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Location: 130 km W from Nashville, Tennessee, United States
279 West Main StreetCamdenUnited StatesTN 38320
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The Titan Project’s location in western Tennessee represents the eastern flank of the Mississippi Embayment, a large, southward plunging syncline within the Gulf Coastal Plain. This feature extends from southern Illinois to the north and to Mississippi and Alabama to the south. The embayment is filled with sediments and sedimentary rocks of Cretaceous to Quaternary age. The McNairy Sand Formation represents a pro-grading deltaic environment during a regressive marine sequence. This is evidenced by the coarsening upward sequence grading from the glauconitic clay rich Coon Creek Formation to the fine lower member of the McNairy Formation to the coarser upper member of the McNairy Formation. The main mineralized zone at the Project is hosted stratigraphically in the lower member of the McNairy Formation, the McNairy Formation dips gently into the west in the Project area. Mineralization averages 31 meters thick and has been traced, to date, for 6.2 kilometers along strike. The upper zone is also mineralized in some areas.
