“…Few data exist dealing with the creep behavior of Opalinus clay (Naumann et al, 2007), Boom clay (Yu et al, 2015), Callovia-Oxfordian Bure Clay (Gasc-Barbier et al, 2004), and other argillaceous rocks (Zhang and Rothfuchs, 2004;Fabre and Pellet, 2006). Creep experiments on shales focus on compaction and consolidation (Cogan, 1976;de Waal and Smits, 1988;Dudley et al, 1998), the effect of adsorption and swelling on creep (Heller and Zoback, 2011;Hol and Zoback, 2013) and on viscoelastic or viscoplastic creep of shales in response to nanoindentation (Mighani et al, 2015) and applied differential stresses at elevated confining pressures (Almasoodi et al, 2014;Zoback, 2009, 2010;Chong et al, p [5] creep is enhanced at high differential stress, high clay content, in the presence of water and if loaded normal to bedding orientation.…”