{"pageNumber":"878","pageRowStart":"21925","pageSize":"25","recordCount":46885,"records":[{"id":70047558,"text":"ds69J8 - 2007 - Source rock potential of upper cretaceous marine shales in the Wind River Basin, Wyoming: Chapter 8 in <i>Petroleum systems and geologic assessment of oil and gas resources in the Wind River Basin Province, Wyoming</i>","interactions":[],"lastModifiedDate":"2013-08-12T10:28:38","indexId":"ds69J8","displayToPublicDate":"2007-01-01T10:23:00","publicationYear":"2007","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":310,"text":"Data Series","code":"DS","onlineIssn":"2327-638X","printIssn":"2327-0271","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"69-J-8","title":"Source rock potential of upper cretaceous marine shales in the Wind River Basin, Wyoming: Chapter 8 in <i>Petroleum systems and geologic assessment of oil and gas resources in the Wind River Basin Province, Wyoming</i>","docAbstract":"Seventy-eight samples collected from marine shales from \nthe Cretaceous Mowry Shale, the lower part of the Frontier \nFormation, and the lower shaly and upper sandy members \nof the Cody Shale in the Wind River Basin, Wyoming, were \nanalyzed using Rock-Eval and total organic carbon analysis \nto determine the source rock potential. Results indicate \nthat the Mowry Shale has a generative potential based on \norganic richness that is considered to be fair to very good, \nand hydrogen indices and S<sub>2</sub>\n/S<sub>3</sub>\n ratios indicate a capability to \ngenerate both oil and gas. Maps of the Mowry indicate that \nit is most organic rich and oil-prone in the eastern part of the \nbasin. Results of total organic carbon and Rock-Eval analyses \nfor the Frontier Formation indicate that it is composed of \nmainly type III gas-prone kerogen, with organic richness \nlevels that are generally poor to fair. Results of similar \nanalyses of samples from the lower shaly member of the \nCody Shale show a generative potential ranging from fair to \nexcellent, and hydrogen indices and S<sub>2</sub>\n/S<sub>3</sub>\n ratios indicate that \nit is capable of generating both oil and gas. Maps showing \nthe distribution of kerogen types and organic richness for \nthe lower shaly member of the Cody Shale are similar to the \nMowry and show that lower shaly member of the Cody is \nmore organic rich and more oil-prone in the eastern part of the \nbasin. Analyses of samples of the upper sandy member of the \nCody Shale indicate that it has little or no potential as a source \nrock. Thermal maturity mapping based on vitrinite reflectance \nmeasurements in the coal-bearing post-Cody Upper \nCretaceous and Paleocene rocks shows that Upper Cretaceous \nmarine shales in the deeper parts of the Wind River Basin are \nthermally mature to overmature with respect to hydrocarbon \ngeneration.","largerWorkType":{"id":18,"text":"Report"},"largerWorkTitle":"Petroleum systems and geologic assessment of oil and gas resources in the Wind River Basin Province, Wyoming (Data Series 69-J)","largerWorkSubtype":{"id":5,"text":"USGS Numbered Series"},"language":"English","publisher":"U.S. Geological  Survey","publisherLocation":"Reston, VA","doi":"10.3133/ds69J8","collaboration":"This report is Chapter 8 in <i>Petroleum systems and geologic assessment of oil and gas resources in the Wind River Basin Province, Wyoming</i>.  For more information, see: <a href=\"http://pubs.er.usgs.gov/publication/ds69J\" target=\"_blank\">Data Series 69-J</a>.","usgsCitation":"Finn, T.M., 2007, Source rock potential of upper cretaceous marine shales in the Wind River Basin, Wyoming: Chapter 8 in <i>Petroleum systems and geologic assessment of oil and gas resources in the Wind River Basin Province, Wyoming</i>: U.S. Geological Survey Data Series 69-J-8, iii, 24 p., https://doi.org/10.3133/ds69J8.","productDescription":"iii, 24 p.","numberOfPages":"27","costCenters":[{"id":674,"text":"Wind River Basin Province Assessment Team","active":false,"usgs":true}],"links":[{"id":276328,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.usgs.gov/dds/dds-069/dds-069-j/"},{"id":276325,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/dds/dds-069/dds-069-j/REPORTS/69_J_CH_8.pdf"},{"id":276330,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/ds69j8.png"}],"country":"United States","state":"Wyoming","otherGeospatial":"Wind River Basin Province","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -110.1,42.0 ], [ -110.1,44.0 ], [ -106.0,44.0 ], [ -106.0,42.0 ], [ -110.1,42.0 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"520a03fde4b0026c2bc11cc3","contributors":{"authors":[{"text":"Finn, Thomas M. 0000-0001-6396-9351 finn@usgs.gov","orcid":"https://orcid.org/0000-0001-6396-9351","contributorId":778,"corporation":false,"usgs":true,"family":"Finn","given":"Thomas","email":"finn@usgs.gov","middleInitial":"M.","affiliations":[{"id":164,"text":"Central Energy Resources Science Center","active":true,"usgs":true}],"preferred":true,"id":482399,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":70101053,"text":"ofr20071047SRP093 - 2007 - The next generation Antarctic digital magnetic anomaly map","interactions":[],"lastModifiedDate":"2014-04-09T12:19:44","indexId":"ofr20071047SRP093","displayToPublicDate":"2007-01-01T10:18:00","publicationYear":"2007","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":330,"text":"Open-File Report","code":"OFR","onlineIssn":"2331-1258","printIssn":"0196-1497","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"2007-1047-SRP-093","title":"The next generation Antarctic digital magnetic anomaly map","docAbstract":"Initiated in 1995, the Antarctic Digital Magnetic Anomaly Project (ADMAP) produced the first magnetic \nanomaly map of the Antarctic region south of 60\no\nS (Golynsky et al., 2001). This map synthesized over 7.1 million line-kms of survey data available up through 1999 from marine, airborne and Magsat satellite observations. Since the \nproduction of the initial map, a large number of new marine and airborne surveys and improved magnetic observations \nfrom the Ørsted and CHAMP satellite missions have become available. In addition, an improved core field model for \nthe Antarctic has been developed to better isolate crustal anomalies in these data. The next generation compilation also \nwill likely represent the magnetic survey observations of the region in terms of a high-resolution spherical cap harmonic \nmodel. In this paper, we review the progress and problems of developing an improved magnetic anomaly map to \nfacilitate studies of the Antarctic crustal magnetic field","largerWorkType":{"id":18,"text":"Report"},"largerWorkTitle":"Antarctica: A Keystone in a Changing World--Online Proceedings for the Tenth International Symposium on Antarctic Earth Sciences. Santa Barbara, California, U.S.A.--August 26 to September 1, 2007","largerWorkSubtype":{"id":5,"text":"USGS Numbered Series"},"language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Reston, VA","doi":"10.3133/ofr20071047SRP093","usgsCitation":"von Frese, R.R., Golynsky, A., Kim, H., Gaya-Pique, L., Thébault, E., Chiappinii, M., Ghidella, M., Grunow, A., and ADMAP Working Group, 2007, The next generation Antarctic digital magnetic anomaly map: U.S. Geological Survey Open-File Report 2007-1047-SRP-093, Report: 4 p.; Plate: 33.11 inches x 46.81 inches, https://doi.org/10.3133/ofr20071047SRP093.","productDescription":"Report: 4 p.; Plate: 33.11 inches x 46.81 inches","additionalOnlineFiles":"Y","costCenters":[],"links":[{"id":285955,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/ofr20071047SRP093.png"},{"id":285953,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/2007/1047/srp/srp093/of2007-1047srp093_plate1.pdf"},{"id":285954,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/2007/1047/srp/srp093/of2007-1047srp093.pdf"}],"otherGeospatial":"Antarctica","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -180.0,-90.0 ], [ -180.0,-60.0 ], [ 180.0,-60.0 ], [ 180.0,-90.0 ], [ -180.0,-90.0 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"535595a0e4b0120853e8c28b","contributors":{"authors":[{"text":"von Frese, Ralph R. B.","contributorId":33953,"corporation":false,"usgs":true,"family":"von Frese","given":"Ralph","email":"","middleInitial":"R. B.","affiliations":[],"preferred":false,"id":492563,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Golynsky, A.V.","contributorId":15513,"corporation":false,"usgs":true,"family":"Golynsky","given":"A.V.","email":"","affiliations":[],"preferred":false,"id":492562,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Kim, H.R.","contributorId":100742,"corporation":false,"usgs":true,"family":"Kim","given":"H.R.","email":"","affiliations":[],"preferred":false,"id":492569,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Gaya-Pique, L.","contributorId":6761,"corporation":false,"usgs":true,"family":"Gaya-Pique","given":"L.","email":"","affiliations":[],"preferred":false,"id":492561,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"Thébault, E.","contributorId":56974,"corporation":false,"usgs":true,"family":"Thébault","given":"E.","affiliations":[],"preferred":false,"id":492565,"contributorType":{"id":1,"text":"Authors"},"rank":5},{"text":"Chiappinii, M.","contributorId":72707,"corporation":false,"usgs":true,"family":"Chiappinii","given":"M.","email":"","affiliations":[],"preferred":false,"id":492566,"contributorType":{"id":1,"text":"Authors"},"rank":6},{"text":"Ghidella, M.","contributorId":95794,"corporation":false,"usgs":true,"family":"Ghidella","given":"M.","affiliations":[],"preferred":false,"id":492567,"contributorType":{"id":1,"text":"Authors"},"rank":7},{"text":"Grunow, A.","contributorId":99892,"corporation":false,"usgs":true,"family":"Grunow","given":"A.","affiliations":[],"preferred":false,"id":492568,"contributorType":{"id":1,"text":"Authors"},"rank":8},{"text":"ADMAP Working Group","contributorId":128064,"corporation":true,"usgs":false,"organization":"ADMAP Working Group","id":535648,"contributorType":{"id":1,"text":"Authors"},"rank":9}]}}
,{"id":70121030,"text":"70121030 - 2007 - The need for sustained and integrated high-resolution mapping of dynamic coastal environments","interactions":[],"lastModifiedDate":"2021-06-08T12:04:20.504596","indexId":"70121030","displayToPublicDate":"2007-01-01T10:13:00","publicationYear":"2007","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":2678,"text":"Marine Technology Society Journal","active":true,"publicationSubtype":{"id":10}},"title":"The need for sustained and integrated high-resolution mapping of dynamic coastal environments","docAbstract":"<p><span>The coastal zone of the United States is a dynamic environment evolving in response to both natural processes and human activities. In order to protect coastal populations and resources, a detailed understanding of the physical setting and of the processes responsible for change is required. A sustained program of mapping coastal areas provides a means to establish baseline conditions, document change, and, in conjunction with models of physical processes, predict future behavior. Recent advances in mapping technology, including airborne lidars and hyperspectral imagers, allow for the rapid collection of high-resolution elevation data and land use information on a national scale. These rich data sets are critical to evaluating risk associated with coastal hazards, such as flooding during extreme storms. For example, coastal elevation data is a fundamental parameter in storm surge models that predict where flooding will occur, and land use maps serve as the foundation of assessments that identify the resources and populations that are most vulnerable. A comprehensive, national coastal mapping plan that is designed to collect, manage, and distribute these data, as well as to take advantage of recent progress in mapping technology, will provide a wealth of information for studying the processes of physical change, for determining areas vulnerable to coastal hazards, and for protecting and managing our coastal communities and resources.</span></p>","language":"English","publisher":"Ingenta Connect","doi":"10.4031/002533206787353241","usgsCitation":"Stockdon, H.F., Lillycrop, J.W., Howd, P.A., and Wozencraft, J.M., 2007, The need for sustained and integrated high-resolution mapping of dynamic coastal environments: Marine Technology Society Journal, v. 40, no. 4, p. 90-99, https://doi.org/10.4031/002533206787353241.","productDescription":"10 p.","startPage":"90","endPage":"99","costCenters":[{"id":186,"text":"Coastal and Marine Geology Program","active":true,"usgs":true}],"links":[{"id":476937,"rank":0,"type":{"id":40,"text":"Open Access 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phowd@usgs.gov","contributorId":4105,"corporation":false,"usgs":true,"family":"Howd","given":"Peter","email":"phowd@usgs.gov","middleInitial":"A.","affiliations":[],"preferred":true,"id":498698,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Wozencraft, Jennifer M.","contributorId":60964,"corporation":false,"usgs":true,"family":"Wozencraft","given":"Jennifer","email":"","middleInitial":"M.","affiliations":[],"preferred":false,"id":498699,"contributorType":{"id":1,"text":"Authors"},"rank":4}]}}
