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...
| المؤلفون الرئيسيون: | , , |
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| التنسيق: | Journal article |
| اللغة: | English |
| منشور في: |
2009
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