No abstract available.
","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Reston, VA","doi":"10.3133/ofr82600","usgsCitation":"O’Leary, D.W., 1982, Mid-range sidescan-sonar data from the Continental Slope off Georges Bank, between Lydonia and Oceanographer canyons: U.S. Geological Survey Open-File Report 82-600, 5 p., https://doi.org/10.3133/ofr82600.","productDescription":"5 p.","costCenters":[],"links":[{"id":365414,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1982/0600/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":144319,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1982/0600/report-thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a60e4b07f02db63527a","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":161628,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":11173,"text":"ofr8270 - 1982 - Granulometry of core CL-73-4, Clear Lake, California","interactions":[],"lastModifiedDate":"2012-02-02T00:06:30","indexId":"ofr8270","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1982","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":"82-70","title":"Granulometry of core CL-73-4, Clear Lake, California","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/ofr8270","usgsCitation":"Sims, J., 1982, Granulometry of core CL-73-4, Clear Lake, California: U.S. Geological Survey Open-File Report 82-70, 7 p., ill., map ;28 cm., https://doi.org/10.3133/ofr8270.","productDescription":"7 p., ill., map ;28 cm.","costCenters":[],"links":[{"id":143944,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1982/0070/report-thumb.jpg"},{"id":38937,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1982/0070/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4abbe4b07f02db672402","contributors":{"authors":[{"text":"Sims, J.D.","contributorId":9230,"corporation":false,"usgs":false,"family":"Sims","given":"J.D.","email":"","affiliations":[],"preferred":false,"id":162671,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":11723,"text":"ofr82313 - 1982 - Fluid-inclusion data on samples from Creede, Colorado, in relation to mineral paragenesis","interactions":[],"lastModifiedDate":"2012-02-02T00:06:31","indexId":"ofr82313","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1982","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":"82-313","title":"Fluid-inclusion data on samples from Creede, Colorado, in relation to mineral paragenesis","docAbstract":"Published and unpublished data on 2575 fluid inclusions in ore and gangue minerals from the Creede, Colorado, Ag-Pb-Zn-Cu vein deposit collected in our laboratories from 1959 to 1981 have shown that the average salinity (wt. % NaCl equivalent, hereinafter termed wt.% eq.) and homogenization temperature (Th), and the ranges of these two parameters for fluid inclusions in sphalerite, quartz, fluorite, and rhodochrosite, respectively, are 8.1 (4.6 - 13.4), 239?C (195-274?C); 6.1 (1.1-10.0), 260?C (190->400?C); 10.7 (6.1-11.1), 217?C (213-229?C) and 260?C (247-268?C) (bimodal distribution of Th); and 9.9 (9.3 - 10.6), 214?C (185-249?C). Inclusions have been measured in minerals from four of the five stages of mineralization previously recognized at Creede. The few inclusions of fluids depositing rhodochrosite (A-stage, earliest in the paragenesis) yield Th and salinity values more similar to those of the low-temperature (average Th 217?C) fluids forming some of the much later fluorite (C-stage) than to any of the other fluids. Th measurements on A-stage quartz range from 192?C to 263?C and average 237?C. The early, fine-grained, B-stage sphalerites yielded Th of 214 to 241?C and salinities of 6.1 to 10.2 wt. % eq. \r\n\r\nD-stage sphalerite (late in the paragenesis) has been studied in detail (growth-zone by growth-zone) for several localities along the OH vein and reveals a generally positive correlation among Th, salinity and iron content of the host sphalerite. The deposition of D-stage sphalerite was characterized by repeated cycling through different regions of salinity/Th space, as Th and salinity generally decreased with time. Seventeen salinity-Th measurements were made on D-stage sphalerite from one locality on the Bulldog Mountain vein system, which, like the OH vein, is one of four major ore-producing vein systems at Creede. These data suggest a lower Th for a given salinity fluid from sphalerite on the Bulldog Mountain vein than on the OH vein. The very high values of Th for some quartz samples (mostly D-stage) are believed to be a result of the trapping of both gas and liquid from a boiling fluid in the upper levels of the vein system. Boiling of fluids depositing D-stage quartz is indicated by the presence of steam inclusions in quartz and the extreme variability of Th values measured on quartz. The pressure was low (< 125 kg/cm 2) throughout ore deposition. \r\n\r\nThree major growth zones in D-stage sphalerite are recognized throughout the OH vein. Deposition of the first major zone began from fluids having intermediate salinities and temperatures (7.8-9.2 wt. % eq., 240?C) but the characteristics of the fluids oscillated after that, ranging from 7.2 to 10.1 wt. % eq. and from 225?C to 270?C. Deposition of the second major, most Fe-rich zone began with the hottest, most saline fluids present during D-stage mineralization (. 