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The AAPG/Datapages Combined Publications Database

Oklahoma City Geological Society

Abstract


The Shale Shaker Digest XII, Volumes XXXVI-XXXIX (1985-1989)
Pages 247-255

The Carter Anticline, Beckham and Washita Counties, Oklahoma

James D. Henry

ABSTRACT

The Carter anticline is a large, reverse-faulted structure on the Beckham-Washita county line just south of the giant Elk City Field in Western Oklahoma. The Carter anticline is a true anticline that occupies a structurally intermediate fault block along the highly deformed Wichita mountain front. Due to the timing of the growth of this structure and the migration of hydrocarbons through the Pennsylvanian granite wash, only the lower part of the Hoxbar (Missourian) section appears to be prospective. Porous and permeable beds in the lower Hoxbar are thin and tight over the crest of the anticline, thereby creating a stratigraphic trap along the north and west flanks. The southeast flank of the structure remains untested.


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