Stanley Shale | |
---|---|
Stratigraphic range: Mississippian | |
Type | Formation |
Unit of | none |
Sub-units | Hatton Tuff Lentil (AR/OK), Hot Springs Sandstone (AR) Member, [1] Chickasaw Creek Shale Formation (OK), Moyers Formation (OK), Tenmile Creek Formation(OK) [2] |
Underlies | Jackfork Sandstone |
Overlies | Arkansas Novaculite |
Thickness | 3,500 to 10,000+ feet [1] |
Lithology | |
Primary | Shale |
Location | |
Region | Arkansas, Oklahoma |
Country | United States |
Type section | |
Named for | Stanley, Pushmataha County, Oklahoma |
Named by | Joseph A. Taff [3] |
The Stanley Shale, or Stanley Group, is a Mississippian stratigraphic unit in the Ouachita Mountains of Arkansas and Oklahoma. First described in Arkansas in 1892, [4] this unit was not named until 1902 by J.A. Taff in his study of the Ouachita Mountains of Oklahoma. [3] Taff assigned the town of Stanley in Pushmataha County, Oklahoma as the type locality, but did not designate a stratotype. After introduction into Arkansas in 1909 by Albert Homer Purdue, [5] the unit was redefined in 1918, when the formation known as the Fork Mountain Slate was abandoned and partially combined into the Stanley Shale. [6] As of 2017, a reference section for the Stanley Shale has yet to be designated.
The Stanley Shale is recognized as a geologic formation with two sub-units in Arkansas, the Hatton Tuff Lentil and the Hot Springs Sandstone Member, [1] however, several others have been proposed. These include the Chickasaw Creek Member, [7] Chickasaw Creek Tuff, [8] Gap Ridge Sandstone Member, [9] Moyers Member, [7] Parker Hill Sandstone Member, [9] Polk County Ash Bed, [10] and Tenmile Creek Member. [7] In 1963, it was first proposed to raise the rank of the Stanley Shale Formation to Group status in Arkansas, [11] with proposed sub-units consisting of the Chickasaw Creek Formation, Moyers Formation (with the Gap Ridge Sandstone and Parker Hill Sandstone Members), and Ten Mile Creek Formation. [12] However, the proposal was not accepted and the unit remained as a formation.
In Oklahoma, this unit is recognized as a group called the Stanley Group composed of three formations: the Chickasaw Creek Shale Formation, the Moyers Formation, and the Tenmile Creek Formation. The Hatton Tuff Lentil, recognized in Arkansas, is also in Oklahoma as a unit of the Tenmile Creek Formation. Several informal members have been noted including the Smithville chert lentil, the Faith chert member, and the Chickasaw Creek tuff among others [2]
Mining in the Stanley Shale is limited to cinnabar, barite, and quartz. Cinnabar is primarily used for mercury, however, production in Arkansas essentially ended by the mid-20th century. Barite mining, mostly useful for oil and gas drilling fluid, is ongoing. [13]