{"pageNumber":"3889","pageRowStart":"97200","pageSize":"25","recordCount":185169,"records":[{"id":31875,"text":"ofr9548 - 1995 - Geologic map of the Cane Springs Southeast Quadrangle, Mohave County, Arizona","interactions":[],"lastModifiedDate":"2012-02-02T00:09:04","indexId":"ofr9548","displayToPublicDate":"1995-07-01T00:00:00","publicationYear":"1995","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":"95-48","title":"Geologic map of the Cane Springs Southeast Quadrangle, Mohave County, Arizona","language":"ENGLISH","doi":"10.3133/ofr9548","usgsCitation":"Lucchitta, I., Dehler, C.M., and Basdekas, P., 1995, Geologic map of the Cane Springs Southeast Quadrangle, Mohave County, Arizona: U.S. Geological Survey Open-File Report 95-48, 1 over-size sheet, scale 1:24,000 (1 inch = 2,000 feet). , https://doi.org/10.3133/ofr9548.","productDescription":"1 over-size sheet, scale 1:24,000 (1 inch = 2,000 feet). ","costCenters":[],"links":[{"id":160235,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":108934,"rank":700,"type":{"id":15,"text":"Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_18382.htm","linkFileType":{"id":5,"text":"html"},"description":"18382"},{"id":19550,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1995/0048/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}}],"scale":"24000","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b0ae4b07f02db69d438","contributors":{"authors":[{"text":"Lucchitta, Ivo","contributorId":94291,"corporation":false,"usgs":true,"family":"Lucchitta","given":"Ivo","email":"","affiliations":[],"preferred":false,"id":207152,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Dehler, Carol M.","contributorId":25187,"corporation":false,"usgs":true,"family":"Dehler","given":"Carol","email":"","middleInitial":"M.","affiliations":[],"preferred":false,"id":207151,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Basdekas, P.O.","contributorId":100433,"corporation":false,"usgs":true,"family":"Basdekas","given":"P.O.","email":"","affiliations":[],"preferred":false,"id":207153,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":31873,"text":"ofr9510 - 1995 - Geologic map of Kious Spring and Garrison 7.5' quadrangles, White Pine County, Nevada and Millard County, Utah","interactions":[],"lastModifiedDate":"2012-02-02T00:09:04","indexId":"ofr9510","displayToPublicDate":"1995-07-01T00:00:00","publicationYear":"1995","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":"95-10","title":"Geologic map of Kious Spring and Garrison 7.5' quadrangles, White Pine County, Nevada and Millard County, Utah","language":"ENGLISH","doi":"10.3133/ofr9510","usgsCitation":"McGrew, A., and Brown, E., 1995, Geologic map of Kious Spring and Garrison 7.5' quadrangles, White Pine County, Nevada and Millard County, Utah: U.S. Geological Survey Open-File Report 95-10, 21 p., 3 over-size sheets; sheets 1-2, scale 1:24,000 (1 inch = 2,000 feet). , https://doi.org/10.3133/ofr9510.","productDescription":"21 p., 3 over-size sheets; sheets 1-2, scale 1:24,000 (1 inch = 2,000 feet). ","costCenters":[],"links":[{"id":108929,"rank":700,"type":{"id":15,"text":"Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_18372.htm","linkFileType":{"id":5,"text":"html"},"description":"18372"},{"id":160221,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1995/0010/report-thumb.jpg"},{"id":60062,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1995/0010/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"scale":"24000","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b13e4b07f02db6a30b6","contributors":{"authors":[{"text":"McGrew, A.J.","contributorId":52616,"corporation":false,"usgs":true,"family":"McGrew","given":"A.J.","email":"","affiliations":[],"preferred":false,"id":207139,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Brown, E.L.","contributorId":106169,"corporation":false,"usgs":true,"family":"Brown","given":"E.L.","email":"","affiliations":[],"preferred":false,"id":207140,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":18850,"text":"ofr9522 - 1995 - Dog \"bites\" earthquake; a handout for the valley/mountain shaking model","interactions":[],"lastModifiedDate":"2012-02-02T00:07:28","indexId":"ofr9522","displayToPublicDate":"1995-07-01T00:00:00","publicationYear":"1995","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":"95-22","title":"Dog \"bites\" earthquake; a handout for the valley/mountain shaking model","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/ofr9522","usgsCitation":"Evans, J.R., and Coakley, J., 1995, Dog \"bites\" earthquake; a handout for the valley/mountain shaking model: U.S. Geological Survey Open-File Report 95-22, 13 p. ill., maps ;28 cm., https://doi.org/10.3133/ofr9522.","productDescription":"13 p. ill., maps ;28 cm.","costCenters":[],"links":[{"id":151946,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1995/0022/report-thumb.jpg"},{"id":48242,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1995/0022/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a61e4b07f02db6360dd","contributors":{"authors":[{"text":"Evans, John R. jrevans@usgs.gov","contributorId":529,"corporation":false,"usgs":true,"family":"Evans","given":"John","email":"jrevans@usgs.gov","middleInitial":"R.","affiliations":[{"id":237,"text":"Earthquake Science Center","active":true,"usgs":true}],"preferred":true,"id":179857,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Coakley, J.M.","contributorId":32557,"corporation":false,"usgs":true,"family":"Coakley","given":"J.M.","email":"","affiliations":[],"preferred":false,"id":179858,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":70205368,"text":"70205368 - 1995 - Wind shear stress measurements in a coastal marsh during Hurricane Andrew","interactions":[],"lastModifiedDate":"2019-09-17T08:31:34","indexId":"70205368","displayToPublicDate":"1995-06-30T11:15:51","publicationYear":"1995","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":2220,"text":"Journal of Coastal Research","active":true,"publicationSubtype":{"id":10}},"title":"Wind shear stress measurements in a coastal marsh during Hurricane Andrew","docAbstract":"<p><span>Hurricane Andrew produced changes to the Louisiana wetlands not normally observed after lesser, more common storms. For example, the &lt;25 m/s wind speeds generated by cold fronts and winter storms, and any accompanying storm surge, do not cause substantial, wide-spread alteration of marsh vegetation. During Hurricane Andrew, however, the wind, the wind-driven storm surge, or both produced severe, wide-spread wetland alteration, especially in areas that primarily consisted of densely vegetated floating mats. In a few hours, vegetated brackish marsh was severely torn and large areas were converted to open water, a process that takes decades when driven by geologic subsidence, human intervention, and lesser storms. During the passage of Hurricane Andrew, wind measurements were taken inside an impoundment within a brackish part of Louisiana's coastal wetlands system. At its closest point, the site lay 50 km to the right of the north-trending storm track, placing it in or near the zone of maximum wind (the eye wall). As the hurricane approached, the wind blew from the north; after it passed, the wind direction swung around to the southeast. Several hours after the eye passed, the southeasterly wind drove a 1.5-m storm surge through the area, causing the collapse of the meteorology tower. Wind shear stress calculations, based on data from two vertically stacked sensors, showed a direct correlation between wind shear stress and wind speed. The greatest increase in wind shear stress occurred when wind speed exceeded 20 m/s. Overall, wind shear stress increased more than three orders of magnitude — from approximately 0.01 N/m² at a wind speed of 6 m/s through 1 N/m² at 20 m/s to 18 N/m² at the maximum sustained speed of 43 m/s. Drag-coefficient calculations show that the open-ocean CD formulations, such as the popular WAMDI model, cannot be employed for wetland use because it overestimates CD for velocities less than approximately 20 m/s and underestimates it for higher velocities.