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","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/i532C","usgsCitation":"Carlson, J.E., and Willden, R., 1968, Transcontinental geophysical survey (35°-39° N) geologic map from 112° W longitude to the coast of California: U.S. Geological Survey IMAP 532, 1 Plate: 54.82 × 27.28 inches, https://doi.org/10.3133/i532C.","productDescription":"1 Plate: 54.82 × 27.28 inches","costCenters":[],"links":[{"id":390632,"rank":4,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_1722.htm"},{"id":255260,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/imap/0532c/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":255259,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/imap/0532c/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":255261,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/imap/0532c/report-thumb.jpg"}],"scale":"1000000","country":"United States","state":"Arizona, California, Nevada, Utah","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -124,35 ], [ -124,39 ], [ -112,39 ], [ -112,35 ], [ -124,35 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a4de4b07f02db627030","contributors":{"authors":[{"text":"Carlson, J. E.","contributorId":83939,"corporation":false,"usgs":true,"family":"Carlson","given":"J.","email":"","middleInitial":"E.","affiliations":[],"preferred":false,"id":272302,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Willden, Ronald","contributorId":107368,"corporation":false,"usgs":true,"family":"Willden","given":"Ronald","affiliations":[],"preferred":false,"id":272303,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":64877,"text":"i533C - 1968 - Transcontinental geophysical survey (35°-39° N) geologic map from 100° to 112° W longitude","interactions":[],"lastModifiedDate":"2021-10-18T18:11:33.703819","indexId":"i533C","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1968","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":320,"text":"IMAP","code":"I","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"533","chapter":"C","title":"Transcontinental geophysical survey (35°-39° N) geologic map from 100° to 112° W longitude","docAbstract":"No abstract available.
","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/i533C","usgsCitation":"Carlson, J.E., and Willden, R., 1968, Transcontinental geophysical survey (35°-39° N) geologic map from 100° to 112° W longitude: U.S. Geological Survey IMAP 533, 1 Plate: 52.46 × 27.26 inches, https://doi.org/10.3133/i533C.","productDescription":"1 Plate: 52.46 × 27.26 inches","costCenters":[],"links":[{"id":390611,"rank":4,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_1721.htm"},{"id":255258,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/imap/0533c/report-thumb.jpg"},{"id":255257,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/imap/0533c/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":255256,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/imap/0533c/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}}],"scale":"1000000","country":"United States","state":"Arizona, Colorado, Kansas, New Mexico, Oklahoma, Texas, Utah","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -112,35 ], [ -112,39 ], [ -100,39 ], [ -100,35 ], [ -112,35 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a4de4b07f02db626ffb","contributors":{"authors":[{"text":"Carlson, J. E.","contributorId":83939,"corporation":false,"usgs":true,"family":"Carlson","given":"J.","email":"","middleInitial":"E.","affiliations":[],"preferred":false,"id":272300,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Willden, Ronald","contributorId":107368,"corporation":false,"usgs":true,"family":"Willden","given":"Ronald","affiliations":[],"preferred":false,"id":272301,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":63927,"text":"gp637 - 1968 - Aeromagnetic map of the Hot Creek Range region, south-central Nevada","interactions":[],"lastModifiedDate":"2022-09-30T20:59:50.401533","indexId":"gp637","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1968","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":317,"text":"Geophysical Investigations Map","code":"GP","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"637","title":"Aeromagnetic map of the Hot Creek Range region, south-central Nevada","docAbstract":"No abstract available.
