{"pageNumber":"148","pageRowStart":"3675","pageSize":"25","recordCount":4111,"records":[{"id":70011186,"text":"70011186 - 1983 - Rare-earth element geochemistry and the origin of andesites and basalts of the Taupo Volcanic Zone, New Zealand","interactions":[],"lastModifiedDate":"2013-01-21T08:47:03","indexId":"70011186","displayToPublicDate":"1983-01-01T00:00:00","publicationYear":"1983","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1213,"text":"Chemical Geology","active":true,"publicationSubtype":{"id":10}},"title":"Rare-earth element geochemistry and the origin of andesites and basalts of the Taupo Volcanic Zone, New Zealand","docAbstract":"Two types of basalt (a high-Al basalt associated with the rhyolitic centres north of Taupo and a \"low-Al\" basalt erupted from Red Crater, Tongariro Volcanic Centre) and five types of andesite (labradorite andesite, labradorite-pyroxene andesite, hornblende andesite, pyroxene low-Si andesite and olivine andesite/low-Si andesite) occur in the Taupo Volcanic Zone (TVZ), North Island, New Zealand. Rare-earth abundances for both basalts and andesites are particularly enriched in light rare-earth elements. High-Al basalts are more enriched than the \"low-Al\" basalt and have values comparable to the andesites. Labradorite and labradorite-pyroxene andesites all have negative Eu anomalies and hornblende andesites all have negative Ce anomalies. The former is probably due to changing plagioclase composition during fractionation and the latter to late-stage hydration of the magma. Least-squares mixing models indicate that neither high-Al nor \"low-Al\" basalts are likely sources for labradorite/labradorite-pyroxene andesites. High-Al basalts are considered to result from fractionation of olivine and clinopyroxene from a garnet-free peridotite at the top of the mantle wedge. Labradorite/labradorite-pyroxene andesites are mainly associated with an older NW-trending arc. The source is likely to be garnet-free but it is not certain whether the andesites result from partial melting of the top of the subducting plate or a hydrated lower portion of the mantle wedge. Pyroxene low-Si andesites probably result from cumulation of pyroxene and calcic plagioclase within labradorite-pyroxene andesites, and hornblende andesites by late-stage hydration of labradorite-pyroxene andesite magma. Olivine andesites, low-Si andesites and \"low-Al\" basalts are related to the NNE-trending Taupo-Hikurangi arc structure. Although the initial source material is different for these lavas they have probably undergone a similar history to the labradorite/labradorite-pyroxene andesites. All lavas show evidence of crustal contamination. ?? 1983.","largerWorkType":{"id":2,"text":"Article"},"largerWorkTitle":"Chemical Geology","largerWorkSubtype":{"id":10,"text":"Journal Article"},"language":"English","publisher":"Elsevier","doi":"10.1016/0009-2541(83)90058-X","issn":"00092541","usgsCitation":"Cole, J.W., Cashman, K.V., and Rankin, P., 1983, Rare-earth element geochemistry and the origin of andesites and basalts of the Taupo Volcanic Zone, New Zealand: Chemical Geology, v. 38, no. 3-4, p. 255-274, https://doi.org/10.1016/0009-2541(83)90058-X.","startPage":"255","endPage":"274","numberOfPages":"20","costCenters":[],"links":[{"id":266112,"type":{"id":10,"text":"Digital Object Identifier"},"url":"https://dx.doi.org/10.1016/0009-2541(83)90058-X"},{"id":221428,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"38","issue":"3-4","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"505a9529e4b0c8380cd81838","contributors":{"authors":[{"text":"Cole, J. W.","contributorId":81315,"corporation":false,"usgs":true,"family":"Cole","given":"J.","email":"","middleInitial":"W.","affiliations":[],"preferred":false,"id":360486,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Cashman, K. V.","contributorId":16831,"corporation":false,"usgs":true,"family":"Cashman","given":"K.","email":"","middleInitial":"V.","affiliations":[],"preferred":false,"id":360485,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Rankin, P.C.","contributorId":6723,"corporation":false,"usgs":true,"family":"Rankin","given":"P.C.","email":"","affiliations":[],"preferred":false,"id":360484,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":1000173,"text":"1000173 - 1983 - Seasonal food of juvenile lake trout in U.S. waters of Lake Ontario","interactions":[],"lastModifiedDate":"2016-03-31T15:06:50","indexId":"1000173","displayToPublicDate":"1983-01-01T00:00:00","publicationYear":"1983","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":2330,"text":"Journal of Great Lakes Research","active":true,"publicationSubtype":{"id":10}},"title":"Seasonal food of juvenile lake trout in U.S. waters of Lake Ontario","docAbstract":"<p><span>Stomach contents of 3,554 lake trout (</span><i>Salvelinus namaycush</i><span>), 100 to 449 mm in total length, captured with bottom trawls during April through October 1978&ndash;81 along the south shore of Lake Ontario were examined. Invertebrates appeared to be an important food of lake trout less than 200 mm long but were only occasionally eaten by larger fish. For all seasons and size groups of juvenile lake trout combined, the slimy sculpin (</span><i>Cottus cognatus</i><span>) was the principal forage fish, making up 42% (by weight) of identifiable fish remains. Young-of-the-year slimy sculpins were a major food of recently stocked yearling lake trout during July through October. Alewives (</span><i>Alosa pseudoharengus</i><span>) were the principal forage during April and May, and made up 28% (by weight) of the identifiable fish remains. They were rarely eaten during July and August, however, when lake trout remained in the hypolimnion and alewives were above it. Over 99% of the alewives eaten from April through August were yearlings and over 99% eaten during October were young-of-the-year. Rainbow smelt (</span><i>Osmerus mordax</i><span>) were the primary forage during July and August, but contributed only a small part of the diet during other seasons; overall, they made up 25% of identifiable fish remains. Johnny darters (</span><i>Etheostoma nigrum</i><span>) made up 4% of identifiable fish remains and were most common in stomachs of small lake trout during October.</span></p>","language":"English","publisher":"Elsevier","doi":"10.1016/S0380-1330(83)71911-8","usgsCitation":"Elrod, J.H., 1983, Seasonal food of juvenile lake trout in U.S. waters of Lake Ontario: Journal of Great Lakes Research, v. 9, no. 3, p. 396-402, https://doi.org/10.1016/S0380-1330(83)71911-8.","productDescription":"7 p.","startPage":"396","endPage":"402","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[{"id":324,"text":"Great Lakes Science Center","active":true,"usgs":true}],"links":[{"id":133221,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"9","issue":"3","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a0ce4b07f02db5fc397","contributors":{"authors":[{"text":"Elrod, Joseph H.","contributorId":72737,"corporation":false,"usgs":true,"family":"Elrod","given":"Joseph","email":"","middleInitial":"H.","affiliations":[],"preferred":false,"id":308186,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":70195580,"text":"70195580 - 1983 - A Canada goose project in Connecticut","interactions":[],"lastModifiedDate":"2023-10-11T01:10:16.48669","indexId":"70195580","displayToPublicDate":"1981-01-01T00:00:00","publicationYear":"1983","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1320,"text":"The Connecticut Warbler","printIssn":"1077-0283","active":true,"publicationSubtype":{"id":10}},"title":"A Canada goose project in Connecticut","docAbstract":"<p>It wasn't so long ago that the wild cries of Canada geese overhead were enough to draw most people out of their homes to look skyward. It was a rare sound heard only in the spring and fall when migrating flocks of these magnificent birds marked the change of the seasons. But today the sound is less delightful to growing numbers of people as goose populations have become permanent residents of the Northeast and caused numerous problems.</p><p>Non-migratory flocks of Canada geese are now present from Cape Cod to Virginia. According to the Atlantic Flyway Council, these geese have provoked nuisance complaints from local communities in every one of the states involved, except Delaware. Delaware has had problems in the past but they are presently under control. These resident populations cause numerous sanitation problems in local communities. Examples are accumulations of feathers and droppings, odor, noise, landscape and crop destruction, the decoying-in of additional geese, and overfertilization of ponds, thus causing algal growth and concerns about health problems, especially in swimming and other recreational areas. </p>","language":"English","publisher":"Connecticut Ornithological Association","usgsCitation":"Converse, K.A., 1983, A Canada goose project in Connecticut: The Connecticut Warbler, v. 1, no. 3, p. 36-38.","productDescription":"3 p.","startPage":"36","endPage":"38","costCenters":[{"id":456,"text":"National Wildlife Health Center","active":true,"usgs":true}],"links":[{"id":351893,"rank":2,"type":{"id":15,"text":"Index Page"},"url":"https://www.ctbirding.org/publications/the-connecticut-warbler/"},{"id":351894,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United States","state":"Connecticut","county":"Fairfield 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Kathryn A. kathy_converse@usgs.gov","contributorId":16802,"corporation":false,"usgs":true,"family":"Converse","given":"Kathryn","email":"kathy_converse@usgs.gov","middleInitial":"A.","affiliations":[],"preferred":false,"id":729349,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":5221782,"text":"5221782 - 1982 - Organochlorine residues in bats after a forest spraying with DDT","interactions":[],"lastModifiedDate":"2018-01-07T17:00:50","indexId":"5221782","displayToPublicDate":"2010-06-16T12:19:23","publicationYear":"1982","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":2900,"text":"Northwest Science","onlineIssn":"2161-9859","printIssn":"0029-344X","active":true,"publicationSubtype":{"id":10}},"title":"Organochlorine residues in bats after a forest spraying with DDT","docAbstract":"<p>Background levels of DDT and its metabolites (ZDDT) were extremely low or not detected in five species of forest-dwelling bats in northeastern Oregon, i.e., areas not sprayed with DDT in 1974. Other organochlorine pesticides were rarely found and no polychlotinated biphenyls (PCBs) were detected at any time during the study. Four of five species of bats showed significant changes in Z:DDT residues in, their carcasses following the single DDT spray application. <i>Myotis californicus</i> and <i>M. volans</i> showed the highest post-spray carcass residues, 6.90 and 6.21 ppm (wet weight). respectively. <i>Lasionycteris noctivagans</i> and <i>Eptesicus fuscus</i> also showed an increase; however, <i>M. evotis</i> exhibited no significant post-spray change. By 1977 (3 years post-spray), residues declined and only <i>M. californicus</i> and <i>M. volans</i> contained levels that were significantly above those in the nonspray (control) area. We are uncertain if the elevated residue levels resulting from the DDT-spray project adversely affected any of the bats. An attempt to relate bat carcass ZDDT residues to food habits, through analysis of stomach contents, yielded no clear relationships.