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    Proterozoic Basic Magmatism of the Siberian Craton: Main Stages and Their Geodynamic Interpretation

    Access Status
    Fulltext not available
    Authors
    Gladkochub, D.
    Donskaya, T.
    Ernst, R.
    Mazukabzov, A.
    Sklyarov, E.
    Pisarevskiy, Sergei
    Wingate, M.
    Söderlund, U.
    Date
    2012
    Type
    Journal Article
    
    Metadata
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    Citation
    Gladkochub, D. and Donskaya, T. and Ernst, R. and Mazukabzov, A. and Sklyarov, E. and Pisarevskiy, S. and Wingate, M. et al. 2012. Proterozoic Basic Magmatism of the Siberian Craton: Main Stages and Their Geodynamic Interpretation. Geotectonics. 46 (4): pp. 273-284.
    Source Title
    Geotectonics
    DOI
    10.1134/S0016852112040024
    ISSN
    00168521
    School
    University of Western Australia
    URI
    http://hdl.handle.net/20.500.11937/49303
    Collection
    • Curtin Research Publications
    Abstract

    Geological data on the Precambrian basic complexes of the Siberian Craton and their isotopic ageare considered. The three main episodes of Precambrian basic magmatism of Siberia correspond to certain stages of the geodynamic evolution of the craton and the Earth as a whole. In the Late Paleoproterozoic, largely in the south and the north of the craton, the basic rocks were emplaced against the background of post collision extension, which followed the preceding collision–accretion stage responsible for the formation of the craton. In the Mesoproterozoic, primarily in the north of the craton, basic magmatism was controlled by dispersed withinplate extension apparently caused by the impact of a mantle plume. Neoproterozoic basic magmatism widespread in the southern and southeastern parts of the craton was caused by rifting, which accompanied breakdown of the Rodinia supercontinent and opening of the Paleoasian ocean along the southern margin of the Siberian Craton.

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