A gamma-ray log, and profiles of sand content, facies, and permeability for another cored well in the Hambert-Aristocrat field area. The vertical profile differs from that of the interval shown in Figure 8-23 in that it becomes sandier upward. The contact between A and B is gradational, and the strata are bioturbated mudstones. Parasequence C is composed of bioturbated sandy mudstone to muddy sandstone, interpreted to have been deposited in a lower shoreface setting. After Slatt (1997).
Reprinted with permission of Soc. Sedimentary Geology (SEPM).