Fig. 4
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Landscape of the Serre Chevalier ski station showing two of the three outcrops of crystalline rocks in this area. The Eocene olistostrome is intercalated between the two outcrops and the more distant one (Eychauda moutain) passes downward to a coarse-grained breccia mainly composed of crystalline fragments (Eychauda breccia).
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