{"pageNumber":"6429","pageRowStart":"160700","pageSize":"25","recordCount":184904,"records":[{"id":5221757,"text":"5221757 - 1970 - DDE thins eggshells of captive American kestrels","interactions":[],"lastModifiedDate":"2024-07-29T20:44:02.689841","indexId":"5221757","displayToPublicDate":"1970-08-15T12:17:49","publicationYear":"1970","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":2840,"text":"Nature","active":true,"publicationSubtype":{"id":10}},"title":"DDE thins eggshells of captive American kestrels","docAbstract":"<p><span>EGGSHELL thinning in several species of raptorial and fish-eating birds, whose populations and/or reproductive success have declined dramatically in recent years, has been correlated with residues of DDE [1,1-dichloro-2,2-</span><i>bis</i><span>&nbsp;(</span><i>p</i><span>-chlorophenyl) ethylene] in their eggs</span><sup>1–3</sup><span>. DDE, a common metabolite of DDT [1,1,1-trichloro-2,2-</span><i>bis</i><span>(</span><i>p</i><span>-chlorophenyl) ethane] and a nearly universal contaminant in the food of these birds, has been considered to be the major chemical responsible for eggshell thinning.</span></p>","language":"English","publisher":"Nature","doi":"10.1038/227737a0","usgsCitation":"Wiemeyer, S.N., and Porter, R.D., 1970, DDE thins eggshells of captive American kestrels: Nature, v. 227, no. 5259, p. 737-738, https://doi.org/10.1038/227737a0.","productDescription":"2 p.","startPage":"737","endPage":"738","numberOfPages":"2","costCenters":[{"id":531,"text":"Patuxent Wildlife Research Center","active":true,"usgs":true}],"links":[{"id":196587,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"},{"id":16105,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://dx.doi.org/10.1038/227737a0","linkFileType":{"id":5,"text":"html"}}],"volume":"227","issue":"5259","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a09e4b07f02db5faef4","contributors":{"authors":[{"text":"Wiemeyer, Stanley N.","contributorId":78279,"corporation":false,"usgs":true,"family":"Wiemeyer","given":"Stanley","email":"","middleInitial":"N.","affiliations":[],"preferred":false,"id":334608,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Porter, Richard D.","contributorId":224624,"corporation":false,"usgs":false,"family":"Porter","given":"Richard","email":"","middleInitial":"D.","affiliations":[],"preferred":false,"id":907201,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":70226516,"text":"70226516 - 1970 - Geochronology of Tertiary igneous rocks in central Nevada","interactions":[],"lastModifiedDate":"2021-11-22T19:14:56.741228","indexId":"70226516","displayToPublicDate":"1970-08-01T13:03:03","publicationYear":"1970","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":5935,"text":"Bulletin of the Geological Society of America","active":true,"publicationSubtype":{"id":10}},"title":"Geochronology of Tertiary igneous rocks in central Nevada","docAbstract":"<p>Potassium-argon dating of Tertiary igneous rocks in Lander County, central Nevada, indicates that igneous activity was episodic and can be separated into three periods. Igneous activity started abruptly about 37 m.y. ago with local extrusion of andesitic to quartz-latitic lava flows and intrusion of hypabyssal rocks of similar composition. This activity ceased about 33 m.y. ago and was followed by extrusion of rhyolite ash-flow sheets that blanketed large parts of the region. These ash-flow sheets range from about 34 to 22 m.y. in age. The final phase, represented by basalt and basaltic-andesite flows and intrusive rhyolite flow-dome complexes, took place about 16 to 10 m.y. ago.</p><p>Andesitic to dacitic lava and hypabyssal rocks about 35 m.y. old are widespread east of Lander County and rhyolitic ash-flow tuffs 34 to 20 m.y. old are found south and east of Lander County. The younger (16 to 10 m.y.) basalt and basaltic-andesite flows are related to volcanism of the Snake River plain province to the north.</p><p>The precision of the ages was evaluated by means of: (1) repeat analyses of the same mineral separate, (2) age determination of mineral pairs from the same hand specimen, and (3) age determinations on widely spaced samples from the same geologic body or formation. The last method seems most meaningful from a geologic point of view.</p>","language":"English","publisher":"Geological Society of America","doi":"10.1130/0016-7606(1970)81[2317:GOTIRI]2.0.CO;2","usgsCitation":"McKee, E.H., and Silberman, M.L., 1970, Geochronology of Tertiary igneous rocks in central Nevada: Bulletin of the Geological Society of America, v. 81, no. 8, p. 2317-2327, https://doi.org/10.1130/0016-7606(1970)81[2317:GOTIRI]2.0.CO;2.","productDescription":"11 p.","startPage":"2317","endPage":"2327","costCenters":[],"links":[{"id":391994,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United States","state":"Nevada","county":"Lander 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Edwin H. mckee@usgs.gov","contributorId":3728,"corporation":false,"usgs":true,"family":"McKee","given":"Edwin","email":"mckee@usgs.gov","middleInitial":"H.","affiliations":[],"preferred":true,"id":827170,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Silberman, Miles L.","contributorId":92536,"corporation":false,"usgs":true,"family":"Silberman","given":"Miles","email":"","middleInitial":"L.","affiliations":[],"preferred":false,"id":827171,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":70226470,"text":"70226470 - 1970 - Latitude dependence of the angular dispersion of the geomagnetic field","interactions":[],"lastModifiedDate":"2021-11-18T17:00:58.059719","indexId":"70226470","displayToPublicDate":"1970-08-01T10:57:09","publicationYear":"1970","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1803,"text":"Geophysical Journal International","active":true,"publicationSubtype":{"id":10}},"title":"Latitude dependence of the angular dispersion of the geomagnetic field","docAbstract":"<p class=\"chapter-para\">Changes in the direction of the Earth's magnetic field at a given site are produced in part by wobble of the main geomagnetic dipole, in part by fluctuations in the intensity and direction of the non-dipole field, and in part by changes in the intensity of the main dipole field. These three processes combine to produce an angular variance that is strongly latitude dependent. A method is presented for isolating the contribution due to variation with latitude of the average intensity of the non-dipole field.</p>","language":"English","publisher":"Oxford University Press","doi":"10.1111/j.1365-246X.1970.tb06069.x","usgsCitation":"Cox, A., 1970, Latitude dependence of the angular dispersion of the geomagnetic field: Geophysical Journal International, v. 20, no. 3, p. 253-269, https://doi.org/10.1111/j.1365-246X.1970.tb06069.x.","productDescription":"17 p.","startPage":"253","endPage":"269","costCenters":[],"links":[{"id":391871,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"otherGeospatial":"Earth","volume":"20","issue":"3","noUsgsAuthors":false,"publicationStatus":"PW","contributors":{"authors":[{"text":"Cox, Allan","contributorId":89949,"corporation":false,"usgs":true,"family":"Cox","given":"Allan","email":"","affiliations":[],"preferred":false,"id":827014,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":70226261,"text":"70226261 - 1970 - Treasure Hill reinterpreted","interactions":[],"lastModifiedDate":"2021-11-17T14:36:29.245223","indexId":"70226261","displayToPublicDate":"1970-08-01T08:23:35","publicationYear":"1970","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":"Treasure Hill reinterpreted","docAbstract":"<p>No abstract available.