{"pageNumber":"5851","pageRowStart":"146250","pageSize":"25","recordCount":184617,"records":[{"id":70012631,"text":"70012631 - 1978 - Minerals produced during cooling and hydrothermal alteration of ash flow tuff from Yellowstone drill hole Y-5","interactions":[],"lastModifiedDate":"2012-03-12T17:19:03","indexId":"70012631","displayToPublicDate":"1978-01-01T00:00:00","publicationYear":"1978","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":2499,"text":"Journal of Volcanology and Geothermal Research","active":true,"publicationSubtype":{"id":10}},"title":"Minerals produced during cooling and hydrothermal alteration of ash flow tuff from Yellowstone drill hole Y-5","docAbstract":"A rhyolitic ash-flow tuff in a hydrothermally active area within the Yellowstone caldera was drilled in 1967, and cores were studied to determine the nature and distribution of primary and secondary mineral phases. The rocks have undergone a complex history of crystallization and hydrothermal alteration since their emplacement 600,000 years ago. During cooling from magmatic temperatures, the glassy groundmass underwent either devitrification to alkali feldspar + ??-cristobalite ?? tridymite or granophyric crystallization to alkali feldspar + quartz. Associated with the zones of granophyric crystallization are prismatic quartz crystals in cavities similar to those termed miarolitic in plutonic rocks. Vapor-phase alkali feldspar, tridymite, magnetite, and sporadic ??-cristobalite were deposited in cavities and in void spaces of pumice fragments. Subsequently, some of the vapor-phase alkali feldspar crystals were replaced by microcrystalline quartz, and the vapor-phase minerals were frosted by a coating of saccharoidal quartz. Hydrothermal minerals occur primarily as linings and fillings of cavities and fractures and as altered mafic phenocrysts. Chalcedony is the dominant mineral related to the present hydrothermal regime and occurs as microcrystalline material mixed with various amounts of hematite and goethite. The chalcedony displays intricate layering and was apparently deposited as opal from silica-rich water. Hematite and goethite also replace both mafic phenocrysts and vapor-phase magnetite. Other conspicuous hydrothermal minerals include montmorillonite, pyrite, mordenite, calcite, and fluorite. Clinoptilolite, erionite, illite, kaolinite, and manganese oxides are sporadic. The hydrothermal minerals show little correlation with temperature, but bladed calcite is restricted to a zone of boiling in the tuff and clearly was deposited when CO2 was lost during boiling. Fractures and breccias filled with chalcedony are common throughout Y-5 and may have been produced by rapid disruption of rock caused by sudden decrease of fluid pressure in fractures, most likely a result of fracturing during resurgent doming in this part of the Yellowstone caldera. The chalcedony probably was deposited as opal or ??-cristobalite from a pre-existing silica floc that moved rapidly into the fractures and breccias immediately after the sudden pressure drop. ?? 1978.","largerWorkType":{"id":2,"text":"Article"},"largerWorkTitle":"Journal of Volcanology and Geothermal Research","largerWorkSubtype":{"id":10,"text":"Journal Article"},"language":"English","issn":"03770273","usgsCitation":"Keith, T.E., and Muffler, L., 1978, Minerals produced during cooling and hydrothermal alteration of ash flow tuff from Yellowstone drill hole Y-5: Journal of Volcanology and Geothermal Research, v. 3, no. 3-4, p. 373-402.","startPage":"373","endPage":"402","numberOfPages":"30","costCenters":[],"links":[{"id":222668,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"3","issue":"3-4","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"505a5ae7e4b0c8380cd6f1df","contributors":{"authors":[{"text":"Keith, T. E. C.","contributorId":11681,"corporation":false,"usgs":true,"family":"Keith","given":"T.","email":"","middleInitial":"E. C.","affiliations":[],"preferred":false,"id":364098,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Muffler, L.J.P.","contributorId":63383,"corporation":false,"usgs":true,"family":"Muffler","given":"L.J.P.","affiliations":[],"preferred":false,"id":364099,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":70012436,"text":"70012436 - 1978 - Formation of lunar basin rings","interactions":[],"lastModifiedDate":"2025-02-27T19:30:39.821293","indexId":"70012436","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":"Formation of lunar basin rings","docAbstract":"

The origin of the multiple concentric rings that characterize lunar impact basins, and the probable depth and diameter of the transient crater have been widely debated. As an alternative to prevailing “megaterrace” hypotheses, we propose that the outer scarps or mountain rings that delineate the topographic rims of basins—the Cordilleran at Orientale, the Apennine at Imbrium, and the Altai at Nectaris—define the transient cavities, enlarged relatively little by slumping, and thus are analogous to the rim crests of craters like Copernicus; inner rings are uplifted rims of craters nested within the transient cavity. The magnitude of slumping that occurs on all scarps is insufficient to produce major inner rings from the outer. These conclusions are based largely on the observed gradational sequence in lunar central uplifts:. from simple peaks through somewhat annular clusters of peaks, peak and ring combinations and double ring basins, culminating in multiring structures that may also include peaks. In contrast, belts of slump terraces are not gradational with inner rings. Terrestrial analogs suggest two possible mechanisms for producing rings. In some cases, peaks may expand into rings as material is ejected from their cores, as apparently occurred at Gosses Bluff, Australia. A second process, differential excavation of lithologically diverse layers, has produced nested experimental craters and is, we suspect, instrumental in the formation of terrestrial ringed impact craters. Peak expansion could produce double-ring structures in homogeneous materials, but differential excavation is probably required to produce multiring and peak-in-ring configurations in large lunar impact structures. Our interpretation of the representative lunar multiring basin Orientale is consistent with formation of three rings in three layers detected seismically in part of the Moon—the Cordillera (basin-bounding) ring in the upper crust, the composite Montes Rook ring in the underlying, more coherent “heald” crust, and an innermost, 320-km ring at the crust-mantle interface. Depth-diameter ratios of 110to115\">110 to 115 are consistent with this interpretation and suggest that volumes of transient cavities and hence of basin ejecta may be considerably greater than commonly assumed.

","language":"English","publisher":"Elsevier","doi":"10.1016/0019-1035(78)90169-0","issn":"00191035","usgsCitation":"Hodges, C.A., and Wilhelms, D., 1978, Formation of lunar basin rings: Icarus, v. 34, no. 2, p. 294-323, https://doi.org/10.1016/0019-1035(78)90169-0.","productDescription":"30 p.","startPage":"294","endPage":"323","numberOfPages":"30","costCenters":[],"links":[{"id":222254,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"34","issue":"2","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"505a1352e4b0c8380cd545f7","contributors":{"authors":[{"text":"Hodges, C. A.","contributorId":104495,"corporation":false,"usgs":true,"family":"Hodges","given":"C.","email":"","middleInitial":"A.","affiliations":[],"preferred":false,"id":363581,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Wilhelms, D.E.","contributorId":82302,"corporation":false,"usgs":true,"family":"Wilhelms","given":"D.E.","email":"","affiliations":[],"preferred":false,"id":363580,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":46273,"text":"ofr78478 - 1978 - Leasable mineral and waterpower land classification map of the Shiprock quadrangle, New Mexico, Arizona, Colorado, and Utah","interactions":[],"lastModifiedDate":"2023-04-18T20:43:13.693648","indexId":"ofr78478","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":"78-478","title":"Leasable mineral and waterpower land classification map of the Shiprock quadrangle, New Mexico, Arizona, Colorado, and Utah","docAbstract":"

No abstract available.

