{"pageNumber":"5845","pageRowStart":"146100","pageSize":"25","recordCount":184617,"records":[{"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":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":70012541,"text":"70012541 - 1978 - Velocity anomalies: An alternative explanation based on data from laboratory experiments","interactions":[],"lastModifiedDate":"2012-03-12T17:19:09","indexId":"70012541","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":"Velocity anomalies: An alternative explanation based on data from laboratory experiments","docAbstract":"Locations and velocities were calculated for microseisms occurring in samples of rock subjected to triaxial loading and injection of pore fluid. This was accomplished by analyzing arrival times of acoustic emission using an automatic first arrival picker. Apparent velocity anomalies were observed prior to both failure of intact samples and violent slip in samples containing saw cuts. Further analysis revealed that these fluctuations in calculated velocity were not due to changes in the true seismie velocity. Instead, variations in calculated velocity are shown to be related to sampling errors in picking first arrivals. The systematic picking of late first arrivals for small magnitude events was found to be a persistent bias resulting in low calculated velocities. This has encouraged the reexamination of earthquake records to determine how important sampling biases are in contributing to reported velocity anomalies. ?? 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/BF00876537","issn":"00334553","usgsCitation":"Lockner, D., and Byerlee, J., 1978, Velocity anomalies: An alternative explanation based on data from laboratory experiments: Pure and Applied Geophysics PAGEOPH, v. 116, no. 4-5, p. 765-772, https://doi.org/10.1007/BF00876537.","startPage":"765","endPage":"772","numberOfPages":"8","costCenters":[],"links":[{"id":205172,"rank":9999,"type":{"id":10,"text":"Digital Object Identifier"},"url":"https://dx.doi.org/10.1007/BF00876537"},{"id":221955,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"116","issue":"4-5","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"505bc1f6e4b08c986b32a855","contributors":{"authors":[{"text":"Lockner, D.A. 0000-0001-8630-6833","orcid":"https://orcid.org/0000-0001-8630-6833","contributorId":85603,"corporation":false,"usgs":true,"family":"Lockner","given":"D.A.","affiliations":[],"preferred":false,"id":363858,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Byerlee, J.D.","contributorId":69982,"corporation":false,"usgs":true,"family":"Byerlee","given":"J.D.","affiliations":[],"preferred":false,"id":363857,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":70012713,"text":"70012713 - 1978 - Microwave remote sensing of sea ice in the AIDJEX Main Experiment","interactions":[],"lastModifiedDate":"2012-03-12T17:19:10","indexId":"70012713","displayToPublicDate":"1978-01-01T00:00:00","publicationYear":"1978","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1072,"text":"Boundary-Layer Meteorology","active":true,"publicationSubtype":{"id":10}},"title":"Microwave remote sensing of sea ice in the AIDJEX Main Experiment","docAbstract":"During the AIDJEX Main Experiment, April 1975 through May 1976, a comprehensive microwave sensing program was performed on the sea ice of the Beaufort Sea. Surface and aircraft measurements were obtained during all seasons using a wide variety of active and passive microwave sensors. The surface program obtained passive microwave measurements of various ice types using four antennas mounted on a tracked vehicle. In three test regions, each with an area of approximately 1.5 ?? 104 m2, detailed ice crystallographic, dielectric properties, and brightness temperatures of first-year, multiyear, and first-year/multiyear mixtures were measured. A NASA aircraft obtained passive microwave measurements of the entire area of the AIDJEX manned station array (triangle) during each of 18 flights. This verified the earlier reported ability to distinguish first-year and multiyear ice types and concentration and gave new information on ways to observe ice mixtures and thin ice types. The active microwave measurements from aircraft included those from an X- and L-band radar and from a scatterometer. The former is used to study a wide variety of ice features and to estimate deformations, while both are equally usable to observe ice types. With the present data, only the scatterometer can be used to distinguish positively multiyear from first-year and various types of thin ice. This is best done using coupled active and passive microwave sensing. ?? 