Resumé
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.
| Originalsprog | Engelsk |
|---|---|
| Sider (fra-til) | 330-333 |
| Antal sider | 4 |
| Tidsskrift | Bollettino di Geofisica teorica ed applicada |
| Vol/bind | 54 |
| Udgave nummer | Supplement 2 |
| Status | Udgivet - 2013 |
| Udgivet eksternt | Ja |
| Begivenhed | GeoSur 2013 : International Geological Congress on the Southern Hemisphere - Viña del Mar, Chile Varighed: 25 nov. 2013 → 27 nov. 2013 |
Programområde
- Programområde 2: Vandressourcer
Fingeraftryk
Dyk ned i forskningsemnerne om 'Dredged rock samples from the southwestern Scotia Sea (SCAN 2013): remnants from the South America-Antarctic continental bridge'. Sammen danner de et unikt fingeraftryk.Citationsformater
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