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. 9

The cover décollement and the cataclastic Triassic breccias in the Saraillé area: some field aspects. A. 20–30 m thick strongly sheared pink chlorite-talcschists at site of sample SAR30. B. Well-bedded Upper Triassic carbonates entirely changed into a 3–5 m thick magnesitite level (site of sample SAR22). C. Polymictic Triassic tectonic breccias (site of samples SAR17a and SAR17b). D. Brecciated meta-ophite (site of sample SAR14). E. Polymictic Triassic tectonic breccia including clasts of meta-ophite (green), Paleozoic schist (black) and cellular dolostone (“cargneules”) (site of sample BCOR250c).

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