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\"}}]}","volume":"70 ","issue":"5","noUsgsAuthors":false,"publicationStatus":"PW","contributors":{"authors":[{"text":"Wells, F. G.","contributorId":7324,"corporation":false,"usgs":true,"family":"Wells","given":"F.","email":"","middleInitial":"G.","affiliations":[],"preferred":false,"id":775264,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Walker, G.W.","contributorId":100917,"corporation":false,"usgs":true,"family":"Walker","given":"G.W.","email":"","affiliations":[],"preferred":false,"id":775265,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Merriam, C.W.","contributorId":51350,"corporation":false,"usgs":true,"family":"Merriam","given":"C.W.","email":"","affiliations":[],"preferred":false,"id":775266,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}} ,{"id":70197729,"text":"70197729 - 1959 - K-feldspar content of Jurassic and Cretaceous graywackes of northern Coast Ranges and Sacramento Valley, California","interactions":[],"lastModifiedDate":"2023-02-01T14:38:56.550016","indexId":"70197729","displayToPublicDate":"1959-12-31T00:00:00","publicationYear":"1959","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":"K-feldspar content of Jurassic and Cretaceous graywackes of northern Coast Ranges and Sacramento Valley, California","docAbstract":"Graywackes of Late Jurassic to Late Cretaceous age are the predominant rocks in the northern Coast Ranges and the western Sacramento Valley provinces in California. These graywackes are similar in appearance, but their content of K-feldspar, which can be readily estimated after selective staining, differs widely. Study of several hundred specimens indicates that K-feldspar content is helpful in correlating or distinguishing these rocks, and sheds light on the geologic history of western California.
In the Sacramento Valley a conformable sequence of Knoxville (Upper Jurassic), Shasta (Lower Cretaceous), and Upper Cretaceous rocks progressively increases in average K-feldspar content with decreasing age. Graywackes of the Franciscan formation, lying in the Coast Ranges farther west, generally contain no K-feldspar, although some contain a trace, and a few of more uncertain affiliation contain large amounts. Another belt of graywackes, west of the Franciscan formation and paralleling the Pacific shore, contains nearly as much K-feldspar as the Upper Cretaceous rocks of the Sacramento Valley, and most of these rocks are probably of middle Cretaceous age.
The writers attribute the increase of K-feldspar with decreasing age of the rocks of the Sacramento Valley to changes in the source area, which is believed to be the Klamath Mountains and the Sierra Nevada. The changes include an increase in proportion of granitic rocks to others as the areas were stripped, and more abundant K-feldspar in the younger granitic rocks. The high K-feldspar content in the middle Cretaceous rocks of the coastal belt suggests that the rocks were deposited in the same basin as the Sacramento Valley rocks.
No abstract available.
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]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b02e4b07f02db698ce8","contributors":{"authors":[{"text":"Kiel, William H. Jr.","contributorId":100449,"corporation":false,"usgs":true,"family":"Kiel","given":"William","suffix":"Jr.","email":"","middleInitial":"H.","affiliations":[],"preferred":false,"id":218239,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":70010688,"text":"70010688 - 1959 - Age of marginal Wisconsin drift at Corry, northwestern Pennsylvania","interactions":[],"lastModifiedDate":"2026-02-27T15:22:26.019651","indexId":"70010688","displayToPublicDate":"1959-12-25T00:00:00","publicationYear":"1959","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":3338,"text":"Science","active":true,"publicationSubtype":{"id":10}},"title":"Age of marginal Wisconsin drift at Corry, northwestern Pennsylvania","docAbstract":"Marl began to accumulate about 14,000 years ago, as determined by radiocarbon dating, in a pond in a kettle hole in Kent drift at Corry, Pa., 9 miles inside the Wisconsin drift margin. This radiocarbon age represents the minimum time since the disappearance of the ice from Corry and confirms an assignment of Cary age to the drift.","language":"English","publisher":"American Association for the Advancement of Science","doi":"10.1126/science.130.3391.1760.a","issn":"00368075","usgsCitation":"Droste, J., Rubin, M., and White, G.W., 1959, Age of marginal Wisconsin drift at Corry, northwestern Pennsylvania: Science, v. 130, no. 3391, p. 1760-1760, https://doi.org/10.1126/science.130.3391.1760.a.","productDescription":"1 p.","startPage":"1760","endPage":"1760","costCenters":[],"links":[{"id":219408,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United States","state":"Pennsylvania","city":"Corry","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"coordinates\": [\n [\n [\n -79.68200482460028,\n 41.947621733403906\n ],\n [\n -79.68200482460028,\n 41.904127695039165\n ],\n [\n -79.60218635375541,\n 41.904127695039165\n ],\n [\n -79.60218635375541,\n 41.947621733403906\n ],\n [\n -79.68200482460028,\n 41.947621733403906\n ]\n ]\n ],\n \"type\": \"Polygon\"\n }\n }\n ]\n}","volume":"130","issue":"3391","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"5059e8efe4b0c8380cd47fb8","contributors":{"authors":[{"text":"Droste, J.B.","contributorId":98463,"corporation":false,"usgs":true,"family":"Droste","given":"J.B.","email":"","affiliations":[],"preferred":false,"id":359432,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Rubin, M.","contributorId":88079,"corporation":false,"usgs":true,"family":"Rubin","given":"M.","email":"","affiliations":[],"preferred":false,"id":359431,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"White, G. W.","contributorId":62293,"corporation":false,"usgs":true,"family":"White","given":"G.","email":"","middleInitial":"W.","affiliations":[],"preferred":false,"id":359430,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}} ,{"id":70207256,"text":"70207256 - 1959 - Peneconcordant uranium deposit: A proposed term","interactions":[],"lastModifiedDate":"2020-06-01T20:02:16.284558","indexId":"70207256","displayToPublicDate":"1959-12-13T13:25:59","publicationYear":"1959","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":"Peneconcordant uranium deposit: A proposed term","docAbstract":"The term peneconcordant is proposed to describe the form of the numerous and highly productive U deposits in sedimentary rocks of the Colorado Plateau, Wyoming, the Dakotas, and Texas. Peneconcordant U deposits are tabular, lenticular, or irregularly-shaped masses of widely differing size that are, in general, concordant to the gross sedimentary structures of the enclosing rock but that in detail cut across sedimentary structures. They differ from vein deposits in that they do not occupy or follow fractures or shear zones in the sedimentary rocks. Furthermore, they are not coextensive with a specific lithologic unit, such as U-bearing marine black shale. The many terms now used to describe these U deposits are based variously on petrographic, mineralogic, geographic, and genetic considerations; none is satisfactory for describing all these deposits having a common and distinctive form. Furthermore, some of the terms are ambiguous and have been commonly used to group together deposits having distinctly different forms. The term peneconcordant U deposit clearly sets apart a widespread and important type of U deposit that has a common and distinctive form, namely, nearly concordant to the bedding of the host rock. The meaning of the term is self-evident, and the term is readily applicable to field usage.
