{"pageNumber":"5272","pageRowStart":"131775","pageSize":"25","recordCount":165309,"records":[{"id":70009768,"text":"70009768 - 1977 - The organic geochemistry of black sedimentary barite: Significance and implications of trapped fatty acids","interactions":[],"lastModifiedDate":"2025-05-27T15:01:27.608064","indexId":"70009768","displayToPublicDate":"2003-04-10T00:00:00","publicationYear":"1977","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":2958,"text":"Organic Geochemistry","active":true,"publicationSubtype":{"id":10}},"title":"The organic geochemistry of black sedimentary barite: Significance and implications of trapped fatty acids","docAbstract":"<p><span>Fatty acids isolated in sedimentary black barite (BaSO</span><sub>4</sub><span>) from Arkansas and Nevada were identified by gas chromatography-mass spectroscopy. The dominant or major fatty acids found in these beds of barite are C</span><sub>16:0</sub><span>, C</span><sub>18:0</sub><span>, and C</span><sub>18:1</sub><span>. The occurrence and distribution of these acids in this type of rock may serve as “molecular fingerprints” of microbial biogeochemical processes. The organic matter and associated microorganisms are shown to be trapped within the finely crystalline barite, thus forming a closed system for microbial diagenesis.</span></p><p><span>Important differences that occur in the distribution of the lesser or minor fatty acids probably result from: (1) the nature of the progenitor organic detritus in the environment of barite deposition: and (2) the subsequent degree of microbiological alteration of the parent organic debris swept into and trapped in the depositional environment.</span></p><p><span>Three general models of sedimentary environments are proposed in which anoxic conditions may prevail and where barium sulfate (BaSO<sub>4</sub>) may precipitate: (1) in a silled basin with semi-restricted circulation; (2) on an outer continental shelf where the slope is encroached upon by water of the oxygen minimum layer; (3) on a low-energy, inner shelf or semi-restricted embayment impinged by a wedge of anoxic water.</span></p><p><span>The major geochemical and geological parameters which are believed to be the significant factors controlling the formation and high grade of these organic-rich, black bedded barites are: (1) a unique source of barium-rich fluid that only contains trace amounts of other elements; (2) the presence of an anoxic bottom environment within the depositional basin; (3) a reflux source of sulfate ion; (4) an adequate source of organic matter.</span></p><div id=\"preview-section-abstract\"><div id=\"abstracts\" class=\"Abstracts u-font-serif\"><div id=\"aep-abstract-id4\" class=\"abstract author\"><div id=\"aep-abstract-sec-id5\"><div class=\"u-margin-s-bottom\">The results of this study may serve as guidelines for future exploration in similar, untested sedimentary basins, especially those with rocks of middle Paleozoic age.</div></div></div></div></div>","language":"English","publisher":"Elsevier","doi":"10.1016/0146-6380(77)90005-5","issn":"01466380","usgsCitation":"Miller, R., Brobst, D., and Beck, P., 1977, The organic geochemistry of black sedimentary barite: Significance and implications of trapped fatty acids: Organic Geochemistry, v. 1, no. 1, p. 11-26, https://doi.org/10.1016/0146-6380(77)90005-5.","productDescription":"16 p.","startPage":"11","endPage":"26","costCenters":[],"links":[{"id":219412,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United States","state":"Arkansas, Nevada","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"coordinates\": [\n          [\n            [\n              -119.946525779522,\n              41.92392900799504\n            ],\n            [\n              -119.92494448500184,\n              38.77192128412841\n            ],\n            [\n              -115.106312449549,\n              35.359933458391424\n            ],\n            [\n              -105.21975936314331,\n              36.72903470007516\n            ],\n            [\n              -94.683700902708,\n              36.0924388118047\n            ],\n            [\n              -94.26257105648864,\n              33.30922133246423\n            ],\n            [\n              -91.0329225003004,\n              32.66552137017362\n            ],\n            [\n              -89.76799531929962,\n              36.750895386489105\n            ],\n            [\n              -113.60074110741138,\n              36.67462457056329\n            ],\n            [\n              -113.78497930050084,\n              41.97629815017764\n            ],\n            [\n              -119.946525779522,\n              41.92392900799504\n            ]\n          ]\n        ],\n        \"type\": \"Polygon\"\n      }\n    }\n  ]\n}","volume":"1","issue":"1","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"505bae5de4b08c986b324040","contributors":{"authors":[{"text":"Miller, R.E.","contributorId":86754,"corporation":false,"usgs":true,"family":"Miller","given":"R.E.","email":"","affiliations":[],"preferred":false,"id":357094,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Brobst, D.A.","contributorId":103688,"corporation":false,"usgs":true,"family":"Brobst","given":"D.A.","affiliations":[],"preferred":false,"id":357095,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Beck, P.C.","contributorId":36285,"corporation":false,"usgs":true,"family":"Beck","given":"P.C.","email":"","affiliations":[],"preferred":false,"id":357093,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":70009875,"text":"70009875 - 1977 - Search for seismic forerunners to earthquakes in central California","interactions":[],"lastModifiedDate":"2025-08-29T16:38:00.182755","indexId":"70009875","displayToPublicDate":"2003-04-10T00:00:00","publicationYear":"1977","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":3525,"text":"Tectonophysics","active":true,"publicationSubtype":{"id":10}},"title":"Search for seismic forerunners to earthquakes in central California","docAbstract":"<p><span>The relatively high seismicity of the San Andreas fault zone in central California provides an excellent opportunity to search for seismic forerunners to moderate earthquakes. Analysis of seismic traveltime and earthquake location data has resulted in the identification of two possible seismic forerunners. The first is a period of apparently late (0.3 sec) P-wave arrival times lasting several weeks preceding one earthquake of magnitude 5.0. The rays for these travel paths passed through — or very close to — the aftershock volume of the subsequent earthquake. The sources for these P-arrival time data were earthquakes in the distance range 20–70 km. Uncertainties in the influence of small changes in the hypocenters of the source earthquakes and in the identification of small P-arrivals raise the possibility that the apparantly delayed arrivals are not the result of a decrease in P-velocity. The second possible precursor is an apparent increase in the average depth of earthquakes preceding two moderate earthquakes. This change might be only apparent, caused by a location bias introduced by a decrease in P-wave velocity, but numerical modeling for realistic possible changes in velocity suggests that the observed effect is more likely a true migration of earthquakes. To carry out this work — involving the manipulation of several thousand earthquake hypocenters and several hundred thousand readings of arrival time — a system of data storage was designed and manipulation programs for a large digital computer have been executed. This system allows, for example, the automatic selection of earthquakes from a specific region, the extraction of all the observed arrival times for these events, and their relocation under a chosen set of assumptions.</span></p>","language":"English","publisher":"Elsevier","doi":"10.1016/0040-1951(77)90163-9","issn":"00401951","usgsCitation":"Wesson, R.L., Robinson, R., Bufe, C., Ellsworth, W., Pfluke, J., Steppe, J., and Seekins, L.C., 1977, Search for seismic forerunners to earthquakes in central California: Tectonophysics, v. 42, no. 2-4, p. 111-126, https://doi.org/10.1016/0040-1951(77)90163-9.","productDescription":"16 p.","startPage":"111","endPage":"126","costCenters":[],"links":[{"id":219269,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United States","state":"California","otherGeospatial":"central California","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"coordinates\": [\n          [\n            [\n              -122.75077435395022,\n              39.095488845528365\n            ],\n            [\n              -120.36360784726932,\n              35.37719892331887\n            ],\n            [\n              -119.70789267854337,\n              35.599454894398846\n            ],\n            [\n              -122.0831329283512,\n              39.20355875635917\n            ],\n            [\n              -122.75077435395022,\n              39.095488845528365\n            ]\n          ]\n        ],\n        \"type\": \"Polygon\"\n      }\n    }\n  ]\n}","volume":"42","issue":"2-4","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"505b884ae4b08c986b3168cf","contributors":{"authors":[{"text":"Wesson, R. L.","contributorId":51752,"corporation":false,"usgs":true,"family":"Wesson","given":"R.","email":"","middleInitial":"L.","affiliations":[],"preferred":false,"id":357334,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Robinson, R.","contributorId":99694,"corporation":false,"usgs":true,"family":"Robinson","given":"R.","affiliations":[],"preferred":false,"id":357338,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Bufe, C. G.","contributorId":79443,"corporation":false,"usgs":true,"family":"Bufe","given":"C. G.","affiliations":[],"preferred":false,"id":357336,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Ellsworth, W.L.","contributorId":48541,"corporation":false,"usgs":true,"family":"Ellsworth","given":"W.L.","email":"","affiliations":[],"preferred":false,"id":357333,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"Pfluke, J. H.","contributorId":77501,"corporation":false,"usgs":true,"family":"Pfluke","given":"J. H.","affiliations":[],"preferred":false,"id":357335,"contributorType":{"id":1,"text":"Authors"},"rank":5},{"text":"Steppe, J.A.","contributorId":22087,"corporation":false,"usgs":true,"family":"Steppe","given":"J.A.","email":"","affiliations":[],"preferred":false,"id":357332,"contributorType":{"id":1,"text":"Authors"},"rank":6},{"text":"Seekins, L. C.","contributorId":99561,"corporation":false,"usgs":true,"family":"Seekins","given":"L.","email":"","middleInitial":"C.","affiliations":[],"preferred":false,"id":357337,"contributorType":{"id":1,"text":"Authors"},"rank":7}]}}