270?C, 10.5-12.5 wt. % eq., 3 mole % FeS in sphalerite). The fluid then oscillated with respect to Th and salinity (213-274?C, 5.2-12.5 wt. % eq.) but showed a general decrease in both with time. Deposition of the youngest major zone began with a very Fe-poor sphalerite (0.25-0.75 mole % FeS), from the least saline, coolest fluids (5-6.5 wt. % eq., 200-212?C) and ended with a trend of increasing temperature at approximately constant salinity.\r\n\r\nThe fluid-inclusion data can best be explained by a mixing model involving at least two fluids--one hot and saline, the other cool and fresher. Sudden changes in the mixing ratio, presumably from changes in the plumbing, punctuated long periods of remarkably uniform conditions of ore fluid flow and deposition. The effects of other processes such as convection and heat exchange with wall rocks must have been superimposed on this simple mixing model, however. In contrast to an earlier interpretation, several aspects of the inclusion data may be interpreted to suggest exceedingly slow ore deposition. Work in progress may resolve some of these ambiguities and refine","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/ofr82313","usgsCitation":"Woods, T., Roedder, E., and Bethke, P.M., 1982, Fluid-inclusion data on samples from Creede, Colorado, in relation to mineral paragenesis: U.S. Geological Survey Open-File Report 82-313, 77 p., ill., maps ;28 cm., https://doi.org/10.3133/ofr82313.","productDescription":"77 p., ill., maps ;28 cm.","costCenters":[],"links":[{"id":143786,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1982/0313/report-thumb.jpg"},{"id":39610,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1982/0313/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e49d6e4b07f02db5de77a","contributors":{"authors":[{"text":"Woods, T.L.","contributorId":6052,"corporation":false,"usgs":true,"family":"Woods","given":"T.L.","email":"","affiliations":[],"preferred":false,"id":163620,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Roedder, Edwin","contributorId":25571,"corporation":false,"usgs":true,"family":"Roedder","given":"Edwin","affiliations":[],"preferred":false,"id":163621,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Bethke, P. M.","contributorId":32921,"corporation":false,"usgs":true,"family":"Bethke","given":"P.","email":"","middleInitial":"M.","affiliations":[],"preferred":false,"id":163622,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}} ,{"id":10794,"text":"ofr82959 - 1982 - Zeolites in the Pine Ridge Indian Reservation, South Dakota","interactions":[],"lastModifiedDate":"2012-02-02T00:06:34","indexId":"ofr82959","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1982","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":"82-959","title":"Zeolites in the Pine Ridge Indian Reservation, South Dakota","docAbstract":"Zeolites of possible commercial value occur in the Brule Formation of Oligocene age and the Sharps Formation (Harksen, 1961) of Miocene age which crop out in a wide area in the northern part of the Pine Ridge Indian Reservation. The thickness of the zeolite-bearing Interval and the extent of areas within the Interval which contain significant amounts of zeolites are far greater than was expected prior to this investigation. The shape of the zeolite-bearing Interval is tabular and the dimensions of Its exposure are roughly 10 ml x 200 mi x 150 ft (16 km x 160 km x 45 m) thick. Within the study area, there are tracts in which the zeolite resource potential is significant (see pl. 2). \r\n\r\nThis report is intended to inform the Oglala Sioux Tribe of some of the most promising zeolite occurrences. Initial steps can then be taken by the Tribe toward possible development of the resources, should they wish to do so. The data contained herein identify areas of high zeolite potential, but are not adequate to establish economic value for the deposits. If development is recommended by the tribal government, we suggest that the tribal government contact companies involved in research and production of natural zeolites and provide them with the data in this report.","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/ofr82959","usgsCitation":"Raymond, W.H., Bush, A., and Gude, A.J., 1982, Zeolites in the Pine Ridge Indian Reservation, South Dakota: U.S. Geological Survey Open-File Report 82-959, 16 p., 1 over-size sheet, ill., map ;28 cm., https://doi.org/10.3133/ofr82959.","productDescription":"16 p., 1 over-size sheet, ill., map ;28 cm.","costCenters":[],"links":[{"id":144931,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1982/0959/report-thumb.jpg"},{"id":20760,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1982/0959/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":20761,"rank":401,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1982/0959/plate-1-preview.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":38591,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1982/0959/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a9ae4b07f02db65d978","contributors":{"authors":[{"text":"Raymond, William H.","contributorId":48555,"corporation":false,"usgs":true,"family":"Raymond","given":"William","email":"","middleInitial":"H.","affiliations":[],"preferred":false,"id":161975,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Bush, Alfred L.","contributorId":48977,"corporation":false,"usgs":true,"family":"Bush","given":"Alfred L.","affiliations":[],"preferred":false,"id":161976,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Gude, Arthur J. 3rd 3rd","contributorId":34932,"corporation":false,"usgs":true,"family":"Gude","given":"Arthur","suffix":"3rd","email":"","middleInitial":"J. 3rd","affiliations":[],"preferred":false,"id":161974,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}} ,{"id":10847,"text":"ofr82496 - 1982 - Occurrence and origin of natural gas in ground water, southern Weld County, Colorado","interactions":[],"lastModifiedDate":"2012-02-02T00:06:35","indexId":"ofr82496","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1982","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":"82-496","title":"Occurrence and origin of natural gas in ground water, southern Weld County, Colorado","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/ofr82496","usgsCitation":"Rice, D.D., and Threlkeld, C.N., 1982, Occurrence and origin of natural gas in ground water, southern Weld County, Colorado: U.S. Geological Survey Open-File Report 82-496, i, 8 p. ;28 cm., https://doi.org/10.3133/ofr82496.","productDescription":"i, 8 p. ;28 cm.","costCenters":[],"links":[{"id":144825,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1982/0496/report-thumb.jpg"},{"id":38639,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1982/0496/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4afbe4b07f02db696168","contributors":{"authors":[{"text":"Rice, D. D.","contributorId":41828,"corporation":false,"usgs":true,"family":"Rice","given":"D.","email":"","middleInitial":"D.","affiliations":[],"preferred":false,"id":162068,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Threlkeld, C. N.","contributorId":80271,"corporation":false,"usgs":true,"family":"Threlkeld","given":"C.","email":"","middleInitial":"N.","affiliations":[],"preferred":false,"id":162069,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":11585,"text":"ofr82986 - 1982 - Radiative transfer from a homogeneous half-space; a fast algorithm solution","interactions":[],"lastModifiedDate":"2012-02-02T00:06:50","indexId":"ofr82986","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1982","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":"82-986","title":"Radiative transfer from a homogeneous half-space; a fast algorithm solution","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/ofr82986","usgsCitation":"Watson, K., 1982, Radiative transfer from a homogeneous half-space; a fast algorithm solution: U.S. Geological Survey Open-File Report 82-986, 8 p., ill. ;28 cm., https://doi.org/10.3133/ofr82986.","productDescription":"8 p., ill. ;28 cm.","costCenters":[],"links":[{"id":146036,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1982/0986/report-thumb.jpg"},{"id":39447,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1982/0986/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a81e4b07f02db649dc0","contributors":{"authors":[{"text":"Watson, Ken","contributorId":90317,"corporation":false,"usgs":true,"family":"Watson","given":"Ken","email":"","affiliations":[],"preferred":false,"id":163398,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":10860,"text":"ofr82980 - 1982 - Integrated model of the shallow and deep hydrothermal systems in the East Mesa area, Imperial Valley, California","interactions":[],"lastModifiedDate":"2012-02-02T00:06:34","indexId":"ofr82980","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1982","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":"82-980","title":"Integrated model of the shallow and deep hydrothermal systems in the East Mesa area, Imperial Valley, California","docAbstract":"Geological, geophysical, thermal, petrophysical and hydrological data available for the East Mesa hydrothermal system that are pertinent to the construction of a computer model of the natural flow of heat and fluid mass within the system are assembled and correlated. A conceptual model of the full system is developed and a subregion selected for quantitative modeling. By invoking the .Boussinesq approximation, valid for