Zobrazeno 1 - 10
of 190
pro vyhledávání: '"Fershtater, A. A."'
Autor:
G. B. Fershtater, N. S. Borodina
Publikováno v:
Литосфера, Vol 18, Iss 5A, Pp 20-36 (2020)
Murzinka massif constitutes an interformational sheet-like body reaching up 6 km in length steeply dipping to the east. Proterozoic metamorphic rocks of predominantly granulite facies (p = 5–6 kbar, T = 750–800℃) occur at the base of the massif
Externí odkaz:
https://doaj.org/article/2a95ad663816455b823c258121abdbb9
Publikováno v:
Литосфера, Vol 0, Iss 5, Pp 672-691 (2018)
Murzinka massif is a sheet-like interformational body steeply deeping to the East with length about 6 km. Proterozoic metamorphic rocks of the predominantly granulite facies ( P = 5-6 kbar, T = 750-800°C) occur at the base of massif, and volcanic-se
Externí odkaz:
https://doaj.org/article/810aa5db3ac54f47967f7ee130a06670
Publikováno v:
Vestnik Permskogo Universiteta: Seriâ Geologiâ, Vol 17, Iss 3, Pp 208-227 (2018)
The mechanisms and sources of magma generation for the large Permian Aduyskiy granite massif, well known for rare metal, semi-precious stone and molybdenum deposits, are considered. Valuable information was obtained from study of the Kamenskiy and Kr
Externí odkaz:
https://doaj.org/article/c35c1dd7285e42cc8c3413d0d63877ca
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 18, Iss 2, Pp 177-207 (2018)
A model of magma formation in the crust of the Urals mobile belt, which is the best example of epioceanic suprasubduction orogen, has been developed. Magma formation occurs both in the relic oceanic and in the newly formed orogen crust. In the first
Externí odkaz:
https://doaj.org/article/c3cc1aad0c70485c9930d2f0db590297
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
Publikováno v:
In LITHOS 1 September 2015 232:286-305
Publikováno v:
Литосфера, Vol 0, Iss 3, Pp 82-111 (2016)
Xenoliths in the Early Cretaceous alkali basalts of Makhtesh Ramon basin (southern Israel) are represented by essentially olivine rocks: dunite (usually including clinopyroxen) - 5% of the total amount, lherzolite - 21%, wehrlite - 28%, clinopyroxeni
Externí odkaz:
https://doaj.org/article/9de326a70b2d4a3784db10760228a41c
Autor:
Yu. P. Maidanik, Vladimir G. Pastukhov, Yu. G. Fershtater, K. G. Smirnov-Vasiliev, V. P. Chernishev, V. V. Dvirniy
Publikováno v:
Proceeding of Heat Pipe Technology: Volume 2. Materials and Applications.
Autor:
G. B. Fershtater
Publikováno v:
Литосфера, Vol 0, Iss 5, Pp 5-29 (2015)
It is established that during all-Uralian stage of mantle-type magmatism of Early Devonian age (410-393 Ma) the mantle Ordovician-Silurian magmatism was changed by mantle-crustal and crustal types. At that time Tagil island arc system completed its e
Externí odkaz:
https://doaj.org/article/bcd6b02740f9412fa045b222288e1590