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,{"id":4522,"text":"cir940 - 1984 - 1984 annual report on Alaska's mineral resources","interactions":[],"lastModifiedDate":"2012-02-02T00:05:43","indexId":"cir940","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1984","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":307,"text":"Circular","code":"CIR","onlineIssn":"2330-5703","printIssn":"1067-084X","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"940","title":"1984 annual report on Alaska's mineral resources","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/cir940","usgsCitation":"Water Resources Division, U.S. Geological Survey, 1984, 1984 annual report on Alaska's mineral resources: U.S. Geological Survey Circular 940, iv, 54 p. :ill., maps ;28 cm.28 cm., https://doi.org/10.3133/cir940.","productDescription":"iv, 54 p. :ill., maps ;28 cm.28 cm.","costCenters":[],"links":[{"id":117549,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/circ/1984/0940/report-thumb.jpg"},{"id":31580,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/circ/1984/0940/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"53cd4913e4b0b290850eedd1","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":528226,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":4195,"text":"cir913 - 1984 - Water-level and water-quality changes in Great Salt Lake, Utah, 1847-1983","interactions":[],"lastModifiedDate":"2017-02-22T12:05:09","indexId":"cir913","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1984","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":307,"text":"Circular","code":"CIR","onlineIssn":"2330-5703","printIssn":"1067-084X","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"913","title":"Water-level and water-quality changes in Great Salt Lake, Utah, 1847-1983","docAbstract":"<p>The surface level of Great Salt Lake, Utah, fluctuates continuously, primarily in response to climatic factors. During 1847-1982 the lake surface fluctuated between a low of about 4,191 feet and a high of about 4,212 feet above sea level but showed no net change. From September 18, 1982, to June 30, 1983, however, the lake rose 5.2 feet-from about 4,200 to about 4,205 feet above sea level-which is the greatest seasonal rise ever recorded. That rise resulted from considerably greater than average rainfall in 1982, greater than average snowfall during the autumn of 1982 through the spring of 1983, and unseasonably cool weather during that spring.</p><p>Man's activities have had a lesser, but still important effect on the lake level. The lake surface would have been about 5 feet higher in 1983 had there been no consumptive use of water owing to man's activities in the lake basin since 1847. The lake has been divided into two parts by a railroad causeway since 1959. The causeway restricts natural circulation, resulting in a difference of salinity and surface level of the lake across the causeway. The difference in surface level between the two parts of the lake varies both seasonally and annually and was as much as 3.25 feet in 1983.</p><p>The water budget for the Great Salt Lake can be expressed as:</p><p>Inflow = Outflow ± Storage change</p><p>The average annual inflow for 1931-76 was about 2.9 million acre-feet-about 1.9 million acre-feet from surface water, about 900,000 acre-feet from direct precipitation, and about 75,000 acre-feet from ground water. The average annual outflow for the same period, all by evaporation, also was about 2.9 million acre-feet. There was no net change in storage during the period.</p><p>The famed buoyancy of the brine in Great Salt Lake results from a dissolved-mineral content of almost 5 billion tons. More than 2 million additional tons have been added to the lake annually in recent years. The major dissolved ions in the brine are chloride, sulfate, sodium, magnesium, and potassium.</p><p>Prior to completion of the railroad causeway, the salinity of the brine varied inversely with the lake level. Since the causeway divided the lake into two parts, the salinity of the brine in the north part has been relatively constant at or close to saturation. The salinity of the brine in the south part has 1 continued to change inversely with the lake level, but the salinity has been less than it would have been without the causeway.</p>","language":"English","publisher":"U.S. Government Printing Office","publisherLocation":"Washington, D.C.","doi":"10.3133/cir913","usgsCitation":"Arnow, T., 1984, Water-level and water-quality changes in Great Salt Lake, Utah, 1847-1983: U.S. Geological Survey Circular 913, iv, 22 p., https://doi.org/10.3133/cir913.","productDescription":"iv, 22 p.","numberOfPages":"28","costCenters":[{"id":610,"text":"Utah Water Science Center","active":true,"usgs":true}],"links":[{"id":31309,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/circ/1984/0913/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":118279,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/circ/1984/0913/report-thumb.jpg"}],"country":"United States","state":"Utah","otherGeospatial":"Great Salt Lake","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -113.3349609375,\n              40.538851525354666\n            ],\n            [\n              -111.8023681640625,\n              40.538851525354666\n            ],\n            [\n              -111.8023681640625,\n              41.82454867985508\n            ],\n            [\n              -113.3349609375,\n              41.82454867985508\n            ],\n            [\n              -113.3349609375,\n              40.538851525354666\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e49e6e4b07f02db5e782d","contributors":{"authors":[{"text":"Arnow, Ted","contributorId":84733,"corporation":false,"usgs":true,"family":"Arnow","given":"Ted","affiliations":[],"preferred":false,"id":148384,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":4008,"text":"cir897 - 1984 - Formation of solution-subsidence sinkholes above salt beds","interactions":[],"lastModifiedDate":"2012-02-02T00:05:34","indexId":"cir897","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1984","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":307,"text":"Circular","code":"CIR","onlineIssn":"2330-5703","printIssn":"1067-084X","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"897","title":"Formation of solution-subsidence sinkholes above salt beds","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/cir897","usgsCitation":"Ege, J.R., 1984, Formation of solution-subsidence sinkholes above salt beds: U.S. Geological Survey Circular 897, iii, 11 p. :ill., map ;28 cm., https://doi.org/10.3133/cir897.","productDescription":"iii, 11 p. :ill., map ;28 cm.","costCenters":[],"links":[{"id":117479,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/circ/1984/0897/report-thumb.jpg"},{"id":31093,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/circ/1984/0897/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b23e4b07f02db6ae3a2","contributors":{"authors":[{"text":"Ege, John R.","contributorId":69534,"corporation":false,"usgs":true,"family":"Ege","given":"John","email":"","middleInitial":"R.","affiliations":[],"preferred":false,"id":147975,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":3651,"text":"cir850L - 1984 - Changes in the organic material in lakes in the blast zone of Mount St. Helens, Washington","interactions":[],"lastModifiedDate":"2018-02-21T17:41:58","indexId":"cir850L","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1984","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":307,"text":"Circular","code":"CIR","onlineIssn":"2330-5703","printIssn":"1067-084X","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"850","chapter":"L","title":"Changes in the organic material in lakes in the blast zone of Mount St. Helens, Washington","docAbstract":"During several periods of volcanic-ash eruption at Mount St. Helens, Wash., (March 30, May 25-26, May 30-June 2, and June 12-13, 1980) strong winds from the north occurred at high altitudes. As a result, the volcanic ash fell some 50 miles to the south in the Bull Run watershed, the principal water-supply