Summary
The Najmah, Sargelu, and Marrat reservoirs are the main Jurassic reservoirs
in Kuwait. These fractured-carbonate reservoirs that have moderate-to-low
porosity were deposited in an inner- to midramp warm marine environment. The
fracture systems play a significant role in production in these reservoirs, and
it is essential to identify areas of high fracture density. It has been
observed that fractures associated with certain faults have facilitated the
flow in the Jurassic reservoirs. Identification of faults and associated
fractures mainly has been on the basis of 3D-/2D-seismic data, image logs,
cores, and thin sections.
The Greater Burgan field consists of the Burgan, Magwa, and Ahmadi
structures. The four main reservoir units in the Greater Burgan field are the
Wara, Mauddud, Burgan Third, and Burgan Fourth sands. The deeper
reservoirs--namely, the Lower Cretaceous Ratawi and Minagish limestone--and the
Jurassic Marrat formation contain significant oil reserves but are of less
importance. However, a recent successful exploratory well in the Arifjan
prospect, which is located on the eastern flank of the Greater Burgan field,
has opened up a large area that was previously considered to be nonproductive.
It has been noticed that there is excellent correlation between the fractures
observed in cores and image logs and those predicted from the converted
component of the zero-offset vertical seismic profile (VSP). After registration
of the z-component image with the converted image for various prominent
reflectors, the discontinuities in the reflectors in the converted-component
image revealed fracture swarms that could be traced away from the wellbore.
This technique of processing the VSP data to identify fracture clusters
could form a bridge between surface and borehole data and improve confidence in
predicting fracture swarms away from the wellbore and also assist in planning
of future surface seismic and 3D VSP surveys.
© 2009. Society of Petroleum Engineers
View full textPDF
(
4,041 KB
)
History
- Original manuscript received:
2 December 2006
- Meeting paper published:
11 March 2007
- Revised manuscript received:
14 September 2008
- Manuscript approved:
11 January 2009
- Published online:
1 June 2009
- Version of record:
1 June 2009