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,{"id":1007817,"text":"1007817 - 1988 - Experimental evidence for sibling recognition in Common Terns (Sterna hirundo)","interactions":[],"lastModifiedDate":"2026-05-12T13:28:37.234729","indexId":"1007817","displayToPublicDate":"1988-01-01T00:00:00","publicationYear":"1988","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":3544,"text":"The Auk","onlineIssn":"1938-4254","printIssn":"0004-8038","active":true,"publicationSubtype":{"id":10}},"displayTitle":"Experimental evidence for sibling recognition in Common Terns (<i>Sterna hirundo</i>)","title":"Experimental evidence for sibling recognition in Common Terns (Sterna hirundo)","docAbstract":"<p>Young Common Terns (<i>Sterna hirundo</i>) did not respond preferentially to calls of siblings at 8 and 9 days of age, but did so by 12 days of age. In experiments with and without visual isolation, and with use of playback, we demonstrated a tendency to approach sibling begging calls. This differential response indicated sibling-recognition occurred, was based on experience, and involved vocal cues.</p>","language":"English","publisher":"American Ornithological Society","doi":"10.1093/auk/105.1.142","usgsCitation":"Burger, J., Gochfeld, M., and Boarman, W., 1988, Experimental evidence for sibling recognition in Common Terns (Sterna hirundo): The Auk, v. 105, no. 1, p. 142-148, https://doi.org/10.1093/auk/105.1.142.","productDescription":"7 p.","startPage":"142","endPage":"148","costCenters":[{"id":651,"text":"Western Ecological Research Center","active":true,"usgs":true}],"links":[{"id":504364,"rank":2,"type":{"id":41,"text":"Open Access External Repository Page"},"url":"https://digitalcommons.usf.edu/auk/vol105/iss1/19","text":"External Repository"},{"id":129848,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"105","issue":"1","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b24e4b07f02db6ae762","contributors":{"authors":[{"text":"Burger, J.","contributorId":25894,"corporation":false,"usgs":true,"family":"Burger","given":"J.","email":"","affiliations":[],"preferred":false,"id":316083,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Gochfeld, M.","contributorId":88309,"corporation":false,"usgs":true,"family":"Gochfeld","given":"M.","affiliations":[],"preferred":false,"id":316085,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Boarman, W.I.","contributorId":73523,"corporation":false,"usgs":true,"family":"Boarman","given":"W.I.","email":"","affiliations":[],"preferred":false,"id":316084,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":2001199,"text":"2001199 - 1988 - Oral toxicity of rotenone to mammals","interactions":[],"lastModifiedDate":"2012-02-02T00:15:00","indexId":"2001199","displayToPublicDate":"1988-01-01T00:00:00","publicationYear":"1988","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":1,"text":"Federal Government Series"},"seriesTitle":{"id":39,"text":"Investigations in Fish Control","active":false,"publicationSubtype":{"id":1}},"seriesNumber":"94","title":"Oral toxicity of rotenone to mammals","docAbstract":"Abstract not submitted to date","language":"English","publisher":"U.S. Fish and Wildlife Service","publisherLocation":"La Crosse, WI","usgsCitation":"Marking, L.L., 1988, Oral toxicity of rotenone to mammals: Investigations in Fish Control 94, 5.","productDescription":"5","startPage":"0","endPage":"5","numberOfPages":"5","costCenters":[{"id":606,"text":"Upper Midwest Environmental Sciences Center","active":true,"usgs":true}],"links":[{"id":198665,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4aeee4b07f02db69134d","contributors":{"authors":[{"text":"Marking, L. L.","contributorId":90661,"corporation":false,"usgs":true,"family":"Marking","given":"L.","middleInitial":"L.","affiliations":[],"preferred":false,"id":325556,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":1004129,"text":"1004129 - 1988 - An outbreak of type E botulism among common loons (<i>Gavia immer</i>) in Michigan's Upper Peninsula","interactions":[],"lastModifiedDate":"2015-05-15T16:41:25","indexId":"1004129","displayToPublicDate":"1988-01-01T00:00:00","publicationYear":"1988","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":2507,"text":"Journal of Wildlife Diseases","active":true,"publicationSubtype":{"id":10}},"title":"An outbreak of type E botulism among common loons (<i>Gavia immer</i>) in Michigan's Upper Peninsula","docAbstract":"<p>An epizootic of type E botulism (Clostridium botulinum) occurred among common loons (Gavia immer) along the Lake Michigan shore of Michigan's Upper Peninsula (USA) during October and November 1983. An estimated 592 dead loons washed ashore along the Garden Peninsula. Type E botulinal toxin was demonstrated in blood samples and stomach contents of dead loons, and in samples of three species of dead fish found on the Lake Michigan shore. We suspect that loons acquired botulism by ingesting sick or dead fish containing type E toxin.</p>","language":"English","publisher":"Wildlife Disease Association","doi":"10.7589/0090-3558-24.3.471","usgsCitation":"Brand, C.J., Schmitt, S., Duncan, R.M., and Cooley, T.M., 1988, An outbreak of type E botulism among common loons (<i>Gavia immer</i>) in Michigan's Upper Peninsula: Journal of Wildlife Diseases, v. 24, no. 3, p. 471-476, https://doi.org/10.7589/0090-3558-24.3.471.","productDescription":"6 p.","startPage":"471","endPage":"476","numberOfPages":"6","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[{"id":456,"text":"National Wildlife Health Center","active":true,"usgs":true}],"links":[{"id":480044,"rank":2,"type":{"id":40,"text":"Open Access Publisher Index Page"},"url":"https://doi.org/10.7589/0090-3558-24.3.471","text":"Publisher Index Page"},{"id":130557,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United States","state":"Michigan","otherGeospatial":"Garden Peninsula of Michigan's Upper Peninsula","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -86.76864624023438,\n              45.670684230297006\n            ],\n            [\n              -86.583251953125,\n              45.88044870856469\n            ],\n            [\n              -86.52969360351562,\n              45.96833360206372\n            ],\n            [\n              -86.2481689453125,\n              45.94064578150488\n            ],\n            [\n              -86.32507324218749,\n              45.789551885661844\n            ],\n            [\n              -86.5887451171875,\n              45.6101948758674\n            ],\n            [\n              -86.62582397460938,\n              45.58232862028087\n            ],\n            [\n              -86.67251586914062,\n              45.618840210489346\n            ],\n            [\n              -86.76864624023438,\n              45.670684230297006\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","volume":"24","issue":"3","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ad6e4b07f02db6841e5","contributors":{"authors":[{"text":"Brand, Christopher J. cbrand@usgs.gov","contributorId":1186,"corporation":false,"usgs":true,"family":"Brand","given":"Christopher","email":"cbrand@usgs.gov","middleInitial":"J.","affiliations":[{"id":456,"text":"National Wildlife Health Center","active":true,"usgs":true}],"preferred":true,"id":315241,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Schmitt, Stephen stschmit@usgs.gov","contributorId":1531,"corporation":false,"usgs":true,"family":"Schmitt","given":"Stephen","email":"stschmit@usgs.gov","affiliations":[],"preferred":true,"id":315243,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Duncan, Ruth M.","contributorId":84720,"corporation":false,"usgs":true,"family":"Duncan","given":"Ruth","email":"","middleInitial":"M.","affiliations":[],"preferred":false,"id":315244,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Cooley, Thomas M.","contributorId":48911,"corporation":false,"usgs":true,"family":"Cooley","given":"Thomas","email":"","middleInitial":"M.","affiliations":[],"preferred":false,"id":315242,"contributorType":{"id":1,"text":"Authors"},"rank":4}]}}
,{"id":70185103,"text":"70185103 - 1988 - Testing for individual variation in breeding success","interactions":[],"lastModifiedDate":"2026-05-11T15:40:36.128095","indexId":"70185103","displayToPublicDate":"1988-01-01T00:00:00","publicationYear":"1988","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":3544,"text":"The Auk","onlineIssn":"1938-4254","printIssn":"0004-8038","active":true,"publicationSubtype":{"id":10}},"title":"Testing for individual variation in breeding success","docAbstract":"<p>No abstracta available.&nbsp;</p>","language":"English","publisher":"American Ornithological Society","doi":"10.1093/auk/105.1.193","usgsCitation":"Hatch, S.A., 1988, Testing for individual variation in breeding success: The Auk, v. 105, no. 1, p. 193-194, https://doi.org/10.1093/auk/105.1.193.","productDescription":"2 p.","startPage":"193","endPage":"194","costCenters":[{"id":114,"text":"Alaska Science Center","active":true,"usgs":true}],"links":[{"id":337568,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United States","state":"Alaska","otherGeospatial":"Semidi Islands","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -156.93832397460938,\n              55.9407405184921\n            ],\n            [\n              -156.46865844726562,\n              55.9407405184921\n            ],\n            [\n              -156.46865844726562,\n              56.272336447630416\n            ],\n            [\n              -156.93832397460938,\n              56.272336447630416\n            ],\n            [\n              -156.93832397460938,\n              55.9407405184921\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","volume":"105","issue":"1","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"58c90130e4b0849ce97abd65","contributors":{"authors":[{"text":"Hatch, Scott A. 0000-0002-0064-8187 shatch@usgs.gov","orcid":"https://orcid.org/0000-0002-0064-8187","contributorId":2625,"corporation":false,"usgs":true,"family":"Hatch","given":"Scott","email":"shatch@usgs.gov","middleInitial":"A.","affiliations":[{"id":116,"text":"Alaska Science Center Biology MFEB","active":true,"usgs":true}],"preferred":true,"id":684355,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":26827,"text":"wri874237 - 1988 - Preliminary evaluation of the ground-water resources of Bainbridge Island, Kitsap County, Washington, with a section on geohydrologic units","interactions":[],"lastModifiedDate":"2023-11-22T22:16:45.298995","indexId":"wri874237","displayToPublicDate":"1988-01-01T00:00:00","publicationYear":"1988","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":342,"text":"Water-Resources Investigations Report","code":"WRI","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"87-4237","title":"Preliminary evaluation of the ground-water resources of Bainbridge Island, Kitsap County, Washington, with a section on geohydrologic units","docAbstract":"<p>No abstract available.