</p>","language":"English","publisher":"Northwest Science Association","usgsCitation":"Henny, C.J., Maser, C., Whitaker, J., and Kaiser, T.E., 1982, Organochlorine residues in bats after a forest spraying with DDT: Northwest Science, v. 56, no. 4, p. 329-337.","productDescription":"9 p.","startPage":"329","endPage":"337","costCenters":[{"id":531,"text":"Patuxent Wildlife Research Center","active":true,"usgs":true}],"links":[{"id":193510,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"},{"id":350354,"rank":2,"type":{"id":15,"text":"Index Page"},"url":"https://www.northwestscience.org/page-937324","text":"<i>Northwest Science</i> homepage"}],"volume":"56","issue":"4","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ae5e4b07f02db68a801","contributors":{"authors":[{"text":"Henny, Charles J. 0000-0001-7474-350X hennyc@usgs.gov","orcid":"https://orcid.org/0000-0001-7474-350X","contributorId":3461,"corporation":false,"usgs":true,"family":"Henny","given":"Charles","email":"hennyc@usgs.gov","middleInitial":"J.","affiliations":[{"id":289,"text":"Forest and Rangeland Ecosys Science Center","active":true,"usgs":true}],"preferred":true,"id":334669,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Maser, Chris","contributorId":13324,"corporation":false,"usgs":false,"family":"Maser","given":"Chris","email":"","affiliations":[{"id":16722,"text":"US Bureau of Land Management","active":true,"usgs":false}],"preferred":false,"id":334670,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Whitaker, John O. Jr.","contributorId":64356,"corporation":false,"usgs":true,"family":"Whitaker","given":"John O.","suffix":"Jr.","affiliations":[],"preferred":false,"id":334671,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Kaiser, T. Earl","contributorId":84826,"corporation":false,"usgs":true,"family":"Kaiser","given":"T.","email":"","middleInitial":"Earl","affiliations":[],"preferred":false,"id":334672,"contributorType":{"id":1,"text":"Authors"},"rank":4}]}}
,{"id":5221785,"text":"5221785 - 1982 - Fall and winter homesite use by wolves in northeastern Minnesota","interactions":[],"lastModifiedDate":"2023-11-15T01:19:25.502508","indexId":"5221785","displayToPublicDate":"2010-06-16T12:19:23","publicationYear":"1982","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1163,"text":"Canadian Field-Naturalist","active":true,"publicationSubtype":{"id":10}},"title":"Fall and winter homesite use by wolves in northeastern Minnesota","docAbstract":"Post-abandonment homesite use by wolves (Canis lupus) was studied by radio-tracking and simulated howling in two packs in Superior National Forest, Minnesota.  Pups, yearlings, and adults returned intermittently to former homesites up to four months after abandonment, usually after prolonged separation from the pack in early fall.  Returns sometimes exceeded one week.  Preferred summer homesites were revisited most frequently.  Visits declined as the season progressed either because attempts to relocate the pack were not facilitated, or simply because separations became rare. While temporarily at homesites, single wolves replied significantly more to simulated howling than when anywhere else, suggesting that homesites may provide reassurance for separated wolves.","language":"English","publisher":"Ottawa Field-Naturalists' Club","usgsCitation":"Harrington, F., and Mech, L., 1982, Fall and winter homesite use by wolves in northeastern Minnesota: Canadian Field-Naturalist, v. 96, no. 1, p. 79-84.","productDescription":"6 p.","startPage":"79","endPage":"84","numberOfPages":"6","costCenters":[{"id":531,"text":"Patuxent Wildlife Research Center","active":true,"usgs":true}],"links":[{"id":422581,"rank":2,"type":{"id":15,"text":"Index Page"},"url":"https://www.biodiversitylibrary.org/part/354767"},{"id":196978,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"96","issue":"1","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e49d8e4b07f02db5df472","contributors":{"authors":[{"text":"Harrington, F.H.","contributorId":14524,"corporation":false,"usgs":true,"family":"Harrington","given":"F.H.","email":"","affiliations":[],"preferred":false,"id":334678,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Mech, L.D. 0000-0003-3944-7769","orcid":"https://orcid.org/0000-0003-3944-7769","contributorId":75466,"corporation":false,"usgs":false,"family":"Mech","given":"L.D.","email":"","affiliations":[],"preferred":false,"id":334679,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":5200024,"text":"5200024 - 1982 - A.B.A. Checklist: Birds of Continental United States and Canada","interactions":[],"lastModifiedDate":"2012-02-02T00:15:18","indexId":"5200024","displayToPublicDate":"2009-06-08T16:49:39","publicationYear":"1982","noYear":false,"publicationType":{"id":4,"text":"Book"},"title":"A.B.A. Checklist: Birds of Continental United States and Canada","docAbstract":"The 'Summary' in this edition of the A BA Checklist has been greatly expanded to include all properly documented records for each accidental species.  These records are published, except for a very few recent ones which are in press or in preparation.  Emphasis is on records supported by specimens or photographs, but sight records are also included. To make these accounts more useful to researchers, a reference has been given for each record.  All records, except those identified as '(photo)' or '(specimen)', or by some other type of objective evidence, are sight records.  Because of the interest shown in this section of the Checklist, coverage has not been confined to accidental species (defined as those which have occurred fewer than ten times in the ABA Checklist area during the twentieth century).  Accounts are also given for selected rare visitors and native species.  Two of the primary references are abbreviated in the accounts: Audubon Field Notes-AFN, and American Birds-AB.","language":"English","publisher":"American Birding Association","publisherLocation":"Austin Texas","usgsCitation":"Keith, G., Balch, L., Gibson, D., McCaskie, R., Robbins, C., Small, A., Sykes, P., and Tucker, J., 1982, A.B.A. Checklist: Birds of Continental United States and Canada, 90.","productDescription":"90","numberOfPages":"90","costCenters":[{"id":531,"text":"Patuxent Wildlife Research Center","active":true,"usgs":true}],"links":[{"id":201035,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b15e4b07f02db6a4a20","contributors":{"authors":[{"text":"Keith, G.S.","contributorId":40319,"corporation":false,"usgs":true,"family":"Keith","given":"G.S.","email":"","affiliations":[],"preferred":false,"id":326826,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Balch, L.G.","contributorId":31502,"corporation":false,"usgs":true,"family":"Balch","given":"L.G.","email":"","affiliations":[],"preferred":false,"id":326825,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Gibson, D.D.","contributorId":104441,"corporation":false,"usgs":true,"family":"Gibson","given":"D.D.","email":"","affiliations":[],"preferred":false,"id":326831,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"McCaskie, R.G.","contributorId":103386,"corporation":false,"usgs":true,"family":"McCaskie","given":"R.G.","email":"","affiliations":[],"preferred":false,"id":326830,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"Robbins, C.S.","contributorId":53907,"corporation":false,"usgs":true,"family":"Robbins","given":"C.S.","email":"","affiliations":[],"preferred":false,"id":326827,"contributorType":{"id":1,"text":"Authors"},"rank":5},{"text":"Small, A.","contributorId":84876,"corporation":false,"usgs":true,"family":"Small","given":"A.","email":"","affiliations":[],"preferred":false,"id":326829,"contributorType":{"id":1,"text":"Authors"},"rank":6},{"text":"Sykes, P.W. Jr.","contributorId":107385,"corporation":false,"usgs":true,"family":"Sykes","given":"P.W.","suffix":"Jr.","email":"","affiliations":[],"preferred":false,"id":326832,"contributorType":{"id":1,"text":"Authors"},"rank":7},{"text":"Tucker, J.A.","contributorId":57992,"corporation":false,"usgs":true,"family":"Tucker","given":"J.A.","email":"","affiliations":[],"preferred":false,"id":326828,"contributorType":{"id":1,"text":"Authors"},"rank":8}]}}
