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Cenozoic contractional deformation in the North-Iberian continental margin (southern Bay of Biscay) led to the uplift of the Cantabrian Mountains and the northward subduction of part of the thick continental crust, down to at least ~55km depth beneath the coastline, and perhaps even ~30–40km deeper. In order to provide a more constrained model of this unique structure and gain insight into the factors...
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