</span></p>","language":"English","publisher":"Coastal Education and Research Foundation Inc","usgsCitation":"Dingler, J.R., Hsu, S., and Foote, A.L., 1995, Wind shear stress measurements in a coastal marsh during Hurricane Andrew: Journal of Coastal Research, p. 295-305.","productDescription":"11 p.","startPage":"295","endPage":"305","costCenters":[{"id":455,"text":"National Wetlands Research Center","active":true,"usgs":true}],"links":[{"id":367434,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"},{"id":367447,"rank":2,"type":{"id":15,"text":"Index Page"},"url":"https://www.jstor.org/stable/25736016"}],"country":"United States","state":"Louisiana","otherGeospatial":"Jug Lake","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -91.0081672668457,\n              29.34582065193874\n            ],\n            [\n              -90.90568542480469,\n              29.34582065193874\n            ],\n            [\n              -90.90568542480469,\n              29.397131972809856\n            ],\n            [\n              -91.0081672668457,\n              29.397131972809856\n            ],\n            [\n              -91.0081672668457,\n              29.34582065193874\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","contributors":{"authors":[{"text":"Dingler, J. R.","contributorId":79043,"corporation":false,"usgs":true,"family":"Dingler","given":"J.","email":"","middleInitial":"R.","affiliations":[],"preferred":false,"id":770951,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Hsu, S.A.","contributorId":94161,"corporation":false,"usgs":true,"family":"Hsu","given":"S.A.","email":"","affiliations":[],"preferred":false,"id":770952,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Foote, A. Lee","contributorId":216145,"corporation":false,"usgs":false,"family":"Foote","given":"A.","email":"","middleInitial":"Lee","affiliations":[],"preferred":false,"id":770953,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":70201973,"text":"70201973 - 1995 - Structural impact of hurricane Andrew on the forested wetlands of the Atchaflaya Basin in South Louisiana","interactions":[],"lastModifiedDate":"2019-02-05T09:40:54","indexId":"70201973","displayToPublicDate":"1995-06-22T09:23:08","publicationYear":"1995","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":2220,"text":"Journal of Coastal Research","active":true,"publicationSubtype":{"id":10}},"title":"Structural impact of hurricane Andrew on the forested wetlands of the Atchaflaya Basin in South Louisiana","docAbstract":"<p>On August 26, 1992, Hurricane Andrew hit the Louisiana coast and traversed a large portion of the lower Atchafalaya Basin, bounding the largest remaining tract of cypress-tupelo and bottomland hardwood swamp in the United States. Permanent field sites were established following the hurricane to assess the extent of forest damage and to monitor the rate and process of forest recovery. Bottomland hardwood forests had significantly greater damage and mortality than did cypress-tupelo communities. Canopy trees suffered the greatest direct damage, particularly in sites within the storm's eyewall and right quadrant. The type and extent of damage (windthrow, branch loss, and defoliation) generally decreased as distance from the storm path increased. Azimuths of downed trees were strongly correlated with predicted wind vectors derived from a hurricane simulation model of Andrew. Species differences were readily apparent, indicating a high degree of tolerance to windthrow by baldcypress and water tupelo, and intolerance by many common hardwood species. Bottomland hardwood forests are particularly susceptible to catastrophic disturbance by hurricanes such as Andrew, which have significant impact on forest structure and dynamics. </p>","language":"English","publisher":"Coastal Education & Research Foundation, Inc.","publisherLocation":"Fort Lauderdale, Florida","usgsCitation":"Doyle, T.W., Keeland, B.D., Gorham, L.E., and Johnson, D.J., 1995, Structural impact of hurricane Andrew on the forested wetlands of the Atchaflaya Basin in South Louisiana: Journal of Coastal Research, no. Special Issue 21, p. 354-364.","productDescription":"11 p.","startPage":"354","endPage":"364","costCenters":[{"id":17705,"text":"Wetland and Aquatic Research Center","active":true,"usgs":true}],"links":[{"id":360951,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"},{"id":361005,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://www.jstor.org/stable/25736020?seq=1#metadata_info_tab_contents"}],"country":"United States","state":"Louisiana","otherGeospatial":"Atchafalaya Basin","issue":"Special Issue 21","noUsgsAuthors":false,"publicationStatus":"PW","contributors":{"authors":[{"text":"Doyle, Thomas W. 0000-0001-5754-0671 doylet@usgs.gov","orcid":"https://orcid.org/0000-0001-5754-0671","contributorId":703,"corporation":false,"usgs":true,"family":"Doyle","given":"Thomas","email":"doylet@usgs.gov","middleInitial":"W.","affiliations":[{"id":455,"text":"National Wetlands Research Center","active":true,"usgs":true}],"preferred":true,"id":756388,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Keeland, Bobby D.","contributorId":103506,"corporation":false,"usgs":true,"family":"Keeland","given":"Bobby","email":"","middleInitial":"D.","affiliations":[{"id":455,"text":"National Wetlands Research Center","active":true,"usgs":true},{"id":17705,"text":"Wetland and Aquatic Research Center","active":true,"usgs":true}],"preferred":true,"id":756389,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Gorham, Lance E.","contributorId":212704,"corporation":false,"usgs":false,"family":"Gorham","given":"Lance","email":"","middleInitial":"E.","affiliations":[],"preferred":false,"id":756390,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Johnson, Darrin J.","contributorId":212705,"corporation":false,"usgs":false,"family":"Johnson","given":"Darrin","email":"","middleInitial":"J.","affiliations":[],"preferred":false,"id":756391,"contributorType":{"id":1,"text":"Authors"},"rank":4}]}}
,{"id":5223286,"text":"5223286 - 1995 - Pathogenicity of Steinernema carpocapsae and S. glaseri (Nematoda: Steinernematidae) to Ixodes scapularis (Acari: Ixodidae)","interactions":[],"lastModifiedDate":"2024-05-09T16:33:47.678692","indexId":"5223286","displayToPublicDate":"1995-06-16T12:17:44","publicationYear":"1995","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":2385,"text":"Journal of Medical Entomology","active":true,"publicationSubtype":{"id":10}},"title":"Pathogenicity of Steinernema carpocapsae and S. glaseri (Nematoda: Steinernematidae) to Ixodes scapularis (Acari: Ixodidae)","docAbstract":"<p><span>The entomopathogenic nematodes&nbsp;</span><i>Steinernema carpocapsae</i><span>&nbsp;(Weiser) and&nbsp;</span><i>S. glaseri</i><span>&nbsp;(Steiner) are pathogenic to engorged adult, blacklegged ticks,&nbsp;</span><i>Ixodes scapularis</i><span>&nbsp;(Say), but not to unfed females, engorged nymphs, or engorged larvae. Nematodes apparently enter the tick through the genital pore, thus precluding infection of immature ticks. The timing of tick mortality, and overall mortality after 17 d, did not differ between infections by&nbsp;</span><i>S. carpocapsae</i><span>&nbsp;and&nbsp;</span><i>S. glaseri</i><span>. These nematodes typically do not complete their life cycles or produce infective juveniles in&nbsp;</span><i>I. scapularis</i><span>. However, both species successfully produced infective juveniles when the tick body was slit before nematode infection. Mortality of engorged&nbsp;</span><i>I. scapularis</i><span>&nbsp;females infected by&nbsp;</span><i>S. carpocapsae</i><span>&nbsp;was greater than uninfected controls, but did not vary significantly with nematode concentration (50–3,000 infective juveniles per 5-cm-diameter petri dish). The LC</span><sub>50</sub><span>&nbsp;was 347.8 infective juveniles per petri dish (5 ticks per dish). Hatched egg masses of infected ticks weighed less than those of uninfected controls. Mortality of infected ticks was greatest between 20 and 30°C, and was lower at 15°C.