{"pageNumber":"5837","pageRowStart":"145900","pageSize":"25","recordCount":184617,"records":[{"id":70188833,"text":"70188833 - 1978 - A paleolimnological comparison of Burntside and Shagawa Lakes, northeastern Minnesota","interactions":[],"lastModifiedDate":"2017-06-26T10:00:51","indexId":"70188833","displayToPublicDate":"1978-12-31T00:00:00","publicationYear":"1978","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":1,"text":"Federal Government Series"},"seriesTitle":{"id":5436,"text":"Ecological Research Series","active":true,"publicationSubtype":{"id":1}},"seriesNumber":"EPA-600/3-78-004 ","title":"A paleolimnological comparison of Burntside and Shagawa Lakes, northeastern Minnesota","docAbstract":"<p>The paleolimnological records of Burntside and Shagawa Lakes in northeastern Minnesota reveal that these two adjacent lakes have been limnologically distinct for many years prior to the late 19th century activities of white men that polluted Shagawa Lake. Although both lakes occur within the same vegetation type and share much of their water, the diatom stratigraphy of their bottom sediments indicates that Burntside Lake was less productive in its natural state than Shagawa Lake. The causes for this natural difference are not clearly known, but differences in relative size of drainage area and in bedrock geology may he responsible. </p><p>Intensive white settlement around Shagawa Lake beginning in 1866 supplied nutrients that increased its productivity and finally supported the massive blooms of blue-green algae that characterize culturally eutrophic lakes. Burntside Lake was spared such intensive eutrophication, but its diatom record shows that nutrients derived from shoreside recreational cabins and related construction activity are increasing the lake's productivity. </p><p>The results of this study show that paleolimnological studies may provide better comparative information for lake rehabilitation programs than do biological and chemical analyses of contemporary unpolluted water bodies. </p>","language":"English","publisher":"Environmental Protection Agency","usgsCitation":"Bradbury, J.P., and Waddington, J., 1978, A paleolimnological comparison of Burntside and Shagawa Lakes, northeastern Minnesota: Ecological Research Series EPA-600/3-78-004 , x, 51 p.","productDescription":"x, 51 p.","costCenters":[],"links":[{"id":342855,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United States","state":"Minnesota","county":"St. Louis County","otherGeospatial":"Burntside Lake, 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Platt","contributorId":91106,"corporation":false,"usgs":true,"family":"Bradbury","given":"J.","email":"","middleInitial":"Platt","affiliations":[],"preferred":false,"id":700555,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Waddington, Jean","contributorId":193473,"corporation":false,"usgs":false,"family":"Waddington","given":"Jean","email":"","affiliations":[],"preferred":false,"id":700556,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":70207380,"text":"70207380 - 1978 - A computer-assisted graphical method for identification and correlation of igneous rock chemistries","interactions":[],"lastModifiedDate":"2020-06-03T15:12:24.719967","indexId":"70207380","displayToPublicDate":"1978-12-18T13:25:02","publicationYear":"1978","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1796,"text":"Geology","active":true,"publicationSubtype":{"id":10}},"title":"A computer-assisted graphical method for identification and correlation of igneous rock chemistries","docAbstract":"<p>We have devised a computer-assisted graphical method for correlating chemical analyses in suites of related igneous rocks. The method provides a direct and empirical means of sample identification using all of the reported chemistry. In a study of basalt of the Columbia River plateau, the method has been used for (1) checking field identifications of rocks, (2) spotting analytical errors in analyses of samples of known chemical type, (3) identifying repetitions of chemistry in thick stratigraphic sections, and (4) matching analyses of dikes to those of flows that the dikes may have fed.</p><p>Program OXVAR creates a set of oxide-oxide variation diagrams on a CALCOMP plotter; any oxide may be used as the base (for example, MgO, SiO<sub>2</sub>). For each oxide-oxide variation diagram, program CTSET creates the smallest convex polygon that encloses all the data points as well as a larger polygon that takes into account the error in determination of each data point. A set of nested polygons, one for each oxide, then represents a chemical type. Program CTYPE identifies unknown analyses by comparing them with all defined chemical types. If all the elements or oxides of an analysis plot within the defined polygons for a given chemical type, then an identification is printed. If at least one element of an analysis falls outside the set of polygons defined for each chemical type, then “unidentified” is printed, and qualitative information on the amount of deviation from the defined chemical types is given.</p>","language":"English","publisher":"GSA","doi":"10.1130/0091-7613(1978)6<16:ACGMFI>2.0.CO;2","usgsCitation":"Wright, T., and Hamilton, M., 1978, A computer-assisted graphical method for identification and correlation of igneous rock chemistries: Geology, v. 6, no. 1, p. 14-20, https://doi.org/10.1130/0091-7613(1978)6<16:ACGMFI>2.0.CO;2.","productDescription":"5 p.","startPage":"14","endPage":"20","costCenters":[{"id":617,"text":"Volcano Science Center","active":true,"usgs":true}],"links":[{"id":370421,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"6","issue":"1","noUsgsAuthors":false,"publicationStatus":"PW","contributors":{"authors":[{"text":"Wright, Thomas L. twright@usgs.gov","contributorId":3890,"corporation":false,"usgs":true,"family":"Wright","given":"Thomas L.","email":"twright@usgs.gov","affiliations":[{"id":617,"text":"Volcano Science Center","active":true,"usgs":true}],"preferred":true,"id":777867,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Hamilton, M.S.","contributorId":221332,"corporation":false,"usgs":false,"family":"Hamilton","given":"M.S.","email":"","affiliations":[],"preferred":false,"id":777868,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":70119871,"text":"70119871 - 1978 - The IFG incremental methodology for physical instream habitat evaluation","interactions":[],"lastModifiedDate":"2014-08-11T10:39:10","indexId":"70119871","displayToPublicDate":"1978-12-03T10:38:00","publicationYear":"1978","noYear":false,"publicationType":{"id":4,"text":"Book"},"publicationSubtype":{"id":12,"text":"Conference publication"},"title":"The IFG incremental methodology for physical instream habitat evaluation","largerWorkTitle":"Surface Mining and Fish/Wildlife Needs in the Eastern United States: Proceedings of a Symposium","conferenceTitle":"Surface mining and fish/wildlife needs in the Eastern United States","conferenceDate":"1978-12-03T00:00:00","conferenceLocation":"Morgantown, WV","language":"English","publisher":"Department of the Interior, Fish and Wildlife Service","publisherLocation":"Washington, D.C.","usgsCitation":"Stalnaker, C., 1978, The IFG incremental methodology for physical instream habitat evaluation.","costCenters":[],"links":[{"id":291942,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"53e9d8d4e4b008eaa4f3f698","contributors":{"authors":[{"text":"Stalnaker, Clair B.","contributorId":30871,"corporation":false,"usgs":true,"family":"Stalnaker","given":"Clair B.","affiliations":[],"preferred":false,"id":497818,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":70221506,"text":"70221506 - 1978 - Biostratigraphy and evolution of the Momipites‐Caryapollenites lineage in the early tertiary in the Wind River Basin, Wyoming","interactions":[],"lastModifiedDate":"2021-06-21T11:43:53.686408","indexId":"70221506","displayToPublicDate":"1978-12-01T17:29:22","publicationYear":"1978","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":3006,"text":"Palynology","active":true,"publicationSubtype":{"id":10}},"title":"Biostratigraphy and evolution of the Momipites‐Caryapollenites lineage in the early tertiary in the Wind River Basin, Wyoming","docAbstract":"<p>Sequential morphologic changes in pollen of the<span>&nbsp;</span><i>Momipites‐Caryapollenites</i><span>&nbsp;</span>lineage from Paleocene strata in the Wind River Basin of Wyoming appear to reflect evolution within the family Juglandaceae. The stratigraphic occurrence of the species within this complex permits the establishment of six biostratigraphic zones that can be correlated between outcropping and subsurface sequences within the basin and to surrounding areas.</p><p>Trends involving changes in shape and size of the pollen and in structure of exine at the poles proceed from a basic form of<span>&nbsp;</span><i>Momipites</i><span>&nbsp;</span>to six other distinguishable species. The genus<span>&nbsp;</span><i>Caryapollenites</i><span>&nbsp;</span>appears to have been derived from the basic form of<span>&nbsp;</span><i>Momipites</i><span>&nbsp;</span>by changes in size and development of heteropolarity in pore position.</p><p>Species of<span>&nbsp;</span><i>Momipites</i><span>&nbsp;</span>described as new are<span>&nbsp;</span><i>M. wyomingensis, M. waltmanensis, M. ventifluminis, M. actinus, M. anellus,</i><span>&nbsp;</span>and<span>&nbsp;</span><i>M, leffingwellii.</i><span>&nbsp;</span>The genus<span>&nbsp;</span><i>Caryapollenites</i><span>&nbsp;</span>is redescribed and<span>&nbsp;</span><i>C. prodromus, C. imparalis, C. inelegans,</i><span>&nbsp;</span>and<span>&nbsp;</span><i>C. wodehousei</i><span>&nbsp;</span>are described as new.