This report lists the geochemical data collected during the course of a reconnaissance study of compositional variation in the bedrock and surficial gelogic untis exposed in Missouri and adjoining parts of Kansas, Oklahoma, and Arkansas. The primar object of the study was to assess scale-related components of geochemical variance with a view of determining the importance of regional geochemical variation in these units (cf. Connor and other, 1972). Geologic evaluation, geochemical interpretation and summaries, and sampling designs employed in the collection of most of these data may be found in U.S. Geological Survey (1972a-1972f, 1973) and Connor and Shacklette (1975).
","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr75137","usgsCitation":"Boerngen, J.G., Van Trump, G., and Ebens, R.J., 1975, Analytical data for geologic units in Missouri and parts of Kansas, Oklahoma and Arkansas: U.S. Geological Survey Open-File Report 75-137, ii, 276 p., https://doi.org/10.3133/ofr75137.","productDescription":"ii, 276 p.","numberOfPages":"282","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[],"links":[{"id":143961,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/ofr75137.jpg"},{"id":318179,"rank":1,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1975/0137/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"country":"United States","state":"Arkansas, Kansas, Missouri, Oklahoma","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4acfe4b07f02db67ff7c","contributors":{"authors":[{"text":"Boerngen, Josephine G.","contributorId":31750,"corporation":false,"usgs":true,"family":"Boerngen","given":"Josephine","email":"","middleInitial":"G.","affiliations":[],"preferred":false,"id":166595,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Van Trump, George","contributorId":19156,"corporation":false,"usgs":true,"family":"Van Trump","given":"George","email":"","affiliations":[],"preferred":false,"id":166593,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Ebens, Richard J.","contributorId":22335,"corporation":false,"usgs":true,"family":"Ebens","given":"Richard","email":"","middleInitial":"J.","affiliations":[],"preferred":false,"id":166594,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}} ,{"id":60467,"text":"mf713 - 1975 - Geologic map of the Spring Hill Creek Quadrangle, Saguache County, Colorado","interactions":[],"lastModifiedDate":"2012-02-10T00:10:25","indexId":"mf713","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1975","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":325,"text":"Miscellaneous Field Studies Map","code":"MF","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"713","title":"Geologic map of the Spring Hill Creek Quadrangle, Saguache County, Colorado","language":"ENGLISH","doi":"10.3133/mf713","usgsCitation":"Olson, J.C., Steven, T.A., and Hedlund, D.C., 1975, Geologic map of the Spring Hill Creek Quadrangle, Saguache County, Colorado: U.S. Geological Survey Miscellaneous Field Studies Map 713, 1 map ;57 x 45 cm. folded to 18 x 27 cm. in envelope 30 x 24 cm., https://doi.org/10.3133/mf713.","productDescription":"1 map ;57 x 45 cm. folded to 18 x 27 cm. in envelope 30 x 24 cm.","costCenters":[],"links":[{"id":104236,"rank":700,"type":{"id":15,"text":"Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_3850.htm","linkFileType":{"id":5,"text":"html"},"description":"3850"},{"id":183830,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"}],"scale":"0","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -107,38.25 ], [ -107,38.3675 ], [ -106.86749999999999,38.3675 ], [ -106.86749999999999,38.25 ], [ -107,38.25 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ae5e4b07f02db68a64a","contributors":{"authors":[{"text":"Olson, J. C.","contributorId":55403,"corporation":false,"usgs":true,"family":"Olson","given":"J.","middleInitial":"C.","affiliations":[],"preferred":false,"id":263802,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Steven, T. A.","contributorId":42575,"corporation":false,"usgs":true,"family":"Steven","given":"T.","middleInitial":"A.","affiliations":[],"preferred":false,"id":263801,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Hedlund, D. C.","contributorId":101624,"corporation":false,"usgs":true,"family":"Hedlund","given":"D.","email":"","middleInitial":"C.","affiliations":[],"preferred":false,"id":263803,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}} ,{"id":12749,"text":"ofr75141 - 1975 - A summary of relative ages of lunar nearside and farside plains","interactions":[],"lastModifiedDate":"2025-03-28T16:56:26.02245","indexId":"ofr75141","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1975","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":"75-141","title":"A summary of relative ages of lunar nearside and farside plains","docAbstract":"This report contains a summary of the moon-wide distribution of relative ages of lunar plains units determined with Apollo and Lunar Orbiter photographs. Relative ages are expressed as the largest diameter of craters (DL, meters) in a mappable unit that are eroded to a slope of 1° by the net accumulated flux of small impacts. New data show that the technique used here generally requires a sample area less than 2,000 km2 for satisfactory results. Additionally, the measurement of relative age (DL) using this technique is unaffected by resolutions of about 0.15 DL or smaller.
