Genesis of Sulfide and Platinum-Metal Mineralization of the Khudolaz Complex (Southern Urals)

2021 ◽  
Vol 498 (1) ◽  
pp. 398-402
Author(s):  
I. R. Rakhimov ◽  
V. N. Puchkov
Author(s):  
A. O. Khotylev ◽  
N. B. Devisheva ◽  
Al. V. Tevelev ◽  
V. M. Moseichuk

Within the Western slope of the Southern Urals, there are plenty of basite dyke complexes of Riphean to Vendian among Precambrian terrigenous-carbonate formations. In metamorphic formations of the Taratash complex (Archean to Early Proterozoic, the northern closure of the Bashkirian meganticlinorium) there was observed the andesitic dyke with isotopic age of 71±1 Ma (U-Pb SHRIMP II on zircons) and near Bakal two bodies of gabbroids with zircons of similar ages were found. These are the first evidence of possible Mezozoic magmatism in this region.


Arctoa ◽  
2015 ◽  
Vol 24 (1) ◽  
pp. 194-203 ◽  
Author(s):  
Elvira Z. Baisheva ◽  
Elena A. Ignatova ◽  
Nijole Kalinauskaite ◽  
Alexey D. Potemkin
Keyword(s):  

2019 ◽  
Vol 5 ◽  
pp. 200-208
Author(s):  
I.N. Kuznetsova ◽  
◽  
A.A. Lavrinenko ◽  
E.A. Shrader ◽  
L.M. Sarkisova ◽  
...  
Keyword(s):  

2017 ◽  
Vol 212 (12) ◽  
pp. 48-50
Author(s):  
Ju.P. Gorichev ◽  
◽  
A.N. Davydychev ◽  
A.Yu. Kulagin ◽  
◽  
...  

2012 ◽  
pp. 109-134
Author(s):  
P. S. Shirokikh ◽  
A. M. Kunafin ◽  
V. B. Martynenko

The secondary birch and aspen forests of middle stages of succession of the central elevated part of the Southern Urals are studied. 4 subassociations, 1 community, and 7 variants in the alliances of Aconito-Piceion and Piceion excelsae are allocated. It is shown that the floristic composition of aspen and birch secondary forests in the age of 60—80 years is almost identical to the natural forests. However, a slight increase the coenotical role of light-requiring species of grasslands and hemiboreal forests in the secondary communities of the class Brachypodio-Betuletea was noticed as well as some reduction of role the shade-tolerant species of nemoral complex and species of boreal forests of the class Vaccinio-Piceetea. Dominant tree layer under the canopy of secondary series is marked by an active growth of natural tree species.


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