Deep structure of the Kayemraveem ore district (Chukotka) and features of epithermal gold-silver mineralization

2008 ◽  
Vol 421 (1) ◽  
pp. 755-759 ◽  
Author(s):  
A. A. Sidorov ◽  
Yu. Ya. Vashchilov ◽  
A. V. Volkov ◽  
V. F. Belyi
1993 ◽  
Vol 88 (2) ◽  
pp. 317-327 ◽  
Author(s):  
James E. Conrad ◽  
Edwin H. McKee ◽  
James J. Rytuba ◽  
J. Thomas Nash ◽  
William C. Utterback

2007 ◽  
Vol 1 (6) ◽  
pp. 405-409 ◽  
Author(s):  
A. S. Lapukhov ◽  
B. V. Guzman ◽  
V. A. Gorev ◽  
E. P. Solotchina ◽  
A. V. Travin

2005 ◽  
Vol 26 (1-2) ◽  
pp. 115-135 ◽  
Author(s):  
Seon-Gyu Choi ◽  
In-Chang Ryu ◽  
Sang Joon Pak ◽  
Soo-Meen Wee ◽  
Chang Seong Kim ◽  
...  

2007 ◽  
Vol 416 (1) ◽  
pp. 1032-1036 ◽  
Author(s):  
A. A. Sidorov ◽  
A. V. Volkov ◽  
V. N. Egorov

2007 ◽  
Vol 57 (4) ◽  
pp. 354-373 ◽  
Author(s):  
Ryohei Takahashi ◽  
Hiroharu Matsueda ◽  
Victor M. Okrugin ◽  
Shuji Ono

2021 ◽  
pp. 90-97
Author(s):  
A.A. Sidorov ◽  
◽  
N.E. Savva ◽  
B.I. Ishkov ◽  
A.V. Volkov ◽  
...  

Geological, structural and mineralogical facts describing the intersection of Paleozoic ore veins with carbon and Mezozoic veins in the Kubaka gold-silver deposit in the Omolon craton terrane are presented. The totality of the above observations does not allow limitation of the age mineralization by Upper Carboniferous based on isotope-geological studies, as V.V.Akinin et al. (2020) did on ore and rock samples selected in one geological exposure of ore body in opencast mine of the Tsokolny zone.


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