A marine geophysical study of the Wilkes Land rifted continental margin, Antarctica
The Wilkes Land margin of East Antarctica, conjugate to the southern Australian margin, is a non-volcanic rifted margin that formed during the Late Cretaceous. During 2000-01 and 2001-02, Geoscience Australia (GA) acquired ~10,000 line km of seismic reflection, magnetic anomaly, and gravity anomaly...
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| Formato: | Tese |
| Idioma: | English |
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2005
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A marine geophysical study of the Wilkes Land rifted continental margin, Antarctica
Publicado em 2009
Journal article