","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Reston, VA","doi":"10.3133/ofr78478","usgsCitation":"DeCicco, D.A., Patterson, E., and Lutz, G., 1978, Leasable mineral and waterpower land classification map of the Shiprock quadrangle, New Mexico, Arizona, Colorado, and Utah: U.S. Geological Survey Open-File Report 78-478, 1 Plate: 38.40 x 23.67 inches, https://doi.org/10.3133/ofr78478.","productDescription":"1 Plate: 38.40 x 23.67 inches","costCenters":[],"links":[{"id":172244,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":415953,"rank":3,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_12955.htm","linkFileType":{"id":5,"text":"html"}},{"id":254787,"rank":2,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1978/0478/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}}],"country":"United States","state":"Arizona, Colorado, New Mexico, Utah","otherGeospatial":"Ship Rock quadrangle","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"coordinates\": [\n [\n [\n -110,\n 37\n ],\n [\n -110,\n 36\n ],\n [\n -108,\n 36\n ],\n [\n -108,\n 37\n ],\n [\n -110,\n 37\n ]\n ]\n ],\n \"type\": \"Polygon\"\n }\n }\n ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b1ae4b07f02db6a8659","contributors":{"authors":[{"text":"DeCicco, Donald A.","contributorId":50173,"corporation":false,"usgs":true,"family":"DeCicco","given":"Donald","email":"","middleInitial":"A.","affiliations":[],"preferred":false,"id":232989,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Patterson, E. D.","contributorId":56278,"corporation":false,"usgs":true,"family":"Patterson","given":"E. D.","affiliations":[],"preferred":false,"id":232990,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Lutz, Gale A.","contributorId":32507,"corporation":false,"usgs":true,"family":"Lutz","given":"Gale A.","affiliations":[],"preferred":false,"id":232988,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}} ,{"id":46208,"text":"ofr7873G - 1978 - Map showing gold determined by atomic absorption and spectrographically determined silver in stream sediments, Ketchikan and Prince Rupert quadrangles, Alaska","interactions":[],"lastModifiedDate":"2023-03-29T21:00:57.895701","indexId":"ofr7873G","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":"78-73","chapter":"G","title":"Map showing gold determined by atomic absorption and spectrographically determined silver in stream sediments, Ketchikan and Prince Rupert quadrangles, Alaska","docAbstract":"

No abstract available.

","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr7873G","usgsCitation":"Koch, R.D., Elliott, R.L., and Diggles, M.J., 1978, Map showing gold determined by atomic absorption and spectrographically determined silver in stream sediments, Ketchikan and Prince Rupert quadrangles, Alaska: U.S. Geological Survey Open-File Report 78-73, 1 Plate: 35.96 x 35.31 inches, https://doi.org/10.3133/ofr7873G.","productDescription":"1 Plate: 35.96 x 35.31 inches","costCenters":[],"links":[{"id":171900,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":414926,"rank":3,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_14858.htm","linkFileType":{"id":5,"text":"html"}},{"id":83174,"rank":2,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1978/0073g/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}}],"scale":"250000","country":"United States","state":"Alaska","otherGeospatial":"Ketchikan and Prince Rupert quadrangles","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"coordinates\": [\n [\n [\n -132,\n 56\n ],\n [\n -132,\n 54.5\n ],\n [\n -130,\n 54.5\n ],\n [\n -130,\n 56\n ],\n [\n -132,\n 56\n ]\n ]\n ],\n \"type\": \"Polygon\"\n }\n }\n ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b15e4b07f02db6a4bd7","contributors":{"authors":[{"text":"Koch, Richard D. rkoch@usgs.gov","contributorId":4413,"corporation":false,"usgs":true,"family":"Koch","given":"Richard","email":"rkoch@usgs.gov","middleInitial":"D.","affiliations":[],"preferred":true,"id":232836,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Elliott, Raymond L.","contributorId":82667,"corporation":false,"usgs":true,"family":"Elliott","given":"Raymond","email":"","middleInitial":"L.","affiliations":[],"preferred":false,"id":232837,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Diggles, M. J.","contributorId":102853,"corporation":false,"usgs":true,"family":"Diggles","given":"M.","email":"","middleInitial":"J.","affiliations":[],"preferred":false,"id":232838,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}} ,{"id":70012438,"text":"70012438 - 1978 - Applications of the VLF induction method for studying some volcanic processes of Kilauea volcano, Hawaii","interactions":[],"lastModifiedDate":"2012-03-12T17:19:09","indexId":"70012438","displayToPublicDate":"1978-01-01T00:00:00","publicationYear":"1978","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":2499,"text":"Journal of Volcanology and Geothermal Research","active":true,"publicationSubtype":{"id":10}},"title":"Applications of the VLF induction method for studying some volcanic processes of Kilauea volcano, Hawaii","docAbstract":"The very low-frequency (VLF) induction method has found exceptional utility in studying various volcanic processes of Kilauea volcano, Hawaii because: (1) significant anomalies result exclusively from ionically conductive magma or still-hot intrusions (> 800??C) and the attendant electrolytically conductive hot groundwater; (2) basalt flows forming the bulk of Kilauea have very high resistivities at shallow depths that result in low geologic noise levels and relatively deep depths of investigation (???100 m); and (3) the azimuths to two of the usable transmitters (NLK and NPM) are aligned favorably with most of the principal geologic features. Measurements of the tilt angle and ellipticity of the polarization ellipse of the magnetic field, using a simple, hand-held receiver, have been used to: (1) delineate the lateral extent of shallow, partially solidified lava lakes, active lava tubes, and recent intrusive dikes; (2) obtain an indication of the attitude of some recent dikes; (3) show that many eruptive fissures cool faster than their intrusive counterparts; (4) show that some fumarolic areas are underlain by shallow, highly altered, and conductive zones; and (5) provide control information for interpreting data obtained with other electrical techniques. Complementary measurements of scalar apparent resistivity and surface impedance phase, using a new attachment for the VLF receiver, have substantially increased the utility of VLF studies in Kilauea. They provide better lateral resolution of conductors and reduce the ambiguity in interpretation. Notwithstanding recent advances in theoretical modeling techniques, the excellent quality of some of the data warrants extension of interpretive techniques, particularly for quantitatively characterizing the configuration and conductivity of small-dimension bodies. These VLF induction methods should have wide application to studies of active volcanic regions in other parts of the world and could provide some insights into the workings of larger-scaled geothermal systems. ?? 1978.","largerWorkType":{"id":2,"text":"Article"},"largerWorkTitle":"Journal of Volcanology and Geothermal Research","largerWorkSubtype":{"id":10,"text":"Journal Article"},"language":"English","issn":"03770273","usgsCitation":"Zablocki, C., 1978, Applications of the VLF induction method for studying some volcanic processes of Kilauea volcano, Hawaii: Journal of Volcanology and Geothermal Research, v. 3, no. 1-2, p. 155-195.","startPage":"155","endPage":"195","numberOfPages":"41","costCenters":[],"links":[{"id":222305,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"3","issue":"1-2","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"5059eccbe4b0c8380cd494c4","contributors":{"authors":[{"text":"Zablocki, C.J.","contributorId":52178,"corporation":false,"usgs":true,"family":"Zablocki","given":"C.J.","affiliations":[],"preferred":false,"id":363584,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":70012623,"text":"70012623 - 1978 - Radon emanation on San Andreas Fault","interactions":[],"lastModifiedDate":"2012-03-12T17:19:05","indexId":"70012623","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":"Radon emanation on San Andreas Fault","docAbstract":"Subsurface radon emanation monitored in shallow dry holes along an active segment of the San Andreas fault in central California shows spatially coherent large temporal variations that seem to be correlated with local seismicity. ??1978 Nature Publishing Group.","largerWorkType":{"id":2,"text":"Article"},"largerWorkTitle":"Nature","largerWorkSubtype":{"id":10,"text":"Journal Article"},"language":"English","doi":"10.1038/271516a0","issn":"00280836","usgsCitation":"King, C., 1978, Radon emanation on San Andreas Fault: Nature, v. 271, no. 5645, p. 516-519, https://doi.org/10.1038/271516a0.","startPage":"516","endPage":"519","numberOfPages":"4","costCenters":[],"links":[{"id":205257,"rank":9999,"type":{"id":10,"text":"Digital Object Identifier"},"url":"https://dx.doi.org/10.1038/271516a0"},{"id":222545,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"271","issue":"5645","noUsgsAuthors":false,"publicationDate":"1978-02-01","publicationStatus":"PW","scienceBaseUri":"505a9435e4b0c8380cd8127d","contributors":{"authors":[{"text":"King, C.-Y.","contributorId":81225,"corporation":false,"usgs":true,"family":"King","given":"C.-Y.","affiliations":[],"preferred":false,"id":364087,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":46122,"text":"ofr78475 - 1978 - Leasable mineral and waterpower land classification map of the Albuquerque quadrangle, New Mexico","interactions":[],"lastModifiedDate":"2023-04-18T21:02:56.884385","indexId":"ofr78475","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":"78-475","title":"Leasable mineral and waterpower land classification map of the Albuquerque quadrangle, New Mexico","docAbstract":"

No abstract available.

