity with the Coast Range thrust of California which thrust Upper Jurassic ophiolite and the Great Valley sedimentary sequence over the Franciscan assemblage. However, relations in the Cascades are complicated by the extraordinarily diverse character of lower plate rocks, of which very few resemble the Franciscan. We conclude that an original subduction system was modified by later tectonic activity so that a variety of terranes was juxtaposed as a family of rootless thrusts, with the ophiolite forming, at least in some areas, the uppermost structural unit. Perhaps the emplacement of Wrangellia, an allochthonous microcontinent west of the San Juan Islands, caused the thrusting.</p>","language":"English","publisher":"GSA","doi":"10.1130/0016-7606(1980)91<359:AJOINW>2.0.CO;2","usgsCitation":"Whetten, J.T., Zartman, R., Blakely, R.J., and Jones, D.L., 1980, Allochthonous Jurassic ophiolite in northwest Washington: GSA Bulletin, v. 91, no. 6, p. 359-368, https://doi.org/10.1130/0016-7606(1980)91<359:AJOINW>2.0.CO;2.","productDescription":"10 p.","startPage":"359","endPage":"368","costCenters":[{"id":312,"text":"Geology, Minerals, Energy, and Geophysics Science Center","active":true,"usgs":true}],"links":[{"id":374270,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United States","state":"Washington","otherGeospatial":"Northwest Washington","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -123.53027343749999,\n              48.100094697973795\n            ],\n            [\n              -121.871337890625,\n              48.100094697973795\n            ],\n            [\n              -121.871337890625,\n              48.90083790234091\n            ],\n            [\n              -123.53027343749999,\n              48.90083790234091\n            ],\n            [\n              -123.53027343749999,\n              48.100094697973795\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","volume":"91","issue":"6","noUsgsAuthors":false,"publicationStatus":"PW","contributors":{"authors":[{"text":"Whetten, John T.","contributorId":102444,"corporation":false,"usgs":true,"family":"Whetten","given":"John","email":"","middleInitial":"T.","affiliations":[],"preferred":false,"id":787941,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Zartman, R. E.","contributorId":15632,"corporation":false,"usgs":true,"family":"Zartman","given":"R. E.","affiliations":[],"preferred":false,"id":787942,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Blakely, Richard J. 0000-0003-1701-5236 blakely@usgs.gov","orcid":"https://orcid.org/0000-0003-1701-5236","contributorId":1540,"corporation":false,"usgs":true,"family":"Blakely","given":"Richard","email":"blakely@usgs.gov","middleInitial":"J.","affiliations":[{"id":662,"text":"Western Mineral and Environmental Resources Science Center","active":true,"usgs":true},{"id":312,"text":"Geology, Minerals, Energy, and Geophysics Science Center","active":true,"usgs":true}],"preferred":true,"id":787943,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Jones, David L.","contributorId":61925,"corporation":false,"usgs":true,"family":"Jones","given":"David","email":"","middleInitial":"L.","affiliations":[],"preferred":false,"id":787944,"contributorType":{"id":1,"text":"Authors"},"rank":4}]}}
,{"id":70112924,"text":"70112924 - 1980 - Need for new sensors to map lithologic units","interactions":[],"lastModifiedDate":"2014-06-18T12:32:41","indexId":"70112924","displayToPublicDate":"1980-04-17T12:14:02","publicationYear":"1980","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":3393,"text":"Sixth Annual Pecora Symposium and Exposition","active":true,"publicationSubtype":{"id":10}},"title":"Need for new sensors to map lithologic units","docAbstract":"<p>One of the most important contributions that remote sensing can make to mineral energy explorations to provide data from satellites to augment regional geological mapping.  Geologic maps, which show information on the subsurface, are the main basis for formulating models of resource genesis that guide exploration.  However, conventional compilation procedures are time-consuming and therefore often slow the pace of exploration, especially in large, inaccessible areas.  Landsat Multispectral Scanner (MSS) images have been applied to a wide variety of specific geological problems, including discrimination of lithologic and delineation of previously unrecognized tectonic features.  However, these lithologic distinctions are based on brightness, spectral reflectance, and, less commonly, the morphology of the unit, which in the wavelength region of MSS images are only rarely diagnostic of specific mineralogical content.  