Abstract
Zealandia is a submerged continent in the southwest Pacific Ocean that can be regarded as a rifted part of eastern Australia and West Antarctica. Described simply, the pre- Gondwana-breakup Zealandia geological record is one of a Cambrian to Early Cretaceous Gondwana convergent margin, followed by Late Cretaceous continental rifting. NEW
Cite
CITATION STYLE
APA
Mortimer, N. (2006). Zealandia. ASEG Extended Abstracts, 2006(1), 1–4. https://doi.org/10.1071/aseg2006ab119
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