1978 D. Reidel Publishing Company.","largerWorkType":{"id":2,"text":"Article"},"largerWorkTitle":"Boundary-Layer Meteorology","largerWorkSubtype":{"id":10,"text":"Journal Article"},"language":"English","publisherLocation":"Kluwer Academic Publishers","doi":"10.1007/BF00913880","issn":"00068314","usgsCitation":"Campbell, W.J., Wayenberg, J., Ramseyer, J., Ramseier, R., Vant, M., Weaver, R., Redmond, A., Arsenaul, L., Gloersen, P., Zwally, H., Wilheit, T., Chang, T., Hall, D., Gray, L., Meeks, D., Bryan, M., Barath, F., Elachi, C., Leberl, F., and Farr, T., 1978, Microwave remote sensing of sea ice in the AIDJEX Main Experiment: Boundary-Layer Meteorology, v. 13, no. 1-4, p. 309-337, https://doi.org/10.1007/BF00913880.","startPage":"309","endPage":"337","numberOfPages":"29","costCenters":[],"links":[{"id":222033,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"},{"id":205188,"rank":9999,"type":{"id":10,"text":"Digital Object Identifier"},"url":"https://dx.doi.org/10.1007/BF00913880"}],"volume":"13","issue":"1-4","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"505a56afe4b0c8380cd6d756","contributors":{"authors":[{"text":"Campbell, W. J.","contributorId":8614,"corporation":false,"usgs":true,"family":"Campbell","given":"W.","email":"","middleInitial":"J.","affiliations":[],"preferred":false,"id":364299,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Wayenberg, J.","contributorId":69018,"corporation":false,"usgs":true,"family":"Wayenberg","given":"J.","affiliations":[],"preferred":false,"id":364311,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Ramseyer, J.B.","contributorId":55285,"corporation":false,"usgs":true,"family":"Ramseyer","given":"J.B.","email":"","affiliations":[],"preferred":false,"id":364307,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Ramseier, R.O.","contributorId":98039,"corporation":false,"usgs":true,"family":"Ramseier","given":"R.O.","email":"","affiliations":[],"preferred":false,"id":364317,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"Vant, M.R.","contributorId":17883,"corporation":false,"usgs":true,"family":"Vant","given":"M.R.","email":"","affiliations":[],"preferred":false,"id":364303,"contributorType":{"id":1,"text":"Authors"},"rank":5},{"text":"Weaver, R.","contributorId":12749,"corporation":false,"usgs":true,"family":"Weaver","given":"R.","email":"","affiliations":[],"preferred":false,"id":364300,"contributorType":{"id":1,"text":"Authors"},"rank":6},{"text":"Redmond, A.","contributorId":15891,"corporation":false,"usgs":true,"family":"Redmond","given":"A.","email":"","affiliations":[],"preferred":false,"id":364301,"contributorType":{"id":1,"text":"Authors"},"rank":7},{"text":"Arsenaul, L.","contributorId":71444,"corporation":false,"usgs":true,"family":"Arsenaul","given":"L.","email":"","affiliations":[],"preferred":false,"id":364312,"contributorType":{"id":1,"text":"Authors"},"rank":8},{"text":"Gloersen, P.","contributorId":55961,"corporation":false,"usgs":true,"family":"Gloersen","given":"P.","affiliations":[],"preferred":false,"id":364309,"contributorType":{"id":1,"text":"Authors"},"rank":9},{"text":"Zwally, H.J.","contributorId":33847,"corporation":false,"usgs":true,"family":"Zwally","given":"H.J.","email":"","affiliations":[],"preferred":false,"id":364305,"contributorType":{"id":1,"text":"Authors"},"rank":10},{"text":"Wilheit, T.T.","contributorId":94923,"corporation":false,"usgs":true,"family":"Wilheit","given":"T.T.","email":"","affiliations":[],"preferred":false,"id":364316,"contributorType":{"id":1,"text":"Authors"},"rank":11},{"text":"Chang, T.C.","contributorId":16713,"corporation":false,"usgs":true,"family":"Chang","given":"T.C.","email":"","affiliations":[],"preferred":false,"id":364302,"contributorType":{"id":1,"text":"Authors"},"rank":12},{"text":"Hall, D.","contributorId":55620,"corporation":false,"usgs":true,"family":"Hall","given":"D.","affiliations":[],"preferred":false,"id":364308,"contributorType":{"id":1,"text":"Authors"},"rank":13},{"text":"Gray, L.","contributorId":92544,"corporation":false,"usgs":true,"family":"Gray","given":"L.","affiliations":[],"preferred":false,"id":364315,"contributorType":{"id":1,"text":"Authors"},"rank":14},{"text":"Meeks, D.C.","contributorId":74641,"corporation":false,"usgs":true,"family":"Meeks","given":"D.C.","email":"","affiliations":[],"preferred":false,"id":364314,"contributorType":{"id":1,"text":"Authors"},"rank":15},{"text":"Bryan, M.L.","contributorId":60080,"corporation":false,"usgs":true,"family":"Bryan","given":"M.L.","email":"","affiliations":[],"preferred":false,"id":364310,"contributorType":{"id":1,"text":"Authors"},"rank":16},{"text":"Barath, F.T.","contributorId":54471,"corporation":false,"usgs":true,"family":"Barath","given":"F.T.","email":"","affiliations":[],"preferred":false,"id":364306,"contributorType":{"id":1,"text":"Authors"},"rank":17},{"text":"Elachi, C.","contributorId":104606,"corporation":false,"usgs":false,"family":"Elachi","given":"C.","affiliations":[],"preferred":false,"id":364318,"contributorType":{"id":1,"text":"Authors"},"rank":18},{"text":"Leberl, F.","contributorId":74245,"corporation":false,"usgs":true,"family":"Leberl","given":"F.","email":"","affiliations":[],"preferred":false,"id":364313,"contributorType":{"id":1,"text":"Authors"},"rank":19},{"text":"Farr, Tom","contributorId":24903,"corporation":false,"usgs":true,"family":"Farr","given":"Tom","affiliations":[],"preferred":false,"id":364304,"contributorType":{"id":1,"text":"Authors"},"rank":20}]}}
