{"pageNumber":"178","pageRowStart":"4425","pageSize":"25","recordCount":36989,"records":[{"id":70094918,"text":"ofr20071047SRP068 - 2007 - The United States Polar Rock Repository: A geological resource for the Earth science community","interactions":[],"lastModifiedDate":"2014-02-25T11:28:24","indexId":"ofr20071047SRP068","displayToPublicDate":"2007-01-01T11:05:00","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-068","title":"The United States Polar Rock Repository: A geological resource for the Earth science community","docAbstract":"The United States Polar Rock Repository (USPRR) is a U. S. national facility designed for the permanent \ncuratorial preservation of rock samples, along with associated materials such as field notes, annotated air photos and \nmaps, raw analytic data, paleomagnetic cores, ground rock and mineral residues, thin sections, and microfossil mounts, \nmicroslides and residues from Polar areas. This facility was established by the Office of Polar Programs at the U. S. \nNational Science Foundation (NSF) to minimize redundant sample collecting, and also because the extreme cold and \nhazardous field conditions make fieldwork costly and difficult. The repository provides, along with an on-line database \nof sample information, an essential resource for proposal preparation, pilot studies and other sample based research that \nshould make fieldwork more efficient and effective. This latter aspect should reduce the environmental impact of \nconducting research in sensitive Polar Regions. The USPRR also provides samples for educational outreach. Rock \nsamples may be borrowed for research or educational purposes as well as for museum exhibits.","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/ofr20071047SRP068","usgsCitation":"Grunow, A.M., Elliot, D.H., and Codispoti, J.E., 2007, The United States Polar Rock Repository: A geological resource for the Earth science community: U.S. Geological Survey Open-File Report 2007-1047-SRP-068, Report: 3 p.; Plate 1: 2 p.; Plate 2: 1 p.; Plate 3: 1 p., https://doi.org/10.3133/ofr20071047SRP068.","productDescription":"Report: 3 p.; Plate 1: 2 p.; Plate 2: 1 p.; Plate 3: 1 p.","additionalOnlineFiles":"N","costCenters":[],"links":[{"id":282748,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/2007/1047/srp/srp068/of2007-1047srp068.pdf"},{"id":282749,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/ofr20071047SRP068.JPG"},{"id":282753,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/2007/1047/srp/srp068/of2007-1047srp068_plate2.pdf"},{"id":282754,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/2007/1047/srp/srp068/of2007-1047srp068_plate3.pdf"},{"id":282752,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/2007/1047/srp/srp068/of2007-1047srp068_plate1.pdf"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"53cd775be4b0b2908510b7b6","contributors":{"authors":[{"text":"Grunow, Annie M.","contributorId":34822,"corporation":false,"usgs":true,"family":"Grunow","given":"Annie","email":"","middleInitial":"M.","affiliations":[],"preferred":false,"id":490948,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Elliot, David H.","contributorId":51597,"corporation":false,"usgs":true,"family":"Elliot","given":"David","email":"","middleInitial":"H.","affiliations":[],"preferred":false,"id":490949,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Codispoti, Julie E.","contributorId":105641,"corporation":false,"usgs":true,"family":"Codispoti","given":"Julie","email":"","middleInitial":"E.","affiliations":[],"preferred":false,"id":490950,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":70074341,"text":"ofr20071047SRP021 - 2007 - Does the late Pliocene change in the architecture of the Antarctic margin correspond to the transition to the modern Antarctic Ice Sheet?","interactions":[],"lastModifiedDate":"2014-01-29T10:57:43","indexId":"ofr20071047SRP021","displayToPublicDate":"2007-01-01T10:45:00","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-021","title":"Does the late Pliocene change in the architecture of the Antarctic margin correspond to the transition to the modern Antarctic Ice Sheet?","docAbstract":"We observe in 6 key sectors of East and West Antarctica continental margin a change in the geometry of the\nsedimentary deposits which is characterized by: margin-wide erosion and subsequent progradation on the continental\nshelf; downlap on the continental slope; major mass wasting deposits on the continental rise. The change occurs in the\nlate Neogene in all sectors, though some natural variation exists, and the stratigraphic position is not obvious for every\nmargin. The change is apparently synchronous and dated about 3 Ma in Antarctic Peninsula and Prydz Bay margins and\nbroadly concomitant in the others sectors. This suggests a common driving force, which we suggest to be the transition\nof the Antarctic ice sheet regime from polythermal to present polar cold, dry-based conditions","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/ofr20071047SRP021","usgsCitation":"Rebesco, M., and Camerlenghi, A., 2007, Does the late Pliocene change in the architecture of the Antarctic margin correspond to the transition to the modern Antarctic Ice Sheet?: U.S. Geological Survey Open-File Report 2007-1047-SRP-021, 5 p., https://doi.org/10.3133/ofr20071047SRP021.","productDescription":"5 p.","additionalOnlineFiles":"N","costCenters":[],"links":[{"id":281646,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/ofr20071047SRP021.png"},{"id":281645,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/2007/1047/srp/srp021/of2007-1047srp021.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":"53cd55c1e4b0b290850f67fd","contributors":{"authors":[{"text":"Rebesco, M.","contributorId":60120,"corporation":false,"usgs":true,"family":"Rebesco","given":"M.","affiliations":[],"preferred":false,"id":489526,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Camerlenghi, Angelo","contributorId":7450,"corporation":false,"usgs":true,"family":"Camerlenghi","given":"Angelo","email":"","affiliations":[],"preferred":false,"id":489525,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":70094914,"text":"ofr20071047SRP067 - 2007 - Influence of submarine morphology on bottom water flow across the western Ross Sea continental margin","interactions":[],"lastModifiedDate":"2014-02-25T11:02:27","indexId":"ofr20071047SRP067","displayToPublicDate":"2007-01-01T10:43:00","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-067","title":"Influence of submarine morphology on bottom water flow across the western Ross Sea continental margin","docAbstract":"Multibeam sonar bathymetry documents a lack of significant channels crossing outer continental shelf and \nslope of the western Ross Sea. This indicates that movement of bottom water across the shelf break into the deep ocean \nin this area is mainly by laminar or sheet flow. Subtle, ~20 m deep and up to 1000 m wide channels extend down the \ncontinental slope, into tributary drainage patterns on the upper rise, and then major erosional submarine canyons. These \ndown-slope channels may have been formed by episodic pulses of rapid down slope water flow, some recorded on \nbottom current meters, or by sub-ice melt water erosion from an icesheet grounded at the margin. Narrow, mostly linear \nfurrows on the continental shelf thought to be caused by iceberg scouring are randomly oriented, have widths generally \nless than 400 m and depths less than 30m, and extend to water depths in excess of 600 m.","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/ofr20071047SRP067","usgsCitation":"Davey, F., and Jacobs, S., 2007, Influence of submarine morphology on bottom water flow across the western Ross Sea continental margin: U.S. Geological Survey Open-File Report 2007-1047-SRP-067, 5 p., https://doi.org/10.3133/ofr20071047SRP067.","productDescription":"5 p.","onlineOnly":"N","costCenters":[],"links":[{"id":282747,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/ofr20071047SRP067.JPG"},{"id":282746,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/2007/1047/srp/srp067/of2007-1047srp067.pdf"}],"otherGeospatial":"Antarctica;Ross