Friday, August 07, 2009 1:28:11 PM
"The rim of the intrusive structure is highly brecciated and locally deformed allowing for the intrusion of epithermal fluids that likely deposited the pyrochlore mineralization which contained and precipitated out the Niobium, tantalum, rare earth elements, uranium and thorium along the fracture and jointing within this unit. To date the property has not seen a lot of detailed exploration work around the rim of this structure since half of it lies under Nemegosenda Lake and the other half is partially obscured by overburden cover and has not has a lot of detailed work done over the ground. The two areas that have seen past exploration have been the ‘D’ Zone and the ‘South-East’ Zone."
Just to think of the FUTURE potential here not just what we already know! Looking foward to seeing what is UNDER THAT LAKE.
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