Avian encephalomyelitis virus (AEV) was purified from infected chick embryos by a gradient centrifugation in cesium chloride. The virus had a buoyant density of 1.31 to 1.32 g/ml and a sedimentation coefficient of 148 S. The purified AEV was resistant to treatments with chloroform, acid pH or trypsin. The presence of Mg++ stabilized the virus against heat inactivation (56°C, 1 h). Electron microscopic study showed the virus to be 24 to 32 nm in diameter. The surface structure of the purified virus was not easily discernable. Nevertheless, with uranyl acetate-stained particles, Markham's rotation technique revealed that AEV has five-fold symmetry with 32 or 42 capsomers. Exact classification of AEV awaits characterization of the viral nucleic acid.
","language":"English","publisher":"Elsevier","publisherLocation":"Amsterdam","doi":"10.1016/0378-1135(80)90013-9","usgsCitation":"Gosting, L., Grinnell, B., and Matsumoto, M., 1980, Physio-chemical and morphological characteristics of avian encephalomyelitis virus: Veterinary Microbiology, v. 5, no. 2, p. 87-100, https://doi.org/10.1016/0378-1135(80)90013-9.","productDescription":"14 p.","startPage":"87","endPage":"100","numberOfPages":"14","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[{"id":654,"text":"Western Fisheries Research Center","active":true,"usgs":true}],"links":[{"id":314468,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"5","issue":"2","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"569f5e33e4b0961cf27fd16b","contributors":{"authors":[{"text":"Gosting, L.H.","contributorId":152327,"corporation":false,"usgs":false,"family":"Gosting","given":"L.H.","email":"","affiliations":[],"preferred":false,"id":588943,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Grinnell, B.W.","contributorId":152328,"corporation":false,"usgs":false,"family":"Grinnell","given":"B.W.","email":"","affiliations":[],"preferred":false,"id":588944,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Matsumoto, M.","contributorId":152329,"corporation":false,"usgs":false,"family":"Matsumoto","given":"M.","email":"","affiliations":[],"preferred":false,"id":588945,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}} ,{"id":70162236,"text":"70162236 - 1980 - Observations of wing-feather molt and summer feeding ecology of Steller's Eiders at Nelson Lagoon, Alaska","interactions":[],"lastModifiedDate":"2018-07-15T10:53:53","indexId":"70162236","displayToPublicDate":"2015-09-09T00:00:00","publicationYear":"1980","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":3764,"text":"Wildfowl","onlineIssn":"2052-6458","printIssn":"0954-6324","active":true,"publicationSubtype":{"id":10}},"title":" Observations of wing-feather molt and summer feeding ecology of Steller's Eiders at Nelson Lagoon, Alaska","docAbstract":"The population size, moult chronology, food habits, and feeding behaviour of Steller's Eiders Polysticta stelleri were studied at Nelson Lagoon, Alaska from May to October 1977. Sub-adults were flightless from late July to late August and the adult males were flightless from late August to mid September. Adult females were rarely flightless at Nelson Lagoon but commonly flightless at Izembek Bay. Steller's Eiders ate primarily bivalve mollusca and amphipod crustacea, with Mytilus edulis and Anisogammarus pugettensis the most important foods. Eiders took amphipoda prior to the wing-feather moult, bivalves during the wing-feather moult, and both types of invertebrates after the wing-feather moult. Steller's Eiders fed primarily at the low tide by diving (flock-feeding) or head-dipping, both during the day and at night. There was no difference in feeding behaviour between ages or sexes. Eiders fed almost exclusively by diving after the wing-feather moult and apparently fed more as the season progressed.
","language":"English","publisher":"Wildfowl & Wetlands Trust","usgsCitation":"Petersen, M.R., 1980, Observations of wing-feather molt and summer feeding ecology of Steller's Eiders at Nelson Lagoon, Alaska: Wildfowl, v. 31, p. 99-106.","productDescription":"7 p.","startPage":"99","endPage":"106","costCenters":[{"id":114,"text":"Alaska Science Center","active":true,"usgs":true},{"id":654,"text":"Western Fisheries Research Center","active":true,"usgs":true}],"links":[{"id":314475,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"},{"id":314474,"rank":1,"type":{"id":15,"text":"Index Page"},"url":"https://wildfowl.wwt.org.uk/index.php/wildfowl/article/view/613"}],"country":"United States","state":"Alaska","otherGeospatial":"Nelson Lagoon","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"type\": \"Polygon\",\n \"coordinates\": [\n [\n [\n -161.45919799804688,\n 55.90072605779239\n ],\n [\n -161.45919799804688,\n 56.083531295736364\n ],\n [\n -160.75195312499997,\n 56.083531295736364\n ],\n [\n -160.75195312499997,\n 55.90072605779239\n ],\n [\n -161.45919799804688,\n 55.90072605779239\n ]\n ]\n ]\n }\n }\n ]\n}","volume":"31","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"569f6c3fe4b0961cf27fd18a","contributors":{"authors":[{"text":"Petersen, Margaret R. 0000-0001-6082-3189 mrpetersen@usgs.gov","orcid":"https://orcid.org/0000-0001-6082-3189","contributorId":167729,"corporation":false,"usgs":true,"family":"Petersen","given":"Margaret","email":"mrpetersen@usgs.gov","middleInitial":"R.","affiliations":[{"id":117,"text":"Alaska Science Center Biology WTEB","active":true,"usgs":true}],"preferred":true,"id":588958,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":70162231,"text":"70162231 - 1980 - Anchialine pool crustaceans of Cape Hinau Maui","interactions":[],"lastModifiedDate":"2021-04-06T15:42:09.499434","indexId":"70162231","displayToPublicDate":"2015-09-08T00:00:00","publicationYear":"1980","noYear":false,"publicationType":{"id":24,"text":"Conference Paper"},"publicationSubtype":{"id":19,"text":"Conference Paper"},"title":"Anchialine pool crustaceans of Cape Hinau Maui","docAbstract":"No abstract available.