Sea","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -175.59,-78.65 ], [ -175.59,-74.01 ], [ -148.95,-74.01 ], [ -148.95,-78.65 ], [ -175.59,-78.65 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"53cd628fe4b0b290850fe403","contributors":{"authors":[{"text":"Davey, F.J.","contributorId":99152,"corporation":false,"usgs":true,"family":"Davey","given":"F.J.","email":"","affiliations":[],"preferred":false,"id":490944,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Jacobs, S.S.","contributorId":19471,"corporation":false,"usgs":true,"family":"Jacobs","given":"S.S.","email":"","affiliations":[],"preferred":false,"id":490943,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":70100984,"text":"ofr20071047SRP089 - 2007 - Airborne laser swath mapping of the Denton Hills, Transantarctic Mountains, Antarctica: Applications for structural and glacial geomorphic mapping","interactions":[],"lastModifiedDate":"2014-04-08T11:30:04","indexId":"ofr20071047SRP089","displayToPublicDate":"2007-01-01T10:35:00","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-089","title":"Airborne laser swath mapping of the Denton Hills, Transantarctic Mountains, Antarctica: Applications for structural and glacial geomorphic mapping","docAbstract":"High-resolution digital elevation data acquired by airborne laser scanning (ALS) for the Denton Hills, along \nthe coastal foothills of the Royal Society Range, Transantarctic Mountains, are examined for applications to bedrock \nand glacial geomorphic mapping. Digital elevation models (DEMs), displayed as shaded-relief images and slope maps, \nportray geomorphic landscape features in unprecedented detail across the region. Structures of both ductile and brittle \norigin, ranging in age from the Paleozoic to the Quaternary, can be mapped from the DEMs. Glacial features, providing \na record of the limits of grounded ice, of lake paleoshorelines, and of proglacial lake-ice conveyor deposits, are also \nprominent on the DEMs. The ALS-derived topographic data have great potential for a range of mapping applications in \nregions of ice-free terrain in Antarctica","largerWorkType":{"id":18,"text":"Report"},"largerWorkTitle":"High-resolution digital elevation data acquired by airborne laser scanning (ALS) for the Denton Hills, along  the coastal foothills of the Royal Society Range, Transantarctic Mountains, are examined for applications to bedrock  and glacial geomorphic mapping. Digital elevation models (DEMs), displayed as shaded-relief images and slope maps,  portray geomorphic landscape features in unprecedented detail across the region. Structures of both ductile and brittle  origin, ranging in age from the Paleozoic to the Quaternary, can be mapped from the DEMs. Glacial features, providing  a record of the limits of grounded ice, of lake paleoshorelines, and of proglacial lake-ice conveyor deposits, are also  prominent on the DEMs. The ALS-derived topographic data have great potential for a range of mapping applications in  regions of ice-free terrain in Antarctica","largerWorkSubtype":{"id":5,"text":"USGS Numbered Series"},"language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Reston, VA","doi":"10.3133/ofr20071047SRP089","usgsCitation":"Wilson, T., and Csatho, B., 2007, Airborne laser swath mapping of the Denton Hills, Transantarctic Mountains, Antarctica: Applications for structural and glacial geomorphic mapping: U.S. Geological Survey Open-File Report 2007-1047-SRP-089, 6 p., https://doi.org/10.3133/ofr20071047SRP089.","productDescription":"6 p.","additionalOnlineFiles":"N","costCenters":[],"links":[{"id":285883,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/2007/1047/srp/srp089/of2007-1047srp089.pdf"},{"id":285885,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/ofr20071047SRP089.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":"53558fc5e4b0120853e8be2b","contributors":{"authors":[{"text":"Wilson, Terry","contributorId":33618,"corporation":false,"usgs":true,"family":"Wilson","given":"Terry","affiliations":[],"preferred":false,"id":492483,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Csatho, Beata","contributorId":17530,"corporation":false,"usgs":true,"family":"Csatho","given":"Beata","email":"","affiliations":[],"preferred":false,"id":492482,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":70094159,"text":"ofr20071047SRP049 - 2007 - Tectonic history of mid-Miocene to present southern Victoria Land Basin,  inferred from seismic stratigraphy in McMurdo Sound, Antarctica","interactions":[],"lastModifiedDate":"2014-02-18T10:39:00","indexId":"ofr20071047SRP049","displayToPublicDate":"2007-01-01T10:26:00","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-049","title":"Tectonic history of mid-Miocene to present southern Victoria Land Basin,  inferred from seismic stratigraphy in McMurdo Sound, Antarctica","docAbstract":"New and existing seismic reflection data in southern McMurdo Sound have been used to investigate\nNeogene tectonic history of the Terror Rift adjacent to the Transantarctic Mountains and along the western margin of the West Antarctic Rift System. Seismic data image a young rifting episode that is largely unsampled by CRP and CIROS drill holes. Data reveal up to 3.5 km of post middle Miocene strata deposited in this part of the NNW-\nSSE trending Terror Rift basin. Mapped fault trends in the southern Terror Rift parallel the axis of the basin and are\nprominent in a 40 km wide zone north of Ross Island. Displacement on individual faults in this zone can exceed 100\nm and faults collectively accommodate approximately 10-15 km of middle Miocene to recent extension.","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/ofr20071047SRP049","usgsCitation":"Henrys, S., Wilson, T., Whittaker, J., Fielding, C., Hall, J., and Naish, T., 2007, Tectonic history of mid-Miocene to present southern Victoria Land Basin,  inferred from seismic stratigraphy in McMurdo Sound, Antarctica: U.S. Geological Survey Open-File Report 2007-1047-SRP-049, 4 p., https://doi.org/10.3133/ofr20071047SRP049.","productDescription":"4 p.","additionalOnlineFiles":"N","costCenters":[],"links":[{"id":282465,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/ofr20071047SRP049.JPG"},{"id":282464,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/2007/1047/srp/srp049/of2007-1047srp049.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":"53cd7668e4b0b2908510ae14","contributors":{"authors":[{"text":"Henrys, S.","contributorId":27632,"corporation":false,"usgs":true,"family":"Henrys","given":"S.","email":"","affiliations":[],"preferred":false,"id":490489,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Wilson, T.","contributorId":49581,"corporation":false,"usgs":true,"family":"Wilson","given":"T.","affiliations":[],"preferred":false,"id":490490,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Whittaker, J.M.","contributorId":26226,"corporation":false,"usgs":true,"family":"Whittaker","given":"J.M.","email":"","affiliations":[],"preferred":false,"id":490488,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Fielding, C.","contributorId":20652,"corporation":false,"usgs":true,"family":"Fielding","given":"C.","email":"","affiliations":[],"preferred":false,"id":490487,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"Hall, J.","contributorId":66425,"corporation":false,"usgs":true,"family":"Hall","given":"J.","affiliations":[],"preferred":false,"id":490491,"contributorType":{"id":1,"text":"Authors"},"rank":5},{"text":"Naish, T.","contributorId":82151,"corporation":false,"usgs":true,"family":"Naish","given":"T.","email":"","affiliations":[],"preferred":false,"id":490492,"contributorType":{"id":1,"text":"Authors"},"rank":6}]}}