","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr78475","usgsCitation":"DeCicco, D.A., Patterson, E., and Lutz, G., 1978, Leasable mineral and waterpower land classification map of the Albuquerque quadrangle, New Mexico: U.S. Geological Survey Open-File Report 78-475, 1 Plate: 39.15 x 23.87 inches, https://doi.org/10.3133/ofr78475.","productDescription":"1 Plate: 39.15 x 23.87 inches","costCenters":[],"links":[{"id":162601,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":83082,"rank":2,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1978/0475/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":415955,"rank":3,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_12956.htm","linkFileType":{"id":5,"text":"html"}}],"country":"United States","state":"New Mexico","otherGeospatial":"Albuquerque quadrangle","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"coordinates\": [\n [\n [\n -106,\n 36\n ],\n [\n -108,\n 36\n ],\n [\n -108,\n 35\n ],\n [\n -106,\n 35\n ],\n [\n -106,\n 36\n ]\n ]\n ],\n \"type\": \"Polygon\"\n }\n }\n ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b1ae4b07f02db6a8809","contributors":{"authors":[{"text":"DeCicco, Donald A.","contributorId":50173,"corporation":false,"usgs":true,"family":"DeCicco","given":"Donald","email":"","middleInitial":"A.","affiliations":[],"preferred":false,"id":232658,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Patterson, E. D.","contributorId":56278,"corporation":false,"usgs":true,"family":"Patterson","given":"E. D.","affiliations":[],"preferred":false,"id":232659,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Lutz, Gale A.","contributorId":32507,"corporation":false,"usgs":true,"family":"Lutz","given":"Gale A.","affiliations":[],"preferred":false,"id":232657,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}} ,{"id":46066,"text":"ofr781056 - 1978 - Landslides and related features, Ohio, West Virginia and Pennsylvania [Clarksburg quadrangle]","interactions":[],"lastModifiedDate":"2023-11-22T20:34:45.486903","indexId":"ofr781056","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":"78-1056","title":"Landslides and related features, Ohio, West Virginia and Pennsylvania [Clarksburg quadrangle]","docAbstract":"

No abstract available.

","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr781056","usgsCitation":"Hackman, R., and Thomas, R.E., 1978, Landslides and related features, Ohio, West Virginia and Pennsylvania [Clarksburg quadrangle]: U.S. Geological Survey Open-File Report 78-1056, 127 Plates: 21.37 x 39.88 inches or smaller, https://doi.org/10.3133/ofr781056.","productDescription":"127 Plates: 21.37 x 39.88 inches or smaller","costCenters":[],"links":[{"id":370924,"rank":127,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1978/1056/plate-h-15.pdf","text":"Plate H-15","linkFileType":{"id":1,"text":"pdf"}},{"id":370923,"rank":126,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1978/1056/plate-h-14.pdf","text":"Plate H-14","linkFileType":{"id":1,"text":"pdf"}},{"id":370922,"rank":125,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1978/1056/plate-h-13.pdf","text":"Plate 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E-14","linkFileType":{"id":1,"text":"pdf"}},{"id":285524,"rank":68,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1978/1056/plate-e-3.pdf","text":"Plate E-3","linkFileType":{"id":1,"text":"pdf"}},{"id":285517,"rank":61,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1978/1056/plate-d-12.pdf","text":"Plate D-12","linkFileType":{"id":1,"text":"pdf"}},{"id":285481,"rank":32,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1978/1056/plate-b-15.pdf","text":"Plate B-15","linkFileType":{"id":1,"text":"pdf"}},{"id":285473,"rank":25,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1978/1056/plate-b-8.pdf","text":"Plate B-8","linkFileType":{"id":1,"text":"pdf"}}],"scale":"24000","datum":"Mean Sea Level","country":"United States","state":"Ohio, Pennsylvania, West Virginia","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"type\": \"Polygon\",\n \"coordinates\": [\n [\n [\n -82,\n 39\n ],\n [\n -80,\n 39\n ],\n [\n -80,\n 40\n ],\n [\n -82,\n 40\n ],\n [\n -82,\n 39\n ]\n ]\n ]\n }\n }\n ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b1de4b07f02db6a9d75","contributors":{"authors":[{"text":"Hackman, Robert J.","contributorId":30999,"corporation":false,"usgs":true,"family":"Hackman","given":"Robert J.","affiliations":[],"preferred":false,"id":232553,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Thomas, Roger E.","contributorId":87899,"corporation":false,"usgs":true,"family":"Thomas","given":"Roger","email":"","middleInitial":"E.","affiliations":[{"id":595,"text":"U.S. Geological Survey","active":false,"usgs":true}],"preferred":false,"id":232554,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":46296,"text":"ofr7873D - 1978 - Map showing lead determined by atomic absorption in stream sediments, Ketchikan and Prince Rupert quadrangles, Alaska","interactions":[],"lastModifiedDate":"2023-03-29T21:03:33.835392","indexId":"ofr7873D","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":"78-73","chapter":"D","title":"Map showing lead determined by atomic absorption in stream sediments, Ketchikan and Prince Rupert quadrangles, Alaska","docAbstract":"

No abstract available.

","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr7873D","usgsCitation":"Koch, R.D., Elliott, R.L., and Diggles, M.J., 1978, Map showing lead determined by atomic absorption in stream sediments, Ketchikan and Prince Rupert quadrangles, Alaska: U.S. Geological Survey Open-File Report 78-73, 1 Plate: 36.72 x 34.05 inches, https://doi.org/10.3133/ofr7873D.","productDescription":"1 Plate: 36.72 x 34.05 inches","costCenters":[],"links":[{"id":172979,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":83295,"rank":2,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1978/0073d/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":414927,"rank":3,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_14855.htm","linkFileType":{"id":5,"text":"html"}}],"scale":"250000","country":"United States","state":"Alaska","otherGeospatial":"Ketchikan and Prince Rupert quadrangles","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"coordinates\": [\n [\n [\n -132,\n 56\n ],\n [\n -132,\n 54.5\n ],\n [\n -130,\n 54.5\n ],\n [\n -130,\n 56\n ],\n [\n -132,\n 56\n ]\n ]\n ],\n \"type\": \"Polygon\"\n }\n }\n ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b15e4b07f02db6a4c36","contributors":{"authors":[{"text":"Koch, Richard D. rkoch@usgs.gov","contributorId":4413,"corporation":false,"usgs":true,"family":"Koch","given":"Richard","email":"rkoch@usgs.gov","middleInitial":"D.","affiliations":[],"preferred":true,"id":233029,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Elliott, Raymond L.","contributorId":82667,"corporation":false,"usgs":true,"family":"Elliott","given":"Raymond","email":"","middleInitial":"L.","affiliations":[],"preferred":false,"id":233030,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Diggles, M. J.","contributorId":102853,"corporation":false,"usgs":true,"family":"Diggles","given":"M.","email":"","middleInitial":"J.","affiliations":[],"preferred":false,"id":233031,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}} ,{"id":9224,"text":"ofr78305 - 1978 - The marine geology of the eastern Santa Barbara Channel, with particular emphasis on the ground water basins offshore from the Oxnard Plain, Southern California","interactions":[],"lastModifiedDate":"2024-10-25T14:41:51.621139","indexId":"ofr78305","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":"78-305","title":"The marine geology of the eastern Santa Barbara Channel, with particular emphasis on the ground water basins offshore from the Oxnard Plain, Southern California","docAbstract":"

Marine geophysical investigations provide new data concerning the stratigraphy, tectonic and sedimentary history, and the ground water geology of the southeastern Santa Barbara Channel region. The offshore stratigraphy identified in seismic reflection profiles includes a succession of Neogene to Quaternary strata. The middle Miocene Conejo volcanics form an acoustical basement and the overlying late Cenozoic sedimentary rocks attain a thickness greater than 2,500 m. These sedimentary deposits fill a structurally controlled, physiographic and depositional depression called the Ventura Basin.

