Deepwater Channel Systems in Turkey as a Comparative
Architectural Analogue for Sinuous Depositional
Channel Systems in High-Resolution
3-D Seismic
L. Faulkenberry1, B. Kneller2, J. Peakall1, and B. T. Cronin3
1University of Leeds, Dept. of
Earth Sciences, Leeds, UK
2University of California, Santa
Barbara, CA
3University of Aberdeen, Aberdeen, UK
Deepwater systems are important hydrocarbon targets for many
plays around the world. Tying the seismic architectural geometries
to those seen in outcrop is essential for understanding deepwater
channel evolution and reservoir potential. Of course, this comparison
is problematic due to both a lack of resolution
within seismic data
and a limited number of continuous outcrop exposures. Improvements
in seismic data quality have led to significant advances in imaging
the internal architectures of channel systems, especially in shallow
high-
resolution
3-dimensional seismic data, which contain the
highest frequencies and show the best preservation of depositional
geometries. Continuous outcrop exposures of the Tertiary Kirkgecit
and Lice Formations in Turkey have excellent potential for direct
mapping of contemporaneous channel and levee deposits at a seismic
and sub-seismic scale. Channel systems within these formations allow
for a more complete analysis of the temporal and spatial evolution
of channel axis and levee deposits. These channel systems
show promise as an architectural analog to near-surface sinuous depositional
channel systems seen in high-
resolution
seismic data.
AAPG Search and Discovery Article #90902©2001 AAPG Foundation Grants-in-Aid