source for the metropolitan area of Portland, Oreg. Water samples collected from three stream sites within the watershed were compared with samples collected during the same season in previous years. No detectable changes were noted in chemical characteristics. Precipitation samples collected immediately after the June 12-13 ash fall ranged in specific conductance from 20 to 41 micromhos per centimeter at 25C and in pH from 4.0 to 4.3 pH units. Stream samples collected during the May-June period ranged in specific conductance from 18 to 28 micromhos per centimeter at 25C and in pH from 6.7 to 7.5 pH units. Volcanic-ash samples were collected and analyzed for particle size, chemical composition, and weight. Significant differences in particle size of ash were found in samples from two separate eruptions. (USGS)","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/cir850L","usgsCitation":"McKnight, D.M., Klein, J.M., and Wissman, R.C., 1984, Changes in the organic material in lakes in the blast zone of Mount St. Helens, Washington: U.S. Geological Survey Circular 850, iv, 26 p. :ill., map ;26 cm., https://doi.org/10.3133/cir850L.","productDescription":"iv, 26 p. :ill., map ;26 cm.","costCenters":[],"links":[{"id":138540,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/circ/1984/0850l/report-thumb.jpg"},{"id":30692,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/circ/1984/0850l/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e49e2e4b07f02db5e4d90","contributors":{"authors":[{"text":"McKnight, Diane M.","contributorId":59773,"corporation":false,"usgs":false,"family":"McKnight","given":"Diane","email":"","middleInitial":"M.","affiliations":[{"id":16833,"text":"INSTAAR, University of Colorado","active":true,"usgs":false}],"preferred":false,"id":147332,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Klein, John M.","contributorId":27036,"corporation":false,"usgs":true,"family":"Klein","given":"John","email":"","middleInitial":"M.","affiliations":[],"preferred":false,"id":147333,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Wissman, Robert C.","contributorId":89119,"corporation":false,"usgs":true,"family":"Wissman","given":"Robert","email":"","middleInitial":"C.","affiliations":[],"preferred":false,"id":147334,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":3517,"text":"cir924 - 1984 - The dangers and handling of hazardous chemicals in the geologic laboratory","interactions":[],"lastModifiedDate":"2012-02-02T00:05:25","indexId":"cir924","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1984","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":307,"text":"Circular","code":"CIR","onlineIssn":"2330-5703","printIssn":"1067-084X","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"924","title":"The dangers and handling of hazardous chemicals in the geologic laboratory","language":"ENGLISH","publisher":"U.S. G.P.O.,","doi":"10.3133/cir924","usgsCitation":"Riedmiller, A., Hauff, P.L., and Mathias, R.W., 1984, The dangers and handling of hazardous chemicals in the geologic laboratory: U.S. Geological Survey Circular 924, iii, 39 p. :ill. ;26 cm., https://doi.org/10.3133/cir924.","productDescription":"iii, 39 p. :ill. ;26 cm.","costCenters":[],"links":[{"id":117112,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/circ/1984/0924/report-thumb.jpg"},{"id":30531,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/circ/1984/0924/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4aaae4b07f02db6689fa","contributors":{"authors":[{"text":"Riedmiller, Alice","contributorId":30214,"corporation":false,"usgs":true,"family":"Riedmiller","given":"Alice","email":"","affiliations":[],"preferred":false,"id":147072,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Hauff, Phoebe L.","contributorId":10402,"corporation":false,"usgs":true,"family":"Hauff","given":"Phoebe","email":"","middleInitial":"L.","affiliations":[],"preferred":false,"id":147071,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Mathias, Richard W.","contributorId":36536,"corporation":false,"usgs":true,"family":"Mathias","given":"Richard","email":"","middleInitial":"W.","affiliations":[],"preferred":false,"id":147073,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":3481,"text":"cir942 - 1984 - Nonprofit sample and core repositories open to the public in the United States","interactions":[{"subject":{"id":20804,"text":"ofr84333 - 1984 - Addresses, telephone numbers, and brief descriptions of publicly available, non-profit samples and core repositories of the United States","indexId":"ofr84333","publicationYear":"1984","noYear":false,"title":"Addresses, telephone numbers, and brief descriptions of publicly available, non-profit samples and core repositories of the United States"},"predicate":"SUPERSEDED_BY","object":{"id":3481,"text":"cir942 - 1984 - Nonprofit sample and core repositories open to the public in the United States","indexId":"cir942","publicationYear":"1984","noYear":false,"title":"Nonprofit sample and core repositories open to the public in the United States"},"id":1}],"lastModifiedDate":"2012-02-02T00:05:38","indexId":"cir942","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1984","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":307,"text":"Circular","code":"CIR","onlineIssn":"2330-5703","printIssn":"1067-084X","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"942","title":"Nonprofit sample and core repositories open to the public in the United States","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/cir942","usgsCitation":"Schmoker, J., Michalski, T.C., and Worl, P.B., 1984, Nonprofit sample and core repositories open to the public in the United States: U.S. Geological Survey Circular 942, v, 102 p. ;26 cm., https://doi.org/10.3133/cir942.","productDescription":"v, 102 p. ;26 cm.","costCenters":[],"links":[{"id":120754,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/circ/1984/0942/report-thumb.jpg"},{"id":30492,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/circ/1984/0942/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4afde4b07f02db696eac","contributors":{"authors":[{"text":"Schmoker, J. W.","contributorId":69964,"corporation":false,"usgs":true,"family":"Schmoker","given":"J. W.","affiliations":[],"preferred":false,"id":147006,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Michalski, Thomas C.","contributorId":97086,"corporation":false,"usgs":true,"family":"Michalski","given":"Thomas","email":"","middleInitial":"C.","affiliations":[],"preferred":false,"id":147007,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Worl, Patricia B.","contributorId":99967,"corporation":false,"usgs":true,"family":"Worl","given":"Patricia","email":"","middleInitial":"B.","affiliations":[],"preferred":false,"id":147008,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":4334,"text":"cir932 - 1984 - Interlaboratory comparison of mineral constituents in a sample from the Herrin (No. 6) coal bed from Illinois","interactions":[],"lastModifiedDate":"2012-02-02T00:05:25","indexId":"cir932","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1984","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":307,"text":"Circular","code":"CIR","onlineIssn":"2330-5703","printIssn":"1067-084X","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"932","title":"Interlaboratory comparison of mineral constituents in a sample from the Herrin (No. 6) coal bed from Illinois","docAbstract":"Approximately 20 kg of the Herrin (No. 6) coal was collected from a strip mine in St. Clair County, Ill. A 10-kg portion was ground to -60 mesh, homogenized, and riffled into 128 splits of 70-80 g each. Homogeneity of these splits was confirmed by moisture, ash, and sulfur analyses of six randomly selected splits. Results of these analyses were within the ASTM (American Society for Testing and Materials) guidelines for interlaboratory precision. Splits of the Herrin (No. 6) coal were then transmitted to more than 30 laboratories for analysis. \r\n\r\nLow-temperature plasma oxidation was used to isolate inorganic matter for quantitative chemical and mineralogical analysis. Despite a wide variation in ashing