Cason Shale
The Cason Shale is a Late Ordovician to Middle Silurian geologic formation in the Ozark Plateaus of Arkansas.[1] The name was introduced in 1894 by Henry Shaler Williams in his study of Arkansas.[2] Williams designated a type locality at what was known as the Cason tract and mine, near Batesville, Independence County, Arkansas, however, he did not assign a stratotype. As of 2017, a reference section has not been designated for this unit.
Cason Shale Stratigraphic range: Ordovician-Silurian | |
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Type | Formation |
Unit of | none |
Underlies | Brassfield Limestone |
Overlies | Fernvale Limestone |
Thickness | up to appx. 23 feet[1] |
Lithology | |
Primary | Shale |
Location | |
Region | Arkansas |
Country | United States |
Type section | |
Named for | Cason tract and mine, near Batesville, Independence County, Arkansas |
Named by | Henry Shaler Williams[2] |
Paleofauna
Conodonts
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References
- McFarland, John David (2004) [1998]. "Stratigraphic summary of Arkansas" (PDF). Arkansas Geological Commission Information Circular. 36: 7. Archived from the original (PDF) on 2016-12-21. Retrieved 2018-01-11.
- Williams, Henry S. (1894). "On the age of the manganese beds of the Batesville region of Arkansas". The American Journal of Science. 3rd Series. 48: 325–331.
- Craig, William (1968). The stratigraphy and conodont paleontology of Ordovician and Silurian strata, Batesville district, Independence and Izard counties, Arkansas (PhD). The University of Texas.
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