Core photograph plate. A. Thin bed, clay clast conglomerate within a massive to laminated, fine grained sandstone, interbedded with organic-rich silty laminations. B. Parallel laminated fine grained sandstones and hummocky cross stratification towards the top. C. Massive fine grained sandstones are usually associated with parallel laminated, fine grained sandstones. These are most frequency facies in the field. D. Presence of oscillatory ripples towards the top opf the photograph, interbedded with thinly laminated carbonaceous rich siltstones and very fine grained sandstones. Very scarce bioturbation is found along the core. E. Heterolithic facies that consists of thinly laminated carbonaceous rich siltstones and very fine grained sandstones interbedded with parallel and ripple laminated, very fine grained sandstones. F. Massive, fine grained sandstones underlain by thinly laminated, carbonaceous rich, siltstones and very fine grained sandstones. No bioturbation effect is observed.