{"pageNumber":"5754","pageRowStart":"143825","pageSize":"25","recordCount":184617,"records":[{"id":5210148,"text":"5210148 - 1978 - Wolf vocalization","interactions":[],"lastModifiedDate":"2012-02-02T00:15:20","indexId":"5210148","displayToPublicDate":"2009-06-09T09:23:16","publicationYear":"1978","noYear":false,"publicationType":{"id":5,"text":"Book chapter"},"publicationSubtype":{"id":24,"text":"Book Chapter"},"title":"Wolf vocalization","largerWorkType":{"id":4,"text":"Book"},"largerWorkTitle":"Wolf and Man: Evolution in Parallel","largerWorkSubtype":{"id":4,"text":"Other Government Series"},"language":"English","publisher":"Academic Press","publisherLocation":"New York, NY","collaboration":"OCLC:  3607816","usgsCitation":"Harrington, F., and Mech, L., 1978, Wolf vocalization, chap. <i>of</i> Wolf and Man: Evolution in Parallel, p. 109-132.","productDescription":"xiv, 210","startPage":"109","endPage":"132","costCenters":[{"id":531,"text":"Patuxent Wildlife Research Center","active":true,"usgs":true}],"links":[{"id":201139,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b24e4b07f02db6aea00","contributors":{"editors":[{"text":"Hall, Roberta L.","contributorId":112851,"corporation":false,"usgs":true,"family":"Hall","given":"Roberta","email":"","middleInitial":"L.","affiliations":[],"preferred":false,"id":506059,"contributorType":{"id":2,"text":"Editors"},"rank":1},{"text":"Sharp, Henry S.","contributorId":113401,"corporation":false,"usgs":true,"family":"Sharp","given":"Henry","email":"","middleInitial":"S.","affiliations":[],"preferred":false,"id":506060,"contributorType":{"id":2,"text":"Editors"},"rank":2}],"authors":[{"text":"Harrington, F.H.","contributorId":14524,"corporation":false,"usgs":true,"family":"Harrington","given":"F.H.","email":"","affiliations":[],"preferred":false,"id":327854,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Mech, 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":327855,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":5210210,"text":"5210210 - 1978 - Feeding-site description of three heron species near Beaufort, North Carolina","interactions":[],"lastModifiedDate":"2012-02-02T00:15:16","indexId":"5210210","displayToPublicDate":"2009-06-09T09:23:16","publicationYear":"1978","noYear":false,"publicationType":{"id":5,"text":"Book chapter"},"publicationSubtype":{"id":24,"text":"Book Chapter"},"title":"Feeding-site description of three heron species near Beaufort, North Carolina","largerWorkType":{"id":4,"text":"Book"},"largerWorkTitle":"Wading Birds","largerWorkSubtype":{"id":4,"text":"Other Government Series"},"language":"English","publisher":"National Audubon Society","publisherLocation":"NY, NY","usgsCitation":"Custer, T., and Osborn, R.G., 1978, Feeding-site description of three heron species near Beaufort, North Carolina, chap. <i>of</i> Wading Birds, p. 355-360.","productDescription":"ix, 381","startPage":"355","endPage":"360","costCenters":[{"id":531,"text":"Patuxent Wildlife Research Center","active":true,"usgs":true}],"links":[{"id":200493,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e49fde4b07f02db5f5ea8","contributors":{"editors":[{"text":"Sprunt, Alexander= IV","contributorId":113629,"corporation":false,"usgs":true,"family":"Sprunt","given":"Alexander=","suffix":"IV","email":"","affiliations":[],"preferred":false,"id":506123,"contributorType":{"id":2,"text":"Editors"},"rank":1},{"text":"Ogden, John C.","contributorId":67895,"corporation":false,"usgs":true,"family":"Ogden","given":"John","email":"","middleInitial":"C.","affiliations":[],"preferred":false,"id":506121,"contributorType":{"id":2,"text":"Editors"},"rank":2},{"text":"Winckler, Suzanne","contributorId":111591,"corporation":false,"usgs":true,"family":"Winckler","given":"Suzanne","email":"","affiliations":[],"preferred":false,"id":506122,"contributorType":{"id":2,"text":"Editors"},"rank":3}],"authors":[{"text":"Custer, T. W. 0000-0003-3170-6519","orcid":"https://orcid.org/0000-0003-3170-6519","contributorId":91802,"corporation":false,"usgs":true,"family":"Custer","given":"T. W.","affiliations":[{"id":531,"text":"Patuxent Wildlife Research Center","active":true,"usgs":true}],"preferred":true,"id":327972,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Osborn, R. G.","contributorId":76700,"corporation":false,"usgs":false,"family":"Osborn","given":"R.","email":"","middleInitial":"G.","affiliations":[],"preferred":false,"id":327971,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":5210123,"text":"5210123 - 1978 - Workshop summary","interactions":[],"lastModifiedDate":"2012-02-02T00:15:18","indexId":"5210123","displayToPublicDate":"2009-06-09T09:23:16","publicationYear":"1978","noYear":false,"publicationType":{"id":5,"text":"Book chapter"},"publicationSubtype":{"id":24,"text":"Book Chapter"},"title":"Workshop summary","largerWorkType":{"id":4,"text":"Book"},"largerWorkTitle":"Proceedings:  Impacts of transmission lines on birds in flight","largerWorkSubtype":{"id":4,"text":"Other Government Series"},"language":"English","publisher":"Oak Ridge Associated Universities","publisherLocation":"Oak Ridge, TN","usgsCitation":"Anderson, S., 1978, Workshop summary, chap. <i>of</i> Proceedings:  Impacts of transmission lines on birds in flight, p. 195-197.","productDescription":"212","startPage":"195","endPage":"197","numberOfPages":"212","costCenters":[{"id":531,"text":"Patuxent Wildlife Research Center","active":true,"usgs":true}],"links":[{"id":201187,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e49d6e4b07f02db5de729","contributors":{"authors":[{"text":"Anderson, S.H.","contributorId":33667,"corporation":false,"usgs":true,"family":"Anderson","given":"S.H.","email":"","affiliations":[],"preferred":false,"id":327820,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":5210128,"text":"5210128 - 1978 - The peregrine falcon and the U.S. Fish and Wildlife Service","interactions":[],"lastModifiedDate":"2012-02-02T00:15:18","indexId":"5210128","displayToPublicDate":"2009-06-09T09:23:16","publicationYear":"1978","noYear":false,"publicationType":{"id":5,"text":"Book chapter"},"publicationSubtype":{"id":24,"text":"Book Chapter"},"title":"The peregrine falcon and the U.S. Fish and Wildlife Service","largerWorkType":{"id":4,"text":"Book"},"largerWorkTitle":"Proceedings of the National Audubon Society's Symposium on the Current Status of Peregrine Falcon Populations in North America","largerWorkSubtype":{"id":4,"text":"Other Government Series"},"language":"English","publisher":"National Audubon Society, Western Education Center","publisherLocation":"Tiburon, CA","usgsCitation":"Wilbur, S., 1978, The peregrine falcon and the U.S. Fish and Wildlife Service, chap. <i>of</i> Proceedings of the National Audubon Society's Symposium on the Current Status of Peregrine Falcon Populations in North America, p. 22-25.","productDescription":"67","startPage":"22","endPage":"25","numberOfPages":"67","costCenters":[{"id":531,"text":"Patuxent Wildlife Research Center","active":true,"usgs":true}],"links":[{"id":201121,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a7ee4b07f02db64859e","contributors":{"editors":[{"text":"Schaeffer, Philip P.","contributorId":113492,"corporation":false,"usgs":true,"family":"Schaeffer","given":"Philip","email":"","middleInitial":"P.","affiliations":[],"preferred":false,"id":506032,"contributorType":{"id":2,"text":"Editors"},"rank":1},{"text":"Ehlers, Sharyn Marie","contributorId":112077,"corporation":false,"usgs":true,"family":"Ehlers","given":"Sharyn","email":"","middleInitial":"Marie","affiliations":[],"preferred":false,"id":506031,"contributorType":{"id":2,"text":"Editors"},"rank":2}],"authors":[{"text":"Wilbur, S.R.","contributorId":53908,"corporation":false,"usgs":true,"family":"Wilbur","given":"S.R.","email":"","affiliations":[],"preferred":false,"id":327826,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":5200077,"text":"5200077 - 1978 - Effects of highways on wildlife populations and habitats. Phase 1.  Selection and evaluation of procedures","interactions":[],"lastModifiedDate":"2012-02-02T00:15:20","indexId":"5200077","displayToPublicDate":"2009-06-08T16:49:39","publicationYear":"1978","noYear":false,"publicationType":{"id":4,"text":"Book"},"title":"Effects of highways on wildlife populations and habitats. Phase 1.  Selection and evaluation of procedures","language":"English","publisher":"Federal Highway Administration.  Office of Research and Development","publisherLocation":"Washington, D.C.","usgsCitation":"Adams, L., and Geis, A.D., 1978, Effects of highways on wildlife populations and habitats. Phase 1.  Selection and evaluation of procedures, ix, 170 .","productDescription":"ix, 170 ","costCenters":[{"id":531,"text":"Patuxent Wildlife Research Center","active":true,"usgs":true}],"links":[{"id":201054,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a29e4b07f02db611f2f","contributors":{"authors":[{"text":"Adams, L.W.","contributorId":108217,"corporation":false,"usgs":true,"family":"Adams","given":"L.W.","email":"","affiliations":[],"preferred":false,"id":326950,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Geis, A. D.","contributorId":72885,"corporation":false,"usgs":true,"family":"Geis","given":"A.","email":"","middleInitial":"D.","affiliations":[],"preferred":false,"id":326949,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":5200221,"text":"5200221 - 1978 - Recovery Plan for the Eastern Timber Wolf","interactions":[],"lastModifiedDate":"2021-03-22T14:48:02.69142","indexId":"5200221","displayToPublicDate":"2009-06-08T16:49:39","publicationYear":"1978","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":4,"text":"Other Government Series"},"title":"Recovery Plan for the Eastern Timber Wolf","docAbstract":"<p>No abstract available.</p>","language":"English","publisher":"U.S. Fish and Wildlife Service","publisherLocation":"Twin Cities, MN","usgsCitation":"Bailey, R.E., Mech, L., Hickling, W.C., Nicotera, R., Rutske, L., Linn, R.M., Radtke, R.E., and Siderits, K., 1978, Recovery Plan for the Eastern Timber Wolf, 102 p.","productDescription":"102 p.","numberOfPages":"102","costCenters":[{"id":531,"text":"Patuxent Wildlife Research Center","active":true,"usgs":true}],"links":[{"id":201428,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a60e4b07f02db635464","contributors":{"authors":[{"text":"Bailey, R. E.","contributorId":22882,"corporation":false,"usgs":false,"family":"Bailey","given":"R.","email":"","middleInitial":"E.","affiliations":[],"preferred":false,"id":327238,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Mech, 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":327242,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Hickling, W. C.","contributorId":20045,"corporation":false,"usgs":false,"family":"Hickling","given":"W.","email":"","middleInitial":"C.","affiliations":[],"preferred":false,"id":327237,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Nicotera, R.","contributorId":59919,"corporation":false,"usgs":true,"family":"Nicotera","given":"R.","affiliations":[],"preferred":false,"id":327241,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"Rutske, L.","contributorId":84478,"corporation":false,"usgs":true,"family":"Rutske","given":"L.","email":"","affiliations":[],"preferred":false,"id":327243,"contributorType":{"id":1,"text":"Authors"},"rank":5},{"text":"Linn, R. M.","contributorId":56769,"corporation":false,"usgs":false,"family":"Linn","given":"R.","email":"","middleInitial":"M.","affiliations":[],"preferred":false,"id":327240,"contributorType":{"id":1,"text":"Authors"},"rank":6},{"text":"Radtke, R. E.","contributorId":27593,"corporation":false,"usgs":true,"family":"Radtke","given":"R.","email":"","middleInitial":"E.","affiliations":[],"preferred":false,"id":327239,"contributorType":{"id":1,"text":"Authors"},"rank":7},{"text":"Siderits, K.","contributorId":12956,"corporation":false,"usgs":false,"family":"Siderits","given":"K.","email":"","affiliations":[],"preferred":false,"id":327236,"contributorType":{"id":1,"text":"Authors"},"rank":8}]}}
