Geologie / Paleontologie / Lithotheek

  1. VAN LIEFFERINGE N. 2011, Een ontsluiting van silex en opaal ('Les Planchettes-vuursteen') in de glauconiethoudende zanden van het Onder-Eoceen (Formatie van Gentbrugge, Lid van Vlierzele/Lid van Pittem, België) (= Quadriga 03).
  2. DE CEUKELAIRE M. & VAN LIEFFERINGE N. 2011, Discovery of green flint incorporated in quartzarenitic sandstone of early eocene age in the Belgian basin (Flobecq, Belgium). Poster presented at GEO REG, forum de la fédération française des géosciences (Villeneuve d'Ascq, 23-27 octobre 2011).
  3. VAN LIEFFERINGE N. 2012, Un ensemble lithique en calcé doine dendritique à Ath-Ferme de Tenre (prov. Hainaut, Belgique) (= Quadriga 04).
  4. VAN LIEFFERINGE N. 2012, Database of lithic raw material types found at prehistoric surface sites in the region of 'Le Pays des Collines', 'Vlaamse Ardennen' and 'Pajottenland' (BELGIUM), part 1 (= Quadriga 06).
  5. VAN LIEFFERINGE N. 2012, The effect of ichnofossils and other ghost structures on the patination of flint artefacts (= Quadriga 09).
  6. VAN LIEFFERINGE N. 2012, Database of lithic raw material types found at prehistoric surface sites in the region of 'Le Pays des Collines', 'Vlaamse Ardennen' and 'Pajottenland' (BELGIUM), part 2 (= Quadriga 10).
  7. VAN LIEFFERINGE N. 2013, Fossil specimens of Pinna margaritacea (Lam.) from Herquegies-Bois de Pétrieux (province of Hainaut, Belgium) (= Quadriga 11).
  8. VAN LIEFFERINGE N. 2013, Tackling the "ploughzone paradox". The case of lithic scatters (= Quadriga 12).
  9. VAN LIEFFERINGE N. 2013, 'Ploughzone lithics'. The surface assemblage of Everbeek-Mierenhoek (Belgium). Flint type EMs1 (= Quadriga 14).
  10. VAN LIEFFERINGE N. 2013, 'Ploughzone lithics'. The surface assemblage of Ath-Bois du Renard (Belgium). Flint type ARs1 (= Quadriga 16).
  11. VAN LIEFFERINGE N. 2013, 'Ploughzone lithics'. The surface assemblage of Vertrijk-Keizerstraat (Belgium). Flint type VKs1 (= Quadriga 17).
  12. VAN LIEFFERINGE N. 2013, Exogenous materials in the Usselo layer caused by a large scale melt-out of "dirty" stagnant ice (= Quadriga 22).