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Re: None

Friday, 06/22/2018 1:53:31 PM

Friday, June 22, 2018 1:53:31 PM

Post# of 47730
When you know totally NOTHING from WAY WAY afar as self-touted expertism? Tendency is to be 100% wrong. NOTHING is being processed from 8 Bros sulfide valley ore. Should be a future
seperate process of oxidation.

VAT process is using only '370' highly fractured oxide scoop and load as shown hauled down the steep peak to the plant going up on near level 8 Bros site. I'm pleased to do your work for the last 7 years on site

"The 370 mine area was briefly traversed around and it contains a sequence of
quartzites and limestone beds roughly N-S and dipping about 30° to the East.
Quartzites are the most cliff- boulder forming rocks in the area, whereas the
limestones are eroded to flat lower topography.
A diorite quartz porphyry dike or mantoe was recognized in contact with the
limestones on the footwall and quartzites on the hangingwall. Hornfels type
alteration show a lower temperature type system with low silica content and
high iron oxide fillings. Some occasions, epidote is present possibly a
constituent of the granitic intrusion. Gold and silver mineralization is
contained in this alteration halo which includes some porphyry and some
cooked limestone.
The 370 area is a hornfels type mineralization system created by diorite
porphyry intrusive, apparently controlled by stratigraphic fracturing planes,
parallel to bedding and also by quartzite bedding planes.
Preferred limestone bedding which are best reactive rocks appear to be of
varying widths and very constant attitude, N-S and 35 dip to the East.
The alteration zone at the contact of the diorite porphyry and the carbonate
rocks are creating an irregular mineralized zone with attractive gold and silver
values. Widths may vary from 3 to 5 meters but depths are still unkown.
A contact area is observed for several meters but is concealed under alluvium.
Continued work in this area includes trenching along contact zone , continued
geologic mapping and sampling to determine best areas for drilling to test
continuity at depth.
There is approximately 2000 to 3000 tons available for testing at the main
outcrop, as fractured alteration zone ready to be mined and leached.
The 370 will be initially mined as a contact hornfels type deposit with
repetitive parallel zones to stratigraphy with a high possibility of a major high
sulphide porphyry Au-Cu-Ag type orebody at depth"

http://mexusgoldus.com/wp-content/uploads/Report-on-Preliminary-Geological-Reconnaissance-of-the-Scorpio.pdf