A total of 250 kilometers of single-channel seismic-reflection data (28 minisparker profiles) were collected in the coastal waters of Massachusetts, north of and immediately south of Cape Ann, and on the western flank of Jeffreys Ledge, western Gulf of Maine, during the September 1978 cruise of the R/V ASTERIAS. The survey was conducted by the U.S. Geological Survey as part of the Massachusetts Cooperative Marine Geologic Program.
The seismic systems used included a 1Del Norte minisparker and streamer, an Energy International Streamer, and EPC 3200 and 4100 recorders. Navigational control was established by Radar and Loran-C. The Loran-C navigation data were recorded on a Northstar 6000 system.
The purpose of the cruise was to discover the significance and extent of the folded and faulted internal reflections that were first noticed on the esternmost tip of Jeffreys Ledge in line 14 of esternmost tip of Jeffreys Ledge in line 14 of rninisparker data from the 1976 R/V FAY 023 cruise.
Sixteen northwest-trending lines were run off Cape Ann to investigate the deformed reflectors, now thought to represent a moraine formed by readvance of continental ice over the last glacial marine Presurnpscot Formation. Lines north and south of Cape Ann were run to locate the offshore extension of the Clinton-Newbury and Bloody Bluff fault systems.
The original records can be studied at the U.S. Geological Survey offices at Woods Hole, Mass. Microfilm copies of the records can be purchased only from the National Geophysical and Solar-Terrestrial Data Center, NOAA/EDIS/NGSDC, Code D621, 325 Broadway; Boulder, CO 80303 (303-497-6338)
","language":"ENGLISH","publisher":"U.S. Geological Survey","publisherLocation":"Reston, VA","doi":"10.3133/ofr80320","usgsCitation":"Eskenasy, D.M., and Bailey, N.G., 1980, Minisparker profiles from Jeffreys Ledge and adjacent areas in the western Gulf of Maine: U.S. Geological Survey Open-File Report 80-320, 2 p. :map ;28 cm., https://doi.org/10.3133/ofr80320.","productDescription":"2 p. :map ;28 cm.","costCenters":[],"links":[{"id":141948,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/ofr80320.PNG"},{"id":259865,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1980/0320/ofr1980320.pdf","text":"Report","size":"1.54 MB","linkFileType":{"id":1,"text":"pdf"},"description":"OFR 1980-320"}],"contact":"Coastal and Marine Geology Program
U.S. Geological Survey
384 Woods Hole Road
Woods Hole, MA 02543
No abstract available.
","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr8091","usgsCitation":"Palacas, J.G., and Roberts, A.A., 1980, Helium anomaly in surficial deposits of south Florida — Possible indicator of deep subsurface petroleum or shallow uranium-associated phosphate deposits: U.S. Geological Survey Open-File Report 80-91, i, 14 p., https://doi.org/10.3133/ofr8091.","productDescription":"i, 14 p.","costCenters":[],"links":[{"id":392658,"rank":3,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_11820.htm"},{"id":38436,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1980/0091/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":143029,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1980/0091/report-thumb.jpg"}],"country":"United States","state":"Florida","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"type\": \"Polygon\",\n \"coordinates\": [\n [\n [\n -82,\n 25.718\n ],\n [\n -81,\n 25.718\n ],\n [\n -81,\n 26.676\n ],\n [\n -82,\n 26.676\n ],\n [\n -82,\n 25.718\n ]\n ]\n ]\n }\n }\n ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a61e4b07f02db635d6e","contributors":{"authors":[{"text":"Palacas, James George","contributorId":72791,"corporation":false,"usgs":true,"family":"Palacas","given":"James","email":"","middleInitial":"George","affiliations":[],"preferred":false,"id":161657,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Roberts, Alan A.","contributorId":106495,"corporation":false,"usgs":true,"family":"Roberts","given":"Alan","email":"","middleInitial":"A.","affiliations":[],"preferred":false,"id":161658,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":8887,"text":"ofr791545 - 1980 - Preliminary report on the hydrogeology of a low-level radioactive waste disposal site near Sheffield, Illinois","interactions":[],"lastModifiedDate":"2024-02-26T18:10:27.022333","indexId":"ofr791545","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1980","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":"79-1545","title":"Preliminary report on the hydrogeology of a low-level radioactive waste disposal site near Sheffield, Illinois","docAbstract":"The Sheffield low-level radioactive-waste disposal site is located on 20 acres of rolling terrain about 3 miles southwest of Sheffield, Illinois. Twenty-one trenches were constructed and filled with radioactive waste from August 1967 through April 1978. Forty-three test wells were installed by the U.S. Geological Survey on and adjacent to the site. Continuous cores were collected from 36 wells to help in defining the subsurface geology. The wells have been used for water sample collection and to monitor water-level changes. A tunnel. 6.5 feet in diameter by 290 feet in length, was constructed beneath four burial trenches to provide access for collection of hydrologic and geologic data.
