{"pageNumber":"5359","pageRowStart":"133950","pageSize":"25","recordCount":184769,"records":[{"id":70221741,"text":"70221741 - 1982 - Late Eocene to early Oligocene calcareous nannofossils in Alabama and Mississippi","interactions":[],"lastModifiedDate":"2021-07-01T12:15:58.442859","indexId":"70221741","displayToPublicDate":"1982-12-31T10:47:07","publicationYear":"1982","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1871,"text":"Gulf Coast Association of Geological Societies Transactions","active":true,"publicationSubtype":{"id":10}},"title":"Late Eocene to early Oligocene calcareous nannofossils in Alabama and Mississippi","docAbstract":"<p>No abstract available.</p>","language":"English","publisher":"Gulf Coast Association of Geological Societies","usgsCitation":"Bybell, L.M., 1982, Late Eocene to early Oligocene calcareous nannofossils in Alabama and Mississippi: Gulf Coast Association of Geological Societies Transactions, v. 32, p. 295-302.","productDescription":"8 p.","startPage":"295","endPage":"302","costCenters":[{"id":243,"text":"Eastern Geology and Paleoclimate Science Center","active":true,"usgs":true}],"links":[{"id":386900,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United States","state":"Alabama, Mississippi","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -87.47314453125,\n              30.32547125932808\n            ],\n            [\n              -87.374267578125,\n              30.675715404167743\n            ],\n            [\n              -87.57202148437499,\n              31.015278981711266\n            ],\n            [\n              -85.02319335937499,\n              31.015278981711266\n            ],\n            [\n              -85.089111328125,\n              31.700129553985924\n            ],\n            [\n              -84.8583984375,\n              32.37996146435729\n            ],\n            [\n              -85.60546875,\n              34.985003130171066\n            ],\n            [\n              -90.252685546875,\n              35.003003395276714\n            ],\n            [\n              -90.867919921875,\n              34.20725938207231\n            ],\n            [\n              -91.153564453125,\n              33.58716733904656\n            ],\n            [\n              -91.12060546875,\n              32.8149783969858\n            ],\n            [\n              -90.999755859375,\n              32.37996146435729\n            ],\n            [\n              -91.58203125,\n              31.25037814985571\n            ],\n            [\n              -91.593017578125,\n              31.034108344903512\n            ],\n            [\n              -89.71435546875,\n              31.034108344903512\n            ],\n            [\n              -89.82421875,\n              30.65681556429287\n            ],\n            [\n              -89.62646484375,\n              30.230594564932193\n            ],\n            [\n              -89.483642578125,\n              30.059585699708215\n            ],\n            [\n              -87.4951171875,\n              30.07860131571654\n            ],\n            [\n              -87.47314453125,\n              30.32547125932808\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","volume":"32","noUsgsAuthors":false,"publicationStatus":"PW","contributors":{"authors":[{"text":"Bybell, Laurel M. 0000-0002-4760-7542 lbybell@usgs.gov","orcid":"https://orcid.org/0000-0002-4760-7542","contributorId":1760,"corporation":false,"usgs":true,"family":"Bybell","given":"Laurel","email":"lbybell@usgs.gov","middleInitial":"M.","affiliations":[{"id":243,"text":"Eastern Geology and Paleoclimate Science Center","active":true,"usgs":true}],"preferred":true,"id":818599,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":70221740,"text":"70221740 - 1982 - Validation of Blackites trochos","interactions":[],"lastModifiedDate":"2021-06-30T15:45:30.633965","indexId":"70221740","displayToPublicDate":"1982-12-31T10:42:32","publicationYear":"1982","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":8947,"text":"INA Newsletter","active":false,"publicationSubtype":{"id":10}},"title":"Validation of Blackites trochos","docAbstract":"<p>No abstract available.</p>","language":"English","publisher":"International Nannoplankton Association","usgsCitation":"Bybell, L.M., 1982, Validation of Blackites trochos: INA Newsletter, v. 4, no. 2.","productDescription":"1 p.","startPage":"101","costCenters":[{"id":243,"text":"Eastern Geology and Paleoclimate Science Center","active":true,"usgs":true}],"links":[{"id":386899,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"},{"id":386898,"rank":1,"type":{"id":15,"text":"Index Page"},"url":"https://ina.tmsoc.org/JNR/NINA/index.htm"}],"volume":"4","issue":"2","noUsgsAuthors":false,"publicationStatus":"PW","contributors":{"authors":[{"text":"Bybell, Laurel M. 0000-0002-4760-7542 lbybell@usgs.gov","orcid":"https://orcid.org/0000-0002-4760-7542","contributorId":1760,"corporation":false,"usgs":true,"family":"Bybell","given":"Laurel","email":"lbybell@usgs.gov","middleInitial":"M.","affiliations":[{"id":243,"text":"Eastern Geology and Paleoclimate Science Center","active":true,"usgs":true}],"preferred":true,"id":818598,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":70221739,"text":"70221739 - 1982 - Biostratigraphy and paleoecology of lower Paleozoic, upper Cretaceous, and lower Tertiary rocks in U.S. Geological Survey New Madrid test wells, Southeastern Missouri","interactions":[],"lastModifiedDate":"2021-06-30T15:40:45.034309","indexId":"70221739","displayToPublicDate":"1982-12-31T10:29:07","publicationYear":"1982","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":8946,"text":"Tulane Studies in Geology and Paleontology","active":false,"publicationSubtype":{"id":10}},"title":"Biostratigraphy and paleoecology of lower Paleozoic, upper Cretaceous, and lower Tertiary rocks in U.S. Geological Survey New Madrid test wells, Southeastern Missouri","docAbstract":"<p><span>The paleontology and biostratigraphy of Tertiary, Cretaceous, and Paleozoic rocks in the upper Mississippi embayment are incompletely known because marine fossils are only locally present in these rocks. This study concerns material from two U.S. Geological Survey test wells drilled in New Madrid County, southeastern Missouri, as part of earthquake hazard studies in the northern Mississippi Embayment. Test well1 sampled lower Tertiary strata to a depth of 146ft; these strata were found to be late Eocene in age on the basis of sporomorphs. Test well1-X, 29ft northwest of well1, provided cuttings and cores from lower Tertiary, Upper Cretaceous, and lower Paleozoic rocks to a total depth of 2,316 ft below the Kelly bushing (at an altitude of 288 ft). Lithologic evidence suggests that the base of the Jackson Formation may be at 270 ft, but sporomorphs indicate that the base of the Jacksonian Stage (upper Eocene) is possibly at a depth of about 350ft in test well1-X. Lithologic units of the Claibornian Stage (middle Eocene) here consist of the Cockfield(?) and Cook Mountain(?) Formations and Memphis Sand, in descending order. The Claibornian could not be subdivided using sporomorphs from cuttings, but sporomorphs show that the top of the Sabinian Stage (top of the lower Eocene) is at about 1,055 ft; lithologically, the top of the Wilcox Group (top of the Flour Island Formation) is at 1,048 ft. Sporomorphs suggest that the top of the lower Sabinian (top of the Paleocene) is within the Flour Island Formation at about 1,105 ft. The next major lithologic break, the top of the Fort Pillow Sand at 1,186 ft, does not coincide with any detectable biostratigraphic boundary. Lithologically, the interval from 1,339 to 1,377 ft may belong to the Old Breastworks Formation; dinoflagellates from cuttings indicate that this interval is likely to be late Midwayan in age and, therefore, correlative with the Naheola Formation of the eastern Gulf Coast. The Porters Creek Clay extends from a probable top at 1,377 ft to 1,691 ft, and the base of the underlying Clayton Formation (Tertiary-Cretaceous contact) is at 1, 703 ft. Calcareous nannofossils, dinoflagellates, foraminifers, mollusks, ostracodes, and sporomorphs from continuous cores of the Porters Creek Clay and Clayton Formation indicate that the upper half of the Porters Creek correlates with the upper part of the same formation or perhaps partly with slightly younger rocks in the eastern Gulf Coast, the lowermost Porters Creek appears to correlate with the upper part of the Clayton Formation of the eastern Gulf Coast and with the Kincaid Formation of Texas, and the thin Clayton of the test well probably correlates with only the lower part of the thicker Clayton of the eastern Gulf Coast. Sporomorphs from McNairy Sand (Upper Cretaceous) cores indicate Maestrichtian and perhaps latest Campanian Age. Lower Paleozoic dolostone from 2,023 ft to total depth at 2,316 ft is barren of identifiable fossils except for a probable fragment of the fish Anatolepis; the dolostone is probably Late Cambrian in age. The McNairy Sand of New Madrid well 1-X seems to have been deposited in nonmarine to nearshore marine environments; the Clayton Formation and lower part of the Porters Creek Clay were deposited under marine conditions during an early Paleocene marine transgression. A major regression followed that continued through the end of Porters Creek time and perhaps into Naheola (late Midwayan) time; the Sabinian, Claibornian, and Jacksonian strata in southeastern Missouri were deposited primarily or entirely in nonmarine environments.