,{"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":70012542,"text":"70012542 - 1978 - Friction of rocks","interactions":[],"lastModifiedDate":"2012-03-12T17:19:09","indexId":"70012542","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":"Friction of rocks","docAbstract":"Experimental results in the published literature show that at low normal stress the shear stress required to slide one rock over another varies widely between experiments. This is because at low stress rock friction is strongly dependent on surface roughness. At high normal stress that effect is diminished and the friction is nearly independent of rock type. If the sliding surfaces are separated by gouge composed of Montmorillonite or vermiculite the friction can be very low. ?? 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/BF00876528","issn":"00334553","usgsCitation":"Byerlee, J., 1978, Friction of rocks: Pure and Applied Geophysics PAGEOPH, v. 116, no. 4-5, p. 615-626, https://doi.org/10.1007/BF00876528.","startPage":"615","endPage":"626","numberOfPages":"12","costCenters":[],"links":[{"id":205173,"rank":9999,"type":{"id":10,"text":"Digital Object Identifier"},"url":"https://dx.doi.org/10.1007/BF00876528"},{"id":221956,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"116","issue":"4-5","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"505a13ece4b0c8380cd54823","contributors":{"authors":[{"text":"Byerlee, J.","contributorId":105838,"corporation":false,"usgs":true,"family":"Byerlee","given":"J.","affiliations":[],"preferred":false,"id":363859,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":40570,"text":"ofr7860 - 1978 - Coal resource occurrence maps of the Seminoe Dam SW Quadrangle, Carbon County, Wyoming","interactions":[],"lastModifiedDate":"2023-04-14T11:18:05.772161","indexId":"ofr7860","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":"78-60","title":"Coal resource occurrence maps of the Seminoe Dam SW Quadrangle, Carbon County, Wyoming","docAbstract":"<p>No abstract available.</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr7860","usgsCitation":"Texas Instruments Incorporated, 1978, Coal resource occurrence maps of the Seminoe Dam SW Quadrangle, Carbon County, Wyoming: U.S. Geological Survey Open-File Report 78-60, Report: 20 p.; 3 Plates: 30.29 × 37.71 inches or smaller, https://doi.org/10.3133/ofr7860.","productDescription":"Report: 20 p.; 3 Plates: 30.29 × 37.71 inches or smaller","costCenters":[],"links":[{"id":76698,"rank":5,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1978/0060/plate-3.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":76699,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1978/0060/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":175766,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1978/0060/report-thumb.jpg"},{"id":76696,"rank":3,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1978/0060/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":76697,"rank":4,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1978/0060/plate-2.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b25e4b07f02db6af03d","contributors":{"authors":[{"text":"Texas Instruments Incorporated","contributorId":128266,"corporation":true,"usgs":false,"organization":"Texas Instruments Incorporated","id":530331,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":10660,"text":"ofr78198 - 1978 - Principal facts and profiles of gravity data from parts of Meade, Pennington, Haakon, and Jackson Counties, South Dakota","interactions":[],"lastModifiedDate":"2022-12-09T21:05:40.699603","indexId":"ofr78198","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":"78-198","title":"Principal facts and profiles of gravity data from parts of Meade, Pennington, Haakon, and Jackson Counties, South Dakota","docAbstract":"<p>No abstract available.</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr78198","usgsCitation":"Peterson, D.L., and Hassemer, J.H., 1978, Principal facts and profiles of gravity data from parts of Meade, 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,{"id":1013682,"text":"1013682 - 1978 - Enteric redmouth bacterium: Comparison of isolates from different geographic areas","interactions":[],"lastModifiedDate":"2025-02-04T16:49:02.345181","indexId":"1013682","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":"Enteric redmouth bacterium: Comparison of isolates from different geographic areas","docAbstract":"<p><span>Characteristics of 18 strains of&nbsp;</span><i>Yersinia ruckeri</i><span>&nbsp;the causative agent of enteric redmouth disease, from a variety of hosts and a wide geographic range were compared. Except for variations in colonial morphology and in citrate, sorbitol, and trehalose reactions, the strains were morphologically and biochemically homogeneous. Sixteen strains reacted with antiserum against the first serotype reported, and one strain reacted with antiserum against a more recently reported serotype. One strain represented a third serotype. Evidence presented indicated that extension of the geographic range may not be entirely a result of the transport of carrier fish.</span></p>","language":"English","publisher":"Wiley","doi":"10.1111/j.1365-2761.1978.tb00039.x","usgsCitation":"Bullock, G.L., Stuckey, H.M., and Shotts, E.B., 1978, Enteric redmouth bacterium: Comparison of isolates from different geographic areas: Journal of Fish Diseases, v. 1, no. 4, p. 351-356, https://doi.org/10.1111/j.1365-2761.1978.tb00039.x.","productDescription":"6 p.","startPage":"351","endPage":"356","numberOfPages":"6","costCenters":[{"id":365,"text":"Leetown Science