Pennsylvanian shale and mudstone deposits are overlain by Pleistocene glacial deposits consisting of the Teneriffe Silt, Glasford Formation, Roxana Silt, Peoria Loess, Parkland Sand, Cahokia Alluvium, and Henry Formation. Three till units of the Glasford Formation, the Hulick Till Member, the Radnor Till Member, and Till A have been identified on the site. Stratigraphic position indicates that the Hulick Till Member and Till A are probably variations of the same till. A continuous pebbly sand deposit, classified as part of the Toulon Member, extends across the middle of the site and continues off site on the northeast and southwest corners. Because of its relatively high hydraulic conductivity, this deposit will be a controlling factor in shallow groundwater movement and in any radionuclide migration.
Ground water at the site is derived through infiltration of precipitation and as underflow from adjacent highlands. Precipitation averages 35 inches per year, 1 or 2 inches of which probably recharge the ground water. Runoff is estimated to be 12 to 15 inches per year and evapotranspiration about 20 inches.
The fluctuation of water levels has been about 2.5 feet in hilltop wells, 3.6 feet in sidehill wells, and 5.9 feet in valley wells.
Hydraulic conductivity of the materials comprising the hydrogeologic system vary widely from about 2.8 to 2.8 x 10-6 feet/day. Tritium in ground water near the southeast corner of the site has moved about 25 feet per year since June 1975.
A method is presented for estimating flood magnitudes for natural drainage basins without urban development or regulated flow. The method was developed by multiple-regression techniques and applies to floods with recurrence intervals from 2 to 100 years.
The State is divided into three regions, and sets of equations for calculating peak discharges based on physical basin characteristics are provided for each region. In the northern region, flood-peak discharges are related to drainage area, forest cover, and 2-year 24-hour rainfall. In the southern region, flood peaks are related to drainage area alone. In the eastern region, peaks are related to drainage area, slope, storage, forest cover, and two composite soil categories. Standard errors of estimate for the regression equations in the northern region range from 38 to 49 percent. For the southern region, the standard errors of estimate vary from 52 to 86 percent, and for the eastern region they vary from 37 to 40 percent.
Maximum observed flood peaks, basin characteristics, and flood-frequency characteristics are tabulated for 234 gaged sites in Maryland and nearby in surrounding states. At 39 of these sites, a rainfall-runoff model was used to obtain synthetic flood-frequency data. These data were combined with observed flood-frequency data to determine the final flood-frequency distributions.
Evaporites are an important potential medium for the storage of radioactive wastes. In order to ascertain the viability of a proposed waste isolation site, it is necessary to study its geology without extensive drilling that might destroy its structural integrity. Hole-to-surface and hole-to-hole geophysical measurements can be useful in supplementing geologic data obtained from a few drill holes and can be used to aid the interpretation of surface geophysical measurements. The study presented in this paper was conducted at Salt Valley, Utah to test the feasibility of using hole-to-surface direct-current resistivity measurements to detect geologic inhomogeneities in evaporites. These measurements show the following:
(1) It is feasible to make hole-to-surface resistivity measurements over evaporites. However, near-surface steel casing can make it difficult to quantitatively analyze the field data with present interpretation techniques. Future investigations should include theoretical studies to solve interpretation problems when steel casing is in the hole and the mud is a high-conductivity brine.
(2) A comparison of measurements made from the three different source drill holes shows that the halite acts as an electrical insulator and most of the current emitted from the source is contained in the caprock.
(3) A comparison of measurements made parallel and perpendicular to the valley walls shows that there are more variations in the halitecaprock interface perpendicular than parallel to the axis of the Salt Valley anticline.
(4) Structurally complex interbeds within the salt may cause differences in the current distribution measured at the surface from current sources buried at different depths.
(5) Total field mapping would be more useful than the single-component data that were collected in this study.
The Middle and (or) Late Triassic Nikolai Greenstone, part of the allochthonous terrane of Wrangellia, is typically altered and locally metamorphosed to prehnite-pumpellyite facies with chlorite and epidote as the most common secondary minerals. Intrinsic copper content averages 155 ppm, and two types of concentrations of copper in the Nikolai are common: (1) native copper fillings of amygdules and rubble zones typically near flow tops, and (2) veins and thin replacement zones that contain native copper and copper-iron sulfides in quartz-epidote or calcite gangue in faults and fractures. Oxygen isotope data from quartz and epidote from three copperbearing veins yield calculated ore fluid temperatures of approximately 200°C and 6180 of approximately +1 per mil in agreement with a metamorphicsegregation origin of these deposits, as suggested by Sinclair (1977).
