{"pageNumber":"6028","pageRowStart":"150675","pageSize":"25","recordCount":184569,"records":[{"id":1014544,"text":"1014544 - 1976 - Rapid diagnostic approaches in the identification of gram-negative bacterial diseases of fish","interactions":[],"lastModifiedDate":"2023-10-27T16:47:56.118351","indexId":"1014544","displayToPublicDate":"1976-03-30T00:00:00","publicationYear":"1976","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1650,"text":"Fish Pathology","active":true,"publicationSubtype":{"id":10}},"title":"Rapid diagnostic approaches in the identification of gram-negative bacterial diseases of fish","docAbstract":"<p>No abstract available.</p>","language":"English","publisher":"Japanese Society of Fish Pathology","doi":"10.3147/jsfp.10.187","usgsCitation":"Shotts, E.B., and Bullock, G.L., 1976, Rapid diagnostic approaches in the identification of gram-negative bacterial diseases of fish: Fish Pathology, v. 10, no. 2, p. 187-190, https://doi.org/10.3147/jsfp.10.187.","productDescription":"4 p.","startPage":"187","endPage":"190","numberOfPages":"4","costCenters":[{"id":365,"text":"Leetown Science Center","active":true,"usgs":true}],"links":[{"id":480620,"rank":2,"type":{"id":40,"text":"Open Access Publisher Index Page"},"url":"https://doi.org/10.3147/jsfp.10.187","text":"Publisher Index Page"},{"id":130881,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"10","issue":"2","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a80e4b07f02db649406","contributors":{"authors":[{"text":"Shotts, E. B. Jr.","contributorId":102414,"corporation":false,"usgs":false,"family":"Shotts","given":"E.","suffix":"Jr.","email":"","middleInitial":"B.","affiliations":[],"preferred":false,"id":320569,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Bullock, G. L.","contributorId":69498,"corporation":false,"usgs":true,"family":"Bullock","given":"G.","email":"","middleInitial":"L.","affiliations":[],"preferred":false,"id":320568,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":70010885,"text":"70010885 - 1976 - An experiment in earthquake control at Rangely, Colorado","interactions":[],"lastModifiedDate":"2026-01-21T16:29:05.404293","indexId":"70010885","displayToPublicDate":"1976-03-26T00:00:00","publicationYear":"1976","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":3338,"text":"Science","active":true,"publicationSubtype":{"id":10}},"title":"An experiment in earthquake control at Rangely, Colorado","docAbstract":"<p><span>An experiment in an oil field at Rangely, Colorado, has demonstrated the feasibility of earthquake control. Variations in seismicity were produced by controlled variations in the fluid pressure in a seismically active zone. Precise earthquake locations revealed that the earthquakes clustered about a fault trending through a zone of high pore pressure produced by secondary recovery operations. Laboratory measurements of the frictional properties of the reservoir rocks and an in situ stress measurement made near the earthquake zone were used to predict the fluid pressure required to trigger earthquakes on preexisting fractures. Fluid pressure was controlled by alternately injecting and recovering water from wells that penetrated the seismic zone. Fluid pressure was monitored in observation wells, and a computer model of the reservoir was used to infer the fluid pressure distributions in the vicinity of the injection wells. The results of this experiment confirm the predicted effect of fluid pressure on earthquake activity and indicate that earthquakes can be controlled wherever we can control the fluid pressure in a fault zone.</span></p>","language":"English","publisher":"American Association for the Advancement of Science","doi":"10.1126/science.191.4233.1230","issn":"00368075","usgsCitation":"Raleigh, C., Healy, J.H., and Bredehoeft, J., 1976, An experiment in earthquake control at Rangely, Colorado: Science, v. 191, no. 4233, p. 1230-1237, https://doi.org/10.1126/science.191.4233.1230.","productDescription":"8 p.","startPage":"1230","endPage":"1237","costCenters":[],"links":[{"id":221078,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United States","state":"Colorado","city":"Rangely","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"coordinates\": [\n          [\n            [\n              -108.84277087243589,\n              40.11930068802104\n            ],\n            [\n              -108.84277087243589,\n              40.06951510909437\n            ],\n            [\n              -108.75431520044876,\n              40.06951510909437\n            ],\n            [\n              -108.75431520044876,\n              40.11930068802104\n            ],\n            [\n              -108.84277087243589,\n              40.11930068802104\n            ]\n          ]\n        ],\n        \"type\": \"Polygon\"\n      }\n    }\n  ]\n}","volume":"191","issue":"4233","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"5059ea61e4b0c8380cd48815","contributors":{"authors":[{"text":"Raleigh, C.B.","contributorId":40219,"corporation":false,"usgs":true,"family":"Raleigh","given":"C.B.","email":"","affiliations":[],"preferred":false,"id":359840,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Healy, J. H.","contributorId":48968,"corporation":false,"usgs":true,"family":"Healy","given":"J.","email":"","middleInitial":"H.","affiliations":[],"preferred":false,"id":359841,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Bredehoeft, J.D.","contributorId":12836,"corporation":false,"usgs":true,"family":"Bredehoeft","given":"J.D.","affiliations":[],"preferred":false,"id":359839,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":70232242,"text":"70232242 - 1976 - Amino acids and gases in some springs and an oil field in California","interactions":[],"lastModifiedDate":"2022-06-16T16:59:58.86099","indexId":"70232242","displayToPublicDate":"1976-03-01T11:53:41","publicationYear":"1976","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":2446,"text":"Journal of Research of the U.S. Geological Survey","active":true,"publicationSubtype":{"id":10}},"title":"Amino acids and gases in some springs and an oil field in California","docAbstract":"<p>Samples of water and gas were collected from six springs and two wells in the Upper Cretaceous Great Valley sequence and Franciscan Formation underlying the Coast Range of northern California and from four oil wells penetrating Tertiary sedimentary rocks in the Kettleman North Dome oil field. Comparison of the dissolved free amino acid compositions of the waters from the two locations show overlapping ranges with many more similarities than differences. The detection of nonprotein amino acids (sarcosine, <i>β</i>-amino <i>n</i>-butyric acid, and others) indicates the protein degradation is partly chemical rather than strictly biological. Other low molecular weight degradation products (methane, ethane, nonvolatile organic acids, and other organic chelating agents) were found. This may be one mechanism for the transportation of organic matter from the source rocks to the reservoir rocks of an oil deposit.</p>","language":"English","publisher":"U.S. Geological Survey","usgsCitation":"Rapp, J., 1976, Amino acids and gases in some springs and an oil field in California: Journal of Research of the U.S. Geological Survey, v. 4, no. 2, p. 227-232.","productDescription":"6 p.","startPage":"227","endPage":"232","costCenters":[],"links":[{"id":402282,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"},{"id":402281,"rank":1,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/journal/1976/vol4issue2/report.pdf"}],"country":"United States","state":"California","otherGeospatial":"Coast Range, Kettleman North Dome","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -124.3212890625,\n              38.28993659801203\n            ],\n            [\n              -121.937255859375,\n              38.28993659801203\n            ],\n            [\n              -121.937255859375,\n              42.02481360781777\n            ],\n            [\n              -124.3212890625,\n              42.02481360781777\n            ],\n            [\n              -124.3212890625,\n              38.28993659801203\n            ]\n          ]\n        ]\n      }\n    },\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -119.79766845703125,\n              35.75765724051559\n            ],\n            [\n              -120.05035400390625,\n              36.055760619006755\n            ],\n            [\n              -120.30029296875,\n              36.292990818063394\n            ],\n            [\n              -120.45135498046875,\n              36.18665862660454\n            ],\n            [\n              -120.03662109374999,\n              35.74428307651204\n            ],\n            [\n              -119.93225097656251,\n              35.67737855391475\n            ],\n            [\n              -119.79766845703125,\n              35.75765724051559\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","volume":"4","issue":"2","noUsgsAuthors":false,"publicationStatus":"PW","contributors":{"authors":[{"text":"Rapp, John B.","contributorId":32028,"corporation":false,"usgs":true,"family":"Rapp","given":"John B.","affiliations":[],"preferred":false,"id":844772,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":70232241,"text":"70232241 - 1976 - Reassessment of mercury in surface water in the Adirondack region, New York","interactions":[],"lastModifiedDate":"2022-06-16T16:52:08.902277","indexId":"70232241","displayToPublicDate":"1976-03-01T11:48:04","publicationYear":"1976","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":2446,"text":"Journal of Research of the U.S. Geological Survey","active":true,"publicationSubtype":{"id":10}},"title":"Reassessment of mercury in surface water in the Adirondack region, New York","docAbstract":"<p>A study in 1970 established a natural background concentration of mercury in surface water in the Adirondack region of New York. In 1974, new methods of sample preservation and analysis were used in determining concentrations of mercury of samples of water from the same surface-water sites sampled in 1970-71. Concentrations of mercury for all sites in the 1974 study were virtually the same as those obtained in 1970-71, less than 0.5 microgram per litre, which is the detection limit of the methods.