,{"id":70162706,"text":"70162706 - 1978 - Significance of age relations above and below upper jurassic ophiolite in the Geysers-Clear Lake region, California","interactions":[],"lastModifiedDate":"2016-01-29T10:51:48","indexId":"70162706","displayToPublicDate":"2008-12-28T04:00:00","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":"Significance of age relations above and below upper jurassic ophiolite in the Geysers-Clear Lake region, California","docAbstract":"<p>In The Geysers-Clear Lake area of northern California, a fragmented Upper Jurassic ophiolite overlain depositionally by the Great Valley sequence is juxtaposed over deformed and metomorphosed rocks of the Franciscan assemblage along the Coast Range thrust. The basal strata of the Great Valley sequence consist of thick breccias of mafic clasts, identical in composition to the upper part of the ophiolite. These breccias and their contact relations suggest that more than 1 km of the upper part of the ophiolite was locally eroded in early Tithonian time. On the basis of their radiolarian faunas, cherts in the Franciscan assemblage below the ophiolite range in age from Late Jurassic (early Tithonian) to Late Cretaceous (early Cenomanian). Of particular significance is an individual chert body (= The Geysers chert) of this age range. The early Cenomanian radiolarians, except for two occurrences associated with pelagic limestone, are significantly younger than those previously reported from the Franciscan assemblage. The existence of a sequence of Late Jurassic to Late Cretaceous radiolarian chert places critical constraints on subduction models for emplacement of the Franciscan assemblage beneath the Coast Range ophiolite and Great Valley sequence in The Geysers-Clear Lake area. From early Tithonian to post-early Cenomanian time, the Franciscan assemblage received pelagic sedimentation far from any site of subduction. By other data, blueschist metamorphism of subducted Franciscan strata also occurred during this time. The radiolarian data from The Geysers area permit a correlation with Upper Cretaceous pelagic limestones in the Laytonville area northwest of The Geysers and also imply that the Great Valley sequence was never depositionally in contact with the Franciscan assemblage.&nbsp;</p>","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Reston, VA","usgsCitation":"McLaughlin, R.J., and Pessagno, E., 1978, Significance of age relations above and below upper jurassic ophiolite in the Geysers-Clear Lake region, California: Journal of Research of the U.S. Geological Survey, v. 6, no. 6, p. 715-726.","productDescription":"12 p.","startPage":"715","endPage":"726","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[],"links":[{"id":315044,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"},{"id":315043,"rank":1,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/journal/1978/vol6issue6/report.pdf","text":"Report","size":"26.93 MB","linkFileType":{"id":1,"text":"pdf"},"description":"Report"}],"country":"United States","state":"California","otherGeospatial":"Geysers-Clear Lake region","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -124.1455078125,\n              41.96765920367816\n            ],\n            [\n              -124.34326171874999,\n              41.85319643776675\n            ],\n            [\n              -124.16748046874999,\n              41.50857729743935\n            ],\n            [\n              -124.18945312500001,\n              41.16211393939692\n            ],\n            [\n              -124.27734374999999,\n              40.93011520598305\n            ],\n            [\n              -124.51904296875,\n              40.58058466412764\n            ],\n            [\n              -124.51904296875,\n              40.27952566881291\n            ],\n            [\n              -124.27734374999999,\n              40.094882122321174\n            ],\n            [\n              -124.03564453125,\n              39.8928799002948\n            ],\n            [\n              -123.96972656249999,\n              39.53793974517628\n            ],\n            [\n              -123.99169921875,\n              39.027718840211605\n            ],\n            [\n              -123.662109375,\n              38.685509760012\n            ],\n            [\n              -123.28857421875,\n              38.28993659801203\n            ],\n            [\n              -123.11279296875001,\n              37.97884504049713\n            ],\n            [\n              -122.84912109375,\n              37.77071473849609\n            ],\n            [\n              -122.71728515624999,\n              37.52715361723378\n            ],\n            [\n              -122.4755859375,\n              37.42252593456307\n            ],\n            [\n              -121.66259765625001,\n              37.38761749978395\n            ],\n            [\n              -121.04736328125,\n              37.38761749978395\n            ],\n            [\n              -120.76171875,\n              37.59682400108367\n            ],\n            [\n              -120.30029296875,\n              38.08268954483802\n            ],\n            [\n              -120.73974609374999,\n              39.027718840211605\n            ],\n            [\n              -121.728515625,\n              40.36328834091583\n            ],\n            [\n              -121.9482421875,\n              40.93011520598305\n            ],\n            [\n              -122.49755859375,\n              41.409775832009565\n            ],\n            [\n              -122.80517578125,\n              42.01665183556825\n            ],\n            [\n              -124.1455078125,\n              41.96765920367816\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","volume":"6","issue":"6","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"56ac9b7ae4b0403299f53b20","contributors":{"authors":[{"text":"McLaughlin, R. 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,{"id":70162699,"text":"70162699 - 1978 - Spectrophotometric determination of tungsten in rocks by using zinc-dithiol","interactions":[],"lastModifiedDate":"2016-01-29T11:02:37","indexId":"70162699","displayToPublicDate":"2008-12-28T04:00:00","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":"Spectrophotometric determination of tungsten in rocks by using zinc-dithiol","docAbstract":"<p>Tungsten is determined in 11 USGS standard rocks by a spectrophotometric procedure that measures the absorbance of the tungsten-dithiol complex. The results are compared with those obtained by other methods. After the samples are dissolved in HClO<sub>4</sub> and HF, the tungsten-dithiol complex is extracted into isoamyl acetate and then back-extracted into isoamyl acetate. The determination of 0.1 part per million in a 500-mg sample can be made routinely.&nbsp;</p>","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Reston, VA","usgsCitation":"Aruscavage, P., and Campbell, E., 1978, Spectrophotometric determination of tungsten in rocks by using zinc-dithiol: Journal of Research of the U.S. Geological Survey, v. 6, no. 6, p. 697-699.","productDescription":"3 p.","startPage":"697","endPage":"699","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[],"links":[{"id":315035,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"},{"id":315034,"rank":1,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/journal/1978/vol6issue6/report.pdf","text":"Report","size":"26.93 MB","linkFileType":{"id":1,"text":"pdf"},"description":"Report"}],"volume":"6","issue":"6","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"56ac9b82e4b0403299f53b4f","contributors":{"authors":[{"text":"Aruscavage, Philip","contributorId":146853,"corporation":false,"usgs":true,"family":"Aruscavage","given":"Philip","email":"","affiliations":[],"preferred":false,"id":590198,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Campbell, Esma","contributorId":92652,"corporation":false,"usgs":true,"family":"Campbell","given":"Esma","email":"","affiliations":[],"preferred":false,"id":590199,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":70162712,"text":"70162712 - 1978 - Phosphorus in hydrothermal waters of Yellowstone National Park, Wyoming","interactions":[],"lastModifiedDate":"2016-01-29T11:40:28","indexId":"70162712","displayToPublicDate":"2008-12-28T04:00:00","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":"Phosphorus in hydrothermal waters of Yellowstone National Park, Wyoming","docAbstract":"<p>Ninety-seven hot-spring and geyser samples (field acidified to pH&lt;1.4 with HCl or HNO<sub>3</sub>) from Yellowstone National Park, Wyo., were analyzed for PO<sub>4</sub>-P using reduced molybdenum-blue and the selective arsenate reducing agent, metabisulfite-thiosulfate. The PO<sub>4</sub>-P&nbsp;concentrations ranged from below detection limit (~1-73 micrograms per liter). Twenty-five springs had PO<sub>4</sub>-P&nbsp;concentrations exceeding 6.8 <span>&mu;</span>g/L; seven spring samples exceeded 20 &mu;g/L. Elevated PO<sub>4</sub>-P&nbsp;contents were invariably associated with mixed springs, as evidenced by diluted chloride concentrations and, commonly, subboiling temperatures, low pH's, and elevated calcium concentrations. Alkaline high-chloride (&gt;400 milligrams per liter) hydrothermal waters from Upper and Norris Geyser Basins had PO<sub>4</sub>-P&nbsp;concentrations below 2 &mu;g/L and represent the low end of the range of PO<sub>4</sub>-P&nbsp;contents in natural waters.