Seven K-Ar ages of chloritized greenstone, including those adjacent to veins fall on an initial argon diagram with a zero intercept and a slope which yields an isochron age of 112 + 11 m.y. The ages define a Cretaceous thermalmetamorphic episode which is responsible for alteration and mineralization. The episode is younger than a major Jurassic progeny, accompanied by granitic intrusion, in the area, and appears to be unaffected by minor granitic intrusion in the middle to late Tertiary. We believe the Cretaceous event is related to accretion of Wrangellia to its present relative position in North America. This age of accretion agrees with stratigraphic and structural evidence cited by other workers.
","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr802019","usgsCitation":"Silberman, M., MacKevett, E., Connor, C.L., and Matthews, A., 1980, Metallogenic and tectonic significance of oxygen isotope data and whole-rock potassium-argon ages of the Nikolai Greenstone, McCarthy Quadrangle, Alaska: U.S. Geological Survey Open-File Report 80-2019, ii, 29 p., https://doi.org/10.3133/ofr802019.","productDescription":"ii, 29 p.","costCenters":[],"links":[{"id":349265,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1980/2019/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":140597,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1980/2019/report-thumb.jpg"}],"country":"United States","state":"Alaska","otherGeospatial":"McCarthy Quadrangle","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"type\": \"Polygon\",\n \"coordinates\": [\n [\n [\n -144,\n 61\n ],\n [\n -141,\n 61\n ],\n [\n -141,\n 62\n ],\n [\n -144,\n 62\n ],\n [\n -144,\n 61\n ]\n ]\n ]\n }\n }\n ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a4fe4b07f02db6286b3","contributors":{"authors":[{"text":"Silberman, M.L.","contributorId":10013,"corporation":false,"usgs":true,"family":"Silberman","given":"M.L.","affiliations":[],"preferred":false,"id":155162,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"MacKevett, E.M. Jr.","contributorId":58613,"corporation":false,"usgs":true,"family":"MacKevett","given":"E.M.","suffix":"Jr.","email":"","affiliations":[],"preferred":false,"id":155163,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Connor, C. L.","contributorId":67508,"corporation":false,"usgs":true,"family":"Connor","given":"C.","email":"","middleInitial":"L.","affiliations":[],"preferred":false,"id":155164,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Matthews, Alan","contributorId":72377,"corporation":false,"usgs":true,"family":"Matthews","given":"Alan","email":"","affiliations":[],"preferred":false,"id":155165,"contributorType":{"id":1,"text":"Authors"},"rank":4}]}} ,{"id":22733,"text":"ofr80909 - 1980 - Summaries of data on and lists of references to metallic and selected nonmetallic mineral deposits in fifteen quadrangles in southwestern and west-central Alaska","interactions":[],"lastModifiedDate":"2023-08-22T21:06:35.143272","indexId":"ofr80909","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1980","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":"80-909","title":"Summaries of data on and lists of references to metallic and selected nonmetallic mineral deposits in fifteen quadrangles in southwestern and west-central Alaska","docAbstract":"These summaries of data on metallic and selected nonmetallic mineral occurrences and lists of selected references to them in Geological Survey, U.S. Bureau of Mines, and State of Alaska Division of Geological and Geophysical Surveys (and predecessor State and Territorial agencies) reports and maps released before Jan. 1, 1980, and in one abstract of a report presented orally at a scientific meeting, are designed to aid in library research on the mineral resources of 14 quadrangles in southwestern Alaska and the Saint Lawrence quadrangle in west—central Alaska. The references are selected in the sense that mainly statistical reports such as the annual Minerals Yearbook of the U.S. Bureau of Mines and many annual and biennial reports of the Alaska Division of Geological and Geophysical Surveys and its predecessor agencies are not included. Also not included are data on many claims about which little more than their locations is known (for example, localities 11 to 14 in MacKevett and Holloway, 1977 (OF 77-169D), p. 28). These omissions should not be interpreted as a judgement that the claims are not on valid mineral occurrences, but only that there are insufficient data to describe any mineral deposit that might be present. Geochemical anomalies determined by analyses of rock and stream—sediment samples in which no metallic mineral was identified are also omitted. Work now in progress should add greatly to the knowledge of mineral resources in several quadrangles on the Alaska Peninsula.
