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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| Muut tekijät: | |
| Aineistotyyppi: | Opinnäyte |
| Kieli: | English |
| Julkaistu: |
2005
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A marine geophysical study of the Wilkes Land rifted continental margin, Antarctica
Julkaistu 2009
Journal article