,{"id":11630,"text":"ofr82740 - 1982 - Diatremes of the Hopi Buttes, Arizona; chemical and statistical analyses","interactions":[],"lastModifiedDate":"2012-02-02T00:06:30","indexId":"ofr82740","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1982","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":330,"text":"Open-File Report","code":"OFR","onlineIssn":"2331-1258","printIssn":"0196-1497","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"82-740","title":"Diatremes of the Hopi Buttes, Arizona; chemical and statistical analyses","docAbstract":"Lacustrine sediments deposited in maar lakes of the Hopi Buttes diatremes are hosts for uranium mineralization of as much as 1500 ppm. The monchiquites and limburgite turfs erupted from the diatremes are distinguished from normal alkalic basalts of the Colorado Plateau by their extreme silica undersaturation and high water, TiO2, and P2O5 contents. Many trace elements are also unusually abundant, including Ag, As, Ba, Be, Ce, Dy, Eu, F, Gd, Hf, La, Nd, Pb, Rb, Se, Sm, Sn, Sr, Ta, Tb, Th, U, V, Zn, and Zr. \r\n\r\nThe lacustrine sediments, which consist predominantly of travertine and clastic rocks, are the hosts for syngenetic and epigenetic uranium mineralization of as much as 1500 ppm uranium. Fission track maps show the uranium to be disseminated within the travertine and clastic rocks, and although microprobe analyses have not, as yet, revealed discrete uranium-bearing phases, the clastic rocks show a correlation of high Fe, Ti, and P with areas of high U. Correlation coefficients show that for the travertines, clastics, and limburgite ruffs, Mo, As, Sr, Co, and V appear to have the most consistent and strongest correlations with uranium. Many elements, including many of the rare-earth elements, that are high in these three rocks are also high in the monchiquites, as compared to the average crustal abundance for the respective rock type. This similar suite of anomalous elements, which includes such immobile elements as the rare earths, suggests that Fluids which deposited the travertines were related to the monchiquitic magma. The similar age of about 5 m.y. for both the lake beds and the monchiquites also appears to support this source for the mineralizing fluids.","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/ofr82740","usgsCitation":"Wenrich, K., and Mascarenas, J., 1982, Diatremes of the Hopi Buttes, Arizona; chemical and statistical analyses: U.S. Geological Survey Open-File Report 82-740, iv, 131 p., ill. ;28 cm., https://doi.org/10.3133/ofr82740.","productDescription":"iv, 131 p., ill. ;28 cm.","costCenters":[],"links":[{"id":143780,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1982/0740/report-thumb.jpg"},{"id":39490,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1982/0740/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a9ae4b07f02db65dac8","contributors":{"authors":[{"text":"Wenrich, K. J.","contributorId":40203,"corporation":false,"usgs":true,"family":"Wenrich","given":"K. J.","affiliations":[],"preferred":false,"id":163475,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Mascarenas, J. F.","contributorId":71179,"corporation":false,"usgs":true,"family":"Mascarenas","given":"J. F.","affiliations":[],"preferred":false,"id":163476,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":8141,"text":"ofr82743 - 1982 - Radioactive mineral spring precipitates, their analytical and statistical data and the uranium connection","interactions":[],"lastModifiedDate":"2012-02-02T00:06:13","indexId":"ofr82743","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1982","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":330,"text":"Open-File Report","code":"OFR","onlineIssn":"2331-1258","printIssn":"0196-1497","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"82-743","title":"Radioactive mineral spring precipitates, their analytical and statistical data and the uranium connection","docAbstract":"Major radioactive mineral springs are probably related to deep zones of active metamorphism in areas of orogenic tectonism. The most common precipitate is travertine, a chemically precipitated rock composed chiefly of calcium carbonate, but also containing other minerals. The mineral springs are surface manifestations of hydrothermal conduit systems which extend downward many kilometers to hot source rocks. Conduits are kept open by fluid pressure exerted by carbon dioxide-charged waters rising to the surface propelled by heat and gas (CO2 and steam) pressure. \r\n\r\nOn reaching the surface, the dissolved carbon dioxide is released from solution, and calcium carbonate is precipitated. Springs also contain sulfur species (for example, H2S and HS-), and radon, helium and methane as entrained or dissolved gases. The HS- ion can react to form hydrogen sulfide gas, sulfate salts, and native sulfur. Chemical salts and native sulfur precipitate at the surface. The sulfur may partly oxidize to produce detectable sulfur dioxide gas. \r\n\r\nRadioactivity is due to the presence of radium-226, radon-222, radium-228, and radon-220, and other daughter products of uranium-238 and thorium-232. Uranium and thorium are not present in economically significant amounts in most radioactive spring precipitates. \r\n\r\nMost radium is coprecipitated at the surface with barite. Barite (barium sulfate) forms in the barium-containing spring water as a product of the oxidation of sulfur species to sulfate ions. The relatively insoluble barium sulfate precipitates and removes much of the radium from solution. Radium coprecipitates to a lesser extent with manganese-barium- and iron-oxy hydroxides. \r\n\r\nR-mode factor analysis of abundances of elements suggests that 65 percent of the variance of the different elements is affected by seven factors interpreted as follows: (1) Silica and silicate contamination and precipitation; (2) Carbonate travertine precipitation; (3) Radium coprecipitation; (4) Evaporite precipitation; (5) Hydrous limonite precipitation and coprecipitated elements including uranium; (6) Rare earth elements deposited with detrital contamination (?); (7) Metal carbonate adsorption and precipitation. \r\n\r\nEconomically recoverable minerals occurring at some localities in spring precipitates are ores of iron, manganese, sulfur, tungsten and barium and ornamental travertine.\r\n\r\nContinental radioactive mineral springs occur in areas of crustal thickening caused by overthrusting of crustal plates, and intrusion and metamorphism. Sedimentary rocks on the lower plate are trapped between the plates and form a zone of metamorphism. Connate waters, carbonate rocks and organic-carbon-bearing rocks react to extreme pressure and temperature to produce carbon dioxide, and steam. Fractures are forced open by gas and fluid pressures. Deep-circulating meteoric waters then come in contact with the reactive products, and a hydrothermal cell forms. When hot mineral-charged waters reach the surface they form the familiar hot mineral springs. Hot springs also occur in relation to igneous intrusive action or volcanism both of which may be products of the crustal plate overthrusting. Uranium and thorium in the sedimentary rocks undergoing metamorphism are sometimes mobilized, but mobilization is generally restricted to an acid hydrothermal environment; much is redeposited in favorable environments in the metamorphosed sediments. Radium and radon, which are highly mobile in both acid and alkaline aqueous media move upward into the hydrothermal cell and to the surface.","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/ofr82743","usgsCitation":"Cadigan, R.A., and Felmlee, J., 1982, Radioactive mineral spring precipitates, their analytical and statistical data and the uranium connection: U.S. Geological Survey Open-File Report 82-743, iv, 127 p. ill., map ;28 cm., https://doi.org/10.3133/ofr82743.","productDescription":"iv, 127 p. ill., map ;28 cm.","costCenters":[],"links":[{"id":142134,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1982/0743/report-thumb.jpg"},{"id":35744,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1982/0743/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4adae4b07f02db685961","contributors":{"authors":[{"text":"Cadigan, R. A.","contributorId":57844,"corporation":false,"usgs":true,"family":"Cadigan","given":"R.","email":"","middleInitial":"A.","affiliations":[],"preferred":false,"id":157217,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Felmlee, J.K.","contributorId":106114,"corporation":false,"usgs":true,"family":"Felmlee","given":"J.K.","email":"","affiliations":[],"preferred":false,"id":157218,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":8139,"text":"ofr82491 - 1982 - Geochemical reconnaissance for uranium occurrences in the Notch Peak intrusive area, House Range, Millard County, Utah","interactions":[],"lastModifiedDate":"2012-02-02T00:06:13","indexId":"ofr82491","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1982","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":330,"text":"Open-File Report","code":"OFR","onlineIssn":"2331-1258","printIssn":"0196-1497","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"82-491","title":"Geochemical reconnaissance for uranium occurrences in the Notch Peak intrusive area, House Range, Millard County, Utah","docAbstract":"Samples collected from the contact metamorphic zone of the Notch Peak intrusive area, House Range, Millard County, Utah, indicate the occurrence of low-grade uranium and thorium ore. Maximum abundances in the altered mineralized rocks in the contact zone are 450 ppm uranium and 480 ppm thorium. Interpretation of factor analysis of the spectrochemical and delayed neutron analytical data suggests the presence of five geological factors which account for 82 percent of element covariance of 34 elements in 61 samples. The factors are identified as (1) limestone source rock reactions; (2) monzonite source rock reactions; (3) hydrothermal element group 1; (4) rare earth group; and (5) hydrothermal element group 2. The last factor effects the distribution of, primarily, beryllium, uranium, copper, molybdenum, tungsten, niobium, and secondarily, thorium, tin, and zinc; it is identified as the prime mineralization factor. \r\n\r\nThe Notch Peak intrusive area has been a tungsten producing area since before the 1940's and the location of small-scale gold placer operations. This reconnaissance study was a 'follow-up' of uranium anomaly data which were developed during the U.S. Dept. of Energy National Uranium Resource Evaluation (NURE) program in 1978-80.","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/ofr82491","usgsCitation":"Cadigan, R.A., and Robinson, K., 1982, Geochemical reconnaissance for uranium occurrences in the Notch Peak intrusive area, House Range, Millard County, Utah: U.S. Geological Survey Open-File Report 82-491, iii, 57 p., ill., maps ;28 cm., https://doi.org/10.3133/ofr82491.","productDescription":"iii, 57 p., ill., maps ;28 cm.","costCenters":[],"links":[{"id":142132,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1982/0491/report-thumb.jpg"},{"id":35742,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1982/0491/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b23e4b07f02db6ade91","contributors":{"authors":[{"text":"Cadigan, R. A.","contributorId":57844,"corporation":false,"usgs":true,"family":"Cadigan","given":"R.","email":"","middleInitial":"A.","affiliations":[],"preferred":false,"id":157214,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Robinson, Keith","contributorId":80277,"corporation":false,"usgs":true,"family":"Robinson","given":"Keith","affiliations":[],"preferred":false,"id":157215,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":7859,"text":"ofr82830 - 1982 - Postglacial volcanic deposits at Glacier Peak, Washington, and potential hazards from future eruptions; a preliminary report","interactions":[],"lastModifiedDate":"2012-02-02T00:06:08","indexId":"ofr82830","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1982","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":330,"text":"Open-File