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The Lord Howe Rise: newly-acquired multi-channel and wide-angle seismic data...
The Lord Howe Rise (LHR) is located to the east of Australia in water depths up to 3,000 m. The LHR is a 600 km wide and 1,600 km long continental ribbon that detached from... -
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.... -
Lord Howe Rise: Project Flyer - 2018 Version
The Lord Howe Rise Project is a collaborative research project between Geoscience Australia and the Japan Agency for Marine-Earth Science and Technology (JAMSTEC) that aims to... -
Crustal structure across the Lord Howe Rise, northern Zealandia, and rifting...
During the Late Cretaceous, the fragmentation of eastern Gondwana led to the formation of the narrow eastern Australian margin and the wide Lord Howe Rise during the opening of... -
Delayed subsidence after rifting and a record of breakup for northwestern Zealandia
Continental rifting and breakup of eastern Gondwana during the Cretaceous separated northern Zealandia from eastern Australia, but the processes leading to this highly-extended... -
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.... -
The Lord Howe Rise: newly-acquired multi-channel and wide-angle seismic data...
The Lord Howe Rise (LHR) is located to the east of Australia in water depths up to 3,000 m. The LHR is a 600 km wide and 1,600 km long continental ribbon that detached from... -
Lord Howe Rise: Project Flyer - 2018 Version
The Lord Howe Rise Project is a collaborative research project between Geoscience Australia and the Japan Agency for Marine-Earth Science and Technology (JAMSTEC) that aims to...
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