</p>","language":"English","publisher":"Taylor & Francis","doi":"10.1080/01916122.1978.9989167","usgsCitation":"Nichols, D.J., and Ott, H.L., 1978, Biostratigraphy and evolution of the Momipites‐Caryapollenites lineage in the early tertiary in the Wind River Basin, Wyoming: Palynology, v. 2, no. 1, p. 93-112, https://doi.org/10.1080/01916122.1978.9989167.","productDescription":"20 p.","startPage":"93","endPage":"112","costCenters":[],"links":[{"id":386601,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United States","state":"Wyoming","otherGeospatial":"Wind River Basin","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -110.21484375,\n              41.77131167976407\n            ],\n            [\n              -104.58984375,\n              41.77131167976407\n            ],\n            [\n              -104.58984375,\n              44.59046718130883\n            ],\n            [\n              -110.21484375,\n              44.59046718130883\n            ],\n            [\n              -110.21484375,\n              41.77131167976407\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","volume":"2","issue":"1","noUsgsAuthors":false,"publicationStatus":"PW","contributors":{"authors":[{"text":"Nichols, Douglas J.","contributorId":87184,"corporation":false,"usgs":true,"family":"Nichols","given":"Douglas","email":"","middleInitial":"J.","affiliations":[],"preferred":false,"id":817895,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Ott, Henry L.","contributorId":260407,"corporation":false,"usgs":false,"family":"Ott","given":"Henry","email":"","middleInitial":"L.","affiliations":[],"preferred":false,"id":817896,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":70114658,"text":"70114658 - 1978 - Summaries of technical reports, volume VII","interactions":[],"lastModifiedDate":"2014-07-15T14:12:27","indexId":"70114658","displayToPublicDate":"1978-12-01T13:58:00","publicationYear":"1978","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"title":"Summaries of technical reports, volume VII","docAbstract":"No abstract available.","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/70114658","collaboration":"Prepared by Participants in the National Earthquake Hazards Reduction Program","usgsCitation":"Evernden, J.F., Seiders, W., and Thomson, J., 1978, Summaries of technical reports, volume VII, 544 p., https://doi.org/10.3133/70114658.","productDescription":"544 p.","numberOfPages":"551","costCenters":[],"links":[{"id":290166,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":290165,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/unnumbered/70114658/report.pdf"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"53ad40ffe4b0729c154181db","contributors":{"authors":[{"text":"Evernden, Jack F.","contributorId":45950,"corporation":false,"usgs":true,"family":"Evernden","given":"Jack","email":"","middleInitial":"F.","affiliations":[],"preferred":false,"id":495398,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Seiders, Wanda","contributorId":34050,"corporation":false,"usgs":true,"family":"Seiders","given":"Wanda","affiliations":[],"preferred":false,"id":495397,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Thomson, Jean","contributorId":75856,"corporation":false,"usgs":true,"family":"Thomson","given":"Jean","affiliations":[],"preferred":false,"id":495399,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":70209704,"text":"70209704 - 1978 - Origin of a South Texas roll-type uranium deposit; I, Alteration of iron-titanium oxide minerals","interactions":[],"lastModifiedDate":"2020-04-21T17:34:49.361483","indexId":"70209704","displayToPublicDate":"1978-12-01T12:31:05","publicationYear":"1978","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1472,"text":"Economic Geology","active":true,"publicationSubtype":{"id":10}},"title":"Origin of a South Texas roll-type uranium deposit; I, Alteration of iron-titanium oxide minerals","docAbstract":"<p><span>The detrital Fe-Ti oxide minerals and their authigenic alteration products in samples from cores spanning 1.7 km across a roll-type uranium deposit in the mid-Tertiary Catahoula Tuff, south Texas, record important information on host-rock preparation and on development of the altered tongue of the deposit. In reduced rock, in front of and enveloping the altered tongue, iron disulfide minerals (pyrite and marcasite) have partially to completely replaced titanomagnetite and, to a lesser extent, titanohematite. Subsequent oxidation of these sulfidized Fe-Ti oxides, by processes that formed the altered tongue and uranium roll, produced ferric oxide and hydroxide phases (limonite) pseudomorphous after the sulfides. Fe-Ti oxides 1.0 km updip from the roll front were never sulfidized; titanomagnetite (partly replaced by hematite) and martite constitute nearly half of the heavy mineral fraction and limonite is absent. Oxidized rocks 210 m and closer to the nose of the roll front, however, are nearly devoid of titanomagnetite and contain abundant limonite. The redox interface that bounds the altered tongue, therefore, moved more than 210 m but less than 1.0 km. Detrital Fe-Ti oxide minerals are increasingly sulfidized in the downdip direction indicating that initial sulfidizaton was more intense in that direction. Organic carbon content is uniformly very low throughout the host sandstone, which implies that heterotrophic sulfate-reducing bacteria were not involved in the generation of sulfide. The H&nbsp;</span><sub>2</sub><span>&nbsp;S for the initial sulfidization may have been derived from oil and gas in formations that underlie the Catahoula Tuff. The H&nbsp;</span><sub>2</sub><span>&nbsp;S probably invaded the Catahoula along a fault that is 1.5 km downdip from the present roll front.</span></p>","language":"English","publisher":"Society of Economic Geologists","doi":"10.2113/gsecongeo.73.8.1677","usgsCitation":"Reynolds, R.L., and Goldhaber, M.B., 1978, Origin of a South Texas roll-type uranium deposit; I, Alteration of iron-titanium oxide minerals: Economic Geology, v. 73, no. 8, p. 1677-1689, https://doi.org/10.2113/gsecongeo.73.8.1677.","productDescription":"13 p.","startPage":"1677","endPage":"1689","costCenters":[{"id":318,"text":"Geosciences and Environmental Change Science Center","active":true,"usgs":true}],"links":[{"id":374169,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United States","state":"Texas","county":"Webb 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,{"id":70170196,"text":"70170196 - 1978 - Status of projects in Minnesota fiscal year 1978","interactions":[],"lastModifiedDate":"2018-02-14T11:24:07","indexId":"70170196","displayToPublicDate":"1978-12-01T12:30:00","publicationYear":"1978","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":6,"text":"USGS Unnumbered Series"},"title":"Status of projects in Minnesota fiscal year 1978","docAbstract":"<p>No abstract available.</p>","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"St. Paul, MN","doi":"10.3133/70170196","usgsCitation":"Adolphson, D.G., and Jannis, J.A., 1978, Status of projects in Minnesota fiscal year 1978, 101 p., https://doi.org/10.3133/70170196.","productDescription":"101 p.","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[{"id":392,"text":"Minnesota Water Science 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,{"id":5221447,"text":"5221447 - 1978 - Short-tailed shrews: Toxicity and residue relationships of DDT, dieldrin, and endrin","interactions":[],"lastModifiedDate":"2023-12-13T14:32:02.043443","indexId":"5221447","displayToPublicDate":"1978-12-01T12:19:30","publicationYear":"1978","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":887,"text":"Archives of Environmental Contamination and Toxicology","active":true,"publicationSubtype":{"id":10}},"title":"Short-tailed shrews: Toxicity and residue relationships of DDT, dieldrin, and endrin","docAbstract":"<p>Experiments involving dietary toxicity and residue relationships of DDT, dieldrin, and endrin were conducted with short-tailed shrews. Dietary concentrations of DDT dissolved in vegetable oils were usually more toxic than diets containing comparable amounts of powdered DDT. Younger shrews, particularly females, were more tolerant of powdered DDT than older animals; yet, there were no conspicuous age differences in toxicity of DDT dissolved in oils. In comparison to other mammals, short-tailed shrews are not unusually sensitive to DDT, dieldrin, or endrin on the basis of two-week feeding tests.</p><p>The influence of age and sex on toxicity of DDT, endrin, and dieldrin was sometimes more important than body weight. Of those shrews of the same age and sex that were fed the same dietary dosage, heavier shrews were more tolerant than lighter individuals; and, heavier shrews tended to lose a greater percentage of body weight before death.</p><p>There was a range of 15 to 105 DDT equivalents in brains of shrews dying on dietary dosages of DDT. Six shrews fed a high level of DDT seemed to have unusual metabolite capabilities and died with apparent lethal levels of DDD in their brains. Levels of dieldrin in brains of shrews that died on a dietary dosage of dieldrin ranged from 3.7 to 12.6 ppm.</p><p>In the rates of gain and loss experiments where shrews were given diets containing 400 ppm DDT or 50 ppm dieldrin up to 17 days, high residues were noted in tissues of shrews after two weeks on a contaminated diet and a few died at that time. After shrews were placed on clean food, it was determined that &gt;50% of the dieldrin residues in carcass and brain were lost in &lt;2 weeks. Males and females fed DDT for 17 days lost &gt;50% of residues of DDT and metabolites in brains after 2 weeks on clean food; males lost nearly 50% of residues in carcasses after two weeks on clean food compared with a loss of only 11% in females.