,{"id":70094912,"text":"ofr20071047SRP065A - 2007 - Pan-African granulites of central Dronning Maud Land and Mozambique: A comparison within the East-African-Antarctic orogen","interactions":[],"lastModifiedDate":"2014-02-25T10:20:33","indexId":"ofr20071047SRP065A","displayToPublicDate":"2007-01-01T10:02:00","publicationYear":"2007","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":330,"text":"Open-File Report","code":"OFR","onlineIssn":"2331-1258","printIssn":"0196-1497","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"2007-1047-SRP-065","title":"Pan-African granulites of central Dronning Maud Land and Mozambique: A comparison within the East-African-Antarctic orogen","docAbstract":"Granulite-facies metamorphism is extensively reported in Late Neoproterozoic/Early Palaeozoic time during formation of the East-African-Antarctic orogen (EAAO). Metamorphic data acquired from the Pan-African orogen of central Dronning Maud Land (cDML) are compared with data from northern Mozambique. The metamorphic rocks of cDML are characterised by Opx±Grt-bearing gneisses and Sil+Kfs-bearing metapelites which indicate medium-P granulite-facies metamorphism. Peak conditions, which are estimated to 800-900ºC at pressures up to 1.0 GPa, were followed by near-isothermal decompression during late Pan-African extension and exhumation. Granulite-facies lithologies are widespread in northern Mozambique, and Grt+Cpx-bearing assemblages show that high-P granulite-facies conditions with PT reaching 1.55 GPa and 900ºC were reached during the Pan-African orogeny. Garnet is replaced by symplectites of Pl+Opx+Mag indicating isothermal decompression, and the subsequent formation of Pl+amphibole-coronas suggests cooling into amphibolite facies. It is concluded that high-T metamorphism was pervasive in EAAO in Late Neoproterozoic/Early Paleozoic time, strongly overprinting evidences of earlier metamorphic assemblages.","largerWorkType":{"id":18,"text":"Report"},"largerWorkTitle":"Antarctica: A Keystone in a Changing World--Online Proceedings for the Tenth International Symposium on Antarctic Earth Sciences. Santa Barbara, California, U.S.A.--August 26 to September 1, 2007","largerWorkSubtype":{"id":5,"text":"USGS Numbered Series"},"language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Reston, VA","doi":"10.3133/ofr20071047SRP065A","usgsCitation":"Engvik, A., Elevevold, S., Jacobs, J., Tveten, E., de Azevedo, S., and Njange, F., 2007, Pan-African granulites of central Dronning Maud Land and Mozambique: A comparison within the East-African-Antarctic orogen: U.S. Geological Survey Open-File Report 2007-1047-SRP-065, 5 p., https://doi.org/10.3133/ofr20071047SRP065A.","productDescription":"5 p.","additionalOnlineFiles":"N","costCenters":[],"links":[{"id":282736,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/ofr20071047SRP065A.JPG"},{"id":282735,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/2007/1047/srp/srp065/of2007-1047srp065.pdf"}],"otherGeospatial":"Antarctica;Queen Maud Land","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -18.83,-78.89 ], [ -18.83,-68.64 ], [ 50.14,-68.64 ], [ 50.14,-78.89 ], [ -18.83,-78.89 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"53cd6a98e4b0b2908510359b","contributors":{"authors":[{"text":"Engvik, A.K.","contributorId":77839,"corporation":false,"usgs":true,"family":"Engvik","given":"A.K.","email":"","affiliations":[],"preferred":false,"id":490937,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Elevevold, S.","contributorId":13535,"corporation":false,"usgs":true,"family":"Elevevold","given":"S.","email":"","affiliations":[],"preferred":false,"id":490933,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Jacobs, J.","contributorId":96999,"corporation":false,"usgs":true,"family":"Jacobs","given":"J.","affiliations":[],"preferred":false,"id":490938,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Tveten, E.","contributorId":48476,"corporation":false,"usgs":true,"family":"Tveten","given":"E.","email":"","affiliations":[],"preferred":false,"id":490935,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"de Azevedo, S.","contributorId":69883,"corporation":false,"usgs":true,"family":"de Azevedo","given":"S.","email":"","affiliations":[],"preferred":false,"id":490936,"contributorType":{"id":1,"text":"Authors"},"rank":5},{"text":"Njange, F.","contributorId":37644,"corporation":false,"usgs":true,"family":"Njange","given":"F.","email":"","affiliations":[],"preferred":false,"id":490934,"contributorType":{"id":1,"text":"Authors"},"rank":6}]}}
,{"id":70093688,"text":"ofr20071047SRP043 - 2007 - East Antarctic ice-sheet dynamics between 5.2 and 0 Ma from a high-resolution terrigenous particle size record, ODP Site 1165, Prydz Bay-Cooperation Sea","interactions":[],"lastModifiedDate":"2014-02-11T10:19:26","indexId":"ofr20071047SRP043","displayToPublicDate":"2007-01-01T10:00:00","publicationYear":"2007","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":330,"text":"Open-File Report","code":"OFR","onlineIssn":"2331-1258","printIssn":"0196-1497","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"2007-1047-SRP-043","title":"East Antarctic ice-sheet dynamics between 5.2 and 0 Ma from a high-resolution terrigenous particle size record, ODP Site 1165, Prydz Bay-Cooperation Sea","docAbstract":"This paper discusses a 5.2-0 Ma high-resolution terrigenous particle size record recovered from a sediment \ndrift off East Antarctica. The particle size properties of Hole 1165B are interpreted in the context of previously acquired \ndata on a continental shelf to slope transect drilled by ODP Leg 188 in Prydz Bay and the Cooperation Sea. The new \ndata indicate that the Lambert ice stream stayed predominantly landward of the shelf break in the early Pliocene (5.2-3.5 \nMa) with periods of ice sheet recession on land. The middle Pliocene (3.5-3.1 Ma) is characterized as major ice \nexpansion during glacials with deposition of laminated clays from meltwater plumes on the continental rise, alternating \nwith periods of ice recession. A change in sedimentary facies and a decrease in sedimentation rates occurred at ~3.1 Ma \nindicating a more retreated Lambert Glacier. Between 2.5 and 1 Ma the ice stream was generally stable and had become \ncold-based with ice flow in a glacial trough extending to the shelf break. Three-four large pulses of coarse-grained \nglacigenic debris mark the record at ~1 Ma. These are interpreted as extensive calving due to decoupling of the marine \nterminus from its bed in response to Northern Hemisphere deglaciations and associated sea level rises.","largerWorkType":{"id":18,"text":"Report"},"largerWorkTitle":"Antarctica: A Keystone in a Changing World--Online Proceedings for the Tenth International Symposium on Antarctic Earth Sciences. Santa Barbara, California, U.S.A.--August 26 to September 1, 2007","largerWorkSubtype":{"id":5,"text":"USGS Numbered Series"},"language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Reston, VA","doi":"10.3133/ofr20071047SRP043","usgsCitation":"Passchier, S., 2007, East Antarctic ice-sheet dynamics between 5.2 and 0 Ma from a high-resolution terrigenous particle size record, ODP Site 1165, Prydz Bay-Cooperation Sea: U.S. Geological Survey Open-File Report 2007-1047-SRP-043, 4 p., https://doi.org/10.3133/ofr20071047SRP043.","productDescription":"4 p.","additionalOnlineFiles":"N","costCenters":[],"links":[{"id":282256,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/ofr20071047SRP043.JPG"},{"id":282255,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/2007/1047/srp/srp043/of2007-1047srp043.pdf"}],"otherGeospatial":"Antarctica","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ 180.0,-90.0 ], [ 180.0,-60.0 ], [ -180.0,-60.0 ], [ -180.0,-90.0 ], [ 180.0,-90.0 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"53cd563ae4b0b290850f6cb4","contributors":{"authors":[{"text":"Passchier, S.","contributorId":15117,"corporation":false,"usgs":false,"family":"Passchier","given":"S.","email":"","affiliations":[],"preferred":false,"id":490148,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":70094157,"text":"ofr20071047SRP048 - 2007 - Geology of the Terre Adélie Craton (135 – 146˚ E)","interactions":[],"lastModifiedDate":"2014-02-18T10:16:19","indexId":"ofr20071047SRP048","displayToPublicDate":"2007-01-01T09:53:00","publicationYear":"2007","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":330,"text":"Open-File Report","code":"OFR","onlineIssn":"2331-1258","printIssn":"0196-1497","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"2007-1047-SRP-048","title":"Geology of the Terre Adélie Craton (135 – 146˚ E)","docAbstract":"More than 15 years of field and laboratory investigations on samples from Terre Adélie to the western \npart of George V<sup>th</sup> Land (135 to 146°E) during the GEOLETA program allow a reassessment of the Terre Adélie \nCraton (TAC) geology. The TAC represents the largest exposed fragment of the East Antarctic Shield preserved from \nboth Grenville and Ross tectono-metamorphic events. Therefore it corresponds to a well-preserved continental \nsegment that developed from the Neoarchean to the Paleoproterozoic. Together with the Gawler Craton in South \nAustralia, the TAC is considered as part of the Mawson continent, i.e. a striking piece of the Rodinia Supercontinent. \nHowever, this craton represents one of the less studied parts of the East Antarctic Shield. The three maps presented \nhere clearly point out the extent of two distinct domains within the Terre Adélie Craton and suggest that the TAC was \nbuilt up through a polyphased evolution during the Neoarchean-Siderian (c.a. 2.5Ga) and the Statherian (c.a. 1.7Ga) \nperiods. These data support a complete re-assessment of the TAC geology and represent a valuable base for the \nunderstanding of global geodynamics changes during Paleoproterozoic times.","largerWorkType":{"id":18,"text":"Report"},"largerWorkTitle":"Antarctica: A Keystone in a Changing World--Online Proceedings for the Tenth International Symposium on Antarctic Earth Sciences. Santa Barbara, California, U.S.A.--August 26 to September 1, 2007","largerWorkSubtype":{"id":5,"text":"USGS Numbered Series"},"language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Reston, VA","doi":"10.3133/ofr20071047SRP048","usgsCitation":"Menot, R., Duclaux, G., Peucat, J., Rolland, Y., Guillot, S., Fanning, M., Bascou, J., Gapais, D., and Pecher, A., 2007, Geology of the Terre Adélie Craton (135 – 146˚ E): U.S. Geological Survey Open-File Report 2007-1047-SRP-048, 5 p., https://doi.org/10.3133/ofr20071047SRP048.","productDescription":"5 p.","additionalOnlineFiles":"N","costCenters":[],"links":[{"id":282463,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/ofr20071047SRP048.JPG"},{"id":282462,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/2007/1047/srp/srp048/of2007-1047srp048.pdf"}],"otherGeospatial":"Antarctica","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ 180.0,-90.0 ], [ 180.0,-60.0 ], [ -180.0,-60.0 ], [ -180.0,-90.0 ], [ 180.0,-90.0 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"53cd5e70e4b0b290850fbb3e","contributors":{"authors":[{"text":"Menot, R.P.","contributorId":41738,"corporation":false,"usgs":true,"family":"Menot","given":"R.P.","email":"","affiliations":[],"preferred":false,"id":490480,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Duclaux, G.","contributorId":67006,"corporation":false,"usgs":true,"family":"Duclaux","given":"G.","email":"","affiliations":[],"preferred":false,"id":490482,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Peucat, J.J.","contributorId":73438,"corporation":false,"usgs":true,"family":"Peucat","given":"J.J.","email":"","affiliations":[],"preferred":false,"id":490483,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Rolland, Y.","contributorId":30137,"corporation":false,"usgs":true,"family":"Rolland","given":"Y.","email":"","affiliations":[],"preferred":false,"id":490479,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"Guillot, S.","contributorId":79401,"corporation":false,"usgs":true,"family":"Guillot","given":"S.","email":"","affiliations":[],"preferred":false,"id":490484,"contributorType":{"id":1,"text":"Authors"},"rank":5},{"text":"Fanning, M.","contributorId":10624,"corporation":false,"usgs":true,"family":"Fanning","given":"M.","email":"","affiliations":[],"preferred":false,"id":490477,"contributorType":{"id":1,"text":"Authors"},"rank":6},{"text":"Bascou, J.","contributorId":60127,"corporation":false,"usgs":true,"family":"Bascou","given":"J.","email":"","affiliations":[],"preferred":false,"id":490481,"contributorType":{"id":1,"text":"Authors"},"rank":7},{"text":"Gapais, D.","contributorId":79798,"corporation":false,"usgs":true,"family":"Gapais","given":"D.","email":"","affiliations":[],"preferred":false,"id":490485,"contributorType":{"id":1,"text":"Authors"},"rank":8},{"text":"Pecher, A.","contributorId":28162,"corporation":false,"usgs":true,"family":"Pecher","given":"A.","email":"","affiliations":[],"preferred":false,"id":490478,"contributorType":{"id":1,"text":"Authors"},"rank":9}]}}