Limonite is the only lithological material that can be identified be analyzing MSS spectral radiance.</p>","largerWorkType":{"id":2,"text":"Article"},"largerWorkTitle":"Sixth Annual Pecora Symposium and Exposition","largerWorkSubtype":{"id":10,"text":"Journal Article"},"language":"English","publisher":"Society of Exploration Geophysicists","publisherLocation":"Tulsa, OK","usgsCitation":"Rowan, L.C., 1980, Need for new sensors to map lithologic units: Sixth Annual Pecora Symposium and Exposition, p. 106-107.","productDescription":"2 p.","startPage":"106","endPage":"107","numberOfPages":"2","costCenters":[],"links":[{"id":288806,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"53ae7783e4b0abf75cf2c164","contributors":{"editors":[{"text":"Barringer, Anthony R.","contributorId":112053,"corporation":false,"usgs":true,"family":"Barringer","given":"Anthony","email":"","middleInitial":"R.","affiliations":[],"preferred":false,"id":509905,"contributorType":{"id":2,"text":"Editors"},"rank":1}],"authors":[{"text":"Rowan, Lawrence C.","contributorId":58629,"corporation":false,"usgs":true,"family":"Rowan","given":"Lawrence","email":"","middleInitial":"C.","affiliations":[],"preferred":false,"id":494945,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":70112923,"text":"70112923 - 1980 - Detection and modeling of subsurface coal oxidation","interactions":[],"lastModifiedDate":"2014-06-18T12:13:03","indexId":"70112923","displayToPublicDate":"1980-04-16T12:07:48","publicationYear":"1980","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":3393,"text":"Sixth Annual Pecora Symposium and Exposition","active":true,"publicationSubtype":{"id":10}},"title":"Detection and modeling of subsurface coal oxidation","docAbstract":"<p>The oxidation and sustained ignition of coal and coaly wastes within surface coal mine spoils in the southwestern U.S. have hampered the success of reclamation efforts at these locations.  To assess better the magnitude, depth, geometry, and dynamics of the oxidation process thermal infrared remote sensing data have been used.  Digital thermal imagery was found to be useful for this purpose and was integrated with finite different heat transfer models to yield predictions of several characteristics of the thermal source.  In addition to thermal infrared imagery, aerial color and false color infrared imagery were found to provide useful information for the interpretation of oxidation phenomena by means of variations in surface vegetation, color of the surface material, subsidence, etc.  The combined use of thermal infrared imagery and thermal modeling techniques are well suited for use in exploration and interpretation of other thermal targets.</p>","largerWorkType":{"id":2,"text":"Article"},"largerWorkTitle":"Sixth Annual Pecora Symposium and Exposition","largerWorkSubtype":{"id":10,"text":"Journal Article"},"language":"English","publisher":"Society of Exploration Geophysicists","publisherLocation":"Tulsa, OK","usgsCitation":"Leonhart, L.S., and Rasmussen, W.O., 1980, Detection and modeling of subsurface coal oxidation: Sixth Annual Pecora Symposium and Exposition, p. 83-83.","productDescription":"1 p.","startPage":"83","endPage":"83","numberOfPages":"1","costCenters":[],"links":[{"id":288805,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"53ae7680e4b0abf75cf2bf72","contributors":{"editors":[{"text":"Barringer, Anthony R.","contributorId":112053,"corporation":false,"usgs":true,"family":"Barringer","given":"Anthony","email":"","middleInitial":"R.","affiliations":[],"preferred":false,"id":509904,"contributorType":{"id":2,"text":"Editors"},"rank":1}],"authors":[{"text":"Leonhart, Leo S.","contributorId":77050,"corporation":false,"usgs":true,"family":"Leonhart","given":"Leo","email":"","middleInitial":"S.","affiliations":[],"preferred":false,"id":494944,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Rasmussen, William O.","contributorId":6376,"corporation":false,"usgs":true,"family":"Rasmussen","given":"William","email":"","middleInitial":"O.","affiliations":[],"preferred":false,"id":494943,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":70112914,"text":"70112914 - 1980 - Integration of geological, geochemical, and geophysical spatial data of the Cement oil field, Oklahoma, test site","interactions":[],"lastModifiedDate":"2014-06-18T11:34:49","indexId":"70112914","displayToPublicDate":"1980-04-16T11:29:37","publicationYear":"1980","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":3393,"text":"Sixth