</p>","language":"English","publisher":"U.S. Geological Survey","usgsCitation":"Buller, W., 1976, Reassessment of mercury in surface water in the Adirondack region, New York: Journal of Research of the U.S. Geological Survey, v. 4, no. 2, p. 223-226.","productDescription":"4 p.","startPage":"223","endPage":"226","costCenters":[],"links":[{"id":402280,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"},{"id":402279,"rank":1,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/journal/1976/vol4issue2/report.pdf"}],"country":"United States","state":"New York","otherGeospatial":"Adirondack region","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -74.190673828125,\n              43.02071359427862\n            ],\n            [\n              -73.3447265625,\n              43.55651037504758\n            ],\n            [\n              -73.377685546875,\n              44.39454219215587\n            ],\n            [\n              -73.67431640625,\n              44.87144275016589\n            ],\n            [\n              -74.739990234375,\n              44.809121700077355\n            ],\n            [\n              -75.498046875,\n              44.22158376545796\n            ],\n            [\n              -75.38818359375,\n              43.48481212891603\n            ],\n            [\n              -74.68505859374999,\n              43.1090040242731\n            ],\n            [\n              -74.190673828125,\n              43.02071359427862\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","volume":"4","issue":"2","noUsgsAuthors":false,"publicationStatus":"PW","contributors":{"authors":[{"text":"Buller, William","contributorId":16449,"corporation":false,"usgs":true,"family":"Buller","given":"William","email":"","affiliations":[],"preferred":false,"id":844771,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":70232240,"text":"70232240 - 1976 - Interstation correlation of peak-flow estimates","interactions":[],"lastModifiedDate":"2022-06-16T16:47:26.789131","indexId":"70232240","displayToPublicDate":"1976-03-01T11:44:53","publicationYear":"1976","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":2446,"text":"Journal of Research of the U.S. Geological Survey","active":true,"publicationSubtype":{"id":10}},"title":"Interstation correlation of peak-flow estimates","docAbstract":"<p>Equations are given for using the correlation coefficient between annual peaks at a pair of stream gaging stations to estimate the interstation correlation coefficient of estimated <i>T</i>-year peaks, computed standard deviations, and computed skew coefficients at the same pair of stations. The equations are based on statistics computed from samples of annual peaks simulated from normal distributions with built-in interstation correlation. The interstation correlation of 50- year peaks was found to be about equal to the square of the interstation correlation coefficient of the annual peaks.</p>","language":"English","publisher":"U.S. Geological Survey","usgsCitation":"Hardison, C.H., 1976, Interstation correlation of peak-flow estimates: Journal of Research of the U.S. Geological Survey, v. 4, no. 2, p. 221-222.","productDescription":"2 p.","startPage":"221","endPage":"222","costCenters":[],"links":[{"id":402278,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"},{"id":402277,"rank":1,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/journal/1976/vol4issue2/report.pdf"}],"volume":"4","issue":"2","noUsgsAuthors":false,"publicationStatus":"PW","contributors":{"authors":[{"text":"Hardison, Clayton H.","contributorId":46073,"corporation":false,"usgs":true,"family":"Hardison","given":"Clayton","email":"","middleInitial":"H.","affiliations":[],"preferred":false,"id":844770,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":70232239,"text":"70232239 - 1976 - Flameless atomic absorption determination of bismuth in soils and rocks","interactions":[],"lastModifiedDate":"2022-06-16T16:42:29.396165","indexId":"70232239","displayToPublicDate":"1976-03-01T11:40:18","publicationYear":"1976","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":2446,"text":"Journal of Research of the U.S. Geological Survey","active":true,"publicationSubtype":{"id":10}},"title":"Flameless atomic absorption determination of bismuth in soils and rocks","docAbstract":"<p>Recent advances in flameless atomic absorption allow determinations of bismuth in concentrations as small as 50 ppb in 0.2 g of rock or soil sample. The sample is fused with sodium bisulfate and the fusion product is leached with hot 2 <i>M</i> hydrochloric acid and treated with ammonium citrate, (ethylenedinitrilo) tetraacetic acid disodium salt, and finally with ammonium 1-pyrrolidinedithiocarbamate to form a complex which is extracted into methyl isobutyl ketone. Aliquots of the latter are pipetted into a graphite furnace and then subjected to an established and automated program of drying, charring, and atomizing. Recorded peak heights provide a measure of the amount of bismuth present.</p>","language":"English","publisher":"U.S. Geological Survey","usgsCitation":"Ficklin, W.H., and Ward, F.N., 1976, Flameless atomic absorption determination of bismuth in soils and rocks: Journal of Research of the U.S. Geological Survey, v. 4, no. 2, p. 217-220.","productDescription":"4 p.","startPage":"217","endPage":"220","costCenters":[],"links":[{"id":402276,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"},{"id":402275,"rank":1,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/journal/1976/vol4issue2/report.pdf"}],"volume":"4","issue":"2","noUsgsAuthors":false,"publicationStatus":"PW","contributors":{"authors":[{"text":"Ficklin, W. H.","contributorId":89517,"corporation":false,"usgs":true,"family":"Ficklin","given":"W.","email":"","middleInitial":"H.","affiliations":[],"preferred":false,"id":844768,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Ward, F. N.","contributorId":96254,"corporation":false,"usgs":true,"family":"Ward","given":"F.","email":"","middleInitial":"N.","affiliations":[],"preferred":false,"id":844769,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":70232238,"text":"70232238 - 1976 - A review of the minerals of the alunite-jarosite, beudantite, and plumbogummite groups","interactions":[],"lastModifiedDate":"2022-06-16T17:01:02.228323","indexId":"70232238","displayToPublicDate":"1976-03-01T11:31:22","publicationYear":"1976","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":2446,"text":"Journal of Research of the U.S. Geological Survey","active":true,"publicationSubtype":{"id":10}},"title":"A review of the minerals of the alunite-jarosite, beudantite, and plumbogummite groups","docAbstract":"<p>Minerals of the alunite-jarosite, beudantlte, and plumbogummite groups can be divided on the basis of iron or aluminum content into two groups which are consistent in optical and X-ray characteristics. Both chemical and X-ray data are needed for identification.</p>","language":"English","publisher":"U.S. Geological Survey","usgsCitation":"Botinelly, T., 1976, A review of the minerals of the alunite-jarosite, beudantite, and plumbogummite groups: Journal of Research of the U.S. Geological Survey, v. 4, no. 2, p. 213-216.","productDescription":"4 p.","startPage":"213","endPage":"216","costCenters":[],"links":[{"id":402274,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"},{"id":402273,"rank":1,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/journal/1976/vol4issue2/report.pdf"}],"volume":"4","issue":"2","noUsgsAuthors":false,"publicationStatus":"PW","contributors":{"authors":[{"text":"Botinelly, Theodore","contributorId":101253,"corporation":false,"usgs":true,"family":"Botinelly","given":"Theodore","email":"","affiliations":[],"preferred":false,"id":844767,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":70232237,"text":"70232237 - 1976 - Definitive X-ray powder data for covellite, anilite, djurleite, and chalcocite","interactions":[],"lastModifiedDate":"2022-06-16T17:01:35.545243","indexId":"70232237","displayToPublicDate":"1976-03-01T11:19:20","publicationYear":"1976","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":2446,"text":"Journal of Research of the U.S. Geological Survey","active":true,"publicationSubtype":{"id":10}},"title":"Definitive X-ray powder data for covellite, anilite, djurleite, and chalcocite","docAbstract":"<p>By using the Guinier-Hägg focusing X-ray powder camera with Cr<i>Kα<sub>1</sub></i> and Cu<i>Kα<sub>1</sub></i> radiations, new powder data for covellite (CuS), anilite (Cu<sub>7</sub>S<sub>4</sub>, djurleite (Cu<sub>1.934</sub>S), and low chalcocite (Cu<sub>2</sub>S) have been obtained from synthetic and natural materials. The powder data were treated by least-squares analysis to obtain the best unit-cell parameters consistent with the data. These powder data are intended to replace inferior and incomplete data previously published and to serve as standards for the study of copper sulflde minerals.</p>","language":"English","publisher":"U.S. Geological Survey","usgsCitation":"Potter, R.W., and Evans, H.T., 1976, Definitive X-ray powder data for covellite, anilite, djurleite, and chalcocite: Journal of Research of the U.S. Geological Survey, v. 4, no. 2, p. 205-212.","productDescription":"8 p.","startPage":"205","endPage":"212","costCenters":[],"links":[{"id":402272,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"},{"id":402271,"rank":1,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/journal/1976/vol4issue2/report.pdf"}],"volume":"4","issue":"2","noUsgsAuthors":false,"publicationStatus":"PW","contributors":{"authors":[{"text":"Potter, Robert W. II","contributorId":67899,"corporation":false,"usgs":true,"family":"Potter","given":"Robert","suffix":"II","email":"","middleInitial":"W.","affiliations":[],"preferred":false,"id":844765,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Evans, Howard T. Jr.","contributorId":70852,"corporation":false,"usgs":true,"family":"Evans","given":"Howard","suffix":"Jr.","email":"","middleInitial":"T.","affiliations":[],"preferred":false,"id":844766,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":70232226,"text":"70232226 - 1976 - The volumetric properties of H2O — A graphical portrayal","interactions":[],"lastModifiedDate":"2022-06-16T13:27:21.573313","indexId":"70232226","displayToPublicDate":"1976-03-01T11:15:53","publicationYear":"1976","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":2446,"text":"Journal of Research of the U.S. Geological Survey","active":true,"publicationSubtype":{"id":10}},"displayTitle":"The volumetric properties of H<sub>2</sub>O — A graphical portrayal","title":"The volumetric properties of H2O — A graphical portrayal","docAbstract":"<p>A graphical display of the volumetric properties of H<sub>2</sub>O is presented as density (0.01 to 1.0 g-cm<sup>-3</sup>) contoured on pressure-temperature coordinates and pressure (1-10,000 bars) contoured on density-temperature coordinates over the temperature range 0-1,000 °C. Data were obtained from sources published during 1964-1969; several minor inconsistencies are observed and attributed to inadequacies in the equations of state used to describe experimental data obtained above 1,000 bars.</p>","language":"English","publisher":"U.S. Geological Survey","usgsCitation":"Fisher, J.R., 1976, The volumetric properties of H2O — A graphical portrayal: Journal of Research of the U.S. Geological Survey, v. 4, no. 2, p. 189-193.","productDescription":"5 p.","startPage":"189","endPage":"193","costCenters":[],"links":[{"id":402214,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"},{"id":402259,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/journal/1976/vol4issue2/report.pdf"}],"volume":"4","issue":"2","noUsgsAuthors":false,"publicationStatus":"PW","contributors":{"authors":[{"text":"Fisher, James R.","contributorId":33583,"corporation":false,"usgs":true,"family":"Fisher","given":"James","email":"","middleInitial":"R.","affiliations":[],"preferred":false,"id":844718,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":70232225,"text":"70232225 - 1976 - Geology of the massifs at the Apollo 17 landing site","interactions":[],"lastModifiedDate":"2022-06-16T13:27:00.195772","indexId":"70232225","displayToPublicDate":"1976-03-01T11:10:09","publicationYear":"1976","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":2446,"text":"Journal of Research of the U.S. Geological Survey","active":true,"publicationSubtype":{"id":10}},"title":"Geology of the massifs at the Apollo 17 landing site","docAbstract":"<p>The Apollo 17 spacecraft landed in a narrow valley that embays mountainous terrain near the southeastern edge of Mare Serenitatis. Two overlapping basin structures underlie Mare Serenitatis: a larger one to the south and a smaller one to the north. The massifs and sculptured hills in the Taurus-Littrow area and the mountains and knobby terrain in the outer Rook ring (third ring) of the Orientale basin are similar in morphology ; the Apollo 17 site lies approximately on the third ring of the southern Serenitatis basin structure. Assuming the third ring represents the approximate rim of the transient cavity of the southern Serenitatis structure, we suggest that ejecta many kilometres thick was deposited in the Taurus-Littrow area by the southern Serenitatis impact. This ejecta is visible in the massifs in the Apollo 17 landing site as discontinuous, irregular lenses of variable lithology. The southern Serenitatis target rocks were predominantly breccias that were invaded by impact-generated melt and redeposited during the southern Serenitatis event.</p>","language":"English","publisher":"U.S. Geological Survey","usgsCitation":"Wolfe, E.W., and Reed, V.S., 1976, Geology of the massifs at the Apollo 17 landing site: Journal of Research of the U.S. Geological Survey, v. 4, no. 2, p. 171-180.","productDescription":"10 p.","startPage":"171","endPage":"180","costCenters":[],"links":[{"id":402213,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"},{"id":402257,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/journal/1976/vol4issue2/report.pdf"}],"otherGeospatial":"Mare Serenitatis, Moon","volume":"4","issue":"2","noUsgsAuthors":false,"publicationStatus":"PW","contributors":{"authors":[{"text":"Wolfe, Edward W.","contributorId":79878,"corporation":false,"usgs":true,"family":"Wolfe","given":"Edward","email":"","middleInitial":"W.","affiliations":[],"preferred":false,"id":844716,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Reed, V. S.","contributorId":58255,"corporation":false,"usgs":true,"family":"Reed","given":"V.","email":"","middleInitial":"S.","affiliations":[],"preferred":false,"id":844717,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":70232224,"text":"70232224 - 1976 - Bog stratigraphy, radiocarbon dates, and Pinedale to Holocene glacial history in the Front Range, Colorado","interactions":[],"lastModifiedDate":"2022-06-15T16:09:05.601311","indexId":"70232224","displayToPublicDate":"1976-03-01T11:01:35","publicationYear":"1976","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":2446,"text":"Journal of Research of the U.S. Geological Survey","active":true,"publicationSubtype":{"id":10}},"title":"Bog stratigraphy, radiocarbon dates, and Pinedale to Holocene glacial history in the Front Range, Colorado","docAbstract":"<p>Radiocarbon dates and stratigraphic cores from bogs, kettle ponds, and former ice-marginal lakes on the east and west sides of the Front Range, Colo., between lat 40°00' and 40°24' N. suggest that (1) valley glaciers of Pinedale age began to recede from their terminal positions between about 14,600 and 13,000 yr ago, (2) revegetation of glaciated areas at altitudes of 2,600-2,900 m (8,600-9,500 ft) was complete by 11,000-10,000 yr ago, (3) at one site, 3,500±1,000 yr elapsed before peat began to form after deglaciation, (4) the formation of bogs within the glaciated areas kept pace with glacier recession in a general way, beginning at progressively later times as deglaciation proceeded upward, (5) Pinedale glaciers had disappeared or were reduced to small remnants by about 8,000 yr ago, (6) moraines that have been mapped as belonging to the early stade of Pinedale Glaciation are no younger than 13,000 yr B.P. and may be older than 14,600 yr, and those delimiting what has been mapped as late stade are no younger than about 7,600 yr B.P. and are probably older than 7,800 yr, and (7) most of the till mapped as Pinedale was deposited between about 14,600 and 8,000 yr ago.