,{"id":70094910,"text":"ofr20071047SRP065 - 2007 - Analysis of continuous GPS measurements from southern Victoria Land, Antarctica","interactions":[],"lastModifiedDate":"2014-02-25T09:55:00","indexId":"ofr20071047SRP065","displayToPublicDate":"2007-01-01T09:37:00","publicationYear":"2007","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":330,"text":"Open-File Report","code":"OFR","onlineIssn":"2331-1258","printIssn":"0196-1497","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"2007-1047-SRP-064","title":"Analysis of continuous GPS measurements from southern Victoria Land, Antarctica","docAbstract":"Several years of continuous data have been collected at remote bedrock Global Positioning System (GPS) \nsites in southern Victoria Land, Antarctica. Annual to sub-annual variations are observed in the position time-series. An \natmospheric pressure loading (APL) effect is calculated from pressure field anomalies supplied by the European Centre \nfor Medium-Range Weather Forecasts (ECMWF) model loading an elastic Earth model. The predicted APL signal has \na moderate correlation with the vertical position time-series at McMurdo, Ross Island (International Global Navigation \nSatellite System Service (IGS) station MCM4), produced using a global solution. In contrast, a local solution in which \nMCM4 is the fiducial site generates a vertical time series for a remote site in Victoria Land (Cape Roberts, ROB4) \nwhich exhibits a low, inverse correlation with the predicted atmospheric pressure loading signal. If, in the future, \nknown and well modeled geophysical loads can be separated from the time-series, then local hydrological loading, of \ninterest for glaciological and climate applications, can potentially be extracted from the GPS time-series.","largerWorkType":{"id":18,"text":"Report"},"largerWorkTitle":"Antarctica: A Keystone in a Changing World--Online Proceedings for the Tenth International Symposium on Antarctic Earth Sciences. Santa Barbara, California, U.S.A.--August 26 to September 1, 2007","largerWorkSubtype":{"id":5,"text":"USGS Numbered Series"},"language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Reston, VA","doi":"10.3133/ofr20071047SRP065","usgsCitation":"Willis, M., 2007, Analysis of continuous GPS measurements from southern Victoria Land, Antarctica: U.S. Geological Survey Open-File Report 2007-1047-SRP-064, 5 p., https://doi.org/10.3133/ofr20071047SRP065.","productDescription":"5 p.","additionalOnlineFiles":"N","costCenters":[],"links":[{"id":282730,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/2007/1047/srp/srp064/of2007-1047srp064.pdf"},{"id":282731,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/ofr20071047SRP065.JPG"}],"otherGeospatial":"Antarctica;Victoria Land","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ 149.96,-79.11 ], [ 149.96,-70.28 ], [ 170.34,-70.28 ], [ 170.34,-79.11 ], [ 149.96,-79.11 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"53cd4cd5e4b0b290850f134b","contributors":{"authors":[{"text":"Willis, Michael J.","contributorId":11118,"corporation":false,"usgs":true,"family":"Willis","given":"Michael J.","affiliations":[],"preferred":false,"id":490932,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":70121022,"text":"70121022 - 2007 - Integrating hydrologic and geophysical data to constrain coastal surficial aquifer processes at multiple spatial and temporal scales","interactions":[],"lastModifiedDate":"2017-09-06T11:32:59","indexId":"70121022","displayToPublicDate":"2007-01-01T09:29:00","publicationYear":"2007","noYear":false,"publicationType":{"id":5,"text":"Book chapter"},"publicationSubtype":{"id":24,"text":"Book Chapter"},"title":"Integrating hydrologic and geophysical data to constrain coastal surficial aquifer processes at multiple spatial and temporal scales","docAbstract":"<p>Since 1997, repeated, coincident geophysical surveys and extensive hydrologic studies in shallow monitoring wells have been used to study static and dynamic processes associated with surface water-groundwater interaction at a range of spatial scales at the estuarine and ocean boundaries of an undeveloped, permeable barrier island in the Georgia part of the U.S. South Atlantic Bight. Because geophysical and hydrologic data measure different parameters, at different resolution and precision, and over vastly different spatial scales, reconciling the coincident data or even combining complementary inversion, hydrogeochemcial analyses and well-based groundwater monitoring, and, in some cases, limited vegetation mapping to demonstrate the utility of an integrative, multidisciplinary approach for elucidating groundwater processes at spatial scales (tens to thousands of meters) that are often difficult to capture with traditional hydrologic approaches. The case studies highlight regional aquifer characteristics, varying degrees of lateral saltwater intrusion at estuarine boundaries, complex subsurface salinity gradients at the ocean boundary, and imaging of submarsh groundwater discharge and possible free convection in the pore waters of a clastic marsh. This study also documents the use of geophysical techniques for detecting temporal changes in groundwater salinity regimes under natural (not forced) gradients at intratidal to interannual (1998-200 Southeastern U.S.A. drought) time scales.","largerWorkType":{"id":4,"text":"Book"},"largerWorkTitle":"Subsurface hydrology: Data integration for properties and processes","language":"English","publisher":"Wiley","publisherLocation":"New York, NY","doi":"10.1029/171GM13","isbn":"9781118666463","usgsCitation":"Schultz, G.M., Ruppel, C., and Fulton, P., 2007, Integrating hydrologic and geophysical data to constrain coastal surficial aquifer processes at multiple spatial and temporal scales, chap. <i>of</i> Subsurface hydrology: Data integration for properties and processes, v. 171, p. 161-182, https://doi.org/10.1029/171GM13.","productDescription":"22 p.","startPage":"161","endPage":"182","costCenters":[{"id":186,"text":"Coastal and Marine Geology Program","active":true,"usgs":true},{"id":678,"text":"Woods Hole Coastal and Marine Science Center","active":true,"usgs":true}],"links":[{"id":292509,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"171","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"53f464cce4b073ff773a7d1c","contributors":{"editors":[{"text":"Hyndman, David W.","contributorId":7868,"corporation":false,"usgs":true,"family":"Hyndman","given":"David","email":"","middleInitial":"W.","affiliations":[],"preferred":false,"id":709623,"contributorType":{"id":2,"text":"Editors"},"rank":1},{"text":"Day-Lewis, Frederick D. 0000-0003-3526-886X daylewis@usgs.gov","orcid":"https://orcid.org/0000-0003-3526-886X","contributorId":1672,"corporation":false,"usgs":true,"family":"Day-Lewis","given":"Frederick","email":"daylewis@usgs.gov","middleInitial":"D.","affiliations":[{"id":37277,"text":"WMA - Earth System Processes Division","active":true,"usgs":true},{"id":486,"text":"OGW Branch of Geophysics","active":true,"usgs":true},{"id":493,"text":"Office of Ground Water","active":true,"usgs":true}],"preferred":true,"id":709624,"contributorType":{"id":2,"text":"Editors"},"rank":2},{"text":"Singha, Kamini 0000-0002-0605-3774","orcid":"https://orcid.org/0000-0002-0605-3774","contributorId":191366,"corporation":false,"usgs":false,"family":"Singha","given":"Kamini","email":"","affiliations":[{"id":6606,"text":"Colorado School of Mines","active":true,"usgs":false}],"preferred":false,"id":709625,"contributorType":{"id":2,"text":"Editors"},"rank":3}],"authors":[{"text":"Schultz, Gregory M.","contributorId":9582,"corporation":false,"usgs":false,"family":"Schultz","given":"Gregory","email":"","middleInitial":"M.","affiliations":[{"id":35646,"text":"Sky Research, Inc., Hanover, NH","active":true,"usgs":false}],"preferred":false,"id":498679,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Ruppel, Carolyn cruppel@usgs.gov","contributorId":2015,"corporation":false,"usgs":true,"family":"Ruppel","given":"Carolyn","email":"cruppel@usgs.gov","affiliations":[{"id":678,"text":"Woods Hole Coastal and Marine Science Center","active":true,"usgs":true}],"preferred":false,"id":498678,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Fulton, Patrick","contributorId":34832,"corporation":false,"usgs":true,"family":"Fulton","given":"Patrick","email":"","affiliations":[],"preferred":false,"id":498680,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":70047556,"text":"ds69J7 - 2007 - Distribution of fluids and pressures in the Wind River Basin, Wyoming: Chapter 7 in <i>Petroleum systems and geologic assessment of oil and gas resources in the Wind River Basin Province, Wyoming</i>","interactions":[],"lastModifiedDate":"2013-08-12T09:34:54","indexId":"ds69J7","displayToPublicDate":"2007-01-01T09:27:00","publicationYear":"2007","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":310,"text":"Data Series","code":"DS","onlineIssn":"2327-638X","printIssn":"2327-0271","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"69-J-7","title":"Distribution of fluids and pressures in the Wind River Basin, Wyoming: Chapter 7 in <i>Petroleum systems and geologic assessment of oil and gas resources in the Wind River Basin Province, Wyoming</i>","docAbstract":"To examine the state of hydrocarbons and water in the\nWind River Basin of Wyoming, the following data types\nare compiled and presented at the basin scale: fluid type,\npressure, and temperature from drillstem tests; watersalinity\nand cumulative hydrocarbon production from oil and gas\nwells; vitrinite reflectance data; and sonic well logs. The\nspatial distribution of produced fluids shows the nearly\nubiquitous presence of mobile water, even in highly productive\ngas-charged formations. Sonic logs record a basin wide\nvelocity decrease in the Lower Cretaceous Thermopolis Shale\nthrough the Upper Cretaceous Cody Shale that is attributed\nto a combination of paleo-overpressuring and present-day\noverpressuring. Pressure-elevation plots and mud weights\nreveal the presence of two large pressure compartments in\nthe Madden area, one above the Waltman Shale Member of\nthe Paleocene Fort Union Formation and the other below it.\nTemperature data reveal hot and cold spots around structures\nin the marginal parts of the basin where the Waltman Shale\nMember of the Fort Union Formation is absent. The highest\ntemperature gradients are in the upper pressure compartment\nin the Madden area. Vitrinite reflectance data record little\nchange with increasing depth throughout much of the geologic\nsection in shallow parts of the basin and a steady increase\nof log (R<sub>o</sub>\n) with depth in the deep parts of the basin. The\nvaried distribution of fluids, pressure, and temperature reflect\nthe complex history of subsidence, thrusting, hydrocarbon\ngeneration, water migration, and uplift in and marginal to this\nlarge, asymmetric intermontane basin.","largerWorkType":{"id":18,"text":"Report"},"largerWorkTitle":"Petroleum systems and geologic assessment of oil and gas resources in the Wind River Basin Province, Wyoming (Data Series 69-J)","largerWorkSubtype":{"id":5,"text":"USGS Numbered Series"},"language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Reston, VA","doi":"10.3133/ds69J7","collaboration":"This report is Chapter 7 in <i>Petroleum systems and geologic assessment of oil and gas resources in the Wind River Basin Province, Wyoming</i>.  For more information, see: <a href=\"http://pubs.er.usgs.gov/publication/ds69J\" target=\"_blank\">Data Series 69-J</a>.","usgsCitation":"Nelson, P.H., and Kibler, J.E., 2007, Distribution of fluids and pressures in the Wind River Basin, Wyoming: Chapter 7 in <i>Petroleum systems and geologic assessment of oil and gas resources in the Wind River Basin Province, Wyoming</i>: U.S. Geological Survey Data Series 69-J-7, iv, 35 p., https://doi.org/10.3133/ds69J7.","productDescription":"iv, 35 p.","numberOfPages":"39","costCenters":[{"id":674,"text":"Wind River Basin Province Assessment Team","active":false,"usgs":true}],"links":[{"id":276301,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/ds69j7.png"},{"id":276299,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/dds/dds-069/dds-069-j/REPORTS/69_J_CH_7.pdf"},{"id":276300,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.usgs.gov/dds/dds-069/dds-069-j/"}],"country":"United States","state":"Wyoming","otherGeospatial":"Wind River Basin Province","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -110.1,42.0 ], [ -110.1,44.0 ], [ -106.0,44.0 ], [ -106.0,42.0 ], [ -110.1,42.0 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"520a03e6e4b0026c2bc11af8","contributors":{"authors":[{"text":"Nelson, Philip H. pnelson@usgs.gov","contributorId":862,"corporation":false,"usgs":true,"family":"Nelson","given":"Philip","email":"pnelson@usgs.gov","middleInitial":"H.","affiliations":[{"id":164,"text":"Central Energy Resources Science Center","active":true,"usgs":true}],"preferred":true,"id":482396,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Kibler, Joyce E.","contributorId":56293,"corporation":false,"usgs":true,"family":"Kibler","given":"Joyce","email":"","middleInitial":"E.","affiliations":[],"preferred":false,"id":482397,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":70104176,"text":"70104176 - 2007 - Pesticides in U.S. streams and groundwater","interactions":[],"lastModifiedDate":"2014-05-14T11:58:34","indexId":"70104176","displayToPublicDate":"2007-01-01T09:26:00","publicationYear":"2007","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1565,"text":"Environmental Science & Technology","onlineIssn":"1520-5851","printIssn":"0013-936X","active":true,"publicationSubtype":{"id":10}},"title":"Pesticides in U.S. streams and groundwater","docAbstract":"<p>A 10­-year study by the U.S. Geological \nSurvey’s (USGS’s) National Water-­Quality Assessment (NAWQA) Program provides a national-­scale view of pesticide \noccurrence in streams and groundwater. The 1992-2001 study builds upon a preliminary \nanalysis from NAWQA’s first phase of studies during \n1992-1996 (1, 2). Pesticide data available from various studies prior to 1992 did not allow national assessment because of limited and variable geographic \ncoverage (usually focusing on individual states or \nregions), sparse and inconsistent inclusion of pesticides in use, and variable sampling designs (3-5).</p>\n<br>\n<p>The expanded geographic coverage and improved \ndata following 10 years of study (Figure 1) confirm \nand reinforce previously reported findings and \nenable more detailed analyses of each topic. This \narticle summarizes selected findings from a comprehensive report (6), with a focus on the nature of \npesticide occurrence and potential significance to \nhuman health and stream ecosystems. Information \non study design and methods as well as additional \nanalysis of geographic patterns and trends in relation to use and management practices are available \nin the full report (6).