By PARKER GAY |
GEOPHYSICAL CORNERMaps: It's the Basements Fault |
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Figure 1 next | main articleCollier Flats Field, Comanche County, Kansas -- production is from an oolite shoal that evidently developed on a fault scarp over an underlying basement fault defined by the gradient in the residual magnetic contours (blue). Structure contours (red) are on top of Pennsylvanian Swope limestone.
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