“…The texture of a crystalline sample can be described as the preferred orientation of its crystallites (Cullity, 1978) and can vary from simple (e.g. random, fibrelike; Pellegrino et al, 2012;Remiens et al, 2011;Fei et al, 2009;Beckers et al, 2010;Deniz & Harper, 2008), to epitaxial (Remiens et al, 2011;Dong et al, 2001;Ö zcan et al, 2002;Barbier et al, 2007;Mocuta et al, 2003), to rather complex (e.g. axiotaxy; Detavernier et al, 2003;Detavernier & Lavoie, 2004).…”