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,{"id":40232,"text":"ofr78362 - 1978 - Complete Bouguer gravity maps and gravity models of the Date Creek basin and vicinity, Maricopa, Mojave, Yavapai, and Yuma Counties, Arizona","interactions":[],"lastModifiedDate":"2023-04-18T21:34:26.786406","indexId":"ofr78362","displayToPublicDate":"1978-01-01T00:00:00","publicationYear":"1978","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":"78-362","title":"Complete Bouguer gravity maps and gravity models of the Date Creek basin and vicinity, Maricopa, Mojave, Yavapai, and Yuma Counties, Arizona","docAbstract":"<p>No abstract available.</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr78362","usgsCitation":"Wynn, J.C., and Otton, J.K., 1978, Complete Bouguer gravity maps and gravity models of the Date Creek basin and vicinity, Maricopa, Mojave, Yavapai, and Yuma Counties, Arizona: U.S. Geological Survey Open-File Report 78-362, 2 Plates: 34.80 x 34.59 inches and 32.80 x 29.22 inches, https://doi.org/10.3133/ofr78362.","productDescription":"2 Plates: 34.80 x 34.59 inches and 32.80 x 29.22 inches","costCenters":[{"id":164,"text":"Central Energy Resources Science Center","active":true,"usgs":true}],"links":[{"id":176906,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":415970,"rank":4,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_14701.htm","linkFileType":{"id":5,"text":"html"}},{"id":71004,"rank":3,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1978/0362/plate-2.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":71003,"rank":2,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1978/0362/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}}],"country":"United States","state":"Arizona","county":"Maricopa County, Mohave County, Yavapai County, Yuma County","otherGeospatial":"Date Creek Basin and vicinity","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"coordinates\": [\n          [\n            [\n              -112.729,\n              34.543\n            ],\n            [\n              -114,\n              34.543\n            ],\n            [\n              -114,\n              33.75\n            ],\n            [\n              -112.729,\n              33.75\n            ],\n            [\n              -112.729,\n              34.543\n            ]\n          ]\n        ],\n        \"type\": \"Polygon\"\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b1ae4b07f02db6a838b","contributors":{"authors":[{"text":"Wynn, Jeffrey C.","contributorId":81081,"corporation":false,"usgs":true,"family":"Wynn","given":"Jeffrey","email":"","middleInitial":"C.","affiliations":[],"preferred":false,"id":223154,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Otton, James K. jkotton@usgs.gov","contributorId":1170,"corporation":false,"usgs":true,"family":"Otton","given":"James","email":"jkotton@usgs.gov","middleInitial":"K.","affiliations":[{"id":164,"text":"Central Energy Resources Science Center","active":true,"usgs":true}],"preferred":true,"id":223153,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":11631,"text":"ofr78843 - 1978 - The effectiveness of stream-sediment sampling along the Rio Ojo Caliente, New Mexico","interactions":[],"lastModifiedDate":"2023-04-04T22:00:49.091698","indexId":"ofr78843","displayToPublicDate":"1978-01-01T00:00:00","publicationYear":"1978","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":"78-843","title":"The effectiveness of stream-sediment sampling along the Rio Ojo Caliente, New Mexico","docAbstract":"<p>No abstract available.</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr78843","usgsCitation":"Wenrich-Verbeek, K.J., 1978, The effectiveness of stream-sediment sampling along the Rio Ojo Caliente, New Mexico: U.S. Geological Survey Open-File Report 78-843, 9 p., https://doi.org/10.3133/ofr78843.","productDescription":"9 p.","costCenters":[],"links":[{"id":415200,"rank":3,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_74940.htm","linkFileType":{"id":5,"text":"html"}},{"id":39491,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1978/0843/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":143781,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1978/0843/report-thumb.jpg"}],"country":"United States","state":"New Mexico","otherGeospatial":"Rio Ojo Caliente","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"coordinates\": [\n          [\n            [\n              -106,\n              36.75\n            ],\n            [\n              -106,\n              36.3278\n            ],\n            [\n              -106.25,\n              36.3278\n            ],\n            [\n              -106.25,\n              36.75\n            ],\n            [\n              -106,\n              36.75\n            ]\n          ]\n        ],\n        \"type\": \"Polygon\"\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4aa8e4b07f02db6675fd","contributors":{"authors":[{"text":"Wenrich-Verbeek, Karen J.","contributorId":101662,"corporation":false,"usgs":true,"family":"Wenrich-Verbeek","given":"Karen","email":"","middleInitial":"J.","affiliations":[],"preferred":false,"id":163477,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":46382,"text":"ofr78435 - 1978 - Map of the Antelope Valley-East Kern Water Agency area, California, showing ground-water subunits and areas and well hydrographs","interactions":[],"lastModifiedDate":"2023-04-18T21:17:58.4951","indexId":"ofr78435","displayToPublicDate":"1978-01-01T00:00:00","publicationYear":"1978","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":"78-435","title":"Map of the Antelope Valley-East Kern Water Agency area, California, showing ground-water subunits and areas and well hydrographs","docAbstract":"<p>The U.S. Geological Survey has released to the open file a map, scale 1:125,000, showing ground-water subunits and areas, and well hydrographs in the Antelope Valley-East Kern Water Agency area, California.&nbsp;</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr78435","usgsCitation":"Lamb, C.E., and McIntyre, M.J., 1978, Map of the Antelope Valley-East Kern Water Agency area, California, showing ground-water subunits and areas and well hydrographs: U.S. Geological Survey Open-File Report 78-435, 1 Plate: 37.92 x 39.67 inches, https://doi.org/10.3133/ofr78435.","productDescription":"1 Plate: 37.92 x 39.67 inches","costCenters":[],"links":[{"id":168289,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":415968,"rank":3,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_14722.htm","linkFileType":{"id":5,"text":"html"}},{"id":83348,"rank":2,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1978/0435/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}}],"country":"United States","state":"California","otherGeospatial":"Antelope Valley-East Kern Water Agency area","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"coordinates\": [\n          [\n            [\n              -118.856,\n              35.361\n            ],\n            [\n              -118.856,\n              34.4\n            ],\n            [\n              -117.6310,\n              34.4\n            ],\n            [\n              -117.6310,\n              35.361\n            ],\n            [\n              -118.856,\n              35.361\n            ]\n          ]\n        ],\n        \"type\": \"Polygon\"\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a93e4b07f02db6582db","contributors":{"authors":[{"text":"Lamb, C. E.","contributorId":59793,"corporation":false,"usgs":true,"family":"Lamb","given":"C.","email":"","middleInitial":"E.","affiliations":[],"preferred":false,"id":233192,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"McIntyre, M. J.","contributorId":53449,"corporation":false,"usgs":true,"family":"McIntyre","given":"M.","email":"","middleInitial":"J.","affiliations":[],"preferred":false,"id":233191,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":70162496,"text":"70162496 - 1978 - Searching for seismic precursors to earthquakes in central California","interactions":[],"lastModifiedDate":"2016-02-05T16:39:03","indexId":"70162496","displayToPublicDate":"1978-01-01T00:00:00","publicationYear":"1978","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1435,"text":"Earthquake Information Bulletin (USGS)","active":true,"publicationSubtype":{"id":10}},"title":"Searching for seismic precursors to earthquakes in central California","language":"English","publisher":"U.S Geological Survey","usgsCitation":"Wesson, R.L., 1978, Searching for seismic precursors to earthquakes in central California: Earthquake Information Bulletin (USGS), v. 10, no. 2, p. 51-54.","productDescription":"4 p.","startPage":"51","endPage":"54","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[],"links":[{"id":314819,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"10","issue":"2","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"56a75569e4b0b28f1184d87b","contributors":{"authors":[{"text":"Wesson, R. L.","contributorId":51752,"corporation":false,"usgs":true,"family":"Wesson","given":"R.","email":"","middleInitial":"L.","affiliations":[],"preferred":false,"id":589691,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":70168608,"text":"70168608 - 1978 - Unusual animal behavior before earthquakes","interactions":[],"lastModifiedDate":"2016-02-20T13:22:10","indexId":"70168608","displayToPublicDate":"1978-01-01T00:00:00","publicationYear":"1978","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1435,"text":"Earthquake Information Bulletin (USGS)","active":true,"publicationSubtype":{"id":10}},"title":"Unusual animal behavior before earthquakes","language":"English","publisher":"U.S Geological Survey","usgsCitation":"Reasenberg, P., 1978, Unusual animal behavior before earthquakes: Earthquake Information Bulletin (USGS), v. 10, no. 2, p. 42-50.","productDescription":"9 p.","startPage":"42","endPage":"50","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[],"links":[{"id":318226,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"10","issue":"2","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"56c99c5fe4b059daa47c9b18","contributors":{"authors":[{"text":"Reasenberg, P.","contributorId":22913,"corporation":false,"usgs":true,"family":"Reasenberg","given":"P.","email":"","affiliations":[],"preferred":false,"id":621016,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":70168596,"text":"70168596 - 1978 - Can animals help to predict earthquakes?","interactions":[],"lastModifiedDate":"2016-02-20T12:50:51","indexId":"70168596","displayToPublicDate":"1978-01-01T00:00:00","publicationYear":"1978","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1435,"text":"Earthquake Information Bulletin (USGS)","active":true,"publicationSubtype":{"id":10}},"title":"Can animals help to predict earthquakes?","language":"English","publisher":"U.S Geological Survey","usgsCitation":"Ling-huang, S., 1978, Can animals help to predict earthquakes?: Earthquake Information Bulletin (USGS), v. 10, no. 6, p. 231-233.","productDescription":"3 p.","startPage":"231","endPage":"233","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[],"links":[{"id":318214,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"10","issue":"6","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"56c99c43e4b059daa47c9a87","contributors":{"authors":[{"text":"Ling-huang, Shen","contributorId":167097,"corporation":false,"usgs":false,"family":"Ling-huang","given":"Shen","email":"","affiliations":[],"preferred":false,"id":620998,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":70162491,"text":"70162491 - 1978 - Sea-level changes before large earthquakes","interactions":[],"lastModifiedDate":"2016-03-10T15:01:26","indexId":"70162491","displayToPublicDate":"1978-01-01T00:00:00","publicationYear":"1978","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1435,"text":"Earthquake Information Bulletin (USGS)","active":true,"publicationSubtype":{"id":10}},"title":"Sea-level changes before large earthquakes","docAbstract":"<p>Changes in sea level have long been used as a measure of local uplift and subsidence associated with large earthquakes. For instance, in 1835, the British naturalist Charles Darwin observed that sea level dropped by 2.7 meters during the large earthquake in Concepcion, CHile. From this piece of evidence and the terraces along the beach that he saw, Darwin concluded that the Andes had grown to their present height through earthquakes. Much more recently, George Plafker and James C. Savage of the U.S Geological Survey have shown, from barnacle lines, that the great 1960 Chile and the 1964 Alaska earthquakes caused several meters of vertical displacement of the shoreline.&nbsp;</p>","language":"English","publisher":"U.S Geological Survey","usgsCitation":"Wyss, M., 1978, Sea-level changes before large earthquakes: Earthquake Information Bulletin (USGS), v. 10, no. 5, p. 165-168.","productDescription":"4 p.","startPage":"165","endPage":"168","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[],"links":[{"id":314813,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"10","issue":"5","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"56a75569e4b0b28f1184d879","contributors":{"authors":[{"text":"Wyss, M.","contributorId":68880,"corporation":false,"usgs":true,"family":"Wyss","given":"M.","email":"","affiliations":[],"preferred":false,"id":589685,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":70168578,"text":"70168578 - 1978 - Clarence Allen talks about the responsibilities in earthquake prediction","interactions":[],"lastModifiedDate":"2016-03-22T14:25:13","indexId":"70168578","displayToPublicDate":"1978-01-01T00:00:00","publicationYear":"1978","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1435,"text":"Earthquake Information Bulletin (USGS)","active":true,"publicationSubtype":{"id":10}},"title":"Clarence Allen talks about the responsibilities in earthquake prediction","docAbstract":"<p>Dr. Clarence R. Allen is professor of geology and geophysics at the California Institute of Technology. He has been a member of advisory panels to the Executive Office of the President, National Academy of Sciences, National Science Foundation, U.S Geological Survey, UNESCO, California State Mining and Geology Board, and the California Department of Water Resources. Dr. Allen has been President of both the Geological Society of America and the Seismological Society of America (SSA). The title of this interview is based on his presidential address to the SSA in 1976.&nbsp;</p>","language":"English","publisher":"U.S Geological Survey","usgsCitation":"Spall, H., 1978, Clarence Allen talks about the responsibilities in earthquake prediction: Earthquake Information Bulletin (USGS), v. 10, no. 4, p. 116-119.","productDescription":"4 p.","startPage":"116","endPage":"119","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[],"links":[{"id":318198,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"10","issue":"4","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"56c84ac4e4b0b3c9ae381012","contributors":{"authors":[{"text":"Spall, H.","contributorId":99290,"corporation":false,"usgs":true,"family":"Spall","given":"H.","affiliations":[],"preferred":false,"id":620946,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":70168598,"text":"70168598 - 1978 - Geodimeter measurements and the Southern California uplift","interactions":[],"lastModifiedDate":"2019-11-14T08:30:51","indexId":"70168598","displayToPublicDate":"1978-01-01T00:00:00","publicationYear":"1978","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1435,"text":"Earthquake Information Bulletin (USGS)","active":true,"publicationSubtype":{"id":10}},"title":"Geodimeter measurements and the Southern California uplift","docAbstract":"<p>Modern surveying instruments, such as geodimeters, are capable of measuring distances in the range of 1 to 30 kilometers with remarkable precision. Indeed, the present limitation upon the precision of measurement is not the resolution of the instruments themselves but rather the uncertainty introduced by variations in the velocity of light in the atmosphere between the two endpoints of the measured distance. This capability in precise distance measurement can be applied to earthquake studies by using repeated distance measurements to determine changes in the distance between monuments located along the major faults. Such measurements have been made along the San Andreas fault since late 1959, and, as a result, a wealth of data on crustal deformation in that area is now available. In fact, geodimeter measurements of this type furnish a more stable measure of secular strain (change in the ratio of length to length) than any continuously recording strain meter. The superiority of the geodimeter measurement stems principally from the long base line measured which averages over local inhomogeneities (cracks and joints in the rock, inclusions, and so forth).