Structure consists generally of a gently folded, east-trending Tertiary synclinorium bordered on the north by a regional thrust fault and on the south by a steep asymmetrical anticlinal ridge. Most structures show evidence of north-south compression that occurred during early Pleistocene time. Three well-defined unconformities represent widespread erosion in late Miocene, early to middle Pleistocene, and late Pleistocene time. The boundaries of Miocene, Pliocene, and lower Pleistocene strata continue uninterrupted eastward along the southern part of Santa Barbara basin to Hueneme Canyon, where they turn northeast and can be traced to the coast near Port Hueneme. These limits probably represent the south edge of the Santa Barbara basin during Pliocene and Pleistocene time.

Fresh water-bearing materials of the Oxnard plain are unconsolidated Quaternary sediment laid down on more consolidated Tertiary rocks. Offshore, the total fresh water-bearing materials distinguished in the seismic reflection profiles attain a thickness of about 356 m and have an areal extent of over 760 km2. Strata that contain the offshore continuation of the five major on-land aquifers (Grimes Canyon, Fox Canyon, Hueneme, Mugu, and Oxnard aquifers) are identified in the seismic reflection profiles. These strata make up the two offshore ground-water basins, the Mound and Oxnard plain ground-water basins, which are separated by the east-west trending Oak Ridge fault.

Possible entrance areas for salt water intrusion into fresh water aquifers are found along the walls of the submarine canyons and along the northern slopes of Santa Barbara and Santa Monica basins. Hueneme and Mugu aquifers are probably exposed locally in all five submarine canyons of the Oxnard offshore area and may also crop out along the upper northern slope of Santa Monica basin. In all of these areas, salt water readily intrudes the aquifers. A salinity-temperature-depth study made in April, 1971, does not indicate any great dilution of surface ocean water by fresh water that could be 'leaking' from the exposed aquifers along the walls of Hueneme Canyon and the landward slope of Santa Barbara Channel.

Earthquakes in the vicinity of the Oxnard plain suggest that the region is seismically active. Epicenters are widely dispersed over the region. No distinct trend or alignment of earthquake epicenters occurs near the trace of any of the faults, although many epicenters are scattered around the Oak Ridge zone of deformation in the northern part of the region. The largest magnitude earthquake recorded in the area was a magnitude 5.7 that occurred on February 21, 1973, offshore of Point Mugu, south of the Oxnard plain.

","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr78305","usgsCitation":"Greene, H., Wolf, S.C., and Blom, K.G., 1978, The marine geology of the eastern Santa Barbara Channel, with particular emphasis on the ground water basins offshore from the Oxnard Plain, Southern California: U.S. Geological Survey Open-File Report 78-305, Report: viii, 104 p.; 13 Plates: 35.60 x 26.85 inches or smaller, https://doi.org/10.3133/ofr78305.","productDescription":"Report: viii, 104 p.; 13 Plates: 35.60 x 26.85 inches or smaller","costCenters":[],"links":[{"id":416018,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1978/0305/report-thumb.jpg"},{"id":416017,"rank":2,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_14675.htm","linkFileType":{"id":5,"text":"html"}},{"id":463159,"rank":3,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1978/0305/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":463160,"rank":4,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1978/0305/plate-01.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":463161,"rank":5,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1978/0305/plate-02.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":463162,"rank":6,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1978/0305/plate-03.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":463163,"rank":7,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1978/0305/plate-04.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":463164,"rank":8,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1978/0305/plate-05.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":463165,"rank":9,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1978/0305/plate-06.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":463166,"rank":10,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1978/0305/plate-07.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":463167,"rank":11,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1978/0305/plate-08.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":463168,"rank":12,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1978/0305/plate-09.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":463169,"rank":13,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1978/0305/plate-10.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":463170,"rank":14,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1978/0305/plate-11.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":463171,"rank":15,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1978/0305/plate-12.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":463172,"rank":16,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1978/0305/plate-13.pdf","linkFileType":{"id":1,"text":"pdf"}}],"country":"United States","state":"California","otherGeospatial":"Santa Barbara Channel","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"coordinates\": [\n [\n [\n -119,\n 34.333\n ],\n [\n -119.533,\n 34.333\n ],\n [\n -119.533,\n 33.917\n ],\n [\n -119,\n 33.917\n ],\n [\n -119,\n 34.333\n ]\n ]\n ],\n \"type\": \"Polygon\"\n }\n }\n ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a81e4b07f02db64a308","contributors":{"authors":[{"text":"Greene, H. Gary","contributorId":78669,"corporation":false,"usgs":true,"family":"Greene","given":"H. Gary","affiliations":[],"preferred":false,"id":510701,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Wolf, Stephen C.","contributorId":38148,"corporation":false,"usgs":true,"family":"Wolf","given":"Stephen","email":"","middleInitial":"C.","affiliations":[],"preferred":false,"id":510699,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Blom, Ken G.","contributorId":44154,"corporation":false,"usgs":true,"family":"Blom","given":"Ken","email":"","middleInitial":"G.","affiliations":[],"preferred":false,"id":510700,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}} ,{"id":70012639,"text":"70012639 - 1978 - Correction of ground-water chemistry and carbon isotopic composition for effects of CO2 outgassing","interactions":[],"lastModifiedDate":"2024-03-11T16:57:53.226526","indexId":"70012639","displayToPublicDate":"1978-01-01T00:00:00","publicationYear":"1978","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}},"displayTitle":"Correction of ground-water chemistry and carbon isotopic composition for effects of CO2 outgassing","title":"Correction of ground-water chemistry and carbon isotopic composition for effects of CO2 outgassing","docAbstract":"

Direct Pco2\">Pco2  measurements on water samples from several CO2-charged warm springs are significantly higher than Pco2\">Pco2 values calculated from field pH and alkalinity (and other constituents). In addition, calcite saturation indices calculated from field pH and solution composition indicated supersaturation in samples which, on the basis of hydrogeologic concepts, should be near saturation or undersaturated. We attribute these discrepancies to uncertainties in field pH, resulting from CO2 outgassing during pH measurement. Because samples for direct Pco2\">Pco2  measurement can be taken with minimal disturbance to the water chemistry, we have used the measured Pco2\">Pco2  to back calculate an estimate of the field pH and the carbon isotopic composition of the water before outgassing. By reconstructing water chemistry in this way, we find generally consistent grouping of δ13C\">δ13C, pH, and degree of calcite saturation in samples taken from the same source at different times, an observation which we expect based on our understanding of the hydrogeology and geochemistry of the ground-water systems. This suggests that for very careful geochemical work, particularly on ground-waters much above ambient temperature, Pco2\">Pco2 measurements may provide more information on the system and a better estimate of its state of saturation with respect to carbonate minerals than can field measurements of pH.

","language":"English","publisher":"Elsevier","doi":"10.1016/0016-7037(78)90235-1","issn":"00167037","usgsCitation":"Pearson, F.J., Fisher, D., and Plummer, N., 1978, Correction of ground-water chemistry and carbon isotopic composition for effects of CO2 outgassing: Geochimica et Cosmochimica Acta, v. 42, no. 12, p. 1799-1807, https://doi.org/10.1016/0016-7037(78)90235-1.","productDescription":"9 p.","startPage":"1799","endPage":"1807","numberOfPages":"9","costCenters":[],"links":[{"id":221837,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"42","issue":"12","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"5059fc1fe4b0c8380cd4e128","contributors":{"authors":[{"text":"Pearson, F. J. Jr.","contributorId":7696,"corporation":false,"usgs":true,"family":"Pearson","given":"F.","suffix":"Jr.","email":"","middleInitial":"J.","affiliations":[],"preferred":false,"id":364116,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Fisher, D.W.","contributorId":77519,"corporation":false,"usgs":true,"family":"Fisher","given":"D.W.","email":"","affiliations":[],"preferred":false,"id":364117,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Plummer, Niel 0000-0002-4020-1013 nplummer@usgs.gov","orcid":"https://orcid.org/0000-0002-4020-1013","contributorId":190100,"corporation":false,"usgs":true,"family":"Plummer","given":"Niel","email":"nplummer@usgs.gov","affiliations":[{"id":436,"text":"National Research Program - Eastern Branch","active":true,"usgs":true}],"preferred":true,"id":364118,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}} ,{"id":9541,"text":"ofr79668 - 1978 - The relationship of morphology, structure, and lithology to the emplacement of the Hot Creek rhyolite flow, Long Valley, California","interactions":[],"lastModifiedDate":"2023-08-31T18:28:21.270467","indexId":"ofr79668","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":"79-668","title":"The relationship of morphology, structure, and lithology to the emplacement of the Hot Creek rhyolite flow, Long Valley, California","docAbstract":"

No abstract available.

