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New structural and petrologic data on Mesozoic schists in the Rhodope (Bulgaria): geodynamic implications

✍ Scribed by Nikolay G Bonev; Gérard M Stampfli


Book ID
117801637
Publisher
Elsevier Science
Year
2003
Tongue
French
Weight
740 KB
Volume
335
Category
Article
ISSN
1631-0713

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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