Anson related media, page-6

http://uscobaltinc.com/project/paradox-basin-lithium-brine-property/

Of particular interest:
Approximately eight wells have been drilled on the Paradox Property with approximately 25 historic wells in the immediate area. Of these 25 historic wells, five near the Paradox Property have analytical data for lithium and are concurrent with a zone determined by the USGS to contain greater than 40% total dissolved solids in oil field brines. Lithium occurs at the basin in oversaturated mineral brine (40 per cent minerals, 60 per cent water) and was discovered during oil exploration when drill wells intercepted the main brine zone (clastic break 31) of the Paradox formation. The main brine zone is approximately 6,000 feet deep, and consists of 28 feet of shale, anhydrite and dolomite; the bed is not part of any oil reservoir. The fractured clastic zones form an excellent reservoir for brines derived from underlying evaporate units. The fracturing is caused by salt flowage, and it is possible that, when brine is removed from the zones, salt will flow into voids assisting to maintain the high reservoir pressure and high recovery of brine (“Concentrated Subsurface Brines in the Moab Region, Utah”, Utah Geological and Mineralogical Survey, June 1965).