{"pageNumber":"1683","pageRowStart":"42050","pageSize":"25","recordCount":46619,"records":[{"id":5881,"text":"pp1101 - 1980 - The Boulder Creek Batholith, Front Range, Colorado","interactions":[{"subject":{"id":14095,"text":"ofr6570 - 1965 - Allanites from the Boulder Creek batholith, Colorado","indexId":"ofr6570","publicationYear":"1965","noYear":false,"title":"Allanites from the Boulder Creek batholith, Colorado"},"predicate":"SUPERSEDED_BY","object":{"id":5881,"text":"pp1101 - 1980 - The Boulder Creek Batholith, Front Range, Colorado","indexId":"pp1101","publicationYear":"1980","noYear":false,"title":"The Boulder Creek Batholith, Front Range, Colorado"},"id":1}],"lastModifiedDate":"2012-02-02T00:05:48","indexId":"pp1101","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1980","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":"1101","title":"The Boulder Creek Batholith, Front Range, Colorado","docAbstract":"The Boulder Creek batholith is the best known of several large Precambrian batholiths of similar rock composition that crop out across central Colorado. The rocks in the batholith belong to the calc-alkaline series and range in composition from granodiorite through quartz diorite (tonalite) to gneissic aplite. Two rock types dominate': the Boulder Creek Granodiorite, the major rock unit, and a more leucocratic and slightly younger unit herein named Twin Spruce Quartz Monzonite. Besides mafic inclusions, which occur mainly in hornblende-bearing phases of the Boulder Creek Granodiorite, there are cogenetic older and younger lenses, dikes, and small plutons of hornblende diorite, hornblendite, gabbro, and pyroxenite. Pyroxenite is not found in the batholith. The Boulder Creek Granodiorite in the batholith represents essentially two contemporaneous magmas, a northern body occurring in the Gold Hill and Boulder quadrangles and a larger southern body exposed in the Blackhawk and the greater parts of the Tungsten and Eldorado Springs quadrangles. The two bodies are chemically and mineralogically distinct. The northern body is richer in CaO and poorer in K2O, is more mafic, and has a larger percentage of plagioclase than the southern body. \r\n\r\nA crude sequence of rock types occurs from west to east in the batholith accompanied by a change in plagioclase composition from calcic plagioclase on the west to sodic on the east. Ore minerals tend to decrease, and the ratio potassium feldspar:plagioclase increases inward from the western contact of the batholith, indicating that the Boulder Creek batholith is similar to granodiorite batholiths the world over. Emplacement of the Boulder Creek batholith was contemporaneous with plastic deformation and high-grade regional metamorphism that folded the country rock and the batholith contact along west-northwest and north-northwest axes. Also, smaller satellitic granodiorite bodies tend to conform to the trends of foliation and fold axes in the country rock, suggesting that emplacement was controlled by preexisting structures in the country rock. \r\n\r\nOn a gross scale, chemical equilibrium in the Boulder Creek Granodiorite is expressed by a near 1:1 ratio, or straight-line relationship in the distribution of iron, magnesium, and manganese in biotite and hornblende. General mineralogical trends in the Boulder Creek Granodiorite indicate that modal biotite, hornblende, and plagioclase tend to increase and quartz and microcline tend to decrease as CaO increases. These trends were not found in the Twin Spruce Quartz Monzonite. \r\n\r\nDifferentiation is believed to have played a major role and assimilation a minor role in the development of the Boulder Creek batholith. The Boulder Creek Granodiorite is of probable mantle or lower crust origin, and, based on the scant data available, the Twin Spruce Quartz Monzonite may be of crustal origin, but the magma was extensively altered by contaminants of ambiguous origin. Mafic inclusions, possibly derived from a dioritic magma which was an early differentiate associated temporally with the Boulder Creek Granodiorite and (or) the Twin Spruce Quartz Monzonite, were in jected into the Boulder Creek Granodiorite during the mush stage and before the batholith was completely crystallized. \r\n\r\nBiotite, hornblende, and potassium feldspar were studied extensively. Their chemistry and petrology indicate a homogeneity throughout the batholith not believed possible by a casual observance of the batholithic rocks in the field. The accessory minerals, where investigated, also tend to indicate this same pervasive homogeneity.","language":"ENGLISH","publisher":"U.S. Govt. Print. Off.,","doi":"10.3133/pp1101","usgsCitation":"Gable, D.J., 1980, The Boulder Creek Batholith, Front Range, Colorado: U.S. Geological Survey Professional Paper 1101, 88 p;  2 plates in pocket, https://doi.org/10.3133/pp1101.","productDescription":"88 p;  2 plates in pocket","costCenters":[],"links":[{"id":104551,"rank":700,"type":{"id":15,"text":"Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_4720.htm","linkFileType":{"id":5,"text":"html"},"description":"4720"},{"id":124378,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/pp/1101/report-thumb.jpg"},{"id":32702,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/pp/1101/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":32703,"rank":401,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/pp/1101/plate-2.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":32704,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/pp/1101/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ad3e4b07f02db68231b","contributors":{"authors":[{"text":"Gable, Dolores J.","contributorId":52957,"corporation":false,"usgs":true,"family":"Gable","given":"Dolores","email":"","middleInitial":"J.","affiliations":[],"preferred":false,"id":151739,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":56919,"text":"wdrKS792 - 1980 - Water resources data for Kansas, water year 1979; Volume 2, Arkansas River basin","interactions":[],"lastModifiedDate":"2018-09-07T10:01:05","indexId":"wdrKS792","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1980","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":340,"text":"Water Data Report","code":"WDR","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"KS-79-2","title":"Water resources data for Kansas, water year 1979; Volume 2, Arkansas River basin","docAbstract":"<p>No abstract available.</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/wdrKS792","usgsCitation":"Water Resources Division, U.S. Geological Survey, 1980, Water resources data for Kansas, water year 1979; Volume 2, Arkansas River basin: U.S. Geological Survey Water Data Report KS-79-2, 373 p., https://doi.org/10.3133/wdrKS792.","productDescription":"373 p.","costCenters":[],"links":[{"id":181148,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e49fbe4b07f02db5f49ee","contributors":{"authors":[{"text":"Water Resources Division, U.S. Geological Survey","contributorId":128075,"corporation":true,"usgs":false,"organization":"Water Resources Division, U.S. Geological Survey","id":533006,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":13922,"text":"ofr80834 - 1980 - Multichannel seismic-reflection profiles collected along the U.S. continental margin in 1978","interactions":[],"lastModifiedDate":"2018-06-18T11:13:35","indexId":"ofr80834","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1980","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":330,"text":"Open-File Report","code":"OFR","onlineIssn":"2331-1258","printIssn":"0196-1497","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"80-834","title":"Multichannel seismic-reflection profiles collected along the U.S. continental margin in 1978","docAbstract":"<p>During 1978, the U.S.. Geological Survey (USGS) contracted with Geophysical Services, Inc. (GSI) for GSI to collect 4,813 km of 48-channel seismic-reflection profiles along the continental margin between North Carolina and Maine. Fifteen lines were acquired perpendicular to the margin Clines 18 through 32), and six lines were acquired parallel to the margin Clines 33 through 38). The profiles were shot by the Motor Vessel (MV) CARINO and MV CECIL GREEN between May and November 1978. A 3,600-long hydrophone streamer was used; it was composed of 24 groups of 100-m length each near the ship, followed by 24 groups of 50-mlength each. Tuned airgun arrays totaling 2,000 and 1,400 cubic inches of air were used by the MV- CARINO and MV CECIL GREEN, respectively.</p><p>The profiles were stacked by GSI and displayed in conventional time-variant scaled format to 12 seconds of recording time with vertical scales of .2.5 inches per second and horizontal scales of 1.2 km per inch. Additional protessing was applied to Line 25 across the Baltimore Canyon Trough and Line 32 across the Carolina Trough. Data collected along Line 25 over the Outer Shelf, Slope and upper Rise were restacked with 1 1/2-km-spaced velocity analyses, signature deconvolution, deep-water multiple deconvolution, velocity filtering Con shelf only), and time migration. The restacked part and remaining parts of Line 25 were converted to depth sections having a vertical scale of 1.2 km per inch (vertical exaggeration: 2/1). Data collected along two parts of Line 32 were also restacked with signature and deep-water multiple deconvolution. Line 32 was also converted to a depth section except for the first 80 km near shore.