,{"id":70094913,"text":"ofr20071047SRP066 - 2007 - Occurrence of a young elasmosaurid plesiosaur skeleton from the Late Cretaceous (Maastrichtian) of Antarctica","interactions":[],"lastModifiedDate":"2014-02-25T10:39:32","indexId":"ofr20071047SRP066","displayToPublicDate":"2007-01-01T10:26:00","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-066","title":"Occurrence of a young elasmosaurid plesiosaur skeleton from the Late Cretaceous (Maastrichtian) of Antarctica","docAbstract":"The most completely articulated fossil skeleton heretofore found on the continent of Antarctica is \nrepresented by a juvenile plesiosaur. The specimen was found in the Sandwich Bluff area of Vega Island east of the \nAntarctic Peninsula from Late Cretaceous (Maastrichtian) marine deposits from the upper Snow Hill Island Formation. \nThe plesiosaur skeleton is represented by a nearly complete torso, partial paddles, and neck and tail sections. Along the \nventral margin of the torso are articulated gastralia, some that are unusual in being forked. Numerous small gastroliths \nare associated within the trunk cavity, indicating that even juveniles ingest gastroliths. Coupled with other known \nspecimens, the skeleton indicates shallow marine environment may have been an area where marine reptiles had their \nyoung, and the young remained until reaching maturity prior to facing open marine environments. The morphology of \nthe specimen suggests the skeleton represents a juvenile Mauisaurus, an elasmosaurid plesiosaur taxon originally \ndescribed from New Zealand and endemic to the Weddellian Province of the austral region.","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/ofr20071047SRP066","usgsCitation":"Martin, J.E., Sawyer, J.F., Reguero, M., and Case, J.A., 2007, Occurrence of a young elasmosaurid plesiosaur skeleton from the Late Cretaceous (Maastrichtian) of Antarctica: U.S. Geological Survey Open-File Report 2007-1047-SRP-066, 4 p., https://doi.org/10.3133/ofr20071047SRP066.","productDescription":"4 p.","additionalOnlineFiles":"N","costCenters":[],"links":[{"id":282740,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/ofr20071047SRP066.JPG"},{"id":282737,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/2007/1047/srp/srp066/of2007-1047srp066.pdf"}],"otherGeospatial":"Antarctica;Vega Island","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -57.7225,-63.9193 ], [ -57.7225,-63.8526 ], [ -57.5134,-63.8526 ], [ -57.5134,-63.9193 ], [ -57.7225,-63.9193 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"53cd69b9e4b0b29085102cb1","contributors":{"authors":[{"text":"Martin, James E.","contributorId":93826,"corporation":false,"usgs":true,"family":"Martin","given":"James","email":"","middleInitial":"E.","affiliations":[],"preferred":false,"id":490942,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Sawyer, J. Foster","contributorId":80344,"corporation":false,"usgs":true,"family":"Sawyer","given":"J.","email":"","middleInitial":"Foster","affiliations":[],"preferred":false,"id":490941,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Reguero, Marcelo","contributorId":50079,"corporation":false,"usgs":true,"family":"Reguero","given":"Marcelo","email":"","affiliations":[],"preferred":false,"id":490940,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Case, Judd A.","contributorId":11945,"corporation":false,"usgs":true,"family":"Case","given":"Judd","email":"","middleInitial":"A.","affiliations":[],"preferred":false,"id":490939,"contributorType":{"id":1,"text":"Authors"},"rank":4}]}}
,{"id":70103155,"text":"ofr20071047SRP097 - 2007 - Subglacial conditions at a sticky spot along Kamb Ice Stream, West Antarctica","interactions":[],"lastModifiedDate":"2014-04-29T11:23:30","indexId":"ofr20071047SRP097","displayToPublicDate":"2007-01-01T10:23:00","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-097","title":"Subglacial conditions at a sticky spot along Kamb Ice Stream, West Antarctica","docAbstract":"We present the results of a seismic reflection experiment performed transverse to flow a few tens of \nkilometers above the main trunk of Kamb Ice Stream, West Antarctica, where we image a basal high surrounded by \nvariable subglacial conditions. This high rises as much as 200 m above the surrounding bed, acting as a major \nsticking point that resists fast flow. Application of the amplitude variation with offset (AVO) seismic technique has \nhighlighted regions of frozen sediments along our profile, suggesting that the ice stream is experiencing basal \nfreeze-on in the region. The bedrock high appears to be at least partially draped in sediment cover, with a \nconcentrated area of weak, dilatant till flanking one edge. This dilatant till is further dispersed along our profile, \nthough it does not possess enough continuity to maintain streaming ice conditions. These results support the \nhypothesis that the ongoing shutdown of Kamb Ice Stream is due to a loss in continuous basal lubrication.","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/ofr20071047SRP097","usgsCitation":"Peters, L., and Anandakrishnan, S., 2007, Subglacial conditions at a sticky spot along Kamb Ice Stream, West Antarctica: U.S. Geological Survey Open-File Report 2007-1047-SRP-097, 5 p., https://doi.org/10.3133/ofr20071047SRP097.","productDescription":"5 p.","additionalOnlineFiles":"N","costCenters":[],"links":[{"id":286762,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/ofr20071047SRP097.JPG"},{"id":286761,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/2007/1047/srp/srp097/of2007-1047srp097.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":"5360c9fce4b082a3ecf53e39","contributors":{"authors":[{"text":"Peters, L.E.","contributorId":106014,"corporation":false,"usgs":true,"family":"Peters","given":"L.E.","email":"","affiliations":[],"preferred":false,"id":493171,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Anandakrishnan, Sridhar","contributorId":29307,"corporation":false,"usgs":true,"family":"Anandakrishnan","given":"Sridhar","email":"","affiliations":[],"preferred":false,"id":493170,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"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":70100555,"text":"ofr20071047SRP087 - 2007 - The \"Golden Shale\": An indicator of coastal stability for Marble Point, McMurdo Sound, over the last four million years","interactions":[],"lastModifiedDate":"2014-04-02T11:02:22","indexId":"ofr20071047SRP087","displayToPublicDate":"2007-01-01T10:15:00","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-087","title":"The \"Golden Shale\": An indicator of coastal stability for Marble Point, McMurdo Sound, over the last four million years","docAbstract":"A small sedimentary deposit near Gneiss Point on the western side of McMurdo Sound, previously identified as \nshale, is described. The deposit is phillipsite, a zeolite that is believed to have formed from the deposition and alteration of \nvolcanic ash in a small ice-marginal saline lake. Other previously recorded occurrences of phillipsite in the dry valleys are \nbelieved to be several million years old. A similar age for this deposit is suggested for the Gneiss Point deposit. This is \nconsistent with other weathering and landscape features found in the immediate area, including traces of halloysite in soils. \nThe deposit is very close to sea level but could not have formed if the site had been below sea level, indicating that there has \nbeen very little uplift following that which caused the sea to retreat from the Wright Fiord.","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/ofr20071047SRP087","usgsCitation":"Claridge, G., and Campbell, I., 2007, The \"Golden Shale\": An indicator of coastal stability for Marble Point, McMurdo Sound, over the last four million years: U.S. Geological Survey Open-File Report 2007-1047-SRP-087, 4 p., https://doi.org/10.3133/ofr20071047SRP087.","productDescription":"4 p.","additionalOnlineFiles":"N","costCenters":[],"links":[{"id":285299,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/ofr20071047SRP087.PNG"},{"id":285298,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/2007/1047/srp/srp087/of2007-1047srp087.