Zobrazeno 1 - 8
of 8
pro vyhledávání: '"T. A. Oitseva"'
Autor:
I. Yu. Annikova, A. G. Vladimirov, S. Z. Smirnov, T. A. Oitseva, E. I. Mikheev, E. N. Jes, A. V. Travin, B. A. D’yachkov, V. I. Maslov, I. F. Gertner
Publikováno v:
Литосфера, Vol 0, Iss 2, Pp 304-326 (2019)
Research subject. The Novo-Akhmirovskoe lithium-bearing deposit in the East Kazakhstan region, which is represented by an intrusive layer of topaz-zinnwaldite granites, is located within of the Kalba-Narym-Koktogai lithium-tantalum raremetal-granite
Externí odkaz:
https://doaj.org/article/d0aa0a4663d84d2d8b2e6f0a6c74594c
Autor:
N. G. Murzintsev, I. Yu. Annikova, A. V. Travin, A. G. Vladimirov, B. A. Dyachkov, V. I. Maslov, T. A. Oitseva, O. A. Gavryushkina
Publikováno v:
Геодинамика и тектонофизика, Vol 10, Iss 2, Pp 375-404 (2019)
The article presents an event correlation of the Permian‐Triassic granites of the Altai collision system, which are associated with industrial ore deposits and occurrences (Mo‐W, Sn‐W, Li‐Ta‐Be). The multi‐system and multi‐mineral isoto
Externí odkaz:
https://doaj.org/article/d0241af8de4c490a980684b02c05aa8b
Autor:
E. V. Levashova, S. G. Skublov, T. A. Oitseva, B. A. Dyachkov, X.-H. Li, Q.-L. Li, N. V. Shatova, V. V. Shatov
Publikováno v:
Geochemistry International. 60:1-15
This paper is dedicated to the isotope-geochemical study of zircon from riebeckite granites of the Verkhnee Espe rare earth-rare metal deposit and the specification of its U–Pb age. Zircon from the Verkhnee Espe massif is peculiar in the high conte
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::a7d8348cb2d0592eb9e0cfd4cfa58308
https://doi.org/10.1134/s0016702922010086
https://doi.org/10.1134/s0016702922010086
Publikováno v:
Gornyi Zhurnal. :90-95
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::3becbb8551c1d7ecad0fdf194b7443a4
https://doi.org/10.17580/gzh.2021.08.17
https://doi.org/10.17580/gzh.2021.08.17
Autor:
S.Z. Smirnov, T. A. Oitseva, O. A. Gavryushkina, A. V. Travin, Alexander Vladimirov, I. Yu. Annikova, N. G. Murzintsev, E. N. Sokolova
Publikováno v:
Russian Geology and Geophysics. 60:890-910
—The Kalguty Mo–W ore-magmatic system (OMS) is a granite batholith (S = 70 km2, V = 12,800 km3 at the recent denudation level, according to geological and geophysical data). This batholith is cut by the East Kalguty belt of rare-metal ongonite–
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::6f1de3beb4ad0487855477158e0de647
https://doi.org/10.15372/rgg2019057
https://doi.org/10.15372/rgg2019057
Publikováno v:
Proceedings of the International Multidisciplinary Scientific GeoConference SGEM; 2022, Vol. 22, p499-506, 8p
Publikováno v:
IOP Conference Series: Earth and Environmental Science. 110:012018
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::cd002fd774a9e5162e07b5c62395cf03
https://doi.org/10.1088/1755-1315/110/1/012018
https://doi.org/10.1088/1755-1315/110/1/012018
Publikováno v:
IOP Conference Series: Earth & Environmental Science; Jan2018, Vol. 110 Issue 1, p1-1, 1p