💰 J - Casino - Occurrence Details - Yukon Geological Survey

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Topographical Map of Yukon. Levelized Cost of Electrical Power Delivered to the Casino Mine. B.1 Map of Yukon's Past-Producing Mines.


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J - Casino - Occurrence Details - Yukon Geological Survey
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See where Type II mine sites are located in Yukon | Government of Yukon
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Tony Barresi: Exploring a New Gold-Rich Porphyry Discovery in the Yukon

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Topographical Map of Yukon. Levelized Cost of Electrical Power Delivered to the Casino Mine. B.1 Map of Yukon's Past-Producing Mines.


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Abandoned Mine Exploration: Broken Boot Mine - Southern California

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The Yukon Type II mine sites map shows you where these 7 mines are located. A series of slides provides information on each site. Abandoned, former, Faro.


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Developing Canada's Premier Copper-Gold Mine - Western Copper \u0026 Gold Corp.

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Selkirk First Nation APPROACH to Mine Development Figure 1-​2: Road to Casino Concentrator Site from the Yukon River ..​ Figure Casino Deposit Structural Geology Map.


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Interview with Western Copper and Gold's CEO West-Sells at Casino

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WHITEHORSE, YUKON — The large scope of Western Copper and Gold's (TSX: WRN; NYSE-MKT: WRN) proposed Casino mine in the Yukon.


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Casino Mine Project

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Location Maps - Casino Mine, Coffee Creek, Whitehorse mining district, Yukon, Canada. Latitude & Longitude (WGS84): 62° 44' 10'' North, ° 49' 45'' West.


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Western Copper and Gold Corporation - Large Casino Deposit in Yukon

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Casino porphyry copper gold mine project Yukon Territory Canada Western is marching back to the drawing board, hoping to map out a new.


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Casino Mine CEO Says Copper Hotter than 24verno.ru’s Why - Kitco News

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The project will undergo the highest level of review by the Yukon Socio-economic Assessment Board (YESAB). (Cathie Archbould/Casino Mining.


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Western Copper and Gold's Casino project set to become flagship mine for the Yukon

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Mine Life, 22 years (as of Jan 1, ). The Casino Project is located in Yukon, Canada and hosts one of the largest undeveloped copper-gold deposits in.


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Western Copper and Gold: How $360M Infrastructure Package for the Yukon Will Impact Shareholders

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Selkirk First Nation APPROACH to Mine Development Figure 1-​2: Road to Casino Concentrator Site from the Yukon River ..​ Figure Casino Deposit Structural Geology Map.


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Building A Luxurious Goliath Drill Gold Mine - New Gold Mine Location - Hydroneer