</p>","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Reston, VA","usgsCitation":"Stauffer, R.E., and Thompson, J.M., 1978, Phosphorus in hydrothermal waters of Yellowstone National Park, Wyoming: Journal of Research of the U.S. Geological Survey, v. 6, no. 6, p. 755-763.","productDescription":"9 p.","startPage":"755","endPage":"763","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[],"links":[{"id":315057,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"},{"id":315055,"rank":1,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/journal/1978/vol6issue6/report.pdf","text":"Report","size":"26.93 MB","linkFileType":{"id":1,"text":"pdf"},"description":"Report"}],"country":"United States","state":"Wyoming","otherGeospatial":"Yellowstone National Park","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -111.09100341796875,\n              45.11617660357484\n            ],\n            [\n              -111.0113525390625,\n              45.11811475546806\n            ],\n            [\n              -110.67626953125,\n              45.10066901851988\n            ],\n            [\n              -110.0390625,\n              45.03277379605973\n            ],\n            [\n              -109.92370605468749,\n              45.01530198999212\n            ],\n            [\n              -109.88800048828125,\n              44.92397370210939\n            ],\n            [\n              -109.92370605468749,\n              44.87533557756195\n            ],\n            [\n              -109.92095947265625,\n              44.820812031724444\n            ],\n            [\n              -109.88525390624999,\n              44.75648588056624\n            ],\n            [\n              -109.83032226562499,\n              44.72136867346628\n            ],\n            [\n              -109.81109619140625,\n              44.692088041727814\n            ],\n            [\n              -109.82757568359375,\n              44.66474608911831\n            ],\n            [\n              -109.92370605468749,\n              44.64716230650056\n            ],\n            [\n              -110.0225830078125,\n              44.610023477890515\n            ],\n            [\n              -110.093994140625,\n              44.56503415498704\n            ],\n            [\n              -110.1214599609375,\n              44.535674532413196\n            ],\n            [\n              -110.1104736328125,\n              44.52001001133986\n            ],\n            [\n              -109.9896240234375,\n              44.49454617990028\n            ],\n            [\n              -109.97863769531249,\n              44.453388800301774\n            ],\n            [\n              -110.0225830078125,\n              44.41024041296011\n            ],\n            [\n              -110.06927490234375,\n              44.396504700115536\n            ],\n            [\n              -110.00885009765625,\n              44.345458103018316\n            ],\n            [\n              -109.97314453125,\n              44.29043508918884\n            ],\n            [\n              -109.94018554687499,\n              44.132942183139654\n            ],\n            [\n              -109.9676513671875,\n              44.12702800650004\n            ],\n            [\n              -111.08001708984375,\n              44.125056482685146\n            ],\n            [\n              -111.09100341796875,\n              45.11617660357484\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","volume":"6","issue":"6","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"56ac9b6de4b0403299f53a9c","contributors":{"authors":[{"text":"Stauffer, R. E.","contributorId":66253,"corporation":false,"usgs":true,"family":"Stauffer","given":"R.","email":"","middleInitial":"E.","affiliations":[],"preferred":false,"id":590227,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Thompson, J. M.","contributorId":119715,"corporation":false,"usgs":true,"family":"Thompson","given":"J.","email":"","middleInitial":"M.","affiliations":[],"preferred":false,"id":590228,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":70162742,"text":"70162742 - 1978 - Application of four input-output models for nutrients in Lake Okeechobee, Florida","interactions":[],"lastModifiedDate":"2016-01-29T13:15:04","indexId":"70162742","displayToPublicDate":"2008-12-28T00:00:00","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":"Application of four input-output models for nutrients in Lake Okeechobee, Florida","docAbstract":"<p>R. A. Vollenweider's (1975) nonconservative model described concentrations of nitrogen and phosphorus for 1969-70 in Lake Okeechobee, Fla., better than the models of F. Biffi in 1963, R. H. Rainey in 1967, and R. Piontelli and V. Tonolli in 1964. Vollenweider's model predicted concentrations of 1.4 milligrams per liter of total nitrogen and 0.09 mg/L of total phosphorus in the lake. The concentration of nitrogen could be approximated with conservation models but phosphorus required a nonconservative model. Unless variations in input concentrations and flow rate of the tributaries are modeled, only short-term predictions of lake concentrations can be made because of variations in inflow concentrations and because of the short time required (400 days) for the lake to be flushed by its inflow.</p>","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Reston, VA","usgsCitation":"Miller, R.L., 1978, Application of four input-output models for nutrients in Lake Okeechobee, Florida: Journal of Research of the U.S. Geological Survey, v. 6, no. 6, p. 821-828.","productDescription":"8 p.","startPage":"821","endPage":"828","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[],"links":[{"id":315096,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"},{"id":315094,"rank":1,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/journal/1978/vol6issue6/report.pdf","text":"Report","size":"26.93 MB","linkFileType":{"id":1,"text":"pdf"},"description":"Report"}],"country":"United States","state":"Florida","otherGeospatial":"Lake Okeechobee","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -80.67260742187499,\n              27.171582284054917\n            ],\n            [\n              -80.7769775390625,\n              27.235094607795503\n            ],\n            [\n              -80.85937499999999,\n              27.23753666659069\n            ],\n            [\n              -80.90606689453124,\n              27.144700797119597\n            ],\n            [\n              -80.99395751953125,\n              27.03711021444808\n            ],\n            [\n              -81.10107421874999,\n              27.012643405861162\n            ],\n            [\n              -81.14501953125,\n              26.963693809276794\n            ],\n            [\n              -81.1175537109375,\n              26.853479438420024\n            ],\n            [\n              -81.046142578125,\n              26.765230565697482\n            ],\n            [\n              -80.86212158203125,\n              26.711266913515747\n            ],\n            [\n              -80.79620361328125,\n              26.66955020082152\n            ],\n            [\n              -80.71105957031249,\n              26.667095801104814\n            ],\n            [\n              -80.6396484375,\n              26.713720362159552\n            ],\n            [\n              -80.6341552734375,\n              26.792202785452883\n            ],\n            [\n              -80.57098388671874,\n              26.86328062676624\n            ],\n            [\n              -80.55999755859375,\n              26.934313833395052\n            ],\n            [\n              -80.5572509765625,\n              26.983276203452657\n            ],\n            [\n              -80.584716796875,\n              27.044449217654016\n            ],\n            [\n              -80.61492919921875,\n              27.127591028502078\n            ],\n            [\n              -80.67260742187499,\n              27.171582284054917\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","volume":"6","issue":"6","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"56ac9b45e4b0403299f539ca","contributors":{"authors":[{"text":"Miller, Ronald L.","contributorId":103245,"corporation":false,"usgs":true,"family":"Miller","given":"Ronald","email":"","middleInitial":"L.","affiliations":[],"preferred":false,"id":590381,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":70162771,"text":"70162771 - 1978 - Reconnaissance for microbial activity in the Magothy aquifer, Bay Park, New York, four years after artificial recharge","interactions":[],"lastModifiedDate":"2016-01-29T13:32:03","indexId":"70162771","displayToPublicDate":"2008-12-28T00:00:00","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":"Reconnaissance for microbial activity in the Magothy aquifer, Bay Park, New York, four years after artificial recharge","docAbstract":"<p>Tertiary-treated sewage effluent was injected into the Magothy aquifer at Bay Park, Long Island, N.Y., between 1968 and 1973. In 1977, the microbial flora in water samples from the injection well and from three nearby wells were surveyed. Differences in the composition of the microbial flora among the four wells were found. A bacterial community dominated by facultative and obligate anaerobes, including two <i>Clostridium</i> species and methanogenic bacteria, was found at a well 6.1 m from the injection well. By contrast, except for isolation of <i>Clostridium sphenoides</i> from a well 30 m away, only obligate aerobes and facultative anaerobes were found in water from the injection well and the 30 m well. Only a small number of obligate aerobes were found in samples from a well 61 m away. These results suggest that nutrients in the recharge water formed an organically enriched zone to at least a distance of 6.1 m from the point of injection but not as far as 61 m. Extensive pumping at the end of the injection program apparently removed exogeneous nutrients near the injection well.