Report","code":"OFR","onlineIssn":"2331-1258","printIssn":"0196-1497","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"82-830","title":"Postglacial volcanic deposits at Glacier Peak, Washington, and potential hazards from future eruptions; a preliminary report","docAbstract":"Eruptions and other geologic events at Glacier Peak volcano in northern Washington have repeatedly affected areas near the volcano as well as areas far downwind and downstream. This report describes the evidence of this activity preserved in deposits on the west and east flanks of the volcano. \r\n\r\nOn the west side of Glacier Peak the oldest postglacial deposit is a large, clayey mudflow which traveled at least 35 km down the White Chuck River valley sometime after 14,000 years ago. Subsequent large explosive eruptions produced lahars and at least 10 pyroclastic-flow deposits, including a semiwelded vitric tuff in the White Chuck River valley. These deposits, known collectively as the White Chuck assemblage, form a valley fill which is locally preserved as far as 100 km downstream from the volcano in the Stillaguamish River valley. At least some of the assemblage is about 11,670-11,500 radiocarbon years old. \r\n\r\nA small clayey lahar, containing reworked blocks of the vitric tuff, subsequently traveled at least 15 km down the White Chuck River. This lahar is overlain by lake sediments containing charred wood which is about 5,500 years old. A 150-m-thick assemblage of pyroclastic-flow deposits and lahars, called the Kennedy Creek assemblage, is in part about 5,500-5,100 radiocarbon years old. Lithic lahars from this assemblage extend at least 100 km downstream in the Skagit River drainage. The younger lahar assemblages, each containing at least three lahars and reaching at least 18 km downstream from Glacier Peak in the White Chuck River valley, are about 2,800 and 1,800 years old, respectively. These are postdated by a lahar containing abundant oxyhornblende dacite, which extends at least 30 km to the Sauk River. A still younger lahar assemblage that contains at least five lahars, and that also extends at least 30 km to the Sauk River, is older than a mature forest growing on its surface. \r\n\r\nAt least one lahar and a flood deposit form a low terrace at the confluence of the White Chuck and Sauk Rivers, and were deposited before 300 years ago, but more recently than about 1,800 years ago. Several small outburst floods, including one in 1975, have affected Kennedy and Baekos Creek and the upper White Chuck River in the last hundred years. \r\n\r\nEast of Glacier Peak the oldest postglacial deposits consist of ash-cloud deposits that underlie tephra erupted by Glacier Peak between 12,750 and 11,250 radiocarbon years ago. Although pyroclastic-flow deposits correlative with the ash-cloud deposits have not been recognized, late Pleistocene pumiceous lahars extend at least 50 km downstream in the Suiattle River valley. A younger clayey mudflow extends at least 6 km down Dusty Creek. This lahar is overlain by deposits of lithic pyroclastic flows and lahars that form the Dusty assemblage. This assemblage is at least 300 m thick in the upper valleys of Dusty and Chocolate Creeks, and contains more than 10 km3 of lithic debris. Lahars derived from the Dusty assemblage extend at least 100 km down the Skagit River valley from Glacier Peak. This assemblage is younger than tephra layer 0 from Mount Mazama, and older than tephra layer Yn from Mount St. Helens, and thus was formed between about 7,000 and 3,400 years ago. The Dusty assemblage may have been formed at the same time as the Kennedy Creek assemblage. \r\n\r\nA 100-m-thick assemblage of pyroclastic flows and lahars preserved in the Chocolate Creek valley is about 1,800 radiocarbon years old. A clayey lahar in the upper Chocolate Creek valley extended at least 2 km downvalley after 1,800 years ago, but before pyroclastic flows and lahars were deposited in upper Chocolate Creek 1,100 radiocarbon years ago. Several clayey lahars in the Dusty Creek valley east of Glacier Peak are also about 1,100 years old. A lahar in the valley of Dusty Creek, which contains rare prismatically jointed blocks of vesiculated dacite, and a white ash that is locally as much as 50 cm thick may be the products of small","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/ofr82830","usgsCitation":"Beget, J.E., 1982, Postglacial volcanic deposits at Glacier Peak, Washington, and potential hazards from future eruptions; a preliminary report: U.S. Geological Survey Open-File Report 82-830, 81 p., ill., maps ;28 cm., https://doi.org/10.3133/ofr82830.","productDescription":"81 p., ill., maps ;28 cm.","costCenters":[],"links":[{"id":141454,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1982/0830/report-thumb.jpg"},{"id":35373,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1982/0830/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ad5e4b07f02db683aa9","contributors":{"authors":[{"text":"Beget, J. E.","contributorId":63392,"corporation":false,"usgs":true,"family":"Beget","given":"J.","email":"","middleInitial":"E.","affiliations":[],"preferred":false,"id":156743,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":7825,"text":"ofr82878 - 1982 - Geochemical data for the Sierra Ancha Wilderness and Salome and Cherry Creek RARE II areas, Arizona","interactions":[],"lastModifiedDate":"2012-02-02T00:06:11","indexId":"ofr82878","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1982","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":330,"text":"Open-File Report","code":"OFR","onlineIssn":"2331-1258","printIssn":"0196-1497","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"82-878","title":"Geochemical data for the Sierra Ancha Wilderness and Salome and Cherry Creek RARE II areas, Arizona","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/ofr82878","usgsCitation":"Barton, H.N., Theobald, P., and Tripp, R.B., 1982, Geochemical data for the Sierra Ancha Wilderness and Salome and Cherry Creek RARE II areas, Arizona: U.S. Geological Survey Open-File Report 82-878, 31 p., ill. ;28 cm., https://doi.org/10.3133/ofr82878.","productDescription":"31 p., ill. ;28 cm.","costCenters":[],"links":[{"id":142162,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1982/0878/report-thumb.jpg"},{"id":35322,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1982/0878/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b24e4b07f02db6ae422","contributors":{"authors":[{"text":"Barton, H. N.","contributorId":99546,"corporation":false,"usgs":true,"family":"Barton","given":"H.","email":"","middleInitial":"N.","affiliations":[],"preferred":false,"id":156682,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Theobald, P. K.","contributorId":45293,"corporation":false,"usgs":true,"family":"Theobald","given":"P. K.","affiliations":[],"preferred":false,"id":156680,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Tripp, R. B.","contributorId":88707,"corporation":false,"usgs":true,"family":"Tripp","given":"R.","middleInitial":"B.","affiliations":[],"preferred":false,"id":156681,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":7742,"text":"ofr82298 - 1982 - Allanite-bearing calc-silicate rocks, southern Bighorn Mountains, Wyoming; geologic setting and resources of thorium, uranium, and rare-earth elements","interactions":[],"lastModifiedDate":"2012-02-02T00:06:04","indexId":"ofr82298","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1982","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":330,"text":"Open-File Report","code":"OFR","onlineIssn":"2331-1258","printIssn":"0196-1497","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"82-298","title":"Allanite-bearing calc-silicate rocks, southern Bighorn Mountains, Wyoming; geologic setting and resources of thorium, uranium, and rare-earth elements","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/ofr82298","usgsCitation":"Armbrustmacher, T.J., and Sargent, K., 1982, Allanite-bearing calc-silicate rocks, southern Bighorn Mountains, Wyoming; geologic setting and resources of thorium, uranium, and rare-earth elements: U.S. Geological Survey Open-File Report 82-298, 13 p., maps ;28 cm., https://doi.org/10.3133/ofr82298.","productDescription":"13 p., maps ;28 cm.","costCenters":[],"links":[{"id":140662,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1982/0298/report-thumb.jpg"},{"id":35202,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1982/0298/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ae0e4b07f02db687f45","contributors":{"authors":[{"text":"Armbrustmacher, Theodore J.","contributorId":31376,"corporation":false,"usgs":true,"family":"Armbrustmacher","given":"Theodore","email":"","middleInitial":"J.","affiliations":[],"preferred":false,"id":156524,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Sargent, Kenneth A.","contributorId":15998,"corporation":false,"usgs":true,"family":"Sargent","given":"Kenneth A.","affiliations":[],"preferred":false,"id":156523,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":7175,"text":"ofr82299 - 1982 - Geologic reconnaissance and geochemical sampling survey of molybdenum mineralization near Schiestler Peak, Temple Peak Quadrangle, Sublette County, Wyoming","interactions":[],"lastModifiedDate":"2012-02-02T00:06:12","indexId":"ofr82299","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1982","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":330,"text":"Open-File Report","code":"OFR","onlineIssn":"2331-1258","printIssn":"0196-1497","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"82-299","title":"Geologic reconnaissance and geochemical sampling survey of molybdenum mineralization near Schiestler Peak, Temple Peak Quadrangle, Sublette County, Wyoming","docAbstract":"A brief geologic reconnaissance and geochemical survey of molybdenum mineralization near Schiestler Peak, Sublette County, Wyo., indicates that molybdenite occurs in this area as disseminations and blebs in granitic or quartz monzonitic rocks intruded by felsic dikes of similar composition. Samples of stream sediments, panned concentrates from stream sediments, soils, rocks, and water were collected in the geochemical survey. Analytical results show that in reconnaissance, panned concentrates are the best of the sample types used in this study to detect molybdenum mineralization. More detailed analysis of the distribution of the molybdenum is best achieved through the collection of rock samples. Hydrothermal alteration is generally not conspicuous in the study area; however, rock samples that contain molybdenite are usually slightly enriched in silver, copper, lead, and