</p>\n<p>This article describes the important features of the measurement technique as well as some results for the region of the southern California uplift. &nbsp;</p>","language":"English","publisher":"U.S Geological Survey","publisherLocation":"Reston, VA","usgsCitation":"Prescott, W., and Savage, J., 1978, Geodimeter measurements and the Southern California uplift: Earthquake Information Bulletin (USGS), v. 10, no. 4, p. 131-135.","productDescription":"5 p.","startPage":"131","endPage":"135","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[],"links":[{"id":318216,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United States","state":"California","otherGeospatial":"Southern California","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -119.66308593749999,\n              34.52466147177172\n            ],\n            [\n              -114.345703125,\n              35.06597313798418\n            ],\n            [\n              -116.1474609375,\n              37.26530995561875\n            ],\n            [\n              -120.673828125,\n              36.27970720524017\n            ],\n            [\n              -119.66308593749999,\n              34.52466147177172\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","volume":"10","issue":"4","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"56c99c52e4b059daa47c9ac7","contributors":{"authors":[{"text":"Prescott, W.H.","contributorId":96337,"corporation":false,"usgs":true,"family":"Prescott","given":"W.H.","email":"","affiliations":[],"preferred":false,"id":621000,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Savage, J.C. 0000-0002-5114-7673","orcid":"https://orcid.org/0000-0002-5114-7673","contributorId":102876,"corporation":false,"usgs":true,"family":"Savage","given":"J.C.","affiliations":[],"preferred":false,"id":621001,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":70162503,"text":"70162503 - 1978 - How often will earthquakes recur on the San Andreas Fault?","interactions":[],"lastModifiedDate":"2017-05-18T12:07:38","indexId":"70162503","displayToPublicDate":"1978-01-01T00:00:00","publicationYear":"1978","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1435,"text":"Earthquake Information Bulletin (USGS)","active":true,"publicationSubtype":{"id":10}},"title":"How often will earthquakes recur on the San Andreas Fault?","docAbstract":"<p>The relationship between magnitude and abundance of earthquakes, called a recurrence curve, has been derived for many regions of the world from seismographic records. AS an example, Clarence Allen and his associates at the California Institute of Technology have obtained recurrence rates for the southern California region by incorporating data from over 10,000 earthquakes recorded between 1934 and 1963.&nbsp;</p>\n<p>My own approach to estimating average recurrence intervals has been somewhat different. I have used the history of slip rates along the San Andreas fault that are preserved in the geologic record. The main advantage in this method is that is samples a very long period of time, which gives a better estimate of the recurrence of small earthquakes. &nbsp;</p>","language":"English","publisher":"U.S. Geological Survey","usgsCitation":"Wallace, R.E., 1978, How often will earthquakes recur on the San Andreas Fault?: Earthquake Information Bulletin (USGS), v. 10, no. 3, p. 76-81.","productDescription":"6 p.","startPage":"76","endPage":"81","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[],"links":[{"id":314828,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United States","state":"California","otherGeospatial":"San Andreas fault","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -124.354248046875,\n              40.59727063442027\n            ],\n            [\n              -123.760986328125,\n              39.926588421909436\n            ],\n            [\n              -122.64038085937499,\n              37.94419750075404\n            ],\n            [\n              -121.497802734375,\n              37.204081555898526\n            ],\n            [\n              -120.0146484375,\n              36.31512514748051\n            ],\n            [\n              -118.751220703125,\n              35.038992046780784\n            ],\n            [\n              -117.01538085937499,\n              34.225429015241396\n            ],\n            [\n              -115.4443359375,\n              33.367237465838315\n            ],\n            [\n              -115.42236328124999,\n              32.96258644191747\n            ],\n            [\n              -115.8837890625,\n              33.04550781490999\n            ],\n            [\n              -117.88330078125,\n              34.31621838080741\n            ],\n            [\n              -119.66308593749999,\n              35.38904996691167\n            ],\n            [\n              -121.31103515625,\n              36.76529191711624\n            ],\n            [\n              -122.64038085937499,\n              37.622933594900864\n            ],\n            [\n              -124.068603515625,\n              39.198205348894795\n            ],\n            [\n              -124.486083984375,\n              40.48038142908172\n            ],\n            [\n              -124.354248046875,\n              40.59727063442027\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","volume":"10","issue":"3","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"56a7555ae4b0b28f1184d845","contributors":{"authors":[{"text":"Wallace, R. E.","contributorId":6823,"corporation":false,"usgs":true,"family":"Wallace","given":"R.","email":"","middleInitial":"E.","affiliations":[],"preferred":false,"id":589699,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":70012492,"text":"70012492 - 1978 - Empirical model of Skeletonema costatum photosynthetic rate, with applications in the San Francisco Bay estuary","interactions":[],"lastModifiedDate":"2023-02-01T17:40:47.965072","indexId":"70012492","displayToPublicDate":"1978-01-01T00:00:00","publicationYear":"1978","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":664,"text":"Advances in Water Resources","active":true,"publicationSubtype":{"id":10}},"displayTitle":"Empirical model of <i>Skeletonema costatum</i> photosynthetic rate, with applications in the San Francisco Bay estuary","title":"Empirical model of Skeletonema costatum photosynthetic rate, with applications in the San Francisco Bay estuary","docAbstract":"<p>An empirical model of<span>&nbsp;</span><i>Skeletonema costatum</i><span>&nbsp;</span>photosynthetic rate is developed and fit to measurements of photosynthesis selected from the literature. Because the model acknowledges existence of: 1) a light-temperature interaction (by allowing optimum irradiance to vary with temperature), 2) light inhibition, 3) temperature inhibition, and 4) a salinity effect, it accurately estimates photosynthetic rates measured over a wide range of temperature, light intensity, and salinity. Integration of predicted instantaneous rate of photosynthesis with time and depth yields daily net carbon assimilation (pg C cell<sup>−1</sup><span>&nbsp;</span>day<sup>−1</sup>) in a mixed layer of specified depth, when salinity, temperature, daily irradiance and extinction coefficient are known. The assumption of constant carbon quota (pg C cell<sup>−1</sup>) allows for prediction of mean specific growth rate (day<sup>−1</sup>), which can be used in numerical models of<span>&nbsp;</span><i>Skeletonema costatum</i><span>&nbsp;</span>population dynamics.