describing the natural flow of heat and mass in a liquid hydrothermal system, it is found practical to carry computer simulations far enough in time to ensure that steady-state conditions are obtained. Initial calculations for an axisymmetric model approximating the system demonstrate that the vertical formation permeability of the deep East Mesa system must be very low (kv ~ 0.25 to 0.5 md). Since subsurface temperature and surface heat flow data exhibit major deviations from the axisymmetric approximation, exploratory three-dimensional calculations are performed to assess the effects of various mechanisms which might operate to produce such observed asymmetries. A three-dimensional model evolves from this iterative data synthesis and computer analysis which includes a hot fluid convective source distributed along a leaky fault radiating northward from the center of the hot spot and realistic variations in the reservoir formation properties.","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/ofr82980","usgsCitation":"Riney, T.D., Pritchett, J., and Rice, L., 1982, Integrated model of the shallow and deep hydrothermal systems in the East Mesa area, Imperial Valley, California: U.S. Geological Survey Open-File Report 82-980, 118 p., ill., maps ;28 cm., https://doi.org/10.3133/ofr82980.","productDescription":"118 p., ill., maps ;28 cm.","costCenters":[],"links":[{"id":144916,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1982/0980/report-thumb.jpg"},{"id":38644,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1982/0980/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e499ee4b07f02db5bcb4b","contributors":{"authors":[{"text":"Riney, T. David","contributorId":92674,"corporation":false,"usgs":true,"family":"Riney","given":"T.","email":"","middleInitial":"David","affiliations":[],"preferred":false,"id":162090,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Pritchett, J.W.","contributorId":29433,"corporation":false,"usgs":true,"family":"Pritchett","given":"J.W.","email":"","affiliations":[],"preferred":false,"id":162088,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Rice, L.F.","contributorId":59799,"corporation":false,"usgs":true,"family":"Rice","given":"L.F.","email":"","affiliations":[],"preferred":false,"id":162089,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}} ,{"id":11520,"text":"ofr82572 - 1982 - Drainage areas in New Jersey; Delaware River basin and streams tributary to Delaware Bay","interactions":[],"lastModifiedDate":"2012-02-02T00:06:49","indexId":"ofr82572","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1982","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":"82-572","title":"Drainage areas in New Jersey; Delaware River basin and streams tributary to Delaware Bay","docAbstract":"Drainage areas of New Jersey streams tributary to the Delaware River and Delaware Bay are listed for over 1,100 sites. Tables show the descriptive location of each site, the latitude and longitude, county, and National Topographic map name. For gaged sites established through 1980, the U.S. Geological Survey station name and number are also listed. The data are presented alphabetically by stream name and in downstream order. Drainage areas were tabulated for most named streams and unnamed streams with a drainage area greater than 5 square miles. The methods used to delineate the drainage divides, measure areas, and determine mouths of streams follow the guidelines developed by the U.S. Water Resources Council. (USGS)","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/ofr82572","usgsCitation":"Velnich, A., 1982, Drainage areas in New Jersey; Delaware River basin and streams tributary to Delaware Bay: U.S. Geological Survey Open-File Report 82-572, ii, 50 p. :map ;28 cm., https://doi.org/10.3133/ofr82572.","productDescription":"ii, 50 p. :map ;28 cm.","costCenters":[],"links":[{"id":146074,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1982/0572/report-thumb.jpg"},{"id":39385,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1982/0572/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a61e4b07f02db635fb3","contributors":{"authors":[{"text":"Velnich, A. J.","contributorId":25149,"corporation":false,"usgs":true,"family":"Velnich","given":"A. J.","affiliations":[],"preferred":false,"id":163291,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":10787,"text":"ofr82829 - 1982 - Organic geochemistry of sediments on the flanks of Tanner and Cortes banks offshore from southern California","interactions":[],"lastModifiedDate":"2012-02-02T00:06:34","indexId":"ofr82829","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1982","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":"82-829","title":"Organic geochemistry of sediments on the flanks of Tanner and Cortes banks offshore from southern California","docAbstract":"Holocene sediment, composed mainly of foram tests, occurs on the flanks of the Tanner and