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- Die Kössen-Formation (auch Kössener Schichten) ist eine lithostratigraphische Einheit der Nördlichen Kalkalpen im Rang einer Formation.Namensgebend und Typlokalität ist der Ort Kössen in Tirol.Gesteine der Kössen-Formation treten auch in den Tegernseer Bergen, im Estergebirge sowie in den Ammergauer, Lechtaler und Allgäuer Alpen zu Tage. Die Kössen-Formation besteht aus einer Wechsellagerung dunkelgrauer Tonsteine, Mergelund toniger Kalksteine, die in der oberen Trias (Rhaetium)auf dem Schelf des westlichen Tethysmeeres abgelagert wurden.Die Gesteine der Kössen-Formation gelten als sehr reich an Fossilien. (de)
- The Kössen Formation is a Late Triassic (Rhaetian-age) geological formation in the Northern Calcareous Alps of Austria and Germany, in the Tiroler-Lech Nature Park. During the Late Triassic, the area now occupied by the Northern Calcareous Alps was instead a long, passive coastline at the western tip of the Neotethys Ocean. The environment was initially dominated by a wide and shallow carbonate platform within a lagoon between the shore and a string of reefs. This carbonate platform is nowadays preserved as the Carnian to Norian-age Hauptdolomit and Dachstein Formation. The Kössen Formation represents a period of increased siliciclastic clay input into the lagoon, covering up the carbonate platform with marls and marly limestones instead of pure limestone or dolomite. The Eiberg Member of the Kössen Formation was deposited in the Eiberg basin, a narrow strip of deeper water which developed between the carbonate platform and the shoreline in the later part of the Rhaetian. (en)
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- Hochalm Member, Eiberg Member, "Zirmenkopf limestone" (en)
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- Die Kössen-Formation (auch Kössener Schichten) ist eine lithostratigraphische Einheit der Nördlichen Kalkalpen im Rang einer Formation.Namensgebend und Typlokalität ist der Ort Kössen in Tirol.Gesteine der Kössen-Formation treten auch in den Tegernseer Bergen, im Estergebirge sowie in den Ammergauer, Lechtaler und Allgäuer Alpen zu Tage. (de)
- The Kössen Formation is a Late Triassic (Rhaetian-age) geological formation in the Northern Calcareous Alps of Austria and Germany, in the Tiroler-Lech Nature Park. During the Late Triassic, the area now occupied by the Northern Calcareous Alps was instead a long, passive coastline at the western tip of the Neotethys Ocean. The environment was initially dominated by a wide and shallow carbonate platform within a lagoon between the shore and a string of reefs. This carbonate platform is nowadays preserved as the Carnian to Norian-age Hauptdolomit and Dachstein Formation. The Kössen Formation represents a period of increased siliciclastic clay input into the lagoon, covering up the carbonate platform with marls and marly limestones instead of pure limestone or dolomite. The Eiberg Member of (en)
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- Kössen-Formation (de)
- Kössen Formation (en)
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