Peak areas and heights for minerals of ODP Leg 113-696B (Table 1)
Seismic data acquired over the eastern shelf and margin of the South Orkney microcontinent, Antarctica, have shown a high-amplitude reflection lying at a sub-bottom two-way traveltime (TWT) of 0.5-0.8 s. There appear to be two causes for the reflection which apply in different parts of the shelf. Th...
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Format: | Dataset |
Language: | English |
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PANGAEA
1990
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Online Access: | https://doi.pangaea.de/10.1594/PANGAEA.753957 https://doi.org/10.1594/PANGAEA.753957 |