Structural and geochemical data on the R
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Elisa Padoa; Emilio Saccani; Michel Durand-Delga
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Article
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2001
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John Wiley and Sons
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English
⚖ 983 KB
The Rio Magno Unit (RMU) tectonically overlies the Schistes Lustrés units in south‐eastern Alpine Corsica. It is represented by an ophiolitic sequence, showing remarkable differences with respect to the commonly recognized Corsican ophiolites. This unit can be distinguished from the Schistes Lustrés