</p><p>Application of the model to northern San Francisco Bay clearly demonstrates the limitation of growth by low light availability, and suggests that large population densities of<span>&nbsp;</span><i>S. costatum</i><span>&nbsp;</span>observed during summer months are not the result of active growth in the central deep channels (where growth rates are consistently predicted to be negative). But predicted growth rates in the lateral shallows are positive during summer and fall, thus offering a testable hypothesis that shoals are the only sites of active population growth by<span>&nbsp;</span><i>S. costatum</i><span>&nbsp;</span>(and perhaps other neritic diatoms) in the northern reach of San Francisco Bay.</p>","language":"English","publisher":"Elsevier","doi":"10.1016/0309-1708(78)90040-4","usgsCitation":"Cloern, J.E., 1978, Empirical model of Skeletonema costatum photosynthetic rate, with applications in the San Francisco Bay estuary: Advances in Water Resources, v. 1, no. 5, p. 267-274, https://doi.org/10.1016/0309-1708(78)90040-4.","productDescription":"8 p.","startPage":"267","endPage":"274","numberOfPages":"8","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[{"id":438,"text":"National Research Program - Western Branch","active":true,"usgs":true},{"id":552,"text":"San Francisco Bay-Delta","active":false,"usgs":true},{"id":5079,"text":"Pacific Regional Director's Office","active":true,"usgs":true}],"links":[{"id":222256,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United States","state":"California","otherGeospatial":"San Francisco Bay estuary","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"coordinates\": [\n          [\n            [\n              -121.22039965621613,\n              38.24440703031118\n            ],\n            [\n              -122.57745968735097,\n              38.24440703031118\n            ],\n            [\n              -122.57745968735097,\n              37.3957605043622\n            ],\n            [\n              -121.22039965621613,\n              37.3957605043622\n            ],\n            [\n              -121.22039965621613,\n              38.24440703031118\n            ]\n          ]\n        ],\n        \"type\": \"Polygon\"\n      }\n    }\n  ]\n}","volume":"1","issue":"5","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"505a090ce4b0c8380cd51d98","contributors":{"authors":[{"text":"Cloern, James E. 0000-0002-5880-6862 jecloern@usgs.gov","orcid":"https://orcid.org/0000-0002-5880-6862","contributorId":1488,"corporation":false,"usgs":true,"family":"Cloern","given":"James","email":"jecloern@usgs.gov","middleInitial":"E.","affiliations":[{"id":438,"text":"National Research Program - Western Branch","active":true,"usgs":true},{"id":37277,"text":"WMA - Earth System Processes Division","active":true,"usgs":true}],"preferred":true,"id":363746,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":93991,"text":"93991 - 1978 - Alternative sources of vitamin C for channel catfish","interactions":[],"lastModifiedDate":"2012-02-02T00:03:53","indexId":"93991","displayToPublicDate":"1978-01-01T00:00:00","publicationYear":"1978","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":9,"text":"Other Report"},"title":"Alternative sources of vitamin C for channel catfish","docAbstract":"No abstract available at this time","language":"English","publisher":"Department of Grain, Science and Industry, Kansas Agricultural Experiment Station","publisherLocation":"Manhattan, KS","collaboration":"None/FF","usgsCitation":"Brandt, T., Deyoe, C., and Seib, P., 1978, Alternative sources of vitamin C for channel catfish.","costCenters":[{"id":365,"text":"Leetown Science Center","active":true,"usgs":true}],"links":[{"id":127185,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4adee4b07f02db687387","contributors":{"authors":[{"text":"Brandt, T.M.","contributorId":91432,"corporation":false,"usgs":true,"family":"Brandt","given":"T.M.","email":"","affiliations":[],"preferred":false,"id":298338,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Deyoe, C.W.","contributorId":28189,"corporation":false,"usgs":true,"family":"Deyoe","given":"C.W.","email":"","affiliations":[],"preferred":false,"id":298336,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Seib, P.A.","contributorId":43294,"corporation":false,"usgs":true,"family":"Seib","given":"P.A.","email":"","affiliations":[],"preferred":false,"id":298337,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":70012643,"text":"70012643 - 1978 - Minor-element and Sr-isotope geochemistry of tertiary stocks, Colorado mineral belt","interactions":[],"lastModifiedDate":"2012-03-12T17:19:10","indexId":"70012643","displayToPublicDate":"1978-01-01T00:00:00","publicationYear":"1978","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1336,"text":"Contributions to Mineralogy and Petrology","active":true,"publicationSubtype":{"id":10}},"title":"Minor-element and Sr-isotope geochemistry of tertiary stocks, Colorado mineral belt","docAbstract":"Rocks of the northeast portion of the Colorado mineral belt form two petrographically, chemically and geographically distinct rock suites: (1) a silica oversaturated granodiorite suite; and (2) a silica saturated, high alkali monzonite suite. Rocks of the granodiorite suite generally have Sr contents less than 1000 ppm, subparallel REE patterns and initial 87Sr/ 86Sr ratios greater than 0.707. Rocks of the monzonite suite are restricted to the northeast part of the mineral belt, where few rocks of the granodiorite suite occur, and generally have Sr contents greater than 1000 ppm, highly variable REE patterns and 87Sr/86Sr initial ratios less than 0.706. Despite forming simple, smooth trends on major element variation diagrams, trace element data for rocks of the granodiorite suite indicate that they were not derived from a single magma. These rocks were derived from magmas having similar REE patterns, but variable Rb and Sr contents, and Rb/Sr ratios. The preferred explanation for these rocks is that they were derived by partial melting of a mixed source, which yielded pyroxene granulite or pyroxenite residues. The monzonite suite is chemically and petrographically more complex than the granodiorite suite. It is subdivided here into alkalic and mafic monzonites, and quartz syenites, based on the textural relations of their ferromagnesian phases and quartz. The geochemistry of these three rock types require derivation from separate and chemically distinct magma types. The preferred explanation for the alkalic monzonites is derivation from a heterogeneous mafic source, leaving a residue dominated by garnet and clinopyroxene. Early crystallization of sphene from these magmas was responsible for the severe depletion of the REE observed in the residual magmas. The lower Sr content and higher Rb/Sr ratios of the mafic monzonites requires a plagioclase-bearing source. The Sr-isotope systematics of the majority of these rocks are interpreted to be largely primary, and not the result of crustal contamination. The positive correlation of Rb/Sr and 87Sr/86Sr ratios for the least fractionated samples indicate that the sources from which parent magmas of both the granodiorite and monzonite suites were derived are Precambrian in age. ?? 