Geological and geophysical survey in the Bellingshausen Basin, off Antarctica
The continental margin in the Bellingshausen Basin off West Antarctica was geologically and geophysically surveyed. The paleo-trench, which has been inferred from the seafloor magnetic anomalies, is found out in the 3-fold seismic reflection profiles. In addition, the paleo-trench-lower-slope-sedime...
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Format: | Article in Journal/Newspaper |
Language: | English Japanese |
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National Institute of Polar Research
1982
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Online Access: | https://doi.org/10.15094/00008303 https://doaj.org/article/0257d662ec77485db478e82c127e1d11 |