{"pageNumber":"872","pageRowStart":"21775","pageSize":"25","recordCount":46733,"records":[{"id":70047562,"text":"ds69J10 - 2007 - Detailed measured sections, cross sections, and paleogeographic reconstructions of the upper cretaceous and lower tertiary nonmarine interval, Wind River Basin, Wyoming: Chapter 10 in Petroleum systems and geologic assessment of oil and gas resources in the Wind River Basin Province, Wyoming","interactions":[],"lastModifiedDate":"2013-08-12T10:56:08","indexId":"ds69J10","displayToPublicDate":"2007-01-01T10:50:00","publicationYear":"2007","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":310,"text":"Data Series","code":"DS","onlineIssn":"2327-638X","printIssn":"2327-0271","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"69-J-10","title":"Detailed measured sections, cross sections, and paleogeographic reconstructions of the upper cretaceous and lower tertiary nonmarine interval, Wind River Basin, Wyoming: Chapter 10 in Petroleum systems and geologic assessment of oil and gas resources in the Wind River Basin Province, Wyoming","docAbstract":"Detailed measured sections and regional stratigraphic \ncross sections are used to reconstruct facies maps and \ninterpret paleogeographic settings for the interval from the \nbase of Upper Cretaceous Mesaverde Formation to top of \nlower member of the Paleocene Fort Union Formation in \nthe Wind River Basin, Wyoming. The Mesaverde Formation \nspans the time during which the Upper Cretaceous seaway \nretreated eastward out of central Wyoming in Campanian time \nand the initial stages of the Lewis transgression in earliest \nMaastrichtian time. This retreat stalled for a considerable \nperiod of time during deposition of the lower part of the \nMesaverde, creating a thick buildup of marginal marine \nsandstones and coaly coastal plain deposits across the western \npart of the basin. \nThe Lewis sea transgressed into the northeast part of \nWind River Basin, beginning in early Maastrichtian time \nduring deposition of the Teapot Sandstone Member of the \nMesaverde Formation. The Meeteetse Formation, which \noverlies the Teapot, was deposited in a poorly-drained coastal \nplain setting southwest of the Lewis seaway. The Lewis \nseaway, at maximum transgression, covered much of the \nnortheast half of the Wind River Basin area but was clearly \ndeflected around the present site of the Wind River Range, \nsouthwest of the basin, providing the first direct evidence of \nLaramide uplift on that range. \nUplift of the Wind River Range continued during \ndeposition of the overlying Maastrichtian Lance Formation. \nThe Granite Mountains south of the basin also became a \npositive feature during this time. A rapidly subsiding trough \nduring the Maastrichtian time formed near the presentday trough of the Wind River Basin in which more than \n6,000 feet of Lance was deposited. The development of this \ntrough appears to have begun before the adjacent Owl Creek \nMountains to the north started to rise; however, a muddy \nfacies in the upper part of Lance in the deep subsurface, just to \nthe south, might be interpreted to indicate that the Cretaceous \nCody Shale was being eroded off a rising Owl Creek \nMountains in latest Cretaceous time. \nThe Paleocene Fort Union Formation unconformably \noverlies older units but with only slight angular discordance \naround much of the margins of the Wind River Basin. Pre-Fort Union erosion was most pronounced toward the Wind \nRiver Range to the southwest, where the Fort Union ultimately \noverlies strata as old as the upper part of the Cretaceous Cody \nShale. The unconformity appears to die out toward the basin \ncenter. Coal-forming mires developed throughout the western \npart of the basin near the beginning of the Paleocene. River \nsystems entering the basin from the Wind River Range to the \nsouthwest and the Granite Mountains to the south produced \nareas of sandy fluvial deposition along mountain fronts. A \nmajor river system appears to have entered the basin from \nabout the same spot along the Wind River Range throughout \nmuch of the Paleocene, probably because it became incised \nand could not migrate laterally. The muddy floodplain \nfacies that developed along the deep basin trough during \nlatest Cretaceous time, expanded during the early part of the \nPaleocene. Coal-forming mires that characterize part of the \nlower Fort Union Formation reached maximum extent near \nthe beginning of the late Paleocene and just prior to the initial \ntransgression of Lake Waltman. \nFrom the time of initial flooding, Lake Waltman \nexpanded rapidly, drowning the coal-forming mires in \nthe central part of the basin and spreading to near basin \nmargins. Outcrop studies along the south margin of the basin \ndocument that once maximum transgression was reached, the \nlake was rapidly pushed basinward and replaced by fluvial \nenvironments.","largerWorkType":{"id":18,"text":"Report"},"largerWorkTitle":"Petroleum systems and geologic assessment of oil and gas resources in the Wind River Basin Province, Wyoming (Data Series 69-J)","largerWorkSubtype":{"id":5,"text":"USGS Numbered Series"},"language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Reston, VA","doi":"10.3133/ds69J10","collaboration":"This report is Chapter 10 in Petroleum systems and geologic assessment of oil and gas resources in the Wind River Basin Province, Wyoming. For more information, see: Data Series 69-J.","usgsCitation":"Johnson, R.C., 2007, Detailed measured sections, cross sections, and paleogeographic reconstructions of the upper cretaceous and lower tertiary nonmarine interval, Wind River Basin, Wyoming: Chapter 10 in Petroleum systems and geologic assessment of oil and gas resources in the Wind River Basin Province, Wyoming: U.S. Geological Survey Data Series 69-J-10, v, 49 p., https://doi.org/10.3133/ds69J10.","productDescription":"v, 49 p.","numberOfPages":"54","costCenters":[{"id":674,"text":"Wind River Basin Province Assessment Team","active":false,"usgs":true}],"links":[{"id":276368,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/ds69j10.png"},{"id":276367,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/dds/dds-069/dds-069-j/REPORTS/69_J_CH_10.pdf"},{"id":276366,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.usgs.gov/dds/dds-069/dds-069-j/"}],"country":"United States","state":"Wyoming","otherGeospatial":"Wind River Basin Province","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -110.1,42.0 ], [ -110.1,44.0 ], [ -106.0,44.0 ], [ -106.0,42.0 ], [ -110.1,42.0 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"520a03e6e4b0026c2bc11af4","contributors":{"authors":[{"text":"Johnson, Ronald C. 0000-0002-6197-5165 rcjohnson@usgs.gov","orcid":"https://orcid.org/0000-0002-6197-5165","contributorId":1550,"corporation":false,"usgs":true,"family":"Johnson","given":"Ronald","email":"rcjohnson@usgs.gov","middleInitial":"C.","affiliations":[{"id":164,"text":"Central Energy Resources Science Center","active":true,"usgs":true}],"preferred":true,"id":482403,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":70120875,"text":"70120875 - 2007 - Spatially continuous interpolation of water stage and water depths using the Everglades depth estimation network (EDEN)","interactions":[],"lastModifiedDate":"2014-08-18T11:03:53","indexId":"70120875","displayToPublicDate":"2007-01-01T10:49:00","publicationYear":"2007","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":3,"text":"Organization Series"},"seriesNumber":"1521","title":"Spatially continuous interpolation of water stage and water depths using the Everglades depth estimation network (EDEN)","docAbstract":"

The Everglades Depth Estimation Network (EDEN) is an integrated network of real-time water-level monitoring, ground-elevation modeling, and water-surface modeling that provides scientists and managers with current (2000-present), online water-stage and water-depth information for the entire freshwater portion of the Greater Everglades. Continuous daily spatial interpolations of the EDEN network stage data are presented on a 400-square-meter grid spacing. EDEN offers a consistent and documented dataset that can be used by scientists and managers to (1) guide large-scale field operations, (2) integrate hydrologic and ecological responses, and (3) support biological and ecological assessments that measure ecosystem responses to the implementation of the Comprehensive Everglades Restoration Plan (CERP) The target users are biologists and ecologists examining trophic level responses to hydrodynamic changes in the Everglades.

