“…Mud-rich surface waters, which prevailed during deposition of these floodplain muds, would percolate into underlying channel and crevasse splay sandstones and thus produced ideal conditions for infiltration of clays into the sandstones towards the base of the HST (Ketzer et al, 2003;El-Ghali et al, 2006). The fibrous, hair-like, flaky and honeycomb-like and with spiny terminations and booklet-like habits of illite indicate diagenetic origin Lemon and Cubitt, 2003). Illite, which typically forms during progressive burial (i.e.…”