</p><p>Profiles 18-38 may be inspected at the USGS in Woods Hole, MA 02543. Copies of the profiles may be, purchased only from the National Geophysical and Solar-Terrestrial Data Center, NOAA, Boulder, Co 80303.</p>","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Reston, VA","doi":"10.3133/ofr80834","usgsCitation":"Grow, J.A., Schlee, J.S., and Dillon, W.P., 1980, Multichannel seismic-reflection profiles collected along the U.S. continental margin in 1978: U.S. Geological Survey Open-File Report 80-834, 3 p., 1 leaf of plates :map ;28 cm., https://doi.org/10.3133/ofr80834.","productDescription":"3 p., 1 leaf of plates :map ;28 cm.","costCenters":[],"links":[{"id":146837,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/ofr80834.PNG"},{"id":259866,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1980/0834/ofr1980834.pdf","text":"Report","size":"210 KB","linkFileType":{"id":1,"text":"pdf"},"description":"OFR 1980-834"}],"contact":"<p><a href=\"https://woodshole.er.usgs.gov\" data-mce-href=\"https://woodshole.er.usgs.gov\">Coastal and Marine Geology Program</a><br> U.S. Geological Survey<br> 384 Woods Hole Road<br> Woods Hole, MA 02543</p>","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b32e4b07f02db6b487e","contributors":{"authors":[{"text":"Grow, John A.","contributorId":25943,"corporation":false,"usgs":true,"family":"Grow","given":"John","email":"","middleInitial":"A.","affiliations":[],"preferred":false,"id":168642,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Schlee, John Stevens","contributorId":46501,"corporation":false,"usgs":true,"family":"Schlee","given":"John","email":"","middleInitial":"Stevens","affiliations":[],"preferred":false,"id":168644,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Dillon, William P. bdillon@usgs.gov","contributorId":79820,"corporation":false,"usgs":true,"family":"Dillon","given":"William","email":"bdillon@usgs.gov","middleInitial":"P.","affiliations":[{"id":678,"text":"Woods Hole Coastal and Marine Science Center","active":true,"usgs":true}],"preferred":false,"id":168643,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":70114231,"text":"70114231 - 1980 - Map data catalog","interactions":[],"lastModifiedDate":"2014-09-24T11:36:54","indexId":"70114231","displayToPublicDate":"1990-01-01T14:42:00","publicationYear":"1980","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":6,"text":"USGS Unnumbered Series"},"title":"Map data catalog","docAbstract":"<p>The National Cartographic Information Center (NCIC) is the information branch of the National Mapping Program, U.S. Geological Survey. NCIC's mission is to help users gain better, faster, low-cost access to the cartographic holdings of Federal, State, and private agencies.</p>\n<br/>\n<p>This catalog tells how to order a wide range of mapping byproducts that may help to fill one or more of your special needs. For each such product, the catalog:<br/>\n-  Describes and illustrates the product offered.<br/>\n-  Explains the scope of geographic coverage available.<br/>\n-  Lists typical uses of the product.<br/>\n-  Explains how to order the products you need.</p>\n<br/>\n<p>Only a few of the products listed in this catalog are stocked. Most of them must be custom-produced to meet your particular requirement. Prices for the variety of products, formats and sizes are contained in a separate and periodically updated list. The price list is available free upon request from any NCIC office.</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/70114231","usgsCitation":"Water Resources Division, U.S. Geological Survey, 1980, Map data catalog, 48 p., https://doi.org/10.3133/70114231.","productDescription":"48 p.","numberOfPages":"50","costCenters":[{"id":409,"text":"National Cartographic Information Center","active":false,"usgs":true}],"links":[{"id":290148,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":290147,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/unnumbered/70114231/report.pdf"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"53aa9df9e4b065055fab1670","contributors":{"authors":[{"text":"Water Resources Division, U.S. Geological Survey","contributorId":128075,"corporation":true,"usgs":false,"organization":"Water Resources Division, U.S. Geological Survey","id":535661,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":70159087,"text":"70159087 - 1980 - A survey of image processing developments in support of remote sensing","interactions":[],"lastModifiedDate":"2017-01-18T15:03:42","indexId":"70159087","displayToPublicDate":"1981-01-01T00:00:00","publicationYear":"1980","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":6,"text":"USGS Unnumbered Series"},"title":"A survey of image processing developments in support of remote sensing","docAbstract":"<p>New algorithm developments for image processing (IP) will occur throughout the 1980's, resulting from evolution in computer hardware and sensors as well as continuing research. This report will describe the areas of algorithm development that are occurring in applications, research, and operational environments. Included is an overview of image processing activities at institutions which are generally regarded as leaders in IP algorithm development and implementation. Finally, this report addresses directions in IP algorithm development that are being proposed for the EROS Data Center (EDC). The major applications of IP at EDC are developed for use in the processing, analysis, and extraction of remote sensing information from Landsat and aircraft data (platforms).</p>","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Sioux Falls, SD","doi":"10.3133/70159087","usgsCitation":"Bauer, B.P., 1980, A survey of image processing developments in support of remote sensing, iv, 33 p., https://doi.org/10.3133/70159087.","productDescription":"iv, 33 p.","numberOfPages":"38","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[{"id":222,"text":"Earth Resources Observation and Science (EROS) Center","active":true,"usgs":true}],"links":[{"id":309915,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/70159087.jpg"},{"id":310361,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/unnumbered/70159087/report.pdf","text":"Report","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"5620ce47e4b06217fc478aba","contributors":{"authors":[{"text":"Bauer, Brian P.","contributorId":58946,"corporation":false,"usgs":true,"family":"Bauer","given":"Brian","email":"","middleInitial":"P.","affiliations":[],"preferred":false,"id":577567,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":70207259,"text":"70207259 - 1980 - Research on interactive genetic-geological models to evaluate favourability for undiscovered uranium resources","interactions":[],"lastModifiedDate":"2020-06-01T19:52:46.74834","indexId":"70207259","displayToPublicDate":"1980-12-13T14:24:19","publicationYear":"1980","noYear":false,"publicationType":{"id":24,"text":"Conference Paper"},"publicationSubtype":{"id":19,"text":"Conference Paper"},"title":"Research on interactive genetic-geological models to evaluate favourability for undiscovered uranium resources","docAbstract":"<p>Current methods of evaluating favourability for undiscovered uranium resources are unduly subjective, quite possibly inconsistent and, as a consequence, of questionable reliability. This research is aimed at reducing the subjectivity and increasing the reliability by designing an improved method that depends largely on geological data and their statistical frequency of occurrence. This progress report outlines a genetic approach to modelling the geological factors that controlled uranium mineralization in order to evaluate the favourability for the occurrence of undiscovered uranium deposits of the type modeled. A genetic model is constructed from all the factors that describe the processes, in chronological sequence, that formed uranium deposits thought to have a common origin. The field and laboratory evidence for the processes constitute a geologic occurrence base that parallels the chronological sequence of events. The genetic model and the geologic-occurrence base are portrayed as two columns of an interactive matrix called the \"genetic-geologic model\". For each column, eight chronological stages are used to describe the overall formation of the uranium deposits. These stages consist of (1) precursor processes; (2) host-rock formation; (3) preparation of host-rock; (4) uranium-source development; (5) transport of uranium; (6) primary uranium deposition; (7) post-deposition modification; and (8) preservation. To apply the genetic-geological model to evaluate favourability, a question is posed that determines the presence or absence of each attribute listed under the geologic-occurrence base. By building a logic circuit of the attributes according to either their essential or non-essential nature, the resultant match between a well-documented control area and the test area may be determined. The degree of match is a measure of favourability for uranium occurrence as hypothesized in the genetic model. This process of geological decision analysis results in a series of favourability maps that can be combined into a final composite favourability map. </p>","largerWorkType":{"id":24,"text":"Conference Paper"},"largerWorkTitle":"Uranium Evaluation and Mining Techniques: Proceedings of a Symposium Held in Buenos Aires, Argentina, 1–4 October 1979","largerWorkSubtype":{"id":19,"text":"Conference Paper"},"conferenceTitle":"Uranium Evaluation