&nbsp;</span></p>","language":"English","publisher":"Howard Tilton Memorial Library Journal Publishing","usgsCitation":"Frederiksen, N.O., Bybell, L.M., Christopher, R.A., Crone, A.J., Edwards, L.E., Gibson, T.G., Hazel, J.E., Repetski, J., Russ, D.P., Smith, C.C., and Ward, L.W., 1982, Biostratigraphy and paleoecology of lower Paleozoic, upper Cretaceous, and lower Tertiary rocks in U.S. Geological Survey New Madrid test wells, Southeastern Missouri: Tulane Studies in Geology and Paleontology, v. 17, no. 2, p. 23-45.","productDescription":"23 p.","startPage":"23","endPage":"45","costCenters":[{"id":243,"text":"Eastern Geology and Paleoclimate Science Center","active":true,"usgs":true}],"links":[{"id":386896,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"},{"id":386895,"rank":1,"type":{"id":15,"text":"Index Page"},"url":"https://journals.tulane.edu/tsgp/article/view/787"}],"country":"United States","state":"Missouri","county":"New Madrid County","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -89.63127136230469,\n              36.352739087358735\n            ],\n            [\n              -89.5330810546875,\n              36.352739087358735\n            ],\n            [\n              -89.5330810546875,\n              36.448351464205075\n            ],\n            [\n              -89.63127136230469,\n              36.448351464205075\n            ],\n            [\n              -89.63127136230469,\n              36.352739087358735\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","volume":"17","issue":"2","noUsgsAuthors":false,"publicationStatus":"PW","contributors":{"authors":[{"text":"Frederiksen, N. O.","contributorId":78356,"corporation":false,"usgs":true,"family":"Frederiksen","given":"N.","email":"","middleInitial":"O.","affiliations":[],"preferred":false,"id":818587,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Bybell, Laurel M. 0000-0002-4760-7542 lbybell@usgs.gov","orcid":"https://orcid.org/0000-0002-4760-7542","contributorId":1760,"corporation":false,"usgs":true,"family":"Bybell","given":"Laurel","email":"lbybell@usgs.gov","middleInitial":"M.","affiliations":[{"id":243,"text":"Eastern Geology and Paleoclimate Science Center","active":true,"usgs":true}],"preferred":true,"id":818588,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Christopher, R. A.","contributorId":53775,"corporation":false,"usgs":true,"family":"Christopher","given":"R.","email":"","middleInitial":"A.","affiliations":[],"preferred":false,"id":818589,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Crone, A. J.","contributorId":84363,"corporation":false,"usgs":true,"family":"Crone","given":"A.","email":"","middleInitial":"J.","affiliations":[],"preferred":false,"id":818590,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"Edwards, L. E.","contributorId":6455,"corporation":false,"usgs":true,"family":"Edwards","given":"L.","email":"","middleInitial":"E.","affiliations":[],"preferred":false,"id":818591,"contributorType":{"id":1,"text":"Authors"},"rank":5},{"text":"Gibson, T. G.","contributorId":260728,"corporation":false,"usgs":false,"family":"Gibson","given":"T.","email":"","middleInitial":"G.","affiliations":[],"preferred":false,"id":818592,"contributorType":{"id":1,"text":"Authors"},"rank":6},{"text":"Hazel, J. E.","contributorId":89187,"corporation":false,"usgs":false,"family":"Hazel","given":"J.","email":"","middleInitial":"E.","affiliations":[],"preferred":false,"id":818593,"contributorType":{"id":1,"text":"Authors"},"rank":7},{"text":"Repetski, J.E.","contributorId":38579,"corporation":false,"usgs":true,"family":"Repetski","given":"J.E.","affiliations":[],"preferred":false,"id":818594,"contributorType":{"id":1,"text":"Authors"},"rank":8},{"text":"Russ, D. P.","contributorId":38538,"corporation":false,"usgs":true,"family":"Russ","given":"D.","email":"","middleInitial":"P.","affiliations":[],"preferred":false,"id":818595,"contributorType":{"id":1,"text":"Authors"},"rank":9},{"text":"Smith, C. C.","contributorId":77205,"corporation":false,"usgs":true,"family":"Smith","given":"C.","email":"","middleInitial":"C.","affiliations":[],"preferred":false,"id":818596,"contributorType":{"id":1,"text":"Authors"},"rank":10},{"text":"Ward, L. W.","contributorId":58704,"corporation":false,"usgs":true,"family":"Ward","given":"L.","email":"","middleInitial":"W.","affiliations":[],"preferred":false,"id":818597,"contributorType":{"id":1,"text":"Authors"},"rank":11}]}}
,{"id":70221738,"text":"70221738 - 1982 - Paleocene-Eocene boundary in the eastern Gulf Coast","interactions":[],"lastModifiedDate":"2021-06-30T15:28:10.766533","indexId":"70221738","displayToPublicDate":"1982-12-31T10:16:05","publicationYear":"1982","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1871,"text":"Gulf Coast Association of Geological Societies Transactions","active":true,"publicationSubtype":{"id":10}},"title":"Paleocene-Eocene boundary in the eastern Gulf Coast","docAbstract":"<p>No abstract avaiable.</p>","language":"English","publisher":"Gulf Coast Association of Geological Societies","usgsCitation":"Frederiksen, N.O., Gibson, T., and Bybell, L.M., 1982, Paleocene-Eocene boundary in the eastern Gulf Coast: Gulf Coast Association of Geological Societies Transactions, v. 32, p. 289-294.","productDescription":"6 p.","startPage":"289","endPage":"294","costCenters":[{"id":243,"text":"Eastern Geology and Paleoclimate Science Center","active":true,"usgs":true}],"links":[{"id":386894,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"32","noUsgsAuthors":false,"publicationStatus":"PW","contributors":{"authors":[{"text":"Frederiksen, N. O.","contributorId":78356,"corporation":false,"usgs":true,"family":"Frederiksen","given":"N.","email":"","middleInitial":"O.","affiliations":[],"preferred":false,"id":818584,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Gibson, T. G.","contributorId":260727,"corporation":false,"usgs":false,"family":"Gibson","given":"T. G.","affiliations":[],"preferred":false,"id":818585,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Bybell, Laurel M. 0000-0002-4760-7542 lbybell@usgs.gov","orcid":"https://orcid.org/0000-0002-4760-7542","contributorId":1760,"corporation":false,"usgs":true,"family":"Bybell","given":"Laurel","email":"lbybell@usgs.gov","middleInitial":"M.","affiliations":[{"id":243,"text":"Eastern Geology and Paleoclimate Science Center","active":true,"usgs":true}],"preferred":true,"id":818586,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":70221737,"text":"70221737 - 1982 - Paleocene to middle Eocene stratigraphy of Alabama","interactions":[],"lastModifiedDate":"2021-06-30T15:14:53.406931","indexId":"70221737","displayToPublicDate":"1982-12-31T10:10:18","publicationYear":"1982","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1871,"text":"Gulf Coast Association of Geological Societies Transactions","active":true,"publicationSubtype":{"id":10}},"title":"Paleocene to middle Eocene stratigraphy of Alabama","docAbstract":"<p>No abstract available.</p>","language":"English","publisher":"Gulf Coast Association of Geological Societies","usgsCitation":"Gibson, T., Mancini, E.A., and Bybell, L.M., 1982, Paleocene to middle Eocene stratigraphy of Alabama: Gulf Coast Association of Geological Societies Transactions, v. 32, p. 449-458.","productDescription":"10 p.","startPage":"449","endPage":"458","costCenters":[{"id":243,"text":"Eastern 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,{"id":70198200,"text":"70198200 - 1982 - Detached crystalline rocks of the Mohave, Buck, and Bill Williams Mountains, western Arizona","interactions":[],"lastModifiedDate":"2018-07-20T09:55:06","indexId":"70198200","displayToPublicDate":"1982-12-31T00:00:00","publicationYear":"1982","noYear":false,"publicationType":{"id":5,"text":"Book chapter"},"publicationSubtype":{"id":24,"text":"Book Chapter"},"title":"Detached crystalline rocks of the Mohave, Buck, and Bill Williams Mountains, western Arizona","docAbstract":"<p>No abstract available.