conditions, only minor variations in ash yields were obtained; these variations were attributed to differences in operating temperature and moisture content. Mineralogical analyses of low-temperature ash (LTA) concentrates prepared by five different laboratories indicated variations within the limits of analytical error. The mean values, in weight percent, for the major minerals are as follows: calcite, 9; quartz, 20; pyrite, 23; kaolinite, 14; and illite+mixed-layer clays, 31. Normative mineralogical calculations and Fourier transform infrared analysis (FTIR) yielded results similar to those obtained from X-ray diffraction (XRD). Choosing appropriate mineral standards was found to be critical for the proper use of analytical techniques such as XRD and FTIR. \r\n\r\nGood interlaboratory agreement was obtained for most major, minor, and trace elements despite differences in analytical procedures and in the type of sample analyzed (coal, high-temperature ash, or LTA). Discrepancies between analyses for zinc, strontium, manganese, and iron may be attributed to sampling inhomogeneity problems. Mossbauer spectroscopy showed that approximately 44 percent of the pyritic sulfur was lost through weathering in the first year after preparation of the interlaboratory sample. Szomolnokite and possibly coquimbite and jarosite were also identified. Scanning electron microscopy studies indicated ubiquitous pyrite framboids and, less commonly, euhedral crystals, skeletal grains, irregularly shaped particles, and vein fillings. Minor accessory minerals such as rare-earth phosphates and possibly silicates, zircon, barium sulfate, titanium oxide, and sphalerite were also found. The textural evidence indicates that the minerals in the banded material are detrital whereas the minerals occurring as vein and pore fillings are authigenic. Magnetic measurements indicate that coal crushed in a steel pulverizer is contaminated by small quantities of abrasion fragments from the crusher, which seriously affect the measured magnetic properties of the coal.","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/cir932","usgsCitation":"Finkelman, R., Fiene, F., Miller, R., and Simon, F., 1984, Interlaboratory comparison of mineral constituents in a sample from the Herrin (No. 6) coal bed from Illinois: U.S. Geological Survey Circular 932, v, 42 p. :ill. ;26 cm., https://doi.org/10.3133/cir932.","productDescription":"v, 42 p. :ill. ;26 cm.","costCenters":[],"links":[{"id":124425,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/circ/1984/0932/report-thumb.jpg"},{"id":31444,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/circ/1984/0932/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ab0e4b07f02db66d3f4","contributors":{"authors":[{"text":"Finkelman, Robert B.","contributorId":38138,"corporation":false,"usgs":false,"family":"Finkelman","given":"Robert B.","affiliations":[{"id":6643,"text":"University of California - Berkeley","active":true,"usgs":false}],"preferred":false,"id":148854,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Fiene, F.L.","contributorId":66237,"corporation":false,"usgs":true,"family":"Fiene","given":"F.L.","email":"","affiliations":[],"preferred":false,"id":148856,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Miller, R.N.","contributorId":100825,"corporation":false,"usgs":true,"family":"Miller","given":"R.N.","email":"","affiliations":[],"preferred":false,"id":148857,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Simon, F.O.","contributorId":41808,"corporation":false,"usgs":true,"family":"Simon","given":"F.O.","email":"","affiliations":[],"preferred":false,"id":148855,"contributorType":{"id":1,"text":"Authors"},"rank":4}]}}
,{"id":3678,"text":"cir922A - 1984 - Assessment of undiscovered conventionally recoverable petroleum resources of the Northwest European region","interactions":[],"lastModifiedDate":"2012-02-02T00:05:24","indexId":"cir922A","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1984","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":307,"text":"Circular","code":"CIR","onlineIssn":"2330-5703","printIssn":"1067-084X","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"922","chapter":"A","title":"Assessment of undiscovered conventionally recoverable petroleum resources of the Northwest European region","docAbstract":"The estimates of undiscovered conventionally recoverable petroleum resources in the northwest European region at probability levels of 95 percent, 5 percent, statistical mean, and mode are for oil (in billions of barrels): 9, 34, 20, and 15; and for gas (in trillions of cubic feet): 92, 258, 167, and 162. The occurrence of petroleum can be accounted for in two distinct geological plays located in the various subbasins of the region. Play I is associated with the distribution of mature source rocks of Late Jurassic age relative to four distinct trapping conditions. The play has been demonstrated productive mostly in the Viking and Central Grabens of the North Sea, where the shale has been buried to optimum depths for the generation of both oil and gas. To the north of 62 ? N. latitude up to the Barents Sea, source rocks become increasingly deeply buried and are interpreted to be dominantly gas prone; a narrow band of potentially oil-prone shales tracks most of the coast of Norway, but water depths in favorable localities commonly range from 600 to 1,200 feet. To the south of the Central Graben, the Jurassic source rocks are either immature or minimally productive because of a change in facies. Undrilled traps remain within the favorable source-rock area, and exploration will continue to challenge the boundaries of conventional wisdom, especially on the Norwegian side where little has .been reported on the geology of the adjoining Bergen High or Horda Basin, though, reportedly, the Jurassic source rocks are missing on the high and are immature in the southern part of the basin. \r\n\r\nPlay II is associated with the distribution of a coal facies of Carboniferous age that is mature for the generation of gas and locally underlies favorable reservoir and sealing rocks. The play is limited largely by facies development to the present area of discovery and production but is limited as well to the southeast into onshore Netherlands and Germany by the unfavorable economics of an increasing nitrogen content in the gas. This increase is apparently caused by excessive temperatures associated with increasing depth of burial of the source rock. \r\n\r\nThe history of discovery in the North Sea would appear to deny the commonly held maxim that large fields are found first and early in the exploration process. However, if the discovery data are examined from the perspective of the award date of each exploration license, then it is clear that the largest fields and most of the reserves have indeed been found early in the exploration process of a particular license. Discoveries made within 1 year of granting the license are on average large giants, and they account for slightly less than two-thirds of the original reserves. Discoveries made within 2 to 5 years of the granting of the license are on average less than giant size and smaller than increment-l-year discoveries by a factor of 4; these fields account for a little less than one-third of the reserves. Those fields found 6 or more years after the granting of the license are relatively small and account for 20 percent of all discoveries but only 4 percent of total original reserves. These data suggest that a measure of an area's exploration maturity is the length of time elapsed since the award of the concession.","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/cir922A","usgsCitation":"Masters, C.D., and Klemme, H.D., 1984, Assessment of undiscovered conventionally recoverable petroleum resources of the Northwest European region: U.S. Geological Survey Circular 922, vi, 22 p. :ill., maps ;26 cm., https://doi.org/10.3133/cir922A.","productDescription":"vi, 22 p. :ill., maps ;26 