Caney Shale Mineral Rights

What Is the Caney Shale?

The Caney Shale is a Mississippian-age organic-rich shale and limestone interval in southern Oklahoma. It is stratigraphically equivalent to the Barnett Shale of Texas and the Woodford Shale of central Oklahoma, and sits in the depth window where the Cherokee Platform overlaps the northern Arkoma Basin — primarily across Hughes, Coal, Pittsburg, Atoka, Pontotoc, Carter, and Johnston counties.

The Caney was historically considered a source rock rather than a primary completion target, but improvements in slickwater fracture stimulation and lateral steering have made the Caney commercially viable as a horizontal target. The U.S. Department of Energy's National Energy Technology Laboratory (DOE/NETL) has used the Caney as a field laboratory for unconventional reservoir research, with multi-well science programs in southern Oklahoma generating publicly available reservoir characterization data.

Geology & Stacked Pay Context

Age: Late Mississippian (~330 million years)

Depth: Approximately 5,000–10,000 feet TVD across the producing trend

Lithology: Black organic-rich shale interbedded with siliceous limestone; high silica content improves fracability

Stacked relationships: Sits above the Woodford Shale and below the Sycamore in much of the producing area; many Caney horizontals are part of multi-zone development plans

Counties With Caney Shale Exposure

Hughes County — Cherokee Platform / Arkoma overlap; active Caney + Woodford development

Coal County — Caney within stacked Woodford / Hartshorne / Caney target sequence

Pittsburg County — Northern Arkoma Caney

Atoka County — Southern Arkoma; Caney in deep stacked sequence

Pontotoc, Carter, Johnston Counties — Southern Oklahoma Caney trend

Selling Caney Shale Mineral Rights

Buckhead provides a free written offer. Our offer comes at no cost and no obligation.