</p>","largerWorkType":{"id":2,"text":"Article"},"largerWorkTitle":"Environmental Science and Technology","largerWorkSubtype":{"id":10,"text":"Journal Article"},"language":"English","publisher":"American Chemical Society","doi":"10.1021/es072531u","usgsCitation":"Gilliom, R.J., 2007, Pesticides in U.S. streams and groundwater: Environmental Science & Technology, v. 41, no. 10, p. 3408-3414, https://doi.org/10.1021/es072531u.","productDescription":"7 p.","startPage":"3408","endPage":"3414","numberOfPages":"7","costCenters":[{"id":451,"text":"National Water Quality Assessment Program","active":true,"usgs":true}],"links":[{"id":287128,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"},{"id":287127,"type":{"id":10,"text":"Digital Object Identifier"},"url":"https://dx.doi.org/10.1021/es072531u"}],"country":"United States","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ 173.0,16.916667 ], [ 173.0,71.833333 ], [ -66.95,71.833333 ], [ -66.95,16.916667 ], [ 173.0,16.916667 ] ] ] } } ] }","volume":"41","issue":"10","noUsgsAuthors":false,"publicationDate":"2007-05-15","publicationStatus":"PW","scienceBaseUri":"53749070e4b0870f4d23cfc8","contributors":{"authors":[{"text":"Gilliom, Robert J. rgilliom@usgs.gov","contributorId":488,"corporation":false,"usgs":true,"family":"Gilliom","given":"Robert","email":"rgilliom@usgs.gov","middleInitial":"J.","affiliations":[{"id":451,"text":"National Water Quality Assessment Program","active":true,"usgs":true}],"preferred":true,"id":493588,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":70100983,"text":"ofr20071047SRP088 - 2007 - Trends in discharge and flow season timing of the Onyx River, Wright Valley, Antarctica since 1969","interactions":[],"lastModifiedDate":"2018-02-21T17:41:22","indexId":"ofr20071047SRP088","displayToPublicDate":"2007-01-01T09:19:00","publicationYear":"2007","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":330,"text":"Open-File Report","code":"OFR","onlineIssn":"2331-1258","printIssn":"0196-1497","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"2007-1047-SRP-088","title":"Trends in discharge and flow season timing of the Onyx River, Wright Valley, Antarctica since 1969","docAbstract":"Flow records at the two stream gauges on the Onyx River represent the longest actively collected \nenvironmental records in the McMurdo Dry Valleys, Antarctica. The downstream gauge, near Lake Vanda, has been \ncollecting data since 1969, and the upstream gauge, at Lower Wright Glacier (LWRT), has collected data since 1972. \nWe analyzed these records to assess the long-term trends in annual discharge, flow season length, flow season start, and \nflow season end. Our results indicate overall decreasing trends in annual discharge (0.4x106\n m3\n/decade at LWRT, 0.8 \nx106\n m3\n/decade at Vanda), and increasing flow season lengths (by 7 d/decade at LWRT, and 2.7 d/decade at Vanda), \ninfluenced by earlier start and later end dates (5.2 and 0.8 d/decade, respectively at LWRT; 4.8, 1.4 d/decade, \nrespectively at Vanda). This suggests that flow season climate patterns in the Dry Valleys are decreasing glacier melt \nintensity overall, but extending the period of meltwater generation","largerWorkType":{"id":18,"text":"Report"},"largerWorkTitle":"Antarctica: A Keystone in a Changing World--Online Proceedings for the Tenth International Symposium on Antarctic Earth Sciences. Santa Barbara, California, U.S.A.--August 26 to September 1, 2007","largerWorkSubtype":{"id":5,"text":"USGS Numbered Series"},"language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Reston, VA","doi":"10.3133/ofr20071047SRP088","usgsCitation":"Gooseff, M.N., McKnight, D.M., Doran, P.T., and Lyons, W.B., 2007, Trends in discharge and flow season timing of the Onyx River, Wright Valley, Antarctica since 1969: U.S. Geological Survey Open-File Report 2007-1047-SRP-088, 4 p., https://doi.org/10.3133/ofr20071047SRP088.","productDescription":"4 p.","additionalOnlineFiles":"N","costCenters":[],"links":[{"id":285879,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/ofr20071047SRP088.PNG"},{"id":285878,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/2007/1047/srp/srp088/of2007-1047srp088.pdf"}],"otherGeospatial":"Antarctica","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ 180.0,-90.0 ], [ 180.0,-60.0 ], [ -180.0,-60.0 ], [ -180.0,-90.0 ], [ 180.0,-90.0 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"535595a3e4b0120853e8c2aa","contributors":{"authors":[{"text":"Gooseff, Michael N.","contributorId":71880,"corporation":false,"usgs":true,"family":"Gooseff","given":"Michael","email":"","middleInitial":"N.","affiliations":[],"preferred":false,"id":492480,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"McKnight, Diane M.","contributorId":59773,"corporation":false,"usgs":false,"family":"McKnight","given":"Diane","email":"","middleInitial":"M.","affiliations":[{"id":16833,"text":"INSTAAR, University of Colorado","active":true,"usgs":false}],"preferred":false,"id":492478,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Doran, Peter T.","contributorId":67007,"corporation":false,"usgs":true,"family":"Doran","given":"Peter","email":"","middleInitial":"T.","affiliations":[],"preferred":false,"id":492479,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Lyons, W. Berry","contributorId":73497,"corporation":false,"usgs":true,"family":"Lyons","given":"W.","email":"","middleInitial":"Berry","affiliations":[],"preferred":false,"id":492481,"contributorType":{"id":1,"text":"Authors"},"rank":4}]}}
,{"id":70094154,"text":"ofr20071047SRP047 - 2007 - Geophysical survey reveals tectonic structures in the Amundsen Sea embayment, West Antarctica","interactions":[],"lastModifiedDate":"2014-02-18T09:50:56","indexId":"ofr20071047SRP047","displayToPublicDate":"2007-01-01T09:11:00","publicationYear":"2007","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":330,"text":"Open-File Report","code":"OFR","onlineIssn":"2331-1258","printIssn":"0196-1497","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"2007-1047-SRP-047","title":"Geophysical survey reveals tectonic structures in the Amundsen Sea embayment, West Antarctica","docAbstract":"The Amundsen Sea embayment of West Antarctica is in a prominent location for a series of tectonic and magmatic events from Paleozoic to Cenozoic times. Seismic, magnetic and gravity data from the embayment and Pine\nIsland Bay (PIB) reveal the crustal thickness and some tectonic features. The Moho is 24-22 km deep on the shelf. NE-SW trending magnetic and gravity anomalies and the thin crust indicate a former rift zone that was active during or in the run-up to breakup between Chatham Rise and West Antarctica before or at 90 Ma. NW-SE trending gravity and magnetic anomalies, following a prolongation of Peacock Sound, indicate the extensional southern boundary to the Bellingshausen Plate which was active between 79 and 61 Ma.","largerWorkType":{"id":18,"text":"Report"},"largerWorkTitle":"Antarctica: A Keystone in a Changing World--Online Proceedings for the Tenth International Symposium on Antarctic Earth Sciences. Santa Barbara, California, U.S.A.--August 26 to September 1, 2007","largerWorkSubtype":{"id":5,"text":"USGS Numbered Series"},"language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Reston, VA","doi":"10.3133/ofr20071047SRP047","usgsCitation":"Gohl, K., Eagles, G., Netzeband, G., Grobys, J., Parsiegla, N., Schluter, P., Leinweber, V., Larter, R., Uenzelmann-Neben, G., and Udintsev, G., 2007, Geophysical survey reveals tectonic structures in the Amundsen Sea embayment, West Antarctica: U.S. Geological Survey Open-File Report 2007-1047-SRP-047, 4 p., https://doi.org/10.3133/ofr20071047SRP047.","productDescription":"4 p.","additionalOnlineFiles":"N","costCenters":[],"links":[{"id":282461,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/ofr20071047SRP047.JPG"},{"id":282460,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/2007/1047/srp/srp047/of2007-1047srp047.pdf"}],"otherGeospatial":"Antarctica","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -180.0,-90.0 ], [ -180.0,-60.0 ], [ 180.0,-60.0 ], [ 180.0,-90.0 ], [ -180.0,-90.0 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"53cd5ed0e4b0b290850fbecd","contributors":{"authors":[{"text":"Gohl, K.","contributorId":53285,"corporation":false,"usgs":true,"family":"Gohl","given":"K.","email":"","affiliations":[],"preferred":false,"id":490470,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Eagles, G.","contributorId":107196,"corporation":false,"usgs":true,"family":"Eagles","given":"G.","email":"","affiliations":[],"preferred":false,"id":490475,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Netzeband, G.","contributorId":61745,"corporation":false,"usgs":true,"family":"Netzeband","given":"G.","email":"","affiliations":[],"preferred":false,"id":490471,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Grobys, J.W.G.","contributorId":32086,"corporation":false,"usgs":true,"family":"Grobys","given":"J.W.G.","email":"","affiliations":[],"preferred":false,"id":490469,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"Parsiegla, N.","contributorId":11116,"corporation":false,"usgs":true,"family":"Parsiegla","given":"N.","email":"","affiliations":[],"preferred":false,"id":490467,"contributorType":{"id":1,"text":"Authors"},"rank":5},{"text":"Schluter, P.","contributorId":102384,"corporation":false,"usgs":true,"family":"Schluter","given":"P.","email":"","affiliations":[],"preferred":false,"id":490473,"contributorType":{"id":1,"text":"Authors"},"rank":6},{"text":"Leinweber, V.","contributorId":81799,"corporation":false,"usgs":true,"family":"Leinweber","given":"V.","email":"","affiliations":[],"preferred":false,"id":490472,"contributorType":{"id":1,"text":"Authors"},"rank":7},{"text":"Larter, R.D.","contributorId":8765,"corporation":false,"usgs":true,"family":"Larter","given":"R.D.","email":"","affiliations":[],"preferred":false,"id":490466,"contributorType":{"id":1,"text":"Authors"},"rank":8},{"text":"Uenzelmann-Neben, G.","contributorId":22682,"corporation":false,"usgs":true,"family":"Uenzelmann-Neben","given":"G.","email":"","affiliations":[],"preferred":false,"id":490468,"contributorType":{"id":1,"text":"Authors"},"rank":9},{"text":"Udintsev, G.B.","contributorId":106411,"corporation":false,"usgs":true,"family":"Udintsev","given":"G.B.","email":"","affiliations":[],"preferred":false,"id":490474,"contributorType":{"id":1,"text":"Authors"},"rank":10}]}}
,{"id":70094354,"text":"ofr20071047SRP061 - 2007 - Geometrical analysis of structural data collected at high South latitude: A  modular arithmetic method that addresses meridional convergence","interactions":[],"lastModifiedDate":"2014-02-24T12:49:04","indexId":"ofr20071047SRP061","displayToPublicDate":"2007-01-01T09:04:00","publicationYear":"2007","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":330,"text":"Open-File Report","code":"OFR","onlineIssn":"2331-1258","printIssn":"0196-1497","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"2007-1047-SRP-061","title":"Geometrical analysis of structural data collected at high South latitude: A  modular arithmetic method that addresses meridional convergence","docAbstract":"The convergence of meridians toward the South Pole causes unique problems for geometrical comparison of \nstructural geological and geophysical datasets from Antarctica. The true North reference direction ordinarily is used for \nmeasuring and reporting vector data (strike, trend) in Antarctica, as elsewhere. However, over a latitude distance of just \n100 km at 85° South, the angular difference in the true North direction exceeds 10°. Consequently, when performing a \nregional tectonic analysis of vector data (strike, trend) for structures such as faults, dike arrays, or geophysical \nlineaments oriented with respect to North at different sites, it is necessary to rotate the data to a common reference \ndirection. A modular arithmetic function, performed as a spreadsheet calculation, offers the means to unify data sets \nfrom sites having different longitude position, by rotation to a common reference direction. The function is \nS<sub>C</sub> ≡ S<sub>M</sub> + ∆L (mod 360), where SC = converted strike; SM = measured strike; ∆L = angle in degrees longitude between \nreference longitude and study site; and 360, the divisor, is the number of degrees in Earth’s circumference. The method \nis used to evaluate 1) paleomagnetic rotation of the Ellsworth-Whitmore Mountains with respect to the Transantarctic \nMountains, and 2) orogenic curvature of the Ross Orogen","largerWorkType":{"id":18,"text":"Report"},"largerWorkTitle":"Antarctica: A Keystone in a Changing World--Online Proceedings for the Tenth International Symposium on Antarctic Earth Sciences. Santa Barbara, California, U.S.A.--August 26 to September 1, 2007","largerWorkSubtype":{"id":5,"text":"USGS Numbered Series"},"language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Reston, VA","doi":"10.3133/ofr20071047SRP061","usgsCitation":"Siddoway, C., and Siddoway, M., 2007, Geometrical analysis of structural data collected at high South latitude: A  modular arithmetic method that addresses meridional convergence: U.S. Geological Survey Open-File Report 2007-1047-SRP-061, Report: 5 p.; Plate: XLS file, https://doi.org/10.3133/ofr20071047SRP061.","productDescription":"Report: 5 p.; Plate: XLS file","additionalOnlineFiles":"Y","costCenters":[],"links":[{"id":282681,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/ofr20071047SRP061.png"},{"id":282676,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/2007/1047/srp/srp061/of2007-1047srp061.pdf"},{"id":282677,"type":{"id":7,"text":"Companion Files"},"url":"https://pubs.usgs.gov/of/2007/1047/srp/srp061/of2007-1047srp061_plate1.xls"}],"otherGeospatial":"Antarctica","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ 180.0,-90.0 ], [ 180.0,-60.0 ], [ -180.0,-60.0 ], [ -180.0,-90.0 ], [ 180.0,-90.0 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"53cd5e97e4b0b290850fbcc2","contributors":{"authors":[{"text":"Siddoway, C.S.","contributorId":28893,"corporation":false,"usgs":true,"family":"Siddoway","given":"C.S.","email":"","affiliations":[],"preferred":false,"id":490582,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Siddoway, M.F.","contributorId":34425,"corporation":false,"usgs":true,"family":"Siddoway","given":"M.F.","email":"","affiliations":[],"preferred":false,"id":490583,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":70098927,"text":"ofr20071047SRP073 - 2007 - Vertical motions in Northern Victoria Land inferred from GPS: A comparison with a glacial isostatic adjustment model","interactions":[],"lastModifiedDate":"2014-03-19T09:33:39","indexId":"ofr20071047SRP073","displayToPublicDate":"2007-01-01T08:55:00","publicationYear":"2007","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":330,"text":"Open-File Report","code":"OFR","onlineIssn":"2331-1258","printIssn":"0196-1497","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"2007-1047-SRP-073","title":"Vertical motions in Northern Victoria Land inferred from GPS: A comparison with a glacial isostatic adjustment model","docAbstract":"Following the densification of GPS permanent and episodic trackers in Antarctica, geodetic observations \nare playing an increasing role in geodynamics research and the study of the glacial isostatic adjustment (GIA). The \nimprovement in geodetic measurements accuracy suggests their use in constraining GIA models. It is essential to have a \ndeeper knowledge on the sensitivity of GPS data to motionsrelated to long-term ice mass changes and the present-day \nmass imbalance of the ice sheets. In order to investigate the geodynamic phenomena in Northern Victoria Land (NVL), \nGPS geodetic observations were made during the last decade within the VLNDEF (Victoria Land Network for \nDeformation control) project. The processed data provided a picture of the motions occurring in NVL with a high level \nof accuracy and depicts, for the whole period, a well defined pattern of vertical motion. The comparison between GPS-derived vertical displacementsand GIA is addressed, showing a good degree of agreement and highlighting the future \nuse of geodetic GPS measurements as constraints in GIA models. In spite of this agreement, the sensitivity of GPS \nvertical rates to non-GIA vertical motions has to be carefully evaluated.","largerWorkType":{"id":18,"text":"Report"},"largerWorkTitle":"Antarctica: A Keystone in a Changing World--Online Proceedings for the Tenth International Symposium on Antarctic Earth Sciences. Santa Barbara, California, U.S.A.