</span></p>","language":"English","publisher":"Entomological Society of America","doi":"10.1093/jmedent/32.6.900","usgsCitation":"Zhioua, E., LeBrun, R., Ginsberg, H., and Aeschliman, A., 1995, Pathogenicity of Steinernema carpocapsae and S. glaseri (Nematoda: Steinernematidae) to Ixodes scapularis (Acari: Ixodidae): Journal of Medical Entomology, v. 32, no. 6, p. 900-905, https://doi.org/10.1093/jmedent/32.6.900.","productDescription":"6 p.","startPage":"900","endPage":"905","numberOfPages":"6","costCenters":[{"id":531,"text":"Patuxent Wildlife Research Center","active":true,"usgs":true}],"links":[{"id":479211,"rank":2,"type":{"id":41,"text":"Open Access External Repository Page"},"url":"https://digitalcommons.uri.edu/pls_facpubs/180","text":"External Repository"},{"id":199346,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"32","issue":"6","noUsgsAuthors":false,"publicationDate":"1995-11-01","publicationStatus":"PW","scienceBaseUri":"4f4e4ae1e4b07f02db688a43","contributors":{"authors":[{"text":"Zhioua, E.","contributorId":27165,"corporation":false,"usgs":true,"family":"Zhioua","given":"E.","affiliations":[],"preferred":false,"id":338311,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"LeBrun, R.A.","contributorId":43068,"corporation":false,"usgs":true,"family":"LeBrun","given":"R.A.","affiliations":[],"preferred":false,"id":338313,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Ginsberg, H. S. 0000-0002-4933-2466","orcid":"https://orcid.org/0000-0002-4933-2466","contributorId":27576,"corporation":false,"usgs":true,"family":"Ginsberg","given":"H. S.","affiliations":[],"preferred":false,"id":338312,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Aeschliman, A.","contributorId":50254,"corporation":false,"usgs":true,"family":"Aeschliman","given":"A.","email":"","affiliations":[],"preferred":false,"id":338314,"contributorType":{"id":1,"text":"Authors"},"rank":4}]}}
,{"id":5222660,"text":"5222660 - 1995 - The cumulative effect of consecutive winters' snow depth on moose and deer populations:  a defence","interactions":[],"lastModifiedDate":"2020-03-13T10:59:19","indexId":"5222660","displayToPublicDate":"1995-06-16T12:17:42","publicationYear":"1995","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":2158,"text":"Journal of Animal Ecology","active":true,"publicationSubtype":{"id":10}},"title":"The cumulative effect of consecutive winters' snow depth on moose and deer populations:  a defence","docAbstract":"<p>1. L. D. Mech et al. presented evidence that moose Alces alces and deer Odocoileus virginianus population parameters re influenced by a cumulative effect of three winters' snow depth. They postulated that snow depth affects adult ungulates cumulatively from winter to winter and results in measurable offspring effects after the third winter. </p><p>2. F. Messier challenged those findings and claimed that the population parameters studied were instead affected by ungulate density and wolf indexes. </p><p>3. This paper refutes Messier's claims by demonstrating that his results were an artifact of two methodological errors. The first was that, in his main analyses, Messier used only the first previous winter's snow depth rather than the sum of the previous three winters' snow depth, which was the primary point of Mech et al. Secondly, Messier smoothed the ungulate population data, which removed 22-51% of the variability from the raw data. </p><p>4. When we repeated Messier's analyses on the raw data and using the sum of the previous three winter's snow depth, his findings did not hold up.</p>","language":"English","publisher":"ITHAKA","doi":"10.2307/5834","usgsCitation":"McRoberts, R., Mech, L., and Peterson, R.O., 1995, The cumulative effect of consecutive winters' snow depth on moose and deer populations:  a defence: Journal of Animal Ecology, v. 64, no. 1, p. 131-135, https://doi.org/10.2307/5834.","productDescription":"5 p.","startPage":"131","endPage":"135","numberOfPages":"5","costCenters":[{"id":531,"text":"Patuxent Wildlife Research Center","active":true,"usgs":true}],"links":[{"id":194295,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"},{"id":15936,"rank":200,"type":{"id":11,"text":"Document"},"url":"https://www.jstor.org/stable/5834","linkFileType":{"id":5,"text":"html"}}],"volume":"64","issue":"1","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4aa9e4b07f02db6688a0","contributors":{"authors":[{"text":"McRoberts, R.E.","contributorId":56749,"corporation":false,"usgs":true,"family":"McRoberts","given":"R.E.","affiliations":[],"preferred":false,"id":336775,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Mech, L.D. 0000-0003-3944-7769","orcid":"https://orcid.org/0000-0003-3944-7769","contributorId":75466,"corporation":false,"usgs":false,"family":"Mech","given":"L.D.","email":"","affiliations":[],"preferred":false,"id":336777,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Peterson, R. O.","contributorId":62175,"corporation":false,"usgs":true,"family":"Peterson","given":"R.","email":"","middleInitial":"O.","affiliations":[],"preferred":false,"id":336776,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":70227566,"text":"70227566 - 1995 - Comet Shoemaker-Levy 9 at Jupiter","interactions":[],"lastModifiedDate":"2022-01-20T15:34:44.778153","indexId":"70227566","displayToPublicDate":"1995-06-15T09:28:35","publicationYear":"1995","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1807,"text":"Geophysical Research Letters","active":true,"publicationSubtype":{"id":10}},"title":"Comet Shoemaker-Levy 9 at Jupiter","docAbstract":"<div class=\"article-section__content en main\"><p>From the 16th to the 22nd of July, 1994, the world was privileged to witness an event that probably recurs less often than once a century. Collision of the brightest nuclei of Periodic Comet Shoemaker-Levy 9 produced enormous dark clouds that were the most dramatic and easily observed features on Jupiter recorded by human visual observation. They were seen by tens of thousands of people through hundreds or thousands of telescopes ranging in aperture from 5 to more than 100 cm. Tens of millions of people participated vicariously in the impact event through viewing on television the magnificent images from the Hubble Space Telescope (HST) and from numerous ground-based telescopes.</p></div>","language":"English","publisher":"Wiley-Blackwell","doi":"10.1029/95GL01529","usgsCitation":"Shoemaker, E.M., 1995, Comet Shoemaker-Levy 9 at Jupiter: Geophysical Research Letters, v. 22, no. 12, p. 1555-1556, https://doi.org/10.1029/95GL01529.","productDescription":"2 p.","startPage":"1555","endPage":"1556","costCenters":[],"links":[{"id":394582,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"otherGeospatial":"Jupiter","volume":"22","issue":"12","noUsgsAuthors":false,"publicationDate":"2012-12-07","publicationStatus":"PW","contributors":{"authors":[{"text":"Shoemaker, Eugene Merle","contributorId":20342,"corporation":false,"usgs":true,"family":"Shoemaker","given":"Eugene","email":"","middleInitial":"Merle","affiliations":[],"preferred":false,"id":831271,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":70210156,"text":"70210156 - 1995 - Seismic velocity structure and composition of the continental crust: A global view","interactions":[],"lastModifiedDate":"2020-05-18T14:58:52.184531","indexId":"70210156","displayToPublicDate":"1995-06-10T09:54:24","publicationYear":"1995","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":2314,"text":"Journal of Geophysical Research B: Solid Earth","active":true,"publicationSubtype":{"id":10}},"title":"Seismic velocity structure and composition of the continental crust: A global view","docAbstract":"<div class=\"article-section__content en main\"><p>Seismic techniques provide the highest‐resolution measurements of the structure of the crust and have been conducted on a worldwide basis. We summarize the structure of the continental crust based on the results of seismic refraction profiles and infer crustal composition as a function of depth by comparing these results with high‐pressure laboratory measurements of seismic velocity for a wide range of rocks that are commonly found in the crust. The thickness and velocity structure of the crust are well correlated with tectonic province, with extended crust showing an average thickness of 30.5 km and orogens an average of 46.3 km. Shields and platforms have an average crustal thickness nearly equal to the global average. We have corrected for the nonuniform geographical distribution of seismic refraction profiles by estimating the global area of each major crustal type. The weighted average crustal thickness based on these values is 