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Summary
| Description |
Deutsch: Obetrias, Karnium- ca.220 mya: Die westliche (Neo-)Tethys teilt die östliche Pangea.
Italiano: Rappresentazione della Terra al passaggio Ladinico-Carnico. Prosegue l'espansione della Neotetide e le micro-placche cimmeriche si avvicinano al margine settentrionale della Paleotetide, ormai molto ridotta. La subduzione di crosta oceanica al margine occidentale della Paleotetide è probabilmente all'origine di un vulcanismo di arco nell'area delle attuali Alpi Meridionali. Nel settore nord-occidentale della Tetide si individuano nuovi piccoli bacini oceanici in fase di espansione. Un sistema di rift attivo interessa l'area corrispondente alla micro-placca Adria almeno dal Triassico Medio. Stampfli e Borel, 2002. Modificato. |
| Source | Stampfli & Borel (2002), modified |
| Author | Antonov |
Licensing
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| Date/Time | Thumbnail | Dimensions | User | Comment | |
|---|---|---|---|---|---|
| current | 17:19, 18 November 2007 | | 720 × 540 (126 KB) | Antonov | {{Information |Description= |Source= Stampfli & Borel (2002), modified |Date= |Author= |Permission= |other_versions= }} |
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