Large-scale vertical movements in Cenomanian to Santonian carbonate platform in Iberia: indicators of a Coniacian pre-orogenic compressive stress

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

Open Access

Fig. 8

Correlation diagram of Cenomanian to Santonian sections along the transect of this study. This diagram incorporates 14 outcrop sections examined in this study and 2 sections modified from Souquet (1967) (Chià and la Muria; locations in Fig. 1). Correlations are based on biostratigraphy (Fig. 3) and 10 recognized stratigraphic cycles (LC1 to LC10) delimited by maximum regressive surfaces (Ce1 to Sa2).

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