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":"5355959ae4b0120853e8c252","contributors":{"authors":[{"text":"Claridge, G.G.C.","contributorId":89059,"corporation":false,"usgs":true,"family":"Claridge","given":"G.G.C.","email":"","affiliations":[],"preferred":false,"id":492261,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Campbell, I.B.","contributorId":40127,"corporation":false,"usgs":true,"family":"Campbell","given":"I.B.","email":"","affiliations":[],"preferred":false,"id":492260,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":70098931,"text":"ofr20071047SRP075 - 2007 - Aeromagnetic search for Cenozoic magmatism over the Admiralty Mountains Block (East Antarctica)","interactions":[],"lastModifiedDate":"2014-03-19T11:49:59","indexId":"ofr20071047SRP075","displayToPublicDate":"2007-01-01T10:12:00","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-075","title":"Aeromagnetic search for Cenozoic magmatism over the Admiralty Mountains Block (East Antarctica)","docAbstract":"Cenozoic magmatic rocks of the Transantarctic Mountains provide an important window on the tectonic and \nmagmatic processes of the West Antarctic Rift System. Previous aeromagnetic investigations in northern Victoria Land \nhave delineated Cenozoic volcanic and intrusive complexes assigned to the McMurdo Volcanic Group and Meander \nIntrusives over the Transantarctic Mountains. We present a new aeromagnetic anomaly map for the region north of the \nMariner Glacier to study the extent and spatial distribution of these Cenozoic rocks over the previously unexplored \nAdmiralty Mountains. The new map shows that the Meander Intrusives are restricted to the coastal region between the \nMalta Plateau and the Daniell Peninsula. However, the McMurdo Volcanic Group rocks extend further inland, and may \ndelineate a hitherto unrecognised volcano-tectonic rift zone, extending as far north as the Trafalgar Glacier.","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 Society","publisherLocation":"Reston, VA","doi":"10.3133/ofr20071047SRP075","usgsCitation":"Armadillo, E., Ferraccioli, F., Zunino, A., Bozzo, E., Rocchi, S., and Armienti, P., 2007, Aeromagnetic search for Cenozoic magmatism over the Admiralty Mountains Block (East Antarctica): U.S. Geological Survey Open-File Report 2007-1047-SRP-075, 4 p., https://doi.org/10.3133/ofr20071047SRP075.","productDescription":"4 p.","additionalOnlineFiles":"N","costCenters":[],"links":[{"id":284213,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/ofr20071047SRP075.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":"53cd4bdee4b0b290850f09d5","contributors":{"authors":[{"text":"Armadillo","contributorId":128038,"corporation":true,"usgs":false,"organization":"Armadillo","id":535642,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"E.","contributorId":128276,"corporation":true,"usgs":false,"organization":"E.","id":535643,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Ferraccioli, Fausto","contributorId":43591,"corporation":false,"usgs":true,"family":"Ferraccioli","given":"Fausto","email":"","affiliations":[],"preferred":false,"id":491741,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Zunino, A.","contributorId":36046,"corporation":false,"usgs":true,"family":"Zunino","given":"A.","email":"","affiliations":[],"preferred":false,"id":491740,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"Bozzo, E.","contributorId":46001,"corporation":false,"usgs":true,"family":"Bozzo","given":"E.","email":"","affiliations":[],"preferred":false,"id":491743,"contributorType":{"id":1,"text":"Authors"},"rank":5},{"text":"Rocchi, S.","contributorId":21063,"corporation":false,"usgs":true,"family":"Rocchi","given":"S.","email":"","affiliations":[],"preferred":false,"id":491739,"contributorType":{"id":1,"text":"Authors"},"rank":6},{"text":"Armienti, P.","contributorId":81009,"corporation":false,"usgs":true,"family":"Armienti","given":"P.","email":"","affiliations":[],"preferred":false,"id":491744,"contributorType":{"id":1,"text":"Authors"},"rank":7}]}}
,{"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":70100554,"text":"ofr20071047SRP086 - 2007 - Active tectonics on Deception Island (West-Antarctica): A new approach by using the fractal anisotropy of lineaments, fault slip measurements and the caldera collapse shape","interactions":[],"lastModifiedDate":"2014-04-02T10:13:29","indexId":"ofr20071047SRP086","displayToPublicDate":"2007-01-01T09:32:00","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-086","title":"Active tectonics on Deception Island (West-Antarctica): A new approach by using the fractal anisotropy of lineaments, fault slip measurements and the caldera collapse shape","docAbstract":"The tectonic field on Deception Island (South Shetlands, West Antarctica) is determined from structural and \nfractal analyses. Three different analyses are applied to the study of the strain and stress fields in the area: (1) field \nmeasurements of faults (strain analysis), (2) fractal geometry of the spatial distribution of lineaments and (3) the caldera \nshape (stress analyses). In this work, the identified strain field is extensional with the maximum horizontal shortening \ntrending NE-SW and NW-SE. The fractal technique applied to the spatial distribution of lineaments indicates a stress \nfield with SHMAX oriented NE-SW. The elliptical caldera of Deception Island, determined from field mapping, satellite \nimagery, vents and fissure eruptions, has an elongate shape and a stress field with SHMAX trending NE-SW.","largerWorkType":{"id":18,"text":"Report"},"largerWorkTitle":"Antarctica: A Keystone in a Changinceedings 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/ofr20071047SRP086","usgsCitation":"Perez-Lopez, R., Giner-Robles, J.L., Martinez-Diaz, J., Rodriguez-Pascua, M., Bejar, M., Paredes, C., and Gonzalez-Casado, J., 2007, Active tectonics on Deception Island (West-Antarctica): A new approach by using the fractal anisotropy of lineaments, fault slip measurements and the caldera collapse shape: U.S. Geological Survey Open-File Report 2007-1047-SRP-086, 4 p., https://doi.org/10.3133/ofr20071047SRP086.","productDescription":"4 p.","additionalOnlineFiles":"N","costCenters":[],"links":[{"id":285277,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/ofr20071047SRP086.PNG"},{"id":285276,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/2007/1047/srp/srp086/of2007-1047srp086.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":"53558fc3e4b0120853e8be1d","contributors":{"authors":[{"text":"Perez-Lopez, R.","contributorId":40039,"corporation":false,"usgs":true,"family":"Perez-Lopez","given":"R.","email":"","affiliations":[],"preferred":false,"id":492257,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Giner-Robles, J. L.","contributorId":22602,"corporation":false,"usgs":true,"family":"Giner-Robles","given":"J.","email":"","middleInitial":"L.","affiliations":[],"preferred":false,"id":492253,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Martinez-Diaz, J.J.","contributorId":32451,"corporation":false,"usgs":true,"family":"Martinez-Diaz","given":"J.J.","email":"","affiliations":[],"preferred":false,"id":492255,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Rodriguez-Pascua, M.A.","contributorId":36853,"corporation":false,"usgs":true,"family":"Rodriguez-Pascua","given":"M.A.","email":"","affiliations":[],"preferred":false,"id":492256,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"Bejar, M.","contributorId":47689,"corporation":false,"usgs":true,"family":"Bejar","given":"M.","email":"","affiliations":[],"preferred":false,"id":492258,"contributorType":{"id":1,"text":"Authors"},"rank":5},{"text":"Paredes, C.","contributorId":28896,"corporation":false,"usgs":true,"family":"Paredes","given":"C.","email":"","affiliations":[],"preferred":false,"id":492254,"contributorType":{"id":1,"text":"Authors"},"rank":6},{"text":"Gonzalez-Casado, J.M.","contributorId":83833,"corporation":false,"usgs":true,"family":"Gonzalez-Casado","given":"J.M.","email":"","affiliations":[],"preferred":false,"id":492259,"contributorType":{"id":1,"text":"Authors"},"rank":7}]}}
