Mantle exhumation at magma-poor passive continental margins. Part II: Tectonic and metasomatic evolution of large-displacement detachment faults preserved in a fossil distal margin domain (Saraillé lherzolites, northwestern Pyrenees, France)

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Fig. 14

A reconstruction of the North Iberia distal margin with emphasis on fluid pathways in the crust-mantle detachment and cover décollement as reconstructed from geological and mineralogical studies in the Saraillé massif (detailed comments in text).

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