1978 Springer-Verlag.","largerWorkType":{"id":2,"text":"Article"},"largerWorkTitle":"Contributions to Mineralogy and Petrology","largerWorkSubtype":{"id":10,"text":"Journal Article"},"language":"English","publisherLocation":"Springer-Verlag","doi":"10.1007/BF00383298","issn":"00107999","usgsCitation":"Simmons, E., and Hedge, C., 1978, Minor-element and Sr-isotope geochemistry of tertiary stocks, Colorado mineral belt: Contributions to Mineralogy and Petrology, v. 67, no. 4, p. 379-396, https://doi.org/10.1007/BF00383298.","startPage":"379","endPage":"396","numberOfPages":"18","costCenters":[],"links":[{"id":205159,"rank":9999,"type":{"id":10,"text":"Digital Object Identifier"},"url":"https://dx.doi.org/10.1007/BF00383298"},{"id":221902,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"67","issue":"4","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"505a5b28e4b0c8380cd6f382","contributors":{"authors":[{"text":"Simmons, E.C.","contributorId":80413,"corporation":false,"usgs":true,"family":"Simmons","given":"E.C.","email":"","affiliations":[],"preferred":false,"id":364123,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Hedge, C. E.","contributorId":73611,"corporation":false,"usgs":true,"family":"Hedge","given":"C. E.","affiliations":[],"preferred":false,"id":364122,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":70012640,"text":"70012640 - 1978 - World's oldest animal traces","interactions":[],"lastModifiedDate":"2012-03-12T17:19:01","indexId":"70012640","displayToPublicDate":"1978-01-01T00:00:00","publicationYear":"1978","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":2840,"text":"Nature","active":true,"publicationSubtype":{"id":10}},"title":"World's oldest animal traces","docAbstract":"[No abstract available]","largerWorkType":{"id":2,"text":"Article"},"largerWorkTitle":"Nature","largerWorkSubtype":{"id":10,"text":"Journal Article"},"language":"English","doi":"10.1038/275344b0","issn":"00280836","usgsCitation":"Cloud, P., 1978, World's oldest animal traces: Nature, v. 275, no. 5678, https://doi.org/10.1038/275344b0.","startPage":"344","costCenters":[],"links":[{"id":487203,"rank":10000,"type":{"id":40,"text":"Open Access Publisher Index Page"},"url":"https://doi.org/10.1038/275344b0","text":"Publisher Index Page"},{"id":221838,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"},{"id":205149,"rank":9999,"type":{"id":10,"text":"Digital Object Identifier"},"url":"https://dx.doi.org/10.1038/275344b0"}],"volume":"275","issue":"5678","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"505bd1d6e4b08c986b32f5a6","contributors":{"authors":[{"text":"Cloud, P.","contributorId":65973,"corporation":false,"usgs":true,"family":"Cloud","given":"P.","affiliations":[],"preferred":false,"id":364119,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":70012641,"text":"70012641 - 1978 - Determination of silver, bismuth, cadmium, copper, lead, and zinc in geologic materials by atomic absorption spectrometry with tricaprylylmethylammonium chloride","interactions":[],"lastModifiedDate":"2023-03-10T17:49:47.054281","indexId":"70012641","displayToPublicDate":"1978-01-01T00:00:00","publicationYear":"1978","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":761,"text":"Analytical Chemistry","active":true,"publicationSubtype":{"id":10}},"title":"Determination of silver, bismuth, cadmium, copper, lead, and zinc in geologic materials by atomic absorption spectrometry with tricaprylylmethylammonium chloride","docAbstract":"Interferences commonly encountered in the determination of silver, bismuth, cadmium, copper, lead, and zinc at crustal abundance levels are effectively eliminated using a rapid, sensitive, organic extraction technique. A potassium chlorate-hydrochloric acid digestion solubilizes the metals not tightly bound in the silicate lattice of rocks, soils, and stream sediments. The six metals are selectively extracted into a 10% Aliquat 336-MIBK organic phase in the presence of ascorbic acid and potassium iodide. Metals in the organic extract are determined by flame atomic absorption spectrometry to the 0.02-ppm level for silver, cadmium, copper, and zinc and to the 0.2-ppm level for bismuth and lead with a maximum relative standard deviation of 18.8% for known reference samples. An additional hydrofluoric acid digestion may be used to determine metals substituted in the silicate lattice.","language":"English","publisher":"ACS Publications","doi":"10.1021/ac50030a023","usgsCitation":"Viets, J.G., 1978, Determination of silver, bismuth, cadmium, copper, lead, and zinc in geologic materials by atomic absorption spectrometry with tricaprylylmethylammonium chloride: Analytical Chemistry, v. 50, no. 8, p. 1097-1101, https://doi.org/10.1021/ac50030a023.","productDescription":"5 p.","startPage":"1097","endPage":"1101","numberOfPages":"5","costCenters":[],"links":[{"id":221839,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"50","issue":"8","noUsgsAuthors":false,"publicationDate":"2002-05-01","publicationStatus":"PW","scienceBaseUri":"5059ffc6e4b0c8380cd4f3bb","contributors":{"authors":[{"text":"Viets, John G.","contributorId":84510,"corporation":false,"usgs":true,"family":"Viets","given":"John","email":"","middleInitial":"G.","affiliations":[],"preferred":false,"id":364120,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":70012423,"text":"70012423 - 1978 - Zur chemie der marsoberfläche","interactions":[],"lastModifiedDate":"2015-06-15T10:27:31","indexId":"70012423","displayToPublicDate":"1978-01-01T00:00:00","publicationYear":"1978","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1390,"text":"Die Naturwissenschaften","active":true,"publicationSubtype":{"id":10}},"title":"Zur chemie der marsoberfläche","docAbstract":"<p><span>Analyses of 13 samples of Martian surface materials with the Viking X-ray fluorescence spectrometers show SiO</span><span>2</span><span>&nbsp;similar to that of terrestrial mafic rocks, whereas Fe</span><span>2</span><span>O</span><span>3</span><span>, Cl, and S are higher and Al</span><span>2</span><span>O</span><span>3</span><span>, K</span><span>2</span><span>O, Rb, Sr, Y, and Zr are lower. Low totals suggest presence of CO</span><span>2</span><span>, H</span><span>2</span><span>O, and Na</span><span>2</span><span>O. Duricrust fragments are higher in S than fines, but samples from both landing sites are surprisingly similar. We suggest that Martian surface materials are aeolian deposits of complex mixtures of weathering products of maficultramafic rocks, possibly consisting of iron-rich clays, sulfates, iron oxides, carbonates, and chlorides.</span></p>","language":"German","publisher":"Springer","doi":"10.1007/BF00368561","issn":"00281042","usgsCitation":"Keil, K., Clark, B., Baird, A.K., Toulmin, P., and Rose, H.J., 1978, Zur chemie der marsoberfläche: Die Naturwissenschaften, v. 65, no. 5, p. 231-238, https://doi.org/10.1007/BF00368561.","productDescription":"8 p.","startPage":"231","endPage":"238","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[],"links":[{"id":222016,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"},{"id":205182,"rank":9999,"type":{"id":10,"text":"Digital Object Identifier"},"url":"https://dx.doi.org/10.1007/BF00368561"}],"volume":"65","issue":"5","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"505bd2a2e4b08c986b32f92d","contributors":{"authors":[{"text":"Keil, Klaus","contributorId":55955,"corporation":false,"usgs":true,"family":"Keil","given":"Klaus","email":"","affiliations":[],"preferred":false,"id":363517,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Clark, Benton C.","contributorId":127516,"corporation":false,"usgs":false,"family":"Clark","given":"Benton C.","affiliations":[{"id":7038,"text":"Space Science Institute, Boulder, Colorado","active":true,"usgs":false}],"preferred":false,"id":363516,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Baird, A. K.","contributorId":65148,"corporation":false,"usgs":true,"family":"Baird","given":"A.","email":"","middleInitial":"K.","affiliations":[],"preferred":false,"id":548675,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Toulmin, Priestley III","contributorId":8522,"corporation":false,"usgs":false,"family":"Toulmin","given":"Priestley","suffix":"III","email":"","affiliations":[{"id":12805,"text":"Univ. of California at San Diego","active":true,"usgs":false}],"preferred":false,"id":363520,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"Rose, Harry J. Jr.","contributorId":39013,"corporation":false,"usgs":true,"family":"Rose","given":"Harry","suffix":"Jr.","email":"","middleInitial":"J.","affiliations":[],"preferred":false,"id":363519,"contributorType":{"id":1,"text":"Authors"},"rank":5}]}}
