{"pageNumber":"6764","pageRowStart":"169075","pageSize":"25","recordCount":184617,"records":[{"id":70010568,"text":"70010568 - 1962 - Hydrology","interactions":[],"lastModifiedDate":"2026-02-25T16:58:59.570241","indexId":"70010568","displayToPublicDate":"1962-03-02T00:00:00","publicationYear":"1962","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":3338,"text":"Science","active":true,"publicationSubtype":{"id":10}},"title":"Hydrology","docAbstract":"An understanding of water in relation to earth processes requires the collaboration of many disciplines.","language":"English","publisher":"American Association for the Advancement of Science","doi":"10.1126/science.135.3505.699","issn":"00368075","usgsCitation":"Hendricks, E.L., 1962, Hydrology: Science, v. 135, no. 3505, p. 699-705.","productDescription":"7 p.","startPage":"699","endPage":"705","costCenters":[],"links":[{"id":218970,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"135","issue":"3505","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"505a36b2e4b0c8380cd6091d","contributors":{"authors":[{"text":"Hendricks, E. L.","contributorId":50126,"corporation":false,"usgs":true,"family":"Hendricks","given":"E.","email":"","middleInitial":"L.","affiliations":[],"preferred":false,"id":359191,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":70220772,"text":"70220772 - 1962 - Correlation of the Carrizo Sand in Arkansas and adjacent states","interactions":[],"lastModifiedDate":"2021-05-25T17:25:38.428381","indexId":"70220772","displayToPublicDate":"1962-03-01T12:21:40","publicationYear":"1962","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1786,"text":"Geological Society of America Bulletin","active":true,"publicationSubtype":{"id":10}},"title":"Correlation of the Carrizo Sand in Arkansas and adjacent states","docAbstract":"

The Carrizo Sand (Eocene), the basal unit of the Claiborne Group, can be recognized in the subsurface throughout much of southeastern Arkansas and is correlated with the Carrizo Sand of Louisiana and the Meridian Sand Member of the Tallahatta Formation of Mississippi. The term Carrizo Sand is appropriate for use in Arkansas, as the stratigraphic terminology most workers apply to the Claiborne Group in Arkansas conforms with the terminology of Louisiana. A surface exposure of the Carrizo Sand in Arkansas is lithologically identical with described exposures of the Carrizo in northwestern Louisiana. 

","language":"English","publisher":"Geological Society of America","doi":"10.1130/0016-7606(1962)73[389:COTCSI]2.0.CO;2","usgsCitation":"Hosman, R., 1962, Correlation of the Carrizo Sand in Arkansas and adjacent states: Geological Society of America Bulletin, v. 73, no. 3, p. 389-394, https://doi.org/10.1130/0016-7606(1962)73[389:COTCSI]2.0.CO;2.","productDescription":"6 p.","startPage":"389","endPage":"394","costCenters":[],"links":[{"id":385946,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United States","state":"Arkansas, Louisiana, Mississippi, Tennessee","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"type\": \"Polygon\",\n \"coordinates\": [\n [\n [\n -94.52636718749999,\n 29.19053283229458\n ],\n [\n -88.24218749999999,\n 29.19053283229458\n ],\n [\n -88.24218749999999,\n 36.63316209558658\n ],\n [\n -94.52636718749999,\n 36.63316209558658\n ],\n [\n -94.52636718749999,\n 29.19053283229458\n ]\n ]\n ]\n }\n }\n ]\n}","volume":"73","issue":"3","noUsgsAuthors":false,"publicationStatus":"PW","contributors":{"authors":[{"text":"Hosman, R. L.","contributorId":42978,"corporation":false,"usgs":true,"family":"Hosman","given":"R.","middleInitial":"L.","affiliations":[],"preferred":false,"id":816458,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":70010811,"text":"70010811 - 1962 - Preliminary geologic report on the 1961 U.S. expedition to Bellingshausen Sea, Antarctica","interactions":[],"lastModifiedDate":"2026-02-25T17:10:03.874934","indexId":"70010811","displayToPublicDate":"1962-02-23T00:00:00","publicationYear":"1962","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":3338,"text":"Science","active":true,"publicationSubtype":{"id":10}},"title":"Preliminary geologic report on the 1961 U.S. expedition to Bellingshausen Sea, Antarctica","docAbstract":"Five areas of outcrop were examined along 120 miles of the coast of the Bellingshausen Sea east of the Thurston Peninsula. Hornblende quartz diorite is the principal rock in the area and occurs in a body of batholithic dimensions. The quartz diorite contains inclusions of older granulitic rock and is cut by mafic dikes. An island in Paradise Harbor on the Palmer Peninsula was also examined briefly.","language":"English","publisher":"American Association for the Advancement of Science","doi":"10.1126/science.135.3504.671","issn":"00368075","usgsCitation":"Drake, A.A., 1962, Preliminary geologic report on the 1961 U.S. expedition to Bellingshausen Sea, Antarctica: Science, v. 135, no. 3504, p. 671-672.","productDescription":"2 p.","startPage":"671","endPage":"672","costCenters":[],"links":[{"id":218738,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"otherGeospatial":"Bellingshausen Sea, Antarctica","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"coordinates\": [\n [\n [\n -69.39594402462191,\n -66.071280772103\n ],\n [\n -90.1472833271104,\n -66.071280772103\n ],\n [\n -90.1472833271104,\n -73.22555094647112\n ],\n [\n -69.39594402462191,\n -73.22555094647112\n ],\n [\n -69.39594402462191,\n -66.071280772103\n ]\n ]\n ],\n \"type\": \"Polygon\"\n }\n }\n ]\n}","volume":"135","issue":"3504","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"505a8775e4b0c8380cd7d388","contributors":{"authors":[{"text":"Drake, Avery A. Jr.","contributorId":81090,"corporation":false,"usgs":true,"family":"Drake","given":"Avery","suffix":"Jr.","middleInitial":"A.","affiliations":[],"preferred":false,"id":359702,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":70238052,"text":"70238052 - 1962 - Browsing habits of white-tailed deer in the western Gulf Region","interactions":[],"lastModifiedDate":"2022-11-07T19:57:52.792816","indexId":"70238052","displayToPublicDate":"1962-02-01T13:41:54","publicationYear":"1962","noYear":false,"publicationType":{"id":24,"text":"Conference Paper"},"publicationSubtype":{"id":19,"text":"Conference Paper"},"title":"Browsing habits of white-tailed deer in the western Gulf Region","docAbstract":"

No abstract available.