</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/wri874237","usgsCitation":"Dion, N.P., Olsen, T.D., Payne, K.L., and Jones, M.A., 1988, Preliminary evaluation of the ground-water resources of Bainbridge Island, Kitsap County, Washington, with a section on geohydrologic units: U.S. Geological Survey Water-Resources Investigations Report 87-4237, v, 82 p., https://doi.org/10.3133/wri874237.","productDescription":"v, 82 p.","costCenters":[],"links":[{"id":55719,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wri/1987/4237/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":422856,"rank":3,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_46890.htm","linkFileType":{"id":5,"text":"html"}},{"id":158175,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wri/1987/4237/report-thumb.jpg"}],"country":"United States","state":"Washington","county":"Kitsap County","otherGeospatial":"Bainbridge Island","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"coordinates\": [\n          [\n            [\n              -122.58617788993861,\n              47.68607949212313\n            ],\n            [\n              -122.59513390533918,\n              47.65941221314023\n            ],\n            [\n              -122.58617788993864,\n              47.58851768341307\n            ],\n            [\n              -122.54923432641083,\n              47.592039045067594\n            ],\n            [\n              -122.51527610134973,\n              47.56334190657415\n            ],\n            [\n              -122.47422769742955,\n              47.5663649084112\n            ],\n            [\n              -122.49213972823098,\n              47.7111953167439\n            ],\n            [\n              -122.53094912830078,\n              47.72776498652425\n            ],\n            [\n              -122.5645341860535,\n              47.71696651344584\n            ],\n            [\n              -122.58617788993861,\n              47.68607949212313\n            ]\n          ]\n        ],\n        \"type\": \"Polygon\"\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ac9e4b07f02db67c3ac","contributors":{"authors":[{"text":"Dion, N. P.","contributorId":33302,"corporation":false,"usgs":true,"family":"Dion","given":"N.","email":"","middleInitial":"P.","affiliations":[],"preferred":false,"id":197075,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Olsen, T. D.","contributorId":41463,"corporation":false,"usgs":true,"family":"Olsen","given":"T.","email":"","middleInitial":"D.","affiliations":[],"preferred":false,"id":197076,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Payne, K. L.","contributorId":31771,"corporation":false,"usgs":true,"family":"Payne","given":"K.","email":"","middleInitial":"L.","affiliations":[],"preferred":false,"id":197074,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Jones, M. A.","contributorId":119985,"corporation":false,"usgs":true,"family":"Jones","given":"M.","email":"","middleInitial":"A.","affiliations":[],"preferred":false,"id":888593,"contributorType":{"id":1,"text":"Authors"},"rank":4}]}}
,{"id":1013664,"text":"1013664 - 1988 - Selection to increase survival of smolts in four successive broods of coho salmon","interactions":[],"lastModifiedDate":"2026-04-08T16:20:09.96662","indexId":"1013664","displayToPublicDate":"1988-01-01T00:00:00","publicationYear":"1988","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":3624,"text":"Transactions of the American Fisheries Society","active":true,"publicationSubtype":{"id":10}},"title":"Selection to increase survival of smolts in four successive broods of coho salmon","docAbstract":"<p><span>Survival from smolt to adult for full and half‐sib families of coho salmon&nbsp;</span><i>Oncorhynchus kisutch</i><span>&nbsp;was used to identify families with the highest survival rates at Big Creek Salmon Hatchery in Oregon. Adult fish from families with high survival were bred selectively for four consecutive generations in an attempt to increase smolt survival. A significant improvement in survival in the select line compared to the control after two generations of selection was not maintained in subsequent generations. We concluded that selection was not an effective method for increasing survival of smolts released at Big Creek Hatchery.</span></p>","language":"English","publisher":"American Fisheries Society","doi":"10.1577/1548-8659(1988)117<0090:NSTISO>2.3.CO;2","usgsCitation":"McIntyre, J., Hemmingsen, A., and Simon, R., 1988, Selection to increase survival of smolts in four successive broods of coho salmon: Transactions of the American Fisheries Society, v. 117, no. 1, p. 90-92, https://doi.org/10.1577/1548-8659(1988)117<0090:NSTISO>2.3.CO;2.","productDescription":"3 p.","startPage":"90","endPage":"92","costCenters":[{"id":365,"text":"Leetown Science Center","active":true,"usgs":true}],"links":[{"id":130201,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United States","state":"Oregon","otherGeospatial":"Big Creek Salmon Hatchery","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"coordinates\": [\n          [\n            [\n              -124.13485451365635,\n              46.19452216461943\n            ],\n            [\n              -124.58829175581805,\n              42.54290420167352\n            ],\n            [\n              -124.32035202127034,\n              41.978754121561565\n            ],\n            [\n              -117.0053561466156,\n              42.001768754233524\n            ],\n            [\n              -117.02181841679823,\n              43.275633112923536\n            ],\n            [\n              -117.00965345489296,\n              43.7991673220707\n            ],\n            [\n              -116.83264365994674,\n              44.17395430878513\n            ],\n            [\n              -117.21045878892383,\n              44.306974334227434\n            ],\n            [\n              -117.15526157185003,\n              44.43996739967921\n            ],\n            [\n              -116.43926486634011,\n              45.62091574643888\n            ],\n            [\n              -116.96431421855638,\n              46.00866280694211\n            ],\n            [\n              -119.94143396626627,\n              46.00863941179975\n            ],\n            [\n              -124.13485451365635,\n              46.19452216461943\n            ]\n          ]\n        ],\n        \"type\": \"Polygon\"\n      }\n    }\n  ]\n}","volume":"117","issue":"1","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a00e4b07f02db5f7d35","contributors":{"authors":[{"text":"McIntyre, J.D.","contributorId":27006,"corporation":false,"usgs":true,"family":"McIntyre","given":"J.D.","email":"","affiliations":[],"preferred":false,"id":318994,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Hemmingsen, A.R.","contributorId":84313,"corporation":false,"usgs":true,"family":"Hemmingsen","given":"A.R.","email":"","affiliations":[],"preferred":false,"id":318996,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Simon, R.C.","contributorId":34454,"corporation":false,"usgs":true,"family":"Simon","given":"R.C.","email":"","affiliations":[],"preferred":false,"id":318995,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":70196327,"text":"70196327 - 1988 - Chemical characteristics of prairie lakes in south-central North Dakota--their potential for influencing use by fish and wildlife","interactions":[],"lastModifiedDate":"2018-04-02T15:26:39","indexId":"70196327","displayToPublicDate":"1988-01-01T00:00:00","publicationYear":"1988","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":1,"text":"Federal Government Series"},"seriesTitle":{"id":91,"text":"Technical Report","active":true,"publicationSubtype":{"id":1}},"seriesNumber":"18","title":"Chemical characteristics of prairie lakes in south-central North Dakota--their potential for influencing use by fish and wildlife","docAbstract":"<p>No abstract available.</p>","language":"English","publisher":"U.S. Fish and Wildlife Service","usgsCitation":"Swanson, G., Winter, T.C., Adomaitis, V.A., and LaBaugh, J.W., 1988, Chemical characteristics of prairie lakes in south-central North Dakota--their potential for influencing use by fish and wildlife: Technical Report 18, 44 p.","productDescription":"44 p.","costCenters":[{"id":478,"text":"North Dakota Water Science Center","active":true,"usgs":true},{"id":34685,"text":"Dakota Water Science Center","active":true,"usgs":true}],"links":[{"id":353059,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"5aff338fe4b0da30c1bfd91d","contributors":{"authors":[{"text":"Swanson, G.A.","contributorId":49299,"corporation":false,"usgs":true,"family":"Swanson","given":"G.A.","email":"","affiliations":[],"preferred":false,"id":732337,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Winter, T. C.","contributorId":169945,"corporation":false,"usgs":false,"family":"Winter","given":"T.","email":"","middleInitial":"C.","affiliations":[{"id":25635,"text":"USGS, Lakewood, CO","active":true,"usgs":false}],"preferred":false,"id":732338,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Adomaitis, V. A.","contributorId":66198,"corporation":false,"usgs":true,"family":"Adomaitis","given":"V.","email":"","middleInitial":"A.","affiliations":[],"preferred":false,"id":732339,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"LaBaugh, James W. 0000-0002-4112-2536 jlabaugh@usgs.gov","orcid":"https://orcid.org/0000-0002-4112-2536","contributorId":1311,"corporation":false,"usgs":true,"family":"LaBaugh","given":"James","email":"jlabaugh@usgs.gov","middleInitial":"W.","affiliations":[{"id":27111,"text":"National Water Quality Program","active":true,"usgs":true},{"id":493,"text":"Office of Ground Water","active":true,"usgs":true}],"preferred":true,"id":732340,"contributorType":{"id":1,"text":"Authors"},"rank":4}]}}
