RE: Podcast11 May 2022 07:12
Hi Strudel
Morning lesson :))
Regarding Paddy’s comments on the base metals and Hydro’s remarks about nickel, well what do we know.
Firstly the historical MMI surveys picked up the base metals of copper, zinc, cobalt and nickel.
Zinc and nickel were only found as trace elements, high levels of copper and cobalt.
Cobalt is not found naturally due to oxygen in the air /ground and chlorine in the ocean .
It can be found in new meteorites attached to iron ores in its natural form.
The first few holes by Greatland itemised mainly gold, copper and cobalt also arsenic
Newcrest have indicated that the cobalt levels are variable and difficult to form Kriging boundaries to include in the resource.
Cobalt is difficult to be retrieved from copper ores.
Cobalt can be found in metallic iron rich compounds and also compounds with arsenic.
Cobalt is commonly found in nickel and copper sulphides.
The temperature of intrusive magmas is important in the formation of copper and nickel sulphides from iron rich magmas, hotter the temperature copper sulphides are formed.
The cooling rate of the magma also separates these 2 metals.
A high nickel content will have a low copper content and vice versa with cobalt fluctuating between the 2.
Quote from a web site I was looking at
“ The sedimenthosted copper deposits are formed when saltbearing fluids flush metals, including copper and cobalt, out of oxidized (red) sediments; if the metalbearing fluids then react with reduced (black) rock or oil or natural gas, they deposit minerals containing copper and cobalt. Magmatic nickel sulfide deposits form when a magnesium and ironrich magma becomes saturated with sulfur. Metals in the magma, such as nickel and cobalt, may then move into a separate dense sulfiderich fluid that sinks to the bottom of the magma chamber where the metal sulfides are then deposited.”
Havieron is a complicated ore body with numerous intrusions bringing in different chemical reactions and mineralisation.
From the above quote Havieron has the red sediments, it has the sulphur rich fluidation and an iron rich ore body.
Back to what could be in Havieron
Nickel has not been mentioned in the top 700-800m from surface
Copper is dominant in top sulphide zone.
Copper is weaker below these levels.
The Northern corridor has recently been found to contain high grade zones this starts from around 700m from surface. These zones are not high grade copper and contain actinolite breccia.
Actinolite breccia contains arsenic important for cobalt compounds.
Also contains high iron content
Nickel sulphides form at the base of magmas.
Suggestions that the nickel is in the Eastern breccia could be a reality.
My assumptions are that the Eastern breccia intrusion has intruded into and formed the northern corridor.
What I’m suggesting is the nickel is in the EB and NC
and more than likely in higher grades than what the copper values have been shown at.
Plus cobalt will be in be