","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr79668","usgsCitation":"Holecek, T.J., 1978, The relationship of morphology, structure, and lithology to the emplacement of the Hot Creek rhyolite flow, Long Valley, California: U.S. Geological Survey Open-File Report 79-668, Report: 50 p.; 2 Plates: 33.30 x 16.86 inches and 33.48 x 16.95 inches, https://doi.org/10.3133/ofr79668.","productDescription":"Report: 50 p.; 2 Plates: 33.30 x 16.86 inches and 33.48 x 16.95 inches","costCenters":[],"links":[{"id":420374,"rank":5,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_75014.htm","linkFileType":{"id":5,"text":"html"}},{"id":37261,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1979/0668/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":37260,"rank":4,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1979/0668/plate-2.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":37259,"rank":3,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1979/0668/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":142832,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1979/0668/report-thumb.jpg"}],"country":"United States","state":"California","otherGeospatial":"Long Valley","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"coordinates\": [\n [\n [\n -119.05,\n 37.75\n ],\n [\n -119.05,\n 37.5833\n ],\n [\n -118.7083,\n 37.5833\n ],\n [\n -118.7083,\n 37.75\n ],\n [\n -119.05,\n 37.75\n ]\n ]\n ],\n \"type\": \"Polygon\"\n }\n }\n ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a6fe4b07f02db640ef4","contributors":{"authors":[{"text":"Holecek, Thomas J.","contributorId":99558,"corporation":false,"usgs":true,"family":"Holecek","given":"Thomas","email":"","middleInitial":"J.","affiliations":[],"preferred":false,"id":159861,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":70012767,"text":"70012767 - 1978 - Mössbauer spectroscopic investigation of iron species in coal","interactions":[],"lastModifiedDate":"2015-06-15T10:23:55","indexId":"70012767","displayToPublicDate":"1978-01-01T00:00:00","publicationYear":"1978","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1709,"text":"Fuel","active":true,"publicationSubtype":{"id":10}},"title":"Mössbauer spectroscopic investigation of iron species in coal","docAbstract":"

A series of Herrin No. 6 coal and three coal-derived samples have been examined by Mo??ssbauer spectroscopy. It is established that Mo??ssbauer spectroscopy can be used to identify multiple iron species in a whole coal or an autoclaved char sample without the need to concentrate the minerals to enhance resolution. Our results indicate that there may be an association between the pyrite in raw coal and the coal matrix. This association appears to be broken down when the coal is heated to temperatures as low as 175 ??C. It is also apparent that the iron sulphide present in the whole coal is converted to pyrite at these low temperatures. For our samples, the total quantity of iron species in different coal lithotypes is about the same, but they differ in their distributions. The fusain has the least amount of Fe2+ species when compared to the vitrain or whole-coal sample used. At least two types of nonstoichiometric pyrrhotite are produced in the heat-treated samples. One of these pyrrhotites is unstable and contains dissolved sulphur which is apparently liberated as the temperature is increased. ?? 1978.

","language":"English","publisher":"Elsevier","doi":"10.1016/0016-2361(78)90089-3","issn":"00162361","usgsCitation":"Smith, G.V., Liu, J., and Saporoschenko, M., 1978, Mössbauer spectroscopic investigation of iron species in coal: Fuel, v. 57, no. 1, p. 41-45, https://doi.org/10.1016/0016-2361(78)90089-3.","productDescription":"5 p.","startPage":"41","endPage":"45","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[],"links":[{"id":221847,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"57","issue":"1","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"505a5b8de4b0c8380cd6f632","contributors":{"authors":[{"text":"Smith, Gerard V.","contributorId":93629,"corporation":false,"usgs":true,"family":"Smith","given":"Gerard","email":"","middleInitial":"V.","affiliations":[],"preferred":false,"id":364471,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Liu, Juei-Ho","contributorId":62745,"corporation":false,"usgs":true,"family":"Liu","given":"Juei-Ho","email":"","affiliations":[],"preferred":false,"id":364470,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Saporoschenko, Mykola","contributorId":31905,"corporation":false,"usgs":true,"family":"Saporoschenko","given":"Mykola","email":"","affiliations":[],"preferred":false,"id":364468,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}} ,{"id":9197,"text":"ofr78426 - 1978 - Tectonic map of the Puget Sound region, Washington, showing locations of faults, principal folds and large scale Quaternary deformation","interactions":[],"lastModifiedDate":"2023-04-18T21:22:57.606618","indexId":"ofr78426","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":"78-426","title":"Tectonic map of the Puget Sound region, Washington, showing locations of faults, principal folds and large scale Quaternary deformation","docAbstract":"

No abstract available.

","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr78426","usgsCitation":"Gower, H.D., 1978, Tectonic map of the Puget Sound region, Washington, showing locations of faults, principal folds and large scale Quaternary deformation: U.S. Geological Survey Open-File Report 78-426, Repott: 21 p.; 1 Plate: 30.84 x 50.51 inches, https://doi.org/10.3133/ofr78426.","productDescription":"Repott: 21 p.; 1 Plate: 30.84 x 50.51 inches","costCenters":[],"links":[{"id":36807,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1978/0426/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":36806,"rank":3,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1978/0426/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":140930,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1978/0426/report-thumb.jpg"},{"id":415969,"rank":4,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_14719.htm","linkFileType":{"id":5,"text":"html"}}],"country":"United States","state":"Washington","otherGeospatial":"Puget Sound region","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"coordinates\": [\n [\n [\n -121,\n 49\n ],\n [\n -123.5,\n 49\n ],\n [\n -123.5,\n 46.396\n ],\n [\n -121,\n 46.396\n ],\n [\n -121,\n 49\n ]\n ]\n ],\n \"type\": \"Polygon\"\n }\n }\n ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4adae4b07f02db685909","contributors":{"authors":[{"text":"Gower, Howard Dale","contributorId":99139,"corporation":false,"usgs":true,"family":"Gower","given":"Howard","email":"","middleInitial":"Dale","affiliations":[],"preferred":false,"id":159267,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":70012548,"text":"70012548 - 1978 - K-Ar age of the late Pleistocene eruption of Toba, north Sumatra","interactions":[],"lastModifiedDate":"2012-03-12T17:19:07","indexId":"70012548","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":"K-Ar age of the late Pleistocene eruption of Toba, north Sumatra","docAbstract":"The late Pleistocene eruption of Toba is the largest magnitude explosive eruption documented from the Quaternary. K-Ar dating of the uppermost unit of the Toba Tuff gives an age of [~amp]sim; 75,000 yr. A chemically and petrographically equivalent ash layer in deep-sea cores helps calibrate the Stage 4-5 boundary of the standard oxygen isotope stratigraphy. A similar ash in Malaya that overlies finds of Tampan Palaeolithic tools indicates that they are older than 75,000 yr. ?? 1978 Nature Publishing Group.","largerWorkType":{"id":2,"text":"Article"},"largerWorkTitle":"Nature","largerWorkSubtype":{"id":10,"text":"Journal Article"},"language":"English","doi":"10.1038/276574a0","issn":"00280836","usgsCitation":"Ninkovich, D., Shackleton, N.J., Abdel-Monem, A.A., Obradovich, J.D., and Izett, G., 1978, K-Ar age of the late Pleistocene eruption of Toba, north Sumatra: Nature, v. 276, no. 5688, p. 574-577, https://doi.org/10.1038/276574a0.","startPage":"574","endPage":"577","numberOfPages":"4","costCenters":[],"links":[{"id":205194,"rank":9999,"type":{"id":10,"text":"Digital Object Identifier"},"url":"https://dx.doi.org/10.1038/276574a0"},{"id":222084,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"276","issue":"5688","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"505a403fe4b0c8380cd64bef","contributors":{"authors":[{"text":"Ninkovich, D.","contributorId":37071,"corporation":false,"usgs":true,"family":"Ninkovich","given":"D.","email":"","affiliations":[],"preferred":false,"id":363871,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Shackleton, N. J.","contributorId":8996,"corporation":false,"usgs":false,"family":"Shackleton","given":"N.","email":"","middleInitial":"J.","affiliations":[],"preferred":false,"id":363869,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Abdel-Monem, A. A.","contributorId":27195,"corporation":false,"usgs":true,"family":"Abdel-Monem","given":"A.","email":"","middleInitial":"A.","affiliations":[],"preferred":false,"id":363870,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Obradovich, J. D.","contributorId":48966,"corporation":false,"usgs":true,"family":"Obradovich","given":"J.","middleInitial":"D.","affiliations":[],"preferred":false,"id":363872,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"Izett, G.","contributorId":69301,"corporation":false,"usgs":true,"family":"Izett","given":"G.","affiliations":[],"preferred":false,"id":363873,"contributorType":{"id":1,"text":"Authors"},"rank":5}]}} ,{"id":70012624,"text":"70012624 - 1978 - Polarographic determination of lead hydroxide formation constants at low ionic strength","interactions":[],"lastModifiedDate":"2023-10-23T11:54:47.325456","indexId":"70012624","displayToPublicDate":"1978-01-01T00:00:00","publicationYear":"1978","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1565,"text":"Environmental Science & Technology","onlineIssn":"1520-5851","printIssn":"0013-936X","active":true,"publicationSubtype":{"id":10}},"title":"Polarographic determination of lead hydroxide formation constants at low ionic strength","docAbstract":"

