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Complex kink folds in the Lower Devonian fine-grained, siliciclastic metasediments of the core of the High-Ardenne Slate Belt (Belgium).
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Kink folds in the Lower Devonian fine-grained, siliciclastic metasediments of the core of the High-Ardenne Slate Belt (Belgium); northern part of the La Fortelle outcrop (Van Baelen 2010).
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Kink folds in the Lower Devonian fine-grained, siliciclastic metasediments of the core of the High-Ardenne Slate Belt (Belgium).
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- 211
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Folded Upper-Carboniferous series in the frontal area of the Rhenohercynian foreland fold-and-thrust betl at the northern extremity of the Pan-European Variscan orogen. World-class outcrops at the Namur Citadel (Belgium). Classic example of a N-verging antiform.
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Folded Upper-Carboniferous series in the frontal area of the Rhenohercynian foreland fold-and-thrust belt at the northern extremity of the Pan-European Variscan orogen. World-class outcrops at the Namur Citadel (Belgium).
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Highly deformed series of the "Plougastel Formation" in the Monts d'Arrée (Brittany, France). The geodynamic interpretation of this particular structure is discussed in the following publication: dx.doi.org/10.1016/j.jsg.2007.01.002
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A first trial of a wide angle view of the Baie des Trépassés at lowest tide. The Baie the Trépassés offers a unique cross-section across the "South Armorican Shear Zone". On the northern side of the Baie (left) one encounters the mylonitized Sizun trondhjemite, cataclasites, sheared Stephanian deposits, ...
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- 776
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The famous unconformity at the northwestern border of the Lower Palaeozoic Stavelot-Venn basement inlier in the valley of the Ninglinspo (Belgium). The layers are overturned and dip to the south. On the outcrop the basal conglomerate and reddish claystone is exposed; both are of Lochkovian age. The slates below the unc...
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- 825
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Le Conquet micaschists in the coastal section between Pointe St-Mathieu and Le conquet (Brittany, France).
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Highly deformed series of the "Plougastel Formation" in the Monts d'Arrée (Brittany, France).
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- 382
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