,{"id":70009874,"text":"70009874 - 1977 - Empirical law for fault-creep events","interactions":[],"lastModifiedDate":"2025-08-29T16:48:18.447247","indexId":"70009874","displayToPublicDate":"2003-04-09T00:00:00","publicationYear":"1977","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":3525,"text":"Tectonophysics","active":true,"publicationSubtype":{"id":10}},"title":"Empirical law for fault-creep events","docAbstract":"<p><span>Fault-creep events measured on the San Andreas and related faults near Hollister, California, can be described by a rheological model consisting of a spring, power-law dashpotand sliding block connected in series. An empirical creep-event law, derived from many creep-event records analyzed within the constraints of the model, provides a remarkably simple and accurate representation of creep-event behavior. The empirical creep law is expressed by the equation:&nbsp;</span><i>D</i><span>(</span><i>t</i><span>)=&nbsp;</span><i>D</i><sub><i>f</i></sub><span>&nbsp;[1−1/{</span><i>ct</i><span>(</span><i>n</i><span>−1)</span><i>D</i><sub><i>f</i></sub><sup><i>n</i>−1</sup><span>+1}/</span><sup>(<i>n</i>−1)</sup><span>] where&nbsp;</span><i>D</i><span>&nbsp;is the value of displacement at time&nbsp;</span><i>t</i><span>&nbsp;following the onset of an event,&nbsp;</span><i>D</i><sub><i>f</i></sub><span>&nbsp;is the final equilibrium value of the event displacementand&nbsp;</span><i>C</i><span>&nbsp;is a proportionality constant. This discovery should help determine whether the time—displacement character of creep events is controlled by the material properties of fault gouge, or by other parameters.</span></p>","language":"English","publisher":"Elsevier","doi":"10.1016/0040-1951(77)90024-5","issn":"00401951","usgsCitation":"Crough, S., and Burford, R.O., 1977, Empirical law for fault-creep events: Tectonophysics, v. 42, no. 1, p. T53-T59, https://doi.org/10.1016/0040-1951(77)90024-5.","productDescription":"7 p.","startPage":"T53","endPage":"T59","costCenters":[],"links":[{"id":219194,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United States","state":"California","otherGeospatial":"Melendy Ranch","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"coordinates\": [\n          [\n            [\n              -121.22342633399354,\n              36.6280481223521\n            ],\n            [\n              -121.22342633399354,\n              36.588697570110256\n            ],\n            [\n              -121.16839941118548,\n              36.588697570110256\n            ],\n            [\n              -121.16839941118548,\n              36.6280481223521\n            ],\n            [\n              -121.22342633399354,\n              36.6280481223521\n            ]\n          ]\n        ],\n        \"type\": \"Polygon\"\n      }\n    }\n  ]\n}","volume":"42","issue":"1","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"505a090ae4b0c8380cd51d91","contributors":{"authors":[{"text":"Crough, S.Thomas","contributorId":85317,"corporation":false,"usgs":true,"family":"Crough","given":"S.Thomas","affiliations":[],"preferred":false,"id":357331,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Burford, Robert O.","contributorId":52560,"corporation":false,"usgs":true,"family":"Burford","given":"Robert","middleInitial":"O.","affiliations":[],"preferred":false,"id":357330,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":70010181,"text":"70010181 - 1977 - Geochemistry of Precambrian mafic dikes, central Bighorn Mountains, Wyoming, U.S.A.","interactions":[],"lastModifiedDate":"2025-06-25T16:14:38.396079","indexId":"70010181","displayToPublicDate":"2003-04-08T00:00:00","publicationYear":"1977","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":3112,"text":"Precambrian Research","active":true,"publicationSubtype":{"id":10}},"title":"Geochemistry of Precambrian mafic dikes, central Bighorn Mountains, Wyoming, U.S.A.","docAbstract":"<p>Precambrian quartz dolerites and metadolerites of the central Bighorn Mountains form dikes that intrude a Precambrian metamorphic and igneous terrane typical of the Laramide uplifts of the middle Rocky Mountains. They have a restricted range of major- and trace-element compositions and are typical of basalts in the middle stages of tholeiitic fractionation. Fractionation in the direction of iron enrichment occurred by removal of plagioclase. Average element concentrations of the two groups are nearly identical to one another, are comparable to those in Archean metabasalts from numerous shield areas, and are intermediate between those of modern oceanic tholeiites and continental tholeiites. These average concentrations suggest a depth of magma generation and thickness of crust intermediate between those for the oceanic and continental environments.