in several instances, gold. Conversely, there appear to be negative associations between molybdenum and zinc and between molybdenum and several of the rare-earth elements. Mo concentrations in the rock samples with no visible molybdenite range from undetectable at a sensitivity of 5 parts per million (ppm) to 700 ppm. Mo content in rock samples containing visible molybdenite ranges from 10 ppm to greater than 2,000 ppm. Stream-sediment values range from undetected to 15 ppm; panned concentrates from undetected to 15 ppm; soils from undetected to 20 ppm. Analyses of the water samples indicate Mo concentrations from 0.8 parts per billion (ppb) to 4.8 ppb. As currently understood, this deposit is not extensive or continuous, but drilling to provide information on the vertical extent of mineralization may alter this opinion.","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/ofr82299","usgsCitation":"Lee, G.K., Antweiler, J., Love, J.D., and Benedict, J., 1982, Geologic reconnaissance and geochemical sampling survey of molybdenum mineralization near Schiestler Peak, Temple Peak Quadrangle, Sublette County, Wyoming: U.S. Geological Survey Open-File Report 82-299, 205 p., 4 over-size sheets, map ;28 cm., https://doi.org/10.3133/ofr82299.","productDescription":"205 p., 4 over-size sheets, map ;28 cm.","costCenters":[],"links":[{"id":141953,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1982/0299/report-thumb.jpg"},{"id":34517,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1982/0299/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":34518,"rank":401,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1982/0299/plate-2.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":34519,"rank":402,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1982/0299/plate-3.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":34520,"rank":403,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1982/0299/plate-4.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":34521,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1982/0299/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ae0e4b07f02db688442","contributors":{"authors":[{"text":"Lee, G. K.","contributorId":76722,"corporation":false,"usgs":true,"family":"Lee","given":"G.","email":"","middleInitial":"K.","affiliations":[],"preferred":false,"id":154626,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Antweiler, J.C.","contributorId":35722,"corporation":false,"usgs":true,"family":"Antweiler","given":"J.C.","email":"","affiliations":[],"preferred":false,"id":154623,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Love, J. D.","contributorId":64620,"corporation":false,"usgs":true,"family":"Love","given":"J.","middleInitial":"D.","affiliations":[],"preferred":false,"id":154624,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Benedict, J.F.","contributorId":66688,"corporation":false,"usgs":true,"family":"Benedict","given":"J.F.","email":"","affiliations":[],"preferred":false,"id":154625,"contributorType":{"id":1,"text":"Authors"},"rank":4}]}}
,{"id":58626,"text":"mf1177C - 1982 - Mineral resource potential map of the North Fork of the American River Wilderness study area (RARE II no. 5-262), Placer County, California","interactions":[],"lastModifiedDate":"2012-02-10T00:10:12","indexId":"mf1177C","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1982","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":325,"text":"Miscellaneous Field Studies Map","code":"MF","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"1177","chapter":"C","title":"Mineral resource potential map of the North Fork of the American River Wilderness study area (RARE II no. 5-262), Placer County, California","language":"ENGLISH","doi":"10.3133/mf1177C","usgsCitation":"Harwood, D.S., Griscom, A., Federspiel, F.E., Leszcykowski, A., and Spicker, F., 1982, Mineral resource potential map of the North Fork of the American River Wilderness study area (RARE II no. 5-262), Placer County, California: U.S. Geological Survey Miscellaneous Field Studies Map 1177, 1 map ;28 x 80 cm. on sheet 66 x 89 cm. folded in envelope 25 x 32 cm. +1 pamphlet (7 p. : map ; 28 cm.), https://doi.org/10.3133/mf1177C.","productDescription":"1 map ;28 x 80 cm. on sheet 66 x 89 cm. folded in envelope 25 x 32 cm. +1 pamphlet (7 p. : map ; 28 cm.)","costCenters":[],"links":[{"id":105548,"rank":700,"type":{"id":15,"text":"Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_6585.htm","linkFileType":{"id":5,"text":"html"},"description":"6585"},{"id":184763,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/mf/1982/1177c/report-thumb.jpg"},{"id":88485,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/mf/1982/1177c/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":88486,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/mf/1982/1177c/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"scale":"62500","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -120.83333333333333,39.166666666666664 ], [ -120.83333333333333,39.333333333333336 ], [ -120.33333333333333,39.333333333333336 ], [ -120.33333333333333,39.166666666666664 ], [ -120.83333333333333,39.166666666666664 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b24e4b07f02db6ae6dd","contributors":{"authors":[{"text":"Harwood, D. S.","contributorId":48937,"corporation":false,"usgs":true,"family":"Harwood","given":"D.","email":"","middleInitial":"S.","affiliations":[],"preferred":false,"id":260130,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Griscom, Andrew","contributorId":23520,"corporation":false,"usgs":true,"family":"Griscom","given":"Andrew","email":"","affiliations":[],"preferred":false,"id":260129,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Federspiel, F. E.","contributorId":18360,"corporation":false,"usgs":true,"family":"Federspiel","given":"F.","email":"","middleInitial":"E.","affiliations":[],"preferred":false,"id":260128,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Leszcykowski, A. M.","contributorId":78735,"corporation":false,"usgs":true,"family":"Leszcykowski","given":"A. M.","affiliations":[],"preferred":false,"id":260132,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"Spicker, F.A.","contributorId":72064,"corporation":false,"usgs":true,"family":"Spicker","given":"F.A.","email":"","affiliations":[],"preferred":false,"id":260131,"contributorType":{"id":1,"text":"Authors"},"rank":5}]}}
,{"id":58619,"text":"mf1201D - 1982 - Mineral resource potential map of the Mokelumne Wilderness and contiguous roadless areas, central Sierra Nevada, California","interactions":[],"lastModifiedDate":"2015-10-01T12:05:54","indexId":"mf1201D","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1982","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":325,"text":"Miscellaneous Field Studies Map","code":"MF","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"1201","chapter":"D","title":"Mineral resource potential map of the Mokelumne Wilderness and contiguous roadless areas, central Sierra Nevada, California","docAbstract":"<p>Under the provisions of the Wilderness Act (Public Law 88-577, September 3, 1964) and the Joint Conference Report on Senate Bill 4, 88th Congress, the U.S. Geological Survey and the U.S. Bureau of Mines have been conducting mineral surveys of wilderness and primitive areas. Areas officially designated as \"wilderness,\" \"wild,\" or \"canoe\" when the act was passed were incorporated into the National Wilderness Preservation System, and some of them are presently being studied. The act provided that areas under consideration for wilderness designation should be studied for suitability for incorporation into the Wilderness System. The mineral surveys constitute one aspect of suitability studies. The act directs that the results of such surveys are to be made available to the public and be submitted to the President and the Congress. This report discusses the results of a mineral survey of the Mokelumne Wilderness, El Dorado National Forest, Amador, Calaveras and Alpine Counties, California and Caples Creek, Raymond Peak, and Tragedy-Elephants Back Roadless Areas, Alpine, Amador, Ca 1 aver as, and El Dorado Counties, California. The Mokelumne Wilderness was established by Public Law 88-577, September 3, 1964, the Roadless Areas were classified as further planning areas during the Second Roadless Area Review and Evaluation (RARE II) by the U.S. Forest Service, 1979.&nbsp;</p>","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Reston, VA","doi":"10.3133/mf1201D","usgsCitation":"McKee, E.H., Chaffee, M.A., Federspiel, F.E., McHugh, E.L., Cather, E.E., Scott, D., and Rumsey, C.M., 1982, Mineral resource potential map of the Mokelumne Wilderness and contiguous roadless areas, central Sierra Nevada, California: U.S. Geological Survey Miscellaneous Field Studies Map 1201, Report: 10 p.; 1 Sheet: 41.11 x 34.66 inches, https://doi.org/10.3133/mf1201D.","productDescription":"Report: 10 p.; 1 Sheet: 41.11 x 34.66 inches","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[],"links":[{"id":184651,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/mf1201D.PNG"},{"id":309404,"rank":2,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/mf/1201-D/plate-1.pdf","text":"Plate","linkFileType":{"id":1,"text":"pdf"}},{"id":309403,"rank":1,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/mf/1201-D/report.pdf","text":"Report","linkFileType":{"id":1,"text":"pdf"}}],"scale":"62500","country":"United States","state":"California","otherGeospatial":"Mokelumne Wilderness","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -120.25,38.416666666666664 ], [ -120.25,39 ], [ -119.75,39 ], [ -119.75,38.416666666666664 ], [ -120.25,38.416666666666664 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b24e4b07f02db6ae474","contributors":{"authors":[{"text":"McKee, Edwin H. mckee@usgs.gov","contributorId":3728,"corporation":false,"usgs":true,"family":"McKee","given":"Edwin","email":"mckee@usgs.gov","middleInitial":"H.","affiliations":[],"preferred":true,"id":260094,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Chaffee, Maurice A. mchaffee@usgs.gov","contributorId":4047,"corporation":false,"usgs":true,"family":"Chaffee","given":"Maurice","email":"mchaffee@usgs.gov","middleInitial":"A.","affiliations":[{"id":171,"text":"Central Mineral and Environmental Resources Science Center","active":true,"usgs":true}],"preferred":true,"id":260099,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Federspiel, Francis E.","contributorId":28290,"corporation":false,"usgs":true,"family":"Federspiel","given":"Francis","email":"","middleInitial":"E.","affiliations":[],"preferred":false,"id":260093,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"McHugh, Edward L.","contributorId":77157,"corporation":false,"usgs":true,"family":"McHugh","given":"Edward","email":"","middleInitial":"L.","affiliations":[],"preferred":false,"id":260096,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"Cather, Eric E.","contributorId":54341,"corporation":false,"usgs":true,"family":"Cather","given":"Eric","email":"","middleInitial":"E.","affiliations":[],"preferred":false,"id":260098,"contributorType":{"id":1,"text":"Authors"},"rank":5},{"text":"Scott, Douglas F.","contributorId":69220,"corporation":false,"usgs":true,"family":"Scott","given":"Douglas F.","affiliations":[],"preferred":false,"id":260097,"contributorType":{"id":1,"text":"Authors"},"rank":6},{"text":"Rumsey, Clayton M.","contributorId":50514,"corporation":false,"usgs":true,"family":"Rumsey","given":"Clayton","email":"","middleInitial":"M.","affiliations":[],"preferred":false,"id":260095,"contributorType":{"id":1,"text":"Authors"},"rank":7}]}}