</p>","language":"English","publisher":"U.S. Geological Survey","usgsCitation":"Madole, R.F., 1976, Bog stratigraphy, radiocarbon dates, and Pinedale to Holocene glacial history in the Front Range, Colorado: Journal of Research of the U.S. Geological Survey, v. 4, no. 2, p. 163-169.","productDescription":"7 p.","startPage":"163","endPage":"169","costCenters":[{"id":318,"text":"Geosciences and Environmental Change Science Center","active":true,"usgs":true}],"links":[{"id":402212,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"},{"id":402211,"rank":1,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/journal/1976/vol4issue2/report.pdf"}],"country":"United States","state":"Colorado","otherGeospatial":"Front Range","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -106,\n              40\n            ],\n            [\n              -105,\n              40\n            ],\n            [\n              -105,\n              40.4\n            ],\n            [\n              -106,\n              40.4\n            ],\n            [\n              -106,\n              40\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","volume":"4","issue":"2","noUsgsAuthors":false,"publicationStatus":"PW","contributors":{"authors":[{"text":"Madole, Richard F. 0000-0002-9081-570X madole@usgs.gov","orcid":"https://orcid.org/0000-0002-9081-570X","contributorId":1340,"corporation":false,"usgs":true,"family":"Madole","given":"Richard","email":"madole@usgs.gov","middleInitial":"F.","affiliations":[{"id":318,"text":"Geosciences and Environmental Change Science Center","active":true,"usgs":true}],"preferred":true,"id":844715,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":70232223,"text":"70232223 - 1976 - The Placer River Silt — An intertidal deposit caused by the 1964 Alaska earthquake","interactions":[],"lastModifiedDate":"2022-06-15T16:00:47.803626","indexId":"70232223","displayToPublicDate":"1976-03-01T10:49:38","publicationYear":"1976","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":2446,"text":"Journal of Research of the U.S. Geological Survey","active":true,"publicationSubtype":{"id":10}},"title":"The Placer River Silt — An intertidal deposit caused by the 1964 Alaska earthquake","docAbstract":"<p>At the head of Turnagain Arm near Anchorage, the major lasting geologic consequence of the Alaska earthquake of 1964 was deposition of the Placer River Silt, an intertidal deposit covering an area of more than 18 km<sup>2</sup> and containing more than 20X10<sup>6</sup> m<sup>3</sup> of sediment. This formation, which was derived from erosion of intertidal bars in Turnagain Arm, averages 1.5 m thick seaward of the Seward Highway and 0.9 m thick landward. Its distribution is controlled both, by the arrangement of the major streams that enter tidewater and by manmade features such as the highway and railroad embankments. The Placer River Silt is still being deposited. The contemporary lowland sedimentation system of the Portage area includes a number of depositional settings: (1) In the Placer River Silt upper tidal flats, levees, and channelway fans, (2) elsewhere in the intertidal zone tidal stream channels, lower tidal flats, and saltwater marsh, and (3) in the supratidal zone gravel levees, freshwater marsh, bogs, and lakes. Since 1964, the critical environmental results of the earthquake-caused deposition have been abandonment of the settlement of Portage, formation of an unsightly blanket of silt, destruction of natural plant communities, localized erosion, and creation of quicksand hazards.</p>","language":"English","publisher":"U.S. Geological Survey","usgsCitation":"Ovenshine, A., Lawson, D.E., and Bartsch-Winkler, S., 1976, The Placer River Silt — An intertidal deposit caused by the 1964 Alaska earthquake: Journal of Research of the U.S. Geological Survey, v. 4, no. 2, p. 151-162.","productDescription":"12 p.","startPage":"151","endPage":"162","costCenters":[],"links":[{"id":402210,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"},{"id":402209,"rank":1,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/journal/1976/vol4issue2/report.pdf"}],"country":"United States","state":"Alaska","city":"Portage","otherGeospatial":"Placer River, Turnagain Arm","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -149.36737060546875,\n              60.784640823564395\n            ],\n            [\n              -148.82217407226562,\n              60.784640823564395\n            ],\n            [\n              -148.82217407226562,\n              60.97976989482837\n            ],\n            [\n              -149.36737060546875,\n              60.97976989482837\n            ],\n            [\n              -149.36737060546875,\n              60.784640823564395\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","volume":"4","issue":"2","noUsgsAuthors":false,"publicationStatus":"PW","contributors":{"authors":[{"text":"Ovenshine, A.T.","contributorId":80268,"corporation":false,"usgs":true,"family":"Ovenshine","given":"A.T.","affiliations":[],"preferred":false,"id":844712,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Lawson, Daniel E.","contributorId":292472,"corporation":false,"usgs":false,"family":"Lawson","given":"Daniel","email":"","middleInitial":"E.","affiliations":[],"preferred":false,"id":844713,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Bartsch-Winkler, S. R.","contributorId":167158,"corporation":false,"usgs":false,"family":"Bartsch-Winkler","given":"S. R.","affiliations":[],"preferred":false,"id":844714,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":70232221,"text":"70232221 - 1976 - Cenozoic deposits of southeastern New Mexico and an outline of the history of evaporite dissolution","interactions":[],"lastModifiedDate":"2022-06-15T15:34:50.74069","indexId":"70232221","displayToPublicDate":"1976-03-01T10:25:51","publicationYear":"1976","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":2446,"text":"Journal of Research of the U.S. Geological Survey","active":true,"publicationSubtype":{"id":10}},"title":"Cenozoic deposits of southeastern New Mexico and an outline of the history of evaporite dissolution","docAbstract":"<p>Sedimentary records of Cenozoic history in southeastern New Mexico begin with the Ogallala Formation of Miocene and Pliocene age. Later records include the Gatuna Formation of early or middle Pleistocene age, Mescalero caliche, an informal term, of middle Pleistocene age, and fluvial deposits of late Pleistocene age but there are many gaps in the record. The modern landscape is the result of erosion and deposition in climates that have ranged from semihumid to semiarid as well as dissolution of soluble rocks in Permian formations in the subsurface. This dissolution may have begun as early as Jurassic time and has continued intermittently to the present.</p>","language":"English","publisher":"U.S. Geological Survey","usgsCitation":"Bachman, G.O., 1976, Cenozoic deposits of southeastern New Mexico and an outline of the history of evaporite dissolution: Journal of Research of the U.S. Geological Survey, v. 4, no. 2, p. 135-149.","productDescription":"15 p.","startPage":"135","endPage":"149","costCenters":[],"links":[{"id":402207,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"},{"id":402205,"rank":1,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/journal/1976/vol4issue2/report.pdf"}],"country":"United States","state":"New 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,{"id":70232219,"text":"70232219 - 1976 - Geology of central Costa Rica and its implications in the geologic history of the region","interactions":[],"lastModifiedDate":"2022-06-15T15:32:37.198402","indexId":"70232219","displayToPublicDate":"1976-03-01T10:07:43","publicationYear":"1976","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":2446,"text":"Journal of Research of the U.S. Geological Survey","active":true,"publicationSubtype":{"id":10}},"title":"Geology of central Costa Rica and its implications in the geologic history of the region","docAbstract":"<p>The oldest rocks in Costa Rica, the Nicoya Complex, crop out in an arcuate belt along the Pacific coast and outside the mapped area. The complex is an ophiolite assemblage and indicates that a Late Cretaceous arc-trench system, probably a southerly extension of the Middle America Trench, lay along and west of the present Pacific coast. Polarity of the system is indicated by the presence of a volcanic olivine basalt arc east of the ophiolite belt and by a younger magmatic arc farther east. Relative lack of metamorphism of the ophiolite assemblage suggests that the rocks were obducted rather than subducted. Fossil evidence indicates that the complex was emplaced no later than the late Campanian. By the late Eocene both the ophiolite assemblage and the olivine basalt arc had been established as major sediment sources for basins that lay to the east, and they continued as such through the Oligocene and possibly into the middle Miocene. Widespread deposition of trachyandesite lava and volcaniclastic sediments, local marine planation, uplift, and renewed volcanism mark what is presumed to be the end of the Miocene. Extreme south-to-north coarsening of the unconformably superposed Doan Formation and the presence of corals in the shaly facies of the Doan in the southern part of the mapped areas suggest that marine sedimentation there was undisturbed by orogeny and that intrusion of the Talamancan magmatic rocks must have followed deposition of the Doan. Volcaniclastic block breccia, characteristic of northern exposures of the Doan, indicates that volcanism in the proto- Cordillera Central had begun by at least Doan time. Volcanism has been a dominant process in central Costa Rica since that time.