&nbsp;</p>","language":"English","publisher":"Elsevier","doi":"10.1016/0301-9268(77)90010-9","issn":"03019268","usgsCitation":"Armbrustmacher, T., 1977, Geochemistry of Precambrian mafic dikes, central Bighorn Mountains, Wyoming, U.S.A.: Precambrian Research, v. 4, no. 1, p. 13-38, https://doi.org/10.1016/0301-9268(77)90010-9.","productDescription":"26 p.","startPage":"13","endPage":"38","costCenters":[],"links":[{"id":218632,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United States","state":"Wyoming","otherGeospatial":"Bighorn Mountains","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"coordinates\": [\n          [\n            [\n              -107.91969680894577,\n              44.808138289688515\n            ],\n            [\n              -107.91969680894577,\n              43.983529012844144\n            ],\n            [\n              -106.84232006071421,\n              43.983529012844144\n            ],\n            [\n              -106.84232006071421,\n              44.808138289688515\n            ],\n            [\n              -107.91969680894577,\n              44.808138289688515\n            ]\n          ]\n        ],\n        \"type\": \"Polygon\"\n      }\n    }\n  ]\n}","volume":"4","issue":"1","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"505a16e6e4b0c8380cd552e1","contributors":{"authors":[{"text":"Armbrustmacher, T.J.","contributorId":92642,"corporation":false,"usgs":true,"family":"Armbrustmacher","given":"T.J.","affiliations":[],"preferred":false,"id":358223,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":70010929,"text":"70010929 - 1977 - Suspended particulate loads and transports in the nepheloid layer of the abyssal Atlantic Ocean","interactions":[],"lastModifiedDate":"2025-04-17T17:26:42.165821","indexId":"70010929","displayToPublicDate":"2003-04-01T00:00:00","publicationYear":"1977","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":2667,"text":"Marine Geology","active":true,"publicationSubtype":{"id":10}},"title":"Suspended particulate loads and transports in the nepheloid layer of the abyssal Atlantic Ocean","docAbstract":"<p><span>Vertical profiles of light scattering from over 1000 L-DGO nephelometer stations in the Atlantic Ocean have been used to calculate mass concentrations of suspended particles based on a calibration from the western North American Basin. From these data are plotted the distributions of particulate concentrations at clear water and in the more turbid near-bottom water. Clear water is the broad minimum in concentration and light scattering that occurs at varying mid-depths in the water column. Concentrations at clear water are as much as one-to-two orders of magnitude lower than those in surface water but still reflect a similar geographic distribution: relatively higher concentrations at ocean margins, especially underneath upwelling areas, and the lowest concentrations underneath central gyre areas. These distributions within the clear water reflect surface-water biogenic productivity, lateral injection of particles from shelf areas and surface circulation patterns and require that the combination of downward vertical and horizontal transport processes of particles retain this pattern throughout the upper water column.</span></p><p><span>Below clear water, the distribution of standing crops of suspended particulate concentrations in the lower water column are presented. The integration of mass of all particles per unit area (gross particulate standing crop) reflects a relative distribution similar to that at the surface and at clear water levels, superimposed on which is the strong imprint of boundary currents along the western margins of the Atlantic. Reducing the gross particulate standing crop by the integral of the concentration of clear water yields a net particulate standing crop. The distribution of this reflects primarily the interaction of circulating abyssal waters with the ocean bottom, i.e. a strong nepheloid layer which is coincident with western boundary currents and which diminishes in intensity equatorward.</span></p><p><span>The resuspended particulate loads in the nepheloid layer of the basins west of the Mid-Atlantic Ridge, resulting from interaction of abyssal currents with the bottom, range from ∼ 2 · 10<sup>6</sup>&nbsp;tons in the equatorial Guyana Basin to ∼ 50 · 10<sup>6</sup>&nbsp;tons in the North American Basin. The total resuspended particulate load in the western basins (111 · 10<sup>6</sup>&nbsp;tons) is almost an order of magnitude greater than that in the basins east of the Mid-Atlantic Ridge (13 · 10<sup>6</sup>&nbsp;tons). The net northward flux of resuspended particles carried in the AABW drops from ∼ 8 · 10<sup>6</sup>&nbsp;tons/year between the southern and northern ends of the Brazil Basin and remains ∼ 1 · 10<sup>6</sup>&nbsp;tons/year across the Guyana Basin.