Mississippian Lithium grade guess thread, page-28

@1sharetrader1 On what geological factors do you base the assertion that being deeper will mean higher lithium concentrations? Ive seen nothing in the known data to suggest such correlation. Concentration is dictated by the rate of fluid movement and disolution of lithium-bearing minerals into fluids. Fluid movement is dictated primarily by secondary porosity (faults, fractures) and trap structures (anticlines, thrust fault structures etc).

What we know of the geology at the Bosydaba location suggests comparable concentrations to Paradox, hence the coys exploration range target of 100-150ppm. One big and exciting difference at Bosydaba is the thickness of the brine-bearing lithologies. If porosity and concentration are comparable to Paradox (expected), then total lithium resource tonnes at GR will be greater per unit surface area.