Nine uranium deposits occur in a small area vest of Clancey,Jefferson County, Mont. These deposits are all in or near silicifiedfracture zones in quarts monsonite and related rocks of the Boulderbatholith. The deposits contain pockets of uranium minerals in cavities in brecciated silicified rock. The primary uranium mineral pitch-blende has been found in one pod. Secondary uranium minerals occur as fracture linings and in pore spaces in and adjacent to the silicified zones.
Uranium in the Clancey district was deposited probably during oneof the later of at least four periods of silicification. The quartsmonsonite, rather than the younger alaskitic dike rocks, is the host rock of the deposits.
Newmont Mining Corp. has leased the properties containing theuranium deposits and has begun development of one of these deposits.
","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr52129","usgsCitation":"Roberts, W.A., and Gude, A.J., 1952, Uranium-bearing deposits west of Clancey, Jefferson County, Montana: U.S. Geological Survey Open-File Report 52-129, Report: iii, 31 p.; 5 Figures: 30.37 x 22.30 inches or smaller, https://doi.org/10.3133/ofr52129.","productDescription":"Report: iii, 31 p.; 5 Figures: 30.37 x 22.30 inches or smaller","costCenters":[],"links":[{"id":486816,"rank":7,"type":{"id":29,"text":"Figure"},"url":"https://pubs.usgs.gov/of/1952/0129/figure-7.pdf","text":"Figure 7","linkFileType":{"id":1,"text":"pdf"}},{"id":486815,"rank":6,"type":{"id":29,"text":"Figure"},"url":"https://pubs.usgs.gov/of/1952/0129/figure-6.pdf","text":"Figure 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New York. each belt contains a known magnetite deposit, partly explored through diamond drilling by the U.S. Bureau of Mines. The Brandy Brook Northwest deposit is a body of low-grade to medium-grade ore, possibly of lathlike shape. The Silver Pond deposit has no commercial interest at the moment. One of more promising magnetic anomalies remain to be tested by drilling.
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The original contained a number of photographs that have been omitted; the titles of the photographs are given in the body of the text. Wherever possible, bibliographic references have been checked, and the full titles given. References given in footnotes in the original have been collected and added at the end of each section as a bibliography.
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","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Reston, VA","doi":"10.3133/ofr5260","usgsCitation":"Hackman, R., 1952, Photogeologic maps of the Elk Ridge 1 and 8 quadrangles, Utah: U.S. Geological Survey Open-File Report 52-60, 2 Plates: 24.30 x 29.60 in., https://doi.org/10.3133/ofr5260.","productDescription":"2 Plates: 24.30 x 29.60 in.","costCenters":[],"links":[{"id":171630,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1952/0060/report-thumb.jpg"},{"id":364680,"rank":2,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1952/0060/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":364681,"rank":3,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1952/0060/plate-2.pdf","linkFileType":{"id":1,"text":"pdf"}}],"country":"United States","state":"Utah","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4adbe4b07f02db685ed6","contributors":{"authors":[{"text":"Hackman, Robert J.","contributorId":30999,"corporation":false,"usgs":true,"family":"Hackman","given":"Robert J.","affiliations":[],"preferred":false,"id":224792,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":3761,"text":"cir180 - 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1952 - Reconnaissance for radioactive deposits along the upper Porcupine and lower Coleen Rivers, northeastern Alaska","interactions":[],"lastModifiedDate":"2012-02-02T00:05:28","indexId":"cir185","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1952","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":"185","title":"Reconnaissance for radioactive deposits along the upper Porcupine and lower Coleen Rivers, northeastern Alaska","language":"ENGLISH","publisher":"[U.S. Geological Survey],","doi":"10.3133/cir185","usgsCitation":"White, M.G., 1952, Reconnaissance for radioactive deposits along the upper Porcupine and lower Coleen Rivers, northeastern Alaska: U.S. Geological Survey Circular 185, iii (i.e. ii), 13 p. :maps, tables. ;27 cm., https://doi.org/10.3133/cir185.","productDescription":"iii (i.e. ii), 13 p. :maps, tables. ;27 cm.","costCenters":[],"links":[{"id":117677,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/circ/1952/0185/report-thumb.jpg"},{"id":30260,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/circ/1952/0185/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a74e4b07f02db6444e0","contributors":{"authors":[{"text":"White, Max Gregg","contributorId":91841,"corporation":false,"usgs":true,"family":"White","given":"Max","email":"","middleInitial":"Gregg","affiliations":[],"preferred":false,"id":146545,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":3265,"text":"cir195 - 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Geological Survey Open-File Report 52-154, 156 p., https://doi.org/10.3133/ofr52154.","productDescription":"156 p.","costCenters":[],"links":[{"id":178303,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"}],"edition":"Superceded by: B-1011","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ae1e4b07f02db688951","contributors":{"authors":[{"text":"Thurston, W. R.","contributorId":9277,"corporation":false,"usgs":true,"family":"Thurston","given":"W.","email":"","middleInitial":"R.","affiliations":[],"preferred":false,"id":243127,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":71187,"text":"tei140 - 1952 - Uranium and thorium deposits in east-central Idaho and southwestern Montana","interactions":[],"lastModifiedDate":"2012-02-02T00:14:03","indexId":"tei140","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1952","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":337,"text":"Trace Elements Investigations","code":"TEI","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"140","title":"Uranium and thorium deposits in east-central Idaho and southwestern Montana","language":"ENGLISH","doi":"10.3133/tei140","usgsCitation":"Trites, A.F., and Tooker, E.W., 1952, Uranium and thorium deposits in east-central Idaho and southwestern Montana (Part 1): U.S. Geological Survey Trace Elements Investigations 140, 98 p. : maps ; 28 cm., https://doi.org/10.3133/tei140.","productDescription":"98 p. : maps ; 28 cm.","costCenters":[],"links":[{"id":256738,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/tei/140/report.pdf","size":"3490","linkFileType":{"id":1,"text":"pdf"}},{"id":256739,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/tei/140/report-thumb.jpg"}],"edition":"Part 1","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a19e4b07f02db605caf","contributors":{"authors":[{"text":"Trites, Albert F. Jr.","contributorId":40652,"corporation":false,"usgs":true,"family":"Trites","given":"Albert","suffix":"Jr.","email":"","middleInitial":"F.","affiliations":[],"preferred":false,"id":283783,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Tooker, Edwin Wilson","contributorId":33295,"corporation":false,"usgs":true,"family":"Tooker","given":"Edwin","email":"","middleInitial":"Wilson","affiliations":[],"preferred":false,"id":283782,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":51117,"text":"ofr5250 - 1952 - Recharge of Texas' underground water reservoirs","interactions":[],"lastModifiedDate":"2012-02-02T00:11:27","indexId":"ofr5250","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1952","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":"52-50","title":"Recharge of Texas' underground water reservoirs","language":"ENGLISH","doi":"10.3133/ofr5250","usgsCitation":"George, W., 1952, Recharge of Texas' underground water reservoirs: U.S. Geological Survey Open-File Report 52-50, 8 p., https://doi.org/10.3133/ofr5250.","productDescription":"8 p.","costCenters":[],"links":[{"id":179073,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b15e4b07f02db6a4c4e","contributors":{"authors":[{"text":"George, W.O.","contributorId":41886,"corporation":false,"usgs":true,"family":"George","given":"W.O.","email":"","affiliations":[],"preferred":false,"id":242975,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":13472,"text":"ofr52172 - 1952 - Clay, near Nenana, Alaska","interactions":[],"lastModifiedDate":"2024-05-08T18:46:07.500206","indexId":"ofr52172","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1952","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":"52-172","title":"Clay, near Nenana, Alaska","docAbstract":"The clay deposit here described is located on the west side of the Alaska Railroad about 3.7 miles south of Nenana in N.E. 1/4 Sec. 3, T. 5 S., R. 8 W. (see figure 1). The surface of the deposit has a relief of less than 10 feet and is covered by grasses, brush, and trees of various species.
No abstract available.
","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr5248","usgsCitation":"Flint, A.E., 1952, Description of rock formations and minerals from holes drilled in Highland area, Wisconsin: U.S. Geological Survey Open-File Report 52-48, 31 p., https://doi.org/10.3133/ofr5248.","productDescription":"31 p.","costCenters":[],"links":[{"id":493132,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1952/0048/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":146026,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1952/0048/report-thumb.jpg"}],"country":"United 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In this part of the report a general account of the operation will be developed. The details will be found in subsequent parts of the report. At this point a statement of the general objective and some mention of the plans for reaching it are in order.
The purpose of the Passamaquoddy survey was to determine the submarine geology in certain areas of Passamaquoddy and Cobscook Bays--the sea-bottom topography, the bedrock topography, the thickness of sediment overlying the bedrock beneath the sea, and the type of sediment. The information is needed for the planning of major engineering structures that may be built in the area. It developed in planning the study that detailed surveys could be limited to several areas where dams may be located.
To determine bottom or bedrock topography, elevations of each were determined by sonic methods at a number of closely spaced locations (about 400 feet apart), evenly distributed on range lines 1,000 or 800 feet apart, in each of eight areas. Contour lines were then drawn to produce the desired topographic maps. Sonic soundings are necessarily referred to the existing water surface. To ascertain specific elevations in an area of large tidal variations is a complex problem. The details are discussed in the section on Vertical Control by Charles E. Knox (part 8). The basic datum is mean low water as determined by the U. S. Coast and Geodetic Survey.
