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    A ca. 200Ma hiatus between the Lower and Upper Transvaal Groups of southern Africa: SHRIMP U–Pb detrital zircon evidence from the Segwagwa Group, Botswana: Implications for Palaeoproterozoic glaciations 

    Mapeo, R.B.M.; Armstrong, R.A.; Kampunzu, A.B.; Modisi, M.P.; Ramokate, L.V.; Modie, B.N.J. (Elsevier B.V. www.elsevier.com/locate/epsl, 2006)
    The Segwagwa Group of southeastern Botswana, a correlate of the Pretoria Group of the Transvaal Supergroup of South Africa, consists of a major sequence of siliciclastic sedimentary rocks, minor carbonates and basaltic ...
    Thumbnail

    A ca. 200Ma hiatus between the Lower and Upper Transvaal Groups of southern Africa: SHRIMP U–Pb detrital zircon evidence from the Segwagwa Group, Botswana: Implications for Palaeoproterozoic glaciations 

    Mapeo, R.B.M.; Armstrong, R.A.; Kampunzu, A.B.; Modisi, M.P.; Ramokate, L.V.; Modie, B.N.J. (Elsevier www.elsevier.com/locate/epsl, 2006)
    The Segwagwa Group of southeastern Botswana, a correlate of the Pretoria Group of the Transvaal Supergroup of South Africa, consists of a major sequence of siliciclastic sedimentary rocks, minor carbonates and basaltic to ...

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    Author
    Armstrong, R.A. (2)
    > Kampunzu, A.B. (2) > Mapeo, R.B.M. (2) > Modie, B.N.J. (2) > Modisi, M.P. (2)
    Ramokate, L.V. (2)
    Subject
    Botswana (2)
    > Segwagwa/Pretoria Group (2) > Transvaal Supergroup (2) > Detrital zircon geochronology (1) > detrital zircon geochronology (1) > Glacial implications (1) > glacial implications (1) > Southern Africa (1) > southern Africa (1) > ... View MoreDate Issued > 2006 (2)

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