Seismic images of contourites forming continental slope terraces at the Argentine Margin: implications for past changes in thermohaline circulation
An extensive (> 11000 km) set of high quality seismic reflection profiles from the Argentine continental margin shows a significant contourite system formed by the interaction of northward flowing Antarctic water masses and southward flowing North Atlantic Deep Water (NADW). Here, we focus on a s...
Main Authors: | , , |
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Format: | Conference Object |
Language: | unknown |
Published: |
2010
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Subjects: | |
Online Access: | https://epic.awi.de/id/eprint/22479/ https://hdl.handle.net/10013/epic.34879 |