KWG Resources Inc C.CACR

Alternate Symbol(s): KWGBF | C.CACR.A

Metals & Mining Industrial Metals & Minerals

KWG Resources Inc. is a Canada-based exploration stage company. It is focused on acquisition of interests in, and the exploration, evaluation and development of deposits of minerals including chromite, base metals and strategic minerals. It is the owner of 100% of the Black Horse chromite project. It also holds other area interests, including a 100% interest in the Hornby claims, a 15% vested interest in the McFaulds copper/zinc project and a vested 30% interest in the Big Daddy chromite project. It has also acquired intellectual property interests, including a method for the direct reduction of chromite to metalized iron and chrome using natural gas. It also owns 100% of Canada Chrome Corporation, a business of KWG Resources Inc., (the Subsidiary), which staked mining claims between Aroland, Ontario (near Nakina) and the Ring of Fire. The Subsidiary has identified deposits of aggregate along the route and made an application for approximately 32 aggregate extraction permits.

CSE:CACR - Post by User

KWG Resources Inc

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Post by hrockon Aug 27, 2008 2:40pm

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Post# 15413871

KWG - Part o' da NOT Ring Players

KWG - Part o' da NOT Ring Players

While da Rock posted dis inna NOT................appplies ta KWG also.

Just da way I see dat!
HardRock

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Rock Ore - NOT 's Hi Grade - Why?

'ere's formal backup..................ta what dey says 'bout NOT's ore formation................only dis one issa 'bout Norlisk inna da Russia.

So...............Norlisk issa 3rd largest ore deposit inna da world!

So........what does dat mean fo' NOT...........anna da others inna da Ring???

Just da way I see dat!
HardRock

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Rock Model - NOT ROF Ore formation

“ The Sulphides have high PGE abundances, which could only be derived from a mass of Magma 200 times that of the host intrusions”

“This contamination resulted in the segregation of immiscible sulphide liquids in the upper zones of density stratified convecting layers that developed in the vertical chamber.

The sulphides continuously settled and reacted with fresh pulses of magma, drawing more Ni, Cu and PGE. In this way, sulphides grogressively richer in Ni, Cu and PGE settled in the lower zone of the vertical chamber.”

Just da way I see dat!
HardRock

from da Book: