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Chapitre d'ouvrage
Palaeozoic Basement of the Pyrenees
Abstract : In the Pyrenees, the Cambrian-Lower Ordovician strata represent a quiescent time span with no remarkable tectonic activity, followed by a late Early-Mid Ordovician episode of uplift and erosion that led to the formation of the Sardic unconformity. Silurian sedimentation was widespread and transgressive followed by a Devonian succession characterized by a complex mosaic of sedi-mentary facies. Carboniferous pre-Variscan sediments (Tournaisian-Viséan cherts and limestones) precede the arrival of the synorogenic siliciclastic supplies of the Culm flysch at the Late Serpukhovian. All this succession was subsequently affected by the Serpukhovian-Bashkirian (Variscan) collision, as a result of which, the Palaeozoic rocks were incorporated into the northeastern branch of the Ibero-Armorican Arc.
Littérature citée [169 références]
https://hal-brgm.archives-ouvertes.fr/hal-02309572
Contributeur : Maxime Padel <>
Soumis le : mercredi 9 octobre 2019 - 13:31:23
Dernière modification le : mercredi 10 février 2021 - 14:40:03
Contributeur : Maxime Padel <>
Soumis le : mercredi 9 octobre 2019 - 13:31:23
Dernière modification le : mercredi 10 février 2021 - 14:40:03
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Casas et al (2019) Cap8_Vol2_G...
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