Au-Bi-Te mineralization of the Kontaktovyi stock in Northeast Russia

Сидоров, В. А.; Волков, А. В.; Wolfson, Albert; Sidorov, A. A.

doi:10.1134/s1028334x07080065

Dokl. Earth Sc.

2007

DOI: 10.1134/s1028334x07080065

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Au-Bi-Te mineralization of the Kontaktovyi stock in Northeast Russia

В. А. Сидоров

А. В. Волков

Albert Wolfson³

et al.

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Cited by 3 publications

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“…The rejuvenated epithermal deposits are widespread in this sector of the OChVB (Goncharov and Sidorov, 1979). At the Kupol deposit in the Anadyr sector of the OChVB, epithermal Au-Ag mineralization is clearly related to porphyry copper mineralization (Sidorov et al, 2007).…”

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“…This difference can be explained by widespread young posthumous tectonic movements in the OChVB and its perivolcanic zone, which result in the exposure of subvolcanic intrusions and deep erosion of them with almost complete elimination of related epithermal deposits. The Au-Te-Bi mineralization in porphyry and even hypabyssal Okhotsk granitoids may be regarded as the roots of epithermal mineralization (Volkov et al, 2007;Sidorov et al, 2007).…”

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The gold-silver Okhotsk-Chukotka volcanic belt

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The Okhotsk-Chukotka volcanic belt (OChVB) formed over 25 Ma from the middle Albian to the Cenomanian at the boundary of the continental Verkhoyansk-Chukotka and the Koryak-Kamchatka collages of terranes as a special tectonic unit of the Earth's crust composed of subaerial volcanic rocks extending for 3000 km. In regard to the oceanic margin, the inner, outer, and flank zones of the OChVB have been recognized. The complex structure of terranes in the basement and the OChVB itself resulted in the formation of diverse epithermal deposits. Porphyry copper-molybdenum deposits are concentrated in the inner zone. The outer zone is characterized by gold-silver ore mineralization and a variety of tin deposits. Silver-base-metal deposits (Dukat, Lunny, Arylakh, etc.) are confined to the rift-related volcanic trough that complicates the OChVB between the Yana-Kolyma and Omolon terranes.

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The gold-silver Okhotsk-Chukotka volcanic belt

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Zavaritskite from Sulfide–Magnetite Ore of the Aktash Skarn Deposit, Western Karamazar

et al. 2022

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Tellurium mineralization of the Priozernoe gold-quartz deposit (Northern Urals, Russia)

Kasatkin¹,

Tsyganko²,

Nestola

2023

Минералогия (Mineralogy)

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Primary and supergene Te minerals are identifed in quartz veins of the Priozernoe deposit (Sverdlovsk oblast, Northern Urals, Russia) and studied by optical methods, electron microprobe analysis, X-ray diffraction and Raman spectroscopy. Tellurides include altaite, hessite, melonite, petzite, and sylvanite. Their individual grains and intergrowths occur as small inclusions in quartz. Supergene minerals include telluroperite, northstarite, adanite, burckhardtite, kuranakhite, and schieffelinite. They replace galena, hessite and cerussite or form monomineral grains and veinlets in quartz. Northstarite, adanite, and schieffelinite are found for the frst time in Russian Federation, while the fndings of telluroperite and burckhardtite are second. Kuranakhite is found for the frst time in the Northern Urals. The fndings of supergene Te minerals in Russia are reviewed. Keywords: Priozernoe deposit, Northern Urals, tellurium mineralization, tellurides, tellurates, north-starite, adanite, schieffelinite, burckhardtite, frst fnds of minerals in Russia, supergene minerals.

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Au-Bi-Te mineralization of the Kontaktovyi stock in Northeast Russia

Cited by 3 publications

References 1 publication

The gold-silver Okhotsk-Chukotka volcanic belt

The gold-silver Okhotsk-Chukotka volcanic belt

Zavaritskite from Sulfide–Magnetite Ore of the Aktash Skarn Deposit, Western Karamazar

Tellurium mineralization of the Priozernoe gold-quartz deposit (Northern Urals, Russia)

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