","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/gp637","usgsCitation":"Water Resources Division, U.S. Geological Survey, 1968, Aeromagnetic map of the Hot Creek Range region, south-central Nevada: U.S. Geological Survey Geophysical Investigations Map 637, Report; 1 p.; 1 Plate: 26.47 × 35.54 inches, https://doi.org/10.3133/gp637.","productDescription":"Report; 1 p.; 1 Plate: 26.47 × 35.54 inches","costCenters":[],"links":[{"id":250259,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/gp/0637/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":253778,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/gp/0637/report-thumb.jpg"},{"id":250260,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/gp/0637/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":407744,"rank":4,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_6004.htm","linkFileType":{"id":5,"text":"html"}}],"scale":"250000","country":"United States","state":"Nevada","otherGeospatial":"Hot Creek Range","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"type\": \"Polygon\",\n \"coordinates\": [\n [\n [\n -117,\n 37.75\n ],\n [\n -115.5,\n 37.75\n ],\n [\n -115.5,\n 39.5\n ],\n [\n -117,\n 39.5\n ],\n [\n -117,\n 37.75\n ]\n ]\n ]\n }\n }\n ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4af4e4b07f02db69216c","contributors":{"authors":[{"text":"Water Resources Division, U.S. Geological Survey","contributorId":128075,"corporation":true,"usgs":false,"organization":"Water Resources Division, U.S. Geological Survey","id":533396,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":41046,"text":"ofr68312 - 1968 - Piezometric surface of principal artesian aquifer in coastal area of Georgia, December 1966","interactions":[],"lastModifiedDate":"2022-05-18T16:05:30.110937","indexId":"ofr68312","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1968","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":"68-312","title":"Piezometric surface of principal artesian aquifer in coastal area of Georgia, December 1966","docAbstract":"No abstract available.
","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr68312","collaboration":"Prepared in cooperation with the Georgia Department of Mines, Mining and Geology, Chatham County, City of Savannah, Glynn County, and City of Brunswick","usgsCitation":"Wait, R.L., and Gregg, D.O., 1968, Piezometric surface of principal artesian aquifer in coastal area of Georgia, December 1966: U.S. Geological Survey Open-File Report 68-312, 1 Plate: 32.71 x 48.62 inches, https://doi.org/10.3133/ofr68312.","productDescription":"1 Plate: 32.71 x 48.62 inches","costCenters":[{"id":13634,"text":"South Atlantic Water Science Center","active":true,"usgs":true}],"links":[{"id":135273,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1968/0312/report-thumb.jpg"},{"id":400712,"rank":2,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1968/0312/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}}],"country":"United States","state":"Georgia","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"type\": \"Polygon\",\n \"coordinates\": [\n [\n [\n -81.6064453125,\n 30.675715404167743\n ],\n [\n -80.85937499999999,\n 30.675715404167743\n ],\n [\n -80.85937499999999,\n 32.43561304116276\n ],\n [\n -81.6064453125,\n 32.43561304116276\n ],\n [\n -81.6064453125,\n 30.675715404167743\n ]\n ]\n ]\n }\n }\n ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4adae4b07f02db68589c","contributors":{"authors":[{"text":"Wait, R. L.","contributorId":15988,"corporation":false,"usgs":true,"family":"Wait","given":"R.","email":"","middleInitial":"L.","affiliations":[],"preferred":false,"id":224381,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Gregg, D. 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","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr68184","usgsCitation":"Moench, R.H., 1968, Geologic maps, structure sections, and fence diagrams of Rangeley and Phillips quadrangles, Franklin and Oxford Counties, Maine, and heavy metals content of stream sediment samples from the Rangeley and parts of the Phillips and Rumford quadrangles, Maine: U.S. Geological Survey Open-File Report 68-184, 7 Plates: 17.00 × 36.00 inches or smaller, https://doi.org/10.3133/ofr68184.","productDescription":"7 Plates: 17.00 × 36.00 inches or smaller","costCenters":[],"links":[{"id":169316,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":398155,"rank":9,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_8265.htm"},{"id":99081,"rank":402,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1968/0184/plate-4.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":99084,"rank":405,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1968/0184/plate-7.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":99083,"rank":404,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1968/0184/plate-6.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":99082,"rank":403,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1968/0184/plate-5.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":99079,"rank":401,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1968/0184/plate-2.