41.1 km. This value is 10% to 20% greater than previous estimates which underrepresented shields, platforms, and orogens. The average compressional wave velocity of the crust is 6.45 km/s, and the average velocity of the uppermost mantle (<i>Pn</i><span>&nbsp;</span>velocity) is 8.09 km/s. We summarize the velocity structure of the crust at 5‐km depth intervals, both in the form of histograms and as an average velocity‐depth curve, and compare these determinations with new measurements of compressional wave velocities and densities of over 3000 igneous and metamorphic rock cores made to confining pressures of 1 GPa. On the basis of petrographic studies and chemical analyses, the rocks have been classified into 29 groups. Average velocities, densities, and standard deviations are presented for each group at 5‐km depth intervals to crustal depths of 50 km along three different geotherms. This allows us to develop a model for the composition of the continental crust. Velocities in the upper continental crust are matched by velocities of a large number of lithologies, including many low‐grade metamorphic rocks and relatively silicic gneisses of amphibolite facies grade. In midcrustal regions, velocity gradients appear to originate from an increase in metamorphic grade, as well as a decrease in silica content. Tonalitic gneiss, granitic gneiss, and amphibolite are abundant midcrustal lithologies. Anisotropy due to preferred mineral orientation is likely to be significant in upper and midcrustal regions. The bulk of the lower continental crust is chemically equivalent to gabbro, with velocities in agreement with laboratory measurements of mafic granulite. Garnet becomes increasingly abundant with depth, and mafic garnet granulite is the dominant rock type immediately above the Mohorovicic discontinuity. Average compressional wave velocities of common crustal rock types show excellent correlations with density. The mean crustal density calculated from our model is 2830 kg/m<sup>3</sup>, and the average SiO<sub>2</sub><span>&nbsp;</span>content is 61.8%.</p></div>","language":"English","publisher":"American Geophysical Union","doi":"10.1029/95JB00259","usgsCitation":"Christensen, N.I., and Mooney, W.D., 1995, Seismic velocity structure and composition of the continental crust: A global view: Journal of Geophysical Research B: Solid Earth, v. 100, no. B6, p. 9761-9788, https://doi.org/10.1029/95JB00259.","productDescription":"28 p.","startPage":"9761","endPage":"9788","costCenters":[{"id":237,"text":"Earthquake Science Center","active":true,"usgs":true}],"links":[{"id":374890,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"100","issue":"B6","noUsgsAuthors":false,"publicationDate":"2012-09-20","publicationStatus":"PW","contributors":{"authors":[{"text":"Christensen, Nikolas I.","contributorId":95927,"corporation":false,"usgs":false,"family":"Christensen","given":"Nikolas","email":"","middleInitial":"I.","affiliations":[{"id":7001,"text":"Department of Earth and Atmospheric Sciences, Purdue University","active":true,"usgs":false}],"preferred":false,"id":789334,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Mooney, Walter D. 0000-0002-5310-3631 mooney@usgs.gov","orcid":"https://orcid.org/0000-0002-5310-3631","contributorId":3194,"corporation":false,"usgs":true,"family":"Mooney","given":"Walter","email":"mooney@usgs.gov","middleInitial":"D.","affiliations":[{"id":237,"text":"Earthquake Science Center","active":true,"usgs":true}],"preferred":true,"id":789335,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":70210412,"text":"70210412 - 1995 - Style and age of deformation, Carolina Slate Belt, central North Carolina","interactions":[],"lastModifiedDate":"2020-06-03T12:13:29.13217","indexId":"70210412","displayToPublicDate":"1995-06-02T14:23:07","publicationYear":"1995","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":3443,"text":"Southeastern Geology","active":true,"publicationSubtype":{"id":10}},"title":"Style and age of deformation, Carolina Slate Belt, central North Carolina","docAbstract":"<p>No abstract available.</p>","language":"English","publisher":"Duke University","usgsCitation":"Offield, T.W., Kunk, M.J., and Koeppen, R.P., 1995, Style and age of deformation, Carolina Slate Belt, central North Carolina: Southeastern Geology, v. 35, no. 2, p. 59-77.","productDescription":"19 p.","startPage":"59","endPage":"77","costCenters":[{"id":40020,"text":"Florence Bascom Geoscience Center","active":true,"usgs":true}],"links":[{"id":375257,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United States","state":"North 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Carolina\",\"nation\":\"USA  \"}}]}","volume":"35","issue":"2","noUsgsAuthors":false,"publicationStatus":"PW","contributors":{"authors":[{"text":"Offield, Terry W.","contributorId":15196,"corporation":false,"usgs":true,"family":"Offield","given":"Terry","email":"","middleInitial":"W.","affiliations":[],"preferred":false,"id":790231,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Kunk, Michael J. 0000-0003-4424-7825 mkunk@usgs.gov","orcid":"https://orcid.org/0000-0003-4424-7825","contributorId":200968,"corporation":false,"usgs":true,"family":"Kunk","given":"Michael","email":"mkunk@usgs.gov","middleInitial":"J.","affiliations":[{"id":243,"text":"Eastern Geology and Paleoclimate Science Center","active":true,"usgs":true},{"id":40020,"text":"Florence Bascom Geoscience Center","active":true,"usgs":true}],"preferred":true,"id":790232,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Koeppen, Robert P.","contributorId":107764,"corporation":false,"usgs":true,"family":"Koeppen","given":"Robert","email":"","middleInitial":"P.","affiliations":[],"preferred":false,"id":790233,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":70246657,"text":"70246657 - 1995 - Mineral resources, environmental issues, and land use","interactions":[],"lastModifiedDate":"2023-07-12T17:20:10.38281","indexId":"70246657","displayToPublicDate":"1995-06-02T12:11:14","publicationYear":"1995","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":3338,"text":"Science","active":true,"publicationSubtype":{"id":10}},"title":"Mineral resources, environmental issues, and land use","docAbstract":"<div id=\"abstracts\" data-extent=\"frontmatter\"><div class=\"core-container\"><div>Contrary to predictions from the 1950s through the mid-1980s, persistent shortages of nonfuel minerals have not occurred, despite prodigious consumption, and world reserves have increased. Global availability of raw materials is relevant to policy decisions regarding mineral development and land use. Justification for environmental protection may exceed that for mining a specific ore body. Demand for environmental accountability is rising worldwide, and new technologies are enabling internalization of costs. Mineral-rich developing nations plagued by inefficient state-owned mining enterprises, high population growth rates, and environmental degradation could realize substantial benefit by reforming government policies to encourage foreign investment in resources and by appropriate allocation of mineral rents.