Results obtained indicate there are two types of plains: 1) light plains and 2) mare plains. The light plains units have two separate and distinct ages (DL ≃ 550 m and D ≃ 1100 m). The range in ages for each of these units is so small that each could represent two separate synchronous lunar events. The maria were deposited in three major stages after the emplacement of the light plains units. The oldest mare units ( > 3.7 b.y. old) are in Mare Tranquillitatis, Mare Vaporum, southeastern Mare Imbrium, the dark ring around Mare Serenitatis and a thin band from the crater Reinhold to Sinus Medii. Young mare volcanism ( < 2.5 b.y. old) occurred in western Mare Serenitatis, southwestern Mare Imbrium and Oceanus Procellarum. All other mare areas investigated are of intermediate age.
","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr75141","usgsCitation":"Boyce, J.M., Dial, A., and Soderblom, L.A., 1975, A summary of relative ages of lunar nearside and farside plains: U.S. Geological Survey Open-File Report 75-141, Report: ii, 26 p.; 3 Plates: 47.79 x 28.71 inches or smaller, https://doi.org/10.3133/ofr75141.","productDescription":"Report: ii, 26 p.; 3 Plates: 47.79 x 28.71 inches or smaller","costCenters":[],"links":[{"id":420743,"rank":5,"type":{"id":29,"text":"Figure"},"url":"https://pubs.usgs.gov/of/1975/0141/figure-5.pdf","text":"Figure 5","linkFileType":{"id":1,"text":"pdf"}},{"id":420742,"rank":4,"type":{"id":29,"text":"Figure"},"url":"https://pubs.usgs.gov/of/1975/0141/figure-6.pdf","text":"Figure 6","linkFileType":{"id":1,"text":"pdf"}},{"id":420741,"rank":3,"type":{"id":29,"text":"Figure"},"url":"https://pubs.usgs.gov/of/1975/0141/figure-7.pdf","text":"Figure 7","linkFileType":{"id":1,"text":"pdf"}},{"id":420740,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1975/0141/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":144956,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1975/0141/report-thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b02e4b07f02db698b8d","contributors":{"authors":[{"text":"Boyce, Joseph M.","contributorId":52963,"corporation":false,"usgs":true,"family":"Boyce","given":"Joseph","email":"","middleInitial":"M.","affiliations":[],"preferred":false,"id":166645,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Dial, Arthur L.","contributorId":66686,"corporation":false,"usgs":true,"family":"Dial","given":"Arthur L.","affiliations":[],"preferred":false,"id":166646,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Soderblom, Laurence A. 0000-0002-0917-853X lsoderblom@usgs.gov","orcid":"https://orcid.org/0000-0002-0917-853X","contributorId":2721,"corporation":false,"usgs":true,"family":"Soderblom","given":"Laurence","email":"lsoderblom@usgs.gov","middleInitial":"A.","affiliations":[{"id":131,"text":"Astrogeology Science Center","active":true,"usgs":true}],"preferred":true,"id":166644,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}} ,{"id":60513,"text":"mf652 - 1975 - Geologic map of the San Andreas fault zone in San Andreas Lake, San Mateo County, California","interactions":[],"lastModifiedDate":"2012-02-10T00:10:23","indexId":"mf652","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1975","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":325,"text":"Miscellaneous Field Studies Map","code":"MF","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"652","title":"Geologic map of the San Andreas fault zone in San Andreas Lake, San Mateo County, California","language":"ENGLISH","doi":"10.3133/mf652","usgsCitation":"Pampeyan, E., 1975, Geologic map of the San Andreas fault zone in San Andreas Lake, San Mateo County, California: U.S. Geological Survey Miscellaneous Field Studies Map 652, 1 map ;78 x 17 cm., https://doi.org/10.3133/mf652.","productDescription":"1 map ;78 x 17 cm.","costCenters":[],"links":[{"id":104211,"rank":700,"type":{"id":15,"text":"Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_3768.htm","linkFileType":{"id":5,"text":"html"},"description":"3768"},{"id":183220,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"}],"scale":"0","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -123,37.5 ], [ -123,38.25 ], [ -122,38.25 ], [ -122,37.5 ], [ -123,37.5 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a28e4b07f02db61144f","contributors":{"authors":[{"text":"Pampeyan, E. H.","contributorId":14493,"corporation":false,"usgs":true,"family":"Pampeyan","given":"E. H.","affiliations":[],"preferred":false,"id":263893,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":12741,"text":"ofr7567 - 1975 - Reconnaissance study of sediment transport by selected streams in the Yakima Indian Reservation, Washington, 1974 water year","interactions":[],"lastModifiedDate":"2012-02-02T00:06:35","indexId":"ofr7567","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1975","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":"75-67","title":"Reconnaissance study of sediment transport by selected streams in the Yakima Indian Reservation, Washington, 1974 water year","docAbstract":"This was a reconnaissance study for information on suspended-sediment