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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...
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