Center","active":true,"usgs":true}],"links":[{"id":129694,"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":"4f4e4a14e4b07f02db6025f6","contributors":{"authors":[{"text":"Bullock, G. L.","contributorId":69498,"corporation":false,"usgs":true,"family":"Bullock","given":"G.","email":"","middleInitial":"L.","affiliations":[],"preferred":false,"id":319035,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Stuckey, H. M.","contributorId":60157,"corporation":false,"usgs":true,"family":"Stuckey","given":"H.","email":"","middleInitial":"M.","affiliations":[],"preferred":false,"id":319034,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Shotts, E. B. Jr.","contributorId":102414,"corporation":false,"usgs":false,"family":"Shotts","given":"E.","suffix":"Jr.","email":"","middleInitial":"B.","affiliations":[],"preferred":false,"id":319036,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":70012445,"text":"70012445 - 1978 - A tubular-scoop sampler for stream sediments","interactions":[],"lastModifiedDate":"2025-03-05T17:41:54.463647","indexId":"70012445","displayToPublicDate":"1978-01-01T00:00:00","publicationYear":"1978","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":2302,"text":"Journal of Geochemical Exploration","active":true,"publicationSubtype":{"id":10}},"title":"A tubular-scoop sampler for stream sediments","docAbstract":"<p>A stream-sediment sampling tool is described.</p>","language":"English","publisher":"Elsevier","doi":"10.1016/0375-6742(78)90019-5","issn":"03756742","usgsCitation":"Curtin, G., 1978, A tubular-scoop sampler for stream sediments: Journal of Geochemical Exploration, v. 10, no. 2, p. 193-194, https://doi.org/10.1016/0375-6742(78)90019-5.","productDescription":"2 p.","startPage":"193","endPage":"194","numberOfPages":"2","costCenters":[],"links":[{"id":222355,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"10","issue":"2","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"5059e607e4b0c8380cd470f6","contributors":{"authors":[{"text":"Curtin, G.C.","contributorId":89501,"corporation":false,"usgs":true,"family":"Curtin","given":"G.C.","email":"","affiliations":[],"preferred":false,"id":363596,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":1014218,"text":"1014218 - 1978 - Mycobacteriosis (tuberculosis) in fishes","interactions":[],"lastModifiedDate":"2012-02-02T00:04:28","indexId":"1014218","displayToPublicDate":"1978-01-01T00:00:00","publicationYear":"1978","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":3040,"text":"Pet Age","active":true,"publicationSubtype":{"id":10}},"title":"Mycobacteriosis (tuberculosis) in fishes","largerWorkType":{"id":2,"text":"Article"},"largerWorkTitle":"Pet Age","largerWorkSubtype":{"id":10,"text":"Journal Article"},"language":"English","collaboration":"615/FH","usgsCitation":"Snieszko, S.F., 1978, Mycobacteriosis (tuberculosis) in fishes: Pet Age, v. 8, no. 1, p. 23-25, 28.","productDescription":"p. 23-25, 28","startPage":"23","endPage":"25, 28","numberOfPages":"3","costCenters":[{"id":365,"text":"Leetown Science Center","active":true,"usgs":true}],"links":[{"id":132289,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"8","issue":"1","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b32e4b07f02db6b4909","contributors":{"authors":[{"text":"Snieszko, S. F.","contributorId":13169,"corporation":false,"usgs":true,"family":"Snieszko","given":"S.","middleInitial":"F.","affiliations":[],"preferred":false,"id":319986,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":1014217,"text":"1014217 - 1978 - Control of fish diseases","interactions":[],"lastModifiedDate":"2012-02-02T00:04:28","indexId":"1014217","displayToPublicDate":"1978-01-01T00:00:00","publicationYear":"1978","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":2665,"text":"Marine Fisheries Review","active":true,"publicationSubtype":{"id":10}},"title":"Control of fish diseases","largerWorkType":{"id":2,"text":"Article"},"largerWorkTitle":"Marine Fisheries Review","largerWorkSubtype":{"id":10,"text":"Journal Article"},"language":"English","collaboration":"306/FH","usgsCitation":"Snieszko, S.F., 1978, Control of fish diseases: Marine Fisheries Review, v. 40, no. 3, p. 65-68.","productDescription":"p. 65-68","startPage":"65","endPage":"68","numberOfPages":"4","costCenters":[{"id":365,"text":"Leetown Science Center","active":true,"usgs":true}],"links":[{"id":132288,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"40","issue":"3","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ae0e4b07f02db6881f4","contributors":{"authors":[{"text":"Snieszko, S. F.","contributorId":13169,"corporation":false,"usgs":true,"family":"Snieszko","given":"S.","middleInitial":"F.","affiliations":[],"preferred":false,"id":319985,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":1013679,"text":"1013679 - 1978 - Corynebacterial kidney disease: egg transmission following iodophore disinfection","interactions":[],"lastModifiedDate":"2012-03-02T17:16:04","indexId":"1013679","displayToPublicDate":"1978-01-01T00:00:00","publicationYear":"1978","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1647,"text":"Fish Health News","active":true,"publicationSubtype":{"id":10}},"title":"Corynebacterial kidney disease: egg transmission following iodophore disinfection","largerWorkType":{"id":2,"text":"Article"},"largerWorkTitle":"Fish Health News","largerWorkSubtype":{"id":10,"text":"Journal Article"},"language":"English","publisher":"U.S. Fish and Wildlife Service","collaboration":"363/FH","usgsCitation":"Bullock, G.L., Stuckey, H.M., and Mulcahy, D., 1978, Corynebacterial kidney disease: egg transmission following iodophore disinfection: Fish Health News, v. 7, no. 2, p. 