","language":"English","publisher":"Society of Economic Geologist","doi":"10.2113/gsecongeo.54.5.944","usgsCitation":"Finch, W., 1959, Peneconcordant uranium deposit: A proposed term: Economic Geology, v. 54, p. 944-946, https://doi.org/10.2113/gsecongeo.54.5.944.","productDescription":"3 p.","startPage":"944","endPage":"946","costCenters":[],"links":[{"id":370263,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"54","noUsgsAuthors":false,"publicationDate":"1959-08-01","publicationStatus":"PW","contributors":{"authors":[{"text":"Finch, W.I.","contributorId":75919,"corporation":false,"usgs":true,"family":"Finch","given":"W.I.","email":"","affiliations":[],"preferred":false,"id":777473,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":70206770,"text":"70206770 - 1959 - Paleozoic and mesozoic fossils in a thick stratigraphic section in the eastern Sierra Nevada, California","interactions":[],"lastModifiedDate":"2019-11-21T13:15:24","indexId":"70206770","displayToPublicDate":"1959-11-21T13:15:01","publicationYear":"1959","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1723,"text":"GSA Bulletin","active":true,"publicationSubtype":{"id":10}},"title":"Paleozoic and mesozoic fossils in a thick stratigraphic section in the eastern Sierra Nevada, California","docAbstract":"A thick section of metamorphosed Paleozoic and Mesozoic rocks is exposed in two roof pend- ants, one each in the Mount Morrison and Devils Postpile quadrangles in the eastern Sierra Nevada near Mammoth Lakes, Cali- fornia (Fig. 1). In the course of geologic mapping in these quadrangles by the U. S. Geo- logical Survey in co-operation with the California Division of Mines, fossils of Ordovician, Pennsylvanian, Permian(P), and Early Jurassic ages were collected from weakly metamorphosed parts of the pendants. Detailed map- ping in the Mount Morrison quadrangle has been completed by Rinehart and Ross, and a report on this area is in preparation. Similar mapping in the Devils Postpile quadrangle by Rinehart and Huber is in progress. In the part of the Devils Postpile quadrangle not yet covered in the present study, the contacts shown on the map (Fig. 1) are after Erwin (1934). Because diagnostic fossils are extremely rare in the metamorphic rocks of the Sierra Nevada, these fossils are considered important enough to merit this short note prior to completion of the detailed mapping in the Devils Postpile quadrangle and the publication of more comprehensive reports on the two quadrangles
","language":"English","publisher":"GSA","doi":"10.1130/0016-7606(1959)70[941:PAMFIA]2.0.CO;2","usgsCitation":"Huber, N., 1959, Paleozoic and mesozoic fossils in a thick stratigraphic section in the eastern Sierra Nevada, California: GSA Bulletin, v. 70, no. 7, p. 141-146, https://doi.org/10.1130/0016-7606(1959)70[941:PAMFIA]2.0.CO;2.","productDescription":"6 p.","startPage":"141","endPage":"146","onlineOnly":"Y","costCenters":[],"links":[{"id":369391,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United States","state":"California","otherGeospatial":"Mammoth Lakes Region","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"type\": \"Polygon\",\n \"coordinates\": [\n [\n [\n -119.15,\n 37.45\n ],\n [\n -118.45,\n 37.45\n ],\n [\n -118.45,\n 37.30\n ],\n [\n -119.15,\n 37.30\n ],\n [\n -119.15,\n 37.45\n ]\n ]\n ]\n }\n }\n ]\n}","volume":"70","issue":"7","noUsgsAuthors":false,"publicationStatus":"PW","contributors":{"authors":[{"text":"Huber, N.K.","contributorId":73610,"corporation":false,"usgs":true,"family":"Huber","given":"N.K.","affiliations":[],"preferred":false,"id":775719,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":70206769,"text":"70206769 - 1959 - Some aspects of the origin of the Ironwood iron-formation of Michigan and Wisconsin ","interactions":[],"lastModifiedDate":"2019-11-21T11:50:28","indexId":"70206769","displayToPublicDate":"1959-11-21T11:41:35","publicationYear":"1959","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":"Some aspects of the origin of the Ironwood iron-formation of Michigan and Wisconsin ","docAbstract":"The Ironwood iron-formation of the Gogebic Range of Michigan and Wisconsin is made up of several rock types, each of which is characterized by a different iron-rich mineral: hematite, magnetite, pyrite, iron carbonate, or iron silicate (minnesotaite, stilpnomelane). Where the Ironwood iron-formation is relatively unaltered the Plymouth, Norrie, and Anvil members consist of wavy-bedded magnetite and silicate-rich rocks, whereas the Yale and Pence members consist of even-bedded carbonate, silicate, magnetite, and pyrite-rich rocks. These rock types represent primary facies of the iron-formation that were deposited under differing physical and chemical conditions during a period of continuous iron-rich sedimentation. Animikie sedimentation in the Gogebic district began with the deposition of sandstone and dolomitic limestone in a shallow sea advancing over a low-lying land mass of lower Precambrian granite and green-stone. Continued advance of the sea, with effective separation of clastic material near shore, permitted the dominantly chemical sedimentation of the iron- formation in somewhat deeper water. The development of an off-shore basin with partially restricted circulation would have facilitated such deposition. Minor fluctuations in the physical and chemical conditions within the depositional environment are reflected in the differing facies of the iron-formation. Deposition of the iron and silica-rich chemical sediments was terminated by increased tectonism and the deposition of the thick sequence of slates and graywackes of the Tyler formation.