No abstract available.

","language":"English","publisher":"American Chemical Society","doi":"10.1021/es60148a010","issn":"0013936X","usgsCitation":"Lind, C.J., 1978, Polarographic determination of lead hydroxide formation constants at low ionic strength: Environmental Science & Technology, v. 12, no. 13, p. 1406-1410, https://doi.org/10.1021/es60148a010.","productDescription":"5 p.","startPage":"1406","endPage":"1410","costCenters":[],"links":[{"id":222546,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"12","issue":"13","noUsgsAuthors":false,"publicationDate":"2002-05-01","publicationStatus":"PW","scienceBaseUri":"505a7cc7e4b0c8380cd79b93","contributors":{"authors":[{"text":"Lind, Carol J.","contributorId":36110,"corporation":false,"usgs":true,"family":"Lind","given":"Carol","email":"","middleInitial":"J.","affiliations":[],"preferred":false,"id":364088,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":70012558,"text":"70012558 - 1978 - Distribution and relations of 4- to 10-km-diameter craters to global geologic units of Mars","interactions":[],"lastModifiedDate":"2025-01-28T16:56:24.410519","indexId":"70012558","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":"Distribution and relations of 4- to 10-km-diameter craters to global geologic units of Mars","docAbstract":"

By correlating the 1:25,000,000 geologic map of Mars of Scott and Carr (1977) with 4- to 10-km-diameter crater density data from Mariner 9 images, the average crater density for 23 of the equatorial geologic-geomorphic units on Mars was computed. The correlation of these two data sets was accomplished by digitizing both the crater density data and geologic map at the same scale and by comparing them in a computer. This technique assigns the crater density value found in the corresponding location on the geologic data set to a discrete computer file assigned each of the 23 geologic units. By averaging the crater density values accumulated in each file, an “average” crater density for each geologic unit was obtained. Condit believes these average crater density values are accurate indicators of the relative age of the geologic units considered. The statistical validity of these average values is strongest for the geologic units of the largest areal extent. The relative ages as obtained from the average crater density values for the seven largest geologic units, from youngest to oldest, are: Tharsis volcanic material, 21 ± 4 craters/106km2; smooth plains material, 57 ± 14 craters/106km2; rolling plains material, 66 ± 16 craters/106km2; plains materials, 80 ± 17 craters/106km2; ridged plains material, 128 ± 25 craters/106km2; hilly and cratered material, 137 ± 38 craters/106km2; and cratered plateau material, 138 ± 27 craters/106km2.

