STRATA BOOKING - PART 2 Do forgive - i forgot he additional picture in last post to show where i feel the strats formed it's booking effect -
Right where the dark
sulfides are showing themselves -
1 - 2- 3 - 4 - himps that were once - most likely - flat terrain - uplifted to form the mountain
in a booking format.
Left to right, the
3rd last hump has an additional upper hump ( slightly seen ) and can be seen better on satelite maps - this strata sheet booking appears to have 2 books back to back - with no in between rock -
There is a main portal seen in pic - white box - entering the mountain.
This portal only runs do far.. .but, how convienient it is, to have access underground and
know what the sulpfides have in them... crickets from the junoor.
The 5th ( strata fold with portal can be identified via diagram belwo with orange extension underground road - this strats may not be the same formation as the other 4 folds.
Potentially far more ore tonnage which is at - surface - easy to access.
And with portals - to allow junior to know if this deposit emminates from the mountain folds.
Or, extends further into mountains.
My hunch says it does...
Which would mean - this deposit could be far larger than what is documented.
If the mineralization going into mountain - is the same as the main depoist - and if the pit
in between was the same as main depoist - then.. high oddsthe mountain is the source.
The junior, went halfcocked - securing a forward contract too soon,
with concentrates.
This mine could be midelled very differently, whereas,
if the mountain is the source then, there's considerable more tonnage - and knowing the main mine is already built with equiptment onsite -there's noreason why this couldn't convert to a ful loperation - churing out pur ecopper plates or bars. Far more profitable.
The question becomes,
how far rwacjing into the mountain could these booked strata layers run ?
It woulddepend upon how the flat strata was uplifted and, if the stratsa kept its form.
Ifit did, the strata would offer up fat sheet like books that could stretch well into the mountain.
As mentioned above - the junior has ready access to the surface sulfides and one protal
of which would provide all the intel it needs to know if it's chalked full of
copper,gold,silver,cobalt, zinc...etc...
Some may disagree,
but like i said in former post,
if i'm wrong, i'll quit stocks.
I'm only in one stock - i don't short - nor day trade.
I usuaally stick to just one or two stocks and devote my time on researching .
If i'm wrong, and i could be... then, cest la vie.
Not investment advice.
But.. the more i analyze this junior, i'm convinced the mine was built right over the deposit.
And the PITS are solidclues that the mineralization extends towards the mountain and given the sulfides are exposed on the side of hte mountain - i feel it's quite apaprent the deposit is not hydrothermal but rather a strabound deposit that uplifted andbooked into mountain formation.
Does hte depoist have hydrothermal signatures ?
Sure... most likely the hydrothermal veining occured while the strata was in lateral flat mode.
Then, uplifted.. .and junior now sees the veining thinking it was an original hydrothermal running on a 45 degree... I feel this is not the correct description but rather, strata shifted and booked itself, created the mountains. and the main mine deposit stil lhas a partial 45 degree booking effect - lessor upright - due to its lower in the valley- less influence to push fully upright.