","language":"English","publisher":"Society for Integrative and Comparative Biology","doi":"10.1093/icb/20.4.723","usgsCitation":"Maciolek, J.A., 1980, Anchialine pool crustaceans of Cape Hinau Maui, v. 20, no. 4, p. 754-754, https://doi.org/10.1093/icb/20.4.723.","productDescription":"1 p.","startPage":"754","endPage":"754","numberOfPages":"1","costCenters":[{"id":654,"text":"Western Fisheries Research Center","active":true,"usgs":true}],"links":[{"id":480584,"rank":0,"type":{"id":40,"text":"Open Access Publisher Index Page"},"url":"https://doi.org/10.1093/icb/20.4.723","text":"Publisher Index Page"},{"id":314470,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United States","state":"Hawaii","otherGeospatial":"Cape Kinau, Maui","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"type\": \"Polygon\",\n \"coordinates\": [\n [\n [\n -156.4961242675781,\n 20.533791292732168\n ],\n [\n -156.4961242675781,\n 20.657843692552532\n ],\n [\n -156.3182830810547,\n 20.657843692552532\n ],\n [\n -156.3182830810547,\n 20.533791292732168\n ],\n [\n -156.4961242675781,\n 20.533791292732168\n ]\n ]\n ]\n }\n }\n ]\n}","volume":"20","issue":"4","noUsgsAuthors":false,"publicationDate":"1980-11-01","publicationStatus":"PW","scienceBaseUri":"569f6c3ae4b0961cf27fd179","contributors":{"authors":[{"text":"Maciolek, J. A.","contributorId":62655,"corporation":false,"usgs":true,"family":"Maciolek","given":"J.","email":"","middleInitial":"A.","affiliations":[],"preferred":false,"id":588946,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":70157466,"text":"70157466 - 1980 - Ground-water resources and geology of Washington and Ozaukee Counties, Wisconsin","interactions":[],"lastModifiedDate":"2018-01-08T19:34:35","indexId":"70157466","displayToPublicDate":"2015-03-02T05:15:00","publicationYear":"1980","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":2,"text":"State or Local Government Series"},"seriesTitle":{"id":5596,"text":"Wisconsin Geological & Natural History Survey Information Circular","active":true,"publicationSubtype":{"id":2}},"seriesNumber":"38","title":"Ground-water resources and geology of Washington and Ozaukee Counties, Wisconsin","docAbstract":"Population growth is placing increased demands on water supplies in Washington and Ozaukee Counties. Water from three principal aquifers supplies most municipal, industrial, irrigation, residential, and farm water needs in these counties. These are the sand-and-gravel, Niagara, and sandstone aquifers. As much as 15 gallons per minute can be obtained from wells almost everywhere in these counties. Yields of 500 to 1,000 gallons per minute are available from the sand-and-gravel aquifer in parts of Washington County. The Niagara aquifer underlies most of the area and can yield as much as 500 gallons per minute in most of Ozaukee and eastern Washington Counties. It yields less than 100 gallons per minute in some areas, notably eastern Mequon in Ozaukee County and parts of western Washington County. The sandstone aquifer underlies the entire area and generally can yield more than 1,000 gallons per minute to wells. However, yields of less than 500 gallons per minute are common in southwestern Washington County, where the aquifer is thinnest.
","language":"English","publisher":"Wisconsin Geological & Natural History Survey","collaboration":"Prepared in cooperation with Wisconsin Geological and Natural History Survey","usgsCitation":"Young, H.L., and Batten, W.G., 1980, Ground-water resources and geology of Washington and Ozaukee Counties, Wisconsin: Wisconsin Geological & Natural History Survey Information Circular 38, iv, 38 p.","productDescription":"iv, 38 p.","numberOfPages":"43","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[],"links":[{"id":308477,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"},{"id":350390,"rank":2,"type":{"id":15,"text":"Index Page"},"url":"https://wgnhs.uwex.edu/pubs/download_ic38/"}],"country":"United States","state":"Wisconsin","county":"Ozaukee County, Washington County","geographicExtents":"{\"type\":\"FeatureCollection\",\"features\":[{\"type\":\"Feature\",\"geometry\":{\"type\":\"Polygon\",\"coordinates\":[[[-88.0402,43.5423],[-87.9215,43.5436],[-87.8009,43.543],[-87.7933,43.5434],[-87.7933,43.542],[-87.7945,43.5202],[-87.7935,43.5075],[-87.794,43.4883],[-87.798,43.4788],[-87.8086,43.4594],[-87.8184,43.4445],[-87.8334,43.4269],[-87.845,43.4152],[-87.8541,43.4044],[-87.8631,43.3946],[-87.8651,43.39],[-87.8665,43.3859],[-87.8647,43.3836],[-87.8641,43.3818],[-87.866,43.3809],[-87.8691,43.3814],[-87.8717,43.3787],[-87.8743,43.3742],[-87.875,43.3728],[-87.8784,43.3606],[-87.8819,43.3479],[-87.8828,43.3365],[-87.8862,43.3257],[-87.8864,43.3179],[-87.889,43.3125],[-87.8891,43.3075],[-87.8918,43.3007],[-87.8977,43.2903],[-87.9017,43.2826],[-87.9056,43.2754],[-87.909,43.2659],[-87.911,43.2577],[-87.9112,43.2523],[-87.9114,43.2436],[-87.9096,43.2372],[-87.9085,43.2327],[-87.9067,43.2276],[-87.9049,43.2226],[-87.9019,43.2176],[-87.8988,43.2153],[-87.8977,43.2102],[-87.8978,43.2057],[-87.8979,43.2007],[-87.8967,43.197],[-87.8949,43.1947],[-87.9433,43.1949],[-87.9873,43.1945],[-88.0639,43.194],[-88.1827,43.1948],[-88.3027,43.1954],[-88.4183,43.1964],[-88.4187,43.2856],[-88.4187,43.3703],[-88.4017,43.3701],[-88.4008,43.4598],[-88.4008,43.5435],[-88.2808,43.5429],[-88.1608,43.5431],[-88.0402,43.5423]]]},\"properties\":{\"name\":\"Ozaukee\",\"state\":\"WI\"}}]}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"56051ec9e4b058f706e512d9","contributors":{"authors":[{"text":"Young, H. L.","contributorId":23922,"corporation":false,"usgs":true,"family":"Young","given":"H.","email":"","middleInitial":"L.","affiliations":[],"preferred":false,"id":573247,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Batten, W. G.","contributorId":89504,"corporation":false,"usgs":true,"family":"Batten","given":"W.","email":"","middleInitial":"G.","affiliations":[{"id":595,"text":"U.S. Geological