Discussion: Basin infill architecture and evolution from magnetostratigraphic cross-basin correlations in the southeastern Pyrenean foreland basin
The chronostratigraphy of the middle Eocene–upper Eocene successions of the southeastern Pyrenean foreland basin has been revised by [Taberner et al. (1999)][1]. This contribution was based on the correlation of the magnetic polarity stratigraphy (MPS) for several partial stratigraphic sections