</p>","largerWorkType":{"id":4,"text":"Book"},"largerWorkTitle":"Mesozoic-Cenozoic tectonic evolution of the Colorado River Region, California, Arizona, and Nevada","language":"English","publisher":"Cordilleran Publishers","publisherLocation":"San Diego, CA","usgsCitation":"Howard, K.A., Goodge, J., and John, B., 1982, Detached crystalline rocks of the Mohave, Buck, and Bill Williams Mountains, western Arizona, chap. <i>of</i> Mesozoic-Cenozoic tectonic evolution of the Colorado River Region, California, Arizona, and Nevada, p. 377-392.","productDescription":"16 p.","startPage":"377","endPage":"392","costCenters":[{"id":312,"text":"Geology, Minerals, Energy, and Geophysics Science Center","active":true,"usgs":true}],"links":[{"id":355837,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","contributors":{"authors":[{"text":"Howard, Keith A. 0000-0002-6462-2947 khoward@usgs.gov","orcid":"https://orcid.org/0000-0002-6462-2947","contributorId":3439,"corporation":false,"usgs":true,"family":"Howard","given":"Keith","email":"khoward@usgs.gov","middleInitial":"A.","affiliations":[{"id":312,"text":"Geology, Minerals, Energy, and Geophysics Science Center","active":true,"usgs":true}],"preferred":true,"id":740541,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Goodge, J. W.","contributorId":102146,"corporation":false,"usgs":true,"family":"Goodge","given":"J. W.","affiliations":[],"preferred":false,"id":740542,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"John, B.E.","contributorId":190690,"corporation":false,"usgs":false,"family":"John","given":"B.E.","email":"","affiliations":[],"preferred":false,"id":740543,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":70198201,"text":"70198201 - 1982 - Geologic and geochronologic reconnaissance of the Turtle Mountains area, California: West border of the Whipple Mountains detachment terrane","interactions":[],"lastModifiedDate":"2018-07-20T09:54:54","indexId":"70198201","displayToPublicDate":"1982-12-31T00:00:00","publicationYear":"1982","noYear":false,"publicationType":{"id":5,"text":"Book chapter"},"publicationSubtype":{"id":24,"text":"Book Chapter"},"title":"Geologic and geochronologic reconnaissance of the Turtle Mountains area, California: West border of the Whipple Mountains detachment terrane","docAbstract":"<p>No abstract available.</p>","largerWorkTitle":"Mesozoic-Cenozoic tectonic evolution of the Colorado River Region, California, Arizona, and Nevada","language":"English","publisher":"Cordilleran Publishers","publisherLocation":"San Diego, CA","usgsCitation":"Howard, K.A., Stone, P., Pernokas, M., and Marvin, R.F., 1982, Geologic and geochronologic reconnaissance of the Turtle Mountains area, California: West border of the Whipple Mountains detachment terrane, chap. <i>of</i> Mesozoic-Cenozoic tectonic evolution of the Colorado River Region, California, Arizona, and Nevada, p. 341-35.","productDescription":"15 p.","startPage":"341","endPage":"35","costCenters":[{"id":312,"text":"Geology, Minerals, Energy, and Geophysics Science Center","active":true,"usgs":true}],"links":[{"id":355838,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","contributors":{"editors":[{"text":"Frost, E.G.","contributorId":206458,"corporation":false,"usgs":false,"family":"Frost","given":"E.G.","email":"","affiliations":[],"preferred":false,"id":740548,"contributorType":{"id":2,"text":"Editors"},"rank":1},{"text":"Martin, D.L.","contributorId":10121,"corporation":false,"usgs":true,"family":"Martin","given":"D.L.","email":"","affiliations":[],"preferred":false,"id":740549,"contributorType":{"id":2,"text":"Editors"},"rank":2}],"authors":[{"text":"Howard, Keith A. 0000-0002-6462-2947 khoward@usgs.gov","orcid":"https://orcid.org/0000-0002-6462-2947","contributorId":3439,"corporation":false,"usgs":true,"family":"Howard","given":"Keith","email":"khoward@usgs.gov","middleInitial":"A.","affiliations":[{"id":312,"text":"Geology, Minerals, Energy, and Geophysics Science Center","active":true,"usgs":true}],"preferred":true,"id":740544,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Stone, Paul 0000-0002-1439-0156 pastone@usgs.gov","orcid":"https://orcid.org/0000-0002-1439-0156","contributorId":273,"corporation":false,"usgs":true,"family":"Stone","given":"Paul","email":"pastone@usgs.gov","affiliations":[{"id":312,"text":"Geology, Minerals, Energy, and Geophysics Science Center","active":true,"usgs":true}],"preferred":true,"id":740545,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Pernokas, M.A.","contributorId":33782,"corporation":false,"usgs":true,"family":"Pernokas","given":"M.A.","email":"","affiliations":[],"preferred":false,"id":740546,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Marvin, R. F.","contributorId":60597,"corporation":false,"usgs":true,"family":"Marvin","given":"R.","middleInitial":"F.","affiliations":[],"preferred":false,"id":740547,"contributorType":{"id":1,"text":"Authors"},"rank":4}]}}
,{"id":70188838,"text":"70188838 - 1982 - The Yellowstone-Snake River Plain seismic profiling experiment: Crustal structure of the Eastern Snake River Plain","interactions":[],"lastModifiedDate":"2017-06-26T11:13:55","indexId":"70188838","displayToPublicDate":"1982-12-31T00:00:00","publicationYear":"1982","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":2314,"text":"Journal of Geophysical Research B: Solid Earth","active":true,"publicationSubtype":{"id":10}},"title":"The Yellowstone-Snake River Plain seismic profiling experiment: Crustal structure of the Eastern Snake River Plain","docAbstract":"<p><span>Seismic refraction profiles recorded along the eastern Snake River Plain (ESRP) in southeastern Idaho during the 1978 Yellowstone-Snake River Plain cooperative seismic profiling experiment are interpreted to infer the crustal velocity and attenuation (Q-1) structure of the ESRP. Travel-time and synthetic seismogram modeling of a 250 km reversed refraction profile as well as a 100 km detailed profile indicate that the crust of the ESRP is highly anomalous. Approximately 3 to 6 km of volcanic rocks (with some interbedded sediments) overlie an upper-crustal layer (compressional velocity ≅6.1 km/s) which thins southwestward along the ESRP from a thickness of 10 km near Island Park Caldera to 2 to 3 km beneath the central and southwestern portions of the ESRP. An intermediate-velocity (≅6.5 km/s) layer extends from ≅10 to ≅20 km depth. A thick (≅22 km) lower crust of compressional velocity 6.8 km/s, a total crustal thickness of ≅42 km, and a P</span><sub>n</sub><span>velocity of ≅7.9 km/s is observed in the ESRP, similar to the western Snake River Plain and the Rocky Mountains Provinces. High attenuation is evident on the amplitude corrected seismic data due to low-Q values in the volcanic rocks (Q</span><sub>p</sub><span> = 20 to 200) and throughout the crust (Q</span><sub>p</sub><span> = 160 to 300). Based on these characteristics of the crustal structure and volcanic-age progression data, it is suggested that the ESRP has resulted from an intensive period of intrusion of mantle-derived basaltic magma into the upper crust generating explosive silicic volcanism and associated regional uplift and caldera collapse. This activity began about 15 m.y. ago in southwestern Idaho and has migrated northeast to its present position at Yellowstone. Subsequent cooling of the intruded upper crust results in the 6.5 km/s velocity intermediate layer. Crustal subsidence and periodic basaltic volcanism as represented by the ESRP complete the sequence of crustal evolution.</span></p>","language":"English","publisher":"Wiley","doi":"10.1029/JB087iB04p02597","usgsCitation":"Braile, L., Smith, R.B., Ansorge, J., Baker, M., Sparlin, M., Prodehl, C., Schilly, M., Healy, J.H., , M., and Olsen, K., 1982, The Yellowstone-Snake River Plain seismic profiling experiment: Crustal structure of the Eastern Snake River Plain: Journal of Geophysical Research B: Solid Earth, v. 87, no. B4, p. 2597-2609, https://doi.org/10.1029/JB087iB04p02597.","productDescription":"13 