Chapter 69 The glacial succession of Sturtian age in South Australia: The Yudnamutana Subgroup

Wolfgang V. Preiss*, Victor A. Gostin, David M. McKirdy, Paul M. Ashley, George E. Williams, Philip W. Schmidt

*Corresponding author for this work

    Research output: Contribution to journalArticlepeer-review

    39 Citations (Scopus)

    Abstract

    The record of two Neoproterozoic glaciations in South Australia has been known for about a century. The earlier glaciation, of Sturtian age, is represented by the Yudnamutana Subgroup and is characterized by widespread diamictites with both intrabasinal and extrabasinal clasts, some locally faceted and striated. Associated facies include shallow-water sandstone, bedded and laminated siltstone with lonestones and dropstones, and sedimentary ironstones (mainly ferruginous siltstone and diamictite). Proximal settings adjacent to the Curnamona Province display massive basement-derived conglomerate and gigantic basement megaclasts (up to hundreds of metres across).

    Original languageEnglish
    Pages (from-to)701-712
    Number of pages12
    JournalGeological Society Memoir
    Volume36
    Issue number1
    DOIs
    Publication statusPublished - 1 Jan 2011

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