</p>","language":"English","publisher":"U.S. Geological Survey","usgsCitation":"Krushensky, R.D., Malavassi, E.V., and Castillo, R.M., 1976, Geology of central Costa Rica and its implications in the geologic history of the region: Journal of Research of the U.S. Geological Survey, v. 4, no. 2, p. 127-134.","productDescription":"8 p.","startPage":"127","endPage":"134","costCenters":[],"links":[{"id":402203,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"},{"id":402202,"rank":1,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/journal/1976/vol4issue2/report.pdf"}],"country":"Costa Rica","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -83.638916015625,\n              9.112944562617598\n            ],\n            [\n              -82.96875,\n              9.893098633379584\n            ],\n            [\n              -83.51806640624999,\n              10.563422129963456\n            ],\n            [\n              -84.88037109375,\n              10.055402736564236\n            ],\n            [\n              -84.66064453125,\n              9.611582210984674\n            ],\n            [\n              -83.638916015625,\n              9.112944562617598\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","volume":"4","issue":"2","noUsgsAuthors":false,"publicationStatus":"PW","contributors":{"authors":[{"text":"Krushensky, Richard D.","contributorId":106994,"corporation":false,"usgs":true,"family":"Krushensky","given":"Richard","email":"","middleInitial":"D.","affiliations":[],"preferred":false,"id":844705,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Malavassi, Enrique V.","contributorId":18853,"corporation":false,"usgs":true,"family":"Malavassi","given":"Enrique","email":"","middleInitial":"V.","affiliations":[],"preferred":false,"id":844706,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Castillo, Rolando M.","contributorId":27143,"corporation":false,"usgs":true,"family":"Castillo","given":"Rolando","email":"","middleInitial":"M.","affiliations":[],"preferred":false,"id":844707,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":70232253,"text":"70232253 - 1976 - Determination, storage, and preservation of low molecular weight hydrocarbon gases in aqueous solution","interactions":[],"lastModifiedDate":"2022-06-17T15:13:32.773557","indexId":"70232253","displayToPublicDate":"1976-03-01T10:00:02","publicationYear":"1976","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":2446,"text":"Journal of Research of the U.S. Geological Survey","active":true,"publicationSubtype":{"id":10}},"title":"Determination, storage, and preservation of low molecular weight hydrocarbon gases in aqueous solution","docAbstract":"<p>A gas chromatograph with a flame ionization detector was used in conjunction with a stripping chamber and cold trap apparatus to measure microgram-per-litre quantities of low molecular weight hydrocarbon gases in water samples. Glass bottles with ground-glass stoppers were used to store the samples. Formalin was added to stop bacterial activity and preserve samples with no measurable losses for as much as 7 days. </p>","language":"English","publisher":"U.S. Geological Survey","usgsCitation":"Schultz, D.J., Pankow, J.F., Tai, D.Y., Stephens, D.W., and Rathbun, R.E., 1976, Determination, storage, and preservation of low molecular weight hydrocarbon gases in aqueous solution: Journal of Research of the U.S. Geological Survey, v. 4, no. 2, p. 247-251.","productDescription":"5 p.","startPage":"247","endPage":"251","costCenters":[],"links":[{"id":402334,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"},{"id":402333,"rank":1,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/journal/1976/vol4issue2/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"volume":"4","issue":"2","noUsgsAuthors":false,"publicationStatus":"PW","contributors":{"authors":[{"text":"Schultz, D. J.","contributorId":292492,"corporation":false,"usgs":false,"family":"Schultz","given":"D.","email":"","middleInitial":"J.","affiliations":[],"preferred":false,"id":844811,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Pankow, J. F.","contributorId":20917,"corporation":false,"usgs":true,"family":"Pankow","given":"J.","email":"","middleInitial":"F.","affiliations":[],"preferred":false,"id":844812,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Tai, D. Y.","contributorId":59778,"corporation":false,"usgs":true,"family":"Tai","given":"D.","email":"","middleInitial":"Y.","affiliations":[],"preferred":false,"id":844813,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Stephens, D. W.","contributorId":68335,"corporation":false,"usgs":true,"family":"Stephens","given":"D.","email":"","middleInitial":"W.","affiliations":[],"preferred":false,"id":844814,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"Rathbun, R. E.","contributorId":61796,"corporation":false,"usgs":true,"family":"Rathbun","given":"R.","email":"","middleInitial":"E.","affiliations":[],"preferred":false,"id":844815,"contributorType":{"id":1,"text":"Authors"},"rank":5}]}}
,{"id":70232250,"text":"70232250 - 1976 - Solute transport and modeling of water quality in a small stream","interactions":[],"lastModifiedDate":"2022-06-17T14:50:02.510847","indexId":"70232250","displayToPublicDate":"1976-03-01T09:40:26","publicationYear":"1976","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":2446,"text":"Journal of Research of the U.S. Geological Survey","active":true,"publicationSubtype":{"id":10}},"title":"Solute transport and modeling of water quality in a small stream","docAbstract":"<p>An injection of chloride, sodium, and stable strontium was made at a constant rate for 3 hours into Uvas Creek, Santa Clara County, Calif., to determine the mass transport processes in a small stream. Five observation points were selected within a 610-metre reach of the stream below the injection site. Water samples were collected at the observation points during and immediately after the injection. A mathematical model of the stream was obtained by solving analytically and optimally the one-dimensional mass transport equation of the solutes in the stream. Comparison of field results with a simplified mathematical model indicates the dominance of convection in the behavior of sodium and chloride. The concentration of chloride and sodium can be closely simulated by the model. However, strontium cannot be well represented by the simplified model, which contains a first-order decay-type sink.</p>","language":"English","publisher":"U.S. Geological Survey","usgsCitation":"Zand, S.M., Kennedy, V.C., Zellweger, G.W., and Avanzino, R., 1976, Solute transport and modeling of water quality in a small stream: Journal of Research of the U.S. Geological Survey, p. 233-240.","productDescription":"8 p.","startPage":"233","endPage":"240","costCenters":[],"links":[{"id":402330,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"},{"id":402329,"rank":1,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/journal/1976/vol4issue2/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"country":"United States","state":"California","county":"Santa Clara County","otherGeospatial":"Uvas Creek","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -121.84627532958984,\n              37.07147779838202\n            ],\n            [\n              -121.74156188964845,\n              37.07147779838202\n            ],\n            [\n              -121.74156188964845,\n              37.10516392042412\n            ],\n            [\n              -121.84627532958984,\n              37.10516392042412\n            ],\n            [\n              -121.84627532958984,\n              37.07147779838202\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","contributors":{"authors":[{"text":"Zand, S. M.","contributorId":292491,"corporation":false,"usgs":false,"family":"Zand","given":"S.","email":"","middleInitial":"M.","affiliations":[],"preferred":false,"id":844805,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Kennedy, V. C.","contributorId":46080,"corporation":false,"usgs":true,"family":"Kennedy","given":"V.","email":"","middleInitial":"C.","affiliations":[],"preferred":false,"id":844806,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Zellweger, G. W.","contributorId":55445,"corporation":false,"usgs":true,"family":"Zellweger","given":"G.","email":"","middleInitial":"W.","affiliations":[],"preferred":false,"id":844807,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Avanzino, R.J.","contributorId":37336,"corporation":false,"usgs":true,"family":"Avanzino","given":"R.J.","affiliations":[],"preferred":false,"id":844808,"contributorType":{"id":1,"text":"Authors"},"rank":4}]}}
