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MGX Minerals Inc MGXMF

MGX Minerals Inc. is a Canada-based diversified resource and technology company with interests in advanced materials, metals, and energy technologies. The Company’s portfolios include Magnesium, Silicon, Lithium, Gold, and Silver. Its Magnesium projects include Driftwood Creek, Marysville, Red Mountain Group and Botts Lake. Its Silicon projects include Gibraltar, Koot and Wonah. Its Lithium projects include GC and Petrolithium. Its Gold projects include Heino, Tillicum and Fran. The Driftwood Creek project is located approximately 164 kilometers (km) north of Cranbrook, British Columbia (B.C.). The Marysville magnesite project is located approximately 12 km (7.7 miles) south of Kimberly, BC. The Red Mountain-Topaz-Cleland magnesite property is located approximately 50 km south of Golden. The Botts Lake magnesite property consists of claims approximately 50 km south of Golden, BC. The Gibraltar project is located approximately 95 kilometers northeast of Cranbrook, BC.


GREY:MGXMF - Post by User

Post by Wangotango67on Sep 27, 2022 10:30pm
118 Views
Post# 34991091

ROCK CANYON - B.C. - DOLOMITES + REE's

ROCK CANYON - B.C. - DOLOMITES + REE's

Interesting it is...
Driftwood Creek is compared the the Mississippi dolomites, and Brusslof dolomites.

Here's another dolomite deposit in B.C. hosting - REE's.


The Rock Canyon Creek deposit, 90 kilometres northeast of Cranbrook
The steeply dipping REE-fl uorite zone was intersected by drilling. It may be more than 50 metres thick for more than 1100 metres along strike, and to a depth of 124 metres. It remains open along strike and dip, and its thickness locally exceeds 50 metres. Based on surface mapping and borehole logging, the deposit appears to be concordant with stratigraphy.

Most of the mineralization occurs as breccias and fracture fi llings in fl uorite-impregnated dolostone. Fluorite concentrations vary from less than 1% to 13.5% by weight, and light REE (Ce+La+Nd) concentrations vary from trace to 2.8%. REE are hosted mainly by bastnasite-(Ce), parisite-(Ce), synchysite-(Ce), and REE-bearing phosphates. Ongoing work will focus on better characterizing the deposit to address questions about the origin of ore forming fl uids and the temporal, structural, and stratigraphic relationship to Mississippi Valley-type and sparry magnesite deposits along the eastern fl ank of the Canadian Cordillera.

OPEN THE LINK - LOOK AT THE PHOTOS - 
Blue colored Dolomites.

https://www.researchgate.net/figure/Geological-setting-of-the-Rock-Canyon-Creek-deposit-Modifi-ed-after-McMechan-and-Leech_fig1_313387687

FULL TEXT REPORT -
https://www.researchgate.net/publication/313387687_Geological_setting_of_the_Rock_Canyon_Creek_REE-fluorite_deposit_British_Columbia_Canada/download


i MYSELF,
Couldn't help but notice the similar size of 1100 m strike, 50m wide and 124m depth....
Similar to, Driftwood.


What else am i tihnking ?
This new topic of - bio geology -  is rather interesting.
Lagoons
Reefs
Organisms or Algae
Process minerals
Always found with dolomites ( calcium + magnesium )
REE's seem to be present
Ree's are colorful


I guess i can still stand on my theory several years ago....
Rockies were first formed - rose out of ocean creating mountains.
Mountains are simply ocean floors.
Middle lowlands of B.C. are still ocean floors but mass sediments overlay
Purcell Group are next on scene rising out of ocean
Again.. .ocean floor - coral reefs - atop of mountain
And the last mountaous range near Vancouver came out of ocean last.

How would they evolve ?
Earth expanding.
Seen on special google maps - ocean floor - has expansion faults - all over hte ocean floor.
Our earh is growing - and as so... land mass shifts occur - 
There's another process - to this evolve - but i'll keep that for myself....
Too scarry for some... wink.


Dolomites - Ree's.


There's lots of literature on this now showing up online.
Makes no sense.. .as prior, i could find hardly anything .
I wonder if it's because it involves algos and how a person searches ?
Or... because biology crosses over into geology ?

Those critters or single cell organisms.... munched on the carbons.
I can just imagine how much volcanic activity there was, depsoiting in the oceans,
Rusty red toxic waters filled with far higher saline conditions - all dorts of minerals and these critters munching away.. .processing the minerals and oozing out with slime goo along with the minerals layering sedimentry depoists along with sands.
Most likely why the magnesium and calcium are in - carbonate forms.


Cheers......

Let's see if one of the photos will show on here....

Blue coloration is the fluorspar - fluorite -
Another article i read - mentioned near the bugaboo - dark colored dolos contained the
Nb + uraniums.


https://www.researchgate.net/profile/Craig-Green-4/publication/313387687/figure/fig3/AS:458881907335170@1486417380966/Photographs-from-the-Rock-Canyon-Creek-deposit-area-a-Intraformational-breccia-composed.png


Small coreection former post -
The extra claims MGX  scooped up ?
Are positioned all around Driftwood.
Here's a map showing - locations.
Do we stil have these extra dolo claims ?
Or is it a case of,  marysville and  Longworth silica ?
Hope not.



https://www.e-know.ca/wp-content/uploads/2016/01/driftwood-mining-district.jpg

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