{"pageNumber":"5059","pageRowStart":"126450","pageSize":"25","recordCount":165579,"records":[{"id":93896,"text":"93896 - 1980 - Viruserkrankungen der Fische (Viral diseases of fishes)","interactions":[],"lastModifiedDate":"2012-02-02T00:04:07","indexId":"93896","displayToPublicDate":"1980-01-01T00:00:00","publicationYear":"1980","noYear":false,"publicationType":{"id":5,"text":"Book chapter"},"publicationSubtype":{"id":24,"text":"Book Chapter"},"title":"Viruserkrankungen der Fische (Viral diseases of fishes)","docAbstract":"No abstract available at this time","largerWorkType":{"id":18,"text":"Report"},"largerWorkTitle":"Krankheiten und Schadigungen der Fische (Diseases and Injuries of Fishes): 2nd Revised ed.","largerWorkSubtype":{"id":9,"text":"Other Report"},"language":"English","publisher":"Gustav Fischer Verlag","publisherLocation":"Stuttgart, Germany","collaboration":"340/FH","usgsCitation":"Ahne, W., and Wolf, K., 1980, Viruserkrankungen der Fische (Viral diseases of fishes), chap. <i>of</i> Krankheiten und Schadigungen der Fische (Diseases and Injuries of Fishes): 2nd Revised ed., p. 56-105.","productDescription":"p. 56-105","startPage":"56","endPage":"105","numberOfPages":"50","costCenters":[{"id":365,"text":"Leetown Science Center","active":true,"usgs":true}],"links":[{"id":129598,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"edition":"2nd Revised ed.","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a0ee4b07f02db5fdbba","contributors":{"editors":[{"text":"Reichenbach-Klinke, H. H.","contributorId":20277,"corporation":false,"usgs":true,"family":"Reichenbach-Klinke","given":"H.","email":"","middleInitial":"H.","affiliations":[],"preferred":false,"id":505192,"contributorType":{"id":2,"text":"Editors"},"rank":1}],"authors":[{"text":"Ahne, W.","contributorId":28554,"corporation":false,"usgs":true,"family":"Ahne","given":"W.","affiliations":[],"preferred":false,"id":298290,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Wolf, K.","contributorId":16344,"corporation":false,"usgs":true,"family":"Wolf","given":"K.","email":"","affiliations":[],"preferred":false,"id":298289,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":1007465,"text":"1007465 - 1980 - Locality records of Rhinocheilus lecontei in the United States and Mexico","interactions":[],"lastModifiedDate":"2012-02-02T00:04:18","indexId":"1007465","displayToPublicDate":"1980-01-01T00:00:00","publicationYear":"1980","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1898,"text":"Herpetological Review","active":true,"publicationSubtype":{"id":10}},"title":"Locality records of Rhinocheilus lecontei in the United States and Mexico","largerWorkType":{"id":2,"text":"Article"},"largerWorkTitle":"Herpetological Review","largerWorkSubtype":{"id":10,"text":"Journal Article"},"language":"English","usgsCitation":"Medica, P., 1980, Locality records of Rhinocheilus lecontei in the United States and Mexico: Herpetological Review, v. 11, no. 2.","productDescription":"p. 42","startPage":"42","numberOfPages":"42","costCenters":[{"id":651,"text":"Western Ecological Research Center","active":true,"usgs":true}],"links":[{"id":130051,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"11","issue":"2","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a68e4b07f02db63b2c3","contributors":{"authors":[{"text":"Medica, P.A.","contributorId":77079,"corporation":false,"usgs":true,"family":"Medica","given":"P.A.","email":"","affiliations":[],"preferred":false,"id":315410,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":13364,"text":"ofr801029 - 1980 - Geophysical, lithologic, and water-quality data from Superior Dry Lake, San Bernardino County, California","interactions":[],"lastModifiedDate":"2023-03-24T18:16:57.114608","indexId":"ofr801029","displayToPublicDate":"1980-01-01T00:00:00","publicationYear":"1980","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":330,"text":"Open-File Report","code":"OFR","onlineIssn":"2331-1258","printIssn":"0196-1497","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"80-1029","title":"Geophysical, lithologic, and water-quality data from Superior Dry Lake, San Bernardino County, California","docAbstract":"<p>No abstract available.</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr801029","usgsCitation":"Dockter, R.D., 1980, Geophysical, lithologic, and water-quality data from Superior Dry Lake, San Bernardino County, California: U.S. Geological Survey Open-File Report 80-1029, 1 Plate: 27.54 x 24.86 inches, https://doi.org/10.3133/ofr801029.","productDescription":"1 Plate: 27.54 x 24.86 inches","costCenters":[],"links":[{"id":146974,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":414713,"rank":3,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_75333.htm","linkFileType":{"id":5,"text":"html"}},{"id":41789,"rank":2,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1980/1029/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}}],"country":"United States","state":"California","county":"San Bernardino County","otherGeospatial":"Superior Dry Lake","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"coordinates\": [\n          [\n            [\n              -117.1333,\n              35.2594\n            ],\n            [\n              -117.1333,\n              35.2197\n            ],\n            [\n              -117.0028,\n              35.2197\n            ],\n            [\n              -117.0028,\n              35.2594\n            ],\n            [\n              -117.1333,\n              35.2594\n            ]\n          ]\n        ],\n        \"type\": \"Polygon\"\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ac7e4b07f02db67b3b8","contributors":{"authors":[{"text":"Dockter, Roger D.","contributorId":81875,"corporation":false,"usgs":true,"family":"Dockter","given":"Roger","email":"","middleInitial":"D.","affiliations":[],"preferred":false,"id":167684,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":5221592,"text":"5221592 - 1980 - Early concentrations of Brown Pelicans along southern Oregon coast","interactions":[],"lastModifiedDate":"2024-10-09T16:39:14.540082","indexId":"5221592","displayToPublicDate":"1980-01-01T00:00:00","publicationYear":"1980","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":2793,"text":"Murrelet","active":true,"publicationSubtype":{"id":10}},"title":"Early concentrations of Brown Pelicans along southern Oregon coast","docAbstract":"<p>The California Brown Pelican (<i>Pelecanus occidentalis californicus</i>), which nests in southern California and Mexico, wanders north along the coast after the breeding season, sometimes as far as southern British Columbia (A.O.U. 1957). Anderson and Anderson (1976) and Ainley (1972) report that Mexico-originating pelicans disperse north in late summer and fall, increasing California coastal counts from late July through early November each year. Gabrielson and Jewett (1940) and Bayer (1977) reported that the northward flight into Oregon apparently occurs in July, and there are usually few present after the first of November. Similarly, Marshall (1969) reported that the Brown Pelican appeared regularly in the Netarts-Tillamook Bay area and more southern coastal points from August through November and indicated that a recent high count in Oregon was 110 in the Netarts-Tillamook Bay area on 27 August 1967. Bayer (1977) simultaneously observed 182 immature and 12 adult Brown Pelicans in the Yaquina estuary in October 1975 but noted that the number of adult pelicans (less than 20) observed in the Yaquina estuary seemed to remain relatively unchanged from year to year. He observed no more than 60 birds at a time in the Yaquina estuary in other years.</p>","language":"English","publisher":"Society for Northwestern Vertebrate Biology","doi":"10.2307/3535191","usgsCitation":"Henny, C.J., and Collins, J., 1980, Early concentrations of Brown Pelicans along southern Oregon coast: Murrelet, v. 61, no. 3, p. 99-100, https://doi.org/10.2307/3535191.","productDescription":"2 p.","startPage":"99","endPage":"100","costCenters":[{"id":531,"text":"Patuxent Wildlife Research Center","active":true,"usgs":true}],"links":[{"id":18394,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://www.jstor.org/stable/3535191","linkFileType":{"id":5,"text":"html"}},{"id":198905,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United States","state":"Oregon","geographicExtents":"{\"type\":\"FeatureCollection\",\"features\":[{\"type\":\"Feature\",\"geometry\":{\"type\":\"Polygon\",\"coordinates\":[[[-121.922236,45.649083],[-121.908267,45.654399],[-121.900858,45.662009],[-121.901855,45.670716],[-121.867167,45.693277],[-121.811304,45.706761],[-121.735104,45.694039],[-121.707358,45.694809],[-121.668362,45.705082],[-121.631167,45.704657],[-121.533106,45.726541],[-121.499153,45.720846],[-121.462849,45.701367],[-121.423592,45.69399],[-121.401739,45.692887],[-121.372574,45.703111],[-121.33777,45.704949],[-121.312198,45.699925],[-121.287323,45.687019],[-121.251183,45.67839],[-121.215779,45.671238],[-121.200367,45.649829],[-121.195233,45.629513],[-121.196556,45.616689],[-121.183841,45.606441],[-121.167852,45.606098],[-121.145534,45.607886],[-121.139483,45.611962],[-121.131953,45.609762],[-121.1222,45.616067],[-121.117052,45.618117],[-121.120064,45.623134],[-121.084933,45.647893],[-121.06437,45.652549],[-121.033582,45.650998],[-121.007449,45.653217],[-120.983478,45.648344],[-120.977978,45.649345],[-120.953077,45.656745],[-120.943977,45.656445],[-120.913476,45.640045],[-120.895575,45.642945],[-120.855674,45.671545],[-120.788872,45.686246],[-120.724171,45.706446],[-120.68937,45.715847],[-120.668869,45.730147],[-120.634968,45.745847],[-120.591166,45.746547],[-120.559465,45.738348],[-120.521964,45.709848],[-120.505863,45.700048],[-120.482362,45.694449],[-120.40396,45.699249],[-120.329057,45.71105],[-120.282156,45.72125],[-120.210754,45.725951],[-120.170453,45.761951],[-120.141352,45.773152],[-120.07015,45.785152],[-120.001148,45.811902],[-119.965744,45.824365],[-119.907461,45.828135],[-119.876144,45.834718],[-119.802655,45.84753],[-119.772927,45.845578],[-119.669877,45.856867],[-119.623393,45.905639],[-119.600549,45.919581],[-119.571584,45.925456],[-119.524632,45.908605],[-119.487829,45.906307],[-119.450256,45.917354],[-119.364396,45.921605],[-119.322509,45.933183],[-119.25715,45.939926],[-119.225745,45.932725],[-119.19553,45.92787],[-119.169496,45.927603],[-119.12612,45.932859],[-119.093221,45.942745],[-119.061462,45.958527],[-119.027056,45.969134],[-119.008558,45.97927],[-118.987129,45.999855],[-118.941242,46.000574],[-118.639332,46.000994],[-118.146028,46.000701],[-118.131019,46.00028],[-117.996911,46.000787],[-117.717852,45.999866],[-117.48013,45.99787],[-117.439943,45.998633],[-117.390738,45.998598],[-117.353928,45.996349],[-117.337668,45.998662],[-117.216