V
V. G. Kazmin
Researcher at Shirshov Institute of Oceanology
Publications - 7
Citations - 2295
V. G. Kazmin is an academic researcher from Shirshov Institute of Oceanology. The author has contributed to research in topics: Plate tectonics & Nappe. The author has an hindex of 7, co-authored 7 publications receiving 2194 citations.
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Journal ArticleDOI
Geological evolution of the tethys belt from the atlantic to the pamirs since the LIAS
J. Dercourt,L.P. Zonenshain,L. E. Ricou,V. G. Kazmin,X. Le Pichon,A. L. Knipper,C. Grandjacquet,I.M. Sbortshikov,J. Geyssant,Claude Lepvrier,D.H. Pechersky,J. Boulin,Jean-Claude Sibuet,L. A. Savostin,O. Sorokhtin,M. Westphal,Mikhail L. Bazhenov,J. P. Lauer,B. Biju-Duval +18 more
TL;DR: In this article, the evolution of the Tethys belt from the Pliensbachian (190 Ma) to the Tortonian (10 Ma) is depicted at 1 20,000,000 scale.
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Presentation de 9 cartes paleogeographiques au 1/20000000000eme s'etendant de l'Atlantique au Pamir pour la periode du Lias a l'Actuel
J. Dercourt,L.P. Zonenshain,L. E. Ricou,V. G. Kazmin,X. Le Pichon,A. L. Knipper,C. Grandjacquet,I. M. Sborshchikov,J. Boulin,O. Sorokhtin,J. Geyssant,Claude Lepvrier,B. Biju-Duval,Jean-Claude Sibuet,L. A. Savostin,M. Westphal,J. P. Lauer +16 more
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Plate tectonic model of the South Urals development
TL;DR: In this article, a fossil spreading pattern similar to present one can be reconstructed for the Mugodjarian back-arc basin with the spreading rate of 5 cm/yr and depth of basaltic eruption of 3000 m.
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Volcanic belts as markers of the Mesozoic-Cenozoic active margin of Eurasia
TL;DR: From the Triassic to the Present linear belts of calc-alkaline volcanism developed along the southern margin of Eurasia as mentioned in this paper, and their development is related to the closure of the Paleo-Tethys, when fragments of Gondwana (Iran, Afghanistan etc.) were approaching Eurasia.
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Structure and evolution of the passive margin of the eastern tethys
TL;DR: An extensive passive margin was formed in the Triassic along the periphery of Arabia, including the Tauric carbonate platform as discussed by the authors, which is related to the opening of the Mesozoic Tethys when a number of microcontinents split off from Gondwana.