p.","startPage":"2597","endPage":"2609","costCenters":[],"links":[{"id":342866,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"87","issue":"B4","noUsgsAuthors":false,"publicationDate":"2012-09-20","publicationStatus":"PW","scienceBaseUri":"59521d2ae4b062508e3c36f1","contributors":{"authors":[{"text":"Braile, L.W.","contributorId":85332,"corporation":false,"usgs":true,"family":"Braile","given":"L.W.","email":"","affiliations":[],"preferred":false,"id":700633,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Smith, R. B.","contributorId":64589,"corporation":false,"usgs":true,"family":"Smith","given":"R.","email":"","middleInitial":"B.","affiliations":[],"preferred":false,"id":700634,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Ansorge, J.","contributorId":38318,"corporation":false,"usgs":true,"family":"Ansorge","given":"J.","email":"","affiliations":[],"preferred":false,"id":700635,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Baker, M.R.","contributorId":193474,"corporation":false,"usgs":false,"family":"Baker","given":"M.R.","email":"","affiliations":[],"preferred":false,"id":700636,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"Sparlin, M.A.","contributorId":193497,"corporation":false,"usgs":false,"family":"Sparlin","given":"M.A.","email":"","affiliations":[],"preferred":false,"id":700637,"contributorType":{"id":1,"text":"Authors"},"rank":5},{"text":"Prodehl, C.","contributorId":100376,"corporation":false,"usgs":true,"family":"Prodehl","given":"C.","affiliations":[],"preferred":false,"id":700638,"contributorType":{"id":1,"text":"Authors"},"rank":6},{"text":"Schilly, M.M.","contributorId":193496,"corporation":false,"usgs":false,"family":"Schilly","given":"M.M.","email":"","affiliations":[],"preferred":false,"id":700639,"contributorType":{"id":1,"text":"Authors"},"rank":7},{"text":"Healy, J. H.","contributorId":48968,"corporation":false,"usgs":true,"family":"Healy","given":"J.","email":"","middleInitial":"H.","affiliations":[],"preferred":false,"id":700640,"contributorType":{"id":1,"text":"Authors"},"rank":8},{"text":" Mueller","contributorId":19328,"corporation":false,"usgs":true,"given":"Mueller","email":"","affiliations":[],"preferred":false,"id":700641,"contributorType":{"id":1,"text":"Authors"},"rank":9},{"text":"Olsen, K.H.","contributorId":95201,"corporation":false,"usgs":true,"family":"Olsen","given":"K.H.","email":"","affiliations":[],"preferred":false,"id":700642,"contributorType":{"id":1,"text":"Authors"},"rank":10}]}}
,{"id":70193890,"text":"70193890 - 1982 - Toxaphene residues in fish: Identification, quantification, and confirmation at part per billion levels","interactions":[],"lastModifiedDate":"2017-11-07T11:49:13","indexId":"70193890","displayToPublicDate":"1982-12-31T00:00:00","publicationYear":"1982","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1565,"text":"Environmental Science & Technology","onlineIssn":"1520-5851","printIssn":"0013-936X","active":true,"publicationSubtype":{"id":10}},"title":"Toxaphene residues in fish: Identification, quantification, and confirmation at part per billion levels","docAbstract":"<p>No abstract available.</p>","language":"English","publisher":"ACS Publications","doi":"10.1021/es00100a003","usgsCitation":"Ribick, M.A., Dubay, G.R., Petty, J.D., Stalling, D.L., and Schmitt, C.J., 1982, Toxaphene residues in fish: Identification, quantification, and confirmation at part per billion levels: Environmental Science & Technology, v. 16, no. 6, p. 310-318, https://doi.org/10.1021/es00100a003.","productDescription":"9 p.","startPage":"310","endPage":"318","costCenters":[{"id":192,"text":"Columbia Environmental Research Center","active":true,"usgs":true}],"links":[{"id":348364,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"16","issue":"6","noUsgsAuthors":false,"publicationDate":"2002-05-01","publicationStatus":"PW","scienceBaseUri":"5a61445ae4b06e28e9c25f5f","contributors":{"authors":[{"text":"Ribick, M. A.","contributorId":82367,"corporation":false,"usgs":true,"family":"Ribick","given":"M.","email":"","middleInitial":"A.","affiliations":[],"preferred":false,"id":720881,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Dubay, George R.","contributorId":200065,"corporation":false,"usgs":false,"family":"Dubay","given":"George","email":"","middleInitial":"R.","affiliations":[],"preferred":false,"id":720882,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Petty, Jimmie D.","contributorId":175402,"corporation":false,"usgs":false,"family":"Petty","given":"Jimmie","email":"","middleInitial":"D.","affiliations":[],"preferred":false,"id":720883,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Stalling, David L.","contributorId":176670,"corporation":false,"usgs":false,"family":"Stalling","given":"David","email":"","middleInitial":"L.","affiliations":[],"preferred":false,"id":720884,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"Schmitt, Christopher J. 0000-0001-6804-2360 cjschmitt@usgs.gov","orcid":"https://orcid.org/0000-0001-6804-2360","contributorId":491,"corporation":false,"usgs":true,"family":"Schmitt","given":"Christopher","email":"cjschmitt@usgs.gov","middleInitial":"J.","affiliations":[{"id":192,"text":"Columbia Environmental Research Center","active":true,"usgs":true}],"preferred":true,"id":720885,"contributorType":{"id":1,"text":"Authors"},"rank":5}]}}
,{"id":70188731,"text":"70188731 - 1982 - Strata-bound sulfide deposits, wall-rock alteration, and associated tin-bearing minerals in the Carolina slate belt, South Carolina and Georgia","interactions":[],"lastModifiedDate":"2019-12-19T10:17:14","indexId":"70188731","displayToPublicDate":"1982-12-31T00:00:00","publicationYear":"1982","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1472,"text":"Economic Geology","active":true,"publicationSubtype":{"id":10}},"title":"Strata-bound sulfide deposits, wall-rock alteration, and associated tin-bearing minerals in the Carolina slate belt, South Carolina and Georgia","docAbstract":"<p><span>Massive sulfide deposits, gold deposits, and tin-bearing minerals occur in rocks of the Carolina slate belt in South Carolina and adjacent Georgia. The belt of greenschist metamorphic rocks in which the ore deposits occur is mostly Cambrian in age. It is divided into an upper metasedimentary unit and a lower unit of predominantly felsic metavolcanic and metavolcaniclastic rocks. The ore deposits occur in the lower unit chiefly near the contact between the two units. The rocks have been deformed into two maior sets of coaxial folds and at least two minor deformations. Coarse-grained unmetamorphosed Carboniferous, I-type granites, and abundant Triassic-Jurassic diabase dikes cut the slate belt and appear largely unrelated to the ore deposits. Remnants of Cretaceous and younger sedimentary rocks overlie the crystalline rocks near several of the larger mineralized areas.Massive sulfides, largely pyrite, and some polymetallic sulfides occur in mines opened for gold in the nineteenth century. The largest of these in South Carolina are the Haile, Brewer, and Dorn mines. These mines and the Little Mountain and Cedar Creek-Blythewood areas have many similar lithologic characteristics. These are: hydrothermally altered wall-rock consisting of quartz-sericite-kaolinite schist and quartz-sericite schist; abundant aluminous silicates such as kyanite, andalusite, pyrophyllite, and topaz; zones of iron-enriched rocks; and a suite of resistant heavy minerals that includes tin-bearing minerals. Heavy mineral concentrates from alluvium of small streams showed 20,000 ppm tin. Cassiterite and nigerite have been identified.At the Brewer mine, gold has been produced from altered felsic volcanic rocks that contain silicified breccia, massive topaz, abundant pyrite, minor enargite, and probably cassiterite. Massive pyrite and gold have been mined at the Haile mine. In the McCormick-Lincolnton area, a near-surface granitoid pluton is thought to be the source for volcaniclastic rocks that contain polymetallic massive sulfide deposits, gold, and associated deposits of kyanite, barite, and manganese. Tin was found there in heavy mineral concentrates, and rutile occurring with kyanite contains 1,000 ppm tin. At Little Mountain, cassiterite and hematite are present in rocks considered to be metamorphosed hot spring deposits. In the Cedar Creek-Blythewood area, nigerite is present, together with cassiterite, chrysoberyl, and seventeen other heavy minerals in concentrates panned from alluvium in streams draining an area of quartz-sericite-kaolinite schist.The deposition of massive sulfides, gold, and tin minerals is considered to be part of a continuum of volcanic activity that included alteration, deformation, and metamorphism. Altered rocks, which host the ore deposits, result from superimposed processes beginning with alteration syngenetic with the massive sulfides and ending with fracture-controlled alteration.