</p>","language":"English","publisher":"Society of Economic Geologists","doi":"10.2113/gsecongeo.65.5.538","usgsCitation":"Smith, R., 1970, Treasure Hill reinterpreted: Economic Geology, v. 65, no. 5, p. 538-540, https://doi.org/10.2113/gsecongeo.65.5.538.","productDescription":"3 p.","startPage":"538","endPage":"540","costCenters":[],"links":[{"id":391797,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United States","state":"Nevada","county":"White Pine County","otherGeospatial":"Treasure Hill","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -115.48330307006836,\n              39.22352664357407\n            ],\n            [\n              -115.47701597213745,\n              39.22352664357407\n            ],\n            [\n              -115.47701597213745,\n              39.22661844131439\n            ],\n            [\n              -115.48330307006836,\n              39.22661844131439\n            ],\n            [\n              -115.48330307006836,\n              39.22352664357407\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","volume":"65","issue":"5","noUsgsAuthors":false,"publicationDate":"1970-08-01","publicationStatus":"PW","contributors":{"authors":[{"text":"Smith, Roscoe M.","contributorId":57747,"corporation":false,"usgs":true,"family":"Smith","given":"Roscoe M.","affiliations":[],"preferred":false,"id":826912,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":70226538,"text":"70226538 - 1970 - Computer ray tracing through complex geological models for ground motion studies","interactions":[],"lastModifiedDate":"2021-11-23T14:20:39.091863","indexId":"70226538","displayToPublicDate":"1970-08-01T08:15:34","publicationYear":"1970","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1808,"text":"Geophysics","active":true,"publicationSubtype":{"id":10}},"title":"Computer ray tracing through complex geological models for ground motion studies","docAbstract":"<p>No abstract available.</p>","language":"English","publisher":"Society of Exploration Geophysicists","doi":"10.1190/1.1440117","usgsCitation":"Yacoub, N.K., Scott, J.H., and McKeown, F.A., 1970, Computer ray tracing through complex geological models for ground motion studies: Geophysics, v. 35, no. 4, p. 586-602, https://doi.org/10.1190/1.1440117.","productDescription":"17 p.","startPage":"586","endPage":"602","costCenters":[],"links":[{"id":392044,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"35","issue":"4","noUsgsAuthors":false,"publicationStatus":"PW","contributors":{"authors":[{"text":"Yacoub, Nazieh K.","contributorId":84389,"corporation":false,"usgs":true,"family":"Yacoub","given":"Nazieh","email":"","middleInitial":"K.","affiliations":[],"preferred":false,"id":827281,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Scott, James H.","contributorId":73579,"corporation":false,"usgs":true,"family":"Scott","given":"James","email":"","middleInitial":"H.","affiliations":[],"preferred":false,"id":827282,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"McKeown, F. A.","contributorId":106100,"corporation":false,"usgs":true,"family":"McKeown","given":"F.","email":"","middleInitial":"A.","affiliations":[],"preferred":false,"id":827283,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":1013644,"text":"1013644 - 1970 - Apollo 11: Exposure of lower animals to lunar material","interactions":[],"lastModifiedDate":"2026-01-29T17:29:41.703695","indexId":"1013644","displayToPublicDate":"1970-07-31T00:00:00","publicationYear":"1970","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":3338,"text":"Science","active":true,"publicationSubtype":{"id":10}},"title":"Apollo 11: Exposure of lower animals to lunar material","docAbstract":"<p><span>Lunar material returned from the first manned landing on the moon was assayed for the presence of replicating agents possibly harmful to life on earth. Ten species of lower animals were exposed to lunar material for 28 days. No pathological effects attributable to contact with lunar material were detected.</span></p>","language":"English","publisher":"American Association for the Advancement of Science","doi":"10.1126/science.169.3944.470","usgsCitation":"Benschoter, C., Allison, T., Boyd, J., Brooks, M., Campbell, J., Groves, R., Heimpel, A., Mills, H., Ray, S., and Warren, J., 1970, Apollo 11: Exposure of lower animals to lunar material: Science, v. 169, no. 3944, p. 470-472, https://doi.org/10.1126/science.169.3944.470.","productDescription":"3 p.","startPage":"470","endPage":"472","costCenters":[{"id":365,"text":"Leetown Science Center","active":true,"usgs":true}],"links":[{"id":131939,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"otherGeospatial":"Moon","volume":"169","issue":"3944","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ac7e4b07f02db67afbf","contributors":{"authors":[{"text":"Benschoter, C.A.","contributorId":102840,"corporation":false,"usgs":true,"family":"Benschoter","given":"C.A.","email":"","affiliations":[],"preferred":false,"id":318960,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Allison, T.C.","contributorId":97858,"corporation":false,"usgs":true,"family":"Allison","given":"T.C.","email":"","affiliations":[],"preferred":false,"id":318959,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Boyd, J.F.","contributorId":74715,"corporation":false,"usgs":true,"family":"Boyd","given":"J.F.","email":"","affiliations":[],"preferred":false,"id":318955,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Brooks, M.A.","contributorId":8417,"corporation":false,"usgs":true,"family":"Brooks","given":"M.A.","email":"","affiliations":[],"preferred":false,"id":318951,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"Campbell, J.W.","contributorId":93440,"corporation":false,"usgs":true,"family":"Campbell","given":"J.W.","email":"","affiliations":[],"preferred":false,"id":318957,"contributorType":{"id":1,"text":"Authors"},"rank":5},{"text":"Groves, R.O.","contributorId":89098,"corporation":false,"usgs":true,"family":"Groves","given":"R.O.","email":"","affiliations":[],"preferred":false,"id":318956,"contributorType":{"id":1,"text":"Authors"},"rank":6},{"text":"Heimpel, A.M.","contributorId":34468,"corporation":false,"usgs":true,"family":"Heimpel","given":"A.M.","email":"","affiliations":[],"preferred":false,"id":318954,"contributorType":{"id":1,"text":"Authors"},"rank":7},{"text":"Mills, H.E.","contributorId":13189,"corporation":false,"usgs":true,"family":"Mills","given":"H.E.","email":"","affiliations":[],"preferred":false,"id":318952,"contributorType":{"id":1,"text":"Authors"},"rank":8},{"text":"Ray, S.M.","contributorId":93861,"corporation":false,"usgs":true,"family":"Ray","given":"S.M.","email":"","affiliations":[],"preferred":false,"id":318958,"contributorType":{"id":1,"text":"Authors"},"rank":9},{"text":"Warren, J.W.","contributorId":20285,"corporation":false,"usgs":true,"family":"Warren","given":"J.W.","email":"","affiliations":[],"preferred":false,"id":318953,"contributorType":{"id":1,"text":"Authors"},"rank":10}]}}
,{"id":70010138,"text":"70010138 - 1970 - Arctic paleo-oceanography in late Cenozoic time","interactions":[],"lastModifiedDate":"2026-01-29T17:35:48.948889","indexId":"70010138","displayToPublicDate":"1970-07-31T00:00:00","publicationYear":"1970","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":3338,"text":"Science","active":true,"publicationSubtype":{"id":10}},"title":"Arctic paleo-oceanography in late Cenozoic time","docAbstract":"Sediment cores from the Arctic Ocean yield significant faunal and lithologic evidence of alternating cold and milder periods for the last 6 million years. Although high-latitude continental glaciation commenced prior to 6 million years ago, the Arctic Ocean remained free of permanent pack ice up to approximately 0.7 million years ago, after which successive ice-covered and ice-free conditions existed.","language":"English","publisher":"American Association for the Advancement of Science","doi":"10.1126/science.169.3944.474","issn":"00368075","usgsCitation":"Herman, Y., 1970, Arctic paleo-oceanography in late Cenozoic time: Science, v. 169, no. 3944, p. 474-477, https://doi.org/10.1126/science.169.3944.474.","productDescription":"4 p.","startPage":"474","endPage":"477","costCenters":[],"links":[{"id":219129,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"otherGeospatial":"Arctic Ocean","volume":"169","issue":"3944","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"5059ed55e4b0c8380cd49746","contributors":{"authors":[{"text":"Herman, Y.","contributorId":95601,"corporation":false,"usgs":true,"family":"Herman","given":"Y.","email":"","affiliations":[],"preferred":false,"id":358089,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":70010268,"text":"70010268 - 1970 - Deuterium content of snow cores from Sierra Nevada area","interactions":[],"lastModifiedDate":"2026-01-29T17:24:31.49247","indexId":"70010268","displayToPublicDate":"1970-07-31T00:00:00","publicationYear":"1970","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":3338,"text":"Science","active":true,"publicationSubtype":{"id":10}},"title":"Deuterium content of snow cores from Sierra Nevada area","docAbstract":"The