Annual Pecora Symposium and Exposition","active":true,"publicationSubtype":{"id":10}},"title":"Integration of geological, geochemical, and geophysical spatial data of the Cement oil field, Oklahoma, test site","docAbstract":"<p>Measurement pertaining to geology, geochemistry, and geophysics of the Cement oil field, Oklahoma, test site were collected employing both airborne sensors and ground-based data collection. The measurements include: (1) airborne gamma-ray spectrometry (supplying bismuth 214, thalium 208, and potassium 40 gamma-ray intensities); (2) aeromagnetic survey data; (3) multi-frequency airborne resistivity survey data (supplying apparent electrical resistivity of near surface materials); (4) gravity data; (5) geological and topographic maps; and (6) image data from Landsat MSS and U-2 photography.</p>","largerWorkType":{"id":2,"text":"Article"},"largerWorkTitle":"Sixth Annual Pecora Symposium and Exposition","largerWorkSubtype":{"id":10,"text":"Journal Article"},"language":"English","publisher":"Society of Exploration Geophysicists","publisherLocation":"Tulsa, OK","usgsCitation":"Termain, P.A., Donovan, T.J., and Chavez, P.S., 1980, Integration of geological, geochemical, and geophysical spatial data of the Cement oil field, Oklahoma, test site: Sixth Annual Pecora Symposium and Exposition, p. 57-57.","productDescription":"1 p.","startPage":"57","endPage":"57","numberOfPages":"1","costCenters":[],"links":[{"id":288797,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United States","state":"Oklahoma","otherGeospatial":"Cement Oil Field","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -95.9512937,36.034963 ], [ -95.9512937,36.0350408 ], [ -95.9512492,36.0350408 ], [ -95.9512492,36.034963 ], [ -95.9512937,36.034963 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"53ae7750e4b0abf75cf2c0f2","contributors":{"editors":[{"text":"Barringer, Anthony R.","contributorId":112053,"corporation":false,"usgs":true,"family":"Barringer","given":"Anthony","email":"","middleInitial":"R.","affiliations":[],"preferred":false,"id":509901,"contributorType":{"id":2,"text":"Editors"},"rank":1}],"authors":[{"text":"Termain, Patricia A.","contributorId":12852,"corporation":false,"usgs":true,"family":"Termain","given":"Patricia","email":"","middleInitial":"A.","affiliations":[],"preferred":false,"id":494914,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Donovan, Terrence J.","contributorId":71529,"corporation":false,"usgs":true,"family":"Donovan","given":"Terrence","email":"","middleInitial":"J.","affiliations":[],"preferred":false,"id":494915,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Chavez, Pat S.","contributorId":82308,"corporation":false,"usgs":true,"family":"Chavez","given":"Pat","email":"","middleInitial":"S.","affiliations":[],"preferred":false,"id":494916,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":70112911,"text":"70112911 - 1980 - Considerations for blending data from various sensors","interactions":[],"lastModifiedDate":"2014-06-18T11:26:44","indexId":"70112911","displayToPublicDate":"1980-04-16T10:58:00","publicationYear":"1980","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":3393,"text":"Sixth Annual Pecora Symposium and Exposition","active":true,"publicationSubtype":{"id":10}},"title":"Considerations for blending data from various sensors","docAbstract":"<p>A project is being proposed at the EROS Data Center to blend the information from sensors aboard various satellites.  The problems of, and considerations for, blending data from several satellite-borne sensors are discussed.  System descriptions of the sensors aboard the HCMM, TIROS-N, GOES-D, Landsat 3, Landsat D, Seasat, SPOT, Stereosat, and NOSS satellites, and the quantity, quality, image dimensions, and availability of these data are summaries to define attributes of a multi-sensor satellite data base.</p>\n<br/>\n<p>Unique configurations of equipment, storage, media, and specialized hardware to meet the data system requirement are described as well as archival media and improved sensors that will be on-line within the next 5 years.  Definitions and rigor required for blending various sensor data are given.  Problems of merging data from the same sensor (intrasensor comparison) and from different sensors (intersensor comparison), the characteristics and advantages of cross-calibration of data, and integration of data into a product matrix field are addressed.  