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Natural Sources of Contaminants in the Yukon
This study investigated background levels and uptake rates of organophilic metals, particularly selenium, in ten streams draining portions of the Yukon-Tanana Terrane and Cassiar Platform between Ross River and Watson Lake, Yukon. The study area is suspected to have elevated background metals concentrations and is of interest for mineral exploration and development due to high mineralization. Information on natural metals levels is lacking for this region and for the Yukon in general. Water, sediments, benthic invertebrates and fish (slimy sculpin; Cottus cognatus) were sampled and analyzed for metals concentrations. Benthic invertebrates were identified to genus and percent composition of each species in each stream was calculated. The lack of anthropogenic activity in the area indicates that selenium concentrations found in all sample media and natural, background concentrations. Of all the sample media, concentrations of selenium were highest in sediment; however, sediment selenium concentrations were found to be in a range similar to levels documented at the Kudz Ze Kayah and Viceroy Brewery Creek mines in other regions of the Yukon. Selenium concentrations in water generally exceeded CCME guidelines, but also fell within a range similar to the Kudz Ze Kayah and Viceroy Brewery Creek mines. These findings with respect to selenium levels in water and stream sediments highlight the importance of developing site-specific selenium guidelines for management of aquatic systems. The rate of uptake of selenium in benthic invertebrate and fish tissues was greater than that of the other organophilic metals investigated. Selenium concentrations were generally higher in benthic invertebrates than in fish, likely owing to the detritus-feeding and bottom-dwelling life history of these invertebrates. Weak positive trends were noted in the relationship between selenium concentrations in fish and benthic invertebrates, and between fish and the water column. A significant positive relationship was noted between selenium concentrations in fish and stream sediments. These findings are consistent with past studies documenting dietary sources as the most common uptake pathways for selenium, with water comprising a secondary source. Examination of benthic invertebrate community composition revealed commonly abundant species and species typical of fast-flowing streams with high water quality, which is characteristic of the streams in the study area. The findings of this study provide valuable baseline information on background concentrations of metals, particularly selenium, as well as documentation of benthic invertebrate community composition, in an aquatic system that may experience resource development in the future.
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Natural Source Contaminants in the Yukon: Focus on Selenium
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This report is a product of the continuation of a study begun in 2007/08. The 2007/08 report focused on selenium concentrations and pathways in the aquatic ecosystems of various tributaries of the Francis, Finlayson and Pelly rivers, which drain portions of the Yukon Tanana-Terrane and Cassiar Platform between Ross River and Watson Lake. In 2008/09 the sampling program was expanded to another area of the Yukon that is recognized as being highly mineralized: areas within the Selwyn Basin. The 2008/09 study area is located along the North Canol Road, northeast of Ross River.
Yukon Mineral Industry 1941-1959
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This report was prepared to provide published information on the lode and placer mining industries in the Yukon during an important part of its history: mining and milling of Elsa and Keno Hill silver-lead ores had begun; significant nickel, copper, lead and zinc deposits were discovered in the White River, Vangorda Creek, and Macmillan Pass areas; and asbestos deposits were discovered. Placer mining activity continued, although pressures in the form of rising costs, and stable gold prices were forcing the industry into decline. Both the lode and placer mining industries were affected during the war years by shortages of men and equipment, although there was a great deal of attention paid to sources of tungsten, a strategic mineral. Records are not complete. Government office changes, lack of storage space and a warehouse fire may be some of the contributing factors..
Arsenic, chromium, and selenium speciation in Selwyn Basin, Yukon
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At present, little metal speciation information exists for most parts of the Yukon. The current database of knowledge is largely based on research from southern stream environments which tend to be warmer than Yukon streams. This presents a challenge for regulators and practitioners interpreting data from northern systems using guidance that is developed and defined by southern baseline data and effects. This study was designed using a preliminary approach to assist in filling the current information gap. The Selwyn Basin in the Yukon has natural elevated concentrations of metals including arsenic, mercury and selenium (EDI 2008, Gartner Lee 2007). Water quality studies that have been conducted within the Selwyn Basin have not considered the importance of metal speciation and changes in mobility and exposure to aquatic organisms inhabiting lotic watercourses likely impacted by both naturally elevated and anthropogenic (mining related) metal input sources. The objective of this project was to increase the understanding of metal speciation in relation to surface water and sediment metal concentrations within the Selwyn Basin at six discrete lotic watercourse sites over two seasons.
Element distribution in Yukon gold-silver deposits
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One third of the gold and gold-silver deposits in Yukon were examined and sampled in 1980 to establish a framework of geology and rock chemistry from which variations within and between deposits could be detected and evaluated. Lithologic units within the samples were analyzed for Au, Ag, B, Mn, Cu, Zn, As, Se, Tl, Pb, Bi, Sb, Te, W, Hg, Mo and Cd - elements commonly associated with precious metal deposits. A problem which prevented systematic sampling of many deposits is the lack of underground access and the locally intense oxidation of vein outcrops. Three aspects of the rock geochemistry are discussed:: 1) different levels of element concentration in the deposits and implications regarding pathfinder elements; 2) distribution of elements in deposit types; and 3) element distribution in specific deposits. The geology of the deposits is summarized from published works and interpreted in light of recent theories on gold deposits. This report emphasizes common features of the deposits and several genetic models.