","language":"English","publisher":"Society of Economic Geologist","doi":"10.2113/gsecongeo.54.1.82","usgsCitation":"Huber, N., 1959, Some aspects of the origin of the Ironwood iron-formation of Michigan and Wisconsin : Economic Geology, v. 54, no. 1, p. 82-118, https://doi.org/10.2113/gsecongeo.54.1.82.","productDescription":"37 p.","startPage":"82","endPage":"118","costCenters":[],"links":[{"id":369389,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United States","state":"Michigan, Wisconsin","otherGeospatial":"The Gogebic Range of Michigan and Wisconsin","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"type\": \"Polygon\",\n \"coordinates\": [\n [\n [\n -88.209228515625,\n 45.01918507438176\n ],\n [\n -87.637939453125,\n 44.83249999349062\n ],\n [\n -85.682373046875,\n 47.19717795172789\n ],\n [\n -85.660400390625,\n 48.42191010942875\n ],\n [\n -93.18603515624999,\n 48.334343174592014\n ],\n [\n -93.42773437499999,\n 46.5286346952717\n ],\n [\n -88.209228515625,\n 45.01918507438176\n ]\n ]\n ]\n }\n }\n ]\n}","volume":"54","issue":"1","noUsgsAuthors":false,"publicationDate":"1959-01-01","publicationStatus":"PW","contributors":{"authors":[{"text":"Huber, N.K.","contributorId":73610,"corporation":false,"usgs":true,"family":"Huber","given":"N.K.","affiliations":[],"preferred":false,"id":775718,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":70010947,"text":"70010947 - 1959 - Modern instruments for surveying and mapping","interactions":[],"lastModifiedDate":"2026-02-27T15:32:47.503419","indexId":"70010947","displayToPublicDate":"1959-10-23T00:00:00","publicationYear":"1959","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":3338,"text":"Science","active":true,"publicationSubtype":{"id":10}},"title":"Modern instruments for surveying and mapping","docAbstract":"New surveying systems utilizing photogrammetry and electronics speed production of topographic maps.","language":"English","publisher":"American Association for the Advancement of Science","doi":"10.1126/science.130.3382.1059","issn":"00368075","usgsCitation":"Whitmore, G., Thompson, M., and Speert, J.L., 1959, Modern instruments for surveying and mapping: Science, v. 130, no. 3382, p. 1059-1066, https://doi.org/10.1126/science.130.3382.1059.","productDescription":"8 p.","startPage":"1059","endPage":"1066","costCenters":[],"links":[{"id":220874,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"130","issue":"3382","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"505a5c96e4b0c8380cd6fddc","contributors":{"authors":[{"text":"Whitmore, G.D.","contributorId":41588,"corporation":false,"usgs":true,"family":"Whitmore","given":"G.D.","email":"","affiliations":[],"preferred":false,"id":359952,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Thompson, M.M.","contributorId":78876,"corporation":false,"usgs":true,"family":"Thompson","given":"M.M.","email":"","affiliations":[],"preferred":false,"id":359954,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Speert, J. L.","contributorId":43100,"corporation":false,"usgs":true,"family":"Speert","given":"J.","email":"","middleInitial":"L.","affiliations":[],"preferred":false,"id":359953,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}} ,{"id":1014250,"text":"1014250 - 1959 - Infectious nature of pancreatic necrosis","interactions":[],"lastModifiedDate":"2026-04-15T17:02:36.647908","indexId":"1014250","displayToPublicDate":"1959-10-01T00:00:00","publicationYear":"1959","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":3624,"text":"Transactions of the American Fisheries Society","active":true,"publicationSubtype":{"id":10}},"title":"Infectious nature of pancreatic necrosis","docAbstract":"To determine if pancreatic necrosis is a communicable disease of trout, lots of eyed brook trout eggs were obtained from four hatcheries. Pancreatic necrosis appeared spontaneously in trout from one of these hatcheries and the other strains were exposed to infection by suspension prepared from diseased fish. In all cases, typical pancreatic necrosis appeared in fish exposed to infection and the control fish remained healthy. Disease was more acute in fry fed brine shrimp nauplii than in those fed beef liver. Mortality data suggest that susceptibility to pancreatic necrosis decreases with the increased age of trout. No treatment for the disease is known, but sanitary measures were effective in preventing its spread.
