| Summary: |
The Schrader Bluff Oil Pool at Milne
Point was discovered in 1969 by the Socal Kavearak Pt.
32-25 well. The pool was initially delineated and
then developed by Conoco, Inc. through drilling programs
that began in 1989. Currently, more than 400 well
bores penetrate the pool. Regular production began during
March 1991, peaked at an average rate of 3,700 barrels
of oil per day (“bopd”) in October 1991, and declined to
an average of about 2,850 bopd (about 15% of MPU production)
by mid-1993. In early 1994, BP became operator of
the Milne Point Unit (“MPU”) and began an aggressive development
program. By June 1996, development drilling at E-Pad
and additional wells at H- and J-Pads caused production
to increase steadily until it reached 12,000 bopd in April
2002. During September 2002, BP’s extensive S-Pad
development began production, and Schrader Bluff production
immediately jumped to 20,000 bopd. Production from the
pool peaked at 23,922 bopd in October 2003, and it currently
averages about 20,650 bopd, or about 40% of current MPU
production. The Schrader Bluff Oil Pool is developed
on 10-acre spacing.
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| Geology: |
The Schrader
Bluff Oil Pool (“SBOP”) was originally defined in the Milne
Point Unit (“MPU”) A-1 well. However, a more typical and
representative section for the pool lies between 4,100
and 4,726 feet measured depth in MPU G-1. The pool
occurs within the Schrader Bluff Formation, which was deposited
in the Late Cretaceous (Maastrichitian). At Milne
Point, the Schrader Bluff is divided into two stratigraphic
intervals designated, from oldest to youngest, the "O-sands" and
the "N-sands.” The O-sands consist of very fine to fine-grained
sandstone interbedded with siltstone and mudstone that
were deposited under shallow marine conditions in the distal
portion of a delta. The overlying N-Sands were deposited
within a muddy marine shelf system. Mudstone and siltstone
dominate the lower portion of this interval, but the sediments
coarsen upward, becoming fine to medium grained sandstone
that dominates the upper part of the N-Sand interval. The
SBOP occurs within a homocline that dips 1 to 2 degrees
to the east-northeast, and lies between 3,400 and 5,200
feet true vertical feet below sea level. NW
and NE-trending faults compartmentalize the pool. Reservoir
intervals average 28% in porosity and 171 md in permeability. Total
estimated original oil n place ("OOIP") for the SBOP at Milne Point ranges from
1.25 to 2 billion barrels, with an estimated solution gas
in place of between 1.3 to 2.1 billion cubic feet. Within
the S-Pad area, the current OOIP estimate for both N and
O sands ranges from 247 to 363 million barrels.
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