</p>","language":"English","publisher":"Springer","doi":"10.1007/BF02332040","usgsCitation":"Blus, L.J., 1978, Short-tailed shrews: Toxicity and residue relationships of DDT, dieldrin, and endrin: Archives of Environmental Contamination and Toxicology, v. 7, no. 1, p. 83-98, https://doi.org/10.1007/BF02332040.","productDescription":"16 p.","startPage":"83","endPage":"98","numberOfPages":"16","costCenters":[{"id":531,"text":"Patuxent Wildlife Research Center","active":true,"usgs":true}],"links":[{"id":199428,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"7","issue":"1","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e49bee4b07f02db5d1336","contributors":{"authors":[{"text":"Blus, Lawrence J.","contributorId":35199,"corporation":false,"usgs":true,"family":"Blus","given":"Lawrence","email":"","middleInitial":"J.","affiliations":[],"preferred":false,"id":333869,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":70209702,"text":"70209702 - 1978 - Origin of a South Texas roll-type deposit; II, Sulfide petrology and sulfur isotope studies","interactions":[],"lastModifiedDate":"2020-04-21T17:22:20.754421","indexId":"70209702","displayToPublicDate":"1978-12-01T12:18:55","publicationYear":"1978","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1472,"text":"Economic Geology","active":true,"publicationSubtype":{"id":10}},"title":"Origin of a South Texas roll-type deposit; II, Sulfide petrology and sulfur isotope studies","docAbstract":"<p><span>Petrologic and sulfur isotopic studies have been carried out on drill core samples from a roll-type uranium deposit in the mid-Tertiary Catahoula Tuff, Webb County, south Texas. Epigenetic iron disulfide minerals formed in two distinct stages. The first stage involved sulfidization of the host rock by sulfide (H&nbsp;</span><sub>2</sub><span>&nbsp;S, HS-)-bearing solutions that emanated from a fault about 1.5 km downdip from and subparallel to the orebody. Pyrite was the dominant iron disulfide mineral formed from this fault sulfide. The isotopic composition (delta&nbsp;</span><sup>34</sup><span>&nbsp;S) of first-stage iron disulfide is quite heavy (&gt;0 per mil), in part because the fault-derived H&nbsp;</span><sub>2</sub><span>&nbsp;S was isotopically heavy. The development of the second-stage sulfides was related to processes that formed the uranium roll. Iron disulfide minerals produced during this second stage commonly occur as rims around the first-stage sulfides. The rims are exclusively marcasite in and adjacent to ore, but the pyrite content in these rims increases with increasing distance from ore. The sulfur of the second-stage sulfides in the vicinity of the roll front is isotopically light (--25 to --40 per mil). The virtual absence of organic carbon in the host sand precludes a bacterial origin for the ore-stage iron disulfide minerals and, therefore, eliminates bacterial metabolism as the mechanism for isotopic fractionation. Instead, the sulfur source for ore-stage sulfides was preore (first stage) sulfides, remobilized via partial oxidation to soluble metastable sulfur oxyanions.</span></p>","language":"English","publisher":"Society of Economic Geologists","doi":"10.2113/gsecongeo.73.8.1690","usgsCitation":"Goldhaber, M.B., Reynolds, R.L., and Rye, R.O., 1978, Origin of a South Texas roll-type deposit; II, Sulfide petrology and sulfur isotope studies: Economic Geology, v. 73, no. 8, p. 1690-1705, https://doi.org/10.2113/gsecongeo.73.8.1690.","productDescription":"16 p.","startPage":"1690","endPage":"1705","costCenters":[{"id":318,"text":"Geosciences and Environmental Change Science Center","active":true,"usgs":true}],"links":[{"id":374167,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United States","state":"Texas","county":"Webb 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Martin B. 0000-0002-1785-4243 mgold@usgs.gov","orcid":"https://orcid.org/0000-0002-1785-4243","contributorId":1339,"corporation":false,"usgs":true,"family":"Goldhaber","given":"Martin","email":"mgold@usgs.gov","middleInitial":"B.","affiliations":[{"id":211,"text":"Crustal Geophysics and Geochemistry Science Center","active":true,"usgs":true},{"id":171,"text":"Central Mineral and Environmental Resources Science Center","active":true,"usgs":true}],"preferred":true,"id":787603,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Reynolds, Richard L. 0000-0002-4572-2942 rreynolds@usgs.gov","orcid":"https://orcid.org/0000-0002-4572-2942","contributorId":139068,"corporation":false,"usgs":true,"family":"Reynolds","given":"Richard","email":"rreynolds@usgs.gov","middleInitial":"L.","affiliations":[{"id":318,"text":"Geosciences and Environmental Change Science Center","active":true,"usgs":true}],"preferred":true,"id":787604,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Rye, Robert O. rrye@usgs.gov","contributorId":1486,"corporation":false,"usgs":true,"family":"Rye","given":"Robert","email":"rrye@usgs.gov","middleInitial":"O.","affiliations":[{"id":211,"text":"Crustal Geophysics and Geochemistry Science Center","active":true,"usgs":true}],"preferred":true,"id":787605,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":70119876,"text":"70119876 - 1978 - Results of testing four methods of habitat evaluation","interactions":[],"lastModifiedDate":"2014-08-11T10:58:40","indexId":"70119876","displayToPublicDate":"1978-12-01T10:55:00","publicationYear":"1978","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":9,"text":"Other Report"},"title":"Results of testing four methods of habitat evaluation","docAbstract":"No abstract available.","largerWorkType":{"id":18,"text":"Report"},"largerWorkTitle":"Report to the Project Impact Evaluation Team, Division of Ecological Services","largerWorkSubtype":{"id":9,"text":"Other Report"},"language":"English","publisher":"University of Missouri","publisherLocation":"Columbia, MO","usgsCitation":"Ellis, J., Burroughs, J., Arumbruster, M., Hallett, D., Korte, P., and Baskett, T., 1978, Results of testing four methods of habitat evaluation, 100 p.","productDescription":"100 p.","numberOfPages":"100","costCenters":[],"links":[{"id":291947,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"53e9d8d4e4b008eaa4f3f686","contributors":{"authors":[{"text":"Ellis, J.A.","contributorId":77856,"corporation":false,"usgs":true,"family":"Ellis","given":"J.A.","email":"","affiliations":[],"preferred":false,"id":497831,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Burroughs, J.N.","contributorId":72717,"corporation":false,"usgs":true,"family":"Burroughs","given":"J.N.","email":"","affiliations":[],"preferred":false,"id":497830,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Arumbruster, M.J.","contributorId":22703,"corporation":false,"usgs":true,"family":"Arumbruster","given":"M.J.","email":"","affiliations":[],"preferred":false,"id":497828,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Hallett, D.L.","contributorId":63736,"corporation":false,"usgs":true,"family":"Hallett","given":"D.L.","email":"","affiliations":[],"preferred":false,"id":497829,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"Korte, P.A.","contributorId":96601,"corporation":false,"usgs":true,"family":"Korte","given":"P.A.","email":"","affiliations":[],"preferred":false,"id":497833,"contributorType":{"id":1,"text":"Authors"},"rank":5},{"text":"Baskett, T.S.","contributorId":83081,"corporation":false,"usgs":true,"family":"Baskett","given":"T.S.","email":"","affiliations":[],"preferred":false,"id":497832,"contributorType":{"id":1,"text":"Authors"},"rank":6}]}}
,{"id":70236553,"text":"70236553 - 1978 - Lithologic analysis of the 1–2mm sand fraction","interactions":[],"lastModifiedDate":"2022-10-07T13:51:16.332567","indexId":"70236553","displayToPublicDate":"1978-12-01T10:40:37","publicationYear":"1978","noYear":false,"publicationType":{"id":5,"text":"Book chapter"},"publicationSubtype":{"id":24,"text":"Book Chapter"},"title":"Lithologic analysis of the 1–2mm sand fraction","docAbstract":"<p>No abstract available.</p>","largerWorkType":{"id":18,"text":"Report"},"largerWorkTitle":"Standard procedures for evaluation of Quaternary materials in Iowa","largerWorkSubtype":{"id":2,"text":"State or Local Government Series"},"language":"English","publisher":"Iowa Geological Survey","usgsCitation":"Lucas, J.R., Hallberg, G.R., Chauff, K.M., and Howes, M., 1978, Lithologic analysis of the 1–2mm sand fraction, chap. <i>of</i> Standard procedures for evaluation of Quaternary materials in Iowa, p. 23-30.","productDescription":"8 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M.","contributorId":296390,"corporation":false,"usgs":false,"family":"Chauff","given":"Karl","email":"","middleInitial":"M.","affiliations":[],"preferred":false,"id":851381,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Howes, Mary","contributorId":100871,"corporation":false,"usgs":true,"family":"Howes","given":"Mary","email":"","affiliations":[],"preferred":false,"id":851382,"contributorType":{"id":1,"text":"Authors"},"rank":4}]}}
