The SWA Property is being assessed by Standard Lithium for its lithium-brine potential. The brine is situated within an aquifer associated with the Late Jurassic Smackover Formation, which has produced hydrocarbons since the 1940s on the Property and brine to the east of the Property since the late 1950s. Hyper-saline brine (total dissolved solids of 293,000 to 448,000 mg/L) with elevated lithium has been verified in the 2018 brine sampling programs conducted by Standard Lithium.
The Smackover Formation in south Arkansas consists of a shoaling-upward cycle capped by ooidal/oncolitic packstone and grainstone (Vestal, 1950), with a maximum thickness of 365 m (1,200 feet). It has been interpreted as a low-gradient slope (<1°) homoclinal ramp succession due to its series of strike-oriented, relatively narrow depositional lithofacies belts across Texas, Arkansas, Louisiana, and Mississippi (Ahr, 1973; Bishop, 1968; Handford and Baria, 2007. These belts include evaporite and redbed sequences in the north that change basin-ward into ooidal (inner ramp beaches and shoals) peloidal facies belt (mid-outer ramp), and laminated mudstone (basin).
During rifting phases, evolving grabens were filled with the earliest Late Triassic-Early Jurassic red-bed sedimentary sequences of the Eagle Mills Formation. This unit comprises a variety of terrestrial sedimentary rocks including red, reddish-brown, purplish, and greenish-gray coloured shale, mudstone, siltstone, and less ........
