| | | | | | | | | Well Registration Number | 22/04- 1 | | Interpretation | Composite | | Date Coded | 12/10/1989 | | Depth Units | Feet |
| | | Datum | KB | | Datum Elevation | 82.00 | | 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 | | 380.0 | 0.00 | 0.00 | 7570 | UNDF | UNDF | * | 0 | GA | 0 | CLST | 96.00 | SLST | 3.00 | SDST | 1.00 | | | N | | | SEABED | | 7950.0 | 7,868.00 | 0.00 | 310 | * | * | GL | 0 | GL | 0 | CLST | 100.00 | | | | | | | N | | | | | 8260.0 | 8,178.00 | 0.00 | 23 | * | * | GL | 0 | GL | 0 | SDST | 100.00 | | | | | | | N | | OS | | | 8283.0 | 8,201.00 | 0.00 | 208 | * | * | GL | 0 | GL | 0 | CLST | 99.00 | DOLO | 1.00 | | | | | N | | | | | 8491.0 | 8,409.00 | 0.00 | 259 | * | * | GY | 0 | GY | 0 | CLST | 100.00 | | | | | | | N | | | | | 8750.0 | 8,668.00 | 0.00 | 120 | BALD | BALD | GC | 0 | GC | 0 | CLST | 60.00 | TFCL | 40.00 | | | | | N | | | | | 8870.0 | 8,788.00 | 0.00 | 178 | SELE | SELE | GC | 0 | GC | 0 | CLST | 100.00 | | | | | | | N | | | | | 9048.0 | 8,966.00 | 0.00 | 202 | LIST | LIST | GC | 0 | GC | 0 | CLST | 90.00 | SLST | 10.00 | | | | | N | | | | | 9250.0 | 9,168.00 | 0.00 | 100 | ANDR | ANDR | GC | 0 | GC | 0 | SDST | 55.00 | CLST | 45.00 | | | | | N | | | | | 9350.0 | 9,268.00 | 0.00 | 250 | MAUR | MAUR | GC | 0 | GC | 0 | SDST | 70.00 | SLST | 20.00 | CLST | 10.00 | | | N | | | | | 9600.0 | 9,520.00 | 0.00 | 288 | MAUR | MAUR | GF | 0 | GF | 0 | LMST | 80.00 | SDST | 15.00 | CLST | 5.00 | | | N | | | | | 9888.0 | 9,806.00 | 0.00 | 212 | EKOF | EKOF | GF | 0 | GF | 0 | LMST | 60.00 | MARL | 40.00 | | | | | N | | | | | 10100.0 | 10,018.00 | 0.00 | 0 | TORF | TORF | KU | 0 | KU | 0 | LMST | 100.00 | | | | | | | N | | | |
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