Equally important is the accurate positioning horizontally of each sounding location or fix. All such positioning was by the use of the standard three point fix procedure, using sextants. A net of shore points tied to the first-order control net of the Coast and Geodetic Survey was set up for this purpose, and all positions were thus accurately located. These problems are discussed in a section on Horizontal Control by Norman Duckworth (part 7).
The general planning was done in conferences held in May 1951 at the Boston office of the Corps of Engineers, and in Eastport, Maine, after a brief reconnaissance of the area. A detailed account of the conferences is given in a memorandum by Herman J. Kropper of the New England Division, Corps of Engineers, reproduced in this report as part 4. Detailed survey procedures were developed on May 18, 1951, at a conference attended by P. J. A. Scott and Norman Duckworth of the Corps of Engineers and W. O. Smith of the Geological Survey.
In order to make the necessary geophysical interpretation of the sound records, adequate geologic control had to be established. A preliminary field
study of the geology was made by G. G. Parker of the Geological Survey during the period May 15-17, 1951. Subsequently Dr. T. E. Upson of the Geological Survey made the detailed geologic study required for the project.
Two sonar units were used for the survey. One was a low-frequency high-power sonar unit developed by the Edo Corp. to meet specifications established by the Geological Survey. It was used to collect the bulk of the bedrock and bottom data. The other, of higher frequency and lower power, was manufactured by Bludworth Marine, Inc., end was required for adequate determination of water depths in shoal areas. The Edo equipment is described by Dr. Charles E. Mongan, Jr., in part 6 of this report.
","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr52140","collaboration":"Prepared in cooperation with the New England Division Corps of Engineers, U.S. Army","usgsCitation":"Smith, W.O., and Upson, J., 1952, Preliminary report on the Passamaquoddy bedrock survey, July-August, 1951: U.S. Geological Survey Open-File Report 52-140, Report: ii, 49 p.; Plates: 14.88 x 10.12 inches and 13.48 x 19.59 inches, https://doi.org/10.3133/ofr52140.","productDescription":"Report: ii, 49 p.; Plates: 14.88 x 10.12 inches and 13.48 x 19.59 inches","costCenters":[],"links":[{"id":396611,"rank":4,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1952/0140/plate-2.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":396610,"rank":3,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1952/0140/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":396609,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1952/0140/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":148479,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1952/0140/report-thumb.jpg"}],"country":"Canada, United States","state":"Maine","city":"Eastport","otherGeospatial":"Passamaquoddy Bay","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"type\": \"Polygon\",\n \"coordinates\": [\n [\n [\n -67.15393066406249,\n 44.85489529604183\n ],\n [\n -66.82708740234375,\n 44.85489529604183\n ],\n [\n -66.82708740234375,\n 45.17622870105657\n ],\n [\n -67.15393066406249,\n 45.17622870105657\n ],\n [\n -67.15393066406249,\n 44.85489529604183\n ]\n ]\n ]\n }\n }\n ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4aafe4b07f02db66c9be","contributors":{"authors":[{"text":"Smith, William Ogden","contributorId":20337,"corporation":false,"usgs":true,"family":"Smith","given":"William","email":"","middleInitial":"Ogden","affiliations":[],"preferred":false,"id":172145,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Upson, J. E.","contributorId":49342,"corporation":false,"usgs":true,"family":"Upson","given":"J. E.","affiliations":[],"preferred":false,"id":172146,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":12436,"text":"ofr525 - 1952 - A field method for the determination of traces of cobalt in soils","interactions":[{"subject":{"id":12436,"text":"ofr525 - 1952 - A field method for the determination of traces of cobalt in soils","indexId":"ofr525","publicationYear":"1952","noYear":false,"title":"A field method for the determination of traces of cobalt in soils"},"predicate":"SUPERSEDED_BY","object":{"id":36126,"text":"b1152 - 1963 - Analytical methods used in geochemical exploration by the U.S. Geological Survey","indexId":"b1152","publicationYear":"1963","noYear":false,"title":"Analytical methods used in geochemical exploration by the U.S. Geological Survey"},"id":1}],"supersededBy":{"id":36126,"text":"b1152 - 1963 - Analytical methods used in geochemical exploration by the U.S. Geological Survey","indexId":"b1152","publicationYear":"1963","noYear":false,"title":"Analytical methods used in geochemical exploration by the U.S. Geological Survey"},"lastModifiedDate":"2012-02-02T00:06:30","indexId":"ofr525","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1952","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":"52-5","title":"A field method for the determination of traces of cobalt in soils","language":"ENGLISH","publisher":"s.n.,","doi":"10.3133/ofr525","usgsCitation":"Almond, H., 1952, A field method for the determination of traces of cobalt in soils: U.S. Geological Survey