Zobrazeno 1 - 10
of 27
pro vyhledávání: '"G. Yu. Shardakova"'
Publikováno v:
Геодинамика и тектонофизика, Vol 12, Iss 2, Pp 332-349 (2021)
Transformation of the oceanic crust into the continental one in orogenic belts is an important problem in petrological studies. In the paleocontinental sector of the Urals, a key object for tracing the stages of metamorphism and investigating the ori
Externí odkaz:
https://doaj.org/article/26cc2e967d164669ae4586dcb7d5e90b
Autor:
V. V. Kholodnov, G. Yu. Shardakova, V. N. Puchkov, G. A. Petrov, E. S. Shagalov, D. N. Salikhov, A. V. Korovko, S. V. Pribavkin, I. R. Rakhimov, N. S. Borodina
Publikováno v:
Геодинамика и тектонофизика, Vol 12, Iss 2, Pp 225-245 (2021)
The Ural mobile belt is an intracontinental epioceanic orogen that has already gone through all stages of the geodynamic development. Igneous rocks formed during each stage are important indicators for understanding the evolution of this belt and det
Externí odkaz:
https://doaj.org/article/211401640e0c42dca02cb6becd3fc775
Publikováno v:
Геодинамика и тектонофизика, Vol 10, Iss 4, Pp 863-878 (2019)
The Main Uralian fault (MUF) zone is a suture at the junction of the Urals and the East European platform (EEP). Its complex tectonic melange is still poorly studied. We obtained new data on compositions and ages of the Krutorechensky granites (KG) c
Externí odkaz:
https://doaj.org/article/b266d5f83ee648e5871ac10b72911534
Publikováno v:
Vestnik Permskogo Universiteta: Seriâ Geologiâ, Vol 17, Iss 4, Pp 308-325 (2018)
Rare metals bearing alkaline complexes are quite uncommon on the western slope of the Urals. The Kozlinogorskiy complex is situated in the Ufaley block related to the junction zone of the Urals and the East European Platform. Gabbro, syenites, granos
Externí odkaz:
https://doaj.org/article/871ff92ef1c7438293b516ade41c53e6
Publikováno v:
Геодинамика и тектонофизика, Vol 9, Iss 2, Pp 365-389 (2018)
The rocks from different stages of the geodynamic evolution have been preserved in the Urals. In its geologic history, the least studied is the transition period between continental rifting and the beginning of oceanic spreading. This article present
Externí odkaz:
https://doaj.org/article/fd09ebdba5cb488183b3a878534f5f8e
Publikováno v:
Литосфера, Vol 0, Iss 2, Pp 5-26 (2017)
The analysis of the evolution of composition and mineral occurences of the Low and Middle Riphean magma-tic rocks from the riftogenic structures of the Bashkirian anticlinorium involving of some neighboring structures from the western slope of the So
Externí odkaz:
https://doaj.org/article/6e268fdc32ab4bd289b475bad579111f
Autor:
G. Yu. Shardakova
Publikováno v:
Литосфера, Vol 0, Iss 4, Pp 133-137 (2016)
There are complex of data about composition, age, isotopic parameters for granites from the Ufaley block, which is situated in the accretion zone on the boundary between the Urals and the East European platform. Granitoides mark the main stage of the
Externí odkaz:
https://doaj.org/article/e2484adf377e4257987294b86c878d9a
Autor:
G. Yu. Shardakova
Publikováno v:
Литосфера, Vol 0, Iss 4, Pp 93-98 (2015)
This is represents the results of dating of the Nikolsky granite massif (by Ar-Ar and Rb-Sr methods) situated within the Ufaley block which is the complicate heterogeneous structure in the accretion zone between the Uralian orogen and the East Europe
Externí odkaz:
https://doaj.org/article/4678cf1b2ad047d993a930978f22cfe8
Autor:
G. Yu. Shardakova, E. N. Volchek, V. S. Chervyakovskiy, M. V. Chervyakovskaya, V. V. Kholodnov
Publikováno v:
Stratigraphy and Geological Correlation. 31:109-134
Publikováno v:
Petrology. 30:392-417