","language":"English","publisher":"American Fisheries Society","doi":"10.1577/1548-8659(1959)88[289:INOPN]2.0.CO;2","usgsCitation":"Snieszko, S.F., Wolf, K., Camper, J., and Pettijohn, L., 1959, Infectious nature of pancreatic necrosis: Transactions of the American Fisheries Society, v. 88, no. 4, p. 289-293, https://doi.org/10.1577/1548-8659(1959)88[289:INOPN]2.0.CO;2.","productDescription":"5 p.","startPage":"289","endPage":"293","costCenters":[{"id":365,"text":"Leetown Science Center","active":true,"usgs":true}],"links":[{"id":131782,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"88","issue":"4","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e49f1e4b07f02db5ee934","contributors":{"authors":[{"text":"Snieszko, S. F.","contributorId":13169,"corporation":false,"usgs":true,"family":"Snieszko","given":"S.","middleInitial":"F.","affiliations":[],"preferred":false,"id":320053,"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":320054,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Camper, J.E.","contributorId":55782,"corporation":false,"usgs":true,"family":"Camper","given":"J.E.","email":"","affiliations":[],"preferred":false,"id":320056,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Pettijohn, L.L.","contributorId":32878,"corporation":false,"usgs":true,"family":"Pettijohn","given":"L.L.","email":"","affiliations":[],"preferred":false,"id":320055,"contributorType":{"id":1,"text":"Authors"},"rank":4}]}} ,{"id":70010644,"text":"70010644 - 1959 - Time-lapse motion picture technique applied to the study of geological processes","interactions":[],"lastModifiedDate":"2026-02-27T15:44:04.188629","indexId":"70010644","displayToPublicDate":"1959-09-25T00:00:00","publicationYear":"1959","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":3338,"text":"Science","active":true,"publicationSubtype":{"id":10}},"title":"Time-lapse motion picture technique applied to the study of geological processes","docAbstract":"Light-weight, battery-operated timers were built and coupled to 16-mm motion-picture cameras having apertures controlled by photoelectric cells. The cameras were placed adjacent to Emmons Glacier on Mount Rainier. The film obtained confirms the view that exterior time-lapse photography can be applied to the study of slow-acting geologic processes.","language":"English","publisher":"American Association for the Advancement of Science","doi":"10.1126/science.130.3378.795","issn":"00368075","usgsCitation":"Miller, R., and Crandell, D.R., 1959, Time-lapse motion picture technique applied to the study of geological processes: Science, v. 130, no. 3378, p. 795-796, https://doi.org/10.1126/science.130.3378.795.","productDescription":"2 p.","startPage":"795","endPage":"796","costCenters":[],"links":[{"id":219314,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United States","state":"Washington","otherGeospatial":"Mount Rainier","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"coordinates\": [\n [\n [\n -122.09680003106901,\n 47.06480388005761\n ],\n [\n -122.09680003106901,\n 46.489924062549875\n ],\n [\n -121.37770581227939,\n 46.489924062549875\n ],\n [\n -121.37770581227939,\n 47.06480388005761\n ],\n [\n -122.09680003106901,\n 47.06480388005761\n ]\n ]\n ],\n \"type\": \"Polygon\"\n }\n }\n ]\n}","volume":"130","issue":"3378","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"505bb3c6e4b08c986b325fbc","contributors":{"authors":[{"text":"Miller, R. D.","contributorId":92693,"corporation":false,"usgs":true,"family":"Miller","given":"R. D.","affiliations":[],"preferred":false,"id":359341,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Crandell, D. R.","contributorId":78385,"corporation":false,"usgs":true,"family":"Crandell","given":"D.","email":"","middleInitial":"R.","affiliations":[],"preferred":false,"id":359340,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":70010966,"text":"70010966 - 1959 - Mummified seal carcasses in the McMurdo Sound region, Antarctica","interactions":[],"lastModifiedDate":"2026-02-27T15:52:29.236893","indexId":"70010966","displayToPublicDate":"1959-09-18T00:00:00","publicationYear":"1959","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":3338,"text":"Science","active":true,"publicationSubtype":{"id":10}},"title":"Mummified seal carcasses in the McMurdo Sound region, Antarctica","docAbstract":"Information was collected on 90 mummified carcasses of the \"crab-eater\" seal in the ice-free areas of the McMurdo Sound region, Antarctica. The carcasses range from relatively well-preserved bodies to merely old, twisted, wind-dissected fragments of tissue. They are hard and dry and lie on the surface of the ground, mostly in valley bottoms. The arid, cold climate is ideal for retarding organic decay. One carcass was dated by radiocarbon analysis and found to be be-tween 1600 and 2600 years old.","language":"English","publisher":"American Association for the Advancement of Science","doi":"10.1126/science.130.3377.716","issn":"00368075","usgsCitation":"Pewe, T.L., Rivard, N., and Llano, G., 1959, Mummified seal carcasses in the McMurdo Sound region, Antarctica: Science, v. 130, no. 3377, p. 716-716, https://doi.org/10.1126/science.130.3377.716.","productDescription":"1 p.","startPage":"716","endPage":"716","costCenters":[],"links":[{"id":221083,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"otherGeospatial":"McMurdo Sound region, Antarctica","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"coordinates\": [\n [\n [\n -197.16416821250053,\n -77.08686092688944\n ],\n [\n -197.16416821250053,\n -77.9860072187833\n ],\n [\n -192.04923168218593,\n -77.9860072187833\n ],\n [\n -192.04923168218593,\n -77.08686092688944\n ],\n [\n -197.16416821250053,\n -77.08686092688944\n ]\n ]\n ],\n \"type\": \"Polygon\"\n }\n }\n ]\n}","volume":"130","issue":"3377","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"505a60c0e4b0c8380cd71662","contributors":{"authors":[{"text":"Pewe, T. L.","contributorId":35786,"corporation":false,"usgs":true,"family":"Pewe","given":"T.","email":"","middleInitial":"L.","affiliations":[],"preferred":false,"id":359986,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Rivard, N.R.","contributorId":81186,"corporation":false,"usgs":true,"family":"Rivard","given":"N.R.","email":"","affiliations":[],"preferred":false,"id":359988,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Llano, G.A.","contributorId":56335,"corporation":false,"usgs":true,"family":"Llano","given":"G.A.","email":"","affiliations":[],"preferred":false,"id":359987,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}} ,{"id":70205258,"text":"70205258 - 1959 - John Day to upper Bear Valley, Field Trip no. 5","interactions":[],"lastModifiedDate":"2019-09-12T10:56:07","indexId":"70205258","displayToPublicDate":"1959-09-12T10:55:56","publicationYear":"1959","noYear":false,"publicationType":{"id":5,"text":"Book chapter"},"seriesNumber":"50","title":"John Day to upper Bear Valley, Field Trip no. 5","docAbstract":"No abstract available
