MGX Minerals Inc MGXMF

EON CLAIMS ( Dolo Magnesite ) 2 kinds

[Wangotango67]

I'm reading - MGX ownership

Strategic location to, Mt Brussilof (  near Bay Mag -  current magnesite mine )

Oddity ?
Not seen on website, nor on stockhouse as one of the claims.

The Mount A s s i n i b o i n e o c c u r r e n c e a r e a is underlain by c a r b o n a t e , shale a n d phyllibc r o c k s or Middle C a m b r i a n a g e which h a v e b e e n m e t a m o r p h o s e d
a n d uplifted into a n anticlinal f o r m . This anticlinal feature has its central a x i s located in the valley of Assiniboine C r e e k . W e s t of this a x i s , the r o c k s dip
f r o m 5 to 35 d e g r e e s s o u t h w e s t and strike northwest f r o m 3 1 0 to 355 d e g r e e s . East of the a x i s , the r o c k s a r e essentially f l a t - l y i n g . T h e entire property
is underlain at shallow depth by the Main R a n g e s thrust fault along which the r o c k s h a v e m o v e d e a s t w a r d s e v e r a l k i l o m e t r e s .

Two distinct t y p e s of dolomite of the Middle C a m b r i a n C a t h e d r a l Formation occur o n the p r o p e r t y . A " g r a n o l a " t e x t u r e d dolomite is host to the m a g n e s i t e
m i n e r a l i z a t i o n a n d is g e n e r a l l y underlain a n d s o m e t i m e s e n c l o s e d by a tight, c r y s t a l l i n e , s o m e t i m e s argillaceous d o l o m i t e .

T h e host rock which contains
the m a g n e s i t e m i n e r a l i z a t i o n is a v e r y c o a r s e - g r a i n e d , recrystallized dolomite which occurs as m a s s i v e , t a n c o l o u r e d , resistant o u t c r o p s . Magnesite
m i n e r a l i z a t i o n in outcrop e x p o s u r e s is r e c o g n i z e d by its e x t r e m e h a r d n e s s , white colour, m a s s i v e a p p e a r a n c e and the p r e s e n c e of l a r g e r h o m b i c
crystals of d o l o m i t e s p a r with m i n o r pyrite.

Two a r e a s of significant buildup of c o a r s e - g r a i n e d m a g n e s i t e - bearing dolomite w e r e identified. T h e b e s t a r e a occurs in a cirque o c c u p i e d by Eon C r e e k
w h e r e 2 7 4 m e t r e s of C a t h e d r a l Formation hosts a 104 metre thick zone of rock which a s s a y s a high of 2 8 . 8 8 per cent MgO. T h e s e c o n d a r e a m a y
r e p r e s e n t the updip continuation of the B a y m a g o r e b o d y (082JNW001) to the s o u t h . The C a t h e d r a l Formation r e a c h e s a m a x i m u m  t h i c k n e s s of 186
m e t r e s a n d contains 101 m e t r e s of f a v o u r a b l e m a g n e s i t e - b e a r i n g rock which a s s a y s a high of 4 3 . 0 7 per cent MgO ( A s s e s s m e n t Report 1 9 0 9 2 ) .

Bibliography EMPR A S S R P T 1 8 2 0 3 . * 1 9 0 9 2
EMPR O F 1 9 9 2 - 1 4
G S C  O F   6 3 4

https://apps.nrs.gov.bc.ca/pub/aris/Report/35289.pdf/

Check out the photo on page 32
See anything interesting ?
Colors ?
Yup.


Marysville Claims
I'm not seeing the photo in this report.... but i downloaded it trs ago.
i still have it.   ( wanna see it just ask )  same colors - lol

https://apps.nrs.gov.bc.ca/pub/aris/Report/37598.pdf/

Former post i said just pay shareholders for, 4 km strike Mg + Rb
hmmmm... upon rethinking -  nah.... all minerals are important - lol
BC will need energy, lots of it.