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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... -
The Lord Howe Rise continental ribbon: a fragment of eastern Gondwana that...
Plate tectonics and resulting changes in crustal architecture profoundly influence global climate, oceanic circulation, and the origin, distribution and sustainability of life.... -
Eastern Gondwana breakup: Rifting and subsidence from the Tasman Basin...
During the Late Cretaceous, the eastern Australian margin rifted to form the Lord Howe Rise continental ribbon. To understand the history of this region since rifting we use... -
First insights into the deep structure of the eastern Australian passive...
The eastern Australian margin was shaped by the fragmentation of eastern Gondwana during the Late Cretaceous. This led to the opening of the Tasman Basin and to the formation of... -
The Lord Howe Rise: new views of enigmatic continental ribbon breakup from...
The Lord Howe Rise is a continental ribbon that rifted from eastern Gondwana during the Late Cretaceous. The processes that lead to this breakup are still not fully understood,... -
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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