Survey","active":false,"usgs":true}],"preferred":false,"id":573248,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":70118039,"text":"70118039 - 1980 - Modern sedimentary facies of the open Pacific coast and Pleistocene analogs from Montery Bay, California","interactions":[],"lastModifiedDate":"2014-07-25T10:30:01","indexId":"70118039","displayToPublicDate":"2013-07-25T10:07:00","publicationYear":"1980","noYear":false,"publicationType":{"id":24,"text":"Conference Paper"},"publicationSubtype":{"id":19,"text":"Conference Paper"},"title":"Modern sedimentary facies of the open Pacific coast and Pleistocene analogs from Montery Bay, California","docAbstract":"Depositional processes and sedimentary structures of wave-dominated Pacific coastal environments vary systematically with water depth. The depth-limited open-coast facies identifiable by their sedimentary structures are the inner shelf, barred or nonbarred nearshore, beach, and coastal dune facies. These facies are most commonly preserved in shallowing-upward progradational sequences.
\nThe vertical sequence of sedimentary structures preserved in marine terrace deposits in the northern Monterey Bay region is very similar to that predicted on the basis of the modern facies. Few marine sediments deposited during the marine transgression that accompanied rising sea level were preserved. Most of the the marine and eolian sediments form a progradational sequence deposited mainly during intervals of falling sea level. In contrast, the sediments that form the adjacent fluvial terraces were deposited mainly during periods of rising sea level and became entrenched during the subsequent lowering of sea level. In combination, these fluvial, marine, and eolian deposits provide a record of a complete eustatic cycle.
\nThe recognition of the role of changing sea level in controlling patterns of coastal sedimentation and landform development during the Quaternary allows the development of a generalized model for Quaternary sedimentation along a wave-dominated coastline. The application of this model has aided in the interpretation of older Pleistocene sediments in the region (e.g. the Aromas Sand). It also has resulted in the recognition of at least eleven glacio-eustatic cycles preserved in the stratigraphic record of the Monterey Bay area during the Quaternary.
","largerWorkType":{"id":4,"text":"Book"},"largerWorkTitle":"Quaternary depositional environments of the Pacific Coast : Pacific Coast Paleogeography Symposium 4","largerWorkSubtype":{"id":12,"text":"Conference publication"},"language":"English","publisher":"Society of Economic Paleontologists and Mineralogists","publisherLocation":"Los Angeles, CA","usgsCitation":"Dupre, W., Clifton, H., Hunter, R.E., and Field, M.E., 1980, Modern sedimentary facies of the open Pacific coast and Pleistocene analogs from Montery Bay, California, in Quaternary depositional environments of the Pacific Coast : Pacific Coast Paleogeography Symposium 4, p. 105-120.","productDescription":"16 p.","startPage":"105","endPage":"120","costCenters":[],"links":[{"id":290982,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"},{"id":290981,"type":{"id":15,"text":"Index Page"},"url":"https://archives.datapages.com/data/pac_sepm/028/028001/pdfs/105.htm"}],"country":"United States","state":"California","otherGeospatial":"Monterey Bay","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -122.145263,36.629278 ], [ -122.145263,36.941309 ], [ -121.827806,36.941309 ], [ -121.827806,36.629278 ], [ -122.145263,36.629278 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"57ff9244e4b0824b2d16eebb","contributors":{"editors":[{"text":"Field, Michael E. mfield@usgs.gov","contributorId":2101,"corporation":false,"usgs":true,"family":"Field","given":"Michael","email":"mfield@usgs.gov","middleInitial":"E.","affiliations":[{"id":520,"text":"Pacific Coastal and Marine Science Center","active":true,"usgs":true}],"preferred":true,"id":509919,"contributorType":{"id":2,"text":"Editors"},"rank":1},{"text":"et al.","contributorId":128369,"corporation":true,"usgs":false,"organization":"et al.","id":536672,"contributorType":{"id":2,"text":"Editors"},"rank":2}],"authors":[{"text":"Dupre, W.R.","contributorId":57540,"corporation":false,"usgs":true,"family":"Dupre","given":"W.R.","email":"","affiliations":[],"preferred":false,"id":496169,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Clifton, H.E.","contributorId":44151,"corporation":false,"usgs":true,"family":"Clifton","given":"H.E.","affiliations":[],"preferred":false,"id":496167,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Hunter, R. E.","contributorId":48148,"corporation":false,"usgs":true,"family":"Hunter","given":"R.","email":"","middleInitial":"E.","affiliations":[],"preferred":false,"id":496168,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Field, Michael E. mfield@usgs.gov","contributorId":2101,"corporation":false,"usgs":true,"family":"Field","given":"Michael","email":"mfield@usgs.gov","middleInitial":"E.","affiliations":[{"id":520,"text":"Pacific Coastal and Marine Science Center","active":true,"usgs":true}],"preferred":true,"id":496166,"contributorType":{"id":1,"text":"Authors"},"rank":4}]}} ,{"id":70047613,"text":"70047613 - 1980 - Ground-water data for the Salt Basin, Eagle Flat, Red Light Draw, Green River Valley