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The AAPG/Datapages Combined Publications Database
AAPG Special Volumes
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The Southwest Lone Grove field, located about 14 miles southwest of Ardmore, was discovered in 1944. The field is located on the Wichita Mountains-Criner Hills anticlinorium, and is an example of a field whose existence is in part due to a normal fault which furnished one of the necessary components of the structural trap. Production is mainly from lenticular sandstones of Missouri and Des Moines age.
There is also included an electric log cross section from the Brock field of Carter County to the Southwest Lone Grove field, and a discussion of the correlation of the formations.
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