,{"id":70012549,"text":"70012549 - 1978 - Ice sheet topography by satellite altimetry","interactions":[],"lastModifiedDate":"2012-03-12T17:19:07","indexId":"70012549","displayToPublicDate":"1978-01-01T00:00:00","publicationYear":"1978","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":2840,"text":"Nature","active":true,"publicationSubtype":{"id":10}},"title":"Ice sheet topography by satellite altimetry","docAbstract":"The surface elevation of the southern Greenland ice sheet and surface features of the ice flow are obtained from the radar altimeter on the GEOS 3 satellite. The achieved accuracy in surface elevation is ???2 m. As changes in surface elevation are indicative of changes in ice volume, the mass balance of the present ice sheets could be determined by repetitive mapping of the surface elevation and the surface could be monitored to detect surging or significant changes in ice flow. ?? 1978 Nature Publishing Group.","largerWorkType":{"id":2,"text":"Article"},"largerWorkTitle":"Nature","largerWorkSubtype":{"id":10,"text":"Journal Article"},"language":"English","doi":"10.1038/274539a0","issn":"00280836","usgsCitation":"Brooks, R., Campbell, W.J., Ramseier, R., Stanley, H., and Zwally, H., 1978, Ice sheet topography by satellite altimetry: Nature, v. 274, no. 5671, p. 539-543, https://doi.org/10.1038/274539a0.","startPage":"539","endPage":"543","numberOfPages":"5","costCenters":[],"links":[{"id":205195,"rank":9999,"type":{"id":10,"text":"Digital Object Identifier"},"url":"https://dx.doi.org/10.1038/274539a0"},{"id":222085,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"274","issue":"5671","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"505a37f2e4b0c8380cd612e3","contributors":{"authors":[{"text":"Brooks, R.L.","contributorId":61960,"corporation":false,"usgs":true,"family":"Brooks","given":"R.L.","email":"","affiliations":[],"preferred":false,"id":363876,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Campbell, W. J.","contributorId":8614,"corporation":false,"usgs":true,"family":"Campbell","given":"W.","email":"","middleInitial":"J.","affiliations":[],"preferred":false,"id":363874,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Ramseier, R.O.","contributorId":98039,"corporation":false,"usgs":true,"family":"Ramseier","given":"R.O.","email":"","affiliations":[],"preferred":false,"id":363878,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Stanley, H.R.","contributorId":65991,"corporation":false,"usgs":true,"family":"Stanley","given":"H.R.","email":"","affiliations":[],"preferred":false,"id":363877,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"Zwally, H.J.","contributorId":33847,"corporation":false,"usgs":true,"family":"Zwally","given":"H.J.","email":"","affiliations":[],"preferred":false,"id":363875,"contributorType":{"id":1,"text":"Authors"},"rank":5}]}}
,{"id":70012550,"text":"70012550 - 1978 - Prediction of capacity factors for aqueous organic solutes adsorbed on a porous acrylic resin","interactions":[],"lastModifiedDate":"2023-03-10T17:47:53.733634","indexId":"70012550","displayToPublicDate":"1978-01-01T00:00:00","publicationYear":"1978","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":761,"text":"Analytical Chemistry","active":true,"publicationSubtype":{"id":10}},"title":"Prediction of capacity factors for aqueous organic solutes adsorbed on a porous acrylic resin","docAbstract":"<p>The capacity factors of 20 aromatic, allphatic, and allcycllc organic solutes with carboxyl, hydroxyl, amine, and methyl functional groups were determined on Amberlite XAD-8, a porous acrylic resin. The logarithm of the capacity factor, <i>k'</i>, correlated inversely with the logarithm of the aqueous molar solubility with significance of less than 0.001. The log <i>k'</i>-log solubility relationship may be used to predict the capacity of any organic solute for XAD-8 using only the solubility of the solute. The prediction is useful as a guide for determining the proper ratio of sample to column size In the preconcentration of organic solutes from water. The inverse relationship of solubility and capacity is due to the unfavorable entropy of solution of organic solutes which affects both solubility and sorption.</p>","language":"English","publisher":"ACS Publications","doi":"10.1021/ac50027a028","usgsCitation":"Thurman, E., Malcolm, R., and Aiken, G., 1978, Prediction of capacity factors for aqueous organic solutes adsorbed on a porous acrylic resin: Analytical Chemistry, v. 50, no. 6, p. 775-779, https://doi.org/10.1021/ac50027a028.","productDescription":"5 p.","startPage":"775","endPage":"779","numberOfPages":"5","costCenters":[],"links":[{"id":222086,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"50","issue":"6","noUsgsAuthors":false,"publicationDate":"2002-05-01","publicationStatus":"PW","scienceBaseUri":"505a81eae4b0c8380cd7b7d1","contributors":{"authors":[{"text":"Thurman, E.M.","contributorId":102864,"corporation":false,"usgs":true,"family":"Thurman","given":"E.M.","affiliations":[],"preferred":false,"id":363879,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Malcolm, Ronald L.","contributorId":46075,"corporation":false,"usgs":true,"family":"Malcolm","given":"Ronald L.","affiliations":[],"preferred":false,"id":866164,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Aiken, G. R. 0000-0001-8454-0984","orcid":"https://orcid.org/0000-0001-8454-0984","contributorId":14452,"corporation":false,"usgs":true,"family":"Aiken","given":"G. R.","affiliations":[],"preferred":false,"id":866165,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":70012598,"text":"70012598 - 1978 - Mars synthetic topographic mapping","interactions":[],"lastModifiedDate":"2025-02-27T19:32:08.863074","indexId":"70012598","displayToPublicDate":"1978-01-01T00:00:00","publicationYear":"1978","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1963,"text":"Icarus","active":true,"publicationSubtype":{"id":10}},"title":"Mars synthetic topographic mapping","docAbstract":"<p><span>Topographic contour maps of Mars are compiled by the synthesis of data acquired from various scientific experiments of the Mariner 9 mission, including S-band radio-occulation, the ultraviolet spectrometer (UVS), the infrared radiometer (IRR), the infrared interferometer spectrometer (IRIS) and television imagery, as well as Earth-based radar information collected at Goldstone, Haystack, and Arecibo Observatories. The entire planet is mapped at scales of 1:25,000,000 and 1:25,000,000 using Mercator, Lambert, and polar stereographic map projections. For the computation of map projections, a biaxial spheroid figure is adopted. The semimajor and semiminor axes are 3393.4 and 3375.7 km, respectively, with a polar flattening of 0.0052. For the computation of elevations, a topographic datum is defined by a gravity field described in terms of spherical harmonics of fourth order and fourth degree combined with a 6.1-mbar occulation pressure surface. This areoid can be approximated by a triaxial ellipsoid with semimajor axes of&nbsp;</span><i>A</i><span>&nbsp;= 3394.6 km and&nbsp;</span><i>B</i><span>&nbsp;= 3393.3 km and a semiminor axis of&nbsp;</span><i>C</i><span>&nbsp;= 3376.3 km. The semimajor axis&nbsp;</span><i>A</i><span>&nbsp;intersects the Martian surface at longitude 105°W. The dynamic flattening of Mars is 0.00525. The contour intercal of the maps is 1 km. For some prominent features where overlapping pictures from Mariner 9 are available, local contour maps at relatively larger scales were also compiled by photogrammetric methods on stereo plotters.