and Presidio Bolson in westernmost Texas","interactions":[{"subject":{"id":17206,"text":"ofr77575 - 1978 - Ground-water data for the Salt Basin, Eagle Flat, Red Light Draw, Green River Valley, and Presidio Bolson in westernmost Texas","indexId":"ofr77575","publicationYear":"1978","noYear":false,"title":"Ground-water data for the Salt Basin, Eagle Flat, Red Light Draw, Green River Valley, and Presidio Bolson in westernmost Texas"},"predicate":"SUPERSEDED_BY","object":{"id":70047613,"text":"70047613 - 1980 - Ground-water data for the Salt Basin, Eagle Flat, Red Light Draw, Green River Valley and Presidio Bolson in westernmost Texas","indexId":"70047613","publicationYear":"1980","noYear":false,"title":"Ground-water data for the Salt Basin, Eagle Flat, Red Light Draw, Green River Valley and Presidio Bolson in westernmost Texas"},"id":1}],"lastModifiedDate":"2016-08-12T15:43:59","indexId":"70047613","displayToPublicDate":"2013-01-01T14:23:00","publicationYear":"1980","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":2,"text":"State or Local Government Series"},"seriesTitle":{"id":133,"text":"Report","active":false,"publicationSubtype":{"id":2}},"seriesNumber":"259","title":"Ground-water data for the Salt Basin, Eagle Flat, Red Light Draw, Green River Valley and Presidio Bolson in westernmost Texas","docAbstract":"From October 1971 through October 1974. the U.S. Geological Survey collected ground-water data in the basins in Texas west of the Pecos River drainage area and northwest of the Big Bend country. The basins included are, from east to west: The Presidio Bolson; the Salt Basin; Green River Valley, Eagle Flat, and Red Light Draw. These data, which were collected in cooperation with the Texas Department of Water Resources (formerly Texas Water Development Board), will provide information for a continuing assessment of water availability within the State.
","language":"English","publisher":"Texas Department of Water Resources","publisherLocation":"San Antonio, TX","collaboration":"This report was prepared by the U.S. Geological Survey under cooperative agreement with the Texas Department of Water Resources","usgsCitation":"White, D.E., Gates, J., Smith, J.T., and Fry, B.J., 1980, Ground-water data for the Salt Basin, Eagle Flat, Red Light Draw, Green River Valley and Presidio Bolson in westernmost Texas: Report 259, iii, 97 p.","productDescription":"iii, 97 p.","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[{"id":583,"text":"Texas Water Science Center","active":true,"usgs":true}],"links":[{"id":276609,"type":{"id":15,"text":"Index Page"},"url":"https://www.twdb.texas.gov/publications/reports/numbered_reports/doc/R259/R259.pdf"},{"id":276610,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/70047613.png"}],"country":"United States","state":"Texas","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -106.65,25.84 ], [ -106.65,36.5 ], [ -93.51,36.5 ], [ -93.51,25.84 ], [ -106.65,25.84 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"520ca6e5e4b081fa6136d3ea","contributors":{"authors":[{"text":"White, Donald E.","contributorId":76787,"corporation":false,"usgs":true,"family":"White","given":"Donald","email":"","middleInitial":"E.","affiliations":[],"preferred":false,"id":482533,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Gates, Joseph S.","contributorId":21647,"corporation":false,"usgs":true,"family":"Gates","given":"Joseph S.","affiliations":[],"preferred":false,"id":482530,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Smith, James T.","contributorId":22670,"corporation":false,"usgs":true,"family":"Smith","given":"James","email":"","middleInitial":"T.","affiliations":[],"preferred":false,"id":482531,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Fry, Bonnie J.","contributorId":74285,"corporation":false,"usgs":true,"family":"Fry","given":"Bonnie","email":"","middleInitial":"J.","affiliations":[],"preferred":false,"id":482532,"contributorType":{"id":1,"text":"Authors"},"rank":4}]}} ,{"id":70047612,"text":"70047612 - 1980 - Development of Ground Water in the Houston District, Texas, 1970-1974","interactions":[{"subject":{"id":8945,"text":"ofr77413 - 1977 - Development of ground water in the Houston District, Texas, 1970-74","indexId":"ofr77413","publicationYear":"1977","noYear":false,"title":"Development of ground water in the Houston District, Texas, 1970-74"},"predicate":"SUPERSEDED_BY","object":{"id":70047612,"text":"70047612 - 1980 - Development of Ground Water in the Houston District, Texas, 1970-1974","indexId":"70047612","publicationYear":"1980","noYear":false,"title":"Development of Ground Water in the Houston District, Texas, 1970-1974"},"id":1}],"lastModifiedDate":"2016-08-12T15:41:55","indexId":"70047612","displayToPublicDate":"2013-01-01T14:03:00","publicationYear":"1980","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":2,"text":"State or Local Government Series"},"seriesTitle":{"id":133,"text":"Report","active":false,"publicationSubtype":{"id":2}},"seriesNumber":"241","title":"Development of Ground Water in the Houston District, Texas, 1970-1974","docAbstract":"Total withdrawals of ground water in the Houston district increased 9 percent from about 488 million gallons per day (21.4 cubic meters per second) in 1970 to about 532 million gallons per day (23.3 cubic meters per second) in 1974. The average annual rate of increase from 1960 to 1969 was about 6.3 percent. During 1970-74, increases in pumpage occurred in the Houston, Katy, and NASA areas; decreases occurred in the Pasadena and Alta Lorna areas; and the pumpage in the Baytown-La Porte and Texas City areas remained almost constant.