Data processing considerations as affected by formation, resolution, and problems of merging large data sets, and organization of data bases for blending data are presented.  Examples utilizing GOES and Landsat data are presented to demonstrate techniques of data blending, and recommendations for future implementation of a set of standard scenes and their characteristics necessary for optimal data blending are discussed.</p>","largerWorkType":{"id":2,"text":"Article"},"largerWorkTitle":"Sixth Annual Pecora Symposium and Exposition","largerWorkSubtype":{"id":10,"text":"Journal Article"},"language":"English","publisher":"Society of Exploration Geophysicists","publisherLocation":"Tulsa, OK","usgsCitation":"Bauer, B.P., 1980, Considerations for blending data from various sensors: Sixth Annual Pecora Symposium and Exposition, p. 56-56.","productDescription":"1 p.","startPage":"56","endPage":"56","numberOfPages":"1","costCenters":[],"links":[{"id":288796,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"53ae7660e4b0abf75cf2bf50","contributors":{"editors":[{"text":"Barringer, Anthony R.","contributorId":112053,"corporation":false,"usgs":true,"family":"Barringer","given":"Anthony","email":"","middleInitial":"R.","affiliations":[],"preferred":false,"id":509900,"contributorType":{"id":2,"text":"Editors"},"rank":1}],"authors":[{"text":"Bauer, Brian P.","contributorId":58946,"corporation":false,"usgs":true,"family":"Bauer","given":"Brian","email":"","middleInitial":"P.","affiliations":[],"preferred":false,"id":494912,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":70112909,"text":"70112909 - 1980 - Interpretation of long- and short-wavelength magnetic anomalies","interactions":[],"lastModifiedDate":"2014-06-18T10:57:11","indexId":"70112909","displayToPublicDate":"1980-04-15T10:40:00","publicationYear":"1980","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":3393,"text":"Sixth Annual Pecora Symposium and Exposition","active":true,"publicationSubtype":{"id":10}},"title":"Interpretation of long- and short-wavelength magnetic anomalies","docAbstract":"<p>Magset was launched on October 30, 1979.  More than a decade of examining existing data, devising appropriate models of the global magnetic field, and extending methods for interpreting long-wavelength magnetic anomalies preceded this launch</p>\n<br/>\n<p>Magnetic data collected by satellite can be interrupted by using a method of analysis that quantitively describes the magnetic field resulting from three-dimensional geologic structures that are bounded by an arbitrary number of polygonal faces,  Each face my have any orientation and three or more sides.  At each point of the external field, the component normal to each face is obtained by using an expression for the solid angle subtended by a generalized polygon.  The \"cross\" of tangential components are relatively easy to obtain for the same polygons.</p>\n<br/>\n<p>No approximations have been made related to orbit height that restrict the dimensions of the polygons relative to the distance from the external field points.  This permits the method to be used to model shorter wavelength anomalies obtained from aircraft or ground surveys.</p>\n<br/>\n<p>The magnetic fields for all the structures considered are determine in the same rectangular coordinate system.  The coordinate system is in depended from the orientation of geologic trends and permits multiple structures or bodies to be included in the same magnetic field calculations.  This single reference system also simplified adjustments in position and direction to account for earth curvature in regional interpretation.</p>","largerWorkType":{"id":2,"text":"Article"},"largerWorkTitle":"Sixth Annual Pecora Symposium and Exposition","largerWorkSubtype":{"id":10,"text":"Journal Article"},"language":"English","publisher":"Society of Exploration Geophysicists","publisherLocation":"Tulsa, OK","usgsCitation":"DeNoyer, J.M., 1980, Interpretation of long- and short-wavelength magnetic anomalies: Sixth Annual Pecora Symposium and Exposition, p. 51-51.","productDescription":"1 p.","startPage":"51","endPage":"51","numberOfPages":"1","costCenters":[],"links":[{"id":288790,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"53ae7753e4b0abf75cf2c0f9","contributors":{"editors":[{"text":"Barringer, Anthony R.","contributorId":112053,"corporation":false,"usgs":true,"family":"Barringer","given":"Anthony","email":"","middleInitial":"R.","affiliations":[],"preferred":false,"id":509899,"contributorType":{"id":2,"text":"Editors"},"rank":1}],"authors":[{"text":"DeNoyer, John