,{"id":70093687,"text":"ofr20071047SRP042 - 2007 - The history of Antarctic Peninsula glaciation","interactions":[],"lastModifiedDate":"2014-02-11T09:51:02","indexId":"ofr20071047SRP042","displayToPublicDate":"2007-01-01T09:28:00","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-042","title":"The history of Antarctic Peninsula glaciation","docAbstract":"As Co-Chief Scientist on DSDP Leg 35 in 1974, Cam Craddock (1930-2006) produced the first useful \ninformation on Cenozoic Antarctic Peninsula glaciation - an early middle Miocene (15-17 Ma) apparent glacial onset. \nSubsequent work, onshore and offshore, has greatly extended our knowledge but that early conclusion stands today. \nCenozoic Antarctic Peninsula palaeoclimate as presently known is broadly consistent with global palaeoclimate proxies. \nInitial glacial onset was within the Eocene-Oligocene boundary interval (although earlier, short-lived glaciations have \nbeen proposed, from indirect measurements) and the peninsula probably became deglaciated in the earliest Miocene (ca. \n24 Ma). The renewed middle Miocene glaciation probably continued to the present and, for the last 9 Myr at least, has \npersisted through glacial (orbital) cycles, with grounded ice advance to the shelf edge during maxima. Although orbital \ncyclicity affected earlier AP palaeoclimate also, the level of glaciation through a complete cycle is uncertain.","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/ofr20071047SRP042","usgsCitation":"Barker, P.F., 2007, The history of Antarctic Peninsula glaciation: U.S. Geological Survey Open-File Report 2007-1047-SRP-042, 5 p., https://doi.org/10.3133/ofr20071047SRP042.","productDescription":"5 p.","additionalOnlineFiles":"N","costCenters":[],"links":[{"id":282254,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/ofr20071047SRP042.JPG"},{"id":282253,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/2007/1047/srp/srp042/of2007-1047srp042.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":"53cd7807e4b0b2908510bdfa","contributors":{"authors":[{"text":"Barker, Peter F.","contributorId":92167,"corporation":false,"usgs":true,"family":"Barker","given":"Peter","email":"","middleInitial":"F.","affiliations":[],"preferred":false,"id":490147,"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":70094153,"text":"ofr20071047SRP046 - 2007 - Cretaceous oblique detachment tectonics in the Fosdick Mountains, Marie Byrd Land, Antarctica","interactions":[],"lastModifiedDate":"2014-02-18T09:08:23","indexId":"ofr20071047SRP046","displayToPublicDate":"2007-01-01T08:57:00","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-046","title":"Cretaceous oblique detachment tectonics in the Fosdick Mountains, Marie Byrd Land, Antarctica","docAbstract":"The Fosdick Mountains form an E-W trending migmatite dome in the northern Ford Ranges of Marie Byrd Land, Antarctica. Pervasively folded migmatites derived from lower Paleozoic greywacke and middle Paleozoic plutonic rocks constitute the dome. New field research documents a transition from melt-present to solid-state deformation across the south flank of the dome, and a mylonitic shear zone mapped for 30 km between Mt. Iphigene and Mt Richardson. Kinematic shear sense is dextral normal oblique, with top-to-the-SW and -WSW transport. A U-Pb age of 107 Ma, from a leucosome-filled extensional shear band, provides a meltpresent deformation age, and a U-Pb age of 96 Ma, from a crosscutting granitic dike, gives a lower age limit for deformation. The shear zone, here named the South Fosdick detachment zone, forms the south flank of the migmatite dome and was in part responsible for the exhumation of mid-crustal rocks.","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/ofr20071047SRP046","usgsCitation":"McFadden, R., Siddoway, C., Teyssier, C., Fanning, C., and Kruckenberg, S., 2007, Cretaceous oblique detachment tectonics in the Fosdick Mountains, Marie Byrd Land, Antarctica: U.S. Geological Survey Open-File Report 2007-1047-SRP-046, 6 p., https://doi.org/10.3133/ofr20071047SRP046.","productDescription":"6 p.","additionalOnlineFiles":"N","costCenters":[],"links":[{"id":282459,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/ofr20071047SRP046.JPG"},{"id":282458,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/2007/1047/srp/srp046/of2007-1047srp046.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":"53cd5370e4b0b290850f526b","contributors":{"authors":[{"text":"McFadden, R.","contributorId":99043,"corporation":false,"usgs":true,"family":"McFadden","given":"R.","email":"","affiliations":[],"preferred":false,"id":490465,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Siddoway, C.S.","contributorId":28893,"corporation":false,"usgs":true,"family":"Siddoway","given":"C.S.","email":"","affiliations":[],"preferred":false,"id":490462,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Teyssier, C.","contributorId":19475,"corporation":false,"usgs":true,"family":"Teyssier","given":"C.","affiliations":[],"preferred":false,"id":490461,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Fanning, C.M.","contributorId":82434,"corporation":false,"usgs":true,"family":"Fanning","given":"C.M.","email":"","affiliations":[],"preferred":false,"id":490464,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"Kruckenberg, S.C.","contributorId":38470,"corporation":false,"usgs":true,"family":"Kruckenberg","given":"S.C.","email":"","affiliations":[],"preferred":false,"id":490463,"contributorType":{"id":1,"text":"Authors"},"rank":5}]}}
,{"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":80850,"text":"ofr20071168 - 2007 - Evaluating the potential for watershed restoration to reduce nutrient loading to Upper Klamath Lake, Oregon","interactions":[],"lastModifiedDate":"2016-04-20T17:32:49","indexId":"ofr20071168","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":"2007-1168","title":"Evaluating the potential for watershed restoration to reduce nutrient loading to Upper Klamath Lake, Oregon","docAbstract":"<p>A literature review of best management practices to reduce nutrient loading was performed to provide information for resource managers in the Klamath Basin, Oregon. Although BMPs have already been implemented in the watershed, some sense of their effectiveness in reducing phosphorus loading and their cost for installation and maintenance is still lacking. This report discusses both causes of nutrient loading and a wide-variety of BMPs used to treat or reduce causal factors. We specifically focused on cattle grazing as the principal land-use and causal factor for nutrient loading in the Klamath Basin above Upper Klamath Lake, Oregon. Several BMP types, including stream corridor fencing, riparian buffer strips and constructed wetlands, seem to have potential for reducing phosphorus loading that may result from cattle grazing. However, no single BMP is likely to be the most effective in all locations or situations.</p>","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Reston, VA","doi":"10.3133/ofr20071168","usgsCitation":"McCormick, P.V., and Campbell, S.G., 2007, Evaluating the potential for watershed restoration to reduce nutrient loading to Upper Klamath Lake, Oregon: U.S. Geological Survey Open-File Report 2007-1168, v, 31 p., https://doi.org/10.3133/ofr20071168.","productDescription":"v, 31 p.","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[{"id":291,"text":"Fort Collins Science Center","active":true,"usgs":true}],"links":[{"id":120977,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/ofr_2007_1168.jpg"},{"id":320213,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/2007/1168/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"country":"United States","state":"Oregon","otherGeospatial":"Upper Klamath Lake","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -122.09037780761719,\n              42.23360155663695\n            ],\n            [\n              -122.09037780761719,\n              42.500453028125584\n            ],\n            [\n              -121.80335998535158,\n              42.500453028125584\n            ],\n            [\n              -121.80335998535158,\n              42.23360155663695\n            ],\n            [\n              -122.09037780761719,\n              42.23360155663695\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ae2e4b07f02db688bcd","contributors":{"authors":[{"text":"McCormick, Paul V.","contributorId":92756,"corporation":false,"usgs":true,"family":"McCormick","given":"Paul","email":"","middleInitial":"V.","affiliations":[],"preferred":false,"id":293690,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Campbell, Sharon