51-52.","productDescription":"p. 51-52","startPage":"51","endPage":"52","numberOfPages":"2","costCenters":[{"id":365,"text":"Leetown Science Center","active":true,"usgs":true}],"links":[{"id":129585,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"7","issue":"2","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ad6e4b07f02db68429b","contributors":{"authors":[{"text":"Bullock, G. L.","contributorId":69498,"corporation":false,"usgs":true,"family":"Bullock","given":"G.","email":"","middleInitial":"L.","affiliations":[],"preferred":false,"id":319027,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Stuckey, H. M.","contributorId":60157,"corporation":false,"usgs":true,"family":"Stuckey","given":"H.","email":"","middleInitial":"M.","affiliations":[],"preferred":false,"id":319026,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Mulcahy, D.","contributorId":82642,"corporation":false,"usgs":true,"family":"Mulcahy","given":"D.","email":"","affiliations":[],"preferred":false,"id":319028,"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":"<p>No abstract available.</p>","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":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":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":"<p><span>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&nbsp;</span><span class=\"math\"><span id=\"MathJax-Element-1-Frame\" class=\"MathJax_SVG\" data-mathml=\"<math xmlns=&quot;http://www.w3.org/1998/Math/MathML&quot;><mtext>1</mtext><mtext>10</mtext><mtext>to</mtext><mtext>1</mtext><mtext>15</mtext></math>\"><span class=\"MJX_Assistive_MathML\">110 to 115</span></span></span><span>&nbsp;are consistent with this interpretation and suggest that volumes of transient cavities and hence of basin ejecta may be considerably greater than commonly assumed.</span></p>","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":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":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":70012524,"text":"70012524 - 1978 - Interpretation of a Landsat image of an unusual flood phenomenon in Australia","interactions":[],"lastModifiedDate":"2017-01-18T15:12:24","indexId":"70012524","displayToPublicDate":"1978-01-01T00:00:00","publicationYear":"1978","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":3254,"text":"Remote Sensing of Environment","printIssn":"0034-4257","active":true,"publicationSubtype":{"id":10}},"title":"Interpretation of a Landsat image of an unusual flood phenomenon in Australia","docAbstract":"A Landsat image of part of the flooded area of Cooper Creek, Queensland, Australia, in February 1974, shows large dark areas within the flooded valley. The dark areas are believed to be wet, but unflooded, areas of dark alluvial soil. These striking features, which have not previously been identified on Landsat images, must be properly interpreted so as not to confuse them with clear water.","language":"English","publisher":"Elsevier","doi":"10.1016/0034-4257(78)90033-0","issn":"00344257","usgsCitation":"Robinove, C.J., 1978, Interpretation of a Landsat image of an unusual flood phenomenon in Australia: Remote Sensing of Environment, v. 7, no. 3, p. 219-225, https://doi.org/10.1016/0034-4257(78)90033-0.","productDescription":"7 p.","startPage":"219","endPage":"225","numberOfPages":"7","costCenters":[{"id":222,"text":"Earth Resources Observation and Science (EROS) Center","active":true,"usgs":true}],"links":[{"id":222664,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"},{"id":289862,"type":{"id":10,"text":"Digital Object Identifier"},"url":"https://dx.doi.org/10.1016/0034-4257(78)90033-0"}],"country":"Australia","state":"Queensland","otherGeospatial":"Cooper Creek","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ 140.8027,-26.8875 ], [ 140.8027,-25.006 ], [ 142.9985,-25.006 ], [ 142.9985,-26.8875 ], [ 140.8027,-26.8875 ] ] ] } } ] }","volume":"7","issue":"3","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"505a3d60e4b0c8380cd6350b","contributors":{"authors":[{"text":"Robinove, Charles J.","contributorId":16983,"corporation":false,"usgs":true,"family":"Robinove","given":"Charles","email":"","middleInitial":"J.","affiliations":[],"preferred":false,"id":363815,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"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":"<p>No abstract available.</p>","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":46853,"text":"ofr79251 - 1978 - Drill-hole location maps, Carlsbad mining district, Eddy and Lea Counties, New Mexico","interactions":[{"subject":{"id":46853,"text":"ofr79251 - 1978 - Drill-hole location maps, Carlsbad mining district, Eddy and Lea Counties, New Mexico","indexId":"ofr79251","publicationYear":"1978","noYear":false,"title":"Drill-hole location maps, Carlsbad mining district, Eddy and Lea Counties, New Mexico"},"predicate":"SUPERSEDED_BY","object":{"id":19052,"text":"ofr81610 - 1981 - Map of core holes and selected oil and gas test wells in the Carlsbad mining district, Eddy and Lea Counties, New Mexico, as of September, 1980","indexId":"ofr81610","publicationYear":"1981","noYear":false,"title":"Map of core holes and selected oil and gas test wells in the Carlsbad mining district, Eddy and Lea Counties, New Mexico, as of September, 1980"},"id":1}],"supersededBy":{"id":19052,"text":"ofr81610 - 1981 - Map of core holes and selected oil and gas test wells in the Carlsbad mining district, Eddy and Lea Counties, New Mexico, as of September, 1980","indexId":"ofr81610","publicationYear":"1981","noYear":false,"title":"Map of core holes and selected oil and gas test wells in the Carlsbad mining district, Eddy and Lea Counties, New Mexico, as of September, 1980"},"lastModifiedDate":"2023-08-25T19:13:37.174632","indexId":"ofr79251","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":"79-251","title":"Drill-hole location maps, Carlsbad mining district, Eddy and Lea Counties, New Mexico","docAbstract":"<p>No abstract available.