Cortes Banks, offshore southern California. The organic matter in this sediment differs in content and composition from the organic matter in nearby basins. Two sources of hydrocarbons are indicated: terrestrial plants and biodegraded or immature petroleum.","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/ofr82829","usgsCitation":"Rapp, J.B., and Kvenvolden, K., 1982, Organic geochemistry of sediments on the flanks of Tanner and Cortes banks offshore from southern California: U.S. Geological Survey Open-File Report 82-829, 18 p., ill., map ;28 cm., https://doi.org/10.3133/ofr82829.","productDescription":"18 p., ill., map ;28 cm.","costCenters":[],"links":[{"id":144867,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1982/0829/report-thumb.jpg"},{"id":38585,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1982/0829/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ae5e4b07f02db68a890","contributors":{"authors":[{"text":"Rapp, J. B.","contributorId":28987,"corporation":false,"usgs":true,"family":"Rapp","given":"J.","email":"","middleInitial":"B.","affiliations":[],"preferred":false,"id":161961,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Kvenvolden, K.A.","contributorId":80674,"corporation":false,"usgs":true,"family":"Kvenvolden","given":"K.A.","email":"","affiliations":[],"preferred":false,"id":161962,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":10865,"text":"ofr82911 - 1982 - Effects of urbanization on the magnitude and frequency of floods on small streams in Tennessee; basic data report no. 2","interactions":[{"subject":{"id":23687,"text":"ofr80572 - 1980 - Effects of Urbanization on the Magnitude and Frequency of Floods on Small Streams in Tennessee - Basic Data Report No. 1","indexId":"ofr80572","publicationYear":"1980","noYear":false,"title":"Effects of Urbanization on the Magnitude and Frequency of Floods on Small Streams in Tennessee - Basic Data Report No. 1"},"predicate":"SUPERSEDED_BY","object":{"id":10865,"text":"ofr82911 - 1982 - Effects of urbanization on the magnitude and frequency of floods on small streams in Tennessee; basic data report no. 2","indexId":"ofr82911","publicationYear":"1982","noYear":false,"title":"Effects of urbanization on the magnitude and frequency of floods on small streams in Tennessee; basic data report no. 2"},"id":1}],"lastModifiedDate":"2013-08-12T10:51:53","indexId":"ofr82911","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1982","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":"82-911","title":"Effects of urbanization on the magnitude and frequency of floods on small streams in Tennessee; basic data report no. 2","docAbstract":"Peak stages, discharges, and rainfall recorded at 22 gaging stations on streams draining small (less than 25 mi super 2) urbanized basins across Tennessee are presented. The gaged basins are in 17 different municipalities with populations ranging between 5,000 and 100,000. The report gives a description of each gaged site along with a data sheet on which peak stages, discharges, and corresponding rainfall are listed. The description gives the station location, type of gage, basin characteristics, and general remarks. (USGS)","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/ofr82911","usgsCitation":"Robbins, C.H., 1982, Effects of urbanization on the magnitude and frequency of floods on small streams in Tennessee; basic data report no. 2: U.S. Geological Survey Open-File Report 82-911, iii, 28 p. :map ;28 cm., https://doi.org/10.3133/ofr82911.","productDescription":"iii, 28 p. :map ;28 cm.","costCenters":[],"links":[{"id":971,"rank":100,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.water.usgs.gov/ofr_82-911","linkFileType":{"id":5,"text":"html"}},{"id":145078,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":276364,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1982/ofr_82-911/pdf/ofr_82-911_a.pdf"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a26e4b07f02db60fce8","contributors":{"authors":[{"text":"Robbins, Clarence H.","contributorId":44159,"corporation":false,"usgs":true,"family":"Robbins","given":"Clarence","email":"","middleInitial":"H.","affiliations":[],"preferred":false,"id":162097,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":11513,"text":"ofr82666D - 1982 - Estimates of undiscovered recoverable resources of total gas by province; statistical background data for U.S. Geological Survey Circular 860","interactions":[],"lastModifiedDate":"2012-02-02T00:06:49","indexId":"ofr82666D","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1982","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":"82-666","chapter":"D","title":"Estimates of undiscovered recoverable resources of total gas by province; statistical background data for U.S. Geological Survey Circular 860","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/ofr82666D","usgsCitation":"Varnes, K.L., Dolton, G., and Charpentier, R., 