relative deuterium content was measured on 37 snow cores collected in April 1969 in the Sierra Nevada. The deuterium content varies inversely with altitude of collection (approximately 40 per mil per 1000 meters) but is unrelated to latitude. The altitude relationship is particularly well defined west of the crest of the range but is not well defined east of the crest. However, samples from east of the crest tend to be depleted by about 10 to 15 per mil relative to samples collected at the same elevation west of the crest. We propose that the deuterium content of snow cores, collected so as to include the total winter's precipitation, can be used as a climatic indicator to compare the climate of one winter with that of another.","language":"English","publisher":"American Association for the Advancement of Science","doi":"10.1126/science.169.3944.467","issn":"00368075","usgsCitation":"Friedman, I., and Smith, G., 1970, Deuterium content of snow cores from Sierra Nevada area: Science, v. 169, no. 3944, p. 467-470, https://doi.org/10.1126/science.169.3944.467.","productDescription":"4 p.","startPage":"467","endPage":"470","costCenters":[],"links":[{"id":218786,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United States","state":"California, Nevada","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"coordinates\": [\n          [\n            [\n              -121.01606059384827,\n              39.24050139709556\n            ],\n            [\n              -121.01606059384827,\n              38.20977649215865\n            ],\n            [\n              -119.38801271817681,\n              38.20977649215865\n            ],\n            [\n              -119.38801271817681,\n              39.24050139709556\n            ],\n            [\n              -121.01606059384827,\n              39.24050139709556\n            ]\n          ]\n        ],\n        \"type\": \"Polygon\"\n      }\n    }\n  ]\n}","volume":"169","issue":"3944","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"505a0003e4b0c8380cd4f531","contributors":{"authors":[{"text":"Friedman, I.","contributorId":95596,"corporation":false,"usgs":true,"family":"Friedman","given":"I.","email":"","affiliations":[],"preferred":false,"id":358485,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Smith, G.I.","contributorId":103694,"corporation":false,"usgs":true,"family":"Smith","given":"G.I.","email":"","affiliations":[],"preferred":false,"id":358486,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":70010167,"text":"70010167 - 1970 - Petrified peat from a Permian coal bed in Antarctica","interactions":[],"lastModifiedDate":"2026-01-30T16:01:46.774886","indexId":"70010167","displayToPublicDate":"1970-07-17T00:00:00","publicationYear":"1970","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":3338,"text":"Science","active":true,"publicationSubtype":{"id":10}},"title":"Petrified peat from a Permian coal bed in Antarctica","docAbstract":"Petrified plant remains that composed a Permian peat deposit occur at a coal horizon in a local area of Mount Augusta near the Beardmore Glacier in Antarctica. This discovery is the first in the entire Gondwana area that yields plant materials as exquisitely preserved as the materials of the well-known coal-ball localities of the Northern Hemisphere. A sampling of anatomical details is illustrated.","language":"English","publisher":"American Association for the Advancement of Science","doi":"10.1126/science.169.3942.274","issn":"00368075","usgsCitation":"Schopf, J.M., 1970, Petrified peat from a Permian coal bed in Antarctica: Science, v. 169, no. 3942, p. 274-277, https://doi.org/10.1126/science.169.3942.274.","productDescription":"4 p.","startPage":"274","endPage":"277","costCenters":[],"links":[{"id":219597,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"otherGeospatial":"Beardmore Glacier, Antarctica","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"coordinates\": [\n          [\n            [\n              153.23439210063793,\n              -79.35558863007742\n            ],\n            [\n              153.23439210063793,\n              -81.35012172739206\n            ],\n            [\n              164.93171924346524,\n              -81.35012172739206\n            ],\n            [\n              164.93171924346524,\n              -79.35558863007742\n            ],\n            [\n              153.23439210063793,\n              -79.35558863007742\n            ]\n          ]\n        ],\n        \"type\": \"Polygon\"\n      }\n    }\n  ]\n}","volume":"169","issue":"3942","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"505a7776e4b0c8380cd784d5","contributors":{"authors":[{"text":"Schopf, J. M.","contributorId":42639,"corporation":false,"usgs":true,"family":"Schopf","given":"J.","middleInitial":"M.","affiliations":[],"preferred":false,"id":358183,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":70010430,"text":"70010430 - 1970 - Nuclear explosions and distant earthquakes: A search for correlations","interactions":[],"lastModifiedDate":"2026-01-29T18:03:08.986234","indexId":"70010430","displayToPublicDate":"1970-07-10T00:00:00","publicationYear":"1970","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":3338,"text":"Science","active":true,"publicationSubtype":{"id":10}},"title":"Nuclear explosions and distant earthquakes: A search for correlations","docAbstract":"An apparent correlation between nuclear explosions and earthquakes has been reported for the events between September 1961 and September 1966. When data from the events between September 1966 and December 1968 are examined, this correlation disappears. No relationship between the size of the nuclear explosions and the number of distant earthquakes is apparent in the data.","language":"English","publisher":"American Association for the Advancement of Science","doi":"10.1126/science.169.3941.176","issn":"00368075","usgsCitation":"Healy, J.H., and Marshall, P., 1970, Nuclear explosions and distant earthquakes: A search for correlations: Science, v. 169, no. 3941, p. 176-177, https://doi.org/10.1126/science.169.3941.176.","productDescription":"2 p.","startPage":"176","endPage":"177","costCenters":[],"links":[{"id":219613,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"169","issue":"3941","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"505a68c2e4b0c8380cd739ab","contributors":{"authors":[{"text":"Healy, J. H.","contributorId":48968,"corporation":false,"usgs":true,"family":"Healy","given":"J.","email":"","middleInitial":"H.","affiliations":[],"preferred":false,"id":358904,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Marshall, P.A.","contributorId":79900,"corporation":false,"usgs":true,"family":"Marshall","given":"P.A.","email":"","affiliations":[],"preferred":false,"id":358905,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":70010104,"text":"70010104 - 1970 - Deformation twins in Hornblende","interactions":[],"lastModifiedDate":"2026-01-29T17:58:11.515529","indexId":"70010104","displayToPublicDate":"1970-07-10T00:00:00","publicationYear":"1970","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":3338,"text":"Science","active":true,"publicationSubtype":{"id":10}},"title":"Deformation twins in Hornblende","docAbstract":"<div class=\"panel-pane pane-highwire-panel-tabs-container article__body\"><div class=\"pane-content\"><div id=\"panels-ajax-tab-container-highwire_article_tabs\" class=\"panels-ajax-tab-container\" data-panels-ajax-tab-preloaded=\"jnl_sci_tab_art\"><div class=\"panels-ajax-tab-wrap-jnl_sci_tab_art\"><div class=\"panel-display panel-1col clearfix\"><div class=\"panel-panel panel-col\"><div><div class=\"panel-pane pane-highwire-markup\"><div class=\"pane-content\"><div class=\"highwire-markup\"><div id=\"content-block-markup\" data-highwire-cite-ref-tooltip-instance=\"highwire_reflinks_tooltip\" data-highwire-glossary-tooltip-instance=\"highwire_reflinks_tooltip\"><div class=\"article abstract-view \"><div id=\"abstract-1\" class=\"section abstract\"><p id=\"p-1\">Hornblende deformation twins with twin planes parallel to (¯101) are produced experimentally in single crystals by compression parallel to the<span>&nbsp;</span><i>c</i><span>&nbsp;</span>axis. Twinning occurs at confining pressures from 5 to 15 kilobars and temperatures from 400° to 600°C (strain rate, 10<sup>-5</sup><span>&nbsp;</span>per second).</p></div></div><span id=\"related-urls\"></span></div></div></div></div></div></div></div></div></div></div></div>","language":"English","publisher":"American Association for the Advancement of Science","doi":"10.1126/science.169.3941.173","issn":"00368075","usgsCitation":"Rooney, T., Riecker, R., and Ross, M., 1970, Deformation twins in Hornblende: Science, v. 169, no. 3941, p. 173-175, https://doi.org/10.1126/science.169.3941.173.","productDescription":"3 p.","startPage":"173","endPage":"175","costCenters":[],"links":[{"id":218627,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"169","issue":"3941","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"5059fe4de4b0c8380cd4ec60","contributors":{"authors":[{"text":"Rooney, T.P.","contributorId":52712,"corporation":false,"usgs":true,"family":"Rooney","given":"T.P.","email":"","affiliations":[],"preferred":false,"id":357909,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Riecker, R.E.","contributorId":41962,"corporation":false,"usgs":true,"family":"Riecker","given":"R.E.","email":"","affiliations":[],"preferred":false,"id":357908,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Ross, M.","contributorId":8026,"corporation":false,"usgs":true,"family":"Ross","given":"M.","email":"","affiliations":[],"preferred":false,"id":357907,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":70211007,"text":"70211007 - 1970 - Radiogenic heat production of contrasting magma series: Bearing on interpretation of heat flow","interactions":[],"lastModifiedDate":"2020-07-09T18:46:27.744971","indexId":"70211007","displayToPublicDate":"1970-07-09T13:43:40","publicationYear":"1970","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1723,"text":"GSA Bulletin","active":true,"publicationSubtype":{"id":10}},"title":"Radiogenic heat production of contrasting magma series: Bearing on interpretation of heat flow","docAbstract":"<p><span>Variation in radiogenic heat production of rocks of diverse magma series (representative of calcic, calc-alkalic, alkali-calcic, and alkalic petrographic provinces on a worldwide basis) is better correlated with some form of magmatic differentiation index, rather than simply with potassium content alone as commonly supposed. The “lime-alkali” (Peacock) index generally gives the best correlation of the various indices tested. Plots of heat production for igneous suites versus indices of differentiation (“heat production trends”) demonstrate systematic correlations of heat productivity as functions of fractionation trends and/or spatial-temporal associations. In general, heat production trends of calcic suites tend to indicate lower radiogenic heat productivity than those of more alkalic suites for a given silica or potassium content. Because many recent measurements of heat flow in plutons can be linearly related to heat production of surface rocks, these “heat production trends” have important bearing on the interpretation of crustal heat flow. Our data suggest possible alternative interpretations of the heat production-heat flow pattern for the Sierra Nevada which differ from that in Lachen-bruch's (1968) preliminary geothermal model.</span></p>","language":"English","publisher":"GSA","doi":"10.1130/0016-7606(1970)81[1447:RHPOCM]2.0.CO;2","usgsCitation":"Tilling, R.I., Gottfried, D., and Dodge, F.C., 1970, Radiogenic heat production of contrasting magma series: Bearing on interpretation of heat flow: GSA Bulletin, v. 81, no. 5, p. 1447-1462, https://doi.org/10.1130/0016-7606(1970)81[1447:RHPOCM]2.0.CO;2.","productDescription":"16 p.","startPage":"1447","endPage":"1462","costCenters":[{"id":153,"text":"California Volcano Observatory","active":false,"usgs":true}],"links":[{"id":376226,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"81","issue":"5","noUsgsAuthors":false,"publicationStatus":"PW","contributors":{"authors":[{"text":"Tilling, Robert I. 0000-0003-4263-7221 rtilling@usgs.gov","orcid":"https://orcid.org/0000-0003-4263-7221","contributorId":2567,"corporation":false,"usgs":true,"family":"Tilling","given":"Robert","email":"rtilling@usgs.gov","middleInitial":"I.","affiliations":[],"preferred":true,"id":792407,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Gottfried, David","contributorId":82295,"corporation":false,"usgs":true,"family":"Gottfried","given":"David","email":"","affiliations":[],"preferred":false,"id":792408,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Dodge, F. C. W.","contributorId":18755,"corporation":false,"usgs":true,"family":"Dodge","given":"F.","email":"","middleInitial":"C. W.","affiliations":[],"preferred":false,"id":792409,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":5221758,"text":"5221758 - 1970 - Propagation of captive American kestrels","interactions":[],"lastModifiedDate":"2025-02-19T17:17:09.722732","indexId":"5221758","displayToPublicDate":"1970-07-02T00:00:00","publicationYear":"1970","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":2508,"text":"Journal of Wildlife Management","active":true,"publicationSubtype":{"id":10}},"title":"Propagation of captive American kestrels","docAbstract":"<p>A colony of kestrels (<i>Palco sparverius</i>) was established at the Patuxent Wildlife Research Center in 1964 in connection with work on pesticides. The kestrels were acquired from the wild, both as nestlings and as full-grown birds, and were housed in several rows of outdoor pens. Each 50 x 20 ft pen was covered with wire netting and had its long sides in common with adjacent pens. During the first two reproductive seasons, untreated parent birds (dosed birds are not included in this paper) ate eggs and young. Cannibalism virtually ceased after the diet was changed from ground beef or horsemeat supplemented with liver, vitamins, and minerals to one containing a finely ground mixture of laboratory rodents, chicken heads, skinned chicken necks, and supplements; hatching success thereafter generally equaled that of a wild population. In 1967, 16 pairs of untreated hawks (3-year-old females) laid clutches averaging 4.9 eggs, hatched 88 percent of their eggs, and fledged 88 percent of their young. In 1968, 10 pairs of this group (4-year-old females) laid clutches averaging 4.9 eggs, hatched 51 percent of their eggs, and fledged 85 percent of their young. Nine yearling pairs (hatched in captivity) laid clutches in 1968 averaging 5.1 eggs, hatched 87 percent of their eggs, and fledged all of their young.</p>","language":"English","publisher":"Wiley","doi":"10.2307/3798868","usgsCitation":"Porter, R.D., and Wiemeyer, S.N., 1970, Propagation of captive American kestrels: Journal of Wildlife Management, v. 34, no. 3, p. 594-604, https://doi.org/10.2307/3798868.","productDescription":"11 p.","startPage":"594","endPage":"604","costCenters":[{"id":531,"text":"Patuxent Wildlife Research Center","active":true,"usgs":true}],"links":[{"id":193515,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.er.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United States","state":"Maryland","otherGeospatial":"Patuxent Wildlife Research Center","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"coordinates\": [\n          [\n            [\n              -76.8166482385359,\n              39.072382156197875\n            ],\n            [\n              -76.8166482385359,\n              39.01305201803032\n            ],\n            [\n              -76.74348687025322,\n              39.01305201803032\n            ],\n            [\n              -76.74348687025322,\n              39.072382156197875\n            ],\n            [\n              -76.8166482385359,\n              39.072382156197875\n            ]\n          ]\n        ],\n        \"type\": \"Polygon\"\n      }\n    }\n  ]\n}","volume":"34","issue":"3","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4aaae4b07f02db669074","contributors":{"authors":[{"text":"Porter, Richard D.","contributorId":224624,"corporation":false,"usgs":false,"family":"Porter","given":"Richard","email":"","middleInitial":"D.","affiliations":[],"preferred":false,"id":907203,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Wiemeyer, Stanley N.","contributorId":78279,"corporation":false,"usgs":true,"family":"Wiemeyer","given":"Stanley","email":"","middleInitial":"N.","affiliations":[],"preferred":false,"id":334610,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":70226522,"text":"70226522 - 1970 - Summary of regional evidence for right-lateral displacement in the western Great Basin: Reply","interactions":[],"lastModifiedDate":"2021-11-22T21:44:19.383842","indexId":"70226522","displayToPublicDate":"1970-07-01T15:38:49","publicationYear":"1970","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":5935,"text":"Bulletin of the Geological Society of America","active":true,"publicationSubtype":{"id":10}},"title":"Summary of regional evidence for right-lateral displacement in the western Great Basin: Reply","docAbstract":"<p>No abstract available.