</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr79251","usgsCitation":"Water Resources Division, U.S. Geological Survey, 1978, Drill-hole location maps, Carlsbad mining district, Eddy and Lea Counties, New Mexico: U.S. Geological Survey Open-File Report 79-251, 4 Plates: 41.97 x 60.21 inches or smaller, https://doi.org/10.3133/ofr79251.","productDescription":"4 Plates: 41.97 x 60.21 inches or smaller","costCenters":[],"links":[{"id":420169,"rank":6,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_29103.htm","linkFileType":{"id":5,"text":"html"}},{"id":99823,"rank":5,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1979/0251/plate-4.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":99822,"rank":4,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1979/0251/plate-3.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":99821,"rank":3,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1979/0251/plate-2.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":99820,"rank":2,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1979/0251/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":168430,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"}],"scale":"31680","country":"United States","state":"New Mexico","county":"Eddy County, Lea County","otherGeospatial":"Carlsbad mining district","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"coordinates\": [\n          [\n            [\n              -104,\n              32.75\n            ],\n            [\n              -104,\n              32.25\n            ],\n            [\n              -103.767,\n              32.25\n            ],\n            [\n              -103.767,\n              32.75\n            ],\n            [\n              -104,\n              32.75\n            ]\n          ]\n        ],\n        \"type\": \"Polygon\"\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a60e4b07f02db6355a6","contributors":{"authors":[{"text":"Water Resources Division, U.S. Geological Survey","contributorId":128075,"corporation":true,"usgs":false,"organization":"Water Resources Division, U.S. Geological Survey","id":531698,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":69546,"text":"hu41 - 1978 - Hydrologic Unit Map-1978, state of South Dakota","interactions":[],"lastModifiedDate":"2023-08-29T21:05:25.336195","indexId":"hu41","displayToPublicDate":"1978-01-01T00:00:00","publicationYear":"1978","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":319,"text":"Hydrologic Unit","code":"HU","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"41","subseriesTitle":"South Dakota 1978","title":"Hydrologic Unit Map-1978, state of South Dakota","docAbstract":"<p>This map and accompanying table show Hydrologic Unites that are basically hydrographic in nature. The Cataloging Unites shown supplant the Cataloging Units previously depicted n the 1974 State Hydrologic Unit Map. The boundaries as shown have been adapted from the 1974 State Hydrologic Unit Map, \"The Catalog of Information on Water Data\" (1972), \"Water Resources Regions and Subregions for the National Assessment of Water and Related Land Resources\" by the U.S. Water Resources Council (1970), \"River Basin of the United States\" by the U.S. Soil Conservation Service (1963, 1970), \"River Basin Maps Showing Hydrologic Stations\" by the Inter-Agency Committee on Water Resources, Subcommittee on Hydrology (1961), and State planning maps.</p>\n<br>\n<p>The Political Subdivision has been adopted from \"Counties and County Equivalents of the States if the United States\" presented in Federal Information Processing Standards Publication 6-2, issued by the National Bureau of Standards (1973) in which each county or county equivalent is identified by a 2-character State code and a 3-character county code.</p>\n<br>\n<p>The Regions, Subregions and Accounting Units are aggregates of the Cataloging Unites. The Regions and Sub regions are currently (1978) used by the U.S> Water Resources Council for comprehensive planning, including the National Assessment, and as a standard geographical framework for more detailed water and related land-resources planning. The Accounting Units are those currently (1978) in use by the U.S. Geological Survey for managing the National Water Data Network.</p>\n<br>\n<p>This map was revised to include a boundary realinement between Cataloging Units 10140103 and 10160009.