","language":"English","publisher":"Texas Water Development Board","publisherLocation":"San Antonio, TX","collaboration":"This report was prepared by the U.S. Geological Survey under cooperative agreement with the Texas Department of Water Resources and the Cities of Houston and Galveston","usgsCitation":"Gabrysch, R., 1980, Development of Ground Water in the Houston District, Texas, 1970-1974: Report 241, v, 49 p.","productDescription":"v, 49 p.","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[{"id":583,"text":"Texas Water Science Center","active":true,"usgs":true}],"links":[{"id":276608,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/70047612.png"},{"id":276607,"type":{"id":15,"text":"Index Page"},"url":"https://www.twdb.texas.gov/publications/reports/numbered_reports/doc/R241/R241.pdf"}],"country":"United States","state":"Texas","county":"Houston County","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -95.72,30.7 ], [ -95.72,31.98 ], [ -94.44,31.98 ], [ -94.44,30.7 ], [ -95.72,30.7 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"520ca6e3e4b081fa6136d3d4","contributors":{"authors":[{"text":"Gabrysch, R.K.","contributorId":105691,"corporation":false,"usgs":true,"family":"Gabrysch","given":"R.K.","affiliations":[],"preferred":false,"id":482529,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":70047765,"text":"70047765 - 1980 - Mineralogy and diagenesis of low-permeability sandstones of Late Cretaceous age, Piceance Creek Basin, northwestern Colorado","interactions":[{"subject":{"id":9341,"text":"ofr791702 - 1979 - Preliminary results of mineralogic and diagenetic studies of low-permeability sandstones of Late Cretaceous age, Piceance Creek basin, northwestern Colorado","indexId":"ofr791702","publicationYear":"1979","noYear":false,"title":"Preliminary results of mineralogic and diagenetic studies of low-permeability sandstones of Late Cretaceous age, Piceance Creek basin, northwestern Colorado"},"predicate":"SUPERSEDED_BY","object":{"id":70047765,"text":"70047765 - 1980 - Mineralogy and diagenesis of low-permeability sandstones of Late Cretaceous age, Piceance Creek Basin, northwestern Colorado","indexId":"70047765","publicationYear":"1980","noYear":false,"title":"Mineralogy and diagenesis of low-permeability sandstones of Late Cretaceous age, Piceance Creek Basin, northwestern Colorado"},"id":1}],"lastModifiedDate":"2013-08-22T13:25:19","indexId":"70047765","displayToPublicDate":"2013-01-01T13:20:00","publicationYear":"1980","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":2789,"text":"Mountain Geologist","active":true,"publicationSubtype":{"id":10}},"title":"Mineralogy and diagenesis of low-permeability sandstones of Late Cretaceous age, Piceance Creek Basin, northwestern Colorado","docAbstract":"This report presents preliminary results of a mineralogic and diagenetic study of some low-permeability sandstones from measured surface sections and cores obtained from drill holes in the Piceance Creek Basin of northwestern Colorado. A documentation of the mineralogy and diagenetic history will aid in the exploration for natural gas and in the development of recovery technology in these low-permability sandstones. These sandstones are in the nonmarine upper part of the Mesaverde Formation (or Group) of Late Cretaceous age and are separated from overlying lower Tertiary rocks by a major regional unconformity. Attention is focused on the sandstone units of the Ohio Creek Member, which directly underlies the unconformity; however, comparisons between the mineralogy of the Ohio Creek strata and that of the underlying sandstone units are made whenever possible. The Ohio Creek is a member of the Hunter Canyon Formation (Mesaverde Group) in the southwestern part of the basin, and the Mesaverde Formation in the southern and central parts of the basin. The detrital mineralogy is fairly constant throughout all of these nonrnarine Cretaceous sandstone units; however, in the southeastern part of the basin, there is an increase in percentage of feldspar, quartzite, and igneous rock fragments in sandstones of the Ohio Creek Member directly underlying the unconformity. In the southwestern part of the basin, sandstones of the Ohio Creek Member are very weathered and are almost-entirely comprised of quartz, chert, and kaolinite. A complex diagenetic history, partly related to the overlying unconformity, appears to be responsible for transforming these sandstones into potential gas reservoirs. The general diagenetic sequence for the entire Upper Cretaceous interval studied is interpreted to be (early to late): early(?) calcite cement, chlorite, quartz overgrowths, calcite cement, secondary porosity, analcime (surface only), kaolinite and illite, and late carbonate cements. Authigenic high-iron chlorite, which occurs on grain rims and in pore throats, is primarily responsible for the low-permeability of the subsurface sandstones of the Ohio Creek Member in the center of the basin. Kaolinite is the most abundant pore-filling authigenic clay in these sandstones, from the southwestern part of the basin and is responsible for their distinctive white-weathering color in outcrop. In the sandstones below the Ohio Creek Member, however, chlorite and kaolinite occur locally, and authigenic calcite and illite are more abundant. The occurrence and distribution of secondary porosity is one of the most important aspects of the diagenetic history of these sandstones. It is present as moldic intra- and intergranular porosity, as well as microporosity among authigenic clay pariicles. Although present locally in most sandstone units, secondary porosity is particularly common in the uppermost sandstone units and is interpreted to have formed primarily asa result ofweathering during the time represented by the Cretaceous-Tertiary unconformity.","largerWorkType":{"id":2,"text":"Article"},"largerWorkTitle":"Mountain Geologist","largerWorkSubtype":{"id":10,"text":"Journal