Morphology and Depositional Processes of a Carbonate-Filled Canyon in the Carboniferous KT-II Formation of the Eastern Precaspian Basin, Kazakhstan: Insight from 3D Seismic Data

Figure 11

(a) RMS amplitude map between SB1 and the basal surface of KT-II. A series of small gullies are located in the head segment of the CFC, and two channels are located in the middle and lower segments, with low RMS amplitude values. (b) RMS amplitude map between SB1 and the top surface of KT-II. Some large-scale channels perpendicular to the slope originating close to the platform edge are dominated by low RMS values. See the position in Figure 2.