</span></p>","language":"English","publisher":"Society of Economic Geologists","doi":"10.2113/gsecongeo.77.2.294","issn":"03610128","usgsCitation":"Bell, H., 1982, Strata-bound sulfide deposits, wall-rock alteration, and associated tin-bearing minerals in the Carolina slate belt, South Carolina and Georgia: Economic Geology, v. 77, p. 294-311, https://doi.org/10.2113/gsecongeo.77.2.294.","productDescription":"18 p.","startPage":"294","endPage":"311","costCenters":[],"links":[{"id":342764,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United States","state":"South Carolina","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -82.77099609375,\n              32.74108223150125\n            ],\n            [\n              -78.321533203125,\n              32.74108223150125\n            ],\n            [\n              -78.321533203125,\n              35.37113502280101\n            ],\n            [\n              -82.77099609375,\n              35.37113502280101\n            ],\n            [\n              -82.77099609375,\n              32.74108223150125\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","volume":"77","noUsgsAuthors":false,"publicationDate":"1982-04-01","publicationStatus":"PW","scienceBaseUri":"594cd742e4b062508e3951f5","contributors":{"authors":[{"text":"Bell, Henry","contributorId":73980,"corporation":false,"usgs":true,"family":"Bell","given":"Henry","affiliations":[],"preferred":false,"id":699439,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":70188680,"text":"70188680 - 1982 - Marine ice-pushed boulder ridge, Beaufort Sea, Alaska","interactions":[],"lastModifiedDate":"2017-06-21T09:48:11","indexId":"70188680","displayToPublicDate":"1982-12-31T00:00:00","publicationYear":"1982","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":894,"text":"Arctic","active":true,"publicationSubtype":{"id":10}},"title":"Marine ice-pushed boulder ridge, Beaufort Sea, Alaska","docAbstract":"<div data-canvas-width=\"135.02486666666667\">A steep-faced boulder&nbsp;ridge up to&nbsp;4m high by 300m&nbsp;long&nbsp;was encountered along the arctic coast&nbsp;east&nbsp;of Prudhoe Bay,&nbsp;Alaska,&nbsp;in&nbsp;the summer&nbsp;of 1979.&nbsp;Marine occurrences of similar ridges are rare. Since ice-push sorts cobble- and boulder-sized material in the construction of a ridge, recent onshore excursions of ice due to wind stress on the fast ice are believed to be responsible for building the boulder ridge. Ice push is a mechanism that preferentially sorts cobble- and boulder-sized material from 1-2m water depths and that forms boulder ridges in areas of high boulder concentrations.</div>","language":"English","publisher":"Arctic Institute of North America","doi":"10.14430/arctic2330","usgsCitation":"Barnes, P.W., 1982, Marine ice-pushed boulder ridge, Beaufort Sea, Alaska: Arctic, v. 35, no. 2, p. 312-316, https://doi.org/10.14430/arctic2330.","productDescription":"5 p.","startPage":"312","endPage":"316","costCenters":[],"links":[{"id":480249,"rank":0,"type":{"id":40,"text":"Open Access Publisher Index Page"},"url":"https://doi.org/10.14430/arctic2330","text":"Publisher Index Page"},{"id":342702,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United States","state":"Alaska","otherGeospatial":"Canning River","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -147.43652343749997,\n              68.86351700272681\n            ],\n            [\n              -141.009521484375,\n              68.86351700272681\n            ],\n            [\n              -141.009521484375,\n              70.91304887381109\n            ],\n            [\n              -147.43652343749997,\n              70.91304887381109\n            ],\n            [\n              -147.43652343749997,\n              68.86351700272681\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","volume":"35","issue":"2","noUsgsAuthors":false,"publicationDate":"1982-01-01","publicationStatus":"PW","scienceBaseUri":"594b85b7e4b062508e382bc0","contributors":{"authors":[{"text":"Barnes, Peter W.","contributorId":6042,"corporation":false,"usgs":true,"family":"Barnes","given":"Peter","email":"","middleInitial":"W.","affiliations":[],"preferred":false,"id":698878,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":70188733,"text":"70188733 - 1982 - The emplacement of ophiolites by collision","interactions":[],"lastModifiedDate":"2017-06-22T14:06:13","indexId":"70188733","displayToPublicDate":"1982-12-31T00:00:00","publicationYear":"1982","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":"The emplacement of ophiolites by collision","docAbstract":"<p><span>Ophiolites, recognized in most of the world's orogenic belts, are generally interpreted to be oceanic crust and upper mantle (lithosphere) fragments that have been incorporated into continental margins at consuming plate boundaries. We suggest that the mechanism for ophiolite emplacement is the same in both the Alpine and Andean-type orogenes. In both geological settings, obduction of oceanic lithosphere onto the continental lithosphere is caused by the convergence of light, buoyant bodies such as oceanic plateaus, continental slivers, island arcs, or old hot spot traces. For example, the Troodos ophiolite complex, previously interpreted by some workers as resulting from continental collision, may have been emplaced by the collision of Cyprus with the Eratosthenes Plateau embedded in the oceanic eastern Mediterranean crust. On the other hand, the Upper Jurassic Coast Range Ophiolites of California, previously interpreted as resulting from typical oceanic subduction, may be the result of a continuous injection of thick nonsubductable packages of light, continentally derived sedimentary rocks, seamounts, and plateaus into the subduction zones. Many other ophiolite complexes may be similarly related to accreted terranes.</span></p>","language":"English","publisher":"American Geophysical Union","doi":"10.1029/JB087iB05p03861","usgsCitation":"Ben-Avraham, Z., 1982, The emplacement of ophiolites by collision: Journal of Geophysical Research, v. 87, no. B5, p. 3861-3867, https://doi.org/10.1029/JB087iB05p03861.","productDescription":"7 p.","startPage":"3861","endPage":"3867","costCenters":[],"links":[{"id":342767,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"87","issue":"B5","noUsgsAuthors":false,"publicationDate":"2012-09-20","publicationStatus":"PW","scienceBaseUri":"594cd742e4b062508e3951f3","contributors":{"authors":[{"text":"Ben-Avraham, Zvi","contributorId":11679,"corporation":false,"usgs":true,"family":"Ben-Avraham","given":"Zvi","email":"","affiliations":[],"preferred":false,"id":699479,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":70188754,"text":"70188754 - 1982 - Miocene actinommid Radiolaria from the equatorial Pacific","interactions":[],"lastModifiedDate":"2017-06-22T16:44:50","indexId":"70188754","displayToPublicDate":"1982-12-31T00:00:00","publicationYear":"1982","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":2735,"text":"Micropaleontology","active":true,"publicationSubtype":{"id":10}},"title":"Miocene actinommid Radiolaria from the equatorial Pacific","docAbstract":"<p>Actinommids (spumellarian Radiolaria) are a group of microfossils in which taxonomy and phylogeny hitherto have been based on features of morphology that change with the growth of individuals. To make Miocene actinommids from the equatorial Pacific useful in biostratigraphy, paleocenography, and paleoecology, ontogenetically invariant morphological features can be analyzed by methods of numerical taxonomy to group the specimens into genera, which are further subdivided into species by visual comparison. According to these criteria, 31 species, 18 of which are new, are recognized in the Late Miocene section of DSDP Sites 77 and 289, and an informal revision of actinommid higher taxa is tentatively proposed.</p>","language":"English","publisher":"Micropaleontology Press","usgsCitation":"Blueford, J.R., 1982, Miocene actinommid Radiolaria from the equatorial Pacific: Micropaleontology, v. 28, no. 2, p. 189-213.","productDescription":"25 p.","startPage":"189","endPage":"213","costCenters":[],"links":[{"id":342790,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"},{"id":342789,"rank":1,"type":{"id":15,"text":"Index Page"},"url":"https://micropal.geoscienceworld.org/content/28/2/189"}],"volume":"28","issue":"2","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"594cd741e4b062508e3951ed","contributors":{"authors":[{"text":"Blueford, J. R.","contributorId":69563,"corporation":false,"usgs":true,"family":"Blueford","given":"J.","email":"","middleInitial":"R.","affiliations":[],"preferred":false,"id":699731,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":70188755,"text":"70188755 - 1982 - Citation analysis of principal sedimentology journals; discussion","interactions":[],"lastModifiedDate":"2017-06-22T16:50:57","indexId":"70188755","displayToPublicDate":"1982-12-31T00:00:00","publicationYear":"1982","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":2451,"text":"Journal of Sedimentary Research","onlineIssn":"1938-3681","printIssn":"1527-1404","active":true,"publicationSubtype":{"id":10}},"title":"Citation analysis of principal sedimentology journals; discussion","docAbstract":"<p>No abstract available</p>","language":"English","publisher":"Society of Economic Paleontologists and Mineralogists","doi":"10.1306/212F800D-2B24-11D7-8648000102C1865D","usgsCitation":"Bodine, M., 1982, Citation analysis of principal sedimentology journals; discussion: Journal of Sedimentary Research, v. 52, no. 2, p. 693-693, https://doi.org/10.1306/212F800D-2B24-11D7-8648000102C1865D.","productDescription":"1 