,{"id":1007845,"text":"1007845 - 1978 - Endocrine function and reproductive impairment in an irradiated population of the lizard Uta stansburiana","interactions":[],"lastModifiedDate":"2025-07-14T15:49:28.306027","indexId":"1007845","displayToPublicDate":"1978-12-01T00:00:00","publicationYear":"1978","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":3224,"text":"Radiation Research","active":true,"publicationSubtype":{"id":10}},"title":"Endocrine function and reproductive impairment in an irradiated population of the lizard Uta stansburiana","docAbstract":"<p><span>This study describes gonadal changes in lizards (</span><i>Uta stansburiana</i><span>) exposed to chronic low levels of γ radiation (1.5-10 R/day) under field conditions and attempts to evaluate endocrine involvement in these changes. Reproductive impairment in irradiated males is demonstrated during the breeding season by reduced testes weights and by seminiferous tubules devoid of germ cells. Ultrastructural morphology of Leydig cells, plasma testosterone levels, and developed accessory sex structures indicate normal steroidogenesis in such males; cytology of the pituitary gonadotropes and pituitary gonadotropin content indicate normal gonadotropin levels. These findings suggest that low levels of radiation affect the spermatogenic process directly, rather than through damage to the pituitary. Comparable irradiation causes complete resorption of ovarian tissue in some female&nbsp;</span><i>Uta</i><span>. The oviducts are atrophic and the pituitary gonadotropes hyperactive. Resemblance of gonadotropes to those of castrated animals and reduced pituitary hormone content suggest elevated levels of gonadotropin production, probably due to the absence of ovarian steroid feedback in affected animals. The continued mitotic activity of oogonia in adult reptiles and their limited number contribute to the vulnerability of germinal tissue in irradiated female lizards. Destruction of the germ cells is accompanied by resorption of all ovarian tissue including steroidogenic elements. Thus, in females as in males, radiation appears to damage gametogenesis rather than pituitary function.</span></p>","language":"English","publisher":"Allen Press","doi":"10.2307/3574809","usgsCitation":"Pearson, A., Licht, P., Nagy, K., and Medica, P., 1978, Endocrine function and reproductive impairment in an irradiated population of the lizard Uta stansburiana: Radiation Research, v. 76, no. 3, p. 610-623, https://doi.org/10.2307/3574809.","productDescription":"14 p.","startPage":"610","endPage":"623","costCenters":[{"id":651,"text":"Western Ecological Research Center","active":true,"usgs":true}],"links":[{"id":130600,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United States","state":"Nevada","county":"Nye County","otherGeospatial":"Rock Valley","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"coordinates\": [\n          [\n            [\n              -114.9074944517024,\n              36.74023583000064\n            ],\n            [\n              -114.9074944517024,\n              36.346000827668476\n            ],\n            [\n              -114.04922320356249,\n              36.346000827668476\n            ],\n            [\n              -114.04922320356249,\n              36.74023583000064\n            ],\n            [\n              -114.9074944517024,\n              36.74023583000064\n            ]\n          ]\n        ],\n        \"type\": \"Polygon\"\n      }\n    }\n  ]\n}","volume":"76","issue":"3","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a16e4b07f02db603d1c","contributors":{"authors":[{"text":"Pearson, A.K.","contributorId":88691,"corporation":false,"usgs":true,"family":"Pearson","given":"A.K.","email":"","affiliations":[],"preferred":false,"id":316136,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Licht, P.","contributorId":55386,"corporation":false,"usgs":true,"family":"Licht","given":"P.","email":"","affiliations":[],"preferred":false,"id":316134,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Nagy, K.A.","contributorId":39727,"corporation":false,"usgs":true,"family":"Nagy","given":"K.A.","email":"","affiliations":[],"preferred":false,"id":316133,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Medica, P.A.","contributorId":77079,"corporation":false,"usgs":true,"family":"Medica","given":"P.A.","email":"","affiliations":[],"preferred":false,"id":316135,"contributorType":{"id":1,"text":"Authors"},"rank":4}]}}
,{"id":70156378,"text":"70156378 - 1978 - Holocene pyroclastic-flow deposits from Shastina and Black Butte, west of Mount Shasta, California","interactions":[],"lastModifiedDate":"2015-08-20T14:29:24","indexId":"70156378","displayToPublicDate":"1978-11-30T18:00:00","publicationYear":"1978","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":2446,"text":"Journal of Research of the U.S. Geological Survey","active":true,"publicationSubtype":{"id":10}},"title":"Holocene pyroclastic-flow deposits from Shastina and Black Butte, west of Mount Shasta, California","docAbstract":"<p>A broad apron of pyroclastic-flow deposits derived from dacitic domes of Holocene age at Black Butte and Shastina covers an area of more than 110 km<sup>2</sup> on the west flank of Mt. Shasta volcano. The stratigraphy of the deposits is exposed in readouts along a northwest-southeast line between the cities of Weed and Mount Shasta and includes, from bottom to top, pre-Shastina diamictons, a Shastina pyroclasticflow assemblage, and a Black Butte pyroclastic-flow assemblage. Pyroclastic flows from Shastina, a volcanic cone on the west flank of Mt. Shasta, form a fan of nonvesicular rock debris that overlies part of the Shastina cone and pre-Shastina deposits; the fan deposits thicken northward and underlie the town of Weed. Pyroclastic-flow deposits of both vesicular and nonvesicular rock debris caused by eruptions at the site of Black Butte, a large volcanic dome at the foot of Mt. Shasta, thicken southward and underlie part of the city of Mount Shasta. Soil-profile oxidation is 75-80 cm thick on deposits from both Shastina and Black Butte. As much as 10 m of vertical displacement occurred along east-trending faults 3.5 km northwest of Black Butte after deposition of the youngest two pyroclastic flows from that source. Evidence that faulting and volcanism were nearly simultaneous suggests that the area northwest of Black Butte subsided during a late eruptive phase of the plug dome. Future eruptions similar to those that produced the pyroclastic flows could endanger people and property in any direction downslope from vents, including the communities of Weed and Mount Shasta and possibly other communities in the Shasta Valley and upper Sacramento River area.</p>","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Arlington, VA","usgsCitation":"Miller, C.D., 1978, Holocene pyroclastic-flow deposits from Shastina and Black Butte, west of Mount Shasta, California: Journal of Research of the U.S. Geological Survey, v. 6, no. 5, p. 611-623.","productDescription":"13 p.","startPage":"611","endPage":"623","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[],"links":[{"id":307032,"rank":1,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/journal/1978/vol6issue5/report.pdf","text":"Report","size":"31.11 MB","linkFileType":{"id":1,"text":"pdf"},"description":"Report"},{"id":307040,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United States","state":"California","city":"Weed, Mount Shasta","otherGeospatial":"Black Butte, Shastina","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -122.2,\n              41.34\n            ],\n            [\n              -122.2,\n              41.45\n            ],\n            [\n              -122.42,\n              41.45\n            ],\n            [\n              -122.42,\n              41.34\n            ],\n            [\n              -122.2,\n              41.34\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","volume":"6","issue":"5","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"55d6fa33e4b0518e3546bc49","contributors":{"authors":[{"text":"Miller, C. Dan","contributorId":38145,"corporation":false,"usgs":true,"family":"Miller","given":"C.","email":"","middleInitial":"Dan","affiliations":[],"preferred":false,"id":568943,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":70156361,"text":"70156361 - 1978 - Petrographic differentiation of depositional environments of sandstones of the Pennsylvanian Breathitt Formation, northeastern Kentucky and southwestern West Virginia","interactions":[],"lastModifiedDate":"2015-08-20T14:28:01","indexId":"70156361","displayToPublicDate":"1978-11-30T18:00:00","publicationYear":"1978","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":2446,"text":"Journal of Research of the U.S. Geological Survey","active":true,"publicationSubtype":{"id":10}},"title":"Petrographic differentiation of depositional environments of sandstones of the Pennsylvanian Breathitt Formation, northeastern Kentucky and southwestern West Virginia","docAbstract":"<p>Petrographic properties of sandstone samples from the lower and middle Pennsylvanian Breathitt Formation in northeastern Kentucky and southwestern West Virginia were utilized to classify their environments of deposition. Simultaneous consideration of mineral composition, grain size, and sorting of the sandstones by using stepwise multiple discriminant-function analysis has permitted differentiation between alluvial-plain and delta-plain sandstones. Stepwise multiple discriminant-function analysis of the sandstone samples- was performed in two parts. The first analysis assigned the sandstones of all grain-size classes to one of three environments of deposition: (1) alluvial plain, (2) upper delta plain, and (3) lower delta plain. The second analysis classed the sandstones by grain size and subdivided each grain-size class into these environmental groups. Discriminant analyses of sandstones of all grain-size classes led to correct assignment of depositional environment to 76 percent of the samples. Analyses of the sandstones classed by grain size led to correct classification of 67 percent of the medium-grained sandstones, 83 percent of the fine-grained sandstones, and 91 percent of the very fine grained sandstones. The discriminantfunction method was adopted to classify the depositional environment and stratigraphic position of test sandstone samples. Analyses of fine-grained and very fine grained sandstones resulted in correct classification of 84 percent of the test samples to their depositional setting and stratigraphic position. The best discrimination is offered by analyses of fine-grained sandstones, which resulted in correct classification of 88 percent of the samples. Thus, this statistical method can be adopted as a powerful tool for exploration programs that concern delineation of genetically similar sandstones.