</p>","language":"English","publisher":"Geological Society of America","doi":"10.1130/0016-7606(1970)81[2175:SOREFR]2.0.CO;2","usgsCitation":"Stewart, J.H., Albers, J., and Poole, F.G., 1970, Summary of regional evidence for right-lateral displacement in the western Great Basin: Reply: Bulletin of the Geological Society of America, v. 81, no. 7, p. 2175-2179, https://doi.org/10.1130/0016-7606(1970)81[2175:SOREFR]2.0.CO;2.","productDescription":"5 p.","startPage":"2175","endPage":"2179","costCenters":[],"links":[{"id":392018,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United States","state":"California, Nevada","otherGeospatial":"Great Basin","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -118.63037109375,\n              35.92019610057511\n            ],\n            [\n              -115.14221191406249,\n              35.92019610057511\n            ],\n            [\n              -115.14221191406249,\n              38.543869175876154\n            ],\n            [\n              -118.63037109375,\n              38.543869175876154\n            ],\n            [\n              -118.63037109375,\n              35.92019610057511\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","volume":"81","issue":"7","noUsgsAuthors":false,"publicationStatus":"PW","contributors":{"authors":[{"text":"Stewart, John H.","contributorId":83086,"corporation":false,"usgs":true,"family":"Stewart","given":"John","email":"","middleInitial":"H.","affiliations":[],"preferred":false,"id":827195,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Albers, John P.","contributorId":55291,"corporation":false,"usgs":true,"family":"Albers","given":"John P.","affiliations":[],"preferred":false,"id":827196,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Poole, Forrest G. 0000-0001-8487-0799 bpoole@usgs.gov","orcid":"https://orcid.org/0000-0001-8487-0799","contributorId":1543,"corporation":false,"usgs":true,"family":"Poole","given":"Forrest","email":"bpoole@usgs.gov","middleInitial":"G.","affiliations":[{"id":171,"text":"Central Mineral and Environmental Resources Science Center","active":true,"usgs":true}],"preferred":true,"id":827197,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":70170770,"text":"70170770 - 1970 - 4 Earthquake: Major offshore earthquakes recall the Aztec myth","interactions":[],"lastModifiedDate":"2016-05-02T14:14:17","indexId":"70170770","displayToPublicDate":"1970-07-01T15:15:00","publicationYear":"1970","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1435,"text":"Earthquake Information Bulletin (USGS)","active":true,"publicationSubtype":{"id":10}},"title":"4 Earthquake: Major offshore earthquakes recall the Aztec myth","docAbstract":"<p>Long before the sun clears the eastern mountains of April 29, 1970, the savanna highlands of Chiapas tremble from a magnitude 6.7 earthquake centered off the Pacific coast near Mexico&rsquo;s southern border. Then, for a few hours, he Isthmus of Tehuantepec is quiet.</p>","language":"English","publisher":"U.S. Government Printing Office","publisherLocation":"Washington, D.C.","usgsCitation":"United States Department of Commerce, 1970, 4 Earthquake: Major offshore earthquakes recall the Aztec myth: Earthquake Information Bulletin (USGS), v. 2, no. 4, p. 4-7.","productDescription":"4 p.","startPage":"4","endPage":"7","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[],"links":[{"id":320828,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"Mexico","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -117.158203125,\n              32.58384932565662\n            ],\n            [\n              -114.78515624999999,\n  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,{"id":70226542,"text":"70226542 - 1970 - Boulder Creek batholith, Colorado part I: Allanite and its bearing upon age patterns","interactions":[],"lastModifiedDate":"2021-11-23T15:36:47.311412","indexId":"70226542","displayToPublicDate":"1970-07-01T09:12:52","publicationYear":"1970","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":5935,"text":"Bulletin of the Geological Society of America","active":true,"publicationSubtype":{"id":10}},"title":"Boulder Creek batholith, Colorado part I: Allanite and its bearing upon age patterns","docAbstract":"<p>Allanite is abundant and commonly attains unusually large size as a late-replacement mineral in: (1) the comagnatic rocks of the Precambrian Boulder Creek batholith; (2) associated amphibolite xenoliths and related hybrid rocks; and (3) distinctly younger intrusions of Silver Plume Granite that cut the complex. Allanite porphyroblasts develop by replacement of biotite, probably in the presence of emanations from the rare earth-rich and thorium-rich Silver Plume Granite. The largest allanite crystals are made up of nearly isotropic (metamict) cores and birefringent (recrystallized) rims. Smaller crystals are made up exclusively of birefringent material. The maximum birefringence is shown to be that expectable in allanite of Late Cretaceous to early Tertiary age. As plotted on maps, the birefringence increases, and the thorium and uranium contents of the allanite decrease toward a Laramide stock. The variation in birefringence is, therefore, largely relatable to variations in the post-Laramide radiation dosage brought about by differences in the amounts of uranium and thorium lost during recrystallization. The recrystallized allanite is itself partly replaced by epidote which characteristically occurs as a border between allanite and biotite.</p><p>Total rare-earth oxides for the eight samples of allanite analyzed range from 17.5 to 21.3 percent by weight. In 13 samples, thorium ranged from 0.50 to 1.14 percent by weight, and uranium from 54 to 158 parts pparts per million. Ranges in optical measurements for 20 samples using the spindle stage are: Nα = 1.719–1.759, Nβ = 1.731-1.774, N<sub>γ</sub><span>&nbsp;</span>= 1.741–1.784, birefringence = 0.020–0.032, 2V<sub>X</sub><span>&nbsp;</span>(calc.) 70°–84°. Ranges for unit-cell data obtained on 8 samples are: a = 8.948–8.985Å, b = 5.721-5.763Å, c = 10.184–10.240Å, β = 115°7.50′–115°25.89′ and volume = 473.02–478.43Å<span>&nbsp;</span><sup>3</sup>. The average value for the ratio a:b:c = 1.561:1:1.778.</p>","language":"English","publisher":"Geological Society of America","doi":"10.1130/0016-7606(1970)81[1973:BCBCPI]2.0.CO;2","usgsCitation":"Hickling, N.L., Phair, G., Moore, R., and Rose, H.J., 1970, Boulder Creek batholith, Colorado part I: Allanite and its bearing upon age patterns: Bulletin of the Geological Society of America, v. 81, no. 7, p. 1973-1993, https://doi.org/10.1130/0016-7606(1970)81[1973:BCBCPI]2.0.CO;2.","productDescription":"21p.","startPage":"1973","endPage":"1993","costCenters":[],"links":[{"id":392049,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United States","state":"Colorado","otherGeospatial":"Boulder Creek batholith","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -105.96450805664062,\n              39.536880650643056\n            ],\n            [\n              -104.98672485351562,\n              39.536880650643056\n            ],\n            [\n              -104.98672485351562,\n              40.263808598903566\n            ],\n            [\n              -105.96450805664062,\n              40.263808598903566\n            ],\n            [\n              -105.96450805664062,\n              39.536880650643056\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","volume":"81","issue":"7","noUsgsAuthors":false,"publicationStatus":"PW","contributors":{"authors":[{"text":"Hickling, Nelson L.","contributorId":16456,"corporation":false,"usgs":true,"family":"Hickling","given":"Nelson","email":"","middleInitial":"L.","affiliations":[],"preferred":false,"id":827291,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Phair, George","contributorId":91512,"corporation":false,"usgs":true,"family":"Phair","given":"George","email":"","affiliations":[],"preferred":false,"id":827292,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Moore, Roosevelt","contributorId":55029,"corporation":false,"usgs":true,"family":"Moore","given":"Roosevelt","email":"","affiliations":[],"preferred":false,"id":827293,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Rose, Harry J. 