Factors Concerning the Development, Distribution and Preservation of
Reservoir
Facies in Jurassic Carbonates and their Impact on Petroleum Systems in
Eastern and Northeastern Saudi Arabia
By
A/Motaleb Al-Qahtani1, Alastair Gray2, Geir K Ytreland2
(1) Saudi Aramco, Dahran, Saudi Arabia (2) Saudi Aramco, Dahran 31311, Saudi Arabia
The Rimthan Arch is a positive feature, which existed from Bajocian until
Portlandian time separating the Gotnia and Arabian intra-shelf basins throughout
this period. This feature, whose lateral extent has varied considerably
throughout time, significantly controls development of Jurassic
reservoir
facies.
The distribution and
quality
of the most important carbonate reservoirs in the
Eastern Province of Saudi Arabia appear to be controlled by a
system
of positive
elements; tectonic and/or depositional highs. Water depth, energy and primary
depositional environment created and/or modified the sediments into
reservoir
rocks in the vicinity of these highs.
Analysis of petrography, paleontology, core description work, core
porosity/permeability analysis and integration with well logs and seismic
interpretation permit a reasonable description of the Upper Jurassic Arab
carbonate facies throughout the area, and are summarized into regional facies
and net pore volume maps. Similarly,
reservoir
distribution maps for the other
reservoir
units from this time are presented. An attempt is made to use sequence
stratigraphy and seismic stratigraphy to describe the systems, and to predict
facies variation as it pertains to the development of petroleum systems and
prediction
of various potential stratigraphic play types such as; dolomitization
as a sealing mechanism, facies variations, biohermal buildups and updip
reservoir
pinchouts. Recent reprocessing of seismic data indicates that such
facies variations may be seismically detectable.
Saudi Aramco oil typing work indicates a distinct separation of oil families into Gotnia and Northeastern Arabian Families and enhances the prospectivity of the Rimthan Arch trend.