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    Age and Sources of Late Precambrian Sedimentary Sequences of the Southern Baikal Region: Results of the U–Pb LA-ICP-MS Dating of Detrital Zircons

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    Authors
    Gladkochub, D.
    Nicoli, G.
    Stanevich, A.
    Mazukabzov, A.
    Sklyarov, E.
    Pisarevsky, Sergei
    Donskaya, T.
    Tait, J.
    Date
    2013
    Type
    Journal Article
    
    Metadata
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    Citation
    Gladkochub, D and Nicoli, G. and Stanevich, A and Mazukabzov, Anatoliy and Sklyarov, E and Pisarevsky, Sergei and Donskaya, Tatiana and Tait, J. 2013. Age and Sources of Late Precambrian Sedimentary Sequences of the Southern Baikal Region: Results of the U–Pb LA-ICP-MS Dating of Detrital Zircons. Doklady Earth Sciences. 450 (1): pp. 494-498.
    Source Title
    Doklady Earth Sciences
    DOI
    10.1134/S1028334X13050097
    ISSN
    1028-334X
    URI
    http://hdl.handle.net/20.500.11937/12520
    Collection
    • Curtin Research Publications
    Abstract

    The first data on the age of detrital zircons are given for Late Precambrian terrigenous rocks of the Baikal Group and Ushakovka Formation of the southern flank of the Siberian Craton. The ages obtained for 348 zircons cover the Paleoarchean to Late Ediacaran period, demonstrate the dynamics of change of sources of the clastic material in the sedimentation basin, and mark the changes of the Late Precambrian tectonic regimes. The age of the youngest group of detrital zircons extracted from the rocks of the Kachergat Formation allows us to restrict the upper age limit of accumulation of the rocks of the Baikal Group to the Late Ediacaran (Late Vendian).

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