KUPOL – вул. Чайковського, 37, Lviv, Ukraine, – Mit bewertet, basierend auf 30 Bewertungen „Most genuine restaurant in Lviv, with many tasty... Kupol ist eine der bekanntesten Attraktionen von Ischewsk. Nur bei timothywilsonphotographs.com finden Besucher die preisgünstigsten Hotels nahe vieler Sportstätten. Kupol bzw. IEMZ „Kupol“, mit vollem Namen Ischewski Elektromechanitscheski Sawod „Kupol“ ist einer der größten russischen Rüstungshersteller mit Sitz in Ischewsk.
Kupol, TerskolKupol, Lviv: 53 Bewertungen - bei Tripadvisor auf Platz von von Lviv Restaurants; mit 4/5 von Reisenden bewertet. Übersetzung Schwedisch-Deutsch für kupol im PONS Online-Wörterbuch nachschlagen! Gratis Vokabeltrainer, Verbtabellen, Aussprachefunktion. The increase was mainly on account of a rising production at the Canadian miner Kinross's Kupol mine property in the Far Eastern corner of Russia.
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From Wikipedia, the free encyclopedia. Kupol Northern view of the Kupol Gold Mine. Kinross Gold.
Retrieved 27 August Retrieved 2 September Canadian Mining Journal. Retrieved 9 December Retrieved 28 August Chirano Tasiast.
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.
Four styles of gold mineralization have been identified: pink quartz gold; carbonate-base metal gold; chalcedony-ginguro gold silver; and green quartz breccia.
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