,{"id":44824,"text":"wri884082 - 1988 - Distribution of dissolved-solids concentrations and temperature in ground water of the Gulf Coast aquifer systems, south-central United States","interactions":[],"lastModifiedDate":"2023-03-20T21:12:22.25239","indexId":"wri884082","displayToPublicDate":"1988-01-01T00:00:00","publicationYear":"1988","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":342,"text":"Water-Resources Investigations Report","code":"WRI","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"88-4082","title":"Distribution of dissolved-solids concentrations and temperature in ground water of the Gulf Coast aquifer systems, south-central United States","docAbstract":"<p>The distribution of dissolved-solids concentrations and temperature in waters of 10 of the aquifers comprising the gulf coast aquifer systems of the Gulf Mexico Coastal Plain are mapped at a scale of 1:3,500,000. Dissolved solids concentration in the aquifers of the Tertiary System ranges from less than 500 mg/L at the outcrop and subcrop areas to as much as 150,000 mg/L at the downdip extent of these aquifers. A distinct band of sharply increasing concentration of dissolved-solids occurs at about middip of each aquifer of the Tertiary System. Dissolved-solids concentration in younger aquifers ranges from less than 500 mg/L in outcrop and subcrop areas to about 70,000 mg/L at the downdip extent of these aquifers. Temperature of waters in permeable Tertiary deposits ranges from about 18 C at the outcrop and subcrop areas to 90 C at the downdip extent of these aquifers. Temperature of waters in younger deposits ranges from about 14 C at the outcrop and subcrop areas to 30 C at their downdip extent.&nbsp;</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/wri884082","usgsCitation":"Pettijohn, R.A., Weiss, J.S., and Williamson, A.K., 1988, Distribution of dissolved-solids concentrations and temperature in ground water of the Gulf Coast aquifer systems, south-central United States: U.S. Geological Survey Water-Resources Investigations Report 88-4082, 5 Plates: 32.00 x 2.82 inches or smaller, https://doi.org/10.3133/wri884082.","productDescription":"5 Plates: 32.00 x 2.82 inches or smaller","costCenters":[],"links":[{"id":82159,"rank":3,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wri/1988/4082/plate-2.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":82158,"rank":2,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wri/1988/4082/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":171182,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":82162,"rank":6,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wri/1988/4082/plate-5.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":82161,"rank":5,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wri/1988/4082/plate-4.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":82160,"rank":4,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wri/1988/4082/plate-3.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":414387,"rank":7,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_47002.htm","linkFileType":{"id":5,"text":"html"}}],"country":"United States","otherGeospatial":"Gulf Coast aquifer systems","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"coordinates\": [\n          [\n            [\n              -100.1667,\n              26\n            ],\n            [\n              -87.1375,\n              26\n            ],\n            [\n              -87.1375,\n              37\n            ],\n            [\n              -100.1667,\n              37\n            ],\n            [\n              -100.1667,\n              26\n            ]\n          ]\n        ],\n        \"type\": \"Polygon\"\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a7fe4b07f02db648707","contributors":{"authors":[{"text":"Pettijohn, Robert A.","contributorId":77502,"corporation":false,"usgs":true,"family":"Pettijohn","given":"Robert","email":"","middleInitial":"A.","affiliations":[],"preferred":false,"id":230503,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Weiss, Jonathan S.","contributorId":32973,"corporation":false,"usgs":true,"family":"Weiss","given":"Jonathan","email":"","middleInitial":"S.","affiliations":[],"preferred":false,"id":230501,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Williamson, Alex K.","contributorId":36543,"corporation":false,"usgs":true,"family":"Williamson","given":"Alex","email":"","middleInitial":"K.","affiliations":[],"preferred":false,"id":230502,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":70180307,"text":"70180307 - 1988 - Off-platform Silurian sequences in the Ambler River quadrangle: A section in <i>Geologic studies in Alaska by the U.S. Geological Survey during 1987</i>","interactions":[{"subject":{"id":70180307,"text":"70180307 - 1988 - Off-platform Silurian sequences in the Ambler River quadrangle: A section in <i>Geologic studies in Alaska by the U.S. Geological Survey during 1987</i>","indexId":"70180307","publicationYear":"1988","noYear":false,"title":"Off-platform Silurian sequences in the Ambler River quadrangle: A section in <i>Geologic studies in Alaska by the U.S. Geological Survey during 1987</i>"},"predicate":"IS_PART_OF","object":{"id":4297,"text":"cir1016 - 1988 - Geologic studies in Alaska by the U.S. Geological Survey during 1987","indexId":"cir1016","publicationYear":"1988","noYear":false,"title":"Geologic studies in Alaska by the U.S. Geological Survey during 1987"},"id":1}],"isPartOf":{"id":4297,"text":"cir1016 - 1988 - Geologic studies in Alaska by the U.S. Geological Survey during 1987","indexId":"cir1016","publicationYear":"1988","noYear":false,"title":"Geologic studies in Alaska by the U.S. Geological Survey during 1987"},"lastModifiedDate":"2018-05-07T21:26:15","indexId":"70180307","displayToPublicDate":"1988-01-01T00:00:00","publicationYear":"1988","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":307,"text":"Circular","code":"CIR","onlineIssn":"2330-5703","printIssn":"1067-084X","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"1016","title":"Off-platform Silurian sequences in the Ambler River quadrangle: A section in <i>Geologic studies in Alaska by the U.S. Geological Survey during 1987</i>","docAbstract":"<p>Lithofacies changes in coeval upper Paleozoic rocks have been used to unravel the tectonic history of northern Alaska (for example, Mayfield and others, 1983). Conodont biostratigraphy and detailed petrologic studies are now revealing facies differences in lower Paleozoic rocks that can also be used to constrain their tectono-sedimentary framework (Dumoulin and Harris, 1987). A basic element of basin analysis is the discrimination of shallow-water shelf and platform sequences from deeper water slope and basinal deposits. This report documents several new localities of deeper water, off-platform Silurian deposits in the Ambler River quadrangle and briefly outlines some of their paleogeographic implications.</p>","largerWorkType":{"id":18,"text":"Report"},"largerWorkTitle":"Geologic studies in Alaska by the U.S. Geological Survey during 1987 (Circular 1016)","largerWorkSubtype":{"id":5,"text":"USGS Numbered Series"},"language":"English","publisher":"U.S. Government Printing Office","publisherLocation":"Washington, D.C.","doi":"10.3133/70180307","usgsCitation":"Dumoulin, J.A., and Harris, A.G., 1988, Off-platform Silurian sequences in the Ambler River quadrangle: A section in <i>Geologic studies in Alaska by the U.S. Geological Survey during 1987</i>: U.S. Geological Survey Circular 1016, 4 p., https://doi.org/10.3133/70180307.","productDescription":"4 p.","startPage":"35","endPage":"38","numberOfPages":"4","costCenters":[{"id":114,"text":"Alaska Science Center","active":true,"usgs":true}],"links":[{"id":334113,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"},{"id":334112,"rank":1,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/circ/1988/1016/report.pdf#page=43","text":"Start page in larger work"}],"country":"United States","state":"Alaska","otherGeospatial":"Ambler River quadrangle","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"588b198be4b0ad67323f986a","contributors":{"authors":[{"text":"Dumoulin, Julie A. 0000-0003-1754-1287 dumoulin@usgs.gov","orcid":"https://orcid.org/0000-0003-1754-1287","contributorId":203209,"corporation":false,"usgs":true,"family":"Dumoulin","given":"Julie","email":"dumoulin@usgs.gov","middleInitial":"A.","affiliations":[{"id":119,"text":"Alaska Science Center Geology Minerals","active":true,"usgs":true},{"id":114,"text":"Alaska Science Center","active":true,"usgs":true}],"preferred":true,"id":661142,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Harris, Anita G.","contributorId":50162,"corporation":false,"usgs":true,"family":"Harris","given":"Anita","email":"","middleInitial":"G.","affiliations":[],"preferred":false,"id":661143,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":70176745,"text":"70176745 - 1988 - Depositional environments of the Cache, Lower Lake, and Kelseyville Formations, Lake County, California","interactions":[],"lastModifiedDate":"2016-10-05T11:13:43","indexId":"70176745","displayToPublicDate":"1988-01-01T00:00:00","publicationYear":"1988","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1727,"text":"GSA Special Papers","active":true,"publicationSubtype":{"id":10}},"title":"Depositional environments of the Cache, Lower Lake, and Kelseyville Formations, Lake County, California","docAbstract":"<p><span>We describe the depositional environments of the Cache, Lower Lake, and Kelseyville Formations in light of habitat preferences of recovered mollusks, ostracodes, and diatoms. Our reconstruction of paleoenvironments for these late Cenozoic deposits provides a framework for an understanding of basin evolution and deposition in the Clear Lake region. The Pliocene and Pleistocene Cache Formation was deposited primarily in stream and debris flow environments; fossils from fine-grained deposits indicate shallow, fresh-water environments with locally abundant aquatic vegetation. The fine-grained sediments (mudstone and siltstone) were probably deposited in ponds in abandoned channels or shallow basins behind natural levees. The abandoned channels and shallow basins were associated with the fluvial systems responsible for deposition of the bulk of the technically controlled Cache Formation. The Pleistocene Lower Lake Formation was deposited in a water mass large enough to contain a variety of local environments and current regimes. The recovered fossils imply a lake with water depths of 1 to 5 m. However, there is strong support from habitat preferences of the recovered fossils for inferring a wide range of water depths during deposition of the Lower Lake Formation; they indicate a progressively shallowing system and the culmination of a desiccating lacustrine system. The Pleistocene Kelseyville Formation represents primarily lacustrine deposition with only minor fluvial deposits around the margins of the basin. Local conglomerate beds and fossil tree stumps in growth position within the basin indicate occasional widespread fluvial incursions and depositional hiatuses. The Kelseyville strata represent a large water mass with a muddy and especially fluid substrate having permanent or sporadic periods of anoxia. Central-lake anoxia, whether permanent or at irregular intervals, is the simplest way to account for the low numbers of benthic organisms recovered from the Kelseyville Formation. Similar low-oxygen conditions for benthic life are represented throughout the sedimentary history of Clear Lake. Water depths for the Kelseyville Formation of 10 to 30 m and 12 m near the margins of the basin are inferred both before and after fluvial incursions. These water-depth fluctuations cannot be correlated with major climatic changes as indicated by pollen and fossil leaves and cones; they may be due to faulting in this technically active region.</span></p>","language":"English","publisher":"Geological Society of America","doi":"10.1130/SPE214-p45","usgsCitation":"Rymer, M.J., Roth, B., Bradbury, J.P., and Forester, R.M., 1988, Depositional environments of the Cache, Lower Lake, and Kelseyville Formations, Lake County, California: GSA Special Papers, v. 214, p. 45-62, https://doi.org/10.1130/SPE214-p45.","productDescription":"18 p.","startPage":"45","endPage":"62","costCenters":[],"links":[{"id":329307,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"214","noUsgsAuthors":false,"publicationDate":"1988-01-01","publicationStatus":"PW","scienceBaseUri":"57febf64e4b0824b2d157938","contributors":{"authors":[{"text":"Rymer, Michael J. mrymer@usgs.gov","contributorId":1522,"corporation":false,"usgs":true,"family":"Rymer","given":"Michael","email":"mrymer@usgs.gov","middleInitial":"J.","affiliations":[{"id":237,"text":"Earthquake Science Center","active":true,"usgs":true}],"preferred":true,"id":650164,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Roth, Barry","contributorId":63298,"corporation":false,"usgs":true,"family":"Roth","given":"Barry","affiliations":[],"preferred":false,"id":650165,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Bradbury, J. Platt","contributorId":91106,"corporation":false,"usgs":true,"family":"Bradbury","given":"J.","email":"","middleInitial":"Platt","affiliations":[],"preferred":false,"id":650166,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Forester, Richard M.","contributorId":71961,"corporation":false,"usgs":true,"family":"Forester","given":"Richard","email":"","middleInitial":"M.","affiliations":[{"id":271,"text":"Federal Center","active":false,"usgs":true}],"preferred":false,"id":650167,"contributorType":{"id":1,"text":"Authors"},"rank":4}]}}
,{"id":70014379,"text":"70014379 - 1988 - Geometry of Upper Cretaceous bentonite beds: Implications about volcanic source areas and paleowind patterns, western interior, United States","interactions":[],"lastModifiedDate":"2024-01-26T01:15:55.438934","indexId":"70014379","displayToPublicDate":"1988-01-01T00:00:00","publicationYear":"1988","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1796,"text":"Geology","active":true,"publicationSubtype":{"id":10}},"title":"Geometry of Upper Cretaceous bentonite beds: Implications about volcanic source areas and paleowind patterns, western interior, United States","docAbstract":"<div id=\"15572124\" class=\"article-section-wrapper js-article-section js-content-section  \" data-section-parent-id=\"0\"><p>Four bentonite beds near the Cenomanian-Turonian Stage boundary (ca. 90 Ma) can be traced through much of the western interior of the United States. Isopach maps constructed for these bentonite beds indicate that volcanic source areas were positioned both northwest and southwest of the central U.S. western interior basin and also indicate both easterly and southeasterly paleowind directions. Volcanism of this age has not been reported previously in the southern source area.</p></div>","language":"English","publisher":"Geological Society of America","doi":"10.1130/0091-7613(1988)016<0835:GOUCBB>2.3.CO;2","issn":"00917613","usgsCitation":"Elder, W., 1988, Geometry of Upper Cretaceous bentonite beds: Implications about volcanic source areas and paleowind patterns, western interior, United States: Geology, v. 16, no. 9, p. 835-838, https://doi.org/10.1130/0091-7613(1988)016<0835:GOUCBB>2.3.CO;2.","productDescription":"4 p.","startPage":"835","endPage":"838","numberOfPages":"4","costCenters":[],"links":[{"id":225507,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"16","issue":"9","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"505a276ce4b0c8380cd59891","contributors":{"authors":[{"text":"Elder, W.P.","contributorId":65467,"corporation":false,"usgs":true,"family":"Elder","given":"W.P.","email":"","affiliations":[],"preferred":false,"id":368263,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":70180308,"text":"70180308 - 1988 - Stromatolite- and coated-grain-bearing carbonate rocks of the western Brooks Range: A section in <i>Geologic studies in Alaska by the U.S. Geological Survey during 1987</i>","interactions":[{"subject":{"id":70180308,"text":"70180308 - 1988 - Stromatolite- and coated-grain-bearing carbonate rocks of the western Brooks Range: A section in <i>Geologic studies in Alaska by the U.S. Geological Survey during 1987</i>","indexId":"70180308","publicationYear":"1988","noYear":false,"title":"Stromatolite- and coated-grain-bearing carbonate rocks of the western Brooks Range: A section in <i>Geologic studies in Alaska by the U.S. Geological Survey during 1987</i>"},"predicate":"IS_PART_OF","object":{"id":4297,"text":"cir1016 - 1988 - Geologic studies in Alaska by the U.S. Geological Survey during 1987","indexId":"cir1016","publicationYear":"1988","noYear":false,"title":"Geologic studies in Alaska by the U.S. Geological Survey during 1987"},"id":1}],"isPartOf":{"id":4297,"text":"cir1016 - 1988 - Geologic studies in Alaska by the U.S. Geological Survey during 1987","indexId":"cir1016","publicationYear":"1988","noYear":false,"title":"Geologic studies in Alaska by the U.S. Geological Survey during 1987"},"lastModifiedDate":"2018-05-07T21:25:17","indexId":"70180308","displayToPublicDate":"1988-01-01T00:00:00","publicationYear":"1988","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":307,"text":"Circular","code":"CIR","onlineIssn":"2330-5703","printIssn":"1067-084X","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"1016","title":"Stromatolite- and coated-grain-bearing carbonate rocks of the western Brooks Range: A section in <i>Geologic studies in Alaska by the U.S. Geological Survey during 1987</i>","docAbstract":"<p>Carbonate rocks characterized by locally abundant stromatolites and coated grains have been found at several localities in the Baird Mountains and Ambler River quadrangles (fig. 1). These rocks are part of a belt of metasedimentary and metaigneous rocks that constitutes the southwestern flank of the Brooks Range; all are included in the parautochthon (Schwatka sequence) of Mayfield and others (1983). The rocks have been deformed and metamorphosed to blueschist and greenschist facies, but primary textures and sedimentary structures are locally well preserved. </p>","largerWorkType":{"id":18,"text":"Report"},"largerWorkTitle":"Geologic studies in Alaska by the U.S. Geological Survey during 1987 (Circular 1016)","largerWorkSubtype":{"id":5,"text":"USGS Numbered Series"},"language":"English","publisher":"U.S. Government Printing Office","publisherLocation":"Washington, D.C.","doi":"10.3133/70180308","usgsCitation":"Dumoulin, J.A., 1988, Stromatolite- and coated-grain-bearing carbonate rocks of the western Brooks Range: A section in <i>Geologic studies in Alaska by the U.S. Geological Survey during 1987</i>: U.S. Geological Survey Circular 1016, 4 p., https://doi.org/10.3133/70180308.","productDescription":"4 p.","startPage":"31","endPage":"34","numberOfPages":"4","costCenters":[{"id":114,"text":"Alaska Science Center","active":true,"usgs":true}],"links":[{"id":334115,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"},{"id":334114,"rank":1,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/circ/1988/1016/report.pdf#page=39","text":"Start page in larger work"}],"country":"United States","state":"Alaska","otherGeospatial":"Brooks Range","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"588b198be4b0ad67323f9868","contributors":{"authors":[{"text":"Dumoulin, Julie A. 0000-0003-1754-1287 dumoulin@usgs.gov","orcid":"https://orcid.org/0000-0003-1754-1287","contributorId":203209,"corporation":false,"usgs":true,"family":"Dumoulin","given":"Julie","email":"dumoulin@usgs.gov","middleInitial":"A.","affiliations":[{"id":114,"text":"Alaska Science Center","active":true,"usgs":true},{"id":119,"text":"Alaska Science Center Geology Minerals","active":true,"usgs":true}],"preferred":true,"id":661144,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":25908,"text":"wri864094 - 1988 - Ground-water geochemistry of the Albuquerque-Belen Basin, central New Mexico","interactions":[],"lastModifiedDate":"2023-03-13T19:24:15.855705","indexId":"wri864094","displayToPublicDate":"1988-01-01T00:00:00","publicationYear":"1988","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":342,"text":"Water-Resources Investigations Report","code":"WRI","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"86-4094","title":"Ground-water geochemistry of the Albuquerque-Belen Basin, central New Mexico","docAbstract":"The purpose of this study was to define the areal distribution of different water types, use the distribution to help define the groundwater flow system, and identify processes resulting in differences in groundwater quality in the Albuquerque-Belen Basin in central New Mexico. The chemistry of surface water inflow from adjacent areas, which infiltrates and recharges the aquifer along the basin margin, affects the groundwater quality in the eastern and southeastern areas of the basin. Groundwater in the eastern area generally has a specific conductance less than 400 microsiemens, and calcium and bicarbonate are the dominant ions. Mixing of recharge, groundwater inflow, and surface inflow from adjacent areas, which have different chemical compositions, is the major process affecting groundwater quality in the southwestern, western, and northern areas of the basin. In these areas, there is a large range in specific conductance and distribution of dissolved ions. Groundwater quality in the Rio Grande valley is affected by the infiltration of excess irrigation water. The excess irrigation water generally has a larger specific conductance than other groundwater in the valley, so mixing of these waters results in shallow groundwater generally having larger specific conductance than the deeper groundwater. (USGS)","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/wri864094","usgsCitation":"Anderholm, S., 1988, Ground-water geochemistry of the Albuquerque-Belen Basin, central New Mexico: U.S. Geological Survey Water-Resources Investigations Report 86-4094, Report: viii, 110 p.; 2 Plates: 15.64 x 31.16 inches and 15.64 x 32.53 inches, https://doi.org/10.3133/wri864094.","productDescription":"Report: viii, 110 p.; 2 Plates: 15.64 x 31.16 inches and 15.64 x 32.53 inches","costCenters":[],"links":[{"id":414037,"rank":5,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_36542.htm","linkFileType":{"id":5,"text":"html"}},{"id":54668,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wri/1986/4094/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":54667,"rank":4,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wri/1986/4094/plate-2.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":54666,"rank":3,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wri/1986/4094/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":125140,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wri/1986/4094/report-thumb.jpg"}],"country":"United States","state":"New Mexico","otherGeospatial":"Albuquerque-Belen Basin","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"coordinates\": [\n          [\n            [\n              -106.25,\n              35.75\n            ],\n            [\n              -107.233,\n              35.75\n            ],\n            [\n              -107.233,\n              34.25\n            ],\n            [\n              -106.25,\n              34.25\n            ],\n            [\n              -106.25,\n              35.75\n            ]\n          ]\n        ],\n        \"type\": \"Polygon\"\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4aaae4b07f02db668f67","contributors":{"authors":[{"text":"Anderholm, S. K.","contributorId":69149,"corporation":false,"usgs":true,"family":"Anderholm","given":"S. K.","affiliations":[],"preferred":false,"id":195464,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":70013934,"text":"70013934 - 1988 - Composition and stable-isotope geochemistry of natural gases from Kansas, Midcontinent, U.S.A.","interactions":[],"lastModifiedDate":"2013-01-20T20:55:17","indexId":"70013934","displayToPublicDate":"1988-01-01T00:00:00","publicationYear":"1988","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1213,"text":"Chemical Geology","active":true,"publicationSubtype":{"id":10}},"title":"Composition and stable-isotope geochemistry of natural gases from Kansas, Midcontinent, U.S.A.","docAbstract":"More than 28??1012 ft.3 (79??1010 m3) of natural gas and 5.3??109 bbl (8.4??108 m3) of oil have been produced in Kansas, U.S.A., from Paleozoic carbonate and sandstone reservoirs on structural uplifts and shallow embayments along the northern margin of the Anadarko basin. A heavily-explored, geologically well-characterized state, Kansas is an excellent place to study hydrocarbon migration and to test geochemical models for the origin of natural gases. Immature to marginally-mature rocks of eastern Kansas (Cherokee and Forest City basins) produce mixed microbial and thermogenic gases. Gases in this region have wetness = 0.03-51%, methane ??13C = -65 to -43??? and methane ??D = -260 to -150???. Gases from central and western Kansas (Nemaha uplift to Hugoton embayment) are entirely thermogenic and have wetness =4-51%, methane ??13C = -48 to -39??? and methane ??D = -195 to -140???. Ethane and propane ??13C-values throughout Kansas vary from -38 to -28??? and from -35 to -24???, respectively. Mature thermogenic gas (generated from source rocks in southwestern Kansas and the Anadarko basin with 1.0% ??? Ro ??? 1.4%) is recognized throughout the state. Lateral migration into shallow reservoirs on the Central Kansas and northern Nemaha uplifts and in the Cherokee basin probably occurred along basal Pennsylvanian conglomerates and weathered Lower Paleozoic carbonates at the regional sub-Pennsylvanian unconformity. Early thermogenic gas (generated by local source rocks with Ro ??? 0.7%) is recognized in isolated fields in the Salina and Forest City basins, in Ordovician reservoirs beneath the sub-Pennsylvanian unconformity in the Cherokee basin, and in reservoirs generally above the unconformity in the Cherokee and Sedgwick basins, the eastern Central Kansas uplift and the Hugoton embayment. ?? 1988.","largerWorkType":{"id":2,"text":"Article"},"largerWorkTitle":"Chemical Geology","largerWorkSubtype":{"id":10,"text":"Journal Article"},"language":"English","publisher":"Elsevier","doi":"10.1016/0009-2541(88)90110-6","issn":"00092541","usgsCitation":"Jenden, P., Newell, K., Kaplan, I., and Watney, W., 1988, Composition and stable-isotope geochemistry of natural gases from Kansas, Midcontinent, U.S.A.: Chemical Geology, v. 71, no. 1-3, p. 117-147, https://doi.org/10.1016/0009-2541(88)90110-6.","startPage":"117","endPage":"147","numberOfPages":"31","costCenters":[],"links":[{"id":266093,"type":{"id":10,"text":"Digital Object Identifier"},"url":"https://dx.doi.org/10.1016/0009-2541(88)90110-6"},{"id":225543,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"71","issue":"1-3","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"5059f922e4b0c8380cd4d45a","contributors":{"authors":[{"text":"Jenden, P.D.","contributorId":61176,"corporation":false,"usgs":true,"family":"Jenden","given":"P.D.","email":"","affiliations":[],"preferred":false,"id":367200,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Newell, K.D.","contributorId":76473,"corporation":false,"usgs":true,"family":"Newell","given":"K.D.","email":"","affiliations":[],"preferred":false,"id":367201,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Kaplan, I.R.","contributorId":24086,"corporation":false,"usgs":true,"family":"Kaplan","given":"I.R.","email":"","affiliations":[],"preferred":false,"id":367198,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Watney, W.L.","contributorId":43087,"corporation":false,"usgs":true,"family":"Watney","given":"W.L.","email":"","affiliations":[],"preferred":false,"id":367199,"contributorType":{"id":1,"text":"Authors"},"rank":4}]}}
,{"id":70014711,"text":"70014711 - 1988 - Conductive heat flux in VC-1 and the thermal regime of Valles caldera, Jemez Mountains, New Mexico","interactions":[],"lastModifiedDate":"2024-06-05T14:35:56.974184","indexId":"70014711","displayToPublicDate":"1988-01-01T00:00:00","publicationYear":"1988","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":6453,"text":"Journal of Geophysical Research Solid Earth","active":true,"publicationSubtype":{"id":10}},"title":"Conductive heat flux in VC-1 and the thermal regime of Valles caldera, Jemez Mountains, New Mexico","docAbstract":"<p><span>Over 5% of heat in the western United States is lost through Quaternary silicic volcanic centers, including the Valles caldera in north central New Mexico. These centers are the sites of major hydrothermal activity and upper crustal metamorphism, metasomatism, and mineralization, producing associated geothermal resources. We present new heat flow data from Valles caldera core hole 1 (VC-1), drilled in the southwestern margin of the Valles caldera. Thermal conductivities were measured on 55 segments of core from VC-1, waxed and wrapped to preserve fluids. These values were combined with temperature gradient data to calculate heat flow. Above 335 m, which is probably unsaturated, heat flow is 247±16 mW m</span><sup>−2</sup><span>. The only deep temperature information available is from an uncalibrated commercial log made 19 months after drilling. Gradients, derived from uncalibrated temperature logs, and conductivities are inversely correlated between 335 and 737 m, indicating a conductive thermal regime, and component heat fluxes over three depth intervals (335–539 m, 549–628 m, and 628–737 m) are in excellent agreement with each other with an average of 504±15 mW m</span><sup>−2</sup><span>. Temperature logs to 518 m depth with well-calibrated temperature sensors result in a revised heat flow of 463±15 mW m. We use shallow thermal gradient data from 75 other sites in and around the caldera to interpret the thermal regime at the VC-1 site. A critical review of published thermal conductivity data from the Valles caldera yields an average thermal conductivity of ≥1 W m</span><sup>−1</sup><span>&nbsp;K</span><sup>−1</sup><span>&nbsp;for the near-surface tuffaceous material, and we assume that shallow gradient values (°C km</span><sup>−1</sup><span>) are approximately numerically equal to heat flow (mW m</span><sup>−2</sup><span>). Heat loss from the caldera is asymmetrically distributed, with higher values (400 mW m</span><sup>−2</sup><span>&nbsp;or higher) concentrated in the west-southwestern quadrant of the caldera. This quadrant also contains the main drainage from the caldera and the youngest volcanism associated with the caldera. We interpret the shallow thermal gradient data and the thermal regime at VC-1 to indicate a long-lived hydrothermal (and magmatic) system in the southwestern Valles caldera that has been maintained through the generation of shallow magma bodies during the long postcollapse history of the caldera. High heat flow at the VC-1 site is interpreted to result from hot water circulating below the base of the core hole, and we attribute the lower heat flow in the unsaturated zone to hydrologic recharge.</span></p>","language":"English","publisher":"American Geophysical Union","doi":"10.1029/JB093iB06p06027","issn":"01480227","usgsCitation":"Sass, J., and Morgan, P., 1988, Conductive heat flux in VC-1 and the thermal regime of Valles caldera, Jemez Mountains, New Mexico: Journal of Geophysical Research Solid Earth, v. 93, no. B6, p. 6027-6039, https://doi.org/10.1029/JB093iB06p06027.","productDescription":"13 p.","startPage":"6027","endPage":"6039","numberOfPages":"13","costCenters":[],"links":[{"id":225656,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"93","issue":"B6","noUsgsAuthors":false,"publicationDate":"2012-09-20","publicationStatus":"PW","scienceBaseUri":"5059f9b9e4b0c8380cd4d753","contributors":{"authors":[{"text":"Sass, J.H.","contributorId":70749,"corporation":false,"usgs":true,"family":"Sass","given":"J.H.","email":"","affiliations":[{"id":595,"text":"U.S. Geological Survey","active":false,"usgs":true}],"preferred":false,"id":369067,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Morgan, P.","contributorId":34096,"corporation":false,"usgs":false,"family":"Morgan","given":"P.","email":"","affiliations":[],"preferred":false,"id":369066,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":70014316,"text":"70014316 - 1988 - An oxygen isotope and geochemical study of meteoric-hydrothermal systems at Pilot Mountain and selected other localities, Carolina slate belt","interactions":[],"lastModifiedDate":"2024-01-05T15:58:47.869304","indexId":"70014316","displayToPublicDate":"1988-01-01T00:00:00","publicationYear":"1988","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1472,"text":"Economic Geology","active":true,"publicationSubtype":{"id":10}},"title":"An oxygen isotope and geochemical study of meteoric-hydrothermal systems at Pilot Mountain and selected other localities, Carolina slate belt","docAbstract":"<p><span>Several epigenetic mineral deposits in the Ca1rolina slate belt are intimately related to meteoric-hydrothermal systems of late Precambrian and early Paleozoic age. At Pilot Mountain, low&nbsp;</span><sup>18</sup><span>&nbsp;O rocks correlate well with zones of strong silicic alteration and alkali leaching