</p>","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Reston, VA","collaboration":"Prepared in cooperation with the Nassau County Department of Public Works","usgsCitation":"Godsy, E., and Ehrlich, G.G., 1978, Reconnaissance for microbial activity in the Magothy aquifer, Bay Park, New York, four years after artificial recharge: Journal of Research of the U.S. Geological Survey, v. 6, no. 6, p. 829-836.","productDescription":"8 p.","startPage":"829","endPage":"836","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[],"links":[{"id":315099,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"},{"id":315098,"rank":1,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/journal/1978/vol6issue6/report.pdf","text":"Report","size":"26.93 MB","linkFileType":{"id":1,"text":"pdf"},"description":"Report"}],"country":"United States","state":"New York","county":"Nassau County","otherGeospatial":"Bay Park, Long Island","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -73.78555297851562,\n              40.56963223359565\n            ],\n            [\n              -73.78555297851562,\n              40.658764163202925\n            ],\n            [\n              -73.56651306152344,\n              40.658764163202925\n            ],\n            [\n              -73.56651306152344,\n              40.56963223359565\n            ],\n            [\n              -73.78555297851562,\n              40.56963223359565\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","volume":"6","issue":"6","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"56ac9b75e4b0403299f53b0d","contributors":{"authors":[{"text":"Godsy, E.M.","contributorId":56685,"corporation":false,"usgs":true,"family":"Godsy","given":"E.M.","email":"","affiliations":[],"preferred":false,"id":590391,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Ehrlich, G. G.","contributorId":89126,"corporation":false,"usgs":true,"family":"Ehrlich","given":"G.","email":"","middleInitial":"G.","affiliations":[],"preferred":false,"id":590392,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":70162739,"text":"70162739 - 1978 - Inventory of land use and land cover of the Puget Sound region using Landsat digital data","interactions":[],"lastModifiedDate":"2016-01-29T12:58:00","indexId":"70162739","displayToPublicDate":"2008-12-28T00:00:00","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":"Inventory of land use and land cover of the Puget Sound region using Landsat digital data","docAbstract":"<p>Landsat multispectral scanner digital data from four bands were analyzed using computers to produce land use and land cover information of the Puget Sound region, Wash., for use by agencies in that area. The data were first geographically registered to map coordinates. This registration enabled samples of known land cover types to be digitized from the maps. Samples of the same land cover were grouped together and then subdivided by cluster analysis into spectrally similar classes. Spectral categories were associated with specific land cover classes and used to determine spectral signatures for classification of the entire region. Reclustering and reclassification techniques were developed and then employed to minimize certain classification errors. The classified data were displayed in color using a film recorder. This color image was enlarged photographically to a 1:100000 scale to match new base maps of the region. Although the result resembles a conventional polygonal land use and land cover map, certain image-like qualities&nbsp;remain and yield additional information about the landscape.</p>","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Reston, VA","usgsCitation":"Gaydos, L., and Newland, W.L., 1978, Inventory of land use and land cover of the Puget Sound region using Landsat digital data: Journal of Research of the U.S. Geological Survey, v. 6, no. 6, p. 807-814.","productDescription":"8 p.","startPage":"807","endPage":"814","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[],"links":[{"id":315079,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"},{"id":315078,"rank":1,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/journal/1978/vol6issue6/report.pdf","text":"Report","size":"26.93 MB","linkFileType":{"id":1,"text":"pdf"},"description":"Report"}],"country":"United States","state":"Washington","otherGeospatial":"Puget Sound region","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -123.431396484375,\n              47.00273390667881\n            ],\n            [\n              -123.431396484375,\n              48.16242149265211\n            ],\n            [\n              -121.95922851562501,\n              48.16242149265211\n            ],\n            [\n              -121.95922851562501,\n              47.00273390667881\n            ],\n            [\n              -123.431396484375,\n              47.00273390667881\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","volume":"6","issue":"6","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"56ac9b68e4b0403299f53a7d","contributors":{"authors":[{"text":"Gaydos, Leonard","contributorId":79888,"corporation":false,"usgs":true,"family":"Gaydos","given":"Leonard","affiliations":[],"preferred":false,"id":590316,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Newland, Willard L.","contributorId":152700,"corporation":false,"usgs":false,"family":"Newland","given":"Willard","email":"","middleInitial":"L.","affiliations":[],"preferred":false,"id":590317,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":70162731,"text":"70162731 - 1978 - lowaphyllum (rugose coral) from the Upper Devonian of Arizona","interactions":[],"lastModifiedDate":"2022-06-15T14:32:31.792124","indexId":"70162731","displayToPublicDate":"2008-12-28T00:00:00","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}},"displayTitle":"<i>lowaphyllum</i> (rugose coral) from the Upper Devonian of Arizona","title":"lowaphyllum (rugose coral) from the Upper Devonian of Arizona","docAbstract":"<p>The rugose coral genus <i>lowaphyllum</i> is uncommon but widely distributed in rocks of Devonian age. It is here reported for the first time from western North America (Late Devonian). <i>lowaphyllum</i> is also known from the late Middle and Late Devonian of Eastern North America, but the lack of Early and early Middle Devonian species anywhere in North America leaves open the question of derivation of these forms and their relationship to Early Devonian species in Europe and Australia.</p>","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Reston, VA","usgsCitation":"Oliver, W.A., 1978, lowaphyllum (rugose coral) from the Upper Devonian of Arizona: Journal of Research of the U.S. Geological Survey, v. 6, no. 6, p. 797-805.","productDescription":"9 p.","startPage":"797","endPage":"805","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[],"links":[{"id":315076,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"},{"id":315075,"rank":1,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/journal/1978/vol6issue6/report.pdf","text":"Report","size":"26.93 MB","linkFileType":{"id":1,"text":"pdf"},"description":"Report"}],"country":"United States","state":"Arizona","otherGeospatial":"Haunted Canyon, J. K. Canyon","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -111.9451904296875,\n              32.45415593941475\n            ],\n            [\n              -111.9451904296875,\n              35.178298352001185\n            ],\n            [\n              -109.1876220703125,\n              35.178298352001185\n            ],\n            [\n              -109.1876220703125,\n              32.45415593941475\n            ],\n            [\n              -111.9451904296875,\n              32.45415593941475\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","volume":"6","issue":"6","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"56ac9b40e4b0403299f53988","contributors":{"authors":[{"text":"Oliver, William Albert Jr.","contributorId":44521,"corporation":false,"usgs":true,"family":"Oliver","given":"William","suffix":"Jr.","email":"","middleInitial":"Albert","affiliations":[],"preferred":false,"id":590312,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":70162722,"text":"70162722 - 1978 - A reexamination of the Pennsylvanian trace fossil <i>Olivellites</i>","interactions":[],"lastModifiedDate":"2016-01-29T12:13:35","indexId":"70162722","displayToPublicDate":"2008-12-28T00:00:00","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":"A reexamination of the Pennsylvanian trace fossil <i>Olivellites</i>","docAbstract":"<p>The original interpretation of <i>Olivellites plummeri</i> Fenton and Fenton as the trace of an infaunal gastropod, is reconsidered and rejected. The original slab bearing several examples of <i>O. plummeri</i> has been reexamined and reillustrated. The slab came from the type-locality of <i>O. plummeri</i>&nbsp;in Eastland County, Tex., and is a shallow sub tidal sandstone of the Graham Formation; the sandstone, which has yielded additional specimens, is presumably a reworked delta-front deposit. <i>Olivellites</i> was also observed in the Caddo Creek Formation in Stephens County, Tex., but, to date, it has not been found elsewhere in north-central Texas. Interpretation of Paleozoic ichnofossils by analogy with modern traces is limited; behavioral characteristics may be the products of post-Paleozoic innovation. The internal morphology and path of <i>Olivellites</i> are unlike those of any modern gastropod trail, and the genus is removed from the Mollusca.</p>","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Reston, VA","usgsCitation":"Yochelson, E.L., and Schindel, D.E., 1978, A reexamination of the Pennsylvanian trace fossil <i>Olivellites</i>: Journal of Research of the U.S. Geological Survey, v. 6, no. 6, p. 789-796.","productDescription":"8 p.","startPage":"789","endPage":"796","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[],"links":[{"id":315072,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"},{"id":315071,"rank":1,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/journal/1978/vol6issue6/report.pdf","text":"Report","size":"26.93 MB","linkFileType":{"id":1,"text":"pdf"},"description":"Report"}],"country":"United States","state":"Texas","county":"Eastland County","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -98.96312713623045,\n              32.32485582675006\n            ],\n            [\n              -98.96312713623045,\n              32.43822086674334\n            ],\n            [\n              -98.8275146484375,\n              32.43822086674334\n            ],\n            [\n              -98.8275146484375,\n              32.32485582675006\n            ],\n            [\n              -98.96312713623045,\n              32.32485582675006\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","volume":"6","issue":"6","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"56ac9b44e4b0403299f539b8","contributors":{"authors":[{"text":"Yochelson, Ellis L.","contributorId":90802,"corporation":false,"usgs":true,"family":"Yochelson","given":"Ellis","email":"","middleInitial":"L.","affiliations":[],"preferred":false,"id":590300,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Schindel, David E.","contributorId":152692,"corporation":false,"usgs":false,"family":"Schindel","given":"David","email":"","middleInitial":"E.","affiliations":[],"preferred":false,"id":590301,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":70162721,"text":"70162721 - 1978 - Upper Devonian radiolarians separated from chert of the Ford Lake Shale, Alaska","interactions":[],"lastModifiedDate":"2016-01-29T12:02:05","indexId":"70162721","displayToPublicDate":"2008-12-28T00:00:00","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":"Upper Devonian radiolarians separated from chert of the Ford Lake Shale, Alaska","docAbstract":"<p>Leaching of black bedded chert from the Ford Lake Shale, Kandik Basin, Alaska, with dilute hydrofluoric acid resulted in the complete separation of moderately well preserved radiolarians. Preliminary study of an assemblage obtained from the lower half of the formation revealed six to eight forms apparently identical to specimens previously known from the Tournaisian of southern France and northwestern Turkey, including four genera not previously described from North America. Sparse, poorly preserved conodonts in the same sample are of Late Devonian age. We conclude that certain radiolarian species, hitherto known only from the early Carboniferous, span the Devonian-Carboniferous boundary. The radiolarian assemblage of the Ford Lake Shale sample contrasts markedly with Late Devonian assemblages known from the Canol Shale of northern Canada and the Huron Member of the Ohio Shale; the Ford Lake Shale fauna may reflect greater oceanic influences than these other localities, which lie farther inland from the Devonian continental margin.