Open-File Report 52-5, 6 p. ;27 cm., https://doi.org/10.3133/ofr525.","productDescription":"6 p. ;27 cm.","costCenters":[],"links":[{"id":143730,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b24e4b07f02db6aebd8","contributors":{"authors":[{"text":"Almond, Hy","contributorId":50138,"corporation":false,"usgs":true,"family":"Almond","given":"Hy","email":"","affiliations":[],"preferred":false,"id":166134,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":16326,"text":"ofr52160 - 1952 - Geology of the Alaska-Juneau lode system, Alaska","interactions":[],"lastModifiedDate":"2012-02-02T00:07:12","indexId":"ofr52160","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1952","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":"52-160","title":"Geology of the Alaska-Juneau lode system, Alaska","docAbstract":"The Alaska-Juneau lode system for many years was one of the world\u0019s leading gold-producing areas. Total production from the years 1893 to 1946 has amounted to about 94 million dollars, with principal values in contained gold but with some silver and lead values. The principal mine is the Alaska-Juneau mine, from which the lode system takes its name.\r\n\r\nThe lode system is a part of a larger gold-bearing belt, generally referred to as the Juneau gold belt, along the western border of the Coast Range batholith.\r\n\r\nThe rocks of the Alaska-Juneau lode system consist of a monoclinal sequence of steeply northeasterly dipping volcanic, state, and schist rocks, all of which have been metamorphosed by dynamic and thermal processes attendant with the intrusion of the Coast Range batholith. The rocks form a series of belts that trend northwest parallel to the Coast Range. In addition to the Coast Range batholith lying a mile to the east of the lode system, there are numerous smaller intrusives, all of which are sill-like in form and are thus conformable to the regional structure.\r\n\r\nThe bedded rocks are Mesozoic in age; the Coast Range batholith is Upper Jurassic and Lower Cretaceous in age. Some of the smaller intrusives pre-date the batholith, others post-date it. All of the rocks are cut by steeply dipping faults.\r\n\r\nThe Alaska-Juneau lode system is confined exclusively to the footwall portion of the Perseverance slate band. The slate band is composed of black slate and black phyllite with lesser amounts of thin-bedded quartzite. Intrusive into the slate band are many sill-like bodies of rocks generally referred to as meta-gabbro.\r\n\r\nThe gold deposits of the lode system are found both within the slate rocks and the meta-gabbro rocks, and particularly in those places where meta-gabbro bodies interfinger with slate. Thus the ore bodies are found in and near the terminations of meta-gabbro bodies.\r\n\r\nThe ore bodies are quartz stringer-lodes composed of a great number of quartz veins from 6 inches to 3 feet wide and extending along their strike and dip for several tens to hundreds of feet. In addition to quartz, the only other vein gangue mineral is ankerite. It occurs in small amounts along the borders of the quartz veins. Metallic vein minerals, in addition to native gold, are, in order of decreasing abundance, pyrrhotite, galena, sphalerite, and arsenopyrite. In the aggregate the metallic minerals comprise only 1 to 2 percent of the total amount of vein material.\r\n\r\nThe wall rock, particularly the meta-gabbro, was profoundly altered by the vein-forming processes. The principal effects on the meta-gabbro were the addition of large amounts of soda, potash, titanium, carbon dioxide, and phosphorous, and the removal of considerable quantities of iron, magnesia, lime, and combined water. Silica also may have been decreased. The mineralogical changes involved in the alteration were the development of biotite and ankerite at the expense of original hornblende and feldspar, resulting in a brown-colored biotite- and ankerite-rich rock. The slates are relatively unaffected by the vein-forming processes.\r\n\r\nBecause of their small size, relatively low grade, and discontinuity, no attempt has been made to mine any individual vein. The prevailing practice has been to mine large blocks of ground by a system of modified block-caving, followed by hand sorting to remove the barren country rock from the gold-bearing quartz prior to milling.","language":"ENGLISH","publisher":"s.n.,","doi":"10.3133/ofr52160","usgsCitation":"Twenhofel, W.S., 1952, Geology of the Alaska-Juneau lode system, Alaska: U.S. Geological Survey Open-File Report 52-160, 175 p. ill., 2 folded maps ;29 cm., https://doi.org/10.3133/ofr52160.","productDescription":"175 p. ill., 2 folded maps ;29 cm.","costCenters":[],"links":[{"id":149434,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1952/0160/report-thumb.jpg"},{"id":45251,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1952/0160/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":45252,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1952/0160/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ad5e4b07f02db6836e9","contributors":{"authors":[{"text":"Twenhofel, William Stephens","contributorId":15597,"corporation":false,"usgs":true,"family":"Twenhofel","given":"William","email":"","middleInitial":"Stephens","affiliations":[],"preferred":false,"id":172633,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ]}