Abstract
The southern Scotia Sea contains several small ocean basins bounded by submarine banks of continental or transitional nature. The majority of the basins were developed during the Oligocene and Miocene as a result of the eastward migration of a tectonic arc over the Weddell Sea and the Atlantic Ocean.
| Original language | English |
|---|---|
| Pages (from-to) | 330-333 |
| Number of pages | 4 |
| Journal | Bollettino di Geofisica teorica ed applicada |
| Volume | 54 |
| Issue number | Supplement 2 |
| Publication status | Published - 2013 |
| Externally published | Yes |
| Event | GeoSur 2013 : International Geological Congress on the Southern Hemisphere - Viña del Mar, Chile Duration: 25 Nov 2013 → 27 Nov 2013 |
Programme Area
- Programme Area 2: Water Resources
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