Detalles del proyecto
Description
Integrated studies of overlapping critical mineral systems in South Central Kentucky and North Central
Tennessee
Abbreviated: EMRI KY-TN 2023
Abstract
The South-Central Kentucky and North-Central Tennessee mineral districts are situated in the
Cumberland Saddle region of the Cincinnati Arch that separates the Illinois and Appalachian Basins.
These mineral districts host deposits of sphalerite, galena, fluorite, and barite related to Mississippi
Valley Type (MVT) (basin brine path) mineralization within units of the Lower Ordovician upper Knox
Group. In addition to the MVT mineralization, Ordovician and Devonian sedimentary rocks that crop out
across the districts are permissive for mineral commodities related to marine chemocline systems. The
objectives of this project are two-fold: (i) generate geological maps and cross sections with emphasis on
the most important factors on the mineral systems, and (ii) collect geochemical data to characterize the
mineralizing fluids and identify the source of the metals and other ore components critical to the
formation of these deposits. The final deliverables of this project are maps, geologic cross sections
through relevant Devonian and Ordovician units, and a peer-reviewed publication integrating the
geochemical and mapping results which will serve as the final report for the project.
| Estado | Activo |
|---|---|
| Fecha de inicio/Fecha fin | 1/23/23 → 1/22/26 |
Financiación
- US Geological Survey: 288.750,00 US$
Huella digital
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