</p>","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Arlington, VA","usgsCitation":"Flores, R.M., 1978, Petrographic differentiation of depositional environments of sandstones of the Pennsylvanian Breathitt Formation, northeastern Kentucky and southwestern West Virginia: Journal of Research of the U.S. Geological Survey, v. 6, no. 5, p. 593-602.","productDescription":"10 p.","startPage":"593","endPage":"602","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[],"links":[{"id":307005,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"},{"id":307004,"rank":1,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/journal/1978/vol6issue5/report.pdf","text":"Report","size":"31.11 MB","linkFileType":{"id":1,"text":"pdf"},"description":"Report"}],"country":"United States","state":"Kentucky, Virginia","otherGeospatial":"Breathitt Formation","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -82.86849975585938,\n              37.85696502054439\n            ],\n            [\n              -82.86849975585938,\n              38.16533520012289\n            ],\n            [\n              -82.47093200683594,\n              38.16533520012289\n            ],\n            [\n              -82.47093200683594,\n              37.85696502054439\n            ],\n            [\n              -82.86849975585938,\n              37.85696502054439\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","volume":"6","issue":"5","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"55d6fa37e4b0518e3546bc54","contributors":{"authors":[{"text":"Flores, Romeo M. rflores@usgs.gov","contributorId":71984,"corporation":false,"usgs":true,"family":"Flores","given":"Romeo","email":"rflores@usgs.gov","middleInitial":"M.","affiliations":[{"id":165,"text":"Central Energy Resources Team","active":false,"usgs":true}],"preferred":false,"id":568886,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":70156366,"text":"70156366 - 1978 - Ferroaxinites from the Feather River area, northern California, and from the McGrath and Russian Mission quadrangles, Alaska","interactions":[],"lastModifiedDate":"2015-08-20T14:28:41","indexId":"70156366","displayToPublicDate":"1978-11-30T18:00:00","publicationYear":"1978","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":2446,"text":"Journal of Research of the U.S. Geological Survey","active":true,"publicationSubtype":{"id":10}},"title":"Ferroaxinites from the Feather River area, northern California, and from the McGrath and Russian Mission quadrangles, Alaska","docAbstract":"<p>In the Feather River area, California, and in the McGrath quadrangle, Alaska, axinite-bearing veins occur as fracture fillings along or near the fault zones, suggesting that boron was introduced along the fractures. An unusual occurrence of axinite as a possible primary constituent of a plutonic rock is in the Russian Mission quadrangle, Alaska. The four analyzed axinites from these widely different localities and from different host rocks are surprisingly similar in chemistry and optics. All are ferroaxinites, having high iron and low manganese and magnesium contents. The number of calcium ions is very close to two, which is in agreement with the idealized formula Ca<sub>2 </sub>(Fe,Mn,Mg)Al<sub>2</sub>BSi<sub>4</sub>O<sub>15</sub>(OH). The indices of refraction increase slightly with increasing FeO:MgO ratio over the small range studied.</p>","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Arlington, VA","usgsCitation":"Hietanen, A., and Erd, R.C., 1978, Ferroaxinites from the Feather River area, northern California, and from the McGrath and Russian Mission quadrangles, Alaska: Journal of Research of the U.S. Geological Survey, v. 6, no. 5, p. 603-609.","productDescription":"7 p.","startPage":"603","endPage":"609","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[],"links":[{"id":307013,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"},{"id":307007,"rank":1,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/journal/1978/vol6issue5/report.pdf","text":"Report","size":"31.11 MB","linkFileType":{"id":1,"text":"pdf"},"description":"Report"}],"country":"United States","state":"California, Alaska","otherGeospatial":"Feather River, McGrath and Russian Mission Quadrangles","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -121.49574279785156,\n              39.65751331590311\n            ],\n            [\n              -121.49574279785156,\n              39.92395554100352\n            ],\n            [\n              -120.95466613769531,\n              39.92395554100352\n            ],\n            [\n              -120.95466613769531,\n              39.65751331590311\n            ],\n            [\n              -121.49574279785156,\n              39.65751331590311\n            ]\n          ]\n        ]\n      }\n    },\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -162,\n              61\n            ],\n            [\n              -162,\n              62\n            ],\n            [\n              -159,\n              62\n            ],\n            [\n              -159,\n              61\n            ],\n            [\n              -162,\n              61\n            ]\n          ]\n        ]\n      }\n    },\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -156,\n              63\n            ],\n            [\n              -153,\n              63\n            ],\n            [\n              -153,\n              62\n            ],\n            [\n              -156,\n              62\n            ],\n            [\n              -156,\n              63\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","volume":"6","issue":"5","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"55d6fa32e4b0518e3546bc3e","contributors":{"authors":[{"text":"Hietanen, Anna","contributorId":43841,"corporation":false,"usgs":true,"family":"Hietanen","given":"Anna","affiliations":[],"preferred":false,"id":568895,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Erd, Richard C.","contributorId":89899,"corporation":false,"usgs":true,"family":"Erd","given":"Richard","email":"","middleInitial":"C.","affiliations":[],"preferred":false,"id":568896,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":70156426,"text":"70156426 - 1978 - Late Miocene mollusks from the Queen Charlotte Islands, British Columbia, Canada","interactions":[],"lastModifiedDate":"2015-08-21T10:52:33","indexId":"70156426","displayToPublicDate":"1978-11-30T18:00:00","publicationYear":"1978","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":2446,"text":"Journal of Research of the U.S. Geological Survey","active":true,"publicationSubtype":{"id":10}},"title":"Late Miocene mollusks from the Queen Charlotte Islands, British Columbia, Canada","docAbstract":"<p>A fauna of bivalve mollusks, scattered gastropods, and an echinoid from exposures of the Skonun Formation in the northeastern part of Graham Island is indicative of an early late Miocene age and correlation with the provincial Wishkahan Stage. The molluscan assemblages are from the upper 600 of the 1800-m-thick marine and nonmarine formation, which appears to be entirely of late Miocene age. The Skonun Formation is the strandline fa.cies of marginal marine and nonmarine deposits of the northwestern part of the Queen Charlotte basin, a Nieogene embayment paralleling the modern mainland coast. The molluscan fauna and associated lignite beds are known from a few widely scattered outcrops; they are indicative of alternating marine and nonmarine to brackish-water environments in the upper part of the formation. The Skonun fauna occurs near the northern boundary of the Pacific Northwest Neogene molluscan province. It is the only marine Neogene molluscan fauna known from the British Columbia coast. The fauna has strong taxonomic ties with the fauna of the Empire Formation of southwestern Oregon and has several species in common with the upper Miocene of the Lituya district, southeastern Alaska, implying that these three faunas are coeval.</p>","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Arlington, VA","usgsCitation":"Addicott, W.O., 1978, Late Miocene mollusks from the Queen Charlotte Islands, British Columbia, Canada: Journal of Research of the U.S. Geological Survey, v. 6, no. 5, p. 677-689.","productDescription":"13 p.","startPage":"677","endPage":"689","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[],"links":[{"id":307118,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"},{"id":307111,"rank":1,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/journal/1978/vol6issue5/report.pdf","text":"Report","size":"31.11 MB","linkFileType":{"id":1,"text":"pdf"},"description":"Report"}],"country":"Canada","otherGeospatial":"Queen Charlotte Islands, Graham Island","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -133.22296142578125,\n              53.1237017988457\n            ],\n            [\n              -133.22296142578125,\n              54.27645123048291\n            ],\n            [\n              -131.81396484375,\n              54.27645123048291\n            ],\n            [\n              -131.81396484375,\n              53.1237017988457\n            ],\n            [\n              -133.22296142578125,\n              53.1237017988457\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","volume":"6","issue":"5","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"55d84bb9e4b0518e3546f01a","contributors":{"authors":[{"text":"Addicott, Warren