Seismic stratigraphy of the Eocene–lower Oligocene in the uruguayan continental margin
The uruguayan continental margin was generated following the fragmentation of the Gondwana supercontinent and the subsequent opening of South Atlantic Ocean. It constitutes an extensive sedimentation area in which three sedimentary basins can be found: the Punta del Este Basin, the southernmost port...
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| Other Authors: | , , |
| Format: | article |
| Language: | English |
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2018
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| Online Access: | https://hdl.handle.net/20.500.12008/22409 |
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