Surficial geology and till geochemistry of Weasel Lake (105G/13), central Yukon
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Till geochemistry includes copper, lead, zinc, gold, silver, chromium, nickel, mercury, antimony, and arsenic.
Industrial Minerals, Gems and Minor Metals in the Yukon
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Group 1: Consists of Yukon industrial mineral and minor metals with proven resource which could be developed, given a change in favourble market conditions: Industrial: barite, Minor: antimony, platinum group elements. Group 2: Consists of industrial minerals and minor metals known to occur in the Yukon for which there is a reasonalbe chance of discovering economic deposits: Industrial:asbestos, barite, cassiterite, chromite, clay minerals, feldspathic minerals, fluorspar, garnet, gemstones, graphite, gypsom, limestone, magnesitemanganese oxides, magnetite, mica, nepheline syenite, olivine, peat, phosphate minerals, rare earth elements, silica and quartz, strontium, sulphur, talc, titanium dioxides, zircon. Minor: bismuth, cadmium, chromite, cobalt, niobium, germanium, mercury, molvbdenum, rhenium, selenium, tellurium, tungsten, thorium, vanadium. Group 3: Based on favourable geology, includes industrial minerals and minor metals which, though presently not documented in the Yukon, could be expected to occur in economic deposits: Industrial: abrasives, bentonite, clay minerals, diatomite, gemstone, sillimanite, andalusite, perlite, pumice, tephra, Minor: beryllium, gallium, indium, lithium, scandium. Group 4: Includes industrial minerals and minor metals which have good world market forecasts and/or would be sufficiently cost competitive to encourage exploration: Industrial: dimension stone, celestite, clay minerals, gemstones, graphite, industrial diamond, magnesite, mica, peat, phosphate, rare earth elements, titanium minerals, zircon. Minor: antimony, beryllium, bismuth, niobium, germanium, platinum, and all 'minor metals' recovered as by-products from base and/or precious metal mines. Group 5: Includes industrial minerals which are known to occur in the Yukon, but for which systematic field evaluation is required to document their occurrence, depositional environment, physical and chemical characteristics and reserve potential, in order to determine their development potential: Industrial: dimension stone, limestone, structural clays, peat, sand, and gravel deposits.
A geochemical survey and the nature of lead-silver ores in Sixty Mile River area, Yukon Territory
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A copy of this thesis is available at the EMR library – QE195 C56, This thesis is available online at https://archive.org/details/Cholach1969/mode/2up.
Yukon Mineral Deposits Summary 2009
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The following tables have been compiled from information derived from the Yukon MINFILE 2008 — An database of mineral occurrences (Deklerk, 2008), and from various technical reports and information that have been filed in the SEDAR system by, or on behalf of, public companies. Reserve and resource figures presented are not calculated by Yukon government personnel, but are quoted from referenced industry sources, publications, assessment and/or technical reports, etc. (see next page). The reader is encouraged to refer to the original data for detailed information.
Character of unoxidized gold-silver mineralization and its relationship to beneficiation at the Brown-McDade Zone, Mt. Nansen Property, south-central Yukon
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not_specified
Geology of the White River Native Copper Deposits, Yukon (115F)
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The White River copper deposit, in upper Triassic Nikolai Greenstone of southwestern Yukon, is representative of the native copper-basalt association. Native copper and chalcocite are the association. Native copper and chalcocite are the most abundant ore minerals, but a substantial amount of bornite is known, as well as lesser amounts of chalcopyrite, pyrite, digenite, covellite, cuprite and native silver. These minerals are found in crosscutting fractures, amygdules, gas release tubes, small crackle zones, and as local disseminations in basalt; and although concentrated near the margins of a single glomeroporphyritic unit, are neither confined to that unit nor to a single zone within it. Two stages of copper mineralization are postulated: Stage I mineralization is thought to account for most of the native copper as a product of continental weathering of Nikolai basalts. Stage II mineralization is a much later event characterized by copper sulphides in crosscutting structures. Native copper and copper sulphides of Stage II appear to form a stable and primary product of a low grade (regional) metamorphism indicated by such minerals as chlorite, epidote, prehnite, pumpellyite, calcite analcite and apophyllite which have essentially the same mode of occurrence as primary copper minerals. Consequently, metamorphism (prehnite-pumpellyite facies) is interpreted to have been the mineralizing process. Whole-rock potassium-argon dating suggests an age no older than 120 million years for the metamorphic mineralizing event; hence, stage II mineralization post-dated host rock formation by at least 80 million years. It is probabe that many other copper occurrences in Nikolai Greenstone have formed in a similar manner. Also, it is likely that some of these mineralizing fluids could have moved higher in the stratigraphic sequence and precipitated copper minerals in other units.