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","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Reston, VA","doi":"10.3133/ofr6448","usgsCitation":"Ekren, E.B., and Sargent, K., 1964, Geologic map of the Skull Mountain quadrangle at the Nevada Test Site, Nye County, Nevada: U.S. Geological Survey Open-File Report 64-48, 1 Plate: 39.15 x 32.59 inches, https://doi.org/10.3133/ofr6448.","productDescription":"1 Plate: 39.15 x 32.59 inches","costCenters":[],"links":[{"id":369585,"rank":2,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1964/0048/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":173155,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1964/0048/report-thumb.jpg"}],"scale":"24000","country":"United States","state":"Nevada","county":"Nye County","geographicExtents":"{\"type\":\"FeatureCollection\",\"features\":[{\"type\":\"Feature\",\"geometry\":{\"type\":\"Polygon\",\"coordinates\":[[[-115.9082,39.1615],[-115.5191,38.9578],[-115.4725,38.9325],[-115.4433,38.9162],[-115.3694,38.8769],[-115.363,38.874],[-115.242,38.8093],[-115.0969,38.7309],[-115.0777,38.721],[-115.0604,38.7107],[-115.0291,38.6937],[-114.999,38.6777],[-114.9996,38.592],[-114.9997,38.4315],[-114.9994,38.3894],[-115.0004,38.0507],[-115.1185,38.0508],[-115.1436,38.0508],[-115.326,38.0515],[-115.3453,38.0514],[-115.4003,38.051],[-115.4587,38.0506],[-115.6394,38.0512],[-115.6581,38.051],[-115.8404,38.0504],[-115.8931,38.0507],[-115.8938,37.723],[-115.8969,37.5498],[-115.8975,37.2796],[-115.8982,37.1926],[-115.8942,36.8425],[-115.8941,36.686],[-115.8945,36.6702],[-115.8949,36.598],[-115.8949,36.5962],[-115.8946,36.5858],[-115.8947,36.5005],[-115.8945,36.4806],[-115.8949,36.462],[-115.8944,36.457],[-115.8948,36.3087],[-115.8945,36.2923],[-115.8943,36.1957],[-115.8945,36.1608],[-115.8948,36.1163],[-115.8948,36.0927],[-115.895,36.0015],[-115.9178,36.0192],[-115.9518,36.0457],[-115.9925,36.0773],[-116.049,36.1211],[-116.0624,36.1314],[-116.1039,36.1636],[-116.1287,36.1829],[-116.1702,36.2152],[-116.173,36.2174],[-116.2311,36.2626],[-116.2834,36.3028],[-116.2954,36.3122],[-116.3752,36.373],[-116.5107,36.4764],[-116.5247,36.4871],[-116.5589,36.5131],[-116.574,36.5245],[-116.5946,36.54],[-116.6556,36.5867],[-116.6583,36.5888],[-116.6764,36.6024],[-116.706,36.6248],[-116.7895,36.6877],[-116.8424,36.7276],[-116.8453,36.7298],[-116.8806,36.7568],[-116.8912,36.7648],[-116.9237,36.7891],[-116.9641,36.8193],[-116.9783,36.8299],[-116.981,36.8319],[-117.0046,36.8495],[-117.164,36.9688],[-117.1639,36.9698],[-117.1637,37.0182],[-117.164,37.0894],[-117.1642,37.171],[-117.1641,37.1909],[-117.1641,37.1936],[-117.1665,37.6995],[-117.1664,37.714],[-117.1663,37.7285],[-117.1663,37.7435],[-117.1662,37.7585],[-117.1657,38.0019],[-117.2198,38.0482],[-117.2397,38.0483],[-117.239,38.0641],[-117.2408,38.0705],[-117.2653,38.0932],[-117.6896,38.4731],[-118.0197,38.7599],[-118.197,38.9154],[-118.1972,38.9993],[-117.8559,39.0746],[-117.7748,39.092],[-117.7008,39.1058],[-117.6409,39.1149],[-117.5946,39.1231],[-117.4742,39.1431],[-117.3823,39.1562],[-117.3609,39.1585],[-117.3318,39.1629],[-117.3063,39.1634],[-117.2849,39.1633],[-117.1995,39.1632],[-117.0856,39.1628],[-117.0322,39.1626],[-117.0144,39.1626],[-116.9871,39.1625],[-116.9158,39.1631],[-116.7562,39.1622],[-116.7301,39.1625],[-116.5996,39.1616],[-116.5859,39.162],[-116.4815,39.1616],[-116.3497,39.1618],[-116.2358,39.1616],[-116.0548,39.1624],[-115.9082,39.1615]]]},\"properties\":{\"name\":\"Nye\",\"state\":\"NV\"}}]}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ae6e4b07f02db68b47d","contributors":{"authors":[{"text":"Ekren, E. B.","contributorId":14371,"corporation":false,"usgs":true,"family":"Ekren","given":"E.","middleInitial":"B.","affiliations":[],"preferred":false,"id":233722,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Sargent, Kenneth A.","contributorId":15998,"corporation":false,"usgs":true,"family":"Sargent","given":"Kenneth A.","affiliations":[],"preferred":false,"id":233723,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":23497,"text":"ofr6491 - 1964 - Geology of the Pluto Site, Area 401, Nevada Test Site, Nye County, Nevada","interactions":[],"lastModifiedDate":"2012-02-02T00:08:09","indexId":"ofr6491","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1964","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":330,"text":"Open-File Report","code":"OFR","onlineIssn":"2331-1258","printIssn":"0196-1497","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"64-91","title":"Geology of the Pluto Site, Area 401, Nevada Test Site, Nye County, Nevada","language":"ENGLISH","publisher":"U.S. Dept. of Interior, Geological Survey,","doi":"10.3133/ofr6491","issn":"0094-9140","usgsCitation":"Johnson, R., and Ege, J.R., 1964, Geology of the Pluto