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The AAPG/Datapages Combined Publications Database
AAPG Special Volumes
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The four fields under discussion are located in Kay County, Oklahoma. Certain general statements are applicable to all these fields: (1) the folds are all of the familiar "granite-ridge" type; (2) due to the absence of notable unconformities above the base of the Pennsylvanian, structure maps of the several key horizons within the Pennsylvanian and Permian are similar in the mathematical sense of the term; and (3) the production in all of these fields is associated with well-defined anticlines or domes.
In the detailed discussion, therefore, the principal emphasis is placed on the seeming anomalies, that is, those structures which are not ideal examples of anticlinal production.
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