--August 26 to September 1, 2007","largerWorkSubtype":{"id":5,"text":"USGS Numbered Series"},"language":"English","publisher":"U.S Geological Survey","publisherLocation":"Reston, VA","doi":"10.3133/ofr20071047SRP073","usgsCitation":"Mancini, F., Negusini, M., Zanutta, A., and Capra, A., 2007, Vertical motions in Northern Victoria Land inferred from GPS: A comparison with a glacial isostatic adjustment model: U.S. Geological Survey Open-File Report 2007-1047-SRP-073, 5 p., https://doi.org/10.3133/ofr20071047SRP073.","productDescription":"5 p.","additionalOnlineFiles":"N","costCenters":[],"links":[{"id":284198,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/ofr20071047SRP073.PNG"}],"otherGeospatial":"Antarctica","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ 180.0,-90.0 ], [ 180.0,-60.0 ], [ -180.0,-60.0 ], [ -180.0,-90.0 ], [ 180.0,-90.0 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"53cd7b0ee4b0b2908510de5a","contributors":{"authors":[{"text":"Mancini, F.","contributorId":93812,"corporation":false,"usgs":true,"family":"Mancini","given":"F.","email":"","affiliations":[],"preferred":false,"id":491735,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Negusini, M.","contributorId":107185,"corporation":false,"usgs":true,"family":"Negusini","given":"M.","email":"","affiliations":[],"preferred":false,"id":491736,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Zanutta, A.","contributorId":86258,"corporation":false,"usgs":true,"family":"Zanutta","given":"A.","email":"","affiliations":[],"preferred":false,"id":491734,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Capra, A.","contributorId":84662,"corporation":false,"usgs":true,"family":"Capra","given":"A.","email":"","affiliations":[],"preferred":false,"id":491733,"contributorType":{"id":1,"text":"Authors"},"rank":4}]}}
,{"id":70047552,"text":"ds69J6 - 2007 - Burial history, thermal maturity, and oil and gas generation history of petroleum systems in the Wind River Basin Province, central Wyoming: Chapter 6 in <i>Petroleum systems and geologic assessment of oil and gas resources in the Wind River Basin Province, Wyoming</i>","interactions":[],"lastModifiedDate":"2013-08-12T09:13:58","indexId":"ds69J6","displayToPublicDate":"2007-01-01T08:48:00","publicationYear":"2007","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":310,"text":"Data Series","code":"DS","onlineIssn":"2327-638X","printIssn":"2327-0271","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"69-J-6","title":"Burial history, thermal maturity, and oil and gas generation history of petroleum systems in the Wind River Basin Province, central Wyoming: Chapter 6 in <i>Petroleum systems and geologic assessment of oil and gas resources in the Wind River Basin Province, Wyoming</i>","docAbstract":"Burial history, thermal maturity, and timing of oil and gas \ngeneration were modeled for eight key source rock units at \nnine well locations throughout the Wind River Basin Province. \nPetroleum source rocks include the Permian Phosphoria \nFormation, the Cretaceous Mowry Shale, Cody Shale, and \nMesaverde, Meeteetse, and Lance Formations, and the Tertiary \n(Paleocene) Fort Union Formation, including the Waltman \nShale Member. Within the province boundary, the Phosphoria \nis thin and only locally rich in organic carbon. Phosphoria oil \nproduced from reservoirs in the province is thought to have \nmigrated from the Wyoming and Idaho thrust belt. \nLocations (wells) selected for burial history \nreconstructions include three in the deepest parts of the \nprovince (Adams OAB-17, Bighorn 1-5, and Coastal Owl \nCreek); three at intermediate depths (Hells Half Acre, Shell \n33X-10, and West Poison Spider); and three at relatively \nshallow locations (Young Ranch, Amoco Unit 100, and \nConoco-Coal Bank). The thermal maturity of source rocks is \ngreatest in the deep northern and central parts of the province \nand decreases to the south and east toward the basin margins. \nThe results of the modeling indicate that, in the deepest areas, \n(1) peak petroleum generation from Cretaceous rocks occurred \nfrom Late Cretaceous through middle Eocene time, and (2) \nonset of oil generation from the Waltman Shale Member \noccurred from late Eocene to early Miocene time. \nBased on modeling results, gas generation from the \ncracking of Phosphoria oil reservoired in the Park City \nFormation reached a peak in the late Paleocene/early Eocene \n(58 to 55 Ma) only in the deepest parts of the province. The \nMowry Shale and Cody Shale (in the eastern half of the basin) \ncontain a mix of Type-II and Type-III kerogens. Oil generation \nfrom predominantly Type-II source rocks of these units in the \ndeepest parts of the province reached peak rates during the \nlatest Cretaceous to early Eocene (65 to 55 Ma). Only in these \nareas of the basin did these units reach peak gas generation \nfrom the cracking of oil, which occurred in the early to middle \nEocene (55 to 42 Ma). \nGas-prone source rocks of the Mowry and Cody Shales \n(predominantly Type-III kerogen), and the Mesaverde, \nMeeteetse, Lance, and Fort Union Formations (Type –III \nkerogen) reached peak gas generation in the latest Cretaceous \nto late Eocene (67 to 38 Ma) in the deepest parts of the \nprovince. Gas generation from the Mesaverde source rocks \nstarted at all of the modeled locations but reached peak \ngeneration at only the deepest locations and at the Hells Half \nAcre location in the middle Paleocene to early Eocene (59 to \n48 Ma). Also at the deepest locations, peak gas generation \noccurred from the late Paleocene to the early Eocene (57 to \n49 Ma) for the Meeteetse Formation, and during the Eocene \nfor the Lance Formation (55 to 48 Ma) and the Fort Union \nFormation (44 to 38 Ma). \nThe Waltman Shale Member of the Fort Union Formation \ncontains Type-II kerogen. The base of the Waltman reached a \nlevel of thermal maturity to generate oil only at the deep-basin \nlocations (Adams OAB-17 and Bighorn 1-5 locations) in the \nmiddle Eocene to early Miocene (36 to 20 Ma).","largerWorkType":{"id":18,"text":"Report"},"largerWorkTitle":"Petroleum systems and geologic assessment of oil and gas resources in the Wind River Basin Province, Wyoming (Data Series 69-J)","largerWorkSubtype":{"id":5,"text":"USGS Numbered Series"},"language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Reston, VA","doi":"10.3133/ds69J6","collaboration":"This report is Chapter 6 in <i>Petroleum systems and geologic assessment of oil and gas resources in the Wind River Basin Province, Wyoming</i>.  For more information, see: <a href=\"http://pubs.er.usgs.gov/publication/ds69J\" target=\"_blank\">Data Series 69-J</a>.","usgsCitation":"Roberts, L.N., Finn, T.M., Lewan, M., and Kirschbaum, M.A., 2007, Burial history, thermal maturity, and oil and gas generation history of petroleum systems in the Wind River Basin Province, central Wyoming: Chapter 6 in <i>Petroleum systems and geologic assessment of oil and gas resources in the Wind River Basin Province, Wyoming</i>: U.S. Geological Survey Data Series 69-J-6, iv, 26 p., https://doi.org/10.3133/ds69J6.","productDescription":"iv, 26 p.","numberOfPages":"30","costCenters":[{"id":674,"text":"Wind River Basin Province Assessment Team","active":false,"usgs":true}],"links":[{"id":276297,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/ds69j6.png"},{"id":276295,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.usgs.gov/dds/dds-069/dds-069-j/"},{"id":276296,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/dds/dds-069/dds-069-j/REPORTS/69_J_CH_6.pdf"}],"country":"United States","state":"Wyoming","otherGeospatial":"Wind River Basin Province","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -110.1,42.0 ], [ -110.1,44.0 ], [ -106.0,44.0 ], [ -106.0,42.0 ], [ -110.1,42.0 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"520a03e3e4b0026c2bc11ad1","contributors":{"authors":[{"text":"Roberts, Laura N.R.","contributorId":79530,"corporation":false,"usgs":true,"family":"Roberts","given":"Laura","email":"","middleInitial":"N.R.","affiliations":[],"preferred":false,"id":482384,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Finn, Thomas M. 0000-0001-6396-9351 finn@usgs.gov","orcid":"https://orcid.org/0000-0001-6396-9351","contributorId":778,"corporation":false,"usgs":true,"family":"Finn","given":"Thomas","email":"finn@usgs.gov","middleInitial":"M.","affiliations":[{"id":164,"text":"Central Energy Resources Science Center","active":true,"usgs":true}],"preferred":true,"id":482381,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Lewan, Michael D. mlewan@usgs.gov","contributorId":940,"corporation":false,"usgs":true,"family":"Lewan","given":"Michael D.","email":"mlewan@usgs.gov","affiliations":[{"id":164,"text":"Central Energy Resources Science Center","active":true,"usgs":true}],"preferred":false,"id":482382,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Kirschbaum, Mark A.","contributorId":25112,"corporation":false,"usgs":true,"family":"Kirschbaum","given":"Mark","email":"","middleInitial":"A.","affiliations":[],"preferred":false,"id":482383,"contributorType":{"id":1,"text":"Authors"},"rank":4}]}}
,{"id":70203722,"text":"ds310 - 2007 - Archive of digital CHIRP seismic reflection data collected during USGS cruise 06SCC02 offshore of the Chandeleur Islands, Louisiana, July 2006","interactions":[],"lastModifiedDate":"2024-03-28T13:44:08.093827","indexId":"ds310","displayToPublicDate":"2007-01-01T08:40:14","publicationYear":"2007","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":310,"text":"Data Series","code":"DS","onlineIssn":"2327-638X","printIssn":"2327-0271","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"310","title":"Archive of digital CHIRP seismic reflection data collected during USGS cruise 06SCC02 offshore of the Chandeleur Islands, Louisiana, July 2006","docAbstract":"<p>In July of 2006, the U.S. Geological Survey (USGS) conducted a geophysical survey offshore of the Chandeleur Islands, Louisiana, as part of the USGS Barrier Island Coastal Monitoring project (BICM), which is part of a broader study focused on Subsidence and Coastal Change (SCC). This report serves as an archive of unprocessed digital Compressed High Intensity Radar Pulse (CHIRP) seismic reflection data, trackline maps, navigation files, Geographic Information System (GIS) files, Field Activity Collection System (FACS) logs, observer's logbook, and formal Federal Geographic Data Committee (FGDC) metadata. Gained (a relative increase in signal amplitude has been applied) digital images of the seismic profiles are also provided.</p>","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Reston, Virginia","doi":"10.3133/ds310","usgsCitation":"Harrison, A.S., Dadisman, S.V., Flocks, J.G., and Wiese, D.S., 2007, Archive of digital CHIRP seismic reflection data collected during USGS cruise 06SCC02 offshore of the Chandeleur Islands, Louisiana, July 2006: U.S. Geological Survey Data Series 310, HTML Document; DVD-ROM, https://doi.org/10.3133/ds310.","productDescription":"HTML Document; DVD-ROM","costCenters":[{"id":574,"text":"St. Petersburg Coastal and Marine Science Center","active":true,"usgs":true}],"links":[{"id":364457,"rank":2,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":427109,"rank":1,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.usgs.gov/ds/310/","text":"Index Page","linkFileType":{"id":5,"text":"html"}}],"country":"United States","state":"Louisiana","otherGeospatial":"Chandeleur Islands","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"coordinates\": [\n          [\n            [\n              -88.97638843437915,\n              29.63123061994284\n            ],\n            [\n              -88.8427472203541,\n              29.764247592634817\n            ],\n            [\n              -88.80933691684783,\n              29.893065321154907\n            ],\n            [\n              -88.8139772367792,\n              29.98394268222883\n            ],\n            [\n              -88.86873301196997,\n              30.056263445613283\n            ],\n            [\n              -88.87986977980538,\n              30.021716772371022\n            ],\n            [\n              -88.8427472203541,\n              29.90835138980472\n            ],\n            [\n              -88.88729429169578,\n              29.82384643207277\n            ],\n            [\n              -88.917920403243,\n              29.747327944632474\n            ],\n            [\n              -89.00794260991272,\n              29.652202556506026\n            ],\n            [\n              -89.01815131376178,\n              29.633650681696338\n            ],\n            [\n              -88.97638843437915,\n              29.63123061994284\n            ]\n          ]\n        ],\n        \"type\": \"Polygon\"\n      }\n    }\n  ]\n}","contact":"<p><a href=\"https://pubs.er.usgs.gov/contact\" data-mce-href=\"https://pubs.er.usgs.gov/contact\">Contact Pubs Warehouse</a></p>","tableOfContents":"<ul><li>Information Statement</li><li>System Requirements</li><li>Project Summary</li><li>Disc Organization</li><li>Getting Started</li><li>Acknowledgments</li><li>References Cited</li></ul>","publishingServiceCenter":{"id":9,"text":"Reston PSC"},"noUsgsAuthors":false,"publicationStatus":"PW","contributors":{"authors":[{"text":"Harrison, Arnell S. 0000-0002-5581-2255","orcid":"https://orcid.org/0000-0002-5581-2255","contributorId":35021,"corporation":false,"usgs":true,"family":"Harrison","given":"Arnell","email":"","middleInitial":"S.","affiliations":[],"preferred":false,"id":763811,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Dadisman, Shawn V. sdadisman@usgs.gov","contributorId":2207,"corporation":false,"usgs":true,"family":"Dadisman","given":"Shawn","email":"sdadisman@usgs.gov","middleInitial":"V.","affiliations":[],"preferred":true,"id":763812,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Flocks, James G. 0000-0002-6177-7433 jflocks@usgs.gov","orcid":"https://orcid.org/0000-0002-6177-7433","contributorId":816,"corporation":false,"usgs":true,"family":"Flocks","given":"James","email":"jflocks@usgs.gov","middleInitial":"G.","affiliations":[{"id":574,"text":"St. Petersburg Coastal and Marine Science Center","active":true,"usgs":true}],"preferred":true,"id":763813,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Wiese, Dana S. dwiese@usgs.gov","contributorId":2476,"corporation":false,"usgs":true,"family":"Wiese","given":"Dana","email":"dwiese@usgs.gov","middleInitial":"S.","affiliations":[{"id":574,"text":"St. Petersburg Coastal and Marine Science Center","active":true,"usgs":true}],"preferred":true,"id":763814,"contributorType":{"id":1,"text":"Authors"},"rank":4}]}}