731,45.998356],[-117.070047,45.99751],[-117.051304,45.996849],[-116.985882,45.996974],[-116.915989,45.995413],[-116.911409,45.988912],[-116.892935,45.974396],[-116.886843,45.958617],[-116.875706,45.945008],[-116.869655,45.923799],[-116.866544,45.916958],[-116.859795,45.907264],[-116.857254,45.904159],[-116.84355,45.892273],[-116.830003,45.886405],[-116.819182,45.880938],[-116.814142,45.877551],[-116.796051,45.858473],[-116.790151,45.849851],[-116.787792,45.844267],[-116.78752,45.840204],[-116.788923,45.836741],[-116.789066,45.833471],[-116.782676,45.825376],[-116.7634,45.81658],[-116.759787,45.816167],[-116.750978,45.818537],[-116.740486,45.82446],[-116.736268,45.826179],[-116.715527,45.826773],[-116.711822,45.826267],[-116.697192,45.820135],[-116.687007,45.806319],[-116.680139,45.79359],[-116.665344,45.781998],[-116.659629,45.780016],[-116.646342,45.779815],[-116.639641,45.781274],[-116.635814,45.783642],[-116.632032,45.784979],[-116.60504,45.781018],[-116.593004,45.778541],[-116.559444,45.755189],[-116.553548,45.753388],[-116.549085,45.752735],[-116.546643,45.750972],[-116.537173,45.737288],[-116.535698,45.734231],[-116.538014,45.714929],[-116.536395,45.69665],[-116.535396,45.691734],[-116.528272,45.681473],[-116.523961,45.677639],[-116.512326,45.670224],[-116.487894,45.649769],[-116.477452,45.631267],[-116.469813,45.620604],[-116.46517,45.617986],[-116.463504,45.615785],[-116.463635,45.602785],[-116.481943,45.577898],[-116.48297,45.577008],[-116.490279,45.574499],[-116.502756,45.566608],[-116.523638,45.54661],[-116.535482,45.525079],[-116.543837,45.514193],[-116.548676,45.510385],[-116.553473,45.499107],[-116.558804,45.481188],[-116.558803,45.480076],[-116.55498,45.472801],[-116.554829,45.46293],[-116.563985,45.460169],[-116.581382,45.448984],[-116.588195,45.44292],[-116.592416,45.427356],[-116.597447,45.41277],[-116.619057,45.39821],[-116.653252,45.351084],[-116.673793,45.321511],[-116.674648,45.314342],[-116.672594,45.298023],[-116.672163,45.288938],[-116.672733,45.283183],[-116.674493,45.276349],[-116.675587,45.274867],[-116.681013,45.27072],[-116.687027,45.267857],[-116.691388,45.263739],[-116.703607,45.239757],[-116.70975,45.217243],[-116.708546,45.207356],[-116.709536,45.203015],[-116.724205,45.171501],[-116.724188,45.162924],[-116.729607,45.142091],[-116.754643,45.113972],[-116.774847,45.105536],[-116.782492,45.09579],[-116.783537,45.093605],[-116.784244,45.088128],[-116.78371,45.076972],[-116.797329,45.060267],[-116.808576,45.050652],[-116.825133,45.03784],[-116.841314,45.030907],[-116.847944,45.022602],[-116.848037,45.021728],[-116.845847,45.01847],[-116.844796,45.015312],[-116.844625,45.001435],[-116.856754,44.984298],[-116.858313,44.978761],[-116.850737,44.958113],[-116.846461,44.951521],[-116.835702,44.940633],[-116.83199,44.933007],[-116.832176,44.931373],[-116.833632,44.928976],[-116.838467,44.923601],[-116.846061,44.905249],[-116.852427,44.887577],[-116.857038,44.880769],[-116.865338,44.870599],[-116.883598,44.858268],[-116.896249,44.84833],[-116.920498,44.81438],[-116.928099,44.808381],[-116.931099,44.804781],[-116.933699,44.798781],[-116.933799,44.796781],[-116.9307,44.789881],[-116.9318,44.787181],[-116.9347,44.783881],[-116.949001,44.777981],[-116.966801,44.775181],[-116.970902,44.773881],[-116.977802,44.767981],[-116.986502,44.762381],[-116.992003,44.759182],[-116.998903,44.756382],[-117.006045,44.756024],[-117.013802,44.756841],[-117.03827,44.748179],[-117.044217,44.74514],[-117.062273,44.727143],[-117.060454,44.721668],[-117.061799,44.706654],[-117.063824,44.703623],[-117.072221,44.700517],[-117.07912,44.692175],[-117.080772,44.684161],[-117.091223,44.668807],[-117.095868,44.664737],[-117.096791,44.657385],[-117.094968,44.652011],[-117.098221,44.640689],[-117.108231,44.62711],[-117.114754,44.624883],[-117.120522,44.614658],[-117.125267,44.593818],[-117.124754,44.583834],[-117.126009,44.581553],[-117.133963,44.57524],[-117.14248,44.57143],[-117.146032,44.568603],[-117.148255,44.564371],[-117.147934,44.562143],[-117.14293,44.557236],[-117.144161,44.545647],[-117.149242,44.536151],[-117.152406,44.531802],[-117.161033,44.525166],[-117.167187,44.523431],[-117.181583,44.52296],[-117.185386,44.519261],[-117.189759,44.513385],[-117.19163,44.509886],[-117.191329,44.506784],[-117.192494,44.503272],[-117.194317,44.499884],[-117.200237,44.492027],[-117.208936,44.485661],[-117.211148,44.485359],[-117.216372,44.48616],[-117.224104,44.483734],[-117.225076,44.482346],[-117.225932,44.479389],[-117.225758,44.477223],[-117.224445,44.473884],[-117.221548,44.470146],[-117.217015,44.459042],[-117.215573,44.453746],[-117.214637,44.44803],[-117.215072,44.427162],[-117.22698,44.405583],[-117.234835,44.399669],[-117.242675,44.396548],[-117.243027,44.390974],[-117.235117,44.373853],[-117.216911,44.360163],[-117.210587,44.357703],[-117.206962,44.355206],[-117.197339,44.347406],[-117.189769,44.336585],[-117.191546,44.329621],[-117.203323,44.313024],[-117.2055,44.311789],[-117.216795,44.308236],[-117.217843,44.30718],[-117.220069,44.301382],[-117.222451,44.298963],[-117.222647,44.297578],[-117.216974,44.288357],[-117.198147,44.273828],[-117.170342,44.25889],[-117.15706,44.25749],[-117.143394,44.258262],[-117.138523,44.25937],[-117.133984,44.262972],[-117.133104,44.264236],[-117.13253,44.267045],[-117.130904,44.269453],[-117.121037,44.277585],[-117.111617,44.280667],[-117.107673,44.280763],[-117.104208,44.27994],[-117.098531,44.275533],[-117.09457,44.270978],[-117.093578,44.269383],[-117.090933,44.260311],[-117.089503,44.258234],[-117.07835,44.249885],[-117.067284,44.24401],[-117.059352,44.237244],[-117.05651,44.230874],[-117.05303,44.229076],[-117.050057,44.22883],[-117.047062,44.229742],[-117.045513,44.232005],[-117.042283,44.242775],[-117.031862,44.248635],[-117.025277,44.248505],[-117.020231,44.246063],[-117.016921,44.245391],[-116.98687,44.245477],[-116.975905,44.242844],[-116.973542,44.23998],[-116.971958,44.235677],[-116.973945,44.225932],[-116.973701,44.208017],[-116.971675,44.197256],[-116.967259,44.194581],[-116.965498,44.194126],[-116.947591,44.191264],[-116.940534,44.19371],[-116.935443,44.193962],[-116.925392,44.191544],[-116.902752,44.179467],[-116.900103,44.176851],[-116.895757,44.171267],[-116.894083,44.160191],[-116.894309,44.158114],[-116.895931,44.154295],[-116.927688,44.109438],[-116.928306,44.107326],[-116.933704,44.100039],[-116.937835,44.096943],[-116.943132,44.09406],[-116.957009,44.091743],[-116.967203,44.090936],[-116.974253,44.088295],[-116.977351,44.085364],[-116.973185,44.049425],[-116.956246,44.042888],[-116.943361,44.035645],[-116.937342,44.029376],[-116.934727,44.023806],[-116.934485,44.021249],[-116.942944,43.987512],[-116.957527,43.972443],[-116.969842,43.967588],[-116.971436,43.964998],[-116.971835,43.962806],[-116.970241,43.958622],[-116.969245,43.957426],[-116.966256,43.955832],[-116.963666,43.952644],[-116.96247,43.928336],[-116.963666,43.921363],[-116.977332,43.905812],[-116.976024,43.895548],[-116.982347,43.86884],[-116.98294,43.86771],[-116.991415,43.863864],[-116.997391,43.864874],[-117.01077,43.862269],[-117.013954,43.859358],[-117.026871,43.832479],[-117.026222,42.000252],[-117.040906,41.99989],[-117.04891,41.998983],[-117.055402,41.99989],[-117.068613,42.000035],[-117.197798,42.00038],[-117.403613,41.99929],[-117.443062,41.999659],[-117.625973,41.998102],[-117.873467,41.998335],[-118.197189,41.996995],[-118.501002,41.995446],[-118.696409,41.991794],[-119.001022,41.993793],[-119.20828,41.993177],[-119.231876,41.994212],[-119.251033,41.993843],[-119.444598,41.995478],[-119.72573,41.996296],[-119.790087,41.997544],[-119.872929,41.997641],[-119.876054,41.997199],[-119.986678,41.995842],[-119.999168,41.99454],[-120.001058,41.995139],[-120.181563,41.994588],[-120.286424,41.993058],[-120.501069,41.993785],[-120.647173,41.993084],[-120.812279,41.994183],[-121.035195,41.993323],[-121.094926,41.994658],[-121.126093,41.99601],[-121.247616,41.997054],[-121.251099,41.99757],[-121.309981,41.997612],[-121.340517,41.99622],[-121.376101,41.997026],[-121.434977,41.997022],[-121.580865,41.998668],[-121.846712,42.00307],[-122.000319,42.003967],[-122.101922,42.005766],[-122.160438,42.007637],[-122.261127,42.007364],[-122.378193,42.009518],[-122.397984,42.008758],[-122.501135,42.00846],[-122.634739,42.004858],[-122.80008,42.004071],[-122.893961,42.002605],[-123.045254,42.003049],[-123.065655,42.004948],[-123.083956,42.005448],[-123.145959,42.009247],[-123.154908,42.008036],[-123.192361,42.005446],[-123.347562,41.999108],[-123.381776,41.999268],[-123.43477,42.001641],[-123.49883,42.000525],[-123.525245,42.001047],[-123.55256,42.000246],[-123.624554,41.999837],[-123.656998,41.995137],[-123.728156,41.997007],[-123.789295,41.996111],[-123.813992,41.995096],[-123.834208,41.996116],[-124.001188,41.996146],[-124.126194,41.996992],[-124.211605,41.99846],[-124.214213,42.005939],[-124.270464,42.045553],[-124.287374,42.046016],[-124.299649,42.051736],[-124.314289,42.067864],[-124.34101,42.092929],[-124.356229,42.114952],[-124.357122,42.118016],[-124.351535,42.129796],[-124.351784,42.134965],[-124.355696,42.141964],[-124.361563,42.143767],[-124.366028,42.152343],[-124.366832,42.15845],[-124.363389,42.158588],[-124.360318,42.162272],[-124.361009,42.180752],[-124.367751,42.188321],[-124.373175,42.190218],[-124.374949,42.193129],[-124.376215,42.196381],[-124.375553,42.20882],[-124.377762,42.218809],[-124.383633,42.22716],[-124.410982,42.250547],[-124.411534,42.254115],[-124.408514,42.260588],[-124.405148,42.278107],[-124.410556,42.307431],[-124.429288,42.331746],[-124.427222,42.33488],[-124.425554,42.351874],[-124.424066,42.377242],[-124.424863,42.395426],[-124.428068,42.420333],[-124.434882,42.434916],[-124.435105,42.440163],[-124.422038,42.461226],[-124.423084,42.478952],[-124.421381,42.491737],[-124.399065,42.539928],[-124.390664,42.566593],[-124.389977,42.574758],[-124.400918,42.597518],[-124.399421,42.618079],[-124.401177,42.627192],[-124.413119,42.657934],[-124.416774,42.661594],[-124.45074,42.675798],[-124.451484,42.677787],[-124.447487,42.68474],[-124.448418,42.689909],[-124.473864,42.732671],[-124.491679,42.741789],[-124.498473,42.741077],[-124.499122,42.738606],[-124.510017,42.734746],[-124.513368,42.735068],[-124.514669,42.736806],[-124.516236,42.753632],[-124.524439,42.789793],[-124.536073,42.814175],[-124.544179,42.822958],[-124.552441,42.840568],[-124.500141,42.917502],[-124.480938,42.951495],[-124.462619,42.99143],[-124.456918,43.000315],[-124.436198,43.071312],[-124.432236,43.097383],[-124.434451,43.115986],[-124.424113,43.126859],[-124.401726,43.184896],[-124.395302,43.211101],[-124.395607,43.223908],[-124.38246,43.270167],[-124.388891,43.290523],[-124.393988,43.29926],[-124.400404,43.302121],[-124.402814,43.305872],[-124.387642,43.325968],[-124.373037,43.338953],[-124.353332,43.342667],[-124.341587,43.