| | | | | | | | | Well Registration Number | 9/23a- 28 | | Interpretation | Composite | | Date Coded | 08/04/1997 | | Depth Units | Feet |
| | | Datum | KB | | Datum Elevation | 80.00 | | 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 | | 452.0 | 372.00 | 153.00 | 1727 | * | | QH | 0 | GN | 0 | SAND | 70.00 | CLST | 30.00 | | | | | N | | | SEABED | | 2179.0 | 2,099.00 | 692.00 | 781 | GOCL | | GO | 0 | | 0 | SLST | 80.00 | CLST | 10.00 | SDST | 10.00 | | | N | | | | | 2960.0 | | | 130 | GOCL | | GO | 0 | | 0 | SLST | 80.00 | CLST | 20.00 | | | | | N | | | FIRST RETURN | | 3090.0 | 3,010.00 | 971.00 | 673 | GRID | | GO | 0 | | 0 | SDST | 80.00 | CLST | 10.00 | SLST | 10.00 | | | N | | | | | 3763.0 | 3,683.00 | | 1365 | HORF | | GE | 0 | | 0 | SLST | 80.00 | CLST | 15.00 | SDST | 4.00 | LMST | 1.00 | N | | | | | 5128.0 | 5,048.00 | 1,527.00 | 338 | UPFR | | GE | 0 | | 0 | SLST | 60.00 | CLST | 30.00 | SDST | 9.00 | LMST | 1.00 | N | | | UPFR EQUIV | | 5466.0 | 5,380.00 | 1,615.00 | 184 | BLDU | | GP | 0 | | 0 | CLST | 85.00 | SLST | 10.00 | SDST | 4.00 | LMST | 1.00 | N | | | | | 5650.0 | 5,570.00 | 1,665.00 | 140 | BLDM | | GP | 0 | | 0 | SLST | 35.00 | CLST | 35.00 | SDST | 30.00 | | | N | | OS | | | 5790.0 | 5,710.00 | 1,701.00 | 107 | BLDL | | GP | 0 | | 0 | SDST | 40.00 | TUFF | 25.00 | CLST | 25.00 | SLST | 10.00 | N | | OS | CORED | | 5897.0 | 5,817.00 | 1,726.00 | 403 | SELE | | GP | 0 | | 0 | CLST | 60.00 | SLST | 25.00 | SDST | 10.00 | TUFF | 5.00 | N | | | | | 6300.0 | 6,220.00 | 1,820.00 | 124 | LIST | | GP | 0 | | 0 | SLST | 35.00 | CLST | 35.00 | SDST | 30.00 | | | N | | | | | 6424.0 | 6,344.00 | 1,848.00 | 0 | LIST | | * | 0 | | 0 | | | | | | | | | N | | | |
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