and Mining Techniques","conferenceDate":"October, 1-4, 1979","conferenceLocation":"Buenos Aires, Argentina","language":"English","publisher":"IAEA","isbn":"9200402801","usgsCitation":"Finch, W., Granger, H., Lupe, R., and McCammon, R., 1980, Research on interactive genetic-geological models to evaluate favourability for undiscovered uranium resources, <i>in</i> Uranium Evaluation and Mining Techniques: Proceedings of a Symposium Held in Buenos Aires, Argentina, 1–4 October 1979, Buenos Aires, Argentina, October, 1-4, 1979, p. 447-462.","productDescription":"16 p.","startPage":"447","endPage":"462","costCenters":[],"links":[{"id":370266,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","contributors":{"authors":[{"text":"Finch, W.I.","contributorId":75919,"corporation":false,"usgs":true,"family":"Finch","given":"W.I.","email":"","affiliations":[],"preferred":false,"id":777481,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Granger, H.C.","contributorId":15203,"corporation":false,"usgs":true,"family":"Granger","given":"H.C.","email":"","affiliations":[],"preferred":false,"id":777482,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Lupe, R.D.","contributorId":107696,"corporation":false,"usgs":true,"family":"Lupe","given":"R.D.","affiliations":[],"preferred":false,"id":777483,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"McCammon, R.B.","contributorId":17218,"corporation":false,"usgs":true,"family":"McCammon","given":"R.B.","email":"","affiliations":[],"preferred":false,"id":777484,"contributorType":{"id":1,"text":"Authors"},"rank":4}]}}
,{"id":70120130,"text":"70120130 - 1980 - The effect of band loss on estimates of annual survival","interactions":[],"lastModifiedDate":"2014-08-12T13:44:06","indexId":"70120130","displayToPublicDate":"1980-12-01T13:37:13","publicationYear":"1980","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":2284,"text":"Journal of Field Ornithology","active":true,"publicationSubtype":{"id":10}},"title":"The effect of band loss on estimates of annual survival","docAbstract":"<p>Banding has proven to be a useful technique in the study of population dynamics of avian species.  However, band loss has long been recognized as a potential problem, (Hickey, 1952; Ludwig, 1967).  Recently, Brownie et al. (1978) presented 14 models based on an array of explicit assumptions for the analysis of band recovery data.  Various estimation models (assumption sets) allowed survival and/or recovery rates to be (a) constant, (b) time-specific, or (c) time- and age-specific.  Optimal inference methods were employed and statistical tests of critical assumptions were developed and emphasized.</p>\n<br/>\n<p>The methods of Brownie et al. (1978), as with all previously published methods of which we are aware, assume no loss of bands during the study.  However, some band loss is certain to occur and this potentially biases the estimates of annual survival rates whatever the analysis method.  A few empirical studies have estimated band loss rates (a notable exception is Ludwig, 1967); consequently, for almost all band recovery data, the exact rate of band loss is unknown.  In this paper we investigate the bias in estimates of annual survival rates due to varying degrees of hypothesized band loss.  Our main results are based on perhaps the most useful model, originally developed by Seber (1970), for estimation of annual survival rate.  Inferences are made concerning the bias of estimated survival rates in other models because the structure of these estimators is similar.</p>","largerWorkType":{"id":2,"text":"Article"},"largerWorkTitle":"Journal of Field Ornithology","largerWorkSubtype":{"id":10,"text":"Journal Article"},"language":"English","publisher":"Northeastern Bird-Banding Association","publisherLocation":"Ipswich, NH","usgsCitation":"Nelson, L.J., Anderson, D.R., and Burnham, K.P., 1980, The effect of band loss on estimates of annual survival: Journal of Field Ornithology, v. 51, no. 1, p. 30-38.","productDescription":"9 p.","startPage":"30","endPage":"38","numberOfPages":"9","costCenters":[],"links":[{"id":292037,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"51","issue":"1","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"53eb2a90e4b0461e44764ad7","contributors":{"authors":[{"text":"Nelson, Louis J.","contributorId":106028,"corporation":false,"usgs":true,"family":"Nelson","given":"Louis","email":"","middleInitial":"J.","affiliations":[],"preferred":false,"id":497945,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Anderson, David R.","contributorId":92722,"corporation":false,"usgs":true,"family":"Anderson","given":"David","email":"","middleInitial":"R.","affiliations":[],"preferred":false,"id":497943,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Burnham, Kenneth P.","contributorId":95025,"corporation":false,"usgs":true,"family":"Burnham","given":"Kenneth","email":"","middleInitial":"P.","affiliations":[{"id":189,"text":"Colorado Cooperative Fish and Wildlife Research Unit","active":false,"usgs":true}],"preferred":false,"id":497944,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":5221569,"text":"5221569 - 1980 - Food use and nutrition of black ducks nesting in Maine","interactions":[],"lastModifiedDate":"2024-10-28T16:49:18.76086","indexId":"5221569","displayToPublicDate":"1980-07-02T00:00:00","publicationYear":"1980","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":2508,"text":"Journal of Wildlife Management","active":true,"publicationSubtype":{"id":10}},"title":"Food use and nutrition of black ducks nesting in Maine","docAbstract":"<p>Based on 32 adult black ducks (<i>Anas rubripes</i>) collected during the nesting seasons of 1974-76, the proportion of macro invertebrates (as aggregate [average] percent of dry weight) in the diet of males, egg-laying females, and postlaying females was 60, 75, and 55%, respectivey. Sample sizes were small, and the differences associated with sex and reproductive condition were not signficant. Molluscs, Isopods, ephemeropteran and odonate nymphs, and coleopteran, trichopteran, and dipteran larvae contributed 74% of the dry weight and 64% of the gross energy ingested. Data from proximate analyses of 9 invertebrate and 9 plant foods were combined with food habits data to estimate the nutrients available to breeding hens. We concluded that females with access to an adequate amount of natural food including invertebrates and the seeds and tubers of aquatic plants would obtain sufficient minerals, protein, and energy for reproduction. Food quality does not appear to limit the density of black ducks nesting in Maine.</p>","language":"English","publisher":"Wiley","doi":"10.2307/3808002","usgsCitation":"Reinecke, K., and Owen, R.B., 1980, Food use and nutrition of black ducks nesting in Maine: Journal of Wildlife Management, v. 44, no. 3, p. 549-558, https://doi.org/10.2307/3808002.","productDescription":"10 p.","startPage":"549","endPage":"558","costCenters":[{"id":531,"text":"Patuxent Wildlife Research Center","active":true,"usgs":true}],"links":[{"id":196546,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United 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 \"}}]}","volume":"44","issue":"3","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b24e4b07f02db6ae6fc","contributors":{"authors":[{"text":"Reinecke, Kenneth J.","contributorId":340946,"corporation":false,"usgs":false,"family":"Reinecke","given":"Kenneth J.","affiliations":[{"id":81683,"text":"Patuxent Retired","active":true,"usgs":false}],"preferred":false,"id":334166,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Owen, Ray B. Jr.","contributorId":35030,"corporation":false,"usgs":true,"family":"Owen","given":"Ray","suffix":"Jr.","email":"","middleInitial":"B.","affiliations":[],"preferred":false,"id":334167,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":70120079,"text":"70120079 - 1980 - Effect of delayed reporting of band recoveries on survival estimates","interactions":[],"lastModifiedDate":"2014-08-12T09:27:31","indexId":"70120079","displayToPublicDate":"1980-07-01T09:18:16","publicationYear":"1980","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":2284,"text":"Journal of Field Ornithology","active":true,"publicationSubtype":{"id":10}},"title":"Effect of delayed reporting of band recoveries on survival estimates","docAbstract":"<p>Brownie et al. (U.S. Fish and Wildl. Serv., Resource Publ. 131, 1978) presented 14 models based on an array of explicit assumptions for the study of survival in avian populations.  These methods are replacing the life table methods previously used to estimate survival rates (e.g., Burnham and Anderson, <i>J. Wildl. Manage.</i>, <b>43:</b> 356-366, 1979).  The new methods allow survival or recovery rates, or both, to be constant, time-specific, or time- and age-specific.</p>\n<br/>\n<p>In studies to estimate survival rates for birds the data are often from recoveries of birds shot or found dead during the hunting season and reported to the Bird Banding Laboratory by sportsmen, conservation agency employees, or the general public.  This note examines the bias in estimating annual survival due to a proportion of the recoveries being incorrectly reported a year late.  Specifically, a few recoveries each year of, for example, adult male American Widgeon (<i>Anas americana</i>) banded in California are reported as being recovered in year i + 1 when in fact they were actually recovered the previous year i.  