| AOGCC Pool Statistics | Prudhoe Bay Unit, PM Stump Island |
|
| Operator: | BP Exploration (Alaska) Inc. | |
| Discovery Well: | Arco / Exxon | ||
| Point McIntyre No. 3 | |||
| Permit #189-003 | |||
| API No. 50-029-21779-90-00 | |||
| Sec. 15, T12N, R14E, UM | |||
|
| Depth: 11,035' MD / 10,483' TVD | ||
|
| March 22, 1988 |
| Status: | Plugged and Abandoned | ||||
| Location: | Central Arctic Slope | Area Location Map | DNR Unit Map | ||
| Orders: | Complete List | ||||
| Summary: |
Discovered in 1993, the Stump Island
Oil Pool lies within the Cretaceous-aged Seabee Formation
in the northernmost portion of the Prudhoe Bay Unit. This
pool is defined as the accumulation of hydrocarbons common
to and which correlates with the interval from 8,759' to
8,930' measured depth in the Pt. McIntyre No. 3 well. It
overlies the gas cap and oil column in the Kuparuk and
Kalubik Formations that comprise the Pt. McIntyre Oil Pool.
The Stump Island Oil Pool is separated from the Pt. McIntyre
Oil Pool by a series of Cretaceous marine shales that range
from approximately fifty to more than two hundred feet
thick.
Oil within the Stump Island reservoir is stratigraphically trapped in discontinuous sandstones of limited areal extent within the Seabee Formation. Only the Pt. McIntyre No. 3 well proved capable of hydrocarbon production from the Stump Island reservoir, and it is thought to be an isolated occurrence. Insufficient subsurface data currently exists to accurately characterize the Stump Island reservoir or estimate the total volume of hydrocarbons in place, but the reserves are believed to be minor in relation to those of the Pt. McIntyre Oil Pool.
|
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| Strat Column | |||||
| Orig. Oil in Place: | Not published |
| Production: | None |
| Oil (bbls) | NGL (bbls) | Gas (mcf) | Water (bbls) | |
| Cumulative | 0 |
0 | 0 | 0 |
| 2001 Total | 0 | 0 | 0 | 0 |
| 2002 Total | 0 | 0 | 0 | 0 |
| 2003 Total | 0 | 0 | 0 | 0 |
| 2004 Total | 0 | 0 | 0 | 0 |
| 2003 Daily Rate | 0 | 0 | 0 | 0 |
| 2004 Daily Rate | 0 | 0 | 0 | 0 |
| Change (%) | 0 | 0 | 0 | 0 |
