Evidence of decoupled deformation during Jurassic rifting and Cenozoic inversion phases in the salt-rich Corbières-Languedoc Transfer Zone (Pyreneo-Provençal orogen, France)

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

Open Access

Fig. 3

Left: table summarizing the general lithostratigraphy of the Corbières Virgation from Paleozoic to Miocene with a synthesis of the main tectonic events. Right: table summarizing the detailed lithostratigraphy subdivisions of the Black Dolomites Group found in the Corbières Virgation, derived from BRGM geological maps (1/50,000) and many others studies. Red dashed lines represent unconformities (H1 to H9). Abreviations are H: Hiatus/Unconformity; L: lower; U: upper.

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