Delayed reporting might typically be caused by people finding a band in their health clothing in the fall of the year and, being embarrassed about their failure to report the band when it was taken, report it a year late not mentioning the actual year of recovery.  Heuristically, delayed reporting should bias estimated annual survival rates upwards because it appears from the data that the birds corresponding to the \"delayed\" recoveries actually lived an additional year.</p>","largerWorkType":{"id":2,"text":"Article"},"largerWorkTitle":"Journal of Field Ornithology","largerWorkSubtype":{"id":10,"text":"Journal Article"},"language":"English","publisher":"Northeastern Bird-Banding Association","publisherLocation":"Ipswich, NH","usgsCitation":"Anderson, D.R., and Burnham, K.P., 1980, Effect of delayed reporting of band recoveries on survival estimates: Journal of Field Ornithology, v. 51, no. 3, p. 244-247.","productDescription":"4 p.","startPage":"244","endPage":"247","numberOfPages":"4","costCenters":[],"links":[{"id":291991,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"51","issue":"3","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"53eb2a68e4b0461e447649f6","contributors":{"authors":[{"text":"Anderson, David R.","contributorId":92722,"corporation":false,"usgs":true,"family":"Anderson","given":"David","email":"","middleInitial":"R.","affiliations":[],"preferred":false,"id":497875,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Burnham, Kenneth P.","contributorId":95025,"corporation":false,"usgs":true,"family":"Burnham","given":"Kenneth","email":"","middleInitial":"P.","affiliations":[{"id":189,"text":"Colorado Cooperative Fish and Wildlife Research Unit","active":false,"usgs":true}],"preferred":false,"id":497876,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":70157201,"text":"70157201 - 1980 - Main image file tape description","interactions":[],"lastModifiedDate":"2015-10-05T13:28:24","indexId":"70157201","displayToPublicDate":"1980-05-31T19:45:00","publicationYear":"1980","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":6,"text":"USGS Unnumbered Series"},"title":"Main image file tape description","docAbstract":"<p>This Main Image File Tape document defines the data content and file structure of the Main Image File Tape (MIFT) produced by the EROS Data Center (EDC). This document also defines an INQUIRY tape, which is just a subset of the MIFT. The format of the INQUIRY tape is identical to the MIFT except for two records; therefore, with the exception of these two records (described elsewhere in this document), every remark made about the MIFT is true for the INQUIRY tape.</p>","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Reston, VA","doi":"10.3133/70157201","usgsCitation":"Warriner, H.W., 1980, Main image file tape description, iii, 84 p., https://doi.org/10.3133/70157201.","productDescription":"iii, 84 p.","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[{"id":222,"text":"Earth Resources Observation and Science (EROS) Center","active":true,"usgs":true}],"links":[{"id":309508,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/70157201.JPG"},{"id":309507,"rank":1,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/unnumbered/70157201/report.pdf","text":"Report","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"55f7efbae4b05d6c4e4fa97e","contributors":{"authors":[{"text":"Warriner, Howard W.","contributorId":46422,"corporation":false,"usgs":true,"family":"Warriner","given":"Howard","email":"","middleInitial":"W.","affiliations":[],"preferred":false,"id":572244,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":70012433,"text":"70012433 - 1980 - Sediment transport in Norton Sound, Alaska","interactions":[],"lastModifiedDate":"2024-10-11T15:35:55.48006","indexId":"70012433","displayToPublicDate":"1980-05-01T00:00:00","publicationYear":"1980","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":2667,"text":"Marine Geology","active":true,"publicationSubtype":{"id":10}},"title":"Sediment transport in Norton Sound, Alaska","docAbstract":"<p>The Yukon River, the largest single source of Bering Sea sediment, delivers &gt; 95% of its sediment load at the southwest comer of Norton Sound during the ice-free months of late May through October. During this period, surface winds in the northern Bering Sea area are generally light from the south and southwest, and surface waves are not significant. Although wind stress may cause some transport of low-density turbid surface water into the head of Norton Sound, the most significant transport of Yukon River suspended matter occurs within advective currents flowing north across the outer part of the sound. The thickest accumulations of modern Yukon silt and very fine sand occur beneath this persistent current.</p><p><span>We monitored temporal variations in bottom currents, pressure, and suspended-matter concentrations within this major transport pathway for 80 days in the summer of 1977 using a Geological Processes Bottom Environmental (GEOPROBE) tripod system. The record reveals two distinctive periods of bottom flow and sediment transport: an initial 59 days (July 8–September 5) of fair-weather conditions, characterized by tidally dominated currents and relatively low, stable suspended-matter concentrations; and a 21-day period (September 5–September 26) during which several storms traversed the northern Bering Sea, mean suspended-matter concentrations near the bottom increased by a factor of five, and the earlier tidal dominance was overshadowed by wind-driven and oscillatory wave-generated currents.</span></p><p><span>Friction velocities (u<sub>*</sub>) at the GEOPROBE site were generally subcritical during the initial fair-weather period. In contrast, the 21-day stormy period was characterized by uFriction velocities (u<sub>*</sub>) at the GEOPROBE site were generally subcritical during the initial fair-weather period. In contrast, the 21-day stormy period was characterized by u<sub>*</sub>values that exceeded the critical level of 1.3 cm/s more than 60% of the time. The GEOPROBE data suggest that the very fine sand constituting about 50% of the sediment on the outer part of the Yukon prodelta is transported during a few late-summer and fall storms each year. A conservative estimate shows that suspended-matter transport during the storms in September 1977 was equal to four months of fair-weather transport.  values that exceeded the critical level of 1.3 cm/s more than 60% of the time. The GEOPROBE data suggest that the very fine sand constituting about 50% of the sediment on the outer part of the Yukon prodelta is transported during a few late-summer and fall storms each year. A conservative estimate shows that suspended-matter transport during the storms in September 1977 was equal to four months of fair-weather transport. </span></p>","language":"English","publisher":"Elsevier","doi":"10.1016/0025-3227(80)90043-2","usgsCitation":"Drake, D., Cacchione, D., Muench, R., and Nelson, C., 1980, Sediment transport in Norton Sound, Alaska: Marine Geology, v. 36, no. 1-2, p. 97-126, https://doi.org/10.1016/0025-3227(80)90043-2.","productDescription":"30 p.","startPage":"97","endPage":"126","costCenters":[],"links":[{"id":222201,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United States","state":"Alaska","otherGeospatial":"Norton Sound","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"coordinates\": [\n          [\n            [\n              -166.93816207810704,\n              65.1847517876121\n            ],\n            [\n              -166.93816207810704,\n              62.997485781439735\n            ],\n            [\n              -160.32671205235334,\n              62.997485781439735\n            ],\n            [\n              -160.32671205235334,\n              65.1847517876121\n            ],\n            [\n              -166.93816207810704,\n              65.1847517876121\n            ]\n          ]\n        ],\n        \"type\": \"Polygon\"\n      }\n    }\n  ]\n}","volume":"36","issue":"1-2","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"505b89d9e4b08c986b316ee5","contributors":{"authors":[{"text":"Drake, D.E.","contributorId":48150,"corporation":false,"usgs":true,"family":"Drake","given":"D.E.","email":"","affiliations":[],"preferred":false,"id":363567,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Cacchione, D.A.","contributorId":65448,"corporation":false,"usgs":true,"family":"Cacchione","given":"D.A.","affiliations":[{"id":520,"text":"Pacific Coastal and Marine Science Center","active":true,"usgs":true}],"preferred":false,"id":363568,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Muench, R.D.","contributorId":83270,"corporation":false,"usgs":true,"family":"Muench","given":"R.D.","email":"","affiliations":[],"preferred":false,"id":363569,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Nelson, C.H.","contributorId":88346,"corporation":false,"usgs":true,"family":"Nelson","given":"C.H.","email":"","affiliations":[],"preferred":false,"id":363570,"contributorType":{"id":1,"text":"Authors"},"rank":4}]}}