Article"},"language":"English","publisher":"Rocky Mountain Association of Geologists","usgsCitation":"Hansley, P.L., and Johnson, R.C., 1980, Mineralogy and diagenesis of low-permeability sandstones of Late Cretaceous age, Piceance Creek Basin, northwestern Colorado: Mountain Geologist, v. 17, no. 4, p. 88-106.","productDescription":"19 p.","startPage":"88","endPage":"106","costCenters":[],"links":[{"id":276902,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"},{"id":276901,"type":{"id":11,"text":"Document"},"url":"https://archives.datapages.com/data/rmag/mg/1980/hansley.pdf"}],"country":"United States","state":"Colorado","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -109.0603,36.9924 ], [ -109.0603,41.0034 ], [ -102.0409,41.0034 ], [ -102.0409,36.9924 ], [ -109.0603,36.9924 ] ] ] } } ] }","volume":"17","issue":"4","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"521732e6e4b043bae8d2e5f6","contributors":{"authors":[{"text":"Hansley, Paula L.","contributorId":29380,"corporation":false,"usgs":true,"family":"Hansley","given":"Paula","email":"","middleInitial":"L.","affiliations":[],"preferred":false,"id":482924,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Johnson, Ronald C. 0000-0002-6197-5165 rcjohnson@usgs.gov","orcid":"https://orcid.org/0000-0002-6197-5165","contributorId":1550,"corporation":false,"usgs":true,"family":"Johnson","given":"Ronald","email":"rcjohnson@usgs.gov","middleInitial":"C.","affiliations":[{"id":164,"text":"Central Energy Resources Science Center","active":true,"usgs":true}],"preferred":true,"id":482923,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":70047454,"text":"70047454 - 1980 - Summary groundwater resources of Centre County, Pennsylvania","interactions":[{"subject":{"id":48452,"text":"ofr791531 - 1979 - Summary of ground-water resources of Centre County, Pennsylvania","indexId":"ofr791531","publicationYear":"1979","noYear":false,"title":"Summary of ground-water resources of Centre County, Pennsylvania"},"predicate":"SUPERSEDED_BY","object":{"id":70047454,"text":"70047454 - 1980 - Summary groundwater resources of Centre County, Pennsylvania","indexId":"70047454","publicationYear":"1980","noYear":false,"title":"Summary groundwater resources of Centre County, Pennsylvania"},"id":1}],"lastModifiedDate":"2013-08-06T13:23:01","indexId":"70047454","displayToPublicDate":"2013-01-01T13:14:00","publicationYear":"1980","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":2,"text":"State or Local Government Series"},"seriesTitle":{"id":143,"text":"Water Resource Report","active":false,"publicationSubtype":{"id":2}},"seriesNumber":"48","title":"Summary groundwater resources of Centre County, Pennsylvania","docAbstract":"The northwest third of Centre County lies in the Appalachian Plateaus physiographic province. The higher altitudes are underlain by the Conemaugh, Allegheny, and Pottsville Groups, which consist of sandstone, shale, and thin limestone and coal beds. The average yield of nondomestic wells in the Allegheny Group is 20 gpm (gallons per minute) and that in the Pottsville Group 100 gpm. Water from wells in these groups commonly has a high concentration of iron. Most of the rest of the Appalachian Plateaus province is underlain by the Burgoon Sandstone. The Burgoon yields soft water, and the average yield of nondomestic wells is 70 gpm.","language":"English","publisher":"Pennsylvania Geological Survey","publisherLocation":"Harrisburg, PA","collaboration":"Prepared by the U. S. Geological Survey, Water Resources Division, in cooperation with the Pennsylvania Geological Survey","usgsCitation":"Wood, C.R., 1980, Summary groundwater resources of Centre County, Pennsylvania: Water Resource Report 48, vii, 60 p.","productDescription":"vii, 60 p.","costCenters":[{"id":629,"text":"Water Resources Division","active":false,"usgs":true}],"links":[{"id":276126,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/70047454.PNG"},{"id":276125,"type":{"id":11,"text":"Document"},"url":"https://www.dcnr.state.pa.us/cs/groups/public/documents/document/dcnr_016331.zip"}],"country":"United States","state":"Pennsylvania","county":"Centre County","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -78.3767,40.6916 ], [ -78.3767,41.2528 ], [ -77.1438,41.2528 ], [ -77.1438,40.6916 ], [ -78.3767,40.6916 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"52021ae8e4b0e21cafa49c90","contributors":{"authors":[{"text":"Wood, Charles R.","contributorId":30259,"corporation":false,"usgs":true,"family":"Wood","given":"Charles","email":"","middleInitial":"R.","affiliations":[],"preferred":false,"id":482071,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":70047502,"text":"70047502 - 1980 - Hydrogeologic atlas, Winfield quadrangle, Carroll County, Maryland","interactions":[{"subject":{"id":43743,"text":"ofr77793 - 1977 - Winfield Quadrangle, geology, hydrology and mineral resoures","indexId":"ofr77793","publicationYear":"1977","noYear":false,"title":"Winfield Quadrangle, geology, hydrology and mineral resoures"},"predicate":"SUPERSEDED_BY","object":{"id":70047502,"text":"70047502 - 1980 - Hydrogeologic atlas, Winfield quadrangle, Carroll County, Maryland","indexId":"70047502","publicationYear":"1980","noYear":false,"title":"Hydrogeologic atlas, Winfield quadrangle, Carroll County, Maryland"},"id":1}],"lastModifiedDate":"2013-08-08T09:57:40","indexId":"70047502","displayToPublicDate":"2013-01-01T09:54:00","publicationYear":"1980","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":2,"text":"State or Local Government Series"},"seriesTitle":{"id":132,"text":"Quadrangle Atlas","active":false,"publicationSubtype":{"id":2}},"seriesNumber":"10","title":"Hydrogeologic atlas, Winfield quadrangle, Carroll County, Maryland","language":"English","publisher":"Maryland Geological Survey","publisherLocation":"Baltimore, MD","collaboration":"Prepared in cooperation with the United States Geological Survey and the Commissioners