Zobrazeno 1 - 6
of 6
pro vyhledávání: '"Boris V. Belyatsky"'
Publikováno v:
Записки Горного института, Vol 252, Pp 801-813 (2021)
The paper presents the results of the comprehensive isotope geochemical (Re-Os, Pb and δ34S) study of sulfide mineralization of the Morozkinskoye deposit. The ore zones of the deposit are localized in the syenite massif of Mount Rudnaya, which is lo
Externí odkaz:
https://doaj.org/article/c701dac32f4c4663acff5802a30b710c
Autor:
Irina L. Nedosekova, Viktor A. Koroteev, Boris V. Belyatsky, Viktor V. Sharygin, Еlena N. Lepechinа, Sergei V. Pribavkin
Publikováno v:
Литосфера, Vol 0, Iss 5, Pp 758-773 (2018)
U-Pb dating of the pyrochlore-group minerals from the Nb-rare metal ore deposits of ilmeny-vishnevogorsky carbonatite-miaskite complex of the Ural fold region was carried out. To date the individual pyrochlore crystals were used a new technique of lo
Externí odkaz:
https://doaj.org/article/b971d56f3c054efdbb06bd27de3d51be
Publikováno v:
Записки Горного института, Vol 243, Pp 266-266 (2020)
The article presents the results of the sulfide mineralization dating of the Mayskoe gold ore deposit using the Re-Os isotope system and isochron age estimation method of the main sulfide minerals: arsenopyrite, pyrite, and antimonite. The complex mu
Externí odkaz:
https://doaj.org/article/9858997e14314f9d84e6357edcd08698
Autor:
Andrei A. Arzamastsev, Boris V. Belyatsky, Nickolay V. Rodionov, Anton V. Antonov, Elena N. Lepekhina, Sergei A. Sergeev
Publikováno v:
Geological Society, London, Special Publications. 537
An U–Pb isotopic investigation combined with rare earth element data for titanites, zircons and coexisting accessories has been undertaken to gain insight into the formation of the Archean peralkaline granites of the northeastern Fennoscandian Shie
Publikováno v:
Zapiski Gornogo Instituta, Vol 243, Pp 266-266 (2020)
В работе приводятся результаты датирования сульфидной минерализации Майского золоторудного месторождения с использованием Re-Os изотоп
Publikováno v:
Journal of Geochemical Exploration. 82:17-33
The Llandoverian black shales of the Prades Mountains, SW Catalonian Coastal Ranges, contain several metamorphosed stratiform sulfide deposits. The mineralized interval, up to 30 m in thickness, consists of interbedded sulfide-rich (mostly pyrrhotite