About This Item

Share This Item

The AAPG/Datapages Combined Publications Database

Oklahoma City Geological Society

Abstract


The Shale Shaker Digest XII, Volumes XXXVI-XXXIX (1985-1989)
Pages 52-55

Doyle Field Sycamore Pool

Robert R. Crifasi

ABSTRACT

Doyle Field is located in the Southern Oklahoma fold belt, in Stephens County, Oklahoma. The Sycamore Formation is a deeper pool objective whose development began with the completion of the Texaco Inc. Hattie Harrell C-1 well in 1981. Gas and condensate are produced from the Sycamore Formation. The Sycamore Formation is a calcareous sandstone in this area. Doyle Field is a highly faulted anticline that developed primarily in Pennsylvanian time. Several phases of transpressional motion summed to form the Doyle Field structure, which is interpreted here to be a good example of a flower structure.


Pay-Per-View Purchase Options

The article is available through a document delivery service. Explain these Purchase Options.

Watermarked PDF Document: $14
Open PDF Document: $24