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,{"id":70226285,"text":"70226285 - 1970 - The Bluebell Mine, British Columbia: I. Mineralogy, paragenesis, fluid inclusions, and the isotopes of hydrogen, oxygen, and carbon","interactions":[],"lastModifiedDate":"2021-11-17T15:19:56.072432","indexId":"70226285","displayToPublicDate":"1970-07-01T09:05:35","publicationYear":"1970","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":"The Bluebell Mine, British Columbia: I. Mineralogy, paragenesis, fluid inclusions, and the isotopes of hydrogen, oxygen, and carbon","docAbstract":"<p>No abstract available.</p>","language":"English","publisher":"Society of Economic Geologists","doi":"10.2113/gsecongeo.65.4.417","usgsCitation":"Ohmoto, H., and Rye, R.O., 1970, The Bluebell Mine, British Columbia: I. Mineralogy, paragenesis, fluid inclusions, and the isotopes of hydrogen, oxygen, and carbon: Economic Geology, v. 65, no. 4, p. 417-437, https://doi.org/10.2113/gsecongeo.65.4.417.","productDescription":"21 p.","startPage":"417","endPage":"437","costCenters":[],"links":[{"id":391800,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"Canada","state":"British Columbia","otherGeospatial":"Bluebell mine, Kootenay Lake","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -116.98516845703126,\n              50.154026111358014\n            ],\n            [\n              -117.41912841796874,\n              50.08886893382965\n            ],\n            [\n              -117.3614501953125,\n              49.990083926193954\n            ],\n            [\n              -117.35870361328124,\n              49.944150351645455\n            ],\n            [\n              -117.43560791015624,\n              49.81317633337614\n            ],\n            [\n              -117.44659423828125,\n              49.690731711357216\n            ],\n            [\n              -117.60589599609374,\n              49.55728898983402\n            ],\n            [\n              -117.44659423828125,\n              49.457413352792216\n            ],\n            [\n              -117.70202636718751,\n              49.14039340493346\n            ],\n            [\n              -117.60314941406249,\n              49.09725059408649\n            ],\n            [\n              -117.57568359374999,\n              49.046869878327136\n            ],\n            [\n              -117.44659423828125,\n              49.0738659012854\n            ],\n            [\n              -117.3504638671875,\n              49.027063474829326\n            ],\n            [\n              -116.64459228515625,\n              49.151173244278\n            ],\n            [\n              -116.83685302734375,\n              49.35733376286064\n            ],\n            [\n              -116.86431884765625,\n              49.468124067331644\n            ],\n            [\n              -116.89453125,\n              49.58756804188783\n            ],\n            [\n              -116.971435546875,\n              49.61248962905261\n            ],\n            [\n              -116.96594238281249,\n              49.66407240384585\n            ],\n            [\n              -116.91925048828124,\n              49.7919038200459\n            ],\n            [\n              -116.93572998046874,\n              50.062428593700936\n            ],\n            [\n              -116.98516845703126,\n              50.154026111358014\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","volume":"65","issue":"4","noUsgsAuthors":false,"publicationDate":"1970-07-01","publicationStatus":"PW","contributors":{"authors":[{"text":"Ohmoto, Hiroshi","contributorId":269034,"corporation":false,"usgs":false,"family":"Ohmoto","given":"Hiroshi","email":"","affiliations":[{"id":6644,"text":"Princeton University","active":true,"usgs":false},{"id":25493,"text":"University of Alberta, Canada","active":true,"usgs":false}],"preferred":false,"id":826921,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Rye, Robert O. rrye@usgs.gov","contributorId":1486,"corporation":false,"usgs":true,"family":"Rye","given":"Robert","email":"rrye@usgs.gov","middleInitial":"O.","affiliations":[{"id":211,"text":"Crustal Geophysics and Geochemistry Science Center","active":true,"usgs":true}],"preferred":true,"id":826922,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":70226269,"text":"70226269 - 1970 - Content of zinc and copper in some fluid inclusions from the Cave-in-Rock district, southern Illinois","interactions":[],"lastModifiedDate":"2021-11-17T14:53:51.993737","indexId":"70226269","displayToPublicDate":"1970-07-01T08:40:03","publicationYear":"1970","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":"Content of zinc and copper in some fluid inclusions from the Cave-in-Rock district, southern Illinois","docAbstract":"<p>No abstract available.</p>","language":"English","publisher":"Society of Economic Geologists","doi":"10.2113/gsecongeo.65.4.451","usgsCitation":"Pinckney, D.M., and Haffty, J., 1970, Content of zinc and copper in some fluid inclusions from the Cave-in-Rock district, southern Illinois: Economic Geology, v. 65, no. 4, p. 451-458, https://doi.org/10.2113/gsecongeo.65.4.451.","productDescription":"8 p.","startPage":"451","endPage":"458","costCenters":[],"links":[{"id":391799,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United States","state":"Illinois","otherGeospatial":"Cave-in-Rock district, Hicks dome","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -88.37333679199219,\n              37.51156412051219\n            ],\n            [\n              -88.31926345825195,\n              37.51156412051219\n            ],\n            [\n              -88.31926345825195,\n              37.545393957073436\n            ],\n            [\n              -88.37333679199219,\n              37.545393957073436\n            ],\n            [\n              -88.37333679199219,\n              37.51156412051219\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","volume":"65","issue":"4","noUsgsAuthors":false,"publicationDate":"1970-07-01","publicationStatus":"PW","contributors":{"authors":[{"text":"Pinckney, Darrell M.","contributorId":54607,"corporation":false,"usgs":true,"family":"Pinckney","given":"Darrell","email":"","middleInitial":"M.","affiliations":[],"preferred":false,"id":826913,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Haffty, Joseph","contributorId":79450,"corporation":false,"usgs":true,"family":"Haffty","given":"Joseph","email":"","affiliations":[],"preferred":false,"id":826914,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":1013867,"text":"1013867 - 1970 - A microsporidan (Protozoa: Cnidospora) in channel catfish (Ictalurus punctatus)","interactions":[],"lastModifiedDate":"2025-04-02T16:31:06.748677","indexId":"1013867","displayToPublicDate":"1970-07-01T00:00:00","publicationYear":"1970","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":"A microsporidan (Protozoa: Cnidospora) in channel catfish (Ictalurus punctatus)","docAbstract":"<p>No abstract available.&nbsp;</p>","language":"English","publisher":"BioOne","doi":"10.7589/0090-3558-6.3.173","usgsCitation":"Herman, R.L., and Putz, R., 1970, A microsporidan (Protozoa: Cnidospora) in channel catfish (Ictalurus punctatus): Journal of Wildlife Diseases, v. 6, no. 3, p. 173-173, https://doi.org/10.7589/0090-3558-6.3.173.","productDescription":"1 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,{"id":5220470,"text":"5220470 - 1970 - An outbreak of fowl cholera in waterfowl on the Chesapeake Bay","interactions":[],"lastModifiedDate":"2025-04-01T16:37:26.892803","indexId":"5220470","displayToPublicDate":"1970-07-01T00:00:00","publicationYear":"1970","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 fowl cholera in waterfowl on the Chesapeake Bay","docAbstract":"<p><span>An outbreak of fowl cholera (</span><i>Pasteurella multocida</i><span>&nbsp;infection) occurred in waterfowl wintering on the Chesapeake Bay during February to March 1970. Losses were primarily confined to sea ducks: oldsquaws (</span><i>Clangula hyemalis</i><span>), white-winged scoters (</span><i>Melanitta deglandi</i><span>), golden-eyes (</span><i>Bucephala clangula</i><span>), and buffleheads (</span><i>Bucephala albeola</i><span>).