","language":"English","publisher":"Elsevier","doi":"10.1016/0019-1035(78)90038-6","issn":"00191035","usgsCitation":"Condit, C., 1978, Distribution and relations of 4- to 10-km-diameter craters to global geologic units of Mars: Icarus, v. 34, no. 3, p. 465-478, https://doi.org/10.1016/0019-1035(78)90038-6.","productDescription":"14 p.","startPage":"465","endPage":"478","numberOfPages":"14","costCenters":[],"links":[{"id":222211,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"34","issue":"3","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"505a029de4b0c8380cd5011d","contributors":{"authors":[{"text":"Condit, C.D.","contributorId":60250,"corporation":false,"usgs":true,"family":"Condit","given":"C.D.","email":"","affiliations":[],"preferred":false,"id":363901,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":70012656,"text":"70012656 - 1978 - Gases and water isotopes in a geochemical section across the Larderello, Italy, geothermal field","interactions":[],"lastModifiedDate":"2012-03-12T17:19:08","indexId":"70012656","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":"Gases and water isotopes in a geochemical section across the Larderello, Italy, geothermal field","docAbstract":"Steam samples from six wells (Colombaia, Pineta, Larderello 57, Larderello 155, Gabbro 6, and Gabbro 1) in a south to north section across the Larderello geothermal field have been analyzed for inorganic and hydrocarbon gases and for oxygen-18 and deuterium of steam. The wells generally decrease in depth and increase in age toward the south. The steam samples are generally characterized by (1) Total gas contents increasing south to north from 0.003 to 0.05 mole fraction; (2) Constant CO2 (95??2 percent); near constant H2S (1.6??0.8), N2 (1.2??0.8), H2 (2??1), CH4 (1.2??1), and no O2 in the dry gas; (3) Presence of numerous, straight chain and branched C2 to C6 hydrocarbons plus benzene in amounts independent of CH4 contents with highest concentrations in the deeper wells; (4) Oxygen-18 contents of steam increasing south to north from -5.0??? to -0.4??? with little change in deuterium (-42??2???). These observations are interpreted as showing: (1) Decreasing gas contents with amount of production because the proportion of steam boiled from liquid water increases with production; (2) Synthesis of CH4 from H2 and CO2 with CO2 and H2 produced by thermal metamorphism and rock-water reactions; (3) Extraction of C2 to C6 hydrocarbons from rock organic matter; (4) Either oxygen isotope exchange followed by distillation of steam from the north toward the south (2 plates at ???220??C) or mixture of deeper more-exchange waters from the north with shallow, less-exchanged recharging waters from the south. ?? 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/BF00879753","issn":"00334553","usgsCitation":"Truesdell, A., and Nehring, N., 1978, Gases and water isotopes in a geochemical section across the Larderello, Italy, geothermal field: Pure and Applied Geophysics PAGEOPH, v. 117, no. 1-2, p. 276-289, https://doi.org/10.1007/BF00879753.","startPage":"276","endPage":"289","numberOfPages":"14","costCenters":[],"links":[{"id":205198,"rank":9999,"type":{"id":10,"text":"Digital Object Identifier"},"url":"https://dx.doi.org/10.1007/BF00879753"},{"id":222091,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"117","issue":"1-2","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"505a14e1e4b0c8380cd54bf3","contributors":{"authors":[{"text":"Truesdell, A.H.","contributorId":52566,"corporation":false,"usgs":false,"family":"Truesdell","given":"A.H.","email":"","affiliations":[{"id":6672,"text":"former: USGS Southwest Biological Science Center, Colorado Plateau Research Station, Flagstaff, AZ. Current address: TN-SCORE, Univ of Tennessee, Knoxville, TN, e-mail: jennen@gmail.com","active":true,"usgs":false}],"preferred":false,"id":364152,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Nehring, N.L.","contributorId":21157,"corporation":false,"usgs":true,"family":"Nehring","given":"N.L.","email":"","affiliations":[],"preferred":false,"id":364151,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":70012765,"text":"70012765 - 1978 - Earthquake swarms and local crustal spreading along major strike-slip faults in California","interactions":[],"lastModifiedDate":"2012-03-12T17:19:02","indexId":"70012765","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":"Earthquake swarms and local crustal spreading along major strike-slip faults in California","docAbstract":"Earthquake swarms in California are often localized to areas within dextral offsets in the linear trend in active fault strands, suggesting a relation between earthquake swarms and local crustal spreading. Local crustal spereading is required by the geometry of dextral offsets when, as in the San Andreas system, faults have dominantly strike-slip motion with right-lateral displacement. Three clear examples of this relation occur in the Imperial Valley, Coso Hot Springs, and the Danville region, all in California. The first two of these areas are known for their Holocene volcanism and geothermal potential, which is consistent with crustal spreading and magmatic intrusion. The third example, however, shows no evidence for volcanism or geothermal activity at the surface. ?? 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/BF00879733","issn":"00334553","usgsCitation":"Weaver, C., and Hill, D., 1978, Earthquake swarms and local crustal spreading along major strike-slip faults in California: Pure and Applied Geophysics PAGEOPH, v. 117, no. 1-2, p. 51-64, https://doi.org/10.1007/BF00879733.","startPage":"51","endPage":"64","numberOfPages":"14","costCenters":[],"links":[{"id":221845,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"},{"id":205153,"rank":9999,"type":{"id":10,"text":"Digital Object Identifier"},"url":"https://dx.doi.org/10.1007/BF00879733"}],"volume":"117","issue":"1-2","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"505a0506e4b0c8380cd50c10","contributors":{"authors":[{"text":"Weaver, C.S.","contributorId":57874,"corporation":false,"usgs":true,"family":"Weaver","given":"C.S.","email":"","affiliations":[],"preferred":false,"id":364464,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Hill, D.P.","contributorId":27432,"corporation":false,"usgs":true,"family":"Hill","given":"D.P.","email":"","affiliations":[],"preferred":false,"id":364463,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":70012535,"text":"70012535 - 1978 - Lower Tertiary laterite on the Iceland-Faeroe Ridge and the Thulean land bridge","interactions":[],"lastModifiedDate":"2012-03-12T17:19:09","indexId":"70012535","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":"Lower Tertiary laterite on the Iceland-Faeroe Ridge and the Thulean land bridge","docAbstract":"CORES of a lower Tertiary lateritic palaeosol resting on basalt were recovered1 from Deep Sea Drilling Project Site 336 (Leg 38) on the north-east flank of the Iceland-Faeroe Ridge (Fig. 1), a major aseismic oceanic ridge that, together with Iceland, forms the Icelandic transverse ridge 2. The transverse ridge extends from the West European continental margin to the East Greenland continental margin, forming the geographic boundary and a partial barrier to flow of water between the Norwegian-Greenland Sea to the north and the northern North Atlantic Ocean to the south. The palaeosol indicates that at least part of the Iceland-Faeroe Ridge was above sea level during early Tertiary time3. Palaeogeographic and palaeooceanographic reconstructions suggest that it formed the main part of the Thulean land bridge that connected South-east Greenland and the Faeroe islands during the early Tertiary4. This report summarises the subsidence history of the Iceland-Faeroe Ridge relative to early Tertiary seafloor spreading, basaltic volcanism, and the development of the proposed Thulean land bridge. ?? 1978 Nature Publishing Group.","largerWorkType":{"id":2,"text":"Article"},"largerWorkTitle":"Nature","largerWorkSubtype":{"id":10,"text":"Journal Article"},"language":"English","doi":"10.1038/274786a0","issn":"00280836","usgsCitation":"Nilsen, T.H., 1978, Lower Tertiary laterite on the Iceland-Faeroe Ridge and the Thulean land bridge: Nature, v. 274, no. 5673, p. 786-788, https://doi.org/10.1038/274786a0.","startPage":"786","endPage":"788","numberOfPages":"3","costCenters":[],"links":[{"id":205158,"rank":9999,"type":{"id":10,"text":"Digital Object Identifier"},"url":"https://dx.doi.org/10.1038/274786a0"},{"id":221897,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"274","issue":"5673","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"505a4a75e4b0c8380cd68d9f","contributors":{"authors":[{"text":"Nilsen, T. H.","contributorId":93057,"corporation":false,"usgs":true,"family":"Nilsen","given":"T.","email":"","middleInitial":"H.","affiliations":[],"preferred":false,"id":363840,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":1014267,"text":"1014267 - 1978 - Parasitology translations reported mainly during 1976 and 1977","interactions":[],"lastModifiedDate":"2012-02-02T00:04:29","indexId":"1014267","displayToPublicDate":"1978-01-01T00:00:00","publicationYear":"1978","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":2414,"text":"Journal of Parasitology","active":true,"publicationSubtype":{"id":10}},"title":"Parasitology translations reported mainly during 1976 and 1977","largerWorkType":{"id":2,"text":"Article"},"largerWorkTitle":"Journal of Parasitology","largerWorkSubtype":{"id":10,"text":"Journal Article"},"language":"English","collaboration":"None/FF","usgsCitation":"Margolis, L., Edwards, S., Hoffman, G.L., Knight, R., Lunde, M.N., and Powers, K.G., 1978, Parasitology translations reported mainly during 1976 and 1977: Journal of Parasitology, v. 64, no. 6, p. 1107-1114.","productDescription":"p. 1107-1114","startPage":"1107","endPage":"1114","numberOfPages":"8","costCenters":[{"id":365,"text":"Leetown Science Center","active":true,"usgs":true}],"links":[{"id":132027,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"64","issue":"6","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b1be4b07f02db6a88df","contributors":{"authors":[{"text":"Margolis, L.","contributorId":42559,"corporation":false,"usgs":true,"family":"Margolis","given":"L.","email":"","affiliations":[],"preferred":false,"id":320076,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Edwards, S.J.","contributorId":72753,"corporation":false,"usgs":true,"family":"Edwards","given":"S.J.","email":"","affiliations":[],"preferred":false,"id":320079,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Hoffman, G. 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G.","contributorId":85537,"corporation":false,"usgs":true,"family":"Powers","given":"K.","email":"","middleInitial":"G.","affiliations":[],"preferred":false,"id":320080,"contributorType":{"id":1,"text":"Authors"},"rank":6}]}} ,{"id":9866,"text":"ofr78156C - 1978 - Analyses of stream-sediment samples from the Ketchikan quadrangle, southeastern Alaska","interactions":[],"lastModifiedDate":"2022-09-14T14:00:22.089432","indexId":"ofr78156C","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":"78-156","chapter":"C","title":"Analyses of stream-sediment samples from the Ketchikan quadrangle, southeastern Alaska","docAbstract":"

No abstract available.

