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 acquired ∼10000 line km of seismic reflection and refraction, magnetic anomaly and gravity...
| Váldodahkkit: | , , |
|---|---|
| Materiálatiipa: | Journal article |
| Giella: | English |
| Almmustuhtton: |
2009
|