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":99078,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1968/0184/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":99080,"rank":401,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1968/0184/plate-3.pdf","linkFileType":{"id":1,"text":"pdf"}}],"scale":"62500","country":"United States","state":"Maine","county":"Franklin County, Oxford County","otherGeospatial":"Rangeley, Phillips, and Rumford quadrangles","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"type\": \"Polygon\",\n \"coordinates\": [\n [\n [\n -70.75,\n 44.625\n ],\n [\n -70.25,\n 44.625\n ],\n [\n -70.25,\n 45\n ],\n [\n -70.75,\n 45\n ],\n [\n -70.75,\n 44.625\n ]\n ]\n ]\n }\n }\n ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ae0e4b07f02db68853e","contributors":{"authors":[{"text":"Moench, R. 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The deposits in this channel were the site of some of the most productive hydraulic gold mines in California between the 1850's and 1884. \r\n\r\nThe gravel occupies a major channel and parts of several tributaries that in Tertiary time cut into a surface of Paleozoic and Mesozoic igneous and metamorphic rocks. The gravel is partly covered by the remains of an extensive sheet of volcanic rocks, but it crops out along the broad crest of the ridge between the canyons of the South and Middle Yuba Rivers. The lower parts of the gravel deposits generally carry the highest values of placer gold. Traditionally, the richest deposits of all are found in the so-called blue gravel, which, when present, lies just above the bedrock and consists of a very coarse, poorly sorted mixture of cobbles, pebbles, sand, and clay. It is unoxidized, and, at least locally, contains appreciable quantities of secondary sulfide minerals, chiefly pyrite. \r\n\r\nInformation in drill logs from private sources indicates that a 2-mile stretch of the channel near North Columbia contains over half a million ounces of gold dispersed through about 22 million cubic yards of gravel at a grade .averaging about 81 cents per cubic yard. The deposit is buried at depths ranging from 100 to 400 feet. \r\n\r\nSeveral geophysical methods have been tested for their feasibility in determining the configuration of the buried bedrock surface, in delineating channel gravel buried under volcanic rocks, and in identifying concentrations of heavy minerals within the gravel. Although the data have not yet been completely processed, preliminary conclusions indicate that some methods may be quite useful. A combination of seismic-refraction and gravity methods was used to determine the depth and configuration of the bottom of the channel to an accuracy within 10 percent as checked by the drill holes. Seismic-refraction methods have identified depressions which are in the bedrock surface, below volcanic rocks, and which may be occupied by gravels. Seismic methods, however, cannot actually recognize the presence of low-velocity gravels beneath the higher velocity volcanic rocks. Electromagnetic methods, supplemented in part by induced-polarization methods, show promise of being able to recognize and trace blue gravel buried less than 200 feet deep. A broad vague magnetic anomaly across the channel suggests that more precise magnetic studies might delineate concentrations of magnetic material. The usefulness of resistivity methods appears from this study to be quite restricted because of irregular topography and the variable conductivity of layers within the gravel.","language":"ENGLISH","doi":"10.3133/cir566","usgsCitation":"Peterson, D.W., Yeend, W., Oliver, H.W., and Mattick, R., 1968, Tertiary gold-bearing channel gravel in northern Nevada County, California: U.S. Geological Survey Circular 566, iii, 22 p. :ill., maps. ;27 cm., https://doi.org/10.3133/cir566.","productDescription":"iii, 22 p. :ill., maps. ;27 cm.","costCenters":[],"links":[{"id":124415,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/circ/1968/0566/report-thumb.jpg"},{"id":31523,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/circ/1968/0566/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ad9e4b07f02db684fd5","contributors":{"authors":[{"text":"Peterson, D. 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W.","contributorId":85570,"corporation":false,"usgs":true,"family":"Oliver","given":"H.","email":"","middleInitial":"W.","affiliations":[],"preferred":false,"id":149091,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Mattick, R.E.","contributorId":85162,"corporation":false,"usgs":true,"family":"Mattick","given":"R.E.","affiliations":[],"preferred":false,"id":149090,"contributorType":{"id":1,"text":"Authors"},"rank":4}]}} ,{"id":2257,"text":"wsp1855 - 1968 - Ground-water levels in the United States, 1961-65, southwestern States","interactions":[],"lastModifiedDate":"2024-01-31T21:32:21.660914","indexId":"wsp1855","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1968","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":341,"text":"Water Supply Paper","code":"WSP","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"1855","title":"Ground-water levels in the United States, 1961-65, southwestern States","docAbstract":"No abstract available.
