Lanfranchi Today

Lanfranchi has extensive mine infrastructure and development which provides the perfect platform to grow the Mineral Resource

Exploration

The proposed exploration program is an extension to the exploration program developed by Mining Associates for Cherish. The additional targets to be drilled are yet to be determined but will come from the Surface and Underground EM programs currently being completed.


Mineralisation

Kambalda-style nickel sulphide mineralisation in the Tramways area typically occurs at the base of channel flow facies as broadly tabular to ribbon-like bodies several hundred metres long, 25 m to 200 m wide and less than 5 m thick. The nickel sulphide ore shoots are largely developed within incised embayments into the underlying Lunnon Basalt with massive sulphide ores developed on or very slightly above the contact (Barnes and Lesher, 2017).

Sulphides can occur as massive (>80% sulphide), matrix (40-80% sulphide) or disseminated (<40% sulphide) styles with pyrrhotite-pentlandite dominant and variable amounts of pyrite and chalcopyrite. Major minerals in the massive and disseminated ores are pyrrhotite, pentlandite, pyrite, chalcopyrite, magnetite, and chromite, with rare millerite and heazlewoodite generally confined to disseminated ores (Hoatson et al, 2006).

Exploration drilling on the north-western overturned fold limb has intersected minor massive sulphide mineralisation but not in sufficient amounts to define a deposit.

Lanfranchi area main nickel deposits. After Hicks and Parkinson (2017).


Current Mineral Resources

The Lanfranchi Mineral Resource was reviewed in 2021 and updated to be compliant with JORC 2012. Mineral Resources currently stand at: 4.26Mt @ 1.8% Ni, for a total of 78,300 tonnes of contained nickel

 
 

Lanfranchi Geological Model

Archaean in age - 2.7 billion years old

Mid-oceanic ridge and sea-floor spreading forming new oceanic crust

Volcanically active hydrothermal vents and hot lavas

Complex geometries, concentrated flows

Topographic features are relatively parallel to rifting


Lanfranchi Nickel Mineralisation

Basalt - Footwall

Mid-oceanic ridge and sea-floor spreading forming new oceanic crust from underwater eruption as pillows

Melting point temperatures of 950 to 1200 degrees Celsius with the consistency of honey

Modern day examples = Hawaii, Iceland

Black Smoker - Nickel Mineralising Event

Hydrothermal vents contained dissolved minerals

Minerals precipitate when exposed to colder sea water

They form a sedimentary layer/blanket over seafloor basalts

Komatiite - Nickel Mineralising Event

Deep mantle plumes with temperatures of 1600 degrees Celsius

Komatiitic lava has the consistency of water and is sometimes called “Blue Lava”

The komatiite lava channel thermally erodes sediments and basalt that it flows over

Sulphur from sediments is mixed with nickel in lava flow and the heavy nickel suphides settles out on bottom of flow