</p>","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Reston, VA","usgsCitation":"Holdsworth, B.K., Jones, D.L., and Allison, C., 1978, Upper Devonian radiolarians separated from chert of the Ford Lake Shale, Alaska: Journal of Research of the U.S. Geological Survey, v. 6, no. 6, p. 775-788.","productDescription":"14 p.","startPage":"775","endPage":"788","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[],"links":[{"id":315070,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"},{"id":315069,"rank":1,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/journal/1978/vol6issue6/report.pdf","text":"Report","size":"26.93 MB","linkFileType":{"id":1,"text":"pdf"},"description":"Report"}],"country":"United States","state":"Alaska","otherGeospatial":"Ford Lake Shale, Kandik Basin, Yukon River","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -141.5,\n              64.75\n            ],\n            [\n              -141.5,\n              65\n            ],\n            [\n              -141,\n              65\n            ],\n            [\n              -141,\n              64.75\n            ],\n            [\n              -141.5,\n              64.75\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","volume":"6","issue":"6","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"56ac9b89e4b0403299f53b82","contributors":{"authors":[{"text":"Holdsworth, Brian K.","contributorId":75571,"corporation":false,"usgs":true,"family":"Holdsworth","given":"Brian","email":"","middleInitial":"K.","affiliations":[],"preferred":false,"id":590297,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Jones, D. L.","contributorId":65045,"corporation":false,"usgs":true,"family":"Jones","given":"D.","email":"","middleInitial":"L.","affiliations":[],"preferred":false,"id":590298,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Allison, C.","contributorId":89842,"corporation":false,"usgs":true,"family":"Allison","given":"C.","email":"","affiliations":[],"preferred":false,"id":590299,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":70162710,"text":"70162710 - 1978 - Pressure gradients and boiling as mechanisms for localizing ore in porphyry systems","interactions":[],"lastModifiedDate":"2016-01-29T11:18:39","indexId":"70162710","displayToPublicDate":"2008-12-28T00:00:00","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":"Pressure gradients and boiling as mechanisms for localizing ore in porphyry systems","docAbstract":"<p>Fluid inclusions in ore zones of porphyry systems indicate that extensive boiling of hydrothermal fluids accompanies deposition of ore and gangue minerals. The boiling commonly accompanied a change from a lithostatic to a hydrostatic environment during evolution of an epizonal stock. Pressure gradients near the margin of the stock can determine whether ore or only a diffuse zone of mineralization is formed. A sharp drop in pressure in an epizonal environment is more likely to cause extensive boiling than a comparable change in a deeper environment, as the slope of the boiling curve steepens with an increase 'in pressure. The drop in pressure causes the hydrothermal fluids to boil and creates a crackle (stockwork) breccia, which hosts the veinlets of gangue quartz and ore minerals. The boiling selectively partitions CO<sub>2</sub>, H<sub>2</sub>S, and HCl into the vapor phase, changing the pH, composition, ionic strength, and thus the solubility product of metal complexes in the remaining liquid and causing the ore and gangue to come out of solution. Fluid inclusions trapped from boiling solutions can exhibit several forms, depending on the physical and chemical conditions of the hydrothermal fluid from which they were trapped. In one case, inclusions when heated can homogenize to either liquid or vapor at the same temperature, which is the true boiling temperature. In another case, homogenization of various inclusions can occur through a range of temperatures. The latter case results from the trapping of mixture of liquid and vapor. Variations in salinity can result from boiling of the hydrothermal fluid, or intermittent incorporation of high-salinity fluids from the magma, or trapping of fluids of varying densities at pressure-temperature conditions above the critical point of the fluid. In places, paleopressure-temperature transition zones can be recognized by fluid-inclusion homogenization temperatures and phase relationships and by the presence of anhydrite daughter minerals. Boiling of a hydrothermal fluid in the porphyry environment affects light stable isotopes. Hydrogen is preferentially fractionated into the vapor phase from water boiling below 223&deg;C; above this temperature deuterium is selectively enriched in the vapor phase. In certain environments boiling creates a vapor-dominated system in which the condensate is swept away by meteoric waters and the H/D in the residual fluids is progressively increased through time.&nbsp;</p>","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Reston, VA","usgsCitation":"Cunningham, C.G., 1978, Pressure gradients and boiling as mechanisms for localizing ore in porphyry systems: Journal of Research of the U.S. Geological Survey, v. 6, no. 6, p. 745-754.","productDescription":"10 p.","startPage":"745","endPage":"754","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[],"links":[{"id":315051,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"},{"id":315050,"rank":1,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/journal/1978/vol6issue6/report.pdf","text":"Report","size":"26.93 MB","linkFileType":{"id":1,"text":"pdf"},"description":"Report"}],"country":"United States","state":"Utah","city":"Bingham","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -112.19547271728516,\n              40.48429842982662\n            ],\n            [\n              -112.19547271728516,\n              40.56598102500838\n            ],\n            [\n              -112.1000289916992,\n              40.56598102500838\n            ],\n            [\n              -112.1000289916992,\n              40.48429842982662\n            ],\n            [\n              -112.19547271728516,\n              40.48429842982662\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","volume":"6","issue":"6","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"56ac9b75e4b0403299f53b0a","contributors":{"authors":[{"text":"Cunningham, Charles G.","contributorId":85940,"corporation":false,"usgs":true,"family":"Cunningham","given":"Charles","email":"","middleInitial":"G.","affiliations":[],"preferred":false,"id":590226,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":70162702,"text":"70162702 - 1978 - Solubility of highly soluble salts in aqueous media - Part 1, NaCl, KCl, CaCl<sub>2</sub>, Na<sub>2</sub>SO<sub>4</sub>, and K<sub>2</sub>SO<sub>4</sub> solubilities to 100°C","interactions":[],"lastModifiedDate":"2016-01-29T11:09:33","indexId":"70162702","displayToPublicDate":"2008-12-28T00:00:00","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":"Solubility of highly soluble salts in aqueous media - Part 1, NaCl, KCl, CaCl<sub>2</sub>, Na<sub>2</sub>SO<sub>4</sub>, and K<sub>2</sub>SO<sub>4</sub> solubilities to 100°C","docAbstract":"<p>&nbsp;A modified visual method for determining the solubility of highly soluble salts in aqueous media up to 100&deg; C is presented. The solubilities of NaCl, KCl, CaCl<sub>2</sub>, Na<sub>2</sub>SO<sub>4</sub>, and K<sub>2</sub>SO<sub>4</sub> were determined up to 100&deg; C. The tabulated experimental data and the fitted equations describing the data indicate that the previous literature data for the solubility of these salts were generally high by 0.05 to 2.0 weight percent salt.&nbsp;</p>","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Reston, VA","usgsCitation":"Potter, R.W., and Clynne, M.A., 1978, Solubility of highly soluble salts in aqueous media - Part 1, NaCl, KCl, CaCl<sub>2</sub>, Na<sub>2</sub>SO<sub>4</sub>, and K<sub>2</sub>SO<sub>4</sub> solubilities to 100°C: Journal of Research of the U.S. Geological Survey, v. 6, no. 6, p. 701-705.","productDescription":"5 p.","startPage":"701","endPage":"705","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[],"links":[{"id":315038,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"},{"id":315037,"rank":1,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/journal/1978/vol6issue6/report.pdf","text":"Report","size":"26.93 BM","linkFileType":{"id":1,"text":"pdf"},"description":"Report"}],"volume":"6","issue":"6","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"56ac9b80e4b0403299f53b35","contributors":{"authors":[{"text":"Potter, Robert W. II","contributorId":67899,"corporation":false,"usgs":true,"family":"Potter","given":"Robert","suffix":"II","email":"","middleInitial":"W.","affiliations":[],"preferred":false,"id":590200,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Clynne, Michael A. 0000-0002-4220-2968 mclynne@usgs.gov","orcid":"https://orcid.org/0000-0002-4220-2968","contributorId":2032,"corporation":false,"usgs":true,"family":"Clynne","given":"Michael","email":"mclynne@usgs.gov","middleInitial":"A.","affiliations":[{"id":617,"text":"Volcano Science Center","active":true,"usgs":true}],"preferred":true,"id":590201,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":70162707,"text":"70162707 - 1978 - Age and composition of igneous rocks, Edna Mountain quadrangle, Humboldt County, Nevada","interactions":[],"lastModifiedDate":"2016-01-29T10:59:35","indexId":"70162707","displayToPublicDate":"2008-12-28T00:00:00","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":"Age and composition of igneous rocks, Edna Mountain quadrangle, Humboldt County, Nevada","docAbstract":"<p>Six pulses of igneous activity ranging in age from Jurassic to Pliocene have been identified in the Edna Mountain quadrangle, Humboldt County, Nev. Porphyritic syenite am! quartz monzonite of Jurassic age (146-164 million years) at Buffalo Mountain are highly potassic through a wide range in SiO<sub>2</sub> content from olivine-bearing syenite to quartz-rich monzonite, and their composition contrasts sharply with plutons elsewhere in north-central Nevada. Granodiorite and quartz monzonite plutons of Cretaceous age (88- 106 m.y.) are chemically and mineralogically similar to other calc-alkaline plutons in north-central Nevada. Four episodes of Tertiary volcanism include rhyolite ashflow tuffs and slightly younger andesitic basalt flows and tuffs of Oligocene age, rhyolite vitrophyre of late Miocene age, and olivine basalt flows of Pliocene age. Their age and mineralogical and chemical compositions are similar to other Tertiary volcanic rocks in north-central Nevada.