351337],[-124.315012,43.388389],[-124.286896,43.436296],[-124.255609,43.502172],[-124.233534,43.55713],[-124.203028,43.667825],[-124.204888,43.673976],[-124.198275,43.689481],[-124.193455,43.706085],[-124.168392,43.808903],[-124.150267,43.91085],[-124.142704,43.958182],[-124.133547,44.035845],[-124.122406,44.104442],[-124.125824,44.12613],[-124.117006,44.171913],[-124.114424,44.198164],[-124.115671,44.206554],[-124.111054,44.235071],[-124.108945,44.265475],[-124.109744,44.270597],[-124.114869,44.272721],[-124.115953,44.274641],[-124.1152,44.286486],[-124.10907,44.303707],[-124.108088,44.309926],[-124.109556,44.314545],[-124.100587,44.331926],[-124.092101,44.370388],[-124.084401,44.415611],[-124.080989,44.419728],[-124.071706,44.423662],[-124.067569,44.428582],[-124.073941,44.434481],[-124.079301,44.430863],[-124.082113,44.441518],[-124.082061,44.478171],[-124.084429,44.486927],[-124.083601,44.501123],[-124.076387,44.531214],[-124.067251,44.60804],[-124.06914,44.612979],[-124.082326,44.608861],[-124.084476,44.611056],[-124.065202,44.622445],[-124.065008,44.632504],[-124.058281,44.658866],[-124.060043,44.669361],[-124.070394,44.683514],[-124.063406,44.703177],[-124.059077,44.737656],[-124.066325,44.762671],[-124.075473,44.771403],[-124.074066,44.798107],[-124.066746,44.831191],[-124.063155,44.835333],[-124.054151,44.838233],[-124.048814,44.850007],[-124.032296,44.900809],[-124.025136,44.928175],[-124.025678,44.936542],[-124.023834,44.949825],[-124.015243,44.982904],[-124.004386,45.046197],[-124.004668,45.048167],[-124.00977,45.047266],[-124.017991,45.049808],[-124.015851,45.064759],[-124.012163,45.076921],[-124.006057,45.084736],[-124.004863,45.084232],[-123.989529,45.094045],[-123.975425,45.145476],[-123.968187,45.201217],[-123.972919,45.216784],[-123.962887,45.280218],[-123.964169,45.317026],[-123.972899,45.33689],[-123.978671,45.338854],[-124.007756,45.336813],[-124.007494,45.33974],[-123.979715,45.347724],[-123.973398,45.354791],[-123.965728,45.386242],[-123.960557,45.430778],[-123.964074,45.449112],[-123.972953,45.467513],[-123.976544,45.489733],[-123.970794,45.493507],[-123.96634,45.493417],[-123.957568,45.510399],[-123.947556,45.564878],[-123.956711,45.571303],[-123.951246,45.585775],[-123.939005,45.661923],[-123.939448,45.708795],[-123.943121,45.727031],[-123.946027,45.733249],[-123.968563,45.757019],[-123.982578,45.761815],[-123.981864,45.768285],[-123.969459,45.782371],[-123.961544,45.837101],[-123.962736,45.869974],[-123.96763,45.907807],[-123.979501,45.930389],[-123.99304,45.938842],[-123.993703,45.946431],[-123.969991,45.969139],[-123.957438,45.974469],[-123.941831,45.97566],[-123.937471,45.977306],[-123.927891,46.009564],[-123.92933,46.041978],[-123.933366,46.071672],[-123.947531,46.116131],[-123.95919,46.141675],[-123.974124,46.168798],[-123.996766,46.20399],[-124.010344,46.223514],[-124.024305,46.229256],[-124.011355,46.236223],[-124.001998,46.237316],[-123.998052,46.235327],[-123.988429,46.224132],[-123.990117,46.21763],[-123.987196,46.211521],[-123.982149,46.209662],[-123.961739,46.207916],[-123.950148,46.204097],[-123.927038,46.191617],[-123.912405,46.17945],[-123.9042,46.169293],[-123.891186,46.164778],[-123.854801,46.157342],[-123.842849,46.160529],[-123.841521,46.169824],[-123.863347,46.18235],[-123.866643,46.187674],[-123.864209,46.189527],[-123.838801,46.192211],[-123.821834,46.190293],[-123.793936,46.196283],[-123.759976,46.2073],[-123.736747,46.200687],[-123.71278,46.198751],[-123.706667,46.199665],[-123.67538,46.212401],[-123.673831,46.215418],[-123.666751,46.218228],[-123.65539,46.217974],[-123.636474,46.214359],[-123.6325,46.216681],[-123.626247,46.226434],[-123.625219,46.233868],[-123.622812,46.23664],[-123.613459,46.239228],[-123.605487,46.2393],[-123.60019,46.234814],[-123.586205,46.228654],[-123.548194,46.248245],[-123.547659,46.259109],[-123.538092,46.26061],[-123.526391,46.263404],[-123.501245,46.271004],[-123.479644,46.269131],[-123.474844,46.267831],[-123.468743,46.264531],[-123.447592,46.249832],[-123.427629,46.229348],[-123.430847,46.181827],[-123.371433,46.146372],[-123.332335,46.146132],[-123.301034,46.144632],[-123.280166,46.144843],[-123.251233,46.156452],[-123.231196,46.16615],[-123.166414,46.188973],[-123.115904,46.185268],[-123.105021,46.177676],[-123.051064,46.153599],[-123.041297,46.146351],[-123.03382,46.144336],[-123.022147,46.13911],[-123.009436,46.136043],[-123.004233,46.133823],[-122.962681,46.104817],[-122.904119,46.083734],[-122.884478,46.06028],[-122.878092,46.031281],[-122.856158,46.014469],[-122.837638,45.98082],[-122.813998,45.960984],[-122.806193,45.932416],[-122.81151,45.912725],[-122.798091,45.884333],[-122.785026,45.867699],[-122.785696,45.844216],[-122.795963,45.825024],[-122.795605,45.81],[-122.769532,45.780583],[-122.761451,45.759163],[-122.760108,45.734413],[-122.772511,45.699637],[-122.774511,45.680437],[-122.76381,45.657138],[-122.738109,45.644138],[-122.713309,45.637438],[-122.691008,45.624739],[-122.675008,45.618039],[-122.643907,45.609739],[-122.602606,45.607639],[-122.581406,45.60394],[-122.548149,45.596768],[-122.523668,45.589632],[-122.492259,45.583281],[-122.479315,45.579761],[-122.474659,45.578305],[-122.453891,45.567313],[-122.438674,45.563585],[-122.410706,45.567633],[-122.391802,45.574541],[-122.380302,45.575941],[-122.352802,45.569441],[-122.331502,45.548241],[-122.294901,45.543541],[-122.266701,45.543841],[-122.262625,45.544321],[-122.248993,45.547745],[-122.2017,45.564141],[-122.183695,45.577696],[-122.14075,45.584508],[-122.112356,45.581409],[-122.101675,45.583516],[-122.044374,45.609516],[-122.022571,45.615151],[-122.00369,45.61593],[-121.983038,45.622812],[-121.963547,45.632784],[-121.955734,45.643559],[-121.951838,45.644951],[-121.935149,45.644169],[-121.922236,45.649083]]]},\"properties\":{\"name\":\"Oregon\",\"nation\":\"USA  \"}}]}","volume":"61","issue":"3","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a54e4b07f02db62c232","contributors":{"authors":[{"text":"Henny, Charles J.","contributorId":12578,"corporation":false,"usgs":true,"family":"Henny","given":"Charles","email":"","middleInitial":"J.","affiliations":[],"preferred":false,"id":334218,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Collins, J.A.","contributorId":72412,"corporation":false,"usgs":true,"family":"Collins","given":"J.A.","email":"","affiliations":[],"preferred":false,"id":334219,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":22555,"text":"ofr80703 - 1980 - Seismic engineering data report; the Imperial Valley earthquake, October 15, 1979: Digitization and processing of accelerograph records","interactions":[],"lastModifiedDate":"2022-12-09T21:09:03.777968","indexId":"ofr80703","displayToPublicDate":"1980-01-01T00:00:00","publicationYear":"1980","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":330,"text":"Open-File Report","code":"OFR","onlineIssn":"2331-1258","printIssn":"0196-1497","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"80-703","title":"Seismic engineering data report; the Imperial Valley earthquake, October 15, 1979: Digitization and processing of accelerograph records","docAbstract":"<p>No abstract available.</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr80703","usgsCitation":"Brady, A., Perez, V., and Mork, P.N., 1980, Seismic engineering data report; the Imperial Valley earthquake, October 15, 1979: Digitization and processing of accelerograph records: U.S. Geological Survey Open-File Report 80-703, 311 p., https://doi.org/10.3133/ofr80703.","productDescription":"311 p.","costCenters":[],"links":[{"id":410229,"rank":2,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_75277.htm","linkFileType":{"id":5,"text":"html"}},{"id":52045,"rank":1,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1980/0703/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":154421,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1980/0703/report-thumb.jpg"}],"country":"United States","state":"California","otherGeospatial":"Central Valley","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"coordinates\": [\n          [\n            [\n              -115.8,\n              33.25\n            ],\n            [\n              -115.8,\n              32.667\n            ],\n            [\n              -115.3083,\n              32.667\n            ],\n            [\n              -115.3083,\n              33.25\n            ],\n            [\n              -115.8,\n              33.25\n            ]\n          ]\n        ],\n        \"type\": \"Polygon\"\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a0ae4b07f02db5fb898","contributors":{"authors":[{"text":"Brady, A. G.","contributorId":61794,"corporation":false,"usgs":true,"family":"Brady","given":"A. G.","affiliations":[],"preferred":false,"id":188460,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Perez, Virgilio","contributorId":37740,"corporation":false,"usgs":true,"family":"Perez","given":"Virgilio","email":"","affiliations":[],"preferred":false,"id":188459,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Mork, P. N.","contributorId":33309,"corporation":false,"usgs":true,"family":"Mork","given":"P.","email":"","middleInitial":"N.","affiliations":[],"preferred":false,"id":188458,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":70175065,"text":"70175065 - 1980 - Calculation of estuarine residual currents using the finite element method","interactions":[],"lastModifiedDate":"2016-07-27T16:13:28","indexId":"70175065","displayToPublicDate":"1980-01-01T00:00:00","publicationYear":"1980","noYear":false,"publicationType":{"id":24,"text":"Conference Paper"},"publicationSubtype":{"id":19,"text":"Conference Paper"},"title":"Calculation of estuarine residual currents using the finite element method","docAbstract":"<p>No abstract available.