O.","contributorId":80668,"corporation":false,"usgs":true,"family":"Addicott","given":"Warren","email":"","middleInitial":"O.","affiliations":[],"preferred":false,"id":569135,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":70156385,"text":"70156385 - 1978 - Geometry and rates of change of fault-generated range fronts, north-central Nevada","interactions":[],"lastModifiedDate":"2015-08-20T14:30:23","indexId":"70156385","displayToPublicDate":"1978-11-30T18:00:00","publicationYear":"1978","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":2446,"text":"Journal of Research of the U.S. Geological Survey","active":true,"publicationSubtype":{"id":10}},"title":"Geometry and rates of change of fault-generated range fronts, north-central Nevada","docAbstract":"<p>Characteristic features of fault-generated range fronts, such as those on the Humboldt and Tobin Ranges, include sets of elongate basins extending normal to the range crest, interbasin spurs having crests sloping 10&deg; to 20&deg; toward the range front, spur facets having slopes of 25&deg; to 35&deg;, basin headwalls having slopes of 20&deg; to 30&deg;, and a basal fault scarp. The basal fault scarp is rejuvenated by vertical movements recurring at intervals on the order of 10 000 years. Fault scarps in colluvium that lie within a few tens of meters of the base of faceted spurs remain clearly recognizable for only a few tens of thousand years. Initial fault-scarp slopes of 50&deg; to 90&deg; are replaced by debris-controlled slopes of 30&deg; to 37&deg; within a few thousand years. In fractured bedrock, slope angles in the range of 25&deg; to 35&deg; remain relatively stable for hundreds of thousands of years and account for the relative stability of facets on spurs. Piedmont slopes are greatly affected by tectonic tilting or warping toward or away from the range front. The formation of pediments is believed to result from a low ratio of uplift relative to downcutting. A few million years is required for the development of a pediment a few kilometers wide.</p>","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Arlington, AV","usgsCitation":"Wallace, R.E., 1978, Geometry and rates of change of fault-generated range fronts, north-central Nevada: Journal of Research of the U.S. Geological Survey, v. 6, no. 5, p. 637-649.","productDescription":"13 p.","startPage":"637","endPage":"649","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[],"links":[{"id":307042,"rank":1,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/journal/1978/vol6issue5/report.pdf","text":"Report","size":"31.11 MB","linkFileType":{"id":1,"text":"pdf"},"description":"Report"},{"id":307043,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United States","state":"Nevada","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -118.3,\n             40\n            ],\n            [\n              -118.3,\n              41\n            ],\n            [\n              -116,\n              41\n            ],\n            [\n              -116,\n              40\n            ],\n            [\n              -118.3,\n              40\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","volume":"6","issue":"5","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"55d6fa32e4b0518e3546bc40","contributors":{"authors":[{"text":"Wallace, Robert E.","contributorId":15570,"corporation":false,"usgs":true,"family":"Wallace","given":"Robert","email":"","middleInitial":"E.","affiliations":[],"preferred":false,"id":568981,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":70156388,"text":"70156388 - 1978 - <i>Tribolbina</i> Latham, 1932, an early Carboniferous through Permian palaeocopid ostracode genus","interactions":[],"lastModifiedDate":"2015-08-20T14:52:13","indexId":"70156388","displayToPublicDate":"1978-11-30T18:00:00","publicationYear":"1978","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":2446,"text":"Journal of Research of the U.S. Geological Survey","active":true,"publicationSubtype":{"id":10}},"title":"<i>Tribolbina</i> Latham, 1932, an early Carboniferous through Permian palaeocopid ostracode genus","docAbstract":"<p>The type-species of <i>Tribolbina</i> Latham, 1932, <i>T. carnegiei</i>, and <i>T. gigantea</i> (Jones, Kirkby, and Brady, 1884) are redefined and reillustrated, and lectotypes for both are designated. <i>T. permiana</i> (Kellett, 1933) and <i>T. tumida</i> (Scott and Borger, 1941) are also redefined and reillustrated. <i>Beyrichiana</i> Kellett, 1933, is considered a junior subjective synonym of <i>Tribolbina</i> Latham, 1932. On the basis of abundant silicified specimens from the Permian of Greece, <i>T. doescheri</i> n. sp. is described, and <i>T.</i> aff. <i>T. doescheri</i> and <i>T</i>. sp. 1 are illustrated. The stratigraphic range of <i>Tribolbina</i> as redefined is lower Carboniferous through Permian, and its known distribution is Europe and North America where representatives lived in shallow seas. Tribolbinidae and Tribolbinecea are established as new suprageneric categories in the Palaeocopida for<i> Tribolbina</i> and the Silurian <i>Kolmodinia</i> Martinsson, 1962.</p>","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Arlington, VA","usgsCitation":"Sohn, I.G., 1978, <i>Tribolbina</i> Latham, 1932, an early Carboniferous through Permian palaeocopid ostracode genus: Journal of Research of the U.S. Geological Survey, v. 6, no. 5, p. 663-675.","productDescription":"13 p.","startPage":"663","endPage":"675","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[],"links":[{"id":307051,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"},{"id":307046,"rank":1,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/journal/1978/vol6issue5/report.pdf","text":"Report","size":"31.11 MB","linkFileType":{"id":1,"text":"pdf"},"description":"Report"}],"country":"Greece","otherGeospatial":"Episkopi","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              23.79638671875,\n              34.867904962568716\n            ],\n            [\n              23.79638671875,\n              35.382332329032984\n            ],\n            [\n              26.3397216796875,\n              35.382332329032984\n            ],\n            [\n              26.3397216796875,\n              34.867904962568716\n            ],\n            [\n              23.79638671875,\n              34.867904962568716\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","volume":"6","issue":"5","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"55d6fa2ae4b0518e3546bbfe","contributors":{"authors":[{"text":"Sohn, I. G.","contributorId":70751,"corporation":false,"usgs":true,"family":"Sohn","given":"I.","email":"","middleInitial":"G.","affiliations":[],"preferred":false,"id":568984,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":70156349,"text":"70156349 - 1978 - Regional gravity and magnetic anomalies in the eastern Snake River Plain, Idaho","interactions":[],"lastModifiedDate":"2015-11-02T11:37:49","indexId":"70156349","displayToPublicDate":"1978-11-30T18:00:00","publicationYear":"1978","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":2446,"text":"Journal of Research of the U.S. Geological Survey","active":true,"publicationSubtype":{"id":10}},"title":"Regional gravity and magnetic anomalies in the eastern Snake River Plain, Idaho","docAbstract":"<p>Over the eastern Snake River Plain, the Bouguer gravity anomaly and the magnetic intensity are, in general, high. In detail, both the gravity and the magnetic anomalies are a complex of highs and lows, in contrast to the simpler anomalies over the western Snake River Plain. The broad gravity high associated with the eastern Snake River Plain cannot be produced by a dense mass at shallow depth under the plain, but must be produced either by a deep feature under the plain or by a broader, shallower feature extending well beyond the plain. The high could be produced by a thinning of the crust under the plain by 4.5 to 7 kilometers. The data suggest that the Cenozoic rocks of the plain are underlain by rocks that have density and magnetization similar to the density and magnetization of the pre-Cenozoic rocks north and south of the plain. The data do not suggest rifting of the upper crust such as is inferred for the western Snake River Plain. The plain is in approximate isostatic equilibrium with adjoining regions to the north and south and thus contrasts with the adjoining areas where the basin-and-range topography is not in isostatic equilibrium. The local gravity anomalies on the plain are probably produced by variations in the thickness of Cenozoic rocks, but the wavelength of the anomalies is about twice that of the basin-and-range structural features in areas adjoining the plain. The gravity expression of basin-and-range structural features does not extend far onto the plain. Magnetic anomalies on the plain are produced by Cenozoic volcanic rocks.