Oomoldic Reservoirs of Central Kansas, Controls on Porosity, Permeability, Capillary Pressure and Architecture |
Kansas Geological Survey Open-file Report 2002-48 |
Isopach map of the thickness of porous carbonate in the Bethany Falls Limestone exceeding 8% in Victory Field area showing areas of existing production. Thicker porous intervals of oolite occur in upper part of this regressive limestone closely conforming to the crestal areas of the present-day structure.
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Last updated March 2004
http://www.kgs.ku.edu/PRS/Poster/2002/2002-48/P1-10.html
3-D view of porosity distribution in the Bethany Falls Limestone in intervals exceeding 17% porosity constructed using Stratamodel. Warmer colors represent higher porosity. Model constructed using layers of equal thickness. High porosity layers pinch out updip.