","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/wsp1855","usgsCitation":"McGuinness, C.L., 1968, Ground-water levels in the United States, 1961-65, southwestern States: U.S. Geological Survey Water Supply Paper 1855, v, 125 p., https://doi.org/10.3133/wsp1855.","productDescription":"v, 125 p.","costCenters":[],"links":[{"id":425180,"rank":3,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_25071.htm","text":"Arizona","linkFileType":{"id":5,"text":"html"}},{"id":28040,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wsp/1855/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":425181,"rank":4,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_25072.htm","text":"Calfornia","linkFileType":{"id":5,"text":"html"}},{"id":425184,"rank":7,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_25075.htm","text":"New 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The locations of the sites are shown on figure 1, and data pertinent to the state of disequilibrium at the time of measurement are tabulated in table 1. In the geothermal profiles (figs. 2 through 13) the temperature is given in decrees centigrade and the depth (Z) in meters.
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Robert J.","contributorId":12039,"corporation":false,"usgs":true,"family":"Munroe","given":"Robert","email":"","middleInitial":"J.","affiliations":[{"id":595,"text":"U.S. Geological Survey","active":false,"usgs":true}],"preferred":false,"id":170591,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Moses, Thomas H. Jr.","contributorId":65861,"corporation":false,"usgs":true,"family":"Moses","given":"Thomas","suffix":"Jr.","email":"","middleInitial":"H.","affiliations":[],"preferred":false,"id":170592,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":23395,"text":"ofr68140 - 1968 - A geologic and hydrologic reconnaissance of Lava Beds National Monument and vicinity, California","interactions":[],"lastModifiedDate":"2012-02-02T00:08:12","indexId":"ofr68140","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1968","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":"68-140","title":"A geologic and hydrologic reconnaissance of Lava Beds National Monument and vicinity, California","docAbstract":"Lava Beds National Monument is on the Modoc Plateau in Modoc and Siskiyou Counties. The principal geologic units in the vicinity are volcanic rocks, which in places are highly permeable and poorly permeable lake sedimentary deposits, all probably post-Oligocene in age. Yields and specific capacities of wells in the unconfined water body within volcanic rocks and lake deposits range widely, but in general are low in the lake deposits and higher in the volcanic rocks. A confined water body occurring in volcanic rocks underlying the lake deposits yields large quantities of water to three wells in the study area. \r\n\r\nDissolved-solids content of ground water generally increases in proportion to the thickness of lake deposits penetrated and to proximity of the lake deposits. Water from wells drilled in the volcanic rocks several miles from the lake deposits and from wells penetrating the confined water body in volcanic rocks underlying the lake deposits contains small to moderate quantities of dissolved solids. \r\n\r\nGround-water supplies can be developed almost anywhere in the study area by drilling wells to depths below the water table. In addition, there is a reasonable possibility of developing wells in a confined water body underlying the water-table system.","language":"ENGLISH","publisher":"U.S. Dept. of the Interior, Geological Survey, Water Resources Division,","doi":"10.3133/ofr68140","issn":"0094-9140","usgsCitation":"Hotchkiss, W.R., 1968, A geologic and hydrologic reconnaissance of Lava Beds National Monument and vicinity, California: U.S. Geological Survey Open-File Report 68-140, ii, 56 p., [1] folded leaf of plates :ill., maps ;27 cm., https://doi.org/10.3133/ofr68140.","productDescription":"ii, 56 p., [1] folded leaf of plates :ill., maps ;27 cm.","costCenters":[],"links":[{"id":156226,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1968/0140/report-thumb.jpg"},{"id":52695,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1968/0140/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":52696,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1968/0140/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b24e4b07f02db6ae67f","contributors":{"authors":[{"text":"Hotchkiss, W. R.","contributorId":61820,"corporation":false,"usgs":true,"family":"Hotchkiss","given":"W.","email":"","middleInitial":"R.","affiliations":[],"preferred":false,"id":190036,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":13639,"text":"ofr68101 - 1968 - Gold gradients and anomalies in the Pedro Dome-Cleary Summit area, Fairbanks district, Alaska","interactions":[],"lastModifiedDate":"2012-02-02T00:06:52","indexId":"ofr68101","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1968","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":"68-101","title":"Gold gradients and anomalies in the Pedro Dome-Cleary Summit area, Fairbanks district, Alaska","docAbstract":"Anomalous gold values have been discovered in hydrothermally altered quartz diorite, quartz monzonite, and quartz mica schist at the head of Fox Creek; and in similarly altered quartz diorite in the Granite Creek area. Channel samples across some of these altered zones have produced anomalous gold values over widths which merit further investigation as potential large tonnage low-grade gold deposits.\r\n\r\nTrace gold gradients have also been detected in the wall rocks adjacent to mineralized veins and in hydrothermal alteration zones in the Pedro Dome-Cleary Summit area. Although most of the gradients may not materially increase the mineable width of the deposit under current economic conditions, such gradients can be used to locate auriferous quartz veins and altered zones by geochemical methods. Gold enrichment is accompanied by anomalous concentrations of arsenic and antimony, and gold bearing quartz veins and altered zones are frequently signaled by peripheral haloes of these metals before trace gold is detectable. Hydrothermally altered and/or sheared zones in both granitic and metamorphic rocks should be carefully prospected, along the trend of the Cleary Antiform.","language":"ENGLISH","publisher":"U.S. Geological Survey],","doi":"10.3133/ofr68101","usgsCitation":"Forbes, R., Pilkington, H., and Hawkins, D.B., 1968, Gold gradients and anomalies in the Pedro Dome-Cleary Summit area, Fairbanks district, Alaska: U.S. Geological Survey Open-File Report 68-101, 49 p. ill., maps ;27 cm., https://doi.org/10.3133/ofr68101.","productDescription":"49 p. ill., maps ;27 cm.","costCenters":[],"links":[{"id":147255,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1968/0101/report-thumb.jpg"},{"id":42164,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1968/0101/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4abde4b07f02db6741ef","contributors":{"authors":[{"text":"Forbes, Robert B.","contributorId":48984,"corporation":false,"usgs":true,"family":"Forbes","given":"Robert B.","affiliations":[],"preferred":false,"id":168154,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Pilkington, H.D.","contributorId":77942,"corporation":false,"usgs":true,"family":"Pilkington","given":"H.D.","email":"","affiliations":[],"preferred":false,"id":168155,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Hawkins, D. B.","contributorId":43366,"corporation":false,"usgs":true,"family":"Hawkins","given":"D.","email":"","middleInitial":"B.","affiliations":[],"preferred":false,"id":168153,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}} ,{"id":42728,"text":"ofr68332 - 1968 - Preliminary structure map of the Buckeye Quadrangle, central Kentucky","interactions":[{"subject":{"id":42728,"text":"ofr68332 - 1968 - Preliminary structure map of the Buckeye Quadrangle, central Kentucky","indexId":"ofr68332","publicationYear":"1968","noYear":false,"title":"Preliminary structure map of the Buckeye Quadrangle, central Kentucky"},"predicate":"SUPERSEDED_BY","object":{"id":62105,"text":"gq843 - 1970 - Geologic map of the Buckeye quadrangle, central Kentucky","indexId":"gq843","publicationYear":"1970","noYear":false,"title":"Geologic map of the Buckeye quadrangle, central Kentucky"},"id":1}],"supersededBy":{"id":62105,"text":"gq843 - 1970 - Geologic map of the Buckeye quadrangle, central Kentucky","indexId":"gq843","publicationYear":"1970","noYear":false,"title":"Geologic map of the Buckeye quadrangle, central Kentucky"},"lastModifiedDate":"2024-03-27T17:33:56.516856","indexId":"ofr68332","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1968","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":"68-332","title":"Preliminary structure map of the Buckeye Quadrangle, central Kentucky","docAbstract":"No abstract available.
