RE: RE:Investor warning
The lithosphere of the west Cote Lake area is highly fractured synonymous with the deformation zone trending through it.
Beachman you have said on occasion the Trelawney mineralized trend runs SW and NE along a controlled structure.
Now if this were true without exception it would be much the same as declaring geology an exact science to which in fact neither is true.
Now about those dotted red and blue lines. What a graphic expose to some of the nature of the extensive folding and fault slip that exists beneath the surface.
Look at the TRR mappie below.,
What do you see between the red 100meter levels and the blue 400 meter levels.
For starters , you see evidence of the deformation zone that runs through here. Now the average distance between these lines is 100 meters denoting extensive raise and dip between the footwall and hanging wall. The mineralization emplaced during the late intrusive stage is highly offset with the slip giving the impression of discontinuation at depth due to drill overshoot missing the offset. Moving the drills another 100meters to the north would bring the bit inline with the offset and mineralization once again at shallower depths as the red and blue lines suggest, and is indeed a feasible assumption givin the nature of these types of shear zones and their structural widths averaging in the area of 7 kilometers across. Given the fact the West Break or CLLDZ extension runs directly through Augen Gold to the North of Trelawney, the shear dimensions of the Zone fall well within bounds of one another.
Picture in your mind a ten foot strip of dried clay 1 foot thick with sand underneath being pushed forward by a steam shovel from a north to south direction for 5 feet. You end up with a pile of clay and sand on top of clay. Now if the steam shoveled pile of clay and sand were to represent the surface rock and the sand the mineralized portion , the portion steeply dipping to the north would hold the mineralization closest to the surface representing the hanging wall while burying the sheared footwall and its mineralization deeper. A continual succession of 100 to 200 meter wide shears of the same dimension looks to be evident in this area that could easily span a 7 kilometer width through Augen and Trelawney lands. Factor this with the numerous northerly trending faults throughout the area and a conduit or a dozen spring to mind.
Have a close look at these two links for a clear picture on locations and general widths synonymous with these deformation zones.
https://www.explorresources.com/_resources/projects/Timarea_Model_Splay_Fault_Corridor_Oct_15_2010.pdf
https://www.trelawneymining.com/pdfs/RPA%20NI-43-101%20technical%20report%20Chester.pdf
