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Fig. 15


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Geological model placing the inferred brecciation processes in the context of a transition from salt-rich to salt-poor rift evolution as suggested for the formation of the rifted domains in the Agly Massif.

Modèles géologiques replaçant les processus de formation des brèches dans un système évoluant depuis un rift riche en évaporites jusqu’à un rift pauvre en évaporites.

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