Abstract
The producing zones of the Hugoton gas area are correlated with the (lower Sumner) and the and limestone (Chase group) of Permian age of central Kansas. Between the Hugoton area and the Texas Panhandle gas and oil fields, the top of the Wellington anhydrite (upper Sumner) is correlated with the top of the Texas Panhandle Big lime, the top of the Herington (lower Sumner) is correlated with the Brown dolomite of the Panhandle Big lime. (Based on the chert in the Herington formation, this is encountered from 30 to 50 feet below the top of the Brown dolomite of the Panhandle Big lime.) The top of the Winfield limestone (Chase group) is correlated with the White dolomite of the Panhandle Big lime.
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