G.","contributorId":23173,"corporation":false,"usgs":true,"family":"Campbell","given":"Sharon","email":"","middleInitial":"G.","affiliations":[],"preferred":false,"id":293689,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":80808,"text":"ofr20071361 - 2007 - Applying radar technology to migratory bird conservation and management: Strengthening and expanding a collaborative","interactions":[],"lastModifiedDate":"2018-01-01T16:59:36","indexId":"ofr20071361","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":"2007-1361","title":"Applying radar technology to migratory bird conservation and management: Strengthening and expanding a collaborative","docAbstract":"<h1>Executive Summary</h1>\n<p>Understanding the factors affecting migratory bird and bat populations during all three phases of their life cycle&mdash;breeding, nonbreeding, and migration&mdash;is critical to species conservation planning. This includes the need for information about these species&rsquo; responses to natural challenges, as well as information about the effects of human activities and structures. Habitats and other resources critical to migrants during passage and stopover are being destroyed, degraded, and threatened by human activities. Birds and bats are also uniquely susceptible to human use of the airspace. Wind turbines, communication and power transmission towers, and other tall structures, known to cause bird and bat mortality, are being erected or proposed in increasing numbers across the country. In addition, the potential for bird/aircraft collisions poses human safety threats. Management and regulatory agencies, conservation organizations, and industry currently lack the information they need to meet their missions and statutory responsibilities. The biological data available from various radar technologies offer a unique opportunity to learn more about the spatiotemporal distribution patterns, flight characteristics, and habitat use of &ldquo;aero-fauna.&rdquo;</p>\n<p>Recognizing the opportunities presented by radar technologies, the U.S. Geological Survey (USGS), the U.S. Fish and Wildlife Service (USFWS), and university partners collaborated first on individual projects and then in a broader, informal &ldquo;collaborative&rdquo; to coordinate their radar-related research and work together to develop the suite of products needed for conservation of birds and bats. Having produced two summary documents (Sojda and others, 2005; Ruth and others, 2005), the next objective was to convene a workshop for researchers, management and regulatory agencies, and other interested parties. The focus of this initial workshop was on strengthening the existing USGS-USFWS-university partnership and expanding the &ldquo;collaborative&rdquo; to include new Federal agency partners. The subject matter was centered on discussing available technologies, appropriate applications, management-related needs, and ways to strengthen collaborative research and conservation efforts.</p>\n<p>The workshop opened with presentations about the history of the &ldquo;radar collaborative,&rdquo; a description of the workshop objectives and focuses, and a summary of resource management and regulatory needs. Scientific presentations describing current research projects or subjects followed, given by USGS scientists, as well as scientists from other Federal agencies, academia, conservation and ornithological organizations, and a private contracting firm. Presenters addressed a wide variety of management issues including siting of wind-power facilities, bird/aircraft collisions, effects of hurricanes Katrina and Rita on bird migration, bird use of Conservation Reserve Program land, defining bird migration patterns at a broad regional scale, and associating migrant birds with their stopover habitats. Presentations described a variety of radar technologies including NEXRAD weather surveillance radar, modified mobile marine radar, military tracking radar, pencil beam radar, and dual polarization radar, as well as complementary techniques and analysis methods such as acoustic monitoring, thermal imaging, artificial intelligence, and individual-based modeling.</p>\n<p>Key issues, themes, and questions identified during the open discussions that followed fell into five main categories: (1) agency needs and challenges; (2) radar technology and applications&mdash;technical questions and issues; (3) tools and resources for managers and researchers; (4) standardization of protocols; and (5) collaborative opportunities. Participants identified the following management, regulatory, or business issues facing them which may be addressed with radar technologies: tall structures; wind turbines; identification and protection of key habitats; assessment of management activities; and bird/aircraft strikes. Participants frequently expressed the need for specific information about which radar technologies are best used for answering particular questions. User groups emphasized the importance of clear, defensible scientific information on which they can base their activities. In turn, researchers emphasized their need for clearly defined, specific questions from&nbsp;managers so that they can design and conduct the required research. Discussions about technical issues requiring further research and collaboration included target identity, ground-truthing, linking migrants to habitat, and standardized protocols for applied research.</p>\n<p>Workshop participants identified and endorsed a series of seven action items that would promote collaboration and begin to address key issues identified at the workshop:</p>\n<p><strong>Action Item #1</strong>: Establish a working subgroup to address large-scale surveillance radar standardization issues.<br /><strong>Action Item #2</strong>: Establish a working subgroup to address small-scale radar standardization issues.<br /><strong>Action Item #3</strong>: Bring management and regulatory agencies together to identify the three most important information needs for each key management issue relating to radar technologies.<br /><strong>Action Item #4</strong>: Develop Fact Sheet(s) to provide information about radar technology applications to migratory bird and bat conservation issues.<br /><strong>Action Item #5</strong>: Create a &ldquo;radar collaborative&rdquo; Website to provide information about radar biology applications, contacts, publications, and so forth.<br /><strong>Action Item #6</strong>: Formalize and expand the USGS-USFWS &ldquo;radar collaborative.&rdquo;<br /><strong>Action Item #7</strong>: Advance basic research, such as target identity and validation, which will support and improve our abilities to apply radar technologies to conservation objectives.</p>\n<p>There was considerable interest in expanding the &ldquo;radar collaborative&rdquo; to include those agencies, organizations, and industries represented at the workshop. It was felt that the publication of the workshop proceedings, implementation of action items, and additional future meetings or workshops will be crucial in strengthening the &ldquo;radar collaborative&rdquo; effort and promoting the use of these valuable technologies for conserving migratory species.