","language":"English","publisher":"University of Florida IFAS Extension","publisherLocation":"Gainesville, FL","usgsCitation":"Pearlstine, L., Higer, A., Palaseanu, M., Fujisaki, I., and Mazzotti, F., 2007, Spatially continuous interpolation of water stage and water depths using the Everglades depth estimation network (EDEN), 21 p.","productDescription":"21 p.","numberOfPages":"21","costCenters":[{"id":186,"text":"Coastal and Marine Geology Program","active":true,"usgs":true}],"links":[{"id":292401,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"},{"id":292400,"type":{"id":15,"text":"Index Page"},"url":"https://edis.ifas.ufl.edu/uw278"}],"country":"United States","state":"Florida","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -81.521,25.0945 ], [ -81.521,26.662 ], [ -80.174,26.662 ], [ -80.174,25.0945 ], [ -81.521,25.0945 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"53f25feee4b033341871895b","contributors":{"authors":[{"text":"Pearlstine, Leonard","contributorId":79174,"corporation":false,"usgs":true,"family":"Pearlstine","given":"Leonard","affiliations":[],"preferred":false,"id":498527,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Higer, Aaron","contributorId":102513,"corporation":false,"usgs":true,"family":"Higer","given":"Aaron","email":"","affiliations":[],"preferred":false,"id":498529,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Palaseanu, Monica 0000-0002-3786-5118","orcid":"https://orcid.org/0000-0002-3786-5118","contributorId":91028,"corporation":false,"usgs":true,"family":"Palaseanu","given":"Monica","affiliations":[],"preferred":false,"id":498528,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Fujisaki, Ikuko","contributorId":31108,"corporation":false,"usgs":false,"family":"Fujisaki","given":"Ikuko","email":"","affiliations":[{"id":12557,"text":"University of Florida, FLREC","active":true,"usgs":false}],"preferred":false,"id":498525,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"Mazzotti, Frank","contributorId":32609,"corporation":false,"usgs":true,"family":"Mazzotti","given":"Frank","affiliations":[],"preferred":false,"id":498526,"contributorType":{"id":1,"text":"Authors"},"rank":5}]}} ,{"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":70047560,"text":"ds69J9 - 2007 - Subsurface stratigraphic cross sections of cretaceous and lower tertiary rocks in the Wind River Basin, central Wyoming: Chapter 9 in Petroleum systems and geologic assessment of oil and gas resources in the Wind River Basin Province, Wyoming","interactions":[],"lastModifiedDate":"2013-08-12T10:41:57","indexId":"ds69J9","displayToPublicDate":"2007-01-01T10:33:00","publicationYear":"2007","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":310,"text":"Data Series","code":"DS","onlineIssn":"2327-638X","printIssn":"2327-0271","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"69-J-9","title":"Subsurface stratigraphic cross sections of cretaceous and lower tertiary rocks in the Wind River Basin, central Wyoming: Chapter 9 in Petroleum systems and geologic assessment of oil and gas resources in the Wind River Basin Province, Wyoming","docAbstract":"The stratigraphic cross sections presented in this \nreport were constructed as part of a project conducted by \nthe U.S. Geological Survey to characterize and evaluate the \nundiscovered oil and gas resources of the Wind River Basin \n(WRB) in central Wyoming. The primary purpose of the \ncross sections is to show the stratigraphic framework and \nfacies relations of Cretaceous and lower Tertiary rocks in \nthis large, intermontane structural and sedimentary basin, \nwhich formed in the Rocky Mountain foreland during the \nLaramide orogeny (Late Cretaceous through early Eocene \ntime). The WRB is nearly 200 miles (mi) long, 70 mi wide, \nand encompasses about 7,400 square miles (mi2) (fig. 1). The \nbasin is structurally bounded by the Owl Creek and Bighorn \nMountains on the north, the Casper arch on the east, the \nGranite Mountains on the south, and the Wind River Range on \nthe west.","largerWorkType":{"id":18,"text":"Report"},"largerWorkTitle":"Petroleum systems and geologic assessment of oil and gas resources in the Wind River Basin Province, Wyoming (Data Series 69-J)","largerWorkSubtype":{"id":5,"text":"USGS Numbered Series"},"language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Reston, VA","doi":"10.3133/ds69J9","collaboration":"This report is Chapter 9 in Petroleum systems and geologic assessment of oil and gas resources in the Wind River Basin Province, Wyoming. For more information, see: Data Series 69-J.","usgsCitation":"Finn, T.M., 2007, Subsurface stratigraphic cross sections of cretaceous and lower tertiary rocks in the Wind River Basin, central Wyoming: Chapter 9 in Petroleum systems and geologic assessment of oil and gas resources in the Wind River Basin Province, Wyoming: U.S. Geological Survey Data Series 69-J-9, iv, 28 p., https://doi.org/10.3133/ds69J9.","productDescription":"iv, 28 p.","numberOfPages":"32","costCenters":[{"id":674,"text":"Wind River Basin Province Assessment Team","active":false,"usgs":true}],"links":[{"id":276363,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/ds69j9.png"},{"id":276362,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/dds/dds-069/dds-069-j/REPORTS/69_J_CH_9.pdf"},{"id":276361,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.usgs.gov/dds/dds-069/dds-069-j/"}],"country":"United States","state":"Wyoming","otherGeospatial":"Wind River Basin Province","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -110.1,42.0 ], [ -110.1,44.0 ], [ -106.0,44.0 ], [ -106.0,42.0 ], [ -110.1,42.0 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"520a03ffe4b0026c2bc11ce4","contributors":{"authors":[{"text":"Finn, Thomas M. 0000-0001-6396-9351 finn@usgs.gov","orcid":"https://orcid.org/0000-0001-6396-9351","contributorId":778,"corporation":false,"usgs":true,"family":"Finn","given":"Thomas","email":"finn@usgs.gov","middleInitial":"M.","affiliations":[{"id":164,"text":"Central Energy Resources Science Center","active":true,"usgs":true}],"preferred":true,"id":482401,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"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":70047558,"text":"ds69J8 - 2007 - Source rock potential of upper cretaceous marine shales in the Wind River Basin, Wyoming: Chapter 8 in Petroleum systems and geologic assessment of oil and gas resources in the Wind River Basin Province, Wyoming","interactions":[],"lastModifiedDate":"2013-08-12T10:28:38","indexId":"ds69J8","displayToPublicDate":"2007-01-01T10:23:00","publicationYear":"2007","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":310,"text":"Data Series","code":"DS","onlineIssn":"2327-638X","printIssn":"2327-0271","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"69-J-8","title":"Source rock potential of upper cretaceous marine shales in the Wind River Basin, Wyoming: Chapter 8 in Petroleum systems and geologic assessment of oil and gas resources in the Wind River Basin Province, Wyoming","docAbstract":"Seventy-eight samples collected from marine shales from \nthe Cretaceous Mowry Shale, the lower part of the Frontier \nFormation, and the lower shaly and upper sandy members \nof the Cody Shale in the Wind River Basin, Wyoming, were \nanalyzed using Rock-Eval and total organic carbon analysis \nto determine the source rock potential. Results indicate \nthat the Mowry Shale has a generative potential based on \norganic richness that is considered to be fair to very good, \nand hydrogen indices and S2\n/S3\n ratios indicate a capability to \ngenerate both oil and gas. Maps of the Mowry indicate that \nit is most organic rich and oil-prone in the eastern part of the \nbasin. Results of total organic carbon and Rock-Eval analyses \nfor the Frontier Formation indicate that it is composed of \nmainly type III gas-prone kerogen, with organic richness \nlevels that are generally poor to fair. Results of similar \nanalyses of samples from the lower shaly member of the \nCody Shale show a generative potential ranging from fair to \nexcellent, and hydrogen indices and S2\n/S3\n ratios indicate that \nit is capable of generating both oil and gas. Maps showing \nthe distribution of kerogen types and organic richness for \nthe lower shaly member of the Cody Shale are similar to the \nMowry and show that lower shaly member of the Cody is \nmore organic rich and more oil-prone in the eastern part of the \nbasin. Analyses of samples of the upper sandy member of the \nCody Shale indicate that it has little or no potential as a source \nrock. Thermal maturity mapping based on vitrinite reflectance \nmeasurements in the coal-bearing post-Cody Upper \nCretaceous and Paleocene rocks shows that Upper Cretaceous \nmarine shales in the deeper parts of the Wind River Basin are \nthermally mature to overmature with respect to hydrocarbon \ngeneration.","largerWorkType":{"id":18,"text":"Report"},"largerWorkTitle":"Petroleum systems and geologic assessment of oil and gas resources in the Wind River Basin Province, Wyoming (Data Series 69-J)","largerWorkSubtype":{"id":5,"text":"USGS Numbered Series"},"language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Reston, VA","doi":"10.3133/ds69J8","collaboration":"This report is Chapter 8 in Petroleum systems and geologic assessment of oil and gas resources in the Wind River Basin Province, Wyoming. For more information, see: Data Series 69-J.","usgsCitation":"Finn, T.M., 2007, Source rock potential of upper cretaceous marine shales in the Wind River Basin, Wyoming: Chapter 8 in Petroleum systems and geologic assessment of oil and gas resources in the Wind River Basin Province, Wyoming: U.S. Geological Survey Data Series 69-J-8, iii, 24 p., https://doi.org/10.3133/ds69J8.","productDescription":"iii, 24 p.","numberOfPages":"27","costCenters":[{"id":674,"text":"Wind River Basin Province Assessment Team","active":false,"usgs":true}],"links":[{"id":276328,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.usgs.gov/dds/dds-069/dds-069-j/"},{"id":276325,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/dds/dds-069/dds-069-j/REPORTS/69_J_CH_8.pdf"},{"id":276330,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/ds69j8.png"}],"country":"United States","state":"Wyoming","otherGeospatial":"Wind River Basin Province","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -110.1,42.0 ], [ -110.1,44.0 ], [ -106.0,44.0 ], [ -106.0,42.0 ], [ -110.1,42.0 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"520a03fde4b0026c2bc11cc3","contributors":{"authors":[{"text":"Finn, Thomas M. 0000-0001-6396-9351 finn@usgs.gov","orcid":"https://orcid.org/0000-0001-6396-9351","contributorId":778,"corporation":false,"usgs":true,"family":"Finn","given":"Thomas","email":"finn@usgs.gov","middleInitial":"M.","affiliations":[{"id":164,"text":"Central Energy Resources Science Center","active":true,"usgs":true}],"preferred":true,"id":482399,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":70101053,"text":"ofr20071047SRP093 - 2007 - The next generation Antarctic digital magnetic anomaly map","interactions":[],"lastModifiedDate":"2014-04-09T12:19:44","indexId":"ofr20071047SRP093","displayToPublicDate":"2007-01-01T10:18:00","publicationYear":"2007","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":330,"text":"Open-File Report","code":"OFR","onlineIssn":"2331-1258","printIssn":"0196-1497","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"2007-1047-SRP-093","title":"The next generation Antarctic digital magnetic anomaly map","docAbstract":"Initiated in 1995, the Antarctic Digital Magnetic Anomaly Project (ADMAP) produced the first magnetic \nanomaly map of the Antarctic region south of 60\no\nS (Golynsky et al., 2001). This map synthesized over 7.1 million line-kms of survey data available up through 1999 from marine, airborne and Magsat satellite observations. Since the \nproduction of the initial map, a large number of new marine and airborne surveys and improved magnetic observations \nfrom the Ørsted and CHAMP satellite missions have become available. In addition, an improved core field model for \nthe Antarctic has been developed to better isolate crustal anomalies in these data. The next generation compilation also \nwill likely represent the magnetic survey observations of the region in terms of a high-resolution spherical cap harmonic \nmodel. In this paper, we review the progress and problems of developing an improved magnetic anomaly map to \nfacilitate studies of the Antarctic crustal magnetic field","largerWorkType":{"id":18,"text":"Report"},"largerWorkTitle":"Antarctica: A Keystone in a Changing World--Online Proceedings for the Tenth International Symposium on Antarctic Earth Sciences. 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B.","affiliations":[],"preferred":false,"id":492563,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Golynsky, A.V.","contributorId":15513,"corporation":false,"usgs":true,"family":"Golynsky","given":"A.V.","email":"","affiliations":[],"preferred":false,"id":492562,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Kim, H.R.","contributorId":100742,"corporation":false,"usgs":true,"family":"Kim","given":"H.R.","email":"","affiliations":[],"preferred":false,"id":492569,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Gaya-Pique, L.","contributorId":6761,"corporation":false,"usgs":true,"family":"Gaya-Pique","given":"L.","email":"","affiliations":[],"preferred":false,"id":492561,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"Thébault, E.","contributorId":56974,"corporation":false,"usgs":true,"family":"Thébault","given":"E.","affiliations":[],"preferred":false,"id":492565,"contributorType":{"id":1,"text":"Authors"},"rank":5},{"text":"Chiappinii, M.","contributorId":72707,"corporation":false,"usgs":true,"family":"Chiappinii","given":"M.","email":"","affiliations":[],"preferred":false,"id":492566,"contributorType":{"id":1,"text":"Authors"},"rank":6},{"text":"Ghidella, M.","contributorId":95794,"corporation":false,"usgs":true,"family":"Ghidella","given":"M.","affiliations":[],"preferred":false,"id":492567,"contributorType":{"id":1,"text":"Authors"},"rank":7},{"text":"Grunow, A.","contributorId":99892,"corporation":false,"usgs":true,"family":"Grunow","given":"A.","affiliations":[],"preferred":false,"id":492568,"contributorType":{"id":1,"text":"Authors"},"rank":8},{"text":"ADMAP Working Group","contributorId":128064,"corporation":true,"usgs":false,"organization":"ADMAP Working Group","id":535648,"contributorType":{"id":1,"text":"Authors"},"rank":9}]}} ,{"id":70121030,"text":"70121030 - 2007 - The need for sustained and integrated high-resolution mapping of dynamic coastal environments","interactions":[],"lastModifiedDate":"2021-06-08T12:04:20.504596","indexId":"70121030","displayToPublicDate":"2007-01-01T10:13:00","publicationYear":"2007","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":2678,"text":"Marine Technology Society Journal","active":true,"publicationSubtype":{"id":10}},"title":"The need for sustained and integrated high-resolution mapping of dynamic coastal environments","docAbstract":"

The coastal zone of the United States is a dynamic environment evolving in response to both natural processes and human activities. In order to protect coastal populations and resources, a detailed understanding of the physical setting and of the processes responsible for change is required. A sustained program of mapping coastal areas provides a means to establish baseline conditions, document change, and, in conjunction with models of physical processes, predict future behavior. Recent advances in mapping technology, including airborne lidars and hyperspectral imagers, allow for the rapid collection of high-resolution elevation data and land use information on a national scale. These rich data sets are critical to evaluating risk associated with coastal hazards, such as flooding during extreme storms. For example, coastal elevation data is a fundamental parameter in storm surge models that predict where flooding will occur, and land use maps serve as the foundation of assessments that identify the resources and populations that are most vulnerable. A comprehensive, national coastal mapping plan that is designed to collect, manage, and distribute these data, as well as to take advantage of recent progress in mapping technology, will provide a wealth of information for studying the processes of physical change, for determining areas vulnerable to coastal hazards, and for protecting and managing our coastal communities and resources.