</span></p>","language":"English","publisher":"Elsevier","doi":"10.1016/0025-3227(77)90087-1","issn":"00253227","usgsCitation":"Biscaye, P., and Eittreim, S., 1977, Suspended particulate loads and transports in the nepheloid layer of the abyssal Atlantic Ocean: Marine Geology, v. 23, no. 1-2, p. 155-172, https://doi.org/10.1016/0025-3227(77)90087-1.","productDescription":"18 p.","startPage":"155","endPage":"172","costCenters":[],"links":[{"id":221786,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"23","issue":"1-2","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"505ba2fee4b08c986b31fae3","contributors":{"authors":[{"text":"Biscaye, P.E.","contributorId":16979,"corporation":false,"usgs":true,"family":"Biscaye","given":"P.E.","affiliations":[],"preferred":false,"id":359908,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Eittreim, S.L.","contributorId":98730,"corporation":false,"usgs":true,"family":"Eittreim","given":"S.L.","affiliations":[],"preferred":false,"id":359909,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":70009782,"text":"70009782 - 1977 - Determination of 30 elements in coal and fly ash by thermal and epithermal neutron-activation analysis","interactions":[],"lastModifiedDate":"2025-08-13T16:17:13.902517","indexId":"70009782","displayToPublicDate":"2002-01-22T00:00:00","publicationYear":"1977","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":3517,"text":"Talanta","active":true,"publicationSubtype":{"id":10}},"title":"Determination of 30 elements in coal and fly ash by thermal and epithermal neutron-activation analysis","docAbstract":"<p>Thirty elements are determined in coal and fly ash by instrumental neutron-activation analysis using both thermal and epithermal irradiation. Gamma-ray spectra were recorded 7 and 20 days after the irradiations. The procedure is applicable to the routine analysis of coals and fly ash. Epithermal irradiation was found preferable for the determination of Ni, Zn, As, Se, Br, Rb, Sr, Mo, Sb, Cs, Ba, Sm, Tb, Hf, Ta, W, Th and U, whereas thermal irradiation was best for Sc, Cr, Fe, Co, La, Ce, Nd, Eu, Yb and Lu. Results for SRM 1632 (coal) and SRM 1633 (fly ash) agree with those of other investigators.&nbsp;</p>","language":"English","publisher":"Elsevier","doi":"10.1016/0039-9140(77)80125-2","issn":"00399140","usgsCitation":"Rowe, J., and Steinnes, E., 1977, Determination of 30 elements in coal and fly ash by thermal and epithermal neutron-activation analysis: Talanta, v. 24, no. 7, p. 433-439, https://doi.org/10.1016/0039-9140(77)80125-2.","productDescription":"7 p.","startPage":"433","endPage":"439","costCenters":[],"links":[{"id":219646,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"24","issue":"7","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"5059ff86e4b0c8380cd4f232","contributors":{"authors":[{"text":"Rowe, J.J.","contributorId":29460,"corporation":false,"usgs":true,"family":"Rowe","given":"J.J.","affiliations":[],"preferred":false,"id":357125,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Steinnes, E.","contributorId":79603,"corporation":false,"usgs":false,"family":"Steinnes","given":"E.","affiliations":[],"preferred":false,"id":357126,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":7821,"text":"ofr77131 - 1977 - Explanation to accompany preliminary map showing bedrock geology superposed on an aeromagnetic base map of the Worcester region, Massachusetts, Connecticut, and Rhode Island","interactions":[],"lastModifiedDate":"2014-03-25T08:18:08","indexId":"ofr77131","displayToPublicDate":"1994-01-01T07:00:00","publicationYear":"1977","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":"77-131","title":"Explanation to accompany preliminary map showing bedrock geology superposed on an aeromagnetic base map of the Worcester region, Massachusetts, Connecticut, and Rhode Island","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Reston, VA","doi":"10.3133/ofr77131","collaboration":"Prepared in cooperation with the Commonwealth of Massachusetts Department of Public Works, The State of Connecticut Geologic and Natural History Survey and U.S. Nuclear Regulatory Commission","usgsCitation":"Barosh, P.J., 1977, Explanation to accompany preliminary map showing bedrock geology superposed on an aeromagnetic base map of the Worcester region, Massachusetts, Connecticut, and Rhode Island: U.S. Geological Survey Open-File Report 77-131, Plate 1: 19.29 x 25.69 inches; Plate 2: 19.43 x 26.85 inches, https://doi.org/10.3133/ofr77131.","productDescription":"Plate 1: 19.29 x 25.69 inches; Plate 2: 19.43 x 26.85 inches","costCenters":[],"links":[{"id":283385,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/ofr77131.png"},{"id":284485,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1977/0131/plate-1.pdf"},{"id":284486,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1977/0131/plate-2.pdf"}],"scale":"125000","country":"United States","state":"Connecticut;Massachusetts;Rhode Island","otherGeospatial":"Worcester Region","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -73.0,41.875 ], [ -73.0,42.5 ], [ -71.5,42.5 ], [ -71.5,41.875 ], [ -73.0,41.875 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"53cd58cce4b0b290850f8507","contributors":{"authors":[{"text":"Barosh, Patrick James","contributorId":42184,"corporation":false,"usgs":true,"family":"Barosh","given":"Patrick","email":"","middleInitial":"James","affiliations":[],"preferred":false,"id":156673,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":37640,"text":"tp92 - 1977 - Verification of a model for predicting the effect of inconstant temperature on embryonic development of lake whitefish (Coregonus clupeaformis)","interactions":[],"lastModifiedDate":"2012-02-02T00:10:01","indexId":"tp92","displayToPublicDate":"1994-01-01T01:00:00","publicationYear":"1977","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":1,"text":"Federal Government Series"},"seriesTitle":{"id":89,"text":"Technical