</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/hu41","collaboration":"Prepared in cooperation with the U.S. Water Resources Council","usgsCitation":"Water Resources Division, U.S. Geological Survey, 1978, Hydrologic Unit Map-1978, state of South Dakota: U.S. Geological Survey Hydrologic Unit 41, Report: 1 p.; 1 Plate: 52.51 x 38.30 inches, https://doi.org/10.3133/hu41.","productDescription":"Report: 1 p.; 1 Plate: 52.51 x 38.30 inches","costCenters":[],"links":[{"id":252493,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/hu/41/report-thumb.jpg"},{"id":251580,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/hu/41/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":251581,"rank":3,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/hu/41/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":420277,"rank":4,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_16250.htm","linkFileType":{"id":5,"text":"html"}}],"scale":"500000","projection":"Lambert conformal conic projection","country":"United States","state":"South Dakota","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -104.05,42.5 ], [ -104.05,45.866667 ], [ -96.5,45.866667 ], [ -96.5,42.5 ], [ -104.05,42.5 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a2de4b07f02db61423e","contributors":{"authors":[{"text":"Water Resources Division, U.S. Geological Survey","contributorId":128075,"corporation":true,"usgs":false,"organization":"Water Resources Division, U.S. Geological Survey","id":534636,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":2679,"text":"wsp2047 - 1978 - Geology and ground water in Door County, Wisconsin, with emphasis on contamination potential in the Silurian dolomite","interactions":[{"subject":{"id":11130,"text":"ofr7761 - 1977 - Geology and ground water in Door County, Wisconsin, with emphasis on contamination potential in the Silurian dolomite","indexId":"ofr7761","publicationYear":"1977","noYear":false,"title":"Geology and ground water in Door County, Wisconsin, with emphasis on contamination potential in the Silurian dolomite"},"predicate":"SUPERSEDED_BY","object":{"id":2679,"text":"wsp2047 - 1978 - Geology and ground water in Door County, Wisconsin, with emphasis on contamination potential in the Silurian dolomite","indexId":"wsp2047","publicationYear":"1978","noYear":false,"title":"Geology and ground water in Door County, Wisconsin, with emphasis on contamination potential in the Silurian dolomite"},"id":1}],"lastModifiedDate":"2023-04-10T21:59:23.676287","indexId":"wsp2047","displayToPublicDate":"1978-01-01T00:00:00","publicationYear":"1978","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":341,"text":"Water Supply Paper","code":"WSP","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"2047","title":"Geology and ground water in Door County, Wisconsin, with emphasis on contamination potential in the Silurian dolomite","docAbstract":"<p>Door County is in northeastern Wisconsin and is an area of 491 square miles. The county forms the main body of the peninsula between Green Bay and Lake Michigan. The land surface is an upland ridge controlled by the underlying bedrock. The west edge of the ridge forms an escarpment facing Green Bay. Silurian dolomite is the upper bedrock unit throughout most of the county and is the most important aquifer. This bedrock is exposed in much of the county, particularly north of Sturgeon Bay; elsewhere, it is covered by a generally thin mantle of soil or drift. The bedrock units are divided into two major aquifer systems in Door County; the Silurian dolomite aquifer system and the sandstone aquifer system, consisting of Ordovician and Cambrian bedrock units. These two major systems are separated by the Maquoketa Shale of Ordovician age, a nearly impermeable, generally nonproductive unit. The Silurian dolomite aquifer system is itself divided into the Niagaran aquifer and the underlying Alexandrian aquifer. Water occurs in the Silurian dolomite aquifer system in two types of openings-nearly vertical joints (fractures) and horizontal to slightly dipping bedding-plane joints. Vertical joints are more common in the upper part of the Niagaran aquifer. These yield small amounts of water to wells. Bedding-plane joints transmit most of the water in the lower part of the Niagaran aquifer and in the Alexandrian aquifer. The bedding-plane joints, because they are poorly interconnected, act as semiartesian conduits separated by impermeable rock. Eight water-bearing zones in generally continuous bedding-plane joints have been mapped. The dolomite is recharged from direct precipitation and snowmelt. It discharges water to pumping wells and by natural springs discharge to Lake Michigan and Green Bay and to interior lakes and streams. Wells in the Silurian dolomite aquifer system have adequate yields to meet most needs, except in the southwest corner of the county, where the dolomite is thin or absent. Transmissivity values range from a low of 4.0 feet squared per day in the Niagaran aquifer near Sturgeon Bay to more than 13 000 feet squared per day for the Alexandrian aquifer near Fish Creek. Water from Silurian dolomite is a very hard calcium magnesium bicarbonate type, with objectionable concentrations of iron and nitrate in water from some wells. Sanitary quality, as indicated by tests for total coliform bacteria, has been a chronic problem in certain areas. Concentrations of indicator organisms are greatest during or immediately after rapid ground-water recharge, with concentrations rapidly decreasing after periods of recharge. Wells close to septic systems and in areas underlain by fractured near-surface bedrock have the greatest incidence of contamination. The