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States\"}}]}","volume":"40","issue":"4","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"53f464d0e4b073ff773a7d73","contributors":{"authors":[{"text":"Stockdon, Hilary F. 0000-0003-0791-4676 hstockdon@usgs.gov","orcid":"https://orcid.org/0000-0003-0791-4676","contributorId":2153,"corporation":false,"usgs":true,"family":"Stockdon","given":"Hilary","email":"hstockdon@usgs.gov","middleInitial":"F.","affiliations":[{"id":186,"text":"Coastal and Marine Geology Program","active":true,"usgs":true},{"id":574,"text":"St. Petersburg Coastal and Marine Science Center","active":true,"usgs":true}],"preferred":true,"id":498697,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Lillycrop, Jeff W.","contributorId":90647,"corporation":false,"usgs":true,"family":"Lillycrop","given":"Jeff","email":"","middleInitial":"W.","affiliations":[],"preferred":false,"id":498700,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Howd, Peter A. phowd@usgs.gov","contributorId":4105,"corporation":false,"usgs":true,"family":"Howd","given":"Peter","email":"phowd@usgs.gov","middleInitial":"A.","affiliations":[],"preferred":true,"id":498698,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Wozencraft, Jennifer M.","contributorId":60964,"corporation":false,"usgs":true,"family":"Wozencraft","given":"Jennifer","email":"","middleInitial":"M.","affiliations":[],"preferred":false,"id":498699,"contributorType":{"id":1,"text":"Authors"},"rank":4}]}} ,{"id":70094912,"text":"ofr20071047SRP065A - 2007 - Pan-African granulites of central Dronning Maud Land and Mozambique: A comparison within the East-African-Antarctic orogen","interactions":[],"lastModifiedDate":"2014-02-25T10:20:33","indexId":"ofr20071047SRP065A","displayToPublicDate":"2007-01-01T10:02:00","publicationYear":"2007","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":330,"text":"Open-File Report","code":"OFR","onlineIssn":"2331-1258","printIssn":"0196-1497","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"2007-1047-SRP-065","title":"Pan-African granulites of central Dronning Maud Land and Mozambique: A comparison within the East-African-Antarctic orogen","docAbstract":"Granulite-facies metamorphism is extensively reported in Late Neoproterozoic/Early Palaeozoic time during formation of the East-African-Antarctic orogen (EAAO). Metamorphic data acquired from the Pan-African orogen of central Dronning Maud Land (cDML) are compared with data from northern Mozambique. The metamorphic rocks of cDML are characterised by Opx±Grt-bearing gneisses and Sil+Kfs-bearing metapelites which indicate medium-P granulite-facies metamorphism. Peak conditions, which are estimated to 800-900ºC at pressures up to 1.0 GPa, were followed by near-isothermal decompression during late Pan-African extension and exhumation. Granulite-facies lithologies are widespread in northern Mozambique, and Grt+Cpx-bearing assemblages show that high-P granulite-facies conditions with PT reaching 1.55 GPa and 900ºC were reached during the Pan-African orogeny. Garnet is replaced by symplectites of Pl+Opx+Mag indicating isothermal decompression, and the subsequent formation of Pl+amphibole-coronas suggests cooling into amphibolite facies. It is concluded that high-T metamorphism was pervasive in EAAO in Late Neoproterozoic/Early Paleozoic time, strongly overprinting evidences of earlier metamorphic assemblages.","largerWorkType":{"id":18,"text":"Report"},"largerWorkTitle":"Antarctica: A Keystone in a Changing World--Online Proceedings for the Tenth International Symposium on Antarctic Earth Sciences. Santa Barbara, California, U.S.A.--August 26 to September 1, 2007","largerWorkSubtype":{"id":5,"text":"USGS Numbered Series"},"language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Reston, VA","doi":"10.3133/ofr20071047SRP065A","usgsCitation":"Engvik, A., Elevevold, S., Jacobs, J., Tveten, E., de Azevedo, S., and Njange, F., 2007, Pan-African granulites of central Dronning Maud Land and Mozambique: A comparison within the East-African-Antarctic orogen: U.S. Geological Survey Open-File Report 2007-1047-SRP-065, 5 p., https://doi.org/10.3133/ofr20071047SRP065A.","productDescription":"5 p.","additionalOnlineFiles":"N","costCenters":[],"links":[{"id":282736,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/ofr20071047SRP065A.JPG"},{"id":282735,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/2007/1047/srp/srp065/of2007-1047srp065.pdf"}],"otherGeospatial":"Antarctica;Queen Maud Land","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -18.83,-78.89 ], [ -18.83,-68.64 ], [ 50.14,-68.64 ], [ 50.14,-78.89 ], [ -18.83,-78.89 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"53cd6a98e4b0b2908510359b","contributors":{"authors":[{"text":"Engvik, A.K.","contributorId":77839,"corporation":false,"usgs":true,"family":"Engvik","given":"A.K.","email":"","affiliations":[],"preferred":false,"id":490937,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Elevevold, S.","contributorId":13535,"corporation":false,"usgs":true,"family":"Elevevold","given":"S.","email":"","affiliations":[],"preferred":false,"id":490933,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Jacobs, J.","contributorId":96999,"corporation":false,"usgs":true,"family":"Jacobs","given":"J.","affiliations":[],"preferred":false,"id":490938,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Tveten, E.","contributorId":48476,"corporation":false,"usgs":true,"family":"Tveten","given":"E.","email":"","affiliations":[],"preferred":false,"id":490935,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"de Azevedo, S.","contributorId":69883,"corporation":false,"usgs":true,"family":"de Azevedo","given":"S.","email":"","affiliations":[],"preferred":false,"id":490936,"contributorType":{"id":1,"text":"Authors"},"rank":5},{"text":"Njange, F.","contributorId":37644,"corporation":false,"usgs":true,"family":"Njange","given":"F.","email":"","affiliations":[],"preferred":false,"id":490934,"contributorType":{"id":1,"text":"Authors"},"rank":6}]}} ,{"id":70093688,"text":"ofr20071047SRP043 - 2007 - East Antarctic ice-sheet dynamics between 5.2 and 0 Ma from a high-resolution terrigenous particle size record, ODP Site 1165, Prydz Bay-Cooperation Sea","interactions":[],"lastModifiedDate":"2014-02-11T10:19:26","indexId":"ofr20071047SRP043","displayToPublicDate":"2007-01-01T10:00:00","publicationYear":"2007","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":330,"text":"Open-File Report","code":"OFR","onlineIssn":"2331-1258","printIssn":"0196-1497","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"2007-1047-SRP-043","title":"East Antarctic ice-sheet dynamics between 5.2 and 0 Ma from a high-resolution terrigenous particle size record, ODP Site 1165, Prydz Bay-Cooperation Sea","docAbstract":"This paper discusses a 5.2-0 Ma high-resolution terrigenous particle size record recovered from a sediment \ndrift off East Antarctica. The particle size properties of Hole 1165B are interpreted in the context of previously acquired \ndata on a continental shelf to slope transect drilled by ODP Leg 188 in Prydz Bay and the Cooperation Sea. The new \ndata indicate that the Lambert ice stream stayed predominantly landward of the shelf break in the early Pliocene (5.2-3.5 \nMa) with periods of ice sheet recession on land. The middle Pliocene (3.5-3.1 Ma) is characterized as major ice \nexpansion during glacials with deposition of laminated clays from meltwater plumes on the continental rise, alternating \nwith periods of ice recession. A change in sedimentary facies and a decrease in sedimentation rates occurred at ~3.1 Ma \nindicating a more retreated Lambert Glacier. Between 2.5 and 1 Ma the ice stream was generally stable and had become \ncold-based with ice flow in a glacial trough extending to the shelf break. Three-four large pulses of coarse-grained \nglacigenic debris mark the record at ~1 Ma. These are interpreted as extensive calving due to decoupling of the marine \nterminus from its bed in response to Northern Hemisphere deglaciations and associated sea level rises.","largerWorkType":{"id":18,"text":"Report"},"largerWorkTitle":"Antarctica: A Keystone in a Changing World--Online Proceedings for the Tenth International Symposium on Antarctic Earth Sciences. Santa Barbara, California, U.S.A.--August 26 to September 1, 2007","largerWorkSubtype":{"id":5,"text":"USGS Numbered Series"},"language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Reston, VA","doi":"10.3133/ofr20071047SRP043","usgsCitation":"Passchier, S., 2007, East Antarctic ice-sheet dynamics between 5.2 and 0 Ma from a high-resolution terrigenous particle size record, ODP Site 1165, Prydz Bay-Cooperation Sea: U.S. Geological Survey Open-File Report 2007-1047-SRP-043, 4 p., https://doi.org/10.3133/ofr20071047SRP043.","productDescription":"4 p.","additionalOnlineFiles":"N","costCenters":[],"links":[{"id":282256,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/ofr20071047SRP043.JPG"},{"id":282255,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/2007/1047/srp/srp043/of2007-1047srp043.pdf"}],"otherGeospatial":"Antarctica","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ 180.0,-90.0 ], [ 180.0,-60.0 ], [ -180.0,-60.0 ], [ -180.0,-90.0 ], [ 180.0,-90.0 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"53cd563ae4b0b290850f6cb4","contributors":{"authors":[{"text":"Passchier, S.","contributorId":15117,"corporation":false,"usgs":false,"family":"Passchier","given":"S.","email":"","affiliations":[],"preferred":false,"id":490148,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":70094157,"text":"ofr20071047SRP048 - 2007 - Geology of the Terre Adélie Craton (135 – 146˚ E)","interactions":[],"lastModifiedDate":"2014-02-18T10:16:19","indexId":"ofr20071047SRP048","displayToPublicDate":"2007-01-01T09:53:00","publicationYear":"2007","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":330,"text":"Open-File Report","code":"OFR","onlineIssn":"2331-1258","printIssn":"0196-1497","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"2007-1047-SRP-048","title":"Geology of the Terre Adélie Craton (135 – 146˚ E)","docAbstract":"More than 15 years of field and laboratory investigations on samples from Terre Adélie to the western \npart of George Vth Land (135 to 146°E) during the GEOLETA program allow a reassessment of the Terre Adélie \nCraton (TAC) geology. The TAC represents the largest exposed fragment of the East Antarctic Shield preserved from \nboth Grenville and Ross tectono-metamorphic events. Therefore it corresponds to a well-preserved continental \nsegment that developed from the Neoarchean to the Paleoproterozoic. Together with the Gawler Craton in South \nAustralia, the TAC is considered as part of the Mawson continent, i.e. a striking piece of the Rodinia Supercontinent. \nHowever, this craton represents one of the less studied parts of the East Antarctic Shield. The three maps presented \nhere clearly point out the extent of two distinct domains within the Terre Adélie Craton and suggest that the TAC was \nbuilt up through a polyphased evolution during the Neoarchean-Siderian (c.a. 2.5Ga) and the Statherian (c.a. 1.7Ga) \nperiods. These data support a complete re-assessment of the TAC geology and represent a valuable base for the \nunderstanding of global geodynamics changes during Paleoproterozoic times.","largerWorkType":{"id":18,"text":"Report"},"largerWorkTitle":"Antarctica: A Keystone in a Changing World--Online Proceedings for the Tenth International Symposium on Antarctic Earth Sciences. Santa Barbara, California, U.S.A.--August 26 to September 1, 2007","largerWorkSubtype":{"id":5,"text":"USGS Numbered Series"},"language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Reston, VA","doi":"10.3133/ofr20071047SRP048","usgsCitation":"Menot, R., Duclaux, G., Peucat, J., Rolland, Y., Guillot, S., Fanning, M., Bascou, J., Gapais, D., and Pecher, A., 2007, Geology of the Terre Adélie Craton (135 – 146˚ E): U.S. Geological Survey Open-File Report 2007-1047-SRP-048, 5 p., https://doi.org/10.3133/ofr20071047SRP048.","productDescription":"5 p.","additionalOnlineFiles":"N","costCenters":[],"links":[{"id":282463,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/ofr20071047SRP048.JPG"},{"id":282462,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/2007/1047/srp/srp048/of2007-1047srp048.pdf"}],"otherGeospatial":"Antarctica","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ 180.0,-90.0 ], [ 180.0,-60.0 ], [ -180.0,-60.0 ], [ -180.0,-90.0 ], [ 180.0,-90.0 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"53cd5e70e4b0b290850fbb3e","contributors":{"authors":[{"text":"Menot, R.P.","contributorId":41738,"corporation":false,"usgs":true,"family":"Menot","given":"R.P.","email":"","affiliations":[],"preferred":false,"id":490480,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Duclaux, G.","contributorId":67006,"corporation":false,"usgs":true,"family":"Duclaux","given":"G.","email":"","affiliations":[],"preferred":false,"id":490482,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Peucat, J.J.","contributorId":73438,"corporation":false,"usgs":true,"family":"Peucat","given":"J.J.","email":"","affiliations":[],"preferred":false,"id":490483,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Rolland, Y.","contributorId":30137,"corporation":false,"usgs":true,"family":"Rolland","given":"Y.","email":"","affiliations":[],"preferred":false,"id":490479,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"Guillot, S.","contributorId":79401,"corporation":false,"usgs":true,"family":"Guillot","given":"S.","email":"","affiliations":[],"preferred":false,"id":490484,"contributorType":{"id":1,"text":"Authors"},"rank":5},{"text":"Fanning, M.","contributorId":10624,"corporation":false,"usgs":true,"family":"Fanning","given":"M.","email":"","affiliations":[],"preferred":false,"id":490477,"contributorType":{"id":1,"text":"Authors"},"rank":6},{"text":"Bascou, J.","contributorId":60127,"corporation":false,"usgs":true,"family":"Bascou","given":"J.","email":"","affiliations":[],"preferred":false,"id":490481,"contributorType":{"id":1,"text":"Authors"},"rank":7},{"text":"Gapais, D.","contributorId":79798,"corporation":false,"usgs":true,"family":"Gapais","given":"D.","email":"","affiliations":[],"preferred":false,"id":490485,"contributorType":{"id":1,"text":"Authors"},"rank":8},{"text":"Pecher, A.","contributorId":28162,"corporation":false,"usgs":true,"family":"Pecher","given":"A.","email":"","affiliations":[],"preferred":false,"id":490478,"contributorType":{"id":1,"text":"Authors"},"rank":9}]}} ,{"id":70094910,"text":"ofr20071047SRP065 - 2007 - Analysis of continuous GPS measurements from southern Victoria Land, Antarctica","interactions":[],"lastModifiedDate":"2014-02-25T09:55:00","indexId":"ofr20071047SRP065","displayToPublicDate":"2007-01-01T09:37:00","publicationYear":"2007","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":330,"text":"Open-File Report","code":"OFR","onlineIssn":"2331-1258","printIssn":"0196-1497","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"2007-1047-SRP-064","title":"Analysis of continuous GPS measurements from southern Victoria Land, Antarctica","docAbstract":"Several years of continuous data have been collected at remote bedrock Global Positioning System (GPS) \nsites in southern Victoria Land, Antarctica. Annual to sub-annual variations are observed in the position time-series. An \natmospheric pressure loading (APL) effect is calculated from pressure field anomalies supplied by the European Centre \nfor Medium-Range Weather Forecasts (ECMWF) model loading an elastic Earth model. The predicted APL signal has \na moderate correlation with the vertical position time-series at McMurdo, Ross Island (International Global Navigation \nSatellite System Service (IGS) station MCM4), produced using a global solution. In contrast, a local solution in which \nMCM4 is the fiducial site generates a vertical time series for a remote site in Victoria Land (Cape Roberts, ROB4) \nwhich exhibits a low, inverse correlation with the predicted atmospheric pressure loading signal. If, in the future, \nknown and well modeled geophysical loads can be separated from the time-series, then local hydrological loading, of \ninterest for glaciological and climate applications, can potentially be extracted from the GPS time-series.","largerWorkType":{"id":18,"text":"Report"},"largerWorkTitle":"Antarctica: A Keystone in a Changing World--Online Proceedings for the Tenth International Symposium on Antarctic Earth Sciences. Santa Barbara, California, U.S.A.--August 26 to September 1, 2007","largerWorkSubtype":{"id":5,"text":"USGS Numbered Series"},"language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Reston, VA","doi":"10.3133/ofr20071047SRP065","usgsCitation":"Willis, M., 2007, Analysis of continuous GPS measurements from southern Victoria Land, Antarctica: U.S. Geological Survey Open-File Report 2007-1047-SRP-064, 5 p., https://doi.org/10.3133/ofr20071047SRP065.","productDescription":"5 p.","additionalOnlineFiles":"N","costCenters":[],"links":[{"id":282730,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/2007/1047/srp/srp064/of2007-1047srp064.pdf"},{"id":282731,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/ofr20071047SRP065.JPG"}],"otherGeospatial":"Antarctica;Victoria Land","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ 149.96,-79.11 ], [ 149.96,-70.28 ], [ 170.34,-70.28 ], [ 170.34,-79.11 ], [ 149.96,-79.11 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"53cd4cd5e4b0b290850f134b","contributors":{"authors":[{"text":"Willis, Michael J.","contributorId":11118,"corporation":false,"usgs":true,"family":"Willis","given":"Michael J.","affiliations":[],"preferred":false,"id":490932,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":70121022,"text":"70121022 - 2007 - Integrating hydrologic and geophysical data to constrain coastal surficial aquifer processes at multiple spatial and temporal scales","interactions":[],"lastModifiedDate":"2017-09-06T11:32:59","indexId":"70121022","displayToPublicDate":"2007-01-01T09:29:00","publicationYear":"2007","noYear":false,"publicationType":{"id":5,"text":"Book chapter"},"publicationSubtype":{"id":24,"text":"Book Chapter"},"title":"Integrating hydrologic and geophysical data to constrain coastal surficial aquifer processes at multiple spatial and temporal scales","docAbstract":"

