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![]() 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.
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Last updated December 2001
http://www.kgs.ku.edu/PRS/publication/OFR2001-38/P1-07.html