,{"id":70112923,"text":"70112923 - 1980 - Detection and modeling of subsurface coal oxidation","interactions":[],"lastModifiedDate":"2014-06-18T12:13:03","indexId":"70112923","displayToPublicDate":"1980-04-16T12:07:48","publicationYear":"1980","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":3393,"text":"Sixth Annual Pecora Symposium and Exposition","active":true,"publicationSubtype":{"id":10}},"title":"Detection and modeling of subsurface coal oxidation","docAbstract":"<p>The oxidation and sustained ignition of coal and coaly wastes within surface coal mine spoils in the southwestern U.S. have hampered the success of reclamation efforts at these locations.  To assess better the magnitude, depth, geometry, and dynamics of the oxidation process thermal infrared remote sensing data have been used.  Digital thermal imagery was found to be useful for this purpose and was integrated with finite different heat transfer models to yield predictions of several characteristics of the thermal source.  In addition to thermal infrared imagery, aerial color and false color infrared imagery were found to provide useful information for the interpretation of oxidation phenomena by means of variations in surface vegetation, color of the surface material, subsidence, etc.  The combined use of thermal infrared imagery and thermal modeling techniques are well suited for use in exploration and interpretation of other thermal targets.</p>","largerWorkType":{"id":2,"text":"Article"},"largerWorkTitle":"Sixth Annual Pecora Symposium and Exposition","largerWorkSubtype":{"id":10,"text":"Journal Article"},"language":"English","publisher":"Society of Exploration Geophysicists","publisherLocation":"Tulsa, OK","usgsCitation":"Leonhart, L.S., and Rasmussen, W.O., 1980, Detection and modeling of subsurface coal oxidation: Sixth Annual Pecora Symposium and Exposition, p. 83-83.","productDescription":"1 p.","startPage":"83","endPage":"83","numberOfPages":"1","costCenters":[],"links":[{"id":288805,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"53ae7680e4b0abf75cf2bf72","contributors":{"editors":[{"text":"Barringer, Anthony R.","contributorId":112053,"corporation":false,"usgs":true,"family":"Barringer","given":"Anthony","email":"","middleInitial":"R.","affiliations":[],"preferred":false,"id":509904,"contributorType":{"id":2,"text":"Editors"},"rank":1}],"authors":[{"text":"Leonhart, Leo S.","contributorId":77050,"corporation":false,"usgs":true,"family":"Leonhart","given":"Leo","email":"","middleInitial":"S.","affiliations":[],"preferred":false,"id":494944,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Rasmussen, William O.","contributorId":6376,"corporation":false,"usgs":true,"family":"Rasmussen","given":"William","email":"","middleInitial":"O.","affiliations":[],"preferred":false,"id":494943,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":70112909,"text":"70112909 - 1980 - Interpretation of long- and short-wavelength magnetic anomalies","interactions":[],"lastModifiedDate":"2014-06-18T10:57:11","indexId":"70112909","displayToPublicDate":"1980-04-15T10:40:00","publicationYear":"1980","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":3393,"text":"Sixth Annual Pecora Symposium and Exposition","active":true,"publicationSubtype":{"id":10}},"title":"Interpretation of long- and short-wavelength magnetic anomalies","docAbstract":"<p>Magset was launched on October 30, 1979.  More than a decade of examining existing data, devising appropriate models of the global magnetic field, and extending methods for interpreting long-wavelength magnetic anomalies preceded this launch</p>\n<br/>\n<p>Magnetic data collected by satellite can be interrupted by using a method of analysis that quantitively describes the magnetic field resulting from three-dimensional geologic structures that are bounded by an arbitrary number of polygonal faces,  Each face my have any orientation and three or more sides.  At each point of the external field, the component normal to each face is obtained by using an expression for the solid angle subtended by a generalized polygon.  The \"cross\" of tangential components are relatively easy to obtain for the same polygons.</p>\n<br/>\n<p>No approximations have been made related to orbit height that restrict the dimensions of the polygons relative to the distance from the external field points.  This permits the method to be used to model shorter wavelength anomalies obtained from aircraft or ground surveys.</p>\n<br/>\n<p>The magnetic fields for all the structures considered are determine in the same rectangular coordinate system.  The coordinate system is in depended from the orientation of geologic trends and permits multiple structures or bodies to be included in the same magnetic field calculations.  This single reference system also simplified adjustments in position and direction to account for earth curvature in regional interpretation.</p>","largerWorkType":{"id":2,"text":"Article"},"largerWorkTitle":"Sixth Annual Pecora Symposium and Exposition","largerWorkSubtype":{"id":10,"text":"Journal Article"},"language":"English","publisher":"Society of Exploration Geophysicists","publisherLocation":"Tulsa, OK","usgsCitation":"DeNoyer, J.M., 1980, Interpretation of long- and short-wavelength magnetic anomalies: Sixth Annual Pecora Symposium and Exposition, p. 51-51.","productDescription":"1 p.","startPage":"51","endPage":"51","numberOfPages":"1","costCenters":[],"links":[{"id":288790,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"53ae7753e4b0abf75cf2c0f9","contributors":{"editors":[{"text":"Barringer, Anthony R.","contributorId":112053,"corporation":false,"usgs":true,"family":"Barringer","given":"Anthony","email":"","middleInitial":"R.","affiliations":[],"preferred":false,"id":509899,"contributorType":{"id":2,"text":"Editors"},"rank":1}],"authors":[{"text":"DeNoyer, John M.","contributorId":96271,"corporation":false,"usgs":true,"family":"DeNoyer","given":"John","email":"","middleInitial":"M.","affiliations":[],"preferred":false,"id":494911,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":70112908,"text":"70112908 - 1980 - Digital mapping of limonitic rocks by using Landsat MSS radio data","interactions":[],"lastModifiedDate":"2014-06-18T10:38:09","indexId":"70112908","displayToPublicDate":"1980-04-15T10:30:00","publicationYear":"1980","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":3393,"text":"Sixth Annual Pecora Symposium and Exposition","active":true,"publicationSubtype":{"id":10}},"title":"Digital mapping of limonitic rocks by using Landsat MSS radio data","docAbstract":"<p>Color-ratio composite images of Landsat MSS (multi-spectral scanner) bands have been used by other workers to map the distribution of limonitic rocks in semi-arid and arid areas as possible indicators of hydrothermal alteration (Rowan et al, 1974).  The images are particularly useful for broad overviews, but detailed analysis at large scales requires both numerical analysis of the ratio values to distinguish consistently among categories of limonitic rocks and a precise transfer of the data to large-scale base maps.  Both requirements can be met by digital classification followed by a precise geometric registration of the classified data.</p>","largerWorkType":{"id":2,"text":"Article"},"largerWorkTitle":"Sixth Annual Pecora Symposium and Exposition","largerWorkSubtype":{"id":10,"text":"Journal Article"},"language":"English","publisher":"Society of Exploration Geophysicists","publisherLocation":"Tulsa, OK","usgsCitation":"Podwysocki, M.H., Segal, D.B., and Simpson, S., 1980, Digital mapping of limonitic rocks by using Landsat MSS radio data: Sixth Annual Pecora Symposium and Exposition, p. 49-51.","productDescription":"3 p.","startPage":"49","endPage":"51","numberOfPages":"3","costCenters":[],"links":[{"id":288779,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"53ae7683e4b0abf75cf2bf7f","contributors":{"editors":[{"text":"Barringer, Anthony R.","contributorId":112053,"corporation":false,"usgs":true,"family":"Barringer","given":"Anthony","email":"","middleInitial":"R.","affiliations":[],"preferred":false,"id":509898,"contributorType":{"id":2,"text":"Editors"},"rank":1}],"authors":[{"text":"Podwysocki, Melvin H.","contributorId":60220,"corporation":false,"usgs":true,"family":"Podwysocki","given":"Melvin","email":"","middleInitial":"H.","affiliations":[],"preferred":false,"id":494910,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Segal, Donald B.","contributorId":40223,"corporation":false,"usgs":true,"family":"Segal","given":"Donald","email":"","middleInitial":"B.","affiliations":[],"preferred":false,"id":494908,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Simpson, Shirley","contributorId":48100,"corporation":false,"usgs":true,"family":"Simpson","given":"Shirley","affiliations":[],"preferred":false,"id":494909,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":70112916,"text":"70112916 - 1980 - Airborne-biogeochemical survey test-case results","interactions":[],"lastModifiedDate":"2014-06-18T12:03:24","indexId":"70112916","displayToPublicDate":"1980-04-14T11:47:59","publicationYear":"1980","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":3393,"text":"Sixth Annual Pecora Symposium and Exposition","active":true,"publicationSubtype":{"id":10}},"title":"Airborne-biogeochemical survey test-case results","docAbstract":"<p>Airborne spectroradiometer surveys over several forest-covered sulfide bodies indicate that mineralization has affected the overlying vegetation; anomalous spectral reflectivity properties can be detected in the vegetation using appropriate remote-sensing interments and data-reduction techniques.  Mineralization induces subtle changes in the shape of the chlorophyll <i>a</i> and <i>b</i> absorption spectrum between 550 and 750 nm.  The observed spectral variations appear specifically to be on the wings of the broad red chlorophyll bars, centered at about 680 nm.</p>","largerWorkType":{"id":2,"text":"Article"},"largerWorkTitle":"Sixth Annual Pecora Symposium and Exposition","largerWorkSubtype":{"id":10,"text":"Journal Article"},"language":"English","publisher":"Society of Exploration Geophysicists","publisherLocation":"Tulsa, OK","usgsCitation":"Collins, W.E., Chang, S., Raines, G.L., Canney, F.C., and Ashley, R., 1980, Airborne-biogeochemical survey test-case results: Sixth Annual Pecora Symposium and Exposition, p. 71-73.","productDescription":"3 p.","startPage":"71","endPage":"73","numberOfPages":"3","costCenters":[],"links":[{"id":288804,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"53ae7624e4b0abf75cf2bea1","contributors":{"editors":[{"text":"Barringer, Anthony R.","contributorId":112053,"corporation":false,"usgs":true,"family":"Barringer","given":"Anthony","email":"","middleInitial":"R.","affiliations":[],"preferred":false,"id":509903,"contributorType":{"id":2,"text":"Editors"},"rank":1}],"authors":[{"text":"Collins, William E.","contributorId":37474,"corporation":false,"usgs":true,"family":"Collins","given":"William","email":"","middleInitial":"E.","affiliations":[],"preferred":false,"id":494921,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Chang, Sheng-Huei","contributorId":37256,"corporation":false,"usgs":true,"family":"Chang","given":"Sheng-Huei","email":"","affiliations":[],"preferred":false,"id":494920,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Raines, Gary L.","contributorId":48162,"corporation":false,"usgs":true,"family":"Raines","given":"Gary","email":"","middleInitial":"L.","affiliations":[],"preferred":false,"id":494922,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Canney, Frank C.","contributorId":91251,"corporation":false,"usgs":true,"family":"Canney","given":"Frank","email":"","middleInitial":"C.","affiliations":[],"preferred":false,"id":494923,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"Ashley, Roger","contributorId":7625,"corporation":false,"usgs":true,"family":"Ashley","given":"Roger","affiliations":[],"preferred":false,"id":494919,"contributorType":{"id":1,"text":"Authors"},"rank":5}]}}
,{"id":23595,"text":"ofr801207 - 1980 - Water-resources investigations, Collier County, Florida","interactions":[],"lastModifiedDate":"2022-01-05T15:17:00.087609","indexId":"ofr801207","displayToPublicDate":"1980-01-01T22:05:00","publicationYear":"1980","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":330,"text":"Open-File Report","code":"OFR","onlineIssn":"2331-1258","printIssn":"0196-1497","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"80-1207","title":"Water-resources investigations, Collier County, Florida","docAbstract":"Early water-resources investigations in Collier County, Fla., were related to saltwater intrusion in Naples. With the advent of canal drainage and land reclamation farther inland, investigations were directed at effects of canals on water resources and the environment. High on the list of investigative needs are: (1) areal and vertical delineation of the shallow aquifer, the prime source of freshwater; (2) delineation of areas of poor quality ground water and the sources of the poor quality; (3) establishment of network of hydrologic data stations; and (4) determination of the relation between canals and the shallow aquifer. 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href=\"https://www.usgs.gov/centers/car-fl-water\" data-mce-href=\"https://www.usgs.gov/centers/car-fl-water\">Caribbean-Florida Water Science Center</a><br>U.S. Geological Survey<br>3321 College Avenue<br>Davie, FL 33314</p><p><a href=\"../contact\" data-mce-href=\"../contact\">Contact Pubs Warehouse</a></p>","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e49e2e4b07f02db5e4df9","contributors":{"authors":[{"text":"Klein, Howard","contributorId":62189,"corporation":false,"usgs":true,"family":"Klein","given":"Howard","email":"","affiliations":[],"preferred":false,"id":190379,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":70236564,"text":"70236564 - 1980 - Vegetation and terrain mapping of Lake Mead National Recreation Area using LANDSAT digital data","interactions":[],"lastModifiedDate":"2022-09-09T19:12:11.041245","indexId":"70236564","displayToPublicDate":"1980-01-01T13:55:49","publicationYear":"1980","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":12583,"text":"Professional Paper","active":false,"publicationSubtype":{"id":10}},"title":"Vegetation and terrain mapping of Lake Mead National Recreation Area using LANDSAT digital data","docAbstract":"<p>No abstract available.</p>","language":"English","publisher":"Department of Geography and Geology, Indiana State University","usgsCitation":"Todd, W.J., and Gehring, D.G., 1980, Vegetation and terrain mapping of Lake Mead National Recreation Area using LANDSAT digital data: Professional Paper, p. 3-24.","productDescription":"22 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,{"id":70236972,"text":"70236972 - 1980 - An assessment of Landsat data acquisition history on identification and area estimation of corn and soybeans","interactions":[],"lastModifiedDate":"2022-09-23T17:51:37.428651","indexId":"70236972","displayToPublicDate":"1980-01-01T12:37:08","publicationYear":"1980","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":3,"text":"Organization Series"},"seriesTitle":{"id":222,"text":"Technical Report","active":false,"publicationSubtype":{"id":3}},"title":"An assessment of Landsat data acquisition history on identification and area estimation of corn and soybeans","docAbstract":"<p>During the past decade, numerous studies have demonstrated the potential of satellite remote sensing for providing accurate and timely crop area information. This study assessed the impact of Landsat data acquisition history on classification and area estimation accuracy of corn and soybeans.</p><p>Multitemporally registered Landsat MSS data from four acquisitions during the 1978 growing season were used in classification of eight sample segments in the U.S. Corn Belt. The results illustrate the importance of selecting Landsat acquisitions based on spectral differences in crops at certain growth stages.</p>","largerWorkType":{"id":18,"text":"Report"},"largerWorkTitle":"LARS technical reports","largerWorkSubtype":{"id":3,"text":"Organization Series"},"language":"English","publisher":"Laboratory for Applications of Remote Sensing","usgsCitation":"Hixon, M., Bauer, M.E., and Scholz, D.K., 1980, An assessment of Landsat data acquisition history on identification and area estimation of corn and soybeans: Technical Report, 53, 6 p.","productDescription":"53, 6 p.","startPage":"72","endPage":"77","costCenters":[{"id":222,"text":"Earth Resources Observation and Science (EROS) Center","active":true,"usgs":true}],"links":[{"id":407277,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"},{"id":407276,"rank":1,"type":{"id":15,"text":"Index Page"},"url":"https://docs.lib.purdue.edu/larstech/53/"}],"noUsgsAuthors":false,"publicationStatus":"PW","contributors":{"authors":[{"text":"Hixon, M.A.","contributorId":111865,"corporation":false,"usgs":true,"family":"Hixon","given":"M.A.","email":"","affiliations":[],"preferred":false,"id":852871,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Bauer, M. E.","contributorId":35605,"corporation":false,"usgs":true,"family":"Bauer","given":"M.","email":"","middleInitial":"E.","affiliations":[],"preferred":false,"id":852872,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Scholz, Donna K.","contributorId":105135,"corporation":false,"usgs":true,"family":"Scholz","given":"Donna","email":"","middleInitial":"K.","affiliations":[],"preferred":false,"id":852873,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":70039234,"text":"70039234 - 1980 - Introduction to the U.S. Geological Survey's EROS Data Center Sioux Falls, South Dakota","interactions":[],"lastModifiedDate":"2012-08-03T01:02:04","indexId":"70039234","displayToPublicDate":"1980-01-01T11:56:00","publicationYear":"1980","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":6,"text":"USGS Unnumbered Series"},"seriesTitle":{"id":362,"text":"General Information Product","active":false,"publicationSubtype":{"id":6}},"title":"Introduction to the U.S. Geological Survey's EROS Data Center Sioux Falls, South Dakota","docAbstract":"The EROS Data Center is a part of the Earth Resources Observation Systems (EROS) Office of the Department of the Interior and is managed by the U.S. Geological Survey. It is the national clearinghouse for the processing and dissemination of spacecraft- and aircraft-acquired images and photographs and electronic data on the Earth's resources. The Center also trains and assists users in the application of such data.","language":"English","publisher":"U.S. Government Printing Office","publisherLocation":"Washington, D.C.","doi":"10.3133/70039234","usgsCitation":"Braconnier, L., and Wiepking, P., 1980, Introduction to the U.S. Geological Survey's EROS Data Center Sioux Falls, South Dakota: General Information Product, 4 p. (11 columns), https://doi.org/10.3133/70039234.","productDescription":"4 p. (11 columns)","costCenters":[{"id":222,"text":"Earth Resources Observation and Science (EROS) Center","active":true,"usgs":true}],"links":[{"id":261420,"rank":800,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/gip/70039234/report.pdf"},{"id":261421,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/gip/70039234/report-thumb.jpg"}],"country":"United