The zone is thought is thought to be related to present day topography and is best developed where oxidation of early secondary copper sulphides occur above the water table, on well drained slopes. The Dawson Range batholith is in turn intruded by the Casino Plutonic Suite which is represented by fine- to medium-grained leucocratic granite, quartz monzonite and alaskite with associated aplite phases. Forty-six exploration drill holes 12 An additional 16 drill holes 2 The study recommends that the Casino project be built as an open pit mine and a mill processing tonnes per day of ore, resulting in the production of 14 grams ounces of gold, The study estimated an initial capital cost of 2. The hypogene zone lies under the supergene sulphide zone. Molybdenite is largely unaffected by supergene processes, other than local alteration to ferrimolybdite. At the Casino deposit, the batholith consists of undeformed granodiorite. The Yukon-Tanana terrane is composed dominantly of metamorphic rocks inferred to be Devonian to Mississippian in age that has been intruded by numerous Mesozoic granitic bodies and plutons hosting copper, molybdenum and gold mineralization. The company continued working on the feasibility study through In January , Western Copper and Gold released a compliant feasibility study. The breccia forms an ovoid band around the main porphyry body with dimensions up to m. This study updated the resource figures for the four zones and introduced further refinements to the statistical analysis used to estimate grade and tonnage. The leached cap oxide gold zone is gold-enriched and copper depleted due to supergene alteration processes as well as the lower specific of this zone relative to the other zones. Twenty-seven holes 6 m were infill holes drilled to upgrade inferred and undefined material to measured and indicated classes. The main body of Patten porphyry, a few hundred metres across, occurs northwest of Patton Hill. Included in this calculation is an expanded high grade open pit mineable core of 90 million tonnes grading 0. In the deposit area, Yukon-Tanana terrane rocks are intruded by the mid-Cretaceous Dawson Range batholith, and subsequent Casino Intrusions. Primary mineralization consists of pyrite, chalcopyrite, molybdenite and minor huebnerite, and is concentrated in the phyllic zone along the inner side of a pyrite halo and is surrounded by weakly developed argillic and propylitic alteration. It is located within the Dawson Range, a west-central portion of the Yukon-Tanana terrane. The supergene sulphide copper zone occurs in an up to m-deep weathered zone below the leached cap and above the hypogene mineralization. It is copper-rich and contains trace molybdenite and likely formed due to more recent fluctuations in the water table. Preliminary metallurgical studies were also completed. As part of the per-feasibility study consultants recommended building a new airstrip to service the Casino project. The deposit has not been glaciated and the high permeability associated with the brecciated and strongly altered mineralization has resulted in very deep weathering up to m and the development of a classic stratified porphyry deposit consisting of: 1 a leached cap, followed by; 2 a narrow supergene oxide zone; and 3 a supergene sulphide zone lying above the main hypogene mineralization. See Capsule Geology for this resource estimate. It occurs mainly in the steeply plunging, in-situ contact breccia surrounding the Patton Porphyry intrusive plug and consists of recrystallization and exsolution of hydrothermal fluids from late Cretaceous magmas of the Prospector Plutonic Suite. Capsule Geology The Casino deposit is one of the largest, highest grade porphyry deposits in Canada. Although the project has lain dormant at times all exploration work since has been aimed at bringing the deposit into production. In , Western Copper completed a Quantec Titan 24 deep-penetration geophysical survey over the Casino deposit in order to identify zones of potential mineralization outside the area of currently defined mineralization. On October 5, the Supreme Court of British Columbia granted the final order approving the previously announced plan of arrangement. This alteration and the copper-molybdenum-gold mineralization are centered on the breccia. At the end of , the company began pre-feasibility studies. The mill ore reserve tonnage figure and the overall gold and copper grades are lower that the resource estimates. Hypogene mineralization or primary consists of pyrite, chalcopyrite and lesser molybdenite. The claims were staked in conjunction with work on the nearby Bomber occurrence Minfile Occurrence J Casino performed soil sampling, mag and EM surveys in and for silver-lead veins but the focus quickly shifted to the bulk tonnage, open pit potential after soil geochemical surveys returned widespread anomalous copper and molybdenum values over an intensely altered and deeply weathered intrusive complex. The Patton porphyry Ma represents two or more episodes of high-level intrusion of porphyritic hypabyssal dacite to rhyodacite. In Wildrose Resources drilled 4 diamond drill holes The company followed up with prospecting and rock sampling in An average mill throughput of 90, tonnes per day of sulphide ore was used in the calculation. The Casino deposit is centred on an Upper Cretaceous-age, east-west elongated porphyry stock Patton porphyry that intrudes the Dawson Range Batholith and Yukon Tanana terrane country rocks. Late Cretaceous igneous activity produced a northwest-trending belt of small stocks, one of which, the Patton porphyry intrudes the Casino Plutonic Suite rocks, producing the copper-gold-molybdenum mineralization present at the Casino deposit. It averages 70 m thick and is characterized by boxwork textures partly filled by jarosite, limonite, goethite and hematite. The remaining 10 holes 4 m targeted geophysical targets identified by the Quantec Titan geophysical survey. The geophysics program was followed-up with 37 diamond drill holes 10 m. Brecciation is best developed in the eastern end of the stock where breccia can be up to m wide in plan view. Wildrose also undertook responsibility to file assessment work on the remaining claims which cover the actual Casino deposit. Hypogene