The oldest granitoids of Transangara (Enisei ridge): U-Th-Pb-data on zircon

A. E. Vernikovskaya, V. A. Vernikovskij, M. T D Wingate, N. V. Popov, A. M. Yasenev

    Research output: Contribution to journalArticle

    5 Citations (Scopus)

    Abstract

    It is established that in Transangara distinctly specified is the most early Neoproterozoic collision event in the range of 865-880 mln years ago. According to the determined geologic position, chemical composition and granitoids formation age, the integral Teiskii complex includes, apart from the considered Teiskii and Kalaminskii massifs, granites of Erudinskii massif with the age 878 mln years. Most likely, the granites of this complex were formed outside Siberian shield, being within Central-Angara terrein already before its collision with Siberia.

    Original languageEnglish
    Pages (from-to)225-230
    Number of pages6
    JournalDoklady Akademii Nauk
    Volume397
    Issue number2
    Publication statusPublished - 2004

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    zircon
    collision
    shield
    chemical composition

    Cite this

    Vernikovskaya, A. E., Vernikovskij, V. A., Wingate, M. T. D., Popov, N. V., & Yasenev, A. M. (2004). The oldest granitoids of Transangara (Enisei ridge): U-Th-Pb-data on zircon. Doklady Akademii Nauk, 397(2), 225-230.
    Vernikovskaya, A. E. ; Vernikovskij, V. A. ; Wingate, M. T D ; Popov, N. V. ; Yasenev, A. M. / The oldest granitoids of Transangara (Enisei ridge) : U-Th-Pb-data on zircon. In: Doklady Akademii Nauk. 2004 ; Vol. 397, No. 2. pp. 225-230.
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    Vernikovskaya, AE, Vernikovskij, VA, Wingate, MTD, Popov, NV & Yasenev, AM 2004, 'The oldest granitoids of Transangara (Enisei ridge): U-Th-Pb-data on zircon' Doklady Akademii Nauk, vol. 397, no. 2, pp. 225-230.

    The oldest granitoids of Transangara (Enisei ridge) : U-Th-Pb-data on zircon. / Vernikovskaya, A. E.; Vernikovskij, V. A.; Wingate, M. T D; Popov, N. V.; Yasenev, A. M.

    In: Doklady Akademii Nauk, Vol. 397, No. 2, 2004, p. 225-230.

    Research output: Contribution to journalArticle

    TY - JOUR

    T1 - The oldest granitoids of Transangara (Enisei ridge)

    T2 - U-Th-Pb-data on zircon

    AU - Vernikovskaya, A. E.

    AU - Vernikovskij, V. A.

    AU - Wingate, M. T D

    AU - Popov, N. V.

    AU - Yasenev, A. M.

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    AB - It is established that in Transangara distinctly specified is the most early Neoproterozoic collision event in the range of 865-880 mln years ago. According to the determined geologic position, chemical composition and granitoids formation age, the integral Teiskii complex includes, apart from the considered Teiskii and Kalaminskii massifs, granites of Erudinskii massif with the age 878 mln years. Most likely, the granites of this complex were formed outside Siberian shield, being within Central-Angara terrein already before its collision with Siberia.

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    Vernikovskaya AE, Vernikovskij VA, Wingate MTD, Popov NV, Yasenev AM. The oldest granitoids of Transangara (Enisei ridge): U-Th-Pb-data on zircon. Doklady Akademii Nauk. 2004;397(2):225-230.