concentrations and basin yields at 21 sites on selected streams in the Yakima Indian Reservation in Washington, and two sites on nearby streams. Suspended-sediment yields were generally low relative to those indicated by data for other streams on southeastern Washington, the southern Cascade Range, and the upper Columbia River basin. The highest long-term sediment yield on the reservation probably is from the Big Muddy Creek basin; the estimated annual yield is about 150 tons per square mile. The suspended sediment transported by this stream is largely from glacial outwash from Mount Adams. Other yields in the basin were estimated to be from 10 to 50 tons per square mile. Mass wasting is considered the principal cause of sediment transport in the streams studied. Some evidence of accelerated sediment production due to road construction was found along Surveyor Creek.\r\n\r\nDuring the flood of January 1974, which has a calculated recurrence interval of more than 100 years, the maximum observed suspended-sediment concentration was 7,830 milligrams per litre, in the North Fork Simcoe Creek. During that flood, an estimated 70,000 tons of sediment was transported from the upper Toppenish Creek basin; this was nearly 600 tons per square mile. However, the long-term average annual yield was estimated to be only about 30 tons per square mile.","language":"ENGLISH","publisher":"[s.n.],","doi":"10.3133/ofr7567","usgsCitation":"Boucher, P.R., 1975, Reconnaissance study of sediment transport by selected streams in the Yakima Indian Reservation, Washington, 1974 water year: U.S. Geological Survey Open-File Report 75-67, iii, 12 leaves :map (folded) ;28 cm.; (20 p. - PGS), https://doi.org/10.3133/ofr7567.","productDescription":"iii, 12 leaves :map (folded) ;28 cm.; (20 p. - PGS)","costCenters":[],"links":[{"id":144746,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1975/0067/report-thumb.jpg"},{"id":41146,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1975/0067/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a62e4b07f02db636279","contributors":{"authors":[{"text":"Boucher, Philip Richard","contributorId":106907,"corporation":false,"usgs":true,"family":"Boucher","given":"Philip","email":"","middleInitial":"Richard","affiliations":[],"preferred":false,"id":166631,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":12737,"text":"ofr75180 - 1975 - Prediction of maximum earthquake intensities for the San Francisco Bay region","interactions":[],"lastModifiedDate":"2012-02-02T00:06:39","indexId":"ofr75180","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1975","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":"75-180","title":"Prediction of maximum earthquake intensities for the San Francisco Bay region","docAbstract":"The intensity data for the California earthquake of April 18, 1906, are strongly dependent on distance from the zone of surface faulting and the geological character of the ground. Considering only those sites (approximately one square city block in size) for which there is good evidence for the degree of ascribed intensity, the empirical relation derived between 1906 intensities and distance perpendicular to the fault for 917 sites underlain by rocks of the Franciscan Formation is: Intensity = 2.69 - 1.90 log (Distance) (km).\r\n\r\nFor sites on other geologic units intensity increments, derived with respect to this empirical relation, correlate strongly with the Average Horizontal Spectral Amplifications (AHSA) determined from 99 three-component recordings of ground motion generated by nuclear explosions in Nevada. The resulting empirical relation is: Intensity Increment = 0.27 +2.70 log (AHSA), and average intensity increments for the various geologic units are -0.29 for granite, 0.19 for Franciscan Formation, 0.64 for the Great Valley Sequence, 0.82 for Santa Clara Formation, 1.34 for alluvium, 2.43 for bay mud. The maximum intensity map predicted from these empirical relations delineates areas in the San Francisco Bay region of potentially high intensity from future earthquakes on either the San Andreas fault or the Hazard fault.","language":"ENGLISH","publisher":"U.S. Dept. of the Interior, Geological Survey, National Center for Earthquake Research,","doi":"10.3133/ofr75180","usgsCitation":"Borcherdt, R.D., and Gibbs, J., 1975, Prediction of maximum earthquake intensities for the San Francisco Bay region: U.S. Geological Survey Open-File Report 75-180, 25 leaves, 2 sheets, :ill., maps (2 fold. in pocket) ;27 cm., https://doi.org/10.3133/ofr75180.","productDescription":"25 leaves, 2 sheets, :ill., maps (2 fold. in pocket) ;27 cm.","costCenters":[],"links":[{"id":145559,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1975/0180/report-thumb.jpg"},{"id":41142,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1975/0180/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":41143,"rank":401,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1975/0180/plate-2.