The Ishkinino Co-Cu massive sulfide deposit hosted in ultramafic rocks of the Main Ural Fault Zone, the southern Urals

2006 ◽  
Vol 48 (3) ◽  
pp. 151-174 ◽  
Author(s):  
V. V. Zaikov ◽  
I. Yu. Melekestseva
Keyword(s):  
Fault Zone ◽  
Massive Sulfide ◽  
Southern Urals ◽  
Ultramafic Rocks ◽  
Sulfide Deposit ◽  
Massive Sulfide Deposit ◽  
The Southern Urals

scholarly journals Mineral and textural-structural features of the ore facies of Yubileynoye massive sulfide deposit (the Southern Urals)

2017 ◽  
pp. 50-56 ◽  
Author(s):  
A. S. Tseluyko ◽  
V. V. Maslennikov ◽  
N. R. Aupova ◽  
S. P. Maslennikova
Keyword(s):  
Massive Sulfide ◽  
Southern Urals ◽  
Structural Features ◽  
Sulfide Deposit ◽  
Massive Sulfide Deposit ◽  
The Urals ◽  
The Southern Urals ◽  
Sulfide Deposits ◽  
Ore Body ◽  
Formation Conditions

A study of the ore facies of the massive sulfide ores from the Yubileynoe deposit (ore body № 2) has been shown. The sub-seafloor and seafloor hydrothermal, biogenic, clastic and seafloor hypergenic facies have been diagnosed in the studied ores, reflecting different formation conditions within the ore body № 2. The seafloor and sub-seafloor hydrothermal facies occur in the central part of the ore body, while clastic with seafloor hypergenic facies dominate at the flanks of the ore body. Rare minerals are native gold, minerals of Ag, Te, Bi and Pb widespread in seafloor hydrothermal and clastic ore facies. The ratio of the ore facies in the ore body № 2 shows the simiiar ore-forming processes within the Yubileynoe deposit and other massive sulfide deposits of the Urals.

Physicochemical parameters of magmatic and hydrothermal processes at the Yaman-Kasy massive sulfide deposit, the southern Urals

2006 ◽  
Vol 48 (5) ◽  
pp. 369-383 ◽  
Author(s):  
V. A. Simonov ◽  
S. V. Kovyazin ◽  
E. O. Terenya ◽  
V. V. Maslennikov ◽  
V. V. Zaykov ◽  
...  
Keyword(s):  
Physicochemical Parameters ◽  
Massive Sulfide ◽  
Southern Urals ◽  
Sulfide Deposit ◽  
Massive Sulfide Deposit ◽  
The Southern Urals ◽  
Hydrothermal Processes

H and O isotopic compositions of layered silicates in metasomatites from the Gai Zn-Cu massive sulfide deposit, southern urals

2000 ◽  
Vol 35 (1) ◽  
pp. 70-75
Author(s):  
A. I. Grabezhev ◽  
B. G. Pokrovskii ◽  
F. P. Buslaev ◽  
V. V. Zaikov ◽  
G. N. Pshenichnyi
Keyword(s):  
Massive Sulfide ◽  
Southern Urals ◽  
Layered Silicates ◽  
Sulfide Deposit ◽  
Massive Sulfide Deposit ◽  
Isotopic Compositions

scholarly journals Trace-elements in sulfides of the Dergamysh cobalt-bearing massive sulfide deposit, the Southern Urals: Mode of occurrence and matter sources

LITOSFERA ◽  
2020 ◽  
Vol 20 (4) ◽  
pp. 499-516
Author(s):  
I. Yu. Melekestseva ◽  
V. V. Maslennikov ◽  
S. P. Maslennikova
Keyword(s):  
Trace Elements ◽  
Inductively Coupled Plasma ◽  
Massive Sulfide ◽  
Sulfide Deposit ◽  
South Urals ◽  
Massive Sulfide Deposit ◽  
The Southern Urals ◽  
Diagenetic Alteration ◽  
Ore Body ◽  
Mode Of Occurrence

Subject of study. The article presents the results of study of trace elements (TEs) in sulfides of the main ore body (borehole 1T) and the northwestern ore body (borehole 200) of the Dergamysh cobalt-bearing massive sulfide deposit hosted in serpentinites (South Urals). Materials and methods. The chalcopyrite-pyrite-marcasite sandstones of the main ore body and pyrite-chalcopyrite-pyrrhotite “gravelites” of its northwestern satellite were studied with laser ablation with inductively coupled plasma. Results. The TE contents, distribution and mode of occurrence differ in sulfides of the main ore body and its northwestern satellite. In ores of the main ore body, most TEs (Ag, Sn, Mn, As, Co, Ni, Te, Pb, Au) accumulate in pyrite-1, pyrite-marcasite aggregates concentrate Tl and Bi, marcasite is a host to Mo and Sb, and chalcopyrite contains Zn, Se and Cd. Pyrite-2 is depleted in TEs relative to other sulfides. In sulfides of the northwestern satellite, most TEs are related to chalcopyrite (Bi, Te, Zn, Cd, Se, Pb, Au, Tl, Ni, Co). Tin accumulates in cubanite, As and Ni are hosted in pyrite-4, Ag, Mn and Mo are concentrated in pyrrhotite, Sb is typical of pyrite-3, and Co accumulates in pyrite-2. Conclusions. Based on the correlation analysis, it is shown that sulfides of the main ore body and its northwestern satellite are characterized by different mode of TE occurrences. The differences are explained by two main reasons: 1) “mafic” and “ultramafic” metal sources for sulfides of the main ore body and its northwestern satellite, respectively, and 2) different degree of diagenetic alteration of sulfides.

Tellurium-Bearing Mineralization in Clastic Ores at the Yubileynoe Copper Massive Sulfide Deposit (Southern Urals)

2019 ◽  
Vol 61 (2) ◽  
pp. 133-161 ◽  
Author(s):  
A. S. Tseluyko ◽  
V. V. Maslennikov ◽  
N. R. Ayupova ◽  
S. P. Maslennikova ◽  
L. V. Danyushevsky
Keyword(s):  
Massive Sulfide ◽  
Southern Urals ◽  
Sulfide Deposit ◽  
Massive Sulfide Deposit

Mineralogical and Geochemical Features of Pyrite Nodules from Sulfide Turbidites in the Talgan Cu-Zn Massive Sulfide Deposit (Southern Urals)

2019 ◽  
Vol 54 (6) ◽  
pp. 447-464 ◽  
Author(s):  
N. R. Ayupova ◽  
V. V. Maslennikov ◽  
D. A. Artem’ev ◽  
I. A. Blinov
Keyword(s):  
Massive Sulfide ◽  
Southern Urals ◽  
Sulfide Deposit ◽  
Massive Sulfide Deposit

scholarly journals Phyllosilicate minerals in the hydrothermal mafic?ultramafic-hosted massive-sulfide deposit of Ivanovka (southern Urals): comparison with modern ocean seafloor analogues

2004 ◽  
Vol 147 (3) ◽  
pp. 363-383 ◽  
Author(s):  
Paolo Nimis ◽  
Svetlana G. Tesalina ◽  
Paolo Omenetto ◽  
Paola Tartarotti ◽  
Catherine Lerouge
Keyword(s):  
Massive Sulfide ◽  
Southern Urals ◽  
Sulfide Deposit ◽  
Massive Sulfide Deposit
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