of Carroll County","usgsCitation":"Otton, E., 1980, Hydrogeologic atlas, Winfield quadrangle, Carroll County, Maryland: Quadrangle Atlas 10, Maps: 5 Sheets.","productDescription":"Maps: 5 Sheets","costCenters":[],"links":[{"id":276197,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United States","state":"Maryl","county":"Carroll County","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -77.125,39.375 ], [ -77.125,39.5 ], [ -77.0,39.5 ], [ -77.0,39.375 ], [ -77.125,39.375 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"5204bdede4b0403aa6262a5a","contributors":{"authors":[{"text":"Otton, E. G.","contributorId":22311,"corporation":false,"usgs":true,"family":"Otton","given":"E. G.","affiliations":[],"preferred":false,"id":482200,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":70047780,"text":"70047780 - 1980 - Geologic field trip guide for the Cenozoic stratigraphy and late Eocene paleoecology of southwestern Washington","interactions":[{"subject":{"id":7744,"text":"ofr80362 - 1980 - Geologic field trip guide for Cenozoic stratigraphy of southwestern Washington","indexId":"ofr80362","publicationYear":"1980","noYear":false,"title":"Geologic field trip guide for Cenozoic stratigraphy of southwestern Washington"},"predicate":"SUPERSEDED_BY","object":{"id":70047780,"text":"70047780 - 1980 - Geologic field trip guide for the Cenozoic stratigraphy and late Eocene paleoecology of southwestern Washington","indexId":"70047780","publicationYear":"1980","noYear":false,"title":"Geologic field trip guide for the Cenozoic stratigraphy and late Eocene paleoecology of southwestern Washington"},"id":1}],"lastModifiedDate":"2013-08-23T09:31:09","indexId":"70047780","displayToPublicDate":"2013-01-01T09:26:00","publicationYear":"1980","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1779,"text":"Geologic field trips in western Oregon and southwestern Washington (Bulletin 101)","active":true,"publicationSubtype":{"id":10}},"title":"Geologic field trip guide for the Cenozoic stratigraphy and late Eocene paleoecology of southwestern Washington","largerWorkType":{"id":18,"text":"Report"},"largerWorkTitle":"Geologic field trips in western Oregon and southwestern Washington (Bulletin 101)","largerWorkSubtype":{"id":2,"text":"State or Local Government Series"},"language":"English","publisher":"Oregon Department of Geology and Mineral Industries","publisherLocation":"Portland, OR","usgsCitation":"Armentrout, J., McDougall, K., Jefferis, P., and Nesbitt, E., 1980, Geologic field trip guide for the Cenozoic stratigraphy and late Eocene paleoecology of southwestern Washington: Geologic field trips in western Oregon and southwestern Washington (Bulletin 101), p. 79-119.","productDescription":"41 p.","startPage":"79","endPage":"119","costCenters":[],"links":[{"id":276932,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United States","state":"Washington","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -124.79,45.54 ], [ -124.79,49.0 ], [ -116.92,49.0 ], [ -116.92,45.54 ], [ -124.79,45.54 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"52188466e4b0e27b926cc69c","contributors":{"authors":[{"text":"Armentrout, J.M.","contributorId":16176,"corporation":false,"usgs":true,"family":"Armentrout","given":"J.M.","email":"","affiliations":[],"preferred":false,"id":482949,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"McDougall, Kristin 0000-0002-8788-3664","orcid":"https://orcid.org/0000-0002-8788-3664","contributorId":85610,"corporation":false,"usgs":true,"family":"McDougall","given":"Kristin","affiliations":[],"preferred":false,"id":482952,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Jefferis, P.T.","contributorId":77830,"corporation":false,"usgs":true,"family":"Jefferis","given":"P.T.","email":"","affiliations":[],"preferred":false,"id":482951,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Nesbitt, Elizabeth","contributorId":34812,"corporation":false,"usgs":true,"family":"Nesbitt","given":"Elizabeth","email":"","affiliations":[],"preferred":false,"id":482950,"contributorType":{"id":1,"text":"Authors"},"rank":4}]}} ,{"id":70047779,"text":"70047779 - 1980 - Salym: potential W. Siberian oil giant","interactions":[{"subject":{"id":8277,"text":"ofr80145 - 1980 - Salym; potential giant oil field in West Siberia; possible reservoir stimulation experiment using a nuclear explosion","indexId":"ofr80145","publicationYear":"1980","noYear":false,"title":"Salym; potential giant oil field in West Siberia; possible reservoir stimulation experiment using a nuclear explosion"},"predicate":"SUPERSEDED_BY","object":{"id":70047779,"text":"70047779 - 1980 - Salym: potential W. Siberian oil giant","indexId":"70047779","publicationYear":"1980","noYear":false,"title":"Salym: potential W. Siberian oil giant"},"id":1}],"lastModifiedDate":"2018-02-19T17:27:34","indexId":"70047779","displayToPublicDate":"2013-01-01T09:08:00","publicationYear":"1980","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":2941,"text":"Oil & Gas Journal","printIssn":"0030-1388","active":true,"publicationSubtype":{"id":10}},"title":"Salym: potential W. Siberian oil giant","docAbstract":"SALYM oil field is on the Lempa high of the Salym uplift in the eastern part of the Khanty-Mansiysk depression in the Middle Ob region of West Siberia.\n\nThe Salym uplift is about 50 km long and 45 km wide and trends north. The Lempa high is 25 km long and 16 km wide; closure is 150 m. The Salym field is about 275 km west of the giant Samotlor field.