1982, Estimates of undiscovered recoverable resources of total gas by province; statistical background data for U.S. Geological Survey Circular 860: U.S. Geological Survey Open-File Report 82-666, 18 p., ill., maps ; 28 cm., https://doi.org/10.3133/ofr82666D.","productDescription":"18 p., ill., maps ; 28 cm.","costCenters":[],"links":[{"id":146054,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1982/0666d/report-thumb.jpg"},{"id":39376,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1982/0666d/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a0ce4b07f02db5fca1a","contributors":{"authors":[{"text":"Varnes, K. L.","contributorId":74386,"corporation":false,"usgs":true,"family":"Varnes","given":"K.","email":"","middleInitial":"L.","affiliations":[],"preferred":false,"id":163284,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Dolton, G.L.","contributorId":51722,"corporation":false,"usgs":true,"family":"Dolton","given":"G.L.","email":"","affiliations":[],"preferred":false,"id":163283,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Charpentier, Ronald R.","contributorId":33674,"corporation":false,"usgs":true,"family":"Charpentier","given":"Ronald R.","affiliations":[],"preferred":false,"id":163282,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}} ,{"id":10786,"text":"ofr82609 - 1982 - Aliphatic Hydrocarbons in Surface Sediments of Willapa Bay and Grays Harbor, Washington","interactions":[{"subject":{"id":10786,"text":"ofr82609 - 1982 - Aliphatic Hydrocarbons in Surface Sediments of Willapa Bay and Grays Harbor, Washington","indexId":"ofr82609","publicationYear":"1982","noYear":false,"title":"Aliphatic Hydrocarbons in Surface Sediments of Willapa Bay and Grays Harbor, Washington"},"predicate":"SUPERSEDED_BY","object":{"id":32588,"text":"pp1273B - 1984 - Correlation of paleostructure and sediment deposition in the Madison Limestone and associated rocks in parts of Montana, North Dakota, South Dakota, Wyoming, and Nebraska","indexId":"pp1273B","publicationYear":"1984","noYear":false,"chapter":"B","title":"Correlation of paleostructure and sediment deposition in the Madison Limestone and associated rocks in parts of Montana, North Dakota, South Dakota, Wyoming, and Nebraska"},"id":1}],"supersededBy":{"id":32588,"text":"pp1273B - 1984 - Correlation of paleostructure and sediment deposition in the Madison Limestone and associated rocks in parts of Montana, North Dakota, South Dakota, Wyoming, and Nebraska","indexId":"pp1273B","publicationYear":"1984","noYear":false,"title":"Correlation of paleostructure and sediment deposition in the Madison Limestone and associated rocks in parts of Montana, North Dakota, South Dakota, Wyoming, and Nebraska"},"lastModifiedDate":"2012-02-02T00:06:34","indexId":"ofr82609","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1982","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":"82-609","title":"Aliphatic Hydrocarbons in Surface Sediments of Willapa Bay and Grays Harbor, Washington","docAbstract":"Willapa Bay and Grays Harbor are two adjacent estuaries along the coast of Washington state. Willapa Bay is a recreational area minimally affected by industry; Grays Harbor, on the other hand, is moderately industrialized. Aliphatic hydrocarbons in surface sediments from these two estuaries reflect the differences in human activities. For example, the mean concentration of aliphatic hydrocarbons for seven stations in Willapa Bay is 1,000 ?g/g (relative to organic carbon) while in Grays Harbor this mean concentration for \r\nsix stations is 1,900 ?g/g. The difference is attributed mainly to the greater urban and industrial pollution in Grays Harbor. The gas chromatographic records of aliphatic hydrocarbons also reflect the extent of hydrocarbon pollution by the presence of a chromatographically unresolved mixture of hydrocarbons. This kind of mixture is more evident in sediments from Grays Harbor, and in both estuaries it is more concentrated in sediments collected nearest to urban centers.","language":"ENGLISH","publisher":"Geological Survey (U.S.)","doi":"10.3133/ofr82609","usgsCitation":"Rapp, J.B., Kvenvolden, K., and Clifton, H., 1982, Aliphatic Hydrocarbons in Surface Sediments of Willapa Bay and Grays Harbor, Washington: U.S. Geological Survey Open-File Report 82-609, 14 p., ill., map ;28 cm., https://doi.org/10.3133/ofr82609.","productDescription":"14 p., ill., map ;28 cm.","costCenters":[{"id":595,"text":"U.S. Geological