","largerWorkType":{"id":4,"text":"Book"},"largerWorkTitle":"Field guidebook: Geologic trips along Oregon highways","largerWorkSubtype":{"id":15,"text":"Monograph"},"language":"English","publisher":"Oregon Department of Geology and Mineral Industries","usgsCitation":"Wilkinson , W., and Thayer, T.P., 1959, John Day to upper Bear Valley, Field Trip no. 5, chap. of Field guidebook: Geologic trips along Oregon highways, p. 99-102.","productDescription":"4 p.","startPage":"99","endPage":"102","costCenters":[],"links":[{"id":367391,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"},{"id":367388,"rank":1,"type":{"id":15,"text":"Index Page"},"url":"https://www.oregongeology.org/pubs/B/p-B.htm"}],"country":"United States","state":"Oregon","city":"John Day","otherGeospatial":"Upper Bear Valley","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"type\": \"Polygon\",\n \"coordinates\": [\n [\n [\n -119.05883789062501,\n 44.17136989600329\n ],\n [\n -118.90914916992188,\n 44.17136989600329\n ],\n [\n -118.90914916992188,\n 44.42691515712095\n ],\n [\n -119.05883789062501,\n 44.42691515712095\n ],\n [\n -119.05883789062501,\n 44.17136989600329\n ]\n ]\n ]\n }\n }\n ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","contributors":{"authors":[{"text":"Wilkinson , William Donald ","contributorId":218871,"corporation":false,"usgs":false,"family":"Wilkinson ","given":"William Donald ","affiliations":[{"id":7198,"text":"Oregon Department Geology and Mineral Industries","active":true,"usgs":false},{"id":6605,"text":"USGS","active":true,"usgs":false}],"preferred":false,"id":770586,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Thayer, Thomas P","contributorId":218870,"corporation":false,"usgs":false,"family":"Thayer","given":"Thomas","email":"","middleInitial":"P","affiliations":[{"id":6605,"text":"USGS","active":true,"usgs":false},{"id":7198,"text":"Oregon Department Geology and Mineral Industries","active":true,"usgs":false}],"preferred":false,"id":770587,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":37826,"text":"37826 - 1959 - Big game inventory for 1958","interactions":[],"lastModifiedDate":"2014-07-24T10:36:52","indexId":"37826","displayToPublicDate":"1959-09-01T10:36:11","publicationYear":"1959","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":1,"text":"Federal Government Series"},"seriesTitle":{"id":98,"text":"Wildlife Leaflet","active":false,"publicationSubtype":{"id":1}},"seriesNumber":"411","title":"Big game inventory for 1958","docAbstract":"No abstract available.","language":"English","publisher":"U.S. Department of the Interior","publisherLocation":"Washington, D.C.","collaboration":"Compiled in the Bird and Mammal Laboratories, Branch of Wildlife Research, Bureau of Sport Fisheries and Wildlife.","usgsCitation":"U.S. Bureau of Sport Fisheries and Wildlife, 1959, Big game inventory for 1958 (Revises Wildlife Leaflet BS-342 (1952).): Wildlife Leaflet 411, 4 p.","productDescription":"4 p.","numberOfPages":"4","costCenters":[],"links":[{"id":290877,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"edition":"Revises Wildlife Leaflet BS-342 (1952).","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"57ffd2a0e4b0824b2d176bcb","contributors":{"authors":[{"text":"U.S. Bureau of Sport Fisheries and Wildlife","contributorId":128149,"corporation":true,"usgs":false,"organization":"U.S. Bureau of Sport Fisheries and Wildlife","id":529746,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":70160572,"text":"70160572 - 1959 - Mycobacterium fortuitum Cruz from the tropical fish Hyphessobrycon innesi","interactions":[],"lastModifiedDate":"2025-03-03T16:47:14.089398","indexId":"70160572","displayToPublicDate":"1959-09-01T00:00:00","publicationYear":"1959","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":2192,"text":"Journal of Bacteriology","active":true,"publicationSubtype":{"id":10}},"title":"Mycobacterium fortuitum Cruz from the tropical fish Hyphessobrycon innesi","docAbstract":"No abstract available.
","language":"English","publisher":"American Society for Microbiology","doi":"10.1128/jb.78.3.392-395.1959","usgsCitation":"Ross, A.J., and Brancato, F., 1959, Mycobacterium fortuitum Cruz from the tropical fish Hyphessobrycon innesi: Journal of Bacteriology, v. 78, no. 3, p. 392-395, https://doi.org/10.1128/jb.78.3.392-395.1959.","productDescription":"4 p.","startPage":"392","endPage":"395","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[{"id":654,"text":"Western Fisheries Research Center","active":true,"usgs":true}],"links":[{"id":488356,"rank":2,"type":{"id":40,"text":"Open Access Publisher Index Page"},"url":"https://doi.org/10.1128/jb.78.3.392-395.1959","text":"Publisher Index Page"},{"id":312780,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"78","issue":"3","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"567bd3bae4b0a04ef491a1ec","contributors":{"authors":[{"text":"Ross, A. J.","contributorId":105267,"corporation":false,"usgs":true,"family":"Ross","given":"A.","email":"","middleInitial":"J.","affiliations":[],"preferred":false,"id":583172,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Brancato, F.P.","contributorId":150826,"corporation":false,"usgs":false,"family":"Brancato","given":"F.P.","email":"","affiliations":[],"preferred":false,"id":583173,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":70211897,"text":"70211897 - 1959 - Chemical composition of argillites of the cobalt series (precambrian) and the problem of soda-rich sediments","interactions":[],"lastModifiedDate":"2020-08-11T16:48:13.547768","indexId":"70211897","displayToPublicDate":"1959-08-11T11:35:58","publicationYear":"1959","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1723,"text":"GSA Bulletin","active":true,"publicationSubtype":{"id":10}},"title":"Chemical composition of argillites of the cobalt series (precambrian) and the problem of soda-rich sediments","docAbstract":"Two new chemical analyses show that the varved argillites of the Precambrian Cobalt series of Ontario, Canada, contain more Na2O than K2O and have a Na2O/K2O ratio higher than most pelitic rocks but similar to that found in many graywackes. Published chemical data substantiate these observations. The Cobalt materials are also low in CaO but otherwise have a composition compatible with their presumed glacial origin.