Site, Area 401, Nevada Test Site, Nye County, Nevada: U.S. Geological Survey Open-File Report 64-91, 128 p., 41 figs., 14 tables, 127 leaves :ill., maps ;27 cm., https://doi.org/10.3133/ofr6491.","productDescription":"128 p., 41 figs., 14 tables, 127 leaves :ill., maps ;27 cm.","costCenters":[],"links":[{"id":156665,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4acce4b07f02db67e855","contributors":{"authors":[{"text":"Johnson, Ross B.","contributorId":96299,"corporation":false,"usgs":true,"family":"Johnson","given":"Ross B.","affiliations":[],"preferred":false,"id":190205,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Ege, John R.","contributorId":69534,"corporation":false,"usgs":true,"family":"Ege","given":"John","email":"","middleInitial":"R.","affiliations":[],"preferred":false,"id":190204,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":70043887,"text":"70043887 - 1964 - Seismic-refraction measurements of crustal structure between Nevada Test Site and Ludlow, California","interactions":[],"lastModifiedDate":"2013-02-25T08:55:50","indexId":"70043887","displayToPublicDate":"1964-02-22T00:00:00","publicationYear":"1964","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":6,"text":"USGS Unnumbered Series"},"seriesTitle":{"id":355,"text":"Crustal Studies Technical Letter","active":false,"publicationSubtype":{"id":6}},"seriesNumber":"26","title":"Seismic-refraction measurements of crustal structure between Nevada Test Site and Ludlow, California","docAbstract":"Seismic-refraction measurements from nuclear and chemical explosions were made along a line from the Nevada Test Site (NTS) to Ludlow, California, and additional recordings from nuclear explosions were made southward toward Calexico, California. The time of first arrivals from the Ludlow shotpoint is expressed as T0 = 0.00 + Δ/2.50 (assumed), T1 = 1.00 + Δ6.10, T2 = 2.81 + Δ/6.80, and T3 = 5.48 + ~7.76, where T is in seconds and distance Δ is in km. First arrival times from NTS fit the lines T1 = 0.74 + Δ/6.10, T2 = 2.81 + Δ/6.80 (assumed), T3 = 6.70 + Δ/8.04 to a distance of 265 km, beyond 265 km T3 = 5.83 + Δ/7.75. The difference in the apparent velocities of the Pn (T3) arrival is caused by variations in the dip of the Mohorovicic discontinuity. The thickness of the successive layers at NTS are H0 s 1.0 km (V0 ~ 2.5 km/sec), H1 = 13 km (v1 = 6.1 km/sec), and H2 = 20 km (v2 = 6.8 km/ sec); the total crustal thickness is 34 km. The successive crustal layers at Ludlow have a thickness of H0 = 1.4 km, H1 = 13 km, and H2 = 13 km; the total crustal thickness is 27 km.","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Reston, VA","doi":"10.3133/70043887","collaboration":"In cooperation with the Defense Advanced Research Projects Agency","usgsCitation":"Gibbs, J., and Roller, J., 1964, Seismic-refraction measurements of crustal structure between Nevada Test Site and Ludlow, California: Crustal Studies Technical Letter 26, iii, 30 p., https://doi.org/10.3133/70043887.","productDescription":"iii, 30 p.","additionalOnlineFiles":"N","costCenters":[{"id":237,"text":"Earthquake Science Center","active":true,"usgs":true},{"id":379,"text":"Menlo Park Science Center","active":false,"usgs":true}],"links":[{"id":268196,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":268194,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/misc/tl/0026/tl0026.pdf"},{"id":268195,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.usgs.gov/misc/tl/0026/"}],"state":"Arizona;California;Nevada","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -116.9975,32.4982 ], [ -116.9975,36.0013 ], [ 114.5009,36.0013 ], [ 114.5009,32.4982 ], [ -116.9975,32.4982 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"512c9621e4b0855fde669816","contributors":{"authors":[{"text":"Gibbs, J. F.","contributorId":50894,"corporation":false,"usgs":true,"family":"Gibbs","given":"J. 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1 Map; 1 Illustration, https://doi.org/10.3133/tei834.","productDescription":"Report: 32 p.; 1 Map; 1 Illustration","costCenters":[],"links":[{"id":290299,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"}],"country":"United States","state":"Nevada","county":"Nye County","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -118.1972,35.9618 ], [ -118.1972,39.1634 ], [ -114.999,39.1634 ], [ -114.999,35.9618 ], [ -118.1972,35.9618 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"53c79efee4b0194841642469","contributors":{"authors":[{"text":"Hasler, J.W.","contributorId":40275,"corporation":false,"usgs":true,"family":"Hasler","given":"J.W.","email":"","affiliations":[],"preferred":false,"id":284754,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":70039486,"text":"70039486 - 1963 - Traveltimes and amplitudes