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- W1968344583 abstract "The Rio Magno unit (eastern Corsica) is represented by an Apenninic-type (Internal Ligurides) ophiolitic sequence: N-MORB basalts, Lower Cretaceous Palombini-bearing limestones, Middle Cretaceous flysch. In addition, it is unaffected by HP–LT alpine metamorphism. These peculiar features further support the hypothesis of close geodynamical relationships between the Corsican and Northern Apenninic ophiolites. We suggest that, in the Jurassic Piedmont-Ligurian oceanic basin, the Rio Magno and Internal Ligurides ophiolitic sequences represent a continuous, internal, oceanic palaeodomain. Afterwards, during Late Cretaceous–Late Eocene, they underwent a similar orogenic evolution, escaping from deep involvement during the subduction beneath the European continental margin. L'unité du rio Magno, située en Corse orientale, en position tectonique supérieure, possède des termes de type apennin (Ligurides internes) : basaltes jurassiques N-MORB, formation de type Palombini du Crétacé inférieur, formation flyschoı̈de du Crétacé moyen. Aucune de ces roches ne montre de trace de métamorphisme alpin de HP–BT. Ces caractéristiques appuient l'hypothèse de relations géodynamiques étroites entre les ophiolites de Corse et celles de l'Apennin septentrional. Il est suggéré que, dans le bassin océanique jurassique Liguro-Piémontais, les successions ophiolitiques du rio Magno et des Ligurides internes étaient voisines dans un même paléo-domaine océanique interne. Par la suite, du Crétacé terminal à l'Éocène supérieur, elles auraient subi la même évolution orogénique, échappant à un enfouissement profond durant la subduction sous la marge continentale européenne." @default.
- W1968344583 created "2016-06-24" @default.
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- W1968344583 date "2001-09-01" @default.
- W1968344583 modified "2023-09-27" @default.
- W1968344583 title "L'unité ophiolitique du rio Magno en Corse alpine, élément des Ligurides de l'Apennin septentrional" @default.
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- W1968344583 doi "https://doi.org/10.1016/s1251-8050(01)01633-0" @default.
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