Browsing Статьи, тезисы докладов by Author "Puchkov V.N."

Browsing Статьи, тезисы докладов by Author "Puchkov V.N."

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  • Baltica in the Cryogenian, 850–630 Ma 
    Pease V.; Daly J.S.; Elming S.A.; Kumpulainen R.; Moczydlowska M.; Puchkov V.N.; Roberts D.; Saintot A.; Stephenson R. (2008)
    This new tectonic synthesis provides a framework for understanding the dynamic evolution of Baltica and for constraining tectonic correlations within the context of the Neoproterozoic break-up of Rodinia–Pannotia. Cryogenian ...
  • Structural stages and evolution of the Urals 
    Puchkov V.N. (2013)
    Five main structural and historical stages are established in the territory of the Urals: 1) Archean-Paleoproterozoic, a time of formation of the Volgo-Uralia subcontinent and its amalgamation with the other blocks of the ...
  • Structure and geodynamics of the Uralian orogen 
    Puchkov V.N. (1997)
    The Urals are a Late Palaeozoic orogenic belt. The relicts of earlier orogens are traced in its basement. In particular, the Late Vendian pre-Uralian orogen is reconstructed and identified as a part of the Late Precambrian ...
  • Tectonics of the Urals and adjacent part of the West-Siberian platform basement: Main features of geology and development 
    Ivanov K.S.; Puchkov V.N.; Fyodorov Yu.N.; Erokhin Yu.V.; Pogromskaya O.E. (2013)
    The Urals had undergone two main complete cycles of geodynamic development in the Riphean–Mesozoic time. The first one took place in the Riphean and Vendian and was completed by formation of the Timanides; the second is ...
  • The East European Craton (Baltica) before and during the assembly of Rodinia 
    Bogdanova S.V.; Bingen B.; Gorbatschev R.; Kheraskova T.N.; Kozlov V.I.; Puchkov V.N.; Volozh Yu.A. (2008)
    Prior to participating in Rodinia, the East European Craton (Baltica) had undergone a complex process of development. Many of the structures, which were important during the amalgamation of Rodinia, were formed between ca. ...
  • The evolution of the Uralian orogen 
    Puchkov V.N. (2009)
    The Uralian orogen is located along the western flank of a huge (>4000 km long) intracontinental Uralo-Mongolian mobile belt. The orogen developed mainly between the Late Devonian and the Late Permian, with a brief resumption ...