|  |  |  |  |  |  |  |  | Well Registration Number | 211/29-D22 |  | Interpretation | Composite |  | Date Coded | 03/11/1989 |  | Depth Units | Feet |  
  |  | | Datum | KB |  | Datum Elevation | 177.00 |  | 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 |  | 643.0 | 0.00 | 0.00 | 10057 | * | * | * | 0 | * | 0 |   |   |   |   |   |   |   |   | N |   |   | SEA BED |  | 10700.0 | 0.00 | 0.00 | 101 | HUMB | HUMB | * | 0 | * | 0 | SHAL | 100.00 |   |   |   |   |   |   | N |   |   | TOP OF LOG |  | 10801.0 | 8,695.00 | 0.00 | 73 | TARB | TARB | * | 0 | * | 0 | SDST | 95.00 | SHAL | 5.00 |   |   |   |   | N |   |   |   |  | 10874.0 | 8,747.00 | 0.00 | 410 | UNES | UNES | * | 0 | * | 0 | SDST | 65.00 | CLST | 30.00 | COAL | 5.00 |   |   | N |   |   |   |  | 11284.0 | 9,035.00 | 0.00 | 75 | MNSS | MNSS | * | 0 | * | 0 | CLST | 100.00 |   |   |   |   |   |   | N |   |   |   |  | 11359.0 | 9,087.00 | 0.00 | 274 | LNES | LNES | * | 0 | * | 0 | SDST | 55.00 | CLST | 45.00 |   |   |   |   | N |   |   |   |  | 11633.0 | 9,275.00 | 0.00 | 67 | ETIV | ETIV | * | 0 | * | 0 | SDST | 90.00 | CLST | 10.00 |   |   |   |   | N |   |   |   |  | 11700.0 | 9,319.00 | 0.00 | 262 | RANN | RANN | * | 0 | * | 0 | SDST | 65.00 | CLST | 35.00 |   |   |   |   | N |   |   |   |  | 11962.0 | 9,491.00 | 0.00 | 38 | DUNL | DUNL | * | 0 | * | 0 | CLST | 100.00 |   |   |   |   |   |   | N |   |   |   |  | 12000.0 | 0.00 | 0.00 | 254 | * | * | * | 0 | * | 0 |   |   |   |   |   |   |   |   | N |   |   | BASE OF LOG |  | 12254.0 | 9,678.00 | 0.00 | 0 | * | * | * | 0 | * | 0 |   |   |   |   |   |   |   |   | N |   |   | TD |  
  |  |  |   |  |  |  |  |  |  |  |  
  |