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":41144,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1975/0180/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b07e4b07f02db69add7","contributors":{"authors":[{"text":"Borcherdt, Roger D. 0000-0002-8668-0849 borcherdt@usgs.gov","orcid":"https://orcid.org/0000-0002-8668-0849","contributorId":2373,"corporation":false,"usgs":true,"family":"Borcherdt","given":"Roger","email":"borcherdt@usgs.gov","middleInitial":"D.","affiliations":[{"id":237,"text":"Earthquake Science Center","active":true,"usgs":true}],"preferred":true,"id":166623,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Gibbs, James F.","contributorId":95880,"corporation":false,"usgs":true,"family":"Gibbs","given":"James F.","affiliations":[],"preferred":false,"id":166624,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":12731,"text":"ofr7541 - 1975 - A review of recently active faults in Taiwan","interactions":[],"lastModifiedDate":"2018-06-21T13:19:34","indexId":"ofr7541","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1975","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":"75-41","title":"A review of recently active faults in Taiwan","docAbstract":"Six faults associated with five large earthquakes produced surface displacements ranging from 1 to 3 m in the period 1906 through 1951. Four of the ruptures occurred in the western coastal plain and foothills, and two occurred in the Longitudinal Valley of eastern Taiwan. Maps are included showing the locations and dimensions of the displacements. The published geological literature probably would not lead one to infer the existence of a fault along most of the 1906 rupture, except for descriptions of the rupture itself. Over most of its length the 1935 rupture on the Chihhu fault is parallel to but more than 0.5 km from nearby faults shown on geologic maps published in 1969 and 1971; only about 1.5 km of its 15 km length coincides with a mapped fault. The coastal plain part of the Tuntzuchio fault which ruptured in 1935 is apparently not revealed by landforms, and only suggested by other data. Part of the 1946 Hsinhua faulting coincides with a fault identified in the subsurface by seismic work but surface indications of the fault are obscure. The 1951 Meilun faulting occurred along a conspicuous pre-1951 scarp and the 1951 Yuli faulting occurred near or in line with pre-1951 scarps. \r\nMore than 40 faults which, according to the published literature, have had Pleistocene or later movement are shown on a small-scale map. Most of these faults are in the densely-populated western part of Taiwan. The map and text calls attention to faults that may be active and therefore may be significant in planning important structures. \r\n\r\nEquivocal evidence suggestive of fault creep was found on the Yuli fault and the Hsinhua fault. Fault creep was not found at several places examined along the 1906 fault trace. \r\n\r\nTectonic uplift has occurred in Taiwan in the last 10,000 years and application of eustatic sea level curves to published radiocarbon dates shows that the minimum rate of uplift is considerably different in different parts of the island. Incomplete data indicate that the rate is high near Hualien, where an uplift of at least 0.6 m and probably more than 1 m occurred in the 1951 earthquake, and near and south of the 1946 faulting. Sudden uplifts can have serious consequences for installations near the shore. Investigation of this process, study of recently active faults, and continuing study of seismicity are necessary parts of a practical earthquake-hazard reduction program.","language":"English","publisher":"U.S. Geological Survey,","publisherLocation":"Reston, VA","doi":"10.3133/ofr7541","usgsCitation":"Bonilla, M.G., 1975, A review of recently active faults in Taiwan (Version 1.1): U.S. Geological Survey Open-File Report 75-41, 43 p., https://doi.org/10.3133/ofr7541.","productDescription":"43 p.","costCenters":[{"id":312,"text":"Geology, Minerals, Energy, and Geophysics Science Center","active":true,"usgs":true}],"links":[{"id":145535,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":976,"rank":100,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.usgs.gov/of/1975/of75-41/","linkFileType":{"id":5,"text":"html"}}],"edition":"Version 1.1","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b19e4b07f02db6a7fa4","contributors":{"authors":[{"text":"Bonilla, Manuel G.","contributorId":74384,"corporation":false,"usgs":true,"family":"Bonilla","given":"Manuel","email":"","middleInitial":"G.","affiliations":[],"preferred":false,"id":166615,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":60485,"text":"mf645A - 1975 - Map showing unconsolidated materials, Marlborough quadrangle, Connecticut","interactions":[],"lastModifiedDate":"2022-04-08T20:27:28.667291","indexId":"mf645A","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1975","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":325,"text":"Miscellaneous Field Studies Map","code":"MF","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"645","chapter":"A","title":"Map showing unconsolidated materials, Marlborough quadrangle, Connecticut","docAbstract":"No abstract available.
