VANCOUVER, BRITISH COLUMBIA--(Marketwired - Feb 22, 2017) - Power Metals Corp. ("Power Metals Corp." or the "Company") (TSX VENTURE:PWM)(OAA1.F) is very pleased to announce that it has acquired the Coyote Project (the "Project") located in the Lisbon Valley area in the Paradox Basin, Utah.
The Project includes 150 placer mineral claims covering an area of 3,000 acres and inclusive of lithium brine mineral rights, on trend and adjoining to the north, the Lisbon Valley oil and gas field, where historic lithium brine content has been reported as high as 730 parts per million lithium (Superior Oil 88-21P).
Johnathan More, CEO of Power Metals noted, "We are extremely excited to have been able to position the company in the Lisbon Valley, as a starting point. As we roll out our plan, we intend to deploy increased resources towards the building of a petro lithium portfolio in the United States including but not limited to the acquisition of oil field assets, lithium brine, oil wells and associated infrastructure."
To view the map accompanying this press release please click the following link: http://media3.marketwire.com/docs/PowerMap221.pdf
More continued, "Structurally, the Coyote Project is situated down dip from an existing oilfield and within a geosyncline basin feature which could represent a fluid trap for migrating brine fluids. The property lies entirely within a zone identified by the United States Geological Survey (USGS) to contain 40% plus TDS (total dissolved solids) within the Pennsylvanian brine aquifers (USGS Report 1962).
To date, the most concentrated brines have been found in Pennsylvanian rocks, especially in the thin clastic breaks which separate the salt beds in the Paradox Formation. The porous Mississippian dolomites and limestones appear to offer the potential of sustained brine flow from a large reservoir, especially where they have been faulted into contact with rich Paradox salt beds."
Geologic Setting
The Lisbon Valley oil and gas field is located approximately 40 miles southeast of Moab, Utah in the salt anticline belt on the southwest edge of the Paradox Basin in San Juan county. The oilfield was first discovered by Pure Oil Company in 1960. The Lisbon field produces oil and gas from the southwest flank of a faulted anticlinal trap in the Devonian sandstones and Mississippian limestones (Segal et al., 1986).
The Paradox Basin covers large parts of San Juan, Garfield, Wayne, Emery, and Grand Counties in southeastern Utah. The Basin was a structural and depositional trough associated with the Pennsylvanian-age Ancestral Rocky Mountains. The subsiding basin developed a shallow-water carbonate shelf that locally contained carbonate buildups along its south and southwest margins.