| | | | | | | | Well Registration Number | 49/26-C70 | Interpretation | Composite | Date Coded | 10/10/1989 | Depth Units | Feet |
| | Datum | KB | Datum Elevation | 90.70 | Loggers TD | 0.00 | TWT Scale | | Thickness Type | |
| | | | | | | | | | | | | | | | | | | | | | | | | | | | | | | | | | | | | Litho Stratigraphy | Chronostraigraphy | Lithology Components | | Top Down Hole Depth | Top Vertical Depth (MSL) | Top TWT (msec) | Thickness | Upper Litho | Lower Litho | Upper Chrono | | Lower Chrono | | 1 | % | 2 | % | 3 | % | 4 | % | Cored | Nature Of Top | Hydro carbon Present | Notes | 208.0 | 0.00 | 0.00 | 352 | * | * | QH | 0 | QP | 0 | | | | | | | | | N | | | SEA BED | 560.0 | 0.00 | 0.00 | 110 | * | * | KL | 0 | KL | 0 | | | | | | | | | N | | | | 670.0 | 0.00 | 0.00 | 735 | KEUP | KEUP | T | 0 | T | 0 | | | | | | | | | N | | | | 1405.0 | 0.00 | 0.00 | 230 | KEUP | KEUP | T | 0 | T | 0 | CLAY | 100.00 | | | | | | | N | | | FIRST RETURN | 1635.0 | 1,515.00 | 0.00 | 703 | MUSC | MUSC | T | 0 | T | 0 | CLAY | 75.00 | HALI | 25.00 | | | | | N | | | | 2338.0 | 2,158.00 | 0.00 | 396 | ROTU | ROTU | T | 0 | T | 0 | CLAY | 100.00 | | | | | | | N | | | | 2734.0 | 2,510.00 | 0.00 | 1316 | BNS | BNS | T | 0 | T | 0 | SAND | 92.00 | CLAY | 8.00 | | | | | N | | | | 4050.0 | 3,691.00 | 0.00 | 1073 | BTSH | BTSH | T | 0 | T | 0 | SHAL | 98.00 | SAND | 2.00 | | | | | N | | | | 5123.0 | 4,678.00 | 0.00 | 202 | Z4 | Z4 | P | 0 | P | 0 | HALI | 100.00 | | | | | | | N | | | | 5325.0 | 4,864.00 | 0.00 | 417 | Z3 | Z3 | P | 0 | P | 0 | HALI | 45.00 | DOLO | 40.00 | PSAL | 10.00 | ANHY | 5.00 | N | | | | 5742.0 | 5,250.00 | 0.00 | 434 | Z2 | Z2 | P | 0 | P | 0 | DOLO | 60.00 | ANHY | 20.00 | HALI | 20.00 | | | N | | | | 6176.0 | 5,651.00 | 0.00 | 654 | Z1 | Z1 | P | 0 | P | 0 | HALI | 60.00 | ANHY | 38.00 | DOLO | 2.00 | | | N | | | | 6830.0 | 6,242.00 | 0.00 | 650 | ROTL | ROTL | P | 0 | P | 0 | SAND | 100.00 | | | | | | | N | | | | 7480.0 | 6,834.00 | 0.00 | 0 | ROTL | ROTL | * | 0 | * | 0 | | | | | | | | | N | | | TD |
| | | | | | | | | | |
|