,{"id":58604,"text":"mf1344E - 1982 - Mineral resource potential map of the Hells Hole further planning area (RARE II), Greenlee County, Arizona, and Grant County, New Mexico","interactions":[],"lastModifiedDate":"2025-05-02T13:25:26.084893","indexId":"mf1344E","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1982","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":325,"text":"Miscellaneous Field Studies Map","code":"MF","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"1344","chapter":"E","title":"Mineral resource potential map of the Hells Hole further planning area (RARE II), Greenlee County, Arizona, and Grant County, New Mexico","docAbstract":"<p>During 1979, the U.S. Geological Survey and the U.S. Bureau of Mines conducted field investigations to evaluate the mineral resource potential of the Hells Hole Further Planning Area. The investigations included geologic mapping, geophysical studies, geochemical sampling, and a survey of known mines, prospects, and mineralized areas. This report summarizes the results of those studies. </p>","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Reston, VA","doi":"10.3133/mf1344E","usgsCitation":"Ratte, J., Hassemer, J., Martin, R., and Briggs, J.P., 1982, Mineral resource potential map of the Hells Hole further planning area (RARE II), Greenlee County, Arizona, and Grant County, New Mexico: U.S. Geological Survey Miscellaneous Field Studies Map 1344, Report: 7 p.; 1 Plate: 57.99 x 34.88 inches, https://doi.org/10.3133/mf1344E.","productDescription":"Report: 7 p.; 1 Plate: 57.99 x 34.88 inches","costCenters":[],"links":[{"id":485320,"rank":4,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_6997.htm","linkFileType":{"id":5,"text":"html"}},{"id":364241,"rank":2,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/mf/1344-E/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":182637,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/mf/1344-E/report-thumb.jpg"},{"id":485228,"rank":3,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/mf/1344-E/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"scale":"62500","country":"United States","state":"New Mexico, Arizona","county":"Greenlee County, Grant County","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -109.33333333333333,32.75 ], [ -109.33333333333333,33.25 ], [ -108.91666666666667,33.25 ], [ -108.91666666666667,32.75 ], [ -109.33333333333333,32.75 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b1be4b07f02db6a90b6","contributors":{"authors":[{"text":"Ratte, J.C.","contributorId":10416,"corporation":false,"usgs":true,"family":"Ratte","given":"J.C.","affiliations":[],"preferred":false,"id":260010,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Hassemer, J.R.","contributorId":18761,"corporation":false,"usgs":true,"family":"Hassemer","given":"J.R.","affiliations":[],"preferred":false,"id":260011,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Martin, R.A.","contributorId":53379,"corporation":false,"usgs":true,"family":"Martin","given":"R.A.","email":"","affiliations":[],"preferred":false,"id":260012,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Briggs, J. P.","contributorId":83920,"corporation":false,"usgs":true,"family":"Briggs","given":"J.","email":"","middleInitial":"P.","affiliations":[],"preferred":false,"id":260013,"contributorType":{"id":1,"text":"Authors"},"rank":4}]}}
,{"id":60300,"text":"mf1192C - 1982 - Mineral resource potential map of the Salmo-Priest Wilderness Study Area (RARE E6-981 A1-981), Pend Oreille County, Washington, and Boundary County, Idaho","interactions":[],"lastModifiedDate":"2022-12-13T19:27:54.705354","indexId":"mf1192C","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1982","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":325,"text":"Miscellaneous Field Studies Map","code":"MF","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"1192","chapter":"C","title":"Mineral resource potential map of the Salmo-Priest Wilderness Study Area (RARE E6-981 A1-981), Pend Oreille County, Washington, and Boundary County, Idaho","docAbstract":"<p>No abstract available.</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/mf1192C","usgsCitation":"Miller, F.K., Schmauch, S., and Rodriguez, E.A., 1982, Mineral resource potential map of the Salmo-Priest Wilderness Study Area (RARE E6-981 A1-981), Pend Oreille County, Washington, and Boundary County, Idaho: U.S. Geological Survey Miscellaneous Field Studies Map 1192, Report: 6 p.; 1 Plate: 29.50 × 24.00 inches, https://doi.org/10.3133/mf1192C.","productDescription":"Report: 6 p.; 1 Plate: 29.50 × 24.00 inches","costCenters":[],"links":[{"id":105562,"rank":3,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_6616.htm","linkFileType":{"id":5,"text":"html"},"description":"6616"},{"id":88775,"rank":1,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/mf/1982/1192c/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":88774,"rank":2,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/mf/1982/1192c/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":183290,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/mf/1982/1192c/report-thumb.jpg"}],"country":"United States","state":"Idaho, Washington","county":"Boundary County, Pend Oreille County","otherGeospatial":"Salmo-Priest Wilderness Study Area","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -117.3292,\n              48.8444\n            ],\n            [\n              -117.3292,\n              49\n            ],\n            [\n              -116.8783,\n              49\n            ],\n            [\n              -116.8783,\n              48.8444\n            ],\n            [\n              -117.3292,\n              48.8444\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b15e4b07f02db6a4d84","contributors":{"authors":[{"text":"Miller, F. K.","contributorId":10803,"corporation":false,"usgs":true,"family":"Miller","given":"F.","email":"","middleInitial":"K.","affiliations":[],"preferred":false,"id":263469,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Schmauch, S. W.","contributorId":53790,"corporation":false,"usgs":true,"family":"Schmauch","given":"S. W.","affiliations":[],"preferred":false,"id":263470,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Rodriguez, Eduardo A.","contributorId":83540,"corporation":false,"usgs":true,"family":"Rodriguez","given":"Eduardo","email":"","middleInitial":"A.","affiliations":[],"preferred":false,"id":263471,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":60299,"text":"mf1192A - 1982 - Geologic maps of Salmo-Priest Wilderness Study Area (RARE E6-981 A1-981), Pend Oreille County, Washington, and Boundary County, Idaho","interactions":[],"lastModifiedDate":"2012-02-10T00:10:19","indexId":"mf1192A","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1982","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":325,"text":"Miscellaneous Field Studies Map","code":"MF","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"1192","chapter":"A","title":"Geologic maps of Salmo-Priest Wilderness Study Area (RARE E6-981 A1-981), Pend Oreille County, Washington, and Boundary County, Idaho","language":"ENGLISH","doi":"10.3133/mf1192A","usgsCitation":"Miller, F.K., 1982, Geologic maps of Salmo-Priest Wilderness Study Area (RARE E6-981 A1-981), Pend Oreille County, Washington, and Boundary County, Idaho: U.S. Geological Survey Miscellaneous Field Studies Map 1192, 1 map ;35 x 70 cm., https://doi.org/10.3133/mf1192A.","productDescription":"1 map ;35 x 70 cm.","costCenters":[],"links":[{"id":105561,"rank":700,"type":{"id":15,"text":"Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_6614.htm","linkFileType":{"id":5,"text":"html"},"description":"6614"},{"id":183289,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"}],"scale":"0","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -117.25,48.8675 ], [ -117.25,49 ], [ -117,49 ], [ -117,48.8675 ], [ -117.25,48.8675 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ae1e4b07f02db688626","contributors":{"authors":[{"text":"Miller, F. K.","contributorId":10803,"corporation":false,"usgs":true,"family":"Miller","given":"F.","email":"","middleInitial":"K.","affiliations":[],"preferred":false,"id":263468,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":58369,"text":"mf1317B - 1982 - Geochemical map showing anomalous drainage basins, Benton Range further planning (RARE II) area, Mono County, California","interactions":[],"lastModifiedDate":"2012-02-10T00:10:27","indexId":"mf1317B","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1982","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":325,"text":"Miscellaneous Field Studies Map","code":"MF","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"1317","chapter":"B","title":"Geochemical map showing anomalous drainage basins, Benton Range further planning (RARE II) area, Mono County, California","language":"ENGLISH","doi":"10.3133/mf1317B","usgsCitation":"Donahoe, J.L., Chaffee, M., Fey, D., Hill, R.H., and Sutley, S.J., 1982, Geochemical map showing anomalous drainage basins, Benton Range further planning (RARE II) area, Mono County, California: U.S. Geological Survey Miscellaneous Field Studies Map 1317, 1 map ;44 x 37 cm., on sheet 66 x 103 cm. folded in envelope 25 x 32 cm., https://doi.org/10.3133/mf1317B.","productDescription":"1 map ;44 x 37 cm., on sheet 66 x 103 cm. folded in envelope 25 x 32 