cm.","costCenters":[],"links":[{"id":124616,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/circ/1984/0922a/report-thumb.jpg"},{"id":30726,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/circ/1984/0922a/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4abae4b07f02db671c62","contributors":{"authors":[{"text":"Masters, Charles D.","contributorId":38969,"corporation":false,"usgs":true,"family":"Masters","given":"Charles","email":"","middleInitial":"D.","affiliations":[],"preferred":false,"id":147395,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Klemme, H. Douglas","contributorId":80653,"corporation":false,"usgs":true,"family":"Klemme","given":"H.","email":"","middleInitial":"Douglas","affiliations":[],"preferred":false,"id":147396,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":4679,"text":"twri03A15 - 1984 - Computation of water-surface profiles in open channels","interactions":[],"lastModifiedDate":"2012-02-02T00:05:31","indexId":"twri03A15","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1984","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":336,"text":"Techniques of Water-Resources Investigations","code":"TWRI","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"03-A15","title":"Computation of water-surface profiles in open channels","docAbstract":"The standard step-backwater method of computing water-surface profiles is described in this chapter. The hydraulic principles and assumptions are reviewed, and the field data requirements are described. Certain special cases of backwater curves and certain special field conditions are discussed in detail. The technique is used to establish or extend stage-discharge ratings; to define areas which will be innundated by flood flows of a given frequency; and to compute profiles through various reaches, including multichannel flows, and past control structures such as bridges, culverts, and road embankments. A brief description of analysis of floodways and effects of encroachments is also presented.","language":"ENGLISH","publisher":"U.S. G.P.O. ;For sale by the Distribution Branch, U.S. Geological Survey,","doi":"10.3133/twri03A15","issn":"0565-596X","usgsCitation":"Davidian, J., 1984, Computation of water-surface profiles in open channels: U.S. Geological Survey Techniques of Water-Resources Investigations 03-A15, x, 48 p. :ill. ;26 cm. Reprinted in 1994., https://doi.org/10.3133/twri03A15.","productDescription":"x, 48 p. :ill. ;26 cm. Reprinted in 1994.","costCenters":[],"links":[{"id":240,"rank":100,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.usgs.gov/twri/twri3-a15/","linkFileType":{"id":5,"text":"html"}},{"id":139151,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b19e4b07f02db6a7baf","contributors":{"authors":[{"text":"Davidian, Jacob","contributorId":80245,"corporation":false,"usgs":true,"family":"Davidian","given":"Jacob","email":"","affiliations":[],"preferred":false,"id":149610,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":4159,"text":"cir904A - 1984 - Geologic and hydrologic characterization and evaluation of the Basin and Range Province relative to the disposal of high-level radioactive waste: Part I, Introduction and guidelines","interactions":[{"subject":{"id":7850,"text":"ofr83759 - 1983 - Geologic and hydrologic characterization and evaluation of the Basin and Range Province relative to the disposal of high-level radioactive waste: Part I, Introduction and guidelines","indexId":"ofr83759","publicationYear":"1983","noYear":false,"title":"Geologic and hydrologic characterization and evaluation of the Basin and Range Province relative to the disposal of high-level radioactive waste: Part I, Introduction and guidelines"},"predicate":"SUPERSEDED_BY","object":{"id":4159,"text":"cir904A - 1984 - Geologic and hydrologic characterization and evaluation of the Basin and Range Province relative to the disposal of high-level radioactive waste: Part I, Introduction and guidelines","indexId":"cir904A","publicationYear":"1984","noYear":false,"chapter":"A","title":"Geologic and hydrologic characterization and evaluation of the Basin and Range Province relative to the disposal of high-level radioactive waste: Part I, Introduction and guidelines"},"id":1}],"lastModifiedDate":"2019-11-07T12:09:06","indexId":"cir904A","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1984","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":307,"text":"Circular","code":"CIR","onlineIssn":"2330-5703","printIssn":"1067-084X","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"904","chapter":"A","title":"Geologic and hydrologic characterization and evaluation of the Basin and Range Province relative to the disposal of high-level radioactive waste: Part I, Introduction and guidelines","docAbstract":"<p>The U.S. Geological Survey's program for geologic and hydrologic evaluation of physiographic provinces to identify areas potentially suitable for locating repository sites for disposal of high-level nuclear wastes was announced to the Governors of the eight States in the Basin and Range Province on May 5, 1981. Representatives of Arizona, California, Idaho, New Mexico, Nevada, Oregon, Texas, and Utah, were invited to cooperate with the Federal Government in the evaluation process. Each Governor was requested to nominate an Earth scientist to represent the State in a province working group composed of State and U.S. Geological Survey representatives. This report, Part I of a three-part report, provides the background, introduction and scope of the study. This part also includes a discussion of geologic and hydrologic guidelines that will be used in the evaluation process and illustrates geohydrologic environments and the effect of individual factors in providing multiple natural barriers to radionuclide migration.</p><p>Part II is a reconnaissance characterization of the geologic and hydrologic factors to be used in the initial screening of the Basin and Range Province. Part III will be the initial evaluation of the Province and will identify regions that appear suitable for further study.</p><p>The plan for study of the Province includes a stepwise screening process by which successively smaller land units are considered in increasing detail. Each step involves characterization of the geology and hydrology and selection of subunits for more intensive characterization. Selection of subunits for further study is by evaluation of geologic and hydrologic conditions following a set of guidelines. By representation on the Province Working Group, the States participate in a consultation and review role in: (1) Establishing geologic and hydrologic guidelines, and (2) characterizing and evaluating the Province. The States also participate in compilation of geologic and hydrologic data used in characterizing the Province.</p><p>The current (1983) needs for a high-level radioactive waste repository include: (1) Disposal in a mined repository; (2) retrievability of the waste for as much as 50 years; and (3) confidence of isolation of the waste from the accessible environment. Isolation of the waste needs to be assured using geologic and hydrologic conditions that: (1) Minimize risk of inadvertent future intrusions by man; (2) minimize the possibility of disturbance by processes that would expose the waste or increase its mobility; and (3) provide a system of natural barriers to the migration of waste by ground water. The guidelines adopted by the Province Working Group are designed to provide a standard with which these conditions can be compared.</p><p>The guidelines can be grouped into four principal categories: (1) Potential host media, (2) ground-water conditions, (3) tectonic conditions, and. (4) occurrence of natural resources. Ideally the host medium constitutes the first natural barrier to migration of radionculides. The host medium ideally should be a rock type that prevents or retards dissolution and transport of radionuclides. Rocks in both the saturated and unsaturated zones may have desirable characteristics for host media. Rocks-other than the host-in the ground-water flow path from the repository ideally should be major barriers to radionuclide migration. Confining beds of low permeability might be present to retard the rate of flow between more permeable beds. Additionally, sorption of radionuclides by materials such as clays and zeolites in the flow path can further retard the flow of radionuclides by several orders of magnitude. Tectonic conditions in an area should not present a probable cause for exhumation or increased mobility of radioactive waste. Natural resources are a factor for consideration because of the problem of future human intrusion and exposure to radioactivity in the quest for minerals, oil, gas, water, and geothermal resources.