","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/mf645A","usgsCitation":"O’Leary, D.W., 1975, Map showing unconsolidated materials, Marlborough quadrangle, Connecticut: U.S. Geological Survey Miscellaneous Field Studies Map 645, 1 Plate:22.94 × 34.00 inches, https://doi.org/10.3133/mf645A.","productDescription":"1 Plate:22.94 × 34.00 inches","costCenters":[],"links":[{"id":398423,"rank":3,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_3762.htm"},{"id":274666,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/mf/0645a/plate-1.pdf"},{"id":183302,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"}],"scale":"24000","country":"United States","state":"Connecticut","otherGeospatial":"Marlborough quadrangle","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"type\": \"Polygon\",\n \"coordinates\": [\n [\n [\n -72.5,\n 41.625\n ],\n [\n -72.375,\n 41.625\n ],\n [\n -72.375,\n 41.75\n ],\n [\n -72.5,\n 41.75\n ],\n [\n -72.5,\n 41.625\n ]\n ]\n ]\n }\n }\n ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b0de4b07f02db69f181","contributors":{"authors":[{"text":"O’Leary, Dennis W.","contributorId":91501,"corporation":false,"usgs":true,"family":"O’Leary","given":"Dennis","email":"","middleInitial":"W.","affiliations":[],"preferred":false,"id":263835,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":16368,"text":"ofr7544 - 1975 - Water resources information needs for the St. Johns River Water Management District","interactions":[],"lastModifiedDate":"2012-02-02T00:07:02","indexId":"ofr7544","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1975","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":"75-44","title":"Water resources information needs for the St. Johns River Water Management District","language":"ENGLISH","publisher":"[s.n.],","doi":"10.3133/ofr7544","usgsCitation":"Vanlier, K.E., 1975, Water resources information needs for the St. Johns River Water Management District: U.S. Geological Survey Open-File Report 75-44, 83 leaves :ill., map (some folded) ;28 cm.; 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","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr75110","usgsCitation":"Van Trump, G., and Pitman, J.K., 1975, Computer program designed to compute oil shale thickness (ft.), average value (gal. per ton), and resource (barrels per acre) from Fischer assay data: U.S. Geological Survey Open-File Report 75-110, 18 p., https://doi.org/10.3133/ofr75110.","productDescription":"18 p.","costCenters":[],"links":[{"id":420667,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1975/0110/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":147638,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1975/0110/report-thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b19e4b07f02db6a793f","contributors":{"authors":[{"text":"Van Trump, George","contributorId":19156,"corporation":false,"usgs":true,"family":"Van Trump","given":"George","email":"","affiliations":[],"preferred":false,"id":172730,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Pitman, Janet K. 0000-0002-0441-779X jpitman@usgs.gov","orcid":"https://orcid.org/0000-0002-0441-779X","contributorId":767,"corporation":false,"usgs":true,"family":"Pitman","given":"Janet","email":"jpitman@usgs.gov","middleInitial":"K.","affiliations":[{"id":241,"text":"Eastern Energy Resources Science Center","active":true,"usgs":true},{"id":164,"text":"Central Energy Resources Science Center","active":true,"usgs":true}],"preferred":true,"id":172729,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":16362,"text":"ofr7564 - 1975 - Self-calibrating seismic amplifier and telemetry system","interactions":[],"lastModifiedDate":"2019-04-30T14:40:54","indexId":"ofr7564","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1975","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":"75-64","title":"Self-calibrating seismic amplifier and telemetry system","docAbstract":"A frequency modulated, constant bandwidth, telemetry system has been designed to transmit simultaneously up to 8 channels of seismograph data from remote locations to a central recording site via radio or voice-grade telephone circuit. By utilizing state-of-the-art integrated circuits, the size of the remote unit has been considerably reduced over previous equipment and the power consumption has been decreased by a factor of over 100 to less than 2 milliwatts. This reduction in size and power makes it possible to package the electronic equipment, together with a year's supply of batteries, in a container the size of a tennis-ball can. The field equipment for a short-period station is now sealed in a 3-inch plastic tube 22 inches long . The tube, together with the connecting cable to the telephone terminal, is buried; greatly reducing losses due to water flooding, pilferage, etc. An important addition to the field unit is a daily calibration of the seismometer and amplifier.
