| | | | | | | | Well Registration Number | 15/17-B10 | Interpretation | Composite | Date Coded | 26/02/2001 | Depth Units | Feet |
| | Datum | KB | Datum Elevation | 206.70 | 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 | 682.0 | | | 818 | NORD | | QH | 0 | GN | 0 | | | | | | | | | Y | | | SEABED | 1500.0 | 1,290.00 | | 493 | HORD | | QH | 0 | GN | 0 | | | | | | | | | Y | | | | 1993.0 | 1,776.00 | | 53 | GLAS | | QH | 0 | GN | 0 | | | | | | | | | Y | | | | 2046.0 | 1,826.00 | | 1677 | HORF | | QH | 0 | GN | 0 | | | | | | | | | Y | | | BASE GLAS | 3723.0 | 3,220.00 | | 384 | BALD | | QH | 0 | GN | 0 | | | | | | | | | Y | | | | 4107.0 | 3,458.00 | | 88 | BEAU | | QH | 0 | GN | 0 | | | | | | | | | Y | | | | 4195.0 | 3,500.00 | | 170 | DORN | | QH | 0 | GN | 0 | | | | | | | | | Y | | | | 4365.0 | 3,605.00 | | 995 | SELE | | QH | 0 | GN | 0 | | | | | | | | | Y | | | | 5360.0 | | | 1070 | SELE | | QH | 0 | GN | 0 | SAND | 83.00 | CLST | 15.00 | LMST | 1.00 | LIGN | 1.00 | Y | | | FIRST RETURNS | 6430.0 | 4,720.00 | | 862 | LIST | | QH | 0 | GN | 0 | CLST | 82.00 | TFCL | 15.00 | SAND | 2.00 | LMST | 1.00 | Y | | GS | | 7292.0 | 5,217.00 | | 528 | BMOR | | QH | 0 | GN | 0 | SAND | 48.00 | CLST | 29.00 | SDST | 16.00 | TFCL | 7.00 | Y | | GS | | 7820.0 | 5,521.00 | | 1630 | LIAN | | QH | 0 | GN | 0 | SAND | 52.00 | SDST | 36.00 | SLCL | 11.00 | LMST | 1.00 | Y | | | | 9450.0 | 6,456.00 | | 447 | MAUR | | QH | 0 | GN | 0 | SDST | 95.00 | CLST | 4.00 | LMST | 1.00 | | | Y | | | MAUR? | 9897.0 | 6,715.00 | | 177 | MACH | | QH | 0 | GN | 0 | CKLS | 44.00 | SDST | 39.00 | ARLM | 11.00 | CLCL | 6.00 | Y | | | | 10074.0 | 6,817.00 | | 137 | EKOF | | QH | 0 | GN | 0 | LMST | 40.00 | ARLM | 40.00 | CLCL | 12.00 | MARL | 8.00 | Y | | | | 10211.0 | 6,894.00 | | 1030 | TORF | | KU | 0 | | 0 | LMST | 39.00 | CKLS | 30.00 | ARLM | 30.00 | MARL | 1.00 | Y | | | | 11241.0 | 7,519.00 | | 404 | FLND | | KC | 0 | KO | 0 | MARL | 99.00 | LMST | 1.00 | | | | | Y | | | | 11645.0 | 7,789.00 | | 90 | HERR | | KT | 0 | | 0 | MARL | 98.00 | LMST | 2.00 | | | | | Y | | | | 11735.0 | 7,847.00 | | 169 | VALH | | KA | 0 | JV | 0 | MARL | 82.00 | CLCL | 18.00 | | | | | Y | U | | | 11904.0 | 7,947.00 | | 242 | KIMM | | KZ | 0 | JV | 0 | SLST | 52.00 | CLST | 46.00 | SLCL | 2.00 | | | Y | U | | | 12146.0 | 8,081.00 | | 62 | PDSD | | JD | 0 | | 0 | SDST | 100.00 | | | | | | | Y | U | OS | CORED | 12208.0 | | | 15 | PDSH | | JD | 0 | | 0 | CLST | 95.00 | SLCL | 2.00 | SACL | 2.00 | | | Y | | | CORED | 12223.0 | | | 46 | PESD | | JD | 0 | | 0 | SDST | 50.00 | ARSS | 50.00 | | | | | Y | | OS | CORED | 12269.0 | | | 11 | PESH | | JD | 0 | JO | 0 | CLST | 97.00 | SACL | 3.00 | | | | | Y | | | CORED | 12280.0 | | | 9 | PF1S | | JD | 0 | JO | 0 | SDST | 95.00 | ARSS | 5.00 | | | | | Y | | OS | CORED | 12289.0 | | | 38 | PF2S | | JD | 0 | JO | 0 | SDST | 95.00 | ARSS | 5.00 | | | | | Y | | OS | CORED | 12327.0 | | | 96 | PG1S | | JD | 0 | JO | 0 | SDST | 90.00 | ARSS | 10.00 | | | | | Y | | OS | CORED | 12423.0 | | | 137 | PHSD | | JD | 0 | JO | 0 | SDST | 78.00 | ARSS | 22.00 | | | | | Y | | OS | | 12560.0 | 8,302.00 | | 53 | PIPI | | JD | 0 | JO | 0 | CLST | 50.00 | SLCL | 50.00 | | | | | Y | | | BASE PIPER SST | 12613.0 | 8,331.00 | | 10 | SGIJ | | JO | 0 | | 0 | TFSS | 100.00 | | | | | | | Y | | OS | | 12623.0 | | | 24 | SGIL | | JO | 0 | | 0 | TFSS | 100.00 | | | | | | | Y | | OS | | 12647.0 | | | 17 | SMSH | | JO | 0 | | 0 | SLCL | 100.00 | | | | | | | Y | | | | 12664.0 | | | 17 | SM2S | | JO | 0 | | 0 | TFSS | 100.00 | | | | | | | Y | | OS | | 12681.0 | 8,368.00 | | 774 | RATT | | JM | 0 | | 0 | TFCL | 90.00 | VOLC | 10.00 | | | | | Y | | | | 13455.0 | 8,824.00 | | 0 | RATT | | * | 0 | | 0 | | | | | | | | | Y | | | |
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