Integrating 3-D Seismic Attributes
and Well
Logs for Mapping Bypassed Reservoir and Meandering Fluvial
Architecture, Stratton and Agua Dulce Fields, Texas Gulf Coast, USA
By
Hamed Zeidan El-Mowafy1, Dennis R. Kerr1, Christopher L. Liner1
(1) The University of Tulsa, Tulsa, OK
A study of the basal section of the Oligocene middle Frio Formation in
Stratton and Agua Dulce fields tests the effect of synthetic and antithetic
growth faults on the fluvial architecture. Gross- and net-sand thickness maps,
log
facies maps, and
well
-
log
cross-sections define channel belts. Correlation
analysis
confirms that seismic amplitude delineates the lateral extent of
channel-fill deposits. RMS amplitude anomaly maps of the F11 interval show that
meandering features relate to net pay and hydrocarbon pore volume thickness.
Bypassed reservoir is indicated from the 3D seismic mapping. This reservoir is a potential candidate for infield reserve growth in the northern Stratton area.
This area is dominated by the major Vicksburg and Agua Dulce growth faults,
along with several synthetic and antithetic faults. Seismic and well
log
analysis
show that subsidiary faults displace the stratigraphic units into
several discrete compartments and result in different stacking patterns of the
fluvial channel-fill deposits. The F11 reservoir unit is made up of several
meandering channel belts. A broad northwest-southeast valley-fill, up to 4300 ft
width, in the footwall block is controlled by the Agua Dulce fault at its
southern boundary. In the hanging wall block, a wide avulsion complex is made up
of east-west trending narrow meander channel-belts that are up to 1980 ft wide.
In the southern part of the field, broad northwest-southeast meander channel
belts are present in the hanging wall block. Post-depositional faulting along
crestal-collapse antithetic faults offset these channel belts.