</div></div></div>","language":"English","publisher":"American Association for the Advancement of Science","doi":"10.1126/science.268.5215.1305","usgsCitation":"Hodges, C.A., 1995, Mineral resources, environmental issues, and land use: Science, v. 268, no. 5215, p. 1305-1312, https://doi.org/10.1126/science.268.5215.1305.","productDescription":"8 p.","startPage":"1305","endPage":"1312","costCenters":[],"links":[{"id":418906,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"268","issue":"5215","noUsgsAuthors":false,"publicationStatus":"PW","contributors":{"authors":[{"text":"Hodges, Carroll Ann","contributorId":99144,"corporation":false,"usgs":true,"family":"Hodges","given":"Carroll","email":"","middleInitial":"Ann","affiliations":[],"preferred":false,"id":877810,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":70169398,"text":"70169398 - 1995 - Biological consequences of relocating grizzly bears in the Yellowstone ecosystem","interactions":[],"lastModifiedDate":"2016-03-25T14:50:37","indexId":"70169398","displayToPublicDate":"1995-06-01T15:45:00","publicationYear":"1995","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":2508,"text":"Journal of Wildlife Management","active":true,"publicationSubtype":{"id":10}},"title":"Biological consequences of relocating grizzly bears in the Yellowstone ecosystem","docAbstract":"<p>Relocating grizzly bears (<i>Ursus arctos</i>) from human/bear conflict situations has been a standard management procedure. Using data from Yellowstone National Park, we present components of situations that may affect the outcome of a relocation. Survival rates of transported bears were lower (<i>l</i><sub>x</sub> = 0.83) (<i>P</i> = 0.001) than those not transported (<i>l</i><sub>x</sub> = 0.89). Survival was largely affected by whether the bear returned to the capture site (<i>P</i> = 0.029). Return rate was most affected by distance transported (<i>P</i> = 0.012) and age-sex group (<i>P</i> = 0.014). Return rates decreased at distances -75 km, and subadult females returned least (<i>P</i> = 0.050) often. Because of low survival and high return rates, transporting grizzly bears should be considered a final action to eliminate a conflict situation. However, transporting females must be considered a viable management technique because transports of some individuals have resulted in contributions to the population through successful reproduction.</p>","language":"English","publisher":"Wildlife Society","publisherLocation":"Washington, D.C.","doi":"10.2307/3802463","usgsCitation":"Blanchard, B.M., and Knight, R.R., 1995, Biological consequences of relocating grizzly bears in the Yellowstone ecosystem: Journal of Wildlife Management, v. 59, no. 3, p. 560-565, https://doi.org/10.2307/3802463.","productDescription":"6 p.","startPage":"560","endPage":"565","numberOfPages":"6","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[{"id":481,"text":"Northern Rocky Mountain Science Center","active":true,"usgs":true}],"links":[{"id":319421,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United States","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -111.87377929687499,\n              43.06086137134326\n            ],\n            [\n              -111.87377929687499,\n              45.57560020947799\n            ],\n            [\n              -109.1162109375,\n              45.57560020947799\n            ],\n            [\n              -109.1162109375,\n              43.06086137134326\n            ],\n            [\n              -111.87377929687499,\n              43.06086137134326\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","volume":"59","issue":"3","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"56f66132e4b07d796bf76ff2","contributors":{"authors":[{"text":"Blanchard, Bonnie M.","contributorId":33633,"corporation":false,"usgs":true,"family":"Blanchard","given":"Bonnie","email":"","middleInitial":"M.","affiliations":[],"preferred":false,"id":624023,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Knight, Richard R.","contributorId":68660,"corporation":false,"usgs":true,"family":"Knight","given":"Richard","email":"","middleInitial":"R.","affiliations":[],"preferred":false,"id":624024,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":70169383,"text":"70169383 - 1995 - Appraising status of the Yellowstone grizzly bear population by counting females with cubs-of-the-year","interactions":[],"lastModifiedDate":"2016-03-25T14:37:17","indexId":"70169383","displayToPublicDate":"1995-06-01T15:30:00","publicationYear":"1995","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":3779,"text":"Wildlife Society Bulletin","onlineIssn":"1938-5463","printIssn":"0091-7648","active":true,"publicationSubtype":{"id":10}},"title":"Appraising status of the Yellowstone grizzly bear population by counting females with cubs-of-the-year","docAbstract":"<p>The grizzly bear (<i>Ursus arctos horriblilis</i>) in the lower United States was declared threatened in 1975 under the Endangered Species Act of 1973 (16 U.S.C. 15-31-1544). According to that Act, the U.S. Fish and Wildlife Service had to prepare a plan to recover populations to levels where the species could be conserved and delisted from its threatened status. The Recovery Plan (U.S. Fish and Wildlife Service 1993) uses counts of distinct females with cubs-of-the-year as a recovery parameter in several grizzly bear ecosystems. The total number of these females is assumed to be the minimum number with cubs born in the current year. To our knowledge, this technique, its methodology, and value as a population indicator have never been adequately explained or discussed. Thus, we describe the methodology and assess its potential for continued use in the Yellowstone ecosystem.</p>","language":"English","publisher":"Wildlife Society","publisherLocation":"Washington, D.C.","usgsCitation":"Knight, R.R., Blanchard, B.M., and Eberhardt, L.L., 1995, Appraising status of the Yellowstone grizzly bear population by counting females with cubs-of-the-year: Wildlife Society Bulletin, v. 23, no. 2, p. 245-248.","productDescription":"4 p.","startPage":"245","endPage":"248","numberOfPages":"4","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[{"id":481,"text":"Northern Rocky Mountain Science Center","active":true,"usgs":true}],"links":[{"id":319420,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"},{"id":319419,"rank":1,"type":{"id":11,"text":"Document"},"url":"https://www.fws.gov/mountain-prairie/species/mammals/grizzly/Knight%20et%20al.%201995.pdf","linkFileType":{"id":1,"text":"pdf"}}],"volume":"23","issue":"2","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"56f6612fe4b07d796bf76fe7","contributors":{"authors":[{"text":"Knight, Richard R.","contributorId":68660,"corporation":false,"usgs":true,"family":"Knight","given":"Richard","email":"","middleInitial":"R.","affiliations":[],"preferred":false,"id":623985,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Blanchard, Bonnie M.","contributorId":33633,"corporation":false,"usgs":true,"family":"Blanchard","given":"Bonnie","email":"","middleInitial":"M.","affiliations":[],"preferred":false,"id":623986,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Eberhardt, L. L.","contributorId":52099,"corporation":false,"usgs":true,"family":"Eberhardt","given":"L.","email":"","middleInitial":"L.","affiliations":[],"preferred":false,"id":623987,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":70248769,"text":"70248769 - 1995 - U-series age equations for uranium assimilation by fossil bones","interactions":[],"lastModifiedDate":"2023-09-20T18:49:12.962165","indexId":"70248769","displayToPublicDate":"1995-06-01T13:34:30","publicationYear":"1995","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":3226,"text":"Radiochimica Acta","active":true,"publicationSubtype":{"id":10}},"title":"U-series age equations for uranium assimilation by fossil bones","docAbstract":"<p>No abstract available.</p>","language":"English","publisher":"De Gruyter","doi":"10.1524/ract.1995.69.2.127","usgsCitation":"Bischoff, J.L., Rosenbauer, R.J., Moench, A.F., and Ku, T., 1995, U-series age equations for uranium assimilation by fossil bones: Radiochimica Acta, v. 69, p. 127-135, https://doi.org/10.1524/ract.1995.69.2.127.","productDescription":"9 p.","startPage":"127","endPage":"135","costCenters":[],"links":[{"id":420981,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"69","noUsgsAuthors":false,"publicationDate":"1995-06-01","publicationStatus":"PW","contributors":{"authors":[{"text":"Bischoff, James L. jbischoff@usgs.gov","contributorId":1389,"corporation":false,"usgs":true,"family":"Bischoff","given":"James","email":"jbischoff@usgs.gov","middleInitial":"L.","affiliations":[],"preferred":true,"id":883532,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Rosenbauer, Robert J. brosenbauer@usgs.gov","contributorId":204,"corporation":false,"usgs":true,"family":"Rosenbauer","given":"Robert","email":"brosenbauer@usgs.gov","middleInitial":"J.","affiliations":[{"id":520,"text":"Pacific Coastal and Marine Science Center","active":true,"usgs":true}],"preferred":true,"id":883533,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Moench, Allen F. afmoench@usgs.gov","contributorId":3903,"corporation":false,"usgs":true,"family":"Moench","given":"Allen","email":"afmoench@usgs.gov","middleInitial":"F.","affiliations":[],"preferred":true,"id":883534,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Ku, Teh-Lung","contributorId":291580,"corporation":false,"usgs":false,"family":"Ku","given":"Teh-Lung","email":"","affiliations":[],"preferred":false,"id":883535,"contributorType":{"id":1,"text":"Authors"},"rank":4}]}}