</p>","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Reston, VA","usgsCitation":"Erickson, R., Silberman, M.L., and Marsh, S., 1978, Age and composition of igneous rocks, Edna Mountain quadrangle, Humboldt County, Nevada: Journal of Research of the U.S. Geological Survey, v. 6, no. 6, p. 727-743.","productDescription":"17 p.","startPage":"727","endPage":"743","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[],"links":[{"id":315047,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"},{"id":315046,"rank":1,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/journal/1978/vol6issue6/report.pdf","text":"Report","size":"26.93 MB","linkFileType":{"id":1,"text":"pdf"},"description":"Report"}],"country":"United States","state":"Nevada","county":"Humboldt County","otherGeospatial":"Edna Mountain quadrangle","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -117.5,\n              40.75\n            ],\n            [\n              -117.5,\n              41\n            ],\n            [\n              -117.25,\n              41\n            ],\n            [\n              -117.25,\n              40.75\n            ],\n            [\n              -117.5,\n              40.75\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","volume":"6","issue":"6","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"56ac9b45e4b0403299f539c3","contributors":{"authors":[{"text":"Erickson, Ralph L.","contributorId":51599,"corporation":false,"usgs":true,"family":"Erickson","given":"Ralph L.","affiliations":[],"preferred":false,"id":590217,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Silberman, Miles L.","contributorId":23947,"corporation":false,"usgs":true,"family":"Silberman","given":"Miles","email":"","middleInitial":"L.","affiliations":[],"preferred":false,"id":590218,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Marsh, S.P.","contributorId":32913,"corporation":false,"usgs":true,"family":"Marsh","given":"S.P.","email":"","affiliations":[],"preferred":false,"id":590219,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":70162703,"text":"70162703 - 1978 - Iron-titanium oxide minerals and associated alteration phases in some uranium-bearing sandstones","interactions":[],"lastModifiedDate":"2016-01-29T10:50:16","indexId":"70162703","displayToPublicDate":"2008-12-28T00:00:00","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":"Iron-titanium oxide minerals and associated alteration phases in some uranium-bearing sandstones","docAbstract":"<p>Detrital iron-titanium (Fe-Ti) oxide minerals of the ulvospinel-magnetite (titanomagnetite) and ilmenite-hematite (titanohematite) solid solution series are common in uranium-bearing sandstones. Alteration of Fe-Ti oxide minerals in oxidizing environments formed secondary products (primarily hematite) that are distinct from those produced under reducing conditions (iron disulfide minerals). Oxidation of sulfidized Fe-Ti oxide minerals, by the processes that formed uranium rolls, produced ferric oxide minerals (limonite) having textures that mimic those of the iron disulfides. Titanomagnetite and titanohematite have been severely depleted in the ore-bearing zones of some uranium deposits. The alteration of detrital Fe-Ti oxide minerals near uranium ore deposits may produce characteristic signatures in the magnetization of the sandstone. Knowledge of the distribution and magnetic properties of these minerals can aid in interpreting data from total magnetic-field and magnetic-susceptibility surveys of uranium deposits.&nbsp;</p>","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Reston, VA","usgsCitation":"Reynolds, R.L., and Goldhaber, M.B., 1978, Iron-titanium oxide minerals and associated alteration phases in some uranium-bearing sandstones: Journal of Research of the U.S. Geological Survey, v. 6, no. 6, p. 707-714.","productDescription":"8 p.","startPage":"707","endPage":"714","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[],"links":[{"id":315040,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"},{"id":315039,"rank":1,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/journal/1978/vol6issue6/report.pdf","text":"Report","size":"26.93 MB","linkFileType":{"id":1,"text":"pdf"},"description":"Report"}],"country":"United States","state":"Colorado, New Mexico, Texas, Wyoming","county":"Live Oak County, Johnson County, Karnes County, Webb County, Weld County","otherGeospatial":"Grants mineral belt, Powder River Basin","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -95.0537109375,\n              28.86391842622456\n            ],\n            [\n              -94.85595703125,\n              29.420460341013133\n            ],\n            [\n              -95.16357421875,\n              29.954934549656144\n            ],\n            [\n              -99.90966796875,\n              30.713503990354965\n            ],\n            [\n              -101.4697265625,\n              30.29701788337205\n            ],\n            [\n              -101.44775390625,\n              29.6880527498568\n 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,{"id":70162720,"text":"70162720 - 1978 - Conductive heat flows in research drill holes in thermal areas of Yellowstone National Park, Wyoming","interactions":[],"lastModifiedDate":"2016-01-29T11:52:13","indexId":"70162720","displayToPublicDate":"2008-12-28T00:00:00","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":"Conductive heat flows in research drill holes in thermal areas of Yellowstone National Park, Wyoming","docAbstract":"<p>In convection systems with boiling springs, geysers, fumaroles, and other thermal features, the modes of heat flow become increasingly complex as a single liquid phase at depth rises into the near-surface environment where heat flows by convection of liquid and vapor and by conduction in high thermal gradients. This paper is mainly concerned with the changing patterns of conductive heat flow as related to channels of subsurface convective flow and to horizontal distance from spring vents. The primary data consist of temperatures measured in 13 cored drill holes as drilling progressed. Some temperatures plot convincingly on straight-line segments that suggest conductive gradients in rocks of nearly constant thermal conductivity. Temperature gradients and the conductive component of total heat flow nearly always decrease drastically downward; the gradient and heat flow of the lowest depth interval recognized in each hole is commonly only about 10 percent of the highest interval; the changes in gradient at interval boundaries are commonly interpreted as channels of near-boiling water or of cooler meteoric water. Temperature reversals are probably related to inflowing cooler water rather than to transient effects from recent changes. Some temperatures plot on curved segments that probably indicate dispersed convective upflow and boiling of water in ground penetrated by the drill hole. Other similar curved segments are too low in temperature for local boiling and are probably on the margins of hot upflow zones, reflecting conductive cooling of flowing water. The conifers of Yellowstone National Park (mainly lodgepole pine) seem to have normal growth characteristics where near-surface conductive heat flow is below about 200 heat-flow units (1 HFU = 10<sup>-6</sup> cal/cm<sup>2</sup> = 41.8 mW/m<sup>2</sup>). Most areas of abnormal \"stunted\" trees (low ratio of height to base diameter, and low density of spacing) are characterized by conductive heat flows of about 250 to 350 HFU. The critical factor affecting growth is probably the seasonal maximum soil temperature at the root depths preferred by each form, rather than the heat flow as such. Heat flows up to 300 HFU are greatly dominated near the surface by conduction and are little affected by convection within the measured intervals. With increasing total heat flow above 300 HFU, the convection component, as indicated by snowfall calorimetry, becomes increasingly important. Snowfall calorimetry and tree growth as related to heat flow are calibrated by the heat-flow data considered here. Both snowfall calorimetry and tree growth patterns can be extrapolated rapidly, although without high precision, to thermal areas that lack subsurface data.