","largerWorkType":{"id":4,"text":"Book"},"largerWorkTitle":"Proceedings of 1st National White-Tailed Deer Disease Symposium","largerWorkSubtype":{"id":12,"text":"Conference publication"},"conferenceTitle":"1st National White-Tailed Deer Disease Symposium","conferenceDate":"February 13-15, 1962","conferenceLocation":"Athens, Georgia, United States","language":"English","publisher":"Southeastern Section of the Wildlife Society","usgsCitation":"Goodrum, P.D., and Reid, V.H., 1962, Browsing habits of white-tailed deer in the western Gulf Region, in Proceedings of 1st National White-Tailed Deer Disease Symposium, Athens, Georgia, United States, February 13-15, 1962, p. 9-14.","productDescription":"6 p.","startPage":"9","endPage":"14","costCenters":[],"links":[{"id":409205,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United States","state":"Alabama, Louisiana, 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No abstract available.

","language":"English","publisher":"American Water Resources Association","publisherLocation":"Herndon, VA","usgsCitation":"Scott, C., and Skinner, J.V., 1962, Valve position indicator for P-46 sampler: Water Resources Bulletin, v. February, p. 9-10.","productDescription":"2 p.","startPage":"9","endPage":"10","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[{"id":392,"text":"Minnesota Water Science Center","active":true,"usgs":true}],"links":[{"id":321725,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"February","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"57481e3ee4b07e28b664dc1d","contributors":{"authors":[{"text":"Scott, C.H.","contributorId":101634,"corporation":false,"usgs":true,"family":"Scott","given":"C.H.","email":"","affiliations":[],"preferred":false,"id":630418,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Skinner, J. V.","contributorId":32504,"corporation":false,"usgs":true,"family":"Skinner","given":"J.","email":"","middleInitial":"V.","affiliations":[],"preferred":false,"id":630419,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":70176600,"text":"70176600 - 1962 - Phenol contamination of an artesian aquifer at Alma, Michigan, 1962","interactions":[],"lastModifiedDate":"2016-09-22T14:14:24","indexId":"70176600","displayToPublicDate":"1962-01-30T00:00:00","publicationYear":"1962","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":5209,"text":"Proceedings of the Society for Water Treatment and Examination","active":true,"publicationSubtype":{"id":10}},"title":"Phenol contamination of an artesian aquifer at Alma, Michigan, 1962","docAbstract":"

No abstract available.

","language":"English","publisher":"Society for Water Treatment and Examination","publisherLocation":"Sutton, England","usgsCitation":"Deutsch, M., 1962, Phenol contamination of an artesian aquifer at Alma, Michigan, 1962: Proceedings of the Society for Water Treatment and Examination, v. 11, p. 94-100.","startPage":"94","endPage":"100","numberOfPages":"7","costCenters":[{"id":382,"text":"Michigan Water Science Center","active":true,"usgs":true}],"links":[{"id":328867,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United States","state":"Michigan","city":"Alma","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"type\": \"Polygon\",\n \"coordinates\": [\n [\n [\n -84.72656249999999,\n 43.33791397478761\n ],\n [\n -84.72656249999999,\n 43.415522593099915\n ],\n [\n -84.60090637207031,\n 43.415522593099915\n ],\n [\n -84.60090637207031,\n 43.33791397478761\n ],\n [\n -84.72656249999999,\n 43.33791397478761\n ]\n ]\n ]\n }\n }\n ]\n}","volume":"11","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"57ffcff4e4b0824b2d17619c","contributors":{"authors":[{"text":"Deutsch, Morris","contributorId":69119,"corporation":false,"usgs":true,"family":"Deutsch","given":"Morris","email":"","affiliations":[],"preferred":false,"id":649338,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":70207936,"text":"70207936 - 1962 - Lava tree molds of the September 1961 eruption, Kilauea Volcano, Hawaii","interactions":[],"lastModifiedDate":"2020-01-20T14:16:14","indexId":"70207936","displayToPublicDate":"1962-01-20T14:04:33","publicationYear":"1962","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":"Lava tree molds of the September 1961 eruption, Kilauea Volcano, Hawaii","docAbstract":"

Well-developed lava tree molds were formed during the September 1961 eruption along the east rift zone of Kilauea Volcano. The upright molds were produced where fluid lava, flowing through dense tropical forest, became chilled against the larger trees and tree ferns and later drained away. Where the lava ponded temporarily in a structural valley, tree molds more than 14 feet high mark the high level attained by the flow.