,{"id":25140,"text":"25140 - 1995 - Cartographic catalog (CC) on CD-ROM","interactions":[],"lastModifiedDate":"2014-07-14T13:17:04","indexId":"25140","displayToPublicDate":"1995-06-01T13:16:21","publicationYear":"1995","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":6,"text":"USGS Unnumbered Series"},"title":"Cartographic catalog (CC) on CD-ROM","docAbstract":"No abstract available.","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Reston, VA","doi":"10.3133/25140","usgsCitation":"Water Resources Division, U.S. Geological Survey, 1995, Cartographic catalog (CC) on CD-ROM, computer laser optical discs, https://doi.org/10.3133/25140.","productDescription":"computer laser optical discs","costCenters":[],"links":[{"id":289916,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"53c4fbf7e4b0b58d96eeb55f","contributors":{"authors":[{"text":"Water Resources Division, U.S. Geological Survey","contributorId":128075,"corporation":true,"usgs":false,"organization":"Water Resources Division, U.S. Geological Survey","id":529181,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":70248333,"text":"70248333 - 1995 - Further evidence for a low U/Pb source in the moon: U-Th-Pb, Sm-Nd, and Ar-Ar, isotopic systematics of lunar meteorite Yamato-793169","interactions":[],"lastModifiedDate":"2023-09-07T18:29:58.727309","indexId":"70248333","displayToPublicDate":"1995-06-01T13:11:38","publicationYear":"1995","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1759,"text":"Geochimica et Cosmochimica Acta","active":true,"publicationSubtype":{"id":10}},"title":"Further evidence for a low U/Pb source in the moon: U-Th-Pb, Sm-Nd, and Ar-Ar, isotopic systematics of lunar meteorite Yamato-793169","docAbstract":"<p><span>The coarse-grained lunar meteorites, Yamato-793169 and Asuka-881757, represent a new type of low-Ti mare basalt. This paper reports the results of a U-Th-Pb, Sm-Nd, and Ar-Ar isotopic study of Yamato-793169 performed as part of a consortium studies of lunar basaltic meteorites. The isotopic study was carried out on a small sample (100 mg) so that only three density fractions could be separated. These fractions were leached with dilute acid in order to eliminate terrestrial Pb contamination. However, the leaching procedure did not completely remove this contamination in some fractions and also apparently caused a fractionation of elements (U, Th, Pb) due to preferential leaching effects, producing a secondary disturbance of the systematics. Furthermore, the Ar-Ar analyses indicate that the isotopic systematics in this meteorite might have been disturbed sometime later than 750 Ma. For these reasons, the ages obtained using different isotopic systems disagree with each other and a precise formation age could not be obtained for this meteorite. However, using what results there are, two reasonable interpretations can be made: (1) the Sm-Nd system yielded an age of 3.4 Ga that could be interpreted as the formation age, assuming that this system is possibly the least disturbed during the metamorphic event(s) that this meteorite experienced at least once, and that all other isotopic systems and their corresponding ages were disturbed, and (2) the U-Pb system yielded a nearly concordant age of 3.8 Ga that could be interpreted as the formation age and the Sm-Nd isotopic systematics were somehow disturbed. We prefer the second interpretation for the reasons discussed below. On a concordia diagram, the CDT (Cañon Diablo troilite)-corrected U-Pb isotopic data yield a discordia line similar to the lunar catastrophic array, indicating that the source of the meteorite formed during early lunar differentiation (∼4.4 Ga) and that the basalt was generated near 3.9 Ga. Total Ar-Ar age on plagioclase is 3.26 Ga, which seems to be too old if the formation age is 3.4 Ga, because low temperature fractions lost large amounts of radiogenic&nbsp;</span><sup>40</sup><span>Ar during the late thermal event. If we assume a formation age of 3.8 Ga, the estimated source&nbsp;</span><sup>238</sup><span>U/</span><sup>204</sup><span>Pb (μ) is 21.6 ± 3.5 and ϵ</span><sub>Nd</sub><span>&nbsp;is 3.9 ± 0.3. These results indicate that the source of Yamato-793169 is more depleted than Apollo 12 and 15 LT basalts, but less depleted than Asuka-881757. Therefore, Yamato-793169 may represent a new type of LT- or VLT-like mare basalt that is different from Asuka-881757. The wide variety of lead and neodymium isotopic characteristics among LT and VLT mare basalts indicate that the lunar mantle was very heterogeneous with respect to trace element abundances.</span></p>","language":"English","publisher":"Elsevier","doi":"10.1016/0016-7037(95)00154-9","usgsCitation":"Torigoye-Kita, N., Misawa, K., Dalrymple, G.B., and Tatsumoto, M., 1995, Further evidence for a low U/Pb source in the moon: U-Th-Pb, Sm-Nd, and Ar-Ar, isotopic systematics of lunar meteorite Yamato-793169: Geochimica et Cosmochimica Acta, v. 59, no. 12, p. 2621-2632, https://doi.org/10.1016/0016-7037(95)00154-9.","productDescription":"12 p.","startPage":"2621","endPage":"2632","costCenters":[],"links":[{"id":420638,"type":{"id":24,"text":"Thumbnail"},"url":"http://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"otherGeospatial":"Moon","volume":"59","issue":"12","noUsgsAuthors":false,"publicationStatus":"PW","contributors":{"authors":[{"text":"Torigoye-Kita, Noriko","contributorId":329532,"corporation":false,"usgs":false,"family":"Torigoye-Kita","given":"Noriko","email":"","affiliations":[],"preferred":false,"id":882553,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Misawa, Keiji","contributorId":105459,"corporation":false,"usgs":true,"family":"Misawa","given":"Keiji","email":"","affiliations":[],"preferred":false,"id":882554,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Dalrymple, G. Brent","contributorId":55146,"corporation":false,"usgs":true,"family":"Dalrymple","given":"G.","email":"","middleInitial":"Brent","affiliations":[],"preferred":false,"id":882555,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Tatsumoto, Mitsunobu","contributorId":10444,"corporation":false,"usgs":true,"family":"Tatsumoto","given":"Mitsunobu","email":"","affiliations":[],"preferred":false,"id":882556,"contributorType":{"id":1,"text":"Authors"},"rank":4}]}}
,{"id":70246577,"text":"70246577 - 1995 - Criteria for incipient motion of spherical sediment particles","interactions":[],"lastModifiedDate":"2023-07-10T17:54:42.369366","indexId":"70246577","displayToPublicDate":"1995-06-01T12:46:04","publicationYear":"1995","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":2338,"text":"Journal of Hydraulic Engineering","active":true,"publicationSubtype":{"id":10}},"title":"Criteria for incipient motion of spherical sediment particles","docAbstract":"<p><span>Initiation of bed-load transport of uniform spherical sediment particles on a horizontal bed in an open-channel flow is studied. On the basis of micromechanical and fluid dynamical considerations, two separate criteria for the initiation of motion are derived: one for rolling and one for lifting. Fluid forces such as drag, shear lift, Magnus lift, and lift due to centrifugal force are included in the derivation. The formulation of the lift force is theoretical. No empirical coefficient is used other than the drag coefficient&nbsp;</span><i>C<span>&nbsp;</span><sub>d</sub></i><span>, which is well established in the literature. In the low particle Reynolds number regime, where&nbsp;</span><i>u</i><span><sub>*</sub></span><i>d/ν</i><span>&nbsp;≤ 1, the dimensionless stress required to initiate lifting is found to be much higher than that of rolling, the former substantially above the Shields' curve while the latter is substantially below it. The theory is compared with Vanoni's 1964 data, with meaningful results. For higher particle Reynolds number, where&nbsp;</span><i>u</i><span><sub>*</sub></span><i>d</i><span>/ν&gt; 10, the dimensionless stress needed to initiate lifting is closer to that of rolling. The Shields' curve for the most part lies between the two theoretical thresholds.