cm.","costCenters":[],"links":[{"id":105741,"rank":700,"type":{"id":15,"text":"Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_6948.htm","linkFileType":{"id":5,"text":"html"},"description":"6948"},{"id":182958,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"}],"scale":"62500","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -118.66666666666667,37.583333333333336 ], [ -118.66666666666667,37.833333333333336 ], [ -118.41666666666667,37.833333333333336 ], [ -118.41666666666667,37.583333333333336 ], [ -118.66666666666667,37.583333333333336 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b23e4b07f02db6ae1b2","contributors":{"authors":[{"text":"Donahoe, J. L.","contributorId":20404,"corporation":false,"usgs":true,"family":"Donahoe","given":"J.","email":"","middleInitial":"L.","affiliations":[],"preferred":false,"id":258911,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Chaffee, M.A.","contributorId":108049,"corporation":false,"usgs":true,"family":"Chaffee","given":"M.A.","affiliations":[],"preferred":false,"id":258915,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Fey, D.L.","contributorId":44537,"corporation":false,"usgs":true,"family":"Fey","given":"D.L.","email":"","affiliations":[],"preferred":false,"id":258912,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Hill, R. H.","contributorId":57059,"corporation":false,"usgs":true,"family":"Hill","given":"R.","email":"","middleInitial":"H.","affiliations":[],"preferred":false,"id":258913,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"Sutley, S. J.","contributorId":91484,"corporation":false,"usgs":true,"family":"Sutley","given":"S.","email":"","middleInitial":"J.","affiliations":[],"preferred":false,"id":258914,"contributorType":{"id":1,"text":"Authors"},"rank":5}]}}
,{"id":38637,"text":"pp1066L - 1982 - Some silicified strophomenacean brachiopods from the Ordovician of Kentucky, with comments on the genus Pionomena","interactions":[],"lastModifiedDate":"2012-02-02T00:10:35","indexId":"pp1066L","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1982","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":331,"text":"Professional Paper","code":"PP","onlineIssn":"2330-7102","printIssn":"1044-9612","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"1066","chapter":"L","title":"Some silicified strophomenacean brachiopods from the Ordovician of Kentucky, with comments on the genus Pionomena","docAbstract":"Eight species of silicified strophomenid brachiopods from Ordovician rocks of Kentucky are described in this report. Seven species are strophomenaceans, including six from the Middle Ordovician and one, Leptaena kentuckiana n. sp., from the Upper Ordovician. Pionomena recens Neuman from the Middle Ordovician is referred to the Davidsoniacea. Three of these species also occur in the Middle Ordovician of the northern Mississippi Valley region. Rafinesquina is abundant at many localities throughout the Middle Ordovician section of Kentucky. Other silicified strophomenaceans are rare and have been recovered only from the lower part of the Middle Ordovician section of the area. Oepikinia minnesotensis has a high degree of polymorphism of outline shape, profile, and ornament. Some Middle Ordovician species heretofore placed in Strophomena are reassigned to Tetraphalerella. Furcitella and Holtedahlina are differentiated only by the presence of a prominent fold in adult valves of Holtedaklina because a bifid dorsal medial ridge occurs in species of both genera and because the transmuscle ridges of both genera are similar. The possession by Pionomena recens of a perideltidium, dentifers, dorsal medial node, and impunctate shell indicates relationship of this genus to the Davidsoniacea.","language":"ENGLISH","doi":"10.3133/pp1066L","usgsCitation":"Pope, J., 1982, Some silicified strophomenacean brachiopods from the Ordovician of Kentucky, with comments on the genus Pionomena: U.S. Geological Survey Professional Paper 1066, p. L1-L30, https://doi.org/10.3133/pp1066L.","productDescription":"p. L1-L30","costCenters":[],"links":[{"id":124452,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/pp/1066l/report-thumb.jpg"},{"id":65468,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/pp/1066l/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e48cde4b07f02db544d2f","contributors":{"authors":[{"text":"Pope, J.K.","contributorId":41502,"corporation":false,"usgs":true,"family":"Pope","given":"J.K.","email":"","affiliations":[],"preferred":false,"id":220198,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":1823,"text":"wsp2193 - 1982 - Streamflow characteristics related to channel geometry of streams in western United States","interactions":[],"lastModifiedDate":"2012-02-02T00:05:15","indexId":"wsp2193","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1982","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":341,"text":"Water Supply Paper","code":"WSP","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"2193","title":"Streamflow characteristics related to channel geometry of streams in western United States","docAbstract":"Assessment of surface-mining and reclamation activities generally requires extensive hydrologic data. Adequate streamflow data from instrumented gaging stations rarely are available, and estimates of surface- water discharge based on rainfall-runoff models, drainage area, and basin characteristics sometimes have proven unreliable. Channel-geometry measurements offer an alternative method of quickly and inexpensively estimating stream-flow characteristics for ungaged streams. The method uses the empirical development of equations to yield a discharge value from channel-geometry and channel-material data. The equations are developed by collecting data at numerous streamflow-gaging sites and statistically relating those data to selected discharge characteristics. Mean annual runoff and flood discharges with selected recurrence intervals can be estimated for perennial, intermittent, and ephemeral streams. The equations were developed from data collected in the western one-half of the conterminous United States. The effect of the channel-material and runoff characteristics are accounted for with the equations.","language":"ENGLISH","publisher":"U.S. G.P.O.,","doi":"10.3133/wsp2193","usgsCitation":"Hedman, E.R., and Osterkamp, W.R., 1982, Streamflow characteristics related to channel geometry of streams in western United States: U.S. Geological Survey Water Supply Paper 2193, iii, 17 p. : ill., map ; 28 cm., https://doi.org/10.3133/wsp2193.","productDescription":"iii, 17 p. : ill., map ; 28 cm.","costCenters":[],"links":[{"id":137056,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wsp/2193/report-thumb.jpg"},{"id":27019,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wsp/2193/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b15e4b07f02db6a4e2f","contributors":{"authors":[{"text":"Hedman, E. R.","contributorId":71527,"corporation":false,"usgs":true,"family":"Hedman","given":"E.","email":"","middleInitial":"R.","affiliations":[],"preferred":false,"id":144211,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Osterkamp, W. R.","contributorId":46044,"corporation":false,"usgs":true,"family":"Osterkamp","given":"W.","email":"","middleInitial":"R.","affiliations":[],"preferred":false,"id":144210,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":60039,"text":"mf1369C - 1982 - Mineral resource potential map of the Ramseys Draft Addition, Augusta and Highland counties, Virginia","interactions":[],"lastModifiedDate":"2025-05-01T13:40:55.361894","indexId":"mf1369C","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1982","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":325,"text":"Miscellaneous Field Studies Map","code":"MF","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"1369","chapter":"C","title":"Mineral resource potential map of the Ramseys Draft Addition, Augusta and Highland counties, Virginia","docAbstract":"<p>Under the provisions of the Wilderness Act (Public Law 88-577, September 3, 1964) and the Joint Conference Report on Senate Bill 4, 88th Congress, the U.S. Geological Survey and the U.S. Bureau of Mines have been conducting mineral surveys of wilderness and primitive areas. Areas officially designated as \"wilderness,\" \"wild,\" or \"canoe\" when the act was passed were incorporated into the National Wilderness Preservation System, and some of them are presently being studied. The act provided that areas under consideration for wilderness designation should be studied for suitability for incorporation into the Wilderness System. The mineral surveys constitute one aspect of the suitability studies. The act directs that the results of such surveys are to be made available to the public and be submitted to the President and the Congress. This report presents the results of a mineral survey of the Ramseys Draft Addition, which is a roadless area adjoining Ramseys Draft Wilderness Study Area in the George Washington National Forest, Augusta and Highland Counties, Virginia. The area was classified as a further planning area during the Second Roadless Area Review and Evaluation (RARE II) by the U.S. Forest Service, January 1979.