</p>","largerWorkType":{"id":4,"text":"Book"},"largerWorkTitle":"Third International Conference on Finite Elements in Flow Problems","largerWorkSubtype":{"id":12,"text":"Conference publication"},"conferenceTitle":"Third International Conference on Finite Elements in Flow Problems","language":"English","usgsCitation":"Walters, R.A., and Cheng, R.T., 1980, Calculation of estuarine residual currents using the finite element method, <i>in</i> Third International Conference on Finite Elements in Flow Problems, v. 2, p. 6-69.","productDescription":"64 p.","startPage":"6","endPage":"69","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[{"id":552,"text":"San Francisco Bay-Delta","active":false,"usgs":true},{"id":5079,"text":"Pacific Regional Director's Office","active":true,"usgs":true}],"links":[{"id":325750,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"2","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"5799db3ce4b0589fa1c7e73e","contributors":{"authors":[{"text":"Walters, R. A.","contributorId":34174,"corporation":false,"usgs":true,"family":"Walters","given":"R.","email":"","middleInitial":"A.","affiliations":[],"preferred":false,"id":643753,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Cheng, R. T.","contributorId":23138,"corporation":false,"usgs":false,"family":"Cheng","given":"R.","email":"","middleInitial":"T.","affiliations":[],"preferred":false,"id":643754,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":70174409,"text":"70174409 - 1980 - Accuracy of an estuarine hydrodynamic model using smooth elements","interactions":[],"lastModifiedDate":"2018-02-05T12:30:47","indexId":"70174409","displayToPublicDate":"1980-01-01T00:00:00","publicationYear":"1980","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":3722,"text":"Water Resources Research","onlineIssn":"1944-7973","printIssn":"0043-1397","active":true,"publicationSubtype":{"id":10}},"title":"Accuracy of an estuarine hydrodynamic model using smooth elements","docAbstract":"<p><span>A finite element model which uses triangular, isoparametric elements with quadratic basis functions for the two velocity components and linear basis functions for water surface elevation is used in the computation of shallow water wave motions. Specifically addressed are two common uncertainties in this class of two-dimensional hydrodynamic models: the treatment of the boundary conditions at open boundaries and the treatment of lateral boundary conditions. The accuracy of the models is tested with a set of numerical experiments in rectangular and curvilinear channels with constant and variable depth. The results indicate that errors in velocity at the open boundary can be significant when boundary conditions for water surface elevation are specified. Methods are suggested for minimizing these errors. The results also show that continuity is better maintained within the spatial domain of interest when &lsquo;smooth&rsquo; curve-sided elements are used at shoreline boundaries than when piecewise linear boundaries are used. Finally, a method for network development is described which is based upon a continuity criterion to gauge accuracy. A finite element network for San Francisco Bay, California, is used as an example.</span></p>","language":"English","publisher":"American Geophysical Union","doi":"10.1029/WR016i001p00187","usgsCitation":"Walters, R.A., and Cheng, R.T., 1980, Accuracy of an estuarine hydrodynamic model using smooth elements: Water Resources Research, v. 16, no. 1, p. 187-195, https://doi.org/10.1029/WR016i001p00187.","productDescription":"9 p.","startPage":"187","endPage":"195","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[{"id":552,"text":"San Francisco Bay-Delta","active":false,"usgs":true},{"id":5079,"text":"Pacific Regional Director's Office","active":true,"usgs":true}],"links":[{"id":325055,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United States","state":"California","otherGeospatial":"San Francisco Bay","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -123.3544921875,\n              37.19533058280065\n            ],\n            [\n              -121.17919921875001,\n              37.19533058280065\n            ],\n            [\n              -121.17919921875001,\n              38.453588708941375\n            ],\n            [\n              -123.3544921875,\n              38.453588708941375\n            ],\n            [\n              -123.3544921875,\n              37.19533058280065\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","volume":"16","issue":"1","noUsgsAuthors":false,"publicationDate":"2010-07-09","publicationStatus":"PW","scienceBaseUri":"5784c335e4b0e02680be58f0","contributors":{"authors":[{"text":"Walters, Roy A.","contributorId":74877,"corporation":false,"usgs":true,"family":"Walters","given":"Roy","email":"","middleInitial":"A.","affiliations":[],"preferred":false,"id":642144,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Cheng, Ralph T.","contributorId":69134,"corporation":false,"usgs":true,"family":"Cheng","given":"Ralph","email":"","middleInitial":"T.","affiliations":[],"preferred":false,"id":642145,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":70174358,"text":"70174358 - 1980 - Studies of San Francisco Bay by the U.S. Geological Survey","interactions":[],"lastModifiedDate":"2016-07-26T16:38:52","indexId":"70174358","displayToPublicDate":"1980-01-01T00:00:00","publicationYear":"1980","noYear":false,"publicationType":{"id":24,"text":"Conference Paper"},"publicationSubtype":{"id":19,"text":"Conference Paper"},"title":"Studies of San Francisco Bay by the U.S. Geological Survey","docAbstract":"<p>No abstract available&nbsp;</p>","largerWorkType":{"id":24,"text":"Conference Paper"},"largerWorkTitle":"Proceedings, 26th annual meeting of the institute of environmental sciences","conferenceTitle":"26th annual meeting of the institute of environmental sciences","conferenceLocation":"Philadelphia, Penn.","language":"English","usgsCitation":"Cheng, R.T., and Conomos, T.J., 1980, Studies of San Francisco Bay by the U.S. Geological Survey, <i>in</i> Proceedings, 26th annual meeting of the institute of environmental sciences, Philadelphia, Penn., p. 299-303.","productDescription":"5 p.","startPage":"299","endPage":"303","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[{"id":552,"text":"San Francisco Bay-Delta","active":false,"usgs":true},{"id":5079,"text":"Pacific Regional Director's Office","active":true,"usgs":true}],"links":[{"id":324976,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"5780cebfe4b08116168223c8","contributors":{"authors":[{"text":"Cheng, R. T.","contributorId":23138,"corporation":false,"usgs":false,"family":"Cheng","given":"R.","email":"","middleInitial":"T.","affiliations":[],"preferred":false,"id":642014,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Conomos, T. J.","contributorId":77515,"corporation":false,"usgs":true,"family":"Conomos","given":"T.","email":"","middleInitial":"J.","affiliations":[],"preferred":false,"id":642015,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":70174181,"text":"70174181 - 1980 - Toxicity of five forest insecticides to cutthroat trout and two species of aquatic invertebrates","interactions":[],"lastModifiedDate":"2017-01-03T11:03:24","indexId":"70174181","displayToPublicDate":"1980-01-01T00:00:00","publicationYear":"1980","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":"Toxicity of five forest insecticides to cutthroat trout and two species of aquatic invertebrates","docAbstract":"<p>The Northern Rocky Mountain region has had scattered infestation of the western spruce budworm <i>Christoneura occidentalis</i> since the early 1900's (U.S. DEPARTMENT OF AGRICULTURE (USDA) 1976b). On the basis of aerial surveys in 1975, TUNNOCK et al. (1976), estimated that budworm defoliation occurred on 2,278,804 acres of six National Forests in Montana. Since the use of DDT was banned in 1972, there has been a need to develop alternative insecticides with the efficacy of DDT but without its environmental risk. These insecticides must be effective in controlling the budworm, but should not persist in the environment or be toxic to other organisms. The organophosphate and carbamate insecticides are relatively nonpersistent and generally present only a moderate hazard to fish when applied according to label recommendations. The USDA Forest Service has been investigating the effectiveness of these two classes of insecticides against the budworm, and the Columbia National Fisheries Research Laboratory of the U.S. Fish and Wildlife Service has been cooperating with the Forest Service conducted pilot control projects in eastern Montana in 1975 and 1976 to determine the efficacy and environmental impact of acephate, carbaryl, and trichlorfon in controlling the western budworm (USDA 1976 b). In 1975, a similar type project was carried out in Maine with aminocarb, fenitrothion, and trichlorfon (USDA 1976 a).</p><p>Acephate, fenitrothion, and trichlorfon (organophosphate insecticides) and aminocarb and carbaryl (carbamate insecticides) were selected for toxicity tests against cutthroat trout (<i>Salmo clarki</i>), a stonefly (<i>Pteronarcella badia</i>), and a freshwater amphipod (<i>Gammarus</i> <i>pseudolimnaeus</i>) edemic in streams of the northern Rocky Mountains. Populations of cutthroat trout inhabit lakes and streams in the Rocky Mountains which include some of the most pristine habitat and fisheries in North America. <i>Pteronarcella</i> and <i>Gammarus</i> provide forage for cutthroat trout and feed on decaying vegetation in riffle areas in streams and rivers. Stonefly naiads and amphipods were selected as test organisms because of their importance as trout food and their wide distribution in mountain stream communities. We determined the effect of various water types representing different biogeographical areas in the Intermountain West on the toxicity of these five forest insecticides.</p>","language":"English","publisher":"Springer-Verlag","doi":"10.1007/BF01985619","usgsCitation":"Woodward, D.F., and Mauck, W., 1980, Toxicity of five forest insecticides to cutthroat trout and two species of aquatic invertebrates: Bulletin of Environmental Contamination and Toxicology, v. 25, no. 1, p. 846-854, https://doi.org/10.1007/BF01985619.","productDescription":"9 p.","startPage":"846","endPage":"854","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[{"id":192,"text":"Columbia Environmental Research Center","active":true,"usgs":true}],"links":[{"id":324572,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"25","issue":"1","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"57739fb8e4b07657d1a90d9b","contributors":{"authors":[{"text":"Woodward, D. F.","contributorId":85645,"corporation":false,"usgs":true,"family":"Woodward","given":"D.","email":"","middleInitial":"F.","affiliations":[],"preferred":false,"id":641159,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Mauck, W.L.","contributorId":36100,"corporation":false,"usgs":true,"family":"Mauck","given":"W.L.","email":"","affiliations":[],"preferred":false,"id":641160,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":70170528,"text":"70170528 - 1980 - Girl Scouts promote earthquake awareness","interactions":[],"lastModifiedDate":"2016-04-24T12:10:35","indexId":"70170528","displayToPublicDate":"1980-01-01T00:00:00","publicationYear":"1980","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":"Girl Scouts promote earthquake awareness","language":"English","publisher":"U.S Geological Survey","usgsCitation":"Campbell, C., 1980, Girl Scouts promote earthquake awareness: Earthquake Information Bulletin (USGS), v. 12, no. 5, p. 177-180.","productDescription":"4 