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Hawkeye Gold and Diamond Inc V.HAWK

Alternate Symbol(s):  HWKDF

Hawkeye Gold & Diamond Inc. is a junior mineral exploration and development company. The Company is engaged in the exploration for and the development of natural resources in Canada. Its projects include Bonanza, 2-Aces, Keithley Creek, Cariboo Valley, Seller Creek, Swift River, Bonanza Lake and Cariboo Lake. The Company owns over four 2% royalty interests which are subject to buy-down provisions on the Railway, McBride, Boomerang and Todagin properties located in the Golden Triangle of northwest British Colum (BC). The Bonanza property is located on the northern end of Vancouver Island, British Columbia, Canada, and is situated approximately 110 kilometers (km) northwest of Campbell River and 69 km southeast of Port Hardy. The 2-Aces property is situated approximately 32 km southeast of the Town of Barkerville, British Columbia (B.C.), Canada. It owns an interest in the 3,599-hectare Keithley Creek property situated approximately 30 km south of the Town of Barkerville, B.C., Canada.


TSXV:HAWK - Post by User

Post by Wangotango67on Mar 12, 2021 1:49pm
96 Views
Post# 32786590

REVIEWING PEER - SADDLE

REVIEWING PEER - SADDLE
GT  drill core pics - 
copper is in the 1% or less bracket - right out of the gates i see green colored cores.
= potentially strong chlorite influence
= salt waters solubilizing the copper into a secondary matrix
= silts = clays = reconsolodated matrix = chlorite water involvement


 


GT's location of deposit -
My takeaway with this pic - simply put - focus on the mineralizarion in what color ?
That's right blue -
Next - if the mineralizatio ncame from the pale green  sidewalls
the deposit would als olook green - but it's not
Revert back to the 1st pic - chlorite involvement = salts

Looking at these massive Nortrhern B.C.  deposits in which most have a salt vector
Places my mind in the value of - large oceanic rivers coursing through.
Erroding the sulkphide minerals - repackaging them in a salt carbonate matirx.


1 - find the minerals in low land ranges or....
      skip to the chase.

2 - look on charge maps for a distinctive bleed and l;each value that runs into a basin.
      after establishing the copper or gold values in lower ranges look for the smear trail
      of mineralizatiomn that redeposited into an entirely didfferent chlotire or carbonate 
      deposit -


https://ml.globenewswire.com/Resource/Download/99d9a80f-3774-4c9e-bf9c-ca16b6591559?size=2



LOOKS TO ME...
like a repackaged deposit - if deposit were involved with the host side wall rock,
There would be blue seen on the side walls... but all is seen is,,, pale green.

Could it be hydrothermal deposit ?
Hard to say... but... i lean moreso to - salt chlorite waters - massive oceanic rivers.
Could be as simple as just a wedge shaped depsoit where salt waters collected sands
and quartz and solubilized gold and copper and eventually solidified into a new rock matrix of carbonatesd with a hint ofsulphide rocks.

Again... looking at deposits with two sets of eyes..
sulphide or... i prefer -alaki eyes... so many depsoits have rthis chlorite and carbonate 
value that goes undetected as an influence of perhaps ocean waters...


And of course the bleed vlaue seen on range going into valley
pink copper sulphide zones merges with alaki valley zones. ( own opinion )

https://ml.globenewswire.com/Resource/Download/83ca4e7b-a37b-4fc4-a350-928260185aab?size=3




Just a simple review of how i look at deposits.
not investment advice... just a topic of sulphure vs alaki.
And of coursew.. my interpretation could be out in left field.
But thern again.. maybe it's not.



Cheers...
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