,{"id":1007781,"text":"1007781 - 1976 - The abundance and diversity of the herpetofaunas of tropical forest litters","interactions":[],"lastModifiedDate":"2023-08-29T15:58:35.649798","indexId":"1007781","displayToPublicDate":"1976-03-01T00:00:00","publicationYear":"1976","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1045,"text":"Biotropica","active":true,"publicationSubtype":{"id":10}},"title":"The abundance and diversity of the herpetofaunas of tropical forest litters","docAbstract":"<p><span>Quantitative and qualitative samples of amphibian and lizard faunas were taken from forest litter in Costa Rica and compared with similar samples collected in Borneo, the Philippines, and Panama. Animal abundance is about ten times greater in Costa Rican lowland wet forest than in Borneo. Radically different routes and rates of energy flow are postulated to account for the difference. In a series of upland (1010-1425 m) samples in the Philippines, the number of litter lizards and frogs increases with elevation. A single upland (1200 m) Costa Rican sample contains about three times as many animals per 100 m2 as two lowland sites. This increase with altitude correlates well with hypotheses that overall tropical forest productivity is greatest at intermediate elevations. Herpetofaunal densities are greater in wet areas compared to dry sites and flat terrain compared to slopes. These observations are linked to the greater variation and lesser total litter fall in dry sites and/or slopes. The number of species of amphibians and lizards regularly inhabiting the litter is similar in all wet lowland forests studied. Increasing elevation and decreasing rainfall correlate with faunas having fewer species. The former is seen as the result of the differential ability of lowland species to invade uplands, and the latter as a decrease in the kind and duration of frog-spawning sites. Reduced equitability with increasing elevation is principally due to the much greater proportional increase of the commonest species. In the evolution of American and Bornean-Philippine wet lowland faunas, frogs with direct development (Eleutherodactylus) have radiated in the former in the same fashion that skinks have in the latter.</span></p>","language":"English","publisher":"Wiley","doi":"10.2307/2387818","usgsCitation":"Scott, N.J., 1976, The abundance and diversity of the herpetofaunas of tropical forest litters: Biotropica, v. 8, p. 41-58, https://doi.org/10.2307/2387818.","productDescription":"18 p.","startPage":"41","endPage":"58","numberOfPages":"18","costCenters":[{"id":651,"text":"Western Ecological Research Center","active":true,"usgs":true}],"links":[{"id":129860,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"8","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4aace4b07f02db66acbe","contributors":{"authors":[{"text":"Scott, Norman J. Jr.","contributorId":112614,"corporation":false,"usgs":true,"family":"Scott","given":"Norman","suffix":"Jr.","email":"","middleInitial":"J.","affiliations":[],"preferred":false,"id":316020,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":1007751,"text":"1007751 - 1976 - Differential seed predation on two species of Arctostaphylos (Ericaceae)","interactions":[],"lastModifiedDate":"2025-05-23T17:03:49.681884","indexId":"1007751","displayToPublicDate":"1976-03-01T00:00:00","publicationYear":"1976","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":2932,"text":"Oecologia","active":true,"publicationSubtype":{"id":10}},"title":"Differential seed predation on two species of Arctostaphylos (Ericaceae)","docAbstract":"<p><span>The fire-prone California chaparral contains two sympatric species of shrubs:&nbsp;</span><i>Arctostaphylos glauca</i><span>&nbsp;and&nbsp;</span><i>A. glandulosa</i><span>. A previous study showed that in a stand where both species had similar amounts of coverage,&nbsp;</span><i>A. glauca</i><span>&nbsp;had fewer seeds in the soil. We attempt to answer the questions: 1) Could ground-foraging seed predators produce the lower population of&nbsp;</span><i>A. glauca</i><span>&nbsp;seeds in the soil? 2) Do predators select fruits randomly with respect to fruit size? 3) Do the fruits of the two species differ in the proportions of fruit components (i.e. seeds, endocarp, mesocarp, and exocarp) in ways that could be important to seed predators? Predation was measured on artificial caches of fruits, for 17 weeks. Selection by predators was examined by comparing weights of fruits recovered from soil samples with newlymatured fruits on the shrubs. Fruits components were characterized by dividing fruits into 3 fractions and weighing. More fruits of&nbsp;</span><i>A. glauca</i><span>&nbsp;were removed from the caches. Fruits of both species recovered from the soil were lighter than those on the shrubs. The weights of seeds, stony and fleshy fruit layers were all larger in&nbsp;</span><i>A. glauca</i><span>. Within fruits of&nbsp;</span><i>A. glandulosa</i><span>, the weights of the three components, various combinations, and ratios were all significantly correlated, while in&nbsp;</span><i>A. glauca</i><span>&nbsp;no other component, combination of components, or ratio examined was significantly correlated with the weights of the seeds.</span></p>","language":"English","publisher":"Springer Nature","doi":"10.1007/BF00545488","usgsCitation":"Keeley, J., and Hays, R., 1976, Differential seed predation on two species of Arctostaphylos (Ericaceae): Oecologia, v. 24, p. 71-81, https://doi.org/10.1007/BF00545488.","productDescription":"11 p.","startPage":"71","endPage":"81","costCenters":[{"id":651,"text":"Western Ecological Research Center","active":true,"usgs":true}],"links":[{"id":130184,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United States","state":"California","county":"San Diego County","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"coordinates\": [\n          [\n            [\n              -117.32686845808135,\n              32.9169897810403\n            ],\n            [\n              -117.32686845808135,\n              32.55935355113901\n            ],\n            [\n              -116.88408260322085,\n              32.55935355113901\n            ],\n            [\n              -116.88408260322085,\n              32.9169897810403\n            ],\n            [\n              -117.32686845808135,\n              32.9169897810403\n            ]\n          ]\n        ],\n        \"type\": \"Polygon\"\n      }\n    }\n  ]\n}","volume":"24","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a9ae4b07f02db65d6cf","contributors":{"authors":[{"text":"Keeley, Jon E. 0000-0002-4564-6521","orcid":"https://orcid.org/0000-0002-4564-6521","contributorId":69082,"corporation":false,"usgs":true,"family":"Keeley","given":"Jon E.","affiliations":[],"preferred":false,"id":315966,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Hays, R.L.","contributorId":40162,"corporation":false,"usgs":true,"family":"Hays","given":"R.L.","email":"","affiliations":[],"preferred":false,"id":315965,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":5223543,"text":"5223543 - 1976 - Establishment of the black-tailed jackrabbit on the Virginia eastern shore","interactions":[],"lastModifiedDate":"2025-03-10T16:38:18.767277","indexId":"5223543","displayToPublicDate":"1976-02-27T00:00:00","publicationYear":"1976","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":2373,"text":"Journal of Mammalogy","onlineIssn":"1545-1542","printIssn":"0022-2372","active":true,"publicationSubtype":{"id":10}},"title":"Establishment of the black-tailed jackrabbit on the Virginia eastern shore","docAbstract":"<p>No abstract available.&nbsp;</p>","language":"English","publisher":"Oxford Academic","doi":"10.2307/1379525","usgsCitation":"Clapp, R.B., Weske, J., and Clapp, T., 1976, Establishment of the black-tailed jackrabbit on the Virginia eastern shore: Journal of Mammalogy, v. 57, no. 1, p. 180-181, https://doi.org/10.2307/1379525.","productDescription":"2 p.","startPage":"180","endPage":"181","costCenters":[{"id":531,"text":"Patuxent Wildlife Research Center","active":true,"usgs":true}],"links":[{"id":201873,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United States","state":"Virginia","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"coordinates\": [\n          [\n            [\n              -76.53318689722039,\n              37.98487341318935\n            ],\n            [\n              -76.53318689722039,\n              36.62076603430651\n            ],\n            [\n              -75.79097825485586,\n              36.62076603430651\n            ],\n            [\n              -75.79097825485586,\n              37.98487341318935\n            ],\n            [\n              -76.53318689722039,\n              37.98487341318935\n            ]\n          ]\n        ],\n        \"type\": \"Polygon\"\n      }\n    }\n  ]\n}","volume":"57","issue":"1","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a0ee4b07f02db5fdd5a","contributors":{"authors":[{"text":"Clapp, R. B.","contributorId":9371,"corporation":false,"usgs":true,"family":"Clapp","given":"R.","email":"","middleInitial":"B.","affiliations":[],"preferred":false,"id":338952,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Weske, J.S.","contributorId":102423,"corporation":false,"usgs":true,"family":"Weske","given":"J.S.","email":"","affiliations":[],"preferred":false,"id":338954,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Clapp, T.C.","contributorId":45812,"corporation":false,"usgs":true,"family":"Clapp","given":"T.C.","email":"","affiliations":[],"preferred":false,"id":338953,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":70200400,"text":"70200400 - 1976 - Geochemistry of thermal waters in Long Valley, Mono