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- W1995514402 abstract "Abstract A small Early Cambrian carbonate platform occurs at the southeast margin of the Bunkers Graben near Wilkawillina Gorge in the Flinders Ranges. Platform sediments are represented by the Wilkawillina Limestone, with biohermal, calcarenite, lagoonal and peritidal facies present. Sedimentation on the platform was interrupted by several periods of subaerial exposure. Platform and off‐platform facies interfinger, deep water sediments include the slope carbonates of the Parara Limestone and the Oraparinna Shale. Shallow marine off‐platform facies are represented by the Bunkers Sandstone and Edeowie Limestone Member. The platform evolved from a shoal‐rimmed to a reef‐rimmed bypass margin. The platform sequence provides a useful model to interpret similar Early Cambrian successions elsewhere in the Delamerian fold belt and further afield. Key words: Early Cambrianpalaeoecologyplatform carbonatesreefsslope carbonatesSouth AustraliaWilkawillina Limestone Notes Present address: Geology Department, Western Mining Corporation, Kambalda, WA 6442, Australia." @default.
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- W1995514402 date "1990-12-01" @default.
- W1995514402 modified "2023-09-25" @default.
- W1995514402 title "An Early Cambrian carbonate platform near Wilkawillina Gorge, South Australia" @default.
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- W1995514402 doi "https://doi.org/10.1080/08120099008727946" @default.
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