","language":"English","publisher":"GSA","doi":"10.1130/0016-7606(1962)73[1153:LTMOTS]2.0.CO;2","usgsCitation":"Moore, J.G., and Richter, D., 1962, Lava tree molds of the September 1961 eruption, Kilauea Volcano, Hawaii: GSA Bulletin, v. 73, no. 9, p. 1153-1158, https://doi.org/10.1130/0016-7606(1962)73[1153:LTMOTS]2.0.CO;2.","productDescription":"6 p.","startPage":"1153","endPage":"1158","costCenters":[{"id":617,"text":"Volcano Science Center","active":true,"usgs":true}],"links":[{"id":371388,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United States","state":"Hawaii","otherGeospatial":"East rift zone","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"type\": \"Polygon\",\n \"coordinates\": [\n [\n [\n -155.2532958984375,\n 19.197053439464852\n ],\n [\n -154.8028564453125,\n 19.197053439464852\n ],\n [\n -154.8028564453125,\n 19.51319789966427\n ],\n [\n -155.2532958984375,\n 19.51319789966427\n ],\n [\n -155.2532958984375,\n 19.197053439464852\n ]\n ]\n ]\n }\n }\n ]\n}","volume":"73","issue":"9","noUsgsAuthors":false,"publicationStatus":"PW","contributors":{"authors":[{"text":"Moore, James G. 0000-0002-7543-2401 jmoore@usgs.gov","orcid":"https://orcid.org/0000-0002-7543-2401","contributorId":2892,"corporation":false,"usgs":true,"family":"Moore","given":"James","email":"jmoore@usgs.gov","middleInitial":"G.","affiliations":[{"id":114,"text":"Alaska Science Center","active":true,"usgs":true},{"id":617,"text":"Volcano Science Center","active":true,"usgs":true}],"preferred":true,"id":779824,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Richter, D.H.","contributorId":43325,"corporation":false,"usgs":true,"family":"Richter","given":"D.H.","email":"","affiliations":[{"id":595,"text":"U.S. Geological Survey","active":false,"usgs":true}],"preferred":false,"id":779825,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":70010743,"text":"70010743 - 1962 - Metallic spherules in tektites from Isabela, Philippine Islands","interactions":[],"lastModifiedDate":"2026-02-25T17:20:30.675416","indexId":"70010743","displayToPublicDate":"1962-01-12T00:00:00","publicationYear":"1962","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":3338,"text":"Science","active":true,"publicationSubtype":{"id":10}},"title":"Metallic spherules in tektites from Isabela, Philippine Islands","docAbstract":"Iron-nickel spherules, as much as 0.5 mm in diameter, have been found completely embedded in some philippinites. The spherules consist mainly of kamacite with unidentified pink inclusions. The meteoritic origin of these spherules seems reasonable, suggesting that the tektites containing them were formed by asteroidal or meteoritic impact.","language":"English","publisher":"American Association for the Advancement of Science","doi":"10.1126/science.135.3498.97","issn":"00368075","usgsCitation":"Chao, E.C., Adler, I., Dwornik, E., and Littler, J., 1962, Metallic spherules in tektites from Isabela, Philippine Islands: Science, v. 135, no. 3498, p. 97-98.","productDescription":"2 p.","startPage":"97","endPage":"98","costCenters":[],"links":[{"id":219636,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"Philippines","otherGeospatial":"Isabela","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"coordinates\": [\n [\n [\n 121.8321580263597,\n 17.61561971503707\n ],\n [\n 121.8321580263597,\n 16.98428859480572\n ],\n [\n 122.52219426023623,\n 16.98428859480572\n ],\n [\n 122.52219426023623,\n 17.61561971503707\n ],\n [\n 121.8321580263597,\n 17.61561971503707\n ]\n ]\n ],\n \"type\": \"Polygon\"\n }\n }\n ]\n}","volume":"135","issue":"3498","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"505a54dbe4b0c8380cd6d071","contributors":{"authors":[{"text":"Chao, E. C. T.","contributorId":96713,"corporation":false,"usgs":true,"family":"Chao","given":"E.","email":"","middleInitial":"C. 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Off.","publisherLocation":"Washington, D.C.","usgsCitation":"Hansen, H., 1962, Waterfowl status report, 1962 (Revises and updates Special Scientific Report-Wildlife 61 (1961)): Special Scientific Report - Wildlife 68, iv, 127 p.","productDescription":"iv, 127 p.","numberOfPages":"131","costCenters":[],"links":[{"id":290180,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"edition":"Revises and updates Special Scientific Report-Wildlife 61 (1961)","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"53c64deae4b0001bd51477d6","contributors":{"authors":[{"text":"Hansen, Henry A.","contributorId":15533,"corporation":false,"usgs":true,"family":"Hansen","given":"Henry A.","affiliations":[],"preferred":false,"id":218252,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":33208,"text":"b1082 - 1962 - Contributions to economic geology, 1958","interactions":[{"subject":{"id":47375,"text":"b1082A - 1958 - Zirconium and hafnium in the southeastern Atlantic States","indexId":"b1082A","publicationYear":"1958","noYear":false,"chapter":"A","title":"Zirconium and hafnium in the southeastern Atlantic States"},"predicate":"IS_PART_OF","object":{"id":33208,"text":"b1082 - 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1962 - Instructions for US P-61-A1 suspended-sediment sampler","interactions":[],"lastModifiedDate":"2018-03-05T12:28:54","indexId":"70170554","displayToPublicDate":"1962-01-01T13:45:00","publicationYear":"1962","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":1,"text":"Federal Government Series"},"seriesTitle":{"id":66,"text":"Report","active":false,"publicationSubtype":{"id":1}},"title":"Instructions for US P-61-A1 suspended-sediment sampler","docAbstract":"