or primary mineralization occurs throughout the various alteration zones of the Casino deposit. In the fall of Western Copper and Gold began initial engineering studies required before initiating a feasibility study. The Dawson batholith measures an approximately km long by 60 km wide and extends northwest of Carmacks to the Alaskan border and dominates the geology of the Dawson Range. This difference attributed to the lower recoveries and higher tonnages required to mine the heap leach cap. In addition 34 geotechnical holes, totaling 2 m were completed for mine engineering design purposes. Yukon Exploration and Geology , p. To the west, and along the north and south contact, the breccia narrows gradually to less than m. The heap leach reserve tonnage figure is higher and the gold grade is lower than that reported in the resource estimate. In late , the Brynelson Group acquired control of Casino and performed grid soil sampling and mapping. The gold-rich leached cap would be mined separately using conventional heap leach technology that would begin in the first year of preproduction and continue until year 4 of commercial production. Elsewhere, Patton porphyry forms many discontinuous dikes ranging from a few cm to 20 m wide; these cut Casino quartz monzonite and less commonly rocks of the Dawson Range batholith. The estimate employed the results of 26 m of core drilled in , and and reinterpretation of the geology which included the re-logging of 90 m of core originally drilled by Pacific Sentinel Gold Corp. Its exact thickness is not yet known as mineralization was present at the bottom of the deepest drilled hole; over m from surface. The contacts between the Patton porphyry and the microbreccia are variable and range from sharply intrusive to gradational. Hansen following identifications of huebnerite in the placer concentrates by the Geological Survey of Canada in Claims partially covering the porphyry were staked on numerous occasions for either tungsten or gold, including the BRC cl in July by H. Big Creek Resources evaluated the gold potential of the deposit with 21 large diameter diamond drill holes 4 In , Pacific Sentinel completed an infill, delineation and geotechnical drilling program comprising 16 m of large diameter diamond drilling in 83 holes. Following completion of the drilling program the company embarked on extensive metallurgical testing of several possible process options for the mineral zones. In , Brameda exchanged its option for a Later that year, Casino with financing from Teck, conducted gold geochemical and EM surveys, drilled 7 holes Although recognized as a major resource, the Casino property was inactive throughout most of the 's and early 's due to low copper prices. The immediate goal of increasing the near-surface supergene sulphide zone was achieved with the size of this zone increasing from million tonnes to million tonnes at the measured and indicated level.{/INSERTKEYS}{/PARAGRAPH} Copper grades in the supergene sulphide zone are almost double the copper grades in the Hypogene 0. Where present the zone averages 10 m thick and can contain chalcanthite, malachite, brocanthite, with minor azurite, tenorite, cuprite and neotocite. Intrusion of the stock into the older rocks caused brecciation of both the intrusive and surrounding country rocks along the northern, southern and eastern contact of the stock. Based on diamond drilling completed to the end of the Casino deposit measures approximately 1. A major breakthrough in the projects history occurred in when Archer, Cathro and Associates Ltd re-assayed Casino core for its gold content. It has an average thickness of 60 m and is in part controlled by the distribution of pyrite, fracture density and by the erosion surface at the time of leaching. Abundant Patton porphyry fragments occur in the adjacent microbreccia. On June 23, Western Copper announced its intention to spin out various assets to two new subsidiaries. In Western Copper continued infill and delineation drilling. Early exploration in the area was centred on the silver-lead vein discovered at the Bomber occurrence Minfile occurrence J located approximately 2 km to the south. This difference is attributed to the actual mining plan as some ore reported in the resource calculation will not actually be mined. Chalcocite also locally coats pyrite grains and clusters, and may extend along fractures deep into the hypogene zone. During the company refurbished the camp facilities, drilled 3 diamond drill holes 1 m and continued collecting baseline environmental studies. The processing of low grade ores would extend commercial production an additional 3 years. The reserve estimate is based on pit design and the mine production schedule developed in the pre-feasibility study and is reported as a mill ore reserve and heap leach reserve. On November 1, Western Copper announced an updated resource estimate for the Casino project. The company immediately optioned the property to Big Creek Resources which carried out a large diamond drill program in In the spring of Pacific Sentinel released a historic resource estimate i. This led to an overall decrease in the tonnage reported for the measured and inferred classes when compared to values reported in the resource estimate. The pre-feasibility study also included the first NI mineral reserve estimate for the Casino project. The high pyrite content of the phyllic zone promotes leaching; thus, secondary enrichment zones are thicker near the contact of the potassic and phyllic alteration zones. In order to achieve this goal Western Copper staked Fly cl YD approximately 14 km to the southwest along the southern branch of Dip Creek. Hydrothermal alteration consists of a potassic alteration zone about m in diameter and a surrounding phyllic zone that extends m into the Dawson Range Batholith. The supergene oxide zone is poorly understood and exists as a few perched bodies within the leached cap. {PARAGRAPH}{INSERTKEYS}Work History The earliest exploration activity in the area was placer mining on Canadian Creek in The first lode claims, Tungsten and Nick cl were staked in by N. Only minor amounts of drilling have been completed at the western end of the stock and it is not known if breccia is present along this contact.