A
A. Yu. Kazansky
Researcher at Moscow State University
Publications - 44
Citations - 678
A. Yu. Kazansky is an academic researcher from Moscow State University. The author has contributed to research in topics: Geology & Paleomagnetism. The author has an hindex of 10, co-authored 34 publications receiving 550 citations. Previous affiliations of A. Yu. Kazansky include Russian Academy of Sciences & Novosibirsk State University.
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Journal ArticleDOI
Evolution of the Paleo-Asian Ocean (Altai-Sayan Region, Central Asia) and collision of possible Gondwana-derived terranes with the southern marginal part of the Siberian continent
M M Buslov,I. Yu. Saphonova,Tsuyoshi Watanabe,O T Obut,Y. Fujiwara,K. Iwata,N. N. Semakov,Y. Sugai,L V Smirnova,A. Yu. Kazansky +9 more
TL;DR: In this article, a revised terrane classification based on Vendian-Cambrian geodynamic units and evolution of terranes is described. And reactivated suture zones along the terrane boundaries are proposed, which suggest the important role of strike-slip deformations in the formation of mosaic block structure of Central Asia.
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Tectonic evolution of the Siberian paleocontinent from the Neoproterozoic to the Late Mesozoic: paleomagnetic record and reconstructions
Dmitry V. Metelkin,Dmitry V. Metelkin,Valery A. Vernikovsky,Valery A. Vernikovsky,A. Yu. Kazansky,A. Yu. Kazansky +5 more
TL;DR: In this article, a new version of the apparent polar wander path for the Siberian continental plate, including the interval from the Mesoproterozoic-NeoproTERozoic boundary up to the end of the Mesozoic, was proposed.
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Neoproterozoic evolution of Rodinia: constraints from new paleomagnetic data on the western margin of the Siberian craton
TL;DR: In this article, a new version of the Neoproterozoic segment of the apparent polar wandering path (APWP) is proposed for the craton and is compared with the Laurentian APWP.
Journal ArticleDOI
New data on the magnetostratigraphy of the Jurassic–Cretaceous boundary interval, Nordvik Peninsula (northern East Siberia)
TL;DR: In this article, a reversed polarity magnetozone (M17r) was identified in Berriasian sections of the Nordvik Peninsula (northern East Siberia) from previous studies.
Journal ArticleDOI
Neoproterozoic tectonic structure of the Yenisei Ridge and formation of the western margin of the Siberian craton based on new geological, paleomagnetic, and geochronological data
Valery A. Vernikovsky,Valery A. Vernikovsky,Dmitry V. Metelkin,Dmitry V. Metelkin,A. E. Vernikovskaya,A. E. Vernikovskaya,N. Yu. Matushkin,N. Yu. Matushkin,A. Yu. Kazansky,P. I. Kadilnikov,P. I. Kadilnikov,I. V. Romanova,I. V. Romanova,Michael T.D. Wingate,A. N. Larionov,N. V. Rodionov +15 more
TL;DR: In this article, the authors focus on the inner structure, composition, and boundaries of the Central Angara terrane, which is the largest in the Transangarian segment of the Yenisei Ridge.