M.","contributorId":96271,"corporation":false,"usgs":true,"family":"DeNoyer","given":"John","email":"","middleInitial":"M.","affiliations":[],"preferred":false,"id":494911,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":70112908,"text":"70112908 - 1980 - Digital mapping of limonitic rocks by using Landsat MSS radio data","interactions":[],"lastModifiedDate":"2014-06-18T10:38:09","indexId":"70112908","displayToPublicDate":"1980-04-15T10:30:00","publicationYear":"1980","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":3393,"text":"Sixth Annual Pecora Symposium and Exposition","active":true,"publicationSubtype":{"id":10}},"title":"Digital mapping of limonitic rocks by using Landsat MSS radio data","docAbstract":"<p>Color-ratio composite images of Landsat MSS (multi-spectral scanner) bands have been used by other workers to map the distribution of limonitic rocks in semi-arid and arid areas as possible indicators of hydrothermal alteration (Rowan et al, 1974).  The images are particularly useful for broad overviews, but detailed analysis at large scales requires both numerical analysis of the ratio values to distinguish consistently among categories of limonitic rocks and a precise transfer of the data to large-scale base maps.  Both requirements can be met by digital classification followed by a precise geometric registration of the classified data.</p>","largerWorkType":{"id":2,"text":"Article"},"largerWorkTitle":"Sixth Annual Pecora Symposium and Exposition","largerWorkSubtype":{"id":10,"text":"Journal Article"},"language":"English","publisher":"Society of Exploration Geophysicists","publisherLocation":"Tulsa, OK","usgsCitation":"Podwysocki, M.H., Segal, D.B., and Simpson, S., 1980, Digital mapping of limonitic rocks by using Landsat MSS radio data: Sixth Annual Pecora Symposium and Exposition, p. 49-51.","productDescription":"3 p.","startPage":"49","endPage":"51","numberOfPages":"3","costCenters":[],"links":[{"id":288779,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"53ae7683e4b0abf75cf2bf7f","contributors":{"editors":[{"text":"Barringer, Anthony R.","contributorId":112053,"corporation":false,"usgs":true,"family":"Barringer","given":"Anthony","email":"","middleInitial":"R.","affiliations":[],"preferred":false,"id":509898,"contributorType":{"id":2,"text":"Editors"},"rank":1}],"authors":[{"text":"Podwysocki, Melvin H.","contributorId":60220,"corporation":false,"usgs":true,"family":"Podwysocki","given":"Melvin","email":"","middleInitial":"H.","affiliations":[],"preferred":false,"id":494910,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Segal, Donald B.","contributorId":40223,"corporation":false,"usgs":true,"family":"Segal","given":"Donald","email":"","middleInitial":"B.","affiliations":[],"preferred":false,"id":494908,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Simpson, Shirley","contributorId":48100,"corporation":false,"usgs":true,"family":"Simpson","given":"Shirley","affiliations":[],"preferred":false,"id":494909,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":70112904,"text":"70112904 - 1980 - Airborne Fraunhofer line discriminator (FLD) luminescence imaging systems and its application to exploration problems","interactions":[],"lastModifiedDate":"2014-06-18T10:19:16","indexId":"70112904","displayToPublicDate":"1980-04-15T09:39:00","publicationYear":"1980","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":3393,"text":"Sixth Annual Pecora Symposium and Exposition","active":true,"publicationSubtype":{"id":10}},"title":"Airborne Fraunhofer line discriminator (FLD) luminescence imaging systems and its application to exploration problems","docAbstract":"<p>Experiments with an imaging airborne Fraunhofer line discriminator (FLD) are being conducted to establish the feasibility of delineating the areal extent of luminescent materials on the earth's surface from aircraft and spacecraft.  All luminescence measurements are related to a standard set of conditions with rhodamine wt dye used as a reference standard.  The FLD has a minimum detectable rhodamine wt concentration of 0.1 parts per billion (ppb) at a signal-to-noise ratio of 5.0.  Luminescence, when expressed in a signal-to-noise ratio (R) is related to equivalent ppb rhodamine wt through the relationship ppb=(0.1R-0.4).  