Specifications and instructions for the three units that compose the system are presented separately, as follows:
1. J302 Preamplifier and voltage controlled oscillator
2. C-4 Calibrator
3. J101 Discriminator
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Although this program has been tested by its contributor, no warranty, expressed or implied, is made by the contributor or the Government, as to the functioning of the program and related program material, nor shall the fact of distribution constitute any such warranty, and no responsibility is assumed by the contributor or the Government, in connection therewith.
The FORTRAN IV program listing (table 1) defines the constants and variables necessary for understanding the mechanics and the output from the program.
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","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr75136","usgsCitation":"Deutsch, M., 1975, East Africa seminar and workshop of remote sensing of natural resources and environment: U.S. Geological Survey Open-File Report 75-136, v, 59 p., https://doi.org/10.3133/ofr75136.","productDescription":"v, 59 p.","numberOfPages":"211","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[],"links":[{"id":147234,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/ofr75136.jpg"},{"id":316468,"rank":1,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1975/0136/report.pdf"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a50e4b07f02db628f9a","contributors":{"authors":[{"text":"Deutsch, Morris","contributorId":69119,"corporation":false,"usgs":true,"family":"Deutsch","given":"Morris","email":"","affiliations":[],"preferred":false,"id":167627,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":13349,"text":"ofr7524 - 1975 - Predicted double-couple S-polarization angles","interactions":[],"lastModifiedDate":"2024-06-07T18:43:44.228096","indexId":"ofr7524","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1975","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":"75-24","title":"Predicted double-couple S-polarization angles","docAbstract":"The main purpose of this paper is to provide a graphical procedure with which to evaluate the orientation of an earthquake source using S-polarization angles. Background material is presented on the use of S-polarization angles, including the necessary material for the use of the catalog and the manner of its construction. A family of plots of theoretically predicted S-polarization angles is presented. There are 162 different diagrams in this catalog which may be used to determine the orientation of the focal planes of an earthquake to within about 5 degrees of the orientation of either plane.
","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr7524","usgsCitation":"Dillinger, W., 1975, Predicted double-couple S-polarization angles: U.S. Geological Survey Open-File Report 75-24, i, 193 p., https://doi.org/10.3133/ofr7524.","productDescription":"i, 193 p.","costCenters":[],"links":[{"id":429675,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1975/0024/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":147518,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1975/0024/report-thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4acce4b07f02db67ea36","contributors":{"authors":[{"text":"Dillinger, W.H.","contributorId":95489,"corporation":false,"usgs":true,"family":"Dillinger","given":"W.H.","email":"","affiliations":[],"preferred":false,"id":167663,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":13460,"text":"ofr7595 - 1975 - Harmonic magnification of the complete telemetered seismic system, from seismometer to film viewer screen","interactions":[],"lastModifiedDate":"2017-06-18T21:47:18","indexId":"ofr7595","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1975","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":"75-95","title":"Harmonic magnification of the complete telemetered seismic system, from seismometer to film viewer screen","docAbstract":"A collection of notes on the standardization, adjustment, and calibration of the seismic systems employed in the USGS central California microearthquake network (compiled 9/15/70; revised 8/20/73) \r\n","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr7595","usgsCitation":"Eaton, J.P., 1975, Harmonic magnification of the complete telemetered seismic system, from seismometer to film viewer screen: U.S. Geological Survey Open-File Report 75-95, 1 v. 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