-
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... -
Towards IODP deep riser stratigraphic drilling in northern Zealandia:...
The Lord Howe Rise, the backbone to northern Zealandia, is a ribbon of submerged and extended continental crust that separated from Australia during the Late Cretaceous.... -
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... -
IODP deep riser stratigraphic drilling in the southwest Pacific: tectonics,...
The Lord Howe Rise is a ribbon of submerged and extended continental crust that separated from Australia during the Late Cretaceous. The Lord Howe Rise is remote and concealed... -
Progress towards deep coring of the Lord Howe Rise, northern Zealandia: a...
Much has been achieved in 50 years of DSDP, ODP and IODP. However, to date deep riser drilling has played a relatively small role in IODP and its predecessors, albeit a role... -
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... -
First insights into the deep structure across the Tasman Basin and Lord Howe...
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...
1 - 9 of 9 results