Since 1997, repeated, coincident geophysical surveys and extensive hydrologic studies in shallow monitoring wells have been used to study static and dynamic processes associated with surface water-groundwater interaction at a range of spatial scales at the estuarine and ocean boundaries of an undeveloped, permeable barrier island in the Georgia part of the U.S. South Atlantic Bight. Because geophysical and hydrologic data measure different parameters, at different resolution and precision, and over vastly different spatial scales, reconciling the coincident data or even combining complementary inversion, hydrogeochemcial analyses and well-based groundwater monitoring, and, in some cases, limited vegetation mapping to demonstrate the utility of an integrative, multidisciplinary approach for elucidating groundwater processes at spatial scales (tens to thousands of meters) that are often difficult to capture with traditional hydrologic approaches. The case studies highlight regional aquifer characteristics, varying degrees of lateral saltwater intrusion at estuarine boundaries, complex subsurface salinity gradients at the ocean boundary, and imaging of submarsh groundwater discharge and possible free convection in the pore waters of a clastic marsh. This study also documents the use of geophysical techniques for detecting temporal changes in groundwater salinity regimes under natural (not forced) gradients at intratidal to interannual (1998-200 Southeastern U.S.A. drought) time scales.","largerWorkType":{"id":4,"text":"Book"},"largerWorkTitle":"Subsurface hydrology: Data integration for properties and processes","language":"English","publisher":"Wiley","publisherLocation":"New York, NY","doi":"10.1029/171GM13","isbn":"9781118666463","usgsCitation":"Schultz, G.M., Ruppel, C., and Fulton, P., 2007, Integrating hydrologic and geophysical data to constrain coastal surficial aquifer processes at multiple spatial and temporal scales, chap. of Subsurface hydrology: Data integration for properties and processes, v. 171, p. 161-182, https://doi.org/10.1029/171GM13.","productDescription":"22 p.","startPage":"161","endPage":"182","costCenters":[{"id":186,"text":"Coastal and Marine Geology Program","active":true,"usgs":true},{"id":678,"text":"Woods Hole Coastal and Marine Science Center","active":true,"usgs":true}],"links":[{"id":292509,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"171","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"53f464cce4b073ff773a7d1c","contributors":{"editors":[{"text":"Hyndman, David W.","contributorId":7868,"corporation":false,"usgs":true,"family":"Hyndman","given":"David","email":"","middleInitial":"W.","affiliations":[],"preferred":false,"id":709623,"contributorType":{"id":2,"text":"Editors"},"rank":1},{"text":"Day-Lewis, Frederick D. 0000-0003-3526-886X daylewis@usgs.gov","orcid":"https://orcid.org/0000-0003-3526-886X","contributorId":1672,"corporation":false,"usgs":true,"family":"Day-Lewis","given":"Frederick","email":"daylewis@usgs.gov","middleInitial":"D.","affiliations":[{"id":37277,"text":"WMA - Earth System Processes Division","active":true,"usgs":true},{"id":486,"text":"OGW Branch of Geophysics","active":true,"usgs":true},{"id":493,"text":"Office of Ground Water","active":true,"usgs":true}],"preferred":true,"id":709624,"contributorType":{"id":2,"text":"Editors"},"rank":2},{"text":"Singha, Kamini 0000-0002-0605-3774","orcid":"https://orcid.org/0000-0002-0605-3774","contributorId":191366,"corporation":false,"usgs":false,"family":"Singha","given":"Kamini","email":"","affiliations":[{"id":6606,"text":"Colorado School of Mines","active":true,"usgs":false}],"preferred":false,"id":709625,"contributorType":{"id":2,"text":"Editors"},"rank":3}],"authors":[{"text":"Schultz, Gregory M.","contributorId":9582,"corporation":false,"usgs":false,"family":"Schultz","given":"Gregory","email":"","middleInitial":"M.","affiliations":[{"id":35646,"text":"Sky Research, Inc., Hanover, NH","active":true,"usgs":false}],"preferred":false,"id":498679,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Ruppel, Carolyn cruppel@usgs.gov","contributorId":2015,"corporation":false,"usgs":true,"family":"Ruppel","given":"Carolyn","email":"cruppel@usgs.gov","affiliations":[{"id":678,"text":"Woods Hole Coastal and Marine Science Center","active":true,"usgs":true}],"preferred":false,"id":498678,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Fulton, Patrick","contributorId":34832,"corporation":false,"usgs":true,"family":"Fulton","given":"Patrick","email":"","affiliations":[],"preferred":false,"id":498680,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}} ,{"id":70047556,"text":"ds69J7 - 2007 - Distribution of fluids and pressures in the Wind River Basin, Wyoming: Chapter 7 in Petroleum systems and geologic assessment of oil and gas resources in the Wind River Basin Province, Wyoming","interactions":[],"lastModifiedDate":"2013-08-12T09:34:54","indexId":"ds69J7","displayToPublicDate":"2007-01-01T09:27:00","publicationYear":"2007","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":310,"text":"Data Series","code":"DS","onlineIssn":"2327-638X","printIssn":"2327-0271","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"69-J-7","title":"Distribution of fluids and pressures in the Wind River Basin, Wyoming: Chapter 7 in Petroleum systems and geologic assessment of oil and gas resources in the Wind River Basin Province, Wyoming","docAbstract":"To examine the state of hydrocarbons and water in the\nWind River Basin of Wyoming, the following data types\nare compiled and presented at the basin scale: fluid type,\npressure, and temperature from drillstem tests; watersalinity\nand cumulative hydrocarbon production from oil and gas\nwells; vitrinite reflectance data; and sonic well logs. The\nspatial distribution of produced fluids shows the nearly\nubiquitous presence of mobile water, even in highly productive\ngas-charged formations. Sonic logs record a basin wide\nvelocity decrease in the Lower Cretaceous Thermopolis Shale\nthrough the Upper Cretaceous Cody Shale that is attributed\nto a combination of paleo-overpressuring and present-day\noverpressuring. Pressure-elevation plots and mud weights\nreveal the presence of two large pressure compartments in\nthe Madden area, one above the Waltman Shale Member of\nthe Paleocene Fort Union Formation and the other below it.\nTemperature data reveal hot and cold spots around structures\nin the marginal parts of the basin where the Waltman Shale\nMember of the Fort Union Formation is absent. The highest\ntemperature gradients are in the upper pressure compartment\nin the Madden area. Vitrinite reflectance data record little\nchange with increasing depth throughout much of the geologic\nsection in shallow parts of the basin and a steady increase\nof log (Ro\n) with depth in the deep parts of the basin. The\nvaried distribution of fluids, pressure, and temperature reflect\nthe complex history of subsidence, thrusting, hydrocarbon\ngeneration, water migration, and uplift in and marginal to this\nlarge, asymmetric intermontane basin.","largerWorkType":{"id":18,"text":"Report"},"largerWorkTitle":"Petroleum systems and geologic assessment of oil and gas resources in the Wind River Basin Province, Wyoming (Data Series 69-J)","largerWorkSubtype":{"id":5,"text":"USGS Numbered Series"},"language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Reston, VA","doi":"10.3133/ds69J7","collaboration":"This report is Chapter 7 in Petroleum systems and geologic assessment of oil and gas resources in the Wind River Basin Province, Wyoming. For more information, see: Data Series 69-J.","usgsCitation":"Nelson, P.H., and Kibler, J.E., 2007, Distribution of fluids and pressures in the Wind River Basin, Wyoming: Chapter 7 in Petroleum systems and geologic assessment of oil and gas resources in the Wind River Basin Province, Wyoming: U.S. Geological Survey Data Series 69-J-7, iv, 35 p., https://doi.org/10.3133/ds69J7.","productDescription":"iv, 35 p.","numberOfPages":"39","costCenters":[{"id":674,"text":"Wind River Basin Province Assessment Team","active":false,"usgs":true}],"links":[{"id":276301,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/ds69j7.png"},{"id":276299,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/dds/dds-069/dds-069-j/REPORTS/69_J_CH_7.pdf"},{"id":276300,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.usgs.gov/dds/dds-069/dds-069-j/"}],"country":"United States","state":"Wyoming","otherGeospatial":"Wind River Basin Province","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -110.1,42.0 ], [ -110.1,44.0 ], [ -106.0,44.0 ], [ -106.0,42.0 ], [ -110.1,42.0 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"520a03e6e4b0026c2bc11af8","contributors":{"authors":[{"text":"Nelson, Philip H. pnelson@usgs.gov","contributorId":862,"corporation":false,"usgs":true,"family":"Nelson","given":"Philip","email":"pnelson@usgs.gov","middleInitial":"H.","affiliations":[{"id":164,"text":"Central Energy Resources Science Center","active":true,"usgs":true}],"preferred":true,"id":482396,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Kibler, Joyce E.","contributorId":56293,"corporation":false,"usgs":true,"family":"Kibler","given":"Joyce","email":"","middleInitial":"E.","affiliations":[],"preferred":false,"id":482397,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":70104176,"text":"70104176 - 2007 - Pesticides in U.S. streams and groundwater","interactions":[],"lastModifiedDate":"2014-05-14T11:58:34","indexId":"70104176","displayToPublicDate":"2007-01-01T09:26:00","publicationYear":"2007","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1565,"text":"Environmental Science & Technology","onlineIssn":"1520-5851","printIssn":"0013-936X","active":true,"publicationSubtype":{"id":10}},"title":"Pesticides in U.S. streams and groundwater","docAbstract":"

