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Fig. 10 | Swiss Journal of Geosciences

Fig. 10

From: Structural and metamorphic evolution of a subducted passive margin: insights from the Briançonnais nappes of the Western Alps (Ubaye–Maira valleys, France–Italy)

Fig. 10

Klippes and large D3 folds in the Combe-Brémond and Roure units. a Interpreted panorama on Bassa di Terrarossa klippe. This klippe overlies the contact between Roure unit and Queyras Schistes Lustrés. Another D3 syncline is visible in the background on Monte Albrage northern wall; b Interpreted panorama of Monte Maniglia from Bassa di Terrarossa; the D3 syncline and the backthrust klippe are highlighted. MRB Upper Jurassic Combe-Brémond marbles, TRM Ladinian-Anisian meta-dolostone and metapelite, TW Lower Triassic quartzite, SL Schistes Lustrés calcschist, φCDC Colle di Ciabriera backthrust, φBDT Bassa di Terrarossa backthrust; φSL Schistes Lustrés thrust

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