1. Late Paleozoic magnetization of mineralized and unmineralized Ordovician carbonates from East Tennessee: evidence for a post-ore chemical event;Bachtadse;J. Geophys. Res.,1987
2. The Alleghanian orogeny and its relationship to the evolution of the eastern interior;Beaumont,1987
3. Revised and synthetic apparent polar wander paths of the African, Eurasian, North American and Indian plates, and true polar wander since 200 Ma;Besse;J. Geophys. Res.,1991
4. Structural control of ore bodies in the Jefferson City area, Tennessee;Brokaw;Econ. Geol.,1945
5. Churnet, H.G., 1979. The relationship between dolomitization and sphalerite mineralization in the Lower Ordovician Upper Knox carbonate rocks of the Copper Ridge district, East Tennessee. Unpublished PhD Dissertation, University of Tennessee, Knoxville, 236 pp.