p.","startPage":"177","endPage":"180","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[],"links":[{"id":320474,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"12","issue":"5","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"571dee2be4b071321fe563ff","contributors":{"authors":[{"text":"Campbell, C.","contributorId":168864,"corporation":false,"usgs":false,"family":"Campbell","given":"C.","affiliations":[],"preferred":false,"id":627530,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":70170536,"text":"70170536 - 1980 - Mount St. Helens Volcano","interactions":[],"lastModifiedDate":"2016-04-24T12:29:09","indexId":"70170536","displayToPublicDate":"1980-01-01T00:00:00","publicationYear":"1980","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":"Mount St. Helens Volcano","language":"English","publisher":"U.S Geological Survey","usgsCitation":"Crandell, D.R., and Mullineaux, D.R., 1980, Mount St. Helens Volcano: Earthquake Information Bulletin (USGS), v. 12, no. 4, p. 135-140.","productDescription":"6 p.","startPage":"135","endPage":"140","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[],"links":[{"id":320482,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"12","issue":"4","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"571dee2ce4b071321fe5640f","contributors":{"authors":[{"text":"Crandell, D. R.","contributorId":78385,"corporation":false,"usgs":true,"family":"Crandell","given":"D.","email":"","middleInitial":"R.","affiliations":[],"preferred":false,"id":627539,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Mullineaux, D. R.","contributorId":64248,"corporation":false,"usgs":true,"family":"Mullineaux","given":"D.","email":"","middleInitial":"R.","affiliations":[],"preferred":false,"id":627540,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":70030385,"text":"70030385 - 1980 - The nature of fracturing and stress distribution in quartzite around the 1128-M (3700-FT) level of the crescent mine, Coeur d'Alene mining district, Idaho","interactions":[],"lastModifiedDate":"2012-03-12T17:21:03","indexId":"70030385","displayToPublicDate":"1980-01-01T00:00:00","publicationYear":"1980","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1517,"text":"Engineering Geology","active":true,"publicationSubtype":{"id":10}},"title":"The nature of fracturing and stress distribution in quartzite around the 1128-M (3700-FT) level of the crescent mine, Coeur d'Alene mining district, Idaho","docAbstract":"Silver and copper are the principal ores mined from the quartzite at the Crescent mine. Both the main ore-bearing veins and foliation in the quartzite are parallel to the nearly vertical formational contacts. Anisotropy of the quartzite is indicated by both dynamic and static tests. Disking and breakage of core from holes perpendicular to the foliation are about twice what they are in core from holes parallel to foliation. Natural cleavage as well as slabbing and blasting fractures around the tunnels are also controlled by the foliation. Extensive overcore deformation measurements indicate that most of the influence of the tunnels on the \"free\" stress field is between the rib and a depth of 2.7 m (1 tunnel diameter). The maximum principal stress axis in the free field is nearly horizontal; its magnitude is not much greater than the vertical component and calculations indicate a nearly hydrostatic free stress field. Stress considerably greater than the free field was measured between about 0.3-2.7 m behind the rib and is caused by a transfer of load from above the tunnel opening. Peak stress is in the vertical direction and about 1.7 m behind the rib. An air-injection survey shows that high permeabilities are confined to the highly fractured annulus around a tunnel to a depth of at least 0.6 m. Air-injection measurements could be taken in the interval of about 0.6-1.8 m, but more fractures with high permeabilities may also be present in the annulus from about 0.6-1.2 m. Permeabilities measured deeper than about 1.8 m by the air-injection technique are either very low or nonexistent. The absence of open and noncontinuous fractures beyond about 1.8 m is also indicated by very low porosities and permeabilities of core, very high stresses (which presumably would close fractures), the lack of stains or secondary fillings in disking fractures, a conspicuous lack of ground water in the tunnels, and the fact that fractures encountered in an experimental 0.9-m tunnel did not extend into the 1.8-m tunnel that was mined over it. Air-injection techniques exceed the accuracy of any field deformation measurement now in use, and they are sensitive to permeabilities as small as one microdarcy and to fracture widths as small as 250 nanometers. This technique was applied for future reference in mining design and, perhaps, to be used later to detect microfracturing prior to rockbursts. ?? 1980 Elsevier Scientific Publishing Company.","largerWorkType":{"id":2,"text":"Article"},"largerWorkTitle":"Engineering Geology","largerWorkSubtype":{"id":10,"text":"Journal Article"},"language":"English","doi":"10.1016/0013-7952(80)90021-6","issn":"00137","usgsCitation":"Miller, C., and Skinner, E., 1980, The nature of fracturing and stress distribution in quartzite around the 1128-M (3700-FT) level of the crescent mine, Coeur d'Alene mining district, Idaho: Engineering Geology, v. 16, no. 3-4, p. 321-338, https://doi.org/10.1016/0013-7952(80)90021-6.","startPage":"321","endPage":"338","numberOfPages":"18","costCenters":[],"links":[{"id":239302,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"},{"id":211921,"rank":9999,"type":{"id":10,"text":"Digital Object Identifier"},"url":"https://dx.doi.org/10.1016/0013-7952(80)90021-6"}],"volume":"16","issue":"3-4","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"505bae04e4b08c986b323eb9","contributors":{"authors":[{"text":"Miller, C.H.","contributorId":19148,"corporation":false,"usgs":true,"family":"Miller","given":"C.H.","email":"","affiliations":[],"preferred":false,"id":426948,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Skinner, E.H.","contributorId":31978,"corporation":false,"usgs":true,"family":"Skinner","given":"E.H.","email":"","affiliations":[],"preferred":false,"id":426949,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":70171194,"text":"70171194 - 1980 - Food of alewives, yellow perch, spottail shiners, trout-perch, and slimy and fourhorn sculpins in southeastern Lake Michigan","interactions":[],"lastModifiedDate":"2016-05-25T13:21:32","indexId":"70171194","displayToPublicDate":"1980-01-01T00:00:00","publicationYear":"1980","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":1,"text":"Federal Government Series"},"seriesNumber":"98","subseriesTitle":"Technical papers of the U.S. Fish and Wildlife Service","title":"Food of alewives, yellow perch, spottail shiners, trout-perch, and slimy and fourhorn sculpins in southeastern Lake Michigan","docAbstract":"<p>Stomachs of 1, 064 alewives (<i>Alosa pseudoharengus</i>), 1, 103 yellow perch (<i>Perca flavescens</i>), 246 spottail shiners (<i>Notropis hudsonius</i>), 288 trout-perch (<i>Percopsis omiscomaycus</i>), 454 slimy sculpins (<i>Cottus cognatus</i>), and 562 fourhorn sculpins (<i>Myoxocephalus quadricornis</i>) from Lake Michigan were examined for food contents. Fish were sampled primarily from March to November and nearly all were caught at the bottom in the southeastern part of the lake near Saugatuck, Michigan. Depths of capture (m) were: alewives, 5 to 110; yellow perch, 5 to 26; spottail shiners, 5 to 31; trout-perch, 9 to 46; slimy sculpins, 31 to 91; and fourhorn sculpins, 73 to 110. Alewives, particularly those less than 140 mm long, fed chiefly on zooplankton;<span>&nbsp;</span><i>Pontoporeia</i><span>&nbsp;</span>usually constituted most of the rest of the food, although<span>&nbsp;</span><i>Mysis</i><span>&nbsp;</span>and immature midges were occasionally eaten in considerable quantity. Yellow perch ate primarily<span>&nbsp;</span><i>Pontoporeia</i>, fish eggs,<span>&nbsp;</span><i>Mysis</i>, and crayfish;<span>&nbsp;</span><i>Pontoporeia</i>was consumed most heavily by perch less than 250 mm long and those in relatively deep water, fish (mainly slimy sculpins) by those 200 mm long or longer, Mysis by those in deep water, and crayfish by those on rocky bottom. Spottail shiners fed most commonly on immature midges,<span>&nbsp;</span><i>Pontoporeia</i>, zooplankton, fingernail clams, and (in July only) fish eggs; immature midges were eaten mainly by shiners in shallow&nbsp;water; and<span>&nbsp;</span><i>Pontoporeia</i><span>&nbsp;</span>by those in deeper areas. The diet of trout-perch was strongly dominated by<span>&nbsp;</span><i>Pontoporeia</i><span>&nbsp;</span>and immature midges. Slimy sculpins ate<span>&nbsp;</span><i>Pontoporeia</i><span>&nbsp;</span>almost exclusively. Fourhorn sculpins fed almost entirely on<span>&nbsp;</span><i>Mysis and</i><span><i>&nbsp;</i></span><i>Pontoporeia</i><span><i>&nbsp;</i></span><i>Pontoporeia</i><span><i>&nbsp;</i></span><i>was particularly important in the diet of the larger fish.</i></p>","language":"English","publisher":"U.S. Fish and Wildlife Service","usgsCitation":"Wells, L., 1980, Food of alewives, yellow perch, spottail shiners, trout-perch, and slimy and fourhorn sculpins in southeastern Lake Michigan, 12 p.","productDescription":"12 p.","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[{"id":324,"text":"Great Lakes Science Center","active":true,"usgs":true}],"links":[{"id":321648,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"5746ccb9e4b07e28b662dcb7","contributors":{"authors":[{"text":"Wells, LaRue","contributorId":75476,"corporation":false,"usgs":true,"family":"Wells","given":"LaRue","email":"","affiliations":[],"preferred":false,"id":630242,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":70171195,"text":"70171195 - 1980 - Chlorinated hydrocarbons as a limiting factor in the reproduction of lake trout in Lake Michigan","interactions":[],"lastModifiedDate":"2016-05-25T13:25:23","indexId":"70171195","displayToPublicDate":"1980-01-01T00:00:00","publicationYear":"1980","noYear":false,"publicationType":{"id":24,"text":"Conference Paper"},"publicationSubtype":{"id":19,"text":"Conference Paper"},"title":"Chlorinated hydrocarbons as a limiting factor in the reproduction of lake trout in Lake Michigan","docAbstract":"<p>No abstract available.