Currently I am holding both AON and ENT. Originally I bought ENT...

Currently I am holding both AON and ENT.
Originally I bought ENT due to its very promising prospective nickel tenements at Fraser Range then.
As all holders aware, ENT (30% free carried up to FS) and AON (70% interest in ENT's FR tenements upon FS) has made JV agreement on early 2015. Since then, I followed AON (by holding shares) as my views on original ENT's tenements were exceptionally prospective.
Still, at this point, I have no any even 1 nano-millimetres of retreat on my views on original ENT's tenements.
　
If anyone ask me why, the followings are my grounds of understanding.
(some already posted partial here and ENT as well)

1. What is mineral pentlandite: http://www.galleries.com/pentlandite
2. Ni-Cu+/-Co Deposits:
Ni-Cu Deposits are the end of a magmatic process known as "liquid immiscibility''. This process involves the separation from the parental magma of a sulphur-rich liquid containing Fe-Ni-Cu. Upon cooling, the sulphur-rich liquid produces an immiscible sulphide phase (droplets of sulphide liquid in silicate liquid, like oil in water) from which minerals such as pyrrhotite (FeS), pentlandite (Fe,Ni)9S8, and chalcopyrite (CuFeS2) crystalize. Typical magmatic Ni-Cu deposits tend to occur in embayments at or near the base of their intrusive hosts.

They occur at the base of the intrusives because
a) immiscible sulphide liquids are heavier than silicate liquids and therefore sink to the bottom of the magma chamber and
b) without the presence of sulphur, metals such as Ni become incorporated into silicate crystal structures, such as pyroxene. Ni-Cu deposits are found in layered intrusions, stocks and ultramafic sills and flows. The largest deposits are of Archean and Proterozoic age.

The ore in Ni-Cu deposits can be massive, net-textured or disseminated. Typical examples of Ni-Cu deposits include the Sudbury orebodies (layered intrusion hosted), the Kambalda orebodies in Australia (ultramafic flow hosted) and the orebodies in the Thompson District of Manitoba (ultramafic sill hosted).

The Noril'sk-Talnakh orebodies are essentially typical Ni-Cu deposits containing anomalously high concentrations of PGM (6 g/tonne material).
source: ( http://earthsci.org/mineral/mindep/depfile/mag_dep.htm )

3. Photo Understanding:
http://www.oriongold.com.au/sites/oriongold.com.au/files/images/FR pic1.jpg
4. Similar photos of SIR/Bollinger massive nickel sulphide that we are seeking:
http://www.asx.com.au/asxpdf/20130311/pdf/42dkr6sz4zkw99.pdf


It seems the following facts and findings could lead the most prior target conductor(s) at Plato north by AON.
1. encountered 'magmatic nickel sulphides' at drill hole #3 at 337m below the surface(2nd after SIR)
2. above has proven by renown geoligists/analysts same rocks and sulphides as SIR's Nova/Bollinger
3. scientific undeniable fact findings of 'must-be-existing' of feeder sills of above sulphides
4. coincident geochemical surveys
5. intense high powered MLEM (GEM) surveys by AON over ENT's
6. more understanding of regional geology/formation
7. consultant from very famous geologists/analysts/geophysicist
8. classified pilot test drillings
9. hi-tech computational geoscientific findings


Regards,