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","language":"English","publisher":"Federal Interagency Sedimentation Project","publisherLocation":"Vickburg, MS","usgsCitation":"Colby, V., and Witzgman, F., 1962, Instructions for US P-61-A1 suspended-sediment sampler: Report, 9 p.","productDescription":"9 p.","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[{"id":392,"text":"Minnesota Water Science Center","active":true,"usgs":true}],"links":[{"id":320513,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"571f3fbee4b071321fe56a42","contributors":{"authors":[{"text":"Colby, V.C.","contributorId":168886,"corporation":false,"usgs":false,"family":"Colby","given":"V.C.","email":"","affiliations":[],"preferred":false,"id":627601,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Witzgman, F.W.","contributorId":168892,"corporation":false,"usgs":false,"family":"Witzgman","given":"F.W.","email":"","affiliations":[],"preferred":false,"id":627602,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":37736,"text":"37736 - 1962 - Fur catch in the United States, 1961","interactions":[],"lastModifiedDate":"2014-07-22T13:26:02","indexId":"37736","displayToPublicDate":"1962-01-01T13:25:11","publicationYear":"1962","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":"444","title":"Fur catch in the United States, 1961","docAbstract":"No abstract available.","language":"English","publisher":"U.S. Department of the Interior","publisherLocation":"Washington, D.C.","collaboration":"Complied in Bird and Mammal Laboratories, Branch of Wildlife Research.","usgsCitation":"U.S. Branch of Wildlife Research, 1962, Fur catch in the United States, 1961 (Updates Wildlife Leaflet BS-140 (1939).): Wildlife Leaflet 444, 3 p.","productDescription":"3 p.","numberOfPages":"3","temporalStart":"1961-01-01","temporalEnd":"1961-12-31","costCenters":[],"links":[{"id":290718,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"edition":"Updates Wildlife Leaflet BS-140 (1939).","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"57ffd085e4b0824b2d1763f6","contributors":{"authors":[{"text":"U.S. Branch of Wildlife Research","contributorId":127903,"corporation":true,"usgs":false,"organization":"U.S. Branch of Wildlife Research","id":529689,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":70207379,"text":"70207379 - 1962 - Metallogenetic provinces of Chile, S. A","interactions":[],"lastModifiedDate":"2019-12-19T08:03:37","indexId":"70207379","displayToPublicDate":"1962-01-01T13:13:11","publicationYear":"1962","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":"Metallogenetic provinces of Chile, S. A","docAbstract":"

The metalliferous deposits of Chile tend to be restricted to well denned metallogenetic provinces, each characterized by a dominant mineral or mineral assemblage. The most important ore deposits are those of copper, iron, silver, gold, and manganese. The primary minerals are few in number and most are simple sulfides and oxides; more complex sulfosalts are scarce. Secondary minerals in great variety are important constituents of the ores. Many of the ore deposits are situated along well defined structural lines, several hundred kilometers long, that parallel the structural grain of the Andes.The deposits, with few exceptions, are found in sedimentary or volcanic rocks that range in age from Jurassic to Late Cretaceous or in intrusive rocks of Late Jurassic to Late Cretaceous age. Most deposits are genetically related to intrusive bodies, which have an average composition within the range of granite-diorite.The metalliferous deposits can be classed as hydrothermal, sedimentary, contact-metasomatic and magmatic. Copper deposits are typically hydro-thermal, manganese deposits are sedimentary, and most of the iron ore deposits are contact-metasomatic. A unique group of iron ore deposits apparently formed by near-surface intrusion and surface flows of a magma consisting of iron oxides. Hydrothermal deposits, the most abundant and most important economically, were formed under conditions ranging from low to high temperature and pressure. © 1962 Society of Economic Geologists, Inc.

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management","interactions":[],"lastModifiedDate":"2019-03-18T10:25:39","indexId":"70202536","displayToPublicDate":"1962-01-01T11:25:13","publicationYear":"1962","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":6,"text":"USGS Unnumbered Series"},"title":"Report on the Geological Survey Library: its history, technical work, resources, management","docAbstract":"

One of the limitations under which any library operates is the image it creates as a storehouse, This aspect can obscure the purposes and activities which make one library differ from another. In an institutional library, like the Survey's, the library purposes are related to the changing life of the organization, and to the world of ideas and facts it mirrors.

What goes on inside the Survey Library is understandable only in part from the standard practices it shares with other libraries as we view them today. For the other part, deeply rooted in the history and traditions of the organization, the understanding arises from the history that has made it what it is. This report will first provide, therefore, an historical sketch of the Survey Library with particular reference to its development over three quarters of a century, to the philosophy of librarianship that has animated it, and to the future growth to which it is committed.

By design and history, the Survey Library is a special library, maintained primarily for the benefit of Survey workers. This report will review the main routines and characteristics of the \"special\" aspects of the library operations.

Personnel and funds of the library have increased many..fold during the past decade, roughly parallel to the growth of the Geological Survey. This expansion is in sharp contrast to a long span of lean years when the library piled up a backlog of tasks partly finished or not done at all because of limited funds and staff. This report will describe the resources in personnel, funds, equipment and space available in the past and now to the library, their sufficiency, and the outlook for future growth. It will be demonstrated that the library's need for resources will continue to expand for reasons that are partly independent of any future growth of Survey employment.

Finally, against the background of history, functions, resources and problems described the report will attempt to express some measure of effectiveness for the management of the library. A measure of effectiveness is simply an expression of the degree to which a system fulfills its objectives.

Throughout this study, the aim has been to develop a body of systematic information about the various activities of the library for uses and judgements that go beyond immediate concerns. No such examination of this important area of the Survey's activities has been undertaken in recent decades, and none whatever in a context of changes such as those of the past decade. Yet the period of most profound change seems to lie ahead, seeded by explorations in the field of information storage and retrieval and forced by the volume of information in the various branches of science.

Acknowledgment of the cooperation given by the Chief Librarian and members of the library staff during the preparation of this report is gratefully made. It is not an easy task for members of an organization to open up their operating field to the questions and judgments of a staff member outside that organization. The willingness to do so, in the face of queries which have often suggested the need of change, is itself favorable to change when it becomes due and when it is sought by management.