</p>","largerWorkType":{"id":24,"text":"Conference Paper"},"largerWorkTitle":"Proceedings of the third USA-USSR Symposium on the Effects of Pollutants Upon Aquatic Ecosystems : theoretical aspects of aquatic toxicology","largerWorkSubtype":{"id":19,"text":"Conference Paper"},"conferenceTitle":"Third USA-USSR Symposium on the Effects of Pollutants Upon Aquatic Ecosystems","conferenceDate":"July 2-6, 1979","conferenceLocation":"Borok, Jaroslav Oblast, USSR","language":"English","publisher":"U.S. Environmental Protection Agency","usgsCitation":"Willford, W.A., 1980, Chlorinated hydrocarbons as a limiting factor in the reproduction of lake trout in Lake Michigan, <i>in</i> Proceedings of the third USA-USSR Symposium on the Effects of Pollutants Upon Aquatic Ecosystems : theoretical aspects of aquatic toxicology, Borok, Jaroslav Oblast, USSR, July 2-6, 1979, p. 75-83.","productDescription":"9 p.","startPage":"75","endPage":"83","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[{"id":324,"text":"Great Lakes Science Center","active":true,"usgs":true}],"links":[{"id":321649,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"5746ccb2e4b07e28b662dc50","contributors":{"authors":[{"text":"Willford, Wayne A.","contributorId":67446,"corporation":false,"usgs":true,"family":"Willford","given":"Wayne","email":"","middleInitial":"A.","affiliations":[],"preferred":false,"id":630243,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":70012397,"text":"70012397 - 1980 - Degradation of the Hebgen Lake fault scarps of 1959","interactions":[],"lastModifiedDate":"2024-02-01T12:15:46.343785","indexId":"70012397","displayToPublicDate":"1980-01-01T00:00:00","publicationYear":"1980","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1796,"text":"Geology","active":true,"publicationSubtype":{"id":10}},"title":"Degradation of the Hebgen Lake fault scarps of 1959","docAbstract":"<div id=\"15739534\" class=\"article-section-wrapper js-article-section js-content-section  \" data-section-parent-id=\"0\"><p>Scarps produced during the Hebgen Lake earthquake of 1959 changed noticeably in 19 yr although they still appeared remarkably fresh in 1978. They have degraded much more rapidly than have those produced in 1915 and 1954 in Nevada, but a quasi-stable slope of more than 40° characterizes the Hebgen Lake scarps as compared to an upper limit of 37° on the Nevada scarps.</p></div>","language":"English","publisher":"Geological Society of America","doi":"10.1130/0091-7613(1980)8<225:DOTHLF>2.0.CO;2","issn":"00917613","usgsCitation":"Wallace, R., 1980, Degradation of the Hebgen Lake fault scarps of 1959: Geology, v. 8, no. 5, p. 225-229, https://doi.org/10.1130/0091-7613(1980)8<225:DOTHLF>2.0.CO;2.","productDescription":"5 p.","startPage":"225","endPage":"229","numberOfPages":"5","costCenters":[],"links":[{"id":222535,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"8","issue":"5","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"5059fe57e4b0c8380cd4ecb2","contributors":{"authors":[{"text":"Wallace, R.W.","contributorId":103795,"corporation":false,"usgs":true,"family":"Wallace","given":"R.W.","email":"","affiliations":[],"preferred":false,"id":363444,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":70012111,"text":"70012111 - 1980 - Crystallization history of Kilauea Iki lava lake as seen in drill core recovered in 1967-1979","interactions":[],"lastModifiedDate":"2012-03-12T17:19:05","indexId":"70012111","displayToPublicDate":"1980-01-01T00:00:00","publicationYear":"1980","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1093,"text":"Bulletin Volcanologique","active":true,"publicationSubtype":{"id":10}},"title":"Crystallization history of Kilauea Iki lava lake as seen in drill core recovered in 1967-1979","docAbstract":"Kilauea Iki lava lake formed during the 1959 summit eruption, one of the most picritic eruptions of Kilauea Volcano in the twentieth century. Since 1959 the 110 to 122 m thick lake has cooled slowly, developing steadily thickening upper and lower crusts, with a lens of more molten lava in between. Recent coring dates, with maximum depths reached in the center of the lake, are: 1967 (26.5 m). 1975 (44.2 m), 1976 (46.0 m) and 1979 (52.7 m). These depths define the base of the upper crust at the time of drilling. The bulk of the core consists of a gray, olivine-phyric basalt matrix, which locally contains coarser-grained diabasic segregation veins. The most important megascopic variation in the matrix rock is its variation in olivine content. The upper 15 m of crust is very olivine-rich. Abundance and average size of olivine decrease irregularly downward to 23 m; between 23 and 40 m the rock contains 5-10% of small olivine phenocrysts. Below 40 m. olivine content and average grainsize rise sharply. Olivine contents remain high (20-45%, by volume) throughout the lower crust, except for a narrow (< 6 m) olivine depleted zone near the basalt contact. Petrographically the olivine phenocrysts in Kilauea Iki can be divided into two types. Type 1 phenocrysts are large (1-12 mm long), with irregular blocky outlines, and often contain kink bands. Type 2 crystals are relatively small (0.5-2 mm in length), euhedral and undeformed. The variations in olivine content of the matrix rock are almost entirely variations in the amount of type 1 olivines. Sharp mineral layering of any sort is rare in Kilauea Iki. However, the depth range 41-52 m is marked by the frequent occurrence of steeply dipping (70??-90??) bands or bodies of slightly vuggy olivine-rich rock locally capped with a small cupola of segregation-vein material. In thin section there is clear evidence for relative movement of melt and crystals within these structures. The segregation veins occur only in the upper crust. The most widely distributed (occurring from 4.5-59.4 m) are thin veins (most < 5 cm thick), which cut the core at moderate angles and appear to have been derived from the immediately adjacent wall-rock by filter pressing. There is also a series of thicker (0.1-1.5 m) segregation veins, which recur every 2-3 m, between 20 and 52 m. These have subhorizontal contacts and appear, from similarities in thickness and spacing, to correlate between drill holes as much as 100 m apart. These large veins are not derived from the adjacent wallrock: their mechanism of formation is still problematical. The total thickness of segregation veins in Kilauea Iki is 3-6 m in the central part of the lake, corresponding to 6-11% of the upper crust. Whole-rock compositions for Kilauea Iki fall into two groups: the matrix rock ranges from 20-7.5% MgO, while the segregation veins all contain between 6.0 and 4.5% MgO. There are no whole-rock compositions of intermediate MgO content. Samples from < 12 m show eruption-controlled chemistry. Below that depth, matrix rock compositions have higher Al2O3, TiO2 and alkalies, and lower CaO and FeO, at a given MgO content than do the eruption pumices. The probable causes of this are assimilation of low-melting components from foundered crust, plus removal of olivine, plus removal of minor augite, for rocks with MgO contents of < 8.0%. Given the observed rate of growth of the upper crust, one can infer that significant removal of the type 1 olivine phenocrysts from the upper part of the lake began in 1963 and ceased sometime prior to 1972. The process. probably gravitative settling, appears to have been inhibited earlier by gas streaming from the lower part of the lens of melt. The olivine cumulate zone, which extends into the upper crust, contains relatively few (25-40%) olivine crystals, few of which actually touch each other. The diffuseness of the cumulate zone raises the possibility that the crystals were coated with a relatively visous boundary layer","largerWorkType":{"id":2,"text":"Article"},"largerWorkTitle":"Bulletin Volcanologique","largerWorkSubtype":{"id":10,"text":"Journal Article"},"language":"English","publisherLocation":"Springer-Verlag","doi":"10.1007/BF02600365","issn":"0366483X","usgsCitation":"Helz, R., 1980, Crystallization history of Kilauea Iki lava lake as seen in drill core recovered in 1967-1979: Bulletin Volcanologique, v. 43, no. 4, p. 675-701, https://doi.org/10.1007/BF02600365.","startPage":"675","endPage":"701","numberOfPages":"27","costCenters":[],"links":[{"id":205176,"rank":9999,"type":{"id":10,"text":"Digital Object Identifier"},"url":"https://dx.doi.org/10.1007/BF02600365"},{"id":221991,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"43","issue":"4","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"5059fd01e4b0c8380cd4e590","contributors":{"authors":[{"text":"Helz, Rosalind Tuthill 0000-0003-1550-0684","orcid":"https://orcid.org/0000-0003-1550-0684","contributorId":16806,"corporation":false,"usgs":true,"family":"Helz","given":"Rosalind Tuthill","affiliations":[{"id":243,"text":"Eastern Geology and Paleoclimate Science Center","active":true,"usgs":true}],"preferred":true,"id":362758,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":70012353,"text":"70012353 - 1980 - Use of altered volcanic ash falls in stratigraphic studies of coal-bearing sequences: an example from the Upper Cretaceous Ferron Sandstone Member of the Mancos Shale in central Utah.","interactions":[],"lastModifiedDate":"2013-02-24T11:49:03","indexId":"70012353","displayToPublicDate":"1980-01-01T00:00:00","publicationYear":"1980","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1786,"text":"Geological Society of America Bulletin","active":true,"publicationSubtype":{"id":10}},"title":"Use of altered volcanic ash falls in stratigraphic studies of coal-bearing sequences: an example from the Upper Cretaceous Ferron Sandstone Member of the Mancos Shale in central Utah.","docAbstract":"The Ferron consists of 5 delta cycles, each of which includes one coal zone which contains at least one, and usually several, laterally persistent kaolinitic claystone partings. Laboratory study of the partings demonstrates that they represent altered volcanic ash falls. These partings have proven particularly useful in reconstructing the depositional history of the C coal bed of the Emery coal field which accumulated in a basin that developed concurrently with subsidence of the delta plain during both the constructive and destructive phases of the third delta cycle.-from Authors","largerWorkType":{"id":2,"text":"Article"},"largerWorkTitle":"Geological Society of America Bulletin","largerWorkSubtype":{"id":10,"text":"Journal Article"},"language":"English","publisher":"Geological Society of America","doi":"10.1130/0016-7606(1980)91<579:UOAVAF>2.0.CO;2","usgsCitation":"Ryer, T., Phillips, R., Bohor, B., and Pollastro, R.M., 1980, Use of altered volcanic ash falls in stratigraphic studies of coal-bearing sequences: an example from the Upper Cretaceous Ferron Sandstone Member of the Mancos Shale in central Utah.: Geological Society of America Bulletin, v. 91, no. 10, p. 579-586, https://doi.org/10.1130/0016-7606(1980)91<579:UOAVAF>2.0.CO;2.","startPage":"579","endPage":"586","numberOfPages":"8","costCenters":[],"links":[{"id":268126,"type":{"id":10,"text":"Digital Object Identifier"},"url":"https://dx.doi.org/10.1130/0016-7606(1980)91<579:UOAVAF>2.0.CO;2"},{"id":221943,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"91","issue":"10","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"505bbeb0e4b08c986b32971d","contributors":{"authors":[{"text":"Ryer, Thomas A.","contributorId":46091,"corporation":false,"usgs":true,"family":"Ryer","given":"Thomas A.","affiliations":[],"preferred":false,"id":363345,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Phillips, R.E.","contributorId":51241,"corporation":false,"usgs":true,"family":"Phillips","given":"R.E.","email":"","affiliations":[],"preferred":false,"id":363346,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Bohor, B.F.","contributorId":96351,"corporation":false,"usgs":true,"family":"Bohor","given":"B.F.","email":"","affiliations":[],"preferred":false,"id":363347,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Pollastro, R. M.","contributorId":6809,"corporation":false,"usgs":true,"family":"Pollastro","given":"R.","email":"","middleInitial":"M.","affiliations":[],"preferred":false,"id":363344,"contributorType":{"id":1,"text":"Authors"},"rank":4}]}}