</span></p>","language":"English","publisher":"Elsevier","doi":"10.1016/0019-1035(78)90182-3","issn":"00191035","usgsCitation":"Wu, S., 1978, Mars synthetic topographic mapping: Icarus, v. 33, no. 3, p. 417-440, https://doi.org/10.1016/0019-1035(78)90182-3.","productDescription":"24 p.","startPage":"417","endPage":"440","numberOfPages":"24","costCenters":[],"links":[{"id":493276,"rank":2,"type":{"id":41,"text":"Open Access External Repository Page"},"url":"http://hdl.handle.net/10150/289440","text":"External Repository"},{"id":222153,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"33","issue":"3","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"505a5226e4b0c8380cd6c1c2","contributors":{"authors":[{"text":"Wu, S.S.C.","contributorId":10421,"corporation":false,"usgs":true,"family":"Wu","given":"S.S.C.","email":"","affiliations":[],"preferred":false,"id":364016,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":70012448,"text":"70012448 - 1978 - Induction of auroral zone electric currents within the Alaska pipeline","interactions":[],"lastModifiedDate":"2012-03-12T17:19:06","indexId":"70012448","displayToPublicDate":"1978-01-01T00:00:00","publicationYear":"1978","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":3209,"text":"Pure and Applied Geophysics PAGEOPH","active":true,"publicationSubtype":{"id":10}},"title":"Induction of auroral zone electric currents within the Alaska pipeline","docAbstract":"The Alaskar pipeline is a highly conducting anomaly extending 800 miles (1300 km) from about 62?? to 69?? geomagnetic latitude beneath the most active regions of the ionospheric electrojet current. The spectral behavior of the magnetic field from this current was analyzed using data from standard geomagnetic observatories to establish the predictable patterns of temporal and spatial changes for field pulsation periods between 5 min and 4 hr. Such behavior is presented in a series of tables, graphs and formulae. Using 2- and 3-layer models of the conducting earth, the induced electric fields associated with the geomagnetic changes were established. From the direct relationship of the current to the geomagnetic field variation patterns one can infer counterpart temporal and spatial characteristics of the pipeline current. The relationship of the field amplitudes to geomagnetic activity indices, Ap, and the established occurrence of various levels of Ap over several solar cycles were employed to show that about half of the time the induced currents in the pipe would be under 1 A for the maximum response oscillatory periods near 1 hr. Such currents should be of minimal consequence in corrosion effects for even a section of the pipeline unprotected by sacrificial electrodes. Of greater interest was the result that the extreme surges of current should reach over one-hundred amperes in the pipeline during high activity. ?? 1978 Birkha??user Verlag.","largerWorkType":{"id":2,"text":"Article"},"largerWorkTitle":"Pure and Applied Geophysics PAGEOPH","largerWorkSubtype":{"id":10,"text":"Journal Article"},"language":"English","publisherLocation":"Birkha??user-Verlag","doi":"10.1007/BF00874677","issn":"00334553","usgsCitation":"Campbell, W., 1978, Induction of auroral zone electric currents within the Alaska pipeline: Pure and Applied Geophysics PAGEOPH, v. 116, no. 6, p. 1143-1173, https://doi.org/10.1007/BF00874677.","startPage":"1143","endPage":"1173","numberOfPages":"31","costCenters":[],"links":[{"id":222417,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"},{"id":205234,"rank":9999,"type":{"id":10,"text":"Digital Object Identifier"},"url":"https://dx.doi.org/10.1007/BF00874677"}],"volume":"116","issue":"6","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"505a3aafe4b0c8380cd61eaa","contributors":{"authors":[{"text":"Campbell, W.H.","contributorId":30749,"corporation":false,"usgs":true,"family":"Campbell","given":"W.H.","email":"","affiliations":[],"preferred":false,"id":363601,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":70012579,"text":"70012579 - 1978 - Transient-pressure analysis in geothermal steam reservoirs with an immobile vaporizing liquid phase","interactions":[],"lastModifiedDate":"2013-02-24T14:05:47","indexId":"70012579","displayToPublicDate":"1978-01-01T00:00:00","publicationYear":"1978","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1828,"text":"Geothermics","active":true,"publicationSubtype":{"id":10}},"title":"Transient-pressure analysis in geothermal steam reservoirs with an immobile vaporizing liquid phase","docAbstract":"A finite-difference model for the radial horizontal flow of steam through a porous medium is used to evaluate transient-pressure behavior in the presence of an immobile vaporizing or condensing liquid phase. Graphs of pressure drawdown and buildup in terms of dimensionless pressure and time are obtained for a well discharging steam at a constant mass flow rate for a specified time. The assumptions are made that the steam is in local thermal equilibrium with the reservoir rocks, that temperature changes are due only to phase change, and that effects of vapor-pressure lowering are negligible. Computations show that when a vaporizing liquid phase is present the pressure drawdown exhibits behavior similar to that observed in noncondensable gas reservoirs, but delayed in time. A theoretical analysis allows for the computation of this delay and demonstrates that it is independent of flow geometry. The response that occurs upon pressure buildup is markedly different from that in a noncondensable gas system. This result may provide a diagnostic tool for establishing the existence of phase-change phenomena within a reservoir. ?? 1979.","largerWorkType":{"id":2,"text":"Article"},"largerWorkTitle":"Geothermics","largerWorkSubtype":{"id":10,"text":"Journal Article"},"language":"English","publisher":"Elsevier","doi":"10.1016/0375-6505(78)90015-9","issn":"03756505","usgsCitation":"Moench, A., and Atkinson, P., 1978, Transient-pressure analysis in geothermal steam reservoirs with an immobile vaporizing liquid phase: Geothermics, v. 7, no. 2-4, p. 253-264, https://doi.org/10.1016/0375-6505(78)90015-9.","startPage":"253","endPage":"264","numberOfPages":"12","costCenters":[],"links":[{"id":221832,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"},{"id":268142,"type":{"id":10,"text":"Digital Object Identifier"},"url":"https://dx.doi.org/10.1016/0375-6505(78)90015-9"}],"volume":"7","issue":"2-4","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"505bb709e4b08c986b327009","contributors":{"authors":[{"text":"Moench, A.F.","contributorId":91495,"corporation":false,"usgs":true,"family":"Moench","given":"A.F.","email":"","affiliations":[],"preferred":false,"id":363962,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Atkinson, P.G.","contributorId":12978,"corporation":false,"usgs":true,"family":"Atkinson","given":"P.G.","email":"","affiliations":[],"preferred":false,"id":363961,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":70012590,"text":"70012590 - 1978 - Distribution of rutile in metamorphic rocks and implications for placer deposits","interactions":[],"lastModifiedDate":"2012-03-12T17:19:09","indexId":"70012590","displayToPublicDate":"1978-01-01T00:00:00","publicationYear":"1978","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":2746,"text":"Mineralium Deposita","active":true,"publicationSubtype":{"id":10}},"title":"Distribution of rutile in metamorphic rocks and implications for placer deposits","docAbstract":"Pelitic units in the eastern Great Smoky Mountains of the North Carolina Blue Ridge contain rutile grains only in kyanite and higher zones. Adjacent non-pelitic rocks do not contain rutile at kyanite grade but commonly contain sphene. Detrital rutile breaks down at metamorphic grades lower than those at which metamorphic rutile forms. Similarly, pelitic rocks in southeastern Connecticut contain rutile grains above, but not below, the sillimanite isograd. Most non-pelitic rocks there contain rutile only in the hypersthene zone. The slight difference in behavior of rutile in the two terranes is attributed primarily to a slight difference in calcium content of the pelites. In both areas, rutile commonly appears first as inclusions in garnet. Geologic maps showing metamorphic and stratigraphic or compositional information should be useful as prospecting tools for placer deposits. A variety of rocks at granulite facies and pelitic rocks of the upper amphibolite facies contain rutile and these could provide an extensive source for rutile in rutile placer deposits. ?? 