“…Gray micaceous fine sand, 1-5 m thick, 300 m wide developed between profiles IIerosional base, lensoid morphology, fining upward fill, large scale (7-10 cm thick) cross-beds, ripple cross-lamination, parallel lamination, animal burrows Deposition in high energy sinuous channels under lower flow regime fluctuating energy conditions (Allen, 1982;Ashley, 1990) Small-scale cross-bedded sand (Fig. 5C, F) Yellowish buff channelized micaceous silty very fine sand, 1-4 m thick, 170-300 m wide sheets, occurring at three levels between profiles I-V, ripple-parallel-laminated, low-angle planar cross-beds, liquefied, animal and plant traces minute calcrete nodules Episodic deposition in shallow channels under lower flow regime conditions (Kraus and Aslan, 1993;Nichols and Fisher, 2007;Ghazi and Mountney, 2009) Interstratified sand-silt-mud Micaceous, silty fine sand, 1-3 m thick, a few cm thick lensoid beds of sand-silt and mud, ripple-parallel-laminated, animal and plant traces, fining up character, muddy beds calcretized Deposition in wide shallow ephemera channels under lower flow regime conditions (Rygel et al, 2004;Shukla et al, 2006) Calcretized clayey silt Common lithofacies developed in sand, silt and mud units,1-4 m thick, sheet like, calcrete nodules range from mm size to 10 cm size, rhyzocretes, animal burrows, charcoal and plant remains common, occasionally ferruginous nodules developed, iron pigmentation Deposition in low-lying over-bank areas by suspension fall out followed by diagenetic changes (Farrel, 1987;Kraus and Gwinn, 1997;Citterio and Pié Gay, 2009) Shell-bearing mud (Fig. 5F) Developed in profile II, 60-70 cm thick, 150 m wide clayey beds succeeded by silt-sand beds forming coarsening up sequences, gastropod shells, charcoal, plant debris, poorly preserved lamination, minute calcrete and iron nodules Deposition in ponds related to overbank areas (Singh et al, 1999a;Srivastava et al, 2003a;Citterio and Pié Gay, 2009) …”