</p><p>The ultimate evaluation of the suitability of a geohydrologic environment for developing a mined repository needs to assess all geologic and hydrologic characteristics and their interaction in providing confidence that a geohydrologic environment will effectively isolate radionuclides from human access. Several hypothetical settings with typical geohydrologic conditions in the Basin and Range Province are used to illustrate the effect of multiple barriers in the isolation of radionuclides.</p>","language":"English","publisher":"U.S. Government Printing Office","publisherLocation":"Washington, D.C.","doi":"10.3133/cir904A","usgsCitation":"Bedinger, M.S., Sargent, K., and Reed, J., 1984, Geologic and hydrologic characterization and evaluation of the Basin and Range Province relative to the disposal of high-level radioactive waste: Part I, Introduction and guidelines: U.S. Geological Survey Circular 904, viii, 16 p., https://doi.org/10.3133/cir904A.","productDescription":"viii, 16 p.","numberOfPages":"26","costCenters":[{"id":610,"text":"Utah Water Science Center","active":true,"usgs":true}],"links":[{"id":335932,"rank":3,"type":{"id":22,"text":"Related Work"},"url":"https://pubs.usgs.gov/publication/cir904B","text":"Circular 904-B","linkHelpText":"Part II, Geologic and hydrologic 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,{"id":3241,"text":"cir923 - 1984 - Acid precipitation; an annotated bibliography","interactions":[],"lastModifiedDate":"2012-02-02T00:05:21","indexId":"cir923","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1984","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":307,"text":"Circular","code":"CIR","onlineIssn":"2330-5703","printIssn":"1067-084X","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"923","title":"Acid precipitation; an annotated bibliography","docAbstract":"This collection of 1660 bibliographies references on the causes and environmental effects of acidic atmospheric deposition was compiled from computerized literature searches of earth-science and chemistry data bases. Categories of information are (1) atmospheric chemistry (gases and aerosols), (2) precipitation chemistry, (3) transport and deposition (wet and dry), (4) aquatic environments (biological and hydrological), (5) terrestrial environments, (6) effects on materials and structures, (7) air and precipitation monitoring and data collection, and (8) modeling studies. References date from the late 1800 's through December 1981. The bibliography includes short summaries of most documents. Omitted are unpublished manuscripts, publications in press, master 's theses and doctoral dissertations, newspaper articles, and book reviews. Coauthors and subject indexes are included. (USGS)","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/cir923","usgsCitation":"Wiltshire, D.A., and Evans, M.L., 1984, Acid precipitation; an annotated bibliography: U.S. Geological Survey Circular 923, 282 p. ;26 cm., https://doi.org/10.3133/cir923.","productDescription":"282 p. ;26 cm.","costCenters":[],"links":[{"id":117773,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/circ/1984/0923/report-thumb.jpg"},{"id":30237,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/circ/1984/0923/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b04e4b07f02db69928c","contributors":{"authors":[{"text":"Wiltshire, Denise A.","contributorId":78717,"corporation":false,"usgs":true,"family":"Wiltshire","given":"Denise","email":"","middleInitial":"A.","affiliations":[],"preferred":false,"id":146495,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Evans, Margaret L.","contributorId":40968,"corporation":false,"usgs":true,"family":"Evans","given":"Margaret","email":"","middleInitial":"L.","affiliations":[],"preferred":false,"id":146494,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":3800,"text":"cir937 - 1984 - Proceedings of the 1980 workshop of the International Association of Seismology and Physics of the Earth's Interior on the seismic modeling of laterally varying structures: Contributions based on data from the 1978 Saudi Arabian refraction profile","interactions":[],"lastModifiedDate":"2020-05-22T12:55:05.658142","indexId":"cir937","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1984","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":307,"text":"Circular","code":"CIR","onlineIssn":"2330-5703","printIssn":"1067-084X","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"937","title":"Proceedings of the 1980 workshop of the International Association of Seismology and Physics of the Earth's Interior on the seismic modeling of laterally varying structures: Contributions based on data from the 1978 Saudi Arabian refraction profile","docAbstract":"<p>No abstract available.</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/cir937","usgsCitation":"Mooney, W.D., and Prodehl, C., 1984, Proceedings of the 1980 workshop of the International Association of Seismology and Physics of the Earth's Interior on the seismic modeling of laterally varying structures: Contributions based on data from the 1978 Saudi Arabian refraction profile: U.S. Geological Survey Circular 937, iv, 158 p., https://doi.org/10.3133/cir937.","productDescription":"iv, 158 p.","costCenters":[{"id":237,"text":"Earthquake Science Center","active":true,"usgs":true}],"links":[{"id":30870,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/circ/1984/0937/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":120800,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/circ/1984/0937/report-thumb.jpg"}],"country":"Saudi Arabia","geographicExtents":"{\"type\":\"FeatureCollection\",\"features\":[{\"type\":\"Feature\",\"geometry\":{\"type\":\"Polygon\",\"coordinates\":[[[42.77933,16.34789],[42.64957,16.77464],[42.34799,17.07581],[42.27089,17.47472],[41.75438,17.83305],[41.22139,18.6716],[40.93934,19.48649],[40.24765,20.17463],[39.80168,20.33886],[39.1394,21.2919],[39.0237,21.98688],[39.06633,22.57966],[38.49277,23.68845],[38.02386,24.07869],[37.48363,24.28549],[37.15482,24.85848],[37.20949,25.08454],[36.93163,25.60296],[36.6396,25.82623],[36.24914,26.57014],[35.64018,27.37652],[35.13019,28.06335],[34.63234,28.05855],[34.78778,28.60743],[34.83222,28.95748],[34.95604,29.35655],[36.06894,29.19749],[36.50121,29.50525],[36.74053,29.86528],[37.50358,30.00378],[37.66812,30.33867],[37.99885,30.5085],[37.00217,31.50841],[39.00489,32.01022],[39.19547,32.16101],[40.39999,31.88999],[41.88998,31.19001],[44.7095,29.17889],[46.56871,29.09903],[47.45982,29.00252],[47.70885,28.52606],[48.41609,28.552],[48.80759,27.68963],[49.29955,27.46122],[49.47091,27.11],[50.15242,26.68966],[50.21294,26.27703],[50.1133,25.94397],[50.23986,25.60805],[50.52739,25.32781],[50.66056,24.9999],[50.81011,24.75474],[51.11242,24.55633],[51.38961,24.62739],[51.57952,24.2455],[51.61771,24.01422],[52.00073,23.00115],[55.0068,22.49695],[55.20834,22.70833],[55.66666,22],[54.99998,19.99999],[52.00001,19],[49.11667,18.61667],[48.18334,18.16667],[47.46669,17.11668],[47,16.95],[46.74999,17.28334],[46.36666,17.23332],[45.4,17.33334],[45.21665,17.43333],[44.06261,17.41036],[43.79152,17.31998],[43.38079,17.57999],[43.1158,17.08844],[43.21838,16.66689],[42.77933,16.34789]]]},\"properties\":{\"name\":\"Saudi Arabia\"}}]}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a9ee4b07f02db6605a0","contributors":{"authors":[{"text":"Mooney, Walter D. 0000-0002-5310-3631 mooney@usgs.gov","orcid":"https://orcid.org/0000-0002-5310-3631","contributorId":3194,"corporation":false,"usgs":true,"family":"Mooney","given":"Walter","email":"mooney@usgs.gov","middleInitial":"D.","affiliations":[{"id":237,"text":"Earthquake Science