accompanied by high alumina minerals (sericite, pyrophyllite, andalusite + or - topaz) and anomalous concentrations of Cu, Mo, Sn, B, and Au. The alteration occurs within andesitic volcanic and volcaniclastic rocks and is associated with a subvolcanic(?) dacite porphyry stock on the southeastern slope of the mountain. Tilting and erosion have exposed an oblique section through the original system, interpreted to expose shallower rocks to the northwest. A 4-km&nbsp;</span><sup>2</sup><span>&nbsp;central zone of slight&nbsp;</span><sup>18</sup><span>&nbsp;O depletion (delta&nbsp;</span><sup>18</sup><span>&nbsp;O (sub whole rock) = 4.3-6.1ppm) occurs on the broad and resistant (silicifled) western flank of Pilot Mountain, predominantly within quartz-sericite schist and quartz granofels containing pods of high A1 minerals. A magmatic source for much of the sulfur and metal is likely, and a subordinate magmatic water component in the fluid of the central zone is possible. This central zone is surrounded by a &gt;30-km&nbsp;</span><sup>2</sup><span>&nbsp;peripheral zone of low&nbsp;</span><sup>18</sup><span>&nbsp;O sericite schists, chlorite-sericite schists, and andesitic volcanic rocks (delta&nbsp;</span><sup>18</sup><span>&nbsp;O (sub whole rock) &lt; 3.8ppm), with the lowest values (1.4ppm) occurring in intensely sericitized rocks on the eastern flank of Pilot Mountain, near the apex of the dacite porphyry stock. Rhyolites of the Uwharrie Formation (delta&nbsp;</span><sup>18</sup><span>&nbsp;O = 3.8-6.3ppm) are not as strongly altered as nearby andesites and may postdate the hydrothermal alteration. The fluid calculated to be in equilibrium with the lowest&nbsp;</span><sup>18</sup><span>&nbsp;O quartz veins and country rocks at 300 degrees + or - 50 degrees C would have delta&nbsp;</span><sup>18</sup><span>&nbsp;O approximately -4.5 + or - 2.0 per mil, whereas analyses of radiating pyrophyllite indicate equilibrium with a fluid having delta D approximately -30 per mil, consistent with a slightly&nbsp;</span><sup>18</sup><span>&nbsp;O-shifted, low-latitude meteoric water. Subsequent greenschist metamorphism caused intermineral isotopic reequilibration in several samples and may have modified preexisting alteration assemblages, but it did not destroy the large delta&nbsp;</span><sup>18</sup><span>&nbsp;O anomaly produced by meteoric-hydrothermal activity at Pilot Mountain. Reconnaissance studies of other alteration zones in the Carolina slate belt have so far disclosed the involvement of meteoric-hydrothermal fluids at the Snow Camp pyrophyllite deposit, at the Hoover Hill and Sawyer Au mines, and probably at the Haile and Brewer Au mines.</span></p>","language":"English","publisher":"Society of Economic Geologists","doi":"10.2113/gsecongeo.83.4.801","issn":"03610128","usgsCitation":"Klein, T.L., and Criss, R., 1988, An oxygen isotope and geochemical study of meteoric-hydrothermal systems at Pilot Mountain and selected other localities, Carolina slate belt: Economic Geology, v. 83, no. 4, p. 801-821, https://doi.org/10.2113/gsecongeo.83.4.801.","productDescription":"21 p.","startPage":"801","endPage":"821","numberOfPages":"21","costCenters":[],"links":[{"id":225372,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"83","issue":"4","noUsgsAuthors":false,"publicationDate":"1988-07-01","publicationStatus":"PW","scienceBaseUri":"5059eaafe4b0c8380cd489f6","contributors":{"authors":[{"text":"Klein, T. L.","contributorId":76322,"corporation":false,"usgs":true,"family":"Klein","given":"T.","email":"","middleInitial":"L.","affiliations":[],"preferred":false,"id":368100,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Criss, R.E.","contributorId":10075,"corporation":false,"usgs":true,"family":"Criss","given":"R.E.","email":"","affiliations":[],"preferred":false,"id":368099,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":1004074,"text":"1004074 - 1988 - Experimental <i>Mycoplasma gallisepticum</i> infections in captive-reared wild turkeys","interactions":[],"lastModifiedDate":"2015-06-22T10:57:31","indexId":"1004074","displayToPublicDate":"1988-01-01T00:00:00","publicationYear":"1988","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":2507,"text":"Journal of Wildlife Diseases","active":true,"publicationSubtype":{"id":10}},"title":"Experimental <i>Mycoplasma gallisepticum</i> infections in captive-reared wild turkeys","docAbstract":"<p><span>The effects of&nbsp;</span><i>Mycoplasma gallisepticum</i><span>&nbsp;(MG) infections on egg production, fertility, and hatchability were studied in captive-reared wild turkeys (</span><i>Meleagris gallopavo</i><span>). Three groups of adult birds, each consisting of four hens and two toms, were exposed to MG by the respiratory route at the beginning of their breeding season. Fourteen control birds received sterile growth medium. Although no mortality of infected or control birds occurred, egg production during the first breeding season after infection was reduced. The mean number of eggs/hen/day produced by infected groups the first breeding season postexposure (PE) was significantly lower than the control value. The mean number of eggs produced daily by the same hens 1 yr later was unaffected by MG infection. The pecentage of fertile eggs produced by infected groups was slightly reduced in both the first and second breeding seasons PE. Hatchability of fertile eggs from infected hens was significantly lower than eggs from control hens. Productivity may be impaired if MG infections occur in free-ranging wild turkey populations.</span></p>","language":"English","publisher":"Wildlife Disease Association","doi":"10.7589/0090-3558-24.3.528","usgsCitation":"Rocke, T.E., Yuill, T.M., and Amundson, T.E., 1988, Experimental <i>Mycoplasma gallisepticum</i> infections in captive-reared wild turkeys: Journal of Wildlife Diseases, v. 24, no. 3, p. 528-532, https://doi.org/10.7589/0090-3558-24.3.528.","productDescription":"5 p.","startPage":"528","endPage":"532","numberOfPages":"5","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[{"id":456,"text":"National Wildlife Health Center","active":true,"usgs":true}],"links":[{"id":480046,"rank":2,"type":{"id":40,"text":"Open Access Publisher Index Page"},"url":"https://doi.org/10.7589/0090-3558-24.3.528","text":"Publisher Index Page"},{"id":135947,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"24","issue":"3","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a07e4b07f02db5f9321","contributors":{"authors":[{"text":"Rocke, Tonie E. 0000-0003-3933-1563 trocke@usgs.gov","orcid":"https://orcid.org/0000-0003-3933-1563","contributorId":2665,"corporation":false,"usgs":true,"family":"Rocke","given":"Tonie","email":"trocke@usgs.gov","middleInitial":"E.","affiliations":[{"id":456,"text":"National Wildlife Health Center","active":true,"usgs":true}],"preferred":true,"id":315105,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Yuill, Thomas M.","contributorId":60580,"corporation":false,"usgs":true,"family":"Yuill","given":"Thomas","email":"","middleInitial":"M.","affiliations":[],"preferred":false,"id":315104,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Amundson, Terry E.","contributorId":99509,"corporation":false,"usgs":true,"family":"Amundson","given":"Terry","email":"","middleInitial":"E.","affiliations":[],"preferred":false,"id":315106,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":70014461,"text":"70014461 - 1988 - The global distribution, abundance, and stability of SO2 on Io","interactions":[],"lastModifiedDate":"2012-03-12T17:19:30","indexId":"70014461","displayToPublicDate":"1988-01-01T00:00:00","publicationYear":"1988","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1963,"text":"Icarus","active":true,"publicationSubtype":{"id":10}},"title":"The global distribution, abundance, and stability of SO2 on Io","docAbstract":"Sulfur dioxide distribution and abundances, bolometric hemispheric albedos, and passive surface temperatures on Io are modeled and mapped globally from Voyager multispectral mosaics, Earth-based spectra, and photometric descriptions. Photometric models indicate global average values for regolith porosity of 75-95% and macroscopic roughness with a mean slope angle of ~30??. Abundances of SO2 suggested by observations at uv-visible wavelengths and at 4.08 ??m are partially reconciled by intimate-mixing models; 30-50% SO2 coverage of the integral disk is indicated. Three major spectral end members, with continuous mixing, are recognized from the Voyager multispectral mosaics; one of these end members is identified as SO2. Intimate-mixing models with the three spectal end members are used to produce abundance maps for the optical surface; ~30% of Io's total optical surface consists of SO2. The SO2 is concentrated in the bright equatorial band and is relatively deficient in the region of Pele-type volcanic reuptions (long 240??-360??) and the polar regions. Temperatures are computed to vary over a 40??K range, at the same illumination angle, according to variations in surface bolometric hemispheric albedo. The brightest (and locally coldest) areas correspond to areas rich in SO2 and are concentrated in an equatorial band (??30?? lat), but many small cold patches occur elsewhere. These cold patches have radiative equilibrium temperatures ???120??K at the subsolar point, resulting in SO2 saturation vapor pressures ???10-8 bar. Midlatitude areas and the region of Pele-type plume eruptions are generally warmer (due to lower albedos). These results for surface temperatures and SO2 abundances and distribution support the regional coldtrapping model for the surface and atmospheric SO2 presented by F.P. Fanale, W.B. Banerdt, L.S. Elson, T.V. Johnson, and R.W. Zurek (1982, In Satellites of Jupiter (D. Morrison, Ed.), pp. 756-781, Univ. of Arizona Press, Tucson), although the region of Pele-type volcanic eruptions may be better characterized by the regolith condtrapping/volcanic-venting model of D.L. Matson and D.B. Nash (1983, J. Geophys. Res. 88, 4771-4783). The bright equatorial band is especially effective at slowing the formation of polar caps of SO2, both by reducing the sublimation rate near the subsolar point and by coldtrapping the SO2 in the equatorial region, so that competing processes of sputtering and volcanic resurfacing may prevent the formation of polar SO2 caps.","largerWorkType":{"id":2,"text":"Article"},"largerWorkTitle":"Icarus","largerWorkSubtype":{"id":10,"text":"Journal Article"},"language":"English","doi":"10.1016/0019-1035(88)90157-1","issn":"00191035","usgsCitation":"McEwen, A.S., Johnson, T.V., Matson, D.L., and Soderblom, L., 1988, The global distribution, abundance, and stability of SO2 on Io: Icarus, v. 75, no. 3, p. 450-478, https://doi.org/10.1016/0019-1035(88)90157-1.","startPage":"450","endPage":"478","numberOfPages":"29","costCenters":[],"links":[{"id":205665,"rank":9999,"type":{"id":10,"text":"Digital Object Identifier"},"url":"https://dx.doi.org/10.1016/0019-1035(88)90157-1"},{"id":225897,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"75","issue":"3","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"505bac8ae4b08c986b32357f","contributors":{"authors":[{"text":"McEwen, A. S.","contributorId":11317,"corporation":false,"usgs":true,"family":"McEwen","given":"A.","email":"","middleInitial":"S.","affiliations":[],"preferred":false,"id":368449,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Johnson, T. V.","contributorId":79619,"corporation":false,"usgs":false,"family":"Johnson","given":"T.","email":"","middleInitial":"V.","affiliations":[],"preferred":false,"id":368451,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Matson, D. L.","contributorId":59940,"corporation":false,"usgs":false,"family":"Matson","given":"D.","email":"","middleInitial":"L.","affiliations":[],"preferred":false,"id":368450,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Soderblom, L.A. 0000-0002-0917-853X","orcid":"https://orcid.org/0000-0002-0917-853X","contributorId":6139,"corporation":false,"usgs":true,"family":"Soderblom","given":"L.A.","affiliations":[],"preferred":false,"id":368448,"contributorType":{"id":1,"text":"Authors"},"rank":4}]}}
