Table 3 Sedimentological characteristics of marine submersions deposits along the TAH17–1 core
Events | Position in the core (cm) | Thickness (cm) | Grading | Sorting | Upper Contact | Basal contact | Other sedimentological characteristics |
|---|---|---|---|---|---|---|---|
E1 | 87–92 125–140 | 20 | No (chaotic structure) | Very poorly sorted | Relatively sharp | Sharp (erosional) | Angular gravels and Mud-clasts |
E2 | 148–149 | 1 | No | Very poorly sorted | Sharp | Sharp | No |
E3 | 150–151 | 1 | No | Very poorly sorted | Sharp | Sharp | No |
E4 | 152–153 | 1 | No | Very poorly sorted | Sharp | Sharp | No |
E5 | 154–155 | < 1 | No | Very poorly sorted | Sharp | Sharp | No |
E6 | 154–155 | < 1 | No | Very poorly sorted | Sharp | Sharp | No |
E7 | 155–156 | < 1 | No | Very poorly sorted | Sharp | Sharp | No |
E8 | 155–156 | < 1 | No | Very poorly sorted | Sharp | Sharp | No |
E9 | 156–157 | 1 | No | Very poorly sorted | Sharp | Sharp | No |
E10 | 159–160 | 1 | No | Very poorly sorted | Slightly Sharp | Slightly Sharp | No |
E11 | 163.5–165 | 1,5 | No | Very poorly sorted | Slightly Sharp | Slightly Sharp | No |
E12 | 172–175 | 3 | No | Very poorly sorted | Slightly Sharp | Slightly Sharp | No |
E13 | 190–230 | 40 | Unclear | Very poorly sorted | Sharp | Gradational | No |
E14 | 248–270 | 22 | Normal grading | Poorly sorted | Gradational | Not found | Mud-clasts |