p.","startPage":"693","endPage":"693","costCenters":[],"links":[{"id":342791,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"52","issue":"2","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"594cd741e4b062508e3951e6","contributors":{"authors":[{"text":"Bodine, Marc W.","contributorId":74765,"corporation":false,"usgs":true,"family":"Bodine","given":"Marc W.","affiliations":[],"preferred":false,"id":699732,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":70188756,"text":"70188756 - 1982 - Kinematic evolution of the junction of the San Andreas, Garlock, and Big Pine faults, California","interactions":[],"lastModifiedDate":"2020-10-21T15:44:58.054907","indexId":"70188756","displayToPublicDate":"1982-12-31T00:00:00","publicationYear":"1982","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1796,"text":"Geology","active":true,"publicationSubtype":{"id":10}},"title":"Kinematic evolution of the junction of the San Andreas, Garlock, and Big Pine faults, California","docAbstract":"<p><span>If the San Andreas fault with about 300 km of right slip, the Carlock fault with about 60 km of left slip, and the Big Pine fault with about 15 km of left slip are considered to have been contemporaneously active, a space problem at their high-angle junctions becomes apparent. Large crustal masses converge in the area of the junctions as a result of the simultaneous large displacements on the faults. We present here a model in which an early straight north-northwest–trending San Andreas deforms to its present bent configuration in response to a westward displacement of crust north of the Garlock fault. During this deformation, the crust north of the Garlock in the vicinity of the junction undergoes north-south shortening, while the fault junction migrates along the trace of the San Andreas fault to the southeast relative to its original position. As a result of this migration, the Mojave area is displaced to the east relative to the original junction position. We suggest a similar history in mirror image for the Big Pine fault and the areas of crust adjacent to it.</span></p>","language":"English","publisher":"Geological Society of America","doi":"10.1130/0091-7613(1982)10<358:KEOTJO>2.0.CO;2","usgsCitation":"Bohannon, R.G., and Howell, D.G., 1982, Kinematic evolution of the junction of the San Andreas, Garlock, and Big Pine faults, California: Geology, v. 10, no. 7, p. 358-363, https://doi.org/10.1130/0091-7613(1982)10<358:KEOTJO>2.0.CO;2.","productDescription":"6 p.","startPage":"358","endPage":"363","costCenters":[],"links":[{"id":342792,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United States","state":"California","otherGeospatial":"Big Pine fault, Garlock fault, San Andreas 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 \"}}]}","volume":"10","issue":"7","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"594cd740e4b062508e3951e3","contributors":{"authors":[{"text":"Bohannon, Robert G. rbohannon@usgs.gov","contributorId":2255,"corporation":false,"usgs":true,"family":"Bohannon","given":"Robert","email":"rbohannon@usgs.gov","middleInitial":"G.","affiliations":[],"preferred":true,"id":699733,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Howell, David G.","contributorId":59874,"corporation":false,"usgs":true,"family":"Howell","given":"David","email":"","middleInitial":"G.","affiliations":[],"preferred":false,"id":699734,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":70188920,"text":"70188920 - 1982 - On the distribution of species occurrence","interactions":[],"lastModifiedDate":"2025-06-05T16:35:42.631441","indexId":"70188920","displayToPublicDate":"1982-12-31T00:00:00","publicationYear":"1982","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":3001,"text":"Paleobiology","active":true,"publicationSubtype":{"id":10}},"title":"On the distribution of species occurrence","docAbstract":"<p>The distribution of species abundance (number of individuals per species) is well documented. The distribution of species occurrence (number of localities per species), however, has received little attention. This study investigates the distribution of species occurrence for five large data sets. For modern benthic foraminifera, species occurrence is examined from the Atlantic continental margin of North America, where 875 species were recorded 10,017 times at 542 localities, the Gulf of Mexico, where 848 species were recorded 18,007 times at 426 localities, and the Caribbean, where 1149 species were recorded 6684 times at 268 localities. For Late Cretaceous molluscs, species occurrence is examined from the Gulf Coast where 716 species were recorded 6236 times at 166 localities and a subset of this data consisting of 643 species recorded 3851 times at 86 localities.</p><p>Logseries and lognormal distributions were fitted to these data sets. In most instances the logseries best predicts the distribution of species occurrence. The lognormal, however, also fits the data fairly well, and, in one instance, better. The use of these distributions allows the prediction of the number of species occurring once, twice, …,<span>&nbsp;</span><span class=\"italic\">n</span><span>&nbsp;</span>times.</p><p>Species abundance data are also available for the molluscan data sets. They indicate that the most abundant species (greatest number of individuals) usually occur most frequently. In all data sets approximately half the species occur four or less times. The probability of noting the presence of rarely occurring species is small, and, consequently, such species must be used with extreme caution in studies requiring knowledge of the distribution of species in space and time.</p>","language":"English","publisher":"Cambridge University Press","doi":"10.1017/S0094837300004486","usgsCitation":"Buzas, M.A., Koch, C.F., Culver, S., and Sohl, N.F., 1982, On the distribution of species occurrence: Paleobiology, v. 8, no. 2, p. 143-150, https://doi.org/10.1017/S0094837300004486.","productDescription":"8 p.","startPage":"143","endPage":"150","costCenters":[],"links":[{"id":343007,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"8","issue":"2","noUsgsAuthors":false,"publicationDate":"2015-07-14","publicationStatus":"PW","scienceBaseUri":"59536ee1e4b062508e3c7b25","contributors":{"authors":[{"text":"Buzas, Martin A.","contributorId":85098,"corporation":false,"usgs":true,"family":"Buzas","given":"Martin","email":"","middleInitial":"A.","affiliations":[],"preferred":false,"id":701233,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Koch, Carl F.","contributorId":8331,"corporation":false,"usgs":true,"family":"Koch","given":"Carl","email":"","middleInitial":"F.","affiliations":[],"preferred":false,"id":701234,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Culver, Stephen J.","contributorId":79331,"corporation":false,"usgs":true,"family":"Culver","given":"Stephen J.","affiliations":[],"preferred":false,"id":701235,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Sohl, Norman F.","contributorId":27906,"corporation":false,"usgs":true,"family":"Sohl","given":"Norman","email":"","middleInitial":"F.","affiliations":[],"preferred":false,"id":701236,"contributorType":{"id":1,"text":"Authors"},"rank":4}]}}
,{"id":70188945,"text":"70188945 - 1982 - The Geoid: Effect of compensated topography and uncompensated oceanic trenches","interactions":[],"lastModifiedDate":"2017-06-27T16:39:53","indexId":"70188945","displayToPublicDate":"1982-12-31T00:00:00","publicationYear":"1982","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1807,"text":"Geophysical Research Letters","active":true,"publicationSubtype":{"id":10}},"title":"The Geoid: Effect of compensated topography and uncompensated oceanic trenches","docAbstract":"<p><span>The geoid is becoming increasingly important in interpretation of global tectonics. Most of the topography of the earth is isostatically compensated, so removal of its effect from the geoid is appropriate before tectonic modeling. The oceanic trenches, however, are dynamically depressed features and cannot be isostatically compensated in the classical way. Continental topography compensated at 35 km gives intracontinental geoidal undulations of up to 15 m over mountain ranges in a spherical harmonic expansion to order and degree 22. Oceanic topography compensated at 40 km, reasonable for the thermally supported long wavelengths, matches the +10 m difference between old continents and old oceans in a detailed NASA/GSFC geoid. Removing the assumed compensation for the oceanic trenches leaves negative anomalies of up to 9 m amplitude caused by their uncompensated mass deficit. This mass deficit acts as a partial \"regional compensation\" for the excess mass of the subducting slabs, and partly explains why geoidal (and gravity) anomalies over the cold slabs are less than thermal models predict.