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The main deposit strikes north-south and has been divided into six contiguous zones. The Kupol deposit is considered to be an example of a low-sulphidation epithermal deposit.
Low-sulphidation epithermal deposits are high-level hydrothermal systems, which vary in crustal depths from depths of about 1 km to surficial hot spring settings.
Host rocks are extremely variable, ranging from volcanic rocks to sediments. Calc alkaline andesitic compositions predominate as volcanic rock hosts, but deposits can also occur in areas with bimodal volcanism and extensive subaerial ashflow deposits.
A third, less common association is with alkalic intrusive rocks and shoshonitic volcanics. Clastic and epiclastic sediments in intra-volcanic basins and structural depressions are the primary non-volcanic host rocks.
Mineralization in the near surface environment takes place in hot spring systems, or the slightly deeper underlying hydrothermal conduits. At greater crustal depth, mineralization can occur above, or peripheral to, porphyry and possibly skarn mineralization.
Normal faults, margins of grabens, coarse clastic caldera moat-fill units, radial and ring dyke fracture sets, and hydrothermal and tectonic breccias can act as mineralized-fluid channelling structures.
Throughgoing, branching, bifurcating, anastomosing and intersecting fracture systems are commonly mineralized. Mineralization forms where dilatational openings and cymoid loops develop, typically where the strike or dip of veins change.
Hanging wall fractures in mineralized structures are particularly favourable for high-grade mineralization.
The mineralization typically includes pyrite, electrum, gold, silver, and argentite. In alkalic host rocks, tellurides, roscoelite and fluorite may be abundant, with lesser molybdenite as an accessory mineral.
The OCVB has four distinct segments: two roughly northwest trending segments separated by a longer northeast trending zone and a shorter northeast zone at the far southwest end.
Host rocks at Dvoinoye are Late Cretaceous intermediate-felsic volcanics of the Tytylveyem Suite, which is divided into three units. At Zone 37, the host rock is assigned to the lower unit of the Tytylveyem Suite.
Other components of the local geology include crosscutting pyritic hydrothermal breccias that may mainly affect the tuff units. Their distribution and geometry are unclear but at least part of the Zone 37 vein is hosted by narrow siliceous pyritic milled breccias that may be related to larger volume hydrothermal breccias.
The Dvoinoye veins are close to the northern margin of the Ilirney granitic massif. As a result, there is substantial development of dykes, sills, and plugs of generally granitic composition.
Dvoinoye is a low sulphidation epithermal gold-silver vein deposit. Ore zone width ranges from a few metres to more than 30 m in the central shoot.
The vein has been drilled over a vertical extent of about m including sills. The vein system has a steep to subvertical dip to the southeast.
There are two main thick quartz veins, within a variably wide envelope of narrower veins and veinlets stockwork zone. The central shoot represents a blowout in width where the shoot may have a pipe-like form.
The bulk of the gold is in the central shoot. At depth and at the southwestern end, the mineralization forms a series of sub-parallel veins, rather than one or two wide veins.
Late to post vein block faults probably disrupt vein continuity along strike, especially to the northeast where the fault-bounded granite intrusion is developed.
Mineralization is characterized by low total sulphide content, generally less than one percent, by variable but low gold:silver ratios average , and by the presence of considerable free gold in parts of the deposit.
The main ore minerals and related sulphides in the vein are native gold, freibergite, pyrite, chalcopyrite, galena, and sphalerite, with minor acanthite.
Ore minerals are generally fine-grained. Gold occurs inter-grown with sulphides, free in quartz-illite aggregates, and in places as rare dendritic growth bands.
The main vein displays a lateral and vertical zonation in mineralization and alteration assemblages, reflecting the evolution of the system spatially and over time.
We have successfully developed more than 50 customized mobile applications for various industries, which have helped our customers significantly reduce costs, increase productivity and enter new markets.
Using the most modern technologies, we will help meet your needs in a mobile format, making your business more efficient. After analyzing your activities, we will advise exactly the mobile solution that will be most useful for your business.
The design department is always following the latest trends in the design world and is ready to use new solutions for you.
We look to the future of mobile development and are ready for the toughest challenges. Together with the product, we create specialized documentation for the customer.
It allows you to use the product without question. Our team works on a Scrum development system. In this regard, we are ready to deliver results quickly and on time.
We are promoting a mobile application on the market, helping with advertising and gaining an audience. Also, the Kupol development team is preparing a prototype product for approval by the customer, which allows the customer to familiarize themselves with the future system and give their feedback at an early stage of development.
After the development of system components in accordance with the plan, the project team integrates the completed components, conducts development testing and creates instructions for use.
Equipment, supplies, and fuel which will be needed during the winter months must be ordered two years in advance and shipped to Pevek, which is open only during the summer for three months.
In , the winter road accommodated 1, truck trips for the delivery of 3, container units, 60, tonnes of supplies, and 25, tonnes of diesel fuel.
At all other times of year, Kupol is accessible only via helicopter and fixed-wing aircraft. The mine is serviced Kupol Airport located 12 km North from it.
As of , the Kupol Gold Mine had produced 2 million ounces of gold and more than 20 million ounces of silver since In , mine owners estimated that the mine could yield up to 2.
From Wikipedia, the free encyclopedia. Kupol Northern view of the Kupol Gold Mine. Kinross Gold.Kupol Airport is an airport which services the eponymously-named gold and silver mine, which is one of the largest gold and silver mines in the Russian Far East.. It was built by the Kinross Gold memorialserviceplanning.com is used to support the needs of its enterprise's operations in the Anadyr region of the Chukotka Autonomous Okrug ( km northwest of the city of Anadyr).Location: 12 km North from, Kupol Gold Mine, Bilibinsky . 2/19/ · The Kupol deposit is located in the 3, km long Cretaceous Okhotsk-Chukotka volcanogenic belt. This belt is interpreted to be an Andean volcanic arc type tectonic setting, with the Mesozoic Anui sedimentary fold belt in a back-arc setting to the northwest of the Kupol region. The Kupol development team has more than 20 professional developers and managers with over 3 years of experience in this field. The department has experience in projects in areas such as electronic commerce, enterprise management system, LBS services, IP-telephony. We have successfully developed more than 50 customized mobile applications for.