</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr20071361","usgsCitation":"Ruth, J.M., Manville, A., Larkin, R., Barrow, W., Johnson-Randall, L., Dawson, D.K., Diehl, R.H., Wang, Y., Sojda, R.S., Angryk, R., Klaver, R.W., Mead, R., Paxton, J., Heglund, P.J., Kirsch, E., Suarez, M.J., Robinson, L., Gauthreaux, S.A., Belser, C.G., Franke, S.J., Bruderer, B., Buler, J., Moore, F.R., Mizrahi, D.S., Fogg, R., Kelly, T., Cryan, P.M., Crum, T., Schuur, T.J., Krueper, D., Diehl, R., and Will, T., 2007, Applying radar technology to migratory bird conservation and management: Strengthening and expanding a collaborative: U.S. Geological Survey Open-File Report 2007-1361, iv, 86 p., https://doi.org/10.3133/ofr20071361.","productDescription":"iv, 86 p.","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[{"id":291,"text":"Fort Collins Science Center","active":true,"usgs":true}],"links":[{"id":191007,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ac6e4b07f02db67a40e","contributors":{"editors":[{"text":"Ruth, Janet M. 0000-0003-1576-5957 janet_ruth@usgs.gov","orcid":"https://orcid.org/0000-0003-1576-5957","contributorId":1408,"corporation":false,"usgs":true,"family":"Ruth","given":"Janet","email":"janet_ruth@usgs.gov","middleInitial":"M.","affiliations":[{"id":291,"text":"Fort Collins Science Center","active":true,"usgs":true}],"preferred":true,"id":631229,"contributorType":{"id":2,"text":"Editors"},"rank":1}],"authors":[{"text":"Ruth, Janet M. 0000-0003-1576-5957 janet_ruth@usgs.gov","orcid":"https://orcid.org/0000-0003-1576-5957","contributorId":1408,"corporation":false,"usgs":true,"family":"Ruth","given":"Janet","email":"janet_ruth@usgs.gov","middleInitial":"M.","affiliations":[{"id":291,"text":"Fort Collins Science Center","active":true,"usgs":true}],"preferred":true,"id":631230,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Manville, Albert","contributorId":65558,"corporation":false,"usgs":true,"family":"Manville","given":"Albert","email":"","affiliations":[],"preferred":false,"id":631197,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Larkin, Ron","contributorId":169829,"corporation":false,"usgs":false,"family":"Larkin","given":"Ron","email":"","affiliations":[{"id":24804,"text":"Illinois Natural History Survey, Prairie Research Institute, University of Illinois Urbana-Champaign","active":true,"usgs":false}],"preferred":false,"id":631198,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Barrow, Wylie C. 0000-0003-4671-2823 barroww@usgs.gov","orcid":"https://orcid.org/0000-0003-4671-2823","contributorId":1988,"corporation":false,"usgs":true,"family":"Barrow","given":"Wylie C.","email":"barroww@usgs.gov","affiliations":[{"id":455,"text":"National Wetlands Research Center","active":true,"usgs":true}],"preferred":false,"id":631199,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"Johnson-Randall, Lori 0000-0003-0100-994X","orcid":"https://orcid.org/0000-0003-0100-994X","contributorId":26906,"corporation":false,"usgs":true,"family":"Johnson-Randall","given":"Lori","affiliations":[],"preferred":false,"id":631200,"contributorType":{"id":1,"text":"Authors"},"rank":5},{"text":"Dawson, Deanna K. ddawson@usgs.gov","contributorId":1257,"corporation":false,"usgs":true,"family":"Dawson","given":"Deanna","email":"ddawson@usgs.gov","middleInitial":"K.","affiliations":[{"id":531,"text":"Patuxent Wildlife Research Center","active":true,"usgs":true}],"preferred":true,"id":631201,"contributorType":{"id":1,"text":"Authors"},"rank":6},{"text":"Diehl, Robert H. 0000-0001-9141-1734 rhdiehl@usgs.gov","orcid":"https://orcid.org/0000-0001-9141-1734","contributorId":3396,"corporation":false,"usgs":true,"family":"Diehl","given":"Robert","email":"rhdiehl@usgs.gov","middleInitial":"H.","affiliations":[{"id":481,"text":"Northern Rocky Mountain Science Center","active":true,"usgs":true}],"preferred":true,"id":631202,"contributorType":{"id":1,"text":"Authors"},"rank":7},{"text":"Wang, Yufang","contributorId":169830,"corporation":false,"usgs":false,"family":"Wang","given":"Yufang","email":"","affiliations":[{"id":12460,"text":"The University of Southern Mississippi","active":true,"usgs":false}],"preferred":false,"id":631203,"contributorType":{"id":1,"text":"Authors"},"rank":8},{"text":"Sojda, Richard S. sojda@usgs.gov","contributorId":1663,"corporation":false,"usgs":true,"family":"Sojda","given":"Richard","email":"sojda@usgs.gov","middleInitial":"S.","affiliations":[{"id":481,"text":"Northern Rocky Mountain Science Center","active":true,"usgs":true}],"preferred":true,"id":631204,"contributorType":{"id":1,"text":"Authors"},"rank":9},{"text":"Angryk, Rafal","contributorId":169831,"corporation":false,"usgs":false,"family":"Angryk","given":"Rafal","email":"","affiliations":[{"id":13655,"text":"Montana State Univ.","active":true,"usgs":false}],"preferred":false,"id":631205,"contributorType":{"id":1,"text":"Authors"},"rank":10},{"text":"Klaver, Robert W. 0000-0002-3263-9701 bklaver@usgs.gov","orcid":"https://orcid.org/0000-0002-3263-9701","contributorId":3285,"corporation":false,"usgs":true,"family":"Klaver","given":"Robert","email":"bklaver@usgs.gov","middleInitial":"W.","affiliations":[{"id":199,"text":"Coop Res Unit Leetown","active":true,"usgs":true},{"id":222,"text":"Earth Resources Observation and Science (EROS) Center","active":true,"usgs":true}],"preferred":true,"id":631206,"contributorType":{"id":1,"text":"Authors"},"rank":11},{"text":"Mead, Reggie","contributorId":169832,"corporation":false,"usgs":false,"family":"Mead","given":"Reggie","email":"","affiliations":[{"id":13655,"text":"Montana State Univ.","active":true,"usgs":false}],"preferred":false,"id":631207,"contributorType":{"id":1,"text":"Authors"},"rank":12},{"text":"Paxton, John","contributorId":22227,"corporation":false,"usgs":true,"family":"Paxton","given":"John","email":"","affiliations":[],"preferred":false,"id":631208,"contributorType":{"id":1,"text":"Authors"},"rank":13},{"text":"Heglund, Patricia J.","contributorId":149499,"corporation":false,"usgs":false,"family":"Heglund","given":"Patricia","email":"","middleInitial":"J.","affiliations":[{"id":17755,"text":"U.S. Fish and Wildlife Service, Upper Midwest Environmental Sciences Center","active":true,"usgs":false}],"preferred":false,"id":631209,"contributorType":{"id":1,"text":"Authors"},"rank":14},{"text":"Kirsch, Eileen","contributorId":43205,"corporation":false,"usgs":true,"family":"Kirsch","given":"Eileen","affiliations":[],"preferred":false,"id":631210,"contributorType":{"id":1,"text":"Authors"},"rank":15},{"text":"Suarez, Manuel J. msuarez@usgs.gov","contributorId":3086,"corporation":false,"usgs":true,"family":"Suarez","given":"Manuel","email":"msuarez@usgs.gov","middleInitial":"J.","affiliations":[{"id":606,"text":"Upper Midwest Environmental Sciences Center","active":true,"usgs":true}],"preferred":true,"id":631211,"contributorType":{"id":1,"text":"Authors"},"rank":16},{"text":"Robinson, Larry","contributorId":57374,"corporation":false,"usgs":true,"family":"Robinson","given":"Larry","affiliations":[],"preferred":false,"id":631212,"contributorType":{"id":1,"text":"Authors"},"rank":17},{"text":"Gauthreaux, Sidney A. Jr.","contributorId":113048,"corporation":false,"usgs":false,"family":"Gauthreaux","given":"Sidney","suffix":"Jr.","email":"","middleInitial":"A.","affiliations":[],"preferred":false,"id":631213,"contributorType":{"id":1,"text":"Authors"},"rank":18},{"text":"Belser, Carroll G.","contributorId":169833,"corporation":false,"usgs":false,"family":"Belser","given":"Carroll","email":"","middleInitial":"G.","affiliations":[{"id":7084,"text":"Clemson University","active":true,"usgs":false}],"preferred":false,"id":631214,"contributorType":{"id":1,"text":"Authors"},"rank":19},{"text":"Franke, Steven J.","contributorId":169834,"corporation":false,"usgs":false,"family":"Franke","given":"Steven","email":"","middleInitial":"J.","affiliations":[{"id":16984,"text":"University of Illinois at Urbana-Champaign","active":true,"usgs":false}],"preferred":false,"id":631215,"contributorType":{"id":1,"text":"Authors"},"rank":20},{"text":"Bruderer, Bruno","contributorId":169835,"corporation":false,"usgs":false,"family":"Bruderer","given":"Bruno","email":"","affiliations":[{"id":12551,"text":"Swiss Ornithological Institute, Sempach, Switzerland","active":true,"usgs":false}],"preferred":false,"id":631216,"contributorType":{"id":1,"text":"Authors"},"rank":21},{"text":"Buler, Jeffrey J.","contributorId":78431,"corporation":false,"usgs":true,"family":"Buler","given":"Jeffrey J.","affiliations":[],"preferred":false,"id":631217,"contributorType":{"id":1,"text":"Authors"},"rank":22},{"text":"Moore, Frank R.","contributorId":54582,"corporation":false,"usgs":false,"family":"Moore","given":"Frank","email":"","middleInitial":"R.","affiliations":[{"id":12981,"text":"Department of Biological Sciences, University of Southern Mississippi","active":true,"usgs":false}],"preferred":false,"id":631218,"contributorType":{"id":1,"text":"Authors"},"rank":23},{"text":"Mizrahi, David