from nuclear explosions; Nevada Test Site to Ordway, Colorado","interactions":[],"lastModifiedDate":"2012-08-08T01:02:14","indexId":"70039486","displayToPublicDate":"2012-01-01T14:27:14","publicationYear":"1963","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":6,"text":"USGS Unnumbered Series"},"seriesTitle":{"id":355,"text":"Crustal Studies Technical Letter","active":false,"publicationSubtype":{"id":6}},"seriesNumber":"10","title":"Traveltimes and amplitudes from nuclear explosions; Nevada Test Site to Ordway, Colorado","docAbstract":"This paper treats the results of a study of seismic waves generated by eight nuclear explosions and recorded at 31 locations between the Nevada Test Site (NTS) and Ordway, Colorado. The line of recording stations crosses the eastern part of the Basin and Range Province, the Colorado Plateau, the southern Rocky Mountains, and extends into the Great Plains. In the eastern Basin and Range Province and the western margin of the Colorado Plateau (0 ≤ Δ ≤ 385 km ), the time-distance curves for Pg and Pn can be expressed, respectively, as T1 = 0.8 + Δ/6.0. T3 = 5.8 + Δ/7.6. A third phase, tentatively identified as P*, is represented by the equation T2 = 3.8 + Δ/6.5. Using the crustal structure and Pn velocity (7.9 km/ sec) found for the NTS region by other authors, these relations indicate that the thickness of the crust increases from about 25 km at NTS to about 42 km in the western part of the Colorado Plateau Province. East of this boundary the velocity of P in the upper mantle increases to 8.0 km/sec; depth to the Mohorovicic discontinuity is approximately constant over the range 435 ≤ Δ ≤ 645 km. Beyond 850 km, first arrivals indicate an apparent velocity of about 8.4 km/sec. Amplitudes of Pn attenuate according to the equation A = Ao Δ-1/2(Δ -d)-3/2 e-0.0022Δ over the distance range 150 ≤ Δ ≤ 850 km. This relation yields a value of Q, for Pn of about 520. The amplitudes of Pg attenuates extremely rapidly, and beyond about 130 km this phase cannot be identified with certainty. An extension of the Pg traveltime branch at large distances could be associated with waves reflected beyond the critical angle, from the base of the crust. This phase, called ?P after Mohorovicic, appears to attenuate as A = Ao e-0.076Δ Δ-1/2. The value of Q indicated by this equation is about 200.","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Reston, VA","doi":"10.3133/70039486","collaboration":"In cooperation with the Defense Advanced Research Projects Agency","usgsCitation":"Ryall, A., and Stuart, D., 1963, Traveltimes and amplitudes from nuclear explosions; Nevada Test Site to Ordway, Colorado: Crustal Studies Technical Letter 10, ill.; map, https://doi.org/10.3133/70039486.","productDescription":"ill.; map","startPage":"1","endPage":"41","numberOfPages":"45","onlineOnly":"Y","additionalOnlineFiles":"N","costCenters":[{"id":237,"text":"Earthquake Science Center","active":true,"usgs":true}],"links":[{"id":259490,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":259481,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/misc/tl/0010/tl0010.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":259480,"rank":100,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.usgs.gov/misc/tl/0010/","linkFileType":{"id":5,"text":"html"}}],"country":"United States","state":"Nevada;Colorado","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"505bb78ae4b08c986b327327","contributors":{"authors":[{"text":"Ryall, Alan","contributorId":16263,"corporation":false,"usgs":true,"family":"Ryall","given":"Alan","email":"","affiliations":[],"preferred":false,"id":466351,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Stuart, David J.","contributorId":25807,"corporation":false,"usgs":true,"family":"Stuart","given":"David J.","affiliations":[],"preferred":false,"id":466352,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":72458,"text":"tei842 - 1963 - Outline of the geology of the U12i and U12i.01 tunnels and lithology of the U12i.01 drill hole, Nevada test site","interactions":[],"lastModifiedDate":"2012-02-02T00:14:01","indexId":"tei842","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1963","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":"842","title":"Outline of the geology of the U12i and U12i.01 tunnels and lithology of the U12i.01 drill hole, Nevada test site","language":"ENGLISH","doi":"10.3133/tei842","usgsCitation":"Bowers, W., 1963, Outline of the geology of the U12i and U12i.01 tunnels and lithology of the U12i.01 drill hole, Nevada test site: U.S. Geological Survey Trace Elements Investigations 842, 24 p., 4 fig. [3 missing], https://doi.org/10.3133/tei842.","productDescription":"24 p., 4 fig. 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