,{"id":70029973,"text":"70029973 - 2007 - Chromosome painting among Proboscidea, Hyracoidea and Sirenia: Support for Paenungulata (Afrotheria, Mammalia) but not Tethytheria","interactions":[],"lastModifiedDate":"2012-03-12T17:21:09","indexId":"70029973","displayToPublicDate":"2007-01-01T00:00:00","publicationYear":"2007","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":3174,"text":"Proceedings of the Royal Society B: Biological Sciences","active":true,"publicationSubtype":{"id":10}},"title":"Chromosome painting among Proboscidea, Hyracoidea and Sirenia: Support for Paenungulata (Afrotheria, Mammalia) but not Tethytheria","docAbstract":"Despite marked improvements in the interpretation of systematic relationships within Eutheria, particular nodes, including Paenungulata (Hyracoidea, Sirenia and Proboscidea), remain ambiguous. The combination of a rapid radiation, a deep divergence and an extensive morphological diversification has resulted in a limited phylogenetic signal confounding resolution within this clade both at the morphological and nucleotide levels. Cross-species chromosome painting was used to delineate regions of homology between Loxodonta africana (2n = 56), Procavia capensis (2n=54), Trichechus manatus latirostris (2n = 48) and an outgroup taxon, the aardvark (Orycteropus afer, 2n = 20). Changes specific to each lineage were identified and although the presence of a minimum of 11 synapomorphies confirmed the monophyly of Paenungulata, no change characterizing intrapaenungulate relationships was evident. The reconstruction of an ancestral paenungulate karyotype and the estimation of rates of chromosomal evolution indicate a reduced rate of genomic repatterning following the paenungulate radiation. In comparison to data available for other mammalian taxa, the paenungulate rate of chromosomal evolution is slow to moderate. As a consequence, the absence of a chromosomal character uniting two paenungulates (at the level of resolution characterized in this study) may be due to a reduced rate of chromosomal change relative to the length of time separating successive divergence events. ?? 2007 The Royal Society.","largerWorkType":{"id":2,"text":"Article"},"largerWorkTitle":"Proceedings of the Royal Society B: Biological Sciences","largerWorkSubtype":{"id":10,"text":"Journal Article"},"language":"English","doi":"10.1098/rspb.2007.0088","issn":"09628436","usgsCitation":"Pardini, A., O’Brien, P.C., Fu, B., Bonde, R., Elder, F., Ferguson-Smith, M.A., Yang, F., and Robinson, T., 2007, Chromosome painting among Proboscidea, Hyracoidea and Sirenia: Support for Paenungulata (Afrotheria, Mammalia) but not Tethytheria: Proceedings of the Royal Society B: Biological Sciences, v. 274, no. 1615, p. 1333-1340, https://doi.org/10.1098/rspb.2007.0088.","startPage":"1333","endPage":"1340","numberOfPages":"8","costCenters":[],"links":[{"id":477288,"rank":10000,"type":{"id":40,"text":"Open Access Publisher Index Page"},"url":"https://doi.org/10.1098/rspb.2007.0088","text":"Publisher Index Page"},{"id":240359,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"},{"id":212815,"rank":9999,"type":{"id":10,"text":"Digital Object Identifier"},"url":"https://dx.doi.org/10.1098/rspb.2007.0088"}],"volume":"274","issue":"1615","noUsgsAuthors":false,"publicationDate":"2007-03-20","publicationStatus":"PW","scienceBaseUri":"5059f5e9e4b0c8380cd4c4ac","contributors":{"authors":[{"text":"Pardini, A.T.","contributorId":57664,"corporation":false,"usgs":true,"family":"Pardini","given":"A.T.","email":"","affiliations":[],"preferred":false,"id":425133,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"O’Brien, P. C. M.","contributorId":55643,"corporation":false,"usgs":true,"family":"O’Brien","given":"P.","email":"","middleInitial":"C. M.","affiliations":[],"preferred":false,"id":425132,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Fu, B.","contributorId":30825,"corporation":false,"usgs":true,"family":"Fu","given":"B.","email":"","affiliations":[],"preferred":false,"id":425131,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Bonde, R. K. 0000-0001-9179-4376","orcid":"https://orcid.org/0000-0001-9179-4376","contributorId":63339,"corporation":false,"usgs":true,"family":"Bonde","given":"R. K.","affiliations":[],"preferred":false,"id":425136,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"Elder, F.F.B.","contributorId":60022,"corporation":false,"usgs":true,"family":"Elder","given":"F.F.B.","email":"","affiliations":[],"preferred":false,"id":425134,"contributorType":{"id":1,"text":"Authors"},"rank":5},{"text":"Ferguson-Smith, M. A.","contributorId":18180,"corporation":false,"usgs":true,"family":"Ferguson-Smith","given":"M.","email":"","middleInitial":"A.","affiliations":[],"preferred":false,"id":425129,"contributorType":{"id":1,"text":"Authors"},"rank":6},{"text":"Yang, F.","contributorId":23326,"corporation":false,"usgs":true,"family":"Yang","given":"F.","email":"","affiliations":[],"preferred":false,"id":425130,"contributorType":{"id":1,"text":"Authors"},"rank":7},{"text":"Robinson, T.J.","contributorId":62836,"corporation":false,"usgs":true,"family":"Robinson","given":"T.J.","email":"","affiliations":[],"preferred":false,"id":425135,"contributorType":{"id":1,"text":"Authors"},"rank":8}]}}
,{"id":80532,"text":"fs20073059 - 2007 - Chronic Wasting Disease Positive Tissue Bank","interactions":[],"lastModifiedDate":"2012-02-02T00:14:14","indexId":"fs20073059","displayToPublicDate":"2007-01-01T00:00:00","publicationYear":"2007","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":313,"text":"Fact Sheet","code":"FS","onlineIssn":"2327-6932","printIssn":"2327-6916","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"2007-3059","title":"Chronic Wasting Disease Positive Tissue Bank","docAbstract":"In 2005, the USGS National Wildlife Health Center entered into an agreement with the Wyoming Game and Fish Department and the Department of Veterinary Sciences at the University of Wyoming to produce a collection of positive tissues from cervids intentionally infected with chronic wasting disease. This agreement was facilitated through the University of Wyoming Cooperative Fish and Wildlife Unit.\r\n\r\nAlso, the investigators on this project sampled the animals incrementally over 2 years to show changes over time, and examined tissues from the animals by immunohistochemistry. CWD positive tissues are catalogued by species, sample site and time of infection. These data and more will soon be published.","language":"ENGLISH","publisher":"Geological Survey (U.S.)","doi":"10.3133/fs20073059","usgsCitation":"Wright, S.D., 2007, Chronic Wasting Disease Positive Tissue Bank: U.S. Geological Survey Fact Sheet 2007-3059, 1 p., https://doi.org/10.3133/fs20073059.","productDescription":"1 p.","startPage":"1","endPage":"1","numberOfPages":"1","costCenters":[{"id":456,"text":"National Wildlife Health Center","active":true,"usgs":true}],"links":[{"id":120908,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/fs_2007_3059.jpg"},{"id":10372,"rank":100,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.usgs.gov/fs/2007/3059/","linkFileType":{"id":5,"text":"html"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e49dde4b07f02db5e219a","contributors":{"authors":[{"text":"Wright, Scott D.","contributorId":45006,"corporation":false,"usgs":true,"family":"Wright","given":"Scott","email":"","middleInitial":"D.","affiliations":[],"preferred":false,"id":292849,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":70180392,"text":"70180392 - 2007 - USGS national surveys and analysis projects: Preliminary compilation of integrated geological datasets for the United States: A section in <i>Digital mapping techniques '06 - Workshop proceedings</i>","interactions":[{"subject":{"id":70180392,"text":"70180392 - 2007 - USGS national surveys and analysis projects: Preliminary compilation of integrated geological datasets for the United States: A section in <i>Digital mapping techniques '06 - Workshop proceedings</i>","indexId":"70180392","publicationYear":"2007","noYear":false,"title":"USGS national surveys and analysis projects: Preliminary compilation of integrated geological datasets for the United States: A section in <i>Digital mapping techniques '06 - Workshop proceedings</i>"},"predicate":"IS_PART_OF","object":{"id":81245,"text":"ofr20071285 - 2007 - Digital mapping techniques '06 - Workshop proceedings","indexId":"ofr20071285","publicationYear":"2007","noYear":false,"title":"Digital mapping techniques '06 - Workshop proceedings"},"id":1}],"isPartOf":{"id":81245,"text":"ofr20071285 - 2007 - Digital mapping techniques '06 - Workshop proceedings","indexId":"ofr20071285","publicationYear":"2007","noYear":false,"title":"Digital mapping techniques '06 - Workshop proceedings"},"lastModifiedDate":"2017-01-30T08:30:56","indexId":"70180392","displayToPublicDate":"2007-01-01T00:00:00","publicationYear":"2007","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":330,"text":"Open-File Report","code":"OFR","onlineIssn":"2331-1258","printIssn":"0196-1497","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"2007-1285","title":"USGS national surveys and analysis projects: Preliminary compilation of integrated geological datasets for the United States: A section in <i>Digital mapping techniques '06 - Workshop proceedings</i>","docAbstract":"<p>The growth in the use of Geographic Information Systems (GIS) has highlighted the need for regional and national digital geologic maps attributed with age and rock type information. Such spatial data can be conveniently used to generate derivative maps for purposes that include mineral-resource assessment, metallogenic studies, tectonic studies, human health and environmental research.</p><p>In 1997, the United States Geological Survey’s Mineral Resources Program initiated an effort to develop national digital databases for use in mineral resource and environmental assessments. One primary activity of this effort was to compile a national digital geologic map database, utilizing state geologic maps, to support mineral resource studies in the range of 1:250,000- to 1:1,000,000-scale. Over the course of the past decade, state databases were prepared using a common standard for the database structure, fields, attributes, and data dictionaries. As of late 2006, standardized geological map databases for all conterminous (CONUS) states have been available on-line as USGS Open-File Reports. For Alaska and Hawaii, new state maps are being prepared, and the preliminary work for Alaska is being released as a series of 1:500,000-scale regional compilations. See below for a list of all published databases.</p>","largerWorkType":{"id":18,"text":"Report"},"largerWorkTitle":"Digital mapping techniques '06 - Workshop proceedings (Open-File Report 2007-1285)","largerWorkSubtype":{"id":5,"text":"USGS Numbered Series"},"conferenceTitle":"Digital mapping techniques '06","conferenceDate":"June 11-14, 2006","conferenceLocation":"Columbus, OH","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Reston, VA","doi":"10.3133/70180392","usgsCitation":"Nicholson, S.W., Stoeser, D.B., Wilson, F.H., Dicken, C., and Ludington, S., 2007, USGS national surveys and analysis projects: Preliminary compilation of integrated geological datasets for the United States: A section in <i>Digital mapping techniques '06 - Workshop proceedings</i>: U.S. Geological Survey Open-File Report 2007-1285, 5 p., https://doi.org/10.3133/70180392.","productDescription":"5 p.","startPage":"203","endPage":"207","numberOfPages":"7","costCenters":[{"id":114,"text":"Alaska Science Center","active":true,"usgs":true},{"id":171,"text":"Central Mineral and Environmental Resources Science Center","active":true,"usgs":true},{"id":245,"text":"Eastern Mineral and Environmental Resources Science Center","active":true,"usgs":true},{"id":312,"text":"Geology, Minerals, Energy, and Geophysics Science Center","active":true,"usgs":true},{"id":596,"text":"U.S. Geological Survey National Center","active":false,"usgs":true}],"links":[{"id":334260,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"},{"id":334258,"rank":1,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.usgs.gov/of/2007/1285/contents.html","text":"Index Page for Larger Work"},{"id":334259,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/2007/1285/pdf/Nicholson.pdf"}],"country":"United States","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"588f0d73e4b072a7ac08c125","contributors":{"authors":[{"text":"Nicholson, Suzanne W. 0000-0002-9365-1894 swnich@usgs.gov","orcid":"https://orcid.org/0000-0002-9365-1894","contributorId":880,"corporation":false,"usgs":true,"family":"Nicholson","given":"Suzanne","email":"swnich@usgs.gov","middleInitial":"W.","affiliations":[],"preferred":true,"id":661511,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Stoeser, Douglas B. dstoeser@usgs.gov","contributorId":1821,"corporation":false,"usgs":true,"family":"Stoeser","given":"Douglas","email":"dstoeser@usgs.gov","middleInitial":"B.","affiliations":[{"id":171,"text":"Central Mineral and Environmental Resources Science Center","active":true,"usgs":true}],"preferred":true,"id":661512,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Wilson, Frederic H. 0000-0003-1761-6437 fwilson@usgs.gov","orcid":"https://orcid.org/0000-0003-1761-6437","contributorId":67174,"corporation":false,"usgs":true,"family":"Wilson","given":"Frederic","email":"fwilson@usgs.gov","middleInitial":"H.","affiliations":[{"id":119,"text":"Alaska Science Center Geology Minerals","active":true,"usgs":true},{"id":114,"text":"Alaska Science Center","active":true,"usgs":true}],"preferred":true,"id":661513,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Dicken, Connie L. cdicken@usgs.gov","contributorId":4714,"corporation":false,"usgs":true,"family":"Dicken","given":"Connie L.","email":"cdicken@usgs.gov","affiliations":[{"id":245,"text":"Eastern Mineral and Environmental Resources Science Center","active":true,"usgs":true}],"preferred":false,"id":661514,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"Ludington, Stephen 0000-0002-6265-4996 slud@usgs.gov","orcid":"https://orcid.org/0000-0002-6265-4996","contributorId":172672,"corporation":false,"usgs":true,"family":"Ludington","given":"Stephen","email":"slud@usgs.gov","affiliations":[{"id":312,"text":"Geology, Minerals, Energy, and Geophysics Science Center","active":true,"usgs":true}],"preferred":true,"id":661515,"contributorType":{"id":1,"text":"Authors"},"rank":5}]}}