","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/70202536","usgsCitation":"Irving, W., 1962, Report on the Geological Survey Library: its history, technical work, resources, management, iv, 140 p., https://doi.org/10.3133/70202536.","productDescription":"iv, 140 p.","costCenters":[],"links":[{"id":362125,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/unnumbered/70202536/report-thumb.jpg"},{"id":362126,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/unnumbered/70202536/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","contributors":{"authors":[{"text":"Irving, W.C.","contributorId":214246,"corporation":false,"usgs":true,"family":"Irving","given":"W.C.","email":"","affiliations":[],"preferred":false,"id":759440,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":70095376,"text":"70095376 - 1962 - Generalized structure contour maps of the New Jersey coastal plain","interactions":[],"lastModifiedDate":"2014-03-25T10:35:02","indexId":"70095376","displayToPublicDate":"1962-01-01T10:06:00","publicationYear":"1962","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":2,"text":"State or Local Government Series"},"seriesTitle":{"id":112,"text":"Geologic report (New Jersey)","active":false,"publicationSubtype":{"id":2}},"seriesNumber":"4","title":"Generalized structure contour maps of the New Jersey coastal plain","docAbstract":"Twelve generalized structural contour maps were prepared from a study of 169 well\nlogs or sample logs of drill cuttings from the Coastal Plain of New Jersey, Delaware, and\nthe E astern Shore of Maryland. The configuration of the tops of the nonmarine Cretaceous\ndeposits (Patuxent , Patapsco, Raritan, and Magothy formations) and the Piney Point Formation\n(Eocene) show the known subsurface extent of these formations in both New Jersey\nand Delaware. The structural contour maps show the tops of the Merchantville Formation\nand Woodbury Clay, the Englishtown Formation, the Marshalltown Formation, the Wenonah\nFormation and Mount Laurel Sand, the Navesink Forma ti on, and the Red Bank\nSand which are a ll of Late Cretaceous age. The maps of the Hornerstown Sand, the Vincentown\nFormation, and the Manasquan Formation and Shark River Marl of early Tertiary\nage show the subsurface extent of these formations only in New Jersey. Also included is an\noutline map showing the locations of wells and seismic station s and a structural contour map\nshowing the configuration of the bedrock surface of the report area.\nStructural contours on top of the Magothy Formation, or on the top of the Raritan Formation\nwhere the Magothy formation is absent, show the configuration of the nonmarine\ndeposits of Cretaceous age. Isopachs of the nonmarine deposits are derived by interpolation\nbetween contours on top of the bedrock and the top of either the Magothy Formation or the\nRaritan Formation where the Magothy is absent.\n\nThe Merchantville Formation and Woodbury Clay are difficult to separate in the subsurface,\nand therefore the contour a re drawn on top of the Woodbury Clay. In New Jersey,\nthe thickness of the combined Merchantville Form a ti on and Woodbury Clay ranges from\nab out 100 to 140 feet near the outcrop, but exceeds 250 feet in the subsurface along the\ncoast in Ocean County.\n\nThe top of the Englishtown Formation is easy to recognize because it generally consists\nof a micaceous white and yellow sand, although locally it is a silty clay . The formation\nthins toward the southwest from about 160 feet in central Ocean County to less than 20 feet\nin Salem County . It has not been recognized in Delaware.\n\nThe Marshalltown Formation varies from black clay to a glauconitic sand. It usually\nranges in thickness from 20 to 60 feet . It is very thin or absent in Delaware.\n\nThe Wenonah Formation and Mount Laurel and arc difficult to separate in New Jersey,\nand therefore are shown as a unit. The combined thickness range from 60 to 100) feet. In\nDelaware the two formations are easily separated.\n\nThe Navesink Formation is generally highly glauconitc and it is difficult to determine\nthe upper limit where overlain by the Hornerstown Sand which is also glauconitic. The contour\nmap on the top of the Navesink is based upon relatively little control.\n\nThe Red Bank Sand reaches a thickness of about 160 feet in Monmouth County. It thins\nsouthwestward and is absent in outcrop in the southern part of the Coastal Plain of New\nJersey. A probable equivalent of the Reel Bank has be recognized in Delaware. The Tinton\nSand Member is the topmost unit of the Red Bank and in Monmouth County.\n\nThe Hornerstown Sand is most glauconitic and is about 30 feet thick in outcrop. This\nis overlain by the Vincentown Formation which consists of two facies (1) calcareous sand\nfacies and (2) quartz sand facies. These a re overlain by the Manasquan Formation and\nShark River Marl which are here treated as a unit . In outcrop the combined thickness of the\nManasquan Formation and Shark River Marl is about 40 feet, but in the subsurface they\nthicken to about 200 feet. The Piney Point Formation of Jackson age occur in the subsurface\nin Cape May and Atlantic Counties, N.J. and in southern Delaware but is not\nexposed in these States.\nBrief notes are given on formation of later Tertiary and Pleistocene age , but no contour\nmaps were constructed.","language":"English","publisher":"New Jersey Deptartment of Conservation and Economic Development","publisherLocation":"Trenton, NJ","usgsCitation":"Richards, H.G., Olmsted, F.H., and Ruhle, J.L., 1962, Generalized structure contour maps of the New Jersey coastal plain: Geologic report (New Jersey) 4, iv, 38 p.","productDescription":"iv, 38 p.","additionalOnlineFiles":"N","costCenters":[],"links":[{"id":283183,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/70095376.jpg"},{"id":284834,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/unnumbered/70095376/report.pdf"}],"country":"United States","state":"Delaware;New Jersey","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -75.9924,38.4977 ], [ -75.9924,40.1894 ], [ -73.9160,40.1894 ], [ -73.9160,38.4977 ], [ -75.9924,38.4977 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"5355943ae4b0120853e8bf94","contributors":{"authors":[{"text":"Richards, Hoarce G.","contributorId":60124,"corporation":false,"usgs":true,"family":"Richards","given":"Hoarce","email":"","middleInitial":"G.","affiliations":[],"preferred":false,"id":491182,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Olmsted, F. H.","contributorId":24765,"corporation":false,"usgs":true,"family":"Olmsted","given":"F.","email":"","middleInitial":"H.","affiliations":[],"preferred":false,"id":491181,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Ruhle, James L.","contributorId":22676,"corporation":false,"usgs":true,"family":"Ruhle","given":"James","email":"","middleInitial":"L.","affiliations":[],"preferred":false,"id":491180,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}} ,{"id":71774,"text":"tei821 - 1962 - Physical properties of evaporite minerals","interactions":[],"lastModifiedDate":"2014-06-11T08:48:06","indexId":"tei821","displayToPublicDate":"1962-01-01T09:37:00","publicationYear":"1962","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":337,"text":"Trace Elements Investigations","code":"TEI","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"821","title":"Physical properties of evaporite minerals","docAbstract":"