A 10­-year study by the U.S. Geological \nSurvey’s (USGS’s) National Water-­Quality Assessment (NAWQA) Program provides a national-­scale view of pesticide \noccurrence in streams and groundwater. The 1992-2001 study builds upon a preliminary \nanalysis from NAWQA’s first phase of studies during \n1992-1996 (1, 2). Pesticide data available from various studies prior to 1992 did not allow national assessment because of limited and variable geographic \ncoverage (usually focusing on individual states or \nregions), sparse and inconsistent inclusion of pesticides in use, and variable sampling designs (3-5).

\n
\n

The expanded geographic coverage and improved \ndata following 10 years of study (Figure 1) confirm \nand reinforce previously reported findings and \nenable more detailed analyses of each topic. This \narticle summarizes selected findings from a comprehensive report (6), with a focus on the nature of \npesticide occurrence and potential significance to \nhuman health and stream ecosystems. Information \non study design and methods as well as additional \nanalysis of geographic patterns and trends in relation to use and management practices are available \nin the full report (6).

","largerWorkType":{"id":2,"text":"Article"},"largerWorkTitle":"Environmental Science and Technology","largerWorkSubtype":{"id":10,"text":"Journal Article"},"language":"English","publisher":"American Chemical Society","doi":"10.1021/es072531u","usgsCitation":"Gilliom, R.J., 2007, Pesticides in U.S. streams and groundwater: Environmental Science & Technology, v. 41, no. 10, p. 3408-3414, https://doi.org/10.1021/es072531u.","productDescription":"7 p.","startPage":"3408","endPage":"3414","numberOfPages":"7","costCenters":[{"id":451,"text":"National Water Quality Assessment Program","active":true,"usgs":true}],"links":[{"id":287128,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"},{"id":287127,"type":{"id":10,"text":"Digital Object Identifier"},"url":"https://dx.doi.org/10.1021/es072531u"}],"country":"United States","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ 173.0,16.916667 ], [ 173.0,71.833333 ], [ -66.95,71.833333 ], [ -66.95,16.916667 ], [ 173.0,16.916667 ] ] ] } } ] }","volume":"41","issue":"10","noUsgsAuthors":false,"publicationDate":"2007-05-15","publicationStatus":"PW","scienceBaseUri":"53749070e4b0870f4d23cfc8","contributors":{"authors":[{"text":"Gilliom, Robert J. rgilliom@usgs.gov","contributorId":488,"corporation":false,"usgs":true,"family":"Gilliom","given":"Robert","email":"rgilliom@usgs.gov","middleInitial":"J.","affiliations":[{"id":451,"text":"National Water Quality Assessment Program","active":true,"usgs":true}],"preferred":true,"id":493588,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":70100983,"text":"ofr20071047SRP088 - 2007 - Trends in discharge and flow season timing of the Onyx River, Wright Valley, Antarctica since 1969","interactions":[],"lastModifiedDate":"2018-02-21T17:41:22","indexId":"ofr20071047SRP088","displayToPublicDate":"2007-01-01T09:19:00","publicationYear":"2007","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":330,"text":"Open-File Report","code":"OFR","onlineIssn":"2331-1258","printIssn":"0196-1497","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"2007-1047-SRP-088","title":"Trends in discharge and flow season timing of the Onyx River, Wright Valley, Antarctica since 1969","docAbstract":"Flow records at the two stream gauges on the Onyx River represent the longest actively collected \nenvironmental records in the McMurdo Dry Valleys, Antarctica. The downstream gauge, near Lake Vanda, has been \ncollecting data since 1969, and the upstream gauge, at Lower Wright Glacier (LWRT), has collected data since 1972. \nWe analyzed these records to assess the long-term trends in annual discharge, flow season length, flow season start, and \nflow season end. Our results indicate overall decreasing trends in annual discharge (0.4x106\n m3\n/decade at LWRT, 0.8 \nx106\n m3\n/decade at Vanda), and increasing flow season lengths (by 7 d/decade at LWRT, and 2.7 d/decade at Vanda), \ninfluenced by earlier start and later end dates (5.2 and 0.8 d/decade, respectively at LWRT; 4.8, 1.4 d/decade, \nrespectively at Vanda). This suggests that flow season climate patterns in the Dry Valleys are decreasing glacier melt \nintensity overall, but extending the period of meltwater generation","largerWorkType":{"id":18,"text":"Report"},"largerWorkTitle":"Antarctica: A Keystone in a Changing World--Online Proceedings for the Tenth International Symposium on Antarctic Earth Sciences. Santa Barbara, California, U.S.A.--August 26 to September 1, 2007","largerWorkSubtype":{"id":5,"text":"USGS Numbered Series"},"language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Reston, VA","doi":"10.3133/ofr20071047SRP088","usgsCitation":"Gooseff, M.N., McKnight, D.M., Doran, P.T., and Lyons, W.B., 2007, Trends in discharge and flow season timing of the Onyx River, Wright Valley, Antarctica since 1969: U.S. Geological Survey Open-File Report 2007-1047-SRP-088, 4 p., https://doi.org/10.3133/ofr20071047SRP088.","productDescription":"4 p.","additionalOnlineFiles":"N","costCenters":[],"links":[{"id":285879,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/ofr20071047SRP088.PNG"},{"id":285878,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/2007/1047/srp/srp088/of2007-1047srp088.pdf"}],"otherGeospatial":"Antarctica","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ 180.0,-90.0 ], [ 180.0,-60.0 ], [ -180.0,-60.0 ], [ -180.0,-90.0 ], [ 180.0,-90.0 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"535595a3e4b0120853e8c2aa","contributors":{"authors":[{"text":"Gooseff, Michael N.","contributorId":71880,"corporation":false,"usgs":true,"family":"Gooseff","given":"Michael","email":"","middleInitial":"N.","affiliations":[],"preferred":false,"id":492480,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"McKnight, Diane M.","contributorId":59773,"corporation":false,"usgs":false,"family":"McKnight","given":"Diane","email":"","middleInitial":"M.","affiliations":[{"id":16833,"text":"INSTAAR, University of Colorado","active":true,"usgs":false}],"preferred":false,"id":492478,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Doran, Peter T.","contributorId":67007,"corporation":false,"usgs":true,"family":"Doran","given":"Peter","email":"","middleInitial":"T.","affiliations":[],"preferred":false,"id":492479,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Lyons, W. Berry","contributorId":73497,"corporation":false,"usgs":true,"family":"Lyons","given":"W.","email":"","middleInitial":"Berry","affiliations":[],"preferred":false,"id":492481,"contributorType":{"id":1,"text":"Authors"},"rank":4}]}} ,{"id":70094154,"text":"ofr20071047SRP047 - 2007 - Geophysical survey reveals tectonic structures in the Amundsen Sea embayment, West Antarctica","interactions":[],"lastModifiedDate":"2014-02-18T09:50:56","indexId":"ofr20071047SRP047","displayToPublicDate":"2007-01-01T09:11:00","publicationYear":"2007","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":330,"text":"Open-File Report","code":"OFR","onlineIssn":"2331-1258","printIssn":"0196-1497","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"2007-1047-SRP-047","title":"Geophysical survey reveals tectonic structures in the Amundsen Sea embayment, West Antarctica","docAbstract":"The Amundsen Sea embayment of West Antarctica is in a prominent location for a series of tectonic and magmatic events from Paleozoic to Cenozoic times. Seismic, magnetic and gravity data from the embayment and Pine\nIsland Bay (PIB) reveal the crustal thickness and some tectonic features. The Moho is 24-22 km deep on the shelf. NE-SW trending magnetic and gravity anomalies and the thin crust indicate a former rift zone that was active during or in the run-up to breakup between Chatham Rise and West Antarctica before or at 90 Ma. NW-SE trending gravity and magnetic anomalies, following a prolongation of Peacock Sound, indicate the extensional southern boundary to the Bellingshausen Plate which was active between 79 and 61 Ma.","largerWorkType":{"id":18,"text":"Report"},"largerWorkTitle":"Antarctica: A Keystone in a Changing World--Online Proceedings for the Tenth International Symposium on Antarctic Earth Sciences. Santa Barbara, California, U.S.A.--August 26 to September 1, 2007","largerWorkSubtype":{"id":5,"text":"USGS Numbered Series"},"language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Reston, VA","doi":"10.3133/ofr20071047SRP047","usgsCitation":"Gohl, K., Eagles, G., Netzeband, G., Grobys, J., Parsiegla, N., Schluter, P., Leinweber, V., Larter, R., Uenzelmann-Neben, G., and Udintsev, G., 2007, Geophysical survey reveals tectonic structures in the Amundsen Sea embayment, West Antarctica: U.S. Geological Survey Open-File Report 2007-1047-SRP-047, 4 p., https://doi.org/10.3133/ofr20071047SRP047.","productDescription":"4 p.","additionalOnlineFiles":"N","costCenters":[],"links":[{"id":282461,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/ofr20071047SRP047.JPG"},{"id":282460,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/2007/1047/srp/srp047/of2007-1047srp047.pdf"}],"otherGeospatial":"Antarctica","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -180.0,-90.0 ], [ -180.0,-60.0 ], [ 180.0,-60.0 ], [ 180.0,-90.0 ], [ -180.0,-90.0 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"53cd5ed0e4b0b290850fbecd","contributors":{"authors":[{"text":"Gohl, K.","contributorId":53285,"corporation":false,"usgs":true,"family":"Gohl","given":"K.","email":"","affiliations":[],"preferred":false,"id":490470,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Eagles, G.","contributorId":107196,"corporation":false,"usgs":true,"family":"Eagles","given":"G.","email":"","affiliations":[],"preferred":false,"id":490475,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Netzeband, G.","contributorId":61745,"corporation":false,"usgs":true,"family":"Netzeband","given":"G.","email":"","affiliations":[],"preferred":false,"id":490471,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Grobys, J.W.G.","contributorId":32086,"corporation":false,"usgs":true,"family":"Grobys","given":"J.W.G.","email":"","affiliations":[],"preferred":false,"id":490469,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"Parsiegla, N.","contributorId":11116,"corporation":false,"usgs":true,"family":"Parsiegla","given":"N.","email":"","affiliations":[],"preferred":false,"id":490467,"contributorType":{"id":1,"text":"Authors"},"rank":5},{"text":"Schluter, P.","contributorId":102384,"corporation":false,"usgs":true,"family":"Schluter","given":"P.","email":"","affiliations":[],"preferred":false,"id":490473,"contributorType":{"id":1,"text":"Authors"},"rank":6},{"text":"Leinweber, V.","contributorId":81799,"corporation":false,"usgs":true,"family":"Leinweber","given":"V.","email":"","affiliations":[],"preferred":false,"id":490472,"contributorType":{"id":1,"text":"Authors"},"rank":7},{"text":"Larter, R.D.","contributorId":8765,"corporation":false,"usgs":true,"family":"Larter","given":"R.D.","email":"","affiliations":[],"preferred":false,"id":490466,"contributorType":{"id":1,"text":"Authors"},"rank":8},{"text":"Uenzelmann-Neben, G.","contributorId":22682,"corporation":false,"usgs":true,"family":"Uenzelmann-Neben","given":"G.","email":"","affiliations":[],"preferred":false,"id":490468,"contributorType":{"id":1,"text":"Authors"},"rank":9},{"text":"Udintsev, G.B.","contributorId":106411,"corporation":false,"usgs":true,"family":"Udintsev","given":"G.B.","email":"","affiliations":[],"preferred":false,"id":490474,"contributorType":{"id":1,"text":"Authors"},"rank":10}]}} ,{"id":70094354,"text":"ofr20071047SRP061 - 2007 - Geometrical analysis of structural data collected at high South latitude: A modular arithmetic method that addresses meridional convergence","interactions":[],"lastModifiedDate":"2014-02-24T12:49:04","indexId":"ofr20071047SRP061","displayToPublicDate":"2007-01-01T09:04:00","publicationYear":"2007","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":330,"text":"Open-File Report","code":"OFR","onlineIssn":"2331-1258","printIssn":"0196-1497","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"2007-1047-SRP-061","title":"Geometrical analysis of structural data collected at high South latitude: A modular arithmetic method that addresses meridional convergence","docAbstract":"The convergence of meridians toward the South Pole causes unique problems for geometrical comparison of \nstructural geological and geophysical datasets from Antarctica. The true North reference direction ordinarily is used for \nmeasuring and reporting vector data (strike, trend) in Antarctica, as elsewhere. However, over a latitude distance of just \n100 km at 85° South, the angular difference in the true North direction exceeds 10°. Consequently, when performing a \nregional tectonic analysis of vector data (strike, trend) for structures such as faults, dike arrays, or geophysical \nlineaments oriented with respect to North at different sites, it is necessary to rotate the data to a common reference \ndirection. A modular arithmetic function, performed as a spreadsheet calculation, offers the means to unify data sets \nfrom sites having different longitude position, by rotation to a common reference direction. The function is \nSC ≡ SM + ∆L (mod 360), where SC = converted strike; SM = measured strike; ∆L = angle in degrees longitude between \nreference longitude and study site; and 360, the divisor, is the number of degrees in Earth’s circumference. The method \nis used to evaluate 1) paleomagnetic rotation of the Ellsworth-Whitmore Mountains with respect to the Transantarctic \nMountains, and 2) orogenic curvature of the Ross Orogen","largerWorkType":{"id":18,"text":"Report"},"largerWorkTitle":"Antarctica: A Keystone in a Changing World--Online Proceedings for the Tenth International Symposium on Antarctic Earth Sciences. Santa Barbara, California, U.S.A.