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.
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.
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.