Center","active":true,"usgs":true}],"preferred":true,"id":147623,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Prodehl, Claus","contributorId":81082,"corporation":false,"usgs":true,"family":"Prodehl","given":"Claus","email":"","affiliations":[],"preferred":false,"id":147624,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":3979,"text":"cir935 - 1984 - Marine geological and geophysical investigations of the Antarctic continental margin, 1984","interactions":[],"lastModifiedDate":"2012-02-02T00:05:26","indexId":"cir935","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1984","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":307,"text":"Circular","code":"CIR","onlineIssn":"2330-5703","printIssn":"1067-084X","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"935","title":"Marine geological and geophysical investigations of the Antarctic continental margin, 1984","language":"ENGLISH","publisher":"U.S. G.P.O.,","doi":"10.3133/cir935","usgsCitation":"Eittreim, S.L., Cooper, A.K., and and others, 1984, Marine geological and geophysical investigations of the Antarctic continental margin, 1984: U.S. Geological Survey Circular 935, 12 p. :ill., maps ;26 cm., https://doi.org/10.3133/cir935.","productDescription":"12 p. :ill., maps ;26 cm.","costCenters":[],"links":[{"id":120856,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/circ/1984/0935/report-thumb.jpg"},{"id":31064,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/circ/1984/0935/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a1ae4b07f02db606b49","contributors":{"authors":[{"text":"Eittreim, Stephen L.","contributorId":8452,"corporation":false,"usgs":true,"family":"Eittreim","given":"Stephen","email":"","middleInitial":"L.","affiliations":[],"preferred":false,"id":147942,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Cooper, Alan K. acooper@usgs.gov","contributorId":2854,"corporation":false,"usgs":true,"family":"Cooper","given":"Alan","email":"acooper@usgs.gov","middleInitial":"K.","affiliations":[{"id":520,"text":"Pacific Coastal and Marine Science Center","active":true,"usgs":true}],"preferred":true,"id":147941,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"and others","contributorId":127886,"corporation":true,"usgs":false,"organization":"and others","id":528170,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":4314,"text":"cir938 - 1984 - U. S. Geological Survey highlights in marine research","interactions":[],"lastModifiedDate":"2018-03-13T17:38:08","indexId":"cir938","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1984","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":307,"text":"Circular","code":"CIR","onlineIssn":"2330-5703","printIssn":"1067-084X","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"938","title":"U. S. Geological Survey highlights in marine research","docAbstract":"<p>No abstract available.</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/cir938","usgsCitation":"1984, U. S. Geological Survey highlights in marine research: U.S. Geological Survey Circular 938, v, 176 p. :ill., maps ;27 cm., https://doi.org/10.3133/cir938.","productDescription":"v, 176 p. :ill., maps ;27 cm.","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[{"id":552,"text":"San Francisco Bay-Delta","active":false,"usgs":true},{"id":5079,"text":"Pacific Regional Director's Office","active":true,"usgs":true}],"links":[{"id":31424,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/circ/1984/0938/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":117319,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/circ/1984/0938/report-thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4afce4b07f02db696542","contributors":{"editors":[{"text":"Clarke, Samuel H.","contributorId":42958,"corporation":false,"usgs":true,"family":"Clarke","given":"Samuel H.","affiliations":[],"preferred":false,"id":730997,"contributorType":{"id":2,"text":"Editors"},"rank":1}]}}
,{"id":10451,"text":"ofr84948 - 1984 - United States earthquakes, 1948","interactions":[],"lastModifiedDate":"2012-02-02T00:06:27","indexId":"ofr84948","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1984","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":"84-948","title":"United States earthquakes, 1948","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/ofr84948","usgsCitation":"Murphy, L., and Ulrich, F., 1984, United States earthquakes, 1948: U.S. Geological Survey Open-File Report 84-948, 51 p. :maps ;26 cm., https://doi.org/10.3133/ofr84948.","productDescription":"51 p. :maps ;26 cm.","costCenters":[],"links":[{"id":143146,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1984/0948/report-thumb.jpg"},{"id":38322,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1984/0948/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a25e4b07f02db60edea","contributors":{"authors":[{"text":"Murphy, L.M.","contributorId":69969,"corporation":false,"usgs":true,"family":"Murphy","given":"L.M.","email":"","affiliations":[],"preferred":false,"id":161425,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Ulrich, F.P.","contributorId":71983,"corporation":false,"usgs":true,"family":"Ulrich","given":"F.P.","email":"","affiliations":[],"preferred":false,"id":161426,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":8892,"text":"ofr84601 - 1984 - Yukon River ice; freeze-up data (1883-1975)","interactions":[],"lastModifiedDate":"2012-02-02T00:06:16","indexId":"ofr84601","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1984","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":"84-601","title":"Yukon River ice; freeze-up data (1883-1975)","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/ofr84601","usgsCitation":"Fountain, A.G., and Vaughn, B.H., 1984, Yukon River ice; freeze-up data (1883-1975): U.S. Geological Survey Open-File Report 84-601, ii, 51 p. :ill., maps ;28 cm., https://doi.org/10.3133/ofr84601.","productDescription":"ii, 51 p. :ill., maps ;28 cm.","costCenters":[],"links":[{"id":141678,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1984/0601/report-thumb.jpg"},{"id":36460,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1984/0601/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e49d6e4b07f02db5de077","contributors":{"authors":[{"text":"Fountain, A. G.","contributorId":29815,"corporation":false,"usgs":true,"family":"Fountain","given":"A.","email":"","middleInitial":"G.","affiliations":[],"preferred":false,"id":158501,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Vaughn, B. H.","contributorId":63806,"corporation":false,"usgs":true,"family":"Vaughn","given":"B.","email":"","middleInitial":"H.","affiliations":[],"preferred":false,"id":158502,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":8891,"text":"ofr84441 - 1984 - South Cascade Glacier bibliography","interactions":[],"lastModifiedDate":"2012-02-02T00:06:16","indexId":"ofr84441","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1984","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":"84-441","title":"South Cascade Glacier bibliography","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/ofr84441","usgsCitation":"Fountain, A.G., and Fulk, M., 1984, South Cascade Glacier bibliography: U.S. Geological Survey Open-File Report 84-441, i, 13 p. ;28 cm., https://doi.org/10.3133/ofr84441.","productDescription":"i, 13 p. ;28 cm.","costCenters":[],"links":[{"id":141677,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1984/0441/report-thumb.jpg"},{"id":36459,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1984/0441/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e49e6e4b07f02db5e7472","contributors":{"authors":[{"text":"Fountain, A. G.","contributorId":29815,"corporation":false,"usgs":true,"family":"Fountain","given":"A.","email":"","middleInitial":"G.","affiliations":[],"preferred":false,"id":158499,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Fulk, M.A.","contributorId":43353,"corporation":false,"usgs":true,"family":"Fulk","given":"M.A.","email":"","affiliations":[],"preferred":false,"id":158500,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":8888,"text":"ofr83926 - 1984 - Geologic and hydrologic data collected during 1976-1983 