","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr68332","collaboration":"Prepared in cooperation with the Commonwealth of Kentucky, the University of Kentucky and the Kentucky Geological Survey","usgsCitation":"Wolcott, D.E., 1968, Preliminary structure map of the Buckeye Quadrangle, central Kentucky: U.S. Geological Survey Open-File Report 68-332, 1 Plate: 22.39 x 28.98 inches, https://doi.org/10.3133/ofr68332.","productDescription":"1 Plate: 22.39 x 28.98 inches","costCenters":[],"links":[{"id":427149,"rank":2,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1968/0332/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":135523,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1968/0332/report-thumb.jpg"}],"scale":"24000","country":"United States","state":"Kentucky","otherGeospatial":"Buckeye Quadrangle","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -84.61749999999999,37.6175 ], [ -84.61749999999999,37.75 ], [ -84.5,37.75 ], [ -84.5,37.6175 ], [ -84.61749999999999,37.6175 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4aace4b07f02db66a503","contributors":{"authors":[{"text":"Wolcott, Don E.","contributorId":48154,"corporation":false,"usgs":true,"family":"Wolcott","given":"Don","email":"","middleInitial":"E.","affiliations":[],"preferred":false,"id":227016,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":20837,"text":"ofr68242 - 1968 - Availability of palynological material from Naval Petroleum Reserve No. 4, VI: South Barrow test well No. 3","interactions":[],"lastModifiedDate":"2025-07-01T17:13:24.972366","indexId":"ofr68242","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1968","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":"68-242","title":"Availability of palynological material from Naval Petroleum Reserve No. 4, VI: South Barrow test well No. 3","docAbstract":"No abstract available.
","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr68242","usgsCitation":"Scott, R., 1968, Availability of palynological material from Naval Petroleum Reserve No. 4, VI: South Barrow test well No. 3: U.S. Geological Survey Open-File Report 68-242, 9 p., https://doi.org/10.3133/ofr68242.","productDescription":"9 p.","costCenters":[],"links":[{"id":491629,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1968/0242/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":152073,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1968/0242/report-thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a9ae4b07f02db65d863","contributors":{"authors":[{"text":"Scott, Richard A.","contributorId":14414,"corporation":false,"usgs":true,"family":"Scott","given":"Richard A.","affiliations":[],"preferred":false,"id":183338,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":18290,"text":"ofr6827 - 1968 - Report on allanite occurrence near Hamdtha on Wadi Tathlith. Saudi Arabia","interactions":[],"lastModifiedDate":"2012-02-02T00:07:14","indexId":"ofr6827","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1968","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":"68-27","title":"Report on allanite occurrence near Hamdtha on Wadi Tathlith. Saudi Arabia","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/ofr6827","usgsCitation":"Brown, G., 1968, Report on allanite occurrence near Hamdtha on Wadi Tathlith. Saudi Arabia: U.S. Geological Survey Open-File Report 68-27, 2 p. ill. ;28 cm., https://doi.org/10.3133/ofr6827.","productDescription":"2 p. ill. ;28 cm.","costCenters":[],"links":[{"id":149249,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a59e4b07f02db62f752","contributors":{"authors":[{"text":"Brown, Glen F.","contributorId":51711,"corporation":false,"usgs":true,"family":"Brown","given":"Glen F.","affiliations":[],"preferred":false,"id":178859,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":67907,"text":"ha310 - 1968 - Saline ground water in Louisiana","interactions":[],"lastModifiedDate":"2019-11-12T09:36:57","indexId":"ha310","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1968","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":318,"text":"Hydrologic Atlas","code":"HA","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"310","title":"Saline ground water in Louisiana","docAbstract":"No abstract available.
","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Reston, VA","doi":"10.3133/ha310","usgsCitation":"Winslow, A.G., Hillier, D.E., and Turcan, A., 1968, Saline ground water in Louisiana: U.S. Geological Survey Hydrologic Atlas 310, 5 Plates: 34.00 x 41.00 inches or smaller, https://doi.org/10.3133/ha310.","productDescription":"5 Plates: 34.00 x 41.00 inches or 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