Seismic-Reflection Signature of Cretaceous Continental Breakup on the Wilkes Land Margin, Antarctica
The passive (rifted) continental margin of Wilkes Land, Antarctica, is characterized on seismic reflection records by (i) in the south, a block-faulted sequence of highly stratified continental beds overlain by two distinct unconformities; (ii) a transitional, greatly thinned continental crust overl...
| Published in: | Science |
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| Main Authors: | , , |
| Format: | Article in Journal/Newspaper |
| Language: | English |
| Published: |
American Association for the Advancement of Science (AAAS)
1985
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| Subjects: | |
| Online Access: | http://dx.doi.org/10.1126/science.229.4718.1082 https://www.science.org/doi/pdf/10.1126/science.229.4718.1082 |