</span></p>","language":"English","publisher":"American Geophysical Union","doi":"10.1029/GL009i001p00029","usgsCitation":"Chase, C., and McNutt, M.K., 1982, The Geoid: Effect of compensated topography and uncompensated oceanic trenches: Geophysical Research Letters, v. 9, no. 1, p. 29-32, https://doi.org/10.1029/GL009i001p00029.","productDescription":"4 p.","startPage":"29","endPage":"32","costCenters":[],"links":[{"id":343045,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"9","issue":"1","noUsgsAuthors":false,"publicationDate":"2012-12-07","publicationStatus":"PW","scienceBaseUri":"59536ee0e4b062508e3c7b19","contributors":{"authors":[{"text":"Chase, C.G.","contributorId":102965,"corporation":false,"usgs":true,"family":"Chase","given":"C.G.","email":"","affiliations":[],"preferred":false,"id":701470,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"McNutt, Marcia K. 0000-0003-0117-7716 mcnutt@usgs.gov","orcid":"https://orcid.org/0000-0003-0117-7716","contributorId":327,"corporation":false,"usgs":true,"family":"McNutt","given":"Marcia","email":"mcnutt@usgs.gov","middleInitial":"K.","affiliations":[{"id":5066,"text":"Office of the Director USGS","active":true,"usgs":true}],"preferred":false,"id":701471,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":70188943,"text":"70188943 - 1982 - Volume of organic-rich Devonian shale in the Appalachian Basin: relating \"black\" to organic-matter content: Geologic notes","interactions":[],"lastModifiedDate":"2023-01-23T17:47:04.286818","indexId":"70188943","displayToPublicDate":"1982-12-31T00:00:00","publicationYear":"1982","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":701,"text":"American Association of Petroleum Geologists Bulletin","active":true,"publicationSubtype":{"id":10}},"title":"Volume of organic-rich Devonian shale in the Appalachian Basin: relating \"black\" to organic-matter content: Geologic notes","docAbstract":"<p><span>Some estimates of natural-gas resources in the Devonian shale of the Appalachian basin depend on the volume of organic-rich shale in the basin. A map by L. G. Wallace and W. de Witt showing the thickness and extent of Devonian \"black\" shale facies in the Appalachian basin is widely used as an indicator of organic-rich shale, but the map is derived from subjective evaluations of shale color. Wallace and de Witt's definition of \"black\" is shown here to correspond to an organic-matter content of approximately 4% or more by volume and a Munsell color value for dry pressed-powder samples of about N5 (medium gray) or darker. The volume of Devonian shale with an organic-matter content greater than 2.0% by volume (a definition of \"organic-rich\" that is preferred by the writers) a erages 1.44 times that of the \"black\" shale of Wallace and de Witt, and totals about 2,574 × 10</span><sup>12</sup><span>&nbsp;cu ft (72.9 × 10</span><sup>12</sup><span>&nbsp;cu m) in the Appalachian basin.</span></p>","language":"English","publisher":"American Association of Petroleum Geologists","doi":"10.1306/03B59B1B-16D1-11D7-8645000102C1865D","usgsCitation":"Charpentier, R., and Schmoker, J.W., 1982, Volume of organic-rich Devonian shale in the Appalachian Basin: relating \"black\" to organic-matter content: Geologic notes: American Association of Petroleum Geologists Bulletin, v. 66, no. 3, p. 375-378, https://doi.org/10.1306/03B59B1B-16D1-11D7-8645000102C1865D.","productDescription":"4 p.","startPage":"375","endPage":"378","costCenters":[],"links":[{"id":343043,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United States","otherGeospatial":"Appalachian Basin","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -85.84716796875,\n              37.63163475580643\n            ],\n            [\n              -85.93505859374999,\n              37.63163475580643\n            ],\n            [\n              -85.7373046875,\n              36.914764288955936\n            ],\n            [\n              -84.9462890625,\n              36.94989178681327\n            ],\n            [\n              -82.85888671875,\n              37.24782120155428\n            ],\n            [\n              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,{"id":70188681,"text":"70188681 - 1982 - The thermodynamic properties of fluor-topaz","interactions":[],"lastModifiedDate":"2017-06-21T10:22:55","indexId":"70188681","displayToPublicDate":"1982-12-31T00:00:00","publicationYear":"1982","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":738,"text":"American Mineralogist","active":true,"publicationSubtype":{"id":10}},"title":"The thermodynamic properties of fluor-topaz","docAbstract":"<p>No abstract available</p>","language":"English","publisher":"Mineralogical Society of America","usgsCitation":"Barton, M., Haselton, H., Hemingway, B.S., Kleppa, O., and Robie, R.A., 1982, The thermodynamic properties of fluor-topaz: American Mineralogist, v. 67, no. 3-4, p. 350-355.","productDescription":"6 p.","startPage":"350","endPage":"355","costCenters":[],"links":[{"id":342704,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"67","issue":"3-4","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"594b85b7e4b062508e382bbe","contributors":{"authors":[{"text":"Barton, M.D.","contributorId":11341,"corporation":false,"usgs":true,"family":"Barton","given":"M.D.","email":"","affiliations":[],"preferred":false,"id":698879,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Haselton, H.T.","contributorId":16437,"corporation":false,"usgs":true,"family":"Haselton","given":"H.T.","affiliations":[],"preferred":false,"id":698880,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Hemingway, B. S.","contributorId":7268,"corporation":false,"usgs":true,"family":"Hemingway","given":"B.","email":"","middleInitial":"S.","affiliations":[],"preferred":false,"id":698881,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Kleppa, O.J.","contributorId":193159,"corporation":false,"usgs":false,"family":"Kleppa","given":"O.J.","email":"","affiliations":[],"preferred":false,"id":698882,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"Robie, R. A.","contributorId":71237,"corporation":false,"usgs":true,"family":"Robie","given":"R.","email":"","middleInitial":"A.","affiliations":[],"preferred":false,"id":698883,"contributorType":{"id":1,"text":"Authors"},"rank":5}]}}
,{"id":70188984,"text":"70188984 - 1982 - Paleoenvironment and age of kaolin deposits in the Andersonville district, Georgia","interactions":[],"lastModifiedDate":"2017-06-28T11:11:04","indexId":"70188984","displayToPublicDate":"1982-12-31T00:00:00","publicationYear":"1982","noYear":false,"publicationType":{"id":24,"text":"Conference Paper"},"publicationSubtype":{"id":19,"text":"Conference Paper"},"title":"Paleoenvironment and age of kaolin deposits in the Andersonville district, Georgia","docAbstract":"<p>The kaolin deposits of the Andersonville district of Georgia are thick and relatively pure; they grade laterally and vertically into sandy kaolin and sand. The sedimentological and mineralogical character of the clay and the enclosing sand suggests deposition in a marine shallow-water to estuarine environment. Palynomorph and invertebrate fossil assemblages from strata adjacent to the kaolin beds support the suggested depositional environment of the kaolin and the subsequent subaerial formation of bauxite. Movement on the Andersonville and related faults probably influenced basinal topography and served to maintain a restricted circulation in the basin. Sporomorph biostratigraphy limits the accumulation of kaolin and the formation of bauxite deposits to early Wilcox (late Paleocene) time.