at the Sheffield low-level radioactive waste disposal site and adjacent areas, Sheffield, Illinois","interactions":[],"lastModifiedDate":"2012-02-02T00:06:18","indexId":"ofr83926","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1984","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":"83-926","title":"Geologic and hydrologic data collected during 1976-1983 at the Sheffield low-level radioactive waste disposal site and adjacent areas, Sheffield, Illinois","docAbstract":"Hydrogeologic studies were conducted at the low-level radioactive-waste disposal site near Sheffield, Illinois, from 1976-84. Data in this report include water levels in wells, lake stages, inorganic, organic, and radiometric chemical analyses of ground and surface water, hydraulic conductivities of glacial materials, grain-size distribution, clay and carbonate mineralogy, and cation exchange capacities of the glacial materials. Also included are results of petrographic analyses, physical measurements of wells, stratigraphy and lithology of cores collected from test wells, and horizontal coordinates of wells.","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/ofr83926","usgsCitation":"Foster, J., Garklavs, G., and Mackey, G., 1984, Geologic and hydrologic data collected during 1976-1983 at the Sheffield low-level radioactive waste disposal site and adjacent areas, Sheffield, Illinois: U.S. Geological Survey Open-File Report 83-926, iv, 339 p. :ill. ;28 cm., https://doi.org/10.3133/ofr83926.","productDescription":"iv, 339 p. :ill. ;28 cm.","costCenters":[],"links":[{"id":142691,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1983/0926/report-thumb.jpg"},{"id":36456,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1983/0926/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b1ae4b07f02db6a81f0","contributors":{"authors":[{"text":"Foster, J.B.","contributorId":12040,"corporation":false,"usgs":true,"family":"Foster","given":"J.B.","email":"","affiliations":[],"preferred":false,"id":158493,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Garklavs, George","contributorId":87139,"corporation":false,"usgs":true,"family":"Garklavs","given":"George","email":"","affiliations":[],"preferred":false,"id":158495,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Mackey, G.W.","contributorId":46529,"corporation":false,"usgs":true,"family":"Mackey","given":"G.W.","email":"","affiliations":[],"preferred":false,"id":158494,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":8878,"text":"ofr8414 - 1984 - Logs and correlation of drill holes within the South Kawishiwi Intrusion, Duluth Complex, northeastern Minnesota","interactions":[],"lastModifiedDate":"2022-09-26T18:05:33.613945","indexId":"ofr8414","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1984","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":"84-14","title":"Logs and correlation of drill holes within the South Kawishiwi Intrusion, Duluth Complex, northeastern Minnesota","docAbstract":"<p>No abstract available.</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr8414","usgsCitation":"Foose, M.P., 1984, Logs and correlation of drill holes within the South Kawishiwi Intrusion, Duluth Complex, northeastern Minnesota: U.S. Geological Survey Open-File Report 84-14, Report: 232 p.; 1 Plate: 17.74 × 22.32 inches, https://doi.org/10.3133/ofr8414.","productDescription":"Report: 232 p.; 1 Plate: 17.74 × 22.32 inches","costCenters":[],"links":[{"id":36441,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1984/0014/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":142634,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1984/0014/report-thumb.jpg"},{"id":407332,"rank":4,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_27485.htm","linkFileType":{"id":5,"text":"html"}},{"id":36442,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1984/0014/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"country":"United States","state":"Minnesota","otherGeospatial":"Duluth Complex","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -92.3,\n              47.502\n            ],\n            [\n              -91.711,\n              47.502\n            ],\n            [\n              -91.711,\n              47.907\n            ],\n            [\n              -92.3,\n              47.907\n            ],\n            [\n              -92.3,\n              47.502\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a69e4b07f02db63c66d","contributors":{"authors":[{"text":"Foose, M. P.","contributorId":97075,"corporation":false,"usgs":true,"family":"Foose","given":"M.","email":"","middleInitial":"P.","affiliations":[],"preferred":false,"id":158475,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":8868,"text":"ofr84633 - 1984 - Characteristics of some silver-, and base metal-bearing, epithermal deposits of Mexico and Peru","interactions":[],"lastModifiedDate":"2018-10-22T08:50:04","indexId":"ofr84633","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1984","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":"84-633","title":"Characteristics of some silver-, and base metal-bearing, epithermal deposits of Mexico and Peru","docAbstract":"<h1>Introduction</h1>\n<p>Lithotectonic, mineralogical, and geochemical data on two silver- and base metal-bearing deposits from Peru and two from Mexico are compiled to facilitate comparisons with other epithermal deposits. Silver and base metal-bearing deposits of Mexico and Peru constitute an important portion of the world silver production derived from shallow, vein-type deposits hosted in volcanic rocks. Although these deposits are generally similar to epithermal deposits of Nevada and Colorado in the western United States, they have some important differences. Because of this, data on the geological attributes of these deposits are very useful for developing models of ore formation that can be used in mineral exploration. The data collected for this compilation are presented in the following pages in summaries of the important characteristics of each deposit. This compilation, which shows the complexities in the geology of epithermal ore deposits in Mexico and Peru, serves as a basis for further comparisons among epithermal deposits throughout the world. The case studies provide data useful to geologists and exploration!'sts interested in developing models of ore formation to be used in exploration for mineral deposits of this type. The deposits described in this report are the Guanajuato district of Guanajuato, Mexico, the Pachuca-Real del Monte district of Hidalgo, Mexico, the Colqui district of Lima, Peru, and the Julcani district of Huancavelica, Peru.</p>\n<p>Although many characteristics of the geology and geochemistry of this type of deposit were considered, the most important criterion for choosing these deposits was that they have substantial quantities of precious- and base-metal mineralization. Additional criteria for selecting the deposits were that they be hosted primarily by calc-alkaline volcanic rocks of intermediate to silicic composition and that they be younger than Tertiary in age. Many deposits in Mexico and Peru and other parts of Central and South America were excluded because the literature describing the districts is not readily available. Furthermore, many districts have not been examined in detail or the information available is of limited geological scope. The four districts that are compiled in this report were chosen because they are described in abundant literature dating from early mining reports on the general geology and mineralogy to very recent data on detailed geochemical and mineralogical studies. They were chosen as being fairly typical, classic examples of near-surface, low-temperature vein deposits as described by Lindgren (1928) in his treatise on ore deposits (Mineral deposits, McGraw-Hill, 1049 p.). These deposits are similar in aspects of their geology and geochemistry to many of the famous, epithermal silver mining districts in Colorado and Nevada including Creede, Colorado, Tonapah, Nevada, and the Sunnyside Mine of the Eureka district, Colorado, and, in the special case of Julcani, to Summitville, Colorado, and Goldfield, Nevada. The characteristics that distinguish them include overall size, production and alteration assemblage. The information documented in each summary will be used in a forthcoming series of papers on the comparative anatomy of precious and base metal deposits in North and South America.