RB 2018/00026 Sedimentology of the late Palaeozoic Cape Jervis Formation, Troubridge Basin, South Australia.
Published: 01 Nov 2018
Created: 15 Nov 2024
Revised: 15 Nov 2024
Author: Normington, V.J.;Hill, S.M.;Tiddy, C.J.;Giles, D.
The late Palaeozoic Cape Jervis Formation of the Troubridge Basin in southern South Australia provides a sedimentological record of the glacial environment during the Permo-Carboniferous glaciation. The sedimentary sequence is divided into five...
The late Palaeozoic Cape Jervis Formation of the Troubridge Basin in southern South Australia provides a sedimentological record of the glacial environment during the Permo-Carboniferous glaciation. The sedimentary sequence is divided into five informal units that comprise the Cape Jervis Formation, and which preserve sedimentological features that have been used to constrain models for the glacial setting and associated depositional mechanisms prevailing during this time. Landscape features such as glaciated pavements and the presence of lodgement till diamictite suggest that the glacial setting was a wet-based, continental icesheet with ice tongue glaciers at the front margin of the icesheet. The icesheet is believed to have advanced in a northwards to north-westwards direction, forming glaciated bedrock surfaces and depositing lodgement till. The presence of fluviolacustrine beds suggests that the icesheet's movement later ceased and its growth stagnated, which facilitated the formation of glacial lakes and meltwater streams. The icesheet then began to melt significantly and its leading edges retreated southward. Ablation of the ice resulted in deposition of a flow till complex and caused a eustatic rise in mean sea level that resulted in a marine transgression and subsequent deposition of glaciomarine sedimentary rocks.
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