--August 26 to September 1, 2007","largerWorkSubtype":{"id":5,"text":"USGS Numbered Series"},"language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Reston, VA","doi":"10.3133/ofr20071047SRP061","usgsCitation":"Siddoway, C., and Siddoway, M., 2007, Geometrical analysis of structural data collected at high South latitude: A modular arithmetic method that addresses meridional convergence: U.S. Geological Survey Open-File Report 2007-1047-SRP-061, Report: 5 p.; Plate: XLS file, https://doi.org/10.3133/ofr20071047SRP061.","productDescription":"Report: 5 p.; Plate: XLS file","additionalOnlineFiles":"Y","costCenters":[],"links":[{"id":282681,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/ofr20071047SRP061.png"},{"id":282676,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/2007/1047/srp/srp061/of2007-1047srp061.pdf"},{"id":282677,"type":{"id":7,"text":"Companion Files"},"url":"https://pubs.usgs.gov/of/2007/1047/srp/srp061/of2007-1047srp061_plate1.xls"}],"otherGeospatial":"Antarctica","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ 180.0,-90.0 ], [ 180.0,-60.0 ], [ -180.0,-60.0 ], [ -180.0,-90.0 ], [ 180.0,-90.0 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"53cd5e97e4b0b290850fbcc2","contributors":{"authors":[{"text":"Siddoway, C.S.","contributorId":28893,"corporation":false,"usgs":true,"family":"Siddoway","given":"C.S.","email":"","affiliations":[],"preferred":false,"id":490582,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Siddoway, M.F.","contributorId":34425,"corporation":false,"usgs":true,"family":"Siddoway","given":"M.F.","email":"","affiliations":[],"preferred":false,"id":490583,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":70098927,"text":"ofr20071047SRP073 - 2007 - Vertical motions in Northern Victoria Land inferred from GPS: A comparison with a glacial isostatic adjustment model","interactions":[],"lastModifiedDate":"2014-03-19T09:33:39","indexId":"ofr20071047SRP073","displayToPublicDate":"2007-01-01T08:55:00","publicationYear":"2007","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":330,"text":"Open-File Report","code":"OFR","onlineIssn":"2331-1258","printIssn":"0196-1497","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"2007-1047-SRP-073","title":"Vertical motions in Northern Victoria Land inferred from GPS: A comparison with a glacial isostatic adjustment model","docAbstract":"Following the densification of GPS permanent and episodic trackers in Antarctica, geodetic observations \nare playing an increasing role in geodynamics research and the study of the glacial isostatic adjustment (GIA). The \nimprovement in geodetic measurements accuracy suggests their use in constraining GIA models. It is essential to have a \ndeeper knowledge on the sensitivity of GPS data to motionsrelated to long-term ice mass changes and the present-day \nmass imbalance of the ice sheets. In order to investigate the geodynamic phenomena in Northern Victoria Land (NVL), \nGPS geodetic observations were made during the last decade within the VLNDEF (Victoria Land Network for \nDeformation control) project. The processed data provided a picture of the motions occurring in NVL with a high level \nof accuracy and depicts, for the whole period, a well defined pattern of vertical motion. The comparison between GPS-derived vertical displacementsand GIA is addressed, showing a good degree of agreement and highlighting the future \nuse of geodetic GPS measurements as constraints in GIA models. In spite of this agreement, the sensitivity of GPS \nvertical rates to non-GIA vertical motions has to be carefully evaluated.","largerWorkType":{"id":18,"text":"Report"},"largerWorkTitle":"Antarctica: A Keystone in a Changing World--Online Proceedings for the Tenth International Symposium on Antarctic Earth Sciences. Santa Barbara, California, U.S.A.--August 26 to September 1, 2007","largerWorkSubtype":{"id":5,"text":"USGS Numbered Series"},"language":"English","publisher":"U.S Geological Survey","publisherLocation":"Reston, VA","doi":"10.3133/ofr20071047SRP073","usgsCitation":"Mancini, F., Negusini, M., Zanutta, A., and Capra, A., 2007, Vertical motions in Northern Victoria Land inferred from GPS: A comparison with a glacial isostatic adjustment model: U.S. Geological Survey Open-File Report 2007-1047-SRP-073, 5 p., https://doi.org/10.3133/ofr20071047SRP073.","productDescription":"5 p.","additionalOnlineFiles":"N","costCenters":[],"links":[{"id":284198,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/ofr20071047SRP073.PNG"}],"otherGeospatial":"Antarctica","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ 180.0,-90.0 ], [ 180.0,-60.0 ], [ -180.0,-60.0 ], [ -180.0,-90.0 ], [ 180.0,-90.0 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"53cd7b0ee4b0b2908510de5a","contributors":{"authors":[{"text":"Mancini, F.","contributorId":93812,"corporation":false,"usgs":true,"family":"Mancini","given":"F.","email":"","affiliations":[],"preferred":false,"id":491735,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Negusini, M.","contributorId":107185,"corporation":false,"usgs":true,"family":"Negusini","given":"M.","email":"","affiliations":[],"preferred":false,"id":491736,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Zanutta, A.","contributorId":86258,"corporation":false,"usgs":true,"family":"Zanutta","given":"A.","email":"","affiliations":[],"preferred":false,"id":491734,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Capra, A.","contributorId":84662,"corporation":false,"usgs":true,"family":"Capra","given":"A.","email":"","affiliations":[],"preferred":false,"id":491733,"contributorType":{"id":1,"text":"Authors"},"rank":4}]}} ,{"id":70047552,"text":"ds69J6 - 2007 - Burial history, thermal maturity, and oil and gas generation history of petroleum systems in the Wind River Basin Province, central Wyoming: Chapter 6 in Petroleum systems and geologic assessment of oil and gas resources in the Wind River Basin Province, Wyoming","interactions":[],"lastModifiedDate":"2013-08-12T09:13:58","indexId":"ds69J6","displayToPublicDate":"2007-01-01T08:48:00","publicationYear":"2007","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":310,"text":"Data Series","code":"DS","onlineIssn":"2327-638X","printIssn":"2327-0271","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"69-J-6","title":"Burial history, thermal maturity, and oil and gas generation history of petroleum systems in the Wind River Basin Province, central Wyoming: Chapter 6 in Petroleum systems and geologic assessment of oil and gas resources in the Wind River Basin Province, Wyoming","docAbstract":"Burial history, thermal maturity, and timing of oil and gas \ngeneration were modeled for eight key source rock units at \nnine well locations throughout the Wind River Basin Province. \nPetroleum source rocks include the Permian Phosphoria \nFormation, the Cretaceous Mowry Shale, Cody Shale, and \nMesaverde, Meeteetse, and Lance Formations, and the Tertiary \n(Paleocene) Fort Union Formation, including the Waltman \nShale Member. Within the province boundary, the Phosphoria \nis thin and only locally rich in organic carbon. Phosphoria oil \nproduced from reservoirs in the province is thought to have \nmigrated from the Wyoming and Idaho thrust belt. \nLocations (wells) selected for burial history \nreconstructions include three in the deepest parts of the \nprovince (Adams OAB-17, Bighorn 1-5, and Coastal Owl \nCreek); three at intermediate depths (Hells Half Acre, Shell \n33X-10, and West Poison Spider); and three at relatively \nshallow locations (Young Ranch, Amoco Unit 100, and \nConoco-Coal Bank). The thermal maturity of source rocks is \ngreatest in the deep northern and central parts of the province \nand decreases to the south and east toward the basin margins. \nThe results of the modeling indicate that, in the deepest areas, \n(1) peak petroleum generation from Cretaceous rocks occurred \nfrom Late Cretaceous through middle Eocene time, and (2) \nonset of oil generation from the Waltman Shale Member \noccurred from late Eocene to early Miocene time. \nBased on modeling results, gas generation from the \ncracking of Phosphoria oil reservoired in the Park City \nFormation reached a peak in the late Paleocene/early Eocene \n(58 to 55 Ma) only in the deepest parts of the province. The \nMowry Shale and Cody Shale (in the eastern half of the basin) \ncontain a mix of Type-II and Type-III kerogens. Oil generation \nfrom predominantly Type-II source rocks of these units in the \ndeepest parts of the province reached peak rates during the \nlatest Cretaceous to early Eocene (65 to 55 Ma). Only in these \nareas of the basin did these units reach peak gas generation \nfrom the cracking of oil, which occurred in the early to middle \nEocene (55 to 42 Ma). \nGas-prone source rocks of the Mowry and Cody Shales \n(predominantly Type-III kerogen), and the Mesaverde, \nMeeteetse, Lance, and Fort Union Formations (Type –III \nkerogen) reached peak gas generation in the latest Cretaceous \nto late Eocene (67 to 38 Ma) in the deepest parts of the \nprovince. Gas generation from the Mesaverde source rocks \nstarted at all of the modeled locations but reached peak \ngeneration at only the deepest locations and at the Hells Half \nAcre location in the middle Paleocene to early Eocene (59 to \n48 Ma). Also at the deepest locations, peak gas generation \noccurred from the late Paleocene to the early Eocene (57 to \n49 Ma) for the Meeteetse Formation, and during the Eocene \nfor the Lance Formation (55 to 48 Ma) and the Fort Union \nFormation (44 to 38 Ma). \nThe Waltman Shale Member of the Fort Union Formation \ncontains Type-II kerogen. The base of the Waltman reached a \nlevel of thermal maturity to generate oil only at the deep-basin \nlocations (Adams OAB-17 and Bighorn 1-5 locations) in the \nmiddle Eocene to early Miocene (36 to 20 Ma).","largerWorkType":{"id":18,"text":"Report"},"largerWorkTitle":"Petroleum systems and geologic assessment of oil and gas resources in the Wind River Basin Province, Wyoming (Data Series 69-J)","largerWorkSubtype":{"id":5,"text":"USGS Numbered Series"},"language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Reston, VA","doi":"10.3133/ds69J6","collaboration":"This report is Chapter 6 in Petroleum systems and geologic assessment of oil and gas resources in the Wind River Basin Province, Wyoming. For more information, see: Data Series 69-J.","usgsCitation":"Roberts, L.N., Finn, T.M., Lewan, M., and Kirschbaum, M.A., 2007, Burial history, thermal maturity, and oil and gas generation history of petroleum systems in the Wind River Basin Province, central Wyoming: Chapter 6 in Petroleum systems and geologic assessment of oil and gas resources in the Wind River Basin Province, Wyoming: U.S. Geological Survey Data Series 69-J-6, iv, 26 p., https://doi.org/10.3133/ds69J6.","productDescription":"iv, 26 p.","numberOfPages":"30","costCenters":[{"id":674,"text":"Wind River Basin Province Assessment Team","active":false,"usgs":true}],"links":[{"id":276297,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/ds69j6.png"},{"id":276295,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.usgs.gov/dds/dds-069/dds-069-j/"},{"id":276296,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/dds/dds-069/dds-069-j/REPORTS/69_J_CH_6.pdf"}],"country":"United States","state":"Wyoming","otherGeospatial":"Wind River Basin Province","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -110.1,42.0 ], [ -110.1,44.0 ], [ -106.0,44.0 ], [ -106.0,42.0 ], [ -110.1,42.0 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"520a03e3e4b0026c2bc11ad1","contributors":{"authors":[{"text":"Roberts, Laura N.R.","contributorId":79530,"corporation":false,"usgs":true,"family":"Roberts","given":"Laura","email":"","middleInitial":"N.R.","affiliations":[],"preferred":false,"id":482384,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Finn, Thomas M. 0000-0001-6396-9351 finn@usgs.gov","orcid":"https://orcid.org/0000-0001-6396-9351","contributorId":778,"corporation":false,"usgs":true,"family":"Finn","given":"Thomas","email":"finn@usgs.gov","middleInitial":"M.","affiliations":[{"id":164,"text":"Central Energy Resources Science Center","active":true,"usgs":true}],"preferred":true,"id":482381,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Lewan, Michael D. mlewan@usgs.gov","contributorId":940,"corporation":false,"usgs":true,"family":"Lewan","given":"Michael D.","email":"mlewan@usgs.gov","affiliations":[{"id":164,"text":"Central Energy Resources Science Center","active":true,"usgs":true}],"preferred":false,"id":482382,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Kirschbaum, Mark A.","contributorId":25112,"corporation":false,"usgs":true,"family":"Kirschbaum","given":"Mark","email":"","middleInitial":"A.","affiliations":[],"preferred":false,"id":482383,"contributorType":{"id":1,"text":"Authors"},"rank":4}]}} ,{"id":70203722,"text":"ds310 - 2007 - Archive of digital CHIRP seismic reflection data collected during USGS cruise 06SCC02 offshore of the Chandeleur Islands, Louisiana, July 2006","interactions":[],"lastModifiedDate":"2024-03-28T13:44:08.093827","indexId":"ds310","displayToPublicDate":"2007-01-01T08:40:14","publicationYear":"2007","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":310,"text":"Data Series","code":"DS","onlineIssn":"2327-638X","printIssn":"2327-0271","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"310","title":"Archive of digital CHIRP seismic reflection data collected during USGS cruise 06SCC02 offshore of the Chandeleur Islands, Louisiana, July 2006","docAbstract":"