,{"id":70012393,"text":"70012393 - 1980 - The provenance of rutile.","interactions":[],"lastModifiedDate":"2024-05-22T11:21:22.645154","indexId":"70012393","displayToPublicDate":"1980-01-01T00:00:00","publicationYear":"1980","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":2450,"text":"Journal of Sedimentary Petrology","active":true,"publicationSubtype":{"id":10}},"title":"The provenance of rutile.","docAbstract":"<div><div id=\"12457817\" class=\"article-section-wrapper js-article-section js-content-section  \" data-section-parent-id=\"0\"><p>Most coarse detrital rutile is derived from high-grade metamorphic rocks. Contrary to a conventional assumption, independent rutile grains are particularly rare in igneous rocks except alkalic rocks. The use of rutile in the ZTR (zircon-tourmaline-rutile) index of mineralogic maturity is only partially valid, owing to its restricted provenance.</p></div></div>","language":"English","publisher":"SEPM","doi":"10.1306/212F7A31-2B24-11D7-8648000102C1865D","issn":"00224472","usgsCitation":"Force, E.R., 1980, The provenance of rutile.: Journal of Sedimentary Petrology, v. 50, no. 2, p. 485-488, https://doi.org/10.1306/212F7A31-2B24-11D7-8648000102C1865D.","productDescription":"4 p.","startPage":"485","endPage":"488","numberOfPages":"4","costCenters":[],"links":[{"id":222476,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"50","issue":"2","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"505baed9e4b08c986b3243ad","contributors":{"authors":[{"text":"Force, E. R.","contributorId":28235,"corporation":false,"usgs":true,"family":"Force","given":"E.","email":"","middleInitial":"R.","affiliations":[],"preferred":false,"id":363436,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":70012289,"text":"70012289 - 1980 - The morphology of the Martian surface","interactions":[],"lastModifiedDate":"2012-03-12T17:19:03","indexId":"70012289","displayToPublicDate":"1980-01-01T00:00:00","publicationYear":"1980","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":3454,"text":"Space Science Reviews","active":true,"publicationSubtype":{"id":10}},"title":"The morphology of the Martian surface","docAbstract":"Most of the southern hemisphere of Mars is densely cratered and stands 1-3 km above the topographic datum. The northern hemisphere is more sparsely cratered and elevations are generally below the datum. A broad rise, the Tharsis bulge, centered at 14?? S, 101?? W, is 8000 km across and 10 km above the datum at its summit. The densely cratered terrain has two main components; very ancient crust, nearly saturated with large craters, and younger intercrater plains. In many areas the older unit is fractured and extensively dissected by small channels. The younger intercrater plains are distinctly layered in places and less dissected, less fractured, and less cratered. Both units probably date from very early in the planet's history. Cratered plains cover much of the northern hemisphere and are highly variegated. Those around the large volcanoes are covered with numerous volcanic flows whereas in other areas the plains are featureless except for craters and lunar mare-like ridges. Between 40?? N and 60?? N the plains are complex with various kinds of striped and patterned ground, low escarpments, and isolated irregularly shaped mesas. Their peculiar morphology has been attributed, in part, to the repeated deposition and removal of volatile-rich debris layers. Along the boundary between the northern plains and the densely cratered terrain to the south, the plains and cratered terrain complexly inter-finger. The old terrain forms the high ground and appears to have undergone mass wasting on a large scale. In several areas, particularly south of Chryse Planitia, the old, cratered surface has collapsed to form chaotic terrain. Large channels, tens of kilometers wide and hundreds of kilometers long, with numerous characteristics suggestive of catastrophic flooding, commonly emerge from the chaotic areas. Much of the area between 50?? W and 180?? W and 50?? N and 50?? S is cut by fractures radial to the center of the Tharsis bulge. The equatorial canyon system, Valles Marineris, is radial to the bulge and appears to have formed largely by faulting along the radial fractures, although it has also been extensively modified by various mass wasting and fluvial processes. Most but not all volcanoes are in the Tharsis and Elysium regions. The largest resemble terrestrial shield volcanoes except for scale; the edifices, flow features and calderas are all far larger than their terrestrial counterparts. Most impact craters on Mars are surrounded by layers of ejecta, each with a distil ridge. This unique morphology coupled with other surface characteristics suggests large amounts of ground ice. Layered deposits at both poles appear to be relatively young, volatile-rich, aeolian deposits. The north pole is also surrounded by a continuous belt of dunes several tens of kilometers across. In most other places, aeolian modification of the surface at a scale of several tens of meters appears slight despite annual global dust storms. ?? 1980 D. Reidel Publishing Co.","largerWorkType":{"id":2,"text":"Article"},"largerWorkTitle":"Space Science Reviews","largerWorkSubtype":{"id":10,"text":"Journal Article"},"language":"English","publisherLocation":"Kluwer Academic Publishers","doi":"10.1007/BF00221929","issn":"00386308","usgsCitation":"Carr, M.H., 1980, The morphology of the Martian surface: Space Science Reviews, v. 25, no. 3, p. 231-284, https://doi.org/10.1007/BF00221929.","startPage":"231","endPage":"284","numberOfPages":"54","costCenters":[],"links":[{"id":205254,"rank":9999,"type":{"id":10,"text":"Digital Object Identifier"},"url":"https://dx.doi.org/10.1007/BF00221929"},{"id":222530,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"25","issue":"3","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"505badeee4b08c986b323e74","contributors":{"authors":[{"text":"Carr, M. H.","contributorId":84727,"corporation":false,"usgs":true,"family":"Carr","given":"M.","email":"","middleInitial":"H.","affiliations":[{"id":131,"text":"Astrogeology Science Center","active":true,"usgs":true}],"preferred":false,"id":363192,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":70012232,"text":"70012232 - 1980 - Experimental study of free-surface flow instability and bedforms in shallow flows.","interactions":[],"lastModifiedDate":"2012-03-12T17:19:09","indexId":"70012232","displayToPublicDate":"1980-01-01T00:00:00","publicationYear":"1980","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":3368,"text":"Sedimentary Geology","active":true,"publicationSubtype":{"id":10}},"title":"Experimental study of free-surface flow instability and bedforms in shallow flows.","docAbstract":"To test erosion and development of bed sculpture in unstable, pulsating shallow flow, 3 series of experiments were performed in a 10-m flume with flows of Reynolds Number up to 103, Froude Number up to 3.0, and slope up to 2%. In the first, the bed was rigid, in the second and third series planar beds were made from well-sorted and poorly sorted sand, respectively. Development of flow surface instability above the rigid bed showed the following stages: smooth surface; small wavelets; well-developed waves; and rough flow. The second series showed the following sequence: smooth bed; flow-aligned ridge and trough pattern; combined ridge and rhomboid pattern; and rhomboid configuration. The third series demonstrated transverse segregation of the bed material across the ridges.- from Authors","largerWorkType":{"id":2,"text":"Article"},"largerWorkTitle":"Sedimentary Geology","largerWorkSubtype":{"id":10,"text":"Journal Article"},"language":"English","doi":"10.1016/0037-0738(80)90016-0","issn":"00370738","usgsCitation":"Karcz, I., and Kersey, D., 1980, Experimental study of free-surface flow instability and bedforms in shallow flows.: Sedimentary Geology, v. 27, no. 4, p. 263-300, https://doi.org/10.1016/0037-0738(80)90016-0.","startPage":"263","endPage":"300","numberOfPages":"38","costCenters":[],"links":[{"id":205279,"rank":9999,"type":{"id":10,"text":"Digital Object Identifier"},"url":"https://dx.doi.org/10.1016/0037-0738(80)90016-0"},{"id":222647,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"27","issue":"4","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"505a0de5e4b0c8380cd5323f","contributors":{"authors":[{"text":"Karcz, I.","contributorId":58779,"corporation":false,"usgs":true,"family":"Karcz","given":"I.","email":"","affiliations":[],"preferred":false,"id":363044,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Kersey, D.","contributorId":49112,"corporation":false,"usgs":true,"family":"Kersey","given":"D.","affiliations":[],"preferred":false,"id":363043,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":70012231,"text":"70012231 - 1980 - A three-dimensional model to predict future oil discoveries in spatially connected multiple plays","interactions":[],"lastModifiedDate":"2012-03-12T17:19:09","indexId":"70012231","displayToPublicDate":"1980-01-01T00:00:00","publicationYear":"1980","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":2554,"text":"Journal of the International Association for Mathematical Geology","active":true,"publicationSubtype":{"id":10}},"title":"A three-dimensional model to predict future oil discoveries in spatially connected multiple plays","docAbstract":"A discovery-process model that had been devised previously to estimate the size distribution of oil and gas fields remaining to be discovered in a single producing horizon was adapted to a basin containing spatially connected multiple plays and producing horizons. This model used the concept of the area of influence of wells to estimate search effort. Other variables estimated from the historical drilling and discovery data are the effective basin size and the exploration-drilling efficiency. Data from the Midland Basin are used to illustrate how the model works. ?? 