1978 Springer-Verlag.","largerWorkType":{"id":2,"text":"Article"},"largerWorkTitle":"Mineralium Deposita","largerWorkSubtype":{"id":10,"text":"Journal Article"},"language":"English","publisherLocation":"Springer-Verlag","doi":"10.1007/BF00206567","issn":"00264598","usgsCitation":"Goldsmith, R., and Force, E.R., 1978, Distribution of rutile in metamorphic rocks and implications for placer deposits: Mineralium Deposita, v. 13, no. 3, p. 329-343, https://doi.org/10.1007/BF00206567.","startPage":"329","endPage":"343","numberOfPages":"15","costCenters":[],"links":[{"id":222026,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"},{"id":205186,"rank":9999,"type":{"id":10,"text":"Digital Object Identifier"},"url":"https://dx.doi.org/10.1007/BF00206567"}],"volume":"13","issue":"3","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"505a02f7e4b0c8380cd502a2","contributors":{"authors":[{"text":"Goldsmith, R.","contributorId":49809,"corporation":false,"usgs":true,"family":"Goldsmith","given":"R.","email":"","affiliations":[],"preferred":false,"id":363991,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Force, E. R.","contributorId":28235,"corporation":false,"usgs":true,"family":"Force","given":"E.","email":"","middleInitial":"R.","affiliations":[],"preferred":false,"id":363990,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":70012444,"text":"70012444 - 1978 - The solubility of the noble gases He, Ne, Ar, Kr, and Xe in water up to the critical point","interactions":[],"lastModifiedDate":"2012-03-12T17:19:07","indexId":"70012444","displayToPublicDate":"1978-01-01T00:00:00","publicationYear":"1978","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":2460,"text":"Journal of Solution Chemistry","active":true,"publicationSubtype":{"id":10}},"title":"The solubility of the noble gases He, Ne, Ar, Kr, and Xe in water up to the critical point","docAbstract":"The solubility of the noble gases Ar, He, Ne, Kr, and Xe in pure water was measured from 298 to 561??K. These data in turn were extrapolated to the critical point of water, thus providing a complete set of Henry's law constants from 274 to 647??K when combined with the existing literature data. Equations describing the behavior of the Henry's law constants over this temperature range are also given. The data do not confirm extrapolations of empirical correlations based on low-temperature solubility data. ?? 1978 Plenum Publishing Corporation.","largerWorkType":{"id":2,"text":"Article"},"largerWorkTitle":"Journal of Solution Chemistry","largerWorkSubtype":{"id":10,"text":"Journal Article"},"language":"English","publisherLocation":"Kluwer Academic Publishers-Plenum Publishers","doi":"10.1007/BF00650811","issn":"00959782","usgsCitation":"Potter, R., and Clynne, M., 1978, The solubility of the noble gases He, Ne, Ar, Kr, and Xe in water up to the critical point: Journal of Solution Chemistry, v. 7, no. 11, p. 837-844, https://doi.org/10.1007/BF00650811.","startPage":"837","endPage":"844","numberOfPages":"8","costCenters":[],"links":[{"id":205226,"rank":9999,"type":{"id":10,"text":"Digital Object Identifier"},"url":"https://dx.doi.org/10.1007/BF00650811"},{"id":222354,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"7","issue":"11","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"505bb045e4b08c986b324d49","contributors":{"authors":[{"text":"Potter, R.W. II","contributorId":16857,"corporation":false,"usgs":true,"family":"Potter","given":"R.W.","suffix":"II","email":"","affiliations":[],"preferred":false,"id":363594,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Clynne, M.A.","contributorId":90722,"corporation":false,"usgs":true,"family":"Clynne","given":"M.A.","affiliations":[],"preferred":false,"id":363595,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":70012446,"text":"70012446 - 1978 - Distinctive sedimentary features of cold-climate eolian deposits, North Park, Colorado","interactions":[],"lastModifiedDate":"2013-02-19T16:20:51","indexId":"70012446","displayToPublicDate":"1978-01-01T00:00:00","publicationYear":"1978","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":2996,"text":"Palaeogeography, Palaeoclimatology, Palaeoecology","printIssn":"0031-0182","active":true,"publicationSubtype":{"id":10}},"title":"Distinctive sedimentary features of cold-climate eolian deposits, North Park, Colorado","docAbstract":"Cold-climate eolianites contain diagnostic sedimentary features that contrast with the sedimentary features of warm-climate eolianites. Distinctive tensional, compressional, and dissipation sedimentary structures related to freezing, thawing and snow melting characterize eolian dune-sand deposits in North Park, Colorado. The North Park dunes have few of the characteristics considered to be diagnostic eolian indicators. A significant difference is the heterogeneous texture and composition of the sand. The migration rate of these active dunes is slow (???1.7 m/year) due to freezing of moisture in the sand or to burial of the sand by snow during half of the year, even though the dunes occur in a unimodal, high-energy wind environment. Bioturbation is common in both active and inactive dunes, although the dunes occur at a high elevation ({reversed tilde} 2500m) in a cold climate (3.0??C mean annual temperature). The distinctive sedimentary features observed in this cold-climate (snow-related) dune field should aid in the interpretation of eolianites and the paleoclimates in which they formed. ?? 1978.","largerWorkType":{"id":2,"text":"Article"},"largerWorkTitle":"Palaeogeography, Palaeoclimatology, Palaeoecology","largerWorkSubtype":{"id":10,"text":"Journal Article"},"language":"English","publisher":"Elsevier","doi":"10.1016/0031-0182(78)90048-2","issn":"00310182","usgsCitation":"Ahlbrandt, T., and Andrews, S., 1978, Distinctive sedimentary features of cold-climate eolian deposits, North Park, Colorado: Palaeogeography, Palaeoclimatology, Palaeoecology, v. 25, no. 4, p. 327-351, https://doi.org/10.1016/0031-0182(78)90048-2.","startPage":"327","endPage":"351","numberOfPages":"25","costCenters":[],"links":[{"id":267790,"type":{"id":10,"text":"Digital Object Identifier"},"url":"https://dx.doi.org/10.1016/0031-0182(78)90048-2"},{"id":222415,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"25","issue":"4","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"505a024de4b0c8380cd4ffb5","contributors":{"authors":[{"text":"Ahlbrandt, Thomas S.","contributorId":58279,"corporation":false,"usgs":true,"family":"Ahlbrandt","given":"Thomas S.","affiliations":[],"preferred":false,"id":363598,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Andrews, S.","contributorId":21282,"corporation":false,"usgs":true,"family":"Andrews","given":"S.","email":"","affiliations":[],"preferred":false,"id":363597,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
]}