Luminescent materials imaged from an aircraft altitude of approximately 2400 m above terrain include fluorite in association with molybdenum, Pinenut Mountains, Nevada (R=62.0); mineralized playas, Claunch, New Mexico (R=960.0); uranium and vanadium-bearing outcrops, Big Indian Valley, Utah (R=105.0); uranophane sandstones, Sandia Mountains, New Mexico (R=60.0); phosphate outcrops, Pine Mountain, California (R=76.0); and marine oil slicks, Santa Barbara Channel, California (R=24.0).  Correlation between the amount of fluorite in the rocks and soils of the Pinenut Mountains and luminescence, measured by the FLD, is as high as 0.88 at the 95 percent confidence level.</p>","largerWorkType":{"id":2,"text":"Article"},"largerWorkTitle":"Sixth Annual Pecora Symposium and Exposition","largerWorkSubtype":{"id":10,"text":"Journal Article"},"language":"English","publisher":"Society of Exploration Geophysicists","publisherLocation":"Tulsa, OK","usgsCitation":"Watson, R.D., Theisen, A.F., and Hemphill, W.R., 1980, Airborne Fraunhofer line discriminator (FLD) luminescence imaging systems and its application to exploration problems: Sixth Annual Pecora Symposium and Exposition, p. 40-42.","productDescription":"3 p.","startPage":"40","endPage":"42","numberOfPages":"3","costCenters":[],"links":[{"id":288766,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"53ae7622e4b0abf75cf2be9b","contributors":{"editors":[{"text":"Barringer, Anthony R.","contributorId":112053,"corporation":false,"usgs":true,"family":"Barringer","given":"Anthony","email":"","middleInitial":"R.","affiliations":[],"preferred":false,"id":509897,"contributorType":{"id":2,"text":"Editors"},"rank":1}],"authors":[{"text":"Watson, Robert D.","contributorId":62605,"corporation":false,"usgs":true,"family":"Watson","given":"Robert","email":"","middleInitial":"D.","affiliations":[{"id":223,"text":"Earth Resources Observation and Science (EROS) Center (Geography)","active":false,"usgs":true}],"preferred":false,"id":494902,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Theisen, Arnold F.","contributorId":12052,"corporation":false,"usgs":true,"family":"Theisen","given":"Arnold","email":"","middleInitial":"F.","affiliations":[{"id":223,"text":"Earth Resources Observation and Science (EROS) Center (Geography)","active":false,"usgs":true}],"preferred":false,"id":494900,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Hemphill, William R.","contributorId":21970,"corporation":false,"usgs":true,"family":"Hemphill","given":"William","email":"","middleInitial":"R.","affiliations":[{"id":595,"text":"U.S. Geological Survey","active":false,"usgs":true}],"preferred":false,"id":494901,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":70112903,"text":"70112903 - 1980 - Evaluation of new spectral bands for multi-spectral imaging: SMIRR aircraft test results","interactions":[],"lastModifiedDate":"2014-06-18T09:37:03","indexId":"70112903","displayToPublicDate":"1980-04-15T09:22:27","publicationYear":"1980","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":3393,"text":"Sixth Annual Pecora Symposium and Exposition","active":true,"publicationSubtype":{"id":10}},"title":"Evaluation of new spectral bands for multi-spectral imaging: SMIRR aircraft test results","docAbstract":"<p>A 10-channel radiometer called the Shuttle Multispectral Infrared Radiometer (SMIRR) is scheduled to take data from orbit on the second shuttle orbital light test.  As part of the instrument test sequence, a series of aircraft flights was carried out over 10 test areas in Utah and Nevada.  Apart from vegetation, the materials exposed at the surface were volcanic sequences ranging from tuffs to basalts, areas of hydrothermally altered volcanic rocks, sedimentary sequences of sandstone and carbonate rocks, and alluvial cover.</p>","largerWorkType":{"id":2,"text":"Article"},"largerWorkTitle":"Sixth Annual Pecora Symposium and Exposition","largerWorkSubtype":{"id":10,"text":"Journal Article"},"language":"English","publisher":"Society of Exploration Geophysicists","publisherLocation":"Tulsa, OK","usgsCitation":"Goetz, A., and Rowan, L.C., 1980, Evaluation of new spectral bands for multi-spectral imaging: SMIRR aircraft test results: Sixth Annual Pecora Symposium and Exposition, p. 38-40.","productDescription":"3 p.","startPage":"38","endPage":"40","onlineOnly":"3","costCenters":[],"links":[{"id":288756,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"53ae76ade4b0abf75cf2bfe0","contributors":{"editors":[{"text":"Barringer, Anthony R.","contributorId":112053,"corporation":false,"usgs":true,"family":"Barringer","given":"Anthony","email":"","middleInitial":"R.","affiliations":[],"preferred":false,"id":509896,"contributorType":{"id":2,"text":"Editors"},"rank":1}],"authors":[{"text":"Goetz, Alexander