| | | | | | | | Well Registration Number | 211/18-A17 | Interpretation | Composite | Date Coded | 06/10/1989 | Depth Units | Feet |
| | Datum | KB | Datum Elevation | 147.50 | 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 | 12570.0 | 0.00 | 0.00 | 480 | | * | * | 0 | * | 0 | CLST | 100.00 | | | | | | | N | | | TOP OF LOG | 13050.0 | 8,678.00 | 0.00 | 85 | * | REDC | KL | 0 | KL | 0 | CLST | 100.00 | | | | | | | N | | | | 13135.0 | 8,728.00 | 0.00 | 68 | REDC | BASL | KL | 0 | KL | 0 | LMST | 60.00 | CLST | 40.00 | | | | | N | | | | 13203.0 | 8,767.00 | 0.00 | 343 | BASL | KIMM | JU | 0 | JU | 0 | CLST | 100.00 | | | | | | | N | | | | 13546.0 | 8,978.00 | 0.00 | 148 | KIMM | HEAT | JU | 0 | JU | 0 | CLST | 100.00 | | | | | | | N | | | | 13694.0 | 9,075.00 | 0.00 | 179 | HEAT | BRNT | JM | 0 | JM | 0 | SDST | 100.00 | | | | | | | N | | | D SAND | 13873.0 | 9,191.00 | 0.00 | 375 | BRNT | BRNT | JM | 0 | JM | 0 | SDST | 65.00 | CLST | 32.00 | COAL | 3.00 | | | N | | | C SAND | 14248.0 | 9,439.00 | 0.00 | 162 | BRNT | BRNT | JM | 0 | JM | 0 | SDST | 90.00 | CLST | 10.00 | | | | | N | | | B2 SAND | 14410.0 | 9,550.00 | 0.00 | 197 | BRNT | BRNT | JM | 0 | JM | 0 | SDST | 100.00 | | | | | | | N | | | B1 SAND | 14607.0 | 9,687.00 | 0.00 | 103 | BRNT | BRNT | JM | 0 | JM | 0 | SDST | 100.00 | | | | | | | N | | | A SAND | 14710.0 | 9,761.00 | 0.00 | 65 | BRNT | BRNT | JM | 0 | JM | 0 | CLST | 80.00 | SDST | 20.00 | | | | | N | | | BASAL UNIT | 14775.0 | 9,809.00 | 0.00 | 60 | BRNT | DUNL | JM | 0 | JM | 0 | CLST | 100.00 | | | | | | | N | | | | 14835.0 | 9,852.00 | 0.00 | 0 | DUNL | DUNL | JM | 0 | JM | 0 | | | | | | | | | N | | | TD DRILLER |
| | | | | | | | | | |
|