Fig. 6.41. West-east (i.e., paleostrike) cross-section through part of the Brent Group correlated with wells between 960 and 280 m apart. Note the
good west-east continuity of the transgressive marine sands of the Tarbert Formation, at the top. Compare this with the lenticular nature of the
channel sands in the Ness Formation beneath. (From Johnson and Stewart, 1985. Courtesy of the Geological Society of London.)
good west-east continuity of the transgressive marine sands of the Tarbert Formation, at the top. Compare this with the lenticular nature of the
channel sands in the Ness Formation beneath. (From Johnson and Stewart, 1985. Courtesy of the Geological Society of London.)