F.H.","contributorId":89805,"corporation":false,"usgs":true,"family":"Goetz","given":"Alexander F.H.","affiliations":[],"preferred":false,"id":494899,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Rowan, Lawrence C.","contributorId":58629,"corporation":false,"usgs":true,"family":"Rowan","given":"Lawrence","email":"","middleInitial":"C.","affiliations":[],"preferred":false,"id":494898,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":1007462,"text":"1007462 - 1980 - Enhydra lutris","interactions":[],"lastModifiedDate":"2025-05-09T16:13:52.805891","indexId":"1007462","displayToPublicDate":"1980-04-15T01:00:00","publicationYear":"1980","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":2654,"text":"Mammalian Species","active":true,"publicationSubtype":{"id":10}},"title":"Enhydra lutris","docAbstract":"<p>No abstract available.&nbsp;</p>","language":"English","publisher":"Oxford Academic","doi":"10.2307/3503844","usgsCitation":"Estes, J.A., 1980, Enhydra lutris: Mammalian Species, no. 133, p. 1-8, https://doi.org/10.2307/3503844.","productDescription":"8 p.","startPage":"1","endPage":"8","costCenters":[{"id":651,"text":"Western Ecological Research Center","active":true,"usgs":true}],"links":[{"id":486821,"rank":2,"type":{"id":40,"text":"Open Access Publisher Index Page"},"url":"https://doi.org/10.2307/3503844","text":"Publisher Index Page"},{"id":130024,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"issue":"133","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a14e4b07f02db602630","contributors":{"authors":[{"text":"Estes, J. A.","contributorId":53319,"corporation":false,"usgs":true,"family":"Estes","given":"J.","email":"","middleInitial":"A.","affiliations":[],"preferred":false,"id":315406,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":70112916,"text":"70112916 - 1980 - Airborne-biogeochemical survey test-case results","interactions":[],"lastModifiedDate":"2014-06-18T12:03:24","indexId":"70112916","displayToPublicDate":"1980-04-14T11:47:59","publicationYear":"1980","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":3393,"text":"Sixth Annual Pecora Symposium and Exposition","active":true,"publicationSubtype":{"id":10}},"title":"Airborne-biogeochemical survey test-case results","docAbstract":"<p>Airborne spectroradiometer surveys over several forest-covered sulfide bodies indicate that mineralization has affected the overlying vegetation; anomalous spectral reflectivity properties can be detected in the vegetation using appropriate remote-sensing interments and data-reduction techniques.  Mineralization induces subtle changes in the shape of the chlorophyll <i>a</i> and <i>b</i> absorption spectrum between 550 and 750 nm.  The observed spectral variations appear specifically to be on the wings of the broad red chlorophyll bars, centered at about 680 nm.</p>","largerWorkType":{"id":2,"text":"Article"},"largerWorkTitle":"Sixth Annual Pecora Symposium and Exposition","largerWorkSubtype":{"id":10,"text":"Journal Article"},"language":"English","publisher":"Society of Exploration Geophysicists","publisherLocation":"Tulsa, OK","usgsCitation":"Collins, W.E., Chang, S., Raines, G.L., Canney, F.C., and Ashley, R., 1980, Airborne-biogeochemical survey test-case results: Sixth Annual Pecora Symposium and Exposition, p. 71-73.","productDescription":"3 p.","startPage":"71","endPage":"73","numberOfPages":"3","costCenters":[],"links":[{"id":288804,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"53ae7624e4b0abf75cf2bea1","contributors":{"editors":[{"text":"Barringer, Anthony R.","contributorId":112053,"corporation":false,"usgs":true,"family":"Barringer","given":"Anthony","email":"","middleInitial":"R.","affiliations":[],"preferred":false,"id":509903,"contributorType":{"id":2,"text":"Editors"},"rank":1}],"authors":[{"text":"Collins, William E.","contributorId":37474,"corporation":false,"usgs":true,"family":"Collins","given":"William","email":"","middleInitial":"E.","affiliations":[],"preferred":false,"id":494921,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Chang, Sheng-Huei","contributorId":37256,"corporation":false,"usgs":true,"family":"Chang","given":"Sheng-Huei","email":"","affiliations":[],"preferred":false,"id":494920,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Raines, Gary L.","contributorId":48162,"corporation":false,"usgs":true,"family":"Raines","given":"Gary","email":"","middleInitial":"L.","affiliations":[],"preferred":false,"id":494922,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Canney, Frank C.","contributorId":91251,"corporation":false,"usgs":true,"family":"Canney","given":"Frank","email":"","middleInitial":"C.","affiliations":[],"preferred":false,"id":494923,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"Ashley, Roger","contributorId":7625,"corporation":false,"usgs":true,"family":"Ashley","given":"Roger","affiliations":[],"preferred":false,"id":494919,"contributorType":{"id":1,"text":"Authors"},"rank":5}]}}
