Shallow marine sedimentation within an active margin basin, James Ross Island, Antarctica
The Santa Marta Formation exposed on northern James Ross Island, Antarctica, represents shallow marine shelf sedimentation within an active margin basin. The formation is approximately 1000 m thick, is of uppermost Santonian to Campanian age and represents part of a 5000–6000 m thick sedimentary seq...
| Published in: | Sedimentary Geology |
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| Main Author: | |
| Format: | Article in Journal/Newspaper |
| Language: | unknown |
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Elsevier
1989
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| Online Access: | http://nora.nerc.ac.uk/id/eprint/521316/ https://doi.org/10.1016/0037-0738(89)90071-7 |