</span></p>","language":"English","publisher":"American Society of Civil Engineers","doi":"10.1061/(ASCE)0733-9429(1995)121:6(472)","usgsCitation":"Ling, C., 1995, Criteria for incipient motion of spherical sediment particles: Journal of Hydraulic Engineering, v. 121, no. 6, p. 472-478, https://doi.org/10.1061/(ASCE)0733-9429(1995)121:6(472).","productDescription":"7 p.","startPage":"472","endPage":"478","costCenters":[],"links":[{"id":418831,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"121","issue":"6","noUsgsAuthors":false,"publicationStatus":"PW","contributors":{"authors":[{"text":"Ling, Chi-Hai","contributorId":55154,"corporation":false,"usgs":true,"family":"Ling","given":"Chi-Hai","email":"","affiliations":[],"preferred":false,"id":877270,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":66198,"text":"i2359 - 1995 - Maps showing growth of the lava dome at Mount St. Helens, Washington, 1980-1986","interactions":[],"lastModifiedDate":"2019-06-06T13:13:27","indexId":"i2359","displayToPublicDate":"1995-06-01T00:00:00","publicationYear":"1995","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":320,"text":"IMAP","code":"I","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"2359","subseriesTitle":"NONE","title":"Maps showing growth of the lava dome at Mount St. Helens, Washington, 1980-1986","docAbstract":"<p>No abstract available&nbsp;</p>","language":"ENGLISH","doi":"10.3133/i2359","usgsCitation":"Holcomb, R.T., and Colony, W., 1995, Maps showing growth of the lava dome at Mount St. Helens, Washington, 1980-1986: U.S. Geological Survey IMAP 2359, 18 maps on 1 sheet :col. ;18 x 14 cm. and 26 x 19 cm., sheet 102 x 143 cm., folded in envelope 30 x 24 cm., https://doi.org/10.3133/i2359.","productDescription":"18 maps on 1 sheet :col. ;18 x 14 cm. and 26 x 19 cm., sheet 102 x 143 cm., folded in envelope 30 x 24 cm.","costCenters":[{"id":615,"text":"Volcano Hazards Program","active":true,"usgs":true}],"links":[{"id":255690,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/imap/2359/plate-1.pdf","size":"16337","linkFileType":{"id":1,"text":"pdf"}},{"id":255691,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/imap/2359/report.pdf","size":"28","linkFileType":{"id":1,"text":"pdf"}},{"id":255692,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/imap/2359/report-thumb.jpg"}],"scale":"5000","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -122.18416666666667,46.18444444444444 ], [ -122.18416666666667,46.20055555555556 ], [ -122.16805555555555,46.20055555555556 ], [ -122.16805555555555,46.18444444444444 ], [ -122.18416666666667,46.18444444444444 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a19e4b07f02db605abb","contributors":{"authors":[{"text":"Holcomb, R. T.","contributorId":99146,"corporation":false,"usgs":true,"family":"Holcomb","given":"R.","email":"","middleInitial":"T.","affiliations":[],"preferred":false,"id":274148,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Colony, W.E.","contributorId":62686,"corporation":false,"usgs":true,"family":"Colony","given":"W.E.","email":"","affiliations":[],"preferred":false,"id":274147,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":65536,"text":"i2403 - 1995 - Controlled photomosaic of the MTM 20182 Quadrangle, Orcus Patera region of Mars","interactions":[],"lastModifiedDate":"2019-12-23T12:38:24","indexId":"i2403","displayToPublicDate":"1995-06-01T00:00:00","publicationYear":"1995","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":320,"text":"IMAP","code":"I","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"2403","title":"Controlled photomosaic of the MTM 20182 Quadrangle, Orcus Patera region of Mars","docAbstract":"<p>No abstract available.</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/i2403","usgsCitation":"Water Resources Division, U.S. Geological Survey, 1995, Controlled photomosaic of the MTM 20182 Quadrangle, Orcus Patera region of Mars: U.S. Geological Survey IMAP 2403, Plate: 26 x 38 inches, https://doi.org/10.3133/i2403.","productDescription":"Plate: 26 x 38 inches","costCenters":[],"links":[{"id":189936,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":100989,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/imap/2403/plate-1.pdf","size":"18749","linkFileType":{"id":1,"text":"pdf"}}],"scale":"502000","otherGeospatial":"Mars","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ae0e4b07f02db688425","contributors":{"authors":[{"text":"Water Resources Division, U.S. Geological Survey","contributorId":128075,"corporation":true,"usgs":false,"organization":"Water Resources Division, U.S. Geological Survey","id":533923,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":20504,"text":"ofr9544 - 1995 - Lithology and X-ray mineralogy of the Shell 410-1 well, U.S. North Atlantic outer continental shelf","interactions":[],"lastModifiedDate":"2012-02-02T00:07:35","indexId":"ofr9544","displayToPublicDate":"1995-06-01T00:00:00","publicationYear":"1995","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":"95-44","title":"Lithology and X-ray mineralogy of the Shell 410-1 well, U.S. North Atlantic outer continental shelf","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/ofr9544","usgsCitation":"Poppe, L., 1995, Lithology and X-ray mineralogy of the Shell 410-1 well, U.S. North Atlantic outer continental shelf: U.S. Geological Survey Open-File Report 95-44, 9 p.  :map ;28 cm., https://doi.org/10.3133/ofr9544.","productDescription":"9 p.  :map ;28 cm.","costCenters":[],"links":[{"id":152669,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1995/0044/report-thumb.jpg"},{"id":50040,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1995/0044/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a61e4b07f02db635bd6","contributors":{"authors":[{"text":"Poppe, Lawrence J. lpoppe@usgs.gov","contributorId":2149,"corporation":false,"usgs":true,"family":"Poppe","given":"Lawrence J.","email":"lpoppe@usgs.gov","affiliations":[{"id":678,"text":"Woods Hole Coastal and Marine Science Center","active":true,"usgs":true}],"preferred":false,"id":182763,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":18655,"text":"ofr9556 - 1995 - Extraction of metals from raw clinoptilolite-rich rocks exposed to water in heavy-metal-polluted drainages","interactions":[],"lastModifiedDate":"2012-02-02T00:07:28","indexId":"ofr9556","displayToPublicDate":"1995-06-01T00:00:00","publicationYear":"1995","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":"95-56","title":"Extraction of metals from raw clinoptilolite-rich rocks exposed to water in heavy-metal-polluted drainages","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/ofr9556","usgsCitation":"Desborough, G.A., and Frishman, D., 1995, Extraction of metals from raw clinoptilolite-rich rocks exposed to water in heavy-metal-polluted drainages: U.S. Geological Survey Open-File Report 95-56, iii, 30 p. ill., map ;28 cm., https://doi.org/10.3133/ofr9556.","productDescription":"iii, 30 p. ill., map ;28 cm.","costCenters":[],"links":[{"id":151725,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1995/0056/report-thumb.jpg"},{"id":47992,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1995/0056/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a06e4b07f02db5f8a14","contributors":{"authors":[{"text":"Desborough, George A.","contributorId":101661,"corporation":false,"usgs":true,"family":"Desborough","given":"George","email":"","middleInitial":"A.","affiliations":[],"preferred":false,"id":179501,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Frishman, David","contributorId":40214,"corporation":false,"usgs":true,"family":"Frishman","given":"David","email":"","affiliations":[],"preferred":false,"id":179500,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":18312,"text":"ofr91596 - 1995 - An empirical equation for modeling rare earth element mineral-mineral partitioning; an application to mantle metasomatism","interactions":[],"lastModifiedDate":"2012-02-02T00:07:29","indexId":"ofr91596","displayToPublicDate":"1995-06-01T00:00:00","publicationYear":"1995","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":"91-596","title":"An empirical equation for modeling rare earth element mineral-mineral partitioning; an application to mantle