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Directory UMM :Data Elmu:jurnal:P:Precambrian Research:Vol101.Issue1.2000:

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Fig. 1. Location of the Adelaide Geosyncline in South Australia showing the inferred distribution of Sturtian ferruginous facies ofthe Umberatana Group in the Baratta Trough (modified from Preiss et al., 1993).
Fig. 2. Outcrop of ferruginous facies (Braemar ironstone facies) and associated Sturtian glaciogenic rocks (Pualco Tillite) in theeastern part of the Adelaide Geosyncline (modified from Rogers, 1978; Forbes, 1991).
Fig. 3. Stratigraphic succession of the Adelaide Geosyncline in the southeastern Nackara Arc (a, b) (modified from Preiss, 1987;Preiss et al., 1998) and (c) Braemar ironstone facies in the Razorback Ridge area (modified from Whitten, 1970).
Fig. 4. (A) Typical outcrop of the Braemar ironstone facies. Ironstone is intercalated with carbonate-bearing siltstone and minordiamictite and dolostone
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