Field Development and Renewed Reservoir Characterization for CO2 Flooding of the Hall-Gurney Field, Central Kansas

Kansas Geological Survey
Open-file Report 2001-38

Structure contour map depicts the current structural variation in a eighty square mile area (ten miles wide by eight miles tall) covering the main portion of the Hall-Gurney Field. The structure on the Lansing reflects that of the L-KC "C" zone and is a result of drape over a strong pre-Pennsylvanian structure. Pre-Pennsylvanian strata was stripped away exposing the Precambrian over much of the apex of the field.

top of report

e-mail :
Last updated December 2001