| | | | | | | | Well Registration Number | 16/08a- 12 | Interpretation | Composite | Date Coded | 12/02/1991 | Depth Units | Feet |
| | Datum | KB | Datum Elevation | 90.00 | 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 | 449.0 | 0.00 | 0.00 | 1611 | NOSG | NOSG | * | 0 | * | 0 | | | | | | | | | N | | | SEA BED | 2060.0 | 0.00 | 0.00 | 4030 | NOSG | NOSG | * | 0 | * | 0 | SILT | 75.00 | CLST | 22.00 | SAND | 3.00 | | | N | | | LOG BEGINS | 6090.0 | 0.00 | 0.00 | 210 | NOSG | NOSG | GA | 0 | GL | 0 | SILT | 100.00 | | | | | | | N | | | CHRONO START | 6300.0 | 0.00 | 0.00 | 130 | NOSG | NOSG | GE | 0 | GE | 0 | SILT | 100.00 | | | | | | | N | | | | 6430.0 | 0.00 | 0.00 | 190 | NOSG | NOSG | GY | 0 | GY | 0 | SILT | 100.00 | | | | | | | N | | | | 6620.0 | 6,526.00 | 0.00 | 150 | BALD | BALD | GY | 0 | GY | 0 | TFCL | 80.00 | SDST | 20.00 | | | | | N | | | | 6770.0 | 6,676.00 | 0.00 | 48 | ROGA | ROGA | GY | 0 | GY | 0 | TFCL | 60.00 | SDST | 40.00 | | | | | N | | | | 6818.0 | 6,724.00 | 0.00 | 52 | SELE | SELE | GY | 0 | GY | 0 | SILT | 100.00 | | | | | | | N | | | | 6870.0 | 6,776.00 | 0.00 | 300 | ROGS | ROGS | GY | 0 | GY | 0 | SDST | 95.00 | SILT | 5.00 | | | | | N | | | | 7170.0 | 0.00 | 0.00 | 40 | ROGS | ROGS | G | 0 | G | 0 | SDST | 70.00 | SILT | 30.00 | | | | | N | | | | 7210.0 | 0.00 | 0.00 | 32 | ROGS | ROGS | GC | 0 | GC | 0 | SDST | 100.00 | | | | | | | N | | | | 7242.0 | 7,148.00 | 0.00 | 213 | LIST | LIST | GC | 0 | GC | 0 | SILT | 80.00 | SDST | 20.00 | | | | | N | | | | 7455.0 | 7,360.00 | 0.00 | 665 | ANDR | ANDR | GC | 0 | GC | 0 | | | | | | | | | N | | | | 8120.0 | 8,025.00 | 0.00 | 0 | ANDR | ANDR | * | 0 | * | 0 | | | | | | | | | N | | | TD |
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