</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr84633","usgsCitation":"Foley, N.K., 1984, Characteristics of some silver-, and base metal-bearing, epithermal deposits of Mexico and Peru: U.S. Geological Survey Open-File Report 84-633, 35 p., https://doi.org/10.3133/ofr84633.","productDescription":"35 p.","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[{"id":245,"text":"Eastern Mineral and Environmental Resources Science Center","active":true,"usgs":true}],"links":[{"id":142811,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1984/0633/report-thumb.jpg"},{"id":36439,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1984/0633/report.pdf","text":"Report","size":"471.64 KB","linkFileType":{"id":1,"text":"pdf"},"description":"Report"}],"country":"Mexico, Peru","state":"Guanajuato, Hidalgo. 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,{"id":8219,"text":"ofr84854 - 1984 - Regional structural setting of Yucca Mountain, southwestern Nevada, and late Cenozoic rates of tectonic activity in part of the southwestern Great Basin, Nevada and California","interactions":[],"lastModifiedDate":"2012-02-02T00:06:08","indexId":"ofr84854","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1984","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":"84-854","title":"Regional structural setting of Yucca Mountain, southwestern Nevada, and late Cenozoic rates of tectonic activity in part of the southwestern Great Basin, Nevada and California","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/ofr84854","usgsCitation":"Carr, W.J., 1984, Regional structural setting of Yucca Mountain, southwestern Nevada, and late Cenozoic rates of tectonic activity in part of the southwestern Great Basin, Nevada and California: U.S. Geological Survey Open-File Report 84-854, iv, 114 p. :ill., maps ;28 cm., https://doi.org/10.3133/ofr84854.","productDescription":"iv, 114 p. :ill., maps ;28 cm.","costCenters":[],"links":[{"id":141327,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1984/0854/report-thumb.jpg"},{"id":35849,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1984/0854/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a60e4b07f02db634e15","contributors":{"authors":[{"text":"Carr, W. J.","contributorId":9245,"corporation":false,"usgs":true,"family":"Carr","given":"W.","email":"","middleInitial":"J.","affiliations":[],"preferred":false,"id":157363,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":10540,"text":"ofr84515 - 1984 - Liquefaction potential in the central Mississippi Valley","interactions":[{"subject":{"id":10540,"text":"ofr84515 - 1984 - Liquefaction potential in the central Mississippi Valley","indexId":"ofr84515","publicationYear":"1984","noYear":false,"title":"Liquefaction potential in the central Mississippi Valley"},"predicate":"SUPERSEDED_BY","object":{"id":35391,"text":"b1832 - 1988 - Liquefaction potential in the central Mississippi Valley","indexId":"b1832","publicationYear":"1988","noYear":false,"title":"Liquefaction potential in the central Mississippi Valley"},"id":1}],"supersededBy":{"id":35391,"text":"b1832 - 1988 - Liquefaction potential in the central Mississippi Valley","indexId":"b1832","publicationYear":"1988","noYear":false,"title":"Liquefaction potential in the central Mississippi Valley"},"lastModifiedDate":"2020-03-02T14:48:00","indexId":"ofr84515","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1984","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":"84-515","title":"Liquefaction potential in the central Mississippi Valley","docAbstract":"<p>No abstract available.</p>","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Reston, VA","doi":"10.3133/ofr84515","usgsCitation":"Obermeier, S., 1984, Liquefaction potential in the central Mississippi Valley: U.S. Geological Survey Open-File Report 84-515, 86 p., https://doi.org/10.3133/ofr84515.","productDescription":"86 p.","costCenters":[],"links":[{"id":142452,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1984/0515/report-thumb.jpg"},{"id":372801,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1984/0515/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b15e4b07f02db6a4f92","contributors":{"authors":[{"text":"Obermeier, S. F.","contributorId":17602,"corporation":false,"usgs":true,"family":"Obermeier","given":"S. F.","affiliations":[],"preferred":false,"id":161566,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":8215,"text":"ofr85185 - 1984 - Index of surface-water stations in Texas, January 1985","interactions":[],"lastModifiedDate":"2016-08-12T13:39:10","indexId":"ofr85185","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1984","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":"85-185","title":"Index of surface-water stations in Texas, January 1985","docAbstract":"<p>The U.S. Geological Survey's investigations of the water resources of Texas are conducted in cooperation with the Texas Department of Water Resources, river authorities, cities, counties, U.S. Army Corps of Engineers, U.S. Bureau of Reclamation, International Boundary and Water Commission, and others.</p>\n<p>As of January 1, 1984, 404 streamflow, 89 reservoir-contents, 32 stage, 10 crest-stage partial-record, 2 periodic discharge through range, 31 flood-hydrograph partial-record, 15 flood-profile partial-record, 41 low-flow partial-record, 11 tide-level, 49 daily chemical-quality, 26 continuous-recording water-quality, 100 periodic biological, 19 lake surveys, 170 periodic organic and (or) nutrient, 3 periodic insecticide, 57 periodic pesticide, 25 automatic sampler, 152 periodic minor elements, 147 periodic chemical-quality y 102 periodic physical-organic, 7 continuous-recording four-parameter water-quality, 3 sediment, 40 periodic sediment, 28 continuous-recording temperature, and 38 national stream-quality accounting network stations were in operation. Plate 1 shows the location of surface-water streamflow or reservoir content and chemical-quality or sediment stations in Texas. Plate 2 shows the location of partial-record surface-water stations.</p>\n<p>This index shows the station number -and name, latitude and longitude, type of data collected, and the office principally responsible for the data collection (table 1). An 8-digit permanent numerical designation for gaging stations has been adopted on a nationwide basis; stations are numbered and listed in downstream order. In the downstream direction along the main stem, all stations on a tributary entering above a main-stem station are listed before that station. A tributary entering between two main-stem stations is listed between them. A similar order is followed in listing stations on first rank, second rank, and other ranks of tributaries. To indicate the rank of any tributary on which a gaging station is situated and the stream to which it is an immediate tributary, each indention in the listing of gaging stations represent one rank. This downstream order and system of indention show which gaging stations are on tributaries between any two stations on a main stem and the rank of the tributary on which each gaging station is situated. On plates 1 and 2, the 8-digit station number is abbreviated because of space limitation.</p>","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Austin, TX","doi":"10.3133/ofr85185","usgsCitation":"Carrillo, E., Buckner, H., and Rawson, J., 1984, Index of surface-water stations in Texas, January 1985: U.S. Geological Survey Open-File Report 85-185, Report: ii, 17 p.; 2 Plates: 17.73 x 16.72 inches and 17.87 x 16.82 inches, https://doi.org/10.3133/ofr85185.","productDescription":"Report: ii, 17 p.; 2 Plates: 17.73 x 16.72 inches and 17.87 x 16.82 inches","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[{"id":583,"text":"Texas Water Science 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