In July of 2006, the U.S. Geological Survey (USGS) conducted a geophysical survey offshore of the Chandeleur Islands, Louisiana, as part of the USGS Barrier Island Coastal Monitoring project (BICM), which is part of a broader study focused on Subsidence and Coastal Change (SCC). This report serves as an archive of unprocessed digital Compressed High Intensity Radar Pulse (CHIRP) seismic reflection data, trackline maps, navigation files, Geographic Information System (GIS) files, Field Activity Collection System (FACS) logs, observer's logbook, and formal Federal Geographic Data Committee (FGDC) metadata. Gained (a relative increase in signal amplitude has been applied) digital images of the seismic profiles are also provided.

","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Reston, Virginia","doi":"10.3133/ds310","usgsCitation":"Harrison, A.S., Dadisman, S.V., Flocks, J.G., and Wiese, D.S., 2007, Archive of digital CHIRP seismic reflection data collected during USGS cruise 06SCC02 offshore of the Chandeleur Islands, Louisiana, July 2006: U.S. Geological Survey Data Series 310, HTML Document; DVD-ROM, https://doi.org/10.3133/ds310.","productDescription":"HTML Document; DVD-ROM","costCenters":[{"id":574,"text":"St. Petersburg Coastal and Marine Science Center","active":true,"usgs":true}],"links":[{"id":364457,"rank":2,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":427109,"rank":1,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.usgs.gov/ds/310/","text":"Index Page","linkFileType":{"id":5,"text":"html"}}],"country":"United States","state":"Louisiana","otherGeospatial":"Chandeleur Islands","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"coordinates\": [\n [\n [\n -88.97638843437915,\n 29.63123061994284\n ],\n [\n -88.8427472203541,\n 29.764247592634817\n ],\n [\n -88.80933691684783,\n 29.893065321154907\n ],\n [\n -88.8139772367792,\n 29.98394268222883\n ],\n [\n -88.86873301196997,\n 30.056263445613283\n ],\n [\n -88.87986977980538,\n 30.021716772371022\n ],\n [\n -88.8427472203541,\n 29.90835138980472\n ],\n [\n -88.88729429169578,\n 29.82384643207277\n ],\n [\n -88.917920403243,\n 29.747327944632474\n ],\n [\n -89.00794260991272,\n 29.652202556506026\n ],\n [\n -89.01815131376178,\n 29.633650681696338\n ],\n [\n -88.97638843437915,\n 29.63123061994284\n ]\n ]\n ],\n \"type\": \"Polygon\"\n }\n }\n ]\n}","contact":"

Contact Pubs Warehouse

","tableOfContents":"","publishingServiceCenter":{"id":9,"text":"Reston PSC"},"noUsgsAuthors":false,"publicationStatus":"PW","contributors":{"authors":[{"text":"Harrison, Arnell S. 0000-0002-5581-2255","orcid":"https://orcid.org/0000-0002-5581-2255","contributorId":35021,"corporation":false,"usgs":true,"family":"Harrison","given":"Arnell","email":"","middleInitial":"S.","affiliations":[],"preferred":false,"id":763811,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Dadisman, Shawn V. sdadisman@usgs.gov","contributorId":2207,"corporation":false,"usgs":true,"family":"Dadisman","given":"Shawn","email":"sdadisman@usgs.gov","middleInitial":"V.","affiliations":[],"preferred":true,"id":763812,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Flocks, James G. 0000-0002-6177-7433 jflocks@usgs.gov","orcid":"https://orcid.org/0000-0002-6177-7433","contributorId":816,"corporation":false,"usgs":true,"family":"Flocks","given":"James","email":"jflocks@usgs.gov","middleInitial":"G.","affiliations":[{"id":574,"text":"St. Petersburg Coastal and Marine Science Center","active":true,"usgs":true}],"preferred":true,"id":763813,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Wiese, Dana S. dwiese@usgs.gov","contributorId":2476,"corporation":false,"usgs":true,"family":"Wiese","given":"Dana","email":"dwiese@usgs.gov","middleInitial":"S.","affiliations":[{"id":574,"text":"St. Petersburg Coastal and Marine Science Center","active":true,"usgs":true}],"preferred":true,"id":763814,"contributorType":{"id":1,"text":"Authors"},"rank":4}]}} ,{"id":80849,"text":"ofr20071266 - 2007 - Field-based evaluations of sampling techniques to support long-term monitoring of riparian ecosystems along wadeable streams on the Colorado Plateau","interactions":[],"lastModifiedDate":"2016-05-26T16:06:14","indexId":"ofr20071266","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":"2007-1266","title":"Field-based evaluations of sampling techniques to support long-term monitoring of riparian ecosystems along wadeable streams on the Colorado Plateau","docAbstract":"

To better plan for and implement long-term ecological monitoring, we measured riparian vegetation and fluvial geomorphic features at pilot study sites on four wadeable perennial stream reaches, representative of drainages across the Colorado Plateau. Our primary objectives were to (1) collect field data, (2) evaluate the efficiency and effectiveness of various ecological measures and measurement techniques for riparian ecosystems, and (3) use field-based sampling to inform and refine the development of standard operating procedures for use in implementing integrated, long-term monitoring of riparian ecosystems. Ultimately, this work was aimed at providing NPS staff with some of the information and methods needed to design and implement long-term monitoring of NPS riparian resources, which is both relevant to management, and fully operational within institutional resource constraints.

\n

Our results suggest that selecting sampling reaches and establishing a sampling frame of 11 transects, across a range of stream types, is feasible given a limited set of decision rules. A distinctive feature of richness across all sites was the high percentage of rare species, defined here as species having a single occurrence at a site. Rare species represented from 33 percent to 47 percent of the species total across the four pilot sites. Our data show that the two smallest quadrat sizes, 0.01 m2 and 0.1 m2 , rarely had any species that occurred in the desired frequency range and can be omitted from the monitoring protocol. Few species fell within the 30–70 percent range in the 1-m2 quadrats, but this quadrat size appears to be useful at the Tsaile Creek (CACH) site. We recommend continuing to collect information at the 1-m2 scale and reevaluating its usefulness after more data are available from different types of sites. The 10-m2 quadrat is adequate for monitoring changes in frequencies of very common species at all sites. Based on pilot study results, we conclude that at sites with low total species numbers (< 60 species), 40–60, 10-m2 quadrats, would be sufficient to characterize overall species diversity for relatively common species. At sites with higher total numbers of species (> 100), 60–80, 10-m2 quadrats would be required to characterize overall species diversity. Rare species of interest should be monitored using alternative approaches, such as a site inventory and/or mapping (see Elzinga and others, 1998). A large number of the systematically placed 10-m2 quadrats span two or more geomorphic surfaces, especially adjacent to the channel. This makes resolution of species affinities with distinct geomorphic landforms difficult. Thus, we provide an amendment to improve characterization of herbaceous and shrub species on narrow, near-channel surfaces by sampling additional 0.5-m by 1-m quadrats on those surfaces. It appears that for sites in narrow valley settings where riparian zones average less than approximately 40 m, the number of 10-m2 quadrats systematically placed on 11 transects will not provide shrub cover estimates at 20 percent precision. In such cases, additional sample reaches should be added in order to attain a minimum of 130 to 140 10-m2 shrub quadrats. 

\n

The line-intercept technique can provide a relatively rapid, reach-scale quantification of proportional cover for woody vegetation and geomorphic surface types and that variance in these measures stabilizes by the eighth or ninth transect sampled. An overlay of the distribution of geomorphic surface data derived from line-intercept sampling on topographic survey information indicates that delineation of geomorphic surfaces could be done in conjunction with the topographic survey of each transect, obviating the need to record surface breaks using the line intercept. To include geomorphic surface identifications with the topographic survey, surface breaks and transitional surfaces should be included and identified in the survey, in addition to systematically placed survey points.