metasomatism","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/ofr91596","usgsCitation":"Budahn, J.R., 1995, An empirical equation for modeling rare earth element mineral-mineral partitioning; an application to mantle metasomatism: U.S. Geological Survey Open-File Report 91-596, 44 leaves :ill. ;28 cm., https://doi.org/10.3133/ofr91596.","productDescription":"44 leaves :ill. ;28 cm.","costCenters":[],"links":[{"id":151685,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1991/0596/report-thumb.jpg"},{"id":47660,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1991/0596/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ad9e4b07f02db684afa","contributors":{"authors":[{"text":"Budahn, James R. 0000-0001-9794-8882 jbudahn@usgs.gov","orcid":"https://orcid.org/0000-0001-9794-8882","contributorId":1175,"corporation":false,"usgs":true,"family":"Budahn","given":"James","email":"jbudahn@usgs.gov","middleInitial":"R.","affiliations":[{"id":171,"text":"Central Mineral and Environmental Resources Science Center","active":true,"usgs":true}],"preferred":true,"id":178891,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":21460,"text":"ofr94489 - 1995 - Selected meteorological data for an arid site near Beatty, Nye County, Nevada, calendar years 1990 and 1991","interactions":[],"lastModifiedDate":"2019-12-08T12:59:36","indexId":"ofr94489","displayToPublicDate":"1995-06-01T00:00:00","publicationYear":"1995","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":"94-489","title":"Selected meteorological data for an arid site near Beatty, Nye County, Nevada, calendar years 1990 and 1991","docAbstract":"<p>Selected meteorological data were collected at a study site adjacent to a low-level radioactive-waste burial facility near Beatty, Nevada, for calendar years 1990 and 1991. Data were collected in support of ongoing studies to estimate the potential for downward movement of radionuclides into the unsaturated sediments beneath waste-burial trenches at the facility. The data include air temperature, relative humidity, vapor pressure, incident solar radiation, windspeed, wind direction, barometric pressure, and precipitation. The data are summarized in tables and graphs.</p><p>Instrumentation used at the site is discussed. The discussion includes the type, reported accuracy, and mounting height of each sensor.</p><p>In 1990, the average hourly air temperatures ranged from -16.2 degrees Celsius, in December, to 44.2 degrees Celsius, in July. Hourly averaged relative humidity ranged from 6 percent to more than 90 percent. Hourly vapor pressures ranged from 0.08 to 1.84 kilopascals. Daily maximum incident solar radiation values ranged from 192 to 1,028 watts per square meter. Daily mean windspeed ranged from less than 1 to 8.7 meters per second. Wind direction was primarily from the northwest in fall, winter, and spring and varied from southeast, southwest, or northwest during the summer. Hourly barometric pressures ranged from 99.47 to 103.12 kilopascals. Total precipitation for 1990 was 32.4 millimeters; almost 45 percent was in September.</p><p>In 1991, the average hourly air temperatures ranged from -9.2 degrees Celsius, in January, to 43.7 degrees Celsius, in July. Hourly averaged relative humidity ranged from 3 percent to more than 95 percent. Hourly vapor pressures ranged from 0.07 to 2.22 kilopascals. Daily maximum incident solar radiation values ranged from 143 to 1,041 watts per square meter. Daily mean windspeed ranged from 1.2 to 8.4 meters per second. Wind direction was primarily from the northwest in fall, winter, and spring and varied from southeast, southwest, or northwest during the summer. Hourly barometric pressures ranged from 99.52 to 103.40 kilopascals. Total precipitation for 1991 was 103.6 millimeters; almost 60 percent was in March.</p>","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Reston, VA","doi":"10.3133/ofr94489","usgsCitation":"Wood, J.L., and Andraski, B.J., 1995, Selected meteorological data for an arid site near Beatty, Nye County, Nevada, calendar years 1990 and 1991: U.S. Geological Survey Open-File Report 94-489, iv, 49 p., https://doi.org/10.3133/ofr94489.","productDescription":"iv, 49 p.","costCenters":[{"id":465,"text":"Nevada Water Science Center","active":true,"usgs":true},{"id":589,"text":"Toxic Substances Hydrology Program","active":true,"usgs":true}],"links":[{"id":51025,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1994/0489/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":154006,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1994/0489/report-thumb.jpg"}],"country":"United States","state":"Nevada","county":"Nye County","geographicExtents":"{\"type\":\"FeatureCollection\",\"features\":[{\"type\":\"Feature\",\"geometry\":{\"type\":\"Polygon\",\"coordinates\":[[[-115.9082,39.1615],[-115.5191,38.9578],[-115.4725,38.9325],[-115.4433,38.9162],[-115.3694,38.8769],[-115.363,38.874],[-115.242,38.8093],[-115.0969,38.7309],[-115.0777,38.721],[-115.0604,38.7107],[-115.0291,38.6937],[-114.999,38.6777],[-114.9996,38.592],[-114.9997,38.4315],[-114.9994,38.3894],[-115.0004,38.0507],[-115.1185,38.0508],[-115.1436,38.0508],[-115.326,38.0515],[-115.3453,38.0514],[-115.4003,38.051],[-115.4587,38.0506],[-115.6394,38.0512],[-115.6581,38.051],[-115.8404,38.0504],[-115.8931,38.0507],[-115.8938,37.723],[-115.8969,37.5498],[-115.8975,37.2796],[-115.8982,37.1926],[-115.8942,36.8425],[-115.8941,36.686],[-115.8945,36.6702],[-115.8949,36.598],[-115.8949,36.5962],[-115.8946,36.5858],[-115.8947,36.5005],[-115.8945,36.4806],[-115.8949,36.462],[-115.8944,36.457],[-115.8948,36.3087],[-115.8945,36.2923],[-115.8943,36.1957],[-115.8945,36.1608],[-115.8948,36.1163],[-115.8948,36.0927],[-115.895,36.0015],[-115.9178,36.0192],[-115.9518,36.0457],[-115.9925,36.0773],[-116.049,36.1211],[-116.0624,36.1314],[-116.1039,36.1636],[-116.1287,36.1829],[-116.1702,36.2152],[-116.173,36.2174],[-116.2311,36.2626],[-116.2834,36.3028],[-116.2954,36.3122],[-116.3752,36.373],[-116.5107,36.4764],[-116.5247,36.4871],[-116.5589,36.5131],[-116.574,36.5245],[-116.5946,36.54],[-116.6556,36.5867],[-116.6583,36.5888],[-116.6764,36.6024],[-116.706,36.6248],[-116.7895,36.6877],[-116.8424,36.7276],[-116.8453,36.7298],[-116.8806,36.7568],[-116.8912,36.7648],[-116.9237,36.7891],[-116.9641,36.8193],[-116.9783,36.8299],[-116.981,36.8319],[-117.0046,36.8495],[-117.164,36.9688],[-117.1639,36.9698],[-117.1637,37.0182],[-117.164,37.0894],[-117.1642,37.171],[-117.1641,37.1909],[-117.1641,37.1936],[-117.1665,37.6995],[-117.1664,37.714],[-117.1663,37.7285],[-117.1663,37.7435],[-117.1662,37.7585],[-117.1657,38.0019],[-117.2198,38.0482],[-117.2397,38.0483],[-117.239,38.0641],[-117.2408,38.0705],[-117.2653,38.0932],[-117.6896,38.4731],[-118.0197,38.7599],[-118.197,38.9154],[-118.1972,38.9993],[-117.8559,39.0746],[-117.7748,39.092],[-117.7008,39.1058],[-117.6409,39.1149],[-117.5946,39.1231],[-117.4742,39.1431],[-117.3823,39.1562],[-117.3609,39.1585],[-117.3318,39.1629],[-117.3063,39.1634],[-117.2849,39.1633],[-117.1995,39.1632],[-117.0856,39.1628],[-117.0322,39.1626],[-117.0144,39.1626],[-116.9871,39.1625],[-116.9158,39.1631],[-116.7562,39.1622],[-116.7301,39.1625],[-116.5996,39.1616],[-116.5859,39.162],[-116.4815,39.1616],[-116.3497,39.1618],[-116.2358,39.1616],[-116.0548,39.1624],[-115.9082,39.1615]]]},\"properties\":{\"name\":\"Nye\",\"state\":\"NV\"}}]}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a03e4b07f02db5f83c8","contributors":{"authors":[{"text":"Wood, James L.","contributorId":10059,"corporation":false,"usgs":true,"family":"Wood","given":"James","email":"","middleInitial":"L.","affiliations":[],"preferred":false,"id":184467,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Andraski, Brian J. 0000-0002-2086-0417 andraski@usgs.gov","orcid":"https://orcid.org/0000-0002-2086-0417","contributorId":168800,"corporation":false,"usgs":true,"family":"Andraski","given":"Brian","email":"andraski@usgs.gov","middleInitial":"J.","affiliations":[{"id":465,"text":"Nevada Water Science Center","active":true,"usgs":true},{"id":38175,"text":"Toxics Substances Hydrology Program","active":true,"usgs":true},{"id":438,"text":"National Research Program - Western Branch","active":true,"usgs":true}],"preferred":false,"id":184468,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
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