1980 Plenum Publishing Corporation.","largerWorkType":{"id":2,"text":"Article"},"largerWorkTitle":"Journal of the International Association for Mathematical Geology","largerWorkSubtype":{"id":10,"text":"Journal Article"},"language":"English","publisherLocation":"Kluwer Academic Publishers-Plenum Publishers","doi":"10.1007/BF01028880","issn":"00205958","usgsCitation":"Schuenemeyer, J., Drew, L., and Bawiec, W., 1980, A three-dimensional model to predict future oil discoveries in spatially connected multiple plays: Journal of the International Association for Mathematical Geology, v. 12, no. 5, p. 459-472, https://doi.org/10.1007/BF01028880.","startPage":"459","endPage":"472","numberOfPages":"14","costCenters":[],"links":[{"id":205278,"rank":9999,"type":{"id":10,"text":"Digital Object Identifier"},"url":"https://dx.doi.org/10.1007/BF01028880"},{"id":222646,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"12","issue":"5","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"5059e5fee4b0c8380cd470ab","contributors":{"authors":[{"text":"Schuenemeyer, J.H.","contributorId":106094,"corporation":false,"usgs":true,"family":"Schuenemeyer","given":"J.H.","affiliations":[],"preferred":false,"id":363042,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Drew, L.J.","contributorId":69157,"corporation":false,"usgs":true,"family":"Drew","given":"L.J.","email":"","affiliations":[],"preferred":false,"id":363040,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Bawiec, W.J.","contributorId":71540,"corporation":false,"usgs":true,"family":"Bawiec","given":"W.J.","affiliations":[],"preferred":false,"id":363041,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":70012296,"text":"70012296 - 1980 - Comparison of three techniques for the determination of uranium and thorium in rocks","interactions":[],"lastModifiedDate":"2013-01-21T12:35:56","indexId":"70012296","displayToPublicDate":"1980-01-01T00:00:00","publicationYear":"1980","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1213,"text":"Chemical Geology","active":true,"publicationSubtype":{"id":10}},"title":"Comparison of three techniques for the determination of uranium and thorium in rocks","docAbstract":"U and Th concentrations have been determined in a series of selected whole-rock samples, using three different techniques: neutron activation analysis (INAA), X-ray fluorescence spectrometry (XRF) and isotope dilution mass spectrometry (ID). The INAA technique yields U and Th data that are comparable with those obtained by ID over the entire concentration range studied. XRF only provides data with comparable precision at relatively high concentrations (> 10 ppm) but has the advantage of being able to determine other useful elements such as Rb, Sr, Pb and K. The choice between INAA and XRF therefore depends on the concentration levels anticipated, together with the overall requirements for the particular study. ?? 1980.","largerWorkType":{"id":2,"text":"Article"},"largerWorkTitle":"Chemical Geology","largerWorkSubtype":{"id":10,"text":"Journal Article"},"language":"English","publisher":"Elsevier","doi":"10.1016/0009-2541(80)90030-3","issn":"00092541","usgsCitation":"Hart, R.J., Reid, D., Stuckless, J., and Welke, H., 1980, Comparison of three techniques for the determination of uranium and thorium in rocks: Chemical Geology, v. 29, no. 1-4, p. 345-350, https://doi.org/10.1016/0009-2541(80)90030-3.","startPage":"345","endPage":"350","numberOfPages":"6","costCenters":[],"links":[{"id":222649,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"},{"id":266130,"type":{"id":10,"text":"Digital Object Identifier"},"url":"https://dx.doi.org/10.1016/0009-2541(80)90030-3"}],"volume":"29","issue":"1-4","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"5059f8b4e4b0c8380cd4d240","contributors":{"authors":[{"text":"Hart, R. J.","contributorId":62607,"corporation":false,"usgs":true,"family":"Hart","given":"R.","email":"","middleInitial":"J.","affiliations":[],"preferred":false,"id":363208,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Reid, D.L.","contributorId":39524,"corporation":false,"usgs":true,"family":"Reid","given":"D.L.","email":"","affiliations":[],"preferred":false,"id":363207,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Stuckless, J. S.","contributorId":6060,"corporation":false,"usgs":true,"family":"Stuckless","given":"J. S.","affiliations":[],"preferred":false,"id":363205,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Welke, H.J.","contributorId":29572,"corporation":false,"usgs":true,"family":"Welke","given":"H.J.","email":"","affiliations":[],"preferred":false,"id":363206,"contributorType":{"id":1,"text":"Authors"},"rank":4}]}}
,{"id":70012372,"text":"70012372 - 1980 - Geologic history of Grecian Rocks, Key Largo Coral Reef Marine Sanctuary.","interactions":[],"lastModifiedDate":"2012-03-12T17:19:01","indexId":"70012372","displayToPublicDate":"1980-01-01T00:00:00","publicationYear":"1980","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1106,"text":"Bulletin of Marine Science","active":true,"publicationSubtype":{"id":10}},"title":"Geologic history of Grecian Rocks, Key Largo Coral Reef Marine Sanctuary.","docAbstract":"Two transects were drilled across the major ecologic zones of the c. 750 by 200 m reef, whose accumulation was controlled by a local Pleistocene topographic feature. The Reef is composed of 5 major ecologic zones: 1) a deep seaward rubble zone, 6-8 m depth; 2) a poorly developed spur and groove zone composed of massive head corals and Millepora (4-6 m water depth); 3) a characteristic high-energy oriented Acropora palmata zone extending from the surface down to 4 m; 4) a distinct broad reef flat composed of in situ A. palmata and coral rubble, followed by 5) a narrow low- energy back-reef zone of unoriented A. palmata, thickets of A. cervicornis, and various massive head corals in water 0-3 m deep. An extensive grass-covered carbonate sand flat 3-4 m deep extends in a landward direction from zone 5. - from Author","largerWorkType":{"id":2,"text":"Article"},"largerWorkTitle":"Bulletin of Marine Science","largerWorkSubtype":{"id":10,"text":"Journal Article"},"language":"English","issn":"00074977","usgsCitation":"Shinn, E., 1980, Geologic history of Grecian Rocks, Key Largo Coral Reef Marine Sanctuary.: Bulletin of Marine Science, v. 30, no. 3, p. 646-656.","startPage":"646","endPage":"656","numberOfPages":"11","costCenters":[],"links":[{"id":222250,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"30","issue":"3","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"505a197be4b0c8380cd559dd","contributors":{"authors":[{"text":"Shinn, E.A.","contributorId":38610,"corporation":false,"usgs":true,"family":"Shinn","given":"E.A.","email":"","affiliations":[],"preferred":false,"id":363400,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":70012348,"text":"70012348 - 1980 - Some factors controlling the concentration of uranium in the world ocean","interactions":[],"lastModifiedDate":"2024-03-14T15:55:28.413937","indexId":"70012348","displayToPublicDate":"1980-01-01T00:00:00","publicationYear":"1980","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1759,"text":"Geochimica et Cosmochimica Acta","active":true,"publicationSubtype":{"id":10}},"title":"Some factors controlling the concentration of uranium in the world ocean","docAbstract":"<p><span>Low-temperature alteration of the oceanic crust is a major sink for the U supplied to the oceans and may account for about 50% of the estimated present-day input of this element. Uranium uptake by organic-rich sediments and coexisting phosphorites on continental margins is also important and may remove in excess of 10% of the total supply. High-temperature alteration of oceanic basalts, metalliferous sediments, carbonate sediments, and sediments in anoxic basins deeper than 200 m play a relatively minor role in the removal of U. Each of these sinks is responsible for the uptake of less than 5% of the overall input.</span></p>","language":"English","publisher":"Elsevier","doi":"10.1016/0016-7037(80)90145-3","issn":"00167037","usgsCitation":"Bloch, S., 1980, Some factors controlling the concentration of uranium in the world ocean: Geochimica et Cosmochimica Acta, v. 44, no. 2, p. 373-377, https://doi.org/10.1016/0016-7037(80)90145-3.","productDescription":"5 p.","startPage":"373","endPage":"377","numberOfPages":"5","costCenters":[],"links":[{"id":221887,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"44","issue":"2","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"505b92a4e4b08c986b31a02b","contributors":{"authors":[{"text":"Bloch, S.","contributorId":81249,"corporation":false,"usgs":true,"family":"Bloch","given":"S.","email":"","affiliations":[],"preferred":false,"id":363335,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":70012125,"text":"70012125 - 1980 - Mapping the Galilean satellites of Jupiter with Voyager data.","interactions":[],"lastModifiedDate":"2012-03-12T17:19:09","indexId":"70012125","displayToPublicDate":"1980-01-01T00:00:00","publicationYear":"1980","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":3052,"text":"Photogrammetric Engineering and Remote Sensing","active":true,"publicationSubtype":{"id":10}},"title":"Mapping the Galilean satellites of Jupiter with Voyager data.","docAbstract":"The four Galilean satellites of Jupiter are being mapped using image data from the Voyager 1 and 2 spacecraft. The maps are published at several scales and in several versions. Preliminary maps at 1:25,000,000-required for mission planning and preliminary science reports-were compiled within three weeks of data acquisition and have been published. Later maps incorporate Rand Corporation photogrammetric triangulations. - from Authors","largerWorkType":{"id":2,"text":"Article"},"largerWorkTitle":"Photogrammetric Engineering and Remote Sensing","largerWorkSubtype":{"id":10,"text":"Journal Article"},"language":"English","usgsCitation":"Batson, R.M., 1980, Mapping the Galilean satellites of Jupiter with Voyager data.: Photogrammetric Engineering and Remote Sensing, v. 46, no. 10, p. 1303-1312.","startPage":"1303","endPage":"1312","numberOfPages":"10","costCenters":[],"links":[{"id":222237,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"46","issue":"10","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"505a5079e4b0c8380cd6b6ed","contributors":{"authors":[{"text":"Batson, R. M.","contributorId":76714,"corporation":false,"usgs":true,"family":"Batson","given":"R.","email":"","middleInitial":"M.","affiliations":[],"preferred":false,"id":362784,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
]}