</p>","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Reston, VA","doi":"10.3133/mf1369C","usgsCitation":"Lesure, F., and Mory, P., 1982, Mineral resource potential map of the Ramseys Draft Addition, Augusta and Highland counties, Virginia: U.S. Geological Survey Miscellaneous Field Studies Map 1369, Report: 8 p.; 1 Plate: 25.75 x 30.75 inches, https://doi.org/10.3133/mf1369C.","productDescription":"Report: 8 p.; 1 Plate: 25.75 x 30.75 inches","costCenters":[],"links":[{"id":485222,"rank":3,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/mf/1369-C/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":180477,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/mf/1369-C/report-thumb.jpg"},{"id":364208,"rank":2,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/mf/1369-C/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}}],"country":"United States","state":"Virginia","county":"Augusta County, Highland County","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -79.41666666666667,38.25 ], [ -79.41666666666667,38.416666666666664 ], [ -79.25,38.416666666666664 ], [ -79.25,38.25 ], [ -79.41666666666667,38.25 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b28e4b07f02db6b14d0","contributors":{"authors":[{"text":"Lesure, F. G.","contributorId":7694,"corporation":false,"usgs":true,"family":"Lesure","given":"F. G.","affiliations":[{"id":595,"text":"U.S. Geological Survey","active":false,"usgs":true}],"preferred":false,"id":263033,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Mory, P. C.","contributorId":47780,"corporation":false,"usgs":true,"family":"Mory","given":"P. C.","affiliations":[],"preferred":false,"id":263034,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":11299,"text":"ofr82280 - 1982 - X-ray diffraction mineral identification charts for use in studies of uranium, thorium, and rare-earth deposits","interactions":[],"lastModifiedDate":"2012-02-02T00:06:21","indexId":"ofr82280","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1982","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":330,"text":"Open-File Report","code":"OFR","onlineIssn":"2331-1258","printIssn":"0196-1497","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"82-280","title":"X-ray diffraction mineral identification charts for use in studies of uranium, thorium, and rare-earth deposits","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/ofr82280","usgsCitation":"Staatz, M., and Brownfield, I.K., 1982, X-ray diffraction mineral identification charts for use in studies of uranium, thorium, and rare-earth deposits: U.S. Geological Survey Open-File Report 82-280, 7 p., 3 over-size sheets, ill. ;28 cm., https://doi.org/10.3133/ofr82280.","productDescription":"7 p., 3 over-size sheets, ill. ;28 cm.","costCenters":[],"links":[{"id":142439,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1982/0280/report-thumb.jpg"},{"id":39099,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1982/0280/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":39096,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1982/0280/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":39097,"rank":401,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1982/0280/plate-2.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":39098,"rank":402,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1982/0280/plate-3.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e49d6e4b07f02db5de4f9","contributors":{"authors":[{"text":"Staatz, M.H.","contributorId":14411,"corporation":false,"usgs":true,"family":"Staatz","given":"M.H.","affiliations":[],"preferred":false,"id":162889,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Brownfield, I. K.","contributorId":77915,"corporation":false,"usgs":true,"family":"Brownfield","given":"I.","email":"","middleInitial":"K.","affiliations":[],"preferred":false,"id":162890,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":10482,"text":"ofr82936 - 1982 - Progress report on geologic studies of the Ranger orebodies, Northern Territory, Australia","interactions":[],"lastModifiedDate":"2012-02-02T00:06:33","indexId":"ofr82936","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1982","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":330,"text":"Open-File Report","code":"OFR","onlineIssn":"2331-1258","printIssn":"0196-1497","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"82-936","title":"Progress report on geologic studies of the Ranger orebodies, Northern Territory, Australia","docAbstract":"The Ranger No. 1 and No. 3 orebodies contain about 124,000 tonnes U3O8 in highly chloritized metasediments of the lower Proterozoic Cahill Formation within about 500 m of the projected sub-Kombolgie Formation unconformity. In both orebodies, oxidized and reduced uranium minerals occur chiefly in quartzose schists that have highly variable amounts of muscovite, sericite, and chlorite. The effects of several periods of alteration are pervasive in the vicinity of orebodies where biotite and garnet are altered to chlorite, and feldspars to white mica or chlorite. Oxidized uranium minerals, associated with earthy iron oxides, occur from the surface to a depth of about 60 m. Below the oxidized zone, uranium occurs chiefly as uraninite and pitchblende disseminated through thick sections of quartz-chlorite-muscovite schist and has no apparent association with graphite or sulfides. In fact, graphite is rare and sulfides are generally low in abundance (<0.5 percent). Higher ore grades occur in disrupted zones a few centimeters thick and in some quartz-chlorite vein-like zones of uncertain origin. Uranium correlates strongly with chlorite, but not all of the many ages of chlorite have associated uranium. At least five textural varieties of chlorite are present and represent at least 3 ages. Preliminary microprobe analyses suggest that Mg-Fe-Al contents are relatively uniform. Apatite commonly occurs with chlorite. Uranium is not common in carbonate rocks and seems to occur only in disrupted zones that have chlorite alteration. Chloritization and silicification are more widespread and intense in the No. 1 orebody than in the No. 3. In both orebodies, hematite occurs tens to hundreds of meters below the weathered zone, in both altered and largely unaltered rocks, with and without uranium. \r\n\r\nThe structure of the orebodies is outwardly simple, particularly in No. 3; dips are less than 40? on most lithologic contacts. The No. 1 orebody is in a basin-like structure about 400 m wide that probably formed in part by progressive removal of carbonate rocks that are as much as 200 m thick adjacent to the No. 1 orebody and below the No. 3 orebody. Quartz-chlorite breccias have formed in the zone of carbonate thinning; uranium is spotty and low grade in these breccias. Chloritized and uraniferous broken and sheared zones, a few centimeters to a few meters thick, have an unknown attitude but must have small displacement. Blocks of altered Kombolgie sandstone are downfaulted into the No. 3 orebody and locally contain reduced uranium minerals. One or more shear zones 5-30 m thick of crushed and smeared fine to coarse rock fragments occur below the orebodies, and other low-angle shears probably occur in the orebodies. The shear zone dips about 40 o and displacement on it is not known. The footwall rocks generally are less retrograded than those in the hanging wall (orebody) and consist of quartz-biotite-feldspar schists and gneisses flanking the Nanambu Complex. A few scattered fractures in the footwall sequence contain pitchblende of unknown age and origin. \r\n\r\nMajor element chemical analyses confirm the lithologic observations of large changes in composition during multiple stages of alteration. Granitic dikes and pelitic schists have gained Fe and Mg and lost Si, Ca, Na, and K during chloritization. Marbles have gained Si, Al, Fe, and P, and lost Mg, Ca, and K during jasperoid-chlorite alteration. Total net chemical gains and losses in the Ranger No. 1 orebody were huge: equal to about 37 percent of the mass of the ore-bearing rock that will be mined. There were net gains in Si and P and net losses in Al, Fe, Mg, Ca, K, and Na. \r\n\r\nThe geologic age(s) of uranium emplacement are obscure because there are few age criteria. Reduced uranium minerals are younger than 1.8-b.y.-old granite dikes, and some occur locally in 1.65-b.y.-old Kombolgie Formation. Diabase dikes (age not known) are thoroughly chloritized and contain sparse ore minerals. Oxidized ura","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/ofr82936","usgsCitation":"Nash, J., and Frishman, D., 1982, Progress report on geologic studies of the Ranger orebodies, Northern Territory, Australia: U.S. Geological Survey Open-File Report 82-936, 31 p., ill., map ;28 cm., https://doi.org/10.3133/ofr82936.","productDescription":"31 p., ill., map ;28 cm.","costCenters":[],"links":[{"id":144007,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1982/0936/report-thumb.jpg"},{"id":38347,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1982/0936/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a9be4b07f02db65debf","contributors":{"authors":[{"text":"Nash, J. T.","contributorId":31751,"corporation":false,"usgs":true,"family":"Nash","given":"J. T.","affiliations":[],"preferred":false,"id":161473,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Frishman, David","contributorId":40214,"corporation":false,"usgs":true,"family":"Frishman","given":"David","email":"","affiliations":[],"preferred":false,"id":161474,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":60932,"text":"mf1353B - 1982 - Map showing geochemical analyses of panned stream sediments, Stansbury Roadless Areas, Tooele County, Utah","interactions":[],"lastModifiedDate":"2018-08-28T13:48:05","indexId":"mf1353B","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1982","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":325,"text":"Miscellaneous Field Studies Map","code":"MF","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"1353","chapter":"B","title":"Map showing geochemical analyses of panned stream sediments, Stansbury Roadless Areas, Tooele County, Utah","docAbstract":"<p>The Wilderness Act (Public Law 88-577, September 3, 1964) and related Acts require the U.S. Geological Survey and the U.S. Bureau of Mines to survey certain areas on Federal lands to determine their mineral resource potential. Results must be made available to the public and be submitted to the Administration and the Congress. This report presents the results of a geochemical survey of the Stansbury Roadless Areas, Tooele County, Utah. Part of this area was classified a Further Planning Area during the Second Roadless Area Review and Evaluation (RARE II) by the U.S. Forest Service, January 1979.</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/mf1353B","usgsCitation":"Sorensen, M.L., 1982, Map showing geochemical analyses of panned stream sediments, Stansbury Roadless Areas, Tooele County, Utah: U.S. Geological Survey Miscellaneous Field Studies Map 1353, 22.90 x 37.76 inches, https://doi.org/10.3133/mf1353B.","productDescription":"22.90 x 37.76 inches","costCenters":[],"links":[{"id":356847,"rank":2,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/mf/1353-B/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":179855,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/mf/1353-B/report-thumb.jpg"}],"scale":"0","country":"United States","state":"Utah","county":"Tooele County","otherGeospatial":"Stansbury Roadless Areas","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -112.75,40.333333333333336 ], [ -112.75,40.583333333333336 ], [ -112.5,40.583333333333336 ], [ -112.5,40.333333333333336 ], [ -112.75,40.333333333333336 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b31e4b07f02db6b41cb","contributors":{"authors":[{"text":"Sorensen, Martin L.","contributorId":36563,"corporation":false,"usgs":true,"family":"Sorensen","given":"Martin","email":"","middleInitial":"L.","affiliations":[],"preferred":false,"id":264640,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
]}