Albitization of the detrital plagioclase feldspar seems to best account for the low lime and high soda content of these rocks. X-ray data confirm the presence of albite.
Spectrographic analyses of the argillites are also given.
","language":"English","publisher":"GSA","doi":"10.1130/0016-7606(1959)70[593:CCOAOT]2.0.CO;2","usgsCitation":"Pettijohn, F., and Bastron, H., 1959, Chemical composition of argillites of the cobalt series (precambrian) and the problem of soda-rich sediments: GSA Bulletin, v. 70, no. 5, p. 593-599, https://doi.org/10.1130/0016-7606(1959)70[593:CCOAOT]2.0.CO;2.","productDescription":"7 p.","startPage":"593","endPage":"599","costCenters":[],"links":[{"id":377340,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"Canada","otherGeospatial":"Ontario","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"type\": \"Polygon\",\n \"coordinates\": [\n [\n [\n -85.18798828125,\n 44.24519901522129\n ],\n [\n -78.50830078125,\n 44.24519901522129\n ],\n [\n -78.50830078125,\n 48.180738507303836\n ],\n [\n -85.18798828125,\n 48.180738507303836\n ],\n [\n -85.18798828125,\n 44.24519901522129\n ]\n ]\n ]\n }\n }\n ]\n}","volume":"70","issue":"5","noUsgsAuthors":false,"publicationStatus":"PW","contributors":{"authors":[{"text":"Pettijohn, F.J.","contributorId":41407,"corporation":false,"usgs":true,"family":"Pettijohn","given":"F.J.","email":"","affiliations":[],"preferred":false,"id":795720,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Bastron, H.","contributorId":20067,"corporation":false,"usgs":true,"family":"Bastron","given":"H.","affiliations":[],"preferred":false,"id":795721,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":70211669,"text":"70211669 - 1959 - Role of fluid pressure in mechanics of overthrust faulting: II. Overthrust belt in geosynclinal area of western Wyoming in light of fluid-pressure hypothesis","interactions":[],"lastModifiedDate":"2020-09-17T20:28:50.7545","indexId":"70211669","displayToPublicDate":"1959-08-06T15:09:47","publicationYear":"1959","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1723,"text":"GSA Bulletin","active":true,"publicationSubtype":{"id":10}},"title":"Role of fluid pressure in mechanics of overthrust faulting: II. Overthrust belt in geosynclinal area of western Wyoming in light of fluid-pressure hypothesis","docAbstract":"Pressures of interstitial fluids significantly greater than the normal hydrostatic pressure are known in many parts of the world. Many occurrences are in thick sections of relatively young sediments; some are in areas that have been intensely deformed. Abnormal fluid pressures in the Gulf Coast region are associated with thick bodies of shale or mudstone, and with high hydraulic gradients across bedding. The rocks there have been buried rather rapidly and are evidently not yet fully compacted. The mechanism by which clay consolidates under pressure affords a quantitative relationship among the variables—depth, strength of clay, and fluid pressure—and this relationship indicates that the Gulf Coast examples agree fairly well with observations on depth and porosity in Paleozoic shales of Oklahoma and Tertiary shales of Venezuela. Critical data are lacking, but permeability clearly decreases tremendously as clay rocks are compacted. This decrease in permeability provides a self-sealing mechanism that greatly retards the escape of pore water from deeply buried clay rocks. The relationship between rate of compaction and the development of abnormal fluid pressures probably applies not only to clay rocks but also to carbonates and possibly to micaceous and chloritic metamorphic rocks. Conditions of geosynclinal deposition are, in general, those most favorable to the development of abnormal fluid pressures.
The hypothesis that large-scale overthrusting is facilitated by abnormal fluid pressures which, in turn, are associated with geosynclinal deposition is applied to the overthrust belt of western Wyoming and adjacent States. This is a long curving belt of several bedding-plane faults which have an aggregate horizontal displacement across the belt of 50 miles or more. The sedimentary rocks that make up the belt were evidently deposited in a major geosyncline bordered by uplands not far to the west. At any given locality, the rate of deposition of the sediments increased continuously until the beginning of intense deformation and overthrusting. The geosynclinal axis and the bordering uplands probably migrated slowly eastward across the belt. Several lines of indirect evidence suggest that abnormal fluid pressures developed in this region during final stages of rapid geosynclinal sinking and that thick plates of Paleozoic and Mesozoic sedimentary rocks sheared off from the underlying rocks and moved slowly eastward. Rate of movement probably was controlled by erosion of upfolds that arose at the front of each moving plate. The fundamental cause of the lateral stresses that propelled the overthrusts is not known, but it may be examined instructively in the light of the fluid-pressure hypothesis. The thrust sheets might, for example, have slid by simple gravitation down the western limb of the geosyncline on reasonable slopes and not improbable fluid pressure-overburden ratios. Such large-scale slumping of thrust sheets, however, seems to require gaps at the rear of the thrust sheets. The long intermontane valleys of Idaho and Utah may possibly have originated as such gaps or rifts, but no proof has yet been recognized that they were formed in this manner. An alternative possibility, regional compression, requires concentration of the lateral stresses within the upper few miles of the earth's crust; in this general region emplacement of the Idaho batholith seems the most likely source of such superficially concentrated stresses. However, this batholith is so far from the front edge of the overthrust belt that it would require extremely high fluid pressure-overburden ratios over a wide area. Perhaps some combination of the two forces—pushing wide thrust plates down a gentle slope—is the most likely explanation.
