The late Ordovician age of camptonites from the Agardag Complex of southeastern Tuva as an indicator of the plume-related magmatism during collision processes

A. E. Izokh, G. V. Polyakov, V. G. Mal'kovets, R. A. Shelepaev, A. V. Travin, Yu D. Litasov, A. A. Gibsher

    Research output: Contribution to journalArticle

    14 Citations (Scopus)
    Original languageEnglish
    Pages (from-to)511-514
    Number of pages4
    JournalDoklady Earth Sciences
    Volume379
    Publication statusPublished - Jun 1 2001

    ASJC Scopus subject areas

    • Earth and Planetary Sciences (miscellaneous)
    • Earth and Planetary Sciences(all)

    Cite this

    Izokh, A. E., Polyakov, G. V., Mal'kovets, V. G., Shelepaev, R. A., Travin, A. V., Litasov, Y. D., & Gibsher, A. A. (2001). The late Ordovician age of camptonites from the Agardag Complex of southeastern Tuva as an indicator of the plume-related magmatism during collision processes. Doklady Earth Sciences, 379, 511-514.