| | | | | | | | | Well Registration Number | 9/18b- 25 | | Interpretation | Composite | | Date Coded | 15/11/2001 | | Depth Units | Feet |
| | | Datum | KB | | Datum Elevation | 85.00 | | 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 | | 457.0 | 374.00 | | 2268 | * | | * | 0 | | 0 | | | | | | | | | N | | | SEABED | | 2725.0 | 2,642.00 | | 290 | HORF | | GL | 0 | GY | 0 | CLST | 78.00 | SDST | 22.00 | | | | | N | | | FIRST RETURN | | 3015.0 | 2,932.00 | | 685 | MGSM | | GL | 0 | GY | 0 | SDST | 96.00 | CLST | 4.00 | | | | | N | | | | | 3700.0 | 3,617.00 | | 1030 | HORF | | GL | 0 | GY | 0 | CLST | 97.00 | LMST | 3.00 | | | | | N | | | | | 4730.0 | | | 791 | HORF | | GY | 0 | | 0 | CLST | 98.00 | LMST | 2.00 | | | | | N | | | | | 5521.0 | 5,438.00 | | 39 | BAB3 | | GY | 0 | GC | 0 | CLST | 100.00 | | | | | | | N | | | | | 5560.0 | | | 158 | BAB3 | | GC | 0 | | 0 | CLST | 98.00 | LMST | 2.00 | | | | | N | | | | | 5718.0 | 5,635.00 | | 94 | BAB2 | | GC | 0 | | 0 | CLST | 78.00 | TFCL | 20.00 | LMST | 2.00 | | | N | | | | | 5812.0 | 5,729.00 | | 52 | BB2S | | GC | 0 | | 0 | SDST | 100.00 | | | | | | | N | | | | | 5864.0 | 5,781.00 | | 22 | BAB2 | | GC | 0 | | 0 | CLST | 100.00 | | | | | | | N | | | | | 5886.0 | 5,803.00 | | 18 | BAB1 | | GC | 0 | | 0 | TFCL | 100.00 | | | | | | | N | | | | | 5904.0 | 5,821.00 | | 31 | BB1S | | GC | 0 | | 0 | SDST | 80.00 | CLST | 20.00 | | | | | N | | | | | 5935.0 | 5,852.00 | | 38 | BAB1 | | GC | 0 | | 0 | CLST | 50.00 | TFCL | 50.00 | | | | | N | | | | | 5973.0 | 5,890.00 | | 127 | SELE | | GC | 0 | | 0 | CLST | 97.00 | LMST | 3.00 | | | | | N | | | | | 6100.0 | 6,017.00 | | 0 | | | * | 0 | | 0 | | | | | | | | | N | | | TD |
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