,{"id":70174801,"text":"70174801 - 2007 - Seabirds as indicators of marine food supplies: Cairns revisited","interactions":[],"lastModifiedDate":"2016-08-22T15:08:26","indexId":"70174801","displayToPublicDate":"2007-01-01T00:00:00","publicationYear":"2007","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":2663,"text":"Marine Ecology Progress Series","active":true,"publicationSubtype":{"id":10}},"title":"Seabirds as indicators of marine food supplies: Cairns revisited","docAbstract":"<p><span>In his seminal paper about using seabirds as indicators of marine food supplies, Cairns (1987, Biol Oceanogr 5:261&ndash;271) predicted that (1) parameters of seabird biology and behavior would vary in curvilinear fashion with changes in food supply, (2) the threshold of prey density over which birds responded would be different for each parameter, and (3) different seabird species would respond differently to variation in food availability depending on foraging behavior and ability to adjust time budgets. We tested these predictions using data collected at colonies of common murre&nbsp;</span><i>Uria aalge</i><span>&nbsp;and black-legged kittiwake&nbsp;</span><i>Rissa tridactyla</i><span>&nbsp;in Cook Inlet, Alaska. (1) Of 22 seabird responses fitted with linear and non-linear functions, 16 responses exhibited significant curvilinear shapes, and Akaike&rsquo;s information criterion (AIC) analysis indicated that curvilinear functions provided the best-fitting model for 12 of those. (2) However, there were few differences among parameters in their threshold to prey density, presumably because most responses ultimately depend upon a single threshold for prey acquisition at sea. (3) There were similarities and some differences in how species responded to variability in prey density. Both murres and kittiwakes minimized variability (CV &lt; 15%) in their own body condition and growth of chicks in the face of high annual variability (CV = 69%) in local prey density. Whereas kittiwake breeding success (CV = 63%, r</span><sup><span>2</span></sup><span>&nbsp;= 0.89) reflected prey variability, murre breeding success did not (CV = 29%, r</span><sup><span>2</span></sup><span>&lt; 0.00). It appears that murres were able to buffer breeding success by reallocating discretionary &lsquo;loafing&rsquo; time to foraging effort in response (r</span><sup><span>2</span></sup><span>&nbsp;= 0.64) to declining prey density. Kittiwakes had little or no discretionary time, so fledging success was a more direct function of local prey density. Implications of these results for using &lsquo;seabirds as indicators&rsquo; are discussed.</span></p>","language":"English","publisher":"Inter-Research","publisherLocation":"Oldendorf/Luhe, Germany","doi":"10.3354/meps07078","issn":"0171-8630","usgsCitation":"Piatt, J.F., Harding, A., Shultz, M.T., Speckman, S., van Pelt, T.I., Drew, G.S., and Kettle, A.B., 2007, Seabirds as indicators of marine food supplies: Cairns revisited: Marine Ecology Progress Series, v. 352, p. 221-234, https://doi.org/10.3354/meps07078.","productDescription":"14 p.","startPage":"221","endPage":"234","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[{"id":114,"text":"Alaska Science Center","active":true,"usgs":true}],"links":[{"id":476939,"rank":0,"type":{"id":40,"text":"Open Access Publisher Index Page"},"url":"https://doi.org/10.3354/meps07078","text":"Publisher Index Page"},{"id":325329,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"352","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"578a0932e4b0c1aacab7d43a","contributors":{"authors":[{"text":"Piatt, John F. 0000-0002-4417-5748 jpiatt@usgs.gov","orcid":"https://orcid.org/0000-0002-4417-5748","contributorId":3025,"corporation":false,"usgs":true,"family":"Piatt","given":"John","email":"jpiatt@usgs.gov","middleInitial":"F.","affiliations":[{"id":114,"text":"Alaska Science Center","active":true,"usgs":true},{"id":116,"text":"Alaska Science Center Biology MFEB","active":true,"usgs":true},{"id":117,"text":"Alaska Science Center Biology WTEB","active":true,"usgs":true}],"preferred":true,"id":642625,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Harding, Ann","contributorId":172489,"corporation":false,"usgs":false,"family":"Harding","given":"Ann","email":"","affiliations":[],"preferred":false,"id":642626,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Shultz, Michael T.","contributorId":172925,"corporation":false,"usgs":false,"family":"Shultz","given":"Michael","email":"","middleInitial":"T.","affiliations":[],"preferred":false,"id":642627,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Speckman, Suzann G.","contributorId":88217,"corporation":false,"usgs":true,"family":"Speckman","given":"Suzann G.","affiliations":[],"preferred":false,"id":642628,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"van Pelt, Thomas I.","contributorId":13392,"corporation":false,"usgs":true,"family":"van Pelt","given":"Thomas","email":"","middleInitial":"I.","affiliations":[{"id":114,"text":"Alaska Science Center","active":true,"usgs":true}],"preferred":false,"id":642629,"contributorType":{"id":1,"text":"Authors"},"rank":5},{"text":"Drew, Gary S. 0000-0002-6789-0891 gdrew@usgs.gov","orcid":"https://orcid.org/0000-0002-6789-0891","contributorId":3311,"corporation":false,"usgs":true,"family":"Drew","given":"Gary","email":"gdrew@usgs.gov","middleInitial":"S.","affiliations":[{"id":116,"text":"Alaska Science Center Biology MFEB","active":true,"usgs":true},{"id":114,"text":"Alaska Science Center","active":true,"usgs":true}],"preferred":true,"id":642630,"contributorType":{"id":1,"text":"Authors"},"rank":6},{"text":"Kettle, Arthur B.","contributorId":98064,"corporation":false,"usgs":false,"family":"Kettle","given":"Arthur","email":"","middleInitial":"B.","affiliations":[],"preferred":false,"id":642631,"contributorType":{"id":1,"text":"Authors"},"rank":7}]}}
,{"id":70032113,"text":"70032113 - 2007 - Relationships between reef fish communities and remotely sensed rugosity measurements in Biscayne National Park, Florida, USA","interactions":[],"lastModifiedDate":"2014-09-02T09:35:34","indexId":"70032113","displayToPublicDate":"2007-01-01T00:00:00","publicationYear":"2007","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1528,"text":"Environmental Biology of Fishes","active":true,"publicationSubtype":{"id":10}},"title":"Relationships between reef fish communities and remotely sensed rugosity measurements in Biscayne National Park, Florida, USA","docAbstract":"<p>The realization that coral reef ecosystem management must occur across multiple spatial scales and habitat types has led scientists and resource managers to seek variables that are easily measured over large areas and correlate well with reef resources. Here we investigate the utility of new technology in airborne laser surveying (NASA Experimental Advanced Airborne Research Lidar (EAARL)) in assessing topographical complexity (rugosity) to predict reef fish community structure on shallow (<10 m deep) patch reefs. Marine portions of Biscayne National Park, Florida, USA, were surveyed remotely using the EAARL, and reef fish populations were visually surveyed on 10 patch reefs at independent, randomly selected stations (<i>n</i> = 10–13 per reef). Rugosity at each station was assessed in situ by divers using the traditional chain-transect method (10-m scale), and remotely using the EAARL submarine topography data at multiple spatial scales (2, 5, and 10 m). The rugosity and biological datasets were analyzed together to elucidate the predictive power of EAARL rugosity in describing the variance in reef fish community variables and to assess the correlation between chain-transect and EAARL rugosity. EAARL rugosity was not well correlated with chain-transect rugosity, or with species richness of fishes (although statistically significant, the amount of variance explained by the model was very low). Variance in reef fish community attributes was better explained in reef-by-reef variability than by physical variables. However, once the reef-by-reef variability was taken into account in a two-way analysis of variance, the importance of rugosity could be seen on individual reefs. Fish species richness and abundance were statistically higher at high rugosity stations compared to medium and low rugosity stations, as predicted by prior ecological research. The EAARL shows promise as an important mapping tool for reef resource managers as they strive to inventory and protect coral reef resources.</p>","largerWorkType":{"id":2,"text":"Article"},"largerWorkTitle":"Environmental Biology of Fishes","largerWorkSubtype":{"id":10,"text":"Journal Article"},"language":"English","publisher":"Springer","doi":"10.1007/s10641-006-9078-4","issn":"03781909","usgsCitation":"Kuffner, I.B., Brock, J., Grober-Dunsmore, R., Bonito, V.E., Hickey, T.D., and Wright, C.W., 2007, Relationships between reef fish communities and remotely sensed rugosity measurements in Biscayne National Park, Florida, USA: Environmental Biology of Fishes, v. 78, no. 1, p. 71-82, https://doi.org/10.1007/s10641-006-9078-4.","productDescription":"12 p.","startPage":"71","endPage":"82","numberOfPages":"12","costCenters":[{"id":186,"text":"Coastal and Marine Geology Program","active":true,"usgs":true}],"links":[{"id":214594,"rank":9999,"type":{"id":10,"text":"Digital Object Identifier"},"url":"https://dx.doi.org/10.1007/s10641-006-9078-4"},{"id":242333,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United States","state":"Florida","otherGeospatial":"Biscayne National Park","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -80.347196,25.291431 ], [ -80.347196,25.671111 ], [ -80.089407,25.671111 ], [ -80.089407,25.291431 ], [ -80.347196,25.291431 ] ] ] } } ] }","volume":"78","issue":"1","noUsgsAuthors":false,"publicationDate":"2006-07-08","publicationStatus":"PW","scienceBaseUri":"505aa64fe4b0c8380cd84db1","contributors":{"authors":[{"text":"Kuffner, Ilsa B. 0000-0001-8804-7847 ikuffner@usgs.gov","orcid":"https://orcid.org/0000-0001-8804-7847","contributorId":3105,"corporation":false,"usgs":true,"family":"Kuffner","given":"Ilsa","email":"ikuffner@usgs.gov","middleInitial":"B.","affiliations":[{"id":574,"text":"St. Petersburg Coastal and Marine Science Center","active":true,"usgs":true}],"preferred":true,"id":434592,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Brock, John 0000-0002-5289-9332 jbrock@usgs.gov","orcid":"https://orcid.org/0000-0002-5289-9332","contributorId":2261,"corporation":false,"usgs":true,"family":"Brock","given":"John","email":"jbrock@usgs.gov","affiliations":[{"id":5061,"text":"National Cooperative Geologic Mapping and Landslide Hazards","active":true,"usgs":true}],"preferred":true,"id":434591,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Grober-Dunsmore, Rikki","contributorId":71292,"corporation":false,"usgs":true,"family":"Grober-Dunsmore","given":"Rikki","email":"","affiliations":[],"preferred":false,"id":434594,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Bonito, Victor E.","contributorId":84994,"corporation":false,"usgs":true,"family":"Bonito","given":"Victor","email":"","middleInitial":"E.","affiliations":[],"preferred":false,"id":434596,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"Hickey, T. Donald","contributorId":71782,"corporation":false,"usgs":true,"family":"Hickey","given":"T.","email":"","middleInitial":"Donald","affiliations":[],"preferred":false,"id":434595,"contributorType":{"id":1,"text":"Authors"},"rank":5},{"text":"Wright, C. Wayne wwright@usgs.gov","contributorId":57422,"corporation":false,"usgs":true,"family":"Wright","given":"C.","email":"wwright@usgs.gov","middleInitial":"Wayne","affiliations":[],"preferred":false,"id":434593,"contributorType":{"id":1,"text":"Authors"},"rank":6}]}}
