“…In this contribution, particular attention is paid to the characterisation of ice-front related stratigraphic architectures and macro-scale deformation structures (see Reinardy and Lukas, 2009 for a micro-scale case study). A well-preserved ice-marginal domain and its related succession were recently identified in the end-Ordovician glacial record of the western Murzuq Basin in Libya (Tihemboka area; Moreau et al, 2005;Moreau 2011;Ghienne et al, 2010;Girard et al, 2012a,b).…”