</p>","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Reston, VA","usgsCitation":"White, D.E., 1978, Conductive heat flows in research drill holes in thermal areas of Yellowstone National Park, Wyoming: Journal of Research of the U.S. Geological Survey, v. 6, no. 6, p. 765-774.","productDescription":"10 p.","startPage":"765","endPage":"774","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[],"links":[{"id":315067,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"},{"id":315066,"rank":1,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/journal/1978/vol6issue6/report.pdf","text":"Report","size":"26.93 MB","linkFileType":{"id":1,"text":"pdf"},"description":"Report"}],"country":"United States","state":"Wyoming","otherGeospatial":"Yellowstone National Park","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -111.09100341796875,\n              45.11423838585088\n            ],\n            [\n              -111.00036621093749,\n              45.11423838585088\n            ],\n            [\n              -110.81085205078125,\n              45.10842333769411\n            ],\n            [\n              -110.53619384765625,\n              45.06576154770312\n            ],\n            [\n              -110.32196044921874,\n              45.05606124274415\n            ],\n            [\n              -110.08026123046874,\n              45.03665569548622\n            ],\n            [\n              -109.918212890625,\n              45.023067895446175\n            ],\n            [\n              -109.90447998046875,\n              44.98034238084973\n            ],\n            [\n              -109.9017333984375,\n              44.89285004222294\n            ],\n            [\n              -109.90997314453125,\n              44.811070253260006\n            ],\n            [\n              -109.8687744140625,\n              44.75453548416007\n            ],\n            [\n              -109.81658935546875,\n              44.72136867346628\n            ],\n            [\n              -109.81109619140625,\n              44.678418678188606\n            ],\n            [\n              -109.87701416015624,\n              44.64716230650056\n            ],\n            [\n              -109.984130859375,\n              44.61784415342067\n            ],\n            [\n              -110.06103515625,\n              44.5826428195842\n            ],\n            [\n              -110.137939453125,\n              44.55133484083592\n            ],\n            [\n              -110.10772705078125,\n              44.53371669765759\n            ],\n            [\n              -110.08026123046874,\n              44.52001001133986\n            ],\n            [\n              -109.97314453125,\n              44.4906276800508\n            ],\n            [\n              -109.97039794921874,\n              44.453388800301774\n            ],\n            [\n              -109.99786376953125,\n              44.44554600843547\n            ],\n            [\n              -110.0445556640625,\n              44.422011314236634\n            ],\n            [\n              -110.06378173828125,\n              44.39454219215587\n            ],\n            [\n              -110.01983642578125,\n              44.33956524809713\n            ],\n            [\n              -109.94018554687499,\n              44.1289994645142\n            ],\n            [\n              -111.082763671875,\n              44.125056482685146\n            ],\n            [\n              -111.09100341796875,\n              45.11423838585088\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","volume":"6","issue":"6","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"56ac9b4be4b0403299f539d4","contributors":{"authors":[{"text":"White, Donald E.","contributorId":76787,"corporation":false,"usgs":true,"family":"White","given":"Donald","email":"","middleInitial":"E.","affiliations":[],"preferred":false,"id":590295,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":79016,"text":"wdrTX773 - 1978 - Water resources data for Texas, water year 1977, volume 3. Colorado River basin, Lavaca River basin, Guadalupe River basin, Nueces River basin, Rio Grande basin, and intervening coastal basins","interactions":[],"lastModifiedDate":"2020-12-15T17:32:46.426867","indexId":"wdrTX773","displayToPublicDate":"2006-08-31T00:00:00","publicationYear":"1978","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":340,"text":"Water Data Report","code":"WDR","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"TX-77-3","title":"Water resources data for Texas, water year 1977, volume 3. Colorado River basin, Lavaca River basin, Guadalupe River basin, Nueces River basin, Rio Grande basin, and intervening coastal basins","docAbstract":"<p>No abstract available.</p>","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Reston, VA","doi":"10.3133/wdrTX773","usgsCitation":"Water Resources Division, U.S. Geological Survey, 1978, Water resources data for Texas, water year 1977, volume 3. 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,{"id":70012507,"text":"70012507 - 1978 - Geology, palynology, and climatic significance of two pre-Pinedale Lake sediment sequences in and near Yellowstone National Park","interactions":[],"lastModifiedDate":"2025-07-14T15:23:10.460409","indexId":"70012507","displayToPublicDate":"2004-11-19T00:00:00","publicationYear":"1978","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":3218,"text":"Quaternary Research","active":true,"publicationSubtype":{"id":10}},"title":"Geology, palynology, and climatic significance of two pre-Pinedale Lake sediment sequences in and near Yellowstone National Park","docAbstract":"<p><span>Pollen analysis of a section of lake sediments at Grassy Lake Reservoir indicates a vegetational sequence changing from tundra, to spruce-fir-pine forest, to pine forest, to tundra at the top. Pollen analysis of a section of lake sediments on Beaverdam Creek indicates a tundra vegetation at the base, followed by a brief episode of spruce-fir forest and a return to a tundra vegetation at the top. The analyses of both sections suggest a cold to cool to cold climatic sequence, interpreted as interstadial in character. However, differences suggest that they represent separate interstadials. Pinedale Till disconformably overlies the lake deposits at Grassy Lake Reservoir. The upper sediments contain wood&nbsp;</span><sup>14</sup><span>C dated at &gt;42,000 yr; the lowermost interfinger with till shown to be more than about 70,000 yr old. The deposits at Beaverdam Creek grade upward into proglacial Pinedale deposits, contain an ash that is probably about 70,000 yr old near their base, and rest comformably on gravel that grades down into lake sediments containing wood debris suggestive of an older climatic amelioration. We conclude that the warmest part of the interstadial at Grassy Lake Reservoir is probably more than 70,000 yr old, and that the warmest part of the interstadial analyzed at Beaverdam Creek is slightly younger than 70,000 yr old.</span></p>","language":"English","publisher":"Elsevier","doi":"10.1016/0033-5894(78)90103-5","issn":"00335894","usgsCitation":"Baker, R.G., and Richmond, G., 1978, Geology, palynology, and climatic significance of two pre-Pinedale Lake sediment sequences in and near Yellowstone National Park: Quaternary Research, v. 10, no. 2, p. 226-240, https://doi.org/10.1016/0033-5894(78)90103-5.","productDescription":"22 p.","startPage":"226","endPage":"240","costCenters":[],"links":[{"id":222482,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United States","state":"Wyoming","otherGeospatial":"Yellowstone National Park","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"coordinates\": [\n          [\n            [\n              -111.0751411481957,\n              44.98990838492284\n            ],\n            [\n              -111.0751411481957,\n              43.84603059555195\n            ],\n            [\n              -109.2200234684439,\n              43.84603059555195\n            ],\n            [\n              -109.2200234684439,\n              44.98990838492284\n            ],\n            [\n              -111.0751411481957,\n              44.98990838492284\n            ]\n          ]\n        ],\n        \"type\": \"Polygon\"\n      }\n    }\n  ]\n}","volume":"10","issue":"2","noUsgsAuthors":false,"publicationDate":"2017-01-20","publicationStatus":"PW","scienceBaseUri":"505a274be4b0c8380cd59758","contributors":{"authors":[{"text":"Baker, R. G.","contributorId":96326,"corporation":false,"usgs":true,"family":"Baker","given":"R.","email":"","middleInitial":"G.","affiliations":[],"preferred":false,"id":363776,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Richmond, G.M.","contributorId":104066,"corporation":false,"usgs":true,"family":"Richmond","given":"G.M.","email":"","affiliations":[],"preferred":false,"id":363777,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":70012474,"text":"70012474 - 1978 - The geochemical nature of the Archean Ancient Gneiss Complex and Granodiorite Suite, Swaziland: A preliminary study","interactions":[],"lastModifiedDate":"2025-06-25T16:21:16.807811","indexId":"70012474","displayToPublicDate":"2003-04-22T00:00:00","publicationYear":"1978","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":"The geochemical nature of the Archean Ancient Gneiss Complex and Granodiorite Suite, Swaziland: A preliminary study","docAbstract":"<p>The Ancient Gneiss Complex (AGC) of Swaziland, an Archean gray gneiss complex, lies southeast and south of the Barberton greenstone belt and includes the most structurally complex and highly metamorphosed portions of the eastern Kaapvaal craton. The AGC is not precisely dated but apparently is older than 3.4 Ga. </p><p>The AGC consists of three major units: (a) a bimodal suite of closely interlayered siliceous, low-K gneisses and metabasalt; (b) homogeneous tonalite gneiss; and (c) interlayered siliceous microcline gneiss, metabasalt, and minor metasedimentary rocks - termed the metamorphite suite. A geologically younger gabbro-diorite-tonalite-trondhjemite suite, the Granodiorite Suite, is spatially associated with the AGC and intrusive into it. </p><p><span>The bimodal suite consists largely of two types of low-K siliceous gneiss: one has SiO</span><sub>2</sub><span>&nbsp;&lt; 75%, Al</span><sub>2</sub><span>O</span><sub>3</sub><span>&nbsp;&gt; 14%, low Rb/Sr ratios, and depleted heavy rare earth elements (REE's); the other has SiO</span><sub>2</sub><span>&nbsp;&gt; 75%, Al</span><sub>2</sub><span>O</span><sub>3</sub><span>&nbsp;&lt; 13%, high Rb/Sr ratios, and relatively abundant REE's except for negative Eu anomalies. The interlayered metabasalt ranges from komatiitic to tholeiitic compositions. Lenses of quartz monzonitic gneiss of K</span><sub>2</sub><span>O/Na</span><sub>2</sub><span>O close to 1 form a minor part of the bimodal suite. Tonalitic to trondhjemitic migmatite locally is abundant and has major-element abundances similar to those of non-migmatitic varieties.</span></p><p><span>The siliceous gneisses of the metamorphic suite show low Al<sub>2</sub>O, K<sub>2</sub>O/Na<sub>2</sub>O ratios of about 1, high Rb/Sr ratios, moderate REE abundances and negative Eu anomalies.</span></p><p><span>K/Rb ratios of siliceous gneisses of the bimodal suite are very low (∼130); of the tonalitic gneiss, low (∼225); of the siliceous gneiss of the metamorphite suite, moderate (∼300); and of the Granodiorite Suite, high (∼400).</span></p><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\">Rocks of the AGC differ geochemically in several ways from the siliceous volcanic and hypabyssal rocks of the Upper Onverwacht Group and from the diapirs of tonalite and trondhjemite that intrude the Swaziland Group.