No abstract available.
","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr80785","usgsCitation":"Staatz, M.H., Conklin, N.M., Bunker, C., and Bush, C.A., 1980, Gamma-ray spectrometric and semiquantitative spectrographic analytical data of the thorium and rare-earth disseminated deposits in the southern Bear Lodge Mountains, Wyoming: U.S. Geological Survey Open-File Report 80-785, Report: 47 p.; 1 Plate: 21.21 × 25.39 inches, https://doi.org/10.3133/ofr80785.","productDescription":"Report: 47 p.; 1 Plate: 21.21 × 25.39 inches","costCenters":[],"links":[{"id":34453,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1980/0785/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":34452,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1980/0785/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":140497,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1980/0785/report-thumb.jpg"},{"id":406094,"rank":4,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_75294.htm","linkFileType":{"id":5,"text":"html"}}],"country":"United States","state":"Wyoming","otherGeospatial":"southern Bear Lodge Mountains","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"type\": \"Polygon\",\n \"coordinates\": [\n [\n [\n -104.4911,\n 44.4458\n ],\n [\n -104.4131,\n 44.4458\n ],\n [\n -104.4131,\n 44.5214\n ],\n [\n -104.4911,\n 44.5214\n ],\n [\n -104.4911,\n 44.4458\n ]\n ]\n ]\n }\n }\n ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b28e4b07f02db6b13d0","contributors":{"authors":[{"text":"Staatz, Mortimer Hay","contributorId":39754,"corporation":false,"usgs":true,"family":"Staatz","given":"Mortimer","email":"","middleInitial":"Hay","affiliations":[],"preferred":false,"id":154463,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Conklin, Nancy M.","contributorId":106108,"corporation":false,"usgs":true,"family":"Conklin","given":"Nancy","email":"","middleInitial":"M.","affiliations":[],"preferred":false,"id":154465,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Bunker, Carl M.","contributorId":45311,"corporation":false,"usgs":true,"family":"Bunker","given":"Carl M.","affiliations":[],"preferred":false,"id":154464,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Bush, Charles A. cbush@usgs.gov","contributorId":1258,"corporation":false,"usgs":true,"family":"Bush","given":"Charles","email":"cbush@usgs.gov","middleInitial":"A.","affiliations":[{"id":318,"text":"Geosciences and Environmental Change Science Center","active":true,"usgs":true}],"preferred":true,"id":154462,"contributorType":{"id":1,"text":"Authors"},"rank":4}]}} ,{"id":8270,"text":"ofr80963 - 1980 - Flood potential of Topopah Wash and tributaries, eastern part of Jackass Flats, Nevada Test Site, southern Nevada","interactions":[],"lastModifiedDate":"2012-02-02T00:05:59","indexId":"ofr80963","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1980","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":"80-963","title":"Flood potential of Topopah Wash and tributaries, eastern part of Jackass Flats, Nevada Test Site, southern Nevada","docAbstract":"Guidelines for the evaluation of potential surface facilities for the storage of high-level radioactive wastes on the Nevada Test Site in southern Nevada include the consideration of the potential for flooding. Those floods that are considered to constitute the principal flood hazards for these facilities are the 100- and 500-year floods, and the maximum potential flood. Flood-prone areas for the three floods with present natural-channel conditions were defined for the eastern part of Jackass Flats in the southwestern part of the Nevada Test Site. The 100-year flood-prone areas would closely parallel most stream channels with very few occurrences of overland flooding between adjacent channels. The 500-year flood and the maximum potential flood would exceed the discharge capacities of main channels and cause overland flooding between adjacent channels throughout most of the study area. Excluded areas would be those located immediately east of the upstream reach of Topopah Wash and between upstream channel reaches of some tributaries. Floodflow characteristics for the three floods were determined at 47 cross sections. The magnitudes of the estimated velocities indicate severe erosion of channels and flood plains would occur in parts of the study area. (USGS)","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/ofr80963","usgsCitation":"Christensen, R.C., and Spahr, N.E., 1980, Flood potential of Topopah Wash and tributaries, eastern part of Jackass Flats, Nevada Test Site, southern Nevada: U.S. Geological Survey Open-File Report 80-963, iv, 26 p. ill., maps ;28 cm., https://doi.org/10.3133/ofr80963.","productDescription":"iv, 26 p. ill., maps ;28 cm.","costCenters":[],"links":[{"id":140099,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1980/0963/report-thumb.jpg"},{"id":35883,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1980/0963/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":35884,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1980/0963/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e49f2e4b07f02db5eeb77","contributors":{"authors":[{"text":"Christensen, Rulon C.","contributorId":73594,"corporation":false,"usgs":true,"family":"Christensen","given":"Rulon","email":"","middleInitial":"C.","affiliations":[],"preferred":false,"id":157463,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Spahr, Norman E. nspahr@usgs.gov","contributorId":1977,"corporation":false,"usgs":true,"family":"Spahr","given":"Norman","email":"nspahr@usgs.gov","middleInitial":"E.","affiliations":[],"preferred":true,"id":157462,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":42937,"text":"ofr80849 - 1980 - Preliminary maps showing Late Cenozoic deposits of the Bruceville, Elk Grove, Florin, and Galt 7.5-minute quadrangles, Sacramento and San Joaquin Counties, California","interactions":[],"lastModifiedDate":"2022-09-06T21:42:35.982501","indexId":"ofr80849","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1980","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":"80-849","title":"Preliminary maps showing Late Cenozoic deposits of the Bruceville, Elk Grove, Florin, and Galt 7.5-minute quadrangles, Sacramento and San Joaquin Counties, California","docAbstract":"No abstract available.