","language":"English","publisher":"GSA","doi":"10.1130/0016-7606(1959)70[167:ROFPIM]2.0.CO;2","usgsCitation":"Rubey, W.W., and Hubbert, M.K., 1959, Role of fluid pressure in mechanics of overthrust faulting: II. Overthrust belt in geosynclinal area of western Wyoming in light of fluid-pressure hypothesis: GSA Bulletin, v. 70, no. 2, p. 167-206, https://doi.org/10.1130/0016-7606(1959)70[167:ROFPIM]2.0.CO;2.","productDescription":"40 p.","startPage":"167","endPage":"206","costCenters":[],"links":[{"id":377109,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"70","issue":"2","noUsgsAuthors":false,"publicationStatus":"PW","contributors":{"authors":[{"text":"Rubey, William W.","contributorId":16899,"corporation":false,"usgs":true,"family":"Rubey","given":"William","email":"","middleInitial":"W.","affiliations":[],"preferred":false,"id":794966,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Hubbert, M. King","contributorId":50197,"corporation":false,"usgs":true,"family":"Hubbert","given":"M.","email":"","middleInitial":"King","affiliations":[],"preferred":false,"id":794967,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":70211668,"text":"70211668 - 1959 - Minimum age of the lower Devonian Slate near Jackman, Maine","interactions":[],"lastModifiedDate":"2020-08-06T20:02:31.422546","indexId":"70211668","displayToPublicDate":"1959-08-06T14:53:43","publicationYear":"1959","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1723,"text":"GSA Bulletin","active":true,"publicationSubtype":{"id":10}},"title":"Minimum age of the lower Devonian Slate near Jackman, Maine","docAbstract":"No abstract available.
","language":"English","publisher":"GSA","doi":"10.1130/0016-7606(1959)70[947:MAOTLD]2.0.CO;2","usgsCitation":"Hurley, P.M., Boucot, A., Albee, A.L., Faul, H., Pinson, W., and Fairbairn, H.W., 1959, Minimum age of the lower Devonian Slate near Jackman, Maine: GSA Bulletin, v. 70, no. 7, p. 947-950, https://doi.org/10.1130/0016-7606(1959)70[947:MAOTLD]2.0.CO;2.","productDescription":"3 p.","startPage":"947","endPage":"950","costCenters":[],"links":[{"id":377106,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"70","issue":"7","noUsgsAuthors":false,"publicationStatus":"PW","contributors":{"authors":[{"text":"Hurley, Patrick M.","contributorId":12121,"corporation":false,"usgs":true,"family":"Hurley","given":"Patrick","email":"","middleInitial":"M.","affiliations":[],"preferred":false,"id":794956,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Boucot, A. J.","contributorId":30620,"corporation":false,"usgs":true,"family":"Boucot","given":"A. J.","affiliations":[],"preferred":false,"id":794957,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Albee, A. L.","contributorId":77595,"corporation":false,"usgs":true,"family":"Albee","given":"A.","email":"","middleInitial":"L.","affiliations":[],"preferred":false,"id":794958,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Faul, H.","contributorId":101976,"corporation":false,"usgs":true,"family":"Faul","given":"H.","email":"","affiliations":[],"preferred":false,"id":794959,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"Pinson, W.H.","contributorId":237001,"corporation":false,"usgs":false,"family":"Pinson","given":"W.H.","email":"","affiliations":[{"id":12444,"text":"Massachusetts Institute of Technology","active":true,"usgs":false}],"preferred":false,"id":794960,"contributorType":{"id":1,"text":"Authors"},"rank":5},{"text":"Fairbairn, Harold W.","contributorId":22627,"corporation":false,"usgs":true,"family":"Fairbairn","given":"Harold","email":"","middleInitial":"W.","affiliations":[],"preferred":false,"id":794961,"contributorType":{"id":1,"text":"Authors"},"rank":6}]}} ,{"id":70211667,"text":"70211667 - 1959 - Role of fluid pressure in mechanics of overthrust faulting: I. Mechanics of fluid-filled porous solids and its application to overthrust faulting","interactions":[],"lastModifiedDate":"2020-09-17T20:26:52.652084","indexId":"70211667","displayToPublicDate":"1959-08-06T14:22:20","publicationYear":"1959","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1723,"text":"GSA Bulletin","active":true,"publicationSubtype":{"id":10}},"title":"Role of fluid pressure in mechanics of overthrust faulting: I. Mechanics of fluid-filled porous solids and its application to overthrust faulting","docAbstract":"No abstract available.
