| Mazarn Shale | |
|---|---|
| Stratigraphic range: Ordovician | |
| Type | Formation | 
| Unit of | none | 
| Sub-units | none | 
| Underlies | Blakely Sandstone | 
| Overlies | Crystal Mountain Sandstone | 
| Thickness | 1000 to 2500+ feet[1] | 
| Lithology | |
| Primary | Shale | 
| Location | |
| Region | Arkansas, Oklahoma | 
| Country | United States | 
| Type section | |
| Named for | Mazarn Creek, Montgomery County, Arkansas | 
| Named by | Hugh Dinsmore Miser[2] | 
The Mazarn Shale is an Early Ordovician geologic formation in the Ouachita Mountains of Arkansas and Oklahoma. This interval was first described in 1892,[3] but remained unnamed until 1918 as part of a study by U.S. Geological Survey geologist Hugh Dinsmore Miser.[2]
Paleofauna
Graptolites
- Caryocaris
- C. wrighti[4]
- Cryptograptus
- C. antennarius[4]
- Diplograptus[4]
- Glossograptus
- G. hystrix[4]
- Mesograptus[4]
- Phyllograptus
- P. typus[4]
- Retiograptus[4]
- Tetragraptus [5]
See also
References
- ↑ McFarland, John David (2004) [1998]. "Stratigraphic summary of Arkansas" (PDF). Arkansas Geological Commission Information Circular. 36: 18. Archived from the original (PDF) on 2016-12-21. Retrieved 2018-01-08.
- 1 2 Miser, H.D. (1918). "Manganese deposits of the Caddo Gap and De Queen quadrangles, Arkansas". U.S. Geological Survey Bulletin. 660-C: 68.
- ↑ Griswold, I.S. (1892). "Whetstones and the novaculites". Annual Report of the Geological Survey of Arkansas for 1890. 3.
- 1 2 3 4 5 6 7 8 9 10 11 12 13 14 15 16 17 18 19 Miser, Hugh D.; Purdue, A.H. (1929). "Geology of the De Queen and Caddo Gap quadrangles, Arkansas". U.S. Geological Survey Bulletin. 808: 27–28.
- 1 2 Pitt, William D.; Cohoon, Richard R.; Lee, Harry C.; Robb, Marion G; Watson, John (January 1961). "Ouachita Mountain core area, Montgomery County, Arkansas". Bulletin of the American Association of Petroleum Geologists. 45 (1): 79–80. Retrieved 8 January 2018.
    This article is issued from Wikipedia. The text is licensed under Creative Commons - Attribution - Sharealike. Additional terms may apply for the media files.