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ted inthe rom ian– e the ntil lba er r to in le– I shall take the interesting paper by Durand-Delga al. [6] as a starting point for making some remarks the puzzle of passive margin turbidites of the so-ca Alpine Corsica and on their relationships with those the northern Apennine Ligurian units, and, in particu regarding those sedimented before the orogenic sta For higher concision I put forward some points:

About the early Late Cretaceous siliciclastic turbidites in Corsica and northern Apennine ophiolitic successions