","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr78156C","usgsCitation":"Koch, R.D., and Elliott, R.L., 1978, Analyses of stream-sediment samples from the Ketchikan quadrangle, southeastern Alaska: U.S. Geological Survey Open-File Report 78-156, Report: i, 214 p.; 1 Plate: 60.00 x 54.67 inches, https://doi.org/10.3133/ofr78156C.","productDescription":"Report: i, 214 p.; 1 Plate: 60.00 x 54.67 inches","costCenters":[],"links":[{"id":94938,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1978/0156c/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":37659,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1978/0156c/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":142003,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1978/0156c/report-thumb.jpg"},{"id":406669,"rank":4,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_14631.htm","linkFileType":{"id":5,"text":"html"}}],"scale":"125000","country":"United States","state":"Alaska","otherGeospatial":"Ketchikan quadrangle","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"type\": \"Polygon\",\n \"coordinates\": [\n [\n [\n -132,\n 55\n ],\n [\n -130,\n 55\n ],\n [\n -130,\n 56\n ],\n [\n -132,\n 56\n ],\n [\n -132,\n 55\n ]\n ]\n ]\n }\n }\n ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ad1e4b07f02db680d9c","contributors":{"authors":[{"text":"Koch, Richard D. rkoch@usgs.gov","contributorId":4413,"corporation":false,"usgs":true,"family":"Koch","given":"Richard","email":"rkoch@usgs.gov","middleInitial":"D.","affiliations":[],"preferred":true,"id":160428,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Elliott, Raymond L.","contributorId":82667,"corporation":false,"usgs":true,"family":"Elliott","given":"Raymond","email":"","middleInitial":"L.","affiliations":[],"preferred":false,"id":160429,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":70012475,"text":"70012475 - 1978 - A pollution history of Chesapeake Bay","interactions":[],"lastModifiedDate":"2024-03-08T17:48:41.327795","indexId":"70012475","displayToPublicDate":"1978-01-01T00:00:00","publicationYear":"1978","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":"A pollution history of Chesapeake Bay","docAbstract":"Present day anthropogenic fluxes of some heavy metals to central Chesapeake Bay appear to be intermediate to those of the southern California coastal region and those of Narragansett Bay. The natural fluxes, however, are in general higher. On the bases of Pb-210 and Pu-239 + 240 geochronologies and of the time changes in interstitial water compositions, there is a mixing of the upper 30 or so centimeters of the sediments in the mid-Chesapeake Bay area through bioturbation by burrowing mollusks and polychaetes. Coal, coke and charcoal levels reach one percent or more by dry weight in the deposits, primarily as a consequence of coal mining operations. ?? 1978.","language":"English","publisher":"Elsevier","doi":"10.1016/0016-7037(78)90047-9","issn":"00167037","usgsCitation":"Goldberg, E., Hodge, V., Koide, M., Griffin, J., Gamble, E., Bricker, O., Matisoff, G., Holdren, G., and Braun, R., 1978, A pollution history of Chesapeake Bay: Geochimica et Cosmochimica Acta, v. 42, no. 9, p. 1413-1425, https://doi.org/10.1016/0016-7037(78)90047-9.","productDescription":"13 p.","startPage":"1413","endPage":"1425","numberOfPages":"13","costCenters":[],"links":[{"id":221951,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.er.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"42","issue":"9","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"5059e4dee4b0c8380cd469b6","contributors":{"authors":[{"text":"Goldberg, E.D.","contributorId":86459,"corporation":false,"usgs":true,"family":"Goldberg","given":"E.D.","email":"","affiliations":[],"preferred":false,"id":363707,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Hodge, V.","contributorId":54736,"corporation":false,"usgs":true,"family":"Hodge","given":"V.","email":"","affiliations":[],"preferred":false,"id":363704,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Koide, M.","contributorId":53524,"corporation":false,"usgs":true,"family":"Koide","given":"M.","email":"","affiliations":[],"preferred":false,"id":363703,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Griffin, J.","contributorId":21261,"corporation":false,"usgs":true,"family":"Griffin","given":"J.","affiliations":[],"preferred":false,"id":363699,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"Gamble, E.","contributorId":63167,"corporation":false,"usgs":true,"family":"Gamble","given":"E.","email":"","affiliations":[],"preferred":false,"id":363706,"contributorType":{"id":1,"text":"Authors"},"rank":5},{"text":"Bricker, O.P.","contributorId":33717,"corporation":false,"usgs":true,"family":"Bricker","given":"O.P.","affiliations":[],"preferred":false,"id":363701,"contributorType":{"id":1,"text":"Authors"},"rank":6},{"text":"Matisoff, G.","contributorId":49929,"corporation":false,"usgs":true,"family":"Matisoff","given":"G.","affiliations":[],"preferred":false,"id":363702,"contributorType":{"id":1,"text":"Authors"},"rank":7},{"text":"Holdren, G.R. Jr.","contributorId":26443,"corporation":false,"usgs":true,"family":"Holdren","given":"G.R.","suffix":"Jr.","email":"","affiliations":[],"preferred":false,"id":363700,"contributorType":{"id":1,"text":"Authors"},"rank":8},{"text":"Braun, R.","contributorId":62746,"corporation":false,"usgs":true,"family":"Braun","given":"R.","email":"","affiliations":[],"preferred":false,"id":363705,"contributorType":{"id":1,"text":"Authors"},"rank":9}]}} ,{"id":1014326,"text":"1014326 - 1978 - A new myxosporidan, Dicauda atherinodi n.g., n. sp. of the minnow, Notropis atherinoides Rafinesque","interactions":[],"lastModifiedDate":"2025-02-04T16:51:24.918868","indexId":"1014326","displayToPublicDate":"1978-01-01T00:00:00","publicationYear":"1978","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":2286,"text":"Journal of Fish Diseases","active":true,"publicationSubtype":{"id":10}},"title":"A new myxosporidan, Dicauda atherinodi n.g., n. sp. of the minnow, Notropis atherinoides Rafinesque","docAbstract":"

Dicauda atherinoidi n.g., n. sp. (Protozoa: Myxosporida) was found in feral minnows, Notropis atherinoides (Cyprinidae), from western Lake Erie (Sterling State Park), Michigan, and the lower Mohawk and Hudson Rivers, New York. Dicauda, closely related to Myxobolus, differs from it in having two, occasionally three or more, rigid tail-like possibly mucoid appendages attached to the sutural ridge. The cysts are subdermal and most abundant on the head. Histological damage is not striking.

","language":"English","publisher":"Wiley","doi":"10.1111/j.1365-2761.1978.tb00038.x","usgsCitation":"Hoffman, G.L., and Walker, R., 1978, A new myxosporidan, Dicauda atherinodi n.g., n. sp. of the minnow, Notropis atherinoides Rafinesque: Journal of Fish Diseases, v. 1, no. 4, p. 343-349, https://doi.org/10.1111/j.1365-2761.1978.tb00038.x.","productDescription":"7 p.","startPage":"343","endPage":"349","numberOfPages":"7","costCenters":[{"id":365,"text":"Leetown Science Center","active":true,"usgs":true}],"links":[{"id":131066,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"1","issue":"4","noUsgsAuthors":false,"publicationDate":"2006-04-07","publicationStatus":"PW","scienceBaseUri":"4f4e4b20e4b07f02db6abbea","contributors":{"authors":[{"text":"Hoffman, G. L.","contributorId":70713,"corporation":false,"usgs":true,"family":"Hoffman","given":"G.","email":"","middleInitial":"L.","affiliations":[],"preferred":false,"id":320202,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Walker, R.","contributorId":64182,"corporation":false,"usgs":true,"family":"Walker","given":"R.","affiliations":[],"preferred":false,"id":320201,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":1007825,"text":"1007825 - 1978 - Forty-first breeding bird census. No. 164. Desert marsh","interactions":[],"lastModifiedDate":"2012-02-02T00:04:16","indexId":"1007825","displayToPublicDate":"1978-01-01T00:00:00","publicationYear":"1978","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":708,"text":"American Birds","active":true,"publicationSubtype":{"id":10}},"title":"Forty-first breeding bird census. No. 164. Desert marsh","largerWorkType":{"id":2,"text":"Article"},"largerWorkTitle":"American Birds","largerWorkSubtype":{"id":10,"text":"Journal Article"},"language":"English","usgsCitation":"Weinstein, M., and Berry, K., 1978, Forty-first breeding bird census. No. 164. Desert marsh: American Birds, v. 32, no. 113.","costCenters":[{"id":651,"text":"Western Ecological Research Center","active":true,"usgs":true}],"links":[{"id":130299,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"32","issue":"113","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4888e4b07f02db51a648","contributors":{"authors":[{"text":"Weinstein, M.","contributorId":6796,"corporation":false,"usgs":true,"family":"Weinstein","given":"M.","email":"","affiliations":[],"preferred":false,"id":316098,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Berry, K.H.","contributorId":17934,"corporation":false,"usgs":true,"family":"Berry","given":"K.H.","email":"","affiliations":[],"preferred":false,"id":316099,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ]}