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Kansas Geological Survey, Open-file Report 2004-65
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Figure 9. Modeled variation in amplitude of the base of the Warsaw Limestone horizon due to increase in porosity of Judica zone.

Velocity model has layers of alternating porosity values above and below Judica zone; 
synthetic seismic section changes as porosity drops from 25% to 5%.

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Kansas Geological Survey, Energy Research
Placed online June 6, 2005
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