The transition from Pyrenean shortening to Gulf of Lion rifting in Languedoc (South France) – A tectonic-sedimentation analysis

Special Issue Orogen lifecycle: learnings and perspectives from Pyrenees, Western Mediterranean and analogues

Open Access

Fig. 19

Interpreted line drawing of a seismic reflection profile across the Gardon Basin showing the syn-depositional migration of the hanging-wall syncline. Modified after Sanchis (2000). Main markers are identified; Priabonian interval in purple overlay; intra-Priabonian marker corresponds to the base of “Grès de Celas” Formation. Location in Figures 2 and 21.

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