type and thickness of unconsolidated material has a direct effect on the entry of bacteria into the ground-water system. Bacterial attenuation increases with increasing soil depth and reduction in soil permeability. After bacterial contaminants reach the water table within fractured bedrock, little attenuation occurs, and the contaminants can travel long distances in a short time. Ground water of good sanitary quality but exceeding recommended limits of the U.S. Public Health Service for sulfate and chloride is probably available from the sandstone aquifer by drilling wells 700 to 1300 feet deep. To minimize the possibility of obtaining contaminated ground water, well construction should include properly locating the wells upgradient and as far as practical from contamination sources, setting and pressure grouting well casings to an adequate depth into firm bedrock, and casing the well into the zone of saturation.</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/wsp2047","collaboration":"Prepared in cooperation with the Wisconsin Department of Natural Resources","usgsCitation":"Sherrill, M.G., 1978, Geology and ground water in Door County, Wisconsin, with emphasis on contamination potential in the Silurian dolomite: U.S. Geological Survey Water Supply Paper 2047, Report: v, 38 p.; 5 Plates: 27.00 x 31.37 inches or smaller, https://doi.org/10.3133/wsp2047.","productDescription":"Report: v, 38 p.; 5 Plates: 27.00 x 31.37 inches or smaller","numberOfPages":"49","onlineOnly":"N","additionalOnlineFiles":"Y","costCenters":[{"id":677,"text":"Wisconsin 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Marvin G.","contributorId":91469,"corporation":false,"usgs":true,"family":"Sherrill","given":"Marvin","email":"","middleInitial":"G.","affiliations":[],"preferred":false,"id":145599,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":70012407,"text":"70012407 - 1978 - Uranium-lead isotope systematics and apparent ages of zircons and other minerals in precambrian granitic rocks, Granite Mountains, Wyoming","interactions":[],"lastModifiedDate":"2012-03-12T17:18:47","indexId":"70012407","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":"Uranium-lead isotope systematics and apparent ages of zircons and other minerals in precambrian granitic rocks, Granite Mountains, Wyoming","docAbstract":"Zircon suites from the two main types of granite in the Granite Mountains, Wyoming, yielded concordia-intercept ages of 2,640??20 m.y. for a red, foliated granite (granite of Long Creek Mountain) and 2,595??40 m.y. for the much larger mass of the granite of Lankin Dome. These ages are statistically distinct (40??20 m.y. difference) and are consistent with observed chemical and textural differences. The lower intercepts of the zircon chords of 50??40 and 100+ 75 m.y. for the granite of Long Creek Mountain and granite of Lankin Dome, respectively, are not consistent with reasonable continuous diffusion lead-loss curves but do correspond well with the known (Laramide) time of uplift of the rocks. Epidote, zircon, and apatite from silicified and epidotized zones in the granites all record at least one postcrystallization disturbance in addition to the Laramide event and do not define a unique age of silicification and epidotization. The lower limit of ???2,500 m.y. provided by the least disturbed epidote, however, suggests that these rocks were probably formed by deuteric processes shortly after emplacement of the granite of the Lankin Dome. The earlier of the two disturbances that affected the minerals of the silicified-epidotized rock can be bracketed between 1,350 and 2,240 m.y. ago and is probably the same event that lowered mineral K-Ar and ages in the region. Zircon suites from both types of granite show well-defined linear correlations among U content, common-Pb content, and degree of discordance. One of the zircon suites has an extremely high common-Pb content (up to 180 ppm) and exhibits a component of radiogenic-Pb loss that is apparently unrelated to radiation damage. ?? 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/BF00375510","issn":"00107999","usgsCitation":"Ludwig, K., and Stuckless, J., 1978, Uranium-lead isotope systematics and apparent ages of zircons and other minerals in precambrian granitic rocks, Granite Mountains, Wyoming: Contributions to Mineralogy and Petrology, v. 65, no. 3, p. 243-254, https://doi.org/10.1007/BF00375510.","startPage":"243","endPage":"254","numberOfPages":"12","costCenters":[],"links":[{"id":205290,"rank":9999,"type":{"id":10,"text":"Digital Object Identifier"},"url":"https://dx.doi.org/10.1007/BF00375510"},{"id":222718,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"65","issue":"3","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"505bbdede4b08c986b3292ef","contributors":{"authors":[{"text":"Ludwig, K.R.","contributorId":97112,"corporation":false,"usgs":true,"family":"Ludwig","given":"K.R.","email":"","affiliations":[{"id":218,"text":"Denver Federal Center","active":false,"usgs":true}],"preferred":false,"id":363467,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Stuckless, J. S.","contributorId":6060,"corporation":false,"usgs":true,"family":"Stuckless","given":"J. S.","affiliations":[],"preferred":false,"id":363466,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
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