States","state":"South Dakota","city":"Sioux Falls","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -96.63333333333334,43.71666666666667 ], [ -96.63333333333334,43.75 ], [ -96.6,43.75 ], [ -96.6,43.71666666666667 ], [ -96.63333333333334,43.71666666666667 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"505a3dfae4b0c8380cd639e1","contributors":{"authors":[{"text":"Braconnier, L.A.","contributorId":35179,"corporation":false,"usgs":true,"family":"Braconnier","given":"L.A.","email":"","affiliations":[],"preferred":false,"id":465848,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Wiepking, P.J.","contributorId":35172,"corporation":false,"usgs":true,"family":"Wiepking","given":"P.J.","email":"","affiliations":[],"preferred":false,"id":465847,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":70012434,"text":"70012434 - 1980 - Computer-composite mapping for geologists","interactions":[],"lastModifiedDate":"2012-03-12T17:19:04","indexId":"70012434","displayToPublicDate":"1980-01-01T00:00:00","publicationYear":"1980","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1539,"text":"Environmental Geology","active":true,"publicationSubtype":{"id":10}},"title":"Computer-composite mapping for geologists","docAbstract":"A computer program for overlaying maps has been tested and evaluated as a means for producing geologic derivative maps. Four maps of the Sugar House Quadrangle, Utah, were combined, using the Multi-Scale Data Analysis and Mapping Program, in a single composite map that shows the relative stability of the land surface during earthquakes. Computer-composite mapping can provide geologists with a powerful analytical tool and a flexible graphic display technique. Digitized map units can be shown singly, grouped with different units from the same map, or combined with units from other source maps to produce composite maps. The mapping program permits the user to assign various values to the map units and to specify symbology for the final map. Because of its flexible storage, easy manipulation, and capabilities of graphic output, the composite-mapping technique can readily be applied to mapping projects in sedimentary and crystalline terranes, as well as to maps showing mineral resource potential. ?? 1980 Springer-Verlag New York Inc.","largerWorkType":{"id":2,"text":"Article"},"largerWorkTitle":"Environmental Geology","largerWorkSubtype":{"id":10,"text":"Journal Article"},"language":"English","publisherLocation":"Springer-Verlag","doi":"10.1007/BF02473490","issn":"09430105","usgsCitation":"van Driel, J., 1980, Computer-composite mapping for geologists: Environmental Geology, v. 3, no. 3, p. 151-157, https://doi.org/10.1007/BF02473490.","startPage":"151","endPage":"157","numberOfPages":"7","costCenters":[],"links":[{"id":205212,"rank":9999,"type":{"id":10,"text":"Digital Object Identifier"},"url":"https://dx.doi.org/10.1007/BF02473490"},{"id":222202,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"3","issue":"3","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"5059f96fe4b0c8380cd4d5ea","contributors":{"authors":[{"text":"van Driel, J.N.","contributorId":29959,"corporation":false,"usgs":true,"family":"van Driel","given":"J.N.","email":"","affiliations":[],"preferred":false,"id":363571,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":70012583,"text":"70012583 - 1980 - Radioactivity method","interactions":[],"lastModifiedDate":"2024-04-18T16:42:03.970695","indexId":"70012583","displayToPublicDate":"1980-01-01T00:00:00","publicationYear":"1980","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1808,"text":"Geophysics","active":true,"publicationSubtype":{"id":10}},"title":"Radioactivity method","docAbstract":"<p><span>Radioactivity measurements have played an important role in geophysics since about 1935, and they have increased in importance to the present. The most important areas of application have been in petroleum and uranium exploration. Radioactivity measurements have proved useful in geologic mapping, as well as in specialized applications such as reactor-site monitoring. The technological development of the method has reached a plateau, and the future of the method for some applications will depend upon development of more sophisticated data processing and interpretation.</span></p>","language":"English","publisher":"Society of Exploration Geophysicists","doi":"10.1190/1.1441059","issn":"00168033","usgsCitation":"Duval, J.S., 1980, Radioactivity method: Geophysics, v. 45, no. 11, p. 1690-1694, https://doi.org/10.1190/1.1441059.","productDescription":"5 p.","startPage":"1690","endPage":"1694","numberOfPages":"5","costCenters":[],"links":[{"id":221836,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"45","issue":"11","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"505a93c2e4b0c8380cd80feb","contributors":{"authors":[{"text":"Duval, J. S.","contributorId":15200,"corporation":false,"usgs":true,"family":"Duval","given":"J.","email":"","middleInitial":"S.","affiliations":[],"preferred":false,"id":363974,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":70012553,"text":"70012553 - 1980 - Computational methods for a three-dimensional model of the petroleum-discovery process","interactions":[],"lastModifiedDate":"2013-01-21T15:55:26","indexId":"70012553","displayToPublicDate":"1980-01-01T00:00:00","publicationYear":"1980","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1315,"text":"Computers & Geosciences","printIssn":"0098-3004","active":true,"publicationSubtype":{"id":10}},"title":"Computational methods for a three-dimensional model of the petroleum-discovery process","docAbstract":"A discovery-process model devised by Drew, Schuenemeyer, and Root can be used to predict the amount of petroleum to be discovered in a basin from some future level of exploratory effort: the predictions are based on historical drilling and discovery data. Because marginal costs of discovery and production are a function of field size, the model can be used to make estimates of future discoveries within deposit size classes. The modeling approach is a geometric one in which the area searched is a function of the size and shape of the targets being sought. A high correlation is assumed between the surface-projection area of the fields and the volume of petroleum. To predict how much oil remains to be found, the area searched must be computed, and the basin size and discovery efficiency must be estimated. The basin is assumed to be explored randomly rather than by pattern drilling. The model may be used to compute independent estimates of future oil at different depth intervals for a play involving multiple producing horizons. We have written FORTRAN computer programs that are used with Drew, Schuenemeyer, and Root's model to merge the discovery and drilling information and perform the necessary computations to estimate undiscovered petroleum. These program may be modified easily for the estimation of remaining quantities of commodities other than petroleum. ?? 1980.","largerWorkType":{"id":2,"text":"Article"},"largerWorkTitle":"Computers and Geosciences","largerWorkSubtype":{"id":10,"text":"Journal Article"},"language":"English","publisher":"Elsevier","publisherLocation":"Amsterdam, Netherlands","doi":"10.1016/0098-3004(80)90013-8","issn":"00983004","usgsCitation":"Schuenemeyer, J., Bawiec, W., and Drew, L., 1980, Computational methods for a three-dimensional model of the petroleum-discovery process: Computers & Geosciences, v. 6, no. 4, p. 323-360, https://doi.org/10.1016/0098-3004(80)90013-8.","startPage":"323","endPage":"360","numberOfPages":"38","costCenters":[],"links":[{"id":266197,"type":{"id":10,"text":"Digital Object Identifier"},"url":"https://dx.doi.org/10.1016/0098-3004(80)90013-8"},{"id":222147,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"6","issue":"4","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"5059f951e4b0c8380cd4d56d","contributors":{"authors":[{"text":"Schuenemeyer, J.H.","contributorId":106094,"corporation":false,"usgs":true,"family":"Schuenemeyer","given":"J.H.","affiliations":[],"preferred":false,"id":363889,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Bawiec, W.J.","contributorId":71540,"corporation":false,"usgs":true,"family":"Bawiec","given":"W.J.","affiliations":[],"preferred":false,"id":363888,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Drew, L.J.","contributorId":69157,"corporation":false,"usgs":true,"family":"Drew","given":"L.J.","email":"","affiliations":[],"preferred":false,"id":363887,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":70012404,"text":"70012404 - 1980 - A lead isotope study of mineralization in the Saudi Arabian Shield","interactions":[],"lastModifiedDate":"2012-03-12T17:19:01","indexId":"70012404","displayToPublicDate":"1980-01-01T00:00:00","publicationYear":"1980","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1336,"text":"Contributions to Mineralogy and Petrology","active":true,"publicationSubtype":{"id":10}},"title":"A lead isotope study of mineralization in the Saudi Arabian Shield","docAbstract":"New lead isotope data are presented for some late Precambrian and early Paleozoic vein and massive sulfide deposits in the Arabian Shield. Using the Stacey Kramers (1975) model for lead isotope evolution, isochron model ages range between 720 m.y. and 420 m.y. Most of the massive sulfide deposits in the region formed before 