","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr80849","usgsCitation":"Atwater, B.F., and Marchand, D.E., 1980, Preliminary maps showing Late Cenozoic deposits of the Bruceville, Elk Grove, Florin, and Galt 7.5-minute quadrangles, Sacramento and San Joaquin Counties, California: U.S. Geological Survey Open-File Report 80-849, Report: 11 p.; 4 Plates: 19.69 × 28.14 inches or smaller, https://doi.org/10.3133/ofr80849.","productDescription":"Report: 11 p.; 4 Plates: 19.69 × 28.14 inches or smaller","costCenters":[],"links":[{"id":80737,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1980/0849/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":108075,"rank":700,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_11798.htm","linkFileType":{"id":5,"text":"html"},"description":"11798"},{"id":172901,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1980/0849/report-thumb.jpg"},{"id":80733,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1980/0849/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":80734,"rank":401,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1980/0849/plate-2.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":80735,"rank":402,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1980/0849/plate-3.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":80736,"rank":403,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1980/0849/plate-4.pdf","linkFileType":{"id":1,"text":"pdf"}}],"country":"United States","state":"California","county":"Sacramento County, San Joaquin County","otherGeospatial":"Bruceville, Elk Grove, Florin, and Galt 7.5-minute quadrangles","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"type\": \"Polygon\",\n \"coordinates\": [\n [\n [\n -121.375,\n 38.25\n ],\n [\n -121.25,\n 38.25\n ],\n [\n -121.25,\n 38.5\n ],\n [\n -121.375,\n 38.5\n ],\n [\n -121.375,\n 38.25\n ]\n ]\n ]\n }\n }\n ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4aafe4b07f02db66ce69","contributors":{"authors":[{"text":"Atwater, Brian F. 0000-0003-1155-2815 atwater@usgs.gov","orcid":"https://orcid.org/0000-0003-1155-2815","contributorId":3297,"corporation":false,"usgs":true,"family":"Atwater","given":"Brian","email":"atwater@usgs.gov","middleInitial":"F.","affiliations":[{"id":237,"text":"Earthquake Science Center","active":true,"usgs":true}],"preferred":true,"id":227443,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Marchand, Denis E.","contributorId":98280,"corporation":false,"usgs":true,"family":"Marchand","given":"Denis","email":"","middleInitial":"E.","affiliations":[],"preferred":false,"id":227444,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":8595,"text":"ofr80358 - 1980 - Undiscovered recoverable resource estimates of crude oil, natural gas, and natural gas liquids for the offshore United States, November 1979","interactions":[],"lastModifiedDate":"2012-02-02T00:06:09","indexId":"ofr80358","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1980","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":"80-358","title":"Undiscovered recoverable resource estimates of crude oil, natural gas, and natural gas liquids for the offshore United States, November 1979","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/ofr80358","usgsCitation":"Dolton, G., 1980, Undiscovered recoverable resource estimates of crude oil, natural gas, and natural gas liquids for the offshore United States, November 1979: U.S. Geological Survey Open-File Report 80-358, 3 p. ;28 cm., https://doi.org/10.3133/ofr80358.","productDescription":"3 p. ;28 cm.","costCenters":[],"links":[{"id":141075,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1980/0358/report-thumb.jpg"},{"id":36187,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1980/0358/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a26e4b07f02db60f619","contributors":{"authors":[{"text":"Dolton, Gordon","contributorId":50509,"corporation":false,"usgs":true,"family":"Dolton","given":"Gordon","email":"","affiliations":[],"preferred":false,"id":158004,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ]}