| | | | | | | | Well Registration Number | 15/25b- 3 | Interpretation | Composite | Date Coded | 18/05/1992 | Depth Units | Feet |
| | Datum | KB | Datum Elevation | 80.00 | 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 | 577.0 | 497.00 | 0.00 | 1923 | NORD | * | QH | 0 | QP | 0 | | | | | | | | | N | | | SEABED | 2500.0 | 0.00 | 0.00 | 655 | NORD | * | QP | 0 | NP | 0 | CLST | 60.00 | SLST | 35.00 | SDST | 5.00 | | | N | | | FIRST RETURNS | 3155.0 | 3,075.00 | 0.00 | 1685 | LARK | * | NA | 0 | GN | 0 | SLST | 50.00 | CLST | 40.00 | SLCL | 5.00 | LMST | 5.00 | N | | | | 4840.0 | 4,760.00 | 0.00 | 225 | HORF | * | GA | 0 | GL | 0 | CLST | 98.00 | LMST | 2.00 | | | | | N | | | | 5065.0 | 4,985.00 | 0.00 | 855 | BELT | * | GL | 0 | * | 0 | CLST | 90.00 | LMST | 5.00 | SDST | 5.00 | | | N | | | | 5920.0 | 5,840.00 | 0.00 | 613 | HORF | * | GL | 0 | GY | 0 | CLST | 85.00 | TFCL | 10.00 | LMST | 5.00 | | | N | | | | 6533.0 | 6,453.00 | 0.00 | 59 | BALC | * | GY | 0 | GC | 0 | TFCL | 95.00 | LMST | 5.00 | | | | | N | | | | 6592.0 | 6,512.00 | 0.00 | 86 | BATF | * | GC | 0 | * | 0 | TFCL | 95.00 | LMST | 5.00 | | | | | N | | | | 6678.0 | 6,598.00 | 0.00 | 166 | SELE | * | GC | 0 | * | 0 | CLST | 98.00 | LMST | 2.00 | | | | | N | | | | 6844.0 | 6,764.00 | 0.00 | 14 | LIST | * | GC | 0 | * | 0 | SLST | 100.00 | | | | | | | N | | | | 6858.0 | 6,778.00 | 0.00 | 158 | FORT | * | GC | 0 | * | 0 | SDST | 65.00 | CLST | 35.00 | | | | | N | | OGS | | 7016.0 | 6,936.00 | 0.00 | 414 | ANDR | * | GC | 0 | * | 0 | SDST | 95.00 | CLST | 5.00 | | | | | N | | | | 7430.0 | 7,350.00 | 0.00 | 0 | * | * | * | 0 | * | 0 | | | | | | | | | N | | | TD DRILLER |
| | | | | | | | | | |
|