Sulfate minerals: their origin in the central kentucky karst
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Publication Date
January 1965
Abstract
Sulfate minerals, especially gypsum, are present in large quantities in most of the extensive limestone caves of the Mississippian plateaus and outliers of Central Kentucky. Many descriptions of these deposits have been published (Locke, 1842; Weller, 1927; Huff, 1940); however, the origin of the deposits has remained obscure.
Keywords
Carbonate, Rocks, Edmonson, County, Kentucky, Geochemistry, Gypsum, Ion, Exchange, Limestone, Mammoth Cave, Mineral Composition, Mineralogy, Origin, Processes, Sedimentary Rocks, Sulfates, United States, Gypsum Origin, Replacement Of Carbonate By Sulfate
Document Type
Article
Notes
American Mineralogist, Vol. 50, no. 9 (1965-01-01).
Identifier
SFS0069888_00001
Recommended Citation
Pohl, E. R. and White, William B., "Sulfate minerals: their origin in the central kentucky karst" (1965). KIP Articles. 5217.
https://digitalcommons.usf.edu/kip_articles/5217