\n\nStratigraphy. The sedimentary cover overlying the Paleozoic Hercynide basement in the Middle Ob region consists of Jurassic, Lower and Upper Cretaceous, Paleogene, and Quaternary marine and continental sediments.","language":"English","publisher":"PennWell Corporation","publisherLocation":"Tulsa, OK","usgsCitation":"Clarke, J.W., and Rachlin, J., 1980, Salym: potential W. Siberian oil giant: Oil & Gas Journal, v. 78, p. 132-135.","productDescription":"4 p.","startPage":"132","endPage":"135","costCenters":[],"links":[{"id":276931,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"Russia","otherGeospatial":"Salym, Siberia","volume":"78","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"5218846be4b0e27b926cc6e1","contributors":{"authors":[{"text":"Clarke, James W.","contributorId":35297,"corporation":false,"usgs":true,"family":"Clarke","given":"James","email":"","middleInitial":"W.","affiliations":[],"preferred":false,"id":482947,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Rachlin, Jack","contributorId":52175,"corporation":false,"usgs":true,"family":"Rachlin","given":"Jack","email":"","affiliations":[],"preferred":false,"id":482948,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":70047777,"text":"70047777 - 1980 - Textural and structural evidence for a predeformation hydrothermal origin of the Tungsten Queen Deposit, Hamme District, North Carolina","interactions":[{"subject":{"id":8881,"text":"ofr78427 - 1978 - Premetamorphic hydrothermal origin of the Tungsten Queen vein, Hamme District, North Carolina, as indicated by mineral textures and minor structures","indexId":"ofr78427","publicationYear":"1978","noYear":false,"title":"Premetamorphic hydrothermal origin of the Tungsten Queen vein, Hamme District, North Carolina, as indicated by mineral textures and minor structures"},"predicate":"SUPERSEDED_BY","object":{"id":70047777,"text":"70047777 - 1980 - Textural and structural evidence for a predeformation hydrothermal origin of the Tungsten Queen Deposit, Hamme District, North Carolina","indexId":"70047777","publicationYear":"1980","noYear":false,"title":"Textural and structural evidence for a predeformation hydrothermal origin of the Tungsten Queen Deposit, Hamme District, North Carolina"},"id":1}],"lastModifiedDate":"2013-08-23T08:57:29","indexId":"70047777","displayToPublicDate":"2013-01-01T08:52:00","publicationYear":"1980","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":"Textural and structural evidence for a predeformation hydrothermal origin of the Tungsten Queen Deposit, Hamme District, North Carolina","docAbstract":"The Hamme tungsten district is composed of a series of steeply dipping quartz-wolframite veins in the Piedmont of North Carolina. Veins are concentrated near the border of the lower Paleozoic Vance County pluton, along its western contact with green-schist-facies metapelites and metavolcanic rocks of the Carolina slate belt. One of these quartz veins, the Snead-Walker, hosts the Tungsten Queen deposit. The vein is 0 to 10 m thick and trends N 35 degrees E for approximately 3,500 m through slate belt rocks and the granitic pluton. The deposit has been worked to a depth of nearly 520 m and contains eight en echelon ore lodes that plunge 42 degrees to 65 degrees between S 10 degrees E and S 10 degrees W. Ore lodes commonly are encased in thin lenses of quartz-sericite greisen. The principal ore mineral is huebnerite and is accompanied by scattered occurrences of pyrite, sphalerite, galena, chalcopyrite, and tetrahedrite. The gangue is predominantly quartz with minor amounts of fluorite, sericite, and carbonate.Studies of minor structures and mineral textures indicate that both the wall rock and the ore and gangue minerals within the vein have been deformed by at least two events. The first event produced relatively gentle, open, and shallow-plunging folds; later, an intense episode of right-lateral shearing developed steeply plunging, tight folds and numerous northeast-trending shears. This latter deformation also developed a prominent alignment of ore and gangue minerals oblique to the vein walls and may have formed the en echelon distribution of ore lodes.In relatively undeformed parts of the vein, clusters of euhedral huebnerite crystals are oriented perpendicular to vein layering. Some prismatic crystals have terminations with cappings of sulfides and in polished thin section show concentric growth zones. These features are similar to textures found in unmetamorphosed tungsten-bearing hydrothermal vein deposits such as those at Pasto Bueno, Peru; Carrock Fell, England; and Panasqueria, Portugal. The relationships of mineral textures and minor structures indicate that the Tungsten Queen deposit formed by open-space fillings of linear faults or fractures and was subsequently deformed by at least two episodes of folding and shearing.","largerWorkType":{"id":2,"text":"Article"},"largerWorkTitle":"Economic Geology","largerWorkSubtype":{"id":10,"text":"Journal Article"},"language":"English","publisher":"Society of Economic Geologists","doi":"10.2113/gsecongeo.75.4.515","usgsCitation":"Foose, M.P., Slack, J.F., and Casadevall, T., 1980, Textural and structural evidence for a predeformation hydrothermal origin of the Tungsten Queen Deposit, Hamme District, North Carolina: Economic Geology, v. 75, no. 4, p. 515-522, https://doi.org/10.2113/gsecongeo.75.4.515.","productDescription":"8 p.","startPage":"515","endPage":"522","costCenters":[],"links":[{"id":276930,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"},{"id":276929,"type":{"id":10,"text":"Digital Object Identifier"},"url":"https://dx.doi.org/10.2113/gsecongeo.75.4.515"}],"country":"United States","state":"North Carolina","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -84.3219,33.841 ], [ -84.3219,36.5882 ], [ -75.46,36.5882 ], [ -75.46,33.841 ], [ -84.3219,33.841 ] ] ] } } ] }","volume":"75","issue":"4","noUsgsAuthors":false,"publicationDate":"1980-07-01","publicationStatus":"PW","scienceBaseUri":"5218846ce4b0e27b926cc6ef","contributors":{"authors":[{"text":"Foose, M. 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Discordant fission track ages of apatite and zircon in the older rocks reveal a major heat source that cooled in late Miocene or early Pliocene and is centered under the mineralized rocks near the townsite of Rico. 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