</span></p>","language":"English","publisher":"Wildlife Disease Association","doi":"10.7589/0090-3558-6.4.404","usgsCitation":"Locke, L.N., Stotts, V., and Wolfhard, G., 1970, An outbreak of fowl cholera in waterfowl on the Chesapeake Bay: Journal of Wildlife Diseases, v. 6, no. 4, p. 404-407, https://doi.org/10.7589/0090-3558-6.4.404.","productDescription":"4 p.","startPage":"404","endPage":"407","costCenters":[{"id":531,"text":"Patuxent Wildlife Research Center","active":true,"usgs":true}],"links":[{"id":488678,"rank":2,"type":{"id":40,"text":"Open Access Publisher Index Page"},"url":"https://doi.org/10.7589/0090-3558-6.4.404","text":"Publisher Index Page"},{"id":193841,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United States","state":"Maryland","otherGeospatial":"Chesapeake Bay","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"coordinates\": [\n          [\n            [\n              -76.5915145620614,\n              39.63448158918419\n            ],\n            [\n              -76.5915145620614,\n              38.20939089287066\n            ],\n            [\n              -75.81938065029263,\n              38.20939089287066\n            ],\n            [\n              -75.81938065029263,\n              39.63448158918419\n            ],\n            [\n              -76.5915145620614,\n              39.63448158918419\n            ]\n          ]\n        ],\n        \"type\": \"Polygon\"\n      }\n    }\n  ]\n}","volume":"6","issue":"4","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e48c1e4b07f02db53c4f9","contributors":{"authors":[{"text":"Locke, L. N.","contributorId":73539,"corporation":false,"usgs":true,"family":"Locke","given":"L.","email":"","middleInitial":"N.","affiliations":[],"preferred":false,"id":331866,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Stotts, V.","contributorId":68841,"corporation":false,"usgs":true,"family":"Stotts","given":"V.","email":"","affiliations":[],"preferred":false,"id":331865,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Wolfhard, G.","contributorId":57969,"corporation":false,"usgs":true,"family":"Wolfhard","given":"G.","email":"","affiliations":[],"preferred":false,"id":331864,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":70139928,"text":"70139928 - 1970 - Saline ground-water resources of the Tularosa Basin, New Mexico","interactions":[],"lastModifiedDate":"2016-02-03T10:09:14","indexId":"70139928","displayToPublicDate":"1970-07-01T00:00:00","publicationYear":"1970","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":1,"text":"Federal Government Series"},"seriesTitle":{"id":3864,"text":"Research and Development Progress Report","active":true,"publicationSubtype":{"id":10}},"seriesNumber":"561","title":"Saline ground-water resources of the Tularosa Basin, New Mexico","docAbstract":"<p>This report describes the location, extent, and quality of saline ground water in the Tularosa Basin, a north-trending elongated, intermontane, desert basin in&nbsp; south-central New Mexico. There are no through-flowing streams; runoff from the bordering mountains flows to ephemeral lakes in the center of the basin.</p>\n<p>Fresh-water supplies in the Tularosa Basin are limited; however, large volumes of saline ground-water underlie most of the basin.</p>\n<p>Consolidated rocks ranging from Precambrian through Cretaceous in age form \"bedrock\" aquifers in the basin. Where these rocks are exposed in the mountains bordering the basin, and in the north part of the basin, they may yield up to 150 gallons per minute, although yields are usually less than 20 gpm. Water at shallow depths in these rocks usually contain 1-3 g/l. Water quality deteriorates with depth, and more than 35 g/l water is present in some rock units. Few wells have penetrated these rocks beneath the alluvial deposits in the central part of the basin, where well yields and water quality are generally unknown.</p>\n<p>The most widely developed aquifer in the basin is the alluvial fill of Tertiary to Holocene age which exceeds 6,000 feet in thickness in the southern part of the basin. Well yields of as much as 1,400 gallons per minute have been measured. Fresh water lenses occur in the alluvial fill adjacent to the mountains on the east and west sides of the southern part of the basin. The water below the fresh-water lenses in the alluvial fill increases in salinity with depth. Salinity also increases toward the center of the basin.</p>\n<p>The altitude of isosaline surfaces and thickness of the saline-water zones are shown on maps of the entire basin and of the following detailed areas within the basin: Alamogordo, Tularosa, Carrizozo, and the western margin of the basin.</p>","language":"English","publisher":"U.S. Government Printing Office","publisherLocation":"Washington, D.C.","usgsCitation":"McLean, J.S., 1970, Saline ground-water resources of the Tularosa Basin, New Mexico: Research and Development Progress Report 561, ix, 128 p.","productDescription":"ix, 128 p.","numberOfPages":"162","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[],"links":[{"id":298745,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/70139928.jpg"},{"id":316473,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/unnumbered/70139928/report.pdf","text":"Report","linkFileType":{"id":1,"text":"pdf"}}],"country":"United States","state":"New Mexico","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -106.787109375,\n              32.00341778396365\n            ],\n            [\n              -106.787109375,\n              34.14363482031264\n            ],\n            [\n              -106.19384765625,\n              34.14363482031264\n            ],\n            [\n              -106.19384765625,\n              32.00341778396365\n            ],\n            [\n              -106.787109375,\n              32.00341778396365\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"550bf335e4b02e76d759cdfa","contributors":{"authors":[{"text":"McLean, J. S.","contributorId":116657,"corporation":false,"usgs":true,"family":"McLean","given":"J.","email":"","middleInitial":"S.","affiliations":[],"preferred":false,"id":539697,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":70010284,"text":"70010284 - 1970 - California earthquakes: Why only shallow focus?","interactions":[],"lastModifiedDate":"2026-01-30T17:13:02.375255","indexId":"70010284","displayToPublicDate":"1970-06-26T00:00:00","publicationYear":"1970","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":3338,"text":"Science","active":true,"publicationSubtype":{"id":10}},"title":"California earthquakes: Why only shallow focus?","docAbstract":"<p><span>Frictional sliding on sawcuts and faults in laboratory samples of granite and gabbro is markedly temperature-dependent. At pressures from 1 to 5 kilobars, stick-slip gave way to stable sliding as temperature was increased from 200 to 500 degrees Celsius. Increased temperature with depth could thus cause the abrupt disappearance of earthquakes noted at shallow depths in California.