| | | | | | | | Well Registration Number | 211/23-A41 | Interpretation | Composite | Date Coded | 30/10/1989 | Depth Units | Feet |
| | Datum | KB | Datum Elevation | 160.00 | 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 | 655.0 | 0.00 | 0.00 | 15245 | * | * | * | 0 | * | 0 | | | | | | | | | N | | | SEA BED | 15900.0 | 0.00 | 0.00 | 32 | CRKN | CRKN | K | 0 | K | 0 | MARL | 100.00 | | | | | | | N | | | TOP OF LOG | 15932.0 | 8,894.00 | 0.00 | 198 | KIMM | KIMM | J | 0 | J | 0 | CLST | 100.00 | | | | | | | N | U | | | 16130.0 | 9,060.00 | 0.00 | 251 | HEAT | HEAT | J | 0 | J | 0 | CLST | 95.00 | LMST | 5.00 | | | | | N | | | | 16381.0 | 9,279.00 | 0.00 | 115 | TARB | TARB | J | 0 | J | 0 | SDST | 80.00 | SLST | 15.00 | COAL | 5.00 | | | N | | | | 16496.0 | 9,382.00 | 0.00 | 176 | UNES | UNES | J | 0 | J | 0 | SDST | 65.00 | SLST | 35.00 | | | | | N | | | | 16672.0 | 9,543.00 | 0.00 | 48 | MNSS | MNSS | J | 0 | J | 0 | CLST | 100.00 | | | | | | | N | | | | 16720.0 | 9,588.00 | 0.00 | 17 | LNES | LNES | J | 0 | J | 0 | CLST | 60.00 | SDST | 40.00 | | | | | N | | | | 16737.0 | 9,604.00 | 0.00 | 108 | ETIV | ETIV | J | 0 | J | 0 | SDST | 90.00 | CLST | 10.00 | | | | | N | | | | 16845.0 | 9,705.00 | 0.00 | 160 | RANN | RANN | J | 0 | J | 0 | SDST | 80.00 | CLST | 20.00 | | | | | N | | | | 17005.0 | 9,857.00 | 0.00 | 51 | BROM | BROM | J | 0 | J | 0 | SDST | 85.00 | SLST | 15.00 | | | | | N | | | | 17056.0 | 9,905.00 | 0.00 | 94 | DRKE | DRKE | J | 0 | J | 0 | CLST | 100.00 | | | | | | | N | | | | 17150.0 | 0.00 | 0.00 | 57 | DRKE | DRKE | J | 0 | J | 0 | | | | | | | | | N | | | BASE OF LOG | 17207.0 | 10,049.00 | 0.00 | 0 | DRKE | DRKE | J | 0 | J | 0 | | | | | | | | | N | | | TD |
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