</p>","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Arlington, VA","usgsCitation":"Mabey, D.R., 1978, Regional gravity and magnetic anomalies in the eastern Snake River Plain, Idaho: Journal of Research of the U.S. Geological Survey, v. 6, no. 5, p. 553-562.","productDescription":"10 p.","startPage":"553","endPage":"562","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[],"links":[{"id":306987,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"},{"id":306986,"rank":1,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/journal/1978/vol6issue5/report.pdf","text":"Report","size":"31.11 MB","linkFileType":{"id":1,"text":"pdf"},"description":"Report"}],"country":"United States","state":"Idaho","otherGeospatial":"Snake River Plain","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {\n        \"stroke\": \"#555555\",\n        \"stroke-width\": 2,\n        \"stroke-opacity\": 1,\n        \"fill\": \"#555555\",\n        \"fill-opacity\": 0.5\n      },\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -114.246826171875,\n              42.032974332441405\n            ],\n            [\n              -112.994384765625,\n              42.2366518803206\n            ],\n            [\n              -111.7529296875,\n              43.26120612479979\n            ],\n            [\n              -111.39038085937499,\n              43.77902662160831\n            ],\n            [\n              -111.368408203125,\n              44.04811573082351\n            ],\n            [\n              -111.961669921875,\n              44.23732831822538\n            ],\n            [\n              -112.39013671875,\n              44.26093725039923\n            ],\n            [\n              -113.04931640625,\n              43.96909818325174\n            ],\n            [\n              -113.917236328125,\n              43.35713822211053\n            ],\n            [\n              -114.774169921875,\n              43.31718491566708\n            ],\n            [\n              -115.6640625,\n              43.26920624914964\n            ],\n            [\n              -116.03759765625,\n              43.54058479482877\n            ],\n            [\n              -116.444091796875,\n              43.810747313446996\n            ],\n            [\n              -116.619873046875,\n              43.929549935614595\n            ],\n            [\n              -116.91650390625,\n              43.95328204198018\n            ],\n            [\n              -116.98242187499999,\n              43.16512263158296\n            ],\n            [\n              -116.71874999999999,\n              42.64204079304428\n            ],\n            [\n              -116.09252929687499,\n              42.13082130188811\n            ],\n            [\n              -114.41162109375,\n              42.00848901572399\n            ],\n            [\n              -114.246826171875,\n              42.032974332441405\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","volume":"6","issue":"5","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"55d6fa37e4b0518e3546bc57","contributors":{"authors":[{"text":"Mabey, Don R.","contributorId":43741,"corporation":false,"usgs":true,"family":"Mabey","given":"Don","email":"","middleInitial":"R.","affiliations":[],"preferred":false,"id":568814,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":70156350,"text":"70156350 - 1978 - Helium in soil gases of the Roosevelt Hot Springs Known Geothermal Resource Ares, Beaver County, Utah","interactions":[],"lastModifiedDate":"2016-01-06T17:29:25","indexId":"70156350","displayToPublicDate":"1978-11-30T18:00:00","publicationYear":"1978","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":2446,"text":"Journal of Research of the U.S. Geological Survey","active":true,"publicationSubtype":{"id":10}},"title":"Helium in soil gases of the Roosevelt Hot Springs Known Geothermal Resource Ares, Beaver County, Utah","docAbstract":"<p>Soil samples were collected in two parallel traverses across the Dome fault zone of the Roosevelt Hot Springs Known Geothermal Resource Area. The samples were sealed in air-tight aluminum cans, and the soil gas was allowed to equilibrate with the atmospheric air in the cans. Gas from the cans was analyzed by mass spectrometry. Samples collected over faults contained anomalously high concentrations of helium. Samples collected close to a geothermal well 884 m deep contained more helium than samples collected near another geothermal well 1370 m deep.</p>","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Arlington, VA","usgsCitation":"Hinkle, M.E., Denton, E., Bigelow, R.C., and Turner, R.L., 1978, Helium in soil gases of the Roosevelt Hot Springs Known Geothermal Resource Ares, Beaver County, Utah: Journal of Research of the U.S. Geological Survey, v. 6, no. 5, p. 563-569.","productDescription":"7 p.","startPage":"563","endPage":"569","onlineOnly":"Y","additionalOnlineFiles":"N","costCenters":[],"links":[{"id":306991,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"},{"id":306990,"rank":1,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/journal/1978/vol6issue5/report.pdf","text":"Report","size":"31.11 MB","linkFileType":{"id":1,"text":"pdf"},"description":"Report"}],"country":"United States","state":"Utah","county":"Beaver County","otherGeospatial":"Roosevelt Hot Springs","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -113.13034057617188,\n              38.28993659801203\n            ],\n            [\n              -113.13034057617188,\n              38.68014968334621\n            ],\n            [\n              -112.66754150390625,\n              38.68014968334621\n            ],\n            [\n              -112.66754150390625,\n              38.28993659801203\n            ],\n            [\n              -113.13034057617188,\n              38.28993659801203\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","volume":"6","issue":"5","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"55d6fa33e4b0518e3546bc46","contributors":{"authors":[{"text":"Hinkle, M. E.","contributorId":11612,"corporation":false,"usgs":true,"family":"Hinkle","given":"M.","email":"","middleInitial":"E.","affiliations":[],"preferred":false,"id":568821,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Denton, E.H.","contributorId":75144,"corporation":false,"usgs":true,"family":"Denton","given":"E.H.","email":"","affiliations":[],"preferred":false,"id":568822,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Bigelow, R. C.","contributorId":90718,"corporation":false,"usgs":true,"family":"Bigelow","given":"R.","email":"","middleInitial":"C.","affiliations":[],"preferred":false,"id":568823,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Turner, R. L.","contributorId":93903,"corporation":false,"usgs":true,"family":"Turner","given":"R.","email":"","middleInitial":"L.","affiliations":[],"preferred":false,"id":568824,"contributorType":{"id":1,"text":"Authors"},"rank":4}]}}
,{"id":70156431,"text":"70156431 - 1978 - New Paleogene pollen species from the Gulf and Atlantic Coastal Plains","interactions":[],"lastModifiedDate":"2015-08-21T11:43:46","indexId":"70156431","displayToPublicDate":"1978-11-30T18:00:00","publicationYear":"1978","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":2446,"text":"Journal of Research of the U.S. Geological Survey","active":true,"publicationSubtype":{"id":10}},"title":"New Paleogene pollen species from the Gulf and Atlantic Coastal Plains","docAbstract":"<p>Four new pollen species are described on the basis of specimens from the Paleocene to early middle Eocene interval of the Gulf and Atlantic Coastal Plains. The species and their known geologic and geographic ranges are <i>Trivestibulopollenitcs fissuratus</i> (Midwayan to early Sabinian, Claibornian?; gulf coast?, Georgia to South Carolina); <i>Pseudoplicapollis limitata</i> (Midwayan to late Sabinian; gulf coast to Massachusetts), <i>Tricolpitcs asper</i> (early Midwayan to early Claibornian; gulf coast to Massachusetts), and <i>Tricolpites redactus</i> (early Midwayan to early Sabinian; South Carolina to Massachusetts).</p>","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Arlington, VA","usgsCitation":"Frederiksen, N.O., 1978, New Paleogene pollen species from the Gulf and Atlantic Coastal Plains: Journal of Research of the U.S. Geological Survey, v. 6, no. 5, p. 691-695.","productDescription":"5 p.","startPage":"691","endPage":"695","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[],"links":[{"id":307129,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"},{"id":307127,"rank":1,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/journal/1978/vol6issue5/report.pdf","text":"Report","size":"31.11 MB","linkFileType":{"id":1,"text":"pdf"},"description":"Report"}],"country":"United States","state":"South Carolina","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -81,\n              32\n            ],\n            [\n              -81,\n              33\n            ],\n            [\n              -80,\n              33\n            ],\n            [\n              -80,\n              32\n            ],\n            [\n              -81,\n              32\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","volume":"6","issue":"5","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"55d84bbae4b0518e3546f028","contributors":{"authors":[{"text":"Frederiksen, Norman O.","contributorId":50880,"corporation":false,"usgs":true,"family":"Frederiksen","given":"Norman","email":"","middleInitial":"O.","affiliations":[],"preferred":false,"id":569155,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":70156353,"text":"70156353 - 1978 - CS<sub>2</sub> and COS in soil gases of the Roosevelt Hot Springs Known Geothermal Resource Area, Beaver County, Utah","interactions":[],"lastModifiedDate":"2015-08-20T14:26:00","indexId":"70156353","displayToPublicDate":"1978-11-30T18:00:00","publicationYear":"1978","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":2446,"text":"Journal of Research of the U.S. Geological Survey","active":true,"publicationSubtype":{"id":10}},"title":"CS<sub>2</sub> and COS in soil gases of the Roosevelt Hot Springs Known Geothermal Resource Area, Beaver County, Utah","docAbstract":"<p>Soil-gas samples were collected in two parallel traverses across the Dome fault zone of the Roosevelt Hot Springs Known Geothermal Resource Area. Gas chromatographic analyses of the samples showed anomalous concentrations of CS<sub>3</sub> and COS east of the Dome fault; higher concentrations of CS<sub>2</sub> and COS also occurred over an area in which the hydrothermal system is close to the surface. Measurement of these gases may be useful in exploration for new geothermal sources.