,{"id":70031107,"text":"70031107 - 2007 - Revised landsat-5 thematic mapper radiometric calibration","interactions":[],"lastModifiedDate":"2017-04-14T13:23:14","indexId":"70031107","displayToPublicDate":"2007-01-01T00:00:00","publicationYear":"2007","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1940,"text":"IEEE Geoscience and Remote Sensing Letters","active":true,"publicationSubtype":{"id":10}},"title":"Revised landsat-5 thematic mapper radiometric calibration","docAbstract":"<p><span>Effective April 2, 2007, the radiometric calibration of Landsat-5 (L5) Thematic Mapper (TM) data that are processed and distributed by the U.S. Geological Survey (USGS) Center for Earth Resources Observation and Science (EROS) will be updated. The lifetime gain model that was implemented on May 5, 2003, for the reflective bands (1-5, 7) will be replaced by a new lifetime radiometric-calibration curve that is derived from the instrument's response to pseudoinvariant desert sites and from cross calibration with the Landsat-7 (L7) Enhanced TM Plus (ETM+). Although this calibration update applies to all archived and future L5 TM data, the principal improvements in the calibration are for the data acquired during the first eight years of the mission (1984-1991), where the changes in the instrument-gain values are as much as 15%. The radiometric scaling coefficients for bands 1 and 2 for approximately the first eight years of the mission have also been changed. Users will need to apply these new coefficients to convert the calibrated data product digital numbers to radiance. The scaling coefficients for the other bands have not changed.</span></p>","language":"English","publisher":"IEEE","doi":"10.1109/LGRS.2007.898285","issn":"1545598X","usgsCitation":"Chander, G., Markham, B.L., and Barsi, J., 2007, Revised landsat-5 thematic mapper radiometric calibration: IEEE Geoscience and Remote Sensing Letters, v. 4, no. 3, p. 490-494, https://doi.org/10.1109/LGRS.2007.898285.","productDescription":"5 p.","startPage":"490","endPage":"494","numberOfPages":"5","costCenters":[{"id":222,"text":"Earth Resources Observation and Science (EROS) Center","active":true,"usgs":true}],"links":[{"id":238875,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"},{"id":211568,"rank":9999,"type":{"id":10,"text":"Digital Object Identifier"},"url":"https://dx.doi.org/10.1109/LGRS.2007.898285"}],"volume":"4","issue":"3","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"505aacc4e4b0c8380cd86dc5","contributors":{"authors":[{"text":"Chander, G.","contributorId":51449,"corporation":false,"usgs":true,"family":"Chander","given":"G.","affiliations":[],"preferred":false,"id":430063,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Markham, B. L.","contributorId":88872,"corporation":false,"usgs":true,"family":"Markham","given":"B.","email":"","middleInitial":"L.","affiliations":[],"preferred":false,"id":430064,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Barsi, J. A.","contributorId":24085,"corporation":false,"usgs":true,"family":"Barsi","given":"J. A.","affiliations":[],"preferred":false,"id":430062,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":70031114,"text":"70031114 - 2007 - Quantifying fluid and bed dynamics for characterizing benthic physical habitat in large rivers","interactions":[],"lastModifiedDate":"2016-06-01T15:19:29","indexId":"70031114","displayToPublicDate":"2007-01-01T00:00:00","publicationYear":"2007","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":2166,"text":"Journal of Applied Ichthyology","active":true,"publicationSubtype":{"id":10}},"title":"Quantifying fluid and bed dynamics for characterizing benthic physical habitat in large rivers","docAbstract":"<p>Sturgeon use benthic habitats in and adjacent to main channels where environmental conditions can include bedload sediment transport and high near-bed flow velocities. Bed velocity measurements obtained with acoustic Doppler instruments provide a means to assess the concentration and velocity of sediment moving near the streambed, and are thus indicative of the bedload sediment transport rate, the near-bed flow velocity, and the stability of the substrate. Acoustic assessments of benthic conditions in the Missouri River were conducted at scales ranging from the stream reach to individual bedforms. Reach-scale results show that spatially-averaged bed velocities in excess of 0.5 m s-1 frequently occur in the navigation channel. At the local scale, bed velocities are highest near bedform crests, and lowest in the troughs. Low-velocity zones can persist in areas with extremely high mean bed velocities. Use of these low-velocity zones may allow sturgeon to make use of portions of the channel where the average conditions near the bed are severe. To obtain bed velocity measurements of the highest possible quality, it is necessary to extract bottom-track and GPS velocity information from the raw ADCP data files on a ping-by-ping basis. However, bed velocity measured from a point can also be estimated using a simplified method that is more easily implemented in the context of routine monitoring. The method requires only the transect distance and direction data displayed in standard ADCP data-logging software. Bed velocity estimates obtained using this method are usually within 5-10% of estimates obtained from ping-by-ping processing. ?? 2007 Blackwell Verlag.</p>","language":"English","publisher":"Wiley","doi":"10.1111/j.1439-0426.2007.00888.x","issn":"01758659","usgsCitation":"Gaeuman, D., and Jacobson, R., 2007, Quantifying fluid and bed dynamics for characterizing benthic physical habitat in large rivers: Journal of Applied Ichthyology, v. 23, no. 4, p. 359-364, https://doi.org/10.1111/j.1439-0426.2007.00888.x.","productDescription":"6 p.","startPage":"359","endPage":"364","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[{"id":192,"text":"Columbia Environmental Research Center","active":true,"usgs":true}],"links":[{"id":477096,"rank":10000,"type":{"id":40,"text":"Open Access Publisher Index Page"},"url":"https://doi.org/10.1111/j.1439-0426.2007.00888.x","text":"Publisher Index Page"},{"id":238945,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"},{"id":211625,"rank":9999,"type":{"id":10,"text":"Digital Object Identifier"},"url":"https://dx.doi.org/10.1111/j.1439-0426.2007.00888.x"}],"volume":"23","issue":"4","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"505a91cbe4b0c8380cd80474","contributors":{"authors":[{"text":"Gaeuman, D.","contributorId":73807,"corporation":false,"usgs":true,"family":"Gaeuman","given":"D.","email":"","affiliations":[],"preferred":false,"id":430091,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Jacobson, R. B. 0000-0002-8368-2064","orcid":"https://orcid.org/0000-0002-8368-2064","contributorId":92614,"corporation":false,"usgs":true,"family":"Jacobson","given":"R. B.","affiliations":[{"id":192,"text":"Columbia Environmental Research Center","active":true,"usgs":true}],"preferred":true,"id":430092,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":70031112,"text":"70031112 - 2007 - Use of a wetland index to evaluate changes in riparian vegetation after livestock exclusion","interactions":[],"lastModifiedDate":"2015-12-16T14:26:48","indexId":"70031112","displayToPublicDate":"2007-01-01T00:00:00","publicationYear":"2007","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":2529,"text":"Journal of the American Water Resources Association","active":true,"publicationSubtype":{"id":10}},"title":"Use of a wetland index to evaluate changes in riparian vegetation after livestock exclusion","docAbstract":"<p>A method was developed to characterize ecological integrity of riparian sites based on the abundance of hydric species. This wetland index can be calculated with species data, or with community type data as performed here. Classified riparian community types were used to describe vegetation at 14 livestock exclosures and adjacent grazed areas. Community type wetland index values were generated and used to calculate site wetland index values. It was hypothesized that removal of livestock would result in higher wetland index values because of release from herbivory and decreased physical disturbance of vegetation, streambanks, and soil. The wetland index for exclosures was about 12% higher than grazed sites; differences were statistically significant (p &lt; 0.01) based on paired t-tests. The increase in hydric vegetation after livestock exclusion may have contributed to the greater bank stability (p = 0.002) and smaller width-to-depth ratio (p = 0.005) in exclosures. Challenges were encountered in using community types to describe and compare site vegetation, which could be avoided with species data collection. The wetland index can be a tool to monitor sites over time, compare sites with similar environments, or compare sites for which environmental differences can be accounted. </p>","language":"English","publisher":"American Water Resources Association","doi":"10.1111/j.1752-1688.2007.00058.x","issn":"1093474X","usgsCitation":"Coles-Ritchie, M.C., Roberts, D., Kershner, J.L., and Henderson, R., 2007, Use of a wetland index to evaluate changes in riparian vegetation after livestock exclusion: Journal of the American Water Resources Association, v. 43, no. 3, p. 731-743, https://doi.org/10.1111/j.1752-1688.2007.00058.x.","productDescription":"13 p.","startPage":"731","endPage":"743","numberOfPages":"13","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[{"id":481,"text":"Northern Rocky Mountain Science Center","active":true,"usgs":true}],"links":[{"id":477244,"rank":10000,"type":{"id":40,"text":"Open Access Publisher Index Page"},"url":"https://doi.org/10.1111/j.1752-1688.2007.00058.x","text":"Publisher Index Page"},{"id":238912,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"},{"id":211597,"rank":9999,"type":{"id":10,"text":"Digital Object Identifier"},"url":"https://dx.doi.org/10.1111/j.1752-1688.2007.00058.x"}],"volume":"43","issue":"3","noUsgsAuthors":false,"publicationDate":"2007-05-14","publicationStatus":"PW","scienceBaseUri":"505bbea3e4b08c986b3296d1","contributors":{"authors":[{"text":"Coles-Ritchie, M. C.","contributorId":40418,"corporation":false,"usgs":true,"family":"Coles-Ritchie","given":"M.","email":"","middleInitial":"C.","affiliations":[],"preferred":false,"id":430079,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Roberts, D.W.","contributorId":11828,"corporation":false,"usgs":true,"family":"Roberts","given":"D.W.","email":"","affiliations":[],"preferred":false,"id":430078,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Kershner, J. L.","contributorId":100322,"corporation":false,"usgs":true,"family":"Kershner","given":"J.","email":"","middleInitial":"L.","affiliations":[],"preferred":false,"id":430081,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Henderson, R.C.","contributorId":58986,"corporation":false,"usgs":true,"family":"Henderson","given":"R.C.","email":"","affiliations":[],"preferred":false,"id":430080,"contributorType":{"id":1,"text":"Authors"},"rank":4}]}}
,{"id":70034492,"text":"70034492 - 2007 - TerraLook: Providing easy, no-cost access to satellite images for busy people and the technologically disinclined","interactions":[],"lastModifiedDate":"2021-06-14T19:46:20.580217","indexId":"70034492","displayToPublicDate":"2007-01-01T00:00:00","publicationYear":"2007","noYear":false,"publicationType":{"id":24,"text":"Conference Paper"},"publicationSubtype":{"id":19,"text":"Conference Paper"},"title":"TerraLook: Providing easy, no-cost access to satellite images for busy people and the technologically disinclined","docAbstract":"<div class=\"abstract-text row\"><div class=\"col-12\"><div class=\"u-mb-1\"><div>Access to satellite images has been largely limited to communities with specialized tools and expertise, even though images could also benefit other communities. This situation has resulted in underutilization of the data. TerraLook, which consists of collections of georeferenced JPEG images and an open source toolkit to use them, makes satellite images available to those lacking experience with remote sensing. Users can find, roam, and zoom images, create and display vector overlays, adjust and annotate images so they can be used as a communication vehicle, compare images taken at different times, and perform other activities useful for natural resource management, sustainable development, education, and other activities.</div></div></div></div>","largerWorkType":{"id":4,"text":"Book"},"largerWorkTitle":"International Geoscience and Remote Sensing Symposium (IGARSS)","largerWorkSubtype":{"id":12,"text":"Conference publication"},"conferenceTitle":"2007 IEEE International Geoscience and Remote Sensing Symposium","conferenceDate":"June 23-28, 2007","conferenceLocation":"Barcelona, Spain","language":"English","doi":"10.1109/IGARSS.2007.4422975","isbn":"1424412129; 9781424412129","usgsCitation":"Geller, G., Fosnight, E.A., and Chaudhuri, S., 2007, TerraLook: Providing easy, no-cost access to satellite images for busy people and the technologically disinclined, <i>in</i> International Geoscience and Remote Sensing Symposium (IGARSS), Barcelona, Spain, June 23-28, 2007, p. 1026-1028, https://doi.org/10.1109/IGARSS.2007.4422975.","productDescription":"3 p.","startPage":"1026","endPage":"1028","numberOfPages":"3","costCenters":[{"id":222,"text":"Earth Resources Observation and Science (EROS) Center","active":true,"usgs":true}],"links":[{"id":243874,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"505ba54de4b08c986b320966","contributors":{"authors":[{"text":"Geller, G.N.","contributorId":7087,"corporation":false,"usgs":true,"family":"Geller","given":"G.N.","email":"","affiliations":[],"preferred":false,"id":446063,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Fosnight, Eugene A. 0000-0002-8557-3697 fosnight@usgs.gov","orcid":"https://orcid.org/0000-0002-8557-3697","contributorId":2961,"corporation":false,"usgs":true,"family":"Fosnight","given":"Eugene","email":"fosnight@usgs.gov","middleInitial":"A.","affiliations":[{"id":223,"text":"Earth Resources Observation and Science (EROS) Center (Geography)","active":false,"usgs":true}],"preferred":true,"id":446065,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Chaudhuri, Sambhudas","contributorId":21708,"corporation":false,"usgs":false,"family":"Chaudhuri","given":"Sambhudas","email":"","affiliations":[],"preferred":false,"id":446064,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
]}