Zobrazeno 1 - 6
of 6
pro vyhledávání: '"V. A. Trunilina"'
Publikováno v:
Литосфера, Vol 0, Iss 2, Pp 81-102 (2015)
This article presents the results of detailed study of geologic structure and composition of Munilkan massif of the Main batholith belt of Verkhoyansk-Kolyma mesozoides (Tas-Khayakhtakh Ridge). Granites include numerous xenoblocks of gabbro, dolerite
Externí odkaz:
https://doaj.org/article/04403ab901a74f12bba16f78af26f5ef
Publikováno v:
Russian Journal of Pacific Geology. 13:82-98
The paper considers the petrographic composition and petro- and geochemical features of high-phosphorous lithium–fluorine granites from the Arga–Ynnakh–Khaya and Burgali ore–magmatic clusters in eastern Yakutia. Granitoids of three successive
Publikováno v:
Russian Journal of Pacific Geology. 9:359-372
For the first time for the region, the composition of the composite dikes is studied on the example of the Takalkan ore–magmatic cluster in the Polousny Range. Mineralogical, petrochemical, and geochemical study shows that the dikes were formed by
Autor:
V. A. Trunilina, S. P. Roev
Publikováno v:
IOP Conference Series: Earth and Environmental Science. 362:012145
The authors identified several varieties of different ore content of the late-orogenic and anorogenic granites of the North-east of the Verkhoyansk-Kolyma orogenic region. The purpose of the research was a detailed study of petrography, chemistry, cr
Publikováno v:
Stephan Mueller Special Publication Series. 4:97-109
The Tommot pluton is located within the continental Omulevka terrane of the inner zone of the Verkhoyansk-Kolyma Mesozoic orogen. It is a small complex (~12 km2) composed of alkaline-ultramafic rocks, alkaline and subalkaline gabbroids, and alkaline
Autor:
Jaime Toro, Elizabeth L. Miller, N. A. Goryachev, Joseph L. Wooden, V. V. Akinin, A. G. Bakharev, V. A. Trunilina, A. V. Alshevsky, Andrei V. Prokopiev
Publikováno v:
Doklady Earth Sciences. 426:605-610
U-Pb SHRIMP-dating of zircons from twenty five intrusions representative of the Main granitoid batholith belt and associated dike swarms (Yano-Kolyma gold bearing province, North East of Asia) are mostly ∼150 ± 3 Ma (Kimmeridgian-Tithonian). Two l