Seismic
Facies Architecture of Canyon-Channel Complexes – Deepwater,
Offshore Mauritania
Caroline J. McKnoe1, Simon C. Lang2, and Tobias H.D.
Payenberg3
1 Woodside Energy Ltd, Perth, Australia
2 University of Adelaide, South Australia, Australia
3 Australian School of Petroleum,
University of Adelaide, Adelaide, Australia
High
resolution
depositional architecture within stacked submarine
canyon-channel complexes can be recognized from shallow 3D
seismic
surveys,
Offshore Mauritania. Detailed shallow
seismic
interpretations using
high-
resolution
data can aid in the characterization of potential similar
reservoirs in deeper sections, which are often accompanied by poorer data
resolution
. Depositional elements such as meandering channels, splays and
frontal splay complexes are identified using root mean squared (RMS) amplitude
extractions with
seismic
data. Reservoir prone elements include outer channel
bends and proximal regions of frontal and channel splays.
RMS amplitude extractions using 40 ms slices indicate that the channels
undergo minimal downward and lateral movement. This confines potential channel
reservoirs to within the channel belt of approximately twice the channel width.
Seismic
data indicate vertical aggradation of the channels, generally
accompanied by minimal lateral migration. Slope gradients of > 2º occur in
the middle slope with gradients < 2º along the outer shelf, upper and lower
slope regions. Varying
seismic
fill patterns are inferred to be linked to
changes in slope profile and accommodation space.
The canyons studied show narrow width:depth (W:D) ratios ranging from 5:1 to 39:1, generally increasing down-slope with shape changes from V to U-shaped. Internal channels show similar narrow W:D ratios and range from 5:1 to 25:1. Downstream and lateral migration of channels with time is minimal and is confined to within the channel belts. Channel belt widths range from 815 m to 1650 m with channel widths ranging from 400 m to 700 m, both increasing down-slope.
AAPG Search and Discovery Article #90039©2005 AAPG Calgary, Alberta, June 16-19, 2005