The data in the following tables were abstracted from measurements of physical properties of evaporite minerals or of equivalent synthetic compounds. The compounds considered are the halide and sulfate salts which supposedly precipitated from evaporating ocean water and which form very extensive and thick \"rock salt\" beds. These beds are composed almost entirely of NaCl. In places where the beds are deeply buried and where fractures occur in the overlying rocks, the salt is plastically extruded upward as in a pipe to form the \"salt domes\".

\n
\n

\nMost of the tables are for NaCl, both the natural (halite) and the synthetic salt, polycrystalline and single crystals. These measurements have been collected for use 1) in studies on storage of radioactive wastes in salt domes or beds, 2) in calculations concerned with nuclear tests in salt domes and beds, and 3) in studies of phenomena in salt of geologic interest.

\n
\n

\nRather than an exhaustive compilation of physical property measurements, there tables represent a summary of data from accessible sources. As limitations of time have presented making a more systematic and comprehensive selection, the data given may seem arbitrarily chosen. Some of the data listed are old, and newer, more accurate data are undoubtedly available.

\n
\n

Halite (an synthetic NaCl) has been very thoroughly studied because of its relatively simple and highly symmetrical crystal structure, its easy availability naturally or synthetically, both in single crystals and polycrystalline, its useful and scientifically interesting properties, and its role as a compound of almost purely ionic bonding. The measurements of NaCl in the tables, however, represent only a small part of the total number of observations; discrimination was necessary to keep the size of the tabulations manageable. The physical properties of the evaporite minerals other than halite and sylvite have received only desultory attention of experiementalists, and appear in only a few tables.

\n
\n

The effects of temperature, hydrostatic pressure, stress difference, and other mechanical, eletrical, and optical conditions on the physical properties have probably been observed more completely on NaCl than on any other solid substance, which makes it a unique and important substance. Several new and important phenomena have been observed first on it. The mechanical properties of NaCl, for example, depend very strongly on the condition and the composition of the gas or liquid in contact with the sample surface; the data are sparse as yet and are not reported here.

","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/tei821","collaboration":"Prepared on behalf of the U.S. Atomic Energy Commission","usgsCitation":"Robertson, E.C., 1962, Physical properties of evaporite minerals: U.S. Geological Survey Trace Elements Investigations 821, 90 p., https://doi.org/10.3133/tei821.","productDescription":"90 p.","numberOfPages":"90","costCenters":[],"links":[{"id":288266,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":288265,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/tei/0821/report.pdf"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"5385b3fbe4b09e18fc023a7b","contributors":{"authors":[{"text":"Robertson, Eugene C.","contributorId":71139,"corporation":false,"usgs":true,"family":"Robertson","given":"Eugene","email":"","middleInitial":"C.","affiliations":[],"preferred":false,"id":284738,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":70220665,"text":"70220665 - 1962 - Diffusion features of uranium-vanadium deposits in Montezuma Canyon, Utah","interactions":[],"lastModifiedDate":"2021-05-24T13:58:30.40077","indexId":"70220665","displayToPublicDate":"1962-01-01T08:53:59","publicationYear":"1962","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":"Diffusion features of uranium-vanadium deposits in Montezuma Canyon, Utah","docAbstract":"

Uranium-vanadium deposits in the Salt Wash Member of the Morrison Formation in Montezuma Canyon, San Juan County, Utah, exhibit zoning that is interpreted as a result of metal transport by diffusion. The concentric zones consist of a brown nonmineralized core, an olive-gray mineralized shell, and a gray nonmineralized outer zone. The brown zone is iron-stained, porous sandstone commonly containing abundant carbonaceous material. The curved mineralized layer completely encloses the brown zone, and is composed of oxidized uranium-vanadium minerals that impregnate sandstone. The gray zone is light-gray sandstone tightly cemented with calcite and commonly freckled with limonitic specks.Formation of the deposits most likely took place during Late Cretaceous or early Tertiary time when the ore-bearing sandstones were deeply buried and saturated with connate waters. The concentration of organic material in the brown zone suggests that this zone was once saturated with a reducing solution containing soluble organic compounds like alcohols and aldehydes derived from the organic material. The gray zone, on the other hand, was probably saturated with an oxidizing solution containing uranium and vanadium. Where these two solutions were in contact, oxidation-reduction reactions took place that caused the precipitation of low-valent uranium and vanadium minerals.The ellipsoidal shape of the ore layer and the lack of any exit or entrance for flowing solutions indicates that the dissolved metals moved through the gray zone by diffusion and were precipitated at the periphery of the reducing zone. Recent weathering and oxidation have altered the primary low-valent minerals to high-valent forms without noticeable leaching of the ore metals. 

