Carbon and U-Pb evidence for a Palaeoproterozoic crustal component in the Central Zone of the Limpopo Belt, South Africa

I. S. Buick*, I. S. Williams, R. L. Gibson, I. Cartwright, J. A. Miller

*Corresponding author for this work

    Research output: Contribution to journalArticlepeer-review

    48 Citations (Scopus)

    Abstract

    Supposedly mid-Archaean (c. 3.3 Ga) granulite-grade marbles from the Gumbu Group, Central Zone, Limpopo Belt (South Africa) have anomalously high δ13C values (+4.6 to +7‰) interpreted as minimum values for their limestone protoliths. Such elevated δ13C values are unknown in any Archaean carbonate worldwide, but occur in Palaeoproterozoic (c. 2.4-2.1 Ga) carbonates; for example, on the adjacent Zimbabwe and Kaapvaal cratons. This suggests that the Central Zone contains a previously unrecognized Palaeoproterozoic cover sequence, contrary to the prevailing view. This conclusion is supported by zircon U-Pb sensitive high-resolution ion microprobe ages from two metasediments, which, in addition to c. 2.02 Ga metamorphic zircon overgrowths, contain detrital zircons no older than c. 2.68 Ga, and some possibly as young as c. 2.2 Ga. The recognition of post-3.3 Ga metasedements in the Central Zone requires a major revision of models of the tectonic evolution of the Limpopo Belt.

    Original languageEnglish
    Pages (from-to)601-612
    Number of pages12
    JournalJournal of the Geological Society
    Volume160
    Issue number4
    DOIs
    Publication statusPublished - Jul 2003

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