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The AAPG/Datapages Combined Publications Database
Oklahoma City Geological Society
Abstract
Genetic Study of the Northwest Butterly Field Garvin County Oklahoma
ABSTRACT
The NW Butterly Field is on the north side of the Arbuckle Mountains. A major angular unconformity separates the Lower Paleozoic section from Pennsylvanian and Permian rocks. Interbedded and lenticular sandstones, conglomerates, shales and limestones form the Deese and Hoxbar Groups. The NW Butterly Field produces from the lower second Tuley sandstone of Missourian age. This sandstone was deposited as a shallow submarine sand body, and varies in thickness and porosity. The lobar shape of a thick, porous section of this sandstone creates a stratigraphic trap near its updip termination. Oil and gas have migrated along the sandstone and accumulated in the NW Butterly Field.
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