Survey","active":false,"usgs":true}],"links":[{"id":144866,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1982/0609/report-thumb.jpg"},{"id":38584,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1982/0609/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ae0e4b07f02db68805c","contributors":{"authors":[{"text":"Rapp, J. B.","contributorId":28987,"corporation":false,"usgs":true,"family":"Rapp","given":"J.","email":"","middleInitial":"B.","affiliations":[],"preferred":false,"id":161958,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Kvenvolden, K.A.","contributorId":80674,"corporation":false,"usgs":true,"family":"Kvenvolden","given":"K.A.","email":"","affiliations":[],"preferred":false,"id":161960,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Clifton, H.E.","contributorId":44151,"corporation":false,"usgs":true,"family":"Clifton","given":"H.E.","affiliations":[],"preferred":false,"id":161959,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}} ,{"id":11512,"text":"ofr82666B - 1982 - Estimates of Federal ownership of undiscovered oil and gas resources by province; statistical background data for U.S. Geological Survey Circular 860","interactions":[],"lastModifiedDate":"2012-02-02T00:06:49","indexId":"ofr82666B","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1982","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":"82-666","chapter":"B","title":"Estimates of Federal ownership of undiscovered oil and gas resources by province; statistical background data for U.S. Geological Survey Circular 860","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/ofr82666B","usgsCitation":"Varnes, K.L., and Dolton, G., 1982, Estimates of Federal ownership of undiscovered oil and gas resources by province; statistical background data for U.S. Geological Survey Circular 860: U.S. Geological Survey Open-File Report 82-666, 15p. ill., maps ;28 cm., https://doi.org/10.3133/ofr82666B.","productDescription":"15p. ill., maps ;28 cm.","costCenters":[],"links":[{"id":146053,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1982/0666b/report-thumb.jpg"},{"id":39375,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1982/0666b/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4abbe4b07f02db6725dc","contributors":{"authors":[{"text":"Varnes, K. L.","contributorId":74386,"corporation":false,"usgs":true,"family":"Varnes","given":"K.","email":"","middleInitial":"L.","affiliations":[],"preferred":false,"id":163281,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Dolton, G.L.","contributorId":51722,"corporation":false,"usgs":true,"family":"Dolton","given":"G.L.","email":"","affiliations":[],"preferred":false,"id":163280,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":11593,"text":"ofr82831 - 1982 - Fortran '77 programs for computing data fitting functions based on a principle of minimum integrated squared curvature","interactions":[],"lastModifiedDate":"2012-02-02T00:06:49","indexId":"ofr82831","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1982","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":"82-831","title":"Fortran '77 programs for computing data fitting functions based on a principle of minimum integrated squared curvature","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/ofr82831","usgsCitation":"Watts, R., 1982, Fortran '77 programs for computing data fitting functions based on a principle of minimum integrated squared curvature: U.S. Geological Survey Open-File Report 82-831, 42 p., 28 cm., https://doi.org/10.3133/ofr82831.","productDescription":"42 p., 28 cm.","costCenters":[],"links":[{"id":145910,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1982/0831/report-thumb.jpg"},{"id":39452,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1982/0831/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e49d5e4b07f02db5dd9b8","contributors":{"authors":[{"text":"Watts, R.D.","contributorId":94666,"corporation":false,"usgs":true,"family":"Watts","given":"R.D.","email":"","affiliations":[],"preferred":false,"id":163411,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":11594,"text":"ofr82704 - 1982 - Interpretation of Schlumberger DC resistivity data from Gibson Dome-Lockhart Basin study area, San Juan County, Utah","interactions":[],"lastModifiedDate":"2012-02-02T00:06:49","indexId":"ofr82704","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1982","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":"82-704","title":"Interpretation of Schlumberger DC resistivity data from Gibson Dome-Lockhart Basin study area, San Juan County, Utah","docAbstract":"A Schlumberger dc resistivity survey of the Gibson Dome-Lockhart Basin area, San Juan County, Utah, has revealed the following electrical characteristics of the area: (1) the area between the northern part of Davis Canyon and Gibson Dome is electrically quite uniform and resistive at the depth of the Pennsylvanian evaporite deposits, (2) there is a deep conductive anomaly at Horsehead Rock, and (3) there are several shallow and deep electrical anomalies in the vicinity of the Lockhart fault system. No adverse indicators were found for nuclear waste repository siting south of Indian Creek, but additional soundings should be made to increase data density and to extend the survey area southward. The Lockhart fault system appears to have triggered salt dissolution or flow outside the limits of Lockhart Basin; further geophysical work and drilling will be required to understand the origin of the Lockhart Basin structure and its present state of activity. This problem is important because geologic processes that lead to enlargement of the Lockhart Basin structure or to development of similar structures would threaten the integrity of a repository in the Gibson Dome area.","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/ofr82704","usgsCitation":"Watts, R., 1982, Interpretation of Schlumberger DC resistivity data from Gibson Dome-Lockhart Basin study area, San Juan County, Utah: U.S. Geological Survey Open-File Report 82-704, 21 p., ill., maps ;28 cm., https://doi.org/10.3133/ofr82704.","productDescription":"21 p., ill., maps ;28 cm.","costCenters":[],"links":[{"id":145911,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1982/0704/report-thumb.jpg"},{"id":39453,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1982/0704/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4aa7e4b07f02db667072","contributors":{"authors":[{"text":"Watts, R.D.","contributorId":94666,"corporation":false,"usgs":true,"family":"Watts","given":"R.D.","email":"","affiliations":[],"preferred":false,"id":163412,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":11511,"text":"ofr82666C - 1982 - Estimated areas and volumes of sedimentary rock in the United States by province; statistical background data for U.S. Geological Survey Circular 860","interactions":[],"lastModifiedDate":"2012-02-02T00:06:49","indexId":"ofr82666C","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1982","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":"82-666","chapter":"C","title":"Estimated areas and volumes of sedimentary rock in the United States by province; statistical background data for U.S. Geological Survey Circular 860","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/ofr82666C","usgsCitation":"Varnes, K.L., and Dolton, G., 1982, Estimated areas and volumes of sedimentary rock in the United States by province; statistical background data for U.S. Geological Survey Circular 860: U.S. Geological Survey Open-File Report 82-666, 12 p. :ill., maps ;28 cm., https://doi.org/10.3133/ofr82666C.","productDescription":"12 p. :ill., maps ;28 cm.","costCenters":[],"links":[{"id":145886,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1982/0666c/report-thumb.jpg"},{"id":39374,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1982/0666c/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a81e4b07f02db64a1b3","contributors":{"authors":[{"text":"Varnes, K. L.","contributorId":74386,"corporation":false,"usgs":true,"family":"Varnes","given":"K.","email":"","middleInitial":"L.","affiliations":[],"preferred":false,"id":163279,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Dolton, G.L.","contributorId":51722,"corporation":false,"usgs":true,"family":"Dolton","given":"G.L.","email":"","affiliations":[],"preferred":false,"id":163278,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":10785,"text":"ofr8289 - 1982 - Specification for procurement of water-level sensing instrumentation, specification number HIF-I-1","interactions":[],"lastModifiedDate":"2012-02-02T00:06:34","indexId":"ofr8289","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1982","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":"82-89","title":"Specification for procurement of water-level sensing instrumentation, specification number HIF-I-1","docAbstract":"This specification is to communicate to instrument manufacturers the U.S. Geological Survey 's requirements. It covers systems for sensing the elevation of the water surface on open channels, rivers, lakes, reservoirs, storm-sewer pipes, and observation wells at Survey data-collection sites. The signal output (mechanical or electrical) must meet the signal input requirements of analog to digital and digital input recorders in use by the Survey. A classification of stage-sensing systems by common characteristics is used to aid Survey people making system selections. These characteristics are (1) system type (contact or noncontact), (2) sensor type and sensing distance, (3) accuracy, (4) range, (5) power requirements, (6) system size and weight, and (7) data output signal. Acceptable system requirements cover system configurations, signal outputs, materials, operation manuals, detailed environmental conditions, calibration procedures, system accuracy, power requirements, installation limitations, maintainability, safety, and workmanship. An outline of the qualification test procedures and failure criteria are also given. The Hydrologic Instrumentation Facility at NSTL Station, Mississippi will test available systems to determine if they meet the specification in this report for inclusion in the Survey 's 'Qualified Products List'. This list will be used for future procurement of water-level sensing systems by the Survey. 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