","language":"English","publisher":"GSA","doi":"10.1130/0016-7606(1959)70[115:ROFPIM]2.0.CO;2","usgsCitation":"Hubbert, M.K., and Rubey, W.W., 1959, Role of fluid pressure in mechanics of overthrust faulting: I. Mechanics of fluid-filled porous solids and its application to overthrust faulting: GSA Bulletin, v. 70, no. 2, p. 115-166, https://doi.org/10.1130/0016-7606(1959)70[115:ROFPIM]2.0.CO;2.","productDescription":"52 p.","startPage":"115","endPage":"166","costCenters":[],"links":[{"id":378544,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"70","issue":"2","noUsgsAuthors":false,"publicationStatus":"PW","contributors":{"authors":[{"text":"Hubbert, M. King","contributorId":50197,"corporation":false,"usgs":true,"family":"Hubbert","given":"M.","email":"","middleInitial":"King","affiliations":[],"preferred":false,"id":794954,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Rubey, William W.","contributorId":16899,"corporation":false,"usgs":true,"family":"Rubey","given":"William","email":"","middleInitial":"W.","affiliations":[],"preferred":false,"id":794955,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":70211666,"text":"70211666 - 1959 - The petroleum potential of the emerged and submerged Atlantic coastal plain of the United States","interactions":[],"lastModifiedDate":"2020-08-06T19:21:22.720799","indexId":"70211666","displayToPublicDate":"1959-08-06T14:02:48","publicationYear":"1959","noYear":false,"publicationType":{"id":24,"text":"Conference Paper"},"publicationSubtype":{"id":19,"text":"Conference Paper"},"title":"The petroleum potential of the emerged and submerged Atlantic coastal plain of the United States","docAbstract":"Increasing geological and geophysical information about the Atlantic continental shelf of the United States is changing the basis for judging the area's petroleum potential. No nation can afford to overlook an area that overlies 175,000 cubic miles (730,000 km3) of possibly petroliferous sediments (including the emerged coastal plain), though the first barrel of oil is yet to be produced. Seismic and magnetic surveys indicate that the basement is deeper and more irregular than previously supposed and that a basement ridge may separate the shelf sediments into two major elongate basins parallel to the shelf edge, thus forming possible entrapping structures and possibly restricted depositional basins. Lower Paleozoic clastic rocks found in the subsurface of Georgia and Florida, and which may occur elsewhere in downfaulted basins, could be source beds and reservoir rocks for oil and gas over wide areas. Lower Cretaceous, Upper Jurassic( ?), and Triassic sedimentary rocks recognized in some wells must wedge out updip, and numerous unconformities probably occur. The marine sediments were presumably deposited in or close to shelf areas that possibly contain reefs and are partially bordered by known granite washes; thus both source and reservoir rocks are probably present. It can be expected that petroleum will eventually be discovered beneath the continental shelf and perhaps the emerged coastal plain, but it will not be discovered (economic factors aside) until geologists have projected paleogeographic settings into the sediments beneath the shelf from the data obtained through onshore and submarine geology, drilling, and geophysics.
","largerWorkType":{"id":24,"text":"Conference Paper"},"largerWorkTitle":"World Petroleum Congress Proceedings","conferenceTitle":"5th World Petroleum Congress","conferenceDate":"May 30- June 5, 1959","conferenceLocation":"New York, New York","language":"English","publisher":"Energy Institute","usgsCitation":"Johnston, J.E., Trumbull, J., and Eaton, G.P., 1959, The petroleum potential of the emerged and submerged Atlantic coastal plain of the United States, in World Petroleum Congress Proceedings, v. 5, New York, New York, May 30- June 5, 1959, p. 435-444.","productDescription":"10 p.","startPage":"435","endPage":"444","costCenters":[],"links":[{"id":377102,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"5","noUsgsAuthors":false,"publicationStatus":"PW","contributors":{"authors":[{"text":"Johnston, J. E.","contributorId":61487,"corporation":false,"usgs":true,"family":"Johnston","given":"J.","email":"","middleInitial":"E.","affiliations":[],"preferred":false,"id":794951,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Trumbull, James","contributorId":92233,"corporation":false,"usgs":true,"family":"Trumbull","given":"James","affiliations":[],"preferred":false,"id":794952,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Eaton, G. P.","contributorId":86334,"corporation":false,"usgs":true,"family":"Eaton","given":"G.","email":"","middleInitial":"P.","affiliations":[],"preferred":false,"id":794953,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}} ,{"id":70211663,"text":"70211663 - 1959 - The Elk Ridge-White Canyon channel system, San Juan County, Utah: Its effect on uranium distribution","interactions":[],"lastModifiedDate":"2020-08-06T19:53:38.206306","indexId":"70211663","displayToPublicDate":"1959-08-06T12:30:09","publicationYear":"1959","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1472,"text":"Economic Geology","active":true,"publicationSubtype":{"id":10}},"title":"The Elk Ridge-White Canyon channel system, San Juan County, Utah: Its effect on uranium distribution","docAbstract":"Reconnaissance in the White Canyon district, San Juan County, Utah, indicates that rocks of the Shinarump member of the Chinle formation of Triassic age were deposited in that district in two different channel systems; sediments deposited in channels of one system were derived from a source to the east and sediments of the other from a source to the south. The channel system containing sediments derived from the east, the Elk Ridge-White C anyon channel system, was apparently formed by a large braided stream that flowed westward from a source in granitic and metamorphic terrane of the ancestral Uncompahgre highland.
All known uranium deposits of any consequence in the White Canyon district are confined to the Shinarump member deposited in the Elk Ridge-White Canyon channel system. The nature of the channels and the lithologic characteristics of the rocks filling this system of channels combine to form a much more favorable environment for the localization of uranium deposits than do the channels formed and the rocks deposited by northward-flowing streams.
Recognition of channel systems in the White Canyon district suggests that channel systems may be recognized elsewhere in the Shinarump member, and that the Shinarump member on the Colorado Plateau may be composed of rocks deposited in many coalescing channel systems. In addition, study in the White Canyon district indicates that rocks deposited in some of these channel systems are more favorable hosts for uranium deposits than the rocks deposited in others. Recognition and delineation of these ancient channel systems may be-of help in making regional appraisals of ore potential and in the search for new mining districts.
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