</span></p>","language":"English","publisher":"American Association for the Advancement of Science","doi":"10.1126/science.168.3939.1573","issn":"00368075","usgsCitation":"Brace, W., and Byerlee, J., 1970, California earthquakes: Why only shallow focus?: Science, v. 168, no. 3939, p. 1573-1575, https://doi.org/10.1126/science.168.3939.1573.","productDescription":"3 p.","startPage":"1573","endPage":"1575","costCenters":[],"links":[{"id":219064,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United 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,{"id":70010222,"text":"70010222 - 1970 - Geological history of the western North Pacific","interactions":[],"lastModifiedDate":"2026-01-30T17:41:16.841041","indexId":"70010222","displayToPublicDate":"1970-06-26T00:00:00","publicationYear":"1970","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":3338,"text":"Science","active":true,"publicationSubtype":{"id":10}},"title":"Geological history of the western North Pacific","docAbstract":"A considerable portion of the abyssal floor of the western North Pacific was already receiving pelagic sediment in late Jurassic time. Carbonate sediments were later replaced by abyssal clays as the basin deepened and bottom waters became more aggressive. The resulting facies boundary, which can be recognized on seismic profiles, is broadly transgressive; it ranges in age from mid-Cretaceous in the western Pacific to Oligocene in the central Pacific. Cherts are encountered at and below the major facies boundary and appear to have been formed by postdepositional processes.","language":"English","publisher":"American Association for the Advancement of Science","doi":"10.1126/science.168.3936.1210","issn":"00368075","usgsCitation":"Fischer, A., Heezen, B., Boyce, R., Bukry, D., Douglas, R., Garrison, R., Kling, S., Krasheninnikov, V., Lisitzin, A., and Pimm, A., 1970, Geological history of the western North Pacific: Science, v. 168, no. 3936, p. 1210-1214, https://doi.org/10.1126/science.168.3936.1210.","productDescription":"5 p.","startPage":"1210","endPage":"1214","costCenters":[],"links":[{"id":219221,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"168","issue":"3936","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"505a2266e4b0c8380cd56ff8","contributors":{"authors":[{"text":"Fischer, A.G.","contributorId":103001,"corporation":false,"usgs":true,"family":"Fischer","given":"A.G.","email":"","affiliations":[],"preferred":false,"id":358355,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Heezen, B.C.","contributorId":6536,"corporation":false,"usgs":true,"family":"Heezen","given":"B.C.","affiliations":[],"preferred":false,"id":358346,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Boyce, R.E.","contributorId":8987,"corporation":false,"usgs":true,"family":"Boyce","given":"R.E.","email":"","affiliations":[],"preferred":false,"id":358347,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Bukry, D.","contributorId":15338,"corporation":false,"usgs":true,"family":"Bukry","given":"D.","affiliations":[],"preferred":false,"id":358350,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"Douglas, R.G.","contributorId":11326,"corporation":false,"usgs":true,"family":"Douglas","given":"R.G.","email":"","affiliations":[],"preferred":false,"id":358348,"contributorType":{"id":1,"text":"Authors"},"rank":5},{"text":"Garrison, R.E.","contributorId":100117,"corporation":false,"usgs":true,"family":"Garrison","given":"R.E.","email":"","affiliations":[],"preferred":false,"id":358354,"contributorType":{"id":1,"text":"Authors"},"rank":6},{"text":"Kling, S.A.","contributorId":64796,"corporation":false,"usgs":true,"family":"Kling","given":"S.A.","email":"","affiliations":[],"preferred":false,"id":358352,"contributorType":{"id":1,"text":"Authors"},"rank":7},{"text":"Krasheninnikov, V.","contributorId":78083,"corporation":false,"usgs":true,"family":"Krasheninnikov","given":"V.","email":"","affiliations":[],"preferred":false,"id":358353,"contributorType":{"id":1,"text":"Authors"},"rank":8},{"text":"Lisitzin, A.P.","contributorId":14105,"corporation":false,"usgs":true,"family":"Lisitzin","given":"A.P.","email":"","affiliations":[],"preferred":false,"id":358349,"contributorType":{"id":1,"text":"Authors"},"rank":9},{"text":"Pimm, A.C.","contributorId":37887,"corporation":false,"usgs":true,"family":"Pimm","given":"A.C.","email":"","affiliations":[],"preferred":false,"id":358351,"contributorType":{"id":1,"text":"Authors"},"rank":10}]}}
,{"id":5221248,"text":"5221248 - 1970 - Residues of O,P'-DDD and O,P'-DDT in brown pelican eggs and mallard ducks","interactions":[],"lastModifiedDate":"2020-09-01T19:12:15.327318","indexId":"5221248","displayToPublicDate":"1970-06-16T12:18:01","publicationYear":"1970","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1103,"text":"Bulletin of Environmental Contamination and Toxicology","active":true,"publicationSubtype":{"id":10}},"title":"Residues of O,P'-DDD and O,P'-DDT in brown pelican eggs and mallard ducks","docAbstract":"<p>No abstract available.</p>","language":"English","doi":"10.1007/BF01558317","usgsCitation":"Lamont, T.G., Bagley, G.E., and Reichel, W.L., 1970, Residues of O,P'-DDD and O,P'-DDT in brown pelican eggs and mallard ducks: Bulletin of Environmental Contamination and Toxicology, v. 5, no. 3, p. 231-236, https://doi.org/10.1007/BF01558317.","productDescription":"6 p.","startPage":"231","endPage":"236","numberOfPages":"6","costCenters":[{"id":531,"text":"Patuxent Wildlife Research Center","active":true,"usgs":true}],"links":[{"id":197184,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"5","issue":"3","noUsgsAuthors":false,"publicationDate":"2013-08-24","publicationStatus":"PW","scienceBaseUri":"4f4e4a52e4b07f02db62a580","contributors":{"authors":[{"text":"Lamont, T. G.","contributorId":51252,"corporation":false,"usgs":true,"family":"Lamont","given":"T.","email":"","middleInitial":"G.","affiliations":[],"preferred":false,"id":333398,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Bagley, George E.","contributorId":46589,"corporation":false,"usgs":true,"family":"Bagley","given":"George","email":"","middleInitial":"E.","affiliations":[],"preferred":false,"id":333396,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Reichel, W. L.","contributorId":50482,"corporation":false,"usgs":true,"family":"Reichel","given":"W.","email":"","middleInitial":"L.","affiliations":[],"preferred":false,"id":333397,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":5221254,"text":"5221254 - 1970 - Identification of polychlorinated biphenyls in two bald eagles by combined gas-liquid chromatography-mass spectrometry","interactions":[],"lastModifiedDate":"2021-10-11T17:26:07.664045","indexId":"5221254","displayToPublicDate":"1970-06-16T12:18:00","publicationYear":"1970","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":2533,"text":"Journal of the Association of Official Analytical Chemists","active":true,"publicationSubtype":{"id":10}},"title":"Identification of polychlorinated biphenyls in two bald eagles by combined gas-liquid chromatography-mass spectrometry","docAbstract":"<p>Polychlorinated biphenyls are widely used industrial compounds marketed in the United States under the trade name Aroclor. They have appeared in fish and wildlife tissues in this country and Europe. They are known to be toxic, but more importantly, their presence in samples along with the commonly occurring organochlorine pesticides complicates the analysis to a serious degree, making identification of pesticide residues by GLC without preliminary separation extremely unreliable. Residues of both polychlorinated biphenyls and organochloride pesticides were present in eagle carcasses. Many of the polychlorinated biphenyl components had retention times identical with those of certain organochlorine pesticide residues. Identification was accomplished by preliminary separations on thin layer plates followed by combined GLC- mass spectromtry.</p>","language":"English","publisher":"Oxford University Press","doi":"10.1093/jaoac/53.2.251","usgsCitation":"Bagley, G.E., Reichel, W.L., and Cromartie, E., 1970, Identification of polychlorinated biphenyls in two bald eagles by combined gas-liquid chromatography-mass spectrometry: Journal of the Association of Official Analytical Chemists, v. 53, no. 2, p. 251-261, https://doi.org/10.1093/jaoac/53.2.251.","productDescription":"11 p.","startPage":"251","endPage":"261","costCenters":[{"id":531,"text":"Patuxent Wildlife Research Center","active":true,"usgs":true}],"links":[{"id":197356,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"53","issue":"2","noUsgsAuthors":false,"publicationDate":"2020-01-29","publicationStatus":"PW","scienceBaseUri":"4f4e4ac9e4b07f02db67c7b5","contributors":{"authors":[{"text":"Bagley, George E.","contributorId":46589,"corporation":false,"usgs":true,"family":"Bagley","given":"George","email":"","middleInitial":"E.","affiliations":[],"preferred":false,"id":333411,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Reichel, W. L.","contributorId":50482,"corporation":false,"usgs":true,"family":"Reichel","given":"W.","email":"","middleInitial":"L.","affiliations":[],"preferred":false,"id":333412,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Cromartie, E.","contributorId":13926,"corporation":false,"usgs":true,"family":"Cromartie","given":"E.","email":"","affiliations":[],"preferred":false,"id":333410,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
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