Paper","active":false,"publicationSubtype":{"id":1}},"seriesNumber":"92","title":"Verification of a model for predicting the effect of inconstant temperature on embryonic development of lake whitefish (Coregonus clupeaformis)","docAbstract":"Eggs stripped from lake whitefish (Coregonus clupeaformis) spawning in Lake Michigan were incubated in the laboratory at temperatures similar to those on whitefish spawning grounds in Lake Michigan during December-April. Observed times from fertilization to attainment of each of 21 developmental stages were used to test a model that predicts the rate of development at daily fluctuating temperatures; the model relates rate of development for any given stage j, expressed as the reciprocal of time (Rj), to temperature (T). The generalized equation for a developmental stage is Rj = abTcT??.\nObserved times agreed well (5.5% mean difference for all stages) with times predicted by the model; the observed time of 135 days from fertilization to hatching (stage 21) was only 5 days (3.7%) less than the predicted time of 140 days. The model was further verified by applying it to unpublished data supplied by the Ontario Ministry of Natural Resources, for eggs from Lake Huron whitefish incubated in the laboratory in untempered Lake Huron water.\nThe model was used to predict the effects of small temperature increases (caused by a hypothetical waste-heat discharge) on the rate of development and time of hatching of lake whitefish eggs. According to this simulation, continuous addition of waste heat sufficient to raise the temperature 1, 2, or 3 C above ambient on the spawning grounds during December-April would advance the time of hatching 8, 16, or 21 days, respectively. Possible effects of this advancement on the reproductive success of whitefish are discussed.","language":"ENGLISH","publisher":"U.S. Fish and Wildlife Service","collaboration":"Out-of-print","usgsCitation":"Berlin, W.H., Brooke, L., and Stone, L.J., 1977, Verification of a model for predicting the effect of inconstant temperature on embryonic development of lake whitefish (Coregonus clupeaformis): Technical Paper 92, [2], 6 p. : graph ; 26 cm.","productDescription":"[2], 6 p. : graph ; 26 cm.","numberOfPages":"6","costCenters":[{"id":324,"text":"Great Lakes Science Center","active":true,"usgs":true}],"links":[{"id":112290,"rank":9999,"type":{"id":10,"text":"Digital Object Identifier"},"url":"https://hdl.handle.net/2027/uc1.31822006841605?urlappend=%3Bseq=479"},{"id":161735,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a13e4b07f02db602221","contributors":{"authors":[{"text":"Berlin, William H.","contributorId":15574,"corporation":false,"usgs":true,"family":"Berlin","given":"William","email":"","middleInitial":"H.","affiliations":[],"preferred":false,"id":218386,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Brooke, L.T.","contributorId":60589,"corporation":false,"usgs":true,"family":"Brooke","given":"L.T.","email":"","affiliations":[],"preferred":false,"id":218388,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Stone, Linda J.","contributorId":30173,"corporation":false,"usgs":true,"family":"Stone","given":"Linda","email":"","middleInitial":"J.","affiliations":[],"preferred":false,"id":218387,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":69280,"text":"a7 - 1977 - Reconnaissance geologic map of the Guest Peninsula Quadrangle, Marie Byrd Land, Antarctica","interactions":[],"lastModifiedDate":"2012-02-10T00:11:32","indexId":"a7","displayToPublicDate":"1994-01-01T01:00:00","publicationYear":"1977","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":305,"text":"Antarctic Map","code":"A","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"7","title":"Reconnaissance geologic map of the Guest Peninsula Quadrangle, Marie Byrd Land, Antarctica","language":"ENGLISH","publisher":"U.S. Geological Survey","publisherLocation":"Reston, VA","doi":"10.3133/a7","usgsCitation":"Wade, F., Cathey, C., and Oldham, J., 1977, Reconnaissance geologic map of the Guest Peninsula Quadrangle, Marie Byrd Land, Antarctica: U.S. Geological Survey Antarctic Map 7, 1 Sheet, 29 x 43 inches, https://doi.org/10.3133/a7.","productDescription":"1 Sheet, 29 x 43 inches","costCenters":[],"links":[{"id":112492,"rank":100,"type":{"id":15,"text":"Index Page"},"url":"https://repository.agic.umn.edu/maps/usgs/geologic/a7_guest_peninsula/","linkFileType":{"id":5,"text":"html"}},{"id":251474,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/a/07/report.pdf","size":"71","linkFileType":{"id":1,"text":"pdf"}},{"id":251475,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/a/07/plate-1.pdf","size":"7067","linkFileType":{"id":1,"text":"pdf"}},{"id":252448,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/a/07/report-thumb.jpg"}],"scale":"250000","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -152,-77 ], [ -152,-76 ], [ -144,-76 ], [ -144,-77 ], [ -152,-77 