Revisiting orogens during the OROGEN Project: Tectonic maturity, a key element to understand orogenic variability

• Published in: Bulletin de la Société géologique de France 2024-12, Vol.195, p.1-35
• Main Authors: Masini, Emmanuel, Chevrot, Sébastien, Manatschal, Gianreto, Vidal, Olivier, Ford, Mary, Mouthereau, Frédéric
• Format: Article
• Language: English
• Subjects: africa-europe plate boundary; bay of biscay-pyrenean system; Earth Sciences; Geophysics; orogenesis; rifting inheritances; Sciences of the Universe; tectonic maturity; wilson cycle
• ISSN: 0037-9409; 1777-5817
• DOI: 10.1051/bsgf/2024021

By demonstrating that extensional inheritance plays a decisive role in the formation of orogens, recent studies have questioned the ability of a unique, complete Wilson cycle model to explain the diversity of collisional orogens. For 5 years, the OROGEN Research Project had therefore the ambition to challenge this classical Wilson cycle model. By focusing on the diffuse Africa-Europe plate boundary in the Biscay-Pyrenean-Western Mediterranean system, the project questioned the preconceived “Orogen singularity” assumption and investigated the role of divergent and convergent maturities in orogenic and post-orogenic processes. This work led us to rethink the development of collisional orogens in a genetic (or process-driven) way and to propose an updated version of the "classical Wilson cycle", the Wilson Cycle 2.0, and the ORO-Genic ID concept presented in this paper. The particularity of the Wilson Cycle 2.0 is to take into account the divergence and convergence maturity reached during extensional and orogenic processes in proposing different tectonic tracks associated with different ORO-Genic ID numbers. The ORO-Genic ID is composed of a letter (or track), corresponding to the maturity of divergence reached and a number corresponding to the maturity of convergence reached during the formation of the orogen. This new concept relies on the observed pre- and syn- convergent tectono-stratigraphic and magmatic record and deformation history and can be identified in using diagnostic criteria presented in this paper. It represents therefore a powerful tool that can be used to characterize the evolution and the architectural type of an orogenic system. Moreover, as a mappable concept, it can be easily used worldwide and can help us to explain differences in the style of deformation at crustal scale between orogens.