Australia: The Land Where Time Began

A biography of the Australian continent 

Barka Basin

The Barka Basin, of Early Devonian to Carboniferous age, overlapping the adjacent Kanmantoo Fold Belt, is a molassic transitional tectonic sequence that comprises the Mulga Downs Group. These fluvial sediments are predominantly comprised of medium to coarse-grained sandstone, as well as some minor siltstone (Glen et al., 1985).

Sources & Further reading

Geology of the Murray-Darling Basin - Simplified Lithostratigraphic Groupings

 
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                                                                                           Author: M.H.Monroe  Email: admin@austhrutime.com     Sources & Further reading