Zobrazeno 1 - 10
of 33
pro vyhledávání: '"A. S. Tychkov"'
Publikováno v:
Геодинамика и тектонофизика, Vol 13, Iss 4 (2022)
We discuss herein the differences both in composition and structure of the lithospheric mantle of the Siberian Platform under kimberlite fields of different ages. Having analyzed the pyrope garnets from kimberlites of different ages this study aimed
Externí odkaz:
https://doaj.org/article/13ffcd73f3734f7583f2c1fe459cf965
Autor:
I. V. Ashchepkov, A. S. Ivanov, S. I. Kostrovitsky, M. A. Vavilov, S. A. Babushkina, N. V. Vladykin, N. S. Tychkov, N. S. Medvedev
Publikováno v:
Геодинамика и тектонофизика, Vol 10, Iss 2, Pp 197-245 (2019)
We have studied variations in the structure and composition of minerals from the pipes of the Yakutian kimberlite province (YKP) in different mantle terranes of the Siberian craton. The study was based on an extensive database, including the micropro
Externí odkaz:
https://doaj.org/article/160d7b38cd0d44b486290cd1aff04103
Publikováno v:
Doklady Earth Sciences. 499:634-638
Comprehensive studies of peridotitic xenoliths from the Udachnaya kimberlite (Yakutian diamond province, Siberian craton) confirm that garnet shows inverse correlation of its volumetric percentage with its Cr2O3 contents in refertilizated peridotites
Autor:
N. S. Tychkov, N. P. Pokhilenko, Dmitriy I. Rezvukhin, E. I. Nikolenko, Igor S. Sharygin, Vladimir Malkovets
Publikováno v:
Doklady Earth Sciences. 497:300-304
Sulfide-bearing polymineralic inclusions in mantle-derived chromium pyrope garnets of lherzolite paragenesis from lamprophyres of the Chompolo field (Aldan shield, southern Siberian craton) have been studied. The inclusions are composed of either onl
Autor:
Nikolay V. Vladykin, Igor Ashchepkov, S. I. Kostrovitsky, N.S. Medvedev, N. S. Tychkov, S.A. Babushkina, M.A. Vavilov, A. S. Ivanov
Publikováno v:
Geodinamika i Tektonofizika, Vol 10, Iss 2, Pp 197-245 (2019)
We have studied variations in the structure and composition of minerals from the pipes of the Yakutian kimberlite province (YKP) in different mantle terranes of the Siberian craton. The study was based on an extensive database, including the micropro
Publikováno v:
Russian Geology and Geophysics. 59:1254-1270
Several thousand clinopyroxene, garnet, and phlogopite inclusions of mantle rocks from Jurassic and Triassic kimberlites in the northeastern Siberian craton have been analyzed and compared with their counterparts from Paleozoic kimberlites, including
Autor:
E. N. Nigmatulina, Hilary Downes, M.A. Vavilov, Nikolay V. Vladykin, S.A. Babushkina, S.S. Kuligin, O. S. Khmelnikova, Igor Ashchepkov, N. S. Tychkov
Publikováno v:
Geoscience Frontiers, Vol 7, Iss 4, Pp 639-662 (2016)
Mantle xenocrysts from early Triassic kimberlite pipes from Kharamai, Ary-Mastakh and Kuranakh fields in the Anabar shield of Siberia revealing similar compositional trends were studied to estimate the superplume influence on the subcratonic lithosph
Autor:
N. P. Pokhilenko, Alexander V. Golovin, Andrey E. Izokh, N. S. Tychkov, O. V. Ilyina, O. A. Kozmenko, A. M. Agashev
Publikováno v:
Doklady Earth Sciences. 467:408-411
The results of the first study of the PGE distribution in deformed lherzolites of the Udachnaya kimberlite pipe (Yakutia) are presented here. The complex character of evolution of the PGE composition in the Deformed lherzolites is assumed to be the r
Publikováno v:
Doklady Earth Sciences. 467:228-231
Paragenetic analysis of pyropes from alluvial deposits of the Muna—Markha interfluve (Sakha–Yakutia Republic) made it possible to distinguish relatively uniform areas that are promising for the discovery of kimberlite bodies.
Autor:
Anna M. Nikolenko, A. M. Agashev, E. I. Nikolenko, Konstantin V. Lobov, Maria V. Chervyakovskaya, N. S. Tychkov, Igor S. Sharygin
Publikováno v:
Minerals
Volume 10
Issue 10
Minerals, Vol 10, Iss 886, p 886 (2020)
Volume 10
Issue 10
Minerals, Vol 10, Iss 886, p 886 (2020)
The alkaline igneous rocks of the Chompolo field (Aldan shield, Siberian craton), previously defined as kimberlites or lamproites, are more correctly classified as low-Ti lamprophyres. The emplacement age of the Ogonek pipe (137.8 ±
1.2 Ma
1.2 Ma