</div></div></div></div>","language":"English","publisher":"Elsevier","doi":"10.1016/0301-9268(78)90030-X","issn":"03019268","usgsCitation":"Hunter, D., Barker, F., and Millard, H.T., 1978, The geochemical nature of the Archean Ancient Gneiss Complex and Granodiorite Suite, Swaziland: A preliminary study: Precambrian Research, v. 7, no. 2, p. 105-127, https://doi.org/10.1016/0301-9268(78)90030-X.","productDescription":"23 p.","startPage":"105","endPage":"127","costCenters":[],"links":[{"id":221950,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"Swaziland","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"coordinates\": [\n          [\n            [\n              30.780899794709285,\n              -26.344636983911485\n            ],\n            [\n              30.76332234900437,\n              -26.832480582339464\n            ],\n            [\n              31.15528888811218,\n              -27.298159794948003\n            ],\n            [\n              31.633001593264552,\n              -27.382290599335775\n            ],\n            [\n              32.03126113798115,\n              -27.34122746106911\n            ],\n            [\n              32.1419333674333,\n              -26.79468549786896\n            ],\n            [\n              32.11986818572147,\n              -25.980812790528415\n            ],\n            [\n              31.881769159493246,\n              -25.94688427657203\n            ],\n            [\n              31.467733137262144,\n              -25.67404709425115\n            ],\n            [\n              31.260986022371213,\n              -25.730037809838826\n            ],\n            [\n              30.780899794709285,\n              -26.344636983911485\n            ]\n          ]\n        ],\n        \"type\": \"Polygon\"\n      }\n    }\n  ]\n}","volume":"7","issue":"2","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"505bac49e4b08c986b3233c4","contributors":{"authors":[{"text":"Hunter, D.R.","contributorId":79909,"corporation":false,"usgs":true,"family":"Hunter","given":"D.R.","email":"","affiliations":[],"preferred":false,"id":363697,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Barker, F.","contributorId":101368,"corporation":false,"usgs":true,"family":"Barker","given":"F.","affiliations":[],"preferred":false,"id":363698,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Millard, Hugh T. Jr.","contributorId":67502,"corporation":false,"usgs":true,"family":"Millard","given":"Hugh","suffix":"Jr.","email":"","middleInitial":"T.","affiliations":[],"preferred":false,"id":363696,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":70012449,"text":"70012449 - 1978 - A sediment-dispersal model for the South Texas continental shelf, northwest Gulf of Mexico","interactions":[],"lastModifiedDate":"2025-04-17T17:36:01.605612","indexId":"70012449","displayToPublicDate":"2003-04-15T00:00:00","publicationYear":"1978","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":"A sediment-dispersal model for the South Texas continental shelf, northwest Gulf of Mexico","docAbstract":"<p>Textural-distribution patterns of sea-floor sediments on the South Texas continental shelf between Matagorda Bay and the U.S.-Mexico international boundary were evaluated as part of a regional environmental-studies program. Sediment textural gradients support a conceptual model for the regional sediment-dispersal system, which is characterized by both net offshore transport and net south-trending coastwise transport components on a wind-dominated shelf. Coastwise transport results in the net southward migration of both palimpsest sandy mud composing the ancestral Brazos-Colorado delta flank in the northern sector, and modern mud composing the central sector; these migrating sediments are encroaching southward onto immobile relict muddy sands composing the ancestral Rio Grande delta in the southern sector. </p><p>In the proposed model, the suspension transport of modern silt-enriched mud derived mainly from coastal sources is the dominant dispersal mechanism. Net offshore transport is attributed both to diffusion, and to the advective ebb-tide discharge of turbid lagoonal-estuarine waters from coastal inlets. Net southward transport is attributed mainly to advection by seasonally residual coastwise drift currents reflecting a winter-dominated hydraulic regime. Frequent winter storms characterized by relatively high-speed northerly winds that accompany the passage of cold fronts appear to be dominant regional dispersal agents.</p>","language":"English","publisher":"Elsevier","doi":"10.1016/0025-3227(78)90064-6","issn":"00253227","usgsCitation":"Shideler, G.L., 1978, A sediment-dispersal model for the South Texas continental shelf, northwest Gulf of Mexico: Marine Geology, v. 26, no. 3-4, p. 289-313, https://doi.org/10.1016/0025-3227(78)90064-6.","productDescription":"25 p.","startPage":"289","endPage":"313","costCenters":[],"links":[{"id":222418,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United States","state":"Texas","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"coordinates\": [\n          [\n            [\n              -97.30823853261406,\n              28.02493852519791\n            ],\n            [\n              -97.30823853261406,\n              25.22865383447872\n            ],\n            [\n              -96.79586019808089,\n              25.22865383447872\n            ],\n            [\n              -96.79586019808089,\n              28.02493852519791\n            ],\n            [\n              -97.30823853261406,\n              28.02493852519791\n            ]\n          ]\n        ],\n        \"type\": \"Polygon\"\n      }\n    }\n  ]\n}","volume":"26","issue":"3-4","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"5059e57fe4b0c8380cd46d8a","contributors":{"authors":[{"text":"Shideler, G. L.","contributorId":63393,"corporation":false,"usgs":true,"family":"Shideler","given":"G.","email":"","middleInitial":"L.","affiliations":[],"preferred":false,"id":363602,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":70012556,"text":"70012556 - 1978 - Distribution and character of upper Mesozoic subduction complexes along the west coast of North America","interactions":[],"lastModifiedDate":"2025-09-02T16:19:17.039021","indexId":"70012556","displayToPublicDate":"2003-04-11T00:00:00","publicationYear":"1978","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":3525,"text":"Tectonophysics","active":true,"publicationSubtype":{"id":10}},"title":"Distribution and character of upper Mesozoic subduction complexes along the west coast of North America","docAbstract":"<p><span>Structurally complex sequences of sedimentary, volcanic, and intrusive igneous rocks characterize a nearly continuous narrow band along the Pacific coast of North America from Baja California, Mexico to southern Alaska. They occur in two modes: (1) as complexly folded but coherent sequences of graywacke and argillite that locally exhibit blueschist-grade metamorphism, and (2) as melanges containing large blocks of graywacke, chert, volcanic and plutonic rocks, high-grade schist, and limestone in a highly sheared pelitic, cherty, or sandstone matrix. Fossils from the coherent graywacke sequences range in age from late Jurassic to Eocene; fossils from limestone blocks in the melanges range in age from mid-Paleozoic to middle Cretaceous. Fossils from the matrix surrounding the blocks, however, are of Jurassic, Cretaceous, and rarely, Tertiary age, indicating that fossils from the blocks cannot be used to date the time of formation of the melanges.</span></p><p><span>Both the deformation of the graywacke, with accompanying blueschist metamorphism, as well as the formation of the melanges, are believed to be the result of late Mesozoic and early Tertiary subduction. The origin of the melanges, particularly the emplacement of exotic tectonic blocks, is not understood.</span></p>","language":"English","publisher":"Elsevier","doi":"10.1016/0040-1951(78)90031-8","issn":"00401951","usgsCitation":"Jones, D.L., Blake, M., Bailey, E.H., and McLaughlin, R.J., 1978, Distribution and character of upper Mesozoic subduction complexes along the west coast of North America: Tectonophysics, v. 47, no. 3-4, p. 207-222, https://doi.org/10.1016/0040-1951(78)90031-8.","productDescription":"16 p.","startPage":"207","endPage":"222","costCenters":[{"id":312,"text":"Geology, Minerals, Energy, and Geophysics Science Center","active":true,"usgs":true}],"links":[{"id":222209,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"Canada, Mexico, United States","state":"Alaska, California, Oregon, Washington","otherGeospatial":"Pacific coast of North America","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"coordinates\": [\n          [\n            [\n              -154.41285894795098,\n              60.39101073090987\n            ],\n            [\n              -139.43492469830107,\n              56.18442278816785\n            ],\n            [\n              -127.41314296806209,\n              47.475629746329844\n            ],\n            [\n              -124.45488000214503,\n              36.374566798936016\n            ],\n            [\n              -110.61276212523683,\n              21.147885276292897\n            ],\n            [\n              -108.04987973063052,\n              22.069396089742753\n            ],\n            [\n              -119.6495023669611,\n              39.75914188879055\n            ],\n            [\n              -122.86602155790652,\n              49.694221938084205\n            ],\n            [\n              -134.69578953504842,\n              60.73706770472893\n            ],\n            [\n              -145.72029861273748,\n              61.97887606686548\n            ],\n            [\n              -154.41285894795098,\n              60.39101073090987\n            ]\n          ]\n        ],\n        \"type\": \"Polygon\"\n      }\n    }\n  ]\n}","volume":"47","issue":"3-4","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"505a027ee4b0c8380cd50082","contributors":{"authors":[{"text":"Jones, D. L.","contributorId":65045,"corporation":false,"usgs":true,"family":"Jones","given":"D.","email":"","middleInitial":"L.","affiliations":[],"preferred":false,"id":363898,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Blake, M.C. Jr.","contributorId":27094,"corporation":false,"usgs":true,"family":"Blake","given":"M.C.","suffix":"Jr.","affiliations":[],"preferred":false,"id":363896,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Bailey, E. H.","contributorId":44509,"corporation":false,"usgs":true,"family":"Bailey","given":"E.","email":"","middleInitial":"H.","affiliations":[],"preferred":false,"id":363897,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"McLaughlin, R. 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