The evolution of the Uralian orogen

@inproceedings{Puchkov2009TheEO,
  title={The evolution of the Uralian orogen},
  author={V. Puchkov},
  year={2009}
}
  • V. Puchkov
  • Published 2009
  • Geology
  • Abstract 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 of orogenic activity in the Lower Jurassic and Pliocene–Quaternary time. Although its evolution is commonly related to the Variscides of Western Europe, its very distinctive features argue against a simple geodynamic connection. To a first order, the evolution of… CONTINUE READING
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    References

    SHOWING 1-10 OF 254 REFERENCES
    Structure and geodynamics of the Uralian orogen
    • V. Puchkov
    • Geology
    • Geological Society, London, Special Publications
    • 1997
    • 205
    Tectonic processes in the Southern and Middle Urals: an overview
    • 35
    Arc–continent collision in the Southern Urals
    • 95
    The Southern Urals: deep subduction, soft collision and weak erosion
    • P. Matte
    • Geology
    • Geological Society, London, Memoirs
    • 2006
    • 5
    The Neoproterozoic Timanide Orogen Of Eastern Baltica
    • 185
    • Highly Influential
    A synthesis of the stratigraphic and tectonic setting of the Uralian ophiolites
    • 61
    The mid-European segment of the Variscides: tectonostratigraphic units, terrane boundaries and plate tectonic evolution
    • W. Franke
    • Geology
    • Geological Society, London, Special Publications
    • 2000
    • 539
    • Highly Influential