,{"id":70013653,"text":"70013653 - 1988 - The surface integral approach to Radarclinometry","interactions":[],"lastModifiedDate":"2012-03-12T17:18:32","indexId":"70013653","displayToPublicDate":"1988-01-01T00:00:00","publicationYear":"1988","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1429,"text":"Earth, Moon and Planets","active":true,"publicationSubtype":{"id":10}},"title":"The surface integral approach to Radarclinometry","docAbstract":"Because radarclinometry is fundamentally describable in terms of a nonlinear, first-order, partial differential equation, one expects that it can, in principle, be carried out by direct deterministic integration beginning at a given threshold profile along the azimuthal coordinate. Such a boundary condition could be provided by the altimetry profile obtained on a preceding or succeeding orbital revolution of the radar-bearing spacecraft. Notwithstanding the mismatched resolutions of the radar altimeter and the radar imaging system as planned for the Megallan mission to Venus, there are fundamental considerations, not involving system noise, that influence the possibility of success of this approach. From the topographic map of the Lake Champlain West quadrangle in the Adirondack Mountains of the U.S., a radar image is synthesized. Radarclinometry, in surface integral form, recaptures the topographic map when the applicable radar reflectance function is weakly variable over the range of application, but it diverges beyond a certain point for nominally variable reflectance functions. The effect can be understood by using results from the \"shape-from-shading\" literature. (This literature is produced by a group within the artificial intelligence community who have been independently attacking, for all practical purposes, photoclinometry, except that they have not given primacy to images of terrain.) The ubiquity of the instability suggests that the value of the surface integral approach is much in doubt. ?? 1988 Kluwer Academic Publishers.","largerWorkType":{"id":2,"text":"Article"},"largerWorkTitle":"Earth, Moon and Planets","largerWorkSubtype":{"id":10,"text":"Journal Article"},"language":"English","publisherLocation":"Kluwer Academic Publishers","doi":"10.1007/BF00056399","issn":"01679295","usgsCitation":"Wildey, R., 1988, The surface integral approach to Radarclinometry: Earth, Moon and Planets, v. 41, no. 2, p. 141-153, https://doi.org/10.1007/BF00056399.","startPage":"141","endPage":"153","numberOfPages":"13","costCenters":[],"links":[{"id":220659,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"},{"id":205049,"rank":9999,"type":{"id":10,"text":"Digital Object Identifier"},"url":"https://dx.doi.org/10.1007/BF00056399"}],"volume":"41","issue":"2","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"505bb0a9e4b08c986b324fd5","contributors":{"authors":[{"text":"Wildey, R.L.","contributorId":9700,"corporation":false,"usgs":true,"family":"Wildey","given":"R.L.","email":"","affiliations":[],"preferred":false,"id":366567,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":70014359,"text":"70014359 - 1988 - Elastic-wave propagation and site amplification in the Salt Lake Valley, Utah, from simulated normal faulting earthquakes","interactions":[],"lastModifiedDate":"2023-10-28T13:29:14.16058","indexId":"70014359","displayToPublicDate":"1988-01-01T00:00:00","publicationYear":"1988","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1135,"text":"Bulletin of the Seismological Society of America","onlineIssn":"1943-3573","printIssn":"0037-1106","active":true,"publicationSubtype":{"id":10}},"title":"Elastic-wave propagation and site amplification in the Salt Lake Valley, Utah, from simulated normal faulting earthquakes","docAbstract":"<p>The two-dimensional seismic response of the Salt Lake valley to near- and far-field earthquakes has been investigated from simulations of vertically incident plane waves and from normal-faulting earthquakes generated on the basin-bounding Wasatch fault. The response to normal faulting earthquakes was simulated using a two-dimensional finite-element method and the plane-wave response was calculated from two-dimensional finite-difference simulations. The plane-wave simulations were then compared with observed site amplifications in the Salt Lake valley, based on seismic recordings from nuclear explosions in southern Nevada, that show 10 times greater amplification within the basin than measured values on hard-rock sites. While previous studies attribute this increased site amplification to the near-surface unconsolidated/consolidated alluvial fill contact, our synthetic seismograms suggest that in the frequency band 0.3 to 1.5 Hz at least one-half the site amplification can be attributed to the impedance contrast between the basin sediments and higher velocity basement rocks. Synthetic seismograms from vertically incident plane-wave sources and buried double-couple sources predict large amplitude Rayleigh-wave propagation from the edges of the basin and, in general, uniform site amplification. In contrast, near-field simulations of basin-bounding, normal-faulting earthquakes predict large-amplitude Rayleigh waves propagating westward from the fault across the basin. Spectra of synthetic accelerograms computed from the normal-faulting earthquakes shows that spectral amplification within the basin is primarily due to source directivity with a maxima near the surface projection of the fault that decays rapidly away from the fault. Importantly, the synthetic modeling of near-field earthquake sources show that near-field directivity effects are important and should be considered in an earthquake hazard assessment of the Salt Lake valley and similar geologic settings along the Wasatch Front.</p>","language":"English","publisher":"Seismological Society of America","doi":"10.1785/BSSA0780061851","usgsCitation":"Benz, H., and Smith, R.B., 1988, Elastic-wave propagation and site amplification in the Salt Lake Valley, Utah, from simulated normal faulting earthquakes: Bulletin of the Seismological Society of America, v. 78, no. 6, p. 1851-1874, https://doi.org/10.1785/BSSA0780061851.","productDescription":"24 p.","startPage":"1851","endPage":"1874","numberOfPages":"24","costCenters":[],"links":[{"id":226151,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United States","state":"Utah","otherGeospatial":"Salt Lake Valley","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"coordinates\": [\n          [\n            [\n              -112.56378026249851,\n              41.01057844273427\n            ],\n            [\n              -112.56378026249851,\n              39.940909170477454\n            ],\n            [\n              -110.98174901249853,\n              39.940909170477454\n            ],\n            [\n              -110.98174901249853,\n              41.01057844273427\n            ],\n            [\n              -112.56378026249851,\n              41.01057844273427\n            ]\n          ]\n        ],\n        \"type\": \"Polygon\"\n      }\n    }\n  ]\n}","volume":"78","issue":"6","noUsgsAuthors":false,"publicationDate":"1988-12-01","publicationStatus":"PW","scienceBaseUri":"505a0883e4b0c8380cd51b5f","contributors":{"authors":[{"text":"Benz, H.M.","contributorId":21594,"corporation":false,"usgs":true,"family":"Benz","given":"H.M.","email":"","affiliations":[],"preferred":false,"id":368213,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Smith, R. B.","contributorId":64589,"corporation":false,"usgs":true,"family":"Smith","given":"R.","email":"","middleInitial":"B.","affiliations":[],"preferred":false,"id":368214,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":70014407,"text":"70014407 - 1988 - Hydraulic fracturing in situ stress measurements to 2.1 km depth at Cajon Pass, California","interactions":[],"lastModifiedDate":"2024-02-14T01:09:48.007359","indexId":"70014407","displayToPublicDate":"1988-01-01T00:00:00","publicationYear":"1988","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1807,"text":"Geophysical Research Letters","active":true,"publicationSubtype":{"id":10}},"title":"Hydraulic fracturing in situ stress measurements to 2.1 km depth at Cajon Pass, California","docAbstract":"<div class=\"\"><div class=\"article-section__content en main\"><p>Stress measurements to 2.1 km reveal stress changes with depth that cannot be explained by an elastic response to uniform crustal strain. The data at about 1 km depth suggest that the stress is limited by the frictional strength of rock and is perturbed at greater depths by faults which intersect the borehole. The stress data indicate that there is little or no right-lateral shear stress acting on planes parallel to the San Andreas fault.