| | | | | | | | Well Registration Number | 49/16-Q2Z | Interpretation | Composite | Date Coded | 19/01/1989 | Depth Units | Feet |
| | Datum | KB | Datum Elevation | 141.00 | 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 | 236.0 | 95.00 | 0.00 | 9464 | | | * | 0 | * | 0 | | | | | | | | | N | | | NO RETURNS | 9700.0 | 0.00 | 0.00 | 631 | RGTN | RGTN | T | 0 | T | 0 | | | | | | | | | N | | | | 10331.0 | 6,917.00 | 0.00 | 161 | BRCK | BRCK | T | 0 | T | 0 | | | | | | | | | N | | | | 10492.0 | 7,028.00 | 0.00 | 52 | AHLT | AHLT | PU | 0 | PU | 0 | | | | | | | | | N | | | | 10544.0 | 7,062.00 | 0.00 | 13 | RSTZ | RSTZ | PU | 0 | PU | 0 | | | | | | | | | N | | | | 10557.0 | 7,072.00 | 0.00 | 259 | LHLT | LHLT | PU | 0 | PU | 0 | | | | | | | | | N | | | | 10816.0 | 7,243.00 | 0.00 | 35 | HPHY | HPHY | PU | 0 | PU | 0 | | | | | | | | | N | | | | 10851.0 | 7,266.00 | 0.00 | 510 | PLDT | PLDT | PU | 0 | PU | 0 | | | | | | | | | N | | | | 11361.0 | 7,594.00 | 0.00 | 8 | GSTZ | GSTZ | PU | 0 | PU | 0 | | | | | | | | | N | | | | 11369.0 | 7,599.00 | 0.00 | 17 | DKHY | DKHY | PU | 0 | PU | 0 | | | | | | | | | N | | | | 11386.0 | 7,609.00 | 0.00 | 482 | STHY | STHY | PU | 0 | PU | 0 | | | | | | | | | N | | | | 11868.0 | 7,913.00 | 0.00 | 389 | WHAN | WHAN | PU | 0 | PU | 0 | | | | | | | | | N | | | | 12257.0 | 8,152.00 | 0.00 | 268 | WHLT | WHLT | PU | 0 | PU | 0 | | | | | | | | | N | | | | 12525.0 | 8,310.00 | 0.00 | 112 | LMNS | LMNS | PL | 0 | PL | 0 | | | | | | | | | N | F | GPW | | 12637.0 | 8,376.00 | 0.00 | 121 | UNDF | UNDF | C | 0 | C | 0 | | | | | | | | | N | | | | 12758.0 | 8,447.00 | 0.00 | 0 | UNDF | UNDF | * | 0 | * | 0 | | | | | | | | | N | | | |
| | | | | | | | | | |
|