S.","contributorId":11100,"corporation":false,"usgs":true,"family":"Mizrahi","given":"David","email":"","middleInitial":"S.","affiliations":[],"preferred":false,"id":631219,"contributorType":{"id":1,"text":"Authors"},"rank":24},{"text":"Fogg, Robert","contributorId":169836,"corporation":false,"usgs":false,"family":"Fogg","given":"Robert","email":"","affiliations":[],"preferred":false,"id":631220,"contributorType":{"id":1,"text":"Authors"},"rank":25},{"text":"Kelly, T. Adam","contributorId":169837,"corporation":false,"usgs":false,"family":"Kelly","given":"T. Adam","affiliations":[],"preferred":false,"id":631221,"contributorType":{"id":1,"text":"Authors"},"rank":26},{"text":"Cryan, Paul M. 0000-0002-2915-8894 cryanp@usgs.gov","orcid":"https://orcid.org/0000-0002-2915-8894","contributorId":147942,"corporation":false,"usgs":true,"family":"Cryan","given":"Paul","email":"cryanp@usgs.gov","middleInitial":"M.","affiliations":[{"id":291,"text":"Fort Collins Science Center","active":true,"usgs":true}],"preferred":true,"id":631222,"contributorType":{"id":1,"text":"Authors"},"rank":27},{"text":"Crum, Tim","contributorId":169838,"corporation":false,"usgs":false,"family":"Crum","given":"Tim","email":"","affiliations":[],"preferred":false,"id":631223,"contributorType":{"id":1,"text":"Authors"},"rank":28},{"text":"Schuur, Terry J.","contributorId":169839,"corporation":false,"usgs":false,"family":"Schuur","given":"Terry","email":"","middleInitial":"J.","affiliations":[],"preferred":false,"id":631224,"contributorType":{"id":1,"text":"Authors"},"rank":29},{"text":"Krueper, Dave","contributorId":169840,"corporation":false,"usgs":false,"family":"Krueper","given":"Dave","email":"","affiliations":[{"id":6654,"text":"USFWS","active":true,"usgs":false}],"preferred":false,"id":631226,"contributorType":{"id":1,"text":"Authors"},"rank":30},{"text":"Diehl, Robb","contributorId":15910,"corporation":false,"usgs":true,"family":"Diehl","given":"Robb","email":"","affiliations":[],"preferred":false,"id":631227,"contributorType":{"id":1,"text":"Authors"},"rank":31},{"text":"Will, Tom","contributorId":149777,"corporation":false,"usgs":false,"family":"Will","given":"Tom","email":"","affiliations":[{"id":17821,"text":"U.S. Fish and Wildlife Service, Division of Migratory Birds","active":true,"usgs":false}],"preferred":false,"id":631228,"contributorType":{"id":1,"text":"Authors"},"rank":32}]}}
,{"id":80149,"text":"ofr20071154 - 2007 - Fort Collins Science Center: 2006 Accomplishments","interactions":[],"lastModifiedDate":"2018-10-25T19:14:54","indexId":"ofr20071154","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":"2007-1154","title":"Fort Collins Science Center: 2006 Accomplishments","docAbstract":"<p>In Fiscal Year 2006 (FY06), the U.S. Geological Survey (USGS) Fort Collins Science Center (FORT) continued research vital to U.S. Department of the Interior (DOI) science and management needs and associated USGS programmatic goals. FORT work also supported the science needs of other governmental departments and agencies as well as private cooperators. Specifically, FORT scientific research and technical assistance focused on client and partner agency needs and goals in the areas of biological information management, fisheries and aquatic systems, invasive species, status and trends of biological resources, terrestrial ecosystems, and wildlife resources. Highlights of FORT project accomplishments are described below under the USGS science program area with which each task is most closely associated.2 The work of FORT&rsquo;s five branches (in 2006: Aquatic Systems and Technology Applications, Ecosystem Dynamics, Invasive Species Science, Policy Analysis and Science Assistance, and Species and Habitats of Federal Interest) often involves major partnerships with other agencies or cooperation with other USGS disciplines (Geology, Geography, Water Resources).</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr20071154","usgsCitation":"2007, Fort Collins Science Center: 2006 Accomplishments: U.S. Geological Survey Open-File Report 2007-1154, iv, 25 p., https://doi.org/10.3133/ofr20071154.","productDescription":"iv, 25 p.","onlineOnly":"N","additionalOnlineFiles":"N","temporalStart":"2005-10-01","temporalEnd":"2006-09-30","costCenters":[{"id":291,"text":"Fort Collins Science Center","active":true,"usgs":true}],"links":[{"id":194764,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/ofr20071154.PNG"},{"id":320211,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/2007/1154/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e486ee4b07f02db50c7fa","contributors":{"editors":[{"text":"Wilson, Juliette T.","contributorId":15299,"corporation":false,"usgs":true,"family":"Wilson","given":"Juliette T.","affiliations":[],"preferred":false,"id":749933,"contributorType":{"id":2,"text":"Editors"},"rank":1}]}}
,{"id":80480,"text":"ofr20071274 - 2007 - Aerial population estimates of wild horses (Equus caballus) in the adobe town and salt wells creek herd management areas using an integrated simultaneous double-count and sightability bias correction technique","interactions":[],"lastModifiedDate":"2025-06-05T17:30:05.030317","indexId":"ofr20071274","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":"2007-1274","displayTitle":"Aerial population estimates of wild horses (<i>Equus caballus</i>) in the adobe town and salt wells creek herd management areas using an integrated simultaneous double-count and sightability bias correction technique","title":"Aerial population estimates of wild horses (Equus caballus) in the adobe town and salt wells creek herd management areas using an integrated simultaneous double-count and sightability bias correction technique","docAbstract":"An aerial survey technique combining simultaneous double-count and sightability bias correction methodologies was used to estimate the population of wild horses inhabiting Adobe Town and Salt Wells Creek Herd Management Areas, Wyoming. Based on 5 surveys over 4 years, we conclude that the technique produced estimates consistent with the known number of horses removed between surveys and an annual population growth rate of 16.2 percent per year. Therefore, evidence from this series of surveys supports the validity of this survey method. Our results also indicate that the ability of aerial observers to see horse groups is very strongly dependent on skill of the individual observer, size of the horse group, and vegetation cover. It is also more modestly dependent on the ruggedness of the terrain and the position of the sun relative to the observer. We further conclude that censuses, or uncorrected raw counts, are inadequate estimates of population size for this herd. Such uncorrected counts were all undercounts in our trials, and varied in magnitude from year to year and observer to observer. As of April 2007, we estimate that the population of the Adobe Town /Salt Wells Creek complex is 906 horses with a 95 percent confidence interval ranging from 857 to 981 horses.","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr20071274","collaboration":"Prepared in collaboration with the U.S. Bureau of Land Management","usgsCitation":"Lubow, B., and Ransom, J.I., 2007, Aerial population estimates of wild horses (Equus caballus) in the adobe town and salt wells creek herd management areas using an integrated simultaneous double-count and sightability bias correction technique: U.S. Geological Survey Open-File Report 2007-1274, iii, 13 p., https://doi.org/10.3133/ofr20071274.","productDescription":"iii, 13 p.","costCenters":[{"id":291,"text":"Fort Collins Science Center","active":true,"usgs":true}],"links":[{"id":489703,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/2007/1274/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":192044,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/2007/1274/report-thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b03e4b07f02db698e75","contributors":{"authors":[{"text":"Lubow, Bruce C.","contributorId":59520,"corporation":false,"usgs":true,"family":"Lubow","given":"Bruce C.","affiliations":[],"preferred":false,"id":292699,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Ransom, Jason I. 0000-0002-5930-4004","orcid":"https://orcid.org/0000-0002-5930-4004","contributorId":71645,"corporation":false,"usgs":true,"family":"Ransom","given":"Jason","email":"","middleInitial":"I.","affiliations":[],"preferred":false,"id":292700,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
]}