\n

Compared to 5-m by 20-m tree quadrats, belt transects were shown to provide similar estimates of stand structure (stem density and stand basal area) in less than 30 percent of the time. Further, for the streams sampled, there were no statistically significant differences in stem density and basal area estimates between 10-m and 20-m belt transects and the smaller belts took approximately half the time to sample. There was, however, high variance associated with estimates of stand structure for infrequently occurring stems, such as large, relict or legacy riparian trees. Legacy riparian trees occurred in limited numbers at all sites sampled. A reachscale population census of these trees indicated that the 10-m belt transects tended to underestimate both stem density and basal area for these riparian forest elements and that a complete reach-scale census of legacy trees averaged less than one hour per site.

","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Reston, VA","doi":"10.3133/ofr20071266","collaboration":"Prepared in cooperation with the Northern and Southern Colorado Plateau Park Networks","usgsCitation":"Scott, M.L., and Reynolds, E.W., 2007, Field-based evaluations of sampling techniques to support long-term monitoring of riparian ecosystems along wadeable streams on the Colorado Plateau: U.S. Geological Survey Open-File Report 2007-1266, iv, 57 p., https://doi.org/10.3133/ofr20071266.","productDescription":"iv, 57 p.","numberOfPages":"63","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[{"id":291,"text":"Fort Collins Science Center","active":true,"usgs":true}],"links":[{"id":192352,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/ofr20071266.PNG"},{"id":320212,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/2007/1266/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"country":"United States","otherGeospatial":"Colorado Plateau","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e48b1e4b07f02db530787","contributors":{"authors":[{"text":"Scott, Michael L. scottm@usgs.gov","contributorId":1169,"corporation":false,"usgs":true,"family":"Scott","given":"Michael","email":"scottm@usgs.gov","middleInitial":"L.","affiliations":[{"id":291,"text":"Fort Collins Science Center","active":true,"usgs":true}],"preferred":true,"id":293687,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Reynolds, Elizabeth W.","contributorId":89986,"corporation":false,"usgs":true,"family":"Reynolds","given":"Elizabeth","email":"","middleInitial":"W.","affiliations":[],"preferred":false,"id":293688,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":70182553,"text":"70182553 - 2007 - The National Elevation Dataset","interactions":[],"lastModifiedDate":"2017-03-31T13:14:51","indexId":"70182553","displayToPublicDate":"2007-01-01T00:00:00","publicationYear":"2007","noYear":false,"publicationType":{"id":5,"text":"Book chapter"},"publicationSubtype":{"id":24,"text":"Book Chapter"},"title":"The National Elevation Dataset","docAbstract":"

No abstract available.

","largerWorkType":{"id":4,"text":"Book"},"largerWorkTitle":"Digital elevation model technologies and applications—the DEM users manual","language":"English","publisher":"American Society for Photogrammetry and Remote Sensing","publisherLocation":"Bethesda, MD","usgsCitation":"Gesch, D., 2007, The National Elevation Dataset, chap. of Digital elevation model technologies and applications—the DEM users manual, p. 99-118.","productDescription":"20 p. ","startPage":"99","endPage":"118","costCenters":[{"id":222,"text":"Earth Resources Observation and Science (EROS) Center","active":true,"usgs":true}],"links":[{"id":336208,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"58b1543de4b01ccd54fc5eb1","contributors":{"editors":[{"text":"Maune, D.","contributorId":182509,"corporation":false,"usgs":false,"family":"Maune","given":"D.","affiliations":[],"preferred":false,"id":671670,"contributorType":{"id":2,"text":"Editors"},"rank":1}],"authors":[{"text":"Gesch, D.B. 0000-0002-8992-4933","orcid":"https://orcid.org/0000-0002-8992-4933","contributorId":26886,"corporation":false,"usgs":true,"family":"Gesch","given":"D.B.","affiliations":[],"preferred":false,"id":671669,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":70031064,"text":"70031064 - 2007 - Prediction of lethal/effective concentration/dose in the presence of multiple auxiliary covariates and components of variance","interactions":[],"lastModifiedDate":"2012-03-12T17:21:16","indexId":"70031064","displayToPublicDate":"2007-01-01T00:00:00","publicationYear":"2007","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1571,"text":"Environmental Toxicology and Chemistry","active":true,"publicationSubtype":{"id":10}},"title":"Prediction of lethal/effective concentration/dose in the presence of multiple auxiliary covariates and components of variance","docAbstract":"Predictors of the percentile lethal/effective concentration/dose are commonly used measures of efficacy and toxicity. Typically such quantal-response predictors (e.g., the exposure required to kill 50% of some population) are estimated from simple bioassays wherein organisms are exposed to a gradient of several concentrations of a single agent. The toxicity of an agent may be influenced by auxiliary covariates, however, and more complicated experimental designs may introduce multiple variance components. Prediction methods lag examples of those cases. A conventional two-stage approach consists of multiple bivariate predictions of, say, medial lethal concentration followed by regression of those predictions on the auxiliary covariates. We propose a more effective and parsimonious class of generalized nonlinear mixed-effects models for prediction of lethal/effective dose/concentration from auxiliary covariates. We demonstrate examples using data from a study regarding the effects of pH and additions of variable quantities 2???,5???-dichloro-4???- nitrosalicylanilide (niclosamide) on the toxicity of 3-trifluoromethyl-4- nitrophenol to larval sea lamprey (Petromyzon marinus). The new models yielded unbiased predictions and root-mean-squared errors (RMSEs) of prediction for the exposure required to kill 50 and 99.9% of some population that were 29 to 82% smaller, respectively, than those from the conventional two-stage procedure. The model class is flexible and easily implemented using commonly available software. ?? 2007 SETAC.","largerWorkType":{"id":2,"text":"Article"},"largerWorkTitle":"Environmental Toxicology and Chemistry","largerWorkSubtype":{"id":10,"text":"Journal Article"},"language":"English","doi":"10.1897/06-630R.1","issn":"07307268","usgsCitation":"Gutreuter, S., and Boogaard, M., 2007, Prediction of lethal/effective concentration/dose in the presence of multiple auxiliary covariates and components of variance: Environmental Toxicology and Chemistry, v. 26, no. 9, p. 1978-1986, https://doi.org/10.1897/06-630R.1.","startPage":"1978","endPage":"1986","numberOfPages":"9","costCenters":[],"links":[{"id":211453,"rank":9999,"type":{"id":10,"text":"Digital Object Identifier"},"url":"https://dx.doi.org/10.1897/06-630R.1"},{"id":238744,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"26","issue":"9","noUsgsAuthors":false,"publicationDate":"2007-09-01","publicationStatus":"PW","scienceBaseUri":"505a81efe4b0c8380cd7b7f1","contributors":{"authors":[{"text":"Gutreuter, S.","contributorId":79829,"corporation":false,"usgs":true,"family":"Gutreuter","given":"S.","email":"","affiliations":[],"preferred":false,"id":429887,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Boogaard, M.A.","contributorId":92994,"corporation":false,"usgs":true,"family":"Boogaard","given":"M.A.","email":"","affiliations":[],"preferred":false,"id":429888,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":70031085,"text":"70031085 - 2007 - Revisiting the cape cod bacteria injection experiment using a stochastic modeling approach","interactions":[],"lastModifiedDate":"2018-10-17T11:32:08","indexId":"70031085","displayToPublicDate":"2007-01-01T00:00:00","publicationYear":"2007","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1565,"text":"Environmental Science & Technology","onlineIssn":"1520-5851","printIssn":"0013-936X","active":true,"publicationSubtype":{"id":10}},"title":"Revisiting the cape cod bacteria injection experiment using a stochastic modeling approach","docAbstract":"

Bromide and resting-cell bacteria tracer tests conducted in a sandy aquifer at the U.S. Geological Survey Cape Cod site in 1987 were reinterpreted using a three-dimensional stochastic approach. Bacteria transport was coupled to colloid filtration theory through functional dependence of local-scale colloid transport parameters upon hydraulic conductivity and seepage velocity in a stochastic advection - dispersion/attachment - detachment model. Geostatistical information on the hydraulic conductivity (K) field that was unavailable at the time of the original test was utilized as input. Using geostatistical parameters, a groundwater flow and particle-tracking model of conservative solute transport was calibrated to the bromide-tracer breakthrough data. An optimization routine was employed over 100 realizations to adjust the mean and variance ofthe natural-logarithm of hydraulic conductivity (InK) field to achieve best fit of a simulated, average bromide breakthrough curve. A stochastic particle-tracking model for the bacteria was run without adjustments to the local-scale colloid transport parameters. Good predictions of mean bacteria breakthrough were achieved using several approaches for modeling components of the system. Simulations incorporating the recent Tufenkji and Elimelech (Environ. Sci. Technol. 2004, 38, 529-536) correlation equation for estimating single collector efficiency were compared to those using the older Rajagopalan and Tien (AIChE J. 1976, 22, 523-533) model. Both appeared to work equally well at predicting mean bacteria breakthrough using a constant mean bacteria diameter for this set of field conditions. Simulations using a distribution of bacterial cell diameters available from original field notes yielded a slight improvement in the model and data agreement compared to simulations using an average bacterial diameter. The stochastic approach based on estimates of local-scale parameters for the bacteria-transport process reasonably captured the mean bacteria transport behavior and calculated an envelope of uncertainty that bracketed the observations in most simulation cases.

","largerWorkType":{"id":2,"text":"Article"},"largerWorkTitle":"Environmental Science and Technology","largerWorkSubtype":{"id":10,"text":"Journal Article"},"language":"English","publisher":"American Chemical Society","doi":"10.1021/es062693a","issn":"0013936X","usgsCitation":"Maxwell, R.M., Welty, C., and Harvey, R.W., 2007, Revisiting the cape cod bacteria injection experiment using a stochastic modeling approach: Environmental Science & Technology, v. 41, no. 15, p. 5548-5558, https://doi.org/10.1021/es062693a.","productDescription":"11 p.","startPage":"5548","endPage":"5558","numberOfPages":"11","costCenters":[{"id":589,"text":"Toxic Substances Hydrology Program","active":true,"usgs":true}],"links":[{"id":486982,"rank":10000,"type":{"id":41,"text":"Open Access External Repository Page"},"url":"https://figshare.com/articles/journal_contribution/Revisiting_the_Cape_Cod_Bacteria_Injection_Experiment_Using_a_Stochastic_Modeling_Approach/2993503","text":"External Repository"},{"id":239045,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"},{"id":211703,"rank":9999,"type":{"id":10,"text":"Digital Object Identifier"},"url":"https://dx.doi.org/10.1021/es062693a"}],"country":"United States","state":"Massachusetts","otherGeospatial":"Cape Cod","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"type\": \"Polygon\",\n \"coordinates\": [\n [\n [\n -70.69427490234375,\n 41.509605687197975\n ],\n [\n -70.69427490234375,\n 42.10943017110108\n ],\n [\n -69.90463256835938,\n 42.10943017110108\n ],\n [\n -69.90463256835938,\n 41.509605687197975\n ],\n [\n -70.69427490234375,\n 41.509605687197975\n ]\n ]\n ]\n }\n }\n ]\n}","volume":"41","issue":"15","noUsgsAuthors":false,"publicationDate":"2007-06-30","publicationStatus":"PW","scienceBaseUri":"505aad2de4b0c8380cd86e4e","contributors":{"authors":[{"text":"Maxwell, Reed M.","contributorId":95373,"corporation":false,"usgs":true,"family":"Maxwell","given":"Reed","email":"","middleInitial":"M.","affiliations":[],"preferred":false,"id":429956,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Welty, Claire","contributorId":39416,"corporation":false,"usgs":true,"family":"Welty","given":"Claire","email":"","affiliations":[],"preferred":false,"id":429957,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Harvey, Ronald W. 0000-0002-2791-8503 rwharvey@usgs.gov","orcid":"https://orcid.org/0000-0002-2791-8503","contributorId":564,"corporation":false,"usgs":true,"family":"Harvey","given":"Ronald","email":"rwharvey@usgs.gov","middleInitial":"W.","affiliations":[{"id":5044,"text":"National Research Program - Central Branch","active":true,"usgs":true}],"preferred":true,"id":429955,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}} ]}