</p>","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Arlington, VA","usgsCitation":"Hinkle, M., and Harms, T.F., 1978, CS<sub>2</sub> and COS in soil gases of the Roosevelt Hot Springs Known Geothermal Resource Area, Beaver County, Utah: Journal of Research of the U.S. Geological Survey, v. 6, no. 5, p. 571-578.","productDescription":"8 p.","startPage":"571","endPage":"578","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[],"links":[{"id":306996,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"},{"id":306995,"rank":1,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/journal/1978/vol6issue5/report.pdf","text":"Report","size":"31.11 MB","linkFileType":{"id":1,"text":"pdf"},"description":"Report"}],"country":"United States","state":"Utah","county":"Beaver County","otherGeospatial":"Roosevelt Hot Springs","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -113.13034057617188,\n              38.28993659801203\n            ],\n            [\n              -113.13034057617188,\n              38.68014968334621\n            ],\n            [\n              -112.66754150390625,\n              38.68014968334621\n            ],\n            [\n              -112.66754150390625,\n              38.28993659801203\n            ],\n            [\n              -113.13034057617188,\n              38.28993659801203\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","volume":"6","issue":"5","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"55d6fa30e4b0518e3546bc2e","contributors":{"authors":[{"text":"Hinkle, Margaret","contributorId":36918,"corporation":false,"usgs":true,"family":"Hinkle","given":"Margaret","affiliations":[],"preferred":false,"id":568840,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Harms, Thelma F.","contributorId":57841,"corporation":false,"usgs":true,"family":"Harms","given":"Thelma","email":"","middleInitial":"F.","affiliations":[],"preferred":false,"id":568841,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":70156358,"text":"70156358 - 1978 - Wood River mining district, Idaho - intrusion-related lead-silver deposits derived from country rock source","interactions":[],"lastModifiedDate":"2015-08-20T14:27:05","indexId":"70156358","displayToPublicDate":"1978-11-30T18:00:00","publicationYear":"1978","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":2446,"text":"Journal of Research of the U.S. Geological Survey","active":true,"publicationSubtype":{"id":10}},"title":"Wood River mining district, Idaho - intrusion-related lead-silver deposits derived from country rock source","docAbstract":"<p>Lead-silver deposits in the Wood River mining district occur in shear zones in hornfelsed argillite of the Devonian Milligen Formation near granitic plutons and under the Wood River thrust fault. The principal ore minerals are argentiferous galena and sphalerite; siderite is the principal gangue. The &delta;<sup>34</sup>S values of the sulfide minerals range from +2.2 to +15.0 permil, indicating that the sulfur had a shallow crustal source. &Delta;<sup>34</sup>S values between sphalerite and galena range from +2.3 to +3.4 permil, corresponding to sulfur isotope temperatures between 280&deg; and 182 &deg;C. Hydrothermal barite has a&nbsp;&delta;<sup>34</sup>S of +13.2 permil. Lead isotope ratios are radiogenic, also pointing to a shallow crustal source. Quartz gangue has &delta;<sup>18</sup>O of +16.4 permil and a calculated &delta;<sup>18</sup>O<sub>H20</sub> at 270&deg;C of +8.4 permil. This value is reasonable for a hydrothermal fluid that had reached equilibrium with the argillite country rock. The siderite gangue has&nbsp;&delta;<sup>18</sup>O and&nbsp;&delta;<sup>13</sup>C values of +14.0 and -5.5 permil, respectively. Fluid inclusions have homogenization temperatures of 244&deg;-307&deg;C and average 270&deg;C. Freezing-stage measurements ranged from -1.85 to -2.8&deg;C, suggesting salinities of 3.2 to 4.8 weight percent. The &delta;D values of inclusion fluid in ore and gangue minerals are -110 to -120 permil. The geology, isotope, and fluid-inclusion data are consistent with a model of hydrothermal systems of meteoric water in faulted and shattered Paleozoic rocks near plutonic masses. This environment permitted deep circulation of the hydrothermal fluids, which dissolved the metals and sulfur from the Paleozoic host rocks and deposited ore in favorable beds or structures under the regional Wood River thrust fault.</p>","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Arlington, VA","usgsCitation":"Hall, W.E., Rye, R.O., and Doe, B.R., 1978, Wood River mining district, Idaho - intrusion-related lead-silver deposits derived from country rock source: Journal of Research of the U.S. Geological Survey, v. 6, no. 5, p. 579-592.","productDescription":"14 p.","startPage":"579","endPage":"592","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[],"links":[{"id":306999,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"},{"id":306998,"rank":1,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/journal/1978/vol6issue5/report.pdf","text":"Report","size":"31.11 MB","linkFileType":{"id":1,"text":"pdf"},"description":"Report"}],"country":"United States","state":"Idaho","county":"Blaine County","city":"Hailey, Bellevue","otherGeospatial":"Wood River","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -114.52629089355469,\n              43.3616313239934\n            ],\n            [\n              -114.52629089355469,\n              43.76514352427404\n            ],\n            [\n              -114.04907226562499,\n              43.76514352427404\n            ],\n            [\n              -114.04907226562499,\n              43.3616313239934\n            ],\n            [\n              -114.52629089355469,\n              43.3616313239934\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","volume":"6","issue":"5","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"55d6fa38e4b0518e3546bc5f","contributors":{"authors":[{"text":"Hall, Wayne E.","contributorId":89955,"corporation":false,"usgs":true,"family":"Hall","given":"Wayne","email":"","middleInitial":"E.","affiliations":[],"preferred":false,"id":568845,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Rye, Robert O. rrye@usgs.gov","contributorId":1486,"corporation":false,"usgs":true,"family":"Rye","given":"Robert","email":"rrye@usgs.gov","middleInitial":"O.","affiliations":[{"id":211,"text":"Crustal Geophysics and Geochemistry Science Center","active":true,"usgs":true}],"preferred":true,"id":568846,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Doe, Bruce R.","contributorId":87554,"corporation":false,"usgs":true,"family":"Doe","given":"Bruce","email":"","middleInitial":"R.","affiliations":[],"preferred":false,"id":568847,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":5221098,"text":"5221098 - 1978 - An unusually long pursuit of a deer by a wolf","interactions":[],"lastModifiedDate":"2025-03-11T15:42:32.484161","indexId":"5221098","displayToPublicDate":"1978-11-24T00:00:00","publicationYear":"1978","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":2373,"text":"Journal of Mammalogy","onlineIssn":"1545-1542","printIssn":"0022-2372","active":true,"publicationSubtype":{"id":10}},"title":"An unusually long pursuit of a deer by a wolf","docAbstract":"<p>No abstract available.&nbsp;</p>","language":"English","publisher":"Oxford Academic","doi":"10.2307/1380155","usgsCitation":"Mech, L., and Korb, M., 1978, An unusually long pursuit of a deer by a wolf: Journal of Mammalogy, v. 59, no. 4, p. 860-861, https://doi.org/10.2307/1380155.","productDescription":"2 p.","startPage":"860","endPage":"861","costCenters":[{"id":531,"text":"Patuxent Wildlife Research 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L.D. 0000-0003-3944-7769","orcid":"https://orcid.org/0000-0003-3944-7769","contributorId":75466,"corporation":false,"usgs":false,"family":"Mech","given":"L.D.","email":"","affiliations":[],"preferred":false,"id":333033,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Korb, M.","contributorId":94001,"corporation":false,"usgs":true,"family":"Korb","given":"M.","email":"","affiliations":[],"preferred":false,"id":333034,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":70012551,"text":"70012551 - 1978 - Regional implications of Triassic or Jurassic age for basalt and sedimentary red beds in the South Carolina coastal plain","interactions":[],"lastModifiedDate":"2026-01-15T16:18:38.693673","indexId":"70012551","displayToPublicDate":"1978-11-24T00:00:00","publicationYear":"1978","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":3338,"text":"Science","active":true,"publicationSubtype":{"id":10}},"title":"Regional implications of Triassic or Jurassic age for basalt and sedimentary red beds in the South Carolina coastal plain","docAbstract":"Whole rock potassium-argon ages for samples of subsurface basalt recovered near Charleston, South Carolina, are interpreted to indicate a Triassic or Jurassic age for the basalt and underlying sedimentary red beds. This age is consistent with existing evidence indicating that an early Mesozoic basin is present in the subsurface of a large part of the coastal plain of South Carolina, Georgia, Florida, and Alabama.","language":"English","publisher":"American Association for the Advancement of Science","doi":"10.1126/science.202.4370.887","issn":"00368075","usgsCitation":"Gohn, G.S., Gottfried, D., Lanphere, M.A., and Higgins, B., 1978, Regional implications of Triassic or Jurassic age for basalt and sedimentary red beds in the South Carolina coastal plain: Science, v. 202, no. 4370, p. 887-890, https://doi.org/10.1126/science.202.4370.887.","productDescription":"4 p.","startPage":"887","endPage":"890","costCenters":[],"links":[{"id":222087,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United States","state":"South 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