</p></div></div>","language":"English","publisher":"American Geophysical Union","doi":"10.1029/GL015i009p01005","issn":"00948276","usgsCitation":"Healy, J.H., and Zoback, M.D., 1988, Hydraulic fracturing in situ stress measurements to 2.1 km depth at Cajon Pass, California: Geophysical Research Letters, v. 15, no. 9, p. 1005-1008, https://doi.org/10.1029/GL015i009p01005.","productDescription":"4 p.","startPage":"1005","endPage":"1008","numberOfPages":"4","costCenters":[],"links":[{"id":226022,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"15","issue":"9","noUsgsAuthors":false,"publicationDate":"2012-12-07","publicationStatus":"PW","scienceBaseUri":"505a32ece4b0c8380cd5eb9a","contributors":{"authors":[{"text":"Healy, J. H.","contributorId":48968,"corporation":false,"usgs":true,"family":"Healy","given":"J.","email":"","middleInitial":"H.","affiliations":[],"preferred":false,"id":368335,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Zoback, Mark D.","contributorId":80275,"corporation":false,"usgs":true,"family":"Zoback","given":"Mark","middleInitial":"D.","affiliations":[],"preferred":false,"id":368336,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":70014395,"text":"70014395 - 1988 - Pb, Nd, and Sr isotopic evidence for a multicomponent source for rocks of Cook-Austral Islands and heterogeneities of mantle plumes","interactions":[],"lastModifiedDate":"2024-04-03T16:29:42.944394","indexId":"70014395","displayToPublicDate":"1988-01-01T00:00:00","publicationYear":"1988","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1759,"text":"Geochimica et Cosmochimica Acta","active":true,"publicationSubtype":{"id":10}},"title":"Pb, Nd, and Sr isotopic evidence for a multicomponent source for rocks of Cook-Austral Islands and heterogeneities of mantle plumes","docAbstract":"<p>Sr, Nd, and Pb isotopic compositions were measured in alkaline volcanic rocks (alkali basalt, ankaramite, nephelinite, phonolite, and trachyte) from the South Cook Islands (Aitutaki, Mauke, Rarotonga, Atiu, and Mangaia) and the Austral Islands (Rimatara and Rurutu). The results show that the Cook-Austral rocks have an extremely wide range in isotopic compositions of Pb:<span>&nbsp;</span><span class=\"math\"><span id=\"MathJax-Element-1-Frame\" class=\"MathJax_SVG\" data-mathml=\"<math xmlns=&quot;http://www.w3.org/1998/Math/MathML&quot;><msup><mi></mi><mn>206</mn></msup><mtext>Pb</mtext><msup><mi></mi><mn>204</mn></msup><mtext>Pb</mtext></math>\"><span class=\"MJX_Assistive_MathML\"><sup>206</sup>Pb<sup>204</sup>Pb</span></span></span><span>&nbsp;</span>from 18.25 to 21.76,<span>&nbsp;</span><span class=\"math\"><span id=\"MathJax-Element-2-Frame\" class=\"MathJax_SVG\" data-mathml=\"<math xmlns=&quot;http://www.w3.org/1998/Math/MathML&quot;><msup><mi></mi><mn>207</mn></msup><mtext>pb</mtext><msup><mi></mi><mn>204</mn></msup><mtext>pb</mtext></math>\"><span class=\"MJX_Assistive_MathML\"><sup>207</sup>pb<sup>204</sup>pb</span></span></span><span>&nbsp;</span>from 15.48 to 15.83, and<span>&nbsp;</span><span class=\"math\"><span id=\"MathJax-Element-3-Frame\" class=\"MathJax_SVG\" data-mathml=\"<math xmlns=&quot;http://www.w3.org/1998/Math/MathML&quot;><mtext>sol</mtext><msup><mi></mi><mn>208</mn></msup><mtext>pb</mtext><msup><mi></mi><mn>204</mn></msup><mtext>Pb</mtext></math>\"><span class=\"MJX_Assistive_MathML\">sol<sup>208</sup>pb<sup>204</sup>Pb</span></span></span><span>&nbsp;</span>from 38.37 to 40.62, whereas isotopic compositions of Sr and Nd are less variable. Isotopically, Mangaia, Rimatara, and Rurutu form one group (Mangaia group), which shows extremely radiogenic Pb isotopic compositions but near-MORB (mid-oceanic ridge basalts) values for Sr and Nd isotopic ratios. In contrast, samples from Aitutaki, Rarotonga, Mauke, and Atiu (Aitutaki group) have high<span>&nbsp;</span><span class=\"math\"><span id=\"MathJax-Element-4-Frame\" class=\"MathJax_SVG\" data-mathml=\"<math xmlns=&quot;http://www.w3.org/1998/Math/MathML&quot;><msup><mi></mi><mn>207</mn></msup><mtext>Pb</mtext><msup><mi></mi><mn>204</mn></msup><mtext>Pb</mtext></math>\"><span class=\"MJX_Assistive_MathML\"><sup>207</sup>Pb<sup>204</sup>Pb</span></span></span><span>&nbsp;</span>and<span>&nbsp;</span><span class=\"math\"><span id=\"MathJax-Element-5-Frame\" class=\"MathJax_SVG\" data-mathml=\"<math xmlns=&quot;http://www.w3.org/1998/Math/MathML&quot;><msup><mi></mi><mn>208</mn></msup><mtext>Pb</mtext><msup><mi></mi><mn>204</mn></msup><mtext>Pb</mtext></math>\"><span class=\"MJX_Assistive_MathML\"><sup>208</sup>Pb<sup>204</sup>Pb</span></span></span><span>&nbsp;</span>and moderately high<span>&nbsp;</span><span class=\"math\"><span id=\"MathJax-Element-6-Frame\" class=\"MathJax_SVG\" data-mathml=\"<math xmlns=&quot;http://www.w3.org/1998/Math/MathML&quot;><msup><mi></mi><mn>87</mn></msup><mtext>Sr</mtext><msup><mi></mi><mn>86</mn></msup><mtext>Sr</mtext></math>\"><span class=\"MJX_Assistive_MathML\"><sup>87</sup>Sr<sup>86</sup>Sr</span></span></span><span>&nbsp;</span>(Dupal anomaly).</p><p>The Aitutaki group could have been derived from heterogeneous mantle plumes, which rose from the enriched deep mantle (the almost primitive lower mantle or recycled continental and oceanic slabs). On the other hand, the Mangaia component could have been derived from the depleted upper mantle which may have been metasomatized with a CO<sub>2</sub>-rich fluid, as indicated by the near-MORB values of Sr and Nd isotopes. Although Pb isotopic data of the two groups cannot be distinguished from each other statistically, the end components of the Pb-Pb system do not match with those of the Nd-Sr system. Thus, the data must be explained by a multi-, at least three, component mixing model: the mantle plumes (Dupal component and a recycled oceanic slab), metasomatized upper mantle, and lithosphere. The K-Ar ages and isotopic characteristics of the Cook-Austral rocks indicate that if one mantle plume rises from the deep mantle in this region, it has separated into at least two segments on the way to the surface.</p>","language":"English","publisher":"Elsevier","doi":"10.1016/0016-7037(88)90157-3","issn":"00167037","usgsCitation":"Nakamura, Y., and Tatsumoto, M., 1988, Pb, Nd, and Sr isotopic evidence for a multicomponent source for rocks of Cook-Austral Islands and heterogeneities of mantle plumes: Geochimica et Cosmochimica Acta, v. 52, no. 12, p. 2909-2924, https://doi.org/10.1016/0016-7037(88)90157-3.","productDescription":"16 p.","startPage":"2909","endPage":"2924","numberOfPages":"16","costCenters":[],"links":[{"id":225772,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"52","issue":"12","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"505a75fae4b0c8380cd77e5c","contributors":{"authors":[{"text":"Nakamura, Y.","contributorId":70117,"corporation":false,"usgs":true,"family":"Nakamura","given":"Y.","email":"","affiliations":[],"preferred":false,"id":368304,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Tatsumoto, M.","contributorId":76798,"corporation":false,"usgs":true,"family":"Tatsumoto","given":"M.","email":"","affiliations":[],"preferred":false,"id":368305,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":1012912,"text":"1012912 - 1988 - Effects of kelp forest removal on associated fish assemblages in central California","interactions":[],"lastModifiedDate":"2024-04-30T15:08:31.924679","indexId":"1012912","displayToPublicDate":"1988-01-01T00:00:00","publicationYear":"1988","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":2277,"text":"Journal of Experimental Marine Biology and Ecology","active":true,"publicationSubtype":{"id":10}},"title":"Effects of kelp forest removal on associated fish assemblages in central California","docAbstract":"<p><span>Visual surveys along subtidal belt transects were used to compare fish assemblages on an experimental and a control site before and after the removal of a canopy-forming kelp forest. The giant kelp&nbsp;</span><i>Macrocystis pyrifera</i><span>&nbsp;(L.) C.A. Agardh was removed at the holdfast from ≈ 1 ha of high relief structurally complex rock substratum. The abundance of seven species of fish, of which five were considered midwater species, significantly declined after the kelp was removed. No increases in abundance were noted within the experimental site. On the control site, two declines in abundance were observed, while two species increased in abundance. These results indicate that the presence of a giant kelp forest may increase the abundance and species diversity of the fish assemblages over a high relief rocky reef in central California, U.S.A.</span></p>","language":"English","publisher":"Elsevier","doi":"10.1016/0022-0981(88)90059-7","usgsCitation":"Bodkin, J.L., 1988, Effects of kelp forest removal on associated fish assemblages in central California: Journal of Experimental Marine Biology and Ecology, v. 117, no. 3, p. 227-238, https://doi.org/10.1016/0022-0981(88)90059-7.","productDescription":"12 p.","startPage":"227","endPage":"238","numberOfPages":"12","costCenters":[{"id":106,"text":"Alaska Biological Science Center","active":false,"usgs":true}],"links":[{"id":128516,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"117","issue":"3","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b24e4b07f02db6ae916","contributors":{"authors":[{"text":"Bodkin, James L. 0000-0003-1641-4438 jbodkin@usgs.gov","orcid":"https://orcid.org/0000-0003-1641-4438","contributorId":748,"corporation":false,"usgs":true,"family":"Bodkin","given":"James","email":"jbodkin@usgs.gov","middleInitial":"L.","affiliations":[{"id":116,"text":"Alaska Science Center Biology MFEB","active":true,"usgs":true},{"id":114,"text":"Alaska Science Center","active":true,"usgs":true}],"preferred":true,"id":318435,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":70013811,"text":"70013811 - 1988 - Normalization of oxygen and hydrogen isotope data","interactions":[],"lastModifiedDate":"2023-11-17T01:03:37.70955","indexId":"70013811","displayToPublicDate":"1988-01-01T00:00:00","publicationYear":"1988","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1214,"text":"Chemical Geology: Isotope Geoscience Section","active":true,"publicationSubtype":{"id":10}},"title":"Normalization of oxygen and hydrogen isotope data","docAbstract":"<p>To resolve confusion due to expression of isotopic data from different laboratories on non-corresponding scales, oxygen isotope analyses of<span>&nbsp;</span><i>all substances</i><span>&nbsp;</span>can be expressed relative to VSMOW or VPDB (Vienna Peedee belemnite) on scales normalized such that the δ<sup>18</sup>O of SLAP is −55.5% relative to VSMOW.</p><p>H<sub>3</sub><sup>+</sup><span>&nbsp;</span>contribution in hydrogen isotope ratio analysis can be easily determined using two gaseous reference samples that differ greatly in deuterium content.</p>","language":"English","publisher":"Elsevier","doi":"10.1016/0168-9622(88)90042-5","issn":"01689622","usgsCitation":"Coplen, T., 1988, Normalization of oxygen and hydrogen isotope data: Chemical Geology: Isotope Geoscience Section, v. 72, no. 4, p. 293-297, https://doi.org/10.1016/0168-9622(88)90042-5.","productDescription":"5 p.","startPage":"293","endPage":"297","numberOfPages":"5","costCenters":[],"links":[{"id":220615,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"72","issue":"4","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"505a67c5e4b0c8380cd734a5","contributors":{"authors":[{"text":"Coplen, T.B.","contributorId":34147,"corporation":false,"usgs":true,"family":"Coplen","given":"T.B.","affiliations":[],"preferred":false,"id":366913,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
]}