Sources of lithium
Lithium is concentrated by magmatic fractional crystallisation and partial melting which results in higher concentrations in some pegmatites and muscovite-bearing granites. During rock weathering, highly soluble lithium is taken into solution and transported with water. Locations where water is trapped inland, under arid conditions, concentrate the lithium into residual brines. These concentration mechanisms have formed the two deposit types: pegmatites and continental lithium brines in closed basins, which are the source of most mined lithium. Other sources of viable lithium resources include geothermal brines, jadarite, oilfield brines, and clay minerals such as hectorite. Lithium is also often produced as a by-product from potash operations. This diverse range of resource types requires a range of analytical methods for lithium measurement.




