","language":"English","publisher":"Society of Economic Geologists","doi":"10.2113/gsecongeo.57.2.226","usgsCitation":"Huff, L., and Lesure, F., 1962, Diffusion features of uranium-vanadium deposits in Montezuma Canyon, Utah: Economic Geology, v. 57, no. 2, p. 226-237, https://doi.org/10.2113/gsecongeo.57.2.226.","productDescription":"12 p.","startPage":"226","endPage":"237","costCenters":[],"links":[{"id":385897,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United States","state":"Utah","otherGeospatial":"Montezuma Canyon","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"type\": \"Polygon\",\n \"coordinates\": [\n [\n [\n -109.654541015625,\n 37.02886944696474\n ],\n [\n -109.061279296875,\n 37.02886944696474\n ],\n [\n -109.061279296875,\n 38.53957267203905\n ],\n [\n -109.654541015625,\n 38.53957267203905\n ],\n [\n -109.654541015625,\n 37.02886944696474\n ]\n ]\n ]\n }\n }\n ]\n}","volume":"57","issue":"2","noUsgsAuthors":false,"publicationDate":"1962-03-01","publicationStatus":"PW","contributors":{"authors":[{"text":"Huff, L.C.","contributorId":32919,"corporation":false,"usgs":true,"family":"Huff","given":"L.C.","email":"","affiliations":[],"preferred":false,"id":816355,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Lesure, F. G.","contributorId":7694,"corporation":false,"usgs":true,"family":"Lesure","given":"F. G.","affiliations":[{"id":595,"text":"U.S. Geological Survey","active":false,"usgs":true}],"preferred":false,"id":816356,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":70227016,"text":"70227016 - 1962 - Diatremes and uranium deposits in the Hopi Buttes, Arizona","interactions":[],"lastModifiedDate":"2021-12-27T15:01:01.710863","indexId":"70227016","displayToPublicDate":"1962-01-01T08:45:58","publicationYear":"1962","noYear":false,"publicationType":{"id":5,"text":"Book chapter"},"publicationSubtype":{"id":24,"text":"Book Chapter"},"title":"Diatremes and uranium deposits in the Hopi Buttes, Arizona","docAbstract":"

The Hopi Buttes diatremes erupted in a shallow lake that was filled in as volcanic activity progressed in Pliocene time. At the end of the period of volcanism the landscape included low lava domes capping some of the diatremes, a few flows, and numerous craters of the maar type, surrounded by rims of volcanic debris with gentle exterior slopes that merged with the surrounding plain. Erosion, probably chiefly during early and middle Pleistocene, has exposed the diatremes in varying stages of denudation.

","largerWorkType":{"id":4,"text":"Book"},"largerWorkTitle":"Petrologic studies: A volume in honor of A. F. Buddington","largerWorkSubtype":{"id":15,"text":"Monograph"},"language":"English","publisher":"Geological Society of America","doi":"10.1130/Petrologic.1962.327","usgsCitation":"Shoemaker, E.M., Roach, C.H., and Byers, F., 1962, Diatremes and uranium deposits in the Hopi Buttes, Arizona, chap. of Petrologic studies: A volume in honor of A. F. Buddington, p. 327-355, https://doi.org/10.1130/Petrologic.1962.327.","productDescription":"29 p.","startPage":"327","endPage":"355","costCenters":[],"links":[{"id":393421,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United States","state":"Arizona","otherGeospatial":"Hopi Buttes","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"type\": \"Polygon\",\n \"coordinates\": [\n [\n [\n -110.621337890625,\n 35.40808023595146\n ],\n [\n -110.62545776367186,\n 35.226550551891116\n ],\n [\n -110.36178588867188,\n 35.12664799144554\n ],\n [\n -110.25741577148438,\n 35.107551518679074\n ],\n [\n -110.09811401367188,\n 35.14349410278418\n ],\n [\n -109.8577880859375,\n 35.34425514918409\n ],\n [\n -109.86740112304688,\n 35.571331599581654\n ],\n [\n -110.06240844726562,\n 35.83896829930447\n ],\n [\n -110.32196044921874,\n 35.83451505415075\n ],\n [\n -110.621337890625,\n 35.40808023595146\n ]\n ]\n ]\n }\n }\n ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","contributors":{"editors":[{"text":"Engel, A.E.J.","contributorId":241621,"corporation":false,"usgs":false,"family":"Engel","given":"A.E.J.","affiliations":[],"preferred":false,"id":829225,"contributorType":{"id":2,"text":"Editors"},"rank":1},{"text":"James, Harold L.","contributorId":88204,"corporation":false,"usgs":true,"family":"James","given":"Harold L.","affiliations":[],"preferred":false,"id":829226,"contributorType":{"id":2,"text":"Editors"},"rank":2},{"text":"Leonard, B. F.","contributorId":117454,"corporation":false,"usgs":true,"family":"Leonard","given":"B.","email":"","middleInitial":"F.","affiliations":[],"preferred":false,"id":829227,"contributorType":{"id":2,"text":"Editors"},"rank":3}],"authors":[{"text":"Shoemaker, Eugene Merle","contributorId":20342,"corporation":false,"usgs":true,"family":"Shoemaker","given":"Eugene","email":"","middleInitial":"Merle","affiliations":[],"preferred":false,"id":829222,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Roach, C. H.","contributorId":12117,"corporation":false,"usgs":true,"family":"Roach","given":"C.","email":"","middleInitial":"H.","affiliations":[],"preferred":false,"id":829223,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Byers, F. M. Jr.","contributorId":270390,"corporation":false,"usgs":false,"family":"Byers","given":"F. M.","suffix":"Jr.","affiliations":[],"preferred":false,"id":829224,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}} ,{"id":70220651,"text":"70220651 - 1962 - Lower temperature terminations of the three-phase region plagioclase-alkali feldspar-liquid","interactions":[],"lastModifiedDate":"2021-05-24T11:47:18.288311","indexId":"70220651","displayToPublicDate":"1962-01-01T06:43:05","publicationYear":"1962","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":2420,"text":"Journal of Petrology","active":true,"publicationSubtype":{"id":10}},"title":"Lower temperature terminations of the three-phase region plagioclase-alkali feldspar-liquid","docAbstract":"

