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Knox Dolomite
Cambrian era geologic formation in Ohio, United States From Wikipedia, the free encyclopedia
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The Knox Dolomite is a geologic formation in Mississippi and Ohio. It dates back to the Cambrian.
 | This article includes a list of references, related reading, or external links, but its sources remain unclear because it lacks inline citations. (August 2024) |
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References
Further reading
- Baird, R. A.; Dennen, W. H. (1 May 1985). "A geochemical survey of the top of the Knox Dolomite; imlications for brine movement and mineralization in central Kentucky". Economic Geology. 80 (3): 688–695. doi:10.2113/gsecongeo.80.3.688.
- Dietrich, Richard V. (January 1953). "Hexagonal Chert Prisms from the Knox Dolomite". The Journal of Geology. 61 (1): 65–68. doi:10.1086/626037.
- Ogden, Albert E.; Ogden, Stephen C. (1997). EXPLORATORY DRILLING IN HIXSON, TENNESSEE DISCOVERS "NEW" AQUIFER OVERLYING THE KARSTIC KNOX DOLOMITE. KARST-WATER ENVIRONMENT SYMPOSIUM PROCEEDINGS.
- Riley, Ronald A.; Resources, Ohio Department of Natural; Survey, Division of Geological; Janssens, OHArie (1996). "CAMBRIAN-ORDOVICIAN KNOX PRODUCTION PATTERNS AND POTENTIAL FOR ENHANCED OIL RECOVERY IN OHIO". Ohio Geological Society-AAPG: 96–142.
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External links
 | This article about a specific stratigraphic formation in Ohio is a stub. You can help Wikipedia by expanding it. |
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