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b04e4b07f02db698ff6","contributors":{"authors":[{"text":"Wade, F.A.","contributorId":85261,"corporation":false,"usgs":true,"family":"Wade","given":"F.A.","email":"","affiliations":[],"preferred":false,"id":279967,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Cathey, C.A.","contributorId":88028,"corporation":false,"usgs":true,"family":"Cathey","given":"C.A.","email":"","affiliations":[],"preferred":false,"id":279968,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Oldham, J.B.","contributorId":7362,"corporation":false,"usgs":true,"family":"Oldham","given":"J.B.","email":"","affiliations":[],"preferred":false,"id":279966,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":62077,"text":"a5 - 1977 - Reconnaissance geologic map of the Alexandra Mountains Quadrangle, Marie Byrd Land, Antarctica","interactions":[],"lastModifiedDate":"2012-02-10T00:10:45","indexId":"a5","displayToPublicDate":"1994-01-01T01:00:00","publicationYear":"1977","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":305,"text":"Antarctic Map","code":"A","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"5","title":"Reconnaissance geologic map of the Alexandra Mountains Quadrangle, Marie Byrd Land, Antarctica","language":"ENGLISH","publisher":"U.S. Geological Survey","publisherLocation":"Reston, VA","doi":"10.3133/a5","usgsCitation":"Wade, F.A., Cathey, C.A., and Oldham, J.B., 1977, Reconnaissance geologic map of the Alexandra Mountains Quadrangle, Marie Byrd Land, Antarctica: U.S. Geological Survey Antarctic Map 5, 1 Sheet, 32 x 32 inches, https://doi.org/10.3133/a5.","productDescription":"1 Sheet, 32 x 32 inches","costCenters":[],"links":[{"id":112494,"rank":100,"type":{"id":15,"text":"Index Page"},"url":"https://repository.agic.umn.edu/maps/usgs/geologic/a5_alexandra_mountains/","linkFileType":{"id":5,"text":"html"}},{"id":248270,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/a/05/report.pdf","size":"71","linkFileType":{"id":1,"text":"pdf"}},{"id":248271,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/a/05/plate-1.pdf","size":"3666","linkFileType":{"id":1,"text":"pdf"}},{"id":253085,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/a/05/report-thumb.jpg"}],"scale":"250000","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -156,-78.25 ], [ -156,-77 ], [ -150,-77 ], [ -150,-78.25 ], [ -156,-78.25 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a73e4b07f02db64371f","contributors":{"authors":[{"text":"Wade, F. Alton","contributorId":104143,"corporation":false,"usgs":true,"family":"Wade","given":"F.","email":"","middleInitial":"Alton","affiliations":[],"preferred":false,"id":266878,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Cathey, Carl A.","contributorId":83202,"corporation":false,"usgs":true,"family":"Cathey","given":"Carl","email":"","middleInitial":"A.","affiliations":[],"preferred":false,"id":266877,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Oldham, Jerry B.","contributorId":40279,"corporation":false,"usgs":true,"family":"Oldham","given":"Jerry","email":"","middleInitial":"B.","affiliations":[],"preferred":false,"id":266876,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":62071,"text":"a6 - 1977 - Reconnaissance geologic map of the Boyd Glacier Quadrangle, Marie Byrd Land, Antarctica","interactions":[],"lastModifiedDate":"2012-02-10T00:10:45","indexId":"a6","displayToPublicDate":"1994-01-01T01:00:00","publicationYear":"1977","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":305,"text":"Antarctic Map","code":"A","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"6","title":"Reconnaissance geologic map of the Boyd Glacier Quadrangle, Marie Byrd Land, Antarctica","language":"ENGLISH","publisher":"U.S. Geological Survey","publisherLocation":"Reston, VA","doi":"10.3133/a6","usgsCitation":"Wade, F., Cathey, C., and Oldham, J., 1977, Reconnaissance geologic map of the Boyd Glacier Quadrangle, Marie Byrd Land, Antarctica: U.S. Geological Survey Antarctic Map 6, 1 Sheet, 29 x 44 inches, https://doi.org/10.3133/a6.","productDescription":"1 Sheet, 29 x 44 inches","costCenters":[],"links":[{"id":112493,"rank":100,"type":{"id":15,"text":"Index Page"},"url":"https://repository.agic.umn.edu/maps/usgs/geologic/a6_boyd_glacier/","linkFileType":{"id":5,"text":"html"}},{"id":248260,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/a/06/report.pdf","size":"71","linkFileType":{"id":1,"text":"pdf"}},{"id":248261,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/a/06/plate-1.pdf","size":"6205","linkFileType":{"id":1,"text":"pdf"}},{"id":253080,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/a/06/report-thumb.jpg"}],"scale":"250000","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -152,-78 ], [ -152,-77 ], [ -144,-77 ], [ -144,-78 ], [ -152,-78 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a72e4b07f02db6432b0","contributors":{"authors":[{"text":"Wade, F.A.","contributorId":85261,"corporation":false,"usgs":true,"family":"Wade","given":"F.A.","email":"","affiliations":[],"preferred":false,"id":266860,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Cathey, C.A.","contributorId":88028,"corporation":false,"usgs":true,"family":"Cathey","given":"C.A.","email":"","affiliations":[],"preferred":false,"id":266861,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Oldham, J.B.","contributorId":7362,"corporation":false,"usgs":true,"family":"Oldham","given":"J.B.","email":"","affiliations":[],"preferred":false,"id":266859,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":62609,"text":"gq1432 - 1977 - Geologic map of the Waterford