County, California","interactions":[],"lastModifiedDate":"2018-10-16T14:58:14","indexId":"70200400","displayToPublicDate":"1976-02-10T14:58:01","publicationYear":"1976","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":2312,"text":"Journal of Geophysical Research","active":true,"publicationSubtype":{"id":10}},"title":"Geochemistry of thermal waters in Long Valley, Mono County, California","docAbstract":"<p><span>Thermal springs and wells in Long Valley, California, issue sodium bicarbonate‐chloride waters containing 1000–1420 mg/l of dissolved solids. Thermal waters of sodium bicarbonate‐chloride composition are usually associated with hot‐water reservoirs. Chloride concentrations and stable isotope data indicate that the thermal waters have had varied histories. All of the thermal springs issue a mixture of fluid from the thermal reservoir and less saline, cooler water from one or more shallow aquifers. The composition of springs in Hot Creek Gorge may have been further altered by minor subsurface boiling. Thermal springs between Hot Creek and Lake Crowley issue mixtures of fresh and thermal waters which have lost heat by conductive cooling and changed composition by reaction with rock in the shallow aquifer. The silica content of water from Magma Richie 5 and mixing calculations based on the concentrations of silica in thermal waters collected from springs in Hot Creek Gorge and along Little Hot Creek indicate a temperature of at least 200°C in the thermal reservoir. The sodium‐potassium‐calcium geothermometer yields a reservoir temperature estimate near 200°C for most of the thermal springs. If geothermal energy is developed in Long Valley, the high concentrations of arsenic (up to 2.2 mg/l), boron (up to 15 mg/l), and total dissolved solids in the thermal fluids will make it necessary to isolate the effluent of production wells from the freshwater system.</span></p>","language":"English","publisher":"AGU","doi":"10.1029/JB081i005p00792","usgsCitation":"Mariner, R.H., and Willey, L.M., 1976, Geochemistry of thermal waters in Long Valley, Mono County, California: Journal of Geophysical Research, v. 81, no. 5, p. 792-800, https://doi.org/10.1029/JB081i005p00792.","productDescription":"9 p.","startPage":"792","endPage":"800","costCenters":[{"id":154,"text":"California Water Science Center","active":true,"usgs":true}],"links":[{"id":358407,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United States","state":"California","county":"Mono County","otherGeospatial":"Long Valley","volume":"81","issue":"5","noUsgsAuthors":false,"publicationDate":"2012-09-20","publicationStatus":"PW","contributors":{"authors":[{"text":"Mariner, Robert H. rmariner@usgs.gov","contributorId":3290,"corporation":false,"usgs":true,"family":"Mariner","given":"Robert","email":"rmariner@usgs.gov","middleInitial":"H.","affiliations":[],"preferred":true,"id":748725,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Willey, Lawrence M.","contributorId":209752,"corporation":false,"usgs":false,"family":"Willey","given":"Lawrence","email":"","middleInitial":"M.","affiliations":[],"preferred":false,"id":748726,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":70119558,"text":"70119558 - 1976 - Roosting ecology of the pallid bat, <i>Antrozous pallidus</i>","interactions":[],"lastModifiedDate":"2014-08-07T12:55:12","indexId":"70119558","displayToPublicDate":"1976-02-01T12:48:31","publicationYear":"1976","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":2373,"text":"Journal of Mammalogy","onlineIssn":"1545-1542","printIssn":"0022-2372","active":true,"publicationSubtype":{"id":10}},"title":"Roosting ecology of the pallid bat, <i>Antrozous pallidus</i>","docAbstract":"Daytime roosting behavior of pallid bats (<i>Antrozous pallidus</i>) was studied in central Arizona.  Bats were present in the area from March or April until November and roosted in cliffs in colonies generally including 20 or more individuals.  Pallid bats were highly selective in their choice of roost sites and minimized diurnal energy output by adaptive hypothermia and behavioral thermo-regulation.  In spring and autumn the bats roosted in vertical crevices responsive to changes in ambient temperatures.  Here temperatures remained low and the bats were torpid for much of the day, but when the crevices became heated in the late afternoon the bats were passively warmed prior to emergence.  Deep, horizontal crevices were preferred in summer; cliffs function as massive heat sinks, and in summer crevice temperatures remained moderate and relatively stable.  Throughout most of the day both the deep parts of the crevices and the body temperatures of the bats remained close to 30ºC; at this body temperature pallid bats have unexpectedly low metabolic rates (Trune, 1974).  By adjusting their positions and closeness to other bats in the thermal gradient within the crevice, bats dissipate heat early in the day, maintain a low metabolic rate through most of the fat and elevate the body temperature prior to emergence in the evening.  Of vital important to pallid bats in the summer are social behaviors that promote communal roosting at \"traditional\" crevices.","largerWorkType":{"id":2,"text":"Article"},"largerWorkTitle":"Journal of Mammalogy","largerWorkSubtype":{"id":10,"text":"Journal Article"},"language":"English","publisher":"American Society of Mammalogists","publisherLocation":"Provo, UT","doi":"10.2307/1379510","usgsCitation":"Vaughan, T.A., and O'Shea, T., 1976, Roosting ecology of the pallid bat, <i>Antrozous pallidus</i>: Journal of Mammalogy, v. 57, no. 1, p. 19-42, https://doi.org/10.2307/1379510.","productDescription":"24 p.","startPage":"19","endPage":"42","numberOfPages":"24","costCenters":[],"links":[{"id":291841,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"},{"id":291840,"type":{"id":10,"text":"Digital Object Identifier"},"url":"https://dx.doi.org/10.2307/1379510"}],"volume":"57","issue":"1","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"53e492cfe4b0fff40428a5e7","contributors":{"authors":[{"text":"Vaughan, Terry A.","contributorId":90648,"corporation":false,"usgs":true,"family":"Vaughan","given":"Terry","email":"","middleInitial":"A.","affiliations":[],"preferred":false,"id":497713,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"O'Shea, Thomas J. 0000-0002-0758-9730","orcid":"https://orcid.org/0000-0002-0758-9730","contributorId":78071,"corporation":false,"usgs":true,"family":"O'Shea","given":"Thomas J.","affiliations":[{"id":291,"text":"Fort Collins Science Center","active":true,"usgs":true}],"preferred":false,"id":497712,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":70010234,"text":"70010234 - 1976 - Application of multi-regional planning models to the scheduling of large-scale water resource systems development","interactions":[],"lastModifiedDate":"2025-04-10T15:32:02.76064","indexId":"70010234","displayToPublicDate":"1976-02-01T00:00:00","publicationYear":"1976","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":2342,"text":"Journal of Hydrology","active":true,"publicationSubtype":{"id":10}},"title":"Application of multi-regional planning models to the scheduling of large-scale water resource systems development","docAbstract":"<p>No abstract available.&nbsp;</p>","language":"English","publisher":"Elsevier","doi":"10.1016/0022-1694(76)90062-7","issn":"00221694","usgsCitation":"Moody, D., 1976, Application of multi-regional planning models to the scheduling of large-scale water resource systems development: Journal of Hydrology, v. 28, no. 2-4, p. 101-125, 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,{"id":70039205,"text":"70039205 - 1976 - Availability of Earth resources data","interactions":[],"lastModifiedDate":"2017-05-19T18:44:38","indexId":"70039205","displayToPublicDate":"1976-01-07T13:43:00","publicationYear":"1976","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":6,"text":"USGS Unnumbered Series"},"seriesTitle":{"id":362,"text":"General Information Product","active":false,"publicationSubtype":{"id":6}},"title":"Availability of Earth resources data","docAbstract":"The purpose of this booklet is to help the reader to become aware of the volume of Earth resources data that have been collected by agencies of the United States Government and to find out where and how these data may be obtained. Earth resources data as discussed here are those obtained by remote-sensing instruments, including aerial cameras, multispectral cameras, multispectral scanners, and radar. They are obtained by spacecraft and high-altitude aircraft. Also, various agencies have been acquiring vast quantities of conventional aerial mapping photography from low and medium altitudes for more than 50 years. There is also brief information to assist the reader in locating published references and identifying research projects relating to application of Earth resources data to a variety of purposes. In all cases, it is not the intent to say what data are needed or how the data are to be used, but to describe where an interested person can begin to locate Earth resources data.","language":"English","publisher":"U.S. Government Printing