Zobrazeno 1 - 7
of 7
pro vyhledávání: '"Anton V. Antonov"'
Publikováno v:
Minerals, Vol 12, Iss 3, p 327 (2022)
Revealing the internal structure of diamonds is key to understanding the general regularities of crystal growth and dissolution. This paper presents and summarizes data on the internal structure of diamonds of different morphological types, colors an
Externí odkaz:
https://doaj.org/article/119be391fd39487bad40fc3bfe090ad6
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
Autor:
Andrei A. Zolotarev, Sergey V. Petrov, A. V. Kuptsova, Sergey N. Britvin, Anatoly N. Zaitsev, Alexander G. Shtukenberg, Anton V. Antonov, John Spratt
Publikováno v:
Mineralogical Magazine. 85:532-553
The Quaternary carbonatite–nephelinite Kerimasi volcano is located within the Gregory rift in northern Tanzania. It is composed of nephelinitic and carbonatitic pyroclastic rocks, tuffs, tuff breccias and pyroclastic breccias, which contain blocks
Publikováno v:
Zapiski Gornogo Instituta, Vol 239, Iss 5, Pp 492-496 (2019)
The article presents the results of a study of the internal structure of highly elongated diamond crystals from placers in the Krasnovishersky district of the Urals. Very elongated crystals are found within diamond-bearing placer with unrevealed prim
Autor:
Alexander V. Kozlov, Vitaly A. Petrovsky, Ksenia Orekhova, E. A. Vasilev, Anton V. Antonov, Andrey A. Kudryavtsev
Publikováno v:
Mineralogical Magazine. 83:515-522
We have investigated a diamond crystal that consists of several misorientated subgrains. The main feature of the crystal is the dark areas in the cathodoluminescent core that has ‘estuary-like’ boundaries extending along the subgrain interfaces.
Publikováno v:
Zapiski RMO (Proceedings of the Russian Mineralogical Society). 148:59-73
The internal structure of cuboid diamonds from contemporary alluvial placers of the Krasnovishersky district at the Urals was investigated with analyzing their spectroscopic characteristics. Crystals were divided into four groups by their anatomy and
Publikováno v:
PRIKASPIYSKIY ZHURNAL: Upravlenie i Vysokie Tekhnologii. 34:058-069