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AAPG
2001 Presentations
3-D Seismic Expression of High-Frequency Sequence Stratigraphy in Vermilion Block 50-Tiger Shoal Area, Offshore Louisiana Zeng, Hongliu, Hentz, Tucker F., and Wood, Lesli J. Bureau of Economic Geology, The University of Texas at Austin, Austin, TX Extracting high-resolution information from
limited bandwidth seismic data is a major challenge when using seismic
to extend well-based high-frequency sequence stratigraphy to a 3-D area.
Critical to such extension is the recognition and interpretation of a
geobody's plano-form. Emphasis should be shifted from interpreting vertical
seismic data to developing new tools capable of extracting more horizontal,
seismic sedimentologic information. This case study shows that proportionally,
stratal slicing between flooding surfaces provides sequential and accurate
seismic imagery of depositional systems, which in turn serves as a basis
for recognizing and mapping high-frequency (fourth-order) systems tracts,
sequence boundaries, and sequences in geologic time domain. This example
illustrates why stratal slices are generally better than time slices and
horizon slices in interpreting depositional morphology. In a 1-s-traveltime
interval, most of the 31 fourth-order sequences from wells in the study
can be seismically mapped at a resolution equivalent to 10 m in depth.
An easy-to-follow procedure to visualize a fourth-order sequence by using
stratal slices includes five steps:
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