Geological and experimental evidence indicate that the three-phase field, plagioclase-alkalifeldspar-liquid, may terminate in several different ways. The possible terminations have been developed from Schreinemakers' rules governing the disappearance of three-phase fields. In igncous rocks, these different terminations may arise from variations in the relative amounts of additional components in magmas, or from changes of total pressure, or from structural changes that effect the extent of solid solution in feldspar.The three-phase region originates from the intersection of the solidus and the feldspar solvus. The available evidence regarding this intersection is reviewed, as is the evidence for the existence and form of the boundary curve on the feldspar liquidus. The data are used to project a series of isobaric polythermal and isobaric isothermal diagrams for each possible termination. Subsequent discussions relate the theoretical arguments to the natural evidence, suggest the more probable geological environments of some of the terminations, and indicate characteristic features of each termination.It may be possible to identify the type of termination involved in the crystallization of some rocks. The necessary data are the amounts and compositions of both kinds of coexisting feldspars and of the feldspar components of the coexisting liquid at one or more stages of the crystallization process. Volcanic rocks are most suitable for such studies.The terminations explain many of the compositional relationships possible between feldspar crystals and silicate melt under geological and experimental conditions. These compositional relationships are fundamental to understanding the crystallization of igneous rocks and the formation of melts by partial fusion. Other geological applications include a simple explanation for some resorbed feldspars, the separation, correlation, and comparison of porphyritic rock units, interpretation of compositional changes of successive zones of zoned feldspars, and mantling of one feldspar by another. With all types of termination, extensive fractionation yields a liquid rich in Or and Ab that may crystallize to alkali feldspar or feldspars. 

","language":"English","publisher":"Oxford University Press","doi":"10.1093/petrology/3.3.280","usgsCitation":"Stewart, D.B., and Roseboom, E.H., 1962, Lower temperature terminations of the three-phase region plagioclase-alkali feldspar-liquid: Journal of Petrology, v. 3, no. 3, p. 280-315, https://doi.org/10.1093/petrology/3.3.280.","productDescription":"36 p.","startPage":"280","endPage":"315","costCenters":[],"links":[{"id":385877,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"3","issue":"3","noUsgsAuthors":false,"publicationStatus":"PW","contributors":{"authors":[{"text":"Stewart, D. B.","contributorId":41809,"corporation":false,"usgs":true,"family":"Stewart","given":"D.","email":"","middleInitial":"B.","affiliations":[],"preferred":false,"id":816300,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Roseboom, E. H. Jr.","contributorId":40730,"corporation":false,"usgs":true,"family":"Roseboom","given":"E.","suffix":"Jr.","email":"","middleInitial":"H.","affiliations":[],"preferred":false,"id":816301,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":2002571,"text":"2002571 - 1962 - Whirling disease of trouts caused by Myxosoma cerebralis in the United States","interactions":[],"lastModifiedDate":"2012-02-02T00:15:01","indexId":"2002571","displayToPublicDate":"1962-01-01T01:00:00","publicationYear":"1962","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":1,"text":"Federal Government Series"},"seriesTitle":{"id":84,"text":"Special Scientific Report - Fisheries","active":false,"publicationSubtype":{"id":1}},"seriesNumber":"427","title":"Whirling disease of trouts caused by Myxosoma cerebralis in the United States","docAbstract":"No abstract available at this time","largerWorkType":{"id":18,"text":"Report"},"largerWorkTitle":"Special Scientific Report-Fisheries ","largerWorkSubtype":{"id":1,"text":"Federal Government Series"},"language":"English","publisher":"U.S. Fish and Wildlife Service","collaboration":"114/FH","usgsCitation":"Hoffman, G.L., Dunbar, C.E., and Bradford, A., 1962, Whirling disease of trouts caused by Myxosoma cerebralis in the United States: Special Scientific Report - Fisheries 427.","costCenters":[{"id":365,"text":"Leetown Science Center","active":true,"usgs":true}],"links":[{"id":197749,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"},{"id":101761,"rank":9999,"type":{"id":10,"text":"Digital Object Identifier"},"url":"https://hdl.handle.net/2027/mdp.39015045826016?urlappend=%3Bseq=13"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e49e1e4b07f02db5e4938","contributors":{"authors":[{"text":"Hoffman, G. L.","contributorId":70713,"corporation":false,"usgs":true,"family":"Hoffman","given":"G.","email":"","middleInitial":"L.","affiliations":[],"preferred":false,"id":326620,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Dunbar, C. E.","contributorId":96623,"corporation":false,"usgs":true,"family":"Dunbar","given":"C.","middleInitial":"E.","affiliations":[],"preferred":false,"id":326622,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Bradford, A.","contributorId":72486,"corporation":false,"usgs":true,"family":"Bradford","given":"A.","email":"","affiliations":[],"preferred":false,"id":326621,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}} ,{"id":70010450,"text":"70010450 - 1962 - Summary of new data on rock samples G-1 and W-1","interactions":[],"lastModifiedDate":"2020-11-19T17:11:56.64249","indexId":"70010450","displayToPublicDate":"1962-01-01T00:00:00","publicationYear":"1962","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1759,"text":"Geochimica et Cosmochimica Acta","active":true,"publicationSubtype":{"id":10}},"title":"Summary of new data on rock samples G-1 and W-1","docAbstract":"

Published and unpublished analyses for major and minor constituents that have become available since April, 1960, are collected for the granite G-1 and diabase W-1. “Best values” are suggested for some of the elements.

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