680 m.y. ago, during evolution of the shield. Vein type mineralization of higher lead content occurred during the Pan African event about 550 m.y. ago and continued through the Najd period of extensive faulting in the shield that ended about 530 m.y. ago. Late post-tectonic metamorphism may have been responsible for vein deposits that have model ages less than 500 m.y. Alternatively some of these younger model ages may be too low due to the mineralizing fluids acquiring radiogenic lead from appreciably older local crustal rocks at the time of ore formation. The low207Pb/204Pb ratios found for the deposits in the main part of the shield and for those in north-eastern Egypt, indicate that the Arabian craton was formed in an oceanic crustal environment during the late Precambrian. Involvement of older, upper-crustal material in the formation of the ore deposits in this part of the shield is precluded by their low207Pb/204Pb and208Pb/204Pb characteristics. In the eastern part of the shield, east of longitude 44??20???E towards the Al Amar-Idsas fault region, lead data are quite different. They exhibit a linear207Pb/204Pb-206Pb/204Pb relationship together with distinctly higher208Pb/204Pb characteristics. These data imply the existence of lower crustal rocks of early Proterozoic age that apparently have underthrust the shield rocks from the east. If most of the samples we have analyzed from this easterly region were mineralized 530 m.y. ago, then the age of the older continental rocks is 2,100??300 m.y. (2??). The presence of upper crustal rocks, possibly also of early Proterozoic age, is indicated by galena data from Hailan in South Yemen and also from near Muscat in Oman. These data are the first to indicate such old continental material in these regions. ?? 1980 Springer-Verlag.","largerWorkType":{"id":2,"text":"Article"},"largerWorkTitle":"Contributions to Mineralogy and Petrology","largerWorkSubtype":{"id":10,"text":"Journal Article"},"language":"English","publisherLocation":"Springer-Verlag","doi":"10.1007/BF01132003","issn":"00107999","usgsCitation":"Stacey, J.S., Doe, B.R., Roberts, R.J., Delevaux, M., and Gramlich, J.W., 1980, A lead isotope study of mineralization in the Saudi Arabian Shield: Contributions to Mineralogy and Petrology, v. 74, no. 2, p. 175-188, https://doi.org/10.1007/BF01132003.","startPage":"175","endPage":"188","numberOfPages":"14","costCenters":[],"links":[{"id":205282,"rank":9999,"type":{"id":10,"text":"Digital Object Identifier"},"url":"https://dx.doi.org/10.1007/BF01132003"},{"id":222657,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"74","issue":"2","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"5059e435e4b0c8380cd464db","contributors":{"authors":[{"text":"Stacey, J. S.","contributorId":72785,"corporation":false,"usgs":true,"family":"Stacey","given":"J.","email":"","middleInitial":"S.","affiliations":[],"preferred":false,"id":363463,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Doe, B. R.","contributorId":52173,"corporation":false,"usgs":true,"family":"Doe","given":"B.","email":"","middleInitial":"R.","affiliations":[],"preferred":false,"id":363460,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Roberts, R. J.","contributorId":58250,"corporation":false,"usgs":true,"family":"Roberts","given":"R.","email":"","middleInitial":"J.","affiliations":[],"preferred":false,"id":363461,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Delevaux, M.H.","contributorId":27853,"corporation":false,"usgs":true,"family":"Delevaux","given":"M.H.","email":"","affiliations":[],"preferred":false,"id":363459,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"Gramlich, J. W.","contributorId":69967,"corporation":false,"usgs":false,"family":"Gramlich","given":"J.","email":"","middleInitial":"W.","affiliations":[],"preferred":false,"id":363462,"contributorType":{"id":1,"text":"Authors"},"rank":5}]}}
,{"id":70012402,"text":"70012402 - 1980 - Asymmetric measures of association, closed data, and multivariate analysis","interactions":[],"lastModifiedDate":"2012-03-12T17:19:10","indexId":"70012402","displayToPublicDate":"1980-01-01T00:00:00","publicationYear":"1980","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":2554,"text":"Journal of the International Association for Mathematical Geology","active":true,"publicationSubtype":{"id":10}},"title":"Asymmetric measures of association, closed data, and multivariate analysis","docAbstract":"The association between constant-sum variables Xiand Xjexpressed as percentages can be calculated as a product-moment correlation between Xiand Xj/(100 - Xi) and a correlation between Xjand Xi/(100 - Xj). An asymmetric, square matrix may be formed from these coefficients, and multivariate analysis performed by two methods: singular value decomposition and canonical decomposition. Either analysis avoids problems in the interpretation of correlation coefficients determined from closed arrays, and provides information about dependencies among the variables beyond that obtained from the usual correlation coefficient between Xiand Xj. Two examples show the canonical decomposition to have the greater usefulness. ?? 1980 Plenum Publishing Corporation.","largerWorkType":{"id":2,"text":"Article"},"largerWorkTitle":"Journal of the International Association for Mathematical Geology","largerWorkSubtype":{"id":10,"text":"Journal Article"},"language":"English","publisherLocation":"Kluwer Academic Publishers-Plenum Publishers","doi":"10.1007/BF01091206","issn":"00205958","usgsCitation":"Hohn, M., and Nuhfer, E., 1980, Asymmetric measures of association, closed data, and multivariate analysis: Journal of the International Association for Mathematical Geology, v. 12, no. 3, p. 235-246, https://doi.org/10.1007/BF01091206.","startPage":"235","endPage":"246","numberOfPages":"12","costCenters":[],"links":[{"id":205281,"rank":9999,"type":{"id":10,"text":"Digital Object Identifier"},"url":"https://dx.doi.org/10.1007/BF01091206"},{"id":222655,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"12","issue":"3","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"5059ee97e4b0c8380cd49e4f","contributors":{"authors":[{"text":"Hohn, M.","contributorId":92427,"corporation":false,"usgs":true,"family":"Hohn","given":"M.","email":"","affiliations":[],"preferred":false,"id":363456,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Nuhfer, E.B.","contributorId":89281,"corporation":false,"usgs":true,"family":"Nuhfer","given":"E.B.","email":"","affiliations":[],"preferred":false,"id":363455,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":22555,"text":"ofr80703 - 1980 - Seismic engineering data report; the Imperial Valley earthquake, October 15, 1979: Digitization and processing of accelerograph records","interactions":[],"lastModifiedDate":"2022-12-09T21:09:03.777968","indexId":"ofr80703","displayToPublicDate":"1980-01-01T00:00:00","publicationYear":"1980","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":330,"text":"Open-File Report","code":"OFR","onlineIssn":"2331-1258","printIssn":"0196-1497","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"80-703","title":"Seismic engineering data report; the Imperial Valley earthquake, October 15, 1979: Digitization and processing of accelerograph records","docAbstract":"<p>No abstract available.</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr80703","usgsCitation":"Brady, A., Perez, V., and Mork, P.N., 1980, Seismic engineering data report; the Imperial Valley earthquake, October 15, 1979: Digitization and processing of accelerograph records: U.S. Geological Survey Open-File Report 80-703, 311 p., https://doi.org/10.3133/ofr80703.","productDescription":"311 p.","costCenters":[],"links":[{"id":410229,"rank":2,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_75277.htm","linkFileType":{"id":5,"text":"html"}},{"id":52045,"rank":1,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1980/0703/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":154421,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1980/0703/report-thumb.jpg"}],"country":"United States","state":"California","otherGeospatial":"Central Valley","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"coordinates\": [\n          [\n            [\n              -115.8,\n              33.25\n            ],\n            [\n              -115.8,\n              32.667\n            ],\n            [\n              -115.3083,\n              32.667\n            ],\n            [\n              -115.3083,\n              33.25\n            ],\n            [\n              -115.8,\n              33.25\n            ]\n          ]\n        ],\n        \"type\": \"Polygon\"\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a0ae4b07f02db5fb898","contributors":{"authors":[{"text":"Brady, A. G.","contributorId":61794,"corporation":false,"usgs":true,"family":"Brady","given":"A. G.","affiliations":[],"preferred":false,"id":188460,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Perez, Virgilio","contributorId":37740,"corporation":false,"usgs":true,"family":"Perez","given":"Virgilio","email":"","affiliations":[],"preferred":false,"id":188459,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Mork, P. N.","contributorId":33309,"corporation":false,"usgs":true,"family":"Mork","given":"P.","email":"","middleInitial":"N.","affiliations":[],"preferred":false,"id":188458,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
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