Office","publisherLocation":"Washington, D.C.","doi":"10.3133/70039205","usgsCitation":"Water Resources Division, U.S. Geological Survey, 1976, Availability of Earth resources data: General Information Product, 46 p., https://doi.org/10.3133/70039205.","productDescription":"46 p.","numberOfPages":"48","costCenters":[],"links":[{"id":261376,"rank":800,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/gip/70039205/report.pdf"},{"id":261377,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/gip/70039205/report-thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"5059ef08e4b0c8380cd4a0dd","contributors":{"authors":[{"text":"Water Resources Division, U.S. Geological Survey","contributorId":128075,"corporation":true,"usgs":false,"organization":"Water Resources Division, U.S. Geological Survey","id":535243,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":70207697,"text":"70207697 - 1976 - Structure and evolution of Bering Sea shelf south of St. Lawrence Island","interactions":[],"lastModifiedDate":"2020-06-15T15:19:07.448226","indexId":"70207697","displayToPublicDate":"1976-01-06T15:44:21","publicationYear":"1976","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":605,"text":"AAPG Bulletin","printIssn":"0149-1423","active":true,"publicationSubtype":{"id":10}},"title":"Structure and evolution of Bering Sea shelf south of St. Lawrence Island","docAbstract":"<p>The virtually featureless Beringian shelf south of St. Lawrence Island is underlain structurally by at least 14 basins. Encompassing a total area of more than 300,000 sq km, most of the basins are either elongate structural sags, grabens, or half (asymmetric) grabens beneath the outer shelf. The regional trend of these basins is northwest, parallel with that of the continental margin. Two of the basins, St. George and Navarin, contain 7 to 10 km of Upper Cretaceous(?) and Cenozoic sedimentary strata. A major divergence in dip of beds in the upper half of the sedimentary section may reflect an abrupt shelf-wide change in the rate of sedimentation and/or subsidence, probably during the Miocene. The outer sub-shelf basement grabens and adjacent ridges (horsts) are bounded by high-angle normal faults that exhibit growth-type structure.</p><p>St. Matthew basin, an elongate, southwest-trending feature of the inner shelf, lies along the offshore expression of the Kaltag fault of western Alaska. The Kaltag fault, like the Denali fault in southwestern Alaska, does not extend to the outer Bering Sea shelf but ends or turns parallel with the margin within the inner shelf.</p><p>The inner shelf is underlain by a broad basement high, Nunivak arch, the seaward half of which is characterized by an arcuate belt of high-frequency and high-amplitude magnetic anomalies. This zone of intense magnetic anomalies along the shelf is probably the signature of a Mesozoic magmatic arc that extends from southwestern Alaska to eastern Siberia and consists of Jurassic to Cretaceous plutonic and volcanic rocks. We speculate that this magmatic arc resulted from oblique convergence and subduction in the Mesozoic between the Kula(?) and North American plates along the eastern Beringian margin. Folding and uplift in the area of the present outer shelf occurred contemporaneously with magmatism along the inner shelf. Plate convergence apparently ceased by the end of the Mesozoic or t e beginning of the Cenozoic. Subsequently, the foldbelt underlying the outer shelf was eroded extensively and rifted extensionally to form large, deep basins. On the average, the shelf has subsided more than 1.5 km. Subsidence and sediment burial of the eroded orogen formed the modern Beringian shelf.</p>","language":"English","publisher":"AAPG","doi":"10.1306/83D92299-16C7-11D7-8645000102C1865D","usgsCitation":"Marlow, M.S., Scholl, D.W., Cooper, A.K., and Buffington, E.C., 1976, Structure and evolution of Bering Sea shelf south of St. Lawrence Island: AAPG Bulletin, v. 60, no. 2, p. 161-183, https://doi.org/10.1306/83D92299-16C7-11D7-8645000102C1865D.","productDescription":"23 p.","startPage":"161","endPage":"183","costCenters":[{"id":186,"text":"Coastal and Marine Geology Program","active":true,"usgs":true},{"id":520,"text":"Pacific Coastal and Marine Science Center","active":true,"usgs":true}],"links":[{"id":371026,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"otherGeospatial":"Bering Sea Shelf","volume":"60","issue":"2","noUsgsAuthors":false,"publicationStatus":"PW","contributors":{"authors":[{"text":"Marlow, Michael S.","contributorId":72775,"corporation":false,"usgs":true,"family":"Marlow","given":"Michael","email":"","middleInitial":"S.","affiliations":[],"preferred":false,"id":779000,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Scholl, David W. 0000-0001-6500-6962 dscholl@usgs.gov","orcid":"https://orcid.org/0000-0001-6500-6962","contributorId":3738,"corporation":false,"usgs":true,"family":"Scholl","given":"David","email":"dscholl@usgs.gov","middleInitial":"W.","affiliations":[{"id":520,"text":"Pacific Coastal and Marine Science Center","active":true,"usgs":true},{"id":186,"text":"Coastal and Marine Geology Program","active":true,"usgs":true}],"preferred":true,"id":779001,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Cooper, Alan K. acooper@usgs.gov","contributorId":2854,"corporation":false,"usgs":true,"family":"Cooper","given":"Alan","email":"acooper@usgs.gov","middleInitial":"K.","affiliations":[{"id":520,"text":"Pacific Coastal and Marine Science Center","active":true,"usgs":true}],"preferred":true,"id":779002,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Buffington, E. C.","contributorId":13948,"corporation":false,"usgs":true,"family":"Buffington","given":"E.","email":"","middleInitial":"C.","affiliations":[],"preferred":false,"id":779003,"contributorType":{"id":1,"text":"Authors"},"rank":4}]}}
,{"id":70207696,"text":"70207696 - 1976 - Plate tectonic model for the evolution of the eastern Bering Sea Basin","interactions":[],"lastModifiedDate":"2020-06-15T15:17:00.551395","indexId":"70207696","displayToPublicDate":"1976-01-06T15:33:44","publicationYear":"1976","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":"Plate tectonic model for the evolution of the eastern Bering Sea Basin","docAbstract":"<p>The eastern Bering Sea Basin, composed of the Aleutian and Bowers Basins, is flanked to the north by Mesozoic foldbelts that probably represent zones of plate subduction in Mesozoic time. Present plate subduction occurs 400 to 1,000 km farther south, at the Aleutian Trench. North-south magnetic lineations that formed at an oceanic spreading ridge, probably in Mesozoic time (117 to 132 m.y. ago), have been identified in the Aleutian Basin. The orientation and age of those anomalies can be explained by reconstructing Kula-Farallon Pacific plate motions during late Mesozoic–early Tertiary time.</p><p>In Mesozoic time, subduction of the Kula plate occurred north of the Aleutian Trench near the present location of the Bering Sea continental margin. At about 70 m.y. B.P. (Late Cretaceous), the zone of subduction shifted south to the present location of the Aleutian Trench, thereby trapping a fragment of oceanic plate imprinted with north-south magnetic lineations within the eastern Bering Sea Basin. A stable basin framework has prevailed behind the Aleutian arc since early Tertiary time.</p>","language":"English","publisher":"GSA","doi":"10.1130/0016-7606(1976)87<1119:PTMFTE>2.0.CO;2","usgsCitation":"Cooper, A.K., Scholl, D.W., and Marlow, M.S., 1976, Plate tectonic model for the evolution of the eastern Bering Sea Basin: GSA Bulletin, v. 87, no. 8, p. 1119-1126, https://doi.org/10.1130/0016-7606(1976)87<1119:PTMFTE>2.0.CO;2.","productDescription":"8 p.","startPage":"1119","endPage":"1126","costCenters":[{"id":520,"text":"Pacific Coastal and Marine Science Center","active":true,"usgs":true}],"links":[{"id":371025,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"otherGeospatial":"Eastern Bering Sea basin","volume":"87","issue":"8","noUsgsAuthors":false,"publicationStatus":"PW","contributors":{"authors":[{"text":"Cooper, Alan K. acooper@usgs.gov","contributorId":2854,"corporation":false,"usgs":true,"family":"Cooper","given":"Alan","email":"acooper@usgs.gov","middleInitial":"K.","affiliations":[{"id":520,"text":"Pacific Coastal and Marine Science Center","active":true,"usgs":true}],"preferred":true,"id":778997,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Scholl, David W. 0000-0001-6500-6962 dscholl@usgs.gov","orcid":"https://orcid.org/0000-0001-6500-6962","contributorId":3738,"corporation":false,"usgs":true,"family":"Scholl","given":"David","email":"dscholl@usgs.gov","middleInitial":"W.","affiliations":[{"id":520,"text":"Pacific Coastal and Marine Science Center","active":true,"usgs":true},{"id":186,"text":"Coastal and Marine Geology Program","active":true,"usgs":true}],"preferred":true,"id":778998,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Marlow, Michael S.","contributorId":72775,"corporation":false,"usgs":true,"family":"Marlow","given":"Michael","email":"","middleInitial":"S.","affiliations":[],"preferred":false,"id":778999,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
]}