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The AAPG/Datapages Combined Publications Database
Tulsa Geological Society
Abstract
Explore the Published Strike-Slip Faults: Abstract
Abstract
Reverse faulting near the edge of a stratigraphic boundary can create a false image of a strike-slip fault
. The Washita Valley
fault
might be an excellent example of such a
fault
. If, in fact, the Washita Valley
fault
is a reverse
fault
and not a strike-slip
fault
, then the Arbuckle Mountains may overlie some unexplored oil and gas prospects.
The Washita Valley fault
is adjacent to two of the most prolific fields in southern Oklahoma: The Eola field and the Cumberland field. These two fields have each produced approximately 850,000 barrels of oil per well. The fields are approximately 70 miles apart, and may be indicative of a structural trend that has not yet been fully explored.
One way to determine the difference between a reverse fault
and a strike-slip
fault
is to examine the direction of force that produced the
fault
. The force that creates a strike-slip
fault
is 90 degrees opposite in direction from a force that will create a reverse
fault
. A study of the Washita Valley
fault
strongly supports the reverse
fault
concept.
Acknowledgments and Associated Footnotes
1 The Daube Co, Ardmore, OK
Copyright © 2006 by the Tulsa Geological Society