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Deep structure offshore Eastern Australia from wide-angle seismic data: what...
The eastern Australian margin was shaped during the fragmentation of eastern Gondwana in the Late Cretaceous. This led to the opening of the Tasman Basin and to the formation of... -
Eastern Gondwana breakup and the Lord Howe Rise continental ribbon from...
The eastern Australian margin of Gondwana rifted during the Late Cretaceous, forming the Lord Howe Rise continental ribbon. This breakup is still poorly understood with only a...
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