</p>","largerWorkType":{"id":24,"text":"Conference Paper"},"largerWorkTitle":"Proceedings: Second Symposium on the Geology of the Southeastern Coastal Plain","largerWorkSubtype":{"id":19,"text":"Conference Paper"},"conferenceTitle":"Second Symposium on the Geology of the Southeastern Coastal Plain","conferenceDate":"March 5-6, 1979","conferenceLocation":"Americus, GA","language":"English","publisher":"Georgia Department of Natural Resources","publisherLocation":"Atlanta, GA","usgsCitation":"Cofer, H.E., and Frederiksen, N.O., 1982, Paleoenvironment and age of kaolin deposits in the Andersonville district, Georgia, <i>in</i> Proceedings: Second Symposium on the Geology of the Southeastern Coastal Plain, no. 53, Americus, GA, March 5-6, 1979, p. 24-37.","productDescription":"14 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,{"id":70195436,"text":"70195436 - 1982 - Northern East Pacific Rise: Magnetic anomaly and bathymetric framework","interactions":[],"lastModifiedDate":"2018-03-05T15:13:24","indexId":"70195436","displayToPublicDate":"1982-12-31T00:00:00","publicationYear":"1982","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":2314,"text":"Journal of Geophysical Research B: Solid Earth","active":true,"publicationSubtype":{"id":10}},"title":"Northern East Pacific Rise: Magnetic anomaly and bathymetric framework","docAbstract":"<p><span>The oceanic crust in the eastern Pacific between 7°N and 30°N and east of 127°W contains a fairly complete history of the spreading centers associated with the East Pacific Rise since 25 m.y. B.P. (late Oligocene). In this paper, we have summarized the seafloor spreading magnetic-anomaly data and the bathymetric data that reflect the record of this tectonic history. The well-defined magnetic lineations north of the Clarion fracture zone, in the mouth of the Gulf of California, and on the east flank of the East Pacific Rise (EPR) are carefully examined and used to provide a guide for interpreting the spreading pattern between the Clarion and Clipperton fracture zones, southward of the Rivera fracture zone over the Mathematician Ridge, and over the entire EPR east of the Mathematician Ridge between the Rivera and Siqueiros fracture zones. The bathymetric data provide a trace of the fracture zone pattern in each of the above mentioned areas. The fracture zone bathymetry and the seafloor spreading magnetic lineations on the EPR south of the Rivera fracture zone have a distinctive fanning pattern caused by close poles of rotation and plate boundary reorganizations. All these data provide a good record of the plate reorganizations in the middle Miocene at magnetic anomaly 5 A time (12.5 to 11 m.y. B.P.), in the late Miocene at magnetic anomaly 3′−4 time (6.5 m.y. B.P.), and in the Pliocene at magnetic anomaly 2′−3 time (3.5 m.y. B.P.). Several abandoned spreading centers, including the Mathematician Ridge, were left behind as a result of these reorganizations. The Mathematician Ridge is shown to be a set of ridges and trough whose origin is related to the tectonic activity associated with each of the above mentioned reorganizations since anomaly 5A.</span></p>","language":"English","publisher":"American Geophysical Union","doi":"10.1029/JB087iB08p06725","usgsCitation":"Klitgord, K.D., and Mammerickx, J., 1982, Northern East Pacific Rise: Magnetic anomaly and bathymetric framework: Journal of Geophysical Research B: Solid Earth, v. 87, no. B8, p. 6725-6750, https://doi.org/10.1029/JB087iB08p06725.","productDescription":"26 p.","startPage":"6725","endPage":"6750","costCenters":[{"id":678,"text":"Woods Hole Coastal and Marine Science Center","active":true,"usgs":true}],"links":[{"id":351623,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"87","issue":"B8","noUsgsAuthors":false,"publicationDate":"2012-09-20","publicationStatus":"PW","scienceBaseUri":"5aff4241e4b0da30c1bfdac1","contributors":{"authors":[{"text":"Klitgord, Kim D.","contributorId":82307,"corporation":false,"usgs":true,"family":"Klitgord","given":"Kim","email":"","middleInitial":"D.","affiliations":[{"id":678,"text":"Woods Hole Coastal and Marine Science Center","active":true,"usgs":true}],"preferred":false,"id":728600,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Mammerickx, Jacqueline","contributorId":202504,"corporation":false,"usgs":false,"family":"Mammerickx","given":"Jacqueline","email":"","affiliations":[],"preferred":false,"id":728601,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":70188931,"text":"70188931 - 1982 - Geologic hazards in Navarin Basin Province, Northern Bering Sea","interactions":[],"lastModifiedDate":"2017-12-08T12:31:48","indexId":"70188931","displayToPublicDate":"1982-12-31T00:00:00","publicationYear":"1982","noYear":false,"publicationType":{"id":24,"text":"Conference Paper"},"publicationSubtype":{"id":19,"text":"Conference Paper"},"title":"Geologic hazards in Navarin Basin Province, Northern Bering Sea","docAbstract":"<p><span>Navarin Basin, scheduled for leasing in 1984 (OCS sale 83), may contain vast accumulations of oil and gas. Several geologic and oceanographic processes that may be active in and around Navarin Basin province could be hazardous to commercial development. These potential hazards include submarine slides; sea-floor instability resulting from disturbance of gas-charged sediment; sediment transport and erosion caused by storm waves, tsunamis, internal waves, or bottom currents; pack ice; and active faults and ground motion. </span></p>","largerWorkType":{"id":4,"text":"Book"},"largerWorkTitle":"Proceedings- Offshore Technology Conference","largerWorkSubtype":{"id":12,"text":"Conference publication"},"conferenceTitle":"Offshore Technology Conference","conferenceDate":"May 3-6, 1982","conferenceLocation":"Houston, TX","language":"English","publisher":"Offshore Technology Conference","doi":"10.4043/4172-MS","usgsCitation":"Carlson, P.R., Karl, H.A., Fischer, J.M., and Edwards, B.D., 1982, Geologic hazards in Navarin Basin Province, Northern Bering Sea, <i>in</i> Proceedings- Offshore Technology Conference, v. 14, Houston, TX, May 3-6, 1982, p. 73-87, https://doi.org/10.4043/4172-MS.","productDescription":"15 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]\n}","volume":"14","noUsgsAuthors":false,"publicationDate":"1982-05-03","publicationStatus":"PW","scienceBaseUri":"59536eece4b062508e3c7b4a","contributors":{"authors":[{"text":"Carlson, Paul R.","contributorId":81469,"corporation":false,"usgs":true,"family":"Carlson","given":"Paul","email":"","middleInitial":"R.","affiliations":[],"preferred":false,"id":701351,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Karl, Herman A.","contributorId":80649,"corporation":false,"usgs":true,"family":"Karl","given":"Herman","email":"","middleInitial":"A.","affiliations":[],"preferred":false,"id":701352,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Fischer, Jeffrey M. 0000-0003-2996-9272 fischer@usgs.gov","orcid":"https://orcid.org/0000-0003-2996-9272","contributorId":138825,"corporation":false,"usgs":true,"family":"Fischer","given":"Jeffrey","email":"fischer@usgs.gov","middleInitial":"M.","affiliations":[{"id":470,"text":"New Jersey Water Science Center","active":true,"usgs":true}],"preferred":false,"id":701353,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Edwards, Brian D. bedwards@usgs.gov","contributorId":3161,"corporation":false,"usgs":true,"family":"Edwards","given":"Brian","email":"bedwards@usgs.gov","middleInitial":"D.","affiliations":[{"id":520,"text":"Pacific Coastal and Marine Science Center","active":true,"usgs":true}],"preferred":true,"id":701354,"contributorType":{"id":1,"text":"Authors"},"rank":4}]}}
,{"id":70188925,"text":"70188925 - 1982 - United States gold resource profile; reply","interactions":[],"lastModifiedDate":"2017-06-27T15:15:13","indexId":"70188925","displayToPublicDate":"1982-12-31T00:00:00","publicationYear":"1982","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1472,"text":"Economic Geology","active":true,"publicationSubtype":{"id":10}},"title":"United States gold resource profile; reply","docAbstract":"<p>No abstract available</p>","language":"English","publisher":"Society of Economic Geologists","doi":"10.2113/gsecongeo.77.5.1244","usgsCitation":"Cargill, S.M., 1982, United States gold resource profile; reply: Economic Geology, v. 77, no. 5, p. 1244-1247, https://doi.org/10.2113/gsecongeo.77.5.1244.","productDescription":"4 p.","startPage":"1244","endPage":"1247","costCenters":[],"links":[{"id":343016,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"77","issue":"5","noUsgsAuthors":false,"publicationDate":"1982-08-01","publicationStatus":"PW","scienceBaseUri":"59536ee1e4b062508e3c7b21","contributors":{"authors":[{"text":"Cargill, Simon M.","contributorId":7256,"corporation":false,"usgs":true,"family":"Cargill","given":"Simon","email":"","middleInitial":"M.","affiliations":[],"preferred":false,"id":701296,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":70195610,"text":"70195610 - 1982 - Marine geologic studies of the inner continental shelf off Massachusetts","interactions":[],"lastModifiedDate":"2018-02-23T12:42:28","indexId":"70195610","displayToPublicDate":"1982-12-31T00:00:00","publicationYear":"1982","noYear":false,"publicationType":{"id":24,"text":"Conference Paper"},"publicationSubtype":{"id":19,"text":"Conference Paper"},"title":"Marine geologic studies of the inner continental shelf off Massachusetts","docAbstract":"<p>No abstract available.</p>","largerWorkTitle":"Geotechnology in Massachusetts","language":"English","publisher":"University of Massachusetts","publisherLocation":"Amherst, MA","usgsCitation":"O’Hara, C.J., Oldale, R.N., and Farquhar, O., 1982, Marine geologic studies of the inner continental shelf off Massachusetts, <i>in</i> Geotechnology in Massachusetts, p. 539-549.","productDescription":"11 p.","startPage":"539","endPage":"549","costCenters":[{"id":678,"text":"Woods Hole Coastal and Marine Science 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