,{"id":70112915,"text":"70112915 - 1980 - Introduction to the workshop","interactions":[],"lastModifiedDate":"2014-06-18T11:43:05","indexId":"70112915","displayToPublicDate":"1980-04-14T11:40:47","publicationYear":"1980","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":3393,"text":"Sixth Annual Pecora Symposium and Exposition","active":true,"publicationSubtype":{"id":10}},"title":"Introduction to the workshop","docAbstract":"<p>The Workshop on Digital Data Processing will examine future needs and requirements for digital aspects of remote sensing.  The session will start with several formal presentations that relate to key areas in digital processing and related technology.  A general panel discussion on future needs and potential problem areas will follow.</p>","largerWorkType":{"id":2,"text":"Article"},"largerWorkTitle":"Sixth Annual Pecora Symposium and Exposition","largerWorkSubtype":{"id":10,"text":"Journal Article"},"language":"English","publisher":"Society of Exploration Geophysicists","publisherLocation":"Tulsa, OK","usgsCitation":"Rice, W., and Chavez, P., 1980, Introduction to the workshop: Sixth Annual Pecora Symposium and Exposition, p. 112-113.","productDescription":"2 p.","startPage":"112","endPage":"113","numberOfPages":"2","costCenters":[],"links":[{"id":288800,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"53ae7753e4b0abf75cf2c0fb","contributors":{"editors":[{"text":"Barringer, Anthony R.","contributorId":112053,"corporation":false,"usgs":true,"family":"Barringer","given":"Anthony","email":"","middleInitial":"R.","affiliations":[],"preferred":false,"id":509902,"contributorType":{"id":2,"text":"Editors"},"rank":1}],"authors":[{"text":"Rice, Wes","contributorId":81808,"corporation":false,"usgs":true,"family":"Rice","given":"Wes","email":"","affiliations":[],"preferred":false,"id":494918,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Chavez, Pat","contributorId":38899,"corporation":false,"usgs":true,"family":"Chavez","given":"Pat","affiliations":[],"preferred":false,"id":494917,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":70112901,"text":"70112901 - 1980 - Laying the groundwork: a review of satellite and airborne remote sensing surfaces and related surface exploration techniques","interactions":[],"lastModifiedDate":"2014-06-18T09:20:59","indexId":"70112901","displayToPublicDate":"1980-04-14T09:07:00","publicationYear":"1980","noYear":false,"publicationType":{"id":24,"text":"Conference Paper"},"publicationSubtype":{"id":19,"text":"Conference Paper"},"title":"Laying the groundwork: a review of satellite and airborne remote sensing surfaces and related surface exploration techniques","docAbstract":"No abstract available.","largerWorkType":{"id":4,"text":"Book"},"largerWorkTitle":"Sixth Annual Pecora Symposium and Exposition","largerWorkSubtype":{"id":12,"text":"Conference publication"},"language":"English","publisher":"Society of Exploration Geophysicists","publisherLocation":"Tulsa, OK","usgsCitation":"Bailey, G.B., 1980, Laying the groundwork: a review of satellite and airborne remote sensing surfaces and related surface exploration techniques, <i>in</i> Sixth Annual Pecora Symposium and Exposition, p. 24-33.","productDescription":"10 p.","startPage":"24","endPage":"33","numberOfPages":"10","costCenters":[{"id":222,"text":"Earth Resources Observation and Science (EROS) Center","active":true,"usgs":true}],"links":[{"id":288752,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"53ae775ae4b0abf75cf2c10f","contributors":{"editors":[{"text":"Barringer, Anthony R.","contributorId":112053,"corporation":false,"usgs":true,"family":"Barringer","given":"Anthony","email":"","middleInitial":"R.","affiliations":[],"preferred":false,"id":509895,"contributorType":{"id":2,"text":"Editors"},"rank":1}],"authors":[{"text":"Bailey, G. Bryan","contributorId":22689,"corporation":false,"usgs":true,"family":"Bailey","given":"G.","email":"","middleInitial":"Bryan","affiliations":[],"preferred":false,"id":494897,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
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