quadrangle, north-central Kentucky","interactions":[],"lastModifiedDate":"2012-02-10T00:10:44","indexId":"gq1432","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1977","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":316,"text":"Geologic Quadrangle","code":"GQ","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"1432","title":"Geologic map of the Waterford quadrangle, north-central Kentucky","language":"ENGLISH","doi":"10.3133/gq1432","usgsCitation":"Luft, S.J., 1977, Geologic map of the Waterford quadrangle, north-central Kentucky: U.S. Geological Survey Geologic Quadrangle 1432, col. map ;58 x 46 cm. on sheet 78 x 95 cm. fold. in envelope 31 x 25 cm., https://doi.org/10.3133/gq1432.","productDescription":"col. map ;58 x 46 cm. on sheet 78 x 95 cm. fold. in envelope 31 x 25 cm.","costCenters":[],"links":[{"id":107856,"rank":700,"type":{"id":15,"text":"Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_10966.htm","linkFileType":{"id":5,"text":"html"},"description":"10966"},{"id":248768,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/gq/1432/report.pdf","size":"36","linkFileType":{"id":1,"text":"pdf"}},{"id":254078,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/gq/1432/report-thumb.jpg"}],"geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -85.5,38 ], [ -85.5,38.1175 ], [ -85.36749999999999,38.1175 ], [ -85.36749999999999,38 ], [ -85.5,38 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ae4e4b07f02db68a0b1","contributors":{"authors":[{"text":"Luft, Stanley J.","contributorId":30634,"corporation":false,"usgs":true,"family":"Luft","given":"Stanley","email":"","middleInitial":"J.","affiliations":[],"preferred":false,"id":267610,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":64708,"text":"i1016 - 1977 - Leasable mineral and waterpower land classification map of the Kalispell 1° x 2° quadrangle, Montana","interactions":[{"subject":{"id":46424,"text":"ofr74171 - 1974 - Leasable mineral and waterpower land classification map, Kalispell Quadrangle, Montana, showing lands withdrawn, classified, and valuable prospectively for leasable minerals and occurrences of other selected minerals, lands withdrawn or classified for waterpower and reservoir sites","indexId":"ofr74171","publicationYear":"1974","noYear":false,"title":"Leasable mineral and waterpower land classification map, Kalispell Quadrangle, Montana, showing lands withdrawn, classified, and valuable prospectively for leasable minerals and occurrences of other selected minerals, lands withdrawn or classified for waterpower and reservoir sites"},"predicate":"SUPERSEDED_BY","object":{"id":64708,"text":"i1016 - 1977 - Leasable mineral and waterpower land classification map of the Kalispell 1° x 2° quadrangle, Montana","indexId":"i1016","publicationYear":"1977","noYear":false,"title":"Leasable mineral and waterpower land classification map of the Kalispell 1° x 2° quadrangle, Montana"},"id":1}],"lastModifiedDate":"2021-11-01T21:31:07.268529","indexId":"i1016","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1977","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":320,"text":"IMAP","code":"I","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"1016","title":"Leasable mineral and waterpower land classification map of the Kalispell 1° x 2° quadrangle, Montana","docAbstract":"<p>No abstract available.</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/i1016","usgsCitation":"Bateman, A., Allen, E.G., and Giles, G.C., 1977, Leasable mineral and waterpower land classification map of the Kalispell 1° x 2° quadrangle, Montana: U.S. Geological Survey IMAP 1016, 1 Plate: 31.42 × 22.99 inches, https://doi.org/10.3133/i1016.","productDescription":"1 Plate: 31.42 × 22.99 inches","costCenters":[],"links":[{"id":391241,"rank":4,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_8888.htm"},{"id":255134,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/imap/1016/report-thumb.jpg"},{"id":255133,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/imap/1016/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":255132,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/imap/1016/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}}],"scale":"250000","country":"United States","state":"Montana","otherGeospatial":"Kalispell 1° x 2° quadrangle","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -116,48 ], [ -116,49 ], [ -114,49 ], [ -114,48 ], [ -116,48 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b1ae4b07f02db6a8205","contributors":{"authors":[{"text":"Bateman, A. F. Jr.","contributorId":24411,"corporation":false,"usgs":true,"family":"Bateman","given":"A. F.","suffix":"Jr.","affiliations":[],"preferred":false,"id":272015,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Allen, E. G.","contributorId":78379